Impacts of landscape management on the hydrological behaviour of small agricultural catchments

被引:16
作者
Bormann, H
Diekkrüger, B
Hauschild, M
机构
[1] Univ Bonn, Inst Geog, D-53115 Bonn, Germany
[2] Univ Gesamthsch Kassel, Ctr Environm Syst Res, D-34109 Kassel, Germany
来源
PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE | 1999年 / 24卷 / 04期
关键词
D O I
10.1016/S1464-1909(99)00002-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Changes of agricultural land use often induce changes of the hydrological behaviour of catchments. Because only the effects on a few processes are measurable, modelling and simulating the hydrological processes can help to estimate the impact of land use changes on distinct hydrological quantities (e.g. evapotranspiration, groundwater recharge, runoff production, channel runoff). While selecting management measures hydrological models can serve as tools for decision making. Possible aims are the reduction of flood events, guaranteeing the supply of drinking water (amount and quality) and optimising use of irrigation water in agriculture. In order to forecast the effects of management on hydrology a physically based, deterministic model system is applied which consists of two model parts, an one dimensional soil-vegetation-atmosphere-transfer model (SVAT) and a distributed catchment model. The sensitivity of the model and its parameters is shown by scenarios whose quantitative model results are transferred to qualitative statements concerning effects of landscape management on hydrology. Especially the effect of land use changes due to EC policy (applying different fallow practices) on the catchment water balance and on the channel runoff (flood events) is investigated, additionally the reestablishment of channels and the impact of plant growth in channels. (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:291 / 296
页数:6
相关论文
共 11 条
[1]   A COMPREHENSIVE SURFACE-GROUNDWATER FLOW MODEL [J].
ARNOLD, JG ;
ALLEN, PM ;
BERNHARDT, G .
JOURNAL OF HYDROLOGY, 1993, 142 (1-4) :47-69
[2]  
ARNOLD JG, 1989, T ASAE, V32, P161, DOI 10.13031/2013.30976
[3]   Effects of data availability on estimation of evapotranspiration [J].
Bormann, H ;
Diekkruger, B ;
Richter, O .
PHYSICS AND CHEMISTRY OF THE EARTH, VOL 21, NO 3, MAY 1996: SOIL-VEGETATION-ATMOSPHERE TRANSFER AT DIFFERENT SCALES, 1996, 21 (03) :171-175
[4]  
BORMANN H, 1998, IN PRESS IAHS PUBLIC
[5]   SIMULATION OF WATER FLUXES USING DIFFERENT METHODS FOR ESTIMATING SOIL PARAMETERS [J].
DIEKKRUGER, B ;
ARNING, M .
ECOLOGICAL MODELLING, 1995, 81 (1-3) :83-95
[6]  
FLACH AJ, 1969, SCHRIFTENREIHE DTSCH
[7]  
RAWLS WJ, P S WAT MAN 80S TEMP, P293
[8]   PARAMETER-EFFICIENT HYDROLOGIC INFILTRATION-MODEL [J].
SMITH, RE ;
PARLANGE, JY .
WATER RESOURCES RESEARCH, 1978, 14 (03) :533-538
[9]  
SMITH RE, 1992, ARS98 USDA, V1, P120
[10]  
VONSCHILFGAARDE J, 1970, ADV HYDROSCI, V6, P43