Results 71 to 80 of about 4,204 (206)
Discrete breathers for understanding reconstructive mineral processes at low temperatures [PDF]
Reconstructive transformations in layered silicates need a high tem- perature in order to be observed. However, very recently, some systems have been found where transformation can be studied at temperatures 600 C below the lowest experimental results ...
Alba, M. D. +4 more
core +2 more sources
Abstract Seismic surveys are essential for studying the Earth's subsurface. However, the interpretation of seismic surveys requires a link between field data and rock physical properties by linking laboratory‐derived data from drill core samples with borehole information and seismic images.
Markus Rast +4 more
wiley +1 more source
The origin and implications of clay minerals from Yellowknife Bay, Gale crater, Mars [PDF]
The Mars Science Laboratory (MSL) rover Curiosity has documented a section of fluvio-lacustrine strata at Yellowknife Bay (YKB), an embayment on the floor of Gale crater, approximately 500 m east of the Bradbury landing site. X-ray diffraction (XRD) data
Bristow, Thomas F. +2 more
core +1 more source
Abstract CM (Mighei‐type) carbonaceous chondrites host abundant OH/H2O‐bearing phyllosilicates formed from water‐rock reactions in primitive planetesimals. Their infrared (IR) spectral features resemble those of C‐type asteroids, making laboratory analyses of CMs essential for interpreting asteroid observations.
W. M. Lawrence, B. L. Ehlmann
wiley +1 more source
Current treatments often fall short in managing IBS effectively. Silicolgel, an enterosorbent, reduced IBS and other gastrointestinal symptoms in 90% of IBS patients compared to 20% in those on placebo. Enterosorbents are not currently recommended for IBS; silicolgel is a widely available, affordable option for patients with IBS‐D and IBS‐M.
O. Kuzminska +3 more
wiley +1 more source
Structural iron in dioctahedral and trioctahedral smectites: a polarized XAS study [PDF]
The chemical form of structural Fe in smectites influences many physicochemical properties of these clay minerals. Powder EXAFS data for structural Fe in smectites have been reported; however, the preferred orientation of clay platelets with respect to the X-ray beam may lead to erroneous conclusions on the local chemical environment.
Finck, N., Schlegel, M. L., Bauer, A.
openaire +4 more sources
Abstract Non‐exchangeable potassium (Nex‐K) released slowly from minerals is a key component of long‐term K fertility of agricultural soils. Two extraction methods are widely used to determine soil Nex‐K: the boiling nitric acid (HNO3) method and the tetraphenylborate (TPB) method.
Kohei Kurokawa +7 more
wiley +1 more source
BACKGROUND The mineralogy, chemistry and crystal structure of hydrothermal clay minerals from various geologic settings have been studied to reflect the fluid-rock interaction and physico-chemical evolution of fluids in hydrothermal environments. However,
CAO Kai-jun +4 more
doaj +1 more source
Weathering of the Ethiopian volcanic province: a new weathering index to characterize and compare soils [PDF]
© Walter de Gruyter Berlin/Boston 2015.Soil formation occurs through numerous physical and chemical weathering processes acting to alter the parent rock on the Earths surface.
Baxter, PJ +6 more
core +1 more source
This review examines how coating Li‐ion battery separators with 1D, 2D, and 3D structured natural clay minerals influences their electrochemical and mechanical performance. It classifies 15 types of clay minerals and highlights structure–property correlations to offer practical design strategies for high‐performance separators in next‐generation energy
Inseo Ko +6 more
wiley +1 more source

