| 砒砂岩岩性特征对抗侵蚀性影响分析 |
| |
| 引用本文： | 叶浩,石建省,李向全,侯宏冰,石迎春,程彦培.砒砂岩岩性特征对抗侵蚀性影响分析[J].地球学报,2006,27(2):145-150. |
| |
| 作者姓名： | 叶浩 石建省 李向全 侯宏冰 石迎春 程彦培 |
| |
| 作者单位： | 中国地质科学院水文地质环境地质研究所，石家庄，050061;中国地质科学院水文地质环境地质研究所，石家庄，050061;同济大学地下建筑与工程系，上海，200092;中国地质科学院水文地质环境地质研究所，石家庄，050061;中国地质科学院水文地质环境地质研究所，石家庄，050061;中国地质科学院水文地质环境地质研究所，石家庄，050061 |
| |
| 基金项目： | 中国地质调查局地质调查项目“黄河中下游重大环境地质问题调查评价”(编号:Z321) |
| |
| 摘 要： | 砒砂岩区是黄河中游集中的基岩产沙区,强烈的岩土侵蚀与砒砂岩的岩性密切相关。通过对砒砂岩原状样品的矿物组成、微结构的测试和定量分析表明:砒砂岩中岩石矿物的组成特征是以不稳定、易风化、亲水性强的粘土矿物为主;岩石微结构特征表现为颗粒大小悬殊、排列无序、孔隙发育、胶结物为粘土矿物,影响岩石的物理力学性质,降低了砒砂岩的抗风化、抗侵蚀性能。
|
| 关 键 词： | 砒砂岩 矿物组成 微结构 抗侵蚀性 |
The Effect of Soft Rock Lithology upon Its Anti-erodibility |
| |
| YE Hao,SHI Jian-sheng,LI Xiang-quan,HOU Hong-bing,SHI Ying-chun and CHENG Yan-pei.The Effect of Soft Rock Lithology upon Its Anti-erodibility[J].Acta Geoscientia Sinica,2006,27(2):145-150. |
| |
| Authors: | YE Hao SHI Jian-sheng LI Xiang-quan HOU Hong-bing SHI Ying-chun and CHENG Yan-pei |
| |
| Institution: | Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061;Department of Geotechnical Engineering, Tongji University, Shanghai, 200092;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061 |
| |
| Abstract: | The soft rock area is a major sediments-producing area resulting from bedrock erosion in the middle valley of the Yellow River. Intense rock-soil erosion in this area is closely related to lithology of the soft rock. Mineral composition and microstructures of undisturbed soft rock samples were tested in laboratory to study the effect of soft rock lithology on anti-erodibility. The soft rock is dominated in mineral composition by clay minerals, which are unstable, liable to weathering, and highly hydrophilic. In addition, the microstructure characteristics of the soft rock, such as different grain sizes, unoriented arrangement, high porosity, and clay mineral cements, promote the weathering process. These characteristics have weakened the anti-erodibility of the soft rock. |
| |
| Keywords: | soft rock mineral composition microstructure anti-erodibility |
| 本文献已被 万方数据 等数据库收录！ |
| 点击此处可从《地球学报》浏览原始摘要信息 |
| 点击此处可从《地球学报》下载免费的PDF全文 |
|
