G2TT
来源类型Monograph (IIASA Interim Report)
规范类型报告
Nitrogen dynamics in Turbic Cryosols from Siberia and Greenland.
Wild B; Schnecker J; Barta J; Capek P; Guggenberger G; Hofhansl F; Kaiser C; Lashchinsky N
发表日期2013
出版者IIASA, Laxenburg, Austria: IR-13-074
出版年2013
语种英语
摘要Turbic Cryosols (permafrost soils characterized by cryoturbation, i.e., by mixing of soil layers due to freezing and thawing) are widespread across the Arctic, and contain large amounts of poorly decomposed organic material buried in the subsoil. This cryoturbated organic matter exhibits retarded decomposition compared to organic material in the topsoil. Since soil organic matter (SOM decomposition is known to be tightly linked to N availability, we investigated N transformation rates in different soil horizons of three tundra sites in north-eastern Siberia and Greenland. We measurd gross rates of protein depolymerization, N mineralization (ammonification) and nitrification, as well as microbial uptake of amino acids and NH4^+ using an array of ^15N pool dilution approaches. We found that all sites and horizons were characterized by low N availability, as indicated by low N mineralization compared to protein depolymerization rates (with gross N mineralization accounting on average for 14% of gross protein depolymerization). The proportion of organic N mineralized was significantly higher at the Greenland than at the Siberian 44 sites, suggesting differences in N limitation. The proportion of organic N mineralized, however, did not differ significantly between soil horizons, pointing to a similar N demand of the microbial community of each horizon. In contrast, absolute transformation rates were significantly lower in cryoturbated than in organic horizons, with cryoturbated horizons reaching not more than 32% of the transformation rates in organic horizons. Our results thus indicate a deceleration of the entire N cycle in cryoturbated soil horizons, especially strongly reduced rates of protein depolymerization (16% of organic horizons) which is cosidred the rate-limiting step in soil N cycling.
主题Evolution and Ecology (EEP)
关键词Arctic tundra cryoturbation soil organic matter ecological stoichiometry nitrogen transformation protein depolymerazation nitrogen mineralization nitrification nitrogen availability
URLhttp://pure.iiasa.ac.at/id/eprint/10693/
来源智库International Institute for Applied Systems Analysis (Austria)
资源类型智库出版物
条目标识符http://119.78.100.153/handle/2XGU8XDN/125919
推荐引用方式
GB/T 7714
Wild B,Schnecker J,Barta J,et al. Nitrogen dynamics in Turbic Cryosols from Siberia and Greenland.. 2013.
条目包含的文件
文件名称/大小 资源类型 版本类型 开放类型 使用许可
IR-13-074.pdf(331KB)智库出版物 限制开放CC BY-NC-SA浏览
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Wild B]的文章
[Schnecker J]的文章
[Barta J]的文章
百度学术
百度学术中相似的文章
[Wild B]的文章
[Schnecker J]的文章
[Barta J]的文章
必应学术
必应学术中相似的文章
[Wild B]的文章
[Schnecker J]的文章
[Barta J]的文章
相关权益政策
暂无数据
收藏/分享
文件名: IR-13-074.pdf
格式: Adobe PDF
此文件暂不支持浏览

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。