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Soil N2O and CO2 emissions from red soils following land conversion in subtropical China

机译:亚热带土地转化后红壤的土壤N2O和CO2排放

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Chinese forestlands and grasslands have undergone great changes in land use in recent decades for arresting soil erosion and degradation, but its impact on trace gas emissions has not well documented. The study was conducted in situ to assess the comprehensive effects of conversion cropland to forestlands, grasslands and agrofoestry systems on soil N2O and CO2 emissions under maize cultivation (June 2003-October 2003). In order to document the dynamics and importance of these emissions, soil carbon, nitrogen, nitrogen mineralization and microbial biomass C, soil potential for N2O and CO2 emissions and soil climatic data were measured. The total amount of soil N2O emission through the growing season in summer maize field, which were slightly lower than the values of 390, 470, 512, 372 and 423 g N2O-N ha-1 in natural fallow, A.fruticosa, A.fruticosa+faba bean-maize, vetiver, vetiver+faba bean-maize plot, respectively. Equivalent values for CO2 emissions were 3480, 1737, 2449, 5335, 2672 and 3309 kg CO2-C ha-1.The differences in N2O and CO2 emissions between different treatments resulted from the climatic conditions and some potential such as soil microbial biomass C, nitrogen mineralization and hedge species to a great extent. The results indicate that conversion from cropland to hedgerow agroforestry might potentially increase the release of soil CO2 and N2O; and conversion from cropland to forestland and/or grassland might potentially decrease the release of soil CO2, whereas the opposite trend for the release of soil N2O was observed. However, the responses to land conversion reported here need be verified in longer term experiments before they can be used to predict the effects of land conversion on the net soil N2O and CO2 balance.
机译:近几十年来,中国的林地和草原在土地利用方面发生了巨大变化,以阻止水土流失和退化,但其对痕量气体排放的影响尚未得到充分记录。该研究是就地进行的,目的是评估退耕还林,草地和农林业系统对玉米种植下土壤N2O和CO2排放的综合影响(2003年6月至2003年10月)。为了记录这些排放物的动态和重要性,测量了土壤中的碳,氮,氮矿化和微生物生物量C,测量了土壤产生N2O和CO2排放的潜力以及土壤气候数据。夏季玉米田整个生长季土壤N2O排放总量略低于自然休养植物A.fruticosa.A的390、470、512、372和423 g N2O-N ha-1值。分别为金丝桃+非洲豆玉米,香根草,香根草+非洲豆玉米地。 CO2排放当量值为3480、1737、2449、5335、2672和3309 kg CO2-C ha-1。不同处理之间的N2O和CO2排放差异是由于气候条件和土壤微生物量C,氮矿化和树篱种类很大。结果表明,从耕地向树篱农林业转变可能会增加土壤CO2和N2O的释放。从农田转变为林地和/或草地可能会减少土壤CO2的释放,而土壤N2O的释放却呈现相反的趋势。但是,这里报道的对土地转化的响应需要在长期实验中进行验证,然后才能用于预测土地转化对土壤净N2O和CO2平衡的影响。

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