四姑娘山区土壤及其垂直分布
文献类型：期刊论文
| 作者 | 郑远昌; 高生淮; 钟祥浩
|
| 刊名 | 山地研究
 |
| 出版日期 | 1988 |
| 卷号 | 6期号:4页码:227-234 |
| 关键词 | 四姑娘山区 土壤 垂直分布 垂直带谱 |
| ISSN号 | 1008-2786 |
| 其他题名 | SOIL IN SIGUNIANG MOUNTAINOUS REGION AND ITS VERTICAL DISTRIBUTION |
| 通讯作者 | 郑远昌 |
| 中文摘要 | 区内土壤型类有:山地黄壤、山地黄棕壤、山地褐土、淋溶褐土、山地棕壤、山地暗棕壤、山地棕色暗针叶林土、亚高山草甸土、高山草甸土和高山寒冻土等。土壤分异的显著特点是:1.土壤垂直带谱结构多样而复杂;2.带谱特性随坡向不同而有差异;3.土壤垂直带内以森林土壤为主;4.区内土壤具过渡性。 |
| 英文摘要 | The Siguniang Mountainous Region is located at the middle-south section of the Qionglai Mountain,and the main mountain body between 30 °50’-31 °40’N and 102°00’ - 103°30’E. In this region, there arc 9 peaks of elevation>5000m, not counting the main peak(Siguniang Mountain at an elevation of 6250m). The mountain is high and valley is deep. The height difference is 3000m and the maximum height is up to 5200m.The Qionglai Mountain is the main one in the north of the Hengduan Mountains. The Siguniang Mountain is the third high peak of the Hengduan Mountainous Region.In this region, bioclimatic conditions vary with the elevation. So the bioc-limatic zone is various.The soil types ara. mountain yellow earth, mountain yellow-brown earth, mountain drab soil, eluvial-drab soil, mountain brown earth, mountain dark-brown, earth,mountain "brown dark coniferous forest soil, subalpine meadow soil, alpine meadow soil and alpine frozen soil, etc.The main characteristics of soil differentiation are.1.The vertical spectral structure :s varied and mixed;2.Spectral characteristics vary with the slope direction;3.The forest soil. is main in the vertical soil zonc;4.The soil is of the features of transition. |
| 语种 | 中文 |
| 公开日期 | 2013-04-27 |
| 源URL | [http://192.168.143.20:8080/handle/131551/5245]  |
| 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） 中国科学院水利部成都山地灾害与环境研究所 |
| 作者单位 | 中国科学院成都山地灾害与环境研究所 |
| 推荐引用方式 GB/T 7714 | 郑远昌,高生淮,钟祥浩. 四姑娘山区土壤及其垂直分布[J]. 山地研究,1988,6(4):227-234. |
| APA | 郑远昌,高生淮,&钟祥浩.(1988).四姑娘山区土壤及其垂直分布.山地研究,6(4),227-234. |
| MLA | 郑远昌,et al."四姑娘山区土壤及其垂直分布".山地研究 6.4(1988):227-234. |
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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