Calcium oxalate minerals
of the general formula CaC
2
O
4
.
x
H
2
O are widely
present in nature and usually associated with pathological calcifications,
constituting up to 70–80% of the mineral component of renal
calculi. The monohydrate phase (CaC
2
O
4
.
H
2
O, COM) is the most stable form, accounting for the
majority of the hydrated calcium oxalates found. These mineral phases
have been studied extensively via X-ray diffraction and IR spectroscopy
and, to a lesser extent, using
1
H,
13
C, and
43
Ca solid-state NMR spectroscopy. However, several aspects
of their structure and reactivity are still unclear, such as the evolution
from low- to high-temperature COM structures (LT-COM and HT-COM, respectively)
and the involvement of water molecules in this phase transition. Here,
we report for the first time a
17
O and
2
H solid-state
NMR investigation of the local structure and dynamics of water in
the COM phase. A new procedure for the selective
17
O- and
2
H-isotopic enrichment of water molecules within the COM mineral
is presented using mechanochemistry, which employs only microliter
quantities of enriched water and leads to exchange yields up to ∼30%.
17
O NMR allows both crystallographically inequivalent water
molecules in the LT-COM structure to be resolved, while
2
H NMR studies provide unambiguous evidence that these water molecules
are undergoing different types of motions at high temperatures without
exchanging with one another. Dynamics appear to be essential for water
molecules in these structures, which have not been accounted for in
previous structural studies on the HT-COM structure due to lack of
available tools, highlighting the importance of such NMR investigations
for refining the overall knowledge on biologically relevant minerals
like calcium oxalates.