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Temporal variation of soil carbon stock and its controlling factors over the last two decades on the southern Song-nen Plain, Heilongjiang Province

机译:黑龙江省南部松嫩平原近二十年来土壤碳储量的时空变化及其影响因素

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Against the current background of global climate change, the study of variations in the soil carbon pool and its controlling factors may aid in the evaluation of soil's role in the mitigation or enhancement of greenhouse gas. This paper studies spatial and temporal variation in the soil carbon pool and their controlling factors in the southern Song-nen Plain in Heilongjiang Province, using soil data collected over two distinct periods by the Multi-purpose Regional Geochemical Survey in 2005-2007, and another soil survey conducted in 1982-1990. The study area is a carbon source of 1479 t/km2 and in the past 20 years, from the 1980s until 2005, the practical carbon emission from the soil was 0.12 Gt. Temperature, which has been found to be linearly correlated to soil organic carbon, is the dominant climatologic factor controlling soil organic carbon contents. Our study shows that in the relevant area and time period the potential loss of soil organic carbon caused by rising temperatures was 0.10 Gt, the potential soil carbon emission resulting from land-use change was 0.09 Gt, and the combined potential loss of soil carbon (0.19 Gt) caused by warming and land-use change is comparable to that of fossil fuel combustion (0.21 Gt). Due to the time delay in soil carbon pool variation, there is still 0.07 Gtin the potential emission caused by warming and land-use change that will be gradually released in the future.
机译:在当前全球气候变化的背景下,研究土壤碳库及其控制因素的变化可能有助于评估土壤在减少或增强温室气体中的作用。本文利用2005-2007年多用途区域地球化学调查在两个不同时期收集的土壤数据,研究了黑龙江省松嫩平原南部土壤碳库的时空变化及其控制因素,以及1982年至1990年进行的土壤调查。研究区域的碳源为1479吨/平方公里,在过去20年中,从1980年代到2005年,土壤中的实际碳排放量为0.12 Gt。已发现温度与土壤有机碳线性相关,温度是控制土壤有机碳含量的主要气候因素。我们的研究表明,在相关区域和时间段内,温度升高引起的土壤有机碳潜在损失为0.10 Gt,土地利用变化导致的潜在土壤碳排放为0.09 Gt,并且土壤碳的综合潜在损失(由变暖和土地利用变化引起的0.19 Gt)与化石燃料燃烧(0.21 Gt)相当。由于土壤碳库变化的时间延迟,由变暖和土地利用变化引起的潜在排放量仍为0.07 Gtin,将来会逐渐释放。

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