The Spatiotemporal Characteristics of Soil Erosion in the Qinling-Daba Mountains Based on RUSLE Model

WANG Liyuan; ZHAO Tixia; ZHU Wenbo; ZHU lianqi

doi:10.13870/j.cnki.stbcxb.2024.01.003

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The Spatiotemporal Characteristics of Soil Erosion in the Qinling-Daba Mountains Based on RUSLE Model

更新时间：2025-03-12

- The Spatiotemporal Characteristics of Soil Erosion in the Qinling-Daba Mountains Based on RUSLE Model
- Vol. 38, Issue 1, Pages: 113-121(2024)
- 作者机构：
  
  河南大学地理与环境学院,河南,开封,475004
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2024.01.003
  CLC： S157.1
- Published：2024
- 稿件说明：
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WANG Liyuan, ZHAO Tixia, ZHU Wenbo, et al. The Spatiotemporal Characteristics of Soil Erosion in the Qinling-Daba Mountains Based on RUSLE Model[J]. 2024, 38(1): 113-121.
DOI：

WANG Liyuan, ZHAO Tixia, ZHU Wenbo, et al. The Spatiotemporal Characteristics of Soil Erosion in the Qinling-Daba Mountains Based on RUSLE Model[J]. 2024, 38(1): 113-121. DOI： 10.13870/j.cnki.stbcxb.2024.01.003.

摘要

[目的] 秦岭—大巴山地(秦巴山地)是我国重要的南北地理—生态过渡带主体

对秦巴山地的土壤侵蚀研究将有助于该区域的生态保护和水土资源管理。[方法] 基于RUSLE模型计算秦巴山地的土壤侵蚀模数

并量化分析了该区域的土壤侵蚀的时空分布格局。[结果] (1)2000—2020年秦巴山地的微度侵蚀面积呈上升趋势

轻度侵蚀及其以上等级的土壤侵蚀面积均呈下降趋势;从空间来看

秦巴山地东北和西南部的土壤侵蚀等级较高

中间较低;(2)秦巴山地的土壤侵蚀相对集中在500~1 500 m、坡度15°~25°区域内;(3)秦巴山地发生土壤侵蚀最主要的土地利用类型为林地

耕地、林地的微度侵蚀以及草地的微度、剧烈侵蚀面积呈上升趋势;(4)秦巴山地土壤侵蚀主要分布在陕西、四川和甘肃

且甘肃和四川的剧烈侵蚀呈上升趋势。[结论] 2000—2020年秦巴山地的侵蚀面积和强度呈"双下降"的态势

其整体侵蚀状况好转

但侵蚀分布存在明显空间差异。

Abstract

[Objective] The Qinling-Daba Mountains region (QDM) is the important geographical transitional zone across the north and south of China. A comprehensive and systematic analysis of soil erosion in QDM is essential for the planning of soil and water conservation measures

and the sustainable agriculture development. [Methods] Based on the Revised Universal Soil Loss Equation (RUSLE)

we calculate the soil erosion modulus in the QDM and analyze the spatiotemporal characteristic of the soil erosion in the study region from 2000 to 2020. [Results] (1) From 2000 to 2020

the areas of soil erosion in the QDM showed an upward trend. Spatially

the areas of higher soil erosion modulus were located in the northeast and southwest of the QDM

while the areas of lower soil erosion modulus were distributed in the central of the study region; (2) The areas with severe soil erosion are mainly concentrated in area with 500 ~ 1 500 m

and areas with 15 °~ 35°; (3) The land-use pattern with the highest soil erosion rates were forest

and the lowest soil erosion rate were found grass; (4) The areas with soil erosion were mainly located in Shaanxi

Sichuan

and Gansu. Severe erosion showed an upward trend in Gansu and Sichuan during 2000-2020. [Conclusion] Both erosion area and erosion intensity in the QDM showed decreasing trend

while the differences in the distribution pattern of erosion intensity were found in this study region.

关键词

Keywords

references

CHEN H, ZHANG X P, ABLA M, et al. Effects of vegetation and rainfall types on surface runoff and soil erosion on steep slopes on the Loess Plateau, China[J].Catena,2018,170:141-149.

李太魁,张香凝,寇长林,等.不同农艺措施对丹江口库区坡耕地茶园水土和磷素流失的影响[J].生态环境学报,2021,30(12):2324-2330. LI T K, ZHANG X N, KOU C L, et al. Effects of different agronomic measures on runoff, water and phosphorous losses of tea garden located in sloping cropland in Danjiangkou Reservoir Area[J].Ecology and Environmental Sciences, 2021,30(12):2324-2330.

