期刊
ANALYTICAL CHEMISTRY
卷 85, 期 14, 页码 6661-6666出版社
AMER CHEMICAL SOC
DOI: 10.1021/ac400351c
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资金
- NSF [1155666]
- NASA [NNX09AE45G S05]
- Old Dominion University Department of Ocean, Earth and Atmospheric Sciences Jacques S. Zaneveld Endowed Scholarship
- Directorate For Geosciences
- Division Of Ocean Sciences [1155666] Funding Source: National Science Foundation
- Directorate For Geosciences
- Division Of Ocean Sciences [1155566] Funding Source: National Science Foundation
Recent studies suggest that cyanate (OCN-) is a potentially important source of reduced nitrogen (N) available to support the growth of aquatic microbes and, thus, may play a role in aquatic N cycling. However, aquatic OCN- distributions have not been previously described because of the lack of a suitable assay for measuring OCN- concentrations in natural waters. Previous methods were designed to quantify OCN- in aqueous samples with much higher reduced N concentrations (micromolar levels) than those likely to be found in natural waters (nanomolar levels). We have developed a method to quantify OCN- in dilute, saline environments. In the method described here, OCN- in aqueous solution reacts with 2-aminobenzoic acid to produce a highly fluorescent derivative, 2,4-quinazolinedione, which is then quantified using high performance liquid chromatography. Derivatization conditions were optimized to simultaneously minimize the reagent blank and maximize 2,4-quinazolinedione formation (>90% reaction yield) in estuarine and seawater matrices. A limit of detection (LOD) of 0.4 nM was achieved with only minor matrix effects. We applied this method to measure OCN- concentrations in estuarine and seawater samples from the Chesapeake Bay and coastal waters from the mid-Atlantic region. OCN- concentrations ranged from 0.9 to 41 nM. We determined that OCN- concentrations were stable in 0.2 mu m filtered seawater samples stored at -80 degrees C for up to nine months.
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