Characteristics of Runoff and Sediment on Slope Land with Different Land Use in Karst Trough Valley Area

Zhang Caiyun; Jiang Yongjun; Ma Lina; Wang Qirong

doi:10.13961/j.cnki.stbctb.2021.01.008

您当前的位置：

首页 >

文章列表页 >

Characteristics of Runoff and Sediment on Slope Land with Different Land Use in Karst Trough Valley Area

- Characteristics of Runoff and Sediment on Slope Land with Different Land Use in Karst Trough Valley Area
- Bulletin of Soiland Water Conservation Vol. 41, Issue 1, Pages: 49-55(2021)
- 作者机构：
  
  西南大学地理科学学院, 岩溶环境重庆市重点实验室,重庆,400715
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2021.01.008
  CLC： S157.1
- Published：2021
- 稿件说明：
移动端阅览
Zhang Caiyun, Jiang Yongjun, Ma Lina, et al. Characteristics of Runoff and Sediment on Slope Land with Different Land Use in Karst Trough Valley Area[J]. Bulletin of Soiland Water Conservation, 2021, 41(1): 49-55.
DOI：

Zhang Caiyun, Jiang Yongjun, Ma Lina, et al. Characteristics of Runoff and Sediment on Slope Land with Different Land Use in Karst Trough Valley Area[J]. Bulletin of Soiland Water Conservation, 2021, 41(1): 49-55. DOI： 10.13961/j.cnki.stbctb.2021.01.008.

摘要

[目的

]

研究岩溶槽谷区坡地产流产沙规律，为槽谷区坡面水土流失防治提供理论基础。[方法

]

基于重庆市北碚区中梁山岩溶槽谷区径流小区，探讨了土地利用类型（耕地、林地、果园和竹林地）、降雨等级、降雨特征对坡地产流产沙的影响。[结果

]

①不同土地利用方式的径流小区坡地总产流量为：耕地（3 534.64 L）>果园地（3 150.60 L）>竹林地（2 347.75 L）>林地（1 957.41 L）；径流系数（3.12%~5.70%）远低于非岩溶区（约20%）；地表产沙量耕地（3.37 kg）>果园地（2.60 kg）>林地（1.60 kg）>竹林地（1.43 kg）；②虽然暴雨占总降雨场次的1.53%，但产流量占年产量的42.28%，产沙量占年总产沙量的33.42%。中雨占年产流总量的16.61%，产沙量占年总产沙量的20.47%，但是由于中雨的降雨次数多，其造成的泥沙流失也不可忽视。③降雨量对不同土地利用方式下的坡面产流的影响最大，是坡面产流的主要影响因素。I

对耕地和果园产沙量的影响最大，降雨量对林地和果园产沙量的影响最大。[结论

]

在相同的降雨条件下，耕地的产流产沙量最大，果园次之。在坡度一定的条件下，不同等级的降雨是影响产流产沙的主要因素，因此，在安排农事活动时，应尽量避开高强度降雨，减少严重侵蚀事件的发生。

Abstract

[Objective] The law of sediment yield in a karst trough valley was studied to provide a theoretical basis for the prevention and control of soil and water loss on the slope of the trough area.[Methods] Based on the runoff plots of Zhongliang Mountain at Beibei District of Chongqing City

the effects of land use types (cultivated land

woodland

orchard

and bamboo forest land)

rainfall grade

and rainfall characteristics on runoff and sediment yield on slopes were investigated.[Results] ① The total runoff of the four runoff plots was as follows:cultivated land (35.35 mm)

followed by orchard land (31.51 mm)

bamboo forest land (23.47 mm)

and forest (19.57 mm). The runoff coefficient of them (3.12%~0.5.70%) was much lower than that of the nonkarst area (approximately 20%). The slope sediment yield of the four land uses decreased orderly

and that of the cultivated land was the largest (3.37 kg)

followed by orchards (2.60 kg)

forest (1.60 kg)

and bamboo forest (1.43 kg). ② Although rainstorm accounted for 1.53% of the total rainfall

the runoff and sediment yield accounted for 42.28% and 33.42%

respectively. Moderate rain accounted for 16.61% of the total annual runoff

and sediment yield accounted for 20.47% of the total annual sediment yield. However

because of the frequent rainfall of moderate rain

the sediment loss caused by it can not be ignored. ③ Rainfall had the greatest impact on the runoff on slopes under different land uses. Moreover

