长江上游山地土壤的粘土矿物组成特征
文献类型：期刊论文
| 作者 | 何毓蓉1; 佐藤幸夫2 |
| 刊名 | 山地研究
 |
| 出版日期 | 1993 |
| 卷号 | 11期号:4页码:241-245;280 |
| ISSN号 | 1000-002X |
| 关键词 | 长江上游 山地土壤 粘土矿物 土壤结构 |
| 其他题名 | FEATURES OF CLAY MINERALS IN MOUNTAIN SOILS AT THE UPPER REACHES OF THE CHANGJIANG RIVER |
| 通讯作者 | 何毓蓉 |
| 中文摘要 | 以X射线衍射分析,研究了长江上游山地土壤的粘土矿物组成。根据土壤粘土矿物组成分类,划分了粘土矿物地带。采用土壤结构恢复试验,比较了不同粘土矿物组成土壤的结构形成特征。 |
| 英文摘要 | Utilizing the method of X-ray diffraction analysis,in detail,dealed with the composition of soil clay minerals of the mountain soil vertical zonality in. the mountain area of the Changjiang River. There were 4 types of soil clay minerals make-up, i. e. . 1. hydromica, kaolinite, chlorite; 2. hydromica, kaolinite, vermiculite; 3. hydromica,kaolinite; 4, unclear principal composition of clay minerals. The distribution-zonality of yellow-brown soils regarded as the boundary line (at the altitude of about 2000m),the zonalities could be divided. Above the line,the zonality of soil clay minerals is that of hydromica, kaolinite, and chlorite (below it,belongs to that of hydromica, kaolinite and vermiculite.To constrast the genesis characters of soil structure among the soils made of different clay minerals, the simulation experiment on soil structure recovery had been done. The soil micro-structure with soil clay minerals mainly consisting of hydromica (kaolinite), vermiculite is the best,and its recovering capabality is the strongest,too. |
| 学科主题 | 土壤学 |
| 收录类别 | CSCD ; 北大中文核心 |
| 语种 | 中文 |
| CSCD记录号 | CSCD:213210 |
| 公开日期 | 2011-08-09 |
| 源URL | [http://192.168.143.20:8080/handle/131551/3330]  |
| 专题 | 成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前） |
| 作者单位 | 1.中国科学院、水利部成都山地灾害与环境研究所 2.日本千叶大学园艺学部 |
| 推荐引用方式 GB/T 7714 | 何毓蓉,佐藤幸夫. 长江上游山地土壤的粘土矿物组成特征[J]. 山地研究,1993,11(4):241-245;280. |
| APA | 何毓蓉,&佐藤幸夫.(1993).长江上游山地土壤的粘土矿物组成特征.山地研究,11(4),241-245;280. |
| MLA | 何毓蓉,et al."长江上游山地土壤的粘土矿物组成特征".山地研究 11.4(1993):241-245;280. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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