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1 INTRODUCTION Soil organic matter (SOM) constitutes a pivotal element of soils and their genesis, also representing the largest store of nutrients supporting plant growth (Bot & Benites, 2007; Montgomery, 2007). Against the backdrop of tighter environmental and economic constraints, understanding SOM dynamics could allow for better matching of fertiliser applications with plant requirements (Ashman & Puri, 2013; Paul, 2014).
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