RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2019, Vol. 28 >> Issue (06): 1491-1501.doi: 10.11870/cjlyzyyhj201906023

Previous Articles     Next Articles

Cooperation Analysis of High-Risk Periods and Priotiry Control Areas of Soil Erosion in the Middle and Lower Reaches of Hanjiang River Basin

RUAN Shu-he1, ZHUANG Yan-hua2, WANG Li-hui2,TANG Xian-qiang3, ZHANG Liang2, DU Yun2, HONG Song1   

  1. (1. School of Resource and Environmental Science, Wuhan University, Wuhan 430079, China; 2. Institute of Geodesy and Geophysics, Chinese Academy of Sciences,Hubei Provincial Engineering Research Center of Xlon-Point Source Pollution Control, Wuhan 430077, China; 3. Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan 430010, China)
  • Online:2019-06-20 Published:2019-06-20

Abstract: High-risk periods and priority control areas refer to the main periods and areas of soil erosion, respectively. Identification of high-risk periods and priority control areas of soil erosion on monthly scale has important practical significance for the protection of soil and water resources. Based on the USLE model, the temporal and spatial distribution characteristics of soil erosion in each month in the middle and lower reaches of the Hanjiang River Basin were analyzed quantitatively. By using the cooperation analysis of high-risk periods and priority control areas, the high-risk periods of soil erosion were identified quantitatively based on the erosion-period curve, and then the priority control areas in high-risk periods were identified based on the erosion-area curve. The results showed that the soil erosion in the middle and lower reaches of the Hanjiang River Basin in 2010 has the characteristic of concentrated distribution. The severe erosion areas were mainly distributed in the northwest and southeast of the basin, accounting for 11.70% of the basin area. The areas with mild and slight erosion were mainly distributed in the east and south of the basin with lower slopes, accounting for 88.30% of the basin area. The high-risk periods of soil erosion in the basin were months 4 and 7, and the amount of soil erosion accounted for 69.12% of the year. And the amount of soil erosion in July was the highest, accounting for 41.83% of the whole year, followed by April, accounting for 27.29% of the year. In the high-risk periods of soil erosion in the middle and lower reaches of the Hanjiang River Basin, the priority control areas accounted for 12.22% of the basin area, and the amount of the erosion reached 82.01% of the basin. The priority control areas were mainly distributed in the north, west and southeast of the basin. The control efficiency of soil erosion can be greatly improved by controlling priority control areas in high-risk periods.

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] XU You-peng, YU Rui-hong, MA Zong-wei. ANALYSIS ON THE CAUSE OF FORMATION OF FLOOD DISASTER AND FLOOD CHARACTERISTICS IN THE MIDDLE AND LOWER REACHES OF THE YANGTZE RIVER[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2005, 14(5): 638 -643 .
[2] HU Zhen-Peng, GE Gang, LIU Cheng-Lin, CHEN Fu-Sheng, LI SHU. STRUCTURE OF POYANG LAKE WETLAND PLANTS ECOSYSTEM AND INFLUENCE OF LAKE WATER LEVEL FOR THE STRUCTURE[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2010, 19(06): 597 .
[3] YI Shi-Yong, LOU Bao-Feng, LIU Hui, LAN Jing, YUAN Lin, ZHANG Qi, ZANG Xiao-Pin. ANALYSIS OF WATER QUALITY OF THE YANGTZE RIVER WITHIN THE THREE GORGES RESERVOIR AREA DURING CONSTRUCTION PERIOD [J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2011, 20(3): 305 .
[4] SUN Pingjun. IDENTIFICATION OF NONCOORDINATION BETWEEN URBANIZATION #br# AND ECOLOGICAL ENVIRONMENT IN JIANGSU #br# PROVINCE DURING 1994-2011[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2014, 23(08): 1051 .
[5] HU Zhengpeng, GE Gang, LIU Chenglin. CAUSE ANALYSIS AND EARLY WARNING FOR WETLAND VEGETATION DEGRADATION IN POYANG LAKE[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(03): 381 .
[6] LI Yangjie1, CHEN Zhenlou1, WANG Chu2, HU Hong1. EXCHANGE FLUXES OF N2O BETWEEN INTERTIDAL WETLANDS AND  ATMOSPHERE DURING THE LOW AND HIGH TIDES IN YANGTZE ESTUARY[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(03): 408 .
[7] SHEN Jinghong1,4, YU Zhaowang2, SHEN Hongting3, LU Yuqi4. EVOLUTION OF SPACE STRUCTURE AND SPATIAL INTEGRATION BASED ON AMENDED FIELD MODEL DIFFERENT〖WT4”BZ〗——A CASE OF THE PAN YANGTZE RIVER DELTA[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(04): 557 .
[8] CHEN Xin-chi, ZHANG Li-ping, SHAN Li-jie, YANG Wei, XU Xia. JOINT DISTRIBUTION OF THE EXTREME RAINFALL AND FLOOD FOR THE UPPER-MIDDLE REACHES OF THE HANJIANG RIVER BASED ON COPULA FUNCTION[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(08): 1425 -1433 .
[9] ZHOU Shao-fu, ZHAO Ming-ling, SU Long. An empirical study of the carbon emissions kuznets curve for china——based on gregory-hansen cointegration test[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(09): 1471 -1476 .
[10] LI Ji-zhou, WU Hai-xu, JIANG Wan, YUAN Xu-yin, LIU Bin-wu. POLLUTION CHARACTERISTICS AND ECOLOGICAL RISK ASSESSMENT OF SEDIMENT FROM MALODOROUS RIVERS IN NANJING CITY[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2015, 24(11): 1913 -1919 .