Results 21 to 30 of about 35,817 (223)

Modelling environmental factors correlated with podoconiosis: a geospatial study of non-filarial elephantiasis [PDF]

open access: yes, 2014
Introduction The precise trigger of podoconiosis — endemic non-filarial elephantiasis of the lower legs — is unknown. Epidemiological and ecological studies have linked the disease with barefoot exposure to red clay soils of volcanic origin ...
Atkinson, Peter M   +6 more
core   +2 more sources

Mineralogy of Vera Rubin Ridge in Gale Crater from the Mars Science Laboratory CheMin instrument [PDF]

open access: yes, 2020
Gale crater was selected as the landing site for the Mars Science Laboratory Curiosity rover because of orbital evidence for a variety of secondary minerals in the lower slopes of Aeolis Mons (aka Mount Sharp) that indicate changes in aqueous conditions ...
Achilles, C. N.   +29 more
core   +4 more sources

Natural Mordenite from Spain as Pozzolana

open access: yesMolecules, 2020
This work deals with anomalous concentrations of natural mordenite in the southeast of Spain. The X-ray diffraction (XRD) and scanning electron microscopy (SEM) studies evidenced that the samples contain mainly monomineral zeolitic phase of mordenite (70%
Leticia Presa   +3 more
doaj   +1 more source

Smectite promotes probiotic biofilm formation in the gut for cancer immunotherapy

open access: yesCell Reports, 2021
Summary: Administration of probiotics to regulate the immune system is a potential anti-tumor strategy. However, oral administration of probiotics is ineffective because of the poor inhabitation of exogenous bacteria in host intestines.
Congwei Han   +11 more
doaj   +1 more source

Weathering microenvironments on feldspar surfaces: implications for understanding fluid-mineral reactions in soils [PDF]

open access: yes, 2008
The mechanisms by which coatings develop on weathered grain surfaces, and their potential impact on rates of fluid-mineral interaction, have been investigated by examining feldspars from a 1.1 ky old soil in the Glen Feshie chronosequence, Scottish ...
Blum   +8 more
core   +2 more sources

Adsorption of sulphuric acid on smectite from acidic aqueous solutions Adsorção de ácido sulfúrico em esmectita de soluções aquosas ácidas

open access: yesCerâmica, 1999
The adsorption of sulphuric acid on smectite from acidic aqueous solutions was studied. The amounts of cations dissolved in each equilibrium solution were determined by chemical analysis.
E. L. Tavani, C. Volzone
doaj   +1 more source

Modification of smectite structure by sulfuric acid and characteristics of the modified smectite [PDF]

open access: yesJournal of Agricultural Sciences (Belgrade), 2011
Bentonite samples from Petrovac and Aleksinac were treated with sulfuric acid of different molarities. Differences in structure and texture of the initial and modified bentonite were determined by chemical analysis and Xraypowder diffraction (XRPD ...
Tomić Zorica P.   +5 more
doaj   +1 more source

<i>LamelODF</i>: a MATLAB-based toolbox for orientation distribution analysis and mapping of lamellar minerals for laboratory and synchrotron X-ray diffractometers. [PDF]

open access: yesJ Appl Crystallogr
LamelODF is a MATLAB‐based toolbox aimed at simplifying the automated extraction of orientation distribution functions from 2D X‐ray diffraction data of lamellar minerals in transmission mode. It accommodates both laboratory and synchrotron data formats, providing an integrated pipeline from raw data to spatially resolved textural maps, enabling robust
Dazas B   +5 more
europepmc   +2 more sources

Evidence for silicate dissolution on Mars from the Nakhla meteorite [PDF]

open access: yes, 2013
Veins containing carbonates, hydrous silicates and sulphates that occur within and between grains of augite and olivine in the Nakhla meteorite are good evidence for the former presence of liquid water in the Martian crust.
Ashworth   +39 more
core   +1 more source

Charge Heterogeneity in Smectites

open access: yesClays and Clay Minerals, 1983
AbstractThe heterogeneity of sites for Ca→K exchange was examined by microcalorimetry in the <0.2-μm fractions of some selected smectites. Six groups of sites, ranging in exothermic exchange enthalpy (-d(ΔHx)/dx) from 5.7 to 10.9 kJ/eq were identified.
Talibudeen, O., Goulding, K. W. T.
openaire   +1 more source

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