Landfill disposal of drill cuttings
FracTracker Alliance

Landfill Disposal of WV Oil and Gas Waste – A Report Review

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By Bill Hughes, WV Community Liaison

As oil and gas drilling increases in West Virginia, the resulting waste stream must also be managed. House Bill 107 required the Secretary of the West Virginia Department of Environmental Protection to investigate the risks associated with landfill disposal of solid drilling waste. On July 1, 2015, a massive report was issued that details the investigation and its results: Examination of Leachate, Drill Cuttings and Related Environmental, Economic and Technical Aspects Associated with Solid Waste Facilities in West Virginia, by Marshall University.

While I must commend the State for looking into this important issue, much more needs to be done, and I have serious concerns about the validity of several aspects of this study. Since the report is almost 200 pages long, I will summarize its findings and my critiques below.

Summary of Waste Disposal Concerns in Report

The page numbers that I reference below refer to the page numbers found within the PDF version of the full study.

  1. Marcellus shale cuttings are radioactive: pgs. 17, 139, 142, 154
  2. We do not know if there is a long term problem: pg. 19
  3. About 30 million tons of waste in next few decades: pg. 176
  4. Landfill liners leak: pg. 20
  5. Owning & operating their own landfill would be expensive & risky for gas companies: pgs. 186-7
  6. Toxicity and biotic risk from drill cuttings is uncharted territory: pg. 78
  7. Landfill leachate is toxic to plants & invertebrates: pgs. 16, 95, 97
  8. Other landfills also have radioactive waste: pgs. 14-15
  9. We have no idea if this will get worse: pgs. 96, 154
  10. If all systems at landfills work as designed, leachate might not affect ground water: pg. 41

Introduction

WV Field Visits 2013

Drilling rig behind a wastewater pond in West Virginia

Any formal report comprised of 195 pages generated by a reputable school like Marshall University with additional input from Glenville State College – supported by over 2,300 pages of semi-raw data and graphs and charts and tables – requires some serious investigation prior to making comprehensive and final conclusions. However, some initial observations are needed to provide independent perspective and to help reflect on how sections of this report might be interpreted.

The overarching perspective that must be kept in mind is that the complete study was first limited by exactly what the legislature told the WV Department of Environmental Protection DEP to do. Secondly, the DEP then added other research guidelines and determined exactly what needed to be in the study and what did not belong. There were also budget and time constraints. The most constricting factor was the large body of existing data possessed by the DEP that was provided to the researchers and report writers. Because of the time restrictions, only a small amount of additional raw data could be added.

And most importantly, similar to the WVU Water Research Institute (WVU WRI) report from two years ago, it must be kept in mind that these types of studies, initiated by those elected to our well-lobbied legislature and funded and overseen by a state agency, do not occur in a political power vacuum. It was surely anticipated that the completed report might have the ability to affect the growing natural gas industry – which is supported by most in the political administration. Therefore, we must be cautious here. The presence and influence of political and economic factors need to be considered. Also, for universities to receive research contracts and government paid study requests, the focus must include keeping the customer satisfied.

My comments below on the report’s methods and findings are organized into three broad and overlapping categories:

  • GOOD  –  positive aspects, good suggestions, important observations
  • GENERAL  –  general comments
  • FLAW  –  problems, flaws, limitations
  • MOVING FORWARD  – my suggestions & recommendations

I. Water Quality: EPA Test Protocols & Datasets

Marcellus Shale (at the surface)

Marcellus Shale (at the surface)

GENERAL  It is obvious that a very smart and well-trained set of researchers put a lot of long, detailed thought into analyzing all of the available data. There must be tens of thousands of data points. Meticulous attention was put into how to assemble all of the existing years’ worth of leachate chemical and radiological information.

GOOD  There is an elaborate and detailed discussion of how to best analyze everything and how to utilize the best statistical methods and generate a uniform and integrated report. This was made difficult with non-uniform time intervals, some non-detect values, and some missing items. The researchers used a credible process, explaining how they applied the various appropriate statistical analysis methods to all the data. They provided some trends and observations and draw some conclusions.

FLAW 1  The most glaring flaw and the greatest limitation pertaining to the data sets is the nature of the very data set, which was provided to the researchers from the DEP. It is to the commendable credit of the DEP that the leachate at landfills receiving black shale drill cuttings from the Marcellus and other shale formations were, from the beginning, required to start bi-monthly testing of leachate samples at landfills that were burying drill waste products. And in general, when compared to on-site disposal as done for conventional wells, it was initially a good requirement to have the drill cuttings put into some type of landfill; that way we could keep track of where the drill cuttings are located when there are future problems.

To the best of my knowledge, until the states in the Marcellus region started allowing massive quantities of black shale waste material to be put into local landfills, we have never knowingly deposited large quantities of known radioactive industrial waste products into generic municipal waste landfills. The various waste products and drill cuttings of Marcellus black shales have been known for decades by geologists and radiochemists to be radioactive. We know better than to depose of hazardous radioactive waste in an improper way. Therefore, it is very understandable that we might not know how to best solve the problems of this particular waste product. This was and still is new territory.

FLAW 2  All of the years of leachate test samples were processed for radioactivity using what is called the clean drinking water test protocols, also referred to as the EPA 900 series. Three years ago, given the unfamiliarity of regulatory agencies with the uniqueness of this waste problem, we chose the wrong test protocol for assessing leachate samples. We speculated that the commonly used and familiar clean drinking water test procedure would work. So now we have a massive set of test results all derived from using the wrong test protocol for the radiologicals. Fortunately, all of the chemistry test results should still be reasonably useful and accurate.

At first, three years ago, this was understandable and possibly not an intentional error. Now it is widely known by hydrogeologists and radiochemists, however, that the plain EPA 900 series of test methods for determining the radioactivity of contaminated liquids do not work on liquids with high TDS — Total Dissolved Solids. Method 900.0 is designed for samples with low dissolved solid like finished drinking water supplies.

Despite this major and significant limitation, the effort by Marshall University still has some utility. For example, doing comparisons between and among the various landfills accepting drill waste might provide some interesting observations and correlations. It is clearly known now, however, that the protocols that were used for all samples from the start when testing for gross alpha, gross beta and radium-226 and radium-228 in leachate, can only result in very inaccurate, under-reported data. Therefore, it is not possible to draw any valid conclusions on several very important topics, including:

  • surface water quality,
  • potential ground water contamination,
  • exposure levels at landfills and public health implications,
  • and policy and regulations considerations.

Labs certified to test for radiological compounds and elements are very familiar with the 900 series of EPA test procedures. These protocols are intended to be used on clean drinking water. They are not intended to be used on “sludgy” waters or liquids contaminated with high dissolved solids like all the many liquid wastes from black shale operations like flowback and produced water and brines and leachate. The required lab process for sample size, preparation, and testing will guarantee that the results will be incorrect.

In no place in the final 195 page report have I seen any discussion of which EPA test protocol was used for the newer samples and why was it used. It has also not yet been seen in the 2,300+ pages of supportive statistical and analytical results, either. The fact that the wrong protocol was used three years ago is very understandable. However, this conventional EPA 900 series was still being used on the additional very recent (done in fall of 2014 and spring of 2015) samples that were included in the final report. The researchers, without any justification or discussion or explanations continued to use the wrong test protocol.

The clean drinking water procedures should have been used along with the 901.1M (gamma spec) process, for comparison. It is understandable for the new data to be consistent and comparable with the very large existing dataset that a case could be made for using the incorrect protocol and the proper one also. There should have been a detailed discussion of what and why any test method was being used, however. That discussion is usually one of the first topics investigated and explained in the Methods section. Having that type of discussion and justification seems to represent a basic science method and accepted research process – and that omission is a serious flaw.

MOVING FORWARD  We all know that if we want to bake an appetizing and attractive cake we must use the correct measuring cups for the ingredients. If we want to take our child’s temperature we need an accurate thermometer. When our doctor helps us understand our blood test results, we all want to be confident the right test was used at the lab. The proper test instrument, recently calibrated and designed for the specific sample, is crucial to get useable test results from which conclusions can be drawn and policy enacted.

It seems that the best suggestion so far to test high TDS liquids similar to leachate would be to use what is referred to as Gamma-ray Spectrometry with a high purity germanium instrument with at least a 21-day hold period (30 days are better), while the sample is sealed then counted for at least 16 hours. Many of the old leachate test results indicate high uncertainties that might be attributed to short hold times and short counting times. This procedure is referred to as the 901.1 M (modified). If the sample is sealed, the sample will reach about 99% equilibrium after 30 days. Radon 222 (a gas) must not be allowed to escape.

The potential environmental impacts to water quality section of this report seems to demonstrate that if you do not want to find out something, there are always justifiable options to avoid some inconvenient facts. Given the very narrow scope as defined, some the Marshall University folks did not seem to have the option to stray into important scientific foundational assumptions and, for the most part, just had to work with the stale data sets given to them. All of which, as we have known for close to a year now, have used the wrong test protocol. Therefore we have incorrect results of limited value.

II. Marcellus is Radioactive

GOOD 1  Of course, geologists have known that the Marcellus Shale is radioactive for many decades, but also for decades there has been great reluctance by the natural gas exploration and production companies to acknowledge this fact to the public. And finally we now have a public report that clearly and unambiguously states that Marcellus shale is radioactive. Interestingly enough, it was not much more than a year ago that some on the WV House of Delegates Judiciary Committee, seemed to be echoing the industry’s intentional deception by declaring that:

…it was only dirt and rock…

So this report represents progress and provides a very valuable contribution to beginning to recognize some of the potential problems with shale wastes and their disposal challenges.

