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Thermal ionization mass spectrometry, TIMS is also known as surface ionization and is a highly sensitive isotope mass spectrometry characterization technique. The isotopic ratios of radionuclides are used to get an accurate measurement for the elemental analysis of a sample [1]. Singly charged ions of the sample are formed by the thermal ionization effect. A chemically purified liquid sample is placed on a metal filament which is then heated to evaporate the solvent. The removal of an electron from the purified sample is consequently achieved by heating the filament enough to release an electron, which consequently ionizes the atoms of the sample [2]. TIMS utilizes a magnetic sector mass analyzer to separate the ions based on their mass to charge ratio. The ions gain velocity by an electrical potential gradient and are focused into a beam by electrostatic lenses. The ion beam then passes through the magnetic field of the electromagnet where it is partitioned into separate ion beams based on the ion's mass/charge ratio. These mass-resolved beams are directed into a detector where it is converted into voltage. The voltage detected is then used to calculate the isotopic ratio.[3]
Ionization source
[edit]The filaments used are made from tantalum (Ta), tungsten (W), platinum (Pt) or Rhenium (Re). Conventionally, there are two filaments used in TIMS. One filament is for the sample and is called the sample filament. The liquid sample is placed on the sample filament which is then evaporated to create ions. Subsequently, these ions land on the other filament, also known as the ionization filament. Here, the ion looses an electron by ionization.[4]
The single filament method is also possible. Once the sample evaporates, the ions can settle back down onto the same filament to get ionized.[4] The use of a triple filament or multifilament set-up improves ionization efficiency and provides the rate of evaporation and ionization to be controlled separately. [4] Filaments need to be loaded with activators. An activator represses the evaporation of the desired element and can either increase or decrease the ionization potential of the filament. This results in high ionization efficiency and a higher total yield. The most common activator is silica gel/phosphoric acid for Pb. [5]
Ion detectors The most common detectors used for TIMS is Faraday cup, daly detector, and electron multiplier. [5]
Thermal ionization mechanism
[edit]When the hot filament heats the liquid sample, the fermi levels within the sample reaches parity with that of the metal. In turn, this allows for an electron to tunnel from the sample to the metal filament. As a result, positive ions are formed from the sample that lost an electron. This transferring of electrons also result in the formation of negative ions. Subsequently, there are two types of thermal ionizations. One is positive thermal ionization (P-TI) and the second is negative thermal ionization (N-TI). [5] The production of ions is parameterized by the Saha ionization equation or the Saha-Langmuir equation. [4]
Isotope ratio measurement
[edit]The relative abundances of different isotopes are then used to describe the chemical fractionation of different isotopes, travel in different reservoirs of non-radiogenic isotopes, and age or origins of solar system objects by the presence of radiogenic daughter isotopes.[6][7]
Elemental analysis is a predominant application of TIMS as it gives reliable isotopic ratios. Following the trend of decreasing ionization energy, elements located towards the bottom left of the periodic table are viable for TIMS. In addition, the high electron affinity seen towards the upper right of the periodic table makes these nonmetals excellent candidates.[4] The technique is used extensively in isotope geochemistry, geochronology, and in cosmochemistry.[6][7]
quantitative isotope ratio techniques include;
isotope dilution thermal ionization mass spectrometry (ID-TIMS) [8] Isotope dilution method is used because the signal intensity in TIMS isn't proportional to the amount that was placed into TIMS. [5]
chemical abrasion thermal ionization mass spectrometry (CA-TIMS) [9]
Age Dating Mass spectrometers with magnetic sectors have better precision than a quadrupole mass spectrometer or quadrupole mass analyzer. Inductively coupled plasma-quadrupole mass spectrometers allows for an even higher precision of detecting the change of isotopic ratios by radioactive decay. The more precision means the higher resolution in age dating.[5]
References
[edit]- ^ Becker. "Chapter 13 Inorganic Mass Spectrometry of Radionuclides". In L'Annunziata, Micheal F. (ed.). Handbook of radioactivity analysis (3rd ed.). Elsevier Science. p. 833-870. ISBN 978-0-12-384873-4.
- ^ A Handbook of Silicate Rock Analysis. ISBN 978-94-015-3990-6.
- ^ Constantinos A. Georgiou; Georgios P. Danezis. "chapter 3- Elemental and Isotopic Mass Spectrometry". In Pico, Yolanda (ed.). Advanced mass spectrometry for food safety and quality (68 ed.). p. 131-243. ISBN 978-0-444-63340-8.
- ^ a b c d e Dass, Chhabil. Fundamentals of contemporary mass spectrometry. Wiley-Interscience. pp. 264–265. ISBN 978-0-471-68229-5.
- ^ a b c d e Makishima, Akio (2016). Thermal ionization mass spectrometry (TIMS) : silicate digestion, separation, and measurement. Weinheim, Germany: Wiley-VCH Verlag GmbH & Co. KGaA, Boschstr. ISBN 3527340246.
- ^ a b Lehto, J., X. Hou, 2011. Chemistry and Analysis of Radionuclides. Wiley-VCH.
- ^ a b Dickin, A.P., 2005. Radiogenic Isotope Geology 2nd ed. Cambridge: Cambridge University Press. pp. 21-22
- ^ Duan, Yixiang; Danen, Ray E.; Yan, Xiaomei; Steiner, Robert; Cuadrado, Juan; Wayne, David; Majidi, Vahid; Olivares, José A. (October 1999). "Characterization of an improved thermal ionization cavity source for mass spectrometry". Journal of the American Society for Mass Spectrometry. 10 (10): 1008–1015. doi:10.1016/S1044-0305(99)00065-3.
- ^ Mattinson, James M. (July 2005). "Zircon U–Pb chemical abrasion ("CA-TIMS") method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages". Chemical Geology. 220 (1–2): 47–66. doi:10.1016/j.chemgeo.2005.03.011.
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