Ch.1. Radioisotopes (Unstable isotopes)

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Presentation transcript:

Ch.1. Radioisotopes (Unstable isotopes) The isotopes do radioactive decay Mode of radioactive decay From https://commons.wikimedia.org/wiki/Image:Radioactive_decay_modes.svg?uselang=ko

List of the radioactive ebvironmental isotopes  See Table 1-3 on p.17. Formed by H-bomb testing (and minorly from cosmic ray bombardment on 14N) Daughter: 3He Measured in absolute amount (in TU). 1 TU=1 T per 1018H Detected w/ LSC or gas counter (for the case of propane preparation) (see text)

14C Formed by cosmic ray bombardment on 14N Daughter: 14N Measured against modern carbon (mC) whose 14C activity is 95% of that of 1950 NBS-oxalic acid standard Due to the fractionation, should be normalized to d13C = -25‰ Converted into graphite and analyzed with AMS

36Cl Formed by cosmic ray bombardment on 36Ar Daughter: 36Ar Often analyzed with AMS

Significance of environmental isotopes (in hydrogeology)? Trace groundwater provenance Estimate groundwater age Interpretation of groundwater quality Understanding geochemical evolution (reactions and reaction rates) and recharge processes Recognizing geochemical & biogeochemical cycles of pollutants among soil-water-atmosphere

Isotopic fractionation A process of resulting disproportion of isotopes due to their mass difference Physicochemical fractionation vs. Diffusive fractionation: Compare the equations on p. 22 to 25. Equilibrium vs. kinetic fractionation See Fig. 1-5 on p.23.

The conditions of isotopic equilibria requires Chemical equilibria: forward and backward reaction rates are same Enough time for mixing between reactant and product reservoir Enough time for complete mixing within each reservoir (homogeneity issues) Temperature effect on fractionation For an equilibrium fractionation, usually the fractionation is reciprocally proportional to T For an kinetic fractionation, the fractionation is dependent upon the nature of the processes (e.g. biocatalysis vs. inorganic burning) See Fig. 1-8 & Table 1-4 on p. 28, Fig. 1-7. on p.29, and Fig. 1-8 on p.30.

Isotope Fractionation, enrichment, and separation Fractionation: a Enrichment: e Separation: D See the equations on p.31 and Fig. 1-9 on p.32.

Assignments Solve problems 1, 3, 5, 7, and 9 on p.33 to 34.