R. Wanninkhof et K. Thoning, MEASUREMENT OF FUGACITY OF CO2 IN SURFACE-WATER USING CONTINUOUS AND DISCRETE SAMPLING METHODS, Marine chemistry, 44(2-4), 1993, pp. 189-204
Instrumentation and methodology is described which is used for measure
ment of the fugacity (or partial pressure) of carbon dioxide (fCO(2) o
r pCO(2)) in surface seawater. Two separate instruments were developed
for the measurements. One is an underway system which measures the mi
xing ratio of CO2, XCO(2), in a headspace in equilibrium with surface
seawater continuously pumped into a 24 1 equilibration chamber. The ot
her is a discrete system in which 460 mi aliquots of water are equilib
rated with a 120 mi headspace. Both systems use a non-dispersive infra
red analyzer as detector. In the underway instrument the average XCO(2
) in the headspace of an equilibration chamber is measured at near in-
situ temperature over 20 min each hour. At a cruising speed of 13 knot
s this translates into a space averaged fCO(2) value over 8 km. The un
derway system is ideally suited for mapping of the surface water fugac
ity over large geographic regions. Samples from the discrete instrumen
t are analyzed at 20 degrees C. The primary function of the system is
for measurement of subsurface fCO(2) values. The discrete system is al
so well suited for determining the relationship between the fugacity o
f CO2 and other (carbon) parameters sub-sampled from the same aliquot.
To calculate the fCO(2) in water for in-situ conditions from the mixi
ng ratio in the headspace of the flask of the discrete system, small c
arbon mass balance and, sometimes significant, temperature corrections
have to be applied. Comparison of 100 surface values obtained in the
South Atlantic using the underway and discrete systems shows that the
average difference of pCO(2) values for the two systems ranges from -4
.3 mu atm to -8.6 mu atm, depending on the temperature correction, wit
h a standard deviation of 4 mu atm. The differences show scatter of up
the 15 mu atm which we attribute to a mismatch between the point samp
les for the discrete system and the integrated samples for the underwa
y system.