矿化(土壤科学)
氮气循环
氮气
环境化学
环境科学
湿地
土壤水分
营养物
土壤科学
农学
生态学
化学
生物
有机化学
作者
Junhong Bai,Haifeng Gao,Rong Xiao,Junjing Wang,Chen Huang
标识
DOI:10.1002/clen.201200055
摘要
Abstract The availability of soil nutrients can have significant influence on water quality and wetland productivity. Nitrogen mineralization is the important process transferred from organic nitrogen to plant‐available inorganic forms by soil animals and microorganism. Soil nitrogen mineralization processes in coastal wetlands will be greatly impacted by the significant changes of soil water and salt conditions caused by global climate change in the future. However, further studies concerning the effects of water and salt on soil nitrogen mineralization is still needed. The influences of other soil physical–chemical properties and plant community on soil nitrogen mineralization processes are also concluded. The influencing mechanism of soil nitrogen mineralization can be explained using the laboratory incubation, whereas the in situ incubation can contribute to reflecting the real nitrogen mineralization information in the field. The laboratory and in situ incubation methods combined with 15 N tracing‐isotope technique should be combined and applied to better reflect and explain soil nitrogen mineralization processes. Moreover, the applications of modern molecular biology techniques are also very necessary to quantitatively and accurately study nitrogen mineralization.
科研通智能强力驱动
Strongly Powered by AbleSci AI