肖理,王章文,殷庆元,等.金沙江干热河谷坡改梯对水土保持的影响[J].西南农业学报,2019,32(12):2856-2861. XIAO L, WANG Z W, YIN Q Y, et al. Effect of terracing slope cropland on soil and water conservation in dry-hot valley of Jinsha River Basin, southwest China[J].Southwest China Journal of Agricultural Sciences,2019,32(12):2856-2861.

李宗善,杨磊,王国梁,等.黄土高原水土流失治理现状、问题及对策[J].生态学报,2019,39(20):7398-7409. LI Z S, YANG L, WANG G L, et al. The management of soil and water conservation in the Loess Plateau of China: Present situations, problems, and counter-solutions[J].Acta Ecologica Sinica,2019,39(20):7398-7409.

吴发启,张玉斌,王健.黄土高原水平梯田的蓄水保土效益分析[J].中国水土保持科学,2004,2(1):34-37. WU F Q, ZHANG Y B, WANG J. Study on the benefits of level terrace on soil and water conservation[J].Science of Soil and Water Conservation, 2004,2(1):34-37.

胡建民,胡欣,谢颂华.南方红壤坡地几种典型治理措施的径流调控效应[J].水土保持通报,2013,33(6):32-36,41. HU J M, HU X, XIE S H. Effects of several typical measures on regulating runoff in slope land of red soil in southern China[J]. Bulletin of Soil and Water Conservation, 2013,33(6):32-36,41.

魏飒,郭永晨,侯克.北方土石山区坡改梯工程建设技术标准与示范[J].中国水土保持,2015(4):28-30. WEI S, GUO Y C, HOU K. Technical standard and demonstration of slope-to-ladder project in northern rocky mountain area[J].Soil and Water Conservation in China,2015(4):28-30.

朱奎,强思远,母小苗,等.不同降雨特征对径流过程的影响研究[J].中国农村水利水电,2021(4):33-37. ZHU K, QIANG S Y, MU X M, et al. Influence of different rainfall characteristics on runoff process[J].China Rural Water and Hydropower,2021(4):33-37.

杨国强,陶虎,雷少伟,等.不同雨型条件下非饱和土边坡渗流及稳定分析[J].水电能源科学,2022,40(6):166-170. YANG G Q, TAO H, LEI S W, et al. Analysis of seepage and stability of unsaturated soil slopes under different rainfall patterns[J].Water Resources and Power,2022,40(6):166-170.

张国华,张展羽,左长清,等.红壤坡地不同类型梯田的水土保持效应[J].水利水电科技进展,2007,27(2):77-79,84. ZHANG G H, ZHANG Z Y, ZUO C Q, et al. Water and soil conservation effect for different types of terraces on red soil slope land[J].Advances in Science and Technology of Water Resources,2007,27(2):77-79,84.

项佳敏,章明奎,丁志峰,等.地形部位对亚热带低丘梯田土壤性态与类型的影响[J].土壤通报,2022,53(1):20-27. XIANG J M, ZHANG M K, DING Z F, et al. Effects of topographic position on soil properties and types of terraced fields in subtropical low hills[J].Chinese Journal of Soil Science,2022,53(1):20-27.

杜若愚,姚成,刘玉环,等.基于蓄满超渗时空动态组合的网格新安江模型[J].河海大学学报(自然科学版),2022,50(6):25-32,122. DU R Y, YAO C, LIU Y H, et al. Grid-Xin'anjiang model based on spatio-temporal dynamic combination of saturation-excess and infiltration-excess runoff[J]. Journal of Hohai University (Natural Sciences), 2022,50(6):25-32,122.

袁志明,卢金锁.雨水花园侧向防渗措施效果的试验与模拟研究[J].中国给水排水,2018,34(13):130-134. YUAN Z M, LU J S. Experiment and simulation on anti-seepage effect of lateral impervious protective measures in rain garden[J].China Water and Wastewater,2018,34(13):130-134.

任加国,范坤,陈清,等.田埂在农业面源污染治理中的应用现状与展望[J].环境工程技术学报,2023,13(1):262-269. REN J G, FAN K, CHEN Q, et al. Application status and prospect of field ridge in agricultural non-point source pollution treatment[J].Journal of Environmental Engineering Technology,2023,13(1):262-269.

汪三树,刘德忠,史东梅,等.紫色丘陵区坡耕地生物埂的蓄水保土效应[J].中国农业科学,2013,46(19):4091-4100. WANG S S, LIU D Z, SHI D M, et al. Analysis on the soil and water conservation benefits of four bunds at edges of sloping land in purple hilly area[J].Scientia Agricultura Sinica,2013,46(19):4091-4100.

