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Chinese Academy of Sciences Institutional Repositories Grid
Heterotrophic nitrification is the predominant NO3- production mechanism in coniferous but not broad-leaf acid forest soil in subtropical China

文献类型:期刊论文

作者Zhang, Jinbo1; Mueller, Christoph2; Zhu, Tongbin1; Cheng, Yi1; Cai, Zucong1
刊名BIOLOGY AND FERTILITY OF SOILS
出版日期2011-07-01
卷号47期号:5页码:533-542
关键词N-15 tracing technique Model Labile and recalcitrant organic N Gross N transformation Heterotrophic nitrification
ISSN号0178-2762
DOI10.1007/s00374-011-0567-z
通讯作者Cai, Zucong(zccai@mail.issas.ac.cn)
英文摘要A study was carried out to investigate the potential gross nitrogen (N) transformations in natural secondary coniferous and evergreen broad-leaf forest soils in subtropical China. The simultaneously occurring gross N transformations in soil were quantified by a N-15 tracing study. The results showed that N dynamics were dominated by NH4+ turnover in both soils. The total mineralization (from labile and recalcitrant organic N) in the broad-leaf forest was more than twice the rate in the coniferous forest soil. The total rate of mineral N production (NH4+ + NO3-) from the large recalcitrant organic N pool was similar in the two forest soils. However, appreciable NO3- production was only observed in the coniferous forest soil due to heterotrophic nitrification (i.e. direct oxidation of organic N to NO3-), whereas nitrification in broad-leaf forest was little (or negligible). Thus, a distinct shift occurred from predominantly NH4+ production in the broad-leaf forest soil to a balanced production of NH4+ and NO3- in the coniferous forest soil. This may be a mechanism to ensure an adequate supply of available mineral N in the coniferous forest soil and most likely reflects differences in microbial community patterns (possibly saprophytic, fungal, activities in coniferous soils). We show for the first time that the high nitrification rate in these soils may be of heterotrophic rather than autotrophic nature. Furthermore, high NO3- production was only apparent in the coniferous but not in broad-leaf forest soil. This highlights the association of vegetation type with the size and the activity of the SOM pools that ultimately determines whether only NH4+ or also a high NO3- turnover is present.
收录类别SCI
WOS关键词ANALYZE N TRANSFORMATIONS ; GROSS NITROGEN TRANSFORMATIONS ; CHILEAN NOTHOFAGUS FOREST ; OLD GRASSLAND SOIL ; N-15 TRACING MODEL ; RETENTION PROCESSES ; PLANTATION FORESTS ; AMMONIA OXIDATION ; TROPICAL FOREST ; POOL DILUTION
WOS研究方向Agriculture
WOS类目Soil Science
语种英语
WOS记录号WOS:000292972400006
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2558893
专题南京土壤研究所
通讯作者Cai, Zucong
作者单位1.Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
2.Univ Giessen, Dept Plant Ecol, D-35392 Giessen, Germany
推荐引用方式
GB/T 7714
Zhang, Jinbo,Mueller, Christoph,Zhu, Tongbin,et al. Heterotrophic nitrification is the predominant NO3- production mechanism in coniferous but not broad-leaf acid forest soil in subtropical China[J]. BIOLOGY AND FERTILITY OF SOILS,2011,47(5):533-542.
APA Zhang, Jinbo,Mueller, Christoph,Zhu, Tongbin,Cheng, Yi,&Cai, Zucong.(2011).Heterotrophic nitrification is the predominant NO3- production mechanism in coniferous but not broad-leaf acid forest soil in subtropical China.BIOLOGY AND FERTILITY OF SOILS,47(5),533-542.
MLA Zhang, Jinbo,et al."Heterotrophic nitrification is the predominant NO3- production mechanism in coniferous but not broad-leaf acid forest soil in subtropical China".BIOLOGY AND FERTILITY OF SOILS 47.5(2011):533-542.

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来源:南京土壤研究所

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