Soil inorganic carbon storage pattern in China

Autores
Mi, Na; Wang, Shaoqiang; Liu, Jiyuan; Yu, Guirui; Zhang, Wenjuan; Jobbagy Gampel, Esteban Gabriel
Año de publicación
2008
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Soils with pedogenic carbonate cover about 30% (3.44 × 106 km2) of China, mainly across its arid and semiarid regions in the Northwest. Based on the second national soil survey (1979–1992), total soil inorganic carbon (SIC) storage in China was estimated to be 53.3±6.3 PgC (1 Pg=1015 g) to the depth investigated to 2 m. Soil inorganic carbon storages were 4.6, 10.6, 11.1, and 20.8 Pg for the depth ranges of 0–0.1, 0.1–0.3, 0.3–0.5, and 0.5–1 m, respectively. Stocks for 0.1, 0.3, 0.5, and 1 m of depth accounted for 8.7%, 28.7%, 49.6%, and 88.9% of total SIC, respectively. In contrast with soil organic carbon (SOC) storage, which is highest under 500–800 mm yr−1 of mean precipitation, SIC storage peaks where mean precipitation is <400 mm yr−1. The amount and vertical distribution of SIC was related to climate and land cover type. Content of SIC in each incremental horizon was positively related with mean annual temperature and negatively related with mean annual precipitation, with the magnitude of SIC content across land cover types showing the following order: desert, grassland >shrubland, cropland >marsh, forest, meadow. Densities of SIC increased generally with depth in all ecosystem types with the exception of deserts and marshes where it peaked in intermediate layers (0.1–0.3 m for first and 0.3–0.5 m for latter). Being an abundant component of soil carbon stocks in China, SIC dynamics and the process involved in its accumulation or loss from soils require a better understanding.
Fil: Mi, Na. Institute of Geographic Sciences and Natural Resources; China
Fil: Wang, Shaoqiang. Institute of Geographic Sciences and Natural Resources; China
Fil: Liu, Jiyuan. Institute of Geographic Sciences and Natural Resources; China
Fil: Yu, Guirui. Institute of Geographic Sciences and Natural Resources; China
Fil: Zhang, Wenjuan. Institute of Geographic Sciences and Natural Resources; China
Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; Argentina
Materia
CARBON CYCLE
CARBON STORAGE
LAND COVER
SOIL INORGANIC CARBON
VERTICAL DISTRIBUTION
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/135137
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/135137
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Soil inorganic carbon storage pattern in ChinaMi, NaWang, ShaoqiangLiu, JiyuanYu, GuiruiZhang, WenjuanJobbagy Gampel, Esteban GabrielCARBON CYCLECARBON STORAGELAND COVERSOIL INORGANIC CARBONVERTICAL DISTRIBUTIONhttps://purl.org/becyt/ford/4.1https://purl.org/becyt/ford/4Soils with pedogenic carbonate cover about 30% (3.44 × 106 km2) of China, mainly across its arid and semiarid regions in the Northwest. Based on the second national soil survey (1979–1992), total soil inorganic carbon (SIC) storage in China was estimated to be 53.3±6.3 PgC (1 Pg=1015 g) to the depth investigated to 2 m. Soil inorganic carbon storages were 4.6, 10.6, 11.1, and 20.8 Pg for the depth ranges of 0–0.1, 0.1–0.3, 0.3–0.5, and 0.5–1 m, respectively. Stocks for 0.1, 0.3, 0.5, and 1 m of depth accounted for 8.7%, 28.7%, 49.6%, and 88.9% of total SIC, respectively. In contrast with soil organic carbon (SOC) storage, which is highest under 500–800 mm yr−1 of mean precipitation, SIC storage peaks where mean precipitation is <400 mm yr−1. The amount and vertical distribution of SIC was related to climate and land cover type. Content of SIC in each incremental horizon was positively related with mean annual temperature and negatively related with mean annual precipitation, with the magnitude of SIC content across land cover types showing the following order: desert, grassland >shrubland, cropland >marsh, forest, meadow. Densities of SIC increased generally with depth in all ecosystem types with the exception of deserts and marshes where it peaked in intermediate layers (0.1–0.3 m for first and 0.3–0.5 m for latter). Being an abundant