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In situ X-ray diffraction study of enstatite up to 12 GPa and 1473 K and equations of state
X-ray diffraction study of enstatite 12 GPa 1473 K equations of state
2012/4/1
Crystal structures and phase transitions of enstatite (MgSiO ) were studied by in situ X-ray dif-fraction experiments using synchrotron radiation and a multi-anvil high-pressure apparatus at pres-/c t...
Quantitative Clay Mineral Analysis Using Simultaneous Linear Equations
Cation-exchange capacity Chemical analysis Linear equations Mineral analysis Quantitative mineralogy Weight loss
2012/1/13
A program of simultaneous linear equations has been developed to calculate component proportions and/or component property values for mineral mixtures in soil clays and sediments. The analysis is base...
Closed Form Equations for X-Ray Diffraction by Interstratified Clay Systems—I: Randomly Occurring Interlamellar Species
Closed Form Equations X-Ray Diffraction Interstratified Clay Systems Randomly Occurring Interlamellar Species
2012/2/14
A closed form equation is derived for the calculation of the oriented diffraction pattern given by single particle size layer silicates having randomly interstratified interlamellar species. A general...