Effect of charging on CdSe/CdS dot-in-rods single-photon emission

The photon statistics of CdSe/CdS dot-in-rods nanocrystals is studied with a method involving post-selection of the photon detection events based on the photoluminescence count rate. We show that flickering between two states needs to be taken into account to interpret the single-photon emission properties. With post-selection we are able to identify two emitting states: the exciton and the charged exciton (trion), characterized by different lifetimes and different second order correlation functions. Measurements of the second order autocorrelation function at zero delay with post- selection shows a degradation of the single photon emission for CdSe/CdS dot-in-rods in a charged state that we explain by deriving the neutral and charged biexciton quantum yields.Comment: 10 pages, 5 figure

Photon correlations for colloidal nanocrystals and their clusters

Images of semiconductor `dot in rods' and their small clusters are studied by measuring the second-order correlation function with a spatially resolving ICCD camera. This measurement allows one to distinguish between a single dot and a cluster and, to a certain extent, to estimate the number of dots in a cluster. A more advanced measurement is proposed, based on higher-order correlations, enabling more accurate determination of the number of dots in a small cluster. Nonclassical features of the light emitted by such a cluster are analyzed.Comment: 4 pages, 4 figure

Современные тенденции развития рекреационного хозяйства в Украине

Chromiferous ultramafic rocks from Campo Formoso (Bahia State, Brazil) exhibit various stages of hydrothermal alteration and weathering, each being characterized by distinct chromiferous parageneses. These Cr-bearing minerals are mainly phyllosilicates, but other phases are also present as chromiferous opal and hydroxycarbonates. Optical absorption spectra and K-edge fine structure allow a better knowledge of chromium crystal chemistry in these minerals. The first stages of chromite oxidation have been precised, and particularly the influence of structural factors was pointed out : the inversion grade of these spinels controls the evolution from a mainly direct chromite to the inverse forms (ferritchromit). Chromium ions inserted in mineral structures do not exhibit any change in the oxidation state during alteration processes. In contrast, crystal field stabilization energy (CFSE) of Cr3+ ions exhibits important variations among the studied minerals. Study of EXAFS spectra demonstrated that Cr-O distances do not change significandy among the investigated minerals, the effective oxygen charge playing the main role in the observed CFSE variations. This latter parameter explains the concentration of chromium in these minerals and contributes to the stability of some phases like clinochlores and hydroxycarbonates, where trivalent chromium has the highest CFSE.Les ultrabasites chromifères de Campo Formoso (Etat de Bahia, Brésil) montrent plusieurs stades successifs d'altération hydrothermale puis superficielle qui s'accompagnent de paragenèses chromifères variées. Les minéraux caractéristiques de ces dernières sont essentiellement des phyllosilicates, mais on note aussi d'autres phases comme la stichtite et l'opale chromifère. Les spectres d'absorption X ont permis de caractériser la cristallochimie du chrome dans ces minéraux. Les premiers stades d'oxydation des chromites ont été précisés, en particulier l'influence de la structure réelle du spinelle (degré d'inversion) qui contrôle les conditions d'évolution de la chromite. Le degré d'oxydation +3 du chrome est conservé lors des processus d'altération et seule l'énergie de stabilisation liée au champ cristallin montre des changements importants. L'étude des spectres EXAFS (Extended X-ray Absorption Fine Structure) a montré que, les distances Cr-O ne changeant pas entre les minéraux étudiés, seule la nature des ligandes a une influence sur la valeur de l'énergie de champ cristallin. Ceci explique la forte concentration en chrome de ces minéraux d'altération et contribue à la stabilité des phases comme les clinochlores ou les hydroxycarbonates où les ions Cr3+ ont la plus forte énergie de stabilisation.Calas Georges, Manceau Alain, Novikoff André, Boukili Hassan. Comportement du chrome dans les minéraux d'altération du gisement de chromite de Campo Formoso (Bahia, Brésil). In: Bulletin de Minéralogie, volume 107, 6, 1984. pp. 755-766

Structure of the Synthetic K-rich Phyllomanganate Birnessite Obtained by High-Temperature Decomposition of KMnO4. Substructures of K-rich Birnessite from 1000°C Experiment

