Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought

The impacts of top down (precipitation) and bottom-up (groundwater rise) wetting processes on carbon sequestration are poorly understood. Here, the authors use incubation experiments to show that drought legacy and pore-scale wetting patterns are important factors controlling short-term carbon dynam...

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Autores principales:	A. Peyton Smith, Ben Bond-Lamberty, Brian W. Benscoter, Malak M. Tfaily, C. Ross Hinkle, Chongxuan Liu, Vanessa L. Bailey
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/0c3eed11783c4c499355f06cdef0cf59
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spelling	oai:doaj.org-article:0c3eed11783c4c499355f06cdef0cf592021-12-02T15:38:37ZShifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought10.1038/s41467-017-01320-x2041-1723https://doaj.org/article/0c3eed11783c4c499355f06cdef0cf592017-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-01320-xhttps://doaj.org/toc/2041-1723The impacts of top down (precipitation) and bottom-up (groundwater rise) wetting processes on carbon sequestration are poorly understood. Here, the authors use incubation experiments to show that drought legacy and pore-scale wetting patterns are important factors controlling short-term carbon dynamics.A. Peyton SmithBen Bond-LambertyBrian W. BenscoterMalak M. TfailyC. Ross HinkleChongxuan LiuVanessa L. BaileyNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-11 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q A. Peyton Smith Ben Bond-Lamberty Brian W. Benscoter Malak M. Tfaily C. Ross Hinkle Chongxuan Liu Vanessa L. Bailey Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
description	The impacts of top down (precipitation) and bottom-up (groundwater rise) wetting processes on carbon sequestration are poorly understood. Here, the authors use incubation experiments to show that drought legacy and pore-scale wetting patterns are important factors controlling short-term carbon dynamics.
format	article
author	A. Peyton Smith Ben Bond-Lamberty Brian W. Benscoter Malak M. Tfaily C. Ross Hinkle Chongxuan Liu Vanessa L. Bailey
author_facet	A. Peyton Smith Ben Bond-Lamberty Brian W. Benscoter Malak M. Tfaily C. Ross Hinkle Chongxuan Liu Vanessa L. Bailey
author_sort	A. Peyton Smith
title	Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
title_short	Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
title_full	Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
title_fullStr	Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
title_full_unstemmed	Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
title_sort	shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/0c3eed11783c4c499355f06cdef0cf59
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Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought

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