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Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China

Studying the responses of soil respiration (R (s)) to soil management changes is critical for enhancing our understanding of the global carbon cycle and has practical implications for grassland management. Therefore, the objectives of this study were (1) quantify daily and seasonal patterns of R (s)...

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Autores principales: Xue, Haili, Tang, Haiping
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5756883/
https://www.ncbi.nlm.nih.gov/pubmed/29321865
http://dx.doi.org/10.1002/ece3.3659
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author Xue, Haili
Tang, Haiping
author_facet Xue, Haili
Tang, Haiping
author_sort Xue, Haili
collection PubMed
description Studying the responses of soil respiration (R (s)) to soil management changes is critical for enhancing our understanding of the global carbon cycle and has practical implications for grassland management. Therefore, the objectives of this study were (1) quantify daily and seasonal patterns of R (s), (2) evaluate the influence of abiotic factors on R (s), and (3) detect the effects of soil management changes on R (s). We hypothesized that (1) most of daily and seasonal variation in R (s) could be explained by soil temperature (T (s)) and soil water content (S (w)), (2) soil management changes could significantly affect R (s), and (3) soil management changes affected R (s) via the significant change in abiotic and biotic factors. In situ R (s) values were monitored in an agropastoral ecotone in Inner Mongolia, China, during the growing seasons in 2009 (August to October) and 2010 (May to October). The soil management changes sequences included free grazing grassland (FG), cropland (CL), grazing enclosure grassland (GE), and abandoned cultivated grassland (AC). During the growing season in 2010, cumulative R (s) for FG, CL, GE, and AC averaged 265.97, 344.74, 236.70, and 226.42 gC m(−2) year(−1), respectively. The T (s) and S (w) significantly influenced R (s) and explained 66%–86% of the variability in daily R (s). Monthly mean temperature and precipitation explained 78%–96% of the variability in monthly R (s). The results clearly showed that R (s) was increased by 29% with the conversion of FG to CL and decreased by 35% and 11% with the conversion of CL to AC and FG to GE. The factors impacting the change in R (s) under different soil management changes sequences varied. Our results confirm the tested hypotheses. The increase in Q (10) and litter biomass induced by conversion of FG to GE could lead to increased R (s) if the climate warming. We suggest that after proper natural restoration period, grasslands should be utilized properly to decrease R (s).
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spelling pubmed-57568832018-01-10 Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China Xue, Haili Tang, Haiping Ecol Evol Original Research Studying the responses of soil respiration (R (s)) to soil management changes is critical for enhancing our understanding of the global carbon cycle and has practical implications for grassland management. Therefore, the objectives of this study were (1) quantify daily and seasonal patterns of R (s), (2) evaluate the influence of abiotic factors on R (s), and (3) detect the effects of soil management changes on R (s). We hypothesized that (1) most of daily and seasonal variation in R (s) could be explained by soil temperature (T (s)) and soil water content (S (w)), (2) soil management changes could significantly affect R (s), and (3) soil management changes affected R (s) via the significant change in abiotic and biotic factors. In situ R (s) values were monitored in an agropastoral ecotone in Inner Mongolia, China, during the growing seasons in 2009 (August to October) and 2010 (May to October). The soil management changes sequences included free grazing grassland (FG), cropland (CL), grazing enclosure grassland (GE), and abandoned cultivated grassland (AC). During the growing season in 2010, cumulative R (s) for FG, CL, GE, and AC averaged 265.97, 344.74, 236.70, and 226.42 gC m(−2) year(−1), respectively. The T (s) and S (w) significantly influenced R (s) and explained 66%–86% of the variability in daily R (s). Monthly mean temperature and precipitation explained 78%–96% of the variability in monthly R (s). The results clearly showed that R (s) was increased by 29% with the conversion of FG to CL and decreased by 35% and 11% with the conversion of CL to AC and FG to GE. The factors impacting the change in R (s) under different soil management changes sequences varied. Our results confirm the tested hypotheses. The increase in Q (10) and litter biomass induced by conversion of FG to GE could lead to increased R (s) if the climate warming. We suggest that after proper natural restoration period, grasslands should be utilized properly to decrease R (s). John Wiley and Sons Inc. 2017-11-26 /pmc/articles/PMC5756883/ /pubmed/29321865 http://dx.doi.org/10.1002/ece3.3659 Text en © 2017 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution (http://creativecommons.org/licenses/by/4.0/) License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
spellingShingle Original Research
Xue, Haili
Tang, Haiping
Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title_full Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title_fullStr Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title_full_unstemmed Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title_short Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia, China
title_sort responses of soil respiration to soil management changes in an agropastoral ecotone in inner mongolia, china
topic Original Research
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5756883/
https://www.ncbi.nlm.nih.gov/pubmed/29321865
http://dx.doi.org/10.1002/ece3.3659
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