GOOD 2  Another very important advance is that finally after eight years of drilling here in Wetzel County, we now have a test sample from near the horizontal bore. The WVU WRI study researchers were never given access to any samples taken from the horizontal bore material itself, however. That was, of course, what they were supposed to have been allowed to do, but they were only given access to study material from the vertical section of the well bore. This report describes how we are getting closer to actually testing good samples of the black shale. It seems that we have gotten closer – but let’s see how close.

Page 11 describes that only three Antero wells in Doddridge County were chosen as the place to try to obtain samples from the horizontal bore. Considering that over 1,000 deviated/horizontal wells or wells with laterals have been drilled in the past few years, that number represents a very small fraction of wells drilled: less than .3%. Even if a high quality sample could have been obtained it might be a challenge to extrapolate test results to the waste being produced from the other wells in WV. These limitations are completely ignored in the report, however. Given the available documentation from the DEP, this seems to be a serious flaw that compromises the reliability of the entire report.

III. Samples From Vertical vs. Horizontal Well Bores

FLAW  The actual samples tested from at least two of the three wells used in the study do not seem to be from the horizontal bore material. The sample from the third well might have come from the horizontal bore, but just barely. There is no way to know for sure. I will try to show this within the below chart using information provided by Antero to DEP Office of Oil & Gas. This information is in state records on Antero’s well plats, which become part of the well work application and also part of the final permit.

Table 1. Details about the samples taken from three Antero wells in Doddridge County, WV – and my concerns about the sampling process*

Antero well ID API # Sample’s drilling depth Marcellus depth** Horizontal bore length** Comments / Issues
Morton 1H 47-017-06559 6,856 ft. 7,900 TVD*** 10,600 ft. ~1,044 ft. short of reaching Marcellus formation
McGee 2H 47-017-06622 6,506 ft. 6,900 TVD 8,652 ft. ~394 ft. short of reaching Marcellus
Wentz1 H 47-017-06476 8,119 ft. 7,900 TVD 8,300 ft. Just drilled into Marcellus by 219 ft.
* Original chart found on page 11 of report
** Based on information from Antero’s well plat
*** TVD = Total Vertical Depth

Antero is an active driller in Doddridge County. If any company knows where to find the Marcellus formation it is that company. Well plats are very detailed, technical documents provided to the DEP by the operator regarding the well location, watershed, and leased acres and property boundaries. We need to trust that the information on those plats is accurate and has been reviewed and approved by the permitting agency. Those plats also give the depth of the Marcellus and the length and heading of the lateral or horizontal bore. The Marshall University report gives the drilling depth when the sample was taken on the surface. Using these available well plat records from the DEP it appears that at two of the wells the sample (and its test results included in the report) came from material produced when the experienced drilling operator was not yet into the shale formation.

On the third well, Wentz 1H, the numbers seem to indicate that the sample was taken when the driller said that they were just barely within the shale layer – by 219 feet. Since the drill cuttings take some time to return to the surface from over 7,000 feet down, drilling just a few hundred feet would not at all guarantee that the returned cuttings were totally from the black shale. The processing of the drill cuttings at the shaker table and separator and centrifuge and the mixing in the tubs all cast some doubt on whether the sample, wherever it was taken from, was truly from the horizontal bore material.

On page 11 there is a clear and unambiguous statement:

Three representative sets of drill cuttings from the horizontal drilling activities within the Marcellus Shale formation were collected.

A successful attempt to get three such samples might have then allowed an appropriate waste characterization to be done as needed to accomplish the five required research topics listed in the report’s cover letter. Only an accurate chemical and radiological waste characterization would have allowed scientifically justifiable conclusions to be formulated and then allow for accurate legislation and regulations. It does not seem that West Virginia yet has the required scientific data upon which to confidently formulate laws and regulations to protect public health with regard to shale waste disposal.

Would it not seem prudent – if one wanted a good, representative sample – to make absolutely sure that the operator was, in fact, drilling in the black shale and that the cuttings returning to the surface were, in fact, from the Marcellus bore? That approach would have been eminently defensible and easily accomplished by just waiting for drilling to progress into the lateral bore far enough that the drill cuttings returning to the surface were in fact from the black shale. There might be plausible explanations for this apparent inconsistency or error. Of course, it might be speculated that the Antero-provided information on the well plats is incorrect and not intended to be accurate, or perhaps the driller is not really sure yet where the Marcellus layer starts. There may be many other possible scenarios of explanations. Time will tell.

IV. Research Observations Review

Landfill disposal of drill cuttings

Landfill disposal of drill cuttings

GOOD There are a number of recommendations and suggestions in the study on landfills and leachate related conditions. It seems that a number of these proposals are very accurate and should be implemented. For example:

The report clearly restates that drill cuttings are known to contain radioactive compounds. Since all landfill liners will eventually leak, and since landfills already have ground water test wells for monitoring for potential ground water contamination due to leaking liners, then the well samples should be tested for radiological isotopes. Good idea. They are not required to do that now, but this recommendation should be implemented immediately (pgs. 17 and 21).

GOOD The report recommends that the Publicly Owned Treatment Works (POTW) or in the case of Wetzel County, the on-site wastewater treatment plants, should also test their effluent for radioactive isotopes. This is very important since there is no way to efficiently filter out many of the radioactive isotopes. Such contaminants will pass through traditional wastewater treatment plants.

It is also very useful that the report recommends that all the National Pollution Discharge Elimination System (NPDES) limits at the POTWs be reviewed and required to take into consideration the significantly more challenging chemical and radiological makeup of the shale waste products.

V. Economic Considerations on an Industry Supported Mono-Fill

The legislature asked that the DEP evaluate the feasibility of the natural gas industry to build, own, or operate its own landfill solely for the disposal of the known radioactive waste. This request seems to be a very reasonable approach, since for decades we have only put known radioactive waste products into dedicated landfills that are exclusively and specifically designed for the long term storage of the special waste material.

The discussion of the economic considerations is extremely complete and detailed. They are given in Appendix I and take into consideration a very thorough economic feasibility study of such a proposed endeavor. This section seems to have been compiled by a very talented professional team.

FLAW  However, some of the basic assumptions are a bit askew. For example:

The initial Abstract of the financial analysis states that two new landfills would be needed because we do not want to have the well operators to drive any further than they do now. Interesting. This seems to be not too different than a homeowner while in search for privacy and quiet, builds a home far out into the country and then expects the public sewage lines to be extended miles to his new home so he would not have to incur the cost of a septic system. Homebuilders in rural settings should know they will have to incur expenses for their waste disposal needs. Should gas companies expect that communities to provide cheap waste disposal for them?

More than 15 pages later, the most important aspect is clearly stated that, “…the most salient benefit of establishing a separate landfill sited specifically to receive (radioactive) drill cuttings would be the preservation of existing disposal capacity of existing fills for future waste disposal”. Meaning for my (our) grandchildren. See page 175.

Comprehensive and sound financial details later explain that having the natural gas operators build, operate, and eventually close their own radioactive waste depository landfill would involve a lot of their capital and involve some risk to them. It is stated that their money would be better used drilling more wells. The conclusion then seems to be that, all around, it is simply cheaper and less risky for the gas industry to put all their waste products into our Municipal Waste Landfills, and later residents should incur the costs and risk to build another land fill for their household garbage when needed.

VI. Report Omissions

  1. Within the report section dealing with the leachate test results, it is casually mentioned that not only do the landfills receiving shale waste materials have radioactive contaminated leachate, but the other tested landfills do, as well. However, rather than raising a very red flag and expressing concern over a problem that no one has looked into, the report implies we should not worry about any radioactive waste because it might be in all landfills (pg. 139).
  2. Nowhere within the radiological discussion is there any mention of what might be called speciation of radioactive isotopes. The report does state that the test for both gross alpha and gross beta, are considered a “scanning procedure.” The speciation process is sort of a slice and dice procedure, showing exactly what isotopes are responsible for the activity that is being indicated. This process, however, does not seem to have been done on the landfill leachate test samples. The general scanning process cannot do that. Appendix H, pages 141-142, contains detailed facts on radiation dose, risk, and exposure. This might have been a good place to also discuss the proper EPA testing protocols, used or not used, and why.
  3. A short discussion of the DEP-required landfill entrance radiation monitors is included on page 146. The installed monitors are the goalpost type. Trucks drive between them at the entrance and when they cross the scales. It seems that the report should have emphasized that that type of monitor will primarily only detect high-energy gamma radiation. However what is omitted on page 144 is that the primary form of decay for radium-226 is releasing alpha particles. The report is ambiguous in saying the decay products of radium-226 include both alpha particles and some gamma radiation, but radium-266 is not a strong gamma emitter. It is very unlikely that a normal steel enclosed roll-off box would ever trip the alarm setting with a load of drill cuttings. However those monitors are still useful since they will detect the high-energy gamma radiation from a truck carrying a lot of medical waste (pg. 17).
  4. It is stated on page 144 that the greatest health risk due to the presence of radium-226 is the fact that its daughter product is radon-222. Radium-226 has a half-life of 1,600 years, compared to radon’s 3.8 days. This difference might seem to imply that radon is less of a concern. Given the multitude of radium-226 going into our landfills means that we will be producing radon for a very long time.

