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OASP 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:
 - Attenuation 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: Block II: OASP options
 Previous: Block III: Source Frequency
henrik schmidt
1999-08-25