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Hydrologic precursors to earthquakes: A review

  • Hydrologic and Geochemical Precursors
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Abstracts

This review summarizes reports of anomalous flow rates or pressures of groundwater, oil, or gas that have been interpreted as earthquake precursors. Both increases and decreases of pressure and flow rate have been observed, at distances up to several hundred kilometers from the earthquake epicenter, with precursor times ranging from less than one day to more than one year. Although information that might rule out nontectonic causes does not appear in many published accounts of hydrologic anomalies, several recent studies have critically evaluated the possible influences of barometric pressure, rainfall, and groundwater or oil exploitation. Anomalies preceding the 1976 Tangshan, China, and the 1978 Izu-Oshima-Kinkai, Japan, earthquakes are especially well-documented and worthy of further examination.

Among hydrologic precursors, pressure head changes in confined subsurface reservoirs are those most amenable to quantitative interpretation in terms of crustal strain. The response of pressure head to earth tides determines coefficients of proportionality between pressure head and crustal strain. The same coefficients of proportionality should govern the fluid pressure response to any crustal strain field in which fluid flow in the reservoir is unimportant. Water level changes in response to independently recorded tectonic events, such as earthquakes and aseismic fault creep, provide evidence that a calibration based on response to earth tides may be applied to crustal strains of tectonic origin.

Several models of earthquake generation predict accelerating stable slip on part of the future rupture plane. If precursory slip has moment less than or equal to that of the impending earthquake, then the coseismic volume strain is an upper bound for precursory volume strain. Although crustal strain can be only crudely estimated from most reported pressure head anomalies, the sizes of many anomalies within 150 kilometers of earthquake epicenters appear consistent with this upper bound. In contrast, water level anomalies at greater epicentral distances appear to be larger than this bound by several orders of magnitude.

It is clear that water level monitoring can yield information about the earthquake generation process, but progress higes on better documentation of the data.

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References

  • Asimov, M. S. Mavlyanov, F. A., Erzhanov, J. S., Kalmurzaev, K. E., Kurbanov, M. K., Kashin, L. N., Negmatulaev, S. H. andNersesov, I. L. (1979)On the state of research concerning earthquake prediction in the Soviet Republics of Central Asia. InEarthquake Prediction Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Bakun, W. H. andLindh, A. G. (1985),The Parkfield, California earthquake predicton experiment. Science229 619–624.

    Google Scholar 

  • Biot, M. A. (1941),General theory of three-dimensional consolidation, J. Appl. Physics12, 155–164.

    Google Scholar 

  • Bodvarsson, G. (1970),Confined fluids as strain meters, J. Geophys. Res.75, 2711–2718.

    Google Scholar 

  • Bower, D. R. (1983),Bedrock fracture parameters from the interpretation of well tides J. Geophys. Res.88, 5025–5035.

    Google Scholar 

  • Bredehoeft, J. D. (1967),Response of well-aquifer systems to earth tides, J. Geophys. Res.72, 3075–3087.

    Google Scholar 

  • Butler, R., Stewart, G. S. andKanamori, H. (1979),The July 27, 1976 Tangshan, China earthquake—A complex sequence of intraplate events. Bull. Seismol. Soc. Am.69, 207–220.

    Google Scholar 

  • Cooper, H. H. Jr, Bredehoeft, J. D., Papadopolos, I. S. andBennett, R. R. (1965),The response of well-aquifer systems to seismic waves. J. Geophys. Res.70, 3915–3926.

    Google Scholar 

  • Deng, Q., Jiang, P., Jones, L. M., andMolnar, P. (1981),A preliminary analysis of reported changes in ground water and anomalous animal behavior before the 4 February 1975 Haicheng earthquake. InEarthquake Prediction: An International Review, Maurice Ewing Series 4 (D. W. Simpson and P. G. Richards, eds.), American Geophysical Union.

  • Dieterich, J. H. (1986a),A model for the nucleation of earthquake slip. InEarthquake Source Mechanics, Geophysical Monograph 37 (Maurice Ewing 6), American Geophysical Union, pp. 37–47.

  • Dieterich, J. H. (1986b),Nucleation and triggering of earthquake slip: Effect of periodic stresses. Tectonophysics, in press.

  • Earthquake Engineering Research Institute (1984),The anticipated Tokai earthquake: Japanese prediction and preparedness activities, Publication No. 84-05.

  • Guha, S. K. (1984),Geoelectrical and geohydrological precursors of earthquakes in northeastern India—A discussion, Geoexploration23, 285–289.

    Google Scholar 

  • Hadley, K. (1973),Laboratory investigation of dilatancy and motion on fault surfaces at low confining pressures, inProceedings of the Conference on Tectonic Problems of the San Andreas Fault System, (R. L. Kovach and A. Nur, eds.), Stanford University Publications, Geological Sciences Vol. XIII.

