Organic carbon density and storage of the major black soil regions in Northeast China

Black soils in the Northeast Plain of China are characterized by high organic carbon (C) density and storage, which can influence C sequestration in local cropland ecosystems. Using GIS, this study analyzed the temporal and spatial distribution and variation of cropland organic C density and storage...

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Autores principales: Li,H, Pei,J.B, Wang,J.K, Li,S.Y, Gao,G.W
Lenguaje:English
Publicado: Chilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo 2013
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162013000400010
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spelling oai:scielo:S0718-951620130004000102014-01-29Organic carbon density and storage of the major black soil regions in Northeast ChinaLi,HPei,J.BWang,J.KLi,S.YGao,G.W Black soil organic carbon density and storage arable layer Northeast China Black soils in the Northeast Plain of China are characterized by high organic carbon (C) density and storage, which can influence C sequestration in local cropland ecosystems. Using GIS, this study analyzed the temporal and spatial distribution and variation of cropland organic C density and storage in the arable layer (0-20 cm) of the major black soil regions in China's Northeast Plain (specifically across the study region of Hailun, Shuangcheng and Gongzhuling counties) over the past 30 years. The results indicate an overall downward trend in soil organic C (SOC) density (SOCd, mean decrease of 0.64 kg m-2) and storage (SOCs, decrease of 4.65 Tg )*1 for the major black soil regions tested during the study period. The mean decrease in SOCd for Hailun, Shuangcheng and Gongzhuling counties was 0.68 kg m-2, 0.18 kg m-2 and 1.05 kg m-2, respectively, with total SOC decreases of 2.30 Tg, 0.49 Tg and 1.86 Tg, respectively. SOCd decreased to a greater extent during the first twenty years in Hailun and Shuangcheng relative to Gongzhuling. Moreover, SOCd tended to stabilize and then slightly increase during the last ten years. There was a downward trend in SOCd and SOCs over the past 30 years for almost all soil types, but the most serious decline in SOCs was observed in black soils, which account for 57.92% of the cropland soil area in all study regions and which lost up to 2.91 Tg of SOC. Therefore, the major black soil region in Northeast China was presenting a C resource trend over the past 20-30 years.info:eu-repo/semantics/openAccessChilean Society of Soil Science / Sociedad Chilena de la Ciencia del SueloJournal of soil science and plant nutrition v.13 n.4 20132013-12-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162013000400010en10.4067/S0718-95162013005000070
institution Scielo Chile
collection Scielo Chile
language English
topic Black soil
organic carbon density and storage
arable layer
Northeast China
spellingShingle Black soil
organic carbon density and storage
arable layer
Northeast China
Li,H
Pei,J.B
Wang,J.K
Li,S.Y
Gao,G.W
Organic carbon density and storage of the major black soil regions in Northeast China
description Black soils in the Northeast Plain of China are characterized by high organic carbon (C) density and storage, which can influence C sequestration in local cropland ecosystems. Using GIS, this study analyzed the temporal and spatial distribution and variation of cropland organic C density and storage in the arable layer (0-20 cm) of the major black soil regions in China's Northeast Plain (specifically across the study region of Hailun, Shuangcheng and Gongzhuling counties) over the past 30 years. The results indicate an overall downward trend in soil organic C (SOC) density (SOCd, mean decrease of 0.64 kg m-2) and storage (SOCs, decrease of 4.65 Tg )*1 for the major black soil regions tested during the study period. The mean decrease in SOCd for Hailun, Shuangcheng and Gongzhuling counties was 0.68 kg m-2, 0.18 kg m-2 and 1.05 kg m-2, respectively, with total SOC decreases of 2.30 Tg, 0.49 Tg and 1.86 Tg, respectively. SOCd decreased to a greater extent during the first twenty years in Hailun and Shuangcheng relative to Gongzhuling. Moreover, SOCd tended to stabilize and then slightly increase during the last ten years. There was a downward trend in SOCd and SOCs over the past 30 years for almost all soil types, but the most serious decline in SOCs was observed in black soils, which account for 57.92% of the cropland soil area in all study regions and which lost up to 2.91 Tg of SOC. Therefore, the major black soil region in Northeast China was presenting a C resource trend over the past 20-30 years.
author Li,H
Pei,J.B
Wang,J.K
Li,S.Y
Gao,G.W
author_facet Li,H
Pei,J.B
Wang,J.K
Li,S.Y
Gao,G.W
author_sort Li,H
title Organic carbon density and storage of the major black soil regions in Northeast China
title_short Organic carbon density and storage of the major black soil regions in Northeast China
title_full Organic carbon density and storage of the major black soil regions in Northeast China
title_fullStr Organic carbon density and storage of the major black soil regions in Northeast China
title_full_unstemmed Organic carbon density and storage of the major black soil regions in Northeast China
title_sort organic carbon density and storage of the major black soil regions in northeast china
publisher Chilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo
publishDate 2013
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162013000400010
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