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Photodegradation leads to increased carbon dioxide losses from terrestrial organic matter

机译:光降解导致陆地有机物二氧化碳损失增加

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摘要

CO production in terrestrial ecosystems is generally assumed to be solely biologically driven while the role of abiotic processes has been largely overlooked. In addition to microbial decomposition, photodegradation - the direct breakdown of organic matter (OM) by solar irradiance - has been found to contribute to litter mass loss in dry ecosystems. Previous small-scale studies have shown that litter degradation by irradiance is accompanied by emissions of CO. However, the contribution of photodegradation to total CO losses at ecosystems scales is unknown. This study determined the proportion of the total CO losses caused by photodegradation in two ecosystems: a bare peatland in New Zealand and a seasonally dry grassland in California. The direct effect of solar irradiance on CO production was examined by comparing daytime CO fluxes measured using eddy covariance (EC) systems with simultaneous measurements made using an opaque chamber and the soil CO gradient technique, and with night-time EC measurements under the same soil temperature and moisture conditions. In addition, a transparent chamber was used to directly measure CO fluxes from OM caused by solar irradiance. Photodegradation contributed 19% of the annual CO flux from the peatland and almost 60% of the dry season CO flux from the grassland, and up to 62% and 92% of the summer mid-day CO fluxes, respectively. Our results suggest that photodegradation may be important in a wide range of ecosystems with exposed OM. Furthermore, the practice of partitioning daytime ecosystem CO exchange into its gross components by assuming that total daytime CO losses can be approximated using estimates of biological respiration alone may be in error. To obtain robust estimates of global ecosystem-atmosphere carbon transfers, the contribution of photodegradation to OM decomposition must be quantified for other ecosystems and the results incorporated into coupled carbon-climate models.
机译:一般认为,陆地生态系统中的一氧化碳生产完全是生物驱动的,而非生物过程的作用却被大大忽略了。除微生物分解外,还发现光降解-太阳辐射直接分解有机物(OM)-导致干旱生态系统中的凋落物质量损失。以前的小规模研究表明,辐照引起的凋落物降解伴随着CO的排放。但是,在生态系统范围内,光降解对总CO损失的贡献是未知的。这项研究确定了两个生态系统中由光降解引起的总CO损失的比例:新西兰的一个泥炭地和加利福尼亚的一个季节性干燥的草地。通过比较使用涡度协方差(EC)系统测量的白天CO通量,使用不透明腔室和土壤CO梯度技术进行的同时测量以及同一土壤下夜间EC测量来比较太阳辐照度对CO产生的直接影响温度和湿度条件。另外,使用透明室直接测量由太阳辐照引起的来自OM的CO通量。光降解贡献了泥炭地年度CO通量的19%,而草地干旱季节CO通量的近60%,分别是夏季中午CO通量的62%和92%。我们的结果表明,光降解在暴露于OM的各种生态系统中可能很重要。此外,通过假设仅使用生物呼吸的估计就可以估算白天的总CO损失,将白天的生态系统CO交换划分为总组分的做法可能是错误的。为了获得对全球生态系统-大气碳转移的可靠估计,必须对其他生态系统的光降解对OM分解的贡献进行量化,并将结果纳入耦合的碳-气候模型。

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