TY - JOUR
T1 - The Role of pH Measurements in Modern Oceanic COsub2/sub-system Characterizations: Precision and Thermodynamic Consistency
AU - Clayton, Tonya D.
AU - Byrne, Robert H.
AU - Breland, Jabe A.
AU - Feely, Richard A.
AU - Millero, Frank J.
AU - Campbell, Douglas M.
AU - Murphy, Paulette P.
AU - Lamb, Marilyn F.
PY - 1995/1/1
Y1 - 1995/1/1
N2 - In May 1992, surface seawater samples were collected along an equatorial transit (130 to 100°W) and analyzed for total hydrogen ion concentration (expressed as spectrophotometric pH T ) total dissolved inorganic carbon (coulometric C T ), and total alkalinity (potentiometric A T and spectrophotometric A T ). This data set, which presents a striking view of the chemical signature of tropical instability waves, is also unusual in that its “overdetermination” of the CO 2 -system in seawater includes both potentiometric A T data and the first spectrophotometric A T data collected at sea using a double-wavelength, one-step acid addition method. Our data set indicates that spectrophotometric A T measurements ( A Tspec ) are both precise (±1.8 μmol/kg) and accurate; the mean observed difference between A Tspec and A T obtained potentiometrically in this study ( A Tpot ) is 1 μmol/kg. As only two of the three measured parameters are required to characterize the CO 2 -system in seawater, this analytical redundancy of our analyses ( C T , A T , pH) afforded an opportunity to evaluate, in terms of thermodynamic consistency, a recent calibration of m -cresol purple, a pH indicator. Using various carbonic acid dissociation constants, measured parameters were combined in pairs ( C T - A T , pH- C T , and pH- A T ) to calculate a third parameter for comparison with the shipboard measurements. Depending on the selected set of carbonic acid dissociation constants, the average offset between directly measured and predicted values of A T and C T was as small as ±1 μmol/kg. The results of this study indicate that the present 25°C m CP calibration, paired with the 25°C combined dissociation constants of Hansson and Mehrbach, produces accurate predictions of A T and C T . Extensive replication of the shipboard spectrophotometric measurements made it possible to examine directly the sensitivity of derived parameters to variations or errors in input A T and pH. In accord with earlier theoretical treatments of this question, the results presented demonstrate that pH is imprecisely predicted from A T and C T , whereas imprecision in measured pH—at the level typical of spectrophotometric measurements (±0.0004)—contributes negligibly (±0.3 μmol/kg) to imprecision in derived A T and C T . In view of the high precision of pH Tspec measurements and both the precision and reliability of C T measurements (supported by the use of certified SIO reference materials) pH Tspec and C Tcoul constitute a particularly useful pair of parameters for shipboard study of the oceanic carbon dioxide system. The results indicate, as well, that the A T -pH Tspec pairing is of particular interest in ocean regions where simple A T vs salinity relationships are observed. In light of recent advances, the role of pH measurements in CO 2 -system characterizations should be re-evaluated. Spectrophotometric measurements of pH have much to contribute in documenting the oceans' evolving response to anthropogenic C0 2 .
AB - In May 1992, surface seawater samples were collected along an equatorial transit (130 to 100°W) and analyzed for total hydrogen ion concentration (expressed as spectrophotometric pH T ) total dissolved inorganic carbon (coulometric C T ), and total alkalinity (potentiometric A T and spectrophotometric A T ). This data set, which presents a striking view of the chemical signature of tropical instability waves, is also unusual in that its “overdetermination” of the CO 2 -system in seawater includes both potentiometric A T data and the first spectrophotometric A T data collected at sea using a double-wavelength, one-step acid addition method. Our data set indicates that spectrophotometric A T measurements ( A Tspec ) are both precise (±1.8 μmol/kg) and accurate; the mean observed difference between A Tspec and A T obtained potentiometrically in this study ( A Tpot ) is 1 μmol/kg. As only two of the three measured parameters are required to characterize the CO 2 -system in seawater, this analytical redundancy of our analyses ( C T , A T , pH) afforded an opportunity to evaluate, in terms of thermodynamic consistency, a recent calibration of m -cresol purple, a pH indicator. Using various carbonic acid dissociation constants, measured parameters were combined in pairs ( C T - A T , pH- C T , and pH- A T ) to calculate a third parameter for comparison with the shipboard measurements. Depending on the selected set of carbonic acid dissociation constants, the average offset between directly measured and predicted values of A T and C T was as small as ±1 μmol/kg. The results of this study indicate that the present 25°C m CP calibration, paired with the 25°C combined dissociation constants of Hansson and Mehrbach, produces accurate predictions of A T and C T . Extensive replication of the shipboard spectrophotometric measurements made it possible to examine directly the sensitivity of derived parameters to variations or errors in input A T and pH. In accord with earlier theoretical treatments of this question, the results presented demonstrate that pH is imprecisely predicted from A T and C T , whereas imprecision in measured pH—at the level typical of spectrophotometric measurements (±0.0004)—contributes negligibly (±0.3 μmol/kg) to imprecision in derived A T and C T . In view of the high precision of pH Tspec measurements and both the precision and reliability of C T measurements (supported by the use of certified SIO reference materials) pH Tspec and C Tcoul constitute a particularly useful pair of parameters for shipboard study of the oceanic carbon dioxide system. The results indicate, as well, that the A T -pH Tspec pairing is of particular interest in ocean regions where simple A T vs salinity relationships are observed. In light of recent advances, the role of pH measurements in CO 2 -system characterizations should be re-evaluated. Spectrophotometric measurements of pH have much to contribute in documenting the oceans' evolving response to anthropogenic C0 2 .
UR - https://digitalcommons.usf.edu/msc_facpub/1616
UR - https://doi.org/10.1016/0967-0645(95)00028-O
U2 - 10.1016/0967-0645(95)00028-O
DO - 10.1016/0967-0645(95)00028-O
M3 - Article
VL - 42
JO - Deep Sea Research Part II: Topical Studies in Oceanography
JF - Deep Sea Research Part II: Topical Studies in Oceanography
ER -