Ten-year long-term organic fertilization enhances carbon sequestration and calcium-mediated stabilization of aggregate-associated organic carbon in a reclaimed Cambisol

Soils play a vital role in the global carbon (C) cycle, yet little is known about the calcium (Ca)-mediated stabilization of soil organic carbon (SOC) in calcareous soils. With wet sieving, density fractionation and an incubation experiment from field soils, we investigated the effects of long-term...

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Published inGeoderma Vol. 355; p. 113880
Main Authors Huang, Xiaolei, Jia, Zhixin, Guo, Junjie, Li, Tingliang, Sun, Dasheng, Meng, Huisheng, Yu, Guanghui, He, Xinhua, Ran, Wei, Zhang, Shusheng, Hong, Jianping, Shen, Qirong
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.12.2019
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Abstract Soils play a vital role in the global carbon (C) cycle, yet little is known about the calcium (Ca)-mediated stabilization of soil organic carbon (SOC) in calcareous soils. With wet sieving, density fractionation and an incubation experiment from field soils, we investigated the effects of long-term fertilization on the Ca-mediated stabilization of aggregate-associated organic C and on the SOC stock at a soil depth of 0–20 cm in a reclaimed Cambisol on the Loess Plateau of China. Compared to the initial soil, after ten years the SOC stock increased by 50%, 76%, 94% and 110% in soils amended with no fertilizer (control), 100% chemical fertilizer, 50% chemical fertilizer plus 50% chicken manure compost and 100% chicken manure compost, respectively. The specific C mineralization rate (SCMR, rate per unit SOC) decreased as silt and clay > macroaggregate > microaggregate, indicating that SOC in microaggregates was more stable than in macroaggregates and the silt and clay fraction. The exchangeable Ca in the bulk soil (P < 0.001) and soil aggregates (P < 0.001) were positively correlated with the SOC, whereas the Ca carbonate (CaCO3) was negatively correlated with the SCMR (P < 0.001). The application of compost not only increased the exogenous C inputs but also promoted the transformation of CaCO3 to exchangeable Ca compared with the sole chemical fertilization. Furthermore, organic fertilization significantly increased the organic C in the heavy fraction (> 2.0 g cm−3) compared with the sole chemical fertilization, which was positively correlated with the mass proportion of macroaggregates (P < 0.001). These results indicate that organic fertilization can enhance the availability of Ca for C binding possibly by forming organo-Ca complexes, which in turn improve soil aggregation, and thus contribute to a long-term SOC sequestration in reclaimed soils of the Loess Plateau of China. •Exchangeable Ca was positively correlated with soil organic carbon (C).•CaCO3 was negatively correlated with the specific C mineralization rate.•Organic C in microaggregates was relatively stable.•The formation of organo-Ca complexes improved soil aggregation.•Organic fertilization promoted soil aggregation and enhanced C sequestration.
AbstractList Soils play a vital role in the global carbon (C) cycle, yet little is known about the calcium (Ca)-mediated stabilization of soil organic carbon (SOC) in calcareous soils. With wet sieving, density fractionation and an incubation experiment from field soils, we investigated the effects of long-term fertilization on the Ca-mediated stabilization of aggregate-associated organic C and on the SOC stock at a soil depth of 0–20 cm in a reclaimed Cambisol on the Loess Plateau of China. Compared to the initial soil, after ten years the SOC stock increased by 50%, 76%, 94% and 110% in soils amended with no fertilizer (control), 100% chemical fertilizer, 50% chemical fertilizer plus 50% chicken manure compost and 100% chicken manure compost, respectively. The specific C mineralization rate (SCMR, rate per unit SOC) decreased as silt and clay > macroaggregate > microaggregate, indicating that SOC in microaggregates was more stable than in macroaggregates and the silt and clay fraction. The exchangeable Ca in the bulk soil (P < 0.001) and soil aggregates (P < 0.001) were positively correlated with the SOC, whereas the Ca carbonate (CaCO3) was negatively correlated with the SCMR (P < 0.001). The application of compost not only increased the exogenous C inputs but also promoted the transformation of CaCO3 to exchangeable Ca compared with the sole chemical fertilization. Furthermore, organic fertilization significantly increased the organic C in the heavy fraction (> 2.0 g cm−3) compared with the sole chemical fertilization, which was positively correlated with the mass proportion of macroaggregates (P < 0.001). These results indicate that organic fertilization can enhance the availability of Ca for C binding possibly by forming organo-Ca complexes, which in turn improve soil aggregation, and thus contribute to a long-term SOC sequestration in reclaimed soils of the Loess Plateau of China. •Exchangeable Ca was positively correlated with soil organic carbon (C).•CaCO3 was negatively correlated with the specific C mineralization rate.•Organic C in microaggregates was relatively stable.•The formation of organo-Ca complexes improved soil aggregation.•Organic fertilization promoted soil aggregation and enhanced C sequestration.
