Spatial differentiation and driving factors of soil erosion in woodland and garden in the northern Dabie Mountain
HUANG Yunan1, QI Fei2, YUAN Li3, LIU Xia1, TAN Lin4, LU Wei1, YAO Xiaoyou3
1. Collaborative Innovation Center of Southern Modern Forestry, Jiangsu Key Laboratory of Soil and Water Conservation and Ecological Restoration, Nanjing Forestry University, 210037, Nanjing, China; 2. Jiangsu Hydraulic Science Institute, 210017, Nanjing, China; 3. Mornitoring Center Station of Soil and Water Conservation, Huaihe River Commission, Ministry of Water Resources, 233001, Bengbu, Anhui, China; 4. High School Affiliated to Nanjing Normal University, 210037, Nanjing, China
Abstract:Background Since the 1980s, the northern foot of Dabie Mountain has experienced the second forestry venture and the reconstruction of low-efficiency forest, Some mixed woodland, shrub woodland and open woodland have been reclaimed as garden at different times, which has become the new source of soil erosion and affected the ecological security of the region. In order to better manage economic forest and effectively carry out the prevention and control of soil erosion, it is necessary to find out the spatial distribution characteristics and soil erosion law of woodland and garden in this area.Methods With Shangcheng county as the research area, woodland and garden as the research object. Woodland and garden types were interpreted based on high-resolution remote sensing images, topographic maps, field surveys and other data. Soil erosion was calculated using the Chinese soil loss equation, and the leading factors of soil erosion and were the interaction of factors were detected by geographic detectors. Results 1) Woodland and garden account for 56.06% of the total land area. Woodland is dominated by Pinus, Quercus and mixed woodland , and garden is mainly tea (Camellia sinensis) garden and oil camellia (Camellia oleifera) garden, which are mainly distributed in the southern, eastern and northwestern areas of 0-500 m and 0-15°. 2) The proportion of soil and water loss 8in woodland and garden was 33.78%, which was mainly slight erosion, mainly distributed in Pinus, Quercus and mixed woodland , and moderate or above erosion intensity was concentrated in oil camellia (C. oleifera) garden, tea (C. sinensis)garden and chestnut (Castanea mollissima) woodland. Oil camellia (C. oleifera) garden and tea (C. sinensis)garden above 15° and without soil and water conservation measures are the main areas where high intensity erosion of soil and water loss occurs. 3) Soil erosion in oil camellia (C. oleifera) garden was dominated by soil and water conservation measures, while slope was dominant in other woodland and garden types. The interaction between woodland and garden types is most significant with slope as the core and other influencing factors.Conclusions This study had investigated the spatial distribution and soil erosion characteristics of woodland and garden , and identified slope as the main factors of soil erosion. The results can provide scientific basis for the comprehensive control of soil and water loss and the spatial layout of soil and water conservation measures in woodland and garden in Dabie Mountain area. In the future, attention should be paid to soil and water loss above 15°, especially in tea (C. sinensis) garden, oil camellia (C. oleifera) garden and chestnut (C. mollissima) woodland which are highly affected by human activities and prone to high intensity soil and water loss.
黄昱楠, 齐斐, 袁利, 刘霞, 谭林, 陆威, 姚孝友. 大别山北麓林地与园地土壤侵蚀空间分异及驱动分析[J]. 中国水土保持科学, 2025, 23(1): 51-61.
HUANG Yunan, QI Fei, YUAN Li, LIU Xia, TAN Lin, LU Wei, YAO Xiaoyou. Spatial differentiation and driving factors of soil erosion in woodland and garden in the northern Dabie Mountain. SSWC, 2025, 23(1): 51-61.
张荣华,刘霞,姚孝友,等. 桐柏大别山区土壤侵蚀敏感性评价及空间分布[J]. 中国水土保持科学,2010,8(1):58.ZHANG Ronghua,LIU Xia,YAO Xiaoyou,et al. Assessment and spatial distribution of soil erosion sensitivity in Tongbai-Dabie mountainous area[J]. Science of Soil and Water Conservation,2010,8(1):58.
[2]
杨伟,李璐,欧阳曙光,等. 大别山区板栗林地水土流失特性研究[J]. 水土保持通报,2022,42(2):259.YANG Wei,LI Lu,OUYANG Shuguang,et al. Characteristics of soil and water loss at Castanea mollissima woodlands in Dabie mountain area[J]. Bulletin of Soil and Water Conservation,2022,42(2):259.
[3]
水利部水土保持监测中心. 全国水土流失动态监测成果预防区卷[R]. 北京,2021:67.Soil and Water Conservation Monitoring Center,Ministry of Water Resources. National soil erosion dynamic monitoring results prevention area volume[R]. Beijing,2021:67.
[4]
张荣华,刘霞,姚孝友,等. 桐柏大别山区土壤侵蚀特征分析[J]. 水土保持研究,2010,17(1):24.ZHANG Ronghua,LIU Xia,YAO Xiaoyou,et al. Analysis on characters of soil erosion in Tongbai-Dabie mountainous area[J]. Research of Soil and Water Conservation,2010,17(1):24.
