Page 319 - Origin and Prediction of Abnormal Formation Pressures
P. 319
288 H.H. RIEKE, G.V. CHILINGAR AND J.O. ROBERTSON JR.
Models employing both thermodynamic and non-thermodynamic approaches explain
some of the field and laboratory observations on a pore-level (microscopic) scale. These
models are not comprehensive enough to explain all aspects of chemical composition
of pore waters in sedimentary basins. The models, however, do serve as an insight into
some of the mechanisms operating in such sedimentary systems and indicate trends of
changes in pore-water composition associated with burial of the sediments.
Findings presented in this chapter can be applied to some of the important aspects of
reservoir characterization and petroleum recovery operations in the petroleum industry
as observed by a number of investigators. These include among others: (1) prediction of
high-pressured fluid zones (Fertl and Chilingarian, 1977); (2) quantitative interpretation
of electric logs (Chilingar et al., 1969), (3) interpretation of the direction of hydro-
dynamic flow over geologic time in compacting sand-shale sequences (Magara, 1969,
1978; Burrus, 1998); and (4) determination of possible water influx into a producing
petroleum reservoir from the surrounding shales (Dzhevanshir et al., 1987; Bourgoyne,
1990).
BIBLIOGRAPHY
Aharon, E, Roberts, H.H. and Snelling, R., 1992. Submarine venting of brines in the deep Gulf of Mexico:
observations and geochemistry. Geology, 20(6): 481-576.
Anderson, D.M. and Low, P.E, 1958. The density of water adsorbed by lithium-, sodium-, and potassium-
bentonite. Soil Sci. Soc. Am. Proc., 22(2): 99-103.
Angino, E.E. and Billings, G.K., 1969. Geochemistry of Surface Brines. Proc. Symp. Univ. Kansas,
Lawrence, KA. Chem. Geol., 4( 1/2): 371 pp.
Aoyagi, K., Kazama, T., Sekiguchi, K. and Chilingarian, G.V., 1985. Experimental compaction of Na-mont-
morillonite clay mixed with crude oil and seawater. Chem. Geol., 49: 385-392.
Appelo, C.A.J., 1977. Chemistry of water expelled from compacting clay layers: a model based on Donnan
equilibrium. Chem. Geol., 19:91-98.
Arps, J.J., 1953. The effect of temperature on the density and electrical resistivity of sodium chloride
solutions. Trans. AIME, 198: 327-330.
Bailey, A.M., Cohen, A.D., Orem, W.H. and Blackson, J.H., 2000. Mobilization of major inorganic ions
during experimental diagenesis of characterized peats. Chem. Geol., 66: 287-300.
Berger, G., Velde, B. and Aigouy, T., 1999. Potassium sources and iilitization in Texas Gulf Coast shale
diagenesis. J. Sediment. Res., 69( ! ): 151 - 157.
Berry, F.A.E, 1959. Hydrodynamics and Geochemistry of the Jurassic and Cretaceous Systems in the San
Juan Basin, Northwestern New Mexico and Southwestern Colorado. Ph.D. Dissertation, Department of
Geology, Stanford University, Palo Alto, CA.
Berry, F.A.E, 1973. High fluid potentials in California Coast Ranges and their tectonic significance. Bull.
Am. Assoc. Pet. Geol., 57(7): 1219-1249.
Bethke, C.M., 1996. Geochemical Reaction Modeling. Oxford Univ. Press, New York, NY, 397 pp.
Bigelow, E.L., 1994. Well logging methods to detect abnormal pressure. In: W.H. Fertl, R.E. Chapman and
R.E Hotz (Eds.), Studies in Abnormal Pressures. Elsevier, Amsterdam, pp. 187-240.
Bischoff, J.L., Greer, R.E. and Lusitro, A.O., 1970. Composition of interstitial waters of marine sediments:
temperature of squeezing effect. Science, 167: 1245-1246.
Boles, J.R. and Franks, S.G., 1979. Clay diagenesis in Wilcox sandstone of southwest Texas: implications
of smectite diagenesis on sandstone cementation. J. Sediment. Petrol., 49(1): 55-70.
Bolt, G.H., 1956. Physico-chemical analysis of the compressibility of pure clays. Geotechnique, 6(1): 86-93.
Bolt, G.H., 1961. The pressure filtrate of colloidal suspensions, I. Theoretical considerations. Kolloid. Z.,
175: 33-39.