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Abstract Serpentine minerals have received a lot of attention because of their unique crystal structures, their wide occurrence in orogenic belts and their potential role in contributing seismic anisotropy in subducting slabs. Several studies have investigated crystal preferred orientation (CPO) in high temperature antigorite serpentinites from Japan, the Alps, Spain, Cuba and Tibet, documenting significant crystal alignment. However, only a limited number of lower grade serpentines have been explored to date. Mainly because of submicroscopic microstructural heterogeneities CPO cannot be measured with conventional methods such as optical microscopy and EBSD. In this study 15 serpentinites from different tectonic settings in California, the Central Alps and Northern Spain have been investigated, mainly with high energy synchrotron X-ray diffraction, to quantify bulk crystal alignment. We find that CPO is strong on sheared surfaces of fractured blocks and secondary veins but the bulk of most serpentinite samples, except high-grade recrystallized antigorite serpentinite, show only weak crystal alignment. Correspondingly calculated seismic anisotropy based on CPO is not very significant. This is supported by very heterogeneous microstructures as documented with SEM and TEM analyses. 

Manganese (Mn) oxides, widely found in aquatic and terrestrial environments, play crucial roles in natural ecosystems and in environmental processes. Previously, it was believed that naturally abundant Mn oxides originated through biotically mediated processes. However, we have revealed the significance of photochemically induced abiotic oxidation of Mn2+(aq) to Mn(IV) oxides. This study further elucidates the photochemically induced co-oxidation of aqueous Mn2+ and cobalt (Co2+), which leads to the predominant formation of Mn(IV)–Co(III) oxide nanosheets. Both pair distribution function analysis and X-ray absorption spectra provide evidence that Co2+ is mainly oxidized to Co(III) within the plane of the Mn oxide structure, where it forms double-edge-sharing arrangements. Additionally, the initial concentration of Co2+ greatly influences the extent of Co incorporation within the final Mn–Co oxides and Mn oxidation states. Increased Co incorporation correlates with a higher concentration of oxygen vacancies within the Mn oxide structures, which reduces their band gap and significantly influences the reactivity of Mn oxides, governing their ability to participate in pollutant degradation and redox transformations. This study advances our understanding of the mechanism of formation of Co-incorporated Mn oxides in the natural environment and provides insights into their occurrence in the natural environment and their applications in environmental processes. 

Carboxylic acid functionalized cellulose nanocrystals have been obtained from biomass and evaluated as aqueous, environmentally sustainable alternatives to conventional polyvinylidene difluoride binders for cathodes of lithium-ion batteries. 

Abstract We communicate a feasibility study for high‐resolution structural characterization of biomacromolecules in aqueous solution from X‐ray scattering experiments measured over a range of scattering vectors (q) that is approximately two orders of magnitude wider than used previously for such systems. Scattering data with such an extendedq‐range enables the recovery of the underlying real‐space atomic pair distribution function, which facilitates structure determination. We demonstrate the potential of this method for biomacromolecules using several types of cyclodextrins (CD) as model systems. We successfully identified deviations of the tilting angles for the glycosidic units in CDs in aqueous solutions relative to their values in the crystalline forms of these molecules. Such level of structural detail is inaccessible from standard small angle scattering measurements. Our results call for further exploration of ultra‐wide‐angle X‐ray scattering measurements for biomacromolecules. 

The rate and pathway of ferrihydrite (Fh) transformation at oxic conditions to more stable products is controlled largely by temperature, pH, and the presence of other ions in the system such as nitrate (NO3–), sulfate (SO42–), and arsenate (AsO43–). Although the mechanism of Fh transformation and oxyanion complexation have been separately studied, the effect of surface complex type and strength on the rate and pathway remains only partly understood. We have developed a kinetic model that describes the effects of surface complex type and strength on Fh transformation to goethite (Gt) and hematite (Hm). Two sets of oxyanion-adsorbed Fh samples were prepared, nonbuffered and buffered, aged at 70 ± 1.5 °C, and then characterized using synchrotron X-ray scattering methods and wet chemical analysis. Kinetic modeling showed a significant decrease in the rate of Fh transformation for oxyanion surface complexes dominated by strong inner-sphere (SO42– and AsO43–) versus weak outer-sphere (NO3–) bonding and the control. The results also showed that the Fh transformation pathway is influenced by the type of surface complex such that with increasing strength of bonding, a smaller fraction of Gt forms compared with Hm. These findings are important for understanding and predicting the role of Fh in controlling the transport and fate of metal and metalloid oxyanions in natural and applied systems.