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Originally posted by Valhall
It's referring to an amplitude that abruptly destroys the rock strength. This isn't a matter of INCREASING amplitude, but a specific amplitude that can destroy rock very efficiently.
In other words, the article speaks of the amplitude of incoming wave - not about what is around the rock (void or otherwise).
Originally posted by loam
I can't see why not?
What are the mechanics, then, of induced earthquake activity caused by drilling? Can it lead to compaction or not? If it does, why does that not reconcile with your own assertion that sound waves travel more freely in denser the material?
Which I assume you mean by either naturally occurring seismic activity or something man-made.
How did you get there? Are you saying this would not even lead to additional compaction?
But Valhall...There is PLENTY of evidence that compaction occurs frequently and on a significant scale. Remember this is a global discussion. You certainly don't maintain that deposits all over the world are substantially the same?
Pumping is also often used for extraction when the pressure is no longer sufficient.
But is still weaker than was true when the deposit was untapped.
This has other concerns...
This isn't a matter of INCREASING amplitude, but a specific amplitude that can destroy rock very efficiently.
Originally posted by Valhall
We are currently in a thread about a false threat based on a misinterpretation of research, and some one has offered up a solution to the factors you have brought up. Your response is to wave it off because of "other factors".
Originally posted by Valhall
I've got one more example, and then I'm leaving this thread behind,
Originally posted by Valhall
I can see why not. They don't have anything to do with each other! Absolutely nothing. You can talk about a human action that might be able to invoke a seismic event. Or you can talk about the post-production state of the reservoir that might behave differently than before the reservoir was produced. BUT THEY DON'T HAVE A CONNECTION. I might add - that the activities that tend to take place in the life of the well that COULD cause a pseudo-seismic event come BEFORE the production typically.
The only mechanics of drilling that could cause compaction of rock is extremely near the wellbore. And that compaction is most likely carried up the wellbore during the drilling operation. Anything left behind is a minute layer (and I'm talking inches NOT feet) about the wellbore wall. It's not doing anything in the grand scheme of things...
...I read your link. It was concerning California, and I'm not convinced. I'm not saying I'm discarding it, I'm just saying that there are a LOT of geographic factors taking place in California...now isn't there? I wouldn't call this PLENTY. But I will read anything further you submit.
Land Subsidence in the United States
Approximate location of maximum subsidence in the United States identified by research efforts of Dr. Joseph F. Poland (pictured). Signs on pole show approximate altitude of land surface in 1925, 1955, and 1977. The site is in the San Joaquin Valley southwest of Mendota, California.
Some of the most spectacular examples of subsidence-related earth fissures occur in south-central Arizona.
Homes at Greens Bayou near Houston, Texas, where 5 to 7 feet of subsidence has occurred, were flooded during a storm in June 1989.
This building at the Everglades Experiment Station was originally constructed at the land surface; latticework and stairs were added after substantial land subsidence.
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Collapse sinkholes, such as this one in Winter Park, Florida (1981), may develop abruptly (over a period of hours) and cause catastrophic damage.
The occurrence of land subsidence is seldom as obvious as it is in the case of catastrophic sinkholes or mine collapses. Where ground-water mining or drainage of organic soils are involved, the subsidence is typically gradual and widespread, and its discovery becomes an exercise in detection. Gazing out over the San Joaquin Valley, California today, one would be hard-pressed to recognize that fewer than 75 years ago the land surface was nearly 30 feet higher in some locations (fig. 2). Subsidence detection and mapping programs are critical to the scientific understanding and management of our land and water resources.
The detection of regional-scale subsidence has historically depended on the discovery that key bench marks have moved. Land surveys establish bench-mark positions to accurately locate roadways, flood and drainage-control structures, pipelines, and other engineered infrastructure. Once unstable bench marks are discovered, and truly stable bench marks have been established, subsidence can be mapped. This has traditionally been accomplished using spirit leveling and, more recently, Global Positioning System (GPS) surveys. A new tool has emerged in the past decade that has dramatically improved our capability to detect and map land-surface deformation.
