Accurate measurement of O2, N2, and Ar gases in water and the solubility of N2

被引:122
作者
Emerson, S [1 ]
Stump, C [1 ]
Wilbur, D [1 ]
Quay, P [1 ]
机构
[1] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA
关键词
gas saturation; mass spectrometry; analytical methods; accuracy; precision;
D O I
10.1016/S0304-4203(98)00090-5
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The degree of atmospheric saturation for O-2, Ar, and N-2 gases in water can be determined to accuracies of +/- 0.1-0.3% using mass spectrometry to determine the gas ratios and Winkler titrations for oxygen analysis. We describe methods used to obtain this level of accuracy and precision. Oxygen accuracy of +/-0.1% can be obtained by careful attention to standardization using KIO3 standards that have been corrected for impurities. Accurate O-2/Ar and O-2/N-2 gas ratios (+/-0.1-0.2%) are obtainable by measuring the mass ratios against the atmosphere if the effect of different gas concentrations on the performance of the mass spectrometer are taken into account. Oxygen and argon saturation values have been determined previously to accuracies of less than or equal to +/-0.1%, but published estimates of the saturation value for nitrogen differ by more than 1%. We have redetermined the N-2 saturation value at 19 degrees C and zero salinity to be 0.92% greater than the results reported in the work of Weiss (1970). (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:337 / 347
页数:11
相关论文
共 19 条
[1]   A HIGH-PRECISION ISOTOPE RATIO MASS-SPECTROMETRY METHOD FOR MEASURING THE O-2 N-2 RATIO OF AIR [J].
BENDER, ML ;
TANS, PP ;
ELLIS, JT ;
ORCHARDO, J ;
HABFAST, K .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1994, 58 (21) :4751-4758
[2]   THE CONCENTRATION AND ISOTOPIC FRACTIONATION OF OXYGEN DISSOLVED IN FRESH-WATER AND SEAWATER IN EQUILIBRIUM WITH THE ATMOSPHERE [J].
BENSON, BB ;
KRAUSE, D .
LIMNOLOGY AND OCEANOGRAPHY, 1984, 29 (03) :620-632
[3]   EMPIRICAL LAWS FOR DILUTE AQUEOUS-SOLUTIONS OF NONPOLAR GASES [J].
BENSON, BB ;
KRAUSE, D .
JOURNAL OF CHEMICAL PHYSICS, 1976, 64 (02) :689-709
[4]  
CARPENTER JAMES H., 1965, LIMNOL OCEANOGR, V10, P141
[5]  
CARRITT DE, 1966, J MAR RES, V24, P286
[6]   OXYGEN SUPERSATURATION IN THE OCEAN - BIOLOGICAL VERSUS PHYSICAL CONTRIBUTIONS [J].
CRAIG, H ;
HAYWARD, T .
SCIENCE, 1987, 235 (4785) :199-202
[7]   Experimental determination of the organic carbon flux from open-ocean surface waters [J].
Emerson, S ;
Quay, P ;
Karl, D ;
Winn, C ;
Tupas, L ;
Landry, M .
NATURE, 1997, 389 (6654) :951-954
[8]   CHEMICAL TRACERS OF PRODUCTIVITY AND RESPIRATION IN THE SUBTROPICAL PACIFIC-OCEAN [J].
EMERSON, S ;
QUAY, PD ;
STUMP, C ;
WILBUR, D ;
SCHUDLICH, R .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1995, 100 (C8) :15873-15887
[9]   O-2, Ar, N-2, AND Rn-222 IN SURFACE WATERS OF THE SUBARCTIC OCEAN: NET BIOLOGICAL O-2 PRODUCTION [J].
Emerson, Steven ;
Quay, Paul ;
Stump, Charles ;
Wilbur, David ;
Knox, Molly .
GLOBAL BIOGEOCHEMICAL CYCLES, 1991, 5 (01) :49-69
[10]   EVIDENCE FOR THE IMPORTANCE OF BUBBLES IN INCREASING AIR SEA GAS FLUX [J].
FARMER, DM ;
MCNEIL, CL ;
JOHNSON, BD .
NATURE, 1993, 361 (6413) :620-623