Oklahoma and Kansas Class II Injection Wells and Earthquakes
By Ted Auch, Great Lakes Program Coordinator, FracTracker Alliance
In collaboration with Caleb Gallemore, Assistant Professor in International Affairs, Lafayette University
The September 3rd magnitude 5.8 earthquake in Pawnee, Oklahoma, is the most violent example of induced seismicity, or “man-made” earthquakes, in U.S. history, causing Oklahoma governor Mary Fallin to declare a state of emergency. This was followed by a magnitude 4.5 earthquake on November 1st prompting the Oklahoma Corporation Commission (OCC) and U.S. EPA to put restrictions on injection wells within a 10-mile radius of the Pawnee quake.
And then on Sunday, November 6th, a magnitude 5.0 earthquake shook central Oklahoma about a mile west of the Cushing Hub, the largest commercial crude oil storage center in North America capable of storing 54 million barrels of crude. This is the equivalent of 2.8 times the U.S. daily oil refinery capacity and 3.1 times the daily oil refinery capacity of all of North America. This massive hub in the North American oil landscape also happens to be the southern terminus of the controversial Keystone pipeline complex, which would transport 590,000 barrel per day over more than 2,000 miles (Fig. 1). Furthermore, this quake demonstrated the growing connectivity between Class II injection well associated induced seismicity and oil transport/storage in the heart of the US version of Saudi Arabia’s Ghawar Oil Fields. This increasing connectivity between O&G waste, production, and processing (i.e., Hydrocarbon Industrial Complex) will eventually impact the wallets of every American.
Figure 1. The Keystone Pipeline would transport 590,000 bpd over more than 2,000 miles.
This latest earthquake caused Cushing schools to close. Magellan Midstream Partners, the major pipeline and storage facility operator in the region, also shut down in order to “check the integrity of our assets.” Compounding concerns about induced seismicity, the Cushing Hub is the primary price settlement point for West Texas Intermediate that, along with Brent Crude, determines the global price of crude oil and by association what Americans pay for fuel at the pump, at their homes, and in their businesses.
Given the significant increase in seismic activity across the U.S. Great Plains, along with the potential environmental, public health, and economic risks at stake, we thought it was time to compile an inventory of Class II injection well volumes. Because growing evidence points to the relationship between induced seismicity and oil and gas waste disposal, our initial analysis focuses on Oklahoma and Kansas. The maps and the associated data downloads in this article represent the first time Class II injection well volumes have been compiled in a searchable and interactive fashion for any state outside Ohio (where FracTracker has compiled class II volumes since 2010). Oklahoma and Kansas Class II injection well data are available to the public, albeit in disparate formats and diffuse locations. Our synthesis makes this data easier to navigate for concerned citizens, policy makers, and journalists.
Induced Seismicity Past, Present, and Future
Figure 2. Central U.S. earthquakes 1973-August 15, 2015 according to the U.S. Geological Survey (Note: Based on our analysis this exponential increasing earthquakes has been accompanied by a 300 feet per quarter increase in the average depth of earthquakes across Oklahoma, Kansas, and Texas).
Oklahoma, along with Arkansas, Kansas, Ohio, and Texas, is at the top of the induced seismicity list, specifically with regard to quakes in excess of magnitude 4.0. However, as the USGS and Virginia Tech Seismological Observatory (VTSO)[1] have recently documented, an average of only 21 earthquakes of magnitude 3.0 or greater occurred in the Central/Eastern US between 1973 and 2008. This trend jumped to an average of 99 between 2009 and 2013. In 2014 there were a staggering 659 quakes. The exponential increase in induced seismic events can be seen in Figure 2 from a recent USGS publication titled “High-rate injection is associated with the increase in U.S. mid-continent seismicity,” where the authors note:
“An unprecedented increase in earthquakes in the U.S. mid-continent began in 2009. Many of these earthquakes have been documented as induced by wastewater injection…We find that the entire increase in earthquake rate is associated with fluid injection wells. High-rate injection wells (>300,000 barrels per month) are much more likely to be associated with earthquakes than lower-rate wells.”
Figure 3. Average freshwater demand per hydraulically fractured well across four U.S. shale plays and the annual percent increase in each of those plays.
This trend suggests that induced seismicity is the new normal and will likely increase given that: 1) freshwater demand per hydraulically fractured well is rising all over the country, from 11-15% per year in the Marcellus and Bakken to 20-22% in the Denver and Midland formations, 2) the amount of produced brine wastewater parallels these increases almost 1-to-1, and 3) the unconventional oil and gas industry is using more and more water as they begin to explore the periphery of primary shale plays or in less productive secondary and tertiary plays (Fig. 3).
Oklahoma
The September, 2016, Pawnee County Earthquake
This first map focuses on the September, 2016 Pawnee, OK Magnitude 5.8 earthquake that many people believe was caused by injecting high volume hydraulic fracturing (HVHF) waste into class II injection wells in Oklahoma and Kansas. This map includes all Oklahoma and Kansas Class II injection wells as well as Oklahoma’s primary geologic faults and fractures.
Oklahoma and Kansas Class II injection wells and geologic faults
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Figure 4. The September, 2016 Pawnee, Oklahoma 5.8M earthquake, neighboring active Class II injection wells, underlying geologic faults and fractures.
Of note on this map is the geological connectivity across Oklahoma resulting from the state’s 129 faults and fractures. Also present are several high volume wells including Territory Resources LLC’s Oldham #5 (1.45 miles from the epicenter, injecting 257 million gallons between 2011 and 2014) and Doyle #5 wells (0.36 miles from the epicenter, injecting 61 million gallons between 2011 and 2015), Staghorn Energy LLC’s Hudgins #1 well (1.43 miles from the epicenter, injecting 11 million gallons between 2011 and 2015 into the Red Fork formation), and Cooke Co Production Co.’s Laird #3-35 well (1.41 miles from the epicenter, injecting 6.5 million gallons between 2011 and 2015). Figure 4 shows a closeup view of these wells relative to the location of the Pawnee quake.
Class II Salt Water Disposal (SWD) Injection Well Volumes
This second map includes annual volumes of disposed wastewater across 10,297 Class II injection wells in Oklahoma between 2011 and 2015 (Note: 2015 volumes also include monthly totals). Additionally, we have included Oklahoma’s geologic faults and fractures for context given the recent uptick in Oklahoma and Kansas’ induced seismicity activity.
Annual volumes of class II injection wells disposal in Oklahoma (2011-2015)
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Oklahoma statistics for 2011 to 2015 (Table 1):
- Maximum volume to date (for a single Class II injection well): 105,979,598 barrels, or 4,080,214,523 gallons (68,003,574 gallons per month), for the New Dominion, LLC “Chambers #1” well in Oklahoma County.
- Total Volume to Date: 10,655,395,179 barrels or 410,232,714,392 gallons (6,837,211,907 gallons per month).
- Mean volume to date across the 10,927 Class II injection wells: approximately 975,144 barrels per well or 37,543,044 gallons (625,717 gallons per month).
- This map also includes 632 Class II wells injecting waste into the Arbuckle Formation which is believed to be the primary geological formation responsible for the 5.0 magnitude last week in Cushing.
Kansas
Below is an inventory of monthly oil and gas waste volumes (barrels) disposed across 4,555 Class II injection wells in Kansas between 2011 and 2015. This map will be updated in the Spring of 2017 to include 2016 volumes. A preponderance of this data comes from 2015 with a scattering of volume reports across Kansas between 2011 and 2014.