I30 had the greatest impact on the sediment yield of cultivated land and orchards

and rainfall had the greatest impact on the sediment yield of forest land and orchards.[Conclusion] Under the same rainfall conditions

the runoff and sediment yield of cultivated land are the largest

followed by those of orchards. Under certain slope conditions

different levels of rainfall are the main factors affecting runoff and sediment yield. Therefore

when arranging agricultural activities

it is necessary to avoid high-intensity rainfall to reduce the occurrence of serious erosion events.

关键词

Keywords

references

王正雄,蒋勇军,张远嘱,等.基于GIS与地理探测器的岩溶槽谷石漠化空间分布及驱动因素分析[J].地理学报,2019,74(5):1025-1039.

杜文鹏,闫慧敏,甄霖,等.西南岩溶地区石漠化综合治理研究[J].生态学报,2019,39(16):5798-5808.

Dlamini P, Orchard C, Jewitt G, et al. Controlling factors of sheet erosion under degraded grasslands in the sloping lands of KwaZulu-Natal, South Africa[J]. Agricultural Water Management, 2011,98(11):1711-1718.

Fu Bojie, Wang Shuai, Liu Yu, et al. Hydrogeomorphic ecosystem responses to natural and anthropogenic changes in the loess plateau of China[J]. Annual Review of Earth and Planetary Sciences, 2017,45(1):223-243.

Raclot D, le Bissonnais Y, Annabi M, et al. Main issues for preserving Mediterranean soil resources from water erosion under global change[J]. Land Degradation & Development, 2018,29(3):789-799.

Liang Yue, Jiao Juying, Tang Bingzhe, et al. Response of runoff and soil erosion to erosive rainstorm events and vegetation restoration on abandoned slope farmland in the Loess Plateau region, China[J]. Journal of Hydrology, 2020,584:124694.

Gao Jiangbo, Wang Huan. Temporal analysis on quantitative attribution of karst soil erosion:A case study of a peak-cluster depression basin in Southwest China[J]. Catena, 2019,172:369-377.

Chen Hongsong, Liu Jianwei, Wang Kelin, et al. Spatial distribution of rock fragments on steep hillslopes in karst region of northwest Guangxi, China[J]. Catena, 2011,84(1/2):21-28.

常勇,姜光辉,康彩霞,等.峰丛洼地坡面流径流过程:以丫吉试验场为例[J].水文,2010,30(6):19-23.

Bookhagen B. Appearance of extreme monsoonal rainfall events and their impact on erosion in the Himalaya[J]. Geomatics, Natural Hazards and Risk, 2010,1(1):37-50.

Bryndal T, Franczak P, Kroczak R, et al. The impact of extreme rainfall and flash floods on the flood risk management process and geomorphological changes in small Carpathian catchments:A case study of the Kasiniczanka river(Outer Carpathians, Poland)[J]. Natural Hazards, 2017,88(1):95-120.

Chen Hao, Zhang Xiaoping, 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.

Wang Zhijie, Jiao Juying, Rayburg S, et al. Soil erosion resistance of "Grain for Green" vegetation types under extreme rainfall conditions on the Loess Plateau, China[J]. Catena, 2016,141:109-116.

Cerdà A, Lucas Borja M E, Ubeda X, et al.

Pinus halepensis

M. versus

Quercus ilex

subsp.

Rotundifolia

L. runoff and soil erosion at pedon scale under natural rainfall in Eastern Spain three decades after a forest fire[J]. Forest Ecology and Management, 2017,400:447-456.

Mohamadi M A, Kavian A. Effects of rainfall patterns on runoff and soil erosion in field plots[J]. International Soil and Water Conservation Research, 2015,3(4):273-281.

González-Pelayo O, Andreu V, Gimeno-García E, et al. Rainfall influence on plot-scale runoff and soil loss from repeated burning in a Mediterranean-shrub ecosystem, Valencia, Spain[J]. Geomorphology, 2010,118(3/4):444-452.

