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. Author manuscript; available in PMC: 2017 Nov 16.
Published in final edited form as: Geochim Cosmochim Acta. 2013 Dec 7;127:326–347. doi: 10.1016/j.gca.2013.11.030

Table 8.

Error-weighted mean isotopic deviations (χ2) of optimized mixtures of fractionated SW, HLa and Sb from Q-gasesc. First line in each section demonstrates the large difference between SW and Q. Second line correspond to mass fractionated SW without addition of presolar components, which are taken into account in 3-rd and 4th lines. Shown fractions are for major isotopes: 84Kr and 132Xe.

Starting SW-Xe composition SW-Xe fractionated by (‰) Xe-HL addition (%) Xe-S addition (%) χ2
Lunar regolithd,e ≡ 0 ≡ 0 ≡ 0 32
10.5 ≡ 0 ≡ 0 2.2
10.2 1.5 ≡ 0 0.22
10.2 1.4 −0.1 0.20
Genesis, Al-collectorsf ≡ 0 ≡ 0 ≡ 0 150
10.9 ≡ 0 ≡ 0 9.4
8.1 1.5 ≡ 0 1.8
8.4 1.5 0.15 1.5
Genesis current best estimate (this work) ≡ 0 ≡ 0 ≡ 0 160
11.1 ≡ 0 ≡ 0 10
8.0 1.6 ≡ 0 1.8
8.2 1.6 0.1 1.6

SW-Kr composition SW-Kr fractionated by (‰) Kr-HL addition % Kr-S addition (%) χ2
Lunar regolithd,e ≡ 0 ≡ 0 ≡ 0 63
8.5 ≡ 0 ≡ 0 2.2
6.9 2.6 ≡ 0 1.9
4.3 5.4 0.4 0.8
Genesis current best estimate (this work) ≡ 0 ≡ 0 ≡ 0 190
10.2 ≡ 0 ≡ 0 8.7
10.1 0.1 ≡ 0 8.7
6.3 4.4 0.4 0.7
b

Productions of s-process isotopes 86Kr and 80Kr are neutron flux and temperature dependent. Ratios 86Kr/84Kr and 80Kr/84Kr vary with the grain size (Lewis et al., 1994). Following Gilmour (2010) we assume the median values of these ratios: 0.83 and 0.02 respectively from the reported ranges of 86Kr/84Kr and 80Kr/84Kr (Ott, 2002).

e

Similar to minimization made by Gilmour, 2010.