• 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

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

土壤非饱和带中的优先流

刘亚平 陈川

刘亚平, 陈川. 土壤非饱和带中的优先流[J]. 水科学进展, 1996, 7(1): 85-89.
引用本文: 刘亚平, 陈川. 土壤非饱和带中的优先流[J]. 水科学进展, 1996, 7(1): 85-89.
Yaping Liu, Chuan Chen. Introduction to Preferential Flow in Unsaturated Soil[J]. Advances in Water Science, 1996, 7(1): 85-89.
Citation: Yaping Liu, Chuan Chen. Introduction to Preferential Flow in Unsaturated Soil[J]. Advances in Water Science, 1996, 7(1): 85-89.

土壤非饱和带中的优先流

详细信息
  • 中图分类号: P641.2

Introduction to Preferential Flow in Unsaturated Soil

  • 摘要: 优先流是近年来研究土壤水运动所提出的术语。在某些条件下,水分在非饱和带中的运移不是简单的一维垂直向下流动,而是越过大部分土壤的体积沿着优先途径流动。优先流通常分为三类:大孔隙流,漏斗流,指流。本文分别介绍了这三类流动形式,并回顾了有关优先流的理论和实验的研究成果。
  • [1] C Chen. R J Wagenet. Simulation of waer and chemicals in macropore soils. I Representation of the equivalent macropore influence and its effect on soil-water flow. Journal of Hydrology.The Netherlands. 1992,130:105-126
    [2] C Chen,R J Wagenet. Simulation of water and chemicals in macropore soils. Q Application of linear filter theory. Journal of Hydrology, The Ne-herlands. 1992,130:127-149
    [3] M Th Van Genuchten,P J Wierenga. Mass transfer studies in sorbing porous media. I analytical solution. Soil Science Society American Journal. 1976. 40:473-480
    [4] K Beven,P F Germann. Macropores and water flow in soils. Water Resources Research.1982. 18:1311-1325
    [5] P F Germann. Kinematic wave approach to infiltration and drainage into and from soil macropores. Transit of American Society Agricultural Engineering. 1985,28 (3):745-749
    [6] W A Jury. Simulation of solute transport using a transfer function model. Water Resources Research. 1982, 18:363-368
    [7] W A Jury, J Gruber. A stochastic analysis of the influence of soil and climatic variability on the estimate of pesticide groundwater pollution potential. Water Resources Research. 1989, 25(12):2465-2474
    [8] T S Steenhuis,J-Y Parlange,M B Parlange, and F Stagnitti. A simple model for preferential flow on hillslopes. Proceedings Symposium Agrohydrology. Dept. of Land and Water Use., Agri. cultural Univ, ersity Wageningen, The Netherlands, 1987
    [9] T S Steenhuis,J-Y Parlange. Simulating preferential flow of water and solutes on hillslopes. The Conference on Validation of Flow and Transport Models for the Unsaturated Zone,Ruidoso. New Mexico,1988
    [10] F J Luxmoore. Micro-,meso-and macro-porosity of soil. Soil Science Society American Journal. 1981,45:671
    [11] C Chen, D M Thomas,R E Green, and R J Wagenet. Two-domain estimation of hydraulic properties in macropore soils. Soil Science Society American Journal. 1993,57 (3):680-683
    [12] D E Hill and J-Y Parlange. Wetting front instability in layered soils. Soil Science Society American Proceeding. 1972,36 (5):697-702
    [13] Y Liu,T S Steenhuis,J-Y Parlange,and J S Selker. Hysteretic finger phenomena in dry and wetted sands. Proceedings of the American Society of Agricultural Engineers National Symposium on Preferential Flow. Chicago, IL.,USA.,Dec. 16-17. 1991,160-172
    [14] Y Liu,J-Y Parlange, and T S Steenhuis. Closed form solution for finger width in sandy soils at different water contents. Water Resources Research. 1994,30 (4):949-952
    [15] Y Liu,B Bierck,J S Selker, T S Steenhuis,and J-Y Parlange. High intensity x-ray and tensiometer measurements in rapidly changing preferential flow fields. Soil Science Society American Journal. 1993,57:1188-1192
