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Study on spatial-temporal change of soil organic carbon and impact factors in Gudao Forestry Farm of Dongying

机译:东营市古道林场土壤有机碳的时空变化及其影响因素研究

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Soil organic carbon (SOC) is one of the important properties to evaluate soil quality, which can indirectly reflect the effect of afforestation on saline-alkali land. In this study, 4 different forest types in Gudao Forestry Centre were selected as experimental plots, and bare land was set as blank group. Spatial differentiation and impact factors of SOC between different forest types were studied by field investigation and laboratory experiment. The results show that (1) SOC content in the study area is lower than 1%. SOC content in forest land is higher than that in bare land. In the upper soil layer, the SOC content of Robinia Pseudoacacia forest is lower, and mixed forest is higher. SOC content of bare land is higher than that of forest land in the lower layer. (2) SOC has a significant positive correlation with available nutrients (P<0.05), and has a weak correlation with pH and water content. There are different correlations with conductivity and bulk density in different soil layers, and they all showed a negative correlation at the upper layer, and a significant positive correlation at the lower layer (P<0.05).
机译:土壤有机碳(SOC)是评价土壤质量的重要属性之一,可以间接反映造林对盐碱地的影响。本研究选取孤岛林业中心的4种不同类型的森林作为试验区,并将裸地设置为空白组。通过田间调查和室内试验研究了不同森林类型之间SOC的空间分异及其影响因素。结果表明:(1)研究区SOC含量低于1%。林地的SOC含量高于裸地。在上层土壤中,刺槐林的SOC含量较低,而混交林则较高。较低层的裸露土壤SOC含量高于林地。 (2)SOC与有效养分呈显着正相关(P <0.05),而与pH和含水量呈弱相关。不同土层与电导率和容重的相关性不同,均在上层呈负相关,在下层呈显着正相关(P <0.05)。

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