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Temperature and Composition Changes

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Part of the book series: Lecture Notes in Earth Sciences ((LNEARTH,volume 114))

Abstract

Changes in the temperature, odor, and taste of groundwater are probably among the earliest reported changes following earthquakes. These changes may be expected, not only because earthquake-induced groundwater flow is effective in transporting heat and solutes, but because significant amounts of frictional heat could be generated along the displaced fault, which may raise groundwater temperature. Progress in our understanding of these processes, however, has been slow, largely because relevant quantitative data are scarce. Systematic measurements of earthquake-induced changes in temperature and composition started only in the late twentieth century. Continuous recording of temperature has become available in a limited number of wells and springs. Composition records are even fewer because most measurements require discrete sampling of water and expensive and time-consuming laboratory analysis. Another complication for the temperature and composition data is that the measured values may depend strongly on the proximity of the point of measurement from hydraulically conductive fractures (e.g., Barton et al., 1995).

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Correspondence to Chi-Yuen Wang .

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Wang, CY., Manga, M. (2010). Temperature and Composition Changes. In: Earthquakes and Water. Lecture Notes in Earth Sciences, vol 114. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-00810-8_6

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