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Research on soil net nitrogen mineralization in Stipa grandis grassland with different stages of degradation

机译:不同退化阶段大针茅草原土壤净氮矿化的研究

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摘要

Net nitrogen mineralization is one of the nitrogen cycling process, and it is very important to understand nitrogen mineralization characteristics in degradation grassland. In the upper 0-10 cm soil layer of Stipa grandis P. A. Smirn. grassland in the Xilin river basin, Inner Mongolia, we studied the soil net nitrogen mineralization and nitrification among three varying stages of degradation grassland and analyzed the relationship between the mineralization rate of the soil net nitrogen and environmental factors, using the resin-core incubation method. Our results demonstrated that, from May to October 2012, the accumulated net nitrogen mineralization was 21.620 mg kg(-1), 12.486 mg kg(-1), and 48.053 mg kg(-1) in the slightly, medium, and heavily degraded grasslands, respectively and varied greatly among the three stages of degradation shown by the S. grandis grassland plots. During the cultivation period, the variation of net nitrogen mineralization and nitrification was similar to the variation of soil mineral nitrogen. The higher soil mineral nitrogen content indicated higher mineralization of net nitrogen. In July and August, soil moisture was positively correlated with the net nitrogen mineralization rate, and the correlation coefficients between these two factors of 0.73, 0.58, and 0.79 for the slightly, medium, and heavily degraded plots, respectively. The rates of net nitrogen mineralization and nitrification were negatively correlated with soil total nitrogen, but positively correlated with C/N ratio, and weakly correlated with other physicochemical properties.
机译:净氮矿化是氮循环过程之一,了解退化草地的氮矿化特征非常重要。在Stipa grandis P.A.Smirn的上部0-10厘米土壤层中。内蒙古锡林河流域草原,研究了退化草地三个不同阶段的土壤净氮矿化和硝化作用,并采用树脂核温育法分析了土壤净氮矿化率与环境因子之间的关系。 。我们的结果表明,从2012年5月到2012年10月,在轻度,中度和重度降解中,累积的净氮矿化量分别为21.620 mg kg(-1),12.486 mg kg(-1)和48.053 mg kg(-1)。草地,并且在S. grandis草地图所示的三个退化阶段之间变化很大。在耕作期间,净氮矿化和硝化作用的变化与土壤矿质氮的变化相似。土壤矿质氮含量越高,表明净氮矿化度越高。在7月和8月,土壤湿度与净氮矿化速率呈正相关,对于轻度,中度和重度退化的地块,这两个因子的相关系数分别为0.73、0.58和0.79。净氮矿化率和硝化率与土壤总氮呈负相关,与碳氮比呈正相关,与其他理化性质呈弱相关。

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