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首页> 外文期刊>Soil Biology & Biochemistry >Regulation of soil phosphorus cycling in grasslands by shrubs
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Regulation of soil phosphorus cycling in grasslands by shrubs

机译:灌木法调节草原循环循环

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The globally expanding colonization of grasslands by shrubs increases soil organic carbon and nitrogen, but the effects of shrubs on phosphorus (P) cycling have been rarely studied. We compared P contents in roots and soil fractions, phosphatase activity in the 1 m profile, and in situ net P mineralization between shrubby Potentilla fruticosa patches and grassy interspaces in grazed shrubby meadows at three representative sites on the eastern Tibetan Plateau. The P uptake of P. fruticosa exceeded 1 m soil depth, whereas grasses acquired P mainly within the upper 0.6 m. The P contents in shoots, aboveground litter and roots under P. fruticosa were greater than those under grasses. Litter P stock under the shrubs was 4-8 times higher than that under grasses and the root P stock doubled compared to that in grass areas. P. fruticosa generally increased the organic P (OP) content in the topsoil but decreased inorganic P (IP) in the subsoil. Phosphorus availability increased in the topsoil but decreased in the subsoil under the shrubs compared to grasses. Microbial biomass P (MBP), the activities of acid and alkaline phosphatases, and OP lability were all greater in the 1 m soil under P. fruticosa than grasses, leading to faster P mineralization and the P turnover under the shrubs. In the 1 m soil, P. fruticosa increased MBP and OP stocks but decreased IP and available P stocks. The larger and deeply distributed root system of P. fruticosa improved its P uptake ability especially from the subsoil. The subsequent greater organic matter input through litter fall and root turnover under P. fruticosa fed a larger microbial biomass that synthesized more microbial-derived OP in the topsoil. We concluded that shrubs increase the biological (plant and microbial) P transformation in the soil, the P uplift in the profile, and P cycling in shrubby grassland ecosystems. Such mechanisms structuring spatial heterogeneity of P content, transformation, turnover and fluxes are common in shrubby grasslands worldwide.
机译:通过灌木扩大草原的殖民化增加了土壤有机碳和氮,但灌木对磷(P)循环的影响已经很少研究。我们将P含量与土壤和土壤部分中的P含量进行比较,磷酸酶活性在1米的曲线中,在西藏高原的三个代表性地区的灌木育龄斑块斑块和草地间隙中原位净P矿化。 P. Fruticosa的P. Fruticosa的土壤深度超过1米,而草地占用P.主要在0.6米内。 P. Fruticosa下的枝条,地上垃圾和根部的P含量大于草丛中的枝条。灌木下的垃圾p库存比草底高4-8倍,与草地区相比,根本P库存增加一倍。 P. Fruticosa通常将底层中的有机P(OP)含量增加,但是在底层中的无机P(IP)降低。磷的可用性在甲状腺素中增加,但与草相比,灌木下的底层减少。微生物生物量P(MBP),酸和碱性磷酸酶的活性,在P.Fruticosa下的1米的土壤中比草的1米土壤更大,导致灌木丛下的P矿化和P营业额较快。在1米的土壤中,P.Fruticosa增加了MBP和OP股,而是降低了IP和可用的P股。 P. Fruticosa的较大和深度分布的根系,尤其是来自底层的P吸收能力。随后通过凋落物的更大的有机物质输入P.Fruticosa根据含有较大的微生物生物量,在TheoSIL中合成更多微生物衍生的OP。我们得出结论,灌木增加了土壤中的生物(植物和微生物)P转化,概况中的P隆起,以及在灌木丛草地生态系统中的P循环。在全世界的灌木草原中,这种机制构成了P含量,转化,周转和助熔剂的空间异质性。

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