1887

Abstract

Permeability of aquifers is a key parameter for geothermal doublet performance. Commonly it is assumed that porosity is marked by a decrease with depth of the aquifer as a result of mechanical compaction. Burial depth should therefore be used in the spati

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/content/papers/10.3997/2214-4609.20144161
2011-11-08
2022-11-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144161
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