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Relationship between carbon and nitrogen in degraded alpine meadow soil

机译:退化高寒草甸土壤碳氮关系

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The distribution of soil organic carbon (SOC), labile organic carbon (LOC), and available nitrogen, as?well as, the corresponding relationships between carbon and nitrogen were analyzed among meadows?with varying degrees of degradation (normal, slight and severe) in Dangxiong, Tibet. The increasing?severity of meadow degradation corresponded with decreasing soil organic carbon, LOC and available?nitrogen. The SOC distributions in the 0 to 10 cm soil layer of the slightly degraded and severely?degraded meadows were lower than that of the normal meadow by 13.2 to 27.5% and 39.5 to 78.6%,?respectively. The LOC distribution in the two areas decreased by 11.1 to 50.9% and by 31.2 to 77.2%.?The corresponding available nitrogen decreased by 25.6 to 38.2% and 48.8 to 68.0%, whereas the SOC?decreased by 6.0 to 29.7% and 53.2 to 73.2%. The degradation of soil carbon and nitrogen occurred first?in the 0 to 10 cm layer. In the 0 to 10 cm and the 10 to 20 cm layers, the relationship between soil?available nitrogen and LOC was more significant than that between soil available nitrogen and SOC.?Grassland degradation caused a decrease in the ratio of soil LOC to available nitrogen. The average?proportions of LOC and available nitrogen in the normal, slightly degraded, and severely degraded?meadows were 24, 19, and 17. These values showed that the nitrogen loss caused by grassland?degradation is faster than LOC loss. During degradation, organic carbon was more stable than soil?available nitrogen.
机译:分析了退化程度不同(正常,轻度和严重)的草地间土壤有机碳(SOC),不稳定有机碳(LOC)和有效氮的分布以及碳氮之间的对应关系。在西藏当雄草地退化的加剧程度与土壤有机碳,LOC和有效氮的减少相对应。轻度退化和严重退化的草地在0至10 cm土层的SOC分布分别比正常草地低13.2%至27.5%和39.5%至78.6%。这两个区域的LOC分布下降了11.1至50.9%,下降了31.2至77.2%。 73.2%。土壤碳和氮的降解首先发生在0至10 cm层。在0〜10 cm和10〜20 cm层,土壤有效氮与LOC的关系比土壤有效氮与SOC之间的关系更为显着。草地退化导致土壤LOC与有效氮的比率降低。在正常,轻度降解和严重降解的草甸中,LOC和可用氮的平均比例为24、19和17。这些值表明,由草地退化引起的氮损失比LOC损失要快。在降解过程中,有机碳比土壤有效氮更稳定。

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