Monthly Class II injection wells volumes in Kansas (2011-2015)
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Kansas statistics for 2015 (Table 1):
- Maximum volume to date (for a single Class II injection well): 9,016,471 barrels, or 347,134,134 gallons (28,927,845 gallons per month), for the Sinclair Prairie Oil Co. “H.J. Vohs #8” well in Rooks County. This is a well that was initially permitted and completed between 1949 and 1950.
- Total Volume to date: 1,060,123,330 barrels or 40,814,748,205 gallons (3,401,229,017 gallons per month).
- Mean volume to date across the 4,555 Class II injection wells: approximately 232,738 barrels per well or 8,960,413 gallons (746,701 gallons per month).
Table 1. Summary of Class II SWD Injection Well Volumes across Kansas and Oklahoma
|
|
Sum | Average | Maximum | |||
| No. of Class II SWD Wells |
Barrels | Sum To Date | Per Year | Sum To Date | Per Year | |
| Kansas* | 4,555 | 1.06 BB | 232,738 | … | 9.02 MB | … |
| Oklahoma** | 10,927 | 10.66 BB | 975,143 | 195,029 | 105.98 MB | 21.20 MB |
* Wells in the counties of Barton (279 wells), Ellis (397 wells), Rooks (220 wells), Russell (199 wells), and Ness (187 wells) account for 29% of Kansas’ active Class II wells.
** Wells in the counties of Carter (1,792 wells), Creek (946 wells), Pontotoc (684 wells), Seminole (476 wells), and Stephens (1,302 wells) account for 48% of Oklahoma’s active Class II wells.
Conclusion
If the U.S. EPA’s Underground Injection Control (UIC) estimates are to be believed, the above Class II volumes account for 19.3% of the “over 2 billion gallons of brine…injected in the United States every day,” and if the connectivity between injection well associated induced seismicity and oil transport/storage continues to grow, this issue will likely impact the lives of every American.
Given how critical the Cushing Hub is to US energy security and price stability one could easily argue that a major accident there could result in a sudden disruption to fuel supplies and an exponential increase in “prices at the pump” that would make the 240% late 1970s Energy Crisis spike look like a mere blip on the radar. The days of $4.15 per gallon prices the country experienced in the summer of 2008 would again become a reality.
In sum, the risks posed by Class II injection wells and are not just a problem for insurance companies and residents of rural Oklahomans and Kansans, induced seismic activity is a potential threat to our nation’s security and economy.
Downloads
FracTracker Induced Seismicity Infographic (print quality)
Oklahoma Class II SWD Injection Well Annual Volumes 2011 to 2015 (Barrels)
Kansas Class II SWD Injection Well Monthly Volumes 2011 to 2015 (Barrels)
Footnotes
[1] To learn more about Induced Seismicity read an exclusive FracTracker two-part series from former VTSO researcher Ariel Conn: Part I and Part II. Additionally, the USGS has created an Induced Earthquakes landing page as part of their Earthquake Hazards Program.
The Dakota Access Pipeline: An Uncertain Future
By Kyle Ferrar, Western Program Coordinator, FracTracker Alliance
Eliza Czolowski, Program Associate, PSE Healthy Energy
Since April 2016, demonstrators in North Dakota have been protesting a section of the Dakota Access Pipeline (DAPL) being built by Dakota Access LLC, a construction subsidiary of Energy Transfer Partners LP. The proposed pipeline passes just 1.5 miles north of the Standing Rock Sioux Tribal Lands, where it is planned to cross Lake Oahe, the largest Army Corps of Engineers reservoir created on the Missouri River. The tribe argues that the project will not only threaten their environmental and economic well-being, but will also cut through land that is sacred.
Given how quickly circumstances have changed on the ground, we have received numerous requests to post an overview on the issue. This article examines the technical aspects of the DAPL proposal and details the current status of protests at Standing Rock. It includes a discussion of what the Army Corps’ recent denial of DAPL’s permits means for the project as well as looks towards the impacts of incoming Trump administration. We have also created the below map to contextualize DAPL and protest activities that have occurred at Standing Rock.
Standing Rock Protest Map
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Background
DAPL is a $3.78 billion dollar project that was initially slated for completion on January 1, 2017. The DAPL is a joint venture of Phillips 66, Sunoco Logistics, and other smaller fossil fuel companies including Marathon Petroleum Corporation, and Enbridge Energy Partners. Numerous banks and investment firms are supporting the project and financing the related infrastructure growth, including Citi Bank, JP Morgan Chase, HSBC, PNC, Community Trust, Bank of America, Morgan Stanley, ING, Tokyo-Mitsubishi, Goldman Sachs, Wells Fargo, SunTrust, Us Bank, UBS, Compass and others.
Its route travels from Northwestern North Dakota, south of Bismarck, and crosses the waterway made up of the Missouri River and Lake Oahe just upriver of the Standing Rock Sioux Tribal Area. From North Dakota the pipeline continues 1,172 miles to an oil tank farm in Pakota, Illinois. DAPL would carry 470,000 barrels per day (75,000 m3/d) of Bakken crude oil with a maximum capacity up to 570,000 barrels per day. That’s the CO2 equivalent of 30 average sized coal fired power plants.
As documented by the NY Times map, in addition to the Missouri River and Lake Oahe, the pipeline crosses 22 other waterways that also require the pipeline to be drilled deep under these bodies of water. But Standing Rock portion is the only section disputed and as of yet unfinished. Now the pipeline project, known by the protesters as “the black snake,” is over 95% complete, despite having no official easement to cross the body of water created by the Missouri River and Lake Oahe. The easement is required for any domestic pipeline to cross a major waterway and because the land on either side of the Army Corps Lake Oahe project is managed by the Army Corps (shown in the protest map). An easement would allow Dakota Access LLC to drill a tunnel for the pipeline under the federally owned lands, including the lake and river.
Safety & Environmental Racism
Proponents of the project tout the opinion that pipelines are the safest method of moving oil large distances. Trucking oil in tankers on highways has the highest accident and spill rates, whereas moving oil by railways presents a major explosive hazard when incidents do occur. Pipeline spills are therefore considered the “safe” alternative. On November 11, Kelcy Warren was interviewed on CBS News, claiming Dakota Access, LLC takes every precaution to reduce leaks and that the likelihood of a leak is highly unlikely. The problem with comparing the risk for each of these transportation methods is that rates of incidence are the only comparison. The resulting hazard and impact is ignored. When pipelines rupture, they present a much larger hazard than trucks and trains. Large volumes of spilled oil result in much greater water and soil contamination.
We know that pipelines do rupture, and quite often. An analysis by the U.S. DOT Pipeline and Hazardous Materials Safety Administration in 2012 shows that there have been 201 major incidents (with volumes over 1,000 gallons) related to liquid leaks in the U.S. over the last ten years that were reported to the Department of Transportation. The “average” pipeline therefore has a 57% probability of experiencing a major leak, with consequences over the $1 million range, in a ten-year period. FracTracker’s recent analysis of PHMSA data shows the systemic issue of pipeline spills: there have been 4,215 pipeline spill incidents just since 2010 resulting in 100 reported fatalities, 470 injuries, and property damage exceeding $3.4 billion! The recent (December 12) spill of 176,000 gallons of crude oil into a stream just 150 miles from the Standing Rock protest site highlights the Tribes’ concerns.
A previously proposed route for the DAPL would have put Bismarck—a city that is 92% white—just downriver of its Missouri River crossing. This initial route was rejected due to its potential threat to Bismarck’s water supply, according to the Army Corps. In addition to being located upriver of Bismarck’s water intake, the route would have been 11 miles longer and would have passed through “wellhead source water protection” areas that are avoided to protect municipal water supply wells. Passing through this “high consequence area” would have required further actions and additional safety measures on the part of Dakota Access LLC. The route would also have been more difficult to stay at least 500 feet away from homes, as required by the North Dakota Public Service Commission. The route was changed and pushed as close to Sioux County as possible, the location of the Standing Rock Indian Reservation.
