May land use change reduce the water deficiency problem caused by reduced brown coal mining in the state of Brandenburg?

被引:29
作者
Wechsung, F [1 ]
Krysanova, V [1 ]
Flechsig, M [1 ]
Schaphoff, S [1 ]
机构
[1] Potsdam Inst Climate Impact Res, D-14412 Potsdam, Germany
关键词
land use change; regional water balance; deintensification of agriculture; buffer zone; river corridors; runoff; evapotranspiration; groundwater recharge;
D O I
10.1016/S0169-2046(00)00108-0
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Surface mining alters the water regime not only locally, but also regionally. The reduced brown coal mining in the southeast of the state Brandenburg (Germany) leads to decreasing river discharge and consequently to a shortage in the water supply. Land use change is one possible option to counteract this development. In this simulation study, we explored the impact of temporary and permanent set-aside of arable land on Brandenburg's regional water balance. Temporary and permanent set-aside were considered as major measures towards deintensification of agriculture. Simulations were performed using the regional ecohydrological model SWIM, which integrates hydrological processes, vegetation growth, erosion and nutrient dynamics. The model was used to simulate the consequences of different land use change scenarios on main components of the regional water balance. Changes in the use of arable land altered clearly its water balance. The impact of these changes on the regional water balance for Brandenburg did not exceed +/-10% for its single components. Opposite tendencies were established in the simulations by contrasting effects of temporary and permanent set-aside of arable cropland. While temporary set-aside increased runoff from the whole area up to 6.7% due to lower evapotranspiration and higher soil moisture in arable land, the conversion of agricultural land within river corridors to meadows had an opposite effect on regional runoff (6.9% decrease) due to higher water retention coefficients and higher evapotranspiration losses. Therefore, only temporary set-aside may compensate to some extent for the anticipated decrease in river discharge. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:177 / 189
页数:13
相关论文
共 27 条
[1]  
[Anonymous], 1980, CREAMS FIELD SCALE M
[2]  
ARNOLD I, 1993, NATUR LANDSCHAFT NIE, V14, P3
[3]  
Arnold J., 1994, SWAT SOIL WATER ASSE
[4]   A COMPREHENSIVE SURFACE-GROUNDWATER FLOW MODEL [J].
ARNOLD, JG ;
ALLEN, PM ;
BERNHARDT, G .
JOURNAL OF HYDROLOGY, 1993, 142 (1-4) :47-69
[5]  
Arnold JG., 1990, SWRRB BASIN SCALE SI
[6]  
BORK HR, 1995, AGRARLANDSCHAFTSWAND
[7]   SIMULATION OF LAND-USE CHANGES AND IMPACTS ON THE WATER-BALANCE - A CASE-STUDY FOR BELGIUM [J].
BULTOT, F ;
DUPRIEZ, GL ;
GELLENS, D .
JOURNAL OF HYDROLOGY, 1990, 114 (3-4) :327-348
[8]  
GRUNEWALD U, 1995, WISS TAG DVWK 22 23, P14
[9]   A SIMPLIFIED SOIL AND PLANT PHOSPHORUS MODEL .1. DOCUMENTATION [J].
JONES, CA ;
COLE, CV ;
SHARPLEY, AN ;
WILLIAMS, JR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1984, 48 (04) :800-805
[10]  
Krysanova V, 1998, IAHS-AISH P, P13