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Scheme 1 Fractionation procedure for HA and FA fractions.
Variation of F and Cl among arc primitive magmas should therefore indicate (1) fractionation processes during transfer of water-rich flux from slab and/or (2) source compositions of the water-rich metasomatic agent.
Such a pattern may occur by one of two processes: 1) fractionation bias is not constant along a chromosome or 2) homeologous regions were exchanged between chromosomes through homeologous recombination.
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However, the most highly purified protein fraction, obtained following P2 fractionation, Mono-Q, SP-sepharose, Mini-S ion exchange, and gel filtration still exhibited zinc stimulation (Figure S2C).
Further SP(2) fractionation to SP 3) increased the SP fraction to 25.6% of total cells, an increase of approximately 50-fold from the original parental population.
In the pool with highest sulfate concentration (FPL, [SO42-] = 5659 μmol L-1) fractionation between sulfide and sulfate is represented by δ34S value of 2.28‰.
Figure 5 Fractionation and separation of AuNPs.
The δ34S fractionation follows a Rayleigh fractionation model with an enrichment factor of 21.6‰.
Phytate/Ca2+ fractionation and TCA/acetone precipitation were combined to design an improved TCA/acetone method.
Purification was achieved using (NH4 2SO4 fractionation, Sephadex G-100 column chromatography, and preparative native-polyacrylamide gel electrophoresis (PAGE).
Sigman et al. (1999) estimated that δ15N fractionation by phytoplankton uptake is 4 6 ‰, based on field observations in the Southern Ocean.
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