Protests: The Water Protectors
The Standing Rock Sioux Tribe has taken an active stance against Bakken Oil Development in the past. In 2007, the Reservation passed a resolution to prevent any oil and gas development or pipelines on the Tribal Lands. However, deep concerns about the safety of DAPL led protesters to begin demonstrations at Standing Rock in April, 2016. The Standing Rock Sioux Tribe then sued the Army Corps in July, after the pipeline was granted most of the final permits over objections of three other federal agencies. Construction of it, they say, will “destroy our burial sites, prayer sites and culturally significant artifacts.” A timeline of The Standing Rock Sioux Tribe’s litigation addressing DAPL through this period can be found on the EARTHJUSTICE website.
Photo by Derrick Broze/cc
In August, a group organized on the Standing Rock Indian Reservation called ReZpect Our Water brought a petition to the Army Corps in Washington, D.C. stating that DAPL interferes with their ancestral land and water rights. The Tribe sued for an injunction citing the endangerment of water and soil, cultural resources, and the improper use of eminent domain. The suit argued that the pipeline presents a risk to Sioux Tribe communities who live near or downstream of the pipeline. The Missouri River is the main water source for the Standing Rock Sioux Tribe. In September, members of the Standing Rock Sioux tribe in North Dakota finally made headlines.
Federal Injunction
On September 9, District Judge James Boasberg denied the Standing Rock Sioux Tribes preliminary injunction request to prevent the Army Corps from granting the easement. The Judge ordered Dakota Access to stop work only on the section of pipeline nearest the Missouri river until the Army Corps granted the crossing easement. The excavation of Standing Rock burial grounds and other sacred sites, where direct action demonstrators were clashing with Dakota Access security and guard dogs, was allowed to continue. Later that same day, a joint statement was released by the U.S. Department of Justice, the Department of the Interior, and the U.S. Army:
“We request that the pipeline company voluntarily pause all construction activity within 20 miles east or west of Lake Oahe.”
In the map above the 20-mile buffer zone is shown in light green. Regardless of the request from the three federal agencies to pause construction, Dakota Access’s parent company Energy Transfer Partners LP ignored requests to voluntarily halt construction. Dakota Access LLC has also disregarded the instructions of the federal judge. The Army Corps declared Dakota Access LLC would not receive the easement required to cross the waterway until after 2016, but that has not stopped the company from pushing forward without the necessary permits. The pipeline has been built across all of Cannonball Ranch right up to Lake Oahe and the Missouri River, which can be seen in the map above and in drone footage taken November 2, 2016 showing the well pad for the drill rig has been built.
On November 4 the Army Corps requested Dakota Access LLC voluntarily halt construction for 30 days; then on November 8 (Election Day), Dakota Access ignored the request and announced they would begin horizontally drilling under the waterway within weeks. On November 14 Dakota Access filed a lawsuit against the Army Corps arguing that permits are not legally required. Later that day, the Army Corps responded with a statement that said any construction on or under Corps land bordering Lake Oahe cannot occur because the Army has not made a final decision on whether to grant an easement. In the issued statement, Assistant Secretary of the Army Jo-Ellen Darcy said “in light of the history of the Great Sioux Nation’s dispossession of lands [and] the importance of Lake Oahe to the Tribe,” the Standing Rock Sioux tribe would be consulted to help develop a timetable for future construction plans. The Army Corps has since denied the easement entirely.
Violence Against Protesters
Law enforcement has used physical violence to disrupt demonstrations on public lands and to prevent direct action activities as protesters aim to shut down construction on private land held by Energy Transfer Partners LP. Since September 4, law enforcement agencies led by the Morton County Sheriff’s Department have maintained jurisdiction over the protests. Officers from other counties and states have also been brought in to assist. Morton County and the State of North Dakota do not have the jurisdiction to evict protesters from the camps located on Army Corps land. Well over 500 activists have been arrested.
The majority of clashes with law enforcement have occurred on the roadways exiting the Army Corps lands, or at the access points to the privately owned Cannonball Ranch (shown on the map). Morton County has spent more than $8 million keeping direct action protesters from shutting down excavation and construction activities along the path of the pipeline. Meanwhile, the state of North Dakota has spent over $10 million on additional law enforcement officials to provide assistance to Morton County.
DAPL protests from video by UnicornRiot/cc
The first violent confrontation occurred on September 3 after Dakota Access bulldozed an area of Cannonball Ranch identified by the Tribe as a sacred site hosting burial grounds. At that time, the site was actively being contested in court and rulings still had not been made. The Tribe was seeking a restraining order, known as a “preliminary injunction” to protect their cultural heritage. Direct action demonstrators put themselves in the way of bulldozers to stop the destructive construction. In response, Dakota Access LLC security personnel assaulted protesters with pepper spray and attack dogs. The encounter was documented by Democracy Now reporter Amy Goodman.
October 27, the Morton County Sheriff’s Department reinforced with 300 police from neighboring counties and states, raided the frontline camp site making mass arrests. In response, demonstrators reinforced a blockade of the 1806 bridge, shown in the map above. The most violent clash was witnessed on public lands on November 20, 2016 at this bridge, which demarcates Army Corps land. The Police forces’ use of “non-lethal” bean bag rounds, rubber bullets, tear gas, pepper spray, water hoses, LRAD, and explosive flash grenades on peaceful demonstrators has been criticized by many groups. Fire hoses were used on protesters in freezing conditions resulting in dozens of demonstrators needing treatment for hypothermia. In total 300 people were injured according to a release from the standing rock medic and healer council.
Most recently, the Army Corps has targeted the Standing Rock Demonstration by determining that it is no longer safe to stay at the Sacred Stone and Oceti Sakowin camps located on Army Corps property. North Dakota Governor Jack Dalrymple has frequently blasted the Army Corps for not removing the protesters.
As of December 5th, federal authorities consider the protesters to be trespassing on federal lands, leaving protesters vulnerable to various citations and possible arrest. The Army Corps has also said that emergency services may no longer be provided in the evacuation area. The Army Corps has jurisdiction on Army Corps lands, and only federal authorities can remove the protesters from federal lands. There are now more than 5,000 activists demonstrating at Standing Rock, and an additional 2,000 U.S. veterans joined the protest this past week for an action of solidarity. Nevertheless, U.S. authorities have said that there are no plans to forcibly remove activists, despite telling them to leave.
Victory and an Uncertain Future
Perhaps as a result of this mass outcry, the Army Corps announced on December 4th—only a day before trespassing claims would be imposed—that Dakota Access LLC’s permit application to cross under the Missouri River and Lake Oahe had been denied. Jo-Ellen Darcy, the Army’s Assistant Secretary for Civil Works, announced:
“Although we have had continuing discussion and exchanges of new information with the Standing Rock Sioux and Dakota Access, it’s clear that there’s more work to do…The best way to complete that work responsibly and expeditiously is to explore alternate routes for the pipeline crossing.”
To determine alternate routes, the Army Corps has announced it will undertake an environmental impact statement which could take years to complete. While this is a major victory for the “water protectors” demonstrating at Standing Rock, it is not a complete victory. Following the Army Corps’ announcement, the two main pipeline investors, Energy Transfer Partners LP and Sunoco Logistics, responded that they:
“…are fully committed to ensuring that this vital project is brought to completion and fully expect to complete construction of the pipeline without any additional rerouting in and around Lake Oahe. Nothing this Administration has done today changes that in any way.”
