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Volume 12, Issue 2, 2005
Civil and Mechanical Engineering
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Behavior of Gravely Sand Using Critical State Concepts
S.M. Hosseini (PhD.)
S.M. Haeri [PhD.]
D.G. Toll [PhD.]
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A series of consolidated undrained triaxial tests were performed in order to understand the behavior of a gravely sand. The material was selected from Tehran alluvium and is classified as gravely sand in the Unified Soil Classification System. Critical state concepts were used for interpretation of the behavior of the soil. The critical state line in q-p' space was reasonably unique. However, it was not possible to define a unique critical state line in e-ln p' space. The overall scatter, in the critical state line for the gravely sand studied, was \pm 0.04, in terms of void ratio. Two reasons can be identified for this scatter. The first reason is the inevitable error in void ratio calculation and the second is that the behavior of this material, even at a critical state, is fabric and structure dependant. On the basis of these tests, it has been concluded that, for this material, a critical state zone with upper and lower limits can be defined. Nevertheless, a unique boundary surface can be defined by presenting the data in normalized stress space. |
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Effect of Gr/Re on Mixed Convection and Combined Mixed Convection-Radiation Heat Transfer Within a Vertical Channel with Variable Wall Temperature
F. Bazdidi-Tehrani (PhD.)
M. Nezamabadi [PhD.]
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The present paper investigates, numerically, the effect of the Grashof number to a Reynolds number ratio (Gr/Re), on fluid flow and heat transfer within a vertical channel for two cases: Mixed (natural-forced) convection and combined mixed convection-radiation. The flow in the channel is assumed to be two-dimensional, laminar and steady. The wall temperature is defined as a linear function of the channel height. When dealing with the combined mixed convection-radiation case, radiational properties have been taken into account, both for the walls and the fluid. The fluid has a Prandtl number of 0.71 and it is radiationally assumed as a participating medium. A comparison between the two cases at a constant Gr/Re is reported, so as to investigate the influence of radiation, as one of the heat transfer modes, more clearly. To solve the governing equations (i.e., mass continuity, momentum and energy) the Finite Volume method is employed and the SIMPLE algorithm is adopted to couple the velocity and pressure fields. The radiative transfer equation is solved using the Discrete Ordinates Method, by adopting its S_4 order quadrature scheme. The results for both cases are presented as the profiles of axial velocity across the channel width, axial centerline velocity, bulk temperature and pressure versus channel height. |
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Determining Awkward Spaces in Ships Using Posture Study
M. Seif (PhD.)
O. Muftic [PhD.]
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In this paper, crew work posture, as one of critical human factor considerations, will be reviewed in different ship spaces. Whether crew members are standing or seated at a workbench or machine, their working posture is extremely important. If the available hardware forces crew members to remain in an awkward position for a long period of time, they will obviously become fatigued and, thus, more apt to make mistakes or incur some type of physical disability. In such spaces, different work postures are one of the most important parameters in affecting crew efficiency and must be studied for each space. In this work, each working space, in some real ships, regarding different work postures has been studied and the profile of each workplace has been determined. In this work, by allocating a grade for each workplace, awkward spaces in ships may be determined. |
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Entropy Generation Analysis of a Flat Plate Boundary Layer with VariousSolution Methods
J.A. Esfahani (PhD.)
M. Malek Jafarian [PhD.]
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Steady state boundary layer equations over a flat plate with a constant wall temperature can be solved by an integral solution (with three profiles for velocity and temperature), a similarity solution (exact) and a Blasius series solution. The analysis of entropy generation for each solution is carried out. The results show that the exact solution (similarity) is the one that minimizes the rate of total entropy generation in the boundary layer. Then, the Blasius solution has the least entropy generation of all. The bell-shaped profile (sinus profile) in the integral solution generates less entropy than the piecewise linear profile, consequently. So, with this method, if the exact solution for a specified problem were not available, one could evaluate the approximate solutions and recognize the best one among them. By introducing a new non-dimensional number (Ej number), which is the ratio of thermal entropy to friction entropy generation, one can recognize which of them is dominant in the boundary layer. Also, it is observed that variation of the total entropy generation is the same as the variation of boundary layer thickness, so, the non-dimensional total entropy generation for various solutions is constant. |
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Transient Laminar Convection Induced by a Line Heat Source: A Numerical Study with Primitive Variables
J.A. Esfahani (PhD.)
M.B. Ayani [PhD.]
H. Niazmand [PhD.]
A.C.M. Sousa [PhD.]
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The present work is addressed to the numerical study of transient laminar natural convection in an open space and induced by a line heat source. The governing equations, full Navier-Stokes and energy equations with primitive variables, are discretized in a staggered grid by a control volume approach. The equations for the fluid and solid (line heat source) phases are solved simultaneously using a segregated technique. Some of the physical and thermo-physical properties of the fluid (air), such as density, thermal conductivity and viscosity, were considered to vary with temperature. The results show that the energy equation reaches the steady state condition more rapidly than the momentum equations. Hence, at that time, the distribution of temperature does not show any change within the accuracy of the solution, while the distribution of the velocity still varies. The steady-state results obtained via the time-marching solution show good agreement with the published steady-state, self-similar results in the vicinity of the centerline of the plume. Also, the steady-state streamlines compare well with the published experimental results. |
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