Physics:Stable isotope ratio

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Short description: Ratio of two stable isotopes
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The term stable isotope has a meaning similar to stable nuclide, but is preferably used when speaking of nuclides of a specific element. Hence, the plural form stable isotopes usually refers to isotopes of the same element. The relative abundance of such stable isotopes can be measured experimentally (isotope analysis), yielding an isotope ratio that can be used as a research tool. Theoretically, such stable isotopes could include the radiogenic daughter products of radioactive decay, used in radiometric dating. However, the expression stable-isotope ratio is preferably used to refer to isotopes whose relative abundances are affected by isotope fractionation in nature. This field is termed stable isotope geochemistry.

Stable-isotope ratios

Measurement of the ratios of naturally occurring stable isotopes (isotope analysis) plays an important role in isotope geochemistry, but stable isotopes (mostly hydrogen, carbon, nitrogen, oxygen and sulfur) are also finding uses in ecological and biological studies. Other workers have used oxygen isotope ratios to reconstruct historical atmospheric temperatures, making them important tools for paleoclimatology.

These isotope systems for lighter elements that exhibit more than one primordial isotope for each element have been under investigation for many years in order to study processes of isotope fractionation in natural systems. The long history of study of these elements is in part because the proportions of stable isotopes in these light and volatile elements is relatively easy to measure. However, recent advances in isotope ratio mass spectrometry (i.e. multiple-collector inductively coupled plasma mass spectrometry) now enable the measurement of isotope ratios in heavier stable elements, such as iron, copper, zinc, molybdenum, etc.

Applications

The variations in oxygen and hydrogen isotope ratios have applications in hydrology since most samples lie between two extremes, ocean water and Arctic/Antarctic snow.[1] Given a sample of water from an aquifer, and a sufficiently sensitive tool to measure the variation in the isotopic ratio of hydrogen in the sample, it is possible to infer the source, be it ocean water or precipitation seeping into the aquifer, and even to estimate the proportions from each source.[2] Stable isotopologues of water are also used in partitioning water sources for plant transpiration and groundwater recharge.[3][4]

Another application is in paleotemperature measurement for paleoclimatology. For example, one technique is based on the variation in isotopic fractionation of oxygen by biological systems with temperature.[5] Species of Foraminifera incorporate oxygen as calcium carbonate in their shells. The ratio of the oxygen isotopes oxygen-16 and oxygen-18 incorporated into the calcium carbonate varies with temperature and the oxygen isotopic composition of the water. This oxygen remains "fixed" in the calcium carbonate when the foraminifera dies, falls to the sea bed, and its shell becomes part of the sediment. It is possible to select standard species of foraminifera from sections through the sediment column, and by mapping the variation in oxygen isotopic ratio, deduce the temperature that the Forminifera encountered during life if changes in the oxygen isotopic composition of the water can be constrained.[6] Paleotemperature relationships have also enabled isotope ratios from calcium carbonate in barnacle shells to be used to infer the movement and home foraging areas of the sea turtles and whales on which some barnacles grow.[7]

In ecology, carbon and nitrogen isotope ratios are widely used to determine the broad diets of many free-ranging animals. They have been used to determine the broad diets of seabirds, and to identify the geographical areas where individuals spend the breeding and non-breeding season in seabirds[8] and passerines.[9] Numerous ecological studies have also used isotope analyses to understand migration, food-web structure, diet, and resource use,[10] such as hydrogen isotopes to measure how much energy from stream-side trees supports fish growth in aquatic habitats.[11] Determining diets of aquatic animals using stable isotopes has been particularly common, as direct observations are difficult.[12] They also enable researchers to measure how human interactions with wildlife, such as fishing, may alter natural diets.[13]

In forensic science, research suggests that the variation in certain isotope ratios in drugs derived from plant sources (cannabis, cocaine) can be used to determine the drug's continent of origin.[14]

In food science, stable isotope ratio analysis has been used to determine the composition of beer,[15] shoyu sauce[16] and dog food.[17]

Stable isotope ratio analysis also has applications in doping control, to distinguish between endogenous and exogenous (synthetic) sources of hormones.[18][19]

The accurate measurement of stable isotope ratios relies on proper procedures of analysis, sample preparation and storage.[20]

Chondrite meteorites are classified using the oxygen isotope ratios. In addition, an unusual signature of carbon-13 confirms the non-terrestrial origin for organic compounds found in carbonaceous chondrites, as in the Murchison meteorite.

