Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment

Despite the widely held assumption that trees negatively affect the local water budget in densely planted tree plantations, we still lack a clear understanding of the underlying processes by which canopy cover influences local soil water dynamics in more open, humid tropical ecosystems. In this study, we propose a new conceptual model that uses a combination of stable isotope and soil moisture measurements throughout the soil profile to assess potential mechanisms by which evaporation (of surface soil water and of canopy‐intercepted rainfall) affects the relationship between surface soil water isotopic enrichment (lc‐excess) and soil water content. Our conceptual model was derived from soil water data collected under deciduous and evergreen plants in a shade grown coffee agroforestry system in Costa Rica. Reduced soil moisture under shade trees during the “drier” season, coinciding when these trees were defoliated, was largely the result of increase soil water evaporation as indicated by the positive relationship between soil water content and lc‐excess of surface soil water. In contrast, the evergreen coffee shrubs had a higher leaf area index during the “drier” season, leading to enhanced rainfall interception and a negative relationship between lc‐excess and soil water content. During the wet season, there was no clear relationship between soil water content and between lc‐excess of surface soil water. Greater surface soil water under coffee during the dry season may, in part, explain greater preferential flow under coffee compared with under trees in conditions of low rainfall intensities. However, with increasing rainfall intensities during the wet season, there was no obvious difference in preferential flow between the two canopy covers. Results from this study indicate that our new conceptual model can be used to help disentangling the relative influence of canopy cover on local soil water isotopic composition and dynamics, yet also stresses the need for additional measurements to better resolve the underlying processes by which canopy structure influences local water dynamics.

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Main Authors: Hasselquist, Niles J., Benegas, Laura, Roupsard, Olivier, Malmer, Anders, Ilstedt, Ulrik
Format: article biblioteca
Language:eng
Published: Wiley
Subjects:F08 - Systèmes et modes de culture, P33 - Chimie et physique du sol, U30 - Méthodes de recherche, agroforesterie, eau du sol, arbre d'ombrage, Coffea arabica, indice de végétation, variation saisonnière, isotope, modèle, http://aims.fao.org/aos/agrovoc/c_207, http://aims.fao.org/aos/agrovoc/c_7205, http://aims.fao.org/aos/agrovoc/c_25548, http://aims.fao.org/aos/agrovoc/c_1721, http://aims.fao.org/aos/agrovoc/c_9000171, http://aims.fao.org/aos/agrovoc/c_24894, http://aims.fao.org/aos/agrovoc/c_11852, http://aims.fao.org/aos/agrovoc/c_4881, http://aims.fao.org/aos/agrovoc/c_1920,
Online Access:http://agritrop.cirad.fr/588137/
http://agritrop.cirad.fr/588137/1/Hasselquist_HP_2018%20Canopy%20cover%20effects%20on%20local%20soil%20water%20dynamics%20Evaporation%20drives%20soil%20water%20isotopic%20enrichment.pdf
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spelling dig-cirad-fr-5881372024-12-18T13:39:23Z http://agritrop.cirad.fr/588137/ http://agritrop.cirad.fr/588137/ Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment. Hasselquist Niles J., Benegas Laura, Roupsard Olivier, Malmer Anders, Ilstedt Ulrik. 2018. Hydrological Processes, 32 (8) : 994-1004.https://doi.org/10.1002/hyp.11482 <https://doi.org/10.1002/hyp.11482> Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment Hasselquist, Niles J. Benegas, Laura Roupsard, Olivier Malmer, Anders Ilstedt, Ulrik eng 2018 Wiley Hydrological Processes F08 - Systèmes et modes de culture P33 - Chimie et physique du sol U30 - Méthodes de recherche agroforesterie eau du sol arbre d'ombrage Coffea arabica indice de végétation variation saisonnière isotope modèle http://aims.fao.org/aos/agrovoc/c_207 http://aims.fao.org/aos/agrovoc/c_7205 http://aims.fao.org/aos/agrovoc/c_25548 http://aims.fao.org/aos/agrovoc/c_1721 http://aims.fao.org/aos/agrovoc/c_9000171 http://aims.fao.org/aos/agrovoc/c_24894 http://aims.fao.org/aos/agrovoc/c_11852 http://aims.fao.org/aos/agrovoc/c_4881 Costa Rica http://aims.fao.org/aos/agrovoc/c_1920 Despite the widely held assumption that trees negatively affect the local water budget in densely planted tree plantations, we still lack a clear understanding of the underlying processes by which canopy cover influences local soil water dynamics in more open, humid tropical ecosystems. In this study, we propose