Effect of rainfall and tillage direction on the evolution of surface crusts, soil hydraulic properties and runoff generation for a sandy loam soil
The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8 ha catchment located in the central region of Senegal. This was done by simulating 30 min rain storms applied at a constant rate of about 70 mm h −1, on 10 ru...
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| Published in | Journal of hydrology (Amsterdam) Vol. 307; no. 1; pp. 294 - 311 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Amsterdam
Elsevier B.V
09.06.2005
Elsevier Science Elsevier |
| Subjects | |
| Online Access | Get full text |
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| Abstract | The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8
ha catchment located in the central region of Senegal. This was done by simulating 30
min rain storms applied at a constant rate of about 70
mm
h
−1, on 10 runoff micro-plots of 1
m
2, five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust-types as well as their spatial distribution within micro-plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust-types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust-type covers more than 60% of the surface after 140
mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160
mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. |
|---|---|
| AbstractList | The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8
ha catchment located in the central region of Senegal. This was done by simulating 30
min rain storms applied at a constant rate of about 70
mm
h
−1, on 10 runoff micro-plots of 1
m
2, five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust-types as well as their spatial distribution within micro-plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust-types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust-type covers more than 60% of the surface after 140
mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160
mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8 ha catchment located in the central region of Senegal. This was done by simulating 30 min rain storms applied at a constant rate of about 70 mm h(-1), on 10 runoff micro-plots of 1 m2, five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust-types as well as their spatial distribution within micro-plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust-types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust-type covers more than 60% of the surface after 140 mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160 mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8 ha catchment located in the central region of Senegal. This was done by simulating 30 min rain storms applied at a constant rate of about 70 mm h−1, on 10 runoff micro-plots of 1 m2, five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust-types as well as their spatial distribution within micro-plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust-types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust-type covers more than 60% of the surface after 140 mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160 mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. The study was aimed at evaluating the effect of rainfall and tillage--induced soil surface characteristics on infiltration and runoff on a 2*8ha catchment located in the central region of Senegal. This was done by simulating 30min rain storms applied at a constant rate of about 70mmh(--1), on 10 runoff micro--plots of 1m(2), five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust--types as well as their spatial distribution within micro--plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust--types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust--type covers more than 60% of the surface after 140mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. The influence of tillage and rainfall energy on infiltration into and runoff from a sandy loam soil and on development of a surface crust was studied at a site in the Thysse-Kaymoor catchment in central Senegal. Soil surface hydraulic properties under near saturation conditions, including capillary sorptivity, hydraulic conductivity, mean characteristic pore size, and time to ponding, were quantified. Simulated rainfall was applied to plots freshly harrowed perpendicular to the slope and along the slope. Surface crust development greatly explained declining hydraulic conductivity and sorptivity as cumulative rainfall since tillage increased. Exponential decay rates were significantly greater for soil tilled along the slope than for soil tilled across the slope. Ponding and runoff were affected by tillage direction as well. Soil hydraulic properties after about 160 mm of rainfall were nearly the same as those for untilled plots not receiving any rain, showing that the effects of tillage were short lived. The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8 ha catchment located in the central region of Senegal. This was done by simulating 30 min rain storms applied at a constant rate of about 70 mm h super(-1), on 10 runoff micro-plots of 1 m super(2), five being freshly harrowed perpendicularly to the slope and five along the slope (1%) of the catchment. Runoff was automatically recorded at the outlet of each plot. Hydraulic properties such as capillary sorptivity and hydraulic conductivity of the sandy loam soil close to saturation were determined by running 48 infiltration tests with a tension disc infiltrometer. That allowed the calculation of a mean characteristic pore size hydraulically active and a time to ponding. Superficial water storage capacity was estimated using data collected with an electronic relief meter. Because the soil was subject to surface crusting, crust-types as well as their spatial distribution within micro-plots and their evolution with time were identified and monitored by taking photographs at different times after tillage. The results showed that the surface crust-types as well as their tillage dependent dynamics greatly explain the decrease of hydraulic conductivity and sorptivity as the cumulative rainfall since tillage increases. The exponential decaying rates were found to be significantly greater for the soil harrowed along the slope (where the runoff crust-type covers more than 60% of the surface after 140 mm of rain) than across to the slope (where crusts are mainly of structural (60%) and erosion (40%) types). That makes ponding time smaller and runoff more important. Also it was shown that soil hydraulic properties after about 160 mm of rain were close to those of untilled plot not submitted to any rain. That indicates that the effects of tillage are short lived. |
| Author | Lapetite, Jean-Marc Ndiaye, Babacar Vauclin, Michel Esteves, Michel Vandervaere, Jean-Pierre |
| Author_xml | – sequence: 1 givenname: Babacar surname: Ndiaye fullname: Ndiaye, Babacar – sequence: 2 givenname: Michel surname: Esteves fullname: Esteves, Michel email: michel.esteves@hmg.inpg.fr – sequence: 3 givenname: Jean-Pierre surname: Vandervaere fullname: Vandervaere, Jean-Pierre – sequence: 4 givenname: Jean-Marc surname: Lapetite fullname: Lapetite, Jean-Marc – sequence: 5 givenname: Michel surname: Vauclin fullname: Vauclin, Michel |
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| Keywords | Rainfall simulation Tension disc infiltrometer Soil crusting Tillage direction Ponding time Senegal rain water digital simulation slopes spatial distribution tillage saturation drainage basins hydraulic conductivity hydraulics water storage relief soils loam rainfall tension Africa runoff infiltration erosion storms |
| Language | English |
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| Snippet | The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8
ha catchment... The study was aimed at evaluating the effect of rainfall and tillage-induced soil surface characteristics on infiltration and runoff on a 2.8 ha catchment... The influence of tillage and rainfall energy on infiltration into and runoff from a sandy loam soil and on development of a surface crust was studied at a site... The study was aimed at evaluating the effect of rainfall and tillage--induced soil surface characteristics on infiltration and runoff on a 2*8ha catchment... |
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| SubjectTerms | agricultural runoff agricultural watersheds Earth Sciences Earth, ocean, space Exact sciences and technology hydraulic conductivity Hydrology Hydrology. Hydrogeology infiltration (hydrology) Ponding time rain Rainfall simulation sandy loam soils Sciences of the Universe Senegal Soil crusting soil crusts soil hydraulic properties Tension disc infiltrometer tillage Tillage direction |
| Title | Effect of rainfall and tillage direction on the evolution of surface crusts, soil hydraulic properties and runoff generation for a sandy loam soil |
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