Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide
T. Gaćeša
; Research Department, Association of Yugoslav Cement Producers, Zagreb, Croatia, Yugoslavia
I. Jelenić
; Research Department, Association of Yugoslav Cement Producers, Zagreb, Croatia, Yugoslavia
APA 6th Edition Gaćeša, T. i Jelenić, I. (1967). Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide. Croatica Chemica Acta, 39 (1), 59-63. Preuzeto s https://hrcak.srce.hr/208110
MLA 8th Edition Gaćeša, T. i I. Jelenić. "Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide." Croatica Chemica Acta, vol. 39, br. 1, 1967, str. 59-63. https://hrcak.srce.hr/208110. Citirano 04.03.2021.
Chicago 17th Edition Gaćeša, T. i I. Jelenić. "Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide." Croatica Chemica Acta 39, br. 1 (1967): 59-63. https://hrcak.srce.hr/208110
Harvard Gaćeša, T., i Jelenić, I. (1967). 'Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide', Croatica Chemica Acta, 39(1), str. 59-63. Preuzeto s: https://hrcak.srce.hr/208110 (Datum pristupa: 04.03.2021.)
Vancouver Gaćeša T, Jelenić I. Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide. Croatica Chemica Acta [Internet]. 1967 [pristupljeno 04.03.2021.];39(1):59-63. Dostupno na: https://hrcak.srce.hr/208110
IEEE T. Gaćeša i I. Jelenić, "Determination of Correction Factor for Preferential Crystallite
Orientation in Quantitative X-ray Analysis of Calcium Hydroxide", Croatica Chemica Acta, vol.39, br. 1, str. 59-63, 1967. [Online]. Dostupno na: https://hrcak.srce.hr/208110. [Citirano: 04.03.2021.]
Sažetak In the work of A. Bezjak and I. Jelenic1 an expression was derived for
correcting the intensities of .X-ray reflections from samples with preferential crystallite orientation.