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首页> 外文期刊>Water, Air, and Soil Pollution >THE ROLE OF PHOSPHORUS AVAILABILITY IN THE RESPONSE OF SOIL NITROGEN CYCLING, UNDERSTORY VEGETATION AND ARBUSCULAR MYCORRHIZAL INOCULUM POTENTIAL TO ELEVATED NITROGEN INPUTS
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THE ROLE OF PHOSPHORUS AVAILABILITY IN THE RESPONSE OF SOIL NITROGEN CYCLING, UNDERSTORY VEGETATION AND ARBUSCULAR MYCORRHIZAL INOCULUM POTENTIAL TO ELEVATED NITROGEN INPUTS

机译:磷的有效性在土壤氮循环,植物性植被和丛枝菌根无菌对高氮输入的响应中的作用

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摘要

The impacts of increased nitrogen (N) inputs into temperate ecosystems via atmospheric nitrogen deposition on nitrogen cycling and nitrogen retention have been described in a variety of ecosystem types. The role of secondary nutrients such as phosphorus (P) in ecosystem responses to increased N inputs is less well-understood. N and P availability are likely to interact to influence ecosystem productivity and N cycling rates, and this interaction would be expected to vary as N inputs increase. Furthermore, N and P inputs may affect plant-mycorrhizal associations and the ability of arbuscular mycorrhizae (AM) to colonize roots. We added nitrogen (97 kg ha~(-1) yr~(-1)) and phosphorus (30 kg ha~(-1) yr~(-1)) to an oak-maple forest in southwestern Virginia (U.S.A.) from 1994 through 1996. Inorganic nitrogen concentrations, net nitrogen mineralization, net nitrification rates and arbuscular mycorrhizal inoculum potential (MIP) were assessed during the growing season in 1996. Responses of the understory vegetation and soil N cycling to N addition suggested that the ecosystem was strongly N-limited. Nitrogen cycling rates were not affected by P inputs, though P addition increased P availability and decreased MIP. It was hypothesized that P availability may have more significant influences on N cycling and the plant-mycorrhizal association in ecosystems showing stronger symptoms of nitrogen saturation. Results suggest that the use of P fertilization would be effective in alleviating P-deficiency in vegetation receiving elevated atmospheric N deposition, but perhaps at the cost of benefits that associations with arbuscular mycorrhizae provide.
机译:在各种生态系统类型中,已经描述了通过大气氮沉积增加进入温带生态系统的氮(N)对氮循环和氮保持的影响。诸如磷(P)等次生养分在生态系统对增加氮输入的响应中的作用尚不为人所知。氮和磷的可用性可能会相互作用,从而影响生态系统生产力和氮循环速率,并且随着氮投入的增加,这种相互作用有望发生变化。此外,氮和磷的输入可能会影响植物与菌根的结合以及丛枝菌根(AM)在根部定植的能力。我们向美国西南弗吉尼亚州的橡树枫林添加了氮(97 kg ha〜(-1)yr〜(-1))和磷(30 kg ha〜(-1)yr〜(-1))。 1994年至1996年。在1996年的生长季节评估了无机氮浓度,净氮矿化度,净硝化率和丛枝菌根接种量(MIP)。林下植被和土壤氮素对氮素循环的响应表明,该生态系统很强。 N限制。氮的循环速率不受磷输入的影响,尽管磷的添加增加了磷的利用率并降低了MIP。据推测,磷的有效性可能对氮循环和生态系统中植物-菌根的缔合具有更显着的影响,而生态系统显示出更强的氮饱和症状。结果表明,磷肥的使用将有效缓解大气氮沉降增加的植被中的磷缺乏症,但可能以与丛枝菌根相关的益处为代价。

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