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  4. Measurement of Attogram Quantities of 231Pa in Dissolved and Particulate Fractions of Seawater by Isotope Dilution Thermal Ionization Mass Spectroscopy
 
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Measurement of Attogram Quantities of 231Pa in Dissolved and Particulate Fractions of Seawater by Isotope Dilution Thermal Ionization Mass Spectroscopy

Journal
Analytical Chemistry
Journal Volume
75
Journal Issue
5
Pages
1075-1079
Date Issued
2003
Date
2003
Author(s)
Shen, Chuan-Chou  
Cheng, Hai
Lawrence Edwards, R.
Bradley Moran, S.
Edmonds, Henrietta N.
Hoff, John A.
Thomas, Rebecca B.
DOI
10.1021/ac026248r
URI
http://ntur.lib.ntu.edu.tw//handle/246246/172683
http://ntur.lib.ntu.edu.tw/bitstream/246246/172683/1/05.pdf
Abstract
A technique has been developed to quantify ultratrace 231Pa (50-2000 ag; 1 ag = 10-18 g) concentrations in seawater using isotope-dilution thermal ionization mass spectrometry (TIMS). The method is a modification of a process developed by Pickett et al. (Pickett, D. A.; Murrell, M. T.; Williams, R. W. Anal. Chem. 1994, 66, 1044-1049) and extends the technique to very low levels of protactinium. The procedural blank is 16 ± 15 ag (2σ), and the ionization efficiency (ions generated/atom loaded) approaches 0.5%. Measurement time is <1 h. The amount of 231Pa needed to produce 231Pa data with an uncertainty of ±4-12% is 100-1000 ag (∼3 × 105 to 3 × 106 atoms). Replicate measurements made on known standards and seawater samples demonstrate that the analytical precision approximates that expected from counting statistics and that, based on detection limits of 38 and 49 ag, protactinium can be detected in a minimum sample size of surface seawater of ∼2 L for suspended particulate matter and <0.1 L for filtered (<0.4 μm) seawater, respectively. The concentration of 231Pa (tens of attograms per liter) can be determined with an uncertainty of ±5-10% (2σ) for suspended particulate matter filtered from 5 to 10 L of seawater. For the dissolved fraction, 0.5-1 L of seawater yields 231Pa measurements with a precision of 1-10%. Sample size requirements are orders of magnitude less than traditional decay-counting techniques and significantly less than previously reported ICP-MS techniques. Our technique can also be applied to other environmental samples, including cave waters, rivers, and igneous rocks.
Subjects
Filtration; Igneous rocks; Ionization; Isotopes; Mass spectrometry; Protactinium; Suspensions (fluids); Thermal ionization mass spectrometry (TIMS); Seawater; isotope; protactinium; sea water; article; dilution; mass spectrometry; particulate matter; statistical analysis; water sampling
Type
journal article
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