2003
DOI: 10.2136/sssaj2003.1344
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Infiltration and Surface Geometry Features of a Swelling Soil following Successive Simulated Rainstorms

Abstract: rangement and distribution of the cracks. Moreover, White (1972) explained the energy implications that The theory of water movement in high shrink/swell soils has expericause the cracks to reappear in the same position from enced consistent revision since Haines first presented the topic in 1923. Several aspects of the infiltration process in cracking soils have event to event. Johnston and Hill (1944) observed that proven to be difficult to measure; seal/crust formation and properties, cracks develop between… Show more

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Cited by 38 publications
(39 citation statements)
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“…In a combined field and modelling study Graeff et al (2009) explained the second delayed peak by fast displacement of groundwater. In 1974 nearby mining activities started to exploit fluorite deposits at a depth of 190 m and a distance of nearly 1 km and bimodal rainfall-runoff events vanished almost completely (Wenk, 2000). Graeff et al (2009) explained this change in hydrological functioning by groundwater pumping activity that significantly lowered groundwater levels in this area.…”
Section: Impacts Of Land Use/land Cover Changesmentioning
confidence: 99%
See 1 more Smart Citation
“…In a combined field and modelling study Graeff et al (2009) explained the second delayed peak by fast displacement of groundwater. In 1974 nearby mining activities started to exploit fluorite deposits at a depth of 190 m and a distance of nearly 1 km and bimodal rainfall-runoff events vanished almost completely (Wenk, 2000). Graeff et al (2009) explained this change in hydrological functioning by groundwater pumping activity that significantly lowered groundwater levels in this area.…”
Section: Impacts Of Land Use/land Cover Changesmentioning
confidence: 99%
“…In temperate climate regions normal shrinkage is the most relevant mechanism, where volume reduction is approximately proportional to the water loss (Chertkov, 2000). When soil moisture drops below a threshold value cracks begin to develop and expand, which might enhance infiltration due to preferential flow (Bronswijk, 1988;Wells et al, 2003;Vogel et al, 2005a, b). Likewise, if the soil again wets up above a certain threshold value, the cracks begin to shrink and eventually close, and the local infiltration capacity is then substantially reduced.…”
Section: Shrinking and Swelling Soils Overland Flow And Infiltrationmentioning
confidence: 99%
“…Several aspects of the infiltration process in cracking soils have proven to be difficult to measure; seal/crust formation and properties, crack network patterns, preferential flow zones and contributions, and soil moisture determinations within the profile (Wells et al, 2003). For many soils, the physical changes that take place (such as swelling, sealing, shrinkage, and cracking) during and after rain following dry periods greatly affect the movement of water in the soil as the cracks develop deeper and transmit water to lower depths within the profile.…”
Section: Changes In Infiltration Through Soilsmentioning
confidence: 99%
“…In addition to swelling and cracking, clay soils form a surface seal, which also greatly affects infiltration (Wells et al, 2003). Surface sealing occurs due to the impact of raindrops on the surface of the soil, causing compaction, and settling of fine-grained detached material on the surface of the soil, effectively clogging the micropores.…”
Section: Changes In Infiltration Through Soilsmentioning
confidence: 99%
“…Deinert et al (2004) presented a method for using real-time neutron radiography to measure rapidly changing moisture profiles in porous media. In an interesting study, Wells et al (2003) used needle penetrometer to measure the depth of the wetting front along a single transect of the soil, immediately after each rainstorm. Wet sand transmits more light than dry sand.…”
Section: Introductionmentioning
confidence: 99%