Simulating the Impact of Slope Shapes on Soil Erosion for the Black Soil Region, Northeastern China

ZHAO Ziyuan; FANG Haiyan; WU Yabing; CAI Qiangguo

doi:10.13870/j.cnki.stbcxb.2022.06.004

您当前的位置：

首页 >

文章列表页 >

Simulating the Impact of Slope Shapes on Soil Erosion for the Black Soil Region, Northeastern China

更新时间：2025-03-12

- Simulating the Impact of Slope Shapes on Soil Erosion for the Black Soil Region, Northeastern China
- Vol. 36, Issue 6, Pages: 23-29(2022)
- 作者机构：
  
  1. 中国科学院大学资源与环境学院,北京,100049
  2. 中国科学院地理科学与资源研究所陆地水循环与地表过程重点实验室,北京,100101
  3. 辽宁师范大学地理科学学院,辽宁,大连,116029
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2022.06.004
  CLC： S157.1
- Published：2022
- 稿件说明：
移动端阅览
ZHAO Ziyuan, FANG Haiyan, WU Yabing, et al. Simulating the Impact of Slope Shapes on Soil Erosion for the Black Soil Region, Northeastern China[J]. 2022, 36(6): 23-29.
DOI：

ZHAO Ziyuan, FANG Haiyan, WU Yabing, et al. Simulating the Impact of Slope Shapes on Soil Erosion for the Black Soil Region, Northeastern China[J]. 2022, 36(6): 23-29. DOI： 10.13870/j.cnki.stbcxb.2022.06.004.

摘要

为探究黑土区不同坡形下的土壤侵蚀特征

基于黑龙江省粮食沟小流域9个耕地径流场侵蚀产沙数据

采用WEPP (Water Erosion Prediction Project)模型进行土壤侵蚀预报与情景模拟。结果表明:径流量和产沙的整体模拟效果较好

径流量决定系数(R2)与纳什系数(NSE)分别为0.71和0.60

产沙决定系数(R2)与纳什系数(NSE)分别为0.61和0.50

表明该模型对该区土壤侵蚀模拟具有较好的适用性。而模型模拟精度则随坡度增大而减小

在3°

5°和8°坡度下

泥沙模拟的NSE分别为0.60

0.55和0.48

R2分别为0.65

0.61和0.60

这与较陡坡度条件下坡面细沟发育有关;径流量在不同坡度坡形下无明显差异

相同降雨、不同坡形下的径流差异普遍在10%以内

而产沙量在不同坡度坡形上呈现较大差异

相同降雨、不同坡形下的产沙差异普遍在20%左右

最高可达到90%以上;同一坡度条件下

直形坡的土壤侵蚀强度最大

次之为凸形坡

而"S"形坡的土壤侵蚀强度最小。该研究结果可以为我国东北黑土区水土保持措施提供科学依据。

Abstract

The black soil in northeastern China is suffering severe soil erosion

which is greatly impacted by slope shapes. In this paper

based on the measured runoff and sediment data derived from 15 erosive rainfalls in 2014—2015 on 9 runoff plots in the Liangshigou catchment

Keshan County

the WEPP (Water Erosion Prediction Project) was used to explore the impacts of different slope shapes on soil erosion characteristics

and meaningful results were obtained. The determination coefficient (R2) and Nash-Sutcliffe efficiency (NSE) of the overall runoff depth and sediment yield simulation results were both greater than 0.5

and the model was suitable for soil erosion simulation for the black soil region under natural rainfall conditions. For both runoff depth and sediment yield

the simulation accuracies of the WEPP model decreased with increasing slope degrees. For the simulated sediment yields from different slopes

the R2 and NSE decreased from 0.60 and 0.65 on 3° slope

0.55 and 0.61 on 5° slope

and 0.48 and 0.60 on 8° slope

respectively. The soil erosion intensities were closely related to the slope shapes. The simulated runoff depths had no obvious difference on different shaped slopes

but the simulated soil erosion intensity was the highest on the straight slope

followed by the convex slope

and the smallest sediment yield on the S-shaped slope. This study can help soil erosion control for the black soil region

northeastern China.

关键词

Keywords

references

Panin A V, Walling D E, Golosov V N. The role of soil erosion and fluvial processes in the post-fallout redistribution of Chernobyl-derived caesium-137: A case study of the Lapki catchment, Central Russia[J].Geomorphology,2001,40(3/4):185-204.

