4.7 Article

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

Journal

EARTH-SCIENCE REVIEWS
Volume 234, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.earscirev.2022.104214

Keywords

Carbon sequestration; Organic matter dynamics; Soil water content; Organic inputs; Modelling; Climate change

Funding

  1. ANR PRIMA project CHANGEUP [ANR-21-PRIM-0005]
  2. FUI project [BIOCHAR21]
  3. Agence Nationale de la Recherche (ANR) [ANR-21-PRIM-0005] Funding Source: Agence Nationale de la Recherche (ANR)

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Water has complex effects on soil organic carbon dynamics, influencing biological processes and soil hydrology at different spatial scales. Understanding the mechanisms involved in the relationship between water and SOC is important for modeling and managing soil resources.
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.

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