The radioactive tracer method of studying the erosion of the refractory lining in the sintering zone of rotary kilns

Refractories ◽  
1977 ◽  
Vol 18 (3-4) ◽  
pp. 223-226
Author(s):  
V. I. Shubin ◽  
V. I. Nikonorov ◽  
Yu. A. Kurbatov ◽  
O. M. Stanulionis ◽  
V. P. Vasil'ev ◽  
...  



1989 ◽  
Vol 25 (8) ◽  
pp. 330-334
Author(s):  
A. Owezarezyk ◽  
M. Strzelecki ◽  
St. Szpilowski ◽  
R. Wierzchnicki ◽  
T. Basiński




1998 ◽  
Vol 180 (1) ◽  
pp. 159-162 ◽  
Author(s):  
Dirk Schüler ◽  
Edmund Baeuerlein

ABSTRACT Iron uptake and magnetite (Fe3O4) crystal formation could be studied in the microaerophilic magnetic bacteriumMagnetospirillum gryphiswaldense by using a radioactive tracer method for iron transport and a differential light-scattering technique for magnetism. Magnetite formation occurred only in a narrow range of low oxygen concentration, i.e., 2 to 7 μM O2 at 30°C. Magnetic cells stored up to 2% iron as magnetite crystals in intracytoplasmic vesicles. This extraordinary uptake of iron was coupled tightly to the biomineralization of up to 60 magnetite crystals with diameters of 42 to 45 nm.









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