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固龄、侵入程度和土壤特性调节了固氮灌木紫穗槐入侵的干旱草原土壤中 C 和 N 循环的变化。

Stand age, degree of encroachment and soil characteristics modulate changes of C and N cycles in dry grassland soils invaded by the N-fixing shrub Amorpha fruticosa.

机构信息

Department of Biology, University of Copenhagen, Universitetsparken 4, 3rd floor, 2100, København Ø, Denmark; Department of Agricultural, Food, Environmental and Animal Sciences, University of Udine, via delle Scienze 206, 33100, Udine, Italy.

Department of Agricultural, Food, Environmental and Animal Sciences, University of Udine, via delle Scienze 206, 33100, Udine, Italy.

出版信息

Sci Total Environ. 2021 Oct 20;792:148295. doi: 10.1016/j.scitotenv.2021.148295. Epub 2021 Jun 17.

Abstract

The N-fixing shrub Amorpha fruticosa L. is rapidly spreading in the dry riparian natural grasslands of Europe, altering ecosystem functions and depleting plant diversity. Alteration of the N cycle represents the key factor involved in invasions by N-fixing plants with cascading effects on plant species richness. We hypothesized that A. fruticosa encroachment strongly impacts not only the N but also the C cycle and that the magnitude of such alterations may be modulated by soil characteristics. To test these hypotheses, we selected four river floodplains in North East of Italy and compared natural uninvaded grasslands with half invaded and completely invaded sites, based on A. fruticosa stand characteristic and relevant leaf traits and on soil properties related to soil texture and to C and N cycles. Soil organic matter mineralisation, ammonification and nitrification rates were determined. Soil nitrification increased remarkably with plant invasion while ammonification was significantly higher only in half invaded sites. Soil organic matter mineralisation, microbial biomass C sustained per soil organic C unit and nitrification positively correlated with stand age, regardless to the stage of the encroachment. Mineralisation and nitrification increased with soil organic C and total N in uninvaded and completely invaded sites, but decreased in half invaded sites. At the half invasion stage, trends in nitrification and CO mineralisation were transitionally reverted and remediation may be facilitated by less pronounced changes in soil properties compared to completely invaded sites. Direct effects of plant invasion are modulated by the action of soil characteristics such as soil organic C and clay contents, with soils rich in organic C showing larger nitrification and mineralisation rates.

摘要

固氮灌木紫穗槐( Amorpha fruticosa L. )在欧洲干旱河岸自然草原迅速蔓延,改变了生态系统功能并减少了植物多样性。氮循环的改变是固氮植物入侵的关键因素,对植物物种丰富度产生级联效应。我们假设,紫穗槐的入侵不仅强烈影响氮循环,而且还影响碳循环,而这种变化的幅度可能受到土壤特性的调节。为了验证这些假设,我们选择了意大利东北部的四个河流泛滥平原,并根据紫穗槐的林分特征和相关叶片特征以及与土壤质地以及碳和氮循环相关的土壤特性,将天然未受干扰的草原与半入侵和完全入侵的地点进行了比较。测定了土壤有机质矿化、氨化和硝化速率。土壤硝化作用随着植物入侵而显著增加,而氨化作用仅在半入侵地点显著增加。土壤有机质矿化、微生物生物量 C 与土壤有机碳单位的固持以及硝化作用与林龄呈正相关,而与入侵阶段无关。在未受干扰和完全入侵的地点,矿化和硝化作用随土壤有机碳和总氮的增加而增加,但在半入侵地点则减少。在半入侵阶段,硝化和 CO 矿化的趋势发生了过渡性逆转,与完全入侵的地点相比,土壤性质的变化不太明显,可能更容易进行修复。植物入侵的直接影响受到土壤特性(如土壤有机碳和粘粒含量)的调节,富含有机碳的土壤表现出更大的硝化和矿化速率。

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