VII. Resource Referenced in Article

Examination of Leachate, Drill Cuttings and Related Environmental, Economic and Technical Aspects Associated with Solid Waste Facilities in West Virginia, by Marshall University.

Injection wells in OH for disposing of oil and gas wastewater
Ted Auch, PhD

Threats to Ohio’s Water Security

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Ohio waterways face headwinds in the form of hydraulic fracturing water demand and waste disposal

By Ted Auch, PhD – Great Lakes Program Coordinator, and Elliott Kurtz, GIS Intern and University of Michigan Graduate Student

In just 44 of its 88 counties, Ohio houses 1,134 wells – including those producing oil and natural gas and Class II injection wells into which the industry’s waste is disposed. Last month we wrote about Ohio’s disturbing fracking waste disposal trend and the disproportionate influence of neighboring states. (Prior to that Ariel Conn at Virginia Tech outlined the relationship between Class II Injection Wells and induced seismicity on FracTracker.) This time around, we are digging deeper into how water demand is related to Class II disposal trends.

Ohio’s Utica oil and gas wells are using 7 million gallons of freshwater – or 2.4-2.8 million more than the average well cited by the US EPA.1 Below we explore the inter-county differences of the water used in these oil and gas wells, and how demand compares to residential water demand and wastewater production.

Please refer to Table 1 at the end of this article regarding the following findings.

Utica Shale Freshwater Demand

Data indicate that there may be serious threats to Ohio’s water security on the horizon due to the oil and gas industry.

OH Water Use

The counties of Guernsey and Monroe are next up with water demand and waste water generation at rates of 14.6 and 10.3 million gallons per year. However, the 11.4 million gallons of freshwater demand and fracking waste produced by these two counties 114 Utica and Class II wells still accounts for roughly 81% of residential water demand.

The wells within the six-county region including Meigs, Washington, Athens, and Belmont along the Ohio River use 73 million gallons of water and generate 51 million gallons of wastewater per year, while the hydraulic fracturing industry’s water-use footprint ranges between 48 and 17% of residential demand in Coshocton and Athens, respectively. Class II Injection well disposal accounts for a lion’s share of this footprint in all but Belmont County, with injection well activities equaling 77 to 100% of the industry’s water footprint (see Figure 1 for county locations and water stress).

Primary Southeast Ohio Counties experiencing Utica Shale and Class II water stress

Figure 1. Primary Southeast Ohio counties experiencing Utica Shale and Class II water stress

The next eight-county cohort is spread across the state from the border of Pennsylvania and the Ohio River to interior Appalachia and Central Ohio. Residential water demand there equals 428 million gallons, while the eight county’s 92 Utica and 90 Class II wells have accounted for 15 million gallons of water demand and disposal. Again the injection well component of the industry accounts for 5.8% of the their 7.7% footprint relative to residential demand. The range is nearly 10% in Vinton and 5.3% in Jefferson County.

The next cohort includes twelve counties that essentially surround Ohio’s Utica Shale region from Stark and Mahoning in the Northeast to Pickaway, Hocking, and Gallia along the southwestern perimeter of “the play.” These counties’ residents consume 405 million gallons of water and generate 329 million gallons of wastewater annually. Meanwhile the industry’s 69 Class II wells account for 53 million gallons – a 2.8% water footprint.

Finally, the 11 counties with the smallest Utica/Class II footprint are not suprisingly located along Lake Erie, as well as the Michigan and Indiana border, with water demand and wastewater production equalling nearly 117 billion gallons per year. Meanwhile the region’s 3 Utica and 18 Class II wells have utilized 59 million gallons. These figures equate to a water footprint of roughly 00.15%, more aligned with the 1% of total annual water use and consumption for the hydraulic fracturing industry cited by the US EPA this past June.

Future Concerns and Projections

Industry will see their share of the region’s hydrology increase in the coming months and years given that injection well volumes and Utica Shale demand is increasing by 1.04 million gallons and 405-410 million gallons per quarter per well, respectively. The number of people living in these 42 counties is declining by 0.6% per year, however, 1.4% in the 10 counties that have seen the highest percentage of their water resources allocated to Utica and Class II operations. Additionally, hydraulic fracturing permitting is increasing by 14% each year.2

Table 1. Residential, Utica Shale, and Class II Injection well water footprint across forty-two Ohio Counties (Note: All volumes are in millions of gallons)

Table1

Footnotes & Resources

1. In their recent “Assessment of the Potential Impacts of Hydraulic Fracturing for Oil and Gas on Drinking Water Resources” (Note: Ohio’s hydraulically fractured wells are using 6% reused water vs. the 18% cited by the EPA).

2. Auch, W E, McClaugherty, C, Gallemore, C, Berghoff, D, Genshock, E, Kurtz, E, & Jurjus, R. (2015). Ramification of current and future production, resource utilization, and land-use change in the Ohio Utica Shale Basin. Paper presented at the National Environmental Monitoring Conference, Chicago, IL.

FracTracker map of the density of wells by U.S. state as of 2015
Matt Kelso, BA

1.7 Million Wells in the U.S. – A 2015 Update

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Please Note

Click here to view an update on this topic


 

Updated National Well Data

By Matt Kelso, Manager of Data & Technology

In February 2014, the FracTracker Alliance produced our first version of a national well data file and map, showing over 1.1 million active oil and gas wells in the United States. We have now updated that data, with the total of wells up to 1,666,715 active wells accounted for.

Density by state of active oil and gas wells in the United States. Click here to access the legend, details, and full map controls. Zoom in to see summaries by county, and zoom in further to see individual well data. Texas contains state and county totals only, and North Carolina is not included in this map. 

While 1.7 million wells is a substantial increase over last year’s total of 1.1 million, it is mostly attributable to differences in how we counted wells this time around, and should not be interpreted as a huge increase in activity over the past 15 months or so. Last year, we attempted to capture those wells that seemed to be producing oil and gas, or about ready to produce. This year, we took a more inclusive definition. Primarily, the additional half-million wells can be accounted for by including wells listed as dry holes, and the inclusion of more types of injection wells. Basically anything with an API number that was not described as permanently plugged was included this time around.

Data for North Carolina are not included, because they did not respond to three email inquiries about their oil and gas data. However, in last year’s national map aggregation, we were told that there were only two active wells in the state. Similarly, we do not have individual well data for Texas, and we use a published list of well counts by county in its place. Last year, we assumed that because there was a charge for the dataset, we would be unable to republish well data. In discussions with the Railroad Commission, we have learned that the data can in fact be republished. However, technical difficulties with their datasets persist, and data that we have purchased lacked location values, despite metadata suggesting that it would be included. So in short, we still don’t have Texas well data, even though it is technically available.

Wells by Type and Status

Each state is responsible for what their oil and gas data looks like, so a simple analysis of something as ostensibly straightforward as what type of well has been drilled can be surprisingly complicated when looking across state lines. Additionally, some states combine the well type and well status into a single data field, making comparisons even more opaque.

Top 10 of 371 published well types for wells in the United States.

Top 10 of 371 published well types for wells in the United States.

Among all of the oil producing states, there are 371 different published well types. This data is “raw,” meaning that no effort has been made to combine similar entries, so “gas, oil” is counted separately from “GAS OIL,” and “Bad Data” has not been combined with “N/A,” either. Conforming data from different sources is an exercise that gets out of hand rather quickly, and utility over using the original published data is questionable, as well. We share this information, primarily to demonstrate the messy state of the data. Many states combine their well type and well status data into a single column, while others keep them separate. Unfortunately, the most frequent well type was blank, either because states did not publish well types, or they did not publish them for all of their wells.

There are no national standards for publishing oil and gas data – a serious barrier to data transparency and the most important takeaway from this exercise… 

Wells by Location

Active oil and gas wells in 2015 by state. Except for Texas, all data were aggregated published well coordinates.

Active oil and gas wells in 2015 by state. Except for Texas, all data were aggregated published well coordinates.

There are oil and gas wells in 35 of the 50 states (70%) in the United States, and 1,673 out of 3,144 (53%) of all county and county equivalent areas. The number of wells per state ranges from 57 in Maryland to 291,996 in Texas. There are 135 counties with a single well, while the highest count is in Kern County, California, host to 77,497 active wells.

With the exception of Texas, where the data are based on published lists of well county by county, the state and county well counts were determined by the location of the well coordinates. Because of this, any errors in the original well’s location data could lead to mistakes in the state and county summary files. Any wells that are offshore are not included, either. Altogether, there are about 6,000 wells (0.4%) are missing from the state and county files.

Wells by Operator

There are a staggering number of oil and gas operators in the United States. In a recent project with the National Resources Defense Council, we looked at violations across the few states that publish such data, and only for the 68 operators that were identified previously as having the largest lease acreage nationwide. Even for this task, we had to follow a spreadsheet of which companies were subsidiaries of others, and sometimes the inclusion of an entity like “Williams” on the list came down to a judgement call as to whether we had the correct company or not.

No such effort was undertaken for this analysis. So in Pennsylvania, wells drilled by the operator Exco Resources PA, Inc. are not included with those drilled by Exco Resources PA, Llc., even though they are presumably the same entity. It just isn’t feasible to systematically go through thousands of operators to determine which operators are owned by whom, so we left the data as is. Results, therefore, should be taken with a brine truck’s worth of salt.

