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Sampling Method and Tree-Age Affect Soil Organic C and N Contents in Larch Plantations

机译:落叶松人工林的取样方法及树龄对土壤有机碳和氮含量的影响

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We currently have a poor understanding of how different soil sampling methods (pedogenetic horizon versus fixed-depth) influence the evaluation of soil properties. Here, 159 soil profiles were sampled from larch ( Larix gmelinii ) plantations in northeast China using both the pedogenetic horizon and fixed-depth sampling methods. Analysis of variance was used to determine how sampling method influences the assessment of the spatial variation in the concentration and storage of soil organic C (SOC) and N (SON), as well as how these properties are affected by tree age-group (40 years). In both the 20 cm (surface) and 80 cm (whole profile) sampling depths, pedogenetic sampling resulted in 1.2- to 1.4-fold higher SOC and SON concentrations than fixed-depth sampling. Surface soil nutrient storage between the two sampling methods was not significantly different, but was it was 1.2-fold higher ( p < 0.05) with pedogenetic sampling than with fixed-depth sampling in the whole soil profile. For a given error limit in SOC and SON assessments, fixed-depth sampling had a 60%~90% minimum sampling intensity requirement compared with pedogenetic horizon sampling. Additionally, SOC was 1.1- to 1.3-fold greater in the >40 years age-group than in the <20 years age-group ( p < 0.05), while SON was the highest in the 20–40 years age-group ( p < 0.05). The total amount of SOC and nutrients in soil is fixed regardless how you sample, it is the different assumptions and different ways of extrapolation from samples to the population that cause sampling by horizon versus fixed depth to lead to different conclusions. Our findings highlight that soil sampling method and tree age-group affect the determination of the spatial variation of SOC and SON and future soil assessments should control for methodological differences.
机译:目前,我们对不同的土壤采样方法(成岩视野与固定深度)如何影响土壤性质的评估知之甚少。在这里,使用土壤成因水平和固定深度采样方法,从中国东北的落叶松(落叶松)人工林中采样了159个土壤剖面。使用方差分析来确定采样方法如何影响土壤有机碳(SOC)和N(SON)的浓度和存储空间变异的评估,以及树木年龄组如何影响这些性质(40年份)。在20 cm(表面)和80 cm(整个剖面)的采样深度中,与固定深度采样相比,成岩采样导致SOC和SON浓度高1.2到1.4倍。两种采样方法之间的表层土壤养分存储没有显着差异,但在整个土壤剖面中,土壤成因采样比固定深度采样高1.2倍(p <0.05)。对于给定的SOC和SON评估误差极限,固定深度采样的最低采样强度要求为土壤成层水平采样的60%〜90%。此外,> 40岁年龄组的SOC比<20岁年龄组的SOC高1.1到1.3倍(p <0.05),而SON在20-40岁年龄组中最高(p <0.05)。无论您如何采样,土壤中SOC和养分的总量都是固定的,是从样本到总体的不同假设和不同的外推方式导致按水平抽样与固定深度抽样得出不同的结论。我们的发现强调,土壤采样方法和树木年龄组会影响SOC和SON空间变异的确定,未来的土壤评估应控制方法上的差异。

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