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논문 기본 정보

자료유형
학술저널
저자정보
Baek, Won-Jin (Department of Rural & Biosystems Engineering, Chonnam National University) Kim, Young-Joo (Department of Agricultural Engineering, Gyeongsang National University) Yun, Seok-In (Department of Applied Plant Science, Chonnam National University) Lee, Sun-Il (Department of Rural & Biosystems Engineering, Chonnam National University) Lim, Sang-Sun (Department of Rural & Biosystems Engineering, Chonnam National University) Kim, Han-Yong (Department of Applied Plant Science, Chonnam National University) Yoon, Kwang-Sik (Department of Rural & Biosystems Engineering, Chonnam National University) Choi, Soo-Myung (Department of Rural & Biosystems Engineering, Chonnam National University) Choi, Woo-Jung (Department of Rural & Biosystems Engineering, Chonnam National University)
저널정보
한국응용생명화학회 Applied Biological Chemistry Applied Biological Chemistry 제54권 제3호
발행연도
2011.1
수록면
403 - 408 (6page)

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Paddy soils are considered to have a great soil organic carbon (SOC) sequestration potential. The present study was conducted to estimate the amount of new C derived from rice-roots in a paddy soil under global warming with elevated $CO_2$ concentration ([$CO_2$]) using ${\delta}^{13}C$ technique. Roots of rice grown with elevated [$CO_2$] were significantly depleted in $^{13}C$ by more than 6% compared to those with ambient [$CO_2$], leading to a low ${\delta}^{13}C$ of SOC via rhizodeposition of $^{13}C$-depleted C under elevated [$CO_2$]. The net C storage derived from roots was estimated to be 0.25 and 0.31 kg $m^{-2}$ under ambient and elevated air temperature ($T_{air}$) conditions, respectively. The greater roots-derived C under elevated $T_{air}$ than that under ambient $T_{air}$ collaborated with increased root biomass by elevated $T_{air}$. However, SOC balance analysis revealed that 0.16 and 0.21 kg $m^{-2}$ of autochthonous SOCs were decomposed under ambient and elevated $T_{air}$, respectively, during the growth season. Therefore, elevated $T_{air}$ may enhance incorporation of new C derived from roots to SOC pool due to increased belowground biomass, but warming may also increase decomposition of old SOC by stimulating temperature-sensitive microbial activities.

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