  • Hanks, T. C. andBoore, D. M. (1984),Moment-magnitude relations in theory and practice. J. Geophys. Res.89, 6229–6235.

    Google Scholar 

  • Hanson, J. M., andOwen, L. B. (1982),Fracture orientation analysis by the solid earth tidal strain method. Paper presented at the 57th Annual Fall Technical Conference of the Society of Petroleum Engineers of AIME.

  • Healy, J. H. andUrban, T. C. (1985),In situ fluid pressure measurements for earthquake prediction: An example from a deep well at Hi Vista, California, Pure and Appl. Geophys.122, 255–279.

    Google Scholar 

  • Hsieh, P. A., Bredehoeft, J. D. andFarr, J. M. (1987),Estimation of aquifer transmissivity from phase analysis of earth-tide fluctuations of water-levels in artesian wells. Water Resources Res., in press, 1987.

  • Ida, Y. (1974),Slow-moving deformation pulses along tectonic faults. Phys. Earth and Planet. Int.9, 328–337.

    Google Scholar 

  • Johnson, A. G. (1973),Pore pressure changes associated with creep events on the San Andreas fault. Ph. D. thesis, 177 pp. Stanford University, Stanford, CA.

    Google Scholar 

  • Johnson, A. G., Kovach, R. L. andNur, A. (1973),Pore pressure changes during creep events on the San Andreas fault. J. Geophys. Res.78, 851–857.

    Google Scholar 

  • Johnston, M. J. S., Linde, A. T., Gladwin, M. T. andBorcherdt, R. D. (1987),Fault failure with moderate earthquakes, Tectonophysics, in press.

  • Kasahara, K. (1979),Migration of crustal deformation. Tectonophysics52, 329–341.

    Google Scholar 

  • Kissin, I. G., Barabanov, V. L., Grinevskiy, A. O., Markov, V. M., andKhudzinskiy, L. L. (1983).Experimental investigations into conditons of groundwaters in order to identify hydrocynamic earthquake forerunners. Izvestiya, Earth Physics19, 6, 482–491.

    Google Scholar 

  • Kovach, R. L., Nur, A., Wesson, R. L. andRobinson, R. (1975).Water-level fluctuations and earthquakes on the San Andreas fault zone, Geology3, 437–440.

    Google Scholar 

  • Lamar, D. L. andMerifield, P. M. (1979),Water-level monitoring along the San Andreas and San Jacinto faults, southern California, During fiscal year 1979. Lamar-Merifield Tech. Report 79-5, Final Report, U. S. Geological Survey Contract 14-08-0001-17680, 65 pp.

  • Lehner, F. K., Li, V. C. andRice, J. R. (1981),Stress diffusion along rupturing plate boundaries. J. Geophys. Res.86, 6155–6169.

    Google Scholar 

  • Li, V. C. andRice, J. R. (1983),Precursory surface deformation in great plate boundary earthquake sequences, Bull. Seismol. Soc. Am.73 1415–1434.

    Google Scholar 

  • Lippincott, D. K., Bredehoeft, J. D. andMoyle, W. R. Jr. (1985),Recent movement on the Garlock fault as suggested by water-level fluctuatons in a well in Fremont Valley, California. J. Geophys. Res.90, 1911–1924.

    Google Scholar 

  • Liu, Lanbo andZheng, Xiangyuan (1985),The geophysical interpretation of waterlevel tides in deep boreholes. Summary of paper presented at 1985 Spring meeting, American Geophysical Union.

  • Madden, T. (1987),Resistivity and magnetic variations as earthquake precursors: A search for possible causes. This volume.

  • Magara, K. (1980),Comparison of porosity-depth relationships of shale and sandstone. J. Petroleum Geology3, 175–185.

    Google Scholar 

  • Melchior, P. (1983),The Tides of the Planet Earth, second edition, Pergamon Press, 641 pp.

  • Merifield, P. M. andLamar, D. L. (1978),Reports on two years of water-level monitoring along the San Andreas and San Jacinto faults, southern California. Lamar-Merifield Tech. Report 78-5, Final Report, U. S. Geological Survey Contract 14-08-0001-15881, 95 pp.

  • Merifield, P. M. andLamar, D. L. (1980),Water-level monitoring along the San Andreas and San Jacinto faults, southern California, during fiscal year 1980. Lamar-Merifield Tech. Report 80-2, Final Report, U. S. Geological Survey Contract 14-08-0001-18358, 77 pp.

  • Merifield, P. M. andLamar, D. L. (1981),Water-level monitoring along the San Andreas and San Jacinto faults, southern California, during fiscal year 1981. Lamar-Merifield Tech. Report 81-3, Final Report, U. S. Geological Survey Contract 14-08-0001-19253, 78 pp.

