Introduction | p. 1 |
References | p. 5 |
Liquefaction | p. 7 |
Introduction | p. 7 |
Observations in the Near Field | p. 9 |
Laboratory Studies | p. 11 |
Cyclic Loading Experiments | p. 14 |
Dissipated Energy for Liquefaction by Undrained Consolidation | p. 15 |
Liquefaction Beyond the Near Field | p. 15 |
Seismic Energy Density as a Metric for Liquefaction Distribution | p. 16 |
Mechanism for Liquefaction Beyond the Near Field | p. 18 |
Experiment at Wildlife Reserve, California | p. 19 |
Dependence of Liquefaction on Seismic Frequency | p. 24 |
Field Observation from Taiwan | p. 24 |
Laboratory Studies | p. 27 |
Numerical Models | p. 28 |
Concluding Remarks | p. 29 |
References | p. 29 |
Mud Volcanoes | p. 33 |
Introduction | p. 33 |
Response of Mud Volcanoes to Earthquakes | p. 34 |
Insights from Triggered Eruptions of Magmatic Volcanoes | p. 35 |
Mechanisms | p. 37 |
Static or Dynamic Stresses? | p. 37 |
Mechanisms for Initiating Eruptions | p. 37 |
Effect of Earthquakes on Already-Erupting Mud Volcanoes | p. 40 |
Concluding Remarks | p. 41 |
References | p. 42 |
Increased Stream Discharge | p. 45 |
Introduction | p. 45 |
Observations | p. 47 |
Characteristics of Increased Discharge | p. 48 |
Recession Analysis | p. 49 |
Estimate Excess Discharge | p. 51 |
Proposed Mechanisms | p. 54 |
Coseismic Elastic Strain | p. 54 |
Enhanced Permeability | p. 54 |
Coseimic Consolidation and Liquefaction | p. 55 |
Debate About Mechanisms | p. 56 |
Geochemical and Temperature Constraints | p. 56 |
Constraints from Multiple Earthquakes | p. 57 |
Constraints from Recession Analysis | p. 58 |
Constraints from Multiple Stream Gauges | p. 59 |
Role of Anisotropic Permeability | p. 59 |
Streamflow Increase in Hydrothermal Areas | p. 61 |
Concluding Remarks | p. 64 |
References | p. 64 |
Groundwater Level Change | p. 67 |
Introduction | p. 67 |
Step-like Changes in the Near Field | p. 70 |
Observations | p. 70 |
Causal Mechanisms | p. 73 |
Sustained Changes in the Intermediate Field | p. 77 |
Observations | p. 77 |
Causal Mechanisms | p. 78 |
Groundwater Oscillations in the Far Field | p. 83 |
Role of S Waves and Love Waves on Groundwater Oscillations | p. 84 |
Pore-Pressure Changes on the Sea Floor | p. 87 |
Postseismic Groundwater Recession | p. 89 |
Recession Analysis | p. 89 |
Interpretation of the Postseismic Recession | p. 91 |
Concluding Remarks | p. 92 |
References | p. 93 |
Temperature and Composition Changes | p. 97 |
Introduction | p. 97 |
Earthquake-Induced Change in Groundwater Temperature | p. 98 |
Hot Springs | p. 98 |
Wells | p. 99 |
Marine Hydrothermal Systems | p. 101 |
Mechanisms | p. 104 |
Earthquake-Induced Changes in Water Composition | p. 106 |
Observations | p. 106 |
Mechanisms | p. 112 |
Concluding Remarks | p. 113 |
References | p. 114 |
Geysers | p. 117 |
Introduction | p. 117 |
Response of Geysers to Earthquakes | p. 117 |
Response of Geysers to Other Sources of Stress | p. 119 |
Mechanisms | p. 120 |
How do Geysers Work? | p. 120 |
Mechanisms for Altering Eruptions | p. 120 |
Concluding Remarks | p. 121 |
References | p. 122 |
Earthquakes Influenced by Water | p. 125 |
Introduction | p. 125 |
Fluids and Rock Failure | p. 125 |
Earthquakes Induced by Fluid Injection and Extraction | p. 127 |
Reservoir-Induced Seismicity | p. 128 |
Natural Hydrological Triggering of Earthquakes | p. 130 |
Earthquake Triggering of Earthquakes via Hydrological Processes | p. 131 |
Concluding Remarks | p. 135 |
References | p. 136 |
Hydrologic Precursors | p. 141 |
Introduction | p. 141 |
What is a Precursor? | p. 143 |
Identifying Hydrologic Precursors | p. 143 |
Examples | p. 145 |
China: Haicheng, 1975 and Tangshan, 1976 | p. 146 |
Kobe, Japan, 1995 | p. 147 |
Nankaido, Japan, 1946 | p. 147 |
Kettleman Hills, California, 1985 | p. 148 |
Chi-Chi, Taiwan, 1999 | p. 148 |
Kamchatka, 1992 | p. 150 |
Pyrenees, France, 1996 | p. 151 |
Reservoir Induced Seismicity, Koyna, India | p. 151 |
Calistoga Geyser, California | p. 154 |
Precursory Changes in Spring Temperature | p. 154 |
Outlook | p. 155 |
References | p. 156 |
Epilogue | p. 161 |
A General Framework | p. 161 |
Directions for Future Research | p. 165 |
References | p. 167 |
Appendices | p. 169 |
Notation | p. 170 |
Basic Equations for Groundwater Flow | p. 171 |
Darcy's law | p. 171 |
Porosity and Permeability | p. 172 |
Elements in a Groundwater System | p. 174 |
Driving Potential | p. 174 |
The Continuum Approach | p. 174 |
Groundwater Flow Equations | p. 174 |
Physical Meaning of the Specific Storage | p. 175 |
Flow Equation for Isotropic Aquifer | p. 175 |
Calculating Permeability from Tidal Response of Groundwater Level | p. 176 |
Equation Derivations | p. 177 |
Groundwater Transport | p. 179 |
Governing Equations for Heat Transport | p. 179 |
Relative Significance of Advective Versus Conductive Heat Transport | p. 180 |
Governing Equations for Solute Transport | p. 180 |
Relative Significance of Advective Versus Diffusive Solute Transport | p. 182 |
Hydromechanical Coupling | p. 182 |
Introduction | p. 182 |
Effective Stress Principle | p. 183 |
Poroelasticity and Hydrodynamic Coupling | p. 184 |
Non-elastic Deformation | p. 187 |
Deformation Under Cyclic Loading | p. 188 |
Data for Hydrologic Responses to Earthquakes | p. 192 |
Stream and Spring Responses | p. 192 |
Groundwater Level Responses | p. 196 |
Hot Spring Responses | p. 208 |
Liquefaction Occurrence During Earthquakes | p. 209 |
Triggered Mud Volcanoes | p. 220 |
Triggered Earthquakes | p. 221 |
Index | p. 223 |
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