[1]王志杰,简金世,焦菊英,等.基于RUSLE的松花江流域不同侵蚀类型区泥沙输移比估算[J].水土保持研究,2013,20(05):50-56.
　WANG Zhi-jie,JIAN Jin-shi,JIAO Ju-ying,et al.Estimation of Sediment Delivery Ratio in Different Soil Erosion Regions in the Songhua River Basin Based on RUSLE[J].Research of Soil and Water Conservation,2013,20(05):50-56.
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基于RUSLE的松花江流域不同侵蚀类型区泥沙输移比估算

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 20 期数: 2013年05期 页码: 50-56 栏目: 出版日期: 2013-10-28
Title:
Estimation of Sediment Delivery Ratio in Different Soil Erosion Regions in the Songhua River Basin Based on RUSLE
作者:
王志杰1, 简金世2, 焦菊英1,3, 苏嫄4
1. 中国科学院 水利部 水土保持研究所, 陕西 杨凌 712100;
2. 常德市水利水电勘测设计院, 湖南 常德 415000;
3. 西北农林科技大学 水土保持研究所, 陕西 杨凌 712100;
4. 西北农林科技大学 资源环境学院, 陕西 杨凌 712100
Author(s):
WANG Zhi-jie1, JIAN Jin-shi2, JIAO Ju-ying1,3, SU Yuan4
1. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China;
2. Design Institute of Water Conservancy and Hydroelectric Power of Changde City, Changde, Hunan 415000, China;
3. Institute of Soil and Water Conservation, Northwest A & F University, Yangling, Shaanxi 712100, China;
4. College of Natural Resources and Environment, Northwest A & F University, Yangling, Shaanxi 712100, China
关键词:
RUSLE; 土壤侵蚀; 河流输沙; 泥沙输移比; 松花江流域
Keywords:
RUSLE; soil erosion; suspended sediment; sediment delivery ratio; Songhua River basin
分类号:
S157.2
摘要:
为摸清东北黑土区土壤侵蚀与泥沙输移特征，以松花江流域为研究对象，选取不同侵蚀类型区8个水文站控制区，利用RUSLE模型，结合水文站实测输沙数据，分析了不同侵蚀类型区泥沙输移比的时空变化特征。结果表明：（1）松花江流域各侵蚀类型区均以微度侵蚀和轻度侵蚀为主，而草地、旱地和裸地侵蚀模数均呈现依次增大趋势，且大于该区容许土壤流失量，特别是松岭站、碾子山站、大石寨站和大山咀子站水文站控制区裸地土壤侵蚀模数均大于20 000 t/（km2·a），达到剧烈侵蚀程度。不同侵蚀类型区之间侵蚀模数表现为丘陵沟壑区Ⅰ > 丘陵沟壑区Ⅱ > 天然林区 > 漫川漫岗区。（2）松花江流域不同侵蚀类型区泥沙输移比总体上表现为漫川漫岗区 > 丘陵沟壑区Ⅱ > 丘陵沟壑区Ⅰ > 天然林区。（3）同一侵蚀类型区不同年际间泥沙输移比波动起伏，而从20世纪60年代到80年代，人类活动影响较小的天然林区和丘陵沟壑区Ⅱ不同时期平均泥沙输移比相差不大，人类活动剧烈的漫川漫岗区和丘陵沟壑区Ⅰ平均泥沙输移比则表现为波动式递增。研究结果对于了解东北黑土区土壤侵蚀和泥沙输移规律，明确该区域土壤侵蚀机理和治理目标具有指导意义。
Abstract:
In order to understand the soil erosion and sediment delivery characteristics of black soil zone in northeast of China, the spatial and temporal variation characteristics of sediment delivery ratio (SDR) of the different soil erosion regions in the Songhua River basin was analyzed by choosing the 8 hydrological control zone in the different erosion regions, using the RUSLE model, and combining with the sediment hydrological data. The results showed: (1) the main soil erosion intensity of different soil erosion regions in Songhua River basin was slight erosion and mild erosion, the soil erosion modulus of different soil erosion regions was as an order of hilly-gully region Ⅰ > hilly-gully region Ⅱ > natural forest region > rolling hills region; (2) the average SDR of different soil erosion regions in Songhua River basin was sorted as rolling hills region > hilly-gully region Ⅱ > hilly-gully region Ⅰ > natural forest region; (3) the different interannual SDR of same soil erosion region fluctuation was caused by the influence of rainfall. However, from 1960s to 1980s, the average SDR in different periods was not obviously changed in the natural forest region and hilly-gully erosion Ⅱ, and fluctuation increased in the rolling hills region and hilly-gully region Ⅰ due to the influence of human activity. The study would have the guiding significance to understand the soil erosion and sediment delivery characteristics of the black soil zone in northeast of China, and to clarify the soil erosion mechanism and management object of this region.