沈昌蒲,龚振平,温锦涛.横坡垄与顺坡垄的水土流失对比研究[J].水土保持通报,2005,25(4):48-49,80.

罗键,尹忠,郑子成,等.不同降雨条件下紫色土横垄坡面地表微地形变化特征[J].中国农业科学,2016,49(16):3162-3173.

王磊,何超,郑粉莉,等.黑土区坡耕地横坡垄作措施防治土壤侵蚀的土槽试验[J].农业工程学报,2018,34(15):141-148.

张晶玲,周丽丽,马仁明,等.天然降雨条件下横垄与顺垄坡面产流产沙过程[J].水土保持学报,2017,31(5):114-119.

Hashim G M, Ciesiolka C A A, Yusoff W A, et al. Soil erosion processes in sloping land in the east coast of Peninsular Malaysia[J].Soil Technology,1995,8(3):215-233.

Napoli M, Marta A D, Zanchi C A, et al. Assessment of soil and nutrient losses by runoff under different soil management practices in an Italian hilly vineyard[J].Soil and Tillage Research,2017,168:71-80.

文安邦,张信宝,张一云,等.黄土峁坡耕地土壤侵蚀与泥沙输移[J].山地研究,1995(2):85-90.

胡国庆,董元杰,史衍玺,等.土壤侵蚀磁性示踪剂两种布设方式下示踪效果的研究[J].水土保持学报,2009,23(2):37-41.

杨丽娜,范昊明,郭成久,等.不同坡形坡面侵蚀规律试验研究[J].水土保持研究,2007,14(4):237-239,243.

于晓杰,魏勇明.不同坡形坡面侵蚀产沙过程的影响研究[J].水土保持研究,2010,17(1):97-100.

Quine T A, Govers G, Walling D E, et al. Erosion processes and landform evolution on agricultural land: New perspectives from caesium-137 measurements and topographic-based erosion modelling[J].Earth Surface Processes and Landforms,1997,22(9):799-816.

Pennock D J. Terrain attributes, landform segmentation, and soil redistribution[J].Soil and Tillage Research,2003,69(1/2):15-26.

杨维鸽,郑粉莉,王占礼,等.地形对黑土区典型坡面侵蚀—沉积空间分布特征的影响[J].土壤学报,2016,53(3):572-581.

Liu L, Zhang K L, Zhang Z D, et al. Identifying soil redistribution patterns by magnetic susceptibility on the black soil farmland in Northeast China[J].Catena,2015,129:103-111.

Rodrigo C J, Senciales J M, Ramos M C, et al. Understanding soil erosion processes in Mediterranean sloping vineyards (Montes de Málaga, Spain)[J].Geoderma,2017,296:47-59.

Chaplot V A M, Le Bissonnais Y. Runoff features for interrill erosion at different rainfall intensities, slope lengths, and gradients in an agricultural loessial hillslope[J].Soil Science Society of America Journal,2003,67(3):844-851.

缪驰远,何丙辉,陈晓燕.水蚀模型USLE与WEPP在紫色土水蚀预测中的应用对比研究[J].农业工程学报,2005,21(1):13-16.

邬铃莉,王云琦,王晨沣,等.降雨类型对北方土石山区坡面土壤侵蚀的影响[J].农业工程学报,2017,33(24):157-164.

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.

范昊明,蔡强国,崔明.东北黑土漫岗区土壤侵蚀垂直分带性研究[J].农业工程学报,2005,21(6):8-11.

Cui M, Cai Q G, Zhu A X, et al. Soil erosion along a long slope in the gentle hilly areas of black soil region in Northeast China[J]. Journal of Geographical Sciences, 2007(3):375-383.

李百安.基于USLE模型的吉林梨树县土壤侵蚀现状初步分析[D].长春:东北师范大学,2015.

胡刚,宋慧,刘宝元,等.黑土区基准坡长和LS算法对地形因子的影响[J].农业工程学报,2015,31(3):166-173.

谢云,高燕,顾治家,等.东北黑土区坡耕地水土流失危险程度评价[J].中国水土保持科学(中英文),2020,18(6):105-114.

汤洁,张爱丽,侯克怡,等.辽河重污染支流招苏台河径流和泥沙模拟研究[J].水土保持研究,2014,21(2):111-115.

郭敏,方海燕,李致颖.基于SWAT东北黑土区乌裕尔河流域径流模型模拟[J].水土保持研究,2016,23(4):43-47,54.

李怡,孙冀程,赵春子,等.基于SWAT模型的布尔哈通河流域径流模拟研究[J].黑龙江大学自然科学学报,2022,39(1):89-95.