Top 10 wells by operator in the US, excluding Texas. Unknown operators are highlighted in red.

Top 10 wells by operator in the US, excluding Texas. Unknown operators are highlighted in red.

Texas does publish wells by operator, but as with so much of their data, it’s just not worth the effort that it takes to process it. First, they process it into thirteen different files, then publish it in PDF format, requiring special software to convert the data to spreadsheet format. Suffice to say, there are thousands of operators of active oil and gas wells in the Lone Star State.

Not counting Texas, there are 39,693 different operators listed in the United States. However, many of those listed are some version of “we don’t know whose well this is.” Sorting the operators by the number of wells that they are listed as having, we see four of the top ten operators are in fact unknown, including the top three positions.

Summary

The state of oil and gas data in the United States is clearly in shambles. As long as there are no national standards for data transparency, we can expect this trend to continue. The data that we looked for in this file is what we consider to be bare bones: well name, well type, well status, slant (directional, vertical, or horizontal), operator, and location. In none of these categories can we say that we have a satisfactory sense of what is going on nationally.

2015 Data Download

Click to download zip file

Click on the above button to download the three sets of data we used to make the dynamic map (once you are zoomed in to a state level). The full dataset was broken into three parts due to the large file sizes.

Bird’s eye view of a sand mine in Wisconsin. Photo by Ted Auch 2013.
Ted Auch, PhD

West Central Wisconsin’s Landscape and What Silica Sand Mining Has Done to It

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By Ted Auch, Great Lakes Program Coordinator, and Elliott Kurtz, GIS Intern

The Great Lakes may see a major increase in the number of sand mines developed in the name of fracking. What impacts has the area already seen, and does future development mean for the region’s ecosystem and land use?

Introduction

Sand is a necessary component of today’s oil and gas extraction industry for use in propping open the cracks that fracking creates. Silica sand is a highly sought after proppant for this purpose and often found in Wisconsin and Michigan. At the present time here in Ohio our Utica laterals are averaging 4,300-5,000 tons of silica sand or “proppant” with demand increasing by 85+ tons per lateral per quarter.

Wisconsin’s 125+ silica sand mines and processing facilities are spread out across 15,739 square miles of the state’s West Central region, adjacent to the Minnesota border in the Northern Mississippi Valley. These mines have dramatically altered the landscape while generating proppant for the shale gas industry; approximately 2.5 million tons of sand are extracted per mine. The length of the average shale gas lateral well grows by > 50 feet per quarter, so we expect silica sand usage will grow from 5,500 tons to > 8,000 tons per lateral. To meet this increase in demand, additional mines are being proposed near the Great Lakes.

Migration of the sand industry from the Southwest to the Great Lakes in search of this silica sand has had a large impact on regional ecosystem productivity and watershed resilience[1]. The land in the Great Lakes region is more productive, from a soil and biomass perspective; much of the Southwest sandstone geology is dominated by scrublands that have accrue plant biomass at much slower rates, while the Great Lakes host productive forests and agricultural land. Great Lakes ecosystems produce 1.92 times more soil organic matter and 1.46 times more perennial biomass than Southwestern ecosystems.

Effects on the Great Lakes

Quantifying what the landscape looks like now will serve as a baseline for understanding how the silica sand industry will have altered the overall landscape, much like Appalachia is doing today in the aftermath of strip-mining and Mountaintop Removal Mining[2]. West Central Wisconsin (WCW) has a chance to learn from the admittedly short-cited and myopic mistakes of their brethren across the coalfields of Appalachia.

Herein we aim to present numbers speaking to the diversity and distribution of WCW’s “working landscape” across eight types of land-cover. We will then present numbers speaking to how the silica mining industry has altered the region to date and what these numbers mean for reclamation. The folks at UC Berkeley’s Department of Environmental Science, Policy , and Management describe “Working Landscapes” as follows:

a broad term that expresses the goal of fostering landscapes where production of market goods and ecosystem services is mutually reinforcing. It means working with people as partners to create landscapes and ecosystems that benefit humanity and the planet… A goal is finding management and policy synergies—practices and policies that enhance production of multiple ecosystem services as well as goods for the market…Collaborative management processes can help discover synergies and create better decisions and policy. Incentives can help private landowners support management that benefits society.

Methods

We used the 1993 WISCLAND satellite imagery to determine how WCW’s landscape is partitioned and then we applied these data to an updated inventory of silica sand mine boundaries to determine what existed within their boundaries prior to mining. The point locations of Wisconsin’s current inventory of silica sand mines was determined using the “Geocode Address” function in ArcMap 10.2 using the Composite_US Address Locator. Addresses were drawn from mine inventory information originally maintained by the West Central WI Regional Planning Commission (WCWRPC) and now managed by the WI Department of Natural Resources’ Mines, pits and quarries division. Meanwhile current mine extent boundary polygons were determined using one of three satellite data-sets:

  1. 2013 imagery from the USDA National Agriculture Imagery Program (NAIP),
  2. 2014 ArcMap 10.2 World Imagery, and
  3. 2014 Google Satellite.

What We Found

Land Cover Types Replaced by Silica Sand Mining

Sand-LandEffects

Fig 1. Square mileage of various land cover types replaced by silica sand mining in WCW

Thirty-nine percent of the WCW landscape is currently allocated to forests, 43% to agriculture broadly speaking, and 13% is occupied by various types of wetlands. Open waters occupy 2.6% of the landscape with tertiary uses including barren lands (1.3%), golf courses (0.03%), high and low-density urban areas (0.9%), and miscellaneous shrublands (0.6%) (See Figure 1).

Effects by Land Cover Type

Figure 2. Forest Cover in WCW

Fig 2. Forest Cover in WCW

Figure 3. Agricultural Cover

Fig 3. Agricultural Cover

Figure 4. Open Water & Wetland Cover

Fig 4. Open Water & Wetland Cover

Figure 5. Forested Wetland Cover

Fig 5. Forested Wetland Cover

Figure 6. Lowland Shrub Wetland Cover

Fig 6. Lowland Shrub Wetlands

Figure 7. Miscellaneous Cover

Fig 7. Miscellaneous Cover

Figure 2. The wood in these forests has a current stumpage value of $253-936 million and by way of photosynthesis accumulates 63 to 131 million tons of CO2 and has accumulated 4.8-9.8 billion tons of CO2 if we assumed that on average forests in this region are 65-85 years old. Putting a finer point on WCW forest cover and associated quantifiables is difficult because most of these tracts (2.7 million acres) fall within a catchall category called “Mixed Forest”. Pine (2.3% of the region), Aspen (4.7%), and Oak (3.8%) most of the remaining 1.2 million forested acres with much less sugar (Acer saccharum) and soft (Acer rubrum) maple acreage than we expected scattered in a horseshoe fashion across the Northeastern portion of the study area.

Figure 3. Seven different agricultural land-uses occupy 4.3 million WCW acres with forage crops and grasslands constituting 29% of the region followed by 1.4 million acres of row crops and miscellaneous agricultural activities. Additionally, 2% of WI’s 19,700 cranberry bog acres are within the study area generating $4.02 million worth of cranberries per year. The larger agricultural categories generate $3.2 billion worth of commodities.

Figure 4. Nearly 16% of WCW is characterized by open waters or various types of wetlands with a total area of 2,396 square miles clustered primarily in two Northeast and one Southeast segment. Open waters occupy 398 square miles with forested wetlands – possibly vernal pool-type systems – amounting to 5.4% of the region or 841 square miles. Lowland shrub and emergent/wet meadows occupy 540 and 618 square miles, respectively.

Figure 5. Of the nine types of wetlands present in this region the forested broad-leaved deciduous and emergent/wet meadow variety constitute the largest fraction of the region at 1,107 square miles (7.1% of region). Some percentage of the former would likely be defined by Wisconsin DNR as vernal pools, which do the following according to their Ephemeral Pond program. The WI DNR doesn’t include silica sand mining in its list of 14 threats to vernal pools or potential conservation actions, however.

These ponds are depressions with impeded drainage (usually in forest landscapes), that hold water for a period of time following snowmelt and spring rains but typically dry out by mid-summer…They flourish with productivity during their brief existence and provide critical breeding habitat for certain invertebrates, as well as for many amphibians such as wood frogs and salamanders. They also provide feeding, resting and breeding habitat for songbirds and a source of food for many mammals. Ephemeral ponds contribute in many ways to the biodiversity of a woodlot, forest stand and the larger landscape…they all broadly fit into a community context by the following attributes: their placement in woodlands, isolation, small size, hydrology, length of time they hold water, and composition of the biological community (lacking fish as permanent predators).

Figure 6. Broad-leaved evergreen lowland shrub wetlands constitute ≈2.1% of the region or 319 square miles with most occurring around the Legacy Boggs silica mines and several cranberry operations turned silica mines in Jackson County. Meanwhile broad-leaved deciduous and needle-leaved lowland shrub wetlands are largely outside the current extent of silica sand mining in the region occupying 1.9% of the region with 293 square miles spread out within the northeastern 1/5th of the study area.