a new conceptual model that uses a combination of stable isotope and soil moisture measurements throughout the soil profile to assess potential mechanisms by which evaporation (of surface soil water and of canopy‐intercepted rainfall) affects the relationship between surface soil water isotopic enrichment (lc‐excess) and soil water content. Our conceptual model was derived from soil water data collected under deciduous and evergreen plants in a shade grown coffee agroforestry system in Costa Rica. Reduced soil moisture under shade trees during the “drier” season, coinciding when these trees were defoliated, was largely the result of increase soil water evaporation as indicated by the positive relationship between soil water content and lc‐excess of surface soil water. In contrast, the evergreen coffee shrubs had a higher leaf area index during the “drier” season, leading to enhanced rainfall interception and a negative relationship between lc‐excess and soil water content. During the wet season, there was no clear relationship between soil water content and between lc‐excess of surface soil water. Greater surface soil water under coffee during the dry season may, in part, explain greater preferential flow under coffee compared with under trees in conditions of low rainfall intensities. However, with increasing rainfall intensities during the wet season, there was no obvious difference in preferential flow between the two canopy covers. Results from this study indicate that our new conceptual model can be used to help disentangling the relative influence of canopy cover on local soil water isotopic composition and dynamics, yet also stresses the need for additional measurements to better resolve the underlying processes by which canopy structure influences local water dynamics. article info:eu-repo/semantics/article Journal Article info:eu-repo/semantics/publishedVersion http://agritrop.cirad.fr/588137/1/Hasselquist_HP_2018%20Canopy%20cover%20effects%20on%20local%20soil%20water%20dynamics%20Evaporation%20drives%20soil%20water%20isotopic%20enrichment.pdf text Cirad license info:eu-repo/semantics/restrictedAccess https://agritrop.cirad.fr/mention_legale.html https://doi.org/10.1002/hyp.11482 10.1002/hyp.11482 info:eu-repo/semantics/altIdentifier/doi/10.1002/hyp.11482 info:eu-repo/semantics/altIdentifier/purl/https://doi.org/10.1002/hyp.11482
institution CIRAD FR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cirad-fr
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CIRAD Francia
language eng
topic F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
U30 - Méthodes de recherche
agroforesterie
eau du sol
arbre d'ombrage
Coffea arabica
indice de végétation
variation saisonnière
isotope
modèle
http://aims.fao.org/aos/agrovoc/c_207
http://aims.fao.org/aos/agrovoc/c_7205
http://aims.fao.org/aos/agrovoc/c_25548
http://aims.fao.org/aos/agrovoc/c_1721
http://aims.fao.org/aos/agrovoc/c_9000171
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_11852
http://aims.fao.org/aos/agrovoc/c_4881
http://aims.fao.org/aos/agrovoc/c_1920
F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
U30 - Méthodes de recherche
agroforesterie
eau du sol
arbre d'ombrage
Coffea arabica
indice de végétation
variation saisonnière
isotope
modèle
http://aims.fao.org/aos/agrovoc/c_207
http://aims.fao.org/aos/agrovoc/c_7205
http://aims.fao.org/aos/agrovoc/c_25548
http://aims.fao.org/aos/agrovoc/c_1721
http://aims.fao.org/aos/agrovoc/c_9000171
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_11852
http://aims.fao.org/aos/agrovoc/c_4881
http://aims.fao.org/aos/agrovoc/c_1920
spellingShingle F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
U30 - Méthodes de recherche
agroforesterie
eau du sol
arbre d'ombrage
Coffea arabica
indice de végétation
variation saisonnière
isotope
modèle
http://aims.fao.org/aos/agrovoc/c_207
http://aims.fao.org/aos/agrovoc/c_7205
http://aims.fao.org/aos/agrovoc/c_25548
http://aims.fao.org/aos/agrovoc/c_1721
http://aims.fao.org/aos/agrovoc/c_9000171
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_11852
http://aims.fao.org/aos/agrovoc/c_4881
http://aims.fao.org/aos/agrovoc/c_1920
F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
U30 - Méthodes de recherche
agroforesterie
eau du sol
arbre d'ombrage
Coffea arabica
indice de végétation
variation saisonnière
isotope
modèle
http://aims.fao.org/aos/agrovoc/c_207
http://aims.fao.org/aos/agrovoc/c_7205
http://aims.fao.org/aos/agrovoc/c_25548
http://aims.fao.org/aos/agrovoc/c_1721
http://aims.fao.org/aos/agrovoc/c_9000171
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_11852
http://aims.fao.org/aos/agrovoc/c_4881
http://aims.fao.org/aos/agrovoc/c_1920
Hasselquist, Niles J.
