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Increased temperature sensitivity of net DOC production from ombrotrophic peat due to water table draw-down

机译:由于地下水位下降,非营养性泥炭净DOC产生的温度敏感性提高

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The production and release of dissolved organic carbon (DOC) from peat soils is thought to be sensitive to changes in climate, specifically changes in temperature and rainfall. However, little is known about the actual rates of net DOC production in response to temperature and water table draw-down, particularly in comparison to carbon dioxide (CO) fluxes. To explore these relationships, we carried out a laboratory experiment on intact peat soil cores under controlled temperature and water table conditions to determine the impact and interaction of each of these climatic factors on net DOC production. We found a significant interaction (P < 0.001) between temperature, water table draw-down and net DOC production across the whole soil core (0 to -55 cm depth). This corresponded to an increase in the Q (i.e. rise in the rate of net DOC production over a 10 pC range) from 1.84 under high water tables and anaerobic conditions to 3.53 under water table draw-down and aerobic conditions between -10 and - 40 cm depth. However, increases in net DOC production were only seen after water tables recovered to the surface as secondary changes in soil water chemistry driven by sulphur redox reactions decreased DOC solubility, and therefore DOC concentrations, during periods of water table draw-down. Furthermore, net microbial consumption of DOC was also apparent at - 1 cm depth and was an additional cause of declining DOC concentrations during dry periods. Therefore, although increased temperature and decreased rainfall could have a significant effect on net DOC release from peatlands, these climatic effects could be masked by other factors controlling the biological consumption of DOC in addition to soil water chemistry and DOC solubility. These findings highlight both the sensitivity of DOC release from ombrotrophic peat to episodic changes in water table draw-down, and the need to disentangle complex and interacting controls on DOC dynamics to fully understand the impact of environmental change on this system.
机译:泥炭土壤中溶解有机碳(DOC)的产生和释放被认为对气候变化特别是温度和降雨变化敏感。但是,人们对于响应温度和地下水位下降的净DOC实际产量的了解甚少,特别是与二氧化碳(CO)流量相比。为了探索这些关系,我们在受控的温度和地下水位条件下对完整的泥炭土芯进行了实验室实验,以确定每种气候因素对净DOC生产的影响和相互作用。我们发现整个土壤核心(0至-55厘米深度)的温度,地下水位下降与净DOC产量之间存在显着的相互作用(P <0.001)。这对应于Q值的增加(即,在10 pC范围内的净DOC产生速率增加),从高水位和厌氧条件下的1.84增加到水位下降和有氧条件下-10至-40的3.53厘米深。但是,只有在地下水位恢复到地表之后才能看到净DOC产量的增加,这是因为在地下水位下降期间,由硫氧化还原反应驱动的土壤水化学的二次变化降低了DOC的溶解度,从而降低了DOC的浓度。此外,DOC的净微生物消耗量在-1 cm深度也很明显,并且是干旱期间DOC浓度下降的另一个原因。因此,尽管温度升高和降雨减少可能对泥炭地的净DOC释放有显着影响,但除土壤水化学和DOC溶解度外,这些气候影响也可能被其他控制DOC生物消耗的因素所掩盖。这些发现既凸显了非营养性泥炭中DOC释放对地下水位下垂变化的敏感性,也需要解开复杂且相互作用的DOC动态控制以充分了解环境变化对该系统的影响。

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