TY - JOUR
T1 - The Effects of Tree Species on Soil Organic Carbon Content in South Korea
AU - Cha, Ji Yeon
AU - Cha, Yoon Kyung
AU - Oh, Neung Hwan
N1 - Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.
PY - 2019/3
Y1 - 2019/3
N2 - The effects of tree species on soil organic carbon (SOC) content have been evaluated in many studies, but only with a relatively small number of sample plots, resulting in ambiguous conclusions. Here we used a total of 595 forest plots in South Korea to investigate the role of four grouped tree species—pines, oaks, other conifers, and other deciduous trees—in the forest SOC content in both forest floors and mineral soils. Significant differences were observed in SOC content among the groups. Pines contained 7.12 Mg C/ha of organic carbon in forest floors, whereas oaks and other deciduous trees contained 5.39 and 5.41 Mg C/ha, respectively. In contrast, oaks and other deciduous trees contained ~66 Mg C/ha of organic carbon each in mineral soils (0- to 30-cm depth), whereas pines contained 49.50 Mg C/ha. The total SOC content including both forest floors and mineral soils was the largest under oaks and the smallest under other coniferous trees, due to SOC being approximately an order of magnitude higher in mineral soils than in forest floors. The effects of tree species on SOC storage became apparent for the forest stands with >20-year-old trees, which suggests that the observed differences in the SOC content are likely due to the current stands rather than remnants of previous stands. The decomposition rates of organic materials could be a controlling factor affecting SOC storage, rather than inputs of photosynthesized products to soils.
AB - The effects of tree species on soil organic carbon (SOC) content have been evaluated in many studies, but only with a relatively small number of sample plots, resulting in ambiguous conclusions. Here we used a total of 595 forest plots in South Korea to investigate the role of four grouped tree species—pines, oaks, other conifers, and other deciduous trees—in the forest SOC content in both forest floors and mineral soils. Significant differences were observed in SOC content among the groups. Pines contained 7.12 Mg C/ha of organic carbon in forest floors, whereas oaks and other deciduous trees contained 5.39 and 5.41 Mg C/ha, respectively. In contrast, oaks and other deciduous trees contained ~66 Mg C/ha of organic carbon each in mineral soils (0- to 30-cm depth), whereas pines contained 49.50 Mg C/ha. The total SOC content including both forest floors and mineral soils was the largest under oaks and the smallest under other coniferous trees, due to SOC being approximately an order of magnitude higher in mineral soils than in forest floors. The effects of tree species on SOC storage became apparent for the forest stands with >20-year-old trees, which suggests that the observed differences in the SOC content are likely due to the current stands rather than remnants of previous stands. The decomposition rates of organic materials could be a controlling factor affecting SOC storage, rather than inputs of photosynthesized products to soils.
UR - http://www.scopus.com/inward/record.url?scp=85063496521&partnerID=8YFLogxK
U2 - 10.1029/2018JG004808
DO - 10.1029/2018JG004808
M3 - Article
AN - SCOPUS:85063496521
SN - 2169-8953
VL - 124
SP - 708
EP - 716
JO - Journal of Geophysical Research: Biogeosciences
JF - Journal of Geophysical Research: Biogeosciences
IS - 3
ER -