土壤水蚀预报模型研究进展

doi:10.11821/yj2001030003

摘要/Abstract

摘要：

对土壤侵蚀进行准确预报,是指导水土保持措施优化配置、水土资源保护与持续利用的有效工具,对于退化生态系统的重建具有重要的意义。在对国外土壤侵蚀模型发展过程进行简单回顾的基础上,重点对我国土壤水蚀预报模型的研究进展做了详尽的分析,并从研究方法和研究内容两个方面,论述了今后我国土壤侵蚀模型研究中亟待解决问题

关键词: 土壤水蚀, 侵蚀模型, 研究进展

Abstract:

Soil erosion is one of the most serious environmental issues in China It is very important to investigate the mechanism of soil erosion and to develop soil erosion model, which is the useful tool to design the measures of soil and water conservation and sustainable use of soil and water resources, and is also closely related with the rehabilitating of the degenerated environment The development of soil erosion models in U S A, Europe, and Australia was reviewed briefly and then the development of soil erosion model in China was analyzed in detail Both empitical models, process based models,and the utilization condition of new techniques such as GIS, RS, REE in soil erosion were evaluated in this paper On the basis of the above evaluations, the issues existing at present research , which need to be enhanced in the future research, were identified The purpose of this paper was to learn the overseas experience and promote future soil erosion model development in China

Key words: water erosion, erosion model, research progress

PACS:

S157.1

张光辉. 土壤水蚀预报模型研究进展[J]. 地理研究, 2001, 20(3): 274-281.

ZHANG Guang hui. Development of soil erosion models in China[J]. GEOGRAPHICAL RESEARCH, 2001, 20(3): 274-281.

