Composition of Dissolved Organic Nitrogen in Continental Precipitation Investigated by Ultra-High Resolution FT-ICR Mass Spectrometry

被引:92
作者
Altieri, Katye E. [1 ]
Turpin, Barbara J. [2 ]
Seitzinger, Sybil P. [1 ,3 ]
机构
[1] Rutgers State Univ, Inst Marine & Coastal Sci, New Brunswick, NJ 08901 USA
[2] Rutgers State Univ, Dept Environm Sci, New Brunswick, NJ 08901 USA
[3] Rutgers State Univ, Rutgers NOAA CMER Program, New Brunswick, NJ 08901 USA
基金
美国国家科学基金会;
关键词
FREE AMINO-ACIDS; ATMOSPHERIC INPUTS; NORTH-CAROLINA; RAINWATER; DEPOSITION; AEROSOL; CALIFORNIA; SPECIATION; CHEMISTRY; OXIDATION;
D O I
10.1021/es9007849
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The atmospheric transport of fixed nitrogen (N) is a critical component of the global N cycle that has been heavily impacted by human activities. It has been shown that organic N is an important contributor to atmospheric N, but its sources and composition are largely unknown. Rainwater samples collected in New Jersey were analyzed by negative and positive ion ultrahigh-resolution electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS). Elemental compositions of 402 N-containing compounds were determined and five main groups of compound classes were identified: compounds containing carbon, hydrogen, oxygen, and N detected as positive ions (CHON+), compounds containing CHON detected as negative ions(CHON-), compounds containing CHN detected as positive ions (CHN+), and CHON compounds that contain sulfur (S) detected as both positive and negative ions (CHONS+, CHONS-, respectively). The CHON+ compound class has the largest number of compounds detected (i.e., 281), with the majority, i.e., 207, containing only one N atom. The elemental ratios of these compounds and their detection in the positive ion mode suggest that they are compounds with reduced N functionality. Known contributors to secondary organic aerosol with anthropogenic sources were also identified including organonitrate compounds and nitrooxy organosulfates.
引用
收藏
页码:6950 / 6955
页数:6
相关论文
共 40 条
[1]   Oligomers formed through in-cloud methylglyoxal reactions: Chemical composition, properties, and mechanisms investigated by ultra-high resolution FT-ICR mass spectrometry [J].
Altieri, K. E. ;
Seitzinger, S. P. ;
Carlton, A. G. ;
Turpin, B. J. ;
Klein, G. C. ;
Marshall, A. G. .
ATMOSPHERIC ENVIRONMENT, 2008, 42 (07) :1476-1490
[2]   Oligomers, organosulfates, and nitrooxy organosulfates in rainwater identified by ultra-high resolution electrospray ionization FT-ICR mass spectrometry [J].
Altieri, K. E. ;
Turpin, B. J. ;
Seitzinger, S. P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (07) :2533-2542
[3]  
[Anonymous], J GEOPHYS RES
[4]   Rainwater monocarboxylic and dicarboxylic acid concentrations in southeastern North Carolina, USA, as a function of air-mass back-trajectory [J].
Avery, GB ;
Kieber, RJ ;
Witt, M ;
Willey, JD .
ATMOSPHERIC ENVIRONMENT, 2006, 40 (09) :1683-1693
[5]  
Bigelow D.S., 2001, Instruction Manual NADP/NTN site selection and installation
[6]   Hygroscopicity of water-soluble organic compounds in atmospheric aerosols: Amino acids and biomass burning derived organic species [J].
Chan, MN ;
Choi, MY ;
Ng, NL ;
Chan, CK .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2005, 39 (06) :1555-1562
[7]   ATMOSPHERIC INPUTS OF DISSOLVED ORGANIC NITROGEN TO THE OCEANS [J].
CORNELL, S ;
RENDELL, A ;
JICKELLS, T .
NATURE, 1995, 376 (6537) :243-246
[8]   Organic nitrogen in Hawaiian rain and aerosol [J].
Cornell, S ;
Mace, K ;
Coeppicus, S ;
Duce, R ;
Huebert, B ;
Jickells, T ;
Zhuang, LZ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D8) :7973-7983
[9]   Water-soluble organic nitrogen in atmospheric aerosol: a comparison of UV and persulfate oxidation methods [J].
Cornell, SE ;
Jickells, TD .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (05) :833-840
[10]   Organic nitrogen deposition on land and coastal environments: a review of methods and data [J].
Cornell, SE ;
Jickells, TD ;
Cape, JN ;
Rowland, AP ;
Duce, RA .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (16) :2173-2191