It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
Originally posted by Valhall
Well, we need to hurry and get this new science out then, because there are a lot of geologists and seismologists that are tremendously misled.
They've been operating off the fact that the greater the density variation between two media at a boundary layer, the greater the reflection angle and the less transmitted through the less dense media.
Furthermore, they've been under the impression that S-waves can't even be transmitted through fluids, so they're in a heap of a mess on that one.
I contend that if we had a giant layer of honeycombs there'd be no way for a quake to transmit from one point on the earth to another...it would just bounce about inside the earth losing a bit of energy each time it reflected against one of these baffles, until it completely dissipated.
But that's because I'm deeply entrenched in the old science.
Originally posted by Valhall
One thing that complicates it further, and tends to weaken the reports referred to originally, is that let's say for this map
it' very easy to jump to the conclusion that we've got this huge plane of orange that now has a "layer" that is some how weakened by the oil extraction. The problem is, it's not showing you the area in 3D. All those areas in orange are at different depths. So it actually isn't a plane. It's very discontinuous "spots" where oil or gas as been produced. One field's producing zone might be at 20,000 ft and the other might be at 3,000 ft. So the orange doesn't actually "connect together"
Hope that made sense.
EDIT: Corrected pre-coffee homonymal dysfunction.
Induced Earthquakes in General (6 references)
Injection Induced Earthquakes (116 references)
Rocky Mountain Arsenal quakes
Reservoir Induced Earthquakes (127 references)
Oil & Gas Production Induced Earthquakes (48 references)
Geothermal Energy Extraction Induced Earthquakes (38 references)
Mining and Quarrying Induced Earthquakes (89 references)
Nuclear Test Induced Earthquakes (20 references)
Seismicity Related to Underground Gas Storage (7 references)
Legal Implications of Induced Earthquakes (13 references)
Miscellaneous References (21 references)
Newspaper & Magazine References
Links to other induced seismicity webpages
Study: Quakes Trigger Quakes
...They discovered that the materials didn't react to the frequency of the seismic vibrations, but were weakened as a whole when hit by shocks exceeding certain seismic strengths, comparable to the "loudness" of the seismic waves.
The sudden weakening at key amplitudes, instead of gradual weakening as amplitudes steadily increased, is why they describe the triggering as nonlinear, Johnson explained.
...To see if the laboratory finding could be applied to real earthquakes, Johnson teamed up with the U.S. Geological Survey's Joan Gomberg to see which sorts of historical quakes seem to be triggering other tremors.
They compared records from a number of remotely triggered quakes and found that the most important factor was amplitude, not frequency, just as in the laboratory.
Originally posted by Thomas Crowne
I do not assume that because you do not let your ignorance in American government stop you from spreading disinforamtion means that you haven't a clue about this topic.
Originally posted by nrky
So now this brings up the argument of the resonance capabilities of air in different states:
1. Differing pressure states, ie. vacuum, atmosphere, concentrated gas, etc.
2. Differing temperatures of the air.
3. Convection forces present in the air.
To argue whether or not air and othe gases act as efficient conductors, or dampeners, is to consider these three principles.
Is the air in a porous rock at the same temperature, pressure, and velocity as that of the air in a water pump, or the air in the upper stratosphere?
Originally posted by Valhall
loam
Thanks for the list. But you do understand that's a totally different issue, right? Those links are talking about earthquakes induced by drilling, producing, mining activities and seismic testing. Not about natural earthquakes being able to amplify or transmit better to another portion of the earth's surface due to the after effects of what oil production does to the reservoir.
Originally posted by Valhall
I fully support the idea that drilling, mining and seismic testing could induce earthquakes. In fact, I believe in one of the threads concerning the Indonesian quake that we actually discussed an article found that talked about some seismic testing that had been taking place in the area just prior to the big quake.
Induced Seismicity
Induced seismicity describes earthquakes that in one way or another are related to human activity. They can be divided in two types:
Triggered. This group of earthquakes are caused by tectonic stresses. They would probably have occurred sooner or later, but their proximity to to human activity in time and space indicates antropogenic activity.
