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~80% yield. Found, %: C 39.3, H 7.8. C8H20ClO4P.
1
31
Calculated, %: C 38.95, H 8.17. The H and P–{1H}
NMR data are discussed in the text.
5. Hu, T.Q., James, B.R., Yawalata, D., and Ezhova, M.B.,
NMR investigation of a 1:1 reaction of the
chloride I with Na2SO3. In a glove-box, I (30 mg,
0.12 mmol) was dissolved in a stirred, air-free D2O
solution (~1.5 ml) containing Na2SO3 (15.4 mg,
0.12 mmol). A sample of the solution (~0.7 ml) was
then placed in a J-Young NMR tube and the spectra
were recorded periodically at r.t. The same procedure
was used for studying 1:1 reactions of I with Et3N
(12.3 mg, 0.12 mmol), Na2S2O3 (19.2 mg, 0.12 mmol),
and NaHSO3 (12.7 mg, 0.12 mmol); reactions using
stoichiometries other than 1:1 were studied similarly.
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CONCLUSIONS
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Tetrakis(α-hydroxyethyl)phosphonium
chloride,
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[HO(Me)CH]4PCl, is characterized for the first time by
1H and 31P{1H} NMR spectroscopy, which reveals that
the compound consists of three diastereomers in a
4:4:1 ratio. Reaction of [HO(Me)CH]4PCl with
Na2SO3 or Et3N in attempts to isolate [HO(Me)CH]3P
leads to an equilibrium between this tertiary phosphine
and the secondary phosphine [HO(Me)CH]2PH.
Except for (HOCH2)3P, tris(α-hydroxyalkyl)phos-
phines are generally unstable in aqueous media.
Established also is that the water-soluble phosphinic
acid [HO(Me)CH]2P(O)OH can be easily obtained by
a 1:4 reaction of [HO(Me)CH]4PCl with NaHSO3 (r.t.,
Ar), the secondary phosphine oxide [HO(Me)CH]2·
P(O)H being an intermediate in this process.
Interaction of [HO(Me)CH]4PCl with Na2S2O3 affords
the sulfide [HO(Me)CH]3PS. Plausible rationales are
presented for differences between the observed and
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ACKNOWLEDGMENTS
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We thank the Natural Sciences and Engineering
Research Council of Canada for funding via a
Discovery Grant.
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RUSSIAN JOURNAL OF GENERAL CHEMISTRY Vol. 83 No. 2 2013