Intensity-duration effects on drainage: Column experiments at near-zero pressure head

被引:9
作者
Torres, R [1 ]
Alexander, LJ [1 ]
机构
[1] Univ S Carolina, Dept Geol Sci, Columbia, SC 29208 USA
关键词
unsaturated; threshold; near-zero; enhanced drainage;
D O I
10.1029/2001WR001048
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We conducted column experiments to examine the effects of rapidly changing upper boundary flux conditions upon an unsaturated, near-zero pressure head flow region. An entire 0.75 m long medium sand column was driven to a quasi-steady pressure head and uniform water content with low-intensity irrigation. We then spike increased the irrigation rate by 2-9 times the background intensity but 3-4 orders of magnitude below the saturated hydraulic conductivity and for various durations. Thereafter, the irrigation rate was reduced to the prespike value for 1 hour and then stopped. Results show that during the postspike irrigation the pressure head, water content, and column storage decreased to values that were lower than those observed during the prespike interval, despite having the same steady irrigation rate. This observation indicates that a rapid decrease in surface flux upon a near-zero pressure head region could lead to an enhanced drainage of an unsaturated profile. The conceptual model explaining these observations relies on the "release'' of stored water from the bulk soil water flow.
引用
收藏
页数:11
相关论文
共 27 条
[1]   SYSTEM FOR AUTOMATING AND MULTIPLEXING SOIL-MOISTURE MEASUREMENT BY TIME-DOMAIN REFLECTOMETRY [J].
BAKER, JM ;
ALLMARAS, RR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1990, 54 (01) :1-6
[2]  
CHAMBERLIN TW, 1972, MOUNTAIN GEOMORPHOLO, P121
[3]  
GERMANN PF, 1990, WATER RESOUR RES, V26, P3055, DOI 10.1029/90WR01505
[4]   Scales and dimensions of momentum dissipation during preferential flow in soils [J].
Germann, PF ;
Di Pietro, L .
WATER RESOURCES RESEARCH, 1999, 35 (05) :1443-1454
[5]   Linearity of basin response as a function of scale in a semiarid watershed [J].
Goodrich, DC ;
Lane, LJ ;
Shillito, RM ;
Miller, SN ;
Syed, KH ;
Woolhiser, DA .
WATER RESOURCES RESEARCH, 1997, 33 (12) :2951-2965
[6]   WATER FLUX IN SOIL AND SUBSOIL ON A STEEP FORESTED SLOPE [J].
HARR, RD .
JOURNAL OF HYDROLOGY, 1977, 33 (1-2) :37-58
[7]   CANOPY AND LITTER INTERCEPTION OF RAINFALL BY HARDWOODS OF EASTERN UNITED STATES [J].
HELVEY, JD ;
PATRIC, JH .
WATER RESOURCES RESEARCH, 1965, 1 (02) :193-&
[8]  
Hendrickx J. M. H., 1990, Process studies in hillslope hydrology., P43
[9]   SHENANDOAH WATERSHED STUDY - CALIBRATION OF A TOPOGRAPHY-BASED, VARIABLE CONTRIBUTING AREA HYDROLOGICAL MODEL TO A SMALL FORESTED CATCHMENT [J].
HORNBERGER, GM ;
BEVEN, KJ ;
COSBY, BJ ;
SAPPINGTON, DE .
WATER RESOURCES RESEARCH, 1985, 21 (12) :1841-1850
[10]  
Jaynes D. B., 1990, Process studies in hillslope hydrology., P93