component of soil carbon stocks in China, SIC dynamics and the process involved in its accumulation or loss from soils require a better understanding.Fil: Mi, Na. Institute of Geographic Sciences and Natural Resources; ChinaFil: Wang, Shaoqiang. Institute of Geographic Sciences and Natural Resources; ChinaFil: Liu, Jiyuan. Institute of Geographic Sciences and Natural Resources; ChinaFil: Yu, Guirui. Institute of Geographic Sciences and Natural Resources; ChinaFil: Zhang, Wenjuan. Institute of Geographic Sciences and Natural Resources; ChinaFil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; ArgentinaWiley Blackwell Publishing, Inc2008-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/mswordapplication/pdfhttp://hdl.handle.net/11336/135137Mi, Na; Wang, Shaoqiang; Liu, Jiyuan; Yu, Guirui; Zhang, Wenjuan; et al.; Soil inorganic carbon storage pattern in China; Wiley Blackwell Publishing, Inc; Global Change Biology; 14; 10; 9-2008; 2380-23871354-1013CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1365-2486.2008.01642.xinfo:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-2486.2008.01642.xinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:03:40Zoai:ri.conicet.gov.ar:11336/135137instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:03:40.39CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Soil inorganic carbon storage pattern in China
title Soil inorganic carbon storage pattern in China
spellingShingle Soil inorganic carbon storage pattern in China
Mi, Na
CARBON CYCLE
CARBON STORAGE
LAND COVER
SOIL INORGANIC CARBON
VERTICAL DISTRIBUTION
title_short Soil inorganic carbon storage pattern in China
title_full Soil inorganic carbon storage pattern in China
title_fullStr Soil inorganic carbon storage pattern in China
title_full_unstemmed Soil inorganic carbon storage pattern in China
title_sort Soil inorganic carbon storage pattern in China
dc.creator.none.fl_str_mv Mi, Na
Wang, Shaoqiang
Liu, Jiyuan
Yu, Guirui
Zhang, Wenjuan
Jobbagy Gampel, Esteban Gabriel
author Mi, Na
author_facet Mi, Na
Wang, Shaoqiang
Liu, Jiyuan
Yu, Guirui
Zhang, Wenjuan
Jobbagy Gampel, Esteban Gabriel
author_role author
author2 Wang, Shaoqiang
Liu, Jiyuan
Yu, Guirui
Zhang, Wenjuan
Jobbagy Gampel, Esteban Gabriel
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv CARBON CYCLE
CARBON STORAGE
LAND COVER
SOIL INORGANIC CARBON
VERTICAL DISTRIBUTION
topic CARBON CYCLE
CARBON STORAGE
LAND COVER
SOIL INORGANIC CARBON
VERTICAL DISTRIBUTION
purl_subject.fl_str_mv https://purl.org/becyt/ford/4.1
https://purl.org/becyt/ford/4
dc.description.none.fl_txt_mv Soils with pedogenic carbonate cover about 30% (3.44 × 106 km2) of China, mainly across its arid and semiarid regions in the Northwest. Based on the second national soil survey (1979–1992), total soil inorganic carbon (SIC) storage in China was estimated to be 53.3±6.3 PgC (1 Pg=1015 g) to the depth investigated to 2 m. Soil inorganic carbon storages were 4.6, 10.6, 11.1, and 20.8 Pg for the depth ranges of 0–0.1, 0.1–0.3, 0.3–0.5, and 0.5–1 m, respectively. Stocks for 0.1, 0.3, 0.5, and 1 m of depth accounted for 8.7%, 28.7%, 49.6%, and 88.9% of total SIC, respectively. In contrast with soil organic carbon (SOC) storage, which is highest under 500–800 mm yr−1 of mean precipitation, SIC storage peaks where mean precipitation is <400 mm yr−1. The amount and vertical distribution of SIC was related to climate and land cover type. Content of SIC in each incremental horizon was positively related with mean annual temperature and negatively related with mean annual precipitation, with the magnitude of SIC content across land cover types showing the following order: desert, grassland >shrubland, cropland >marsh, forest, meadow. Densities of SIC increased generally with depth in all ecosystem types with the exception of deserts and marshes where it peaked in intermediate layers (0.1–0.3 m for first and 0.3–0.5 m for latter). Being an abundant component of soil carbon stocks in China, SIC dynamics and the process involved in its accumulation or loss from soils require a better understanding.
