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|dc.identifier.citation||Journal of Hazardous Materials, 2019; 374:11-19||-|
|dc.description.abstract||The interactive effects of the types and contents of soil clay fractions (SCFs) and plant-residue addition rates on soil organic carbon (SOC) stabilisation are largely unknown. We conducted incubation experiments by amending a sandy soil sample with kaolinitic-illitic, smectitic and allophanic SCFs and adding wheat residues to the mineral mixtures to compare their C stabilisation capacity. The rate of carbon (C) decomposition was higher in the kaolinitic-illitic SCF followed by smectitic and allophanic clay minerals. The supply of easily degradable C substrate from decomposing residues markedly influenced the SCFs' abilities to stabilise SOC. The removal of sesquioxides from the SCFs significantly decreased their C stabilisation capacity, which coincided with a decrease in the dehydrogenase activity of the mineral-residue mixture. The allophanic SCF showed the least microbial activity and the greatest C stabilisation due to having a higher proportion of micropores (75%). The high C stabilisation capacity of allophanic SCF could also be explained by its high specific surface area (119 m2 g-1). The results of this study are helpful to understand the role of various SCFs in stabilising added C originating from external wheat residue addition but warrant further validation under field conditions.||-|
|dc.description.statementofresponsibility||Mandeep Singh, Binoy Sarkar, Nanthi S.Bolan, Yong Sik Ok, Gordon Jock Churchman||-|
|dc.rights||© 2019 Elsevier B.V. All rights reserved.||-|
|dc.subject||Organic carbon stabilisation||-|
|dc.subject||Soil clay fractions||-|
|dc.subject||Wheat plant residue||-|
|dc.title||Decomposition of soil organic matter as affected by clay types, pedogenic oxides and plant residue addition rates||-|
|Appears in Collections:||Agriculture, Food and Wine publications|
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