The effect of microtopography on soil-water movement is a topic of interest for a range of disciplines, with experimental studies investigating the relationship between the two lacking. Laboratory experiments were conducted by simulating rainfall across packed soil surfaces to investigate the effect of microtopography on wetting front movement within experimental soil profiles. In small soil box experiments, the observed wetting fronts for soil profiles showed considerably deeper movement beneath a smooth surface than depressions for 12–60 min rainfalls. For large soil box experiments, the wetting front reached moisture sensors installed at 5 and 10 cm depths and corresponding to various rough and smooth surface features at significantly di...
International audienceSoil surface crusting has a major impact on water infiltration and erosion in ...
Plain farmland areas without significant topographic slope exhibit microtopographic features of diff...
This study presents the results of laboratory experiments, conducted on an impermeable smooth plane ...
Microtopography is an important factor in hydrologic processes. The purpose of this research was to ...
In the study we evaluated spatial and quantitative changes in soil surface microtopography to descri...
Soil surface characteristics (SSCs) are highly variable even at a small scale (< 1m2) and the infilt...
Proceedings of the 1989 Georgia Water Resources Conference, May 16-17, 1989, Athens, Georgia.Site pr...
The detachment of soil by flowing water on a hillslope is dependent upon the hydraulics of shallow o...
Tillage-induced microtopography may affect hydrological and erosion processes. Nevertheless, how the...
This research combines field, laboratory and numerical investigations to estimate the development of...
Different points in a field can be wetted with different natural or artificial rainfall amounts and ...
This paper describes laboratory experimental evidence for lateral flow in the top layer of unsaturat...
International audienceA good understanding of the soil strength profile under wetting-drying (W-D) c...
At finer scales, raindrops are the sources of the onset of soil erosion. Understanding the effects o...
International audienceSoil surface crusting has a major impact on water infiltration and erosion in ...
Plain farmland areas without significant topographic slope exhibit microtopographic features of diff...
This study presents the results of laboratory experiments, conducted on an impermeable smooth plane ...
Microtopography is an important factor in hydrologic processes. The purpose of this research was to ...
In the study we evaluated spatial and quantitative changes in soil surface microtopography to descri...
Soil surface characteristics (SSCs) are highly variable even at a small scale (< 1m2) and the infilt...
Proceedings of the 1989 Georgia Water Resources Conference, May 16-17, 1989, Athens, Georgia.Site pr...
The detachment of soil by flowing water on a hillslope is dependent upon the hydraulics of shallow o...
Tillage-induced microtopography may affect hydrological and erosion processes. Nevertheless, how the...
This research combines field, laboratory and numerical investigations to estimate the development of...
Different points in a field can be wetted with different natural or artificial rainfall amounts and ...
This paper describes laboratory experimental evidence for lateral flow in the top layer of unsaturat...
International audienceA good understanding of the soil strength profile under wetting-drying (W-D) c...
At finer scales, raindrops are the sources of the onset of soil erosion. Understanding the effects o...
International audienceSoil surface crusting has a major impact on water infiltration and erosion in ...
Plain farmland areas without significant topographic slope exhibit microtopographic features of diff...
This study presents the results of laboratory experiments, conducted on an impermeable smooth plane ...