Truly induced. This group of earthquakes are purely antropogenic in that stress buildup can be traced directly to human activity.
For convenience we use the term `induced' for both types.
Earthquakes are mainly induced in three antropogenic settings, (1) in mines, (2) in connection with large water reservoirs and (3) in oil or gas fields where hydrocarbons are extracted. Furthermore earthquakes are induced in hydrothermal fields, but since this industry is young compared to the three above less data exist.
more...
Originally posted by Valhall
What I am arguing against is that an air chamber would act as a better transmitter of a seismic wave than continuous rock. If you place an air chamber in the path of a wave you are going to decrease the wave transmission to the next layer of "solid media". Every time! It's a baffle!
Originally posted by Valhall
Concerning statements made prior about the change in rock properties due to production. You don't actually leave the pores of the rock empty. The fluids are stacked according to their density, just as they would be in a glass. You've got gas on top, oil in the middle and water below. As you produce a zone (whether it be gas or oil) the fluids will migrate (unless there is an impermeable barrier between them) up the reservoir. That's why eventually oil wells start producing water. So you haven't really left the rock empty, you've just changed the filler in areas.
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...
Conclusions
We have used interferometric analysis of spaceborne ERS SAR to map the subsidence of the surface over oilfields in central California. We measure very rapid subsidence rates of up to 400 mm yr-1 or >1 mm day-1 (Plate 3), and show the subsidence is largely limited to the petroleum production properties (Figures 1 and 2). In the Lost Hills oilfield, preliminary elastic strain modelling using an implementation of the Okada [1985]model [Feigl and Dupré, in press] indicates a net compaction of 1.7 mm day-1 at the center of the subsidence bowl decreasing to 0.6 mm day-1 to the south. That much compaction over a total area 0.8 x 5 km could account for the observed surface subsidence of the 35-day interferogram (Plates 1 and 3). This modeling shows that the volume change in the rock units at depth sufficient to cause the observed signal is roughly 1.5x106 m3 yr-1 for the Lost Hills oilfield. More detailed modelling of the deformation in the fluid reservoirs [e.g., Segall et al., 1994] would require data on pressure changes within the reservoir from the operating companies...
Originally posted by Valhall
But let's just say, for the sake of argument, that all your little pores in your rock were left dry. That rock would be less likely to transmit a wave on upward toward the surface than a rock with pores filled with water or oil. The more "compressive" the fluid filling a pore is, the more it will absorb the energy in an "echo chamber" type style and not transmit the energy on up. Again, a little bitty baby baffle.
The sudden weakening at key amplitudes, instead of gradual weakening as amplitudes steadily increased, is why they describe the triggering as nonlinear, Johnson explained.
Originally posted by Valhall
I don't think we can extrapolate the potential to cause minor quake activity via sub-surface activities to the POST-production state of the reservoir and then jump over to - and so quakes will transmit better afterwards. No, I don't see that connection at all.
The quake inducing activities (which by the way, we can only say MAY cause quakes not definitively DO cause quakes)
...would be through a dynamic vibration-inducing event.
It has nothing to do with later reservoir-rock property changes.
As far as talking about "compaction". I'm not going to sit here and say there couldn't be ANY compaction EVER, but it would be highly unlikely.
Primarily because once a reservoir is depleted down to where the pore pressure no longer can produce the hydrocarbons up to the wellhead, the well is P&A'd.
The hydrocarbons are going to continue to produce (at an unprofitable rate) into the wellbore until the pressure below the plug in the wellbore and the reservoir equalize.
So it doesn't go to "zero" is basically what I'm saying. You're still going to have both pore pressure - not a vacuum in the little pores.
Compaction, if you mean destruction of the pore spaces and breaking down of the matrix of the rock, isn't very likely.
Originally posted by Valhall
P.S. loam - if you ARE concerned there could be compaction due to decreased pore pressure, then you need to support CO2 sequestration in depleted oil fields.
Two birds - one gas. LOL!