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Biotic degradation at night, abiotic degradation at day: positive feedbacks on litter decomposition in drylands

机译:夜间生物降解,白天非生物降解:干旱地区垃圾分解的积极反馈

摘要

The arid and semi-arid drylands of the world are increasingly recognized for their role in the terrestrial net carbon dioxide (CO) uptake, which depends largely on plant litter decomposition and the subsequent release of CO back to the atmosphere. Observed decomposition rates in drylands are higher than predictions by biogeochemical models, which are traditionally based on microbial (biotic) degradation enabled by precipitation as the main mechanism of litter decomposition. Consequently, recent research in drylands has focused on abiotic mechanisms, mainly photochemical and thermal degradation, but they only partly explain litter decomposition under dry conditions, suggesting the operation of an additional mechanism. Here we show that in the absence of precipitation, absorption of dew and water vapor by litter in the field enables microbial degradation at night. By experimentally manipulating solar irradiance and nighttime air humidity, we estimated that most of the litter CO efflux and decay occurring in the dry season was due to nighttime microbial degradation, with considerable additional contributions from photochemical and thermal degradation during the daytime. In a complementary study, at three sites across the Mediterranean Basin, litter CO efflux was largely explained by litter moisture driving microbial degradation and ultraviolet radiation driving photodegradation. We further observed mutual enhancement of microbial activity and photodegradation at a daily scale. Identifying the interplay of decay mechanisms enhances our understanding of carbon turnover in drylands, which should improve the predictions of the long-term trend of global carbon sequestration.
机译:人们越来越认识到世界干旱和半干旱旱地在陆地净二氧化碳(CO)吸收中的作用,这主要取决于植物凋落物的分解以及随后向大气中释放的CO。干旱地区的观测到的分解速率高于生物地球化学模型的预测,该模型传统上是基于降水导致的微生物(生物)降解作为凋落物分解的主要机制。因此,最近在干旱地区的研究集中在非生物机制上,主要是光化学降解和热降解,但它们仅部分解释了干旱条件下的凋落物分解,表明了另一种机制的运行。在这里,我们表明,在没有降水的情况下,野外凋落物吸收露水和水蒸气可使夜间微生物降解。通过实验控制太阳辐照度和夜间空气湿度,我们估计干旱季节发生的大部分垫料CO外排和腐烂是由于夜间微生物降解引起的,白天白天的光化学降解和热降解也有相当大的贡献。在一项补充研究中,在整个地中海盆地的三个地点,垃圾的CO外排主要是由垃圾的水分驱动微生物降解和紫外线辐射引起的光降解引起的。我们进一步观察到微生物活性和光降解在日常规模上相互增强。识别衰减机制的相互作用可以增进我们对旱地碳转换的了解,这应该可以改善对全球碳固存长期趋势的预测。

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