Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry

Time domain reflectometry [TDR] was used to investigate the spatial and temporal variation in surface soil water dynamics under a number of types of vegetation, including both trees and crops grown in isolation, and grown together as an agroforestry system. The installation and operation of this tec...

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Main Authors: N. A. Jackson, J. C. Wallace
Format: Article
Language:English
Published: Copernicus Publications 1999-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/3/517/1999/hess-3-517-1999.pdf
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spelling doaj-88866dc8625a4017823525a4e41391802020-11-24T22:30:09ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79381999-01-0134517527Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometryN. A. JacksonN. A. JacksonJ. C. WallaceJ. C. WallaceTime domain reflectometry [TDR] was used to investigate the spatial and temporal variation in surface soil water dynamics under a number of types of vegetation, including both trees and crops grown in isolation, and grown together as an agroforestry system. The installation and operation of this technique are presented, and discussed in terms of its suitability to monitor rapid fluctuations in soil-water content in a spatially heterogeneous system such as that described in this experiment. <br>The relatively small sampling volume of each of the TDR waveguides permitted discrete measurements to be made of soil water content (&#952;<sub>v</sub>). In the tree-only and tree&#43;crop treatments, this revealed considerable variation in &#952;<sub>v</sub> resulting from spatial redistribution of rainfall under the tree canopies, with a significant input to soil close to the base of the trees being made by stemflow, i.e. water intercepted by the tree canopy and channelled down the stem. <br>Over the experimental period (one rainy season) the TDR data suggested that net recharge to the soil profile in the sole crop system was 53 mm, almost 75% more than occurred in either of the two treatments containing trees, reflecting greater rainfall interception by the tree canopies.http://www.hydrol-earth-syst-sci.net/3/517/1999/hess-3-517-1999.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. A. Jackson
N. A. Jackson
J. C. Wallace
J. C. Wallace
spellingShingle N. A. Jackson
N. A. Jackson
J. C. Wallace
J. C. Wallace
Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
Hydrology and Earth System Sciences
author_facet N. A. Jackson
N. A. Jackson
J. C. Wallace
J. C. Wallace
author_sort N. A. Jackson
title Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
title_short Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
title_full Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
title_fullStr Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
title_full_unstemmed Analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
title_sort analysis of soil water dynamics in an agroforestry system based on detailed soil water records from time-domain reflectometry
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 1999-01-01
description Time domain reflectometry [TDR] was used to investigate the spatial and temporal variation in surface soil water dynamics under a number of types of vegetation, including both trees and crops grown in isolation, and grown together as an agroforestry system. The installation and operation of this technique are presented, and discussed in terms of its suitability to monitor rapid fluctuations in soil-water content in a spatially heterogeneous system such as that described in this experiment. <br>The relatively small sampling volume of each of the TDR waveguides permitted discrete measurements to be made of soil water content (&#952;<sub>v</sub>). In the tree-only and tree&#43;crop treatments, this revealed considerable variation in &#952;<sub>v</sub> resulting from spatial redistribution of rainfall under the tree canopies, with a significant input to soil close to the base of the trees being made by stemflow, i.e. water intercepted by the tree canopy and channelled down the stem. <br>Over the experimental period (one rainy season) the TDR data suggested that net recharge to the soil profile in the sole crop system was 53 mm, almost 75% more than occurred in either of the two treatments containing trees, reflecting greater rainfall interception by the tree canopies.
url http://www.hydrol-earth-syst-sci.net/3/517/1999/hess-3-517-1999.pdf
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