参考文献/References:

[1] 焦菊英,景可,李林育,等.应用输沙量推演流域侵蚀量的方法探讨[J].泥沙研究,2007(4):1-7.
[2] 水利学会泥沙专业委员会.泥沙手册[M].北京:中国环境科学出版社,1989.
[3] Vanoni V A. Sedimentation Engineering[M]. New York:The Society,1975.
[4] 景可.长江上游泥沙输移比初探[J].泥沙研究,2002(1):53-59.
[5] 李林育,焦菊英,陈杨.泥沙输移比的研究方法及成果分析[J].中国水土保持科学,2009,7(6):113-122.
[6] 水利部,中国科学院,中国工程院.中国水土流失与生态安全综合考察报告:东北黑土区卷[M].北京:科学出版社,2010.
[7] 蔡强国,范昊明.泥沙输移比影响因子及其关系模型研究现状与评述[J].地理科学进展,2004,23(5):1-9.
[8] 景可.黄土高原的新构造运动对侵蚀影响的研究[J].水土保持通报,1982,2(6):10-15.
[9] 赵晓光,石辉.黄土塬区坡面及小集水区泥沙输移比变化特征[J].山地学报,2002,20(6):718-722.
[10] 卜兆宏,刘绍清.土壤流失量及其参数实测的新方法[J].土壤学报,1995,32(2):210-220.
[11] Maner S B. Factors influencing sediment delivery ratios in the Blackland Prairie land resource area[M]. Fort Worth, Tex:U.S.Department of Agriculture, Soil Conservation Service,1962.
[12] Williams J R, Berndt H D. Sediment yield computed with universal equation[J]. Journal of the Hydraulics Division,1972,98(12):2087-2098.
[13] Haith D A, Tubbs L J. Watershed loading functions for nonpoint sources[J]. Journal of the Environmental Engineering Division,1981,107(1):121-137.
[14] Mutchler C K, Bowie A J. Effect of land use on sediment delivery ratios[C]//Proceedings of the Third Federal Inter-Agency Sedimentation Conference. U.S Water Resources Council, Washington D C, Sedimentation Committee, Denver, Colorado,1975.
[15] Robert H F, Paul K B, Tomlin C D. SEDMOD:a GIS-based method for estimating distributed sediment delivery ratios[M]//Symposium on Geographic Information Systems and Water Resources, American Water Resources Association, Fort Lauderdale, Florida,1996.
[16] 张光科,刘东,方铎.山区流域泥沙输移比计算公式[J].成都科技大学学报,1996,16(6):85-90.
[17] 张光科,刘东,方铎.山区流域坡面径流侵蚀和泥沙输移分析[J].四川联合大学学报:工程科学版,1997,1(6):12-20.
[18] 牟金泽,孟庆枚.论流域产沙量计算中的泥沙输移比[J].泥沙研究,1982(2):60-65.
[19] 刘纪根,蔡强国,张平仓.岔巴沟流域泥沙输移比时空分异特征及影响因素[J].水土保持通报,2007,27(5):6-10.
[20] 曹文洪,张启舜,姜乃森.黄土地区一次暴雨产沙数学模型的研究[J].泥沙研究,1993(1):1-13.
[21] Leopold L B. Channel and hill slope processes in semiarid area[J]. New Mexico:Unite states geological survey professional paper,1966,352G:193-253.
