RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2016, Vol. 25 >> Issue (01): 63-70.doi: 10.11870/cjlyzyyhj201601008

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RESEARCH ON DIFFERENT SOIL LAYERS OF COLLAPSING GULLY FRACTAL CHARACTERISTICS AND EROSION CHARACTERISTICS IN TONGCHENG

DENG Yu-song1, LI Shuang-xi2, DING Shu-wen1, CAI Chong-fa1, XIA Dong1, LIU Dan-lu1   

  1. 1. Research Center of Water and Soil Conservation, Huazhong Agricultural University, Wuhan 430070, China;
    2. Changjiang Soil Conservation Monitoring Centre, CWRC, Wuhan 430010, China
  • Received:2015-05-06 Revised:2015-07-22 Online:2016-01-20

Abstract: Collapsing gully is an extremely serious soil erosion type in the southeast of Hubei Province, which has a wide range of influence and destruction. Therefore, it is important to study the mechanism of the collapsing gully and erosion mechanism for improving the ecological environment of agricultural areas. We chose the granite in Tongcheng County, Southeastern Hubei collapsing at different levels to study soil, mainly toanalyze collapsing gully profile fractal dimension of soil particle, erodibility, permeability and water stability, and through regression analysis and other methods to establish the relationship between soil properties. Results showed that:the soil of collapsing gully in Tongcheng County in Southeastern Hubei topsoil layer, clay layer and markings layer and debris layer properties are quite different, soil particle fractal dimension D from surface soil to detritus layer showed a decreasing trend, soil erodibility K values from surface soil to detritus layer showed an increasing trend, water stable index showed a decreasing trend, permeability is laterite layer and the surface soil layer and debris layer of rules. At the same time, the correlation analysis and multivariate linear regression analysis showed that profiles of slope disintegration of soil particle fractal dimension, can be erosion resistance, permeability and water stability between closely related, the correlation between anti erodibility and soil properties significantly. The purpose of this study is to clarify the internal factors of the occurrence of collapsing gully, and to provide a basis for the occurrence mechanism of the collapsing gully.

Key words: Collapsing Gully, fractal dimension, erodibility, permeability, water stability

CLC Number: 

