熱帯山地土壌の急速な侵食による地層有機炭素の微生物による酸化
Jordon D Hemingway1,2, Robert G Hilton3, Niels Hovius4,5
1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution (WHOI), 266 Woods Hole Road, Woods Hole, MA 02543, USA. jordon_hemingway@fas.harvard.edu.
まとめ
台湾における石油性有機炭素 (OCpetro) の酸化
科学分野:
- 地化学
- 地形学
- 生地化学
背景:
- 岩層の有機炭素 (OCpetro) の酸化により,CO2が放出されます.
- 景観におけるOCpetro酸化率を制御するメカニズムは十分に理解されていません.
研究 の 目的:
- 台湾のセントラル・レンジからのCO2排出量とOCpetroの酸化を定量化する.
- 山の土壌におけるOCpetro再鉱化に関する制御を調査する.
主な方法:
- 土壌における大量OCと脂質バイオマーカーの分析
- OCpetroの含有量と同位体成分の測定
- 酸化率に基づくCO2排出量流の推定
主要な成果:
- 発掘されたOCpetroの平均67%が土壌で酸化されます.
- CO2の排出量は6.1~18.6トンのC/km2/年である.
- 微生物の活動がOCpetroの再鉱化を媒介する.
結論:
- 山の土壌における急速なOCpetro酸化は,大気中のCO2の重要な源である.
- 二酸化炭素の排出量は 侵食率に伴い増加し 炭素の蓄積を防ぎます
- これらのシステムにおけるOCpetro酸化の主な要因は微生物の再鉱化です.
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