Lcation

DNRA contribution to total ${\text{NO}}_3^{-}$ reduction (%)

reference

氮源缺乏的热带雨林

75%~99%

Huygens et al., 2007 [30]

人工淡水湿地

5%~15%

Scott et al., 2008 [40]

低洼的湖泊

3%~15%

Nizzoli et al., 2010 [31]

海底底泥

80%~100%

Karlson et al., 2005 [46]

大陆架

<0.02%

Trimmer and Nicholls, 2009 [47]

海湾

43%~68%

4%~11%

Gardner et al., 2006 [48]

Hou et al., 2012 [49]

土壤

16.7%~92.9%

Chen et al., 2015 [32] [36]

厌氧酸化反应器

14.5%~56.3%

Xie et al., 2015 [42]

河底底泥

3%~45%

邓峰煜，2016 [29]

氮缺乏的活性污泥系统

12%~13%

张新艳，2014 [1]

红树林

12%~99%

Fernandes et al., 2012 [50] ; Molnal et al., 2013 [51]

中国东海大陆架

26 (20~31)

Song et al., 2013 [52]

中碱性大米田地

98

Zhang et al., 2015 [34]

湖泊底泥

98

Gilbert et al., 1997 [53]

河口

11~91

Dong et al., 2009, 2011 [54] [55]