This is a work in progress...
I want to expand the narrative text, but for dnow,
we're going to explain, in pictures,
How and why fracking commonly contaminates underground water sources.
Section I. Understanding Potential Energy
First, a physics lesson.
Energy can be translated between forms,
such as translating kinetic energy into potential energy.
But energy can neither be created nor destroyed.
https://en.wikipedia.org/wiki/Conservation_of_energy
This is how a pendulum works:
Another way to visualize this is if we imagine a giant lifting a ball on to a mountaintop:
With work, Kinetic Energy can be transformed... |
... into Potential Energy |
Potential Energy is a system waiting to release stored energy via the path of least resistance, so we can expect the ball to come rolling down the mountain any time now! |
If you put energy into a system, that energy doesn't vanish. It can be translated into other forms, such as heat, or as stored (potential) energy.
Section II. Understanding Water Volumes, Visualizing an underground frac job.
Ferris Wheel at Pleasure Pier in Galveston, TX is BIG! at ~100' in diameter. |
Another view of Ferris Wheel at Pleasure Pier in Galveston, TX 100' in diameter. |
According to Skytruth, the average frac in Pennsylvania is 4.3 Million Gallons of water. http://blog.skytruth.org/2012/09/water-water-everywhere-20-months-of.html 4.3 million gallons is a sphere about 103' in diameter. Let's call it 100'. |
Cabot's typical horizontal well in 2012 was 4,100 ft long, with 17.7 frac stages (let's call it 18 stages). WPX was the operator in Franklin Forks, but let's assume they are doing about the same. |
Fracking the Oliver Well Pad, Susquehanna County, PA (Chief) Fracking involves massive pumping trucks all working in concert to generate explosive pressures underground. Photo: Vera Scroggins: http://www.youtube.com/watch?v=TQ1YldfSUV4 |
Average PA frack = 4.3 Million gallons. 4.3M / 18 stages = 238,888 gallons. This is the volume of a sphere 19.7' in diameter. (Let's call it 20'ft) |
Now think about this 100' diameter sphere made up of 18 smaller 20' diameter spheres, each holding ~240,000 gallons. Each of these represents one frac stage. |
LESSON from Section II:
Hydraulic Fracturing involves massive amounts of fluids, and tremendous energy at the surface. This energy at the surface is converted into heat, and stored, potential energy underground.
Section III. Understanding the local geology near Franklin Forks.
According to maps by the Penn State Marcellus Center for Outreach and Research, the depth of the Marcellus Shale in Northern Franklin Twp. Susquehanna County is 5,000-6,000'ft. |
The Depue 8H well in Franklin Forks was 4804'ft deep (TVD). Strange: in Franklin Forks, the Marcellus is 5,000-6000'ft. deep. |
TVD, Total Vertical Depth is the linear vertical depth from the well pad to bottom-of-hole independent of curved path. |
- http://onlinelibrary.wiley.com/doi/10.1111/gwat.12056/pdf
- http://www.gwpc.org/sites/default/files/event-sessions/Molofsky_Lisa2_0.pdf
According Molofsky, et.al., GSI Environmental, the Upper Devonian strata above the Marcellus in the region of Franklin Forks is marked by "Large Scale Faults", |
Combining two graphics from Molofsky, et.al., GSI Environmental. Upper Devonian Formation in this area marked by "Large Scale Faults" |
"Large Scale Faults" in upper Devonian strata near Franklin Forks. (from Molofsky, et.al., GSI Environmental) |
The Upper Devonian strata above the Marcellus near Franklin Forks, in Susquehanna County PA is marked by Large Scale Faults. The shale depth in this area is between 5,000 and 6,000 ft. HOWEVER-- the operator in the area, WPX (Williams Company) drilled one early well, the Depue 8H, only to 4,604', which according to the above charts, seems to be the Tully Sandstone formation, not Marcellus.
Section IV. Putting it all together
According to this article by Haliburton's Kevin Fisher, fractures commonly can extend 1,500' above the horizontal well bore:
http://www.halliburton.com/public/pe/contents/Papers_and_Articles/web/A_through_P/AOGR%20Article-%20Data%20Prove%20Safety%20of%20Frac.pdf
Haliburton's Kevin Fisher reveals that fractures can extend >1,500'ft above the horizontal bore depth. (July 2010, AOGR) |
Matt and Tammy here say their well is ~160' deep:
http://www.youtube.com/watch?v=af0HAhMrxlA
3104'ft - 160'ft = 2944'ft ==> This is all that fluids/gas must travel to contaminate the aquifer.
This is only 3x the distance reported in Fisher's data as being observed.
And in Franklin Forks, this was through the Upper Devonian layer which was marked by "Large Scale Faults".
Each frac stage releases ~240,000 gallons into the surrounding rock. This volume is equal to a sphere ~20' in diameter. |
Fluids injected want to find a path of least resistance back to the surface. |
The pressures involved in hydraulically fracturing rock are similar to a fuel-air bomb. |
LESSONS from Section IV: The fluids injected underground in the Hydraulic Fracturing process are under extreme pressures.
The energy expended at the surface is translated into stored (potential) energy in the fluids, which want to release this energy by returning to the surface via the Path of Least Resistance, which is likely natural faults and fissures in the surrounding geology.
V. Conclusions:
Far from being a fringe scenario, water contamination from the drilling operations in Franklin Forks seems likely, once we understand the geology and the physics.
Extreme pressures are induced into large volumes of fluid underground by expending tremendous energy at the surface. Like the energy transferred into the rubber band of a slingshot, or like lifting a heavy weight up, this energy is not lost, but STORED.
The "charged" fluids pumped underground do not want to stay there, and will find the way back to the surface using the path-of-least resistance, which in the case of Franklin Forks, is likely to be the fault-network in the Upper Devonian formation which lies above the Marcellus.
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