Reactive transport modeling of the Dixie Valley geothermal area: Insights on flow and geothermometry
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文摘

A reactive transport model of the Dixie Valley geothermal area is presented.

Chemical compositions observed in geothermal springs are accurately reproduced.

Assessment of classical and multicomponent geothermometry.

Classical geothermometers perform best if only conductive cooling is occurring.

Multicomponent geothermometry works well at v > 0.1 m/d and at low fracture reactivity.

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