In fact, prior to the Army Corps denying the easement, numerous democrats in congress called for President Obama to shut down the pipeline. While President Obama has not heeded these calls to shut down the project entirely, he also has not given the green light for the project either. Instead the President stated that the situation needed to be handled carefully and urged the Army Corps to consider rerouting the pipeline. “We’re monitoring this closely and I think, as a general rule, my view is that there’s a way for us to accommodate sacred lands of Native Americans…. I think right now the Army Corps is examining whether there are ways to reroute this pipeline,” the President said.
The Corps decision to conduct a lengthy environmental impact statement is encouraging but, ultimately, the Trump administration may have the final say on the DAPL easement. President-elect Trump has voiced support for the easement in the past, and on December 5th, just one day following the Army Corps’ decision, Trump spokesman Jason Miller commented:
“That’s something we support construction of, and we will review the full situation in the White House and make an appropriate determination at that time.”
Energy Transfer Partners LP CEO Kelcy Warren donated $103,000 to the Trump campaign and the President-elect has investments in Energy Transfer Partners LP totaling up to $1 million according to campaign financial disclosures. President-elect Trump has made it clear that pipeline projects, specifically the Keystone Access Pipeline rejected by President Obama, will be allowed to move forward along with additional fossil fuel extraction projects.
If the construction company, Dakota Access LLC, continues building the pipeline they are liable to be fined. It is not yet clear whether Dakota Access LLC will “eat” the fine to continue building and drilling, or whether the Army Corps will forcefully stop DAPL. Analysts say the expense of changing the route, such as to the south of the tribal lands, would make the economics of the pipeline a total loss. It is cheaper for Dakota Access LLC to continue to fight the protest despite overwhelming disapproval of the project.
Meanwhile, protestors have refused to leave Standing Rock in fear that the Army Corp will reverse its decision and allow DAPL to proceed, despite requests by the chairman of the Sioux Tribe that demonstrators go home. Many are hopeful that, by stalling the project past January 1st—the deadline by which Energy Transfer Partners LP promised oil companies it would complete construction—the possibility exists that contracts will expire and DAPL loses support from investors.
Other Mapping Resources
This web map shows the current construction progress of the pipeline.
The New York Times website is hosting a map focusing on the many water crossings of the pipeline route.
The Guardian has a static map on their website similar to our interactive map.
Header photograph by Joe Brusky/flickr/cc
Mariner East 2: At-Risk Schools and Populations
by Kirk Jalbert, Manager of Community-Based Research & Engagement
with technical assistance from Seth Kovnant
In September, the Pennsylvania Department of Environmental Protection (DEP) rejected a number of permits for wetland crossings and sedimentation control that were required for Sunoco Pipeline’s proposed “Mariner East 2” pipeline. According to Sunoco, the proposed Mariner East 2 is a $2.5 billion, 350-mile-long pipeline that would be one of the largest pipeline construction projects in Pennsylvania’s history.
If built, Mariner East 2 could transport up to 450,000 barrels (18,900,000 gallons) per day of propane, ethane, butane, and other liquefied hydrocarbons from the shale fields of western Pennsylvania to export terminals in Marcus Hook, located just outside Philadelphia. A second proposed pipeline, if constructed, could carry an additional 250,000 barrels (10,500,000 gallons) per day of these same materials. Sunoco submitted revised permit applications to PADEP on Tuesday, December 6th.
The industry often refers to ethane, propane and butane collectively as “natural gas liquids.” They are classified by the federal government as “hazardous, highly volatile liquids,” but that terminology is also misleading. These materials, which have not been transported through densely populated southeast Pennsylvania previously, are liquid only at very high pressure or extremely cold temperatures. At the normal atmospheric conditions experienced outside the pipeline, these materials volatilize into gas which is colorless; odorless; an asphyxiation hazard; heavier than air; and extremely flammable of explosive. This gas can travel downhill and downwind for long distances while remaining combustible. It can collect (and remain for long periods of time) in low-lying areas; and things as ordinary as a cell phone, a doorbell or a light switch are capable of providing an ignition source.
Many who have followed the proposed Mariner East 2 project note that, while much has been written about the likely environmental impacts, insufficient investigation has been conducted into safety risks to those who live, work and attend schools in the proposed pipeline’s path. We address these risks in this article, and, in doing so, emphasize the importance of regulatory agencies allowing public comments on the project’s resubmitted permit applications.
The Inherent Risks of Artificially Liquified Gas
Resident of Pennsylvania do not need to look far for examples of how pipeline accidents pose serious risk. For instance, the 2015 explosion of the Enterprise ATEX (Appalachia to Texas) pipeline near Follansbee, WV, provides a depiction of what a Mariner East 2 pipeline failure could look like. This 20-inch diameter pipeline carrying liquid ethane is similar in many ways to the proposed Mariner East 2. When it ruptured in rural West Virginia, close to the Pennsylvania border, it caused damage in an area that extended 2,000 feet—about ½ square mile—from the place where the pipeline failed.
In another recent instance, the Spectra Energy Texas Eastern methane natural gas pipeline ruptured in Salem, PA, this April as a result of corroded welding. The explosion, seen above (photo by PA NPR State Impact), completely destroyed a house 200ft. away. Another house, 800ft. away, sustained major damage and its owner received 3rd degree burns. These incidents are not unique. FracTracker’s recent analysis found that there have been 4,215 pipeline incidents nation-wide since 2010, resulting in 100 reported fatalities, 470 injuries, and property damage exceeding $3.4 billion (“incident” is an industry term meaning “a pipeline failure or inadvertent release of its contents.” It does not necessarily connote “a minor event”).
Calculating Immediate Ignition Impact Zones
It is difficult to predict the blast radius for materials like ethane, propane and butane. Methane, while highly flammable or explosive, is lighter than air and so tends to disperse upon release into the atmosphere. Highly volatile liquids like ethane, propane and butane, on the other hand, tend to concentrate close to the ground and to spread laterally downwind. A large, dispersed vapor cloud of these materials may quickly spread great distances, even under very light wind conditions. A worst-case scenario would by highly variable since gas migration and dispersion is dependent on topography, leak characteristics, and atmospheric conditions. In this scenario, unignited gas would be allowed to migrate as an unignited vapor cloud for a couple miles before finding an ignition source that causes an explosion that encompasses the entire covered area tracing back to the leak source. Ordinary devices like light switches or cell phones can serve as an ignition source for the entire vapor cloud. One subject matter expert recently testified before a Municipal Zoning Hearing board that damage could be expected at a distance of three miles from the source of a large scale release.
The federal government’s “potential impact radius” (PIR) formula, used for natural gas (methane) isn’t directly applicable because of differences in the characteristics of the material. It may however be possible to quantify an Immediate Ignition Impact Zone. This represents the explosion radius that could occur if ignition occurs BEFORE the gas is able to migrate.