参考文献

[1] Meyer L D 1Evaluation of the universal soil loss equation
[J].Journal of Soil and Water Conservation,1984,39:99～104.
[2] Cook M F. The natural and controlling variables of t he water erosion process
[J].Soi. Sci. Soc. Am. Proceeding .
[C],1936,1:60～64.
[3] Zingg A W.Degree and lengt h of land slope as it affects soil loss in runoff
[J].Agricultural Engineering,1940,21:59～64.
[4] Smit h D D. Interpretation of soil conservation data for field use
[J].Agricultural Engineering,1941,22:173～175.
[5] Wischmeier W H,Smit h D D. Predicting rainfall-erosion losses from cropland east of t he Rocky Mountains
[M].USDAAgricultural Handbook,No. 282,1965.
[6] Wischmeier W H,Smit h D D. Predicting rainfall erosion losses
[M].USDA Handbook,No1537,1978.
[7] Renard K G,Foster G R,Weesies G A,et al. Predicting soil erosion by water:a guide to conservation planning wit ht he Revised Universal Soil Loss Equation(RUSL E)
[M].USDA Handbook,No1537,1997.
[8] Nearing M A,Lane L J,Alberts E E and Laflen J M. Prediction technology for soil erosion by water:Status and research needs
[J].Soil Sci. Soc. Am. J.,1990,54(6):1702～1711.
[9] Morgan R. The European Soil Erosion Model:an update on its structure and research base
[A].In:Rickson,R1(ed1),ConservingSoil Resources:European perspectives
[M].CAB International,Cambridge,1994,286～299.
[10] De Roo A,Wesseling C G,Ritsma C G1 L ISEM:A single-event,physical based hydrological and soils erosion modelfor drainage basin1 I:theory,input and output
[J].Hydrological Processes,1996,10:1107～1117.
[11] Rose C W,Williams J R,Sander G C,Barry D A. A mat hematical model of soil erosion and deposition processes:I.Theory for a plane land element
[J].Soil Sci. Soc. of Am. J.,1983,47(5):991～995.
[12] Yang C T. Unit stream power and sediment transport
[J].Journal of t he Hydraulics Division,ASAE,98(HY10),Proc. Paper 9295. 1972,1805～1826.
[13] Bagnold R A1 An approach to t he sediment-transport problem from general physics
[R].U1S1 Geol1 Surv1 Prof1 Paper1 1966,422～4371
[14] Elliot W J,Laflen J M. A process-based rill erosion model
[J].Transactions of the ASAE,1993,36(1):65～72.
[15] Nearing M A,Simanton J R,Norton L D,et al1 Soil erosion by surface water flow on a stony,semiarid hillslope
[J].Eart h Surf. Process. Landforms,1999,24:677～686.
[16] Govers G. Relationship between discharge,velocit y and flow area for rills eroding loose,non-layered materials
[J].Eart h Surf. Process1 Landforms,1992,17:515～528.
[17] Gary Li and Abrahams A D. Controls of sediment transport capacity in laminar interrill flow on stone-covered surfaces
[J].Water Resources Research,1999,35(1):305～310 .
[18] Rauws G. Laboratory experiments on resistance to overland flow due to composite roughness
[J].J .Hydrol.,1988,103:37～52.
[19] Abrahams A D,Gary Li and Parsons A J . Rill hydraulics on a semiarid hillslope,sout hern Arizona
[J].Eart h Surf. Process1 Landforms,1996,21:35～47.
[20] Nearing M A,Norton L D,Bulgakov D A,et al. Hydraulics and erosion in eroding rills
[J].Water Resources Research,1997,33(4):865～876.
[21] 蔡强国.坡面侵蚀产沙模型的研究
[J].地理研究,1988,7(4):94～102.
[22] 朱显谟.甘肃中部土壤侵蚀调查报告
[J].土壤专辑,1958,第32号:53～109.
[23] 白清俊.流域土壤侵蚀预报模型的回顾与展望