[5]
张杰,赵冰,杨伟,等. 基于ArcGIS的淮河流域大别山区土地利用变化与土壤侵蚀特征研究[J]. 水土保持通报,2009,29(1):119.ZHANG Jie,ZHAO Bing,YANG Wei,et al. Landuse changes and soil erosion in the Dabie mountain area of Huaihe River Basin based on ArcGIS[J]. Bulletin of Soil and Water Conservation,2009,29(1):119.
[6]
郭珂歆,艾刚,马兴祥,等. 北方土石山区土壤侵蚀对典型地形因子的响应:以北京市房山区为例[J]. 中国水土保持科学,2021,19(4):137.GUO Kexin,AI Gang,MA Xingxiang,et al. Response of soil erosion to typical topographic factors in the rocky mountain area of North China:Taking Fangshan district as an example[J]. Science of Soil and Water Conservation,2021,19(4):137.
[7]
王慧琴,孙保平,余新晓,等. 华北北部区域土壤侵蚀及影响因素的时空变化[J]. 中国水土保持科学,2021,19(3):8.WANG Huiqin,SUN Baoping,YU Xinxiao,et al. Spatio-temporal variations of soil erosion and its drivers in the northern region of North China[J]. Science of Soil and Water Conservation,2021,19(3):8.
王欢,高江波,侯文娟. 基于地理探测器的喀斯特不同地貌形态类型区土壤侵蚀定量归因[J]. 地理学报,2018,73(9):1674.WANG Huan,GAO Jiangbo,HOU Wenjuan. Quantitative attribution analysis of soil erosion in different morphological types of geomorphology in karst areas:Based on the geographical detector method[J]. Acta Geographica Sinica,2018,73(9):1674.
[10]
常梦迪,王新军,李娜,等. 基于CSLE模型的天山北坡中段山区水力侵蚀时空变化特征及影响因素研究[J]. 干旱区研究,2021,38(4):939.CHANG Mengdi,WANG Xinjun,LI Na,et al. Study on temporal and spatial variation characteristics and influencing factors of hydraulic erosion in the middle of the northern slope of Tianshan Mountains based on CSLE model[J]. Arid Zone Research,2021,38(4):939.
[11]
姚昆,周兵,何磊,等. 基于地理探测器的岷江上游地区土壤侵蚀变化[J]. 水土保持研究,2022,29(2):85.YAO Kun,ZHOU Bing,HE Lei,et al. Changes in soil erosion in the upper reaches of the Minjiang River based on geo-detector[J]. Research of Soil and Water Conservation,2022,29(2):85.
[12]
李亚平,卢小平,张航,等. 基于GIS和RUSLE的淮河流域土壤侵蚀研究:以信阳市商城县为例[J]. 国土资源遥感,2019,31(4):243.LI Yaping,LU Xiaoping,ZHANG Hang,et al. Soil erosion in Huaihe River Basin based on GIS and RUSLE:Exemplified by Shangcheng county,Xinyang city[J]. Remote Sensing for Land & Resources,2019,31(4):243.
[13]
刘荷芬,王令超,崔波. 桐柏大别山区森林植被及其开发利用研究[J]. 河南林业科技,1996(2):8.LIU Hefen,WANG Lingchao,CUI Bo. Study on forest vegetation and its exploitation and utilization in Tongbai Dabie mountain area[J]. Journal of Henan Forestry Science and Technology,1996(2):8.
[14]
商城县土壤普查办公室. 商城土壤[M]. 河南商城:商城县土壤普查办公室,1986:43.Soil Census Office of Shangcheng County. Soil of Shangcheng cocunty[M]. Shangcheng,Henan: Soil Census Office in Shangcheng County,1986:43.
[15]
YU B,ROSEWELL C J. A robust estimator of the R-factor for the universal soil loss equation[J]. Transactions of the ASAE,1996,39(2):559.
[16]
KIANI F,GHEZELSEFLO A. Evaluation of soil erodibility factor (k) for loess derived landforms of Kechik watershed in Golestan province,North of Iran[J]. Journal of Mountain Science,2016,13(11):2028.
[17]
符素华,刘宝元,周贵云,等. 坡长坡度因子计算工具[J]. 中国水土保持科学,2015,13(5):105.FU Suhua,LIU Baoyuan,ZHOU Guiyun,et al. Calculation tool of topographic factors[J]. Science of Soil and Water Conservation,2015,13(5):105.
[18]
ZHANG YAN,LIU BAOYUAN,ZHANG QINGCHUN,et al. Effect of different vegetation types on soil erosion by water[J]. Acta Botanica Sinica,2003,45(10):1204.
[19]
水利部办公厅. 区域水土流失动态监测技术规定(试行)[R]. 北京:水利部办公厅,2021:145.Soil and Water Conservation Monitoring Center,Ministry of Water Resources. Technical provisions for dynamic monitoring of regional soil and water loss (Trial)[R]. Beijing: General Ofice of Minitry of Water Resources,2021:145.
[20]
王飞,陈安磊,彭英湘,等. 不同土地利用方式对红壤坡地水土流失的影响[J]. 水土保持学报,2013,27(1):22.WANG Fei,CHEN Anlei,PENG Yingxiang,et al. Effects of red soil slope field under different land-use patterns on surface runoff and soil erosion[J]. Journal of Soil and Water Conservation,2013,27(1):22.