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贵州施秉白云岩溶蚀特性及孔隙特征实验研究

刘琦 顾展飞 卢耀如 刘之葵

地球学报Issue(4):413-418,6.
地球学报Issue(4):413-418,6.DOI:10.3975/cagsb.2015.04.04

贵州施秉白云岩溶蚀特性及孔隙特征实验研究

The Experimental Study of Dolomite Dissolution and Pore Characteristics in Shibing, Guizhou

刘琦 1顾展飞 2卢耀如 1刘之葵2

作者信息

  • 1. 同济大学地下建筑与工程系,上海 200092
  • 2. 教育部城市环境与可持续发展联合研究中心,上海 200092
  • 折叠

摘要

Abstract

With dolomite in Shibing of Guizhou Province as the study object, the authors analyzed its dissolution characteristics and pore characteristics macroscopically and microscopically. Some conclusions have been reached: (1) In many factors that influence the development of Shibing karst, the most fundamental factor is mineral composition, the most critical factor is water, and pore characteristics play a supporting role; (2) The dissolution amount on per unit surface area of superfine grain Shibing dolomite is generally greater than the amount of fine-grained dolomite rock sam-ple. Under the same circumstances of grain dissolution principle, the dissolution amount of dolomite is in positive proportion with CaO and MgO content and the influence of MgO content is larger than that of CaO content. (3) The dissolution rate of Shibing dolomite is not only controlled by particle size of the mineral particles, but also by the internal pore structure characteristics of the rock. The larger the particle size, the higher the porosity, the better the connectivity, the more the beneficial solution seeps into pore, and the greater the amount of dissolution; (4) Dissolution of dolomite is the result of many factors, and all factors must be separated one by one to make a detailed analysis from the macroscopic and microscopic view. On such a basis, more information about the regularity of the karst development can be obtained through a comprehensive study.

关键词

贵州施秉/白云岩/溶蚀实验/压汞实验/孔隙特征

Key words

Shibing in Guizhou/dolomite/dissolution experiment/mercury experiment/pore characteristics

分类

天文与地球科学

引用本文复制引用

刘琦,顾展飞,卢耀如,刘之葵..贵州施秉白云岩溶蚀特性及孔隙特征实验研究[J].地球学报,2015,(4):413-418,6.

基金项目

本文由国家十二五科技支撑计划重大课题“喀斯特高原峡谷石漠化综合治理技术与示范”(编号:2011BAC09B01)、国家自然科学基金资助项目(编号:41302220 (编号:2011BAC09B01)

41201565)、高等学校博士学科点专项科研基金(编号:20120072120032)和广西自然科学基金创新研究团队项目(编号:2012GXNSFGA060001)联合资助。 (编号:20120072120032)

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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