[J].1999,21(4):18～21.
[24] 窦保章,周佩华.雨滴的观测与计算方法
[J].水土保持通报,1982,(2):43～47.
[25] 牟金泽.雨滴速度计算公式
[J].中国水土保持,1983,(3):13～171
[26] 王万忠,焦菊英.黄土高原降雨侵蚀产沙与黄河输沙
[A].科学出版社,北京,1996.
[27] 卜兆宏,等.降雨侵蚀力因子的算法
[J].土壤学报,1992,29(4):408～417.
[28] 张宪奎.黑龙江省土壤流失预报方程中R指标的研究
[C].水土保持保持科学理论与实践,北京:林业出版社,1992,63～66.
[29] 杨艳生,史德明.关于土壤流失方程中K因子的探讨
[J].中国水土保持,1982,(4):39～41
[30] 陈明华,周伏建,黄炎和,等.土壤可蚀性因子的研究
[J].水土保持学报,1995,9(1):19～24.
[31] 刘保元,张科利,焦菊英.土壤可蚀性及其在侵蚀预报中的应用
[J].自然资源学报,1999,14(4):345～350.
[32] Liu B Y,Nearing M A,Risse L M1Slope gradient effects on soil loss for steep slopes
[J].transactions of t he ASAE,1994,37(6):1835～1840.
[33] Liu B Y,Nearing M A,Shi P J,Jia Z W. Slope lengt h effects on soil loss for steep slopes
[J].Soil Sci. Soc. of Am. J .,2000,64(5):1759～1763.
[34] 蔡强国,陈浩.影响降雨击溅侵蚀过程的多元正交试验研究
[J].地理研究,1989,8(4):28～36.
[35] 张光辉,梁一民.黄土丘陵区人工草地产流起始时间研究
[J].水土保持学报,1995,9(3):78～83.
[36] 毕华兴,朱金兆,吴斌.晋西黄土区防护林体系水沙效益评价和预测系统的研究
[J].土壤侵蚀与水土保持学报,1996,2(1):69～74.
[37] 史衍玺,唐克丽.林地开垦加速侵蚀下土壤养分退化的研究
[J].土壤侵蚀与水土保持学报,1996,2(4):26～33.
[38] 王万忠,焦菊英.中国的土壤侵蚀因子定量评价研究
[J].水土保持通报,1996,16(5):1～20.
[39] 张科利,刘宝元,蔡永明.土壤侵蚀预报研究中的标准小区问题论证
[J].地理研究,2001,19(30):297～302.
[40] 张光辉,梁一民.黄土丘陵区沙打网草地截留试验研究
[J].水土保持通报,1995,15(3):28～32.
[41] 石生新,蒋定生.几种水土保持措施对强化降水入渗和减沙的影响试验研究
[J].水土保持研究,1994,1(1).
[42] 余新晓,毕华兴,朱金兆,等.黄土地区森林植被水土保持作用研究
[J].植物生态学报,1997,21(5):433～440.
[43] 吴钦孝,刘向东.山杨次生林枯枝落叶蓄积量及其水文作用
[J].水土保持学报,1992,6(1):71～76.
[44] 李勇,朱显谟,田积莹.黄土高原植物根系提高土壤抗冲性的有效性
[J].科学通报,1991,36(12):935～938.
[45] 张宪奎,许靖华,卢绣琴,等.黑龙江省土壤流失方程的研究
[J].水土保持通报,1992,12(4):1～9.
[46] 于东升,史学正,吕喜玺.低丘红壤区不同土地利用方式C值及可持续性评价
[J].土壤侵蚀与水土保持学报,1998,4(1):71～76.
[47] 林素兰,黄毅,聂振刚,等.辽北低山丘陵区坡耕地土壤流失方程的建立
[J].土壤通报,1997,28(6):251～253.
[48] 江忠善,王志强,刘志.黄土丘陵区小流域土壤侵蚀空间变化定量研究
[J].土壤侵蚀与水土保持学报,1996,2(1).
[49] 张光辉,刘国彬.黄土丘陵区小流域土壤表面特性变化规律研究
[J].地理科学,2001,21(2):1～5.
[50] 孟庆华,傅伯杰.景观格局与土壤养分流动
[J].水土保持学报,2000,14(3):116～121.
[51] 张兴昌,卢宗凡.农作物水土保持效益的数值化综合评价
[J].1993,7(2):51～56.
[52] 张光辉,梁一民.黄土丘陵区人工草地盖度季动态及其水保效益
[J].水土保持通报,1995,15(2):38～43.
[53] 陈云明,侯喜绿,刘文兆.黄土丘陵半干旱区不同类型植被水保生态效益研究
[J].水土保持学报,2000,14(3).
[54] 牟金泽,孟庆枚.陕北中小流域年产沙量计算
[A].黄土高原水土流失综合治理科学讨论会资料汇编
[C],陕西:中国科学院水利部水土保持研究所内部资料,1981,251～255.
[55] 谢树楠,王孟楼,张仁.黄河中游黄土沟壑区暴雨产沙模型的研究
[R].北京:清华大学,1990.
[56] 汤立群.流域产沙模型的研究
[J].水科学进展,1996,7(1):47～53.
[57] 蔡强国,王贵平,陈永宗.黄土高原小流域侵蚀产沙过程与模拟
[M].北京:科学出版社,1998.
[58] 陈国祥,姚文艺.降雨对浅层水流阻力的影响
[J].水科学进展,1996,7(1),42～46.
[59] 张光辉,卫海燕,刘宝元.坡面流水动力特性研究
[J].水土保持学报,2001,15(1),58～61.
[60] 郑粉莉,唐克丽,周佩华.坡耕地细沟侵蚀影响因素研究
[J].土壤学报,1989,26(2),109～116.
[61] 张科利,唐克丽.黄土坡面细沟侵蚀能力的水动力学试验研究
[J].土壤学报,2000,37(1),9～15.
[62] 曹问洪.坡面流输沙能力的初步研究
[A].第二届全国泥沙基本理论研究学术讨论会论文集
[C].北京,1995.
[63] 杨勤科,李锐,李智广,等.区域水土流失调查研究初报
[J].水土保持通报,1999,19(3):36～39.
[64] 武春龙,江忠善,郑世清.安塞县纸纺沟流域土壤侵蚀遥感制图
[J].水土保持通报,1990,10(4):6～12.
[65] 徐国礼,周佩华,王文龙,等.沟道侵蚀与地面遥感监测研究
[J].水土保持学报,1991,5(2):22～24.
[66] 付炜.黄土丘陵沟壑区土壤侵蚀预测模型建立方法的研究
[J].水土保持学报,1992,6(3):6～13.
[67] 傅伯杰,汪西林.DEM在研究黄土丘陵沟壑区土壤侵蚀类型和过程中的应用
[J].水土保持学报,1994,8(3).
[68] 吴礼福.黄土高原土壤侵蚀模型及其应用
[J].水土保持通报,1996,16(5):29～35.
[69] 杨浩,杜明远,赵其国等.基于137 Cs地表富集作用的土壤侵蚀速率的定量模型
[J].土壤侵蚀与水土保持学报,1999,5(3):42～48.
[70] 周维芝.137Cs法研究不同地貌类型土壤侵蚀强度分异
[D] .中国科学院水土保持研究所96届硕士论文,1996.
[71] 杨明义,田均良,刘普灵.应用137Cs研究小流域泥沙来源
[J],土壤侵蚀与水土保持学报,1999,5(3):49～53.
[72] 张光辉.国外坡面径流分离土壤过程水动力学研究进展
[J].水土保持学报,2000,14(3):112～115.