低温低压下水—岩反应动力学实验中一些主要元素的变化规律
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The Varying Laws of Some Main Elements in the Dynamic Experiments for the Reactions of Rocks with Water Under Low Temperatures and Pressures
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    摘要:

    作者根据北京小汤山一带热、矿泉水文地质特征,把90%的白云岩和10%的花岗岩作为试料,把二次蒸馏水作为反应溶液,将它们一起放在纯钛高压釜内,在50—200℃的温度和(200—50)×10-5Pa的压力下进行水—岩反应动力学的实验。实验结果表明:水从岩石中萃取出的K+, Na+, Ca2+, Mg2+,Al3+,HCO3-,N03-,F-,C1-,SO42-,∑Fe和Si02等离子和氧化物的含量随着岩石的成分、温度、压力、水的pH值、岩石粒度、氧化—还原环境、时间和水的循环次数呈规律性变化。这些规律揭示了小汤山一带热、矿泉形成的机理。为热田的开发和人造温泉提供了理论上的依据。

    Abstract:

    On the basis of the hydrogeological characteristics of hot mineral springs in Xiaotangshan area,Beijing,authors engaged in the experiments of water-rock reaction using dolomite (90%)and granite (10%)as starting materials and quadratic distilled water as reactive solution, which were put into Ti-high pressure vessels under 50-200℃and (200一500)×lO5Pa. The results of experiment showed that the quantites of ions and oxides for K+, Na+, Ca2+, Mg2+,Al3+,HCO3-,N03-,F-,C1-,SO42-,∑Fe and Si02 extracted from the rocks into the solution cange with the variations of rock compositions, temperatures,pressures, pH values of water, grain sizes of rock, redox state, and numbers of time for water cycle etc. These laws brought to light the mechanism of the main elemental change in the formation of hot mineral springs in Xiaotangshan area. Authors provided the oretical evidences for opening up hot fields and man-made hot springs.

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梁祥济,乔 莉,王福生, 1994. 低温低压下水—岩反应动力学实验中一些主要元素的变化规律[J]. 岩石矿物学杂志, 13(1):10~18.
Liang Xiangji, Qiao Li, Wang Fusheng, 1994. The Varying Laws of Some Main Elements in the Dynamic Experiments for the Reactions of Rocks with Water Under Low Temperatures and Pressures[J]. Acta Petrologica et Mineralogica, 13(1): 10~18.

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