Figure 7. Finally, miscellaneous land-covers include 200 square miles of barren land, 145 square miles of low/high intensity urban areas including the cities of Eau Claire (Pop. 67,545) and Stevens Point (Pop. 26,670) as well as towns like Marshfield, Wisconsin Rapids, Merrill, and Rib Mountain-Weston. WCW also hosts 3,204 acres (0.03% of region) worth of golf courses which amounts to roughly 21 courses assuming the average course is 157 acres. Shrublands broadly defined occur throughout 0.6% of the region scattered throughout the southeast corner and north-central sixth of the region, with the both amalgamations poised to experience significant replacement or alteration as they are adjacent to two large silica mine groupings.

Producing Mine Land-Use/Land-Cover Change

To date we have established the current extent of land-use/land-cover change associated with 25 producing silica mines occupying 12 square miles of WCW. These mines have displaced 3 square miles of forests and 7 square miles of agricultural land-cover. These forested tracts accumulated 31,446-64,610 tons of CO2 per year or 2.4-4.9 million tons over the average lifespan of a typical Wisconsin forest. These values equate to the emissions of 144,401-295,956 Wisconsinites or 2.5-5.1% of the state’s population. The annual wood that was once generated on these parcels would have had a market value of $126,097-197,084 per year. Meanwhile the above agricultural lands would be generating roughly $1.5-3.3 million in commodities if they had not been displaced.

However, putting aside measurable market valuations it turns out the most concerning result of this analysis is that these mines have displaces 871 acres of wetlands which equals 11% of all mined lands. This alteration includes 158 acres of formerly forested wetlands, 352 acres of lowland shrub wetlands, and 361 acres of emergent/wet meadows. As we mentioned previously, the chance that these wetlands will be reconstituted to support their original plant and animal assemblages is doubtful.

We know that the St. Peter Sandstone formation is the primary target of the silica sand industry with respect to providing proppant for the shale gas industry. We also know that this formation extend across seven states and approximately 8,884 square miles, with all 91 square miles overlain by wetlands in Wisconsin. To this end carbon-rich grasslands soils or Mollisols, which we discussed earlier, sit atop 36% of the St. Peter Sandstone and given that these soils are alread endangered from past agricultural practices as well as current O&G exploration this is just another example of how soils stand to be dramatically altered by the full extent of the North American Hydrocarbon Industrial Complex. The following IFs would undoubtedly have a dramatic effect on the ability of the ecosystems overlying the St. Peter Sandstone to capture and store CO2 to the extent that they are today not to mention dramatically alter the landscape’s ability to capture, store, and purify precipitation inputs.

  • IF silica sand mining continues at the rate it is on currently
  • IF reclamation continues to result in “very poor stand of grass with some woody plants of very poor quality and little value on the whole for wildlife. Some areas may be reclaimed as crop land, however it is our opinion that substantial inputs such as commercial fertilizer as well as irrigation will be required in most if not all cases in order to produce an average crop.”
  • IF the highly productive temperate forests described above are not reassembled on similar acreage to their extent prior to mining and reclamation is largely to the very poor stands of grass mentione above
    • For example: Great Lakes forests like the ones sitting atop the St. Peter Sandstone capture 20.9 tons of CO2 per acre per year Vs their likely grass/scrublands replacement which capture 10.6-12.8 tons of CO2 per acre per year… You do the math!
  • “None two sites are capable of supporting the growing of food. They grow trees and some cover grass, but that is all. General scientific research says that the reclaimed soils lose up to 75% of their agricultural productivity.”

Quote from a concerned citizen:

I often wonder what it was like before the boom, before fortunes were built on castles of sand and resultant moonscapes stretched as far as the eye could see. In the past few years alone, the nickname the “Silica Sand Capital of the World” has become a curse rather than a blessing for the citizens of LaSalle County, Illinois. Here, the frac sand industry continues to proliferate and threaten thewellbeing of our people and rural ecosystem.

Additional Testimonials

References & Resources

  1. The US Forest Service defined Watershed Resilience as “Over time, all watersheds experience a variety of disturbance events such as fires and floods [and mining]. Resilient watersheds have the ability to recover promptly from such events and even be renewed by them. Much as treating forests can make them more resilient to wildfire, watershed restoration projects can improve watershed resilience to both natural and human disturbances.”
  2. Great example: Virginia Tech’s Powell River Project
Bird’s eye view of a sand mine in Wisconsin. Photo by Ted Auch 2013.
Ted Auch, PhD

Quick Sand: Frack Sand Mining in Wisconsin

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Each silica sand mine displaces 871 acres of wetlands and more than 12 square miles of forests and agriculture land in Wisconsin to provide the shale gas industry with fracking proppant.

By Juliana Henao, Communications Intern

Silica sand is used by the oil and gas industry as a way to prop open the fractures made during fracking – and is also referred to as a proppant. The industry’s demand for silica sand is steadily increasing (i.e., 4-5K tons per shale lateral, +86 tons per lateral per quarter), directly affecting the Great Lakes, their ecosystems, and land use. Silica sand is often found in Wisconsin and Michigan, which have felt the effects of increased sand mining demands through altered landscapes, impacted ecosystem productivity, and altering watershed resilience; these impacts will only continue to increase as the demand for silica sand increases.

To better understand frack sand mining’s current and potential effects, FracTracker’s Ted Auch and intern Elliott Kurtz, with generous support from the Save The Hills Alliance, explored mining and land use changes data in West Central Wisconsin (WCW). In their research paper, Auch and Kurtz show the current and future environmental impacts of increased sand mining in WCW in order to supply the oil and gas industry with sand. Not only does this research illustrate what is at risk in the WCW landscape, it also showcases what sand mining has already done to the region.

Read Full Report

Key Frack Sand Mining Findings

Land alterations due to silica sand mining in WI

Sixteen percent, or 2,396 square miles, of the West Central Wisconsin (WCW) is made up of wetlands or open waters. These and the other existing WCW landscapes are unquestionably profitable. The forests buffer climate change impacts – to date accumulating between 4.8-9.8 billion tons of CO2 assuming they are 65-85 years old – and have a current stumpage value of $253-936 million.

The 25 producing silica mines in this region occupy 12 square miles of WCW and have already displaced:

  • 3 mi2 of forests
  • 7 mi2 of agricultural land-cover
  • 1.36 mi2 of wetlands (equal to 11% of all mined lands)
    Formerly, these wetlands were one of three types:

    • 18% (158 acres) forested wetlands
    • 41% (353 acres) lowland shrub wetlands, and
    • 41% (361 acres) emergent/wet meadows
Breakdown of the current landscape types near these expanding mines, based on an analysis of satellite imagery

Breakdown of the current landscape types near these expanding mines, based on an analysis of satellite imagery

Why Wisconsin?

There are more than 125 silica sand mines throughout WCW, a stretch of ~16,000 square miles. Previously, the mining industry focused their efforts in Oklahoma and Texas’s Riley, Hickory/Brady, and Old Creek formations, where the land is not as agriculturally or ecologically productive as WCW. Now, more and more mines are being proposed and built in the WCW region. We wanted to determine what this change would mean for such an ecosystem diverse area of Wisconsin – many of which are considered “globally imperiled” or “globally rare” including oak savanna, dry prairies, southern dry-mesic forests, pine barrens, moist cliffs and oak openings.

The St. Peter Sandstone – along with the early Devonian and much smaller Sylvania Sandstone in Southeastern Michigan – is the primary target of the silica sand industry. Carbon-rich grassland soils cover 36% of the St. Peter, where they aid the ecosystem by capturing and sorting 20.9 tons of CO2 per year, as well as purifying precipitation inputs. This ecosystem, amongst many others around sand mining activities, will be dramatically altered if silica sand mining continues at its increasing rate. We will see CO2 capturing levels drop from 20.9 tons to 10.6 tons per acre per year if the highly productive temperate forests are not reassembled and reclaimed to their original acreage, as well as a significant loss (75%) in agricultural productivity on sites that are not reclaimed properly.

Out-of-state mining companies are settling into Wisconsin and displacing the land at a very high rate. As the president of Iowa’s Allamakee County Protectors Ric Zarwell told us by email “Frac sand mining companies do not come from the area where I live.  So efforts to destroy landscapes for frac sand are going to involve Neighbors Opposing Invaders.”

A high demand in silica sand from the shale gas industry will continue to drive this influx of mining companies into WI, providing a potentially collapsed ecosystem in the future. Factors at play include additional – and often much larger – mines under consideration, the average shale gas lateral grows by > 50 feet per quarter, and silica sand usage will grow from 5,500 tons to > 8,000 tons per lateral (i.e., 85 tons per quarter per lateral). Auch and Kurtz’s research paper describes in detail where how much silica sand might be needed in the future, as well as a detailed set of maps depicting land cover and usage in WI.

Kyle Ferrar, MPH

Largest Coastal Spill in 25 years [in California]

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By Kyle Ferrar, Western Program Coordinator

The Santa Barbara Pipeline Spill

On May 19, 2015, just 20 miles north of Santa Barbara, a heavily corroded section of pipeline ruptured spilling upwards of 101,000 gallons. The pipeline was operated by Plains All American LLC, based out of Houston Texas, and was used to move crude oil from offshore rigs to inland refineries. The spill occurred on a section of pipe running parallel to the coastline at a distance of only a tenth of a mile to the ocean. As a result, the ruptured oil traveled through a drainage culvert and onto the beach where 21,000 gallons spilled into the ocean. The oil spread into a slick that covered 4 miles of coastline, and has since spread to southern California beaches more than 100 miles to the south. Santa Barbara county officials immediately closed two beaches, Refugio and El Capitan, and southern California beaches were also closed June 3rd through June 5th. Commercial fishing has been prohibited near the spill, and nearly 300 dead marine mammals and birds have been found, as well as dead cephalopods (octopi).1

Mapping the Impacts


Santa Barbara 2015 Oil Spill at Refugio Beach. To view the legend and map full screen, click here.

