PDF Download

[1]WU Yabing,FANG Haiyan,ZHANG Wei,et al.Contribution of Snowmelt Runoff to Sediment Yield in the Black Soil Region of Northeast China and Factor Analysis[J].Research of Soil and Water Conservation,2023,30(03):86-93.[doi:10.13869/j.cnki.rswc.2023.03.053]

Copy

Contribution of Snowmelt Runoff to Sediment Yield in the Black Soil Region of Northeast China and Factor Analysis

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 30 Number of periods: 2023 03 Page number: 86-93 Column: Public date: 2023-04-10

Title:: Contribution of Snowmelt Runoff to Sediment Yield in the Black Soil Region of Northeast China and Factor Analysis

Author(s):: WU Yabing^1,2, FANG Haiyan^2,3, ZHANG Wei¹, WANG Shuo², ZHAI Yuyu^2,3, ZHAO Ziyuan^2,3; (1.School of Geography, Liaoning Normal University, Dalian, Liaoning 116029, China; 2.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3.College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100101, China)

Keywords:: snowmelt; specific sediment yield; catchment; spatial variation; influencing factors

CLC:: S157.1

DOI:: 10.13869/j.cnki.rswc.2023.03.053

Abstract:: [Objective]The aim of this study is to explore the contribution of catchment sediment yield to annual total as well as its main influencing factors, and then to provide scientific support. [Methods] Based on precipitation data from 203 meteorological stations and runoff and sediment data from 15 hydrological stations in northeastern China, the rainfall and snowfall, topographic, climatic, and land use characteristics in the selected catchments were examined, and the annual sediment yield contributions to annual total derived from snowmelt runoff were quantified. The factors influencing catchment runoff and sediment yield during snowmelt period were further analyzed through correlation analysis and multiple regression methods. [Results] Spatially, more snowfall occurred in the southeast and less in the northwest. The annual snowfall amount accounted for 3.8%～24.7% of the annual precipitation. The snowmelt runoff depth accounted for 13.7%～32.5% of the annual totals. The contributions of sediment yield(SY)derived from snowmelt to annual total were 3.8%～23.47%, and the specific sediment yields(SSYs)derived from snowmelt runoff were 3.1%～35.9% of the annual total. Their distributions were disorderly in space. The contribution of snowmelt induced SY was significantly correlated with mean annual precipitation, the ratio of snowfall amount to annual precipitation, and the ratio of snowmelt runoff depth to annual runoff depth at the 0.05 significant level. The catchment SY and SSY contributions by the ratio of annual snowfall to annual precipitation were 25.41% and 30.22%, respectively. [Conclusion] Sediment yield derived from snowmelt runoff contributed a large part of catchment annual total, and was influenced by many factors. Field monitoring of snowmelt erosion and sediment yield in the black soil region ofnortheastern China should be strengthened in the future study.

References:: [1] 蒋玲梅,崔慧珍,王功雪,等.积雪、土壤冻融与土壤水分遥感监测研究进展[J].遥感技术与应用,2020,35(6):1237-1262.
[2] 焦剑,谢云,林燕,等.东北地区融雪期径流及产沙特征分析[J].地理研究,2009,28(2):333-344.
[3] Dickinson W T, Scott A, Wall G. Fluvial sedimentation in southern Ontario[J]. Canadian Journal of Earth Sciences, 1975,12(11):1813-1819.
[4] Demidov V V, Ostroumov V Y, Nikitishena I A, et al. Seasonal freezing and soil erosion during snowmelt [J]. Eurasian Soil Science, 1995,28(10):78-87.
[5] Ollesch G, Kistner I, Meissner R, et al. Modelling of snowmelt erosion and sediment yield in a small low-mountain catchment in Germany[J]. Catena, 2006,68(2/3):161-176.
[6] Wischmeier W H, Smith D D. Predicting Rainfall Erosion Losses: A Guide To Conservation Planning [M]. United States: Department of Agriculture. Agriculture Handbook,1978.
[7] Maltsev K, Yermolaev O. Assessment of soil loss by water erosion in small river basins in Russia [J]. Catena, 2020,27(9):607-621.
[8] 雷廷武,李法虎.水土保持学[M].北京:中国农业大学出版社,2012.
[9] 徐兴奎.1970—2000年中国降雪量变化和区域性分布特征[J].冰川冻土,2011,33(3):497-503.
[10] 范昊明,武敏,周丽丽,等.融雪侵蚀研究进展[J].水科学进展,2013,24(1):146-152.
[11] 范昊明,郭萍,武敏,等.春季解冻期白浆土融雪侵蚀模拟研究[J].水土保持通报, 2011,31(6):130-133.
[12] 桑琦明,郑粉莉,王一菲,等.东北黑土区冻融、风力、水力交互作用对坡面侵蚀的影响[J].水土保持学报,2021,35(2):87-95.
[13] 王平,李浩,陈强,等.典型黑土区不同尺度观测场地融雪径流[J].水土保持通报,2014,34(5):244-247,253.
[14] 刘育成.中国土地资源调查数据集[M].北京:中华商务联合印刷有限公司,2000.
[15] 刘宝元,阎百兴,沈波,等.东北黑土区农地水土流失现状与综合治理对策[J].中国水土保持科学,2008,6(1):1-8.
[16] Sharpley A N. EPIC-Erosion/Productivity Impact Calculator:1, Model Documentation [J]. Usda Techn. Bull, 1990,17(5):225-235.
[17] Williams J R, Renard K G, Dyke P T. EPIC:A new method for assessing erosion's effect on soil productivity [J]. Journal of Soil and Water Conservation, 1983,38(5):381-383.
[18] 张科利,彭文英,杨红丽.中国土壤可蚀性值及其估算[J].土壤学报,2007,44(1):7-13.
[19] 梁石正雄,方海燕.钱塘江流域产沙空间变异特征及影响因素[J].陕西师范大学学报:自然科学版,2019,47(4):67-75.
[20] 方海燕,蔡强国,李秋艳.产沙模数与流域面积关系研究进展[J].地理科学进展,2008,27(6):63-69.
[21] 方海燕,蔡强国,李秋艳.东北典型黑土区乌裕尔河中游泥沙输移月年时间尺度特征[J].泥沙研究,2009,6(2):16-21.
[22] 冷疏影,冯仁国,李锐,等.土壤侵蚀与水土保持科学重点研究领域与问题[J].水土保持学报,2004,18(1):1-6,26.
[23] 王硕,方海燕,和继军.植被覆盖和降雨因子变化及对东北黑土区土壤侵蚀的影响[J].水土保持通报,2021,41(2):66-75.
[24] Rajbanshi J, Bhattacharya S. Assessment of soil erosion, sediment yield and basin specific controlling factors using RUSLE-SDR and PLSR approach in Konar river basin, India [J]. Journal of Hydrology, 2020,587:124935.
[25] Tamene L, Park S J, Dikau R, et al. Analysis of factors determining sediment yield variability in the highlands of northern Ethiopia [J]. Geomorphology, 2006,76(1/2):76-91.
[26] Fang H Y. Quantifying farmland shelterbelt impacts on catchment soil erosion and sediment yield for the black soil region, northeastern China [J]. Soil Use and Management, 2021,31:181-195.
[27] 李建伟,焦剑,高燕,等.松花江流域产沙时间变化特征及影响因素分析[J].泥沙研究,2014,8(3):12-19.
[28] 李致颖,方海燕.基于TETIS模型的黑土区乌裕尔河流域径流与侵蚀产沙模拟研究[J].地理科学进展,2017,36(7):873-885.

Similar References:

Memo

Last Update: 2023-04-10