This tool, interferometric synthetic aperture radar (InSAR), uses repeat-pass radar images from Earth-orbiting satellites to measure subsidence and uplift at unprecedented levels of spatial detail (80 m x 80 m) and measurement resolution (sub-centimeter) (Galloway and others, 2000) (fig. 10).
Once subsidence is identified and mapped, subsidence-monitoring programs can be implemented and scientific studies can be launched to improve our understanding of the subsidence processes. A combination of scientific understanding and careful management can minimize the subsidence that results from developing our land and water resources.
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Rapid subsidence over oil fields measured by SAR interferometry
Ground subsidence is a major worldwide hazard. One recent estimate placed the annual cost of subsidence damage and mitigation within the U.S. alone at over $100 million [National Research Council, 1991]. Relatively slow subsidence caused by the natural process of sediment compaction is widespread but seldom causes problems on human timescales. More rapid subsidence of the ground surface is usually attributable to human activities, such as the extraction of fluids from beneath the surface. Fast local changes in land elevation and associated surface strains can cause damage to structures that is costly to replace or repair, and can also greatly increase flooding potential.
Rapid ground subsidence over areas of petroleum and gas extraction has been observed previously [Mayuga and Allen, 1970; Pratt and Johnson, 1926; Vanhasselt, 1992]. The effects are most noticeable on a coastline where a small elevation decrease may cause inundation, first described over an oilfield near Houston, Texas [Pratt and Johnson, 1926]. Parts of the city and port of Long Beach, California, suffered major problems due to rapid (up to 0.75 m yr-1) land subsidence related to extraction of oil from the underlying Wilmington oil field [Mayuga and Allen, 1970]. Problems were caused both by inundation and by horizontal strains on the sides of the subsidence bowl. Subsidence over petroleum extraction zones can also cause significant damage to extraction infrastructure itself, including expensive well failures. In this paper, we report subsidence rates as high as 40 mm in 35 days or an annual rate of > 400 mm yr-1 in two California oilfields.
Measuring Land Subsidence from Space
Land subsidence is a gradual settling or sudden sinking of the Earth's surface owing to subsurface movement of earth materials. Subsidence in the United States has directly affected more than 17,000 square miles in 45 states, and associated annual costs are estimated to be approximately $125 million.
Originally posted by Valhall
Are you speaking of wellhead pumping to extract hydrocarbons from a well that no longer can flow to surface? If so, yes, you are correct. That has nothing to do with this conversation. I stated that at some point the well would not produce at a profitable rate that include having to put a popping-johnnie on it or whatever. At some point the well will be closed in and P&A'd. period.
Originally posted by Valhall
You totally missed the point. The less the pore pressure the more dampening.
Originally posted by Valhall
We are currently in a thread about a false threat based on a misinterpretation of research, and some one has offered up a solution to the factors you have brought up. Your response is to wave it off because of "other factors".
Cool! At least the original premise of the threat is not something that will kill us tomorrow, so I guess it is acceptable to wring our hands a bit longer on how to deal with GHG's. Meanwhile, we move on...blaming it on somebody else.
Originally posted by loam
OK, if the post production state is "caused" by man (drilling, mining & pumping), and that leads potentially to more impactful seismic events, isn't that the point of this thread? Shouldn't we more fully understand that?
quotes as you provided them above...
I still do not understand why you believe that has no impact on the geology of the field.
And the more subsidence/compaction (therefore, density), the less dampening?
I'm not even sure what you are ranting about. Who is misrepresenting research on this thread? Really, Val, it sounds so paranoid and uncivilized......unfriendly...
And on a broader note: Does everyone, you believe wrong, harbor a secret agenda to perpetrate fraud? (That question probably should be left a rhetorical one. In other words, I at least hope that is not true.)
Again, let's keep it civil, please. I greatly respect your intelligence and like your input. It's the degree of your emotional restraint I'm less confident of.