The map above shows details of the oil spill, including the location on the coastline, the extent that the spill traveled south, and the Exxon offshore platforms forced to suspend operations due to their inability to transport crude to onshore refineries.

The dynamic map also shows the wildlife habitats that are impacted by this oil spill, putting these species at risk. This area of Central California coastline is incredibly unique. The Santa Barbara Channel Islands are formed and molded as colder northern swells meet warmer southern swells, generating many temperature gradients and microhabitats able to support an incredible amount of biodiversity. Many species are endemic to only this region of the California coastline, and therefore are very sensitive to the impacts of pollution. In addition to the many bird species, including the endangered Western Snow Plover and Golden Eagle, this area of coastline is home to a number of whale and porpoise species, and, as seen in the map, the Leatherback Sea Turtle and the Black Abolone Sea Snail, both threatened.

Santa Barbara Channel_10.7.13

Figure 1. Offshore Drilling Near Santa Barbara from 2013

For California’s harbor seal populations, this kill event reinforces existing environmental pressures that have been shrinking the seal and sea lion (pinniped) communities, increasing the threat of shark attacks on humans. For the potential impact that this could have on California’s sensitive sea otter population, see FracTracker’s recent story on the West Coast Sea Otter.

In 2013, The FracTracker Alliance collaborated with the Environmental Defense Center on the report Dirty Water: Fracking Offshore California. The report showed that much of the offshore oil is extracted by hydraulic fracturing (Fig 1.), and outlined the environmental impacts that would result from a spill of this magnitude.

Clean Up Efforts

Workers are currently cleaning the spill by hand using buckets and shovels. These old fashioned techniques may be painstaking, but they are the least invasive and they are necessary to ensure that there is not additional damage to the sensitive ecosystems. Even scraping the coastline with wire brushes and putty knives cannot remove the stain of oil that has been absorbed by porous rocks. The oil will only wear away with time as it is diluted back into the ocean. Costs of the clean-up response alone have already reached $92 million, which is being paid by Texas-based Plains All American Pipeline. There have not been any reports yet on the financial impacts to the recreational and fishing industries.2

Prevention Opportunities

By comparison, the Santa Barbara oil spill in 1969 was estimated at 200 million gallons. After over 45 years, nearly a half decade, one would think that advancements in pipeline engineering and technology would prevent these types of accidents. Plains All American, the pipeline operator states that their pressure monitors can detect leaks the size of pinholes. Why, then, did the ruptured pipe continue to spill crude for three hours after the public was notified of the incident?

This section of pipeline (falsely reported by the media to be abandoned) was built in 1987. At capacity the pipeline could transport 50,400 gallons of oil per hour, but during the time of the spill the pipeline was running under capacity. Pipeline inspections had occurred in 2012 and in April of 2014, just weeks prior. The Pipeline and Hazardous Material Safety Administration said testing conducted in May had identified extensive corrosion of the pipeline that required maintenance. It is possible that this incident is an isolated case of mismanagement, but the data tell a different story as this is not an isolated event.

Plains released a statement that a spill of this magnitude was “highly unlikely,” although this section of the pipeline has experienced multiple other spills, the largest of which being 1,200 gallons. Just a year prior, May 2014, the same company, Plains, was responsible for a 19,000 gallon spill of crude in Atwater Village in Los Angeles County. According to a joint hearing of two legislative committees, the operators, Plains did not meet state guidelines for reporting the spill. According to the county, the operator should have been able to shut down the pipeline much faster.3 It is not clear how long the pipeline was actually leaking.

NASA Spill Visualizations

As a result of the spill and to assist with the clean-up and recovery, NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, CA has developed new technology to track the oil slick and locate contamination of beaches along the coastline. The JPL deployed a De Havilland Twin Otter aircraft carrying a unique airborne instrument developed to study the spill and test the ability of imaging spectroscopy to map tar on area beaches. What this means is that from aircraft special cameras can take pictures of the beach. Based on the nature of the light waves reflecting off the beach in the pictures, tar balls and oil contamination can be identified. Clean-up crews can then be dispatched to these areas. On their website, NASA states “The work is advancing our nation’s ability to respond to future oil spills.”4 A picture generated using this technology, and showing oil contamination in water and on the beach, is shown below.

SBOilSpill_NASA

References

  1.  Maza, C. 2015. California oil spill: Regulators, lawmakers scrutinize company response. Christian Science Monitor. Accessed 7/1/15.
  2. Chang, A. 2015. Workers clean up oil spill on California beaches by hand. The Washington Times. Accessed 7/5/15.
  3. Panzar, J. 2015. Official says pipeline firm violated state guidelines for reporting Santa Barbara spill. Los Angeles Times. Accessed 7/6/15.
  4. NASA. 2015. NASA Maps Beach Tar from California Oil Pipeline Spill. NASA Jet Propulsion Laboratory California Institute of Technology. Accessed 7/7/17.
Proposed Atlantic Coast Pipeline route
Karen Edelstein

An urgent need? Atlantic Coast Pipeline Discussion and Map

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By Karen Edelstein, Eastern Program Coordinator

This article was originally posted on 10 July 2015, and then updated on 22 January 2016 and 16 February 2016.

Proposed Pipeline to Funnel Marcellus Gas South

In early fall 2014, Dominion Energy proposed a $5 billion pipeline project, designed provide “clean-burning gas supplies to growing markets in Virginia and North Carolina.” Originally named the “Southeast Reliability Project,” the proposed pipeline would have a 42-inch diameter in West Virginia and Virginia. It would narrow to 36 inches in North Carolina, and narrow again to 20 inches in the portion that would extend to the coast at Hampton Roads. Moving 1.5 billion cubic feet per day of gas, with a maximum allowable operating pressure of 1440 psig (pounds per square inch gage), the pipeline would be designed for larger customers (such as manufacturers and power generators) or local gas distributors supplying homes and businesses to tap into the pipeline along the route, making the pipeline a prime mover for development along its path.

The project was renamed the Atlantic Coast Pipeline (ACP) when a coalition of four major US energy companies—Dominion (45% ownership), Duke Energy (40%), Piedmont Natural Gas (15%), and AGL Resources (5%)— proposed a joint venture in building and co-owning the pipeline. Since then, over 100 energy companies, economic developers, labor unions, manufacturers, and civic groups have joined the new Energy Sure Coalition, supporting the ACP. The coalition asserts that the pipeline is essential because the demand for fuel for power generation is predicted more than triple over the next 20 years. Their website touts the pipeline as a “Path to Cleaner Energy,” and suggests that the project will generate significant tax revenue for Virginia, North Carolina, and West Virginia.

Map of Proposed Atlantic Coast Pipeline


View map fullscreen – including legend and measurement tools.

Development Background

Lew Ebert, president of the North Carolina Chamber of Commerce, optimistically commented:

Having the ability to bring low-cost, affordable, predictable energy to a part of the state that’s desperately in need of it is a big deal. The opportunity to bring a new kind of energy to a part of the state that has really struggled over decades is a real economic plus.

Unlike older pipelines, which were designed to move oil and gas from the Gulf Coast refineries northward to meet energy demands there, the Atlantic Coast Pipeline would tap the Marcellus Shale Formation in Ohio, West Virginia and Pennsylvania and send it south to fuel power generation stations and residential customers. Dominion characterizes the need for natural gas in these parts of the country as “urgent,” and that there is no better supplier than these “four homegrown companies” that have been economic forces in the state for many years.

In addition to the 550 miles of proposed pipeline for this project, three compressor stations are also planned. One would be at the beginning of the pipeline in West Virginia, a second midway in County Virginia, and the third near the Virginia-North Carolina state line.  The compressor stations are located along the proposed pipeline, adjacent to the Transcontinental Pipeline, which stretches more than 1,800 miles from Pennsylvania and the New York City Area to locations along the Gulf of Mexico, as far south as Brownsville, TX.

In mid-May 2015, in order to avoid requesting Congressional approval to locate the pipeline over National Park Service lands, Dominion proposed rerouting two sections of the pipeline, combining the impact zones on both the Blue Ridge Parkway and the Appalachian Trail into a single location along the border of Nelson and Augusta Counties, VA. National Forest Service land does not require as strict of approvals as would construction on National Park Service lands. Dominion noted that over 80% of the pipeline route has already been surveyed.

Opposition to the Pipeline on Many Fronts

The path of the proposed pipeline crosses topography that is well known for its karst geology feature—underground caverns that are continuous with groundwater supplies. Environmentalists have been vocal in their concern that were part of the pipeline to rupture, groundwater contamination, along with impacts to wildlife could be extensive. In Nelson County, VA, alone, 70% of the property owners in the path of the proposed pipeline have refused Dominion access for survey, asserting that Dominion has been unresponsive to their concerns about environmental and cultural impacts of the project.