Fil: Mi, Na. Institute of Geographic Sciences and Natural Resources; China
Fil: Wang, Shaoqiang. Institute of Geographic Sciences and Natural Resources; China
Fil: Liu, Jiyuan. Institute of Geographic Sciences and Natural Resources; China
Fil: Yu, Guirui. Institute of Geographic Sciences and Natural Resources; China
Fil: Zhang, Wenjuan. Institute of Geographic Sciences and Natural Resources; China
Fil: Jobbagy Gampel, Esteban Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Luis. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi". Universidad Nacional de San Luis. Facultad de Ciencias Físico, Matemáticas y Naturales. Instituto de Matemática Aplicada de San Luis "Prof. Ezio Marchi"; Argentina
description Soils with pedogenic carbonate cover about 30% (3.44 × 106 km2) of China, mainly across its arid and semiarid regions in the Northwest. Based on the second national soil survey (1979–1992), total soil inorganic carbon (SIC) storage in China was estimated to be 53.3±6.3 PgC (1 Pg=1015 g) to the depth investigated to 2 m. Soil inorganic carbon storages were 4.6, 10.6, 11.1, and 20.8 Pg for the depth ranges of 0–0.1, 0.1–0.3, 0.3–0.5, and 0.5–1 m, respectively. Stocks for 0.1, 0.3, 0.5, and 1 m of depth accounted for 8.7%, 28.7%, 49.6%, and 88.9% of total SIC, respectively. In contrast with soil organic carbon (SOC) storage, which is highest under 500–800 mm yr−1 of mean precipitation, SIC storage peaks where mean precipitation is <400 mm yr−1. The amount and vertical distribution of SIC was related to climate and land cover type. Content of SIC in each incremental horizon was positively related with mean annual temperature and negatively related with mean annual precipitation, with the magnitude of SIC content across land cover types showing the following order: desert, grassland >shrubland, cropland >marsh, forest, meadow. Densities of SIC increased generally with depth in all ecosystem types with the exception of deserts and marshes where it peaked in intermediate layers (0.1–0.3 m for first and 0.3–0.5 m for latter). Being an abundant component of soil carbon stocks in China, SIC dynamics and the process involved in its accumulation or loss from soils require a better understanding.
publishDate 2008
dc.date.none.fl_str_mv 2008-09
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/135137
Mi, Na; Wang, Shaoqiang; Liu, Jiyuan; Yu, Guirui; Zhang, Wenjuan; et al.; Soil inorganic carbon storage pattern in China; Wiley Blackwell Publishing, Inc; Global Change Biology; 14; 10; 9-2008; 2380-2387
1354-1013
CONICET Digital
CONICET
url http://hdl.handle.net/11336/135137
identifier_str_mv Mi, Na; Wang, Shaoqiang; Liu, Jiyuan; Yu, Guirui; Zhang, Wenjuan; et al.; Soil inorganic carbon storage pattern in China; Wiley Blackwell Publishing, Inc; Global Change Biology; 14; 10; 9-2008; 2380-2387
1354-1013
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1365-2486.2008.01642.x
info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-2486.2008.01642.x
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/msword
application/pdf
dc.publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.13397

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