  • Merifield, P. M. andLamar, D. L. (1985),Possible strain events reflected in water levels in wells along San Jacinto fault zone, southern California. Pure Appl. Geophys.122, 245–254.

    Google Scholar 

  • Merifield, P. M., Lamar, D. L. andBean, R. T. (1982),Water-level monitoring along the San Andreas and San Jacinto faults, southern California, during fiscal year 1982. Lamar-Merifield Tech. Report 82-5, Final Report, U. S. Geological Survey Contract 14-08-0001-19253, 93 pp.

  • Merifield, P. M., Lamar, D. L. andBean, R. T. (1983),Water-level monitoring along the San Andreas and San Jacinto faults, southern California, during fiscal year 1983. Lamar-Merifield Tech. Report 83-3, Final Report, U. S. Geological Survey Contract 14-08-0001-20660, 77 pp.

  • Monakhov, F. I., Khantayev, A. M., Kechaykina, V. S., andShishkin, A. A. (1983),Comparative characteristics of the response of groundwater level and outflow to earthquake preparation. Izvestiya, Earth Physics19, 405–408.

    Google Scholar 

  • Narasimhan, T. N., Kanehiro, B. Y. andWitherspoon, P. A. (1984),Interpretation of earth tide response of three deep, confined aquifers, J. Geophys. Res.89, 1913–1924.

    Google Scholar 

  • Nayak, P. N., Saha, S. N., Dutta, S., Rama Rao, M. S. V., andSarker, N. C. (1983),Geoelectrical and geohydrological precursors of earthquakes in northeastern India. Geoexploration21, 137–157.

    Google Scholar 

  • Nur, A. (1972),Dilatancy, pore fluids, and premonitory variations of ts/tp travel times. Bull. Seismol. Soc. Am.62, 1217–1222.

    Google Scholar 

  • Nuttli, O. W. (1985),Average seismic source-parameter relations for plate-margin earthquakes. Tectonophysics118, 161–174.

    Google Scholar 

  • Oki, Y. andHiraga, S. (1979),Water level anomalies prior to the Izu-Oshima earthquake, January 14, 1978. Translated from the Japanese by E. Silberman, in Technical Report 79-2, Lamar-Merifield Geologists, Special Technical Report for the U. S. Geological Survey.

  • Oki, Y. andHiraga, S. (1987),Groundwater-level monitoring for predicton of earthquakes. This volume.

  • Rhoads, G. H. Jr. andRobinson, E. S. (1979),Determination of aquifer parameters from well tides. J. Geophys. Res.84, 6071–6082.

    Google Scholar 

  • Rice, J. R. andCleary (1976),Some basic stress-diffusion solutions for fluid-saturated elastic porous media with compressible constituents. Rev. Geophys. Space Phys.14, 227–241.

    Google Scholar 

  • Rice, J. R. andRudnicki, J. W. (1979),Earthquake precursory effects due to pore fluid stabilization of a weakening fault zone. J. Geophys. Res.84, 2177–2193.

    Google Scholar 

  • Rikitake, T. (1982),Earthquake Forecasting and Warning, Developments in Earth and Planetary Sciences 03, Center for Academic Publications Japan/Tokyo (D. Reidel Publishing Co., Dordrecht) 402 pp.

    Google Scholar 

  • Roeloffs, E. andRudnicki, J. W. (1985),Coupled deformaton-diffusion effects on water-level changes due to propagating creep events. Pure and Appl. Geophys.122, 560–582.

    Google Scholar 

  • Roeloffs, E. andBredehoeft, J. D. (1985),Coseismic response of water wells near Parkfield, California, to the August 4, 1985 North Kettleman Hills earthquake, (abstract) EOS. Trans. Am. Geophys. Union66, 986.

    Google Scholar 

  • Roeloffs, E. andRudnicki, J. W. (1986),The effect of fault plane impermeability on pore pressure changes induced by propagating creep events (abstract) EOS. Trans. Am. Geophys. Union67, 272.

    Google Scholar 

  • Sadovsky, M. A., Monakhov, F. I., Kissin, I. G. andShirokov, B. D. (1979),Short-term hydrogeodynamic precursors of earthquakes, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Savage, J. C. (1971),A theory of creep waves propagating along a transform fault. J. Geophys. Res.76, 1954–1966.

    Google Scholar 

  • Scholz, C. H. (1977),A physical interpretation of the Haicheng earthquake prediction. Nature267, 121–124.

    Google Scholar 

  • Schwartz, D. P., Coppersmith, K. J. andSwan, F. H. (1984),Methods for estimating maximum earthquake magnitudes, inProceedings of the Eighth World Conference on Earthquake Engineering. Volum I (Prentice-Hall, New Jersey) 279–285.

