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A Mass Spectrometric System for the Analysis of Noble Gases and Tritium from Water Samples

Urs Beyerle, Werner Aeschbach, Dieter M. Imboden, H. Baur, T. Graf, Rolf Kipfer

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Abstract

The design, setup, and performance of a mass spectrometric system for the analysis of noble gas isotopes ( 3 He, 4 He, 20 Ne, 21 Ne, 22 Ne, 36 Ar, 40 Ar, 84 Kr, 136 Xe) and tritium ( 3 H) from water samples are described. The 3 H concentration is measured indirectly by the 3 He ingrowth from radioactive decay. After extraction, purification, and separation, the noble gases are measured in two noncommercial double-collector 90° magnetic sector mass spectrometers. We present a new approach for the analysis of the heavy noble gas isotopes that enables, in principle, simultaneous measurement of Ar, Kr, and Xe. Typical precisions of the measurements of 3 H, He, Ne, Ar, Kr, and Xe concentrations are ±2.7%, ±0.3%, ±0.9%, ±0.3%, ±0.8%, and ±1.0%, respectively. For the isotopic ratios 3 He/ 4 He, 20 Ne/ 22 Ne, and 40 Ar/ 36 Ar the typical precisions are ±0.7%, ±0.3%, and ±0.2%. These values express the reproducibility of the measurement of an internal freshwater standard and include the overall stability of the system as well as of the extraction procedure. To verify the method, the noble gas concentrations of air-saturated water samples prepared under controlled conditions are compared with noble gas solubility data. The 20 Ne/ 22 Ne and 36 Ar/ 40 Ar fractionation during solution is estimated from 70 surface water samples to be −2.0 ± 0.2‰ and −1.3 ± 0.2‰, respectively.

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What this paper is about

The design, setup, and performance of a mass spectrometric system for the analysis of noble gas isotopes ( 3 He, 4 He, 20 Ne, 21 Ne, 22 Ne, 36 Ar, 40 Ar, 84 Kr, 136 Xe) and tritium ( 3 H) from water samples are described. The 3 H concentration is measured indirectly by the 3 He ingrowth from radioactive decay. After extraction, purification, and separation, the noble gases are measured in two noncommercial double-collector 90° magnetic sector mass spectrometers. We present a new approach for the analysis of the heavy noble gas isotopes that enables, in principle, simultaneous measurement of Ar, Kr, and Xe. Typical precisions of the measurements of 3 H, He, Ne, Ar, Kr, and Xe concentrations are ±2.7%, ±0.3%, ±0.9%, ±0.3%, ±0.8%, and ±1.0%, respectively. For the isotopic ratios 3 He/ 4 He, 20 Ne/ 22 Ne, and 40 Ar/ 36 Ar the typical precisions are ±0.7%, ±0.3%, and ±0.2%. These values express the reproducibility of the measurement of an internal freshwater standard and include the overall stability of the system as well as of the extraction procedure. To verify the method, the noble gas concentrations of air-saturated water samples prepared under controlled conditions are compared with noble gas solubility data. The 20 Ne/ 22 Ne and 36 Ar/ 40 Ar fractionation during solution is estimated from 70 surface water samples to be −2.0 ± 0.2‰ and −1.3 ± 0.2‰, respectively.

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Available abstract

The design, setup, and performance of a mass spectrometric system for the analysis of noble gas isotopes ( 3 He, 4 He, 20 Ne, 21 Ne, 22 Ne, 36 Ar, 40 Ar, 84 Kr, 136 Xe) and tritium ( 3 H) from water samples are described. The 3 H concentration is measured indirectly by the 3 He ingrowth from radioactive decay. After extraction, purification, and separation, the noble gases are measured in two noncommercial double-collector 90° magnetic sector mass spectrometers. We present a new approach for the analysis of the heavy noble gas isotopes that enables, in principle, simultaneous measurement of Ar, Kr, and Xe. Typical precisions of the measurements of 3 H, He, Ne, Ar, Kr, and Xe concentrations are ±2.7%, ±0.3%, ±0.9%, ±0.3%, ±0.8%, and ±1.0%, respectively. For the isotopic ratios 3 He/ 4 He, 20 Ne/ 22 Ne, and 40 Ar/ 36 Ar the typical precisions are ±0.7%, ±0.3%, and ±0.2%. These values express the reproducibility of the measurement of an internal freshwater standard and include the overall stability of the system as well as of the extraction procedure. To verify the method, the noble gas concentrations of air-saturated water samples prepared under controlled conditions are compared with noble gas solubility data. The 20 Ne/ 22 Ne and 36 Ar/ 40 Ar fractionation during solution is estimated from 70 surface water samples to be −2.0 ± 0.2‰ and −1.3 ± 0.2‰, respectively.

Key concepts: Noble gas, Mass spectrometry, Tritium, Chemistry, Analytical Chemistry (journal), Isotope, Extraction (chemistry), Solubility

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