Results 51 to 60 of about 416 (180)

Structural and spectroscopic studies of alkali-metal exchanged stilbites [PDF]

open access: yesMicroporous and Mesoporous Materials, 2016
Abstract The structural, infrared (IR) and Raman spectroscopic properties of alkali-metal exchanged (Na+, K+, Rb+, Cs+) zeolites with the stilbite (STI) framework have been studied by Rietveld analysis of high-resolution synchrotron X-ray powder diffraction data, micro-Raman and synchrotron IR spectroscopy at ambient conditions.
Yanmei Ma   +4 more
openaire   +1 more source

Not Available

open access: yes, 2023
Not AvailableIn-depth mineralogical understanding and characterization are necessary to explore potential applications of clinoptilolites. In this study, the clinoptilolite collected from quarries and identified as stilbite microscopically and ...
D. Arunkumar, K. K. Krishnani, Neeraj Kumar, B. Sarkar,· A. K. Upadhyay, P. B. Sawant, N. K. Chadha and R. Abisha
core   +1 more source

Stilbite from bomeki, Miyagi Prefecture, Japan.

open access: yesThe Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 1981
A calcium-rich stilbite occurs in the amygdaloidal cavity of the Upper Miocene dacite dyke at Bomeki, Miyagi Town, Miyagi Prefecture. Chemical analysis gave SiO2 56.38, Al2O3 15.89, CaO 7.94, Na2O 1.08, K2O.10, H2O+16.23 and H2O- 1.93wt%. Fe, Mn, Mg and P were not detected. This corresponds to Na1.00K.06Ca4.07Al8.96Si26.98O72•28.98H2O.
TANIGUCHI, MASAHIRO, ABE, TOMOHIKO
openaire   +2 more sources

Dissolution Kinetics of Stilbite at Various Temperatures under Alkaline Conditions

open access: yes, 2010
Experiments measuring the dissolution rates of stilbite (NaCa [Al Si O ].14H O) in pH-buffered solutions were 2 5 13 36 2 performed in batch reactors at 4, 25, 40 and 60 oC. The pH conditions of the buffer solutions ranged from 8.5 to 12.5.
ET Glover   +5 more
core   +1 more source

Controlled growth of nano-hydroxyapatite on stilbite: Defluoridation performance

open access: yes, 2017
In Ethiopia, fluoride-contaminated groundwater used for drinking has become a matter of great concern, particularly in the Rift Valley region, due to its serious health hazard (fluorosis).
Chebude, Yonas   +11 more
core   +1 more source

Amygdaloidal and other Cavity Filling Zeolites of Kuh-e-Aradeh, Central Iran [PDF]

open access: yesJournal of Sciences, Islamic Republic of Iran, 2004
Amygdaloidal, cavity- and fracture-filling zeolites in Eocene volcanic rocks from the Kuh-e-Aradeh of southern Kahrizak, in the northernmost part of Central Iran have been studied in some detail by optical, chemical analysis, SEM, and XRD techniques. The
doaj  

Zeolites occurrences prognostic using image spectral analysis in the volcanic sequences of Pequenos Lembombos, Mozambique

open access: yesMinería y Geología, 2018
The research aims at evaluating the mineral potential of the basaltic lavas of the Movene Formation, to host microcrystalline zeolites. In order to attain this goal the methods of digital image processing, geological traversing and mineralogical analysis
Elmidio Estévez-Cruz   +1 more
doaj  

Catalysis in Zeolites and Zeotypes—Cornerstone of Chemical Industry and Permanent Subject of Research

open access: yes, 2022
Mankind has been aware of zeolites since 1756, when the Swede, Axel Fredrik Cronstedt (1722–1765), observed the strange behavior of a certain natural mineral (probably stellerite with some amounts of stilbite) [...
Roman Bulánek
core   +1 more source

Controlled growth of hydroxyapatite on the surface of natural stilbite from Ethiopia: Application in mitigation of fluorosis

open access: yes, 2019
This contribution reports the preparation of a composite material based on a natural zeolite rich in calcium, stilbite, on which surface nanosized hydroxyapatite is grown under controlled conditions.
Chebude, Yonas   +3 more
core   +1 more source

Zeolites in the Granitic Rocks of Chugoku District, Southwest Japan [PDF]

open access: yes, 1994
Ca-zeolites such as laumontite, stilbite and chabazite were found in the granitic rocks of both magnetite and ilmenite series of late Cretaceous to Tertiary age developed widely in the Chugoku district. These zeolites occur (1) in veins of various scale,
KITAGAWA, Ryuji   +4 more
core   +1 more source

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