The Pipeline and Hazardous Materials Safety Administration (PHMSA) provides instructions for calculating the PIR of a methane natural gas pipeline. The PIR estimates the range within which a potential failure could have significant impact on people or property. The PIR is established using the combustion energy and pipeline-specific fuel mass of methane to determine a blast radius: PIR = 0.69*sqrt(p*d^2). Where: PIR = Potential Impact Radius (in feet), p = maximum allowable operating pressure (in pounds per square inch), d = nominal pipeline diameter (in inches), and 0.69 is a constant applicable to natural gas
The Texas Eastern pipeline can use the PIR equation as-is since it carries methane natural gas. However, since Mariner East 2 is primarily carrying ethane, propane, and butane NGLs, the equation must be altered. Ethane, propane, butane, and methane have very similar combustion energies (about 50-55 MJ/kg). Therefore, the PIR equation can be updated for each NGL based on the mass density of the flow material as follows: PIR = 0.69*sqrt(r*p*d^2). Where: r = the density ratio of hydrocarbons with similar combustion energy to methane natural gas. At 1,440 psi, methane remains a gas with a mass density 5 times less than liquid ethane at the same pressure:
The methane density relationships for ethane, propane, and butane can be used to calculate an immediate-ignition blast radius for each hydrocarbon product. The below table shows the results assuming a Mariner East 2-sized 20-inch diameter pipe operating at Mariner East 2’s 1,440psi maximum operating pressure:
Using these assumptions, the blast radius can be derived as a function of pressure for each hydrocarbon for the same 20in. diameter pipe:
ME2 Immediate Ignition Blast Radius
Note the sharp increase in blast radius for each natural gas liquid product. The pressure at which this sharp increase occurs corresponds with the critical pressure where each product transitions to a liquid state and becomes significantly denser, and in turn, contains more explosive power. These products will always be operated above their respective critical pressures when in transport, meaning their blast radius will be relatively constant, regardless of operating pressure.
Averaging the “Immediate Ignition Blast Radius” for ethane, propane, and butane gives us a 1,300 ft (about 0.25 mile) potential impact radius. However, we must recognize that this buffer represents a best case scenario in the event of a major pipeline accident.
Additional information on these calculations can be found in the Delaware County-based Middletown Coalition for Community Safety’s written testimony to the Pennsylvania Legistlature.
Living near the Mariner East 2
FracTracker has created a new map of the Mariner East 2 pipeline using a highly-detailed GIS shapefile recently supplied by the DEP. On this map, we identify a 0.5 mile radius “buffer” from Mariner East 2’s proposed route. We then located all public and private schools, environmental justice census tracts, and estimated number of people who live within this buffer in order to get a clearer picture of the pipeline’s hidden risks.
Proposed Mariner East 2 and At-Risk Schools and Populations
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Populations at Risk
In order to estimate the number of people who live within this 0.5 mile radius, we first identified census blocks that intersect the hazardous buffer. Second, we calculated the percentage of that census block’s area that lies within the buffer. Finally, we used the ratio to determine the percentage of the block’s population that lies within the buffer. In total, there are an estimated 105,419 people living within the proposed Mariner East 2’s 0.5 mile radius impact zone. The totals for each of the 17 counties in Mariner East 2’s trajectory can be found in the interactive map. The top five counties with the greatest number of at-risk residents are:
- Chester County (31,632 residents in zone)
- Delaware County (17,791 residents in zone)
- Westmoreland County (11,183 residents in zone)
- Cumberland County (10,498 residents in zone)
- Berks County (7,644 residents in zone)
Environmental Justice Areas
Environmental justice designations are defined by the DEP as any census tract where 20% or more of the population lives in poverty and/or 30% or more of the population identifies as a minority. These numbers are based on data from the U.S. Census Bureau, last updated in 2010, and by the federal poverty guidelines. Mariner East 2 crosses through four environmental justice areas:
- Census Tract 4064.02, Delaware County
- Census Tract 125, Cambria County
- Census Tract 8026, Westmoreland County
- Census Tract 8028, Westmoreland County
DEP policies promise enhanced public participation opportunities in environmental justice communities during permitting processes for large development projects. No additional public participation opportunities were provided to these communities. Furthermore, no public hearings were held whatsoever in Cambria County and Delaware County. The hearing held in Westmoreland County took place in Youngwood, nine miles away from Jeanette. Pipelines are not specified on the “trigger list” that determines what permits receive additional scrutiny, however the policy does allow for “opt-in permits” if the DEP believes they warrant special consideration. One would assume that a proposed pipeline project with the potential to affect the safety of tens of thousands of Pennsylvanians qualifies for additional attention.
At-Risk Schools
One of the most concerning aspects of our findings is the astounding number of schools in the path of Mariner East 2. Based on data obtained from the U.S. Department of Education on the locations of schools in Pennsylvania, a shocking 23 public (common core) schools and 17 private schools were found within Mariner East 2’s 0.5 mile impact zone. In one instance, a school was discovered to be only 7 feet away from the pipeline’s intended path. Students and staff at these schools have virtually no chance to exercise their only possible response to a large scale release of highly volatile liquids, which is immediate on-foot evacuation.
Middletown High School in Dauphin County in close proximity to ME2
One reason for the high number of at-risk schools is that Mariner East 2 is proposed to roughly follow the same right of way as an older pipeline built in the 1930s (now marketed by Sunoco as “Mariner East 1.”). A great deal of development has occurred since that time, including many new neighborhoods, businesses and public buildings. It is worth noting that the U.S. Department of Education’s data represents the center point of schools. In many cases, we found playgrounds and other school facilities were much closer to Mariner East 2, as can be seen in the above photograph. Also of note is the high percentage of students who qualify for free or reduced lunch programs at these schools, suggesting that many are located in disproportionately poorer communities.
Conclusion
Now that PADEP has received revised permit applications from Sunoco, presumably addressing September’s long list of technical deficiencies, the agency will soon make a decision as to whether or not additional public participation is required before approving the project. Given the findings in our analysis, it should be clear that the public must have an extended opportunity to review and comment on the proposed Mariner East 2. In fact, public participation was extremely helpful to DEP in the initial review process, providing technical and contextual information.
It is, furthermore, imperative that investigations into the potential impacts of Mariner East 2 extend to assess the safety of nearby residents and students, particularly in marginalized communities. Thus far, no indication has been made by the DEP that this will be the case. However, the Pennsylvania Sierra Club has established a petition for residents to voice their desire for a public comment period and additional hearings.
Seth Kovnat is the chief structural engineer for an aerospace engineering firm in Southeastern PA, and regularly consults with regard to the proposed Mariner East 2 pipeline. In November, Seth’s expertise in structural engineering and his extensive knowledge of piping and hazardous materials under pressure were instrumental in providing testimony at a Pennsylvania Senate and House Veterans Affairs and Emergency Preparedness Committee discussion during the Pennsylvania Pipeline Infrastructure Citizens Panel. Seth serves on the board of Middletown Coalition for Community Safety and is a member of the Mariner East 2 Safety Advisory Committee for Middletown Township, PA. He is committed to demonstrating diligence in gathering, truth sourcing, and evaluating technical information in pipeline safety matters in order to provide data driven information-sharing on a community level.
NOTE: This article was modified on 12/9/16 at 4pm to provide additional clarification on how the 1,300ft PIR was calculated, and the map was modified on 11/4/2021 to add the 1,300 ft Thermal Impact Zone Buffer, which was previously mislabeled as the half-mile Buffer
The Sabal Trail Pipeline: A Sinking Feeling
Construction is underway for a $3.2 billion, 515-mile-long interstate gas pipeline, running from central Alabama, through southwestern Georgia, and deep into Central Florida. The Sabal Trail Pipeline is a project of Duke Energy, NextEra Energy, and Spectra Energy. Spectra is the fossil fuel corporation responsible for other controversial pipelines also under construction – notably the Algonquin Incremental Market (AIM) Project. AIM, the target of ongoing protests in the Hudson Valley (NY) and elsewhere, would run from central New Jersey to ports in the Boston, MA area, passing within a few hundred feet of Indian Point Nuclear Power Plant on the Hudson River.
The Sabal Trail project is touted by Spectra to be crucial to aiding economic development along its route, and fueling gas-fired power generators in the Southeast United States. Environmentalists, however, view the project quite differently. Such development plans rarely come without a cost to communities, and to the environment.
