[1] 李英年,王勤学,古松,等. 高寒植被类型及其植物生产力的监测[J]. 地理学报,2004,59(1):40-48 [2] 周兴民. 中国嵩草草甸[M]. 北京:科学出版社,2001:1-5 [3] 中国植被编辑委员会. 中国植被[M]. 北京:科学出版社,1980 [4] 王启基,李世雄,王文颖,等. 江河源区高山嵩草(Kobresia pygmaea)草甸植物和土壤碳、氮储量对覆被变化的响应[J]. 生态学报,2008,28(3):885-894 [5] 马玉寿,郎百宁,王启基. "黑土型"退化草地研究工作的回顾与展望[J]. 草业科学,1999,16(2):5-9 [6] 刘伟,王启基,王溪,等. 高寒草甸"黑土型"退化草地的成因及生态过程[J].草地学报,1999,7(4):300-307 [7] 李文华,周兴民. 青藏高原生态系统与可持续管理方法[M]. 广东:广东科技出版社,1998:56-101 [8] Yang J P, Ding Y J, Chen R S. Spatial and temporal variations of alpine vegetation cover in the source regions of the Yangtze and Yellow rivers of the Tibetan Plateau from 1982 to 2001[J]. Environmental Geology,2006,50(3):313-322 [9] 刘晓玲. 三江源自然保护区"黑土滩"退化草地调查[J]. 青海师范大学学报:自然科学版,2007(1):93-96 [10] 欧阳志云,王效科,苗鸿. 中国生态环境敏感性及其区域差异规律研究[J]. 生态学报,2000,20(1):10-13 [11] Zhang C L, Zou X Y, Yang P, et al. Wind tunnel test and Cs-137 tracing study on wind erosion of several soils in Tibet[J]. Soil & Tillage Research,2007,94(2):269-282 [12] 刘国华,傅伯杰,陈利顶,等. 中国生态退化的主要类型、特征及分布[J]. 生态学报,2000,20(1):14-20 [13] Wang X D, Zhong X H, Fan J R. Spatial distribution of soil erosion sensitivity on the Tibet Plateau[J]. Pedosphere,2005,15(4):465-472 [14] Wang Y B, Wang G X, Hu H C, et al. Erosion rates evaluated by the Cs-137 technique in the high altitude area of the Qinghai-Tibet plateau of China[J]. Environmental Geology,2008,53(8):1743-1749 [15] 刘敏超,李迪强,温琰茂,等. 三江源地区生态系统水源涵养功能分析及其价值评估[J]. 长江流域资源与环境,2006,15(3):405-408 [16] Wang G X, Wang Y B, Li Y S, et al. Influences of alpine ecosystem responses to climatic change on soil properties on the Qinghai-Tibet Plateau, China[J]. Catena,2007,70(3):506-514 [17] Wang G X, Li Y S, Wang Y B, et al. Effects of permafrost thawing on vegetation and soil carbon pool losses on the Qinghai-Tibet Plateau, China[J]. Geoderma,2008,143(1/2):143-152 [18] Liu J Y, Xu X L, Shao Q Q. Grassland degradation in the "Three-River Headwaters" region, Qinghai Province[J]. Journal of Geographical Sciences,2008,18(3):259-273 [19] Feng J M, Wang T, Qi S Z, et al. Land degradation in the source region of the Yellow River, northeast Qinghai-Xizang Plateau: Classification and evaluation[J]. Environmental Geology,2005,47(4):459-466 [20] Walling D E, Quine T A. Use of Caesium-137 as a tracer of erosion and sedimentation: Handbook for the application of the Caesium-137 technique (U. K. Overseas Development Administration Research Scheme R4579)[M]//Department of Geography, University of Exeter.Exeter,1993:15-34 [21] Zhang X B, Long Y, He X B. A simplified 137Cs transport model for estimating erosion rates in undisturbed soil[J]. Journal of Environmental Radioactivity,2008,99(8):1242-1246 [22] Wei X H, Li S, Yang P, et al. Soil erosion and vegetation succession in alpine Kobresia steppe meadow caused by plateau pika-A case study of Nagqu County, Tibet[J]. Chinese Geographical Science,2007,17(1):75-81 [23] 邵全琴,肖桐,刘纪远,等. 三江源区典型高寒草甸土壤侵蚀的137Cs定量分析[J]. 科学通报,2011,56(13):1019-1025 [24] 蔡晓布,张永青,邵伟. 不同退化程度高寒草原土壤肥力变化特征[J]. 生态学报,2008,28(3):1034-1044 [25] 冯瑞章,周万海,龙瑞军,等. 江河源区不同退化程度高寒草地土壤物理、化学及生物学特征研究[J]. 土壤通报,2010,41(2):263-269 [26] Ammer U, Probstl U, Mossmer E M. Erosion on alpine mountain meadows-a contribution to timely questions of soil protection[J]. Forstwissenschaftliches Centralblatt,1986,105(1):48-59 |