Spatial distribution of cropland soil erosion in Guizhou province based on sample data of the first national water census
YANG Zhicheng, ZHANG Zhuodong, ZHANG Keli, WEI Xin
State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, 100875, Beijing, China
Abstract:[Background] The Karst region of Southwest China is characterized with the fragile ecological environment. Guizhou province is suffering from high intensity of soil erosion and sloping cropland is the most vulnerable to soil erosion in this region. Soil erosion of sloping cropland in Guizhou province had been studied on a provincial scale, and the results are beneficial to providing a basis for promoting soil and water conservation in this region. The spatial distribution and erosion intensity of cropland are greatly affected by regional divisions by geomorphy and topographic factors; therefore, it is necessary to take regional divisions and topographic factors into consideration to determine key areas for ecological restoration in this region.[Methods] 1) The digital map of regional divisions by geomorphy was created in ArcGIS 10.2 software according to related articles. 2) By using SPSS 19.0 software (Statistical Product and Service Solutions 19.0), we explored the proportion of cropland area and the cropland soil erosion intensity in Guizhou province. 3) By using ArcGIS 10.2 software, we built spatial distribution map of the proportion of cropland area and the cropland soil erosion intensity in Guizhou province.[Results] 1) The spatial distribution pattern of cropland area proportion in Guizhou province was obvious, which decreased from west to east. The proportion of cropland in non-karst plateau was the lowest, on the contrary, it was the highest in western Karst plateau. 2) The cropland with slope gradient of 8-35° accounted for 91.28% of the total cropland, and cropland with slope length >25 m accounted for 97.81%. With the increase of slope gradient, the soil erosion modulus increased correspondingly, especially in karst area; however, with the increase of slope length, the soil erosion modulus showed no obvious trend. 3) 71.17% of the total cropland area in Guizhou province belonged to middle erosion (<200 t/km2). The soil erosion in Peak-cluster depression and Karst fractured basin region were more serious with the acute erosion areas accounting for 34.97% and 15.16% of the total cropland, respectively.[Conculsions] On the whole, the Peak-cluster depression region and the Karst fractured basin region are the key areas for soil erosion control. These findings hold important implications for agricultural management, regional soil and water conservation and ecological management in Guizhou province.
杨志成, 张卓栋, 张科利, 魏欣. 基于普查样点的贵州省耕地土壤侵蚀空间分布[J]. 中国水土保持科学, 2020, 18(2): 62-68.
YANG Zhicheng, ZHANG Zhuodong, ZHANG Keli, WEI Xin. Spatial distribution of cropland soil erosion in Guizhou province based on sample data of the first national water census. SSWC, 2020, 18(2): 62-68.
PIMENTEL D. Soil Erosion:A food and environmental threat[J]. Environment, Development and Sustainability, 2006, 8(1):119.
[2]
中华人民共和国水利部. 第一次全国水利普查水土保持情况公报[J]. 中国水土保持, 2013(10):58. Ministry of Water Resource of the People's Republic of China. The first national water conservancy survey of water and soil conservation bulletin[J]. Soil and Water Conservation in China, 2013(10):58.
[3]
王恒松, 熊康宁, 张芳美. 地形因子对喀斯特坡面水土流失影响的机理研究[J]. 水土保持通报, 2015, 35(4):2. WANG Hengsong, XIONG Kangning, ZHANG Fangmei, et al.Mechanism study on effect of terrain on soil erosion of Karst slope[J]. Bulletin of Soil and Water Conservation, 2015, 35(4):2.
[4]
陈美淇, 魏欣, 张科利, 等. 基于CSLE模型的贵州省水土流失规律分析[J]. 水土保持学报, 2017, 31(3):16. CHEN Meiqi, WEI Xin, ZHANG Keli, et al.Analysis of the characteristics of soil and water loss in Guizhou province based in CSLE[J]. Journal of Soil and Water Conservation, 2017, 31(3):16.
[5]
SHEN Haiou, ZHENG Fenli, WEN Leilei, et al. Impacts of rainfall intensity and slope gradient on rill erosion processes at loessial hillslope[J]. Soil and Tillage Research, 2016(155):436.
[6]
付兴涛, 张丽萍. 红壤丘陵区坡长对作物覆盖坡耕地土壤侵蚀的影响[J]. 农业工程学报, 2014, 30(5):94. FU Xingtao, ZHANG Liping.Impact of slope length on soil erosion of sloping farmland with crop in red soil hilly region[J]. Transactions of the CSAE, 2014, 30(5):94.
[7]
ZHANG Xingqi, HU Maochuan, GUO Xinya. Effects of topographic factors on runoff and soil loss in Southwest China[J]. Catena, 2018(160):398.
