Öz
Fluorescence radiation is being known as "unwanted incident", while XRD determination, and various methods arc in use to
solve this secondary radiation. In this study, fluorescence radiation is especially created in order to show the possibility of quantitative analysis
with the help of this secondary radiation. Some selected standards, which have different quantity of iron content, were chosen and Cutarget
was intentionaly used during XRD determination, in order to cause fluorescence radiation in different intensity. Finally the positive relation
was detected between the total iron content and fluorescence radiation intensity. It takes only 40 seconds to find the quantity of total
iron in the analysed sample with the suggested method. In addition, another important result of this study is that the radiation intensity have
direct relation with the total iron content in the sample, regardless of iron combination with other elements.
Anahtar Kelimeler
Kaynakça
- Graham, A.R., 1969, Quantitative determination of hexagonal and monoclinic pyrrotite by X—ray diffraction: Can.Mineralogist, 10,4-24.
- Gulbrandsen, R.A., 1969, A method of X-ray analysis for determining the ratio of calcite to dolomite in mineral mixture: US, Geol.Surv.Bull., 1111-D, 147-152.
- Gunatilaka, H.A. ve Till, R. 1971, A precise and accurate method for the quantitative determination of carbonate minerals by X—ray diffraction using a spiking technique: Mineral Mag., 38, 481-487.
- Hutchinson, C.S., 1976, Laboratory handbook of Petrografic techniques.: A Wiley-lnterscience Publication, John Wiley and Sons, Nevv York, London, Sydney, Toronto.
- Johnson, W. ve Andrevvs, K.W., 1962, X-ray examination of aluminosilicatcs:Trans.Brit.Ceram.Soc., 61, 724.
- Klug, H.P. ve Alexandre, L., 1973, X-ray diffraction procedures: John Wiley and Sons Inc., Nevv York, London.
- Norrish, K. ve Taylor, R.M., 1962, Quantitative analysis by X-ray diffraction: Clay Minerals Bull., 5, 98-109.
- Schoen, R., 1962, Semi-quantitative analysis of chlorites by X—ray diffraction: Am.Mineralogist, 47, 1384.
Öz
Kaynakça
- Graham, A.R., 1969, Quantitative determination of hexagonal and monoclinic pyrrotite by X—ray diffraction: Can.Mineralogist, 10,4-24.
- Gulbrandsen, R.A., 1969, A method of X-ray analysis for determining the ratio of calcite to dolomite in mineral mixture: US, Geol.Surv.Bull., 1111-D, 147-152.
- Gunatilaka, H.A. ve Till, R. 1971, A precise and accurate method for the quantitative determination of carbonate minerals by X—ray diffraction using a spiking technique: Mineral Mag., 38, 481-487.
- Hutchinson, C.S., 1976, Laboratory handbook of Petrografic techniques.: A Wiley-lnterscience Publication, John Wiley and Sons, Nevv York, London, Sydney, Toronto.
- Johnson, W. ve Andrevvs, K.W., 1962, X-ray examination of aluminosilicatcs:Trans.Brit.Ceram.Soc., 61, 724.
- Klug, H.P. ve Alexandre, L., 1973, X-ray diffraction procedures: John Wiley and Sons Inc., Nevv York, London.
- Norrish, K. ve Taylor, R.M., 1962, Quantitative analysis by X-ray diffraction: Clay Minerals Bull., 5, 98-109.
- Schoen, R., 1962, Semi-quantitative analysis of chlorites by X—ray diffraction: Am.Mineralogist, 47, 1384.
Ayrıntılar
| Birincil Dil | İngilizce |
|---|---|
| Konular | Mühendislik |
| Bölüm | Makaleler |
| Yazarlar | |
| Yayımlanma Tarihi | 1 Nisan 1990 |
| Yayımlandığı Sayı | Yıl 1990 Cilt: 111 Sayı: 111 |
Kaynak Göster
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