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土地利用管理和土壤性质对纳米比亚稀树草原反硝化细菌群落的影响

Impact of Land Use Management and Soil Properties on Denitrifier Communities of Namibian Savannas.

作者信息

Braker Gesche, Matthies Diethart, Hannig Michael, Brandt Franziska Barbara, Brenzinger Kristof, Gröngröft Alexander

机构信息

Max Planck Institute for Terrestrial Microbiology, Marburg, Germany.

Kiel University, Kiel, Germany.

出版信息

Microb Ecol. 2015 Nov;70(4):981-92. doi: 10.1007/s00248-015-0623-6. Epub 2015 May 15.

Abstract

We studied potential denitrification activity and the underlying denitrifier communities in soils from a semiarid savanna ecosystem of the Kavango region in NE Namibia to help in predicting future changes in N(2)O emissions due to continuing changes of land use in this region. Soil type and land use (pristine, fallow, and cultivated soils) influenced physicochemical characteristics of the soils that are relevant to denitrification activity and N(2)O fluxes from soils and affected potential denitrification activity. Potential denitrification activity was assessed by using the denitrifier enzyme activity (DEA) assay as a proxy for denitrification activity in the soil. Soil type and land use influenced C and N contents of the soils. Pristine soils that had never been cultivated had a particularly high C content. Cultivation reduced soil C content and the abundance of denitrifiers and changed the composition of the denitrifier communities. DEA was strongly and positively correlated with soil C content and was higher in pristine than in fallow or recently cultivated soils. Soil type and the composition of both the nirK- and nirS-type denitrifier communities also influenced DEA. In contrast, other soil characteristics like N content, C:N ratio, and pH did not predict DEA. These findings suggest that due to greater availability of soil organic matter, and hence a more effective N cycling, the natural semiarid grasslands emit more N(2)O than managed lands in Namibia.

摘要

我们研究了纳米比亚东北部卡万戈地区半干旱稀树草原生态系统土壤中的潜在反硝化活性及潜在反硝化菌群落,以帮助预测该地区土地利用持续变化导致的未来一氧化二氮(N₂O)排放变化。土壤类型和土地利用方式(原始、休耕和耕作土壤)影响了与反硝化活性及土壤N₂O通量相关的土壤理化特性,并影响了潜在反硝化活性。通过使用反硝化酶活性(DEA)测定法作为土壤中反硝化活性的指标来评估潜在反硝化活性。土壤类型和土地利用方式影响了土壤的碳和氮含量。从未耕种过的原始土壤碳含量特别高。耕作降低了土壤碳含量和反硝化菌的丰度,并改变了反硝化菌群落的组成。DEA与土壤碳含量呈强正相关,在原始土壤中高于休耕或近期耕作的土壤。土壤类型以及nirK型和nirS型反硝化菌群落的组成也影响了DEA。相比之下,其他土壤特性如氮含量、碳氮比和pH值并不能预测DEA。这些发现表明,由于土壤有机质的可用性更高,因此氮循环更有效,纳米比亚的天然半干旱草原比管理土地排放更多的N₂O。

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