1) Chengdu clay
成都粘土
1.
In order to study the genetic mechanism of Chengdu clay, the authors made analysis on the characteristics of Chengdu clay, such as distribution, structure, mineral constituent and so on, and objectively interpreted the essence of Chengdu clay in this paper on the basis of the studies on Chengdu clay in past decades.
为了解成都粘土的成因机制 ,在总结前人资料的基础上 ,从分析成都粘土的分布、结构、矿物组成等特征入手 ,客观地展示了成都粘土的本质 ,进而将其与我国北方的马兰黄土和长江中下游的下蜀粘土之间的特性进行比较以及对龙门山和成都平原的第四纪晚更新世的古环境的分析 ,最终得出典型的成都粘土的成因是属于风成“黄土”的结
2.
The eastern section of Chengdu ring road, which is 20 km long, is located at Chengdu clay region.
成都外环路高速公路东半环超过有 2 0km的路段处在成都粘土分布区 ,针对成都粘土的易滑性 ,本文提出了全封闭的浆砌片石护坡 ,土钉墙 ,非全封闭的锚杆框架护坡 ,钢纤维混凝土喷锚全封闭护坡 ,重力式挡土墙等五种方法处理成都粘土路堑边坡工程 ,施工实践表明 ,这些方法行之有效 ,在该类土的边坡防护中值得推广。
3.
This paper simply introduces the extension project of Chengdu East Railway Station, the harm of Chengdu clay on constructions (such as subgrade), and the reaction between lime and soil.
介绍了成都东站扩建工程的概况，成都粘土对工程结构物（路基）的危害，分析了石灰与土的反应机理。
2) Chengdu red clay
成都红土
3) clay component
粘土成分
1.
Based on analysis of heavy minerals, detrital components of gravel - bearing coarse fragments, maturity of minerals and clay components of mudstones, it is believed that Jurassic would have sourced mainly from two directions, which are the southern Kuluke Mountain and the western Tashidian area respectively.
通过对该区重矿物、含砾粗碎屑组分、矿物成熟度及泥岩粘土成分等的分析,认为该区侏罗系存在两个主要的物源方向,一个来自南部库鲁克山,另一个来自西部的塔什店地区。
5) aeolian clay
风成粘土
6) marine clay
海成粘土
补充资料：成都社会大学是民盟成都市委主办的一所民办大学
成都社会大学是民盟成都市委主办的一所民办大学
梦 成都社会大学是民盟成 都市委主办的一所民办 大学胡文琪供稿
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