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核磁必备文献 JOC NMR Chemical Shifts
7512 J. Org. Chem. 1997, 62, 7512-7515
NMR Chemical Shifts of Common
Laboratory Solvents as Trace Impurities
Hugo E. Gottlieb,* Vadim Kotlyar, and
Abraham Nudelman*
Department of Chemistry, Bar-Ilan University,
Ramat-Gan 52900, Israel
Received June 27, 1997
In the course of the routine use of NMR as an aid for
organic chemistry, a day-to-day problem is the identifica-
tion of signals deriving from common contaminants
(water, solvents, stabilizers, oils) in less-than-analyti-
cally-pure samples. This data may be available in the
literature, but the time involved in searching for it may
be considerable. Another issue is the concentration
dependence of chemical shifts (especially 1H); results
obtained two or three decades ago usually refer to much Figure 1. Chemical shift of HDO as a function of tempera-
more concentrated samples, and run at lower magnetic ture.
fields, than today’s practice.
1 13
We therefore decided to collect H and C chemical dependent (vide infra). Also, any potential hydrogen-
shifts of what are, in our experience, the most popular bond acceptor will tend to shift the water signal down-
“extra peaks” in a variety of commonly used NMR field; this is particularly true for nonpolar solvents. In
solvents, in the hope that this will be of assistance to contrast, in e.g. DMSO the water is already strongly
the practicing chemist. hydrogen-bonded to the solvent, and solutes have only a
negligible effect on its chemical shift. This is also true
Experimental Section for D2O; the chemical shift of the residual HDO is very
NMR spectra were taken in a Bruker DPX-300 instrument temperature-dependent (vide infra) but, maybe counter-
(300.1 and 75.5 MHz for 1H and 13C, respectively). Unless
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