  • S157.1
[1] 李双喜, 桂惠中, 丁树文. 中国南方崩岗空间分布特征[J].华中农业大学学报, 2013, 32(1):83-86.[LI S X, GUI H Z, DING S W. Features of special layout of hill collapse in south China[J]. Journal of Huazhong Agricultural University, 2013, 32(1):83-88.]
[2] 唐克丽.中国水土保持[M].北京:科学出版社,2004:80-82.[TANG K L. Soil and water conservation in China[M].Beijing:Science Press, 2004:80-82.]
[3] XU J X. Benggang erosion:the influencing factors[J]. Catena, 1996, 27(3/4):249-263.
[4] 邓羽松,丁树文,梁传平,等.安溪崩岗洪积扇不同培肥方式的土壤理化效应[J].水土保持学报,2014,28(4):168-171.[DENG Y S, DING S W, LIANG C P, et al.Effect of different fertilization methods on physico-chemical properties of collapsing gully alluvial sector in Anxi county[J]. Journal of soil and water conservation, 2014, 28(4):168-171.]
[5] 龙莉, 丁树文, 蔡崇法, 等. 花岗岩红壤丘陵区崩岗侵蚀对农田的危害及治理[J]. 中国水土保持, 2013(12):24-26.[LONG L, DING S W, CAI C F, et al. Damage and treatment of farmland in granite red soil hilly region incollapsing gully[J]. Soil and water conservation in China, 2013 (12):24-26.]
[6] 邓羽松,丁树文,蔡崇法,等.鄂东南崩岗洪积扇土壤物理性质空间分异特征[J].中国农业科学,2014,47(24):4850-4857.[DENG Y S, DING S W, CAI C F, et al. Spatial Distribution of the Collapsing Alluvial Soil Physical Properties in Southeastern Hubei[J]. Scientia Agricultura Sinica, 2014, 47(24):4850-4857.]
[7] GONG J G, JIA Y W, ZHOU Z H, et al. An experimental study on dynamic processes of ephemeral gully erosion in loess landscapes[J]. Geomorphology, 2011, 125(1):203-213.
[8] 陈晓安,杨洁,熊永,等.红壤区崩岗侵蚀的土壤特性与影响因素研究[J].水利学报,2013,44(10):1175-1181.[CHEN X A, YANG J, XIONG Y, et al. Research on the soil characteristics and factors of collapsing erosion in the red soil zone[J]. SHULI XUEBAO, 2013, 44(010):1175-1181.]
[9] 任兵芳,丁树文,吴大国,等.鄂东南崩岗土体特性分析[J].人民长江,2013,44(3):93-96.[REN B F, DING S W, WU D G, et al. Analysis on soil characteristics of collapse hills in southeast of Hubei Province[J]. Yangtze River, 2013, 44(3):93-96.]
[10] 林敬兰,黄炎和,蒋芳市,等.崩岗土体的渗透性能机理研究[J].水土保持学报,2013,27(2):53-56,144.[LIN J L, HUANG Y H, JIANG F S, et al. Study on the mechanis of different soil layer's permeability in Benggang[J]. Journal of soil and water conservation, 2013, 27(2):53-56, 144.]
[11] 张晓明,丁树文,蔡崇法.干湿效应下崩岗区岩土抗剪强度衰减非线性分析[J].农业工程学报,2012,28(5):241-245.[ZHANG X M, DING S W, CAI C F. Effects of drying and wetting on nonlinear decay of soil shear strength in slope disintegration erosion area[J]. Transactions of the Chinese Society of Agricultural Engineering, 2012, 28(5):241-245.]
[12] 李万能,金平伟,李岚斌,等.南方红壤丘陵区崩岗成因机理的研究进展[J].亚热带水土保持,2014,26(3):30-33, 43.[LI W N, JIN P W, LI L B, et al. Research progress of formation mechanism of collapse in red soil hilly region in South China[J]. subtropical soil and water conservation, 2014, 26 (3):30-33.]
[13] XIA D, DENG Y S, Wang S L, et al. Fractal features of soil particle-size distribution of different weathering profiles of the collapsing gullies in the hilly granitic region, south China[J]. Natural Hazards, 2015 (79):455-478.
[14] 徐冰,陈亚新,郭克贞.半干旱草地土壤粒径分形维数及空间变异特征[J].水利学报,2008(S1):691-695.[XU B, CHEN Y X, GUO K Z. Spatial variability of fractal dimension for soil particle in semi-arid grassland[J]. Journal of Hydraulic Engineering, 2008(S1):691-695.]
[15] HUANG G H, ZHANG R D. Evaluation of soil water retention curve with the pore-solid fractal model[J]. Geoderma, 2005, 127(1/2):52-61.
[16] MANDELBROT B B. The Fractal Geometry of Nature[M]. New York:The Fractal Geometry of Nature. W. H. Freeman and Company, 1982.
[17] TYLER S W, WHEATCRAFT S W. Fractal scaling of soil particle-size distributions:analysis and limitations[J]. Soil Science Society of America Journal, 1992, 56(2):362-369.
[18] 杨培岭,罗远培,石元春.用粒径的重量分布表征的土壤分形特征[J].科学通报,1993,38(20):1896-1899.[YANG P L, LUO Y P, SHI Y C.Fractal characteristics of soil by weight distribution of particle size[J]. Science Bulletin, 1993, 38(20):1896-1899.]
[19] WANG B, ZHENG F L, RÖMKENS M J M, et al. Soil erodibility for water erosion:a perspective and Chinese experiences[J]. Geomorphology, 2013, 187:1-10.