[8]
张兴奇, 顾礼彬, 张科利, 等. 坡度对黔西北地区坡面产流产沙的影响[J]. 水土保持学报, 2015, 29(4):19. ZHANG Xingqi, GU Libin, ZHANG Keli, et al. Impacts of slope gradient on runoff and sediment in Northwest Guizhou[J]. Journal of Soil and Water Conservation, 2015, 29(4):19.
[9]
蔡强国. 坡长对坡耕地侵蚀产沙过程的影响[J]. 云南地理环境研究, 1998, 10(1):36. CAI Qiangguo. Soil erosion processes influenced by slope length on slopeland[J]. Yunnan Geographic Environment Research, 1998, 10(1):36.
[10]
高儒学, 高华端, 宋江平, 等. 坡长对贵州喀斯特区黄壤坡耕地土壤侵蚀的影响[J]. 水土保持研究, 2018, 25(2):55. GAO Ruxue, GAO Huaduan, SONG Jiangping, et al. Influence of slope length on soil erosion in yellow sloping farmland of Karst[J]. Research of Soil and Water Conservation, 2018, 25(2):55.
[11]
熊康宁, 胡顺光. 贵州喀斯特地区水土流失研究进展[J]. 贵州师范大学学报(自然科学版) 2011, 29(4):109. XIONG Kangning, HU Shunguang. Evolution of soil and water loss in Guizhou Karst area[J]. Journal of Guizhou Normal University (Natural Sciences) 2011, 29(4):109.
[12]
刘宝元, 郭索彦, 李智广, 等. 中国水力侵蚀抽样调查[J]. 中国水土保持, 2013, 34(10):29. LIU Baoyuan, GUO Suoyan, LI Zhiguang, et al. Sampling program of water erosion inventory of China[J]. Soil and Water Conservation in China, 2013, 34(10):29.
[13]
郭继成, 顾再柯, 苑爽, 等. 西南喀斯特地区水土保持措施因子值计算与评价[J]. 中国水土保持, 2014(10):50. GUO Jicheng, GU Zaike, YUAN Shuang, et al. Calculation and evaluation of factor value of water and soil conservation measures of Southwest Karst region[J]. Soil and Water Conservation in China, 2014(10):50.
[14]
吴协保, 孙继霖, 林琼, 等. 我国西南岩溶石漠化土地生态建设分区治理思路与途径探讨[J].中国岩溶, 2009, 28(4):392. WU Xiebao, SUN Jilin, LIN Qiong, et al. Research on division treatment to eco-construction of karst rock deserted land in southwest China karst area[J]. Carsologica Sinica, 2009, 28(4):392.
[15]
王世杰, 张信宝, 白晓永. 中国南方喀斯特地貌分区纲要[J]. 山地学报, 2015, 33(6):646. WANG Shijie, ZHANG Xinbao, BAI Xiaoyong. An outline of Karst geomorphology zoning in the Karst areas of Southern China[J]. Mountain Research, 2015, 33(6):646.
[16]
蒋荣. 地形因子对贵州喀斯特地区坡面土壤侵蚀的影响[D]. 南京:南京大学, 2013:29. JIANG Rong. Impacts of topographic factors on soil erosion of slope land in karst areas in Guizhou province[D]. Nanjing:Nanjing University, 2013:29.
[17]
王占礼, 王亚云, 黄新会, 等. 黄土裸坡土壤侵蚀过程研究[J]. 水土保持研究, 2004, 11(4):86. WANG Zhanli, WANG Yayun, HUANG Xinhui, et al. Soil erosion process research of the loess bare slope[J]. Research of Soil and Water Conservation, 2004, 11(4):86.
[18]
LIU Quan, ZHU Bo, TANG Jialiang, et al. Hydrological processes and sediment yields from hillslope croplands of regosol under different slope gradients at loessial hillslope[J]. Soil Science Society of America Journal, 2017, 81(6):1523.
[19]
WU Lei, PENG Mengling, QIAO Shanshan, et al. Effects of rainfall intensity and slope gradient on runoff and sediment yield characteristics of bare loess soil[J]. Environmental Science and Pollution Research, 2018, 25(4):3483.
[20]
MOHAMMAD A G, MOHAMMADA. A. The impact of vegetative cover type on runoff and soil erosion under different land uses[J]. Catena, 2010, 81(2):102.
[21]
WEI Wei, CHEN Liding, FU Bojie, et al. Water erosion response to rainfall and land use in different drought-level years in a loess hilly area of China[J]. Catena, 2010, 81(1):29.