We used a newly developed in situ laser Ra
manspectro
meter (LRS) for detection of elevated levels ofdissolved CO
2 in seawater. The experi
ment was carriedout at 500
m depth, 6
mages/entities/deg.gif">C, to exa
mine new protocols fordetection of CO
2-enriched seawater e
manating fro
m a liquidCO
2 source in the ocean, and to deter
mine currentdetection li
mits under field conditions. A syste
m of twointerconnected 5 L cha
mbers was built, with flow betweenthe
m controlled by a valve and pu
mp syste
m, and thisunit was
mounted on an ROV. The first cha
mber was fittedwith a pH electrode and the optical probe of the LRS. Inthe second cha
mber ~580
mL of liquid CO
2 was introduced.Dissolution of CO
2 across the CO
2-seawater interfacethen occurred, the valves were opened, and a fixed volu
meof low-pH/CO
2-enriched seawater was transferred to thefirst cha
mber for co
mbined pH/Ra
man sensing, where weesti
mate a
mean dissolution rate of ~0.5 (
mages/entities/
mgr.gif">
mol/c
m2)/s.This sequence was repeated, resulting in
measure
ment ofa progressively CO
2 enriched seawater sa
mple. Therapid in-growth of CO
2 was readily detected as the Fer
midyad of the dissolved state with a detection li
mit of~10
mM with spectral acquisition ti
mes of 150 s. Thedetection of background levels of CO
2 species in seawater(~2.2
mM, do
minantly HCO
3-) will require an i
mprove
mentin instru
ment sensitivity by a factor of 5-10, whichcould be obtained by the use of a liquid core waveguide.