On the grassroots front, 38 conservation and environmental groups in Virginia and West Virginia have combined efforts to oppose the ACP. The group, called the Allegany-Blue Ridge Alliance (ABRA), cites among its primary concerns the ecologically-sensitive habitats the proposed pipeline would cross, including over 49.5 miles of the George Washington and Monongahela State Forests in Virginia and West Virginia. The “alternative” version of the pipeline route would traverse 62.7 miles of the same State Forests. Scenic routes, including the Blue Ridge Parkway and the Appalachian Scenic Trail would also be impacted. In addition, it would pose negative impacts on many rural communities but not offset these impacts with any longer-term economic benefits. ABRA is urging for a programmatic environmental impact statement (PEIS) to assess the full impact of the pipeline, and also evaluate “all reasonable, less damaging” alternatives. Importantly, ABRA is urging for a review that explores the cumulative impacts off all pipeline infrastructure projects in the area, especially in light of the increasing availability of clean energy alternatives.

Environmental and political opposition to the pipeline has been strong, especially in western Virginia. Friends of Nelson, based in Nelson County, VA, has taken issue with the impacts posed by the 150-foot-wide easement necessary for the pipeline, as well as the shortage of Department of Environmental Quality staff that would be necessary to oversee a project of this magnitude.

Do gas reserves justify this project?

Dominion, an informational flyer, put forward an interesting argument about why gas pipelines are a more environmentally desirable alternative to green energy:

If all of the natural gas that would flow through the Atlantic Coast Pipeline is used to generate electricity, the 1.5 billion cubic feet per day (bcf/d) would yield approximately 190,500 megawatt-hours per day (mwh/d) of electricity. The pipeline, once operational, would affect approximately 4,600 acres of land. To generate that much electricity with wind turbines, utilities would need approximately 46,500 wind turbines on approximately 476,000 acres of land. To generate that much electricity with solar farms, utilities would need approximately 1.7 million acres of land dedicated to solar power generation.

Nonetheless, researchers, as well as environmental groups, have questioned whether the logic is sound, given production in both the Marcellus and Utica Formations is dropping off in recent assessments.

Both Nature, in their article Natural Gas: The Fracking Fallacy, and Post Carbon Institute, in their paper Drilling Deeper, took a critical look at several of the current production scenarios for the Marcellus Shale offered by EIA and University of Texas Bureau of Economic Geology (UT/BEG). All estimates show a decline in production over current levels. The University of Texas report, authored by petroleum geologists, is considerably less optimistic than what has been suggested by the Energy Information Administration (EIA), and imply that the oil and gas bubble is likely to soon burst.

Natural Gas Production Projections for Marcellus Shale

Natural Gas Production Projections for Marcellus Shale

David Hughes, author of the Drilling Deeper report, summarized some of his findings on Marcellus productivity:

  • Field decline averages 32% per year without drilling, requiring about 1,000 wells per year in Pennsylvania and West Virginia to offset.
  • Core counties occupy a relatively small proportion of the total play area and are the current focus of drilling.
  • Average well productivity in most counties is increasing as operators apply better technology and focus drilling on sweet spots.
  • Production in the “most likely” drilling rate case is likely to peak by 2018 at 25% above the levels in mid-2014 and will cumulatively produce the quantity that the Energy Information Administration (EIA) projected through 2040. However, production levels will be higher in early years and lower in later years than the EIA projected, which is critical information for ongoing infrastructure development plans.
  • The EIA overestimates Marcellus production by between 6% and 18%, for its Natural Gas Weekly and Drilling Productivity reports, respectively.
  • Five out of more than 70 counties account for two-thirds of production. Eighty-five percent of production is from Pennsylvania, 15% from West Virginia and very small amounts from Ohio and New York. (The EIA has published maps of the depth, thickness and distribution of the Marcellus shale, which are helpful in understanding the variability of the play.)
  • The increase in well productivity over time reported in Drilling Deeper has now peaked in several of the top counties and is declining. This means that better technology is no longer increasing average well productivity in these counties, a result of either drilling in poorer locations and/or well interference resulting in one well cannibalizing another well’s recoverable gas. This declining well productivity is significant, yet expected, as top counties become saturated with wells and will degrade the economics which have allowed operators to sell into Appalachian gas hubs at a significant discount to Henry hub gas prices.
  • The backlog of wells awaiting completion (aka “fracklog”) was reduced from nearly a thousand wells in early 2012 to very few in mid-2013, but has increased to more than 500 in late 2014. This means there is a cushion of wells waiting on completion which can maintain or increase overall play production as they are connected, even if the rig count drops further.
  • Current drilling rates are sufficient to keep Marcellus production growing on track for its projected 2018 peak (“most likely” case in Drilling Deeper).

Post Carbon Institute estimates that Marcellus predictions overstate actual production by 45-142%. Regardless of the model we consider, production starts to drop off within a year or two after the proposed Atlantic Coast Pipeline would go into operation. This downward trend leads to some serious questions about whether moving ahead with the assumption of three-fold demand for gas along the Carolina coast should prompt some larger planning questions, and whether the availability of recoverable Marcellus gas over the next twenty years, as well as the environmental impacts of the Atlantic Coast Pipeline, justify its construction.

Next steps

The Federal Energy Regulatory Commission, FERC, will make a final approval on the pipeline route later in the summer of 2015, with a final decision on the pipeline construction itself expected by fall 2016.

UPDATE #1: On January 19, 2016, the Richmond Times-Dispatch reported that the United States Forest Service had rejected the pipeline, due to the impact its route would have on habitats of sensitive animal species living in the two National Forests it is proposed to traverse.

UPDATE #2: On February 12, 2016, Dominion Pipeline Company released a new map showing an alternative route to the one recently rejected by the United States Forest Service a month earlier. Stridently condemned by the Dominion Pipeline Monitoring Coalition as an “irresponsible undertaking”, the new route would not only cross terrain the Dominion had previously rejected as too hazardous for pipeline construction, it would–in avoiding a path through Cheat and Shenandoah Mountains–impact terrain known for its ecologically sensitive karst topography, and pose grave risks to water quality and soil erosion.

Northeast Ohio Class II injection wells taken via FracTracker's mobile app, May 2015
Ted Auch, PhD

OH Class II Injection Wells – Waste Disposal and Industry Water Demand

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By Ted Auch, PhD – Great Lakes Program Coordinator

Waste Trends in Ohio

Map of Class II Injection Volumes and Utica Shale Freshwater Demand in Ohio

Map of Class II Injection Volumes and Utica Shale Freshwater Demand in Ohio. Explore dynamic map

It has been nearly 2 years since last we looked at the injection well landscape in Ohio. Are existing disposals wells receiving just as much waste as before? Have new injection wells been added to the list of those permitted to receive oil and gas waste? Let’s take a look.

Waste disposal is an issue that causes quite a bit of consternation even amongst those that are pro-fracking. The disposal of fracking waste into injection wells has exposed many “hidden geologic faults” across the US as a result of induced seismicity, and it has been linked recently with increases in earthquake activity in states like Arkansas, Kansas, Texas, and Ohio. Here in OH there is growing evidence – from Ashtabula to Washington counties – that injection well volumes and quarterly rates of change are related to upticks in seismic activity.

Origins of Fracking Waste

Furthermore, as part of this analysis we wanted to understand the ratio of Ohio’s Class II waste that has come from within Ohio and the proportion of waste originating from neighboring states such as West Virginia and Pennsylvania. Out of 960 Utica laterals and 245+ Class II wells, the results speak to the fact that a preponderance of the waste is coming from outside Ohio with out-of-state shale development accounting for ≈90% of the state’s hydraulic fracturing brine stream to-date. However, more recently the tables have turned with in-state waste increasing by 4,202 barrels per quarter per well (BPQPW). Out-of-state waste is only increasing by 1,112 BPQPW. Such a change stands in sharp contrast to our August 2013 analysis that spoke to 471 and 723 BPQPW rates of change for In- and Out-Of-State, respectively.

Brine Production

Ohio Class II Injection Well trends In- and Out-Of-State, Cumulatively, and on Per Well basis (n = 248).

Figure 1. Ohio Class II Injection Well trends In- and Out-Of-State, Cumulatively, and on Per Well basis (n = 248).

For every gallon of freshwater used in the fracking process here in Ohio the industry is generating .03 gallons of brine (On average, Ohio’s 758 Utica wells use 6.88 million gallons of freshwater and produce 225,883 gallons of brine per well).

Back in August of 2013 the rate at which brine volumes were increasing was approaching 150,000 BPQPW (Learn more, Fig 5), however, that number has nearly doubled to +279,586 BPQPW (Note: 1 barrel of brine equals 32-42 gallons). Furthermore, Ohio’s Class II Injection wells are averaging 37,301 BPQPW (1.6 MGs) per quarter over the last year vs. 12,926 barrels BPQPW – all of this between the initiation of frack waste injection in 2010 and our last analysis up to and including Q2-2013. Finally, between Q3-2010 and Q1-2015 the exponential increase in injection activity has resulted in a total of 81.7 million barrels (2.6-3.4 billion gallons) of waste disposed of here in Ohio. From a dollars and cents perspective this waste has generated $2.5 million in revenue for the state or 00.01% of the average state budget (Note: 2.5% of ODNR’s annual budget).

Freshwater Demand Growing

Ohio Class II Injection Well disposal as a function of freshwater demand by the shale industry in Ohio between Q3-2010 and Q1-2015.

Figure 2. Ohio Class II Injection Well disposal as a function of freshwater demand by the shale industry in Ohio between Q3-2010 and Q1-2015.