International audienceThe structure of a synthetic potassium-rich birnessite prepared from the thermal decomposition of KMnO4 at 1000°C in air has been refined by Rietveld analysis of the powder X-ray diffraction (XRD) data, and the structure model shown to be consistent with extended X-ray absorption fine structure data. K-rich birnessite structure is a two-layer orthorhombic polytype (2O) with unit-cell parameters a = 5.1554(3) Ä, b = 2.8460(1) Ä, c = 14.088(1) Ä, α = β = γ = 90°, a/b = √3.281, and was refined in the Ccmm space group. The structure is characterized by the regular alternation of octahedral layers rotated with respect to each other by 180°. Octahedral layers are essentially devoid of vacant sites, the presence of 0.25 Mn 3+ layer cations within these layers being the main source of their deficit of charge, which is compensated for by interlayer K + cations. Mn3+ octahedra, which are distorted by the Jahn-Teller effect, are systematically elongated along the a axis (cooperative Jahn-Teller effect) to minimize steric strains, thus yielding an orthogonal layer symmetry. In addition, Mn 3+ octahedra are segregated in Mn3+-rich rows parallel to the b axis that alternate with two Mn 4+ rows according to the sequence ...-Mn3+-Mn4+-Mn4+-Mn3+-... along the a direction, thus leading to a A = 3a super-periodicity. At 350°C, the structure partially collapses due to the departure of interlayer H2O molecules and undergoes a reversible 2O-to-2H phase transition. This transition results from the relaxation of the cooperative Jahn-Teller effect, that is from the random orientation of elongated Mn 3+ octahedra

Localization and speciation of Zn in mycorrihizd roots by μSXRF and μEXAFS.

Mycorrhizae are symbiotic associations between soil fungi and plant roots, which enhance mineral nutrition for the plant, and might play an important role in metals acquisition and accumulation. The processes allowing metals mobilization in the soil, absorption by the root and/or the fungus, transfer or bioaccumulation are still poorly understood. However, the properties of mycorrhizal fungi could be used for phytoremediation, a soft technique using plants for the clean-up of metal polluted soils. In this work, mycorrhized roots of tomato plants grown in a Zn-contaminated soil were investigated. The distribution of metals and the speciation of Zn were studied at the micron scale using micro synchrotron-based X-ray fluorescence (μSXRF) and micro X-ray absorption spectroscopy (μEXAFS). Zn associated to the root was Zn malate and/or Zn citrate, and Zn associated to the fungus was Zn phyllosilicate. This study illustrates the great potential of X-ray microbeams for the study of biological samples containing various amounts of metals

Analysis of a spatio-temporal advection-diffusion model for human behaviors during a catastrophic event

In this work, using the theory of first-order macroscopic crowd models, we introduce a compartmental advection-diffusion model, describing the spatio-temporal dynamics of a population in different human behaviors (alert, panic and control) during a catastrophic event. For this model, we prove the local existence, uniqueness and regularity of a solution, as well as the positivity and $L^1$--boundedness of this solution. Then, in order to study the spatio-temporal behavioral dynamics of a population during a catastrophic event, we present several numerical simulations for different evacuation scenarios.Comment: I will correct and modify some facts and I will submit again the new versio

Formation of Zn–Ca phyllomanganate nanoparticles in grass roots

International audienceIt is now well established that a number of terrestrial and aquatic microorganisms have the capacity to oxidize and precipitate Mn as phyllomanganate. However, this biomineralization has never been shown to occur in plant tissues, nor has the structure of a natural Mn(IV) biooxide been characterized in detail. We show that the graminaceous plant Festuca rubra (red fescue) produces a Zn-rich phyllomanganate with constant Zn:Mn and Ca:Mn atomic ratios (0.46 and 0.38, respectively) when grown on a contaminated sediment. This new phase is so far the Zn-richest manganate known to form in nature (chalcophanite has a Zn:Mn ratio of 0.33) and has no synthetic equivalent. Visual examination of root fragments under a microscope shows black precipitates about ten to several tens of microns in size, and their imaging with backscattered and secondary electrons demonstrates that they are located in the root epidermis. In situ measurements by Mn and Zn K-edge extended X-ray absorption fine structure (EXAFS) spectroscopy and X-ray diffraction (XRD) with a micro-focused beam can be quantitatively described by a single-phase model consisting of Mn(IV) octahedral layers with 22% vacant sites capped with tetrahedral and octahedral Zn in proportions of 3:1. The layer charge deficit is also partly balanced by interlayer Mn and Ca. Diffracting crystallites have a domain radius of 33 Å in the ab plane and contain only 1.2 layers (not, vert, similar8.6 Å) on average. Since this biogenic Mn oxide consists mostly of isolated layers, basal 00l reflections are essentially absent despite its lamellar structure. Individual Mn layers are probably held together in the Mn–Zn precipitates by stabilizing organic molecules. Zinc biomineralization by plants likely is a defense mechanism against toxicity induced by excess concentrations of this metal in the rhizosphere