Paths of soil erosion controlled by typical soil and water conservation practices based on the SIMWE model: A case study of the Tongshuang watershed.

doi:10.13287/j.1001-9332.202203.016

Abstract

Abstract: Due to the basic topographical characteristics of the gentle and long slope lengths in the Mollisol region of Northeast China, severe soil erosion is easily aggravated by the concentration of surface flow. The spatial distribution of water depth and hydrological connectivity index were introduced to evaluate the effects of typical soil and water conservation practices on the overland flow path and hydrological connectivity based on the GIS and SIMWE (SIMulated Water Erosion) model. We analyzed the effects of different soil and water conservation practices on the hydrological connectivity, water flow path, and spatial distribution of soil erosion and sediment yield by quantifying the variations of soil infiltration rate and surface manning roughness, as well as by constructing an artificial terrain digital elevation model (DEM). The results showed that: 1) terraces could effectively affect the hydrological connectivity of the slope and regulate flow path, with significant differences between the responses of hydrological connectivity and flow path under different forms of terraced fields and ridges. The characteristics of spatial distribution of soil erosion and sediment yield varied with changes in water flow path, which would eventually lead to the intensification of local erosion; 2) practices of vegetated buffer strips and contour tillage presented limited effectiveness on runoff path controlling, though they played a significant role in sediment retention; and 3) conservation tillage could reduce the hydrological connectivity and improve the retention capacity of runoff by increasing surface roughness. This study quantified the effects of different soil and water conservation practices on the hydrological connectivity, flow path, and spatial distribution of soil erosion and sediment yield, and could provide a theoretical reference for scientific layout of soil and water conservation practices in black soil region.

Key words: soil and water conservation practice, flow path, hydrological connectivity, paths of soil erosion control, black soil region of Northeast China

CHEN Zu-ming, WANG Bin. Paths of soil erosion controlled by typical soil and water conservation practices based on the SIMWE model: A case study of the Tongshuang watershed.[J]. Chinese Journal of Applied Ecology, 2022, 33(3): 703-710.

