Discrimination of perceived movement velocity for fused auditory image in dichotic stimulation

1977 ◽  
Vol 61 (3) ◽  
pp. 816-819 ◽  
Author(s):  
J. A. Altman ◽  
O. V. Viskov
2018 ◽  
pp. 36-39
Author(s):  
N Ikramov ◽  
T Majidov

The article brings up data on sediment diversity at watercourse bed and on their movement in the form of ridges. The ridge form movement of sediment leads to the reduction of reservoir volume and canal cross section area, which has an effect on their carrying capacity, filling of pump station forechambers and hydroelectric station pressure basins with sediment. The presence of sediment in flow leads to abrasive deterioration of pumps, water motors and pressure pipes and to other negative consequences. Research work tasks on the study of these effects have been examined with the purpose of preventing such negative consequences. On the basis of laboratory data diagrams and relationships were obtained for ridge length, height and movement velocity vs. sediment hydraulic and geometric sizes.


2020 ◽  
Vol 11 ◽  
Author(s):  
Bruno Fernández-Valdés ◽  
Jaime Sampaio ◽  
Juliana Exel ◽  
Jacob González ◽  
Julio Tous-Fajardo ◽  
...  

Author(s):  
Michael Rheese ◽  
Eric J. Drinkwater ◽  
Hans Leung ◽  
Justin W. Andrushko ◽  
Jacob Tober ◽  
...  

2014 ◽  
Vol 40 (2) ◽  
pp. 58-67
Author(s):  
Ruta Puziene ◽  
Asta Anikeniene ◽  
Gitana Karsokiene

In the research of vertical movements of the earth’s crust, examination of statistical correlations between the measured vertical movements of the earth’s crust and territorial geo-indexes is accomplished with the help of mathematical statistical analysis. Availability of the precise repeated levelling measuring data coupled with the preferred research methodology offer a chance to determine and predict recent vertical movements of the earth’s crust. For the inquiry into recent vertical movements of the earth’s crust, a Lithuanian class I vertical network levelling polygon was used. Drawing on measurements made in the polygon, vertical velocities of earth’s crust movements were calculated along the following levelling lines. For determining the relations shared by vertical movements of the earth’s crust and territorial geo-parameters, the following territory-defining parameters are accepted. Examination of the special qualities of relations shared by vertical movements of the earth’s crust and geo-parameters in the territory under research contributed to the computation of correlation matrices. Regression models are worked out taking into consideration only particular territory-defining geo-parameters, i.e. only those parameters which exhibit the following correlation coefficient value of the vertical earth’s crust movement velocity: r ≥ 0.50. A forecast of the velocities pertaining to vertical movements of the earth’s crust in the territory under examination was made with the application of regression models. Further in the process of this research, a map was compiled specifying the velocities of vertical movements of the earth’s crust in the territory. In the eastern part of this territory, the earth’s crust rises at a rate of up to 3 mm/year; while in the western part of it, the earth crust lowers at a rate of up to –1.5 mm/year. In order to pinpoint territories characterised by temperate and regular rising/lowering or intensive rising/lowering, a map of horizontal gradients of recent vertical earth crust movements in the territory enclosed by levelling polygon was compiled.


2016 ◽  
Vol 27 ◽  
pp. 7-14 ◽  
Author(s):  
Ryo Nonaka ◽  
Takahiro Emoto ◽  
Udantha R. Abeyratne ◽  
Osamu Jinnouchi ◽  
Ikuji Kawata ◽  
...  

1998 ◽  
Vol 35 (4) ◽  
pp. 431-437 ◽  
Author(s):  
Michael P. Caligiuri ◽  
James B. Lohr ◽  
Robert K. Ruck
Keyword(s):  

1969 ◽  
Vol 1 (7) ◽  
pp. 257-258 ◽  
Author(s):  
Aubrey J. Yates ◽  
Peter J. Smith ◽  
Bryan D. Burke ◽  
Maureen A. Keane
Keyword(s):  

Sign in / Sign up

Export Citation Format

Share Document