Thanks for the reply.
I am still confused by the alternative methods of calculating ground
attenuation.
For Method 7.3.1:
Assuming the ground is porous, G = 1
Dp = 500 m
hs = hr = 1.5 m
I calculate a'(h) =4.53
b'(h) =8.52
c'(h) =6.47
d'(h) =2.16
This gives As and Ar to be: -1.5, 3.0, 7.0, 4.9, 0.66, 0,0,0 for the
Nominal frequencies 63 - 8 000
Summing these in the same way as combining noise sources (Eq 5,
ignoring A weighting) gives 11.7 dB which should be doubled according
to equation 9 giving 23 dB of attenuation.
Method 7.3.2 gives Agr to be 4.7 dB, if hm = 1.5m and d =500 m and D
to be 3 dB which must be subtracted to give 1.7 dB
Finally according to Note 1 the 500Hz band can be used as an
approximation for attenuation. In 7.3.1 this would give Agr to be 4.9
X 2 = 9.8 dB
With results ranging from 1.7 dB to 23 dB attenuation from ground
effects I am confused, or maybe I am misreading the standard.
Again, any comments will be very useful,
Rod
> > Hi,
> > I wonder if there is an error in the formula in Table 3 for a'(h), or
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> which would appear to generally agree with Figure 2a. Seems as though
> there might be something wrong with your calc???
Thanks for confirmation - some of the text appears to be a subscript
of a subscript!
> As for 7.3.1 vs. 7.3.2, there are more variables in use that you
> haven't provided. Negative attenuation, which should generally be
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>
> - Show quoted text -
Mark B - 15 Jan 2008 13:58 GMT
> Thanks for the reply.
> I am still confused by the alternative methods of calculating ground
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>
> - Show quoted text -
I am glad to see that I anot the only one confused by ground
attenuation calculations.
MarkB
Savant - 16 Jan 2008 04:25 GMT
Rod,
Wow. Let me see if I can help focus this...
> For Method 7.3.1:
>
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> ignoring A weighting) gives 11.7 dB which should be doubled according
> to equation 9 giving 23 dB of attenuation.
The misstep here is that you summed attenuations logarithmically,
which cannot be done. I believe you did this with the intention of
getting an A-wtd. value for Agr. While the intention is good, it's an
improper us of Eq 5.
> Method 7.3.2 gives Agr to be 4.7 dB, if hm = 1.5m and d =500 m and D
> to be 3 dB which must be subtracted to give 1.7 dB
Here, you corrected the Agr term for D(omega). The standard states
that D(omega) is to be included in the Dc term of Eq 3. Therefore,
your value for Agr is still 4.7 dB. When you calculate for Dc to
input into Eq 3, be sure to include D(omega).
> Finally according to Note 1 the 500Hz band can be used as an
> approximation for attenuation. In 7.3.1 this would give Agr to be 4.9
> X 2 = 9.8 dB
At first glance, this does appear to be a contradiction. However -
and this is a BIG "However" - the first bullet from Section 7.3.2
specifically states that the 7.3.2 method - Eq 10 - should be used
when only the A-wtd SPL at the receiver is of interest. To me, this
supercedes the instruction in Note 1. Considering that the Table 3
term is an estimate for the 500 Hz band and Eq 10 is what the standard
states to use for estimating Agr for A-wtd SPL receiver calcs, my
money would be on the latter as the correct approach.
So, it looks like you should be using Agr = 4.7 dB if your intention
is to estimate A-wtd ground attenuation.
HTH.
All the best,
Savant