Benegas, Laura
Roupsard, Olivier
Malmer, Anders
Ilstedt, Ulrik
Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
description Despite the widely held assumption that trees negatively affect the local water budget in densely planted tree plantations, we still lack a clear understanding of the underlying processes by which canopy cover influences local soil water dynamics in more open, humid tropical ecosystems. In this study, we propose a new conceptual model that uses a combination of stable isotope and soil moisture measurements throughout the soil profile to assess potential mechanisms by which evaporation (of surface soil water and of canopy‐intercepted rainfall) affects the relationship between surface soil water isotopic enrichment (lc‐excess) and soil water content. Our conceptual model was derived from soil water data collected under deciduous and evergreen plants in a shade grown coffee agroforestry system in Costa Rica. Reduced soil moisture under shade trees during the “drier” season, coinciding when these trees were defoliated, was largely the result of increase soil water evaporation as indicated by the positive relationship between soil water content and lc‐excess of surface soil water. In contrast, the evergreen coffee shrubs had a higher leaf area index during the “drier” season, leading to enhanced rainfall interception and a negative relationship between lc‐excess and soil water content. During the wet season, there was no clear relationship between soil water content and between lc‐excess of surface soil water. Greater surface soil water under coffee during the dry season may, in part, explain greater preferential flow under coffee compared with under trees in conditions of low rainfall intensities. However, with increasing rainfall intensities during the wet season, there was no obvious difference in preferential flow between the two canopy covers. Results from this study indicate that our new conceptual model can be used to help disentangling the relative influence of canopy cover on local soil water isotopic composition and dynamics, yet also stresses the need for additional measurements to better resolve the underlying processes by which canopy structure influences local water dynamics.
format article
topic_facet F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
U30 - Méthodes de recherche
agroforesterie
eau du sol
arbre d'ombrage
Coffea arabica
indice de végétation
variation saisonnière
isotope
modèle
http://aims.fao.org/aos/agrovoc/c_207
http://aims.fao.org/aos/agrovoc/c_7205
http://aims.fao.org/aos/agrovoc/c_25548
http://aims.fao.org/aos/agrovoc/c_1721
http://aims.fao.org/aos/agrovoc/c_9000171
http://aims.fao.org/aos/agrovoc/c_24894
http://aims.fao.org/aos/agrovoc/c_11852
http://aims.fao.org/aos/agrovoc/c_4881
http://aims.fao.org/aos/agrovoc/c_1920
author Hasselquist, Niles J.
Benegas, Laura
Roupsard, Olivier
Malmer, Anders
Ilstedt, Ulrik
author_facet Hasselquist, Niles J.
Benegas, Laura
Roupsard, Olivier
Malmer, Anders
Ilstedt, Ulrik
author_sort Hasselquist, Niles J.
title Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
title_short Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
title_full Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
title_fullStr Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
title_full_unstemmed Canopy cover effects on local soil water dynamics in a tropical agroforestry system: Evaporation drives soil water isotopic enrichment
title_sort canopy cover effects on local soil water dynamics in a tropical agroforestry system: evaporation drives soil water isotopic enrichment
publisher Wiley
url http://agritrop.cirad.fr/588137/
http://agritrop.cirad.fr/588137/1/Hasselquist_HP_2018%20Canopy%20cover%20effects%20on%20local%20soil%20water%20dynamics%20Evaporation%20drives%20soil%20water%20isotopic%20enrichment.pdf
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