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首页> 外文会议>Geothermal Resources Council Annual Meeting >Mineralogy and Geochemistry of the Two Hydrothermal Reservoirs in the Los Humeros Geothermal System
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Mineralogy and Geochemistry of the Two Hydrothermal Reservoirs in the Los Humeros Geothermal System

机译：LOS Humeros地热系统中两种热热水库的矿物学和地球化学

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摘要

From the hydrochemical point of view the Los Humeros geothermal field is a complex system. It has been subject of research work in several aspects. A very important conclusion of this work has been to recognize the occurrence of two hydrothermal reservoirs. A shallow liquid rich reservoir with temperatures between 300°C and 340°C and a deep vapor rich reservoir with low liquid saturation and temperature above 300°C and below 380°C. The former is located between 1600 and 1025 masl and the latter between 850 masl and 100 masl. Fluid geochemistry shows the occurrence of a mixture of fluids; in the shallow reservoir fluids are of the bicarbonate type and fluids from the deep reservoir are of the sodium chloride type. Pressure distribution tests and hydrothermal mineralogy have been very useful to confirm the occurrence of two reservoirs in Los Humeros geothermal field.
机译：从水化学的角度来看，Los Humeros地热场是一个复杂的系统。它一直在几个方面的研究工作。这项工作的非常重要的结论是识别出两种水热储层的发生。浅液体富含储层，温度为300°C和340°C，富含液体饱和度低的深蒸汽储层，温度高于300℃，低于380°C。前者位于1600和1025 MasL之间，后者在850 masL和100 masl之间。流体地球化学显示出流体混合物的发生;在浅层储存器中，流体是碳酸氢盐的碳酸氢盐类型，来​​自深层储存器的流体是氯化钠类型。压力分布试验和水热矿物学对于确认LOS Humeros地热场中的两个水库的发生是非常有用的。

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