Next: Execution of OASR
Up: Input Files for OASR
Previous: Block II: OASR options
OASR supports all the environmental models allowed for SAFARI as well as the
ones described above in Section 4.1. The significance of
the standard environmental parameters is as follows
- NL:
- Number of layers, including the upper and lower
half-spaces. These should Always be included,
even in cases where they are vacuum.
- D:
- Depth in m of upper boundary of layer or
halfspace. The reference depth can be choosen
arbitrarily, and D() is allowed to be negative.
For layer no. 1, i.e. the upper half-space, this
parameter is dummy.
- CC:
- Velocity of compressional waves in m/s.
If specified to 0.0, the layer or half-space is
vacuum.
- CS:
- Velocity of shear waves in m/s.
If specified to 0.0, the layer or half-space is fluid.
If CS()< 0, it is the compressional velocity at bottom of
layer, which is treated as fluid with
1/c(z)2 linear.
- AC:
- Attennuation of compressional waves in
.
If the layer is fluid, and AC() is specified to
0.0, then an imperical water attenuation is
used (Skretting & Leroy).
- AS:
- Attenuation of shear waves in
- RO:
- Density in g/cm3.
- RG:
- RMS roughness of interface in m. RG(1) is dummy.
If RG<0 it represents the negative of the RMS roughness, and
the associated correlation length CL should follow. If RG>0
the correlation length is assumed to be infinite.
- CL:
- Roughness correlation length in m.
Next: Execution of OASR
Up: Input Files for OASR
Previous: Block II: OASR options
henrik schmidt
1999-08-25