scholarly journals A brief summary on formalizing parallel tensor distributions redistributions and algorithm derivations.

2015 ◽  
Author(s):  
Martin D. Schatz ◽  
Tamara G. Kolda ◽  
Robert van de Geijn
Keyword(s):  
2005 ◽  
Vol 400-401 ◽  
pp. 18-21 ◽  
Author(s):  
Craig S. Hartley ◽  
Y. Mishin
Keyword(s):  

1991 ◽  
Vol 113 (1) ◽  
pp. 119-125 ◽  
Author(s):  
G. L. Morrison ◽  
M. C. Johnson ◽  
G. B. Tatterson

The flow field inside a seven-cavity labyrinth seal with a 0.00127-m clearance was measured using a 3-D laser-Doppler anemometer system. Through the use of this system, the mean velocity vector and the entire Reynolds stress tensor distributions were measured for the first, third, fifth, and seventh cavities of the seal. There was one large recirculation region present in the cavity for the flow condition tested, Re = 28,000 and Ta = 7000. The axial and radial mean velocities as well as all of the Reynolds stress terms became cavity independent by the third cavity. The azimuthal mean velocity varied from cavity to cavity with its magnitude increasing as the flow progressed downstream.


2000 ◽  
Vol 32 (3) ◽  
pp. 491-503 ◽  
Author(s):  
David Hartley ◽  
Robin W. Tucker ◽  
Philip A. Tuckey ◽  
Tevian Dray
Keyword(s):  

2015 ◽  
Vol 58 (4) ◽  
Author(s):  
Claudio Ferrari ◽  
Maurizio Bonafede ◽  
Elisa Trasatti

Pressurized cavities are commonly used to compute ground deformation in volcanic areas: the set of available solutions is limited and in some cases the moment tensors inferred from inversion of geodetic data cannot be associated with any of the available models. Two different source models (pure tensile source, TS and mixed tensile/shear source, MS) are studied using a boundary element approach for rectangular dislocations buried in a homogeneous elastic medium employing a new C/C++ code which provides a new implementation of the dc3d Okada fortran code. Pressurized triaxial cavities are obtained assigning the overpressure in the middle of each boundary element distributed over the cavity surface. The MS model shows a moment domain very similar to triaxial ellipsoidal cavities. The TS and MS models are also compared in terms of the total volume increment limiting the analysis to cubic sources: the observed discrepancy (~10%) is interpreted in terms of the different deformation of the source interior which provides significantly different internal contributions (~30%). Comparing the MS model with a Mogi source with the some volume, the overpressure of the latter must be ~37% greater than the former, in order to obtain the same surface deformation; however the outward expansion and the inner contraction separately differ by ~±10% and the total volume increments differ only by ~2%. Thus, the density estimations for the intrusion extracted from the MS model and the Mogi model are nearly identical.


1997 ◽  
Vol 06 (06) ◽  
pp. 717-740 ◽  
Author(s):  
Tevian Dray
Keyword(s):  

Tensor distributions and their derivatives are described without assuming the presence of a metric. This provides a natural framework for discussing tensor distributions on manifolds with degenerate metrics, including in particular metrics which change signature.


1988 ◽  
Author(s):  
G. L. Morrison ◽  
M. C. Johnson ◽  
G. B. Tatterson

The flow field inside an annular seal with a 0.00127 m clearance was measured using a 3-D laser Doppler anemometer system. Through the use of this system, the mean velocity vector and the entire Reynolds stress tensor distributions were measured for the entire length of the seal (0.0373 m). The seal was operated at a Reynolds number of 27,000 and a Taylor number of 6,600.


2007 ◽  
Vol 40 (2) ◽  
pp. 362-370 ◽  
Author(s):  
Andreas Leineweber

The anisotropic microstrain distribution resulting from an isotropic distribution of a field tensor (rank 0 or 2), the latter being connected with strain by an anisotropic property tensor (rank 2 or 4), is analyzed. It is shown that the anisotropy of the resulting line broadening is a direct consequence of the anisotropy of the property tensor. Various physical scenarios leading to such a type of line broadening are discussed.


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