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We describe probes of a local electric field, which are capable of detecting an electric charge as small as the charge of one electron e, operational under ambient conditions and having a spatial resolution down to 100nm. The submicron-sized probes were made from a high-density high-mobility two-dimensional electron gas, which is sensitive to the presence of electric charges near its surface. We demonstrate the possibility of using such microprobes for life-science applications by measuring an electric response of individual yeast cells to abrupt changes in their environment.
No abstract is provided for this article.
Iron is an important element involved in the formation of sedimentary-hosted copper deposits. Its accumulation in sedimentary basins and subsequent redistribution ultimately affect the position of copper mineralization. The Udokan copperstone deposit contains considerable Fe reserves as magnetite and hematite. The Fe oxides form disseminated and layered aggregates in both Cu-bearing horizons and host metasandstones. The layered aggregates of Fe oxides contain detrital (zircon, chromite and apatite) and authigenic (a Th silicate) components. The ironstones bear chemical features both of clastic and chemical sediments. The enrichment of ironstones in Cr, Zr and Hf is due to the presence of relics of detrital chromite and zircon. The presence of rare earth elements (REEs), U, and Th in composition of ironstones is a result of chemical precipitation/sorption. According to the LA-ICP-MS data, Al, Mg, and V are the most significant trace elements of magnetite, whereas Ti and V are hosted in hematite. The extremely high Ti, Cr and Cu contents of magnetite are associated with inclusions of minerals of these elements. In hematite, the high Ti contents are due to inclusions of rutile or titanite. The correlations between the trace elements in Fe oxides reflect the mineral assemblages characteristic of two stages of sediment transformation: (i) earlier diagenetic with the formation of a hematite-rutile assemblage and early Cu sulphides and Th and REE mineralization and (ii) later metamorphic, which is related to the formation of magnetite metacrysts and recrystallization of Cu sulphides. The Fe-rich sediments formed at a river–sea geochemical barrier as a result both of sedimentation of clastic Fe oxides and flocculation of dissolved iron. The maturation of gel and lithification of sediments were accompanied by desorption of metals that accumulated in the ferruginous sediments. Some of them formed the authigenic phases (like Th), while others were isomorphically incorporated in other authigenic minerals (e.g., Nb, Ta and Sn in rutile).
All known superfluid and superconducting states of condensed matter are enabled by composite bosons (atoms, molecules, Cooper pairs) made of an even number of fermions. Temperatures where such macroscopic quantum phenomena occur are limited by the lesser of the binding energy and the degeneracy temperature of the bosons. High critical temperature cuprate superconductors set the present record of ~100 K. Here we propose a design for artificially structured materials to rival this record. The main elements of the structure are two monolayers of a transition metal dichalcogenide (TMD) and an atomically thin hexagonal boron nitride (hBN) spacer. Electrons and holes generated in the system would accumulate in the separate TMD layers and form bosonic bound states --- the indirect excitons. The resultant degenerate Bose gas of excitons would exhibit macroscopic occupation of a quantum state, vanishing viscosity, and superconductivity at high temperatures.
We report strong variations in the Raman spectra for different single-layer graphene samples obtained by micromechanical cleavage. This reveals the presence of excess charges, even in the absence of intentional doping. Doping concentrations up to ∼1013cm−2 are estimated from the G peak shift and width and the variation of both position and relative intensity of the second order 2D peak. Asymmetric G peaks indicate charge inhomogeneity on a scale of less than 1μm.
Geological position and composition data for ferruginous-siliceous sediments from Babaryk massive sulfide field of Alexandrinka ore area of Southern Urals are presented. Ore control (gossans) and ore free (jasperites) facies are diagnosed by mineralogical composition and trace elements content. The relicts of chloritized hyaloclasts, zonal crystals of pyrite and hematite-quartz pseudomorph on chalcopyrite clasts were established in gossans. Biomorphiс and clasts-like structure carbonate consist of monheimite. Composition of the accessory minerals such as apatite, monazite, REE-containing epidote, and leucoxene is described. In jasperites hematite-quartz isolations are characterized breccia texture with a non-uniform internal structure, spherolitic and cocarde microstructure with garnet and needle crystals of hematite. Biomorphic structures sharply differ in ore control and ore free facies. Distribution of trace elements in ferruginous-siliceous sediments is considered. The received data are compared with similar sediments from Alexandrinka VMS deposit.