How does grazing affect soil water availability in the Patagonian steppe?

In the Patagonian steppe, grazing may or may not reduce soil water availability: it may increase evaporative losses, because it reduces plant cover, but may decrease transpiration losses because it decreases plant biomass. Therefore, grazing could reduce soil water availability in the superficial la...

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Autores principales: Golluscio, Rodolfo Ángel, Garcia Martinez, Guillermo Carlos, Cavagnaro, Fernando Pablo
Formato: Artículo
Lenguaje:Inglés
Publicado: Elsevier 2022
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12123/12021
https://www.sciencedirect.com/science/article/pii/S0140196322000957
https://doi.org/10.1016/j.jaridenv.2022.104800
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author Golluscio, Rodolfo Ángel
Garcia Martinez, Guillermo Carlos
Cavagnaro, Fernando Pablo
author_browse Cavagnaro, Fernando Pablo
Garcia Martinez, Guillermo Carlos
Golluscio, Rodolfo Ángel
author_facet Golluscio, Rodolfo Ángel
Garcia Martinez, Guillermo Carlos
Cavagnaro, Fernando Pablo
author_sort Golluscio, Rodolfo Ángel
collection INTA Digital
description In the Patagonian steppe, grazing may or may not reduce soil water availability: it may increase evaporative losses, because it reduces plant cover, but may decrease transpiration losses because it decreases plant biomass. Therefore, grazing could reduce soil water availability in the superficial layer, mostly affected by evaporation, but could increase it in the subsurface layers, mostly affected by transpiration. Our hypothesis is that such effects would be most evident in the bare soil spaces, with higher evaporative losses and lower root density than vegetated microsites. Therefore, we analyzed the proportion of four microsites (shrubs, bare soil, preferred- and unpreferred grasses), and their soil water availability at 0–5 and 5–15 cm depth in four sampling areas, each one with an ungrazed, a moderately- and an intensely-grazed site. Our results supported the initial hypothesis: bare soil microsites had the lowest surface, but the highest subsurface water availability. However, grazing did not cause any change in the mean soil water availability (net effect) because it did not affect soil water availability in any microsite and depth (direct effects), and only caused a replacement of preferred-by unpreferred grasses (indirect effects), two groups that induced small differences in water availability.
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language Inglés
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spelling INTA120212022-06-06T11:01:38Z How does grazing affect soil water availability in the Patagonian steppe? Golluscio, Rodolfo Ángel Garcia Martinez, Guillermo Carlos Cavagnaro, Fernando Pablo Desertificación Pastoreo Evaporación Transpiración Disponibilidad del Agua Características del Sitio Estepas Desertification Grazing Evaporation Transpiration Water Availability Site Factors Steppes Región Patagónica In the Patagonian steppe, grazing may or may not reduce soil water availability: it may increase evaporative losses, because it reduces plant cover, but may decrease transpiration losses because it decreases plant biomass. Therefore, grazing could reduce soil water availability in the superficial layer, mostly affected by evaporation, but could increase it in the subsurface layers, mostly affected by transpiration. Our hypothesis is that such effects would be most evident in the bare soil spaces, with higher evaporative losses and lower root density than vegetated microsites. Therefore, we analyzed the proportion of four microsites (shrubs, bare soil, preferred- and unpreferred grasses), and their soil water availability at 0–5 and 5–15 cm depth in four sampling areas, each one with an ungrazed, a moderately- and an intensely-grazed site. Our results supported the initial hypothesis: bare soil microsites had the lowest surface, but the highest subsurface water availability. However, grazing did not cause any change in the mean soil water availability (net effect) because it did not affect soil water availability in any microsite and depth (direct effects), and only caused a replacement of preferred-by unpreferred grasses (indirect effects), two groups that induced small differences in water availability. EEA Esquel Fil: Golluscio, Rodolfo Ángel. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Forrajicultura; Argentina Fil: Golluscio, Rodolfo Ángel. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Golluscio, Rodolfo Ángel. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a La Agricultura (IFEVA); Argentina Fil: García Martínez, Guillermo Carlos. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agroforestal Esquel; Argentina Fil: Cavagnaro, Fernando Pablo. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Forrajicultura; Argentina 2022-06-06T10:56:14Z 2022-06-06T10:56:14Z 2022-06-01 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/12021 https://www.sciencedirect.com/science/article/pii/S0140196322000957 0140-1963 https://doi.org/10.1016/j.jaridenv.2022.104800 eng info:eu-repo/semantics/restrictedAccess application/pdf Elsevier Journal of Arid Environments 205 : 104800. (October 2022)
spellingShingle Desertificación
Pastoreo
Evaporación
Transpiración
Disponibilidad del Agua
Características del Sitio
Estepas
Desertification
Grazing
Evaporation
Transpiration
Water Availability
Site Factors
Steppes
Región Patagónica
Golluscio, Rodolfo Ángel
Garcia Martinez, Guillermo Carlos
Cavagnaro, Fernando Pablo
How does grazing affect soil water availability in the Patagonian steppe?
title How does grazing affect soil water availability in the Patagonian steppe?
title_full How does grazing affect soil water availability in the Patagonian steppe?
title_fullStr How does grazing affect soil water availability in the Patagonian steppe?
title_full_unstemmed How does grazing affect soil water availability in the Patagonian steppe?
title_short How does grazing affect soil water availability in the Patagonian steppe?
title_sort how does grazing affect soil water availability in the patagonian steppe
topic Desertificación
Pastoreo
Evaporación
Transpiración
Disponibilidad del Agua
Características del Sitio
Estepas
Desertification
Grazing
Evaporation
Transpiration
Water Availability
Site Factors
Steppes
Región Patagónica
url http://hdl.handle.net/20.500.12123/12021
https://www.sciencedirect.com/science/article/pii/S0140196322000957
https://doi.org/10.1016/j.jaridenv.2022.104800
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