HAL (France)
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Effets des conditions micro-environnementales sur la minéralisation du carbone organique en milieux poreux
Les sols constituent le réservoir principal de carbone terrestre et jouent un rôle clé dans l'atténuation du changement climatique. Le devenir du carbone organique du sol dépend largement de l'activité des micro-organismes, qui transforment ce carbone organique en biomasse microbienne ou en CO₂. L'e
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