Erosive Rainfall Thresholds for Five Typical Soils in Water Erosion Region of China

Wang Ying; Yang Yang; Liu Baoyuan; Liu Yingna

doi:10.13961/j.cnki.stbctb.2022.04.029

您当前的位置：

首页 >

文章列表页 >

Erosive Rainfall Thresholds for Five Typical Soils in Water Erosion Region of China

- Erosive Rainfall Thresholds for Five Typical Soils in Water Erosion Region of China
- Bulletin of Soiland Water Conservation Vol. 42, Issue 4, Pages: 227-233(2022)
- 作者机构：
  
  1. 北京师范大学地理科学学部地表过程与资源生态国家重点实验室,北京,100875
  2. 北京师范大学地理科学学部地理学院,北京,100875
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2022.04.029
  CLC： S157.1
- Published：2022
- 稿件说明：
移动端阅览
Wang Ying, Yang Yang, Liu Baoyuan, et al. Erosive Rainfall Thresholds for Five Typical Soils in Water Erosion Region of China[J]. Bulletin of Soiland Water Conservation, 2022, 42(4): 227-233.
DOI：

Wang Ying, Yang Yang, Liu Baoyuan, et al. Erosive Rainfall Thresholds for Five Typical Soils in Water Erosion Region of China[J]. Bulletin of Soiland Water Conservation, 2022, 42(4): 227-233. DOI： 10.13961/j.cnki.stbctb.2022.04.029.

摘要

[目的

]

准确拟定侵蚀性降雨阈值，区分侵蚀性与非侵蚀性降雨事件，为有效减少土壤侵蚀预报的工作量以及区域土壤侵蚀防治提供科学参考。[方法

]

在北京市房山区布设中国5个水蚀二级区典型土壤休闲小区，收集各小区2006—2019年的产流产沙监测资料，利用降雨侵蚀力偏差法分析各小区的侵蚀性降雨量(P)和最大30 min雨强(I

)阈值。[结果

]

①相比P阈值，I

在识别侵蚀性降雨方面更为有效。②黑土和褐土小区侵蚀性降雨阈值较高，二者P阈值均为10.0 mm，I

阈值均为10.2 mm/h；黄土小区次之，其P和I

阈值分别为9.5 mm和8.9 mm/h。紫色土与红壤小区较低，二者的P阈值分别为5.4和6.1 mm，I

阈值分别为3.2和5.2 mm/h。③各径流小区的监测资料年限达到12 a时，侵蚀性降雨阈值才可达到稳定。[结论

]

不同地区土壤的侵蚀性降雨阈值存在较大差异。侵蚀性降雨阈值不仅受土壤自身特性如粒径分布和有机质含量的影响，还与当地的气候状况如降雨雨型有关。

Abstract

[Objective] The practical thresholds separating erosive from non-erosive rainfall events were determined to effectively reduce the workload of soil erosion prediction

and to provide references for regional soil erosion prevention.[Methods] Five bare fallow runoff plots packed with typical soils from five water erosion subregions of China were established in the Fangshan District of Beijing City. We used the rainfall erosivity deviation method to derive the two thresholds of rainfall amount (P) and maximum 30-minute rainfall intensity (I30) for each plot based on runoff and soil loss data obtained during 2006-2019.[Results] ① The I30 thresholds were more effective than the P thresholds in identifying erosive rainfall events. ② The erosive rainfall thresholds were highest for the black and cinnamon soil plots

both having P thresholds of 10.0 mm and I30 thresholds of 10.2 mm/h

followed by the loess plot with P and I30 thresholds of 9.5 mm and 8.9 mm/h

respectively. The thresholds were lower for the purple and red soil plots. The corresponding P thresholds were 5.4 and 6.1 mm

respectively

and the I30 thresholds were 3.2 and 5.2 mm/h

respectively. ③ To acquire reliable and stable thresholds

at least 12 years of runoff and soil loss monitoring data were required for each plot.[Conclusion] Erosive rainfall thresholds differed among soils in different regions due to differences in soil properties such as particle size distribution and organic matter content

as well as in local climate factors such as rainfall pattern.