Surface subsidence results from the combined effects of the subsurface reservoir compressing or compacting a sufficient amount that it causes a displacement in geological formations above that are not strong enough to withstand the underlying structural force changes. If the changes in reservoir conditions are small enough or the upper geological structures are strong enough, surface displacement will not occur or will be only negligible. Reservoir compaction is a function of the extent of pressure reduction, the thickness of the producing zone, and the compressibility of the formation structure. Most reservoirs in which OGE has caused significant compaction consist of a sequence of unconsolidated sands and shales. Studies have shown that the amount of surface subsidence caused by reservoir compaction decreases with increasing depth of the reservoir from the surface and increases with the effective diameter of the reservoir and thickness of the reservoir. In other words, large scale subsidence results from special conditions such as large pressure declines in shallow, thick, large, highly compressible reservoirs. Production practices that include artificial pressure maintenance by gas drive or water injection counteract the reservoir compacting that would otherwise occur.
The preceding indicates that oil reservoirs produced by pressure depletion in loose sands or, and extremely large gas reservoirs in unconsolidated sands or friable rocks, are the types most susceptible to subsidence. This is indeed what Geertsma2 and Martin and Serdengecti3 found to be true in their studies, leading to the conclusion that other reservoirs are not a real concern in regard to surface subsidence.
Originally posted by Valhall
loam, yes! But giving me a link of bibliographies concerning man's potential earthquake inducing activities, doesn't help with this discussion...
Originally posted by Valhall
First off, I'm not ranting. Did that accusation come because I disagree with something here, or because I challenged that dismisisng a possible solution simply because it may not be perfected might not be the best action? If disagreeing equates to ranting, I guess I'll probably "rant" at some point in the future as well when we meet again. I don't believe I've done anything in this thread with you but have a discussion on the points you have brought up, right?
I don't think you have an agenda. At least I don't see one from where I'm sitting. I also haven't accused you of manipulating research. My statement was toward the fact that the original take on the reports referenced in this thread was based on a misinterpretation of what those reports said. So....??? Where'd that come from? I actually have no problem with anything you've said and I haven't been dismissive of any of it....other than refusing to go buy all the references on a link that is about another topic. I'm now going to go read your compaction links.
Originally posted by Valhall
So what we've got is the compaction of unconsolidated sand. It's packing. But it is not rock breaking down. I would agree that if you have a layer of unconsolidated sand that is compacted by overburden pressures after the zone's pressure has been decreased, it would become more transmissive of a wave than the uncompacted sand would have been before.
Originally posted by Valhall
TA
In reference to your podcast. We agree on the destructive nature of harmonic resonance being dependent on amplitude. My statement was ill-worded and should have read that harmonic resonance is not dependent on amplitude. The destructive force of it would be. Good correction, thanks!
About your statement on oil extraction. Please note that I said that by majority it being recovered from the porous, permeable rock is the case. There are exceptions where there are great pools (i.e. a vugular or cavernous reservoir). By majority the great pools were way in the past.
Originally posted by soficrow
Now loam is asking - Can we agree that the larger the chamber, the more it will impede waves at ALL frequencies?
Originally posted by soficrow
Now on the issue of sound waves in larger cavernous voids, I would ask whether there is any localized effect caused by these sound waves? Could these effects contribute to the destabilization of the overall structure of these voids?
Originally posted by soficrow
...So - you're saying that one impact of a 'rogue seismic wave' might be the sudden collapse of a void (or now-empty underground chamber), right?
...Brain burp - I cannot remember the term for those big holes that keep opening up all over...? Can you help me out here? And do you think they might be related, sometimes?
Originally posted by soficrow
That pic is GREAT! Thanks for posting it. Looks like the ground level in the San Joaquin Valley has dropped by what? maybe 30 feet in the last 70-odd years? ...and that area is above what? the now-almost-dry underground Colorado River?
...So if that drop happened suddenly, what kind of cascade might follow? Would the final impact be greater than the sum of its parts?
Originally posted by loam
...compaction will facilitate the transmission of sound waves more so than would have been true prior to compaction, the question becomes have we unwittingly made some areas more vulnerable to the effects of seismic waves because of such subsidence?