Quote: (02-21-2015 06:19 PM)rudder Wrote:
Where's the frac page?
Gas prices are already surging. Anyone know where the next boom will be and what jobs will be in demand?
Rudder, you sent me a PM with a similar question but for some reason my PM Inbox keeps crashing whenever I try to hit send, my internet must be having a bad day.
It's pretty tough to tell where the next "boom" will be, though. So many things come into play- engineering technology, geopolitics, the economy, etc. Nobody will ever really know until some oil company figures out the next best thing.
You did mention specifically the Green River Formation in UT, CO and WY.
Yes, there are more hydrocarbons in that formation than in all of Saudi Arabia. But it will remain impossible to economically extract for the foreseeable future. Why? Let me explain, with a comparison between the Bakken and the GR:
Imagine you are on a boat, anchored in the ocean in one spot, a mile or so from the shore. Below you, on the ocean floor, are deep marine clays, closer to shore are silts (sort of like a mix between sand and mud) and then on shore is a sandy beach. Over time, you feel like the shoreline is coming towards you. The beach is now only a stones throw from your boat. It's not the tide- the sea level is actually falling. Then, suddenly, the sea level rises again, and once again, the shoreline is a mile away from your anchored boat. That is sort of what happened when the Bakken formation came to be.
Where North Dakota, southern Saskatchewan and Eastern Montana currently sit was once an ocean not too far from the equator- around 300 million years ago. Multiple sea level rises and falls (called regressions and transgressions, respectively) create different deposits of rocks. So go back to that boat analogy- when we started, you were on a boat in deep water in the middle of the sea. This was the first transgressive event that created the bottom of the Bakken. The clays at the bottom of the sea created the "Lower Bakken Shale." Then, when the sea level fell and the shore came towards you, the rocks deposited under your boat became coarser grained. You know how you walk from the beach, you have coarser sand grains when high-energy waves crash on shore, but as you walk out, the sand transitions into mud? It's similar out at sea, just at a smaller scale. This is the Middle Bakken, a coarser-grained silty thing. Then, once again, the sea level rose, and you were back out at the middle of the sea, creating a little 'sandwich,' with the Upper Bakken shale on top:
Anyways, now that you know how the geology of the Bakken works, where does the oil come into play? Well, those deep muds get buried by sea level fluctuations, sedimentation from shore (ie, rivers etc) and so on, and when loose muds are buried and heated by the Earth's interior, they start to cook and harden, creating shale. Shale is sort of neat though- it concentrates tons of organic material. When phytoplankton and zooplankton at the surface of the sea die, they fall down to the bottom of the ocean floor. If they die when they are close to the shoreline, their remains are consumed by scavengers like bacteria. But if they die further out at sea, their remains are preserved, where there is little oxygen at depth to sustain scavengers. These dead plankton mingle and mix with the mud at the ocean floor, and are eventually buried, and become part of the shale once the rock hardens after burial.
However, over time (millions of years), the shale gets buried deeper and deeper, and in turn, heats up. When that shale gets over about 75 degrees C, the organic component of the dead plankton turns into Kerogen, which is a precursor to oil. It's sort of like an oily coal substance. At about 125-150 degrees C, the kerogen turns into oil, and since oil is buoyant with respect to water, it will migrate upwards.
This is how oil deposits are formed- the shale is cooked, and the oil migrates upwards towards surface, and flows very easily through material like sandstone (like beach sand). But if it hits an overlying rock layer with no permeability through which it can flow, it is trapped. This is how big hydrocarbon deposits form. Shale is a rock with no permeability.
In the Bakken, oil came up from the Lower member, and, in theory, could have flown right up and been perfectly trapped by the Upper member. The oil formed at the bottom of the Bakken hit a roadblock on its journey upwards, though. The Middle Bakken is not very permeable at all, so it sort of got stuck. Some of the oil worked its way up, some of it got trapped in the silty pores of the Middle Bakken.
We knew there was oil stuck in limbo in the Middle Bakken for 50 years, but since the rock has no permeability, efforts to drill holes into it and pump it out were fruitless. The silty grains of the rock were just packed too tightly together. Fluid will flow well through a bunch of boulders because the voids between the rocks are interconnected, but when you have clays and silts, fluid gets trapped easily.
When fracking came to be, we could just drill a horizontal well, pump water and sand down, and crack open those shales, crack them open with pressurized water, and prop those cracks open with sand. All that oil trapped in the Middle Bakken was freed from the tight permeability of the silty rock it was trapped in, and the Boom began.
Anyways, you now understand how oil is formed and how the Bakken was exploited.
What is different about the Green River Formation?
We now travel back in time to the Eocene period, about 40-50 million years ago. This is what it looked like:
Yeah, not much different than now. Those three blobs on the left represent the Green River Formation. They were once Lakes along the shadow of the newly-formed Rocky Mountains. When big mountain ranges form, they often create big depressions in the ground called foreland basins, and they fill with water. These were some big ass lakes- Great Lake sized almost.
Lakes have thriving aquatic ecosystems, as you know. Tons of plankton in here too, with the added advantage being that when they die, they fall to the bottom of the lake, trapped in the basin. In theory, it should be a beautiful hydrocarbon trapping system, and it is. However, lakes have one major difference when compared to the ocean: they are much more susceptible to seasonality.
In winter, the lake will freeze. All of the plankton at the surface dies, and sinks to the bottom, creating a thin layer of organic material. But then spring comes, and snow melts. Tons of sediment off the mountains comes into the lake, and in deeper parts, thin layers of mud cover the organic material. Then comes summer, and the lake water begins to really heat up. Evaporation of the water follows. Think of boiling a pot of water on your stove- eventually, the water boils off, and you will have a thin layer of solute in your pan. Salt, carbonates, gypsum, whatever was floating in that water at the time.
This lake was somewhat rich in sulfates and calcium instead of salt, so when summer heat evaporated just a bit of the lakewater, some of those solids dropped out of the water and created a thin film of gypsum on the ocean floor. Summer ends, the lake freezes, plankton dies and the cycle continues.
Here is a picture of what the layering looks like in the Green River Formation:
The black stuff is the organic material and mud, the greyer stuff is mud, and the white stuff is gypsum.
Eventually the lakes dried out and were infilled by sediment, leaving what was once these lakes buried under Wyoming, Utah and Colorado, and it was dubbed the Green River Formation.
But hey- we have all this organic material in place- more than Saudi Arabia! Why can't we just frack it?
Remember how I told you how, before oil is formed, organic material has to go through a transition phase in which it is immature, called Kerogen? Well, that is where we are now. Kerogen is super easy to convert into oil once we get our hands on it, but the problem is pumping it. You can't really pump that stuff to surface- it's like oily coal, like I said earlier. The Green River Formation hasn't been cooked sufficiently to convert that stuff to oil yet.
I'm not sure if it will be produced anytime soon. It would be too intrusive to mine- there is too much civilization around (at least, compared to the Oil Sands in Northern Canada), plus a couple National Parks nearby. It is over 1000 feet deep in places, which is pretty shallow compared to most deposits like the Bakken, but that is too deep to open-pit mine like what they can do in Canada. They've tried drilling wells that inject steam down hole to mobilize it, but the technology isn't there yet.
Anyways, sorry for the long winded explanation. I think about it a lot, because it is such an incredible resource. I hope that one day the engineering falls in place to exploit it within environmental reason, but until that day, I don't see anything changing in the industry.
We are really good at geology now, and have known where the oil is for decades. Geology is way ahead of the engineering (it's a lot easier!), so now all we do is tap out these unconventional plays that we have now like the Bakken and wait for the next frontier to develop...