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首页> 外文期刊>Global change biology >The temperature dependence of organic matter decomposition: seasonal temperature variations turn a sharp short-term temperature response into a more moderate annually averaged response
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The temperature dependence of organic matter decomposition: seasonal temperature variations turn a sharp short-term temperature response into a more moderate annually averaged response

机译:有机物分解的温度依赖性:季节性温度变化将短期的急剧温度响应转变为较温和的年平均响应

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The temperature dependence of organic matter decomposition is a critically important determinant of any long-term changes of soil-carbon stocks in response to global warming. Because of practical experimental constraints, most knowledge of this temperature dependence is based on short-term studies. These studies generally show a strong temperature dependence of organic matter decomposition. At the same time, many modelling studies, especially global studies, or studies that investigate the effects of climate change, use longer time steps, such as annual. It is investigated here to what extent the use of short-term temperature dependencies are appropriate, or how they may need to be modified, for application over longer time steps. The work indicated that for global applications, it is critically important to explicitly consider seasonal temperature variations. Across the globe, observed annual mean temperature and the annual temperature range are negatively correlated. Inclusion of this correlation means that the strong short-term temperature dependence becomes much weaker when data are expressed as annual averages for the temperatures experienced across the globe. For short-term responses, the temperature dependence of organic matter decomposition is greater at low than high temperature and deviates strongly from an assumption of a constant Q(10) across temperature. For annually averaged values, this pattern also weakens, and temperature dependencies change only slightly with temperature. Using short time steps for simulations leads to the expectation of more positive changes (sequestration) in soil carbon especially for cold regions of the globe than would be predicted for simulations at annual time steps without explicit consideration of seasonal temperature variations. These considerations help to reconcile some of the apparent differences in temperature dependencies obtained by different workers using different approaches.
机译:有机物分解的温度依赖性是响应全球变暖而土壤碳库的任何长期变化的至关重要的决定因素。由于实际的实验限制,有关温度依赖性的大多数知识都是基于短期研究。这些研究通常显示出有机物分解的强烈温度依赖性。同时,许多建模研究(尤其是全球研究)或调查气候变化影响的研究使用更长的时间步长,例如年度时间。在此研究在更长的时间范围内应用短期温度依赖性的合适程度,或者可能需要修改它们的方式。这项工作表明,对于全球应用而言,明确考虑季节温度变化至关重要。在全球范围内,观测到的年平均温度与年温度范围呈负相关。包含这种相关性意味着当将数据表示为全球平均温度的年度平均值时,强烈的短期温度依赖性变得更弱。对于短期响应,有机物分解的温度依赖性在低温下要高于高温,并且与整个温度恒定Q(10)的假设有很大偏差。对于年均值,这种模式也会减弱,温度相关性仅随温度而略有变化。使用短时间步长进行模拟会导致对土壤碳的积极变化(固存)的期望,特别是对于地球上的寒冷地区,这比在不明确考虑季节性温度变化的情况下按年时间步长进行模拟所期望的变化更大。这些考虑因素有助于调和不同工人使用不同方法获得的温度依赖性的一些明显差异。

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