The uses of stable isotope ratios described above pertain to measurements of naturally occurring ratios. Scientific research also relies on the measurement of stable isotope ratios that have been artificially perturbed by the introduction of isotopically enriched material into the substance, process or system under study. Isotope dilution involves adding enriched stable isotope to a substance in order to quantify the amount of that substance by measuring the resulting isotope ratios. Isotope labeling uses enriched isotope to label a substance in order to trace its progress through, for example, a chemical reaction, metabolic pathway or biological system. Some applications of isotope labeling rely on the measurement of stable isotope ratios to accomplish this.

See also

Bibliography

  • Allègre C.J., 2008. Isotope Geology (Cambridge University Press ).
  • Faure G., Mensing T.M. (2004), Isotopes: Principles and Applications (John Wiley & Sons ).
  • Hoefs J., 2004. Stable Isotope Geochemistry (Springer Verlag).
  • Sharp Z., 2006. Principles of Stable Isotope Geochemistry (Prentice Hall).

References

  1. ↑ "Reliable determination of oxygen and hydrogen isotope ratios in atmospheric water vapour adsorbed on 3A molecular sieve". Rapid Commun. Mass Spectrom. 20 (23): 3612–8. 2006. doi:10.1002/rcm.2772. PMID 17091470. Bibcode: 2006RCMS...20.3612H. 
  2. ↑ "155,000 years of West African monsoon and ocean thermal evolution". Science 316 (5829): 1303–7. 2007. doi:10.1126/science.1140461. PMID 17540896. Bibcode: 2007Sci...316.1303W. 
  3. ↑ Good, Stephen P.; Noone, David; Bowen, Gabriel (2015-07-10). "Hydrologic connectivity constrains partitioning of global terrestrial water fluxes" (in en). Science 349 (6244): 175–177. doi:10.1126/science.aaa5931. ISSN 0036-8075. PMID 26160944. Bibcode: 2015Sci...349..175G. 
  4. ↑ Evaristo, Jaivime; Jasechko, Scott; McDonnell, Jeffrey J. (2015). "Global separation of plant transpiration from groundwater and streamflow". Nature 525 (7567): 91–94. doi:10.1038/nature14983. PMID 26333467. Bibcode: 2015Natur.525...91E. 
  5. ↑ "Carbon isotope ratio monitoring-gas chromatography mass spectrometric measurements in the marine environment: biomarker sources and paleoclimate applications". Sci. Total Environ. 237–238: 473–81. 1999. doi:10.1016/S0048-9697(99)00159-X. PMID 10568296. Bibcode: 1999ScTEn.237..473T. 
  6. ↑ "A 10-fold improvement in the precision of boron isotopic analysis by negative thermal ionization mass spectrometry". Anal. Chem. 75 (9): 1972–7. 2003. doi:10.1021/ac020589f. PMID 12720329. 
  7. ↑ Pearson, Ryan M.; van de Merwe, Jason P.; Gagan, Michael K.; Limpus, Colin J.; Connolly, Rod M. (2019). "Distinguishing between sea turtle foraging areas using stable isotopes from commensal barnacle shells" (in en). Scientific Reports 9 (1): 6565. doi:10.1038/s41598-019-42983-4. ISSN 2045-2322. PMID 31024029. Bibcode: 2019NatSR...9.6565P. 
  8. ↑ Graña Grilli, M.; Cherel, Y. (2017). "Skuas (Stercorarius spp.) moult body feathers during both the breeding and inter-breeding periods: implications for stable isotope investigations in seabirds". Ibis 159 (2): 266–271. doi:10.1111/ibi.12441. 
  9. ↑ Franzoi, A.; Bontempo, L.; Kardynal, K.J.; Camin, F.; Pedrini, P.; Hobson, K.A. (2020). "Natal origins and timing of migration of two passerine species through the southern Alps: inferences from multiple stable isotopes (δ 2H, δ 13C, δ 15N, δ 34S) and ringing data". Ibis 162 (2): 293–306. doi:10.1111/ibi.12717. 