    Google Scholar 

  • Shimazaki, K. andSomerville, P. (1978),Summary of the static and dynamic parameters of the Izu-Oshima-Kinkai earthquake of January 14, 1978. Bull. Earthquake Research Institute, Tokyo University53, 613.

    Google Scholar 

  • Shimazaki, K. (1987),Intermediate-term earthquake precursors: Case histories in the Izu Peninsula, Japan. This volume.

  • Sidorenko, A. V., Sadovsky, M. A., Nersesov, I. L., Popov, E. A., andSoloviev, S. L. (1979),Soviet experience in earthquake prediction in the USSR and the prospects for its development, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Simpson, D. W. (1979),Soviet prediction of a major earthquake. Earthquake Information Bulletin11, 234–235.

    Google Scholar 

  • Stuart, W. D., Archuleta, R. J. andLindh, A. G. (1985),Forecast model for moderate earthquakes near Parkfield, California. J. Geophys. Res.90, 592–604.

    Google Scholar 

  • Talwani, P. andVan Nieuwenhuise, R. E. (1980),Water level and geochemical anomalies at Lake Jocassee, South Carolina, EOS. Trans. Am. Geophys. Union61, p. 1035.

    Google Scholar 

  • Toksoz, M. N. (1979),Field investigation and precursors of the 6 September 1975 and 24 November 1976 earthquakes in Turkey, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Tullis, T. E. (1987),Rock friction constitutive behavior from laboratory experiments and its implications for an earthquake prediction field monitoring program. This volume.

  • Van der Kamp, G. andGale, J. E. (1983),Theory of earth tide and barometric effects in porous formations with compressible grains. Water Resources Research19, 538–544.

    Google Scholar 

  • Vorhis, R. C. (1968),Effects outside Alaska, inThe Great Alaska Earthquake of 1964: Hydrology, Part A. (National Academy of Sciences, 1968.)

  • Wakita, H. (1975),Water wells as possible indicators of tectonic strain, Science189, 553–555.

    Google Scholar 

  • Wakita, H. (1981),Precursory changes in groundwater prior to the 1978 Izu-Oshima-Kinkai earthquake, inEarthquake Prediction: An International Review. Maurice Ewing Series 4 (D. W. Simpson and P. G. Richards, eds.) (American Geophysical Union).

  • Wallace, R. E. andTeng, T.-L. (1980),Prediction of the Sungpan-Pingwu earthquakes, August 1976. Bull. Seismol. Soc. Am.70, 1199–1223.

    Google Scholar 

  • Wang, C.-M., Wang, Y.-L., Zhang, H.-P., Li, Y. andZhao, S. (1979),Characteristics of water-level variations in deep wells before and after the Tangshan earthquake of 1976, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Wang, C. M. (1985),Ground-water studies for earthquake prediction in China. Pure and Applied Geophys.122, 215–217.

    Google Scholar 

  • Wang, C.-M., andWu, F. T. (1986),Groundwater water level changes and earthquakes in China, in Wu, F. T., and Teng, T-L. Final Report to the U. S. Geological Survey on Cooperative Earthquake Prediction Research with Institute of Geophysics, SSB, PRC.

  • Wang, L.-C. andLi, S.-Y. (1979),Study of the phenomena and mechanism of the pre-earthquake stimulation of oil and water wells, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Whitcomb, J. H., Garmany, J. D. andAnderson, D. L. (1973),Earthquake prediction: Variation of seismic velocities before the San Fernando earthquake. Science180, 632–635.

    Google Scholar 

  • Wesson, R. L. (1981),Interpretation of changes in water level accompanying fault creep and implications for earthquake prediction. J. Geophys. Res.86, 9259–9267.

    Google Scholar 

  • Wu, F. T., Han, D. andZheng, Z. (1984),Filtration of short baseline and water level data before and after the Tangshan earthquake, inA Collection of Papers of the International Symposium on Continental Seismicity and Earthquake Prediction, Seismological Press, Beijing, China, 549–570.

    Google Scholar 

  • Wyss, M. (1979),Estimating maximum expectable magnitude of earthquakes from fault dimensions. Geology7, 336–340.

    Google Scholar 

  • Zhang, Y-Z. (1982),On the anomalous land uplift and aseismic creep prior to the 1976 Tangshan earthquake. Tectonophysics85, 107–121.

    Google Scholar 

  • Zhang andQiuo (1979), An analysis of the process of preparation and the medium-term precursors of the 1976 Tangshan earthquake, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

  • Zhu, F.-M. andZhong, Y.-Z. (1979),Anomalous macroscopic phenomena and their significance in the prediction of strong earthquakes, inEarthquake Prediction. Proceedings of the International (UNESCO) Symposium on Earthquake Prediction, 1979, Paris, France.

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Roeloffs, E.A. Hydrologic precursors to earthquakes: A review. PAGEOPH 126, 177–209 (1988). https://doi.org/10.1007/BF00878996

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