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71.
This preliminary study presents the experimental results concerning the concentrations of selected radionuclides (238U, 232K, 226Ra, 232Th) in Af?in-Elbistan, Çan, Çay?rhan, Erzurum, Göynük, Kangal, Orhaneli, Saray, Seyitömer, Soma, Tunçbilek, Yata?an and Yeniköy lignites, which are primarily utilized as fuel for thermal power plants in Turkey. Gamma-spectrometry of 39 representative lignite samples gave results with the following concentration ranges: 8 to 296 Bq/kg for 238U, 3 to 79 Bq/kg for 232Th, 17 to 360 Bq/kg for 40K, and 5 to 130 Bq/kg for 226Ra. The 238U results reported here are higher than other literature values for various world coals, earth's crust and world average. 相似文献
72.
73.
Institute of Chemical Physics, Academy of Sciences of the USSR. Translated from Zhurnal Strukturnoi Khimii, Vol. 32, No. 3, pp. 113–115, May–June, 1991. 相似文献
74.
75.
76.
S. V. Lev R. P. Zakirova Z. Saatov M. V. Gorovits N. K. Abubakirov 《Chemistry of Natural Compounds》1990,26(1):40-41
The possibility has been studied of obtaining ecdysteroids — ecdysterone and turkesterone — with the aid of a culture of the tissues and cells of the plantAjuga turkestanica. Conditions have been selected under which the yield of ecdysteroids in the culture of tissues and cells is comparable with amounts of the same substances in the organs of the whole plant.Institute of the Chemistry of Plant Substances, Academy of Sciences of the Uzbek SSR, Tashkent. Translated from Khimiya Prirodnykh Soedinenii, No. 1, pp. 51–52, January–February, 1990. 相似文献
77.
Mössbauer study of iron reduction in hematite containing mineral originated from Aswan area in Egypt
E. Kuzmann N. Eissa B. Molnár A. Vértes 《Journal of Radioanalytical and Nuclear Chemistry》1988,127(3):169-176
Mössbauer spectroscopy was used to study iron reduction in mineral originated from Aswan area in Egypt. The Mössbauer spectra of samples heat treated at 1000 °C in hydrogen atmosphere show a gradually reduction process of hematite. The main phase of sample aged for 1 h is magnetite, while alpha-iron as well as some silicates and wustite type oxide can be detected in sample aged for 3 h. Further aging of sample results in dissolution of alloying elements /Si, Al/, being present in the samples. This process starts already in samples aged at 1000 °C for 4 h, but it is more expressive in minerals heat treated at 1200 °C or 1300 °C, when all paramagnetic phases disappeared. 相似文献
78.
79.
M. S. Vigdergauz N. V. Zakharova T. R. Bankovskaya F. Z. Safaeva 《Chromatographia》1978,11(6):316-320
Summary The regularities of changes of the polarity factors with the composition of mixed stationary phases are discussed. Values
of the polarity factors of active solids, partitioning liquids and also colloidal stationary phases are compared.
Part I: ref. [1]. 相似文献
80.