首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Relative contribution of plant traits and soil properties to the functioning of a temperate forest ecosystem in the Indian Himalayas
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Relative contribution of plant traits and soil properties to the functioning of a temperate forest ecosystem in the Indian Himalayas

机译:植物性状和土壤性质对印度喜马拉雅山温带森林生态系统运作的相对贡献

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摘要

Plant-soil interactions are a major determinant of changes in forest ecosystem processes and functioning. We conducted a trait-based study to quantify the contribution of plant traits and soil properties to above- and below-ground ecosystem properties in temperate forest in the Indian Himalayas. Nine plant traits (leaf area, specific leaf area, leaf water content, leaf dry matter content, leaf carbon (C), nitrogen (N), phosphorus (P), leaf C/N, and leaf N/P) and eight soil properties (pH, moisture, available N, P, potassium (K), total C, N, P) were selected for determination of their contribution to major ecosystem processes (above-ground biomass C, soil organic C, soil microbial C, soil microbial N, soil microbial P, and soil respiration) in temperate forest. Among the plant traits leaf C, N, P, and leaf N/P ratio proved to be the main contributors to above-ground biomass, explaining 20-27% of variation. Leaf N, P, and leaf N/P were the main contributors to below-ground soil organic C, soil microbial C, soil microbial N, soil microbial P, and soil respiration (explaining 33% of variation). Together, the soil properties, pH, available P, total N and C explained 60% of variation in above-ground biomass, while pH and total C explained 56% of variation in soil organic C. Other soil properties (available P, total C and N) also explained much of the variation in soil microbial C (52%) and soil microbial N (67%), while soil pH explained some of variation in soil microbial N (14%). Available P, total N, and pH explained soil microbial P (81%), while soil respiration was only explained by soil total C (70%). Thus, leaf traits and soil characteristics significantly explaining variations in above- and below-ground ecosystem processes and functioning in temperate forest in the Indian Himalayas. Consequently, tree species for afforestation, restoration, and commercial forestry should be carefully selected, as they can influence the climate change mitigation potential of forest in terms of C stocks in biomass and soils.
机译:植物 - 土壤相互作用是森林生态系统过程变化和运作的主要决定因素。我们进行了一种以特征为基础的研究,以量化植物性状和土壤性质在印度喜马拉雅山脉温带林中的上述和低于地下生态系统性质的贡献。九种植物特征(叶面积,特定叶面积,叶水含量,叶片干物质含量,叶碳(C),氮(N),磷(P),叶C / N和叶N / P)和八种土壤选择性质(pH,水分,可用N,P,钾(K),总C,N,P)用于测定它们对主要生态系统方法的贡献(地上生物质C,土壤有机C,土壤微生物C,土壤温带林中的微生物N,土壤微生物P和土壤呼吸。在植物性状叶C,N,P和叶片N / P比中被证明是地上生物质的主要贡献者,解释了20-27%的变异。叶N,P和叶片N / P是地下土壤有机C,土壤微生物C,土壤微生物N,土壤微生物P和土壤呼吸的主要贡献者(解释了33%的变化)。在一起,土壤性质,pH,可用P,总N和C在地上生物质的60%中解释了60%的变化,而pH和总C解释了土壤有机C.其他土壤性质的56%的变化(可用P,总C.并且N)还解释了土壤微生物C(52%)和土壤微生物N(67%)的大部分变化,而土壤pH解释了土壤微生物N(14%)的一些变化。可用的P,总N和pH解释土壤微生物P(81%),而土壤呼吸仅通过土壤总C(70%)解释。因此,叶状性状和土壤特性显着解释了地下生态系统过程的变化,在印度喜马拉雅山的温带林中运作。因此,应仔细选择造林,恢复和商业林业的树种,因为它们可以影响森林的气候变化减缓潜力,以生物质和土壤中的碳股票。

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