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        http://www.people.cornell.edu/pages/tg21/recharging/
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                 Recharging of oil and gas fields.

                   Thomas Gold -- September 1999

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 There have been numerous reports in recent times, of oil and gas
 fields not running out at the expected time, but instead showing a
 higher content of hydrocarbons after they had already produced more
 than the initially estimated amount. This has been seen in the
 Middle East, in the deep gas wells of Oklahoma, on the Gulf of
 Mexico coast, and in other places. It is this apparent refilling
 during production that has been responsible for the series of gross
 underestimate of reserves that have been published time and again,
 the most memorable being the one in the early seventies that firmly
 predicted the end of oil and gas globally by 1987, a prediction
 which produced an energy crisis and with that a huge shift in the
 wealth of nations. Refilling is an item of the greatest economic
 significance, and also a key to understanding what the sources of
 all this petroleum had been. It is also of practical engineering
 importance, since we may be able to exercise some control over the
 refilling process.

 The debate about the origin of all the petroleum on Earth lies in
 the center of the subject. If we really knew that it is only
 biological materials, which, in their decay, could produce
 hydrocarbons, then the quanities that could ever be produced would
 be limited by the biological content of the sediments. But then the
 clear and strong association of petroleum with the inert gas helium
 would have no explanation; the finding of hydrocarbon gases,
 liquids and solids on most other planetary bodies in our solar
 system which have surface conditions quite unsuitable for surface
 life, could not be understood; the presence of hydrocarbons which
 we now find in abundance in basement rocks would also remained
 unexplained.

 If we accept the fact, now known full well, that hydrocarbons are a
 common constituent of the cosmos and the planetary condensations
 that formed in it, then we have a totally different viewpoint.
 Hydrocarbons are stable down to great depths and the high
 temperatures there, contrary to many statements that have been made
 that the temperature reached at depths between 30,000 and 40,000 ft
 would dissociate most of the hydrocarbons. But these calculations
 are seriously in error, because they ignored the strong stabilizing
 effect of pressure at depth, that had been calculated by Soviet
 (Ukrainian and Russian) thermodynamicists.

 The existence of diamonds, crystals of pure carbon that form at
 pressures which are not reached on earth at depths of less than 140
 kilometers, proves that unoxidized carbon exists at such depths,
 and also carbon-bearing liquids must flow there that can deposit
 carbon at high purity. High pressure fluid inclusions in diamonds
 prove that liquid or gaseous hydrocarbons were present at their
 formation. Present day meteorites give us examples of the solids
 responsible for the building up of the Earth; among those only one
 class, the carbonaceous chondrites, contain much carbon, mostly in
 unoxidized form. That this material is present in the Earth's
 interior in large abundance is shown by the distribution of noble
 gases and their isotopes that have emerged into our atmosphere and
 show distributions that are strikingly similar to those in
 carbonaceous chondrites, but dissimilar to those of any other class
 of meteorites. The presence of this type of material would account
 for a continuous supply of hydrocarbons to the atmosphere, as the
 outer layers of the mantle heat up over time and make fluids form
 from the solid hydrocarbons that were included in the forming Earth
 (as also in most of the other planets and their satellites, in the
 asteroids, comets and interplanetary dust grains). Such fluids are
 less dense than the rocks, and buoyancy forces will propel them
 upwards.

 Rocks and lower density fluids can co-exist at any level in a solid
 planetary body, provided that the pressure of the pore fluids is
 sufficiently high to make the differential pressure between rocks
 and fluids less than the crushing strength of the rocks. For a
 static case (with no upward flow of the fluid), this would result
 in pressure domains, within which the fluid pressure shows a
 pressure gradient with depth given just by the density of the fluid
 (the "head"), and where the bottom of each domain is at the level
 at which the fluid pressure is insufficient to maintain pore spaces
 against the higher pressure of the rock. (See Figure 1.) It is
 assumed here (for the static case) that this makes a complete
 barrier. As for the top of any domain, this cannot be at a level
 higher than that at which the fluid pressure equals the rock
 pressure, since fluid pressures in excess of this value cannot be
 maintained in rocks that on a large scale and in long
 time-intervals, have no tensile strength and therefore cannot
 resist the intrusion of the fluids and the generation of new pores.

 If we consider the case of a slow upward migration of fluids
 (liquids or gases), then this picture changes to one in which each
 domain

                           [Image]

   http://www.people.cornell.edu/pages/tg21/recharging/Image3.gif

   Idealized stacked pore pressure domains that make up a stepwise
   approximation to the rock pressure.