盛美玲,方海燕.WaTEM/SEDEM模型及其应用研究进展与展望[J].地理科学进展,2014,33(1):85-91.

刘远利,郑粉莉,王彬,等.WEPP模型在东北黑土区的适用性评价:以坡度和水保措施为例[J].水土保持通报,2010,30(1):139-145.

缪驰远,何丙辉,陈晓燕,等.USLE与WEPP土壤可蚀性因子的关联性分析[J].中国水土保持,2004(6):27-29,48.

王建勋,郑粉莉,江忠善,等.WEPP模型坡面版在黄土丘陵沟壑区的适用性评价:以坡长因子为例[J].水土保持通报,2007,27(2):50-55.

Zheng F L, Zhang X-C (John), Wang J X, et al. Assessing applicability of the WEPP hillslope model to steep landscapes in the northern Loess Plateau of China[J].Soil and Tillage Research,2020,197:e104492.

Mohammed S, Hussien M, Alsafadi K, et al. Assessing the WEPP model performance for predicting daily runoff in three terrestrial ecosystems in western Syria[J].Heliyon,2021,7(4):e06764.

Nearing M A, Deer-Ascough L, Laflen J M. Sensitivity analysis of the WEPP hillslope profile erosion model[J].Transactions of the ASAE,1990,33(3):839-849.

Laflen J M, Flanagan D C, Engel B A. Soil erosion and sediment yield prediction accuracy using WEPP1[J].Journal of the American Water Resources Association,2004,40(2):289-297.

Pandey A, Himanshu S K, Mishra S K, et al. Physically based soil erosion and sediment yield models revisited[J].Catena,2016,147:595-620.

Saghafian B, Meghdadi A R, Sima S. Application of the WEPP model to determine sources of run-off and sediment in a forested watershed: Using WEPP for run-off and sediment simulation in a forested watershed[J].Hydrological Processes,2015,29(4):481-497.

Grønsten H A, Lundekvam H. Prediction of surface runoff and soil loss in southeastern Norway using the WEPP Hillslope model[J].Soil and Tillage Research,2006,85(1/2):186-199.

Albaradeyia I, Hani A, Shahrour I. WEPP and ANN models for simulating soil loss and runoff in a semi-arid Mediterranean region[J].Environmental Monitoring and Assessment,2011,180(1/4):537-556.

Nasir N, Selvakumar R. Influence of land use changes on spatial erosion pattern, a time series analysis using RUSLE and GIS: The cases of Ambuliyar sub-basin, India[J].Acta Geophysica,2018,66(5):1121-1130.

安娟.东北黑土区土壤侵蚀过程机理和土壤养分迁移研究[D]. 陕西杨凌:中国科学院研究生院(教育部水土保持与生态环境研究中心), 2012.

邢伟民,王镱潼,徐浩林,等.坡形和PAM对黄土坡地水土养分迁移特征的影响[J].水土保持学报,2020,34(6):135-142.

Assouline S, Ben-Hur M. Effects of rainfall intensity and slope gradient on the dynamics of interrill erosion during soil surface sealing[J].Catena,2006,66(3):211-220.

Wu S B, Chen L, Wang N L, et al. Two-dimensional rainfall-runoff and soil erosion model on an irregularly rilled hillslope[J].Journal of Hydrology,2020,580:e124346.

Views

816

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Using Study of Sloping WEPP Model in Sichuan Hilly Basin

Effects of Polyacrylamide and Slope Shape on Transportation of Soil Water and Nutrients from the Loess Sloping Land

Small Watershed Erosion Model （SWEM）

Response of Soil Total Nitrogen Distribution to Erosion under Ecological Restoration in Qinling Water Source Area

Response of Slope Runoff Hydrodynamic Characteristics to Gravel Coverage in Alpine Regions under Artificial Rainfall Simulation

Related Author

YAN Dong-chun

WEN An-bang

ZHANG Zhong-qi

ZHENG Jin-jun

XING Weimin

WANG Yitong

XU Haolin

YANG Peiling

Related Institution

College of Hydraulic Science and Engineering, Yangzhou University

College of Water Resources and Civil Engineering, China Agricultural University

State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction， Faculty of Geographical Science， Beijing Normal University

Faculty of Arts and Sciences， Beijing Normal University at Zhuhai

State Key Laboratory of Water Engineering Ecology and Environment in Arid Area， Xi'an University of Technology

⁰