Variations of Rainfall Erosivity of Different Magnitudes in Shaoguan from 1951 to 2018

WU Jieling; ZHA Xuan; CHEN Shifa; MAO Lanhua; HUANG Bowen

doi:10.13870/j.cnki.stbcxb.2021.04.004

您当前的位置：

首页 >

文章列表页 >

Variations of Rainfall Erosivity of Different Magnitudes in Shaoguan from 1951 to 2018

更新时间：2025-03-12

- Variations of Rainfall Erosivity of Different Magnitudes in Shaoguan from 1951 to 2018
- Vol. 35, Issue 4, Pages: 21-26(2021)
- 作者机构：
  
  1. 福建师范大学地理科学学院,福州,350007
  2. 福建省亚热带资源与环境重点实验室,福州,350007
  3. 韶关学院旅游与地理学院,广东,韶关,512005
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2021.04.004
  CLC： S157.1
- Published：2021
- 稿件说明：
移动端阅览
WU Jieling, ZHA Xuan, CHEN Shifa, et al. Variations of Rainfall Erosivity of Different Magnitudes in Shaoguan from 1951 to 2018[J]. 2021, 35(4): 21-26.
DOI：

WU Jieling, ZHA Xuan, CHEN Shifa, et al. Variations of Rainfall Erosivity of Different Magnitudes in Shaoguan from 1951 to 2018[J]. 2021, 35(4): 21-26. DOI： 10.13870/j.cnki.stbcxb.2021.04.004.

摘要

降雨是引起土壤水蚀的主要动力因子之一，为探讨韶关市不同量级降雨对土壤水蚀特征造成的影响，选取1951—2018年韶关市逐日降雨量数据，采用日降雨侵蚀力模型计算降雨侵蚀力，利用变异系数、趋势系数分析不同时间尺度各量级降雨侵蚀力的变化。结果表明：（1）68年来韶关市年均降雨侵蚀力为9 314（MJ·mm）/（hm2·h·a），变异系数为0.29，属于中等变异；（2）年降雨量、降雨日数、侵蚀性降雨量和降雨日数均呈上升趋势，而非侵蚀性降雨量和降雨日数则呈下降趋势，且暴雨量和暴雨侵蚀力呈较明显上升趋势，说明韶关市降雨更为集中，降雨侵蚀力增加；（3）大雨以上量级的降雨日数和降雨量占总降雨日数和总降雨量的比例分别为43.91%，51.15%，而其引起的降雨侵蚀力占总降雨侵蚀力比例却高达77.05%。研究结果为韶关市的土壤侵蚀的监测和水土保持工作提供参考。

Abstract

Rainfall is one of the main dynamic factors that cause soil water erosion. In order to explore the effects of different levels of rainfall on the characteristics of soil water erosion in Shaoguan City

the daily rainfall data of Shaoguan City from 1951 to 2018 were selected

the daily rainfall erosivity model was used to calculate the rainfall erosivity

and the variation coefficient and trend coefficient were used to analyze the changes of rainfall erosivity indifferent time scales. The results indicated that: (1) The average annual rainfall erosivity of Shaoguan City in 68 years was 9 314 (MJ·mm)/(hm2·h·a)

and the variation coefficient was 0.29

which was a medium variation. (2) The annual rainfall

rainfall days

erosive rainfall and rainfall days showed an upward trend

while the non-erosive rainfall and rainfall days showed a downward trend

and heavy rainfall volume and rainstorm erosivity showed an obvious upward trend

indicating that rainfall was more concentrated and rainfall erosivity increased in Shaoguan City. (3) The proportion of rainfall days and rainfall over heavy rain to total rainfall days and total rainfall was 43.91% and 51.15%

respectively

while the proportion of rainfall erosivity caused by heavy rain to total rainfall erosivity was 77.05%. The results could provide reference for soil erosion monitoring and soil and water conservation in Shaoguan City.

关键词

Keywords

references

中华人民共和国水利部.2019年中国水土保持公报[R].北京:中华人民共和国水利部,2020-09-24.

章文波,谢云,刘宝元.降雨侵蚀力研究进展[J].水土保持学报,2002,16(5):43-46.

Wei W, Chen L D, Fu B J, et al. The effect of land uses and rainfall regimes on runoff and soil erosion in the semi-arid loess hilly area, China[J].Journal of Hydrology,2007,335(3/4):247-258.

章文波,谢云,刘宝元.利用日雨量计算降雨侵蚀力的方法研究[J].地理科学,2002,22(6):705-711.

Richardson C W, Forster G R, Wright D A. Estimation of erosion index from daily rainfall amount[J].Transaction of the ASAE,1983,26(1):153-156.

