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O2流体对岩屑长石砂岩的改造作用实验研究

he experiment of debris-arkosic sandstone reformation by the CO2 fluid

中文摘要英文摘要

通过密闭容器中CO2-H2O-砂岩体系的相互作用实验,研究了不同温度和压力下CO2流体对岩屑长石砂岩的改造作用。反应后溶液中总矿化度的变化、样品的质量损失及扫描电子显微镜(SEM)的观察结果表明,长石、方解石和石英的溶蚀强度随着温度的升高逐渐增大,CO2对砂岩的溶蚀作用与温度正相关。同时,扫描电镜观察发现,在200℃和300℃时样品表面均有一种未知的铝硅酸盐矿物生成,并通过反应液的pH值及各种离子浓度的变化解释了新矿物生成的原因。

he reformation of debris-arkosic sandstone by the CO2 fluid is researched at different temperature and pressures by interaction experiments of the CO2/H2O/sandstone system in inclosed container. The results of the total mineralization degree of reaction liquid, the loss of sample weight after reaction and Scanning Electronic Microscope (SEM), indicate that the corrosion intensity of felspar, calcite and quartz gradually enhance with the temperature increasing, the corrosion of sandstone dissolved by CO2 has positive correlation to the temperature. At the same time, the observation of SEM find that a kind of unknown silicate mineral generates on the surface of sample at 200 ℃and 300 ℃, and the genesis of this new mineral is explaned by the pH of reaction liquid and the variation of ionic density.

刘立、胡大千、马瑞、陈雪、曲希玉

地质学

O2,岩屑长石砂岩,水热实验,溶解,沉淀

O2 debris-arkosic sandstone hydrothermal experiment solution precipitation

刘立,胡大千,马瑞,陈雪,曲希玉.O2流体对岩屑长石砂岩的改造作用实验研究[EB/OL].(2008-04-17)[2025-08-10].http://www.paper.edu.cn/releasepaper/content/200804-652.点此复制

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