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OAST 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: Block V: Sources
Up: Input Files for OAST
Previous: Block III: Frequencies
henrik schmidt
1999-08-25