Simultaneous spectrophotometric flow-through measurements of pH, carbon dioxide fugacity, and total inorganic carbon in seawater

被引:66
作者
Wang, Zhaohui Aleck
Liu, Xuewu
Byrne, Robert H.
Wanninkhof, Rik
Bernstein, Renate E.
Kaltenbacher, Eric A.
Patten, James
机构
[1] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA
[2] NOAA, Atlantic Oceanog & Meteorol Lab, Ocean Chem Div, Miami, FL 33149 USA
基金
美国海洋和大气管理局;
关键词
autonomous carbon measurements; spectrophotometric; carbon dioxide; pH; fugacity; dissolved inorganic carbon;
D O I
10.1016/j.aca.2007.05.048
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
An autonomous multi-parameter flow-through CO, system has been developed to simultaneously measure surface seawater pH, carbon dioxide fugacity (fCO(2)), and total dissolved inorganic carbon (DIC). All three measurements are based on spectrophotometric determinations of solution pH at multiple wavelengths using sulfonephthalein indicators. The pH optical cell is machined from a PEEK polymer rod bearing a bore-hole with an optical pathlength of similar to 15 cm. The fCO(2), optical cell consists of Teflon AF 2400 (DuPont) capillary tubing sealed within the bore-hole of a PEEK rod. This Teflon AF tubing is filled with a standard indicator solution with a fixed total alkalinity, and forms a liquid core waveguide (LCW). The LCW functions as both a long pathlength (similar to 15 cm) optical cell and a membrane that equilibrates the internal standard solution with external seawater. fCO(2), is then determined by measuring the pH of the internal solution. DIC is measured by determining the pH of standard internal solutions in equilibrium with seawater that has been acidified to convert all forms of DIC to CO2. The system runs repetitive measurement cycles with a sampling frequency of similar to 7 samples (21 measurements) per hour. The system was used for underway measurements of sea surface pH, fCO(2), and DIC during the CLIVAR/CO2, A16S cruise in the South Atlantic Ocean in 2005. The field precisions were evaluated to be 0.0008 units for pH, 0.9 mu atm for fCO(2), and 2.4 mu mol kg(-1) for DIC. These field precisions are close to those obtained in the laboratory. Direct comparison of our measurements and measurements obtained using established standard methods revealed that the system achieved field agreements of 0.0012 +/- 0.0042 units for pH, 1.0 +/- 2.5 mu atm for fCO(2), and 2.2 +/- 6.0 mu mol kg(-1) for DIC. This system integrates spectrophotometric measurements of multiple CO2 parameters into a single package suitable for observations of both seawater and freshwater. (c) 2007 Elsevier B.V. All rights reserved.
引用
收藏
页码:23 / 36
页数:14
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