植被分布对小流域产流影响的数值实验
Effects of the distribution of vegetation on small catchment runoff during rainstorm events
查看参考文献15篇
文摘
|
基于二维运动波模型,建立了一个适用于小流域场次降雨产汇流过程的动力学模型。通过对典型小流域内不同区域(坡顶、坡中及坡底区域及距离流域出口的远近)种植植被时产流过程的数值模拟,分析了小流域内植被分布对产流过程的影响。结果表明:植被分布及其特性对小流域场次降雨产流有较明显的影响;下游区域种植植被的减水效果和延滞洪峰作用优于上游区域,陡坡区域减水效果优于缓坡区域,且郁闭度越大,这种差别越明显;在该研究条件下,下游区的减水效果可达到上游区的3倍;30%郁闭度条件下减水效果可达10%和20%郁闭度条件下的3倍和1.4倍。 |
其他语种文摘
|
The distribution of vegetation in small catchments is an essential factor determining the generation of runoff during rainstorm events. Using a novel two-dimensional dynamic runoff model,we studied the influence of the distribution of vegetation on rainstorm runoff. First,a kinematic hydrological model of rainstorm events in small watersheds was developed based on a two-dimensional overland flow model. It included canopy interception,surface infiltration, overland flow,and gully flow processes. Data from three rainstorm events in the Heicaohe catchment were then used to verify the model,and good agreement was found. Last,the model was used to examine how the distribution of vegetation and the canopy density affected the runoff process. Model results showed that: First,the vegetation significantly reduces flood discharge and postpones the flood peak,depending on the location and crown density of the vegetation. Second,the efficiency of runoff reduction is substantially higher in downstream and steeply sloped areas (vs. upstream and gently sloping areas) ,and the degree of crown closure enhances this effect. In fact,in this study,the efficiency of runoff reduction was three times higher in downstream compared with upstream areas,and 30% crown closure resulted in 1. 4 times higher efficiency than 20% closure and three times higher than 10% closure. |
来源
|
水科学进展
,2015,26(2):187-195 【核心库】
|
DOI
|
10.14042/j.cnki.32.1309.2015.02.005
|
关键词
|
小流域
;
降雨产流
;
动力学模型
;
植被分布
;
郁闭度
;
减水效果
|
地址
|
中国科学院力学研究所, 中国科学院流固耦合重点实验室, 北京, 100190
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
1001-6791 |
学科
|
地球物理学 |
基金
|
国家自然科学基金
|
文献收藏号
|
CSCD:5414375
|
参考文献 共
15
共1页
|
1.
李岩. 小流域综合治理及其效益评价研究进展.
北京林业大学学报: 社会科学版,2008,7(3):62-66
|
CSCD被引
3
次
|
|
|
|
2.
游珍. 坡面植被对径流的减流减沙作用机理及试验研究.
泥沙研究,2011(3):59-62
|
CSCD被引
12
次
|
|
|
|
3.
刘窑军. 植被措施与路面汇水对三峡库区土质道路边坡侵蚀影响.
水科学进展,2014,25(1):98-105
|
CSCD被引
7
次
|
|
|
|
4.
高光耀. 干旱半干旱区坡面覆被格局的水土流失效应研究进展.
生态学报,2013(1):12-22
|
CSCD被引
59
次
|
|
|
|
5.
Fu B J. Agricultural landscape spatial pattern analysis in the semi-arid hill area of the Loess Plateau,China.
Journal of Arid Environments,2000,44(3):291-303
|
CSCD被引
42
次
|
|
|
|
6.
Zheng M G. Effect of vegetation on runoff-sediment yield relationship at different spatial scales in hilly areas of the Loess Plateau,North China.
Acta Ecologica Sinica,2007,27(9):3572-3581
|
CSCD被引
6
次
|
|
|
|
7.
史晓亮. 滦河流域土地利用/覆被变化的水文响应.
水科学进展,2014,25(1):21-27
|
CSCD被引
40
次
|
|
|
|
8.
贾媛媛. 黄土高原小流域分布式水蚀预报模型.
水利学报,2005,36(3):328-332
|
CSCD被引
20
次
|
|
|
|
9.
李文杰. 基于物理过程的分布式流域水沙预报模型.
水利学报,2012,43(3):264-274
|
CSCD被引
8
次
|
|
|
|
10.
曹文洪. 小流域产汇流分布式模型.
水利学报,2003,34(9):48-54
|
CSCD被引
12
次
|
|
|
|
11.
祁伟. 小流域侵蚀产沙分布式数学模型的研究.
中国水土保持科学,2004,2(1):13-18
|
CSCD被引
1
次
|
|
|
|
12.
Liu Q Q. Two-dimensional kinematic wave model of overland-flow.
Journal of Hydrology,2004,291(1/2):28-41
|
CSCD被引
9
次
|
|
|
|
13.
Liu Q Q. Hydraulic modeling of runoff yield in small watershed.
Proceeding of the XXII ICTAM. CDROM Proceedings ISBN 978-0-9805142-1-6,2008:25-29
|
CSCD被引
1
次
|
|
|
|
14.
杨立文. 林冠对降雨截留过程的研究.
河北林学院学报,1995,10(1):7-12
|
CSCD被引
8
次
|
|
|
|
15.
张洪江. 晋西几种不同土地利用状况下糙率系数的研究.
北京林业大学学报,1994,16(4):86-92
|
CSCD被引
15
次
|
|
|
|
|