An S, Gardner W S, Kana T
Marine Science Institute, University of Texas at Austin, Port Aransas, Texas 78373, USA.
Appl Environ Microbiol. 2001 Mar;67(3):1171-8. doi: 10.1128/AEM.67.3.1171-1178.2001.
A method for estimating denitrification and nitrogen fixation simultaneously in coastal sediments was developed. An isotope-pairing technique was applied to dissolved gas measurements with a membrane inlet mass spectrometer (MIMS). The relative fluxes of three N(2) gas species ((28)N(2), (29)N(2), and (30)N(2)) were monitored during incubation experiments after the addition of (15)NO(3)(-). Formulas were developed to estimate the production (denitrification) and consumption (N(2) fixation) of N(2) gas from the fluxes of the different isotopic forms of N(2). Proportions of the three isotopic forms produced from (15)NO(3)(-) and (14)NO(3)(-) agreed with expectations in a sediment slurry incubation experiment designed to optimize conditions for denitrification. Nitrogen fixation rates from an algal mat measured with intact sediment cores ranged from 32 to 390 microg-atoms of N m(-2) h(-1). They were enhanced by light and organic matter enrichment. In this environment of high nitrogen fixation, low N(2) production rates due to denitrification could be separated from high N(2) consumption rates due to nitrogen fixation. Denitrification and nitrogen fixation rates were estimated in April 2000 on sediments from a Texas sea grass bed (Laguna Madre). Denitrification rates (average, 20 microg-atoms of N m(-2) h(-1)) were lower than nitrogen fixation rates (average, 60 microg-atoms of N m(-2) h(-1)). The developed method benefits from simple and accurate dissolved-gas measurement by the MIMS system. By adding the N(2) isotope capability, it was possible to do isotope-pairing experiments with the MIMS system.
开发了一种同时估算沿海沉积物中反硝化作用和固氮作用的方法。采用同位素配对技术,通过膜进样质谱仪(MIMS)对溶解气体进行测量。在添加(^{15}NO_3^-)后的培养实验中,监测了三种(N_2)气体种类((^{28}N_2)、(^{29}N_2)和(^{30}N_2))的相对通量。根据不同同位素形式(N_2)的通量,推导出了估算(N_2)气体产生(反硝化作用)和消耗(固氮作用)的公式。在旨在优化反硝化条件的沉积物浆液培养实验中,由(^{15}NO_3^-)和(^{14}NO_3^-)产生的三种同位素形式的比例与预期相符。使用完整沉积物岩芯测量的藻席固氮率范围为(32)至(390)微克原子(N)·(m^{-2})·(h^{-1})。光照和有机物质富集可提高固氮率。在这种高固氮环境中,可将反硝化作用导致的低(N_2)产生率与固氮作用导致的高(N_2)消耗率区分开来。2000年4月,对得克萨斯州海草床(拉古纳马德雷)的沉积物估算了反硝化作用和固氮作用速率。反硝化作用速率(平均为(20)微克原子(N)·(m^{-2})·(h^{-1}))低于固氮作用速率(平均为(60)微克原子(N)·(m^{-2})·(h^{-1}))。所开发的方法受益于MIMS系统简单而准确的溶解气体测量。通过增加(N_2)同位素功能,可使用MIMS系统进行同位素配对实验。