The zone of vegetation influence on baseflow revealed by diet patterns of streamflow and vegetation water use in a headwater basin

被引:122
作者
Bond, BJ
Jones, JA
Moore, G
Phillips, N
Post, D
McDonnell, JJ
机构
[1] Oregon State Univ, Dept Forest Sci, Corvallis, OR 97331 USA
[2] Oregon State Univ, Dept Geosci, Corvallis, OR 97331 USA
[3] Boston Univ, Dept Geog, Boston, MA 02215 USA
[4] CSIRO Land & Water, Aitkenvale, Qld 4814, Australia
[5] Oregon State Univ, Dept Forest Engn, Corvallis, OR 97331 USA
关键词
D O I
10.1002/hyp.5022
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Water use by vegetation can be closely linked to streamflow patterns on a variety of time scales. However, many of the details of these linkages are poorly understood. We compared diel (24 h) patterns of transpirational water use with streamflow patterns in a small headwater basin that displays a marked diel variation during summer months. The study site was in western Oregon. Our objectives were to: (1) determine the phase shift, i.e. the time lag between maximum transpiration and minimum streamflow, and the strength of the correlation at that time lag; (2) determine the amount of streamflow that is 'missing' during each diel cycle (i.e. the difference between base flow, defined by the daily maxima, and actual flow) and use it to estimate the zone, or area, of vegetation that influences daily streamflow patterns; (3) test and refine a conceptual model of how the coupling between vegetation water use and streamflow changes over the period of summer drought in this basin. We found that vegetation water use in the summer is coupled to streamflow over time scales of 4 to 8 h, and water-use-related fluctuations accounted for 1 to 6% of summer base flow. Direct evaporation from the channel was an order of magnitude less than the diel streamflow decrease. Transpiration within only 0.1 to 0.3% of the basin area accounted for the diel variation in streamflow. As the basin drained further through the summer, the coupling between vegetation and streamflow was diminished and occurred at longer time scales, and the zone of vegetation influence became smaller. This pattern is in accordance with our conceptual model, which attributes the summer decline in the strength of the vegetation-streamflow coupling to the increasing depth of plant-available water in the soil profile. Although this study is preliminary, we believe it is an important first step in describing better the coupling of vegetation water use to streamflow. Copyright (C) 2002 John Wiley Sons, Ltd.
引用
收藏
页码:1671 / 1677
页数:7
相关论文
共 34 条
[1]  
Bencala KE, 2000, HYDROL PROCESS, V14, P2797, DOI 10.1002/1099-1085(20001030)14:15<2797::AID-HYP402>3.0.CO
[2]  
2-6
[3]   A dynamic TOPMODEL [J].
Beven, K ;
Freer, J .
HYDROLOGICAL PROCESSES, 2001, 15 (10) :1993-2011
[4]   DIURNAL-VARIATIONS IN STREAM DISCHARGE AND THROUGHFLOW DURING A PERIOD OF LOW FLOW [J].
BURT, TP .
JOURNAL OF HYDROLOGY, 1979, 41 (3-4) :291-301
[5]   MODULATION OF THE DIURNAL STREAMFLOW RESPONSE BY THE SEASONAL SNOWCOVER OF AN ALPINE BASIN [J].
CAINE, N .
JOURNAL OF HYDROLOGY, 1992, 137 (1-4) :245-260
[6]   INFLUENCE OF DIURNAL-VARIATIONS IN STREAM TEMPERATURE ON STREAMFLOW LOSS AND GROUNDWATER RECHARGE [J].
CONSTANTZ, J ;
THOMAS, CL ;
ZELLWEGER, G .
WATER RESOURCES RESEARCH, 1994, 30 (12) :3253-3264
[7]   EARLY STAGES OF PLANT SUCCESSION FOLLOWING LOGGING AND BURNING IN WESTERN CASCADES OF OREGON [J].
DYRNESS, CT .
ECOLOGY, 1973, 54 (01) :57-69
[8]  
DYRNESS T, 1967, 42 PNW FOR RANG EXPT
[9]   Practical applications of spectral analysis to hydrologic time series [J].
Fleming, SW ;
Lavenue, AM ;
Aly, AH ;
Adams, A .
HYDROLOGICAL PROCESSES, 2002, 16 (02) :565-574
[10]   A NEW METHOD OF SAP FLOW MEASUREMENT IN TREE STEMS [J].
GRANIER, A .
ANNALES DES SCIENCES FORESTIERES, 1985, 42 (02) :193-200