• 全国中文核心期刊
  • 中国科技核心期刊
  • 美国工程索引(EI)收录期刊

紫色土坡地壤中流特征

徐勤学, 王天巍, 李朝霞, 蔡崇法, 史志华

徐勤学, 王天巍, 李朝霞, 蔡崇法, 史志华. 紫色土坡地壤中流特征[J]. 水科学进展, 2010, 21(2): 229-234.
引用本文: 徐勤学, 王天巍, 李朝霞, 蔡崇法, 史志华. 紫色土坡地壤中流特征[J]. 水科学进展, 2010, 21(2): 229-234.
XU Qin-xue, WANG Tian-wei, LI Zhao-xia, CAI Chong-fa, SHI Zhi-hua. Characteristics of interflow in purple soil of hillslope[J]. Advances in Water Science, 2010, 21(2): 229-234.
Citation: XU Qin-xue, WANG Tian-wei, LI Zhao-xia, CAI Chong-fa, SHI Zhi-hua. Characteristics of interflow in purple soil of hillslope[J]. Advances in Water Science, 2010, 21(2): 229-234.

紫色土坡地壤中流特征

基金项目: 国家重点基础研究发展计划(973)资助项目(2007CB407201);国家自然科学基金资助项目(40501040;40671114)
详细信息
    作者简介:

    徐勤学(1982- ),男,湖南新宁人,博士研究生,主要从事水土保持与农业生态研究.E-mail:xqx@webmail.hzau.edu.cn

    通讯作者:

