MATPE1

Bulk Data Entry Defines the material properties for poro-elastic materials.

Format

(1) (2) (3) (4) (5) (6) (7) (8) (9) (10)
MATPE1 MID MAT1 MAT10 BIOT          
  GAMMA PRANDTL POR TOR AFR VLE TLE  

Example

(1) (2) (3) (4) (5) (6) (7) (8) (9) (10)
MATPE1 17 1 10 1.0          
  1.8-8 1.41 7.0-1 8.0-1 1.2 2.-5 1.0-1 9.3-2  

Definitions

Field Contents SI Unit Example
MID Unique material identification number.

No default (Integer > 0)

 
MAT1 Material identification number of the MAT1 Bulk Data Entry (or MATF1 if it is frequency-dependent) for the skeleton.

No default (Integer > 0)

 
MAT10 MAT10 Bulk Data Entry identification number for the porous material.

No default (Integer > 0)

 
BIOT BIOT factor.

Default = 1.0 (Real > 0.0)

 
Fluid dynamic viscosity.

No default (Real > 0.0)

 
GAMMA Fluid ratio of specific heats.

Default = 1.402 (Real > 0.0)

 
PRANDTL Fluid Prandtl number.

Default = 0.71 (Real 0.0)

 
POR Porosity of the porous material.

No default (Real > 0.0)

 
TOR Tortuosity of the porous material. 2

Default = 1.0 (Real ≥ 1.0)

 
AFR Flow resistivity. 3

No default (Real > 0.0)

 
VLE Viscous characteristic length. 4

No default (Real > 0.0)

 
TLE Thermal characteristic length. 5

No default (Real > 0.0)

 

Comments

  1. This entry is represented as a material in HyperMesh.
  2. Tortuosity is defined as the complexity of the inner structure of a porous material. In the Biot material model, it is measured as the complexity of the flow path of the fluid in the porous medium. The fluid particles usually do not flow in a straight path. It is the measurement of the ratio of the square of microscopic velocity ( V mi ) of the fluid in the entwined path to the square of macroscopic velocity ( V = V m a ). (1)
    α = ( V m i 2 vol V ma 2 )


    Figure 1. Microscopic Velocity within a Macroscopic System

    If φ is the angle between the axis of the cylindrical microscopic pores, and the surface is normal, the tortuosity is inversely proportional to the square of cos φ ( α 1.0 cos 2 φ ) . The tortuosity of the material increases as the number of pores and complexity increases. Tortuosity is a dimensionless quantity and if it is equal to 1.0, then the directions of microscopic and macroscopic velocities are parallel ( φ = 0 ).

  3. Flow resistivity represents the resistance of a porous material to the flow of fluid. In the Biot material model, it is used to characterize the ease with which fluid can flow through the porous medium. The fluid in the porous medium is affected by two opposing forces: viscosity and pressure gradient. Flow resistivity is defined as the ratio of the pressure differential across a sample of the material to the normal mean flow velocity (macroscopic velocity ( V = V ma )) through the material. (2)
    σ = ( p 2 p 1 Vh )
    Where, σ is the flow resistivity, ( p 2 p 1 ) is the pressure difference in the sample of thickness, h and V = V ma is the normal mean flow velocity of fluid per unit area (macroscopic velocity).


    Figure 2. Macroscopic Model of the Porous Medium

    In the Biot material formulation, viscosity is frequency-dependent, so the flow resistivity is also frequency-dependent. Static flow resistivity is usually in the range of 10e3 Nm-4s to 10e6 Nm-4s. A very high AFR number indicates that the poro-elastic material is highly resistant to the propagation of fluid. The SI unit of flow resistivity is: Nm-4s.

  4. The effective density of the poro-elastic material and its bulk modulus depend on the tortuosity and hydraulic radius. This takes into account the non-uniform channels of the porous medium. The viscous characteristic length can be used to replace the hydraulic radius. Viscous characteristic length is defined as: (3)
    Λ = 2 ( V v iv 2 S v is 2 )
    Where,
    Λ
    Viscous characteristic length
    v iv
    Velocity of the fluid inside the pores of the poro-elastic material
    v is
    Velocity of the fluid inside the surface of the poro-elastic material
  5. The bulk modulus, at higher frequencies can be characterized by a second characteristic length defined as: (4)
    Λ = 2 ( V dv S ds )
    Where,
    Λ
    Thermal characteristic length
    dv
    Microscopic volume of the poro-elastic material medium
    ds
    Microscopic surface of the poro-elastic material

    The thermal characteristic length is also used to account for the non-uniform channels of the porous medium.