[1]张有为,徐则民*,张期树,等.植被发育斜坡根土间隙降雨入渗研究[J].山地学报,2017,(05):734-741.[doi:10.16089/j.cnki.1008-2786.000273]
 ZHANG Youwei,XU Zemin*,ZHANG Qishu,et al.Research on Rainfall Infiltration into Soil-Root Interstice of a Well Vegetated Slope[J].Mountain Research,2017,(05):734-741.[doi:10.16089/j.cnki.1008-2786.000273]
点击复制

植被发育斜坡根土间隙降雨入渗研究()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2017年05期
页码:
734-741
栏目:
山地环境
出版日期:
2017-09-30

文章信息/Info

Title:
Research on Rainfall Infiltration into Soil-Root Interstice of a Well Vegetated Slope
文章编号:
1008-2786-(2017)5-734-08
作者:
张有为徐则民*张期树郭丽丽曾 强
昆明理工大学 建筑工程学院,昆明650500
Author(s):
ZHANG Youwei XU Zemin* ZHANG Qishu GUO Lili ZENG Qiang
Institute of Civil Engineering, Kunming University of Science and Technology, Kunming, Yunnan 650500, China
关键词:
降雨入渗 根土间隙 土柱三维重建 CT扫描技术 格子Boltzmann方法
Keywords:
Infiltration Soil-root interstice 3D reconstruction of soil CT scanning technique Lattice Boltzmann Method
分类号:
U418.5+2
DOI:
10.16089/j.cnki.1008-2786.000273
文献标志码:
A
摘要:
基于土柱CT扫描数据,运用Volview软件重构土体三维图及根系分布图,精确了解土体根系分布情况; 应用Navier-Stokes方程计算根土间隙物理概念模型,分析横向间隙流速分布情况; 采用格子Boltzmann方法,并结合Matlab程序,实现渗流场细观模拟。为研究根土间隙在土体降雨入渗过程中的作用,综合以上多种方法,深入并全面分析根土间隙在植被发育斜坡降雨入渗过程中的作用。结果表明,(1)CT扫描技术结合Volview软件能够进行土柱三维重建,从而获取根系在土体分布实际情况,为研究根土间隙导流奠定基础;(2)横向根土间隙流速分布情况,中心线位置流速最大,为平均速度的1.5倍;(3)格子Boltzmann方法作为一种基于流体离散粒子的计算方法,能够结合编程软件进行土体渗流细观模拟;(4)随着深度的增加,竖向根土间隙渗流速度逐渐降低,其渗流作用主要依赖于一些连通性好的间隙通道,且流速在30 cm左右深度降低为零。以上各分析手段可有效评估根土间隙对植被发育斜坡在降雨入渗过程中的贡献,并深入分析植被发育斜坡根土间隙降雨入渗机理。
Abstract:
Based on CT original data of soil columns, a three-dimensional distribution pattern of grass roots in well vegetated slope was reconstructed in this research by Volview software for visual recognition of root formation; Navier-Stokes equation was applied to build a physical concept model of root-soil interstices, to analyze the lateral speed of pore flow through interstices of soil; Lattice Boltzmann method was combined with Matlab programming to realize macroscopic simulation of slope seepage field.In order to investigate the behavior of root-soil interstice towards rainfall infiltration, several methods were combined to comprehensively examine the application of root-soil interstices developed in well vegetated slope to infiltration.Results showed that(1)CT scanning technology in connection with Volview software could be used for acquisition of interior formation of slope grass roots, laying a solid foundation for study on slope flow;(2)lateral porous flow in root-soil interstices had the maximum velocity at the center line, 1.5 times of average speed;(3)As a method based on the fluid discrete particle, Lattice Boltzmann Method could be well applied to simulation of subsurface flow;(4)The vertical interflow rate inside root-soil interstices gradually decreased with increases in depth.The seepage in root-soil interstices mainly depended on the state of connected soil interstices and channels, and flow rate reduced to zero at a depth of about 30cm below.In this research it found that, by proper combination of the aforesaid methods, the existence of root-soil interstices in a well vegetated slope considerably contributed to rainfall infiltration and it provided an insight for slope seepage research.

参考文献/References:

