How does soil water status influence the fate of soil organic matter? A review of processes across scales

Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic carbon (SOC) dynamics. On all scales, water availability influences biological processes, such as plant growth and (micro-)biological activit...

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Published inEarth-science reviews Vol. 234; p. 104214
Main Authors Védère, Charlotte, Lebrun, Manhattan, Honvault, Nicolas, Aubertin, Marie-Liesse, Girardin, Cyril, Garnier, Patricia, Dignac, Marie-France, Houben, David, Rumpel, Cornelia
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.11.2022
Elsevier
Subjects
bioactive properties
biomass production
Carbon sequestration
Climate change
crops
drought
hydrologic cycle
irrigation
landscapes
Life Sciences
Modelling
Organic inputs
Organic matter dynamics
plant growth
porosity
soil aggregates
soil organic carbon
soil water
Soil water content
systematic review
uncertainty
vegetation types
wettability
Organic inputs
Climate change
Organic matter dynamics
Modelling
Soil water content
Carbon sequestration
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Abstract Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic carbon (SOC) dynamics. On all scales, water availability influences biological processes, such as plant growth and (micro-)biological activity, leading to organic matter input, its decomposition and stabilisation. On the other hand, SOC influences soil hydrology via its impact on soil wettability and its structural organisation. Our objectives were to review the mechanisms involved in the complex relationship between water and SOC at different scales and to discuss levers of action to improve its modelling and management. We carried out a systematic review and synthesised the information of 987 articles dealing with SOC sequestration and soil water. At the landscape scale, precipitation levels influence vegetation type and biomass production as well as horizontal and vertical transport, determining SOC stocks and their spatial distribution. At the profile scale, SOC and water both control biological processes including those involved in soil aggregate formation, and organisation of soil porosity. Soil organic matter (SOM) decomposition and stabilisation processes occur at the microscale, where water movement facilitates the co-occurrence of SOM and microorganisms. All these multiscale processes may change the nature and distribution of SOM, leading to promotion or inhibition not only of biogeochemical cycling but also of the water cycle. Taking into account these mutual feedback mechanisms in mechanistic models requires their representation at multiple scales through developing modelling parameters in particular for microbial processes occurring in the pore space. This could greatly reduce modelling uncertainty and improve our understanding of global carbon cycling. Levers of action to improve soil water status and consequently SOC accrual include irrigation, and use of organic amendments. Sustainable agricultural practices should focus on (1) optimising the management of water resources and (2) choosing crop species adapted to various water levels to maintain and foster SOC sequestration, to adapt to climate change and in particular extreme events, such as drought and flooding.
AbstractList Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic carbon (SOC) dynamics. On all scales, water availability influences biological processes, such as plant growth and (micro-)biological activity, leading to organic matter input, its decomposition and stabilisation. On the other hand, SOC influences soil hydrology via its impact on soil wettability and its structural organisation. Our objectives were to review the mechanisms involved in the complex relationship between water and SOC at different scales and to discuss levers of action to improve its modelling and management. We carried out a systematic review and synthesised the information of 987 articles dealing with SOC sequestration and soil water. At the landscape scale, precipitation levels influence vegetation type and biomass production as well as horizontal and vertical transport, determining SOC stocks and their spatial distribution. At the profile scale, SOC and water both control biological processes including those involved in soil aggregate formation, and organisation of soil porosity. Soil organic matter (SOM) decomposition and stabilisation processes occur at the microscale, where water movement facilitates the co-occurrence of SOM and microorganisms. All these multiscale processes may change the nature and distribution of SOM, leading to promotion or inhibition not only of biogeochemical cycling but also of the water cycle. Taking into account these mutual feedback mechanisms in mechanistic models requires their representation at multiple scales through developing modelling parameters in particular for microbial processes occurring in the pore space. This could greatly reduce modelling uncertainty and improve our understanding of global carbon cycling. Levers of action to improve soil water status and consequently SOC accrual include irrigation, and use of organic amendments. Sustainable agricultural practices should focus on (1) optimising the management of water resources and (2) choosing crop species adapted to various water levels to maintain and foster SOC sequestration, to adapt to climate change and in particular extreme events, such as drought and flooding.
Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic carbon (SOC) dynamics. On all scales, water availability influences biological processes, such as plant growth and (micro-)biological activity, leading to organic matter input, its decomposition and stabilisation. On the other hand, SOC influences soil hydrology via its impact on soil wettability and its structural organisation. Our objectives were to review the mechanisms involved in the complex relationship between water and SOC at different scales and to discuss levers of action to improve its modelling and management. We carried out a systematic review and synthesised the information of 987 articles dealing with SOC sequestration and soil water.At the landscape scale, precipitation levels influence vegetation type and biomass production as well as horizontal and vertical transport, determining SOC stocks and their spatial distribution. At the profile scale, SOC and water both control biological processes including those involved in soil aggregate formation, and organi-sation of soil porosity. Soil organic matter (SOM) decomposition and stabilisation processes occur at the microscale, where water movement facilitates the co-occurrence of SOM and microorganisms.All these multiscale processes may change the nature and distribution of SOM, leading to promotion or in-hibition not only of biogeochemical cycling but also of the water cycle. Taking into account these mutual feedback mechanisms in mechanistic models requires their representation at multiple scales through developing modelling parameters in particular for microbial processes occurring in the pore space. This could greatly reduce modelling uncertainty and improve our understanding of global carbon cycling.Levers of action to improve soil water status and consequently SOC accrual include irrigation, and use of organic amendments. Sustainable agricultural practices should focus on (1) optimising the management of water resources and (2) choosing crop species adapted to various water levels to maintain and foster SOC sequestration, to adapt to climate change and in particular extreme events, such as drought and flooding.
Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic carbon (SOC) dynamics. On all scales, water availability influences biological processes, such as plant growth and (micro-)biological activity, leading to organic matter input, its decomposition and stabilisation. On the other hand, SOC influences soil hydrology via its impact on soil wettability and its structural organisation. Our objectives were to review the mechanisms involved in the complex relationship between water and SOC at different scales and to discuss levers of action to improve its modelling and management. We carried out a systematic review and synthesised the information of 987 articles dealing with SOC sequestration and soil water. At the landscape scale, precipitation levels influence vegetation type and biomass production as well as horizontal and vertical transport, determining SOC stocks and their spatial distribution. At the profile scale, SOC and water both control biological processes including those involved in soil aggregate formation, and organisation of soil porosity. Soil organic matter (SOM) decomposition and stabilisation processes occur at the microscale, where water movement facilitates the co-occurrence of SOM and microorganisms. All these multiscale processes may change the nature and distribution of SOM, leading to promotion or inhibition not only of biogeochemical cycling but also of the water cycle. Taking into account these mutual feedback mechanisms in mechanistic models requires their representation at multiple scales through developing modelling parameters in particular for microbial processes occurring in the pore space. This could greatly reduce modelling uncertainty and improve our understanding of global carbon cycling. Levers of action to improve soil water status and consequently SOC accrual include irrigation, and use of organic amendments. Sustainable agricultural practices should focus on (1) optimising the management of water resources and (2) choosing crop species adapted to various water levels to maintain and foster SOC sequestration, to adapt to climate change and in particular extreme events, such as drought and flooding.
ArticleNumber 104214
Author Lebrun, Manhattan
Rumpel, Cornelia
Aubertin, Marie-Liesse
Garnier, Patricia
Girardin, Cyril
Honvault, Nicolas
Védère, Charlotte
Houben, David
Dignac, Marie-France
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  givenname: Manhattan
  surname: Lebrun
  fullname: Lebrun, Manhattan
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  organization: National Institute for Agricultural Research, Ecosys Soil, UMR INRAE-AgroParisTech, 78820 Thiverval-Grignon, France
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  givenname: Nicolas
  surname: Honvault
  fullname: Honvault, Nicolas
  email: nicolas.honvault@umontpellier.fr
  organization: Ecotron Européen de Montpellier, Univ Montpellier, CNRS, Montferrier sur Lez, France
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  surname: Aubertin
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  organization: National Institute for Agricultural Research, Ecosys Soil, UMR INRAE-AgroParisTech, 78820 Thiverval-Grignon, France
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  surname: Girardin
  fullname: Girardin, Cyril
  email: cyril.girardin@inrae.fr
  organization: National Institute for Agricultural Research, Ecosys Soil, UMR INRAE-AgroParisTech, 78820 Thiverval-Grignon, France
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  givenname: Patricia
  surname: Garnier
  fullname: Garnier, Patricia
  email: patricia.garnier@inrae.fr
  organization: National Institute for Agricultural Research, Ecosys Soil, UMR INRAE-AgroParisTech, 78820 Thiverval-Grignon, France
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  givenname: Marie-France
  surname: Dignac
  fullname: Dignac, Marie-France
  email: marie-france.dignac@inrae.fr
  organization: Institute of Ecology and Environmental Sciences, UMR 7618, CNRS-Sorbonne University-INRAE-UPEC-IRD, 75005 Paris, France
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  surname: Houben
  fullname: Houben, David
  email: david.houben@unilasalle.fr
  organization: UniLaSalle, AGHYLE, 60026 Beauvais, France
– sequence: 9
  givenname: Cornelia
  surname: Rumpel
  fullname: Rumpel, Cornelia
  email: cornelia.rumpel@inrae.fr
  organization: Institute of Ecology and Environmental Sciences, UMR 7618, CNRS-Sorbonne University-INRAE-UPEC-IRD, 75005 Paris, France
BackLink https://normandie-univ.hal.science/hal-03831825$$DView record in HAL
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Climate change
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Modelling
Soil water content
Carbon sequestration
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Snippet Due to its influence on multiple soil processes, water intervenes in biogeochemical cycles at multiple spatial scales with contrasting effects on soil organic...
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SubjectTerms bioactive properties
biomass production
Carbon sequestration
Climate change
crops
drought
hydrologic cycle
irrigation
landscapes
Life Sciences
Modelling
Organic inputs
Organic matter dynamics
plant growth
porosity
soil aggregates
soil organic carbon
soil water
Soil water content
systematic review
uncertainty
vegetation types
wettability
Title How does soil water status influence the fate of soil organic matter? A review of processes across scales
URI https://dx.doi.org/10.1016/j.earscirev.2022.104214
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https://normandie-univ.hal.science/hal-03831825
Volume 234
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