三峡地区侵蚀泥沙的^137Cs法研究
文献类型：期刊论文
| 作者 | 汪阳春 ; 文安邦; 贺秀斌; 张信宝
|
| 刊名 | 水土保持学报
 |
| 出版日期 | 2005 |
| 卷号 | 19期号:2页码:33-36 |
| 关键词 | 三峡地区 侵蚀泥沙 ^137Cs法 侵蚀速率 陡坡耕地 泥沙淤积 侵蚀模数 1989年 60年代 输沙模数 遥感普查 土壤侵蚀 紫色土 坡度 抗蚀性 数量级 滩地 小流域 草地 开县 厚度 黄壤 |
| 其他题名 | Study on Erosion and Sedimentation in Yangtze Three Gorge Region |
| 通讯作者 | 文安邦 |
| 合作状况 | 其它 |
| 中文摘要 | 1989年以来三峡地区开展的侵蚀泥沙^137Cs示踪的初步研究表明：三峡地区紫色土陡坡耕地侵蚀强烈，坡度>25°的坡耕地，侵蚀速率高达7126～9452t／(km^2·a)；黄壤质地粘重，抗蚀性好，坡度29°的陡坡耕地的侵蚀速率仅2509t／(km^2·a)。林草地侵蚀轻微，坡度25°林草地的侵蚀速率为306～688t／(km^2·a)，较坡耕地大致低一个数量级。上世纪60年代以来，开县小江河床上涨强烈，两岸滩地也有淤积发生，淤积厚度10～70cm不等，低滩地泥沙淤积厚度大于高滩地。开县春秋水库小流域输沙模数为1560t／(km^2·a)，由于谷地泥沙淤积极为有限，此值基本可代表该流域的侵蚀模数。全国土壤侵蚀遥感普查公布的川东平行岭谷区侵蚀模数为3000～5000t／(km^2·a)。 |
| 英文摘要 | A study on erosion and sedimentation in the YangtzeThree Gorge Region by using the 137 Cs technique, which has been carried out since 1989, provides valuable information on erosion and sedimentation severities in the region. Erosion is very severe on cultivated purple soils of steep slopes and the erosion rates on the slopes of> 25brange between 7 126 t/ ( km2 #a) and 9 452 t/ ( km2#a) . However, erosion on cultivated yellow soils is not as severe as on the purple soils because of its clayey texture and high erosion resistance. The erosion rate on the slope of 29b is 2 509 t/ ( km2#a) . Erosion is slight on forest and grass slopes and erosion rates on the purple soil slopes of 25b ranges between 306 t/ ( km2#a) and 688 t / ( km2# a) , which are less than one tenth of the rates on the cult ivated slopes. The channel bed of Xiaojiang River in the Kaixian County has risen significantly since 1960s. Sedimentation has also occurred on the flood plains and deposition thicknesses since 1960s range between 10 cm and 70 cm, and the thickness is greater on the lower flood plain than it on the higher plain. The specif ic sediment yield of the small Chunqu Gully Catchment is 1 560 t / ( km2#a) , which may be representative of the average erosion rate over the catchment due to little deposit ion in the gully bottom. The erosion rates of 3 0005 000 t/ ( km 2#a) for the Parallel Mountain Ridge and Valley Region in East Sichuan, announced by the state soil erosion survey using the remote sensing method, may be overestimated. |
| 分类号 | S157 |
| 资助信息 | 中科院知识创新项目 (KZCX3 -SW330 ;42 2 );科技部 973项目 (2 0 0 3CB41 580 2 );国家自然科学基金项目 (40 2 71 0 1 5);国际原子能机构资助项目 (1 2 30 0 /RO) |
| 语种 | 中文 |
| 公开日期 | 2010-07-15 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/755]  |
| 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_山地表生过程与生态调控重点实验室 成都山地灾害与环境研究所_数字山地与遥感应用中心 科技与合作处 |
| 推荐引用方式 GB/T 7714 | 汪阳春,文安邦,贺秀斌,等. 三峡地区侵蚀泥沙的^137Cs法研究[J]. 水土保持学报,2005,19(2):33-36. |
| APA | 汪阳春,文安邦,贺秀斌,&张信宝.(2005).三峡地区侵蚀泥沙的^137Cs法研究.水土保持学报,19(2),33-36. |
| MLA | 汪阳春,et al."三峡地区侵蚀泥沙的^137Cs法研究".水土保持学报 19.2(2005):33-36. |
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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