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贵州施秉白云岩溶蚀特性及孔隙特征实验研究
  • ISSN号:1006-3021
  • 期刊名称:地球学报
  • 时间:2015.7.15
  • 页码:413-418
  • 分类:K171[历史地理—历史学;历史地理—世界史] P595[天文地球—地球化学;天文地球—地质学]
  • 作者机构:[1]同济大学土木工程学院地下建筑与工程系,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
  • 相关基金:国家自然科学基金资助项目(41302220,41201565);国家重点基础研究发展计划(973)项目(2013CB036001)
  • 相关项目:西南典型岩溶区石漠化综合治理对岩溶作用的影响机制及其碳汇效应-以贵州花江为例
中文摘要:

不同等级石漠化地区岩体和土体中化学元素有较大的差异,表现在石漠化演化过程中不断被改变,化学元素的差异性对石漠化等级差异性的形成有着内在的关联性。文章以贵州贞丰-关岭花江石漠化治理示范区为研究区,选取11处样地的岩石样和土样,对其进行室内实验分析,以了解该地区岩石和土壤的化学元素含量,从而研究其含量的差异性与石漠化等级之间的关系。结果显示:1岩体中CaO/MgO的值越大,Rb/Sr值越低,石漠化等级越高。2在碳酸盐母岩逐渐溶蚀和风化成土的过程中,岩体中Ca、Mg离子被带走,导致成土后土体中Ca、Mg离子含量降低,但强度石漠化地区的土体中Mg离子含量却增加。3不同等级石漠化地区的样品化学元素流失和富集的程度略有差异,一般强度和潜在石漠化地区(离子)含量要高于轻度和中度石漠化地区。4土体中Rb/Sr值越大,石漠化等级越强。该研究可以为示范区的水土流失及石漠化治理提供理论和实践依据。

英文摘要:

The Zhenfeng-Guanling--Huajiang rock desertification demonstration area is a typical karst canyon in Guizhou, where the water and soil losses are serious and many places have suffered from intense rocky desertification. In order to study the intensity and diversity of rocky desertification in the area, llrock and soil samples from the 11 quadrats in the demonstration were collected and their chemical compositions were analysed. The results show that, (1) When the ratio of CaO/MgO in rock is larger and ratio of Rb/Sr is lower, the level of rocky desertification is higher. It means the strength of rocky desertification increases with the ratio of CaO/MgO increasing, and reduces with the ratio of Rb/Sr increases. (2) In the process of carbonate rock dissolution and weathering into the soil, Ca and Mg ions in rocks are taken away. As a result,their contentsin the rock are accordingly reduces, while the content of Mg ion in soil increases in intense rocky desertification areas. (3) The degree of chemical element loss and concen tration has slightly differences in different rocky desertification areas. Generally the content instrong and potential rocky desertification area are higher than the mild and moderate rocky desertification area. (4) The ratio of Rb/Sr in the soil is higher, the degree of rocky desertification is more intense, that is the ratio of Rb/Sr increases with the in tensity of growing rocky desertification. According to the different chemical elements in different rock desertification areas, this work studies the mechanism of water and soil loss in this area, which provides theoretical and practical ba sis for research of the water and soil loss and rocky desertification control in the demonstration area.

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期刊信息
  • 《地球学报》
  • 北大核心期刊(2011版)
  • 主管单位:国土资源部
  • 主办单位:中国地质科学院
  • 主编:董树文
  • 地址:北京市西城区百万庄大街26号
  • 邮编:100037
  • 邮箱:cagsb@qq.com
  • 电话:010-68992351
  • 国际标准刊号:ISSN:1006-3021
  • 国内统一刊号:ISSN:11-3474/P
  • 邮发代号:82-53
  • 获奖情况:
  • 中国精品科技期刊,SCI总被引频次100以上中国期刊...
  • 国内外数据库收录:
  • 美国化学文摘(网络版),波兰哥白尼索引,荷兰文摘与引文数据库,美国工程索引,美国地质文献预评数据库,美国剑桥科学文摘,英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:13049