Abstract

The intensive exploitation of agricultural land has caused a depletion of soil organic carbon (SOC) and a decline in soil fertility, with a consequent decrease in the productivity of agroecosystems, also contributing to atmospheric GHG emissions. The ability of soil to storage organic carbon (OC) depends on its persistence and susceptibility to decomposition. SOC is generally partitioned into fractions differing in protection mechanisms and in turn decomposability. This study aimed to compare the OC pool repartition in soils managed with three different fertilization practices (mineral – CONV, manure – ORGM and green manure – ORG-GM) during a medium-term trial in vineyard, in order to understand the best solution in increasing C sequestration. The OC fractionation by acid hydrolysis allowed separating three fractions of OC: a labile, quickly mineralizable pool, a recalcitrant pool with a slower turnover and a stable pool protected by microbial attack. The results showed that the periodic application of organic matrices (manure and green manure), although did not increase total OC, enriched the soil along time with readily available OC, thus promoting the release of nutrients. Green manure has also been shown to promote the accumulation of stabilized OC, able to improve the structure of the soil and, therefore, its fertility.

Highlights

  • The intensive exploitation of agricultural soils managed by unsustainable agronomic practices has caused a depletion of soil organic carbon (SOC)

  • A different repartition of Organic carbon (OC) in fractions with different susceptibility to decomposition was observed along time

  • Studying the repartition into three OC pools with different degree of susceptibility to decomposition in a vineyard managed with different fertilization practices from 2011 to 2018, this research shed light on the ability of selected organic matrices in soil carbon sequestration

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Summary

Introduction

The intensive exploitation of agricultural soils managed by unsustainable agronomic practices has caused a depletion of soil organic carbon (SOC). This has led to a decline in soil fertility and an alteration of biogeochemical cycles, with a consequent decrease in the productivity of agroecosystems. The persistence of OC is a result of three main processes [3] that lead to stabilization: chemical resistance to decomposition, physical inaccessibility to microorganisms and enzymes and interactions with soil mineral components. More labile OC fractions ensure substrates for the microbial community and nutrient availability for crops, refractory pools guarantee a long-term stock of nutrients and stable pools provide good soil structure and physic-chemical properties.

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