CARBON-ISOTOPE FRACTIONATION DURING GAS-WATER EXCHANGE AND DISSOLUTION OF CO2

被引:317
作者
ZHANG, J
QUAY, PD
WILBUR, DO
机构
[1] School of Oceanography, University of Washington, Seattle
关键词
D O I
10.1016/0016-7037(95)91550-D
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The kinetic and equilibrium fractionation effects for C-13 during CO2 gas transfer (epsilon(k) and epsilon(aq-g)) have been measured in acidified distilled water. The equilibrium fractionation effects between bicarbonate and carbonate and gaseous CO2 (epsilon(HCO3-g) and epsilon(CO3-g) have been measured in NaHCO3 and NaHCO3 + Na2CO3 solutions, respectively, from 5-degrees to 25-degrees-C. The measured fractionations, except epsilon(CO3-g), agreed with earlier work to within 0.2 parts per thousand. epsilon(CO3-g) was about 2 parts per thousand smaller than most values previously reported. The temperature dependence of the fractionation for C-13 between bicarbonate and carbonate and gaseous CO2 was found to be epsilon(HCO3-g) = -(0.141 +/- 0.003)T(degrees-C) + (10.78 +/- 0.05) parts per thousand and epsilon(CO3-g) = -(0.052 +/- 0.03)T(degrees-C) + (7.22 +/- 0.46) parts per thousand, respectively. The fractionation during gas dissolution was epsilon(aq-g) = -(0.0049 +/- 0.003)T(degrees-C) - (1.31 +/- 0.06) parts per thousand and the kinetic effect during gas transfer, epsilon(k), was -0.81 +/- 0.16 parts per thousand at 21-degrees-C and -0.95 +/- 0.20 parts per thousand at 5-degrees-C. The equilibrium fractionation between total DIC in seawater and CO2 in air (epsilon(DIC-g)) was measured and compared with that calculated from the concentration of aqueous CO2, HCO3-, and CO3= and individual fractionations between the three C species and CO2 gas. The measured and calculated results showed a significant difference of up to 0.2 parts per thousand. We hypothesize that carbonate ion complexes likely complicate the calculation of epsilon(DIC-g) from individula C species. We obtain the following empirical function of epsilon(DIC-g) in seawater vs. temperature and the carbonate fraction (fCO3), epsilon(DIC-g) = (0.014 +/- 0.01)Tf(CO-3) - (0.105 +/- 0.002)T + (10.353 +/- 0.05) parts per thousands, when 0.05 < f(CO3) < 0.20 and 5-degrees-C < T < 25-degrees-C.
引用
收藏
页码:107 / 114
页数:8
相关论文
共 27 条
[1]  
Bevington P. R., 2002, DATA REDUCTION ERROR
[2]   CARBON ISOTOPE FRACTIONATION IN SYSTEM CO2(GAS)-CO2(AQUEOUS)-HCO3-(AQUEOUS) [J].
DEUSER, WG ;
DEGENS, ET .
NATURE, 1967, 215 (5105) :1033-&
[3]   CARBON ISOTOPE FRACTIONATION DURING PRECIPITATION OF CALCIUM CARBONATE [J].
EMRICH, K ;
VOGEL, JC .
EARTH AND PLANETARY SCIENCE LETTERS, 1970, 8 (05) :363-&
[4]   ICE CORE RECORD OF THE C-13/C-12 RATIO OF ATMOSPHERIC CO2 IN THE PAST 2 CENTURIES [J].
FRIEDLI, H ;
LOTSCHER, H ;
OESCHGER, H ;
SIEGENTHALER, U ;
STAUFFER, B .
NATURE, 1986, 324 (6094) :237-238
[5]   NEW DETERMINATION OF CARBONIC-ACID DISSOCIATION-CONSTANTS IN SEAWATER AS A FUNCTION OF TEMPERATURE AND SALINITY [J].
GOYET, C ;
POISSON, A .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1989, 36 (11) :1635-1654
[6]  
Harned H. S., 1941, J AM CHEM SOC, V63, P1706, DOI DOI 10.1021/JA01851A058
[7]   The ionization constant of carbonic acid in water and the solubility of carbon dioxide in water and aqueous salt solutions from 0 to 50 degrees [J].
Harned, HS ;
Davis, R .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1943, 65 :2030-2037
[8]   CARBON ISOTOPIC FRACTIONATION DURING THE CO2 EXCHANGE PROCESS BETWEEN AIR AND SEA-WATER UNDER EQUILIBRIUM AND KINETIC CONDITIONS [J].
INOUE, H ;
SUGIMURA, Y .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (11) :2453-2460
[9]   CARBON-DIOXIDE HYDRATION AND DEHYDRATION KINETICS IN SEA-WATER [J].
JOHNSON, KS .
LIMNOLOGY AND OCEANOGRAPHY, 1982, 27 (05) :849-855
[10]  
Keeling C.D., 1989, ASPECTS CLIMATE VARI, V55, P165, DOI [DOI 10.1029/GM055P0165, 10.1029/GM055p0165]