Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models

Evaporation of water from 'micro-lysimeters' collected from four types of field tillage treatments, namely, ploughed to a depth of 30cm (P), ploughed and then harrowed (P + H), ploughed, harrowed and rolled (P + H + R) and untilled (UNT) plots, was studied in a controlled laboratory environment at f...

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Main Authors: Mwendera, E.J., Feyen, J.
Format: Journal Article
Language:Inglés
Published: Elsevier 1997
Subjects:
Online Access:https://hdl.handle.net/10568/35268
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author Mwendera, E.J.
Feyen, J.
author_browse Feyen, J.
Mwendera, E.J.
author_facet Mwendera, E.J.
Feyen, J.
author_sort Mwendera, E.J.
collection Repository of Agricultural Research Outputs (CGSpace)
description Evaporation of water from 'micro-lysimeters' collected from four types of field tillage treatments, namely, ploughed to a depth of 30cm (P), ploughed and then harrowed (P + H), ploughed, harrowed and rolled (P + H + R) and untilled (UNT) plots, was studied in a controlled laboratory environment at five rates of atmospheric evaporativity close to those found under field conditions. Evaporative demand (E(o)) in the field was determined by measuring evaporation from open water with a recording evaporation balance. Actual evaporation from the field soil was determined by daily measurement of water content in the top 10 and 20cm layers. Drying was best described by a modified version of the square root of time behaviour model of T.A. Black, W.R. Gardener and G.W. Thurtell (The prediction of evaporation drainage and soil water storage for a bare soil. Soil Sci. Am. Proc., 33: 655-660, 1969) and a simple parametric model similar to that proposed by J.J.T.I. Boesten and L. Stroosnijder (Simple model for daily evaporation from fallow tilled soil under spring conditions in a temperate climate. Neth. J. Agric. Sci., 34: 75-80, 1986). The parametric model was incorporated in a model describing water dynamics in a silt loam soil (Typic Hapludalf) on field plots located near Ter Munck, 5 km southwest of Leuven, Belgium. The results show that drying characteristics of tilled soils are influenced by factors such as tillage depth, surface micro-relief, soil type, and the nature of the evaporative demand, and that it is possible to incorporate such effects in evaporation models. However, more research is needed to study the combined effects of tillage type and depth and atmospheric evaporativity on the drying characteristics of different soils, and to compare the relative effect of radiation-dominated evaporativity on the evaporation parameters with that of wind-dominated evaporativity.
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spelling CGSpace352682024-08-27T12:27:46Z Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models Mwendera, E.J. Feyen, J. farming systems water research Evaporation of water from 'micro-lysimeters' collected from four types of field tillage treatments, namely, ploughed to a depth of 30cm (P), ploughed and then harrowed (P + H), ploughed, harrowed and rolled (P + H + R) and untilled (UNT) plots, was studied in a controlled laboratory environment at five rates of atmospheric evaporativity close to those found under field conditions. Evaporative demand (E(o)) in the field was determined by measuring evaporation from open water with a recording evaporation balance. Actual evaporation from the field soil was determined by daily measurement of water content in the top 10 and 20cm layers. Drying was best described by a modified version of the square root of time behaviour model of T.A. Black, W.R. Gardener and G.W. Thurtell (The prediction of evaporation drainage and soil water storage for a bare soil. Soil Sci. Am. Proc., 33: 655-660, 1969) and a simple parametric model similar to that proposed by J.J.T.I. Boesten and L. Stroosnijder (Simple model for daily evaporation from fallow tilled soil under spring conditions in a temperate climate. Neth. J. Agric. Sci., 34: 75-80, 1986). The parametric model was incorporated in a model describing water dynamics in a silt loam soil (Typic Hapludalf) on field plots located near Ter Munck, 5 km southwest of Leuven, Belgium. The results show that drying characteristics of tilled soils are influenced by factors such as tillage depth, surface micro-relief, soil type, and the nature of the evaporative demand, and that it is possible to incorporate such effects in evaporation models. However, more research is needed to study the combined effects of tillage type and depth and atmospheric evaporativity on the drying characteristics of different soils, and to compare the relative effect of radiation-dominated evaporativity on the evaporation parameters with that of wind-dominated evaporativity. 1997-03 2014-04-14T10:55:44Z 2014-04-14T10:55:44Z Journal Article https://hdl.handle.net/10568/35268 en Limited Access Elsevier Mwendera, E.J. and Feyen, J. 1997. Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models. Soil and Tillage Research 41(1-2): 127 - 140
spellingShingle farming systems
water
research
Mwendera, E.J.
Feyen, J.
Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title_full Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title_fullStr Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title_full_unstemmed Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title_short Tillage and evaporativity effects on the drying characteristics of a silty loam: Evaporation prediction models
title_sort tillage and evaporativity effects on the drying characteristics of a silty loam evaporation prediction models
topic farming systems
water
research
url https://hdl.handle.net/10568/35268
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