Spatial and temporal variations in percolation fluxes in a tropical Andosol influenced by banana cropping patterns

被引:25
作者
Cattan, P. [1 ]
Voltz, M.
Cabidoche, Y. -M.
Lacas, J-G.
Sansoulet, J.
机构
[1] CIRAD, UPR 26, Stn Neufchateau, F-97130 Capesterre Belle Eau, Guadeloupe, France
[2] INRA, LISAH, UMR AgroM, IRD, F-34060 Montpellier 1, France
[3] INRA, UR Agropedoclimat Zone Caraibe, Petit Bourg, Guadeloupe, France
关键词
percolation; rainfall partitioning; spatial variability; andosols; banana; lysimeters;
D O I
10.1016/j.jhydrol.2006.11.009
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Spatial variability in percolation fluxes was studied in field plots cropped with banana plants, which induce very heterogeneous rainfall partitioning at the soil surface, with high subsequent infiltration in Andosols. Percolation fluxes were measured for just over a year at 1-7 day intervals in eight wick (WL) and gravity lysimeters (GL) that had been buried in the soil at a depth of 60 cm. The results revealed that WL captured unsaturated fluxes while GL only functioned after ponding occurred. The percolation flux measurements were highly biased with both systems, i.e. overpercolation with WL and underpercolation with GL. Percolation fluxes seemed, however, to be mainly unsaturated in the soil types studied. High percolation flux variability was noted on a plot scale, which could be explained by the vegetation structure: total percolation flux (WL) was 2.1-fold higher under banana plants; saturated percolation flux (GL) was 7-fold higher under banana plants and almost absent between banana plants. Eighty-eight per cent of the total variance in percolation flux could be explained by the rainfall intensity under the banana canopy, calculated while taking the rainfall partitioning by the vegetation and the initial water status into account. The number of Lysimeters required for assessing percolation flux in a field plot can be reduced by taking the spatial patterns of the flux boundary conditions into account. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:157 / 169
页数:13
相关论文
共 44 条
[1]   Application of a two-dimensional model to simulate flow and transport in a macroporous agricultural soil with tile drains [J].
Abbaspour, KC ;
Kohler, A ;
Simunek, J ;
Fritsch, M ;
Schulin, R .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2001, 52 (03) :433-447
[2]   Simulation of water flow and solute transport in free-drainage lysimeters and field soils with heterogeneous structures [J].
Abdou, HM ;
Flury, M .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2004, 55 (02) :229-241
[3]  
ARYA LM, 1975, SOIL SCI SOC AM J, V39, P433
[4]   Mechanisms of surface runoff genesis on a subsurface drained soil affected by surface crusting: A field investigation [J].
Augeard, B ;
Kao, C ;
Chaumont, C ;
Vauclin, M .
PHYSICS AND CHEMISTRY OF THE EARTH, 2005, 30 (8-10) :598-610
[5]  
BASSETTE C, 2005, MODELISATION 3D LINT, P153
[6]  
BASTERGUE P, 1988, MESURE ESTIMATION LE
[7]  
BOLL J, 1991, LYSIMETERS FOR EVAPOTRANSPIRATION AND ENVIRONMENTAL MEASUREMENTS, P290
[8]   FIBERGLASS WICKS FOR SAMPLING OF WATER AND SOLUTES IN THE VADOSE ZONE [J].
BOLL, J ;
STEENHUIS, TS ;
SELKER, JS .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (03) :701-707
[9]  
BONAN H, 2001, 2001070 MIN AM TERR
[10]   Field evaluation of passive capillary samplers [J].
BrandiDohrn, FM ;
Dick, RP ;
Hess, M ;
Selker, JS .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1996, 60 (06) :1705-1713