The relationship between brine (waste) produced and freshwater needed by the hydraulic fracturing industry is an interesting one; average freshwater demand during the fracking process accounts for 87% of the trend in brine disposal here in Ohio (Fig. 2). The more water used, the more waste produced. Additionally, the demand for OH freshwater is growing to the tune of 405-410,000 gallons PQPW, which means brine production is growing by roughly 12,000 gallons PQPW. This says nothing for the 450,000 gallons of freshwater PQPW increase in West Virginia and their likely demand for injection sites that can accommodate their 13,500 gallons PQPW increase.

Where will all this waste go? I’ll give you two guesses, and the first one doesn’t count given that in the last month the ODNR has issued 7 new injection well permits with 9 pending according to the Center For Health and Environmental Justice’s Teresa Mills.

Matt Kelso, BA

Unconventional Drilling Activity Down In Pennsylvania

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By Matt Kelso, Manager of Data & Technology

Wells Spudded (Drilled)

The number of newly drilled unconventional wells in Pennsylvania peaked in 2011.

Figure 1: Newly drilled unconventional wells in Pennsylvania peaked in 2011.

Unconventional oil and gas drilling is well established in Pennsylvania, with over 9,200 drilled wells, an additional 7,200 permitted locations that have not yet been drilled, and 5,300 violations all happening since the turn of the millennium. It took a while for the industry to gather steam, with just one unconventional well drilled in 2002, and only eight in 2005. But by 2010, that figure had ballooned to 1,599 wells, which was greater than the previous eight years combined. There were 1,956 wells drilled in 2011, representing the peak for unconventional drilling activity in Pennsylvania (Figure 1).

None of the three full years since then, however, have seen more than 70% of the 2011 total. Halfway through 2015, the industry is on pace to drill only 842 unconventional wells statewide, which would be the lowest total since 2009, and only 43% of the 2011 total.


Pennsylvania Shale Viewer. Click here to access the full screen view with a legend, layer details, and other tools.

Taken cumulatively, the footprint on the state is immense, as is shown in the map above, and impacts remain for some time. Of Pennsylvania’s 9,234 unconventional wells 8,187 (89%) are still active. Only 474 wells have been permanently plugged so far, with 570 given an inactive status, and one well listed as “proposed but never materialized,” despite being included on the spud report.

Permits & Violations

The number of permits and violations issued have been declining over the past five years as well.

Five years of unconventional oil and gas activity in Pennsylvania, July 2010 through June 2015.

Figure 2: Five years of unconventional oil and gas activity in Pennsylvania, July 2010 through June 2015.

Figure 2 shows the monthly totals of permits, wells, and violations over the last 60 months. Linear trendlines were added to the chart to give a visual representation of changes over time if we ignore the noise of the peaks and troughs of activity, which is an inherent attribute of the industry. Each of the three trendlines has a negative slope1, showing downward trends in each category.

In fact, permits for new wells are declining more rapidly than the drilled wells, and violations issued are declining at a still faster rate. Over the course of five years, these declines are substantial. In July 2010, the smoothed totals that are “predicted” by the trendline show 304 permits issued, 159 wells drilled, and 128 violations issued per month.  60 months later, one would expect 213 permits, 81 wells drilled, and just 12 violations issued2.

Location of Drilling Activity

The oil and gas industry has been more selective about where unconventional wells are being drilled in recent years, as well. Altogether, there are unconventional wells in 39 different counties, with 32 counties seeing action in both 2010 and 2011. That number is down to 22 for both 2014 and the first half of 2015. There has been drilling in 443 different municipalities since 2002, with a maximum of 241 municipal regions in 2011, which shrank to 161 last year, and just 88 in the first half of 2015.


Summary of unconventional wells drilled in each Pennsylvania county by year, through June 30, 2015. Click here to access the full screen view with a legend, layer details, and other tools

Clicking on any of the counties above will show the number of unconventional wells drilled in that county by year since the first unconventional well was spudded in Pennsylvania back in 2002.  The color scheme shows the year that the maximum number of unconventional wells were drilled in each county, with blues, greens, and yellows showing counties where the activity has already peaked, oranges showing a peak in 2014, and red showing a peak in 2015, despite only six months of activity.  30 of the 39 counties with unconventional wells in the state saw a peak in activity in 2013 or before.

Notes

  1. The equations for the three trendlines are as follows:
    • Permits: y = -1.5128x + 303.81
    • Wells: y = -1.2939x + 158.95
    • Violations: y = -1.9334x + 127.53
  2. The lowest actual value for each category are as follows:
    • Permits: 117, in July 2012
    • Wells: 43, in February 2015
    • Violations: 16, in August 2014.
FracTracker Alliance

Offshore Oil and Gas Drilling: Risks to the Sea Otter

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By Emily Watson, FracTracker Summer Intern

Sea otters, an endangered keystone species, are at risk due to offshore oil and gas drilling spills. Along the west coast of the U.S., this marine mammal’s habitat is commonly near offshore drilling sites, specifically in California and Alaska.

Sea Otters – a Keystone Species

Sea otter numbers used to range from several hundred thousand to more than a million. Today, there are estimated to be just over 106,000 in existence worldwide, with fewer than 3,000 living in California. Their habitats range from Canada, Russia, Japan, California and Washington, but the majority of all wild sea otters are found in Alaskan waters.

Sea otters play a significant role in their local environments, and a much greater ecosystem role than any other species in their habitat area. Sea otters are predators, critical to maintaining the balance of the near-shore kelp ecosystems, and are referred to as keystone species. Without this balancing act, coastal kelp forests in California would be devoured by other aquatic life.  Sea otter predation helps to ensure that the kelp community continues to provide cover and food for many of the marine animals. Additionally, kelp plays a tremendous role in capturing carbon in the coastal ecosystems. In that sense, sea otters also inadvertently help to reduce levels of atmospheric carbon dioxide.

Oil Spills and their Health Implications

Recently, Alaska and California, home to a wide variety of marine life, have been popular areas for offshore oil and gas drilling, which may include the use of fracking to extract hydrocarbons. Oil spills are a great concern for the sea otter; unlike other marine animals that may be able to eventually rid themselves of the oil, contact with the oil causes the sea otters fur to mat, preventing insulation, which can lead to hypothermia. Additionally, the ingestion of toxic oil chemicals while cleansing their fur can cause liver and kidney failure, as well as severe damage to their lungs and eyes.

Because their numbers are low and their geographic location area is rather small compared to other sea otter populations, the California sea otter is especially vulnerable, and could be devastated by oil contamination.

Prince William Sound, Alaska

Exxon Valdez cleanup. Photograph by Natalie Fobes, National Geographic

Exxon Valdez cleanup. Photograph by Natalie Fobes, National Geographic

On March 24, 1989, the tanker vessel Exxon Valdez ran aground on Bligh Reef in Prince William Sound, Alaska, spilling an estimated 42 million liters of Prudhoe Bay crude oil. This incident affected marine life throughout western Prince William Sound, the Gulf of Alaska, and lower Cook Inlet. An estimated 3500–5500 otters from a total population of about 30,000 may have died as a direct result of the oil spill. Oiling and ingestion of oil-contaminated shellfish may have affected reproduction and caused a variety of long-term sublethal effects. Necropsies of sea otter carcasses indicated that most deaths of sea otters were attributed to the oil, and pathologic and histologic changes were associated with oil exposure in the lung, liver, and kidney. Studies of long-term effects indicate that the sea otter population in the Prince William Sound area suffered from chronic effects of oil exposure at least through 1991. While some populations may recover after a spill, it would seem that the threat of oil pollution impacts is intensified for populations in deteriorating habitats and to those that are in decline.

Santa Barbara Coast, California

LA Santa Barbara Oil Spill Cleanup - Photo by: Brian van der Brug / Los Angeles Times

LA Santa Barbara Oil Spill Cleanup – Photo by: Brian van der Brug / Los Angeles Times

On Tuesday, May 19, 2015, a pipeline was found to be leaking into the Santa Barbara Coast in California. This broken pipeline, owned by Plains All American, spilled approximately 105,000 gallons of crude oil into the ocean, according to various news reports, stretching out into a 4-mile radius along the central California coastline.

These waters are home to an array of shore birds, seals, sea lions, otters and whales. Numerous amounts of marine life have been found washed up on the shore, including crabs, octopuses, fish, birds, and dolphins. Elephant seals, sea lions, and other marine wildlife have been taken to Seaworld in San Diego for treatment and recovery.

The Santa Barbara accident occurred on the same stretch of coastline as spill in 1969 that – at the time – was the largest ever incident in U.S. waters and contributed to the rise of the American environmental movement. Several hundred-thousand gallons spilled from a blowout on an oil platform, and thousands of seabirds were killed and numerous ocean wildlife, including sea lions, elephant seals, and fish perished.

Conclusion

Overall, the ocean is home to a great diversity of marine wildlife, all of which are vulnerable to oil contamination. Offshore gas drilling is a significant threat to the survival of sea otters and other marine life, wherein spills and accidents could cause health problems, toxicity, and even death. Oil spills are exceptionally problematic for sea otters, due to the vulnerable state of this animal and its endangered species state. Keeping keystone species healthy is instrumental to maintaining a well flourished ecosystem, while protecting habitats for a large array of marine and wildlife. The potential impacts on CA sea otters and other marine life due to events such as the 2015 oil spill in California should not be taken lightly.