[1]原立峰,常春平.坡面细沟自组织形成过程的CA模拟[J].水土保持研究,2008,15(03):7-10,30.
　YUAN Li-feng,CHANG Chun-ping.A Cellular Automata Approach to the Simulation of Rill Self-Organizing Development Process on Hillslope[J].Research of Soil and Water Conservation,2008,15(03):7-10,30.
点击复制

坡面细沟自组织形成过程的CA模拟

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 15 期数: 2008年03期 页码: 7-10,30 栏目: 出版日期: 2008-06-20
Title:
A Cellular Automata Approach to the Simulation of Rill Self-Organizing Development Process on Hillslope
作者:
原立峰1, 常春平2
1. 南京邮电大学 电子信息科学系, 南京 210003;
2. 河北师范大学 资源与环境科学学院, 石家庄 050016
Author(s):
YUAN Li-feng1, CHANG Chun-ping2
1. Department of Electronics and Information Science, Nanjing University of Posts and Telecommunications, Nanjing 210003, China;
2. College of Resources and Environment Sciences, Hebei Normal University, Shijiazhuang 050016, China
关键词:
细沟侵蚀; 自组织; 元胞自动机
Keywords:
rill erosion; self-organizing; cellular automata
分类号:
S157
摘要:
细沟侵蚀作为由面蚀向沟蚀转化的重要环节，是坡面水蚀物理过程的一个重要组成部分，在坡面侵蚀产沙机理研究中具有重要意义。传统侵蚀模型很难精确地动态模拟和再现这一自组织现象的形成过程。元胞自动机是一种“自下而上”的动态模拟建模框架，通过元胞间的相互作用，能够在整体上表现出许多复杂的非线性行为和现象，具有模拟复杂地理系统时空演化过程的能力。运用元胞自动机理论和方法建立了黄土坡面细沟侵蚀时空演化过程模型——CA-Rill，对坡面细沟发育过程进行了动态虚拟实验，生动地模拟了坡面细沟自组织形成过程，并对结果进行了分析。研究突破传统试验方法的束缚，为细沟侵蚀研究提供了新的途径。
Abstract:
Rill erosion is an important link on the transition from sheet erosion to gully erosion,and is an important component of water erosion physical process on hillslope.Rill erosion research is of great importance to comprehend erosion and sediment mechanism on slope surface.Traditional erosion model is difficult to accurately dynamic simulate and reproduce rill initiation and development process on slope,and this process is self-organizing.Cellular automata,simple named ‘CA’,is a ‘from down to up’ dynamic modeling framework.It is able to simulate the spatial-temporal evolutionary processes of complex geographical system.By interaction between one cell and another,CA can show a great deal of complex non-linear action and phenomena as a whole.CA-Rill,a rill erosion dynamic model on loess slope,is constructed by use of theory and method of cellular automata.The dynamical virtual experiment is carried out for rill self-organizing process on slope.A rill initiation and development process is simulated vividly.The experimental results are analyzed.This research is a breakthrough in traditional test approach,and gives us a new way for researches in rill erosion.

参考文献/References:

