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[1]XU Jingjing,DU Pengfei,QU Liqin,et al.Sediment Sources in Watersheds with Various Areas in Transitional Region from Plateau to Plain[J].Research of Soil and Water Conservation,2021,28(06):39-45.
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Sediment Sources in Watersheds with Various Areas in Transitional Region from Plateau to Plain

References:
[1] Poesen J. Soil erosion in the Anthropocene: research needs[J]. Earth Surface Processes and Landforms,2017,43(1):64-84.
[2] Wood P J,Armitage P D. Biological effects of fine sediment in the lotic environment[J]. Environmental Management,1997,21(2):203-217.
[3] 南秋菊,华珞.国内外土壤侵蚀研究进展[J].首都师范大学学报:自然科学版,2003,24(2):86-95.
[4] Walling D E,Webb B W,Russell M A. Sediment-associated nutrient transport in UK rivers[J]. Freshwater Contamination,1990,243:69-81.
[5] 曹文洪,刘冰.应用指纹识别方法确定泥沙来源研究进展[J].中国水利水电科学研究院学报,2018,16(5):353-361.
[6] 周慧平,常维娜,张龙江.基于泥沙指纹识别的小流域颗粒态磷来源解析[J].农业工程学报,2015,31(13):251-256.
[7] 金一鸣,杨建英,王志明,等.冀北接坝山区风场特征与风蚀沙埋分布的关系[J].水土保持通报,2016,36(2):32-37.
[8] 郭雨华,赵廷宁,孙保平,等.河北丰宁小坝子乡土地沙化成因分析及对策研究[J].水土保持应用技术,2006,26(4):18-20.
[9] 冯长红.冀北接坝山区沙化土地动态与生态工程模式研究[D].北京:北京林业大学,2010.
[10] 刘玲,赵廷宁,郑文龙,等.基于GIS的冀北接坝山地地形特征数值研究[J].中国水土保持,2011,32(11):49-51.
[11] 文安邦,张信宝,Walling D.黄土丘陵区小流域泥沙来源及其动态变化137Cs法研究[J].地理学报,1998,53(S1):124-133.
[12] 杨明义,徐龙江.黄土高原小流域泥沙来源的复合指纹识别法分析[J].水土保持学报,2010,24(2):30-34.
[13] 陈方鑫,张含玉,方怒放,等.利用两种指纹因子判别小流域泥沙来源[J].水科学进展,2016,27(6):867-875.
[14] 赵恬茵.复合指纹识别法研究黄土高原小流域泥沙来源[D].陕西杨凌:西北农林科技大学,2017.
[15] 张加琼,刘章,杨明义,等.黄土高原水蚀风蚀交错带坡面土壤侵蚀特征及其影响因素[J].水土保持研究,2018,25(1):1-6,22.
[16] 张信宝,汪阳春,李少龙,等.蒋家沟流域土壤侵蚀及泥石流细粒物质来源的137Cs法初步研究[J].中国水土保持,1992,13(2):32-35,66.
[17] 张信宝,贺秀斌,文安邦,等.川中丘陵区小流域泥沙来源的137Cs和210Pb双同位素法研究[J].科学通报,2004,49(15):1537-1541.
[18] 文安邦,张信宝,王玉宽,等.长江上游137Cs法土壤侵蚀量研究[J].水土保持学报,2002,16(6):1-3.
[19] 郭进,文安邦,严冬春,等.复合指纹识别技术定量示踪流域泥沙来源[J].农业工程学报,2014,30(2):94-104.
[20] 程倩云,彭韬,张信宝,等.西南喀斯特小流域地表、地下河流细粒泥沙来源的137Cs和磁化率双指纹示踪研究[J].水土保持学报,2019,33(2):140-145,154.
[21] Huang D,Du P,Wang J,et al. Using reservoir deposits to quantify the source contributions to the sediment yield in the Black Soil Region,Northeast China,based on the fingerprinting technique[J]. Geomorphology,2019,339:1-18.
[22] 林金石,黄炎和,张旭斌,等.南方花岗岩区典型崩岗侵蚀产沙来源分析[J].水土保持学报,2012,26(3):53-57.
[23] 周曼,林嘉辉,黄炎和,等.复合指纹法分析红壤区强度开发小流域泥沙来源[J].水土保持学报,2019,33(1):20-24.
[24] Collins A L,Walling D E,Leeks G J L. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique[J]. Catena,1997,29(1):1-27.
[25] 杜鹏飞,黄东浩,秦伟,等.基于不同模型不同指纹因子的东北黑土区小流域泥沙来源分析[J].水土保持学报,2020,34(1):84-91.
[26] Du P,Huang D,Ning D,et al. Application of Bayesian model and discriminant function analysis to the estimation of sediment source contributions[J]. International Journal of Sediment Research,2019,34(6):577-590.
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