[1] 徐则民,黄润秋,范柱国等.滑坡灾害孕育-激发过程中的水-岩相互作用[J].自然灾害学报,2005,14(1):1-9 [XU Zemin, HUANG Runqiu, FANG Zhuguo, et al.Landslide disaster preparation-excitation process in water rock interaction[J].Journal of Natural Disasters, 2005, 14(1):1-9]
[2] SHOAEI Zieaoddin.Mechanism of the giant Seimareh Landslide, Iran, and the longevity of its landslide dams[J].Environmental Earth Sciences, 2014, 727: 2411-2422.
[3] FIORILLO Francesco.Geological features and landslide mechanisms of an unstable coastal slope(Petacciato, Italy)[J].Engineering Geology, 2002, 673:255-267.
[4] 张丽华,王成武.非饱和土壤优先流运动特性的染色示踪研究[J].节水灌溉,2010(5):35-36 [ZHANG Lihua, WANG Chengwu.Study on the flow characteristics of non-saturated soil referential flow characteristics[J].Water Saving Irrigation, 2010(5):35-36]
[5] HEIJS A W J,RITSEMA C J,DEKKER L W.Three-dimensional visualization of preferential flow patterns in two soils[J].Geoderma, 1996,702:101-116.
[6] MITCHELL A R, ELLSWORTH T R, MEEK B D.Effect of root systems on preferential flow in swelling soil[J].Communications in Soil Science and Plant Analysis, 1995, 2615-16:2655-2666.
[7] RONKANEN Anna-Kaisa, KLOVE Bjørn.Use of stabile isotopes and tracers to detect preferential flow patterns in a peatland treating municipal wastewater[J].Journal of Hydrology, 2007, 3473:418-429.
[8] SANDER Till, H.GERKE Horst.Modelling field-data of preferential flow in paddy soil induced by earthworm burrows[J].Journal of Contaminant Hydrology, 2008, 1041:126-136.
[9] SHIPITALO M J, NUUTINEN V, KEVIN R B.Interaction of earthworm burrows and cracks in a clayey, subsurface-drained, soil[J].Applied Soil Ecology, 2004, 263:209-217.
[10] 冯杰,郝振纯.CT扫描确定土壤大孔隙分布[J].水科学进展,2002,13(5):611-617 [FENG Jie, HAO Zhenchun.CT scan to determine the distribution of soil[J].Advances in Water Science,2002,13(5):611-617]
[11] 解河海,冯杰,冯青等.考虑大孔隙的土壤入渗模型[J].水利水电科技进展,2011,31(5):35-38[JIE Hehai, FENG Jie, FENG Qing, et al.Consider the macropore soil infiltration model[J].Advances in Science and Technology of Water resources, 2011,31(5):35-38]
[12] 王凤,邓念东,马逢清等.基于CT的黄土大孔隙形态三维分形研究[J].计算机工程, 2014,40(7):217-220 [WANG Feng, DENG Niandong, MA Fengqing, et al.Based on CT of the three dimensional fractal of the Loess Plateau[J].Computer Engineering, 2014, 40(7):217-220]
[13] 张家明,徐则民,裴银鸽.植被发育斜坡非饱和带大孔隙[J].山地学报,2012,30(4):439-449[ZHANG Jiaming, XU Zemin, Pei Yinge.Macropores of unsaturated zone in the slope of vegetation development[J].Mountain Research, 2012, 30(4):439-449]
[14] ALLAIRE S E, GUPTA S C, NIEBER J, MONCRIEF J F.Role of macropore continuity and tortuosity on solute transport in soils[J].Journal of Contaminant Hydrology, 2002, 583:299-321.
[15] CHRISTIANSEN Jesper Skovdal, THORSEN Mette, CLAUSEN Thomas, et al.Modelling of macropore flow and transport processes at catchment scale[J].Journal of Hydrology, 2004, 2991:136-158.
[16] 王帮团,徐则民,王帮圆.植被发育斜坡土体中根-土间隙的导流特性[J].山地学报, 2015,33(3):257-267[WANG Gang, XU Zemin, WANG Bangyuan.The diversion characteristics of soil in the soil of the slope of vegetation development[J].Mountain Research, 2015, 33(3):257-267]
[17] PANKHURST C E, PIERRET A, HAWKE B G, et al.Microbiological and chemical properties of soil associated with macropores at different depths in a red-duplex soil in NSW Australia[J].Plant and Soil, 2002, 238:11-20.
[18] 张霞,李凤滨,盛金昌等.格子Boltzmann方法模拟土体渗流场研究 [J].水电能源科学, 2012,30(10):61-64 [ZHANG Xia, LI Fengbin, SHENG Jinchang, et al.Lattice Boltzmann method simulation of seepage field [J].Water Resources and Power, 2012,30(10):61-64]

相似文献/References:

[1]王帮团,徐则民,王帮圆,等.植被发育斜坡土体中根-土间隙的导流特性[J].山地学报,2015,(03):257.
 WANG Bangtuan,XU Zemin,WANG Bangyuan.The Diversion Characteristics of the Soilroot Interstice on a Vegetated Slope[J].Mountain Research,2015,(05):257.

备注/Memo

备注/Memo:
收稿日期(Received date):2015-12-02; 改回日期(Accepted date):2016-03-30
基金项目(Foundation item):NSFC-云南联合基金重点项目(U1502232); 高等学校博士学科点专项科研基金(20135314110005)[NSFC-Yunnan Joint Fund(U1502232); Research Fund for the Ph.D.Program of Higher Education of China(20135314110005)]
作者简介(Biography):张有为(1990-),男,湖南衡阳人,硕士研究生,主要研究方向:滑坡灾害学[Zhang Youwei(1990-), male, born in Hengyang, Hunan province, M.Sc.candidate, research on slope hydrology] Email:1558131704@qq.com
*通讯作者(Corresponding author):徐则民(1963-),男, 博士,教授,主要研究方向:斜坡水文学[Xu Zemin(1963-), male, Ph.D., professor, specialized in hydrology, slope hydrology] E-mail:abc5100@188.com
更新日期/Last Update: 2017-09-30