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Effects of soil C:N:P stoichiometry on biomass allocation in the alpine and arid steppe systems

机译:土壤C:N:P化学计量对高寒干旱草原系统生物量分配的影响

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Abstract Soil nutrients strongly influence biomass allocation. However, few studies have examined patterns induced by soil C:N:P stoichiometry in alpine and arid ecosystems. Samples were collected from 44 sites with similar elevation along the 220-km transect at spatial intervals of 5 km along the northern Tibetan Plateau. Aboveground biomass (AGB) levels were measured by cutting a sward in each plot. Belowground biomass (BGB) levels were collected from soil pits in a block of 1 m ???? 1 m in actual root depth. We observed significant decreases in AGB and BGB levels but increases in the BGB:AGB ratio with increases in latitude. Although soil is characterized by structural complexity and spatial heterogeneity, we observed remarkably consistent C:N:P ratios within the cryic aridisols. We observed significant nonlinear relationships between the soil N:P and BGB:AGB ratios. The critical N:P ratio in soils was measured at approximately 2.0, above which the probability of BGB:AGB response to nutrient availability is small. These findings serve as interesting contributions to the global data pool on arid plant stoichiometry, given the previously limited knowledge regarding high-altitude regions.
机译:摘要土壤养分强烈影响生物量的分配。但是,很少有研究检查在高山和干旱生态系统中土壤C:N:P化学计量引起的模式。从青藏高原北部沿5公里的空间间隔沿220公里断面收集了44个海拔相似的地点的样本。地上生物量(AGB)的水平是通过在每块土地上割草来测量的。在1 m的区域内从土壤坑中收集地下生物量(BGB)。实际根深1 m。我们发现,随着纬度的增加,AGB和BGB的水平显着下降,但BGB:AGB的比率却增加了。尽管土壤的特征是结构复杂性和空间异质性,但我们观察到冰冻干旱地区的C:N:P比值非常一致。我们观察到土壤N:P和BGB:AGB比率之间存在显着的非线性关系。土壤中关键的N:P比值约为2.0,高于该值时,BGB:AGB对养分利用率的响应的可能性很小。鉴于先前有关高海拔地区的知识有限,这些发现为有关干旱植物化学计量的全球数据库提供了有趣的贡献。

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