关键词

Keywords

references

Todisco F. The internal structure of erosive and non-erosive storm events for interpretation of erosive processes and rainfall simulation[J]. Journal of Hydrology, 2014,519:3651-3663.

Fang Nufang, Wang Ling, Shi Zhihua. Runoff and soil erosion of field plots in a subtropical mountainous region of China[J]. Journal of Hydrology, 2017,552:387-395.

王万忠.黄土地区降雨特性与土壤流失关系的研究(Ⅲ):关于侵蚀性降雨的标准问题[J].水土保持通报,1984,4(2):58-63.

Xie Yun, Liu Yuanbao, Nearing M A. Practical thresholds for separating erosive and non-erosive storms[J]. Transactions of the ASAE, 2002,45(6):1843-1847.

夏露,宋孝玉,符娜,等.陇东黄土塬区不同下垫面条件下侵蚀产沙的降雨阈值[J].水科学进展,2018,29(6):828-838.

王万忠,焦菊英.中国的土壤侵蚀因子定量评价研究[J].水土保持通报,1996,16(5):1-20.

马良,左长清,邱国玉.赣北红壤坡地侵蚀性降雨的特征分析[J].水土保持通报,2010,30(1):74-79.

李林育,王志杰,焦菊英.紫色丘陵区侵蚀性降雨与降雨侵蚀力特征[J].中国水土保持科学,2013,11(1):8-16.

Liu Yu, Fu Bojie, Lü Yihe, et al. Hydrological responses and soil erosion potential of abandoned cropland in the Loess Plateau, China[J]. Geomorphology, 2012,138(1):404-414.

Feng Qiang, Zhao Wenwu,Wang Jun, et al. Effects of different land-use types on soil erosion under natural rainfall in the Loess Plateau, China[J]. Pedosphere, 2016,26(2):243-256.

金建君,谢云,张科利.不同样本序列下侵蚀性雨量标准的研究[J].水土保持通报,2001,21(2):31-33.

孙正宝,陈治谏,廖晓勇,等.侵蚀性降雨识别的模糊隶属度模型建立及应用[J].水科学进展,2011,22(6):801-806.

中华人民共和国水利部.SL190-2007土壤侵蚀分类分级标准[S].北京:中国水利水电出版社,2008.

张奇.遂宁组母质侵蚀规律的初步研究[J].水土保持通报,1992,12(3):34-39.

张宪奎,许靖华,卢秀琴,等.黑龙江省土壤流失方程的研究[J].水土保持通报,1992,12(4):1-9.

刘和平,袁爱萍,路炳军,等.北京侵蚀性降雨标准研究[J].水土保持研究,2007,14(1):215-217.

汪邦稳,方少文,宋月君,等.赣北第四纪红壤区侵蚀性降雨强度与雨量标准的确定[J].农业工程学报,2013,29(11):100-106.

Wang Wenting, Yin Shuiqing, Xie Yun, et al. Effects of four storm patterns on soil loss from five soils under natural rainfall[J]. Catena, 2016,141:56-65.

Hao Yanfang, Yang Yang, Liu Baoyuan, et al. Size characteristics of sediments eroded from three soils in China under natural rainfall[J]. Journal of Soils and Sediments, 2016,16(8):2153-2165.

Brown L C, Foster G R. Storm erosivity using idealized intensity distributions[J]. Transactions of the ASAE, 1987,30(2):379-386.

Wischmeier W H, Smith D D. Predicting rainfall erosion losses:A guide to conservation planning[M]. Agriculture Handbook, No.537. 1978.

Todisco F, Vergni L, Vinci A, et al. Practical thresholds to distinguish erosive and rill rainfall events[J]. Journal of Hydrology, 2019,579:124173.

张文源,王百田,杨光檄,等.喀斯特黄壤区侵蚀性降雨及产沙特征分析[J].生态环境学报,2014,23(11):1776-1782.

Mamedov A I, Levy G J, Shainberg I, et al. Wetting rate, sodicity, and soil texture effects on infiltration rate and runoff[J]. Soil Research, 2001,39(6):1293-1305.

