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阔叶红松林4种演替阶段不同土层深度磷组分的特征
Characteristics of Soil Phosphorus Fractions at Different Depths Across 4 Successional Stages in a Broadleaved Pinus koraiensis Forest
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摘要: 为探究阔叶红松林土壤磷组分在不同森林群落演替阶段和不同土层深度的差异,以小兴安岭地区处于4种不同演替阶段的阔叶红松林(天然枫桦次生林、次生阔叶林、次生针阔混交林和原始阔叶红松林)土壤为对象,分析阔叶红松林不同演替阶段和不同土层深度(0~10、10~20、20~40 cm)对土壤磷组分(全磷、有效磷、有机磷和无机磷)的影响。结果表明:随着森林群落演替的进行,土壤全磷、有效磷、有机磷、无机磷、活性有机磷、中等活性有机磷、Al−P、Fe−P整体呈现先降低后升高的变化趋势,中稳性有机磷、高稳性有机磷、O−P、Ca−P整体呈现先升高后降低的变化趋势;有效磷、中等活性有机磷、Fe−P含量未随土层变化而明显下降,Ca−P含量随土层加深而增加,全磷,有机磷、无机磷、活性有机磷、中稳性有机磷、高等稳定性有机磷、Al−P、O−P含量均随土层加深而降低。Abstract: In order to explore the differences of soil phosphorus fractions in different forest community succession stages and different soil depths in broad-leaved Pinus koraiensis forest, the soil of broad-leaved P. koraiensis forest(natural Betula costata secondary forest, secondary broad-leaved forest, secondary coniferous and broad-leaved mixed forest and original broad-leaved P. koraiensis forest) in 4 different succession stages in Lesser Khingan Range was taken as the object to analyze the effects of different succession stages and different soil depths(0–10, 10–20, 20–40 cm) on soil phosphorus fractions(total phosphorus, available phosphorus, organic phosphorus and inorganic phosphorus). The findings demonstrate that with the progress of forest community succession, soil total phosphorus, available phosphorus, organic phosphorus, inorganic phosphorus, active organic phosphorus, moderately active organic phosphorus, Al-P and Fe-P showed a trend of first decreasing and then increasing, while moderately stable organic phosphorus, highly stable organic phosphorus, O-P and Ca-P showed a trend of first increasing and then decreasing. The contents of available phosphorus, moderately active organic phosphorus and Fe-P did not decrease significantly with the change of soil layer, and the content of Ca-P increased with the deepening of soil layer. The contents of total phosphorus, organic phosphorus, inorganic phosphorus, active organic phosphorus, moderately stable organic phosphorus, highly stable organic phosphorus, Al-P and O-P decreased with the deepening of soil layer.
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