Book Details
Format
Paperback / Softback
Book Series
Lecture Notes in Earth Sciences
ISBN-10
3642263240
ISBN-13
9783642263248
Edition
2009 ed.
Publisher
Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
Imprint
Springer-Verlag Berlin and Heidelberg GmbH & Co. K
Country of Manufacture
DE
Country of Publication
GB
Publication Date
May 28th, 2012
Print length
225 Pages
Ksh 16,200.00
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Based on the graduate course in Earthquake Hydrology at Berkeley University, this text introduces the basic materials, provides a comprehensive overview of the field to interested readers and beginning researchers, and acts as a convenient reference point.
Distantearthquakesarewellknowntoinduceawiderangeofresponsesinsurface water and groundwater. These responses are often viewed as mere curiositiesas theiroccurrenceislimitedinspaceandtime.Thefrequentemphasisonearthquake precursorsinstudiesofthesephenomenaalsotendstopushthestudyof'earthquake hydrology' away from the mainstream of geoscience. The observed phenomena, however,probetheinteractionbetweenhydrogeologicalprocessesandmechanical deformationintheshallowcrust.Hencetheyprovideinsightintotheinteraction among water cycle, tectonics, and properties of the crust. As such, the study of earthquakehydrologyalsohasthepotentialtoprovideamorequantitativeand- depthunderstandingofthenatureofearthquakeprecursorsandevaluatewhether theyareinfactprecursors. The title of this book re ects the nature of the connections we address: we focus on how earthquakes affect hydrology. Water also in uences earthquakes as it affects the strength of faults and the rheology of rocks. Our emphasis here, however, is not on the hydrology of earthquakes, but on understanding the hydrological phenomena induced or modi ed by earthquakes. The boundary betweenthe'hydrologyofearthquakes'andthe'earthquake-inducedhydrological phenomena', however, can sometimes be blurred. For example, triggered ear- quakes are sometimes explained by a re-distribution of pore pressure following the triggering earthquake. Hence, triggered seismicity may be an example of an earthquake-induced hydrological phenomenon. Thestudyofthelatter,therefore, canbeimportanttowardsabetterunderstandingofthemechanicsofatleastsome earthquakes. Therearemanystudents,postdocsandcolleagueswewishtothankforcolla- ratingonresearchprojectsrelatedtothetopicsreviewedinthisbook,orparticip- inginstimulatingdiscussionsintheclasswetaughtcalled'Earthquakehydrology'. In particular, we wish to thank Emily Brodsky, Yeeping Chia, Douglas Dreger, Shemin Ge, Fu-qiong Huang, Tom Holzer, Chris Huber, Joel Rowland, Martin Saar, Yaolin Shi, Chung-Ho Wang, Kelin Wang, Pei-ling Wang and Alex Wong forenlighteningexchanges.HunterPhilsonhelpedwith guresandtheindex.We v vi Preface alsothanktheNationalScienceFoundation,theMillerInstituteforBasicResearch inScience,andNASAforsupportingtheresearchandsynthesisinthisvolume.
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