Cation Exchange Geothermometry: A critique

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Cation Exchange Geothermometry: A critique

机译：阳离子交换地热法：一种批评

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The geochemical studies of geothermal systems provide insight into the physiochemical processes responsible for their origin and evolution on the basis of the chemical composition of fluids (separated vapor and water) collected from fumaroles, hot springs and drilled wells. Using chemical geothermometers and the conservation of mass, energy and alkalinity, the chemical concentrations are converted to the reservoir conditions to predict the state of water-rock interaction and reservoir processes like boiling, condensation, mixing with other fluids, mineral dissolution-precipitation, etc. (Verma, 2002).

机译：地热系统的地球化学研究基于从喷气孔，温泉和钻井中收集的流体（分离的蒸气和水）的化学成分，提供了对造成其起源和演化的理化过程的深入了解。使用化学地热仪并保留质量，能量和碱度，将化学浓度转换为储层条件，以预测水-岩石相互作用和储层过程的状态，例如沸腾，冷凝，与其他流体混合，矿物溶解-沉淀等（Verma，2002年）。

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《Geotermia》 |2012年第1期|共5页
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中图分类地热学;
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Cation Exchange Geothermometry: A critique

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