A Unique Geology
Reflecting its geological origins as part of a shallow ancient ocean, the southeastern United States is underlain by porous limestone bedrock, known as karst. Water running through the karst bedrock flows not only through small pores, but often through extensive underground caves. When under under pressure, water can bubble up to the surface in a multitude of freshwater springs throughout the region. It’s not hard to imagine how contamination to the limestone aquifer in one area can spread rapidly and widely.
The karst bedrock, due to the sometimes large voids in its structure, is also prone to the formation of sinkholes, some of which are small; others are large enough to swallow whole buildings. Recognizing these risks, opponents of the Sabal Trail pipeline frequently cite the inherent danger of pipelines bending and rupturing should the ground beneath them give way, leading to potentially dangerous gas leakages or explosions.
One piece of recent research from the University of Georgia maps the prevalence of sinkholes in Doughterty County, GA, one of the many counties the Sabal Trail pipeline would pass through. For reference, FracTracker has added the path of the pipeline to the Dougherty County map, above.
In the interactive map below, we show the full proposed pipeline route and associated compressor stations. Karst geology, documented sinkholes, and springs near the route of the pipeline are also shown. The double-arrows in the upper right corner of the map will launch a full-screen view of the map, including a map legend. Use the “Layers” dropdown along the top bar of that map to turn on locations of nearby schools and hospitals that could be impacted by a nearby pipeline emergency. In addition, a “Bookmarks” dropdown menu along the same top bar that will allow zooming to locations along the pipeline mentioned in this article.
Map of the proposed Sabal Trail pipeline route, karst geology, and known sinkholes
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Growing Opposition
In October 2015, the United States Environmental Protection Agency (EPA) issued a scathing letter detailing the impacts that the proposed pipeline would have on the Floridan Aquifer, water quality, and ecology in this region of sensitive karst geology. Two months later, however, in mid-December, the EPA suddenly reversed its position. While reasons included an endorsement of industry’s choices to avoid “many of the most sensitive areas” that could be impacted, ABC News has suggested that political favoritism could have played a role, as well. This video, published on November 24, 2016 by ABC/FirstCoast News, describes that situation, and also includes excellent footage of construction impacts.
Currently, the construction is proceeding. Federal Energy Regulatory Commission (FERC) has granted eminent domain to industry to build the project through seized private property. Although all federal permits for the pipeline construction are in place, a joint lawsuit filed by the Sierra Club, the Gulf Restoration Network, and Flint Riverkeeper has challenged that permitting process. There is opposition to the pipeline in Alabama, Georgia, and Florida–the three states in which construction is occurring.
The video clips below documents the noise associated with the pipeline’s construction, as well as views of the sinkhole terrain along its route.
Sabal Trail gas pipeline noise pollution at the Santa Fe River (Nov. 25, 2016).
Credit: Merrillee on Vimeo.
Sabal Trail gas transmission, at O’Brien (Hildreth) Compressor Station in Northern Florida.
Credit: Merrillee on Vimeo.
Water Protectors
As winter descends on the northern Plains, thousands of indigenous people representing hundreds of tribes, as well as non-Native allies, have gathered in camps near the Sioux Standing Rock Reservation to pray and protest the Dakota Access Pipeline (DAPL), which would drill an oil pipeline through sacred Native lands and under the Missouri River. Participants in this movement are united by the words “Water Is Life” (Mni Wiconi), in recognition of the threats that an oil spill would present to their homeland and the source of drinking water for the tribe. Hundreds of arrests of peaceful protesters have been made there in recent months, many resulting in serious injuries to the protesters as water cannons, rubber bullets, concussion grenades, and attack dogs have been used in efforts to intimidate the activists.
Coordination among First Nations groups against other fossil fuel infrastructure is happening elsewhere, too. For example, in September 2016, at least fifty US and Canadian aboriginal groups signed a treaty, saying they will work together to fight proposals that would bring crude oil from the Alberta tar sands via pipeline, tanker, and rail.
The protests against the Sabal Trail Project are similarly themed to those at Standing Rock, but have not resulted in violence towards protesters thus far. Along the Suwanee River in Florida, peaceful protesters have assembled at the Sacred Waters encampment and, on November 12, 2016, faced off with authorities in an effort to stop pipeline drilling under the Santa Fe River between Branford and Fort White, Florida. 14 people were arrested in that protest. Demonstrations at the site continue, with a dawn march and demonstration that began just after sunrise on November 26th. No arrests were made on that day. Another protest encampment, the Crystal Waters Camp, is also in place near Fort Drum, Florida, where observers noted hydrocarbon releases from the pipeline construction into Fort Drum Creek and destruction of wildlife by a pipeline crew. Still other protests about the potential environmental risks posed by the Sabal Trail have taken place recently in both Orlando and Live Oak, Florida.
Even in the phases of construction, environmentalists in Georgia discovered that the Sabal Trail pipeline had started leaking drilling mud from a pilot hole into the Withlacooche River in late October, and continued to ooze turbid mud for at least three weeks. Environmental advocates from the WWALS (the Withlacoochee, Alapaha, Little, and Upper Suwannee River) Watershed Coalition raised concerns that if a pilot hole could cause such a leakage, what could happen once full-scale directional drilling was occurring?
By Karen Edelstein, Eastern Program Coordinator
Updated Pipeline Incident Analysis
By Matt Kelso, Manager of Data & Technology
As massive new pipeline projects continue to generate news, the existing midstream infrastructure that’s hidden beneath our feet continues to be problematic on a daily basis. Since 2010, there have been 4,215 pipeline incidents resulting in 100 reported fatalities, 470 injuries, and property damage exceeding $3.4 billion.
Figure 1: Cumulative impacts pipeline incidents in the US. Data collected from PHMSA on November 4th, 2016. Operators are required to submit incident reports within 30 days.
In our previous analyses, pipeline incidents occurred at a rate of 1.6 per day nationwide, according to data from the Pipeline and Hazardous Materials Safety Administration (PHMSA). Rates exceeding 1.9 incidents per day in 2014 and 2015 have brought the average rate up to 1.7 incidents per day. Incidents have been a bit less frequent in 2016, coming in at a rate of 1.43 incidents per day, or 1.59 if we roll results back to October 4th in order to capture all incidents that are reported within the mandatory 30 day window.
Figure 2: Pipeline incidents per day for years between 2010 and 2016. Incidents after October 4, 2016 may not be included in these figures.
These figures are the aggregation of three reports, namely natural gas transmission and gathering pipelines (828 incidents since 2010), natural gas distribution (736 incidents), and hazardous liquids (2,651 incidents). Not all of the hazardous liquids are petroleum related, but the vast majority are. 1,321 of the releases involved crude oil, and an additional 896 involved other liquid petroleum products, accounting for 84% of hazardous liquid incidents. The number could be higher, depending on the specific substances involved in the 399 highly volatile liquid (HVL) related incidents. The HVL category includes propane, butane, liquefied petroleum gases, ethylene, and propylene, as well as other volatile liquids that become gaseous at ambient conditions.
What is causing all of these pipeline incidents?
Figure 3: Cause of pipeline incidents for all reports received from January 1, 2010 through November 4, 2016.
Nonprofits, academics, and concerned citizens looking for accurate pipeline data will find that it is restricted, with the argument that releasing accurate pipeline data constitutes a threat to national security. This makes little sense for several reasons. First, with over 2.4 million miles of pipelines, they are nearly omnipresent. Additionally, similar data access restrictions only apply to midstream infrastructure such as pipelines and compressor stations, whereas the locations for wells, refineries, and power plants are all publicly available, despite the presence of the same volatile hydrocarbons at these facilities. Additionally, pipelines are purposefully marked with surface placards to help prevent unintentionally impacting the infrastructure.
