Abstract

Farming management practices are of paramount importance for soil organic carbon (SOC) sequestration in carbon (C) cycling at different scales. However, due to a lack of proper methodologies, estimating the impacts of different soil management practices on overall SOC stock remains inadequately quantified. In this paper, a process-based model, Denitrification-Decomposition (DNDC), was validated on midterm (9 years) and employed depending on the local climate, soil and management conditions, to assess the impacts of alternative management practices on SOC stock under two tillage systems, in a semi-arid region of Morocco. Validated results showed a good agreement between model simulated and observed values, based on the normalized root mean square error (RMSE) and Pearson correlation coefficient (r). This agreement indicates that the DNDC model could capture patterns and magnitudes changes across the climate zone, soil type, and management practices. Modeled results pointed out that, under no-tillage practice (NT), the SOC content increased by 30% compared to conventional tillage (CT). During the simulated period (9 years), the SOC sequestration potential (CSP) has been greatly improved with increased crop residue rate and application of farmyard manure (FY-manure). This increase ranged from 415 kg C/ha to 1787 kg C/ha under NT practice, and from 150 kg C/ha to 818 kg C/ha under CT system. In contrast, increasing fertilizer rate had low to negligible effect on SOC stock. On the other hand, CSP declined by 107–335 kg C/ha and by 177–354 kg C/ha under NT and CT practices respectively, when decreasing N-fertilizer rates. In light of these results, an increase in crop residue rate returned at surface after harvest and application of organic fertilizer, especially under NT practice, can substantially improve SOC stock in a semi-arid region.

Highlights

  • Soil organic carbon (SOC) is considered as a key component in agroecosystems

  • The present paper aims to assess the impact of different farming management practices on SOC stock

  • The modeled results demonstrated that no-tillage practice (NT) system showed a trend with an increase in SOC content compared to conventional tillage (CT) during the 9 simulated years (Figure 4)

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Summary

Introduction

Soil organic carbon (SOC) is considered as a key component in agroecosystems. The first meter of the soil contains 54% of stored SOC, from which 41% are warehoused in the top 20 cm (Jobbagy and Jackson, 2000; Lackner, 2002). C sequestration has been displayed as an inexpensive approach to relieve greenhouse effect. This process converts the atmospheric carbon dioxide (CO2) into biotic or abiotic C stored in agroecosystems (Lackner, 2003). Important decisions need to be made regarding future tolerable levels of atmospheric CO2 content, as well as the land and fossil fuel use strategies that will permit us to achieve these goals (Sarmiento and Bender, 1994). A small change of SOC may induce a significant change in large-scale C cycling which can add important amounts of biomass to the soil, lead to minimal soil disturbance, preserve soil and water, enhance soil structure, and raise soil biotic activity (Mrabet, 2010a)

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