Soilerosionratesandcharacteristicsoftypicalalpinemeadowusing137CstechniqueinQinghai-TibetPlateau

被引:0
作者
SHAO QuanQin XIAO Tong LIU JiYuan QI YongQing Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China Graduate University of Chinese Academy of Sciences Beijing China Center for Agricultural Resources Research Institute of Genetics and Developmental Biology Chinese Academy of Sciences Shijiazhuang China [1 ,1 ,2 ,1 ,3 ,1 ,100101 ,2 ,100049 ,3 ,50021 ]
机构
关键词
three Rivers headwater; soil erosion; alpine meadow; ~137Cs nuclide tracing;
D O I
暂无
中图分类号
S812.2 [草原土壤学];
学科分类号
0713 ;
摘要
Alpine meadow is the predominant ecosystem in Qinghai-Tibet Plateau.The firm turf of alpine meadow formed by sub-surface anfractuous roots can be effective in conserving water and soil.Alpine meadow is a primary contributor to the Chinese Water Tower.For quantitative assess anti-erosion ability of alpine meadow,this paper selected three typical meadow slopes with>60% vegetation coverage to evaluate soil erosion rates using 137Cs.The results showed that(1)soil erosion intensity of typical alpine meadow was slight to light.Erosion rates were 464 t km–2 a–1 in Malong Village,415 t km–2 a–1 in Yeniugou Town and 875 t km–2 a–1 in Zhenqin Town respectively;(2)soil erosion rates were correlated negatively with vegetation coverage,and the relationship was clearer at the slope scale than plot scale;(3)the relationship between soil erosion and vegetation coverage showed that vegetation coverage was a predominant factor in retaining soil and water on slopes.With complete turf and high vegetation coverage, alpine meadow was of great significance for soil conservation and prevention of soil erosion.
引用
收藏
页码:1708 / 1713
页数:6
相关论文
共 20 条
[1]   30年来青海三江源生态系统格局和空间结构动态变化 [J].
徐新良 ;
刘纪远 ;
邵全琴 ;
樊江文 .
地理研究, 2008, (04) :829-838+974
[2]  
Using 137Cs tracing technique to estimate wind erosion rates in the typical steppe region, northern Mongolian Plateau[J]. QI YongQing1, LIU JiYuan1, SHI HuaDing1,2, HU YunFeng1 & ZHUANG DaFang1 1 Institute of Geographic Sciences and Resources Research, Chinese Academy of Sciences, Beijing 100101, China;2 Chinese Research Academy of Environmental Sciences, Beijing 100012, China.Chinese Science Bulletin. 2008(09)
[3]  
Estimation of wind erosion rates by using 137Cs tracing technique:A case study in Tariat-Xilin Gol transect, Mongolian Plateau[J]. LIU JiYuan1, QI YongQing1, SHI HuaDing1,2, ZHUANG DaFang1 & HU YunFeng1? 1 Institute of Geographic Sciences and Resources Research, Chinese Academy of Sciences, Beijing 100101, China;2 Chinese Research Academy of Environmental Sciences, Beijing 100012, China.Chinese Science Bulletin. 2008(05)
[4]   137Cs示踪法研究青藏高原草甸土的土壤侵蚀 [J].
李元寿 ;
王根绪 ;
王军德 ;
王一博 ;
吴青柏 .
山地学报, 2007, (01) :114-121
[5]   无侵蚀非农耕地土壤137Cs深度分布入渗过程模型 [J].
伏介雄 ;
张信宝 ;
齐永青 ;
贺秀斌 ;
文安邦 .
核技术, 2006, (03) :189-193
[6]   中国137Cs本底值区域分布研究 [J].
齐永青 ;
张信宝 ;
贺秀斌 ;
文安邦 ;
伏介雄 .
核技术, 2006, (01) :42-50
[7]   137Cs示踪技术研究坡耕地黑土侵蚀和沉积特征 [J].
方华军 ;
杨学明 ;
张晓平 ;
梁爱珍 .
生态学报, 2005, (06) :1376-1382
[8]  
Distribution characteristics of 137Cs in wind-eroded soil profile and its use in estimating wind erosion modulus[J]. HU Yunfeng, LIU Jiyuan, ZHUANG Dafang, CAO Hongxia,YAN Huimin & YANG Fengting Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China Correspondence should be addressed to Liu Jiyuan (email:liujy@ igsnrr.ac.cn).Chinese Science Bulletin. 2005(11)
[9]   Cs示踪红壤丘陵区坡地土壤侵蚀的研究——以江西丰城市为例 [J].
濮励杰 ;
赵姚阳 ;
金平华 ;
王金磊 ;
黄贤金 ;
不详 .
长江流域资源与环境 , 2004, (06) :562-567
[10]   137Cs在黄土高原地区土壤侵蚀示踪中的应用研究 [J].
李仁英 ;
杨浩 ;
赵晓光 ;
唐翔宇 .
土壤, 2004, (01) :96-98