In fact, a quick look at the causes of pipeline incidents reveal that it it much more dangerous to not know where the pipelines are located. In the “Other Incident Cause” category (Figure 3) there are 152 incidents that were caused by unsuspecting motor vehicles. When this is combined with incidents resulting from excavation damage, we have 558 cases where “not knowing” about the pipeline’s location likely contributed to the failure. On the other hand, there are 14 incidents (only .003%) where the cause is identified as intentional. While even one case of tampering with pipeline infrastructure is unacceptable, PHMSA incident data indicate that obfuscated pipelines are 40 times more likely to cause a problem when compared to sabotage. Equipment failures and corrosion account for more than half of all incidents.
Where do these incidents occur?
PHMSA is not allowed to make accurate pipeline location data available for download, but such rules apparently do not apply to pipeline incidents. The following map shows the 4,215 pipeline releases since 2010, highlighting those that have resulted in injuries and fatalities.
Pipeline incidents in the US. Please zoom in to access specific incident data. To see the legend and other tools, Please click here.
Figure 4: Pipeline incidents by state for reports received 1/1/2010 through 11/4/2016.
While operators are required to submit the incident’s location as a part of their report to PHMSA, data entry errors are common in the dataset. The FracTracker Alliance has been able to identify and correct a few of the higher profile errors, such as the February 9, 2011 explosion in Allentown, PA, the report for which had mangled the latitude and longitude values so badly that the incident was rendered in Greenland. Other errors persist in the dataset, however. Since 2010, pipeline incidents have occurred in Washington, DC, Puerto Rico, and 49 states (the exception being Vermont). Ten states have at least 100 incidents apiece during the past six years (see Figure 4), and more than a quarter of all pipeline incidents in that time frame have occurred in Texas.
Which operators are responsible?
Figure 5: This table shows the ten operators with the most reported incidents, along with the length of their pipeline network.
Altogether, there are 521 pipeline operators with reported releases, although many of these are affiliated with one another in some fashion. For example, the top two results in Figure 5 are almost certainly both subsidiaries of Enterprise Products Partners, L.P.
The real outlier in Figure 5, in terms of incidents per 100 miles, is Kinder Morgan Liquid Terminals; LLC. However, this is one of ten or more companies that share the Kinder Morgan name when reporting pipeline inventories. When taken in aggregate, companies with the Kinder Morgan name accounted for 142 incidents over a reported 7,939 miles, for a rate of 1.8 incidents per 100 miles. It should be noted that this, along with all of the statistics in Figure 5, are entirely based on matching the operator name between the incident and inventory reports. Kinder Morgan’s webpage boasts of 84,000 miles of pipelines in the US — there are numerous possible explanations for the discrepancy in pipeline length, including additional Kinder Morgan subsidiaries, as well as whether gathering lines that aren’t considered to be mains are on both lists.
The operators responsible for the most deaths from pipeline incidents since 2010 include Pacific Gas & Electric (15), Washington Gas Light (9), and Consolidated Edison Co. of New York (8). Of course, the greatest variable in whether or not a pipeline explosion kills people or not is whether or not the incident happens in a populated location. In the course of this analysis, there were 230 explosions and 635 fires over 2,500 days, meaning that there is pipeline explosion somewhere in the United States every 11 days, on average, and a fire every fourth day. The fact that only 65 of the incidents resulted in fatalities indicates that we have been rather lucky with incidents in the midstream sector.
Interactive maps show nearness of oil and gas wells to communities in 5 states
As an American, you are part owner of 640 million acres of our nation’s shared public lands managed by the federal government. And chances are, you’ve enjoyed a few of these lands on family picnics, weekend hikes or summer camping trips. But did you know that some of your lands may also be leading to toxic air pollution and poor health for you or your neighbors, especially in 5 western states that have high oil and gas drilling activity?
A set of new interactive maps created by FracTracker, The Wilderness Society, and partner groups show the threatened populations who live within a half mile of federal oil and gas wells – people who may be breathing in toxic pollution on a regular basis.
Altogether, air pollution from oil and gas development on public lands threatens at least 73,900 people in the 5 western states we examined. The states, all of which are heavy oil and gas leasing areas, include Colorado, New Mexico, North Dakota, Utah and Wyoming.
Figure 1. Close up of threat map in Colorado
In each state, the data show populations living near heavy concentrations of wells. For example just northeast of Denver, Colorado, in the heavily populated Weld County, at least 11,000 people are threatened by oil and gas development on public lands (Figure 1).
Western cities, like Farmington, New Mexico; Gillette, Wyoming; and Grand Junction, Colorado are at highest risk of exposure from air pollution. In New Mexico, especially, concentrated oil and gas activity disproportionately affects the disadvantaged and minorities. Many wells can be found near population centers, neighborhoods and even schools.
Colorado: Wells concentrated on Western Slope, Front Range
Note: The threatened population in states are a conservative estimate. It is likely that the numbers affected by air pollution are higher.
In 2014, Colorado became the first state in the nation to try to curb methane pollution from oil and gas operations through comprehensive regulations that included inspections of oil and gas operations and an upgrade in oil and gas infrastructure technology. Colorado’s new regulations are already showing both environmental and financial benefits.
But nearly 16,000 people – the majority living in the northwestern and northeastern part of the state – are still threatened by pollution from oil and gas on public lands.
Many of the people whose health is endangered from pollution are concentrated in the fossil-fuel rich area of the Western Slope, near Grand Junction. In that area, three counties make up 65% of the total area in Colorado threatened by oil and gas development.
In Weld County, just northeast of Denver, more than 11,000 residents are threatened by air pollution from oil and gas production on federal lands. But what’s even more alarming is that five schools are within a half mile radius of wells, putting children at risk on a daily basis of breathing in toxins that are known to increase asthma attacks. Recent studies have shown children miss 500,000 days of school nationally each year due to smog related to oil and gas production.
State regulations in Colorado have helped improve air quality, reduce methane emissions and promote worker care and safety in the past two years, but federal regulations expected by the end of 2016 will have a broader impact by regulating pollution from all states.
New Mexico: Pollution seen from space threatens 50,000 people
With more than 30,000 wells covering 4.6 million acres, New Mexico is one of the top states for oil and gas wells on public lands. Emissions from oil and gas infrastructure in the Four Corners region are so great, they have formed a methane hot spot that has been extensively studied by NASA and is clearly visible from space.
Nearly 50,000 people in northwestern New Mexico – 40% of the population in San Juan County – live within a half mile of a well.
Dangerous emissions from those wells in San Juan County disproportionately affect minorities and disadvantaged populations, with about 20% Hispanic, almost 40% Native American, and over 20% living in poverty.
Another hot spot of oil and activity is in southeastern New Mexico stretching from the lands surrounding Roswell to the southern border with Texas. Wells in this region also cover the lands outside of Carlsbad Caverns National Park, potentially affecting the air quality and visibility for park visitors. Although less densely populated, another 4,000 people in two counties – with around 50% of the population Hispanic – are threatened by toxic air pollution.
Wyoming: Oil and gas emissions add to coal mining pollution
Pollution from oil and gas development in Wyoming, which has about as many wells as New Mexico, is focused in the Powder River Basin. This region in the northeast of the state provides 40% of the coal produced in the United States.
Oil and gas pollution threatens approximately 4,000 people in this region where scarred landscapes and polluted waterways are also prevalent from coal mining.
With the Obama administration’s current pause on federal coal leasing and a review of the federal coal program underway, stopping pollution from oil and gas on public lands in Wyoming would be a major step in achieving climate goals and preserving the health of local communities.
