Structural features hindering deformation-band formation in thermally hardened carbon steels

2007 ◽  
Vol 2007 (1) ◽  
pp. 33-35
Author(s):  
I. A. Vakulenko ◽  
V. G. Razdobreev
Author(s):  
Larry F. Lemanski

Electron-dense plaques, often seen in association with the plasma membranes of pre-heartbeat salamander myocardial cells, appear to be directly involved in early Z band formation. In differentiating myocardial cells of higher vertebrates, Z band material has been observed in close proximity to the plasma membranes and as isolated electron-dense material in the deep cytoplasm. The present study explores the fine structural features of Z band formation in salamander myocardium from early tailbud embryos (Harrison stage 25) through the adult. Hearts were fixed In a 0.1 M phosphate buffered formaldehyde-glutaraldehyde-picric acid-styphnic acid mixture and were post-fixed and embedded using standard methods.


2003 ◽  
Vol 140 (1) ◽  
pp. 1-9 ◽  
Author(s):  
S. E. TINDALL ◽  
G. H. DAVIS

Tectonic joints localized within deformation band shear zones on the Kaibab uplift in Utah, USA, show the same spacing and distribution characteristics as joints controlled by primary lithological mechanical stratigraphy, despite the fact that deformation band shear zones are secondary structural features oblique to primary sedimentary layers. The spacing and distribution of joints that traverse deformation band shear zones are important factors in the permeability and connectivity of sandstone reservoirs compartmentalized by deformation band shear zones.


2019 ◽  
Vol 1 (1) ◽  
pp. 71-76
Author(s):  
Myanovska Ya ◽  
Kamkina L ◽  
Ivaschenko V ◽  
Ankudinov R ◽  
Dvorkovyy O

The purpose of the work is to develop methods for the treatment of oxidized quartzite, using methods of electochemical effects on hematite grains, converting it into magnetite for further magnetic separation. In laboratory conditions, the basic parameters of the process of recovery of hematite component of oxidized quartzite in aqueous suspension to magnetite with its magnetic properties have been established. When conducting the process of recovery of hematite to magnetite, the possibility of replacement of high-alkaline electrolytes with neutral salts formed by solutions has been established.The influence of structural features of experimental reactors on the recovery of hematite to magnetite has been developed and analyzed; the ability of membrane materials to effectively separate the anolytic and catholic spaces; the influence of electrode materials - anode and cathode, on the magnetization process; electrical parameters of electrical influence on the course of the process; composition of the electrolyte in the process of magnetization. The fiberglass membrane was shown to have a better ability to separate the anolytic and katholyte; maximum degrees of magnetization obtained when using electrodes from low carbon steels; optimal values of the degree of recovery of hematite in laboratory conditions were obtained at 15-25 V and 2.0-4.0 A. The thermodynamic possibility and realization of the processes of reduction of oxidized ores in aqueous solutions of electrolytes at low temperatures with obtaining the magnetic phase are shown. For electrolysis, high alkaline electrolytes can be replaced by electrolytes based on chloride and sulfate salts. The best results are obtained using NH4Cl ammonium chloride.


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