Abstract

Afforestation or abandonment of agricultural fields to forest regeneration is a method of sequestering carbon to offset the increasing atmospheric concentration of CO2. We selected 11 sites with altitudes ranging from 14 to 2056 m and with paired forest regenerated and adjacent agricultural fields. Our objectives were to (1) examine the changes in soil organic carbon (SOC) concentration and stock after forest regeneration of agricultural fields and (2) identify the factors related to elevation and adjacent agricultural practices that affect the SOC accumulation rate. Our results demonstrated overall increases in both SOC concentrations and stocks after forest regeneration of the abandoned agricultural fields. The average increase rates of SOC concentrations in the forest regenerated soil samples were 1.65 and 0.95 g C kg−1 at 0–10 and 10–20 cm depths, respectively, representing 101% and 65% increases relative to those in the soil samples from agricultural fields. The average accumulation rates of SOC stocks in the regenerated forests were 13.0 and 6.7 ton C ha−1 at the 0–10 and 10–20 cm depths, respectively, representing 96% and 62% increases relative to those in the agricultural soil samples. The average annual sequestration rate was 1.03 Mg C ha−1 year−1 for the top 0–20 cm soils, which is greater than that observed by previous reviews and meta-analyses. The tropical/subtropical climate, sampling soil depth, forest regeneration period, and tree species in this study are likely to have contributed to the high average SOC accumulation levels. In addition, the SOC stock accumulation rates were higher at low-elevation sites than at middle-elevation sites, which could also be attributed to the favorable climatic conditions at the low-elevation sites. Along with the build-up of carbon sequestration in the forest floor and tree biomass, the afforestation/abandonment of agricultural fields to forest regeneration appears to be a promising carbon offset mechanism.

Highlights

  • Because of the increase in global warming and the frequency of extreme climate events, our attention to the development of approaches for mitigating climate change has increased.Afforestation or abandonment of surplus arable lands contributes to the mitigation of the increasing atmospheric CO2 concentration [1]

  • Our results reveal a clear increase in soil organic carbon (SOC) concentrations and stocks after the forest regeneration of agricultural fields, confirming most of the findings of relevant studies [2,3,4,5,6,7,8,9,10,11,12]

  • Our results demonstrate overall increases in both SOC concentrations and stocks after the abandonment/afforestation of agricultural fields

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Summary

Introduction

Because of the increase in global warming and the frequency of extreme climate events, our attention to the development of approaches for mitigating climate change has increased.Afforestation or abandonment of surplus arable lands contributes to the mitigation of the increasing atmospheric CO2 concentration [1]. Changing land use from agriculture to forest regeneration triggers a series of differences in soil carbon fluxes. Soil organic carbon (SOC) concentrations and stocks can be enhanced through increased biomass input and minor soil disturbance under forest regeneration [2,3]. Several reviews and meta-analyses have demonstrated the SOC sequestration potential after forest regeneration of agricultural fields in tropical zones [4,5], in temperate regions [6,7,8,9], and worldwide [2,3,10,11,12]. Some studies have demonstrated that forest regeneration could produce a decrease [13] or a minor change [14] in the soil C pool

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