[1] Kirkby M J, Morgan R P C.Soil erosion[M].Chichester:John Wiley & Sons, 1980.
[2] Govern G, Rauws G.Transporting capacity of overland flow on plane and on irregular beds[J].Earth Surface Processes Landforms, 1986, 11:15-24.
[3] Selby M J.Hillslope materials & processes[M].Oxford:Oxford University Press, 1993.
[4] 张科利, 秋吉康宏.坡面细沟侵蚀发生的临界水力条件研究[J].土壤侵蚀与水土保持学报, 1998, 4(1):41-46.
[5] 倪晋仁, 韩鹏, 张剑.基于自组织理论的黄土坡面细沟发育特征分析[J].水利学报, 2002(1):6-9.
[6] 张晴雯.细沟水蚀动力过程试验研究[D].陕西杨陵:中科院水土保持研究所, 2001.
[7] 雷廷武, 姚春梅, 张晴雯, 等.细沟侵蚀动态过程模拟数学模型和有限元计算方法[J].农业工程学报, 2004, 20(4):7-13.
[8] Bryan R B.Processes and significance of rill development[J].Catena Supplement, 1987, 8:1-15.
[9] Parsons A J, Wainwright J, Abrahams A D, et al.Distributed dynamic modeling of interrill overland flow[J].Hydrological Processes, 1997, 11:1833-1859.
[10] Price W E.A random-walk simulation model of alluvial-fan deposition[M]//Merriam D F.Random processes in geology.Berlin:Springer-Verlag, 1991:55-62.
[11] Fujiwara T, Fukada M, et al.Simulation analysis of rill patterns that develop on hill-slopes[R]//Technology reports of the Yamaguchi university, 1989, 4(3):247-256.
[12] Wright A C, Webster R A.Stochastic distributed mo-del of soil erosion by overland flow[J].Earth Surface Processes and Landforms, 1991, 16:207-226.
[13] Favis-Mortlock D T, Quinton J N, Dickinson W T.The GCTE validation of soil erosion models for global change studies[J].Journal of Soil and Water Conservation, 1996, 51(5):397-403.
[14] 倪晋仁, 张剑, 韩鹏.基于自组织理论的黄土坡面细沟形成机理模型[J].水利学报, 2001(12):1-7.
[15] 周成虎, 孙战利, 谢一春.地理元胞自动机研究[M].北京:科学出版社, 1999.
[16] 孙战利.空间复杂性与地理元胞自动机模拟研究[J].地球信息科学, 1999:32-37.
[17] Foster G R, Huggins L F, Meyer L D.A Hydraulics velocity relationship[J].Laboratory Study of Rill Trans of ASAE, 1984, 27(3):790-796.
[18] 张科利, 张竹梅.黄土陡坡细沟侵蚀及其产沙特征的实验研究[J].自然科学进展, 2000(10):1136-1139.
[19] Nearing M A, Norton L D, Bulgakov D A, et al.Hydraulic sand erosion in eroding rills[J].Water Resources Research, 1997, 33(4):865-876.

相似文献/References:

[1]王玉宽.暴雨细沟侵蚀的调查研究[J].水土保持研究,1990,(02):45.
　Wang Yukuan.Study on the Rill Erosion Under Heavy Rainstorm[J].Research of Soil and Water Conservation,1990,(03):45.
[2]郑粉莉,唐克丽,蔡庆,等.人为破坏植被开垦耕种对坡面细沟侵蚀的影响[J].水土保持研究,1993,(01):50.
　Zheng Fenli,Tang Keli,Cai Qing,et al.Impact of Vegetation Being Destroyed and Reclaimed on Rill Erosion of the sloping Lands[J].Research of Soil and Water Conservation,1993,(03):50.
[3]吴普特,周佩华,武春龙,等.坡面细沟侵蚀垂直分布特征研究[J].水土保持研究,1997,4(02):47.
　Wu Pute,Zhou Peihua,Wu Chuniong,et al.Research on the Spatial Distribution Characteristics of Slope Rill Erosion[J].Research of Soil and Water Conservation,1997,4(03):47.
[4]景清华,杨郁挺,鲁向晖.土壤侵蚀自组织分析[J].水土保持研究,2007,14(02):79.
　JING Qing-hua,YANG Yu-ting,LU Xiang-hui.Self Organization Analysis of Soil Erosion[J].Research of Soil and Water Conservation,2007,14(03):79.
[5]郭玲梅,王克勤,苏备,等.尖山河小流域坡耕地的细沟侵蚀研究[J].水土保持研究,2015,22(02):12.
　GUO Lingmei,WANG Keqin,SU Bei,et al.Rill Erosion in Slope Farmland in Jianshan River Small Watershed[J].Research of Soil and Water Conservation,2015,22(03):12.
[6]蒋芳市,黄炎和,林金石,等.坡度和雨强对花岗岩崩岗崩积体细沟侵蚀的影响[J].水土保持研究,2014,21(01):1.
　JIANG Fang-shi,HUANG Yan-he,LIN Jin-shi,et al.Effects of Different Rainfall Intensities and Slope Gradients on Rill Erosion of Coluvial Deposits in Granite Benggang[J].Research of Soil and Water Conservation,2014,21(03):1.

备注/Memo

收稿日期:2007-9-21。
基金项目:南京邮电大学“攀登计划”项目（XK0020906075）；国家自然科学基金项目（40301025）；国家科技攻关课题（2005BA517A06）
作者简介:原立峰（1978- ），男，山西太原人，讲师，主要从事遥感技术和GIS应用研究。E-mail：yuanlifeng7833@126.com

更新日期/Last Update: 1900-01-01