    [16] P A C Raats. Unstable wetting fronts in uniform and nonuniform soils. Soil Science Society American Proceeding. 1973,37:681-685
    [17] J R Philip. Stability analysis of infiltration. Soil Science Society American Proceeding. 1975,39:1042-1053
    [18] J-Y Parlange and D E Hill. Theoretical analysis of wetting front instability in soils. Soil Science. 1976,122 (4):236-239
    [19] R J Glass,J-Y Parlange,and T S Steenhuis. Wetting front instability 1. theoretical discussion and dimensional analysis. Water Resources Research. 1989, 25 (6):1187-1194
    [20] K-J S Kung,J Boll,J S Selker, W F Ritter,and T S 5teenhuis. Use of ground penetrating radar to improve water quality monitoring in the vadose zone. Proceedings of the American Society of Agricultural Engineers National Symposium on Preferential Flow. Chicago, IL. Dec. 16-17. 1991. 142-149
  • [1] 李彬权, 梁忠民, 付宇鹏, 王军, 胡义明.  基于变动饱和带的产汇流模型及其参数确定方法 . 水科学进展, 2022, 33(2): 208-218. doi: 10.14042/j.cnki.32.1309.2022.02.005
    [2] 靳孟贵, 鲜阳, 刘延锋.  脱节型河流与地下水相互作用研究进展 . 水科学进展, 2017, 28(1): 149-160. doi: 10.14042/j.cnki.32.1309.2017.01.017
    [3] 张在勇, 王文科, 陈立, 王周锋, 段磊, 安可栋.  非饱和带有限分析数值模拟的误差分析 . 水科学进展, 2016, 27(1): 70-80. doi: 10.14042/j.cnki.32.1309.2016.01.008
    [4] 杨永刚, 李国琴, 焦文涛, 黄磊.  黄土高原丘陵沟壑区包气带土壤水运移过程 . 水科学进展, 2016, 27(4): 529-534. doi: 10.14042/j.cnki.32.1309.2016.04.006
    [5] 杨磊, 周启友.  基于流动电位正演模型的非饱和带水流过程监测 . 水科学进展, 2012, 23(5): 673-679. doi: CNKI: 32.1309.P.20120824.1606.008
    [6] 付智勇, 李朝霞, 蔡崇法, 郭忠录.  三峡库区不同厚度紫色土坡耕地产流机制分析 . 水科学进展, 2011, 22(5): 680-688.
    [7] 张文贤, 张展羽, 王康.  垃圾填埋场覆盖层土壤水运动信息测度分析 . 水科学进展, 2009, 20(6): 838-844.
    [8] 裴元生, 王金生, 田朝晖, 崔鹏.  非饱和流节点间导水率估计及达西平均分析 . 水科学进展, 2006, 17(2): 216-221.
    [9] 王康, 张仁铎, 王富庆.  基于连续分形理论的土壤非饱和水力传导度的研究 . 水科学进展, 2004, 15(2): 206-210.
    [10] 奚成刚, 陈家军, 许兆义.  水气二相流方程的一种离散数值解法 . 水科学进展, 2002, 13(3): 287-291.
    [11] 刘建国, 聂永丰.  非饱和土壤水力参数预测的分形模型 . 水科学进展, 2001, 12(1): 99-106.
    [12] 陈家军, 彭胜, 王金生, 王志明, 李书绅.  非饱和带水气二相流动参数确定实验研究 . 水科学进展, 2001, 12(4): 467-472.
    [13] 秦耀东, 任理, 王济.  土壤中大孔隙流研究进展与现状 . 水科学进展, 2000, 11(2): 203-207.
    [14] 陈家军, 奚成刚, 王金生.  非饱和带水-气二相流数值模拟研究进展 . 水科学进展, 2000, 11(2): 208-214.
    [15] 黄冠华, 谢永华.  非饱和水分运动参数空间变异与最优估值研究 . 水科学进展, 1999, 10(2): 101-106.
    [16] 郭仁东, 朴芬淑.  非饱和土壤渗透的快速数值计算 . 水科学进展, 1998, 9(3): 231-236.
    [17] 秦耀东, 胡克林.  大孔隙对农田耕作层饱和导水率的影响 . 水科学进展, 1998, 9(2): 107-111.
    [18] 黄冠华, 沈荣开.  非均质土壤中二维非饱和土壤水分运动的随机分析 . 水科学进展, 1997, 8(2): 117-122.
    [19] 杨金忠, 叶自桐.  野外非饱和土壤水流运动速度的空间变异性及其对溶质运移的影响 . 水科学进展, 1994, 5(1): 9-17.
    [20] 杨金忠, 叶自桐, 贾维钊, 阎世龙.  野外非饱和土壤中溶质运移的试验研究 . 水科学进展, 1993, 4(4): 245-252.
  • 加载中
计量
  • 文章访问数:  293
  • HTML全文浏览量:  96
  • PDF下载量:  522
  • 被引次数: 0
出版历程
  • 收稿日期:  1994-07-10
  • 修回日期:  1994-12-20
  • 刊出日期:  1996-01-25

土壤非饱和带中的优先流

  • 中图分类号: P641.2

摘要: 优先流是近年来研究土壤水运动所提出的术语。在某些条件下,水分在非饱和带中的运移不是简单的一维垂直向下流动,而是越过大部分土壤的体积沿着优先途径流动。优先流通常分为三类:大孔隙流,漏斗流,指流。本文分别介绍了这三类流动形式,并回顾了有关优先流的理论和实验的研究成果。

English Abstract

刘亚平, 陈川. 土壤非饱和带中的优先流[J]. 水科学进展, 1996, 7(1): 85-89.
引用本文: 刘亚平, 陈川. 土壤非饱和带中的优先流[J]. 水科学进展, 1996, 7(1): 85-89.
Yaping Liu, Chuan Chen. Introduction to Preferential Flow in Unsaturated Soil[J]. Advances in Water Science, 1996, 7(1): 85-89.
Citation: Yaping Liu, Chuan Chen. Introduction to Preferential Flow in Unsaturated Soil[J]. Advances in Water Science, 1996, 7(1): 85-89.
参考文献 (20)

目录

    /

    返回文章
    返回