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.
While oxygen-17 NMR is increasingly being used for elucidating the structure and reactivity of complex molecular and materials systems, much effort is still required for it to become a routine analytical technique. One of the main difficulties for its development comes from the very low natural abundance of oxygen-17, which implies that isotopic labeling is generally needed prior to NMR analyses. However, 17O-enrichment protocols are often unattractive in terms of cost, safety, and/or practicality, even for compounds as simple as metal oxides. Here, we demonstrate how mechanochemistry can be used in a highly efficient way for the direct 17O-isotopic labeling of a variety of s-, p- and d-block oxides which are of major interest for the preparation of functional ceramics and glasses: Li2O, CaO, Al2O3, SiO2, TiO2, and ZrO2. For each oxide, the enrichment step was performed under ambient conditions in less than 1 hour and at low cost, which makes these synthetic approaches highly appealing in comparison to the existing literature. Using high-resolution 17O solid state NMR and Dynamic Nuclear Polarization, atomic-level insight into the enrichment process is achieved, especially for titania and alumina. Indeed, it was possible to demonstrate that enriched oxygen sites are present not only at the surface, but also within the oxide particles. Moreover, information on the actual reactions occurring during the milling step could be obtained by 17O NMR, both in terms of their kinetics and the nature of the reactive species. Finally, it was demonstrated how high resolution 17O NMR can be used for studying the reactivity at the interfaces between different oxide particles during ball-milling, especially in cases when X-ray diffraction techniques are uninformative. More generally, such investigations will be useful not only for producing 17O-enriched precursors efficiently, but also for understanding better mechanisms of mechanochemical processes themselves. <br>
While oxygen-17 NMR is increasingly being used for elucidating the structure and reactivity of complex molecular and materials systems, much effort is still required for it to become a routine analytical technique. One of the main difficulties for its development comes from the very low natural abundance of oxygen-17, which implies that isotopic labeling is generally needed prior to NMR analyses. However, 17O-enrichment protocols are often unattractive in terms of cost, safety, and/or practicality, even for compounds as simple as metal oxides. Here, we demonstrate how mechanochemistry can be used in a highly efficient way for the direct 17O-isotopic labeling of a variety of s-, p- and d-block oxides which are of major interest for the preparation of functional ceramics and glasses: Li2O, CaO, Al2O3, SiO2, TiO2, and ZrO2. For each oxide, the enrichment step was performed under ambient conditions in less than 1 hour and at low cost, which makes these synthetic approaches highly appealing in comparison to the existing literature. Using high-resolution 17O solid state NMR and Dynamic Nuclear Polarization, atomic-level insight into the enrichment process is achieved, especially for titania and alumina. Indeed, it was possible to demonstrate that enriched oxygen sites are present not only at the surface, but also within the oxide particles. Moreover, information on the actual reactions occurring during the milling step could be obtained by 17O NMR, both in terms of their kinetics and the nature of the reactive species. Finally, it was demonstrated how high resolution 17O NMR can be used for studying the reactivity at the interfaces between different oxide particles during ball-milling, especially in cases when X-ray diffraction techniques are uninformative. More generally, such investigations will be useful not only for producing 17O-enriched precursors efficiently, but also for understanding better mechanisms of mechanochemical processes themselves. <br>
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