    李朝霞, E-mail: zxli@mail.hzau.edu.cn

  • 中图分类号: P334.2

Characteristics of interflow in purple soil of hillslope

Funds: The study is financially supported by the NationalBasic Research Program of China (No.2007CB407201) and the National Natural Science Foundation of China (No.40501040;No.40671114)
  • 摘要: 壤中流是紫色土坡地径流的重要组成部分。通过野外人工模拟降雨试验,研究了不同降雨条件下紫色土坡地壤中流特征和地表状况变化对壤中流的影响,结果表明:①未扰动荒坡地壤中流径流系数是裸露坡耕地的3~15倍,平均流量是坡耕地的7~33倍,荒坡地和坡耕地壤中流特征差异在大雨强条件下表现更为明显;②坡耕地壤中流径流系数随降雨强度的增加而显著减少,但荒坡地壤中流受雨强的影响不明显;③荒坡地壤中流随地表状况变化而改变,植被覆盖的减少和降雨对疏松地表的压实导致壤中流明显减少。
    Abstract: The interflow constitutes an important portion of total runoff in purple soil of a hillslope.A series of artificial field simulation experiments were conducted to explore the characteristic of interflow in the purple soil of hillslpoe in the different rainfall intensities and land surface conditions.Experimental results show that the observed runoff coefficient and the average interflow for the interflow on undisturbed wastelands are 3 to 15 times and 7 to 33 times that of the observed on bare cultivated lands,respectively.Such characteristic differences in interflow generations on the two lands will become more evident with the increase of rainfall intensities.The observed runoff coefficient for the interflow on bare cultivated lands decreases significantly with the increase of rainfall intensities,while such a characteristic of interflow is not found on undisturbed wastelands.Interflow generations on undisturbed wastelands vary with land surface conditions such as soil compactions and vegetation densities.Surface soil compaction due to heavy rainfall and the decrease in vegetation cover will contribute to a significant reduction of interflow generations on undisturbed wastelands.
  • [1] ANDERSON M G,MCDONNEll J J.Encyclopedia of hydrological sciences[M].Chichester:John Wiley and Sons,2005.1719-1732
    [2] HEWLETT J D,HIBBERT A R.Forest hydrology[M].New York:Pergamon,1965.275-291
    [3] 张洪江,程金花,史玉虎,等.三峡库区花岗岩林地坡面优先流对降雨的响应[J].北京林业大学学报,2004,26(5):6-9.(ZHANG Hong-jiang,CHENG Jin-hua,SHI Yu-hu,et al.Response of preferential flow to rainfall on the forestland slope in the granite area of Three Gorges[J].Journal of Beijing Forestry University,2004,26(5):6-9.(in Chinese))
    [4] UCHIDA T,TROMP-VAN MEERVELD H J,et al.The role of lateral pipe flow in hillslope runoff response:An intercomparison of nonlinear hillslope response[J].Journal of Hydrology.2005,311(1/2/3/4):117-133.
    [5] TROMP-VAN H J,MCDONNELL J J.Threshold relations in subsurface stormflow:1.A 147-storm analysis of the Panola hillslope[J].Water Resources Research,2006,42(2):1-11.
    [6] KIENZLER P M,NAEF F.Temporal variability of subsurface stormflow formation[J].Hydrological Earth System Science,2008,12(1):257-265.
    [7] 王峰,沈阿林,陈洪松,等.红壤丘陵区坡地降雨壤中流产流过程试验研究[J].水土保持学报,2007,21(5):15-17.(WANG Feng,SHEN A-lin,CHEN Hong-song,et al.Experimental study of rainfall-interflow processes on sloping land in red soil hilly region[J].Journal of soil and water conservation,2007,21(5):5-17.(in Chinese))
    [8] 刘刚才,林三益,刘淑珍,等.四川丘陵区常规耕作制下紫色土径流发生特征及其表面流数值模拟[J].水利学报,2002,33(12):101-107.(LIU Gang-cai,LIN San-yi,LIU Shu-zhen,et al.Characteristics of runoff generation and its numerical simulation of surface flow in hilly area with purple soil under conventional tillage systems[J].Journal of hydrology engineering,2002,33(12):101-107.(in Chinese))
    [9] 贾海燕,雷阿林,雷俊山,等.紫色土地区水文特征对硝态氮流失的影响研究[J].环境科学学报,2006,26(10):1658-1664.(JIA Hai-yan,LEI A-lin,LEI Jun-shan,et al.Nitrate-N loss effected by the runoff process in purple soil-a simulation study[J].Acta Scientiae Circumstantiae,2006,26 (10):1658-1664.(in Chinese))
    [10] 丁文峰,张平仓,王一峰.紫色土坡面壤中流形成与坡面侵蚀产沙关系试验研究[J].长江科学院院报,2008,25(3):14-17.(DING Wen-feng,ZHANG Ping-cang,WANG Yi-feng.Experimental study on runoff and sediment yield characteristics on purple soil slope[J].Journal of Yangtze River Scientific Research Institute,2008,25(3):14-17.(in Chinese))
    [11] 中国科学院南京土壤研究所.土壤理化分析[M].上海:上海科学技术出版社,1978.466-532.(ISSAS.Soil physical and chemical analysis[M].Shanghai:Shanghai Science and Technology Press,1978.466-532.(in Chinese))
    [12] LUK S,ABRAHAMS A D,PARSONS A J.A simple rainfall simulator and trickle system for hydro-geo-morphical experiments[J].Physical Geography,1986,7(1):344-356.
    [13] 李毅,邵明安.草地覆盖坡面流水动力参数的室内降雨试验[J].农业工程学报,2008,24(10):1-5.(LI Yi,SHAO Ming-an.Hydro-dynamic parameters of overland flow during laboratory rainfall experiments under grass coverage[J].Transactions of the CSAE,2008,24(10):1-5.(in Chinese))
    [14] 李元寿,王根绪,王一博,等.长江黄河源区覆被变化下降水的产流产沙效应研究[J].水科学进展,2006,17 (5):616-623.(LI Yuan-shou,WANG Gen-xu,WANG Yi-bo,et al.Impacts of land cover change on runoff and sediment yields in the headwater areas of the Yangtze River and the Yellow River,China[J].Advances in Water Science,2006,17 (5):616-623.(in Chinese))
    [15] 蔡崇法,丁树文,张光远,等.三峡库区紫色土坡地养分状况及养分流失[J].地理研究,1996,15 (3):77-84.(CAI Chong-fa,Ding Shu-wen,ZHANG Guang-yuan,et al.A preliminary study on the conditions and losses of nutrients of purple soils in the Three Gorge Reservior Area (TGRA)[J].Geographical Research,1996,15 (3):77-84.(in Chinese))
    [16] 尹忠东,左长清,高国雄,等.江西红壤缓坡地壤中流特征研究[J].西北林学院学报,2006,21(4):47-49.(YIN Zhong-dong,ZUO Chang-qing,GAO Guo-xiong,et al.On interflow of gentle hill in Jiangxi province[J].Journal of Northwest Forestry University,2006,21(4):47-49.(in Chinese))
    [17] 卜崇峰,蔡强国,张兴昌,等.土壤结皮的发育特征及其生态功能研究述评[J].地理科学进展,2008,27 (2):26-31.(BU Chong-feng,CAI Qiang-guo,ZHANG Xing-chang,et al.Review on developmental characteristics and ecological functions of soil crust[J].Progress in Geography,2008,27 (2):26-31.(in Chinese))
    [18] 秦耀东,任理,王济.土壤中大孔隙流研究进展与现状[J].水科学进展,2000,11(2):203-207.(QIN Yao-dong,REN Li,WANG Ji.Review on the study of macropore flow in soil[J].Advances in Water Science,2000,11 (2):203-207.(in Chinese))
    [19] MORET D,ARRUE J L.Dynamics of soil hydraulic properties during fallow as affected by tillage[J].Soil & Tillage Research,2007,96(1/2):103-113.
    [20] POULENARD J,PODWOJEWSKI P,JANEAU J P,et al.Runoff and soil erosion under rainfall simulation of Andisols from the Ecuadorian páramo:Effect of tillage and burning[J].Catena,2001,45(2):185-207.
计量
  • 文章访问数:  111
  • HTML全文浏览量:  33
  • PDF下载量:  770
  • 被引次数: 0
出版历程
  • 收稿日期:  2009-04-05
  • 刊出日期:  2010-03-24

目录

    /

    返回文章
    返回