水-岩相互作用研究的回顾与展望

沈照理; 王焰新

水-岩相互作用研究的回顾与展望

沈照理^1,,
王焰新²

1.
中国地质大学水资源与环境工程系, 北京 100083
2.
中国地质大学工程学院, 湖北武汉 430074

基金项目:

国家自然科学基金重点项目 49832005

详细信息

作者简介:
沈照理(1932 -), 男, 教授, 博士生导师, 1952年毕业于清华大学, 1961年毕业于莫斯科地质勘探学院, 获矿物-地质学副博士学位, 长期从事水文地质和环境工程教学和研究工作.E-mail : envir@cugb.edu.cn

中图分类号: P641
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出版历程
- 收稿日期: 2001-10-12
- 刊出日期: 2002-03-25

Review and Outlook of Water-Rock Interaction Studies

SHEN Zhao-li^1
,,
WANG Yan-xin²

1.
Department of Water Resources and Environmental Engineering, China University of Geosciences, Beijing 100083
2.
Engineering Faculty, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 总结了2 0世纪5 0年代末以来的水-岩相互作用研究历史, 初步划分为3个阶段: 第一阶段, 5 0年代末— 70年代初; 第二阶段, 70年代初— 80年代末; 第三阶段, 80年代末至今.近年来, 环境问题在水-岩相互作用研究中占的比重越来越大, 也使水-岩相互作用研究获得了更大、更持续的发展空间.简要回顾了地下水成因和地壳中水的地球化学循环, 控制水的化学成分的地球化学过程, 以及水-岩相互作用与地质灾害等方面的重大研究成果.认为有望取得创新成果的领域包括: 地下水地质作用及其资源环境效应, 地下水环境演化与全球变化, 和极端条件下的水-岩相互作用研究.
- 水-岩相互作用 /
- 地质流体 /
- 地下水 /
- 水文地质 /
- 环境
Abstract: The history of water rock interaction studies since the 1950s' is divided into three periods: the first (late 1950s' - early 1970s'), the second (early 1970s' - late 1980s') and the third (late 1980s' - present). In recent years, environmental problems become increasingly important for water rock interaction studies and provide more opportunities for the greater and sustainable development of water rock interaction studies. Some important advances in the following aspects are briefly reviewed in this paper: the genesis of groundwaters and the geochemical cycle of water in the earth's crust; geochemical processes controlling the chemical compositions of water, and water rock interaction and geohazards. Perspectives concerning the following research fields where innovative results may occur are discussed: the geological role of groundwaters and the resource environmental effects; groundwater environment evolution and global change; water rock interaction studies under extreme conditions.
- water rock interaction /
- geofluids /
- groundwater /
- hydrogeology /
- environment

HTML全文

图 1 水-岩系统演化过程中分散和富集元素相互关系原则^[10]

A—I为新次生相形成的起点.1.水中元素累积曲线; 2.次生相富集的元素; 3.与岩石接触的水可能进入的带; 4.水—岩相互作用可能结束处

Fig. 1. Principle plot of relationship between disseminated and concentrated elements in evolution of water-rock system

下载: 全尺寸图片幻灯片

图 2 U⁶⁺的DLM模型计算值与吸附实验数据的对比

a.c=4.3×10^-4 mol/L, 实圆点表示第1组实验数据点, 点线表示模型的拟合曲线; b.c=4.3×10^-3 mol/L, 实圆点、上三角形和菱形块分别表示第2、3和4组的实验数据点, 实线、点线和短连线分别表示在这3种实验条件下的模型计算值

Fig. 2. Simulation of U⁶⁺ sorption experimental data with computed values from DLM model

下载: 全尺寸图片幻灯片

表 1 第5、7、10届WRI学术会议的主题和大会发言题目对比

Table 1. Keynote talks and themes of the fifth, the seventh and the tenth WRI symposium

表 2 沉积环境的氧化还原分类^{[12, 13]}

Table 2. Redox conditions of sedimentary environments

表 3 水库区水岩作用的类型及特征^[15]

Table 3. Types and characteristics of water-rock interaction in reservoir areas

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