Soil evolution features of debris flow waste-shoal land
文献类型：期刊论文
| 作者 | Cui Peng1,2 ; Ge Yonggang1,2,3; Zhuang Jianqi1,2,3; Wang Daojie1,2,3
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| 刊名 | JOURNAL OF MOUNTAIN SCIENCE
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| 出版日期 | 2009-06-01 |
| 卷号 | 6期号:2页码:181-188 |
| 关键词 | Debris flow waste-shoal land Reclamation mode Utilization time Soil properties Soil microstructure |
| ISSN号 | 1672-6316 |
| 通讯作者 | Peng Cui |
| 合作状况 | 其它 |
| 英文摘要 | The reclamation and utilization of debris flow waste-shoal land plays an important role in the mitigation and control of debris flow hazards, which thus contributes a lot to the exploitation of insufficient land resources in mountainous areas and the reduction of losses caused by debris flow. The aim of this paper is to discuss the features and mechanism of soil evolution of debris flow waste-shoal land so as to search for the available modes of its reclamation and utilization. The Jiangjiagou Ravine, a typical debris flow ravine, was selected to study soil evolution features of debris flow waste-shoal land based on the analysis of soil physicochemical properties and soil microstructure. It was found that the soil evolution rates of debris flow waste-shoal land varied with different modes of reclamation. For the land which had been reclaimed for less than 10 years, soil evolved most rapidly in paddy fields, and more rapidly in dry farmland than in naturally restored waste-shoal land. For the land which had been used for more than 10 years, the soil evolution rates of dry farmland, naturally restored waste-shoal land and paddy farmland decreased in the file. For the same utilization period of time, significant differences were recognized in soil evolution features under different modes of reclamation. Analysis data showed that soil clay content, soil thickness, the psephicity of skeleton particles and contents of microaggregates (< 0.02 mm) in paddy farmland were all highest. Soil nutrients and porosity of dry farmland were better than those of paddy farmland and naturally restored waste-shoal land, and those of paddy farmland were superior to those of naturally restored waste-shoal land. Paddy farmland characterized by rapid pedogenesis, stable evolution and high utilizability was the priority candidate for the reclamation and utilization of debris flow waste -shoal land. |
| WOS标题词 | Science & Technology ; Life Sciences & Biomedicine |
| 类目[WOS] | Environmental Sciences |
| 研究领域[WOS] | Environmental Sciences & Ecology |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000265964200011 |
| 公开日期 | 2010-10-12 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/2132]  |
| 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） 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Mt Hazards & Land Surface Proc, Chengdu 610041, Peoples R China 2.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China 3.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Cui Peng,Ge Yonggang,Zhuang Jianqi,et al. Soil evolution features of debris flow waste-shoal land[J]. JOURNAL OF MOUNTAIN SCIENCE,2009,6(2):181-188. |
| APA | Cui Peng,Ge Yonggang,Zhuang Jianqi,&Wang Daojie.(2009).Soil evolution features of debris flow waste-shoal land.JOURNAL OF MOUNTAIN SCIENCE,6(2),181-188. |
| MLA | Cui Peng,et al."Soil evolution features of debris flow waste-shoal land".JOURNAL OF MOUNTAIN SCIENCE 6.2(2009):181-188. |
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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