Soils play a vital role in the global carbon (C) cycle, yet little is known about the calcium (Ca)-mediated stabilization of soil organic carbon (SOC) in calcareous soils. With wet sieving, density fractionation and an incubation experiment from field soils, we investigated the effects of long-term fertilization on the Ca-mediated stabilization of aggregate-associated organic C and on the SOC stock at a soil depth of 0–20 cm in a reclaimed Cambisol on the Loess Plateau of China. Compared to the initial soil, after ten years the SOC stock increased by 50%, 76%, 94% and 110% in soils amended with no fertilizer (control), 100% chemical fertilizer, 50% chemical fertilizer plus 50% chicken manure compost and 100% chicken manure compost, respectively. The specific C mineralization rate (SCMR, rate per unit SOC) decreased as silt and clay > macroaggregate > microaggregate, indicating that SOC in microaggregates was more stable than in macroaggregates and the silt and clay fraction. The exchangeable Ca in the bulk soil (P < 0.001) and soil aggregates (P < 0.001) were positively correlated with the SOC, whereas the Ca carbonate (CaCO3) was negatively correlated with the SCMR (P < 0.001). The application of compost not only increased the exogenous C inputs but also promoted the transformation of CaCO3 to exchangeable Ca compared with the sole chemical fertilization. Furthermore, organic fertilization significantly increased the organic C in the heavy fraction (> 2.0 g cm−3) compared with the sole chemical fertilization, which was positively correlated with the mass proportion of macroaggregates (P < 0.001). These results indicate that organic fertilization can enhance the availability of Ca for C binding possibly by forming organo-Ca complexes, which in turn improve soil aggregation, and thus contribute to a long-term SOC sequestration in reclaimed soils of the Loess Plateau of China.
ArticleNumber 113880
Author He, Xinhua
Shen, Qirong
Sun, Dasheng
Ran, Wei
Yu, Guanghui
Zhang, Shusheng
Hong, Jianping
Huang, Xiaolei
Guo, Junjie
Jia, Zhixin
Li, Tingliang
Meng, Huisheng
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  fullname: Jia, Zhixin
  organization: College of Resources and Environment, Shanxi Agricultural University, Taigu, Shanxi 080301, China
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  givenname: Junjie
  surname: Guo
  fullname: Guo, Junjie
  organization: Jiangsu Provincial Key Lab for Organic Solid Waste Utilization, National Engineering Research Center for Organic-based Fertilizers, Jiangsu Collaborative Innovation Center for Solid Organic Waster Resource Utilization, Nanjing Agricultural University, Nanjing 210095, China
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  givenname: Tingliang
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  organization: College of Resources and Environment, Shanxi Agricultural University, Taigu, Shanxi 080301, China
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  organization: College of Resources and Environment, Shanxi Agricultural University, Taigu, Shanxi 080301, China
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  surname: Yu
  fullname: Yu, Guanghui
  organization: Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
– sequence: 8
  givenname: Xinhua
  surname: He
  fullname: He, Xinhua
  organization: College of Resources and Environment, Southwest University, Beibei, Chongqing 400715, China
– sequence: 9
  givenname: Wei
  surname: Ran
  fullname: Ran, Wei
  email: ranwei@njau.edu.cn
  organization: Jiangsu Provincial Key Lab for Organic Solid Waste Utilization, National Engineering Research Center for Organic-based Fertilizers, Jiangsu Collaborative Innovation Center for Solid Organic Waster Resource Utilization, Nanjing Agricultural University, Nanjing 210095, China
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  givenname: Shusheng
  surname: Zhang
  fullname: Zhang, Shusheng
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  surname: Hong
  fullname: Hong, Jianping
  organization: College of Resources and Environment, Shanxi Agricultural University, Taigu, Shanxi 080301, China
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  givenname: Qirong
  surname: Shen
  fullname: Shen, Qirong
  organization: Jiangsu Provincial Key Lab for Organic Solid Waste Utilization, National Engineering Research Center for Organic-based Fertilizers, Jiangsu Collaborative Innovation Center for Solid Organic Waster Resource Utilization, Nanjing Agricultural University, Nanjing 210095, China
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Keywords Specific carbon mineralization rate
CaCO3
Carbon sequestration
Calcaric Cambisol
Microaggregates
Macroaggregates
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Snippet Soils play a vital role in the global carbon (C) cycle, yet little is known about the calcium (Ca)-mediated stabilization of soil organic carbon (SOC) in...
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StartPage 113880
SubjectTerms CaCO3
calcareous soils
Calcaric Cambisol
calcium
calcium carbonate
Cambisols
Carbon sequestration
China
clay
clay fraction
composted manure
exchangeable calcium
fertilizer application
fractionation
long term experiments
Macroaggregates
Microaggregates
mineral fertilizers
mineralization
poultry manure
reclaimed soils
sieving
silt
soil aggregation
soil amendments
soil depth
soil organic carbon
Specific carbon mineralization rate
Title Ten-year long-term organic fertilization enhances carbon sequestration and calcium-mediated stabilization of aggregate-associated organic carbon in a reclaimed Cambisol
URI https://dx.doi.org/10.1016/j.geoderma.2019.113880
https://www.proquest.com/docview/2305157669
Volume 355
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