[22] Trimble S W. A sediment budget for Coon Creek Basin in the Driftless area, Wisconsin, 1853-1977[J]. American Journal of Science,1985,283(5):454-474.
[23] 许炯心,孙季.水土保持措施对流域泥沙输移比的影响[J].水科学进展,2004,15(1):29-34.
[24] 花利忠.基于AnnAGNPS模型的流域侵蚀产沙评价:以三峡库区大宁河流域为例[D].成都:中国科学院水利部成都山地灾害与环境研究所,2007.
[25] 张宪奎,许靖华,卢秀琴,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.
[26] 杨晓晖,吴波.大兴安岭东部林区森林水土保持功能初步评价[J].中国水土保持科学,2004,2(4):11-16.
[27] 王禹,杨明义,刘普灵.东北黑土区坡耕地水蚀与风蚀速率的定量区分[J].核农学报,2010,24(4):790-795.
[28] 简金世.松花江流域不同侵蚀类型区泥沙输移比的估算[D].陕西杨凌:西北农林科技大学,2011.
[29] 章文波,付金生.不同类型雨量资料估算降雨侵蚀力[J].资源科学,2003,25(1):35-41.
[30] 章文波,谢云,刘宝元.利用日雨量计算降雨侵蚀力的方法研究[J].地理科学,2002,22(6):705-711.
[31] Wischmeier W H, Smith D D. Predicting Rainfall Erosion Losses:A guide to conservation planning[C]. U.S, Dep. Agric. Agric. Handb.,1978,No.537.
[32] Foster G R, Meyer L D, Onstad C A. A runoff erosivity factor and variable slope length exponents for soil loss estimates[J]. Transactions of ASAE,1977,20(4):683-687.
[33] McCool D K, Brown L C, Foster G R. Revised slope steepness factor for the Universal Soil Loss Equation[J]. Transactions of the ASAE,1987,30(5):1387-1396.
[34] Liu B Y, Nearing M A, Risse L M. Slope gradient effects on soil loss for steep slopes[J]. Transaction of American Society of Agriculture Engineers,1994,37(6):1835-1840.
[35] 刘宝元,谢云,张科利.土壤侵蚀预报模型[M].北京:中国科学出版社,2001.
[36] 张树文,李颖.东北地区土地利用/覆被时空特征分析[M].北京:北京科学出版社,2006.
[37] 沈波,杨海军.松辽流域水土流失及其防治对策[J].水土保持通报,1993,13(2):28-32.
[38] 焦剑,赵登峰.松花江流域侵蚀产沙演变特征分析[J].水土保持通报,2010,30(2):87-91.
[39] 龚时旸,熊贵枢.黄河泥沙来源和地区分布[J].人民黄河,1979,1(1):7-17.
[40] 景可.黄土高原泥沙输移比的研究[C]//黄河粗泥沙来源及侵蚀产沙机理研究文集.北京:气象出版社,1989.
[41] 许炯心.三峡水库修建前长江宜昌-武汉段泥沙输移比及其影响因子[J].山地学报,2008,26(1):15-21.
[42] 刘运河,陈礼耕,石长金,等.大兴安岭地区的水土流失及其防治[J].中国水土保持,1992(10):1-3.

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备注/Memo

收稿日期:2012-12-12;改回日期:2013-03-12。
基金项目:国家重点基础发展规划项目（973）（2007CB407203）
作者简介:王志杰(1986-),男,甘肃会宁人,博士研究生,主要从事土壤侵蚀研究。E-mail:wzhijie86@gmail.com
通讯作者:焦菊英(1965-),女,陕西宝鸡人,研究员,主要从事流域侵蚀产沙、土壤侵蚀与植被关系及水土保持效益评价。E-mail:jyjiao@ms.iswc.ac.cn

更新日期/Last Update: 1900-01-01