   Pc is the critical pressure at which the pore fluid pressure
   cannot support the rock against crushing.



 will be stacked on another one below, all the way down to the level
 of origin of the fluid. The fluid pressure would thus make a
 stepwise approximation to the pressure in the rocks. Now none of
 the barriers can be absolute, since they would be torn open by the
 fluids that arise from deeper and higher pressured domains. But the
 barriers would be torn open in each case only to the point at which
 the flow to the overlying domain causes it to suffer a pressure
 drop resembling that of the static case. This rule will apply
 whatever the nature of the rock. The heights of the domains will be
 determined by the rock and fluid densities and the crushing
 strength of the rocks; this height has been found to be between
 10,000 ft and 15,000 ft in many sedimentary rocks, and in excess of
 20,000 ft in granitic basement rocks. The upward seepage of methane
 is very widespread all over the Earth, as is shown by the great
 extent of methane hydrates on the ocean floors and in permafrost
 regions on land, where mostly no shallow source of methane can be
 invoked.

 Vertically stacked domains of hydrocarbons have been found in all
 cases where drilling was sufficient to display them. The consistent
 tendency to find hydrocarbons below any producing region has been
 given the name of "Koudyavtsev's Rule", after the important Russian
 petroleum investigator who discovered this effect and collected a
 very large number of examples of it from all parts of the world.
 This rule would be the consequence of a deep origin of hydrocarbons
 and a steady process of outgassing.

 With this picture in mind we would readily understand that
 refilling of hydrocarbon fields is possible and even probable. But
 if merely the steady upward flow from deep sources had been
 responsible, the refilling time scales would be much too slow to be
 of commercial interest, or to match the speed that appears to have
 been observed. A limit to the global average of that flow speed can
 be derived from the approximately known supply of carbon to the
 atmosphere over time. On that basis a large gas field may be
 recharging in times reckoned in tens of thousands of years, still
 very short compared with many millions of years, as had been the
 widespread belief. But observed refill times of just a few tens of
 years cannot be explained by this. However another effect will set
 in when a field is under production and the pressure in its domain
 is thereby diminished. The pressure difference between the
 producing domain and the one below it will then be increased,
 resulting in a higher rate of flow through the low permeability
 layer that divides these domains, or it may even result in a
 physical rupture of that layer.

 There is an analogous case known in Kuwait. The extraction of
 goundwater at the shallow levels results in the disintegration of
 the barrier to the oil levels just below, and the water in the
 wells is suddenly replaced by oil. The delicate pressure balance
 that had established itself, just up to the level that the strength
 of the rock could bear, had been upset. Similarly in stacked
 domains of hydrocarbons, the lower domains will be opened quickly,
 once the upper ones had been depleted and the fluid pressure
 thereby reduced sufficiently. This process can be fast, just as it
 is in Kuwait, where we had the advantage that a different liquid
 (water) filled the upper domain, so that one could identify the
 rupture to the oil filled domain below.

 This type of refilling process thus allows exploitation of the
 domain below that from which production had been obtained before.
 In turn, when this lower domain had suffered a sufficient pressure
 loss, the process may continue to the next lower domain. How much
 more than the original content of a hydrocarbon field can be
 produced in any one case will depend on numerous details of the
 formation, but present indications are that it is often at least
 double. The present global gas and oil glut appears to be due to
 this effect, and we have not yet seen the end of it, or any
 indication that it will end soon. Gas fields will be subject to
 faster refilling than oil fields, and moreover the volumes of gas
 in lower domains will in general be greater due to the higher
 pressures there and the higher compressibility of gas. Gas will
 thus become more plentiful than oil for this reason alone, but gas
 seems to be generally more plentiful and more widespread than oil.
 The environmental advantages of changing from coal or oil to gas,
 by far the cleanest of all combustible fuels, are very large, and
 the changeover is at present still handicapped by the mistaken
 belief that the supplies of gas will run out soon.



Thomas Gold :
  http://www.people.cornell.edu/pages/tg21/index.html

The Origin of Methane (and Oil) in the Crust of the Earth :
  http://www.people.cornell.edu/pages/tg21/usgs.html

Scientist Says Earth's Petroleum Supply Is Replenishing Itself :
  http://www.elsi.org/renewable.htm

The Theory of Unlimited Oil :

http://www.abcnews.go.com/onair/CloserLook/wnt_000316_CL_oilheretic_f
eature.html

A Scientific Heretic Delves Beneath the Surface :
  http://www.washingtonpost.com/wp-dyn/style/A3196-1999Oct31.html



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