  10. ↑ Pearson, RM; van de Merwe, JP; Limpus, CJ; Connolly, RM (2017). "Realignment of sea turtle isotope studies needed to match conservation priorities" (in en). Marine Ecology Progress Series 583: 259–271. doi:10.3354/meps12353. ISSN 0171-8630. Bibcode: 2017MEPS..583..259P. 
  11. ↑ Doucett, Richard R.; Marks, Jane C.; Blinn, Dean W.; Caron, Melanie; Hungate, Bruce A. (June 2007). "Measuring Terrestrial Subsidies to Aquatic Food Webs Using Stable Isotopes of Hydrogen". Ecology 88 (6): 1587–1592. doi:10.1890/06-1184. ISSN 0012-9658. PMID 17601150. http://dx.doi.org/10.1890/06-1184. 
  12. ↑ Gutmann Roberts, Catherine; Britton, J. Robert (2018-09-01). "Trophic interactions in a lowland river fish community invaded by European barbel Barbus barbus (Actinopterygii, Cyprinidae)" (in en). Hydrobiologia 819 (1): 259–273. doi:10.1007/s10750-018-3644-6. ISSN 1573-5117. 
  13. ↑ Gutmann Roberts, Catherine; Bašić, Tea; Trigo, Fatima Amat; Britton, J. Robert (2017). "Trophic consequences for riverine cyprinid fishes of angler subsidies based on marine-derived nutrients" (in en). Freshwater Biology 62 (5): 894–905. doi:10.1111/fwb.12910. ISSN 1365-2427. http://eprints.bournemouth.ac.uk/26407/1/Marine%20derived%20nutrients%20in%20cyprinids_Freshwater%20Biology.pdf. 
  14. ↑ "Stable isotope analyses of heroin seized from the merchant vessel Pong Su". J. Forensic Sci. 51 (3): 603–6. 2006. doi:10.1111/j.1556-4029.2006.00123.x. PMID 16696708. 
  15. ↑ Brooks, J. Renée; Buchmann, Nina; Phillips, Sue; Ehleringer, Bruce; Evans, R. David; Lott, Mike; Martinelli, Luiz A.; Pockman, William T. et al. (October 2002). "Heavy and Light Beer: A Carbon Isotope Approach To Detect C4 Carbon in Beers of Different Origins, Styles, and Prices". Journal of Agricultural and Food Chemistry 50 (22): 6413–6418. doi:10.1021/jf020594k. PMID 12381126. 
  16. ↑ Morais, M.C.; Pellegrinetti, T.A.; Sturion, L.C.; Sattolo, T.M.S.; Martinelli, L.A. (February 2019). "Stable carbon isotopic composition indicates large presence of maize in Brazilian soy sauces (shoyu)". Journal of Food Composition and Analysis. doi:10.1016/j.jfca.2019.01.020. 
  17. ↑ Galera, Leonardo de Aro; Abdalla Filho, Adibe Luiz; Reis, Luiza Santos; Souza, Janaina Leite de; Hernandez, Yeleine Almoza; Martinelli, Luiz Antonio (20 February 2019). "Carbon and nitrogen isotopic composition of commercial dog food in Brazil". PeerJ 7: e5828. doi:10.7717/peerj.5828. PMID 30809425. 
  18. ↑ Author, A (2012). "Stable isotope ratio analysis in sports anti-doping". Drug Testing and Analysis 4 (12): 893–896. doi:10.1002/dta.1399. PMID 22972693. 
  19. ↑ Cawley, Adam T.; Kazlauskas, Rymantas; Trout, Graham J.; Rogerson, Jill H.; George, Adrian V. (1985). "Isotopic Fractionation of Endogenous Anabolic Androgenic Steroids and Its Relationship to Doping Control in Sports". Journal of Chromatographic Science 43 (1): 32–38. doi:10.1093/chromsci/43.1.32. PMID 15808004. 
  20. ↑ Tsang, Man-Yin; Yao, Weiqi; Tse, Kevin (2020). Kim, Il-Nam. ed. "Oxidized silver cups can skew oxygen isotope results of small samples" (in en). Experimental Results 1: e12. doi:10.1017/exp.2020.15. ISSN 2516-712X. 



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