References 40

[1]	王岩松, 姜艳艳, 常诚, 等. 2018年度松辽流域水土流失动态监测结果分析. 中国水土保持, 2019(12): 7-10
[2]	阎百兴, 杨育红, 刘兴土, 等. 东北黑土区土壤侵蚀现状与演变趋势. 中国水土保持, 2008(12): 26-30
[3]	郑粉莉, 张加琼, 刘刚, 等. 东北黑土区坡耕地土壤侵蚀特征与多营力复合侵蚀的研究重点. 水土保持通报, 2019, 39(4): 314-319
[4]	李浩, 杨薇, 刘晓冰, 等. 沟蚀发生的地貌临界理论计算中数据获取方法及应用. 农业工程学报, 2019, 35(18): 127-133
[5]	Bracken LJ, Wainwright J, Ali GA, et al. Concepts of hydrological connectivity: Research approaches, pathways and future agendas. Earth-Science Review, 2013, 119: 17-34
[6]	Klik A, Rosner J. Long-term experience with conservation tillage practices in Austria: Impacts on soil erosion processes. Soil and Tillage Research, 2020, 203, 104669
[7]	Engman T. Roughness coefficients for routing surface runoff. Journal of Irrigation and Drainage Engineering 1986, 112: 39-53
[8]	许晓鸿, 隋媛媛, 张瑜, 等. 黑土区不同耕作措施的水土保持效益. 中国水土保持科学, 2013, 11(3): 12-16
[9]	冯瑶. 基于梯田DEM的水流路径模拟. 硕士论文. 西安: 西北大学, 2015
[10]	Wen Y, Kasielke T, Li H, et al. May agricultural terraces induce gully erosion? A case study from the black soil region of northeast China. Science of the Total Environment, 2021, 750: 141715
[11]	Zhu P, Zhang G, Wang H, et al. Land surface roughness affected by vegetation restoration age and types on the Loess Plateau of China. Geoderma, 2020, 366: 114240
[12]	王鹏飞. 紫色土区玉米季横垄坡面细沟侵蚀过程研究. 硕士论文. 成都: 四川农业大学, 2016
[13]	杨洁, 莫明浩, 宋月君, 等. 红壤坡地水土保持植物措施下柑橘林地水文生态效应. 长江流域资源与环境, 2012, 21(8): 994-999
[14]	陈强, Yuriy SK, 陈渊, 等. 少免耕土壤结构与导水能力的季节变化及其水保效果. 土壤学报, 2014, 51(1): 11-21
[15]	Zhao G, Gao P, Tian P, et al. Assessing sediment connectivity and soil erosion by water in a representative catchment on the Loess Plateau, China. Catena, 2019, 185: 104284, doi: 10.1016/j.catena.2019.104284
[16]	López-Vicente M, Poesen J, Navas A, et al. Predicting runoff and sediment connectivity and soil erosion by water for different land use scenarios in the Spanish Pre-Pyrenees. Catena, 2013, 102: 62-73
[17]	冯园, 赵牡丹, 冯瑶, 等. 基于梯田DEM水流路径模拟算法的比较. 山东农业大学学报: 自然科学版, 2017, 48(1): 41-45
[18]	Pijl A, Reuter LEH, Quarella E, et al. GIS-based soil erosion modelling under various steep-slope vineyard practices. Catena, 2020, 193: 104604
[19]	Zanandrea F, Michel GP, Kobiyama M. Impedance influence on the index of sediment connectivity in a forested mountainous catchment. Geomorphology, 2020, 351: 106962
[20]	Mitasova H, Barton CM, Ullah IIT, et al. 3.9 GIS-based soil erosion modeling. Treatise on Geomorphology, 2013, 3: 228-258
[21]	刘宇. 土壤侵蚀研究中的景观连通度: 概念、作用及定量. 地理研究, 2016, 35(1): 195-202
[22]	张光辉. 从土壤侵蚀角度诠释泥沙连通性. 水科学进展, 2021, 32(2): 295-308
[23]	Xie CJ, Cui BS, Xie T, et al. Hydrological connectivity dynamics of tidal flat systems impacted by severe reclamation in the Yellow River Delta. Science of the Total Environment, 2020, 739: 139860
[24]	Zanandrea F, Michel GP, Kobiyama M, et al. Evaluation of different DTMs in sediment connectivity determination in the Mascarada River Watershed, southern Brazil. Geomorphology, 2019, 332: 80-87
[25]	Fernandes J, Bateira C, Soares L, et al. SIMWE model application on susceptibility analysis to bank gully erosion in Alto Douro wine region agricultural terraces. Catena, 2017, 153: 39-49
[26]	孙莉英, 蔡强国, 陈生永, 等. 东北典型黑土区小流域水土流失综合防治体系. 水土保持研究, 2012, 19(3): 36-41
[27]	Mitasova H, Mitas L, Brown WM. Multiscale simulation of land use impact on soil erosion and deposition patterns. 10th International Soil Conservation Meeting, West Lafayette, 2001: 1163-1169
[28]	高峰, 詹敏, 战辉. 黑土区农地侵蚀性降雨标准研究. 中国水土保持, 1989(11): 21-23
[29]	曾建辉, 李占斌, 马波, 等. 小麦秸秆长度、覆盖量对坡面产流产沙的影响. 水土保持学报, 2020, 34(4): 98-103
[30]	齐智娟, 张忠学, 杨爱峥. 黑土坡耕地不同水土保持措施的土壤水蚀特征研究. 水土保持通报, 2012, 32(1): 89-92
[31]	魏永霞. 黑龙江西部坡耕地不同耕作措施水分转化与土壤侵蚀特征. 博士论文. 哈尔滨: 东北林业大学, 2009
[32]	Gilley JE, Kottwitz ER, Wieman GA. Roughness coefficients for selected residue materials. Journal of Irrigation and Drainage Engineering, 1991, 117: 503-514
[33]	Laboratory Uanse. USDA-Water Erosion Prediction Project Hillslope Profile and Watershed Model Documentation. West Lafayette: NSERL Report, 1995: 7.42
[34]	Zhang GH, Wang LL, Li G, et al. Relationship between sediment particle size and transport coefficient on steep slopes. Transactions of the American Society of Agricultural and Biological Engineers, 2011, 54: 869-874
[35]	祝士杰, 汤国安, 张维, 等. 梯田DEM快速构建方法研究. 测绘通报, 2011(4): 68-70
[36]	Cavalli M, Trevisani S, Comiti F, et al. Geomorphometric assessment of spatial sediment connectivity in small Alpine catchments. Geomorphology, 2013, 188: 31-41
[37]	Borselli L, Cassi P, Torri D. Prolegomena to sediment and flow connectivity in the landscape: A GIS and field numerical assessment. Catena, 2008, 75: 268-277
[38]	谌芸, 何丙辉, 向明辉, 等. 紫色土坡耕地植物篱的水土保持效应研究. 水土保持学报, 2013, 27(2): 47-52
[39]	王禹, 杨明义, 刘普灵. 典型黑土直型坡耕地土壤侵蚀强度的小波分析. 核农学报, 2010, 24(1): 98-103
[40]	孙传生, 黄长海, 朱大为, 等. 东北黑土区水土保持保护性耕作措施探讨. 水土保持研究, 2006, 13(5): 132-133