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| 贵州茂兰峰丛草地洼地小流域侵蚀产沙的137Cs法研究 | |
| 引用本文： | 何永彬,李豪,张信宝,严冬春,文安邦.贵州茂兰峰丛草地洼地小流域侵蚀产沙的137Cs法研究[J].中国岩溶,2009,28(2):181-188. |
| 作者姓名： | 何永彬 李豪 张信宝 严冬春 文安邦 |
| 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,四川,成都,610041;中国科学院研究生院,北京,100049 2. 中国科学院、水利部成都山地灾害与环境研究所,四川,成都,610041;中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,陕西,西安,710075 3. 中国科学院、水利部成都山地灾害与环境研究所,四川,成都,610041 |
| 基金项目： | 国家重点基础研究发展规划(973计划)，中国科学院知识创新工程项目，中国科学院水土保持研究所国家重点实验室基金 |
| 摘 要： | 在贵州茂兰峰丛洼地区的工程碑草地洼地典型小流域进行了洼地沉积泥沙^137Cs示踪分析研究。研究结果表明：（1）草地洼地土壤剖面属于堆积土壤剖面,土壤剖面中^137Cs浓度分布特征反映了泥沙堆积与表层土壤侵蚀的信息。受岩土分布、微地形的影响,^137Cs初始沉降后出现不均匀再分布,面积活度的空间变化较大,变异系数为1.35,不能表征土壤侵蚀状况。（2）根据草地洼地典型堆积农耕地土壤剖面A-1的^137Cs浓度分布特征,1963年以来的流域平均堆积泥沙数量是16.6t/km^2.a,流域平均土壤侵蚀速率为45.95t/km^2.a,约占侵蚀产沙数量63.88%的泥沙以地下流失的形式散失;（3）草地洼地小流域内地面土壤流失与地下土壤流失的相对贡献率分别是70.13%和29.87%;（4）以茂兰地区最大成土速率为依据推算出的允许土壤侵蚀量是13.51t/km^2.a,草地洼地的土壤侵蚀危险程度极高。 |
| 关 键 词： | 137Cs含量 堆积剖面 草地小流域 侵蚀产沙 喀斯特峰丛洼地 茂兰 贵州 |
| 收稿时间： | 2008/12/21 0:00:00 |
137Cs method study on soil erosion and sediment yield in grass-covered peak cluster depression in Maolan, Guizhou |
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| HE Yong-bin,LI Hao,ZHANG Xin-bao,YAN Dong-chun and WEN An-bang.137Cs method study on soil erosion and sediment yield in grass-covered peak cluster depression in Maolan, Guizhou[J].Carsologica Sinica,2009,28(2):181-188. | |
| Authors: | HE Yong-bin LI Hao ZHANG Xin-bao YAN Dong-chun and WEN An-bang |
| Institution: | HE Yong-bin, LI Hao,ZHANG Xin-bao,YAN Dong-chun, WEN An-bang (1. Institute of Mountain Hazards and Environment, CAS , Chengdu , S hichuan 610041 ,China 2. State Key Laboratory of Loess and Quaternary Geology , Institute of Earth Environment, CAS , Xi＇an, Shanxi 710075, China; 3. Graduate School, CAS , Beijing 100049 ,China) |
| Abstract: | Sand and clay sediments are studied by means of 137 Cs tracing test in typical grass-covered peak cluster depression in Maolan, southern Guizhou. It proves that:The grass-covered soil profile in depression is formed by accumulation, and the 137 Cs concentration variation with the depth of the profile reflects the information of sediment accumulation and surface soil erosion. Affected by earth-rock distribution and micro topography, the spatial redistribution of the 137 Cs after primary fallout is uneven, and 137 Cs inventories occurs greater spatial variation with the variation coefficient being 1.35, which shows that the 137 Cs inventory can not characterize the status of soil erosion.According to the 137 Cs concentration distribution along a typical profile A-1 , the sediment accumulation rate and the natural surface soil erosion rate are respectively 16.6 t/km2*a and 45.95 t/km2*a, which shows that about 63.88% of the eroded surface soil is removed by way of underground loss. The relative contribution ratio of surface soil loss and underground soil loss are respectively 70.13% and 29.87%.By comparison to the utmost soil formation rate 13.51 t/km2*a in Maolan, the risk of soil erosion in the Engineering Monument grass-covered depression is higher. |
| Keywords: | 137 Cs content accumulated profile grassland small catchment soil erosion and sediment yield peak cluster depression Maolan Guizhou |
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