赖成光,陈晓宏,王兆礼,等.珠江流域1960-2012年降雨侵蚀力时空变化特征[J].农业工程学报,2015,31(8):159-167.

戴金梅,查轩,黄少燕,等.1980-2013年闽西地区降雨侵蚀力时空变化特征[J] 中国水土保持科学,2017,15(4):1-7.

鲁向晖,张海娜,白桦,等.赣江流域1986-2015年降雨侵蚀力时空变化特征[J].长江科学院院报,2020,37(10):51-58.

郑哲,邹进,潘锋,等.1961-2010年怒江流域降雨侵蚀力的时空变化特征.[J].中国水土保持科学,2018,16(5):16-22.

周琳,许武成,尹义星.近61年四川省降雨侵蚀力的时空变化趋势[J].水土保持研究,2018,25(4):8-14.

陈国清,赵银军,莫德丽,等.广西南流江流域降雨侵蚀力时空变化特征[J].广西科学,2020,27(3):303-310.

阮欧,刘绥华,杨广斌,等.1966-2017年贵州省降雨侵蚀力的时空分布特征[J].水土保持通报,2020,40(3):35-42.

姬志军,张连明.鄱阳湖流域降雨量及降雨侵蚀力时空分布特征[J].人民黄河,2019,41(6):81-84.

芦鑫,殷淑燕,高涛涛.1960-2017年秦岭南北地区降雨侵蚀力的时空变化特征研究[J].浙江大学学报(理学版),2019,46(3):380-390.

赵平伟,郭萍,李成武,等.云南不同量级降雨下的降雨侵蚀力特征分析的[J].长江流域资源与环境,2015,24(12):2135-2142.

赵平伟,郭萍.1980-2013年滇西北地区降雨侵蚀力变化特征[J].地理科学,2015,35(10):1306-1312.

章文波,付金生.不同类型雨量资料估算降雨侵蚀力[J].资源科学,2003,25(1):35-41.

章文波,谢云,刘宝元.中国降雨侵蚀力空间变化特征[J].山地学报,2003,21(1):33-40.

曹洁萍,迟道才,武立强,等. Mann-kendall检验方法在降水趋势分析中的应用研究[J].农业科技与装备,2008(5):35-37,40.

简虹,骆云中,谢德体.基于Mann-Kendall法和小波分析的降水变化特征研究:以重庆市沙坪坝区为例[J].西南师范大学学报(自然科学版),2011,36(4):217-222.

雷璐,孙春敏.Mann-Kendall检验方法在增江径流趋势分析中的应用[J].中国科技信息,2012(19):39,73.

李春晖,郑小康,杨志峰,等.黄河天然径流量变化趋势及其影响分析[J].北京师范大学学报(自然科学版),2009,45(1):80-85.

殷兵,吴健平,章文波.基于GIS的降雨侵蚀力计算器实现研究[J].水土保持研究,2014,21(4):123-126.

冯若昂,刘加珍,陈永金,等.山东省多年均降雨侵蚀力及其增长率变化分析[J].自然灾害学报,2017,26(5):83-93.

陈世发.ENSO对韶关市1951-2013年均降雨侵蚀力影响研究[J].地理科学,2016,36(10):1573-1581.

高涛,谢立安.近50年来中国极端降水趋势与物理成因研究综述[J].地球科学进展,2014,29(5):577-589.

何绍浪,郭小君,李凤英,等.中国南方地区近60 a来降雨量与降雨侵蚀力时空变化研究[J].长江流域资源与环境,2017,26(9):1406-1416.

Views

1007

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area

Effects of Prune Measure on Vegetation Characteristics and Soil Physical and Chemical Properties of

Variation Characteristics of Meteorological and Hydrological Factors in Gurt River and the Relationship Between Ebinur Lake Downstream Ecology

Soil Moisture Variation Characteristics of Different Land Use Types in the Moderate Slope Sandy Area of Loess Hilly Region

Spatial Distribution of Soil Water and Salt Under Sand Hole Planting with Drip Irrigation of Brackish Water

Related Author

WAN Jinhong

YI Jun

WANG Weijie

LU Shiguo

LIU Muxing

LI Xueting

GUO Jing

WEI Yajuan

Related Institution

Institute of Water Conservancy History, China Institute of Water Resources and Hydropower Research

College of Urban and Environmental Sciences,Central China Normal University

Hubei Key Laboratory of Geographic Process Analyzing and Simulation

Department of Resource and Environment, Baotou Teachers College

Inner Mongolia Institute of Meteorological Science

⁰