The history of agriculture in Taiwan spans more than 250 years. ![]() The study was conducted in Taiwan, an island located at the subtropical and tropical climate zone boundary. Our objectives were to (1) examine the changes in 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. The wide geographic coverage of the study sites offered an ideal opportunity to examine changes in SOC concentration and stock after the forest regeneration of agricultural fields. Accordingly, this study selected 11 pairwise sites with forest regenerated and adjacent agricultural fields whose elevation gradient ranged from lowlands to montane areas. Examining possible SOC enhancement at a national scale requires the use of an extensive data set to estimate the SOC sequestration potential and reduce possible uncertainties robustly. focused on sites confined to the lowlands. is among the few studies reporting changes in SOC after land-use change from agricultural fields nevertheless, the study by Lin et al. The connection between SOC changes and land-use change from agricultural fields to forest regeneration is still poorly quantified in Taiwan. ![]() 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. 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. ![]() 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. 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 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 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. Our results demonstrated overall increases in both SOC concentrations and stocks after forest regeneration of the abandoned 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. We selected 11 sites with altitudes ranging from 14 to 2056 m and with paired forest regenerated and adjacent agricultural fields. Afforestation or abandonment of agricultural fields to forest regeneration is a method of sequestering carbon to offset the increasing atmospheric concentration of CO 2.
0 Comments
Leave a Reply. |