Utah: Air quality far below federal standards
Utah has almost 9,000 active wells on public lands. Oil and gas activity in Utah has created air quality below federal standards in one-third of Utah’s counties, heightening the risk of asthma and respiratory illnesses. Especially in the Uintah Basin in northeastern Utah – where the majority of oil and development occurs – a 2014 NOAA-led study found oil and gas activity can lead to high levels of ozone in the wintertime that exceed federal standards.
North Dakota: Dark skies threatened by oil and gas activity
The geology of western North Dakota includes the Bakken Formation, one of the largest deposits of oil and gas in the United States. As a result, high oil and gas production occurs on both private and public lands in the western part of the state.
Nearly 650 wells on public lands are clustered together here, directly impacting popular recreational lands like Theodore Roosevelt National Park.
The 70,000-plus-acre park – named after our president who first visited in 1883 and fell in love with the incredible western landscape – is completely surrounded by high oil and gas activity. Although drilling is not allowed in the park, nearby private and public lands are filled with active wells, producing pollution, traffic and noise that can be experienced from the park. Due to its remote location, the park is known for its incredible night sky, but oil and gas development increases air and light pollution, threatening visibility of the Milky Way and other astronomical wonders.
You own public lands, but they may be hurting you
Pollution from oil and gas wells on public lands is only a part of a larger problem. Toxic emissions from oil and gas development on both public and private lands threaten 12.4 million people living within a half mile of wells, according to an oil and gas threat map created by FracTracker for a project by Earthworks and the Clean Air Task Force.
Now that we can see how many thousands of people are threatened by harmful emissions from our public lands, it is more important than ever that we finalize strong federal regulations that will help curb the main pollutant of natural gas – methane – from being leaked, vented, and flared from oil and gas infrastructure on public lands.
Federal oil and gas wells in western states produce unseen pollution that threatens populations at least a half mile away. Photo: WildEarth Guardians, flickr.
We need to clean up our air now
With U.S. public lands accounting for 1/5 of the greenhouse gas footprint in the United States, we need better regulations to reduce polluting methane emissions from the 96,000 active oil and gas wells on public lands.
Right now, the Bureau of Land Management is finalizing federal regulations that are expected by the end of 2016. These regulations are expected to curb emissions from existing sources – wells already in production – that are a significant source of methane pollution on public lands. This is crucial, since by 2018, it is estimated that nearly 90% of methane emissions will come from sources that existed in 2011.
Federal regulations by the BLM should also help decrease the risk to communities living near oil and gas wells and helping cut methane emissions by 40 to 45% by 2025 to meet climate change reduction goals.
Final regulations from the Bureau of Land Management will also add to other regulations from the EPA and guidance from the Obama administration to modernize energy development on public lands for the benefit of the American people, landscapes and the climate. In the face of a changing climate, we need to continue to monitor fossil fuel development on public lands and continue to push the government towards better protections for land, air, wildlife and local communities.
Learn more through maps
Oil and Gas Pollution from Public Lands
By The Wilderness Society – The Wilderness Society is the leading conservation organization working to protect wilderness and inspire Americans to care for our wild places. Founded in 1935, and now with more than 700,000 members and supporters, The Wilderness Society has led the effort to permanently protect 109 million acres of wilderness and to ensure sound management of our shared national lands.
Documenting Oil and Gas Industry Damage in North Dakota
North Dakota is now in its third oil boom due to the drilling technologies of horizontal drilling and hydraulic fracturing that have made once-inaccessible oil accessible. The Bakken formation covers western North Dakota, eastern Montana, and parts of Manitoba and Saskatchewan. At the height of the boom in 2014, just under 12,000 wells were active across the west, extracting 1.1 million barrels (bbl) of oil per day and flaring at 32%. The boom has bumped North Dakota to the second largest oil and gas producing state, second only to Texas.
Dakota Resource Council (DRC) is a member-led, grassroots organization that has been working in extraction-impacted communities in North Dakota since 1978. DRC’s members work on oil and gas campaigns that aim to eliminate impacts to land, air, water, and livelihoods of the citizens of North Dakota. Campaign issues on oil and gas industry damage include: flaring, pipelines, radioactive/oilfield waste, state accountability, and oil-by-rail.
The following photos from DRC show impacts of current and legacy oil and gas extraction in western North Dakota – an area in the heart of the Bakken that is historically a rich agricultural and ranching region. The vast contrast between the two industries are not complementary.
Bear Den Bay Incident
Fort Berthold Indian Reservation is the epicenter of fracking in the Bakken. On July 8, 2014 a wastewater pipeline rupture was accidentally discovered in rural Mandaree on the reservation. The pipeline is owned by Crestwood Midstream, LLC – a Texas-based company.
An estimated 1 million gallons of toxic saltwater ran down a ravine, ending up in the tributary of Bear Den Bay, which is located ¼ mile from the city of Mandaree’s water intake. The spill was contained, but the state doesn’t know exactly how much waste went into the bay. Tribal administration released a statement that beaver dams prevented the fluids from reaching the lake.
Weeks after the incident Crestwood released a statement saying:
… while assessment of the effect is ongoing, examination and testing to date show that an area of grass, brush and trees about 200 yards long sustained damage. Some produced water ran down a ravine into natural pools in a small stream at the bottom, but it appears that the produced water stopped there… The impact on fish and wildlife appears to have been minimal, in fact beavers, turtles, frogs, deer and pelicans have been seen returning to and re-inhabiting the impacted area.
To date, there has been no penalty for the damage that has been done to the land and reclamation is ongoing. Below are photos documenting the incident’s effects:
The Legacy of North Dakota Oil Booms
Western North Dakota has weathered through two previous oil booms in the early 1950’s and 1980’s. Previous booms left behind infrastructure that sits abandoned today. Due to hydraulic fracking technology, once-inaccessible oil is now accessible. These pre-existing wells are called legacy wells, that produce roughly 5% of North Dakota’s 1.2 million barrels per day.
Much of these wells contain infrastructure that has been in place for over 60 years. Pipelines have not been mapped or regulated in North Dakota until recently. Farmers are finding underground tanks and pipelines filled with toxic sludge. Just like previous oil booms, North Dakota was not prepared for the cost of extraction. Scroll through the following gallery showing a variety of legacy sites in ND.
By Nicole Donaghy, Dakota Resource Council
Sensitive Receptors near Fracked Oil & Gas Wells
Cover of Dangerous and Close report. Click to view report
FracTracker Alliance has been working with the Frontier Group and Environment America on a nationwide assessment of “fracked” oil and gas wells. The report is titled Dangerous and Close, Fracking Puts the Nation’s Most Vulnerable People at Risk. The assessment analyzed the locations of fracked wells and identified where the fracking has occurred near locations where sensitive populations are commonly located. These sensitive sites include schools and daycare facilities because they house children, hospitals because the sick are not able to fight off pollution as effectively, and nursing homes where the elderly need and deserve clean environments so that they can be healthy, as well. The analysis used data on fracked wells from regulatory agencies and FracFocus in nine states. Maps of these nine states, as well as a full national map are shown below.
No one deserves to suffer the environmental degradation that can accompany oil and gas development – particularly “fracking” – in their neighborhoods. Fracked oil and gas wells are shown to have contaminated drinking water, degrade air quality, and sicken both aquatic and terrestrial ecosystems. Additionally, everybody responds differently to environmental pollutants, and some people are much more sensitive than others. In fact, certain sects of the population are known to be more sensitive in general, and exposure to pollution is much more dangerous for them. These communities and populations need to be protected from the burdens of industries, such as fracking for oil and gas, that have a negative effect on their environment. Commonly identified sensitive groups or “receptors” include children, the immuno-compromised and ill, and the elderly. These groups are the focus of this new research.
National Map
National interactive map of sensitive receptors near fracked wells
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State-By-State Maps in Dangerous and Close Report
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