[20] 宋春风,陶和平,刘斌涛,等.长江上游地区土壤可蚀性空间分异特征[J].长江流域资源与环境,2012,21(9):1123-1130.[SONG C F, TAO H P, LIU B T, et al. Spatial distribution characteristics of soil erodibility Kvariation in the upper Yangtze River[J]. Resources and environment in the Yangtze River Basin, 2012, 21(9):1123-1130.]
[21] WANG B, ZHENG F L, MATHIAS J M. Comparison of soil erodibility factors in USLE, RUSLE2, EPIC and Dg models based on a Chinese soil erodibility database[J]. Acta Agriculturae Scandinavica, Section B-Soil & Plant Science, 2013, 63(1):69-79.
[22] 朱明勇,谭淑端,张全发.南水北调中线工程水源地的土壤可蚀性特征[J].长江流域资源与环境,2014,23(8):1161-1165.[ZHU M Y, TAN S D, ZHANG Q F. Characteristic of soil erodibility in the south to north warer transfer project(middle route), China[J]. Resources and environment in the Yangtze River Basin, 2014, 23(8):1161-1165.]
[23] 刘震.水土保持监测技术[M].北京:中国大地出版社,2004.[LIU Z. Soil and water conservation monitoring technology[M]. Beijing:China earth press, 2004.]
[24] 张甘霖,龚子同.土壤调查实验室分析方法[M].北京:科学出版社,2012.[ZHANG G L. Analytical method of soil survey laboratory[M]. Science Press, 2012.]
[25] 南京农学院.土壤农化分析[M].北京:农业出版社,1980.[Nanjing agricultural college.[M]. Agriculture Press agricultural soil analysis, 1980.]
[26] 雷廷武, 张婧, 王伟, 等. 土壤环式入渗仪测量效果分析[J]. 农业机械学报, 2013, 44(12):99-104.[LEI T W, ZHANG J, WANG W, et al. Assessment on soil infiltration[J].Transactions of the Chinese Society for Agricultural Machinery, 2013, 44(12):99-104.]
[27] 单奇华,李卫正,俞元春,等.南京城市林业土壤可蚀性及影响因素[J].南京林业大学学报(自然科学版),2008,32(2):47-50.[SHAN Q H, LI W Z, YU Y C, et al. Erodibility of urban forest soil in Nanjing[J].Journal of Nanjing Forestry University (Natural Sciences Edition), 2008, 32(2):47-50.]
[28] 蒋芳市,黄炎和,林金石,等.花岗岩崩岗崩积体颗粒组成及分形特征[J].水土保持研究,2014,21(6):175-180.[JIANG F S, HUANG Y H, LIN J S, et al.Soil particle size distribution and fractal dimension of colluvial deposit in granite Benggang[J]. Research of Soil and water conservation, 2014, 6:175-180.]
[29] 吴志峰,王继增.华南花岗岩风化壳岩土特性与崩岗侵蚀关系[J].水土保持学报,2000,14(2):31-35.[WU Z F, WANG J Z. Relationship Between Slope Disintegration and Rock-soil Characteristics of Granite Weathering Mantle in South China[J]. Journal of soil and water conservation, 2000, 14(2):31-35.]
[30] 党亚爱,李世清,王国栋,等.黄土高原典型土壤剖面土壤颗粒组成分形特征[J].农业工程学报,2009,25(9):74-78.[DANG Y A, LI S Q, WANG G D, et al. Fractal characteristics of soil particle composition for typical types of soil profile on Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering, 2009 (9):74-78.]
[31] 王艳忠,胡耀国,李定强,等.粤西典型崩岗侵蚀剖面可蚀性因子初步分析[J].生态环境,2008,17(1):403-410.[WANG Y Z, HU Y G, LI D Q, et al. The preliminary investigation of soil erosive factors in granitic weathering rinds in western Guangdong province[J]. Ecology and Environment, 2008, 17(1):403-410.]
[32] 马云,何丙辉,何建林,等.三峡库区皇竹草植物篱对坡面土壤分形特征及可蚀性的影响[J].水土保持学报,2012,25(4):79-82,87.[MA Y, HE B H, HE J L, et al. Effects of Herba and rographitis Hedgerow on Soil Fractal Characteristics and Erodibility on Sloping Cropland in Three Gorges Reservoir Region[J]. Journal of soil and water conservation, 2012, 25(4):79-82.]
[33] 刘杰,谢定松,崔亦昊.江河大堤双层地基渗透破坏机理模型试验研究[J].水利学报,2009,39(11):1211-1220.[LIU J, XIE D S, CUI Y H. Failure mechanism of seepage in levees with double-layer foundation[J]. SHUILI XUEBAO, 2009, 39(11):1211-1220.]
[34] 丁树文,蔡崇法,张光远.鄂东南花岗地区重力侵蚀及崩岗形成规律的研究[J].南昌水专学报,1995(S1):50-54.[DING S W, CAI C F, ZHANG G Y. A study on gravitational crosion and the formation of collapse mound in the granite area of Southeast Hubei. Journal of Nanchang College of Water Conservancy and Hydroelectric Power, 1995, 1:50-54.]
[35] 邓羽松, 丁树文, 刘辰明, 等. 鄂东南花岗岩崩岗崩壁土壤水分特征研究[J]. 水土保持学报, 2015, 29(4):132-137.[DENG Y S, DING S W, LIU C M, et al. Soil moisture characteristics of collaping gully wall in granite area of southeastern Hubei (In Chinese). Journal of Soil and Water Conservation, 2015, 29(04):132-137.]
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