Wakindiki I I C, Ben-Hur M. Soil mineralogy and texture effects on crust micromorphology, infiltration, and erosion[J]. Soil Science Society of America Journal, 2002,66(3):897-905.

Tisdall J M, Oades J M. Organic matter and water-stable aggregates in soils[J]. Journal of Soil Science, 1982,33(2):141-163.

Causarano H. Factors affecting the tensile strength of soil aggregates[J]. Soil and Tillage Research, 1993,28(1):15-25.

Ben-Hur M, Shainberg I, Bakker D, et al. Effect of soil texture and CaCO

content on water infiltration in crusted soil as related to water salinity[J]. Irrigation Science, 1985,6(4):281-294.

郝燕芳,刘宝元,杨扬,等.中国5种典型土壤的侵蚀泥沙粒径分布特征[J].水土保持学报,2018,32(2):150-159.

赵光耀.唐秦地区侵蚀性降雨及降雨侵蚀力时空变化研究[D].河北保定:河北农业大学,2019.

Liang Yue, Jiao Juying, Dang Weiqin, et al. The thresholds of sediment-generating rainfall from hillslope to watershed scales in the Loess Plateau, China[J]. Water, 2019,11(11):2392.

涂安国,谢颂华,李英,等.长期野外监测红壤裸露坡地侵蚀性降雨分布及产沙分析[J].农业工程学报,2019,35(7):129-135.

郑粉莉,边锋,卢嘉,等.雨型对东北典型黑土区顺坡垄作坡面土壤侵蚀的影响[J].农业机械学报,2016,47(2):90-97.

焦菊英,王万忠,郝小品.黄土高原不同类型暴雨的降水侵蚀特征[J].干旱区资源与环境,1999,13(1):34-42.

谢云,林小鹃,殷水清,等.中国次雨量特征及其区域分异[J].地理学报,2009,64(3):323-330.

张向炎,史学正,于东升,等.前期土壤含水量对红壤坡面产流产沙特性的影响[J].水科学进展,2010,21(1):23-29.

Boix-Fayos C, Calvo-Cases A, Imeson A C, et al. Influence of soil properties on the aggregation of some Mediterranean soils and the use of aggregate size and stability as land degradation indicators[J]. Catena, 2001,44(1):47-67.

王春明,包维楷,陈建中,等.岷江上游干旱河谷区褐土不同亚类剖面及养分特征[J].应用与环境生物学报,2003,9(3):230-234.

Yang Yang, Ye Zhihan, Liu Baoyuan, et al. Nitrogen enrichment in runoff sediments as affected by soil texture in Beijing Mountain area[J]. Environmental Monitoring and Assessment, 2014,186(2):971-978.

包昂,范昊明,许秀泉,等.东北半干旱区不同耕作方式下的侵蚀性降雨标准比较[J].土壤通报,2022,53(1):81-88.

战云健,鞠晓慧,范邵华,等.1965-2019年中国夏季分钟降水空间分布与长期趋势分析[J].气象学报,2021,79(4):598-611.

Views

806

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Analysis of Soil Erosion on Suining Group Parent Material After Closing Management

Comparison of Particle Size Distributions Determined by Pipette Method and Scanning Electron Microscopy for Typical Soils in Water Erosion Region of China

Influence of different amendments on salt ions and maize growth in coastal saline soil

Remote sensing monitoring and soil and water conservation effects of abandoned farmland in core black soil protection area of Jilin Province from 2000 to 2023

Impacts of seasonal drought on carbon-water coupling mechanism in China’s terrestrial ecosystems

Related Author

YANG Yuan-xiang

ZHU Xue-mei

SHAO Ji-rong

LIN Li-ji

WU Yong

JIANG Xiao-jun

Peng Tingting

Bai Xue

Related Institution

College of Resources and Environment, Sichuan Agricultural University, Ya’an

College of Life Sciences, Sichuan Agricultural University, Ya’an

Soil and Water Conservation Station of Suining

State Key Laboratory Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University

⁰