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Dynamics of phosphorus nutrition, allocation and growth of young beech (Fagus sylvatica L.) trees in P-rich and P-poor forest soil

机译:富含P-ob贫困林地土壤中幼山(Fagus Sylvatica L.)树的磷营养,分配和生长的动态

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To investigate how long-lived forest trees cope with low soil phosphorus (P) availabilities, we characterized P nutrition of beech (Fagus sylvatica, L.) in soils from P-rich and P-poor beech forests throughout an annual growth cycle. Young trees were excavated with intact soil cores in mono-specific beech forests, kept under common garden conditions, and used for 33P labeling, analyses of P uptake, P content and biomass during five phenological stages (dormancy in winter, bud swelling in early spring, mature leaves in early and late summer, and senescent leaves in fall). Seasonal allocation patterns showed that young, emerging leaves were preferred sinks for P under P-poor conditions, thereby keeping foliar P concentrations at levels similar to those of trees grown in P-rich soil. Phosphorus concentrations in stems and roots of trees from the P-poor conditions were lower than those from P-rich conditions. Coarse roots were the main P storage tissue, supplying inorganic P to newly formed leaves, originating from the inorganic and organic P pools under low and high P conditions, respectively. Beech trees in P-poor soil exhibited net biomass increment early in the annual growth along with a strong P deficit, which was replenished by enhanced uptake in late summer and fall. Trees in P-rich soil grew until late summer, and showed a moderate P decline in organic pools and recovery late in fall, which coincided with elevated P uptake from soil. Beech in P-poor soil produced more biomass per unit of P but at a slower growth rate than those in P-rich soil, thereby exhibiting similar P-use efficiencies. Temporal decoupling of growth and P acquisition in combination with internal P trade-off between storage tissues and leaves facilitated flexible acclimation of beech to a wide range of soil P availabilities.
机译:调查多久森林树木如何应对低土磷(P)可用性,我们在每年生长周期中为P-Rich和P-Povate Beech森林中的土壤中的P营养(Fagus Sylvatica,L.)的p营养。在常见的庭院条件下,在单一特定的山毛榉森林中挖掘了幼小的树木,在常见的庭院条件下,并用于33p标记,在五个牙权阶段(冬季休眠,冬季芽肿胀)分析p吸收,p含量和生物量。 ,成熟的叶子在早期和深夜,秋天的衰老叶)。季节性分配模式表明,在P差的条件下P优选的叶片是P差的P差,从而将叶酸P浓度保持在与在富富型土壤中生长的树木的水平相似。来自P差的条件的茎和树根的磷浓度低于来自富力的条件。粗根是主P储存组织,将无机P供应到新形成的叶片,分别在低和高P条件下源自无机和有机P池。 P-ob贫困土壤中的山毛榉树在年初提前展现了净生物量增量以及强大的P赤字,通过增强夏季和秋季的增强补充,补充了。富含土地的树木增长至深夜,并在秋天的有机游泳池中展现了适度的P减少,这与土壤的P升高了P升高。 P-差土壤中的山毛榉生产每单位P的生物量,但增长速度较慢,比富含P富含土壤,从而表现出类似的P-Meedicies。在储存组织和叶片之间的内部P折衷和叶片之间的颞下P折衷和叶子的颞次去耦合促进了山毛榉的柔性地适应范围。

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