ESR spectra were recorded in the X-band (9.6 GHz) and in the W-band (94 GHz)
and electron spin relaxation was measured by electron spin echo (ESE) in the
temperature range 4.2–300 K for radicals in natural calcite samples obtained
from a cave stalactite and a dripstone layer. Four types of carbonate radical
spectra and two sulfate radical spectra were identified and high accuracy
g-factors were derived. Time and temperature behaviour of the spectra show that the dominating
CO2−
radicals are rigidly bonded or undergo free reorientations, whereas
CO3−,
SO2−
and SO3−
only undergo free reorientations. Below 200 K the free reorientations of
CO2−
are suppressed and a hindered rotation around single local axis appears. The ESE detected
spectrum proves that the lines of free rotating radicals are homogeneously broadened, thus
they cannot participate in electron spin echo formation. Spin–lattice relaxation data show that
CO2−
radicals are decoupled from lattice phonons and relax via local
mode tunnelling motion between inequivalent oxygen positions of
CO2−
molecules. The tunnelling appears in two excited vibrational states of energy 71 and
138 cm−1. Librational
motions of CO2−
molecules were detected by electron spin echo decay (phase relaxation) with energy
153 cm−1. Two kinds of impurity hydrogen atoms were distinguished from ESEEM: in-water
inclusions and water coordinated to the calcium ions.