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Responses of soil respiration to warming vary between growing season and non-growing season in a mountain forest of southwestern China

机译:在中国西南山区的森林中,土壤呼吸对变暖的响应在生长季节和非生长季节之间有所不同

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Understanding the temperature sensitivity of soil respiration is very important to quantify the climate–carbon cycle feedback. Most existing studies have only focused on responses of growing-season respiration to warming. Soil respiration of non-growing season may be more sensitive to warming. However, to our knowledge, this hypothesis remains poorly understood. An experiment was conducted in a mountain pine forest of southwestern China to compare the sensitivity of soil respiration to warming (+5 °C) between growing and non-growing seasons. Experimental warming decreased soil moisture but increased soil respiration on most of the measuring dates. Warming-caused increase in soil respiration and Q10 value was greater during the growing season than during the non-growing season. Q10 values decreased linearly with warming-induced changes in soil moisture. This study provides preliminary evidence that soil respiration of non-growing season is less sensitive to warming compared with that of growing season in the mountain forests experiencing monsoon climate
机译:了解土壤呼吸的温度敏感性对于量化气候-碳循环反馈非常重要。现有的大多数研究仅集中于生长季节呼吸对变暖的响应。非生长季节的土壤呼吸可能对变暖更为敏感。但是,据我们所知,这个假设仍然知之甚少。在中国西南山区的松树林中进行了一项实验,比较了生长季节和非生长季节土壤呼吸对变暖(+5°C)的敏感性。在大多数测量日期,实验性增温减少了土壤水分,但增加了土壤呼吸。在生长季节,变暖引起的土壤呼吸增加和Q10值大于非生长季节。 Q10值随着温度升高而引起的土壤水分变化呈线性下降。这项研究提供了初步的证据,与经历季风气候的山区森林中的生长季节相比,非生长季节的土壤呼吸对变暖的敏感性较低。

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