instrumental techniques applied to mineralogy and geochemistry
instrumental techniques applied to mineralogy and geochemistry
instrumental techniques applied to mineralogy and geochemistry
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Radiogenic iso<strong>to</strong>pes <strong>and</strong> their applications within a range of scientific fields 127<br />
undeclared additives with a unique iso<strong>to</strong>pic composition could be detected. Montgomery<br />
et al. (2006) analyzed mineral waters across Britain <strong>and</strong> found that their 87 Sr/ 86 Sr ratios<br />
varied systematically as a reflec<strong>to</strong>r of the geology of the aquifer rocks (Figure 6). It is<br />
implied from their study that the knowledge of the spatial Sr iso<strong>to</strong>pe variations in water<br />
will be important also for his<strong>to</strong>rical <strong>and</strong> archeological studies. The origin of various<br />
food, wine, waters. etc., based on iso<strong>to</strong>pic determinations, have been reviewed by Kelly<br />
et al. (2005) who stress the importance of combining as many elemental <strong>and</strong> iso<strong>to</strong>pic<br />
signatures as possible.<br />
Environmental sciences<br />
Past climate variations, underst<strong>and</strong>ing path-ways of elements in reactions, <strong>and</strong><br />
anthropogenic contamination are only a few of numerous issues where iso<strong>to</strong>pes have<br />
played an important role <strong>to</strong> clarify the nature of processes.<br />
Dust transport<br />
Continental dust, released from arid regions, are transported over long distances<br />
<strong>and</strong> deposited on the oceans <strong>and</strong> continents. Obviously, the knowledge of the origin of<br />
dust could help in under-st<strong>and</strong>ing atmospheric circulation mechanisms (Grousset <strong>and</strong><br />
Biscaye, 2005). Satelite imaging <strong>and</strong> air-mass trajec<strong>to</strong>ry <strong>techniques</strong> have been used <strong>to</strong><br />
trace transport patterns, <strong>and</strong> also iso<strong>to</strong>pe tracer methods (Figure 7).<br />
FIGURE 6. The 87 Sr/ 86 Sr iso<strong>to</strong>pe composition of bottled waters plotted against the geological<br />
stratigraphy of the aquifer source rock (after Montgomery et al., 2006).