Model Investigations of the Spreading of Heavy Gases Released from an Instantaneous Volume Source at the Ground

Author(s):  
A. Lohmeyer ◽  
R. N. Meroney ◽  
E. J. Plate
Keyword(s):  
Author(s):  
H. Ramebäck ◽  
S. Jonsson ◽  
T. Vidmar

AbstractThe efficiency transfer procedure from a geometry where a volume source was placed directly on the endcap of a germanium detector to three different distant geometries was carried out using the EFFTRAN code. One of these distant geometries included absorbers consisting of poly(methyl methacrylate). The efficiency transfer to this geometry therefore had to be realized as a two-stage transfer, since a direct efficiency transfer is not possible using EFFTRAN in such a case. Efficiency transfer to all three distant geometries yielded results which can be considered as fit-for-purpose in e.g. most of the applications of gamma ray spectrometry.


1992 ◽  
Author(s):  
Hiroshi Naitou ◽  
Osamu Fukumasa ◽  
Kouji Mutou

1998 ◽  
Vol 69 (2) ◽  
pp. 974-976 ◽  
Author(s):  
M. Nishiura ◽  
M. Sasao ◽  
M. Wada

2014 ◽  
Vol 77 (13) ◽  
pp. 1563-1566
Author(s):  
M. I. Gurevich ◽  
O. V. Tel’kovskaya ◽  
B. K. Chukbar ◽  
D. A. Shkarovskiy

2020 ◽  
Vol 32 (11) ◽  
pp. 116602
Author(s):  
Yuhang Li ◽  
Ke Chen ◽  
Hongwei Wang ◽  
Yunxiang You

Wave Motion ◽  
1988 ◽  
Vol 10 (5) ◽  
pp. 453-463
Author(s):  
D.G.H. Tan ◽  
R.H.T. Bates
Keyword(s):  

2010 ◽  
Vol 77 (1) ◽  
pp. 385-391 ◽  
Author(s):  
Kristen E. Gibson ◽  
Kellogg J. Schwab

ABSTRACTTangential-flow ultrafiltration was optimized for the recovery ofEscherichia coli,Enterococcus faecalis,Clostridium perfringensspores, bacteriophages MS2 and PRD1, murine norovirus, and poliovirus seeded into 100-liter surface water (SW) and drinking water (DW) samples. SW and DW collected from two drinking water treatment plants were then evaluated for human enteric viruses.


Geophysics ◽  
1993 ◽  
Vol 58 (4) ◽  
pp. 475-475 ◽  
Author(s):  
Michel Bouchon

We present a method of calculation to simulate the propagation of acoustic and elastic waves generated by a borehole source embedded in a layered medium. The method is formulated as a boundary element technique where the Green’s functions are calculated by the discrete wavenumber method. The restrictive assumptions are that the borehole is cylindrical and that its axis runs normal to the layer interfaces. The physics of the method rely on Huygens’s principle that states that a diffracting boundary—the borehole wall in the present case—can be represented as a distribution of secondary sources. The borehole is discretized into small cylindrical elements and each element is represented by three sources: a volume source representing the wavefield diffracted in the fluid and two surface forces that give rise to the elastic wavefield radiated outside the borehole. The strength of each source is obtained by solving the linear system of equations that describes the boundary conditions at the borehole wall. The method is used to generate synthetic acoustic logs and to investigate the wavefield radiated into the formation. The simulations considered display the Stoneley wave reflections at the bed boundaries and show the importance of the diffraction that takes place where the borehole wall intersects the layer interfaces.


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