Yan Youjin, Dai Quanhou, Yuan Yingfei, et al. Effects of rainfall intensity on runoff and sediment yields on bare slopes in a karst area, SW China[J]. Geoderma, 2018,330:30-40.

Peng Tao, Wang Shijie. Effects of land use, land cover and rainfall regimes on the surface runoff and soil loss on karst slopes in southwest China[J]. Catena, 2012,90:53-62.

张晶晶,王力.坡面产流产沙影响因素的灰色关联法分析[J].水土保持通报,2011,31(2):159-162.

路炳军,王志强.北京西部山区径流小区产流产沙和土壤养分流失特征[J].中国水土保持科学,2015,13(6):33-39.

Fu Z Y, Chen H S, Zhang W, et al. Subsurface flow in a soil-mantled subtropical dolomite karst slope:A field rainfall simulation study[J]. Geomorphology, 2015,250:1-14.

Wischmeier W H, Smith D D. Rainfall energy and its relationship to soil loss[J]. Eos, Transactions American Geophysical Union, 1958,39(2):285-291.

肖金强,张志强,武军.坡面尺度林地植被对地表径流与土壤水分的影响初步研究[J].水土保持研究,2006,13(5):227-231.

彭韬,王世杰,张信宝,等.喀斯特坡地地表径流系数监测初报[J].地球与环境,2008,36(2):125-129.

何周窈,苏正安,熊东红,等.金沙江干热河谷区坡面剑麻的水土保持效应[J].山地学报,2018,36(5):731-739.

田太强,何丙辉,闫建梅.不同施肥与耕作模式下紫色土坡地产流特征[J].水土保持通报,2014,34(3):1-5.

吴泽,蒋勇军,姜光辉,等.中梁山岩溶槽谷区不同土地利用方式坡地产流规律[J].生态学报,2019,39(16):6072-6082.

Zhou Ji, Fu Bojie, Gao Guangyao, et al. Effects of precipitation and restoration vegetation on soil erosion in a semi-arid environment in the Loess Plateau, China[J]. Catena, 2016,137:1-11.

Sun Long, Zhang Guanghui, Liu Fa, et al. Effects of incorporated plant litter on soil resistance to flowing water erosion in the Loess Plateau of China[J]. Biosystems Engineering, 2016,147:238-247.

Wang Lunjiang, Zhang Guanghui, Wang Xue, et al. Soil loss:Effect of plant litter incorporation rate under simulated rainfall conditions[J]. Land Degradation & Development, 2019,30(10):1193-1203.

Patin J, Mouche E, Ribolzi O, et al. Effect of land use on interrill erosion in a montane catchment of Northern Laos:An analysis based on a pluri-annual runoff and soil loss database[J]. Journal of Hydrology, 2018,563:480-494.

陈利顶,贾福岩,汪亚峰.黄土丘陵区坡面形态和植被组合的土壤侵蚀效应研究[J].地理科学,2015,35(9):1176-1182.

张远瞩,蒋勇军,李勇,等.隧道工程对喀斯特槽谷区坡面产流及土壤侵蚀的影响[J].生态学报,2019,39(16):6126-6135.

Views

1303

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Runoff and sediment yield characteristics of typical soil slopes in Xin’an River basin under different rainfall intensities and slope gradients

Soil and water conservation effects of two urban shrubs under simulated rainfall conditions

Simulation of soil erosion resistance and soil erosion process in arid valley region of southeastern Xizang Autonomous Region

Effects of rainfall characteristics on runoff and sediment yield under different land use types in typical small watershed of Jialing River

Soil Erosion Processes on Sloping Grassland in Heaven Lake Nature Reserve of Xinjiang Wei Autonomous Region

Related Author

Yuan Wei

Yue Zhongshuai

Ren Jijun

Sun Zelong

Song Zhen

Chen Juanjuan

Wang Xinyu

Zhao Tonghui

Related Institution

Huangshan Observation and Research Station for Land-Water Resources

Changsha General Survey of Natural Resources Center， China Geological Survey

Zhanyi Karst Ecosystem Positioning Observation;Research Station， National Forestry and Grassland Administration

College of Soil and Water Conservation， Southwest Forestry University

Soil and Water Conservation Bureau of the Xizang Autonomous Region，， Xizang

⁰