程冬兵,张平仓,蔡崇法.等高绿篱系统土壤水分入渗特性研究[J].水土保持学报,2009,23(3):221-226. CHENG D B, ZHANG P C, CAI C F. Study on the soil water infiltration properties in contour hedgerow system[J]. Journal of Soil and Water Conservation, 2009,23(3):221-226.

LIU X Y, XIN L J, LU Y H. National scale assessment of the soil erosion and conservation function of terraces in China[J].Ecological Indicators,2021,129:e107940.

WEI W, FENG X R, YANG L, et al. The effects of terracing and vegetation on soil moisture retention in a dry hilly catchment in China[J]. The Science of the Total Environment, 2019,647:1323-1332.

包耀贤.黄土高原坝和梯田土壤质量特征及评价[D]. 陕西杨凌:西北农林科技大学,2009. BAO Y X. The characteristics and assessment on soil quality of dam land and terrace in Loess Plateau[D]. Yangling, Shaanxi: Northwest A&F University, 2009.

张宇恒,王忠诚,王亚楠,等.基于最小数据集沂蒙山区不同治理模式下的土壤质量评价[J].水土保持研究,2023,30(1):241-247. ZHANG Y H, WANG Z C, WANG Y N, et al. Soil quality evaluation with different treatment models in Yimeng mountainous area based on minimum data set[J].Research of Soil and Water Conservation,2023,30(1):241-247.

陈新军,阮芬,廉士增,等.沂蒙山区不同水土保持措施下土壤物理性状分析[J].中国水土保持,2014(8):30-32. CHEN X J, RUAN F, LIAN S Z,et al. Analysis of soil physical properties under different soil and water conservation measures in Yimeng Mountain area[J].Soil and Water Conservation in China,2014(8):30-32.

张靖宇. 红壤丘陵区不同类型梯田水土保持效益研究[D]. 南昌: 江西农业大学, 2011. ZHNAG J Y. Study on soil and water conservation benefit of different terrace types in red soil hilly region[D]. Nanchang: Jiangxi Agricultural University, 2011.

李源,宋维峰,马建刚.哈尼梯田典型区域土壤水分特征曲线模拟研究[J].西南林业大学学报(自然科学),2023,43(2):90-98. LI Y, SONG W F, MA J G. Simulation of soil moisture characteristic curve in the typical region of Hani Terraces[J].Journal of Southwest Forestry University (Natural Sciences),2023,43(2):90-98.

刘澄静,角媛梅,高璇,等.哈尼梯田水源区不同景观类型土壤水分的入渗特性及影响因子[J].水土保持通报,2018,38(3):99-105,111. LIU C J, JIAO Y M, GAO X, et al. Soil water infiltration characteristics and its influencing factors in different landscape types in water source area of Hani Terrace[J].Bulletin of Soil and Water Conservation, 2018,38(3):99-105,111.

殷水清,王杨,谢云,等.中国降雨过程时程分型特征[J].水科学进展,2014,25(5):617-624. YIN S Q, WANG Y, XIE Y, et al. Characteristics of intra-storm temporal pattern over China[J].Advances in Water Science,2014,25(5):617-624.

WANG W T, YIN S Q, XIE Y, et al. Effects of four storm patterns on soil loss from five soils under natural rainfall[J].Catena,2016,141:56-65.

黎俊佑,马岚,刘京晶,等.雨型对华北土石山区坡面土壤侵蚀的影响[J].水土保持学报,2020,34(4):1-6. LI J Y, MA L, LIU J J, et al. Effects of rainfall patterns on slope soil erosion in the rocky mountain area of North China[J].Journal of Soil and Water Conservation, 2020,34(4):1-6.

DUNKERLEY D. Effects of rainfall intensity fluctuations on infiltration and runoff: Rainfall simulation on dryland soils, Fowlers Gap, Australia[J].Hydrological Processes,2012,26(15):2211-2224.

刘凤丽,熊玉江,范乐,等.水稻灌区降雨径流特征及其影响因素研究[J].中国农村水利水电,2022(5):95-100. LIU F L, XIONG Y J, FAN L, et al. Characteristics and influencing factors of rainfall-runoff in rice irrigation district[J].China Rural Water and Hydropower,2022(5):95-100.

DUNKERLEY D. Rain event properties in nature and in rainfall simulation experiments: A comparative review with recommendations for increasingly systematic study and reporting[J].Hydrological Processes, 2008,22(22):4415-4435.

ALAVINIA M, SALEH F N, ASADI H. Effects of rainfall patterns on runoff and rainfall-induced erosion[J]. International Journal of Sediment Research, 2019,34(3):270-278.

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