146 research outputs found
Clay mineralogy and its effect on physical properties in the Gulf of Mexico northwestern continental slope
The clay mineral composition of sediments deposited in the last six oxygen isotope stages in the Gulf of Mexico continental slope was characterized. Smectite and illite were found to be the two major clay minerals of the clay fraction while kaolinite, chlorite and quartz were present in the clay fraction but in less proportions. Variations in clay mineral abundances, especially in the relative abundances of smectite and illite, were identified in relation to climate changes. Smectite was the most abundant mineral in sediments of the current (stage 1) and last interglacial maxima (stage 5) while illite dominates the clay min-eralogy of sediments from the last glacial maximum (stage 2). Relationships between clay mineralogy and physical properties were investigated as well. Significant positive correla-tions were found between Atterberg limits with the smectite content of the bulk sediment and with clay content. However, the relationship with smectite yielded a significantly higher correlation coefficient. Smectite and clay content also affect the natural water con-tent of sediments and its changes with depth
Functional liposomes and supported lipid bilayers: towards the complexity of biological archetypes
Ultrafine Mineral Associations in Superhigh-Organic-Sulfur Kentucky Coals
Two high-organic-sulfur Kentucky coals, the eastern Kentucky River Gem coal and the western Kentucky Davis coal, are examined by scanning electron microscopy (SEM) and transmission electron microscopy (TEM), both including elemental analysis by energy-dispersive spectroscopy (EDS). From the SEM–EDS analysis, it is observed that the western Kentucky coal had areas with Pb and Cd in addition to the expected Fe and S and the eastern Kentucky coal had individual Fe–S-rich areas with La and Ni and with Si, Al, Cr, Ni, and Ti. TEM and selected area electron diffraction (SAED) analyses demonstrate that anglesite with a rim of Pb-bearing amorphous Fe-oxide occurs in the western Kentucky coal. Melanterite, an Fe-sulfate, with minor Al, Si, and K EDS peaks, suggests that clay minerals may be in close association with the sulfate, is also detected in the coal. A polycrystalline metal in the eastern Kentucky sample with a composition similar to stainless steel is adjacent to an Al-rich shard. Euhedral pyrite grains surrounded by kaolinite and gibbsite are detected. Overall, it is noted that element associations should not be assumed to be organic just because minerals cannot be seen with optical microscopy or with standard bulk analytical techniques, such as X-ray diffraction (XRD)
Nanostructured Surfactant-Based Systems for the Removal of Polymers from Wall Paintings: A Small-Angle Neutron Scattering Study
n/
Parallel and perpendicular cascades in solar wind turbulence
MHD-scale fluctuations in the velocity, magnetic, and density fields of the solar wind are routinely observed. The evolution of these fluctuations, as they are transported radially outwards by the solar wind, is believed to involve both wave and turbulence processes. The presence of an average magnetic field has important implications for the anisotropy of the fluctuations and the nature of the turbulent wavenumber cascades in the directions parallel and perpendicular to this field. In particular, if the ratio of the rms magnetic fluctuation strength to the mean field is small, then the parallel wavenumber cascade is expected to be weak and there are difficulties in obtaining a cascade in frequency. The latter has been invoked in order to explain the heating of solar wind fluctuations (above adiabatic levels) via energy transfer to scales where ion-cyclotron damping can occur. Following a brief review of classical hydrodynamic and magnetohydrodynamic (MHD) cascade theories, we discuss the distinct nature of parallel and perpendicular cascades and their roles in the evolution of solar wind fluctuations
Removal of acrylic coatings from works of art by means of nanofluids: understanding the mechanism at the nanoscale
n/
On the interaction and nanoplasmonics of gold nanoparticles and lipoproteins
The extracellular space is nanostructured, populated by heterogeneous classes of nanoparticles, e.g., extracellular vesicles and lipoproteins, which “made by cells for cells'' mediate intercellular, inter-organ, cross-species, and cross-kingdom communication. However, while techniques to study ENP biology in-vitro and in-vivo are becoming available, knowledge of their colloidal and interfacial properties is poor, although much needed. This paper experimentally shows, for the first time, that the aggregation of citrate-capped gold nanoparticles (AuNPs) triggered by lipid vesicle membranes and the related characteristic redshift of the plasmonic signature also applies/extends to lipoproteins. Such interaction leads to the formation of AuNP-lipoprotein hybrid nanostructures and is sensitive to lipoprotein classes and AuNP/lipoprotein molar ratio, paving the way to further synthetic and analytical developments
Polymer Film Dewetting by Water/Surfactant/Good-Solvent Mixtures: A Mechanistic Insight and Its Implications for the Conservation of Cultural Heritage
Inorganic Nanoparticles Modify the Phase Behavior and Viscoelastic Properties of Non-lamellar Lipid Mesophases
- …