Misinformation. or misleading information, like scum floating up in a still pool has a way of becoming the only available information if an attempt is not made to point out that other viewpoints exist.
When it comes to the question of estimating the yields of the Indian nuclear tests, there is a whole lot of information available, from a plethora of sources, but the only two names whose work gets quoted and propagated is one [url=http://www.geo.arizona.edu/geophysics/f ... Wallace</a> and a <a href="http://www.iisc.ernet.in/~currsci/jul10 ... Douglas</a>. I see this situation as akin to the "selling" of Chuck Yeager's "Invincible PAF" even after decades of dismal performance and defeats.
I want to add to the efforts of a <a href="http://www.bharat-rakshak.com/MONITOR/I ... .html">few concerned people</a> by writing something that can hopefully be understood by the seismic non techie, and by a person who can only understand as much math as I do, - i.e. elementary, high school maths.
MEASURING YIELDS OF UNDERGROUND NUCLEAR TESTS:
First let us get some things straight. The ONLY RELIABLE methods of estimating nuclear test yields (as per <a href="http://tejas.serc.iisc.ernet.in/currsci ... .pdf">open sources</a>) is to have instruments close to the test site, and post-test radiochemical testing AT THE TEST SITE. Anything else can be way way out.
But what if you are not invited to come near a nuclear test site? That is where seismic methods come in. Since most people are not allowed near nuclear test sites, the whole "scientific", "debating" and gossiping world depends on the speculation of seismologists reading squiggles caused on instruments thousands of kilometers from a test site. This fact, more than accuracy, makes seismology important.
SEISMOLOGY AND NUCLEAR TESTING:
According to one dictionary Seismology is the science that studies earthquakes. It so happens that underground nuclear explosions also cause little squiggles in the instruments that are set up to study earthquakes (seismographs), putting seismologists in the unique position of talking about nuclear tests.
So how do people arrive at the yield of a nuclear test from squiggles on seismographs?
The "magic formula" is given below:
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mb = attenuation constant + 0.75(Log of Yield)
or
mb = a + 0.75 Log Y
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For this formula, "mb" is measured from the squiggle on the seismograph, and "Y" is the Yield of the nuclear test that the magic formula will reveal after you fill in the value of "a".
Now what the hell is "a"? "a" is a number that is supposed to indicate the amount by which the seismic signal of the explosion has petered out as is gets to you. The value can be anywhere from <a href="http://www.geo.arizona.edu/geophysics/f ... .pak/">3.9 to 4.5</a>
Now that is really really funny, and its called science. If some seismographs indicate a value of 5.2 for mb you apply the magic formula and get a nuclear yield of 53 kilotons if you use a value of "a" as 3.9, and the SAME NUCLEAR EXPLOSION will show a yield of only 8 kilotons if you use the value 4.5 for "a". How convenient.
When it comes to using a value for "a" in calculating Indian Test Yields, let me quote a <a href="http://www.iisc.ernet.in/~currsci/jul10 ... ">paper</a>:
10)From the Douglas paper:in the value of a: Sikka et al use 4.04 on the assumption that the yield of the first Indian test (18 May 1974 referred to below as 740518) was 13 kt, Wallace uses 4.45 on the assumption that a for Pokhran is the same as that of eastern Kazakhstan . In fact I have not cross checked to see if these alleged Kazakh values are accurate.
IT GETS WORSE THAN THIS:
Now all that is written above is just great for single shot nuke tests. Now what if some sneaky people set off two or more nuclear tests simultaneously? The seismologists of this world have next to zero experience of seismic signals from nuclear tests set off simultaneoulsy. And that was what was done on May 11th at Pokhran.
OK - if nobody has PRACTICAL experience, what does the theory say? What's in the textbook?
When two sources situated close together produce waves of any kind the waves interfere with each other and may add up or subtract from each other depending on the direction. Imagine a "double simultaneous nuclear test" conducted by Pakistan midway between Lahore and Islamabad 100 meters below the Lahore-Islamabad expressway. The people in Lahore and in Islamabad who are in line with the two devices will experience interference such that the signals will be weaker than the total energy of the two tests, but those of us watching from Jammu, at right angles to the road, will see the two test signals add up. That is the theory. What does the little practical experience available say?
In fact, the practical experience says that the theory is correct. East-West seismic stations have recorded smaller signals from the East-West oriented Pokhran tests, as opposed to stations situated North and South. This can be seen in the tables in <a href="a href="http://www.iisc.ernet.in/~currsci/jul10 ... .pdf">this paper</a> and in the <a href="http://www.bharat-rakshak.com/MONITOR/I ... a.html">BR paper</a>. The same thing is <a href="http://www.bharat-rakshak.com/MONITOR/I ... ">depicted grahically</a> on BR.
When such interference occurs - adding up the signals from different seismic stations around the world and taking an "average value" to calculate the yield is utter nonsense. Garbage in, garbage out. But what can we say? "Seismology experts" understand rocks, but perhaps not physics or maths.
I'll stop here, but I will leave you with some relevant notes and references (some are repeats, so check before you click)
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1)The inaccuracy and problems associated with trying to detect and calculate yields from seismic signals has led to a continuing search for better methods - as shown by these two papers:
<a href="http://www.nemre.nn.doe.gov/review2001/ ... /04-03.pdf]http://www.nemre.nn.doe.gov/review2001/ ... /04-03.pdf[/url]
and
http://www.nemre.nn.doe.gov/review2000/3-Seismic%20Source%20Characterization/03-08.pdf
The latter paper acknowledges the existing problems of innacurate yield estimation by seismologic methods with the words: "to address a long-standing problem in observational seismology, namely accurate estimation of the radiated seismic energy"
These papers are quite difficult to read and digest - especially for the seismic non-techie, but I would advise that at least some should try and read them, if only to try and pick holes in my interpretation.
2)Another , also available in <a href="http://216.239.39.100/search?q=cache:0aCNIib3HqYC:www.princeton.edu/~globsec/publications/pdf/3_3-4Adushkin.pdf+seismic+attenuation+and+mb+values+in+nuclear+yield&hl=en&ie=UT F-8&e=619">html</a> lists some of the unknown variables that can affect yield measurements:
3)This fits in well with a quote from <a href="http://tejas.serc.iisc.ernet.in/currsci/nov102000/1359.pdf">another source:</a>
4)<a href="http://www.barc.ernet.in/webpages/milestones/drs_03.html">Indian Explosions of May 11, 1998 : An Analysis of Global Seismic Bodywave Magnitude Estimates</a>S. K. Sikka, Falguni Roy and G. J. Nair, High Pressure Physics Division, Bhabha Atomic Research Centre, Mumbai 400085, India
5)BRM article <a href="http://www.bharat-rakshak.com/MONITOR/ISSUE3-6/Figure2.jpg">graph</a> of North South east west mb value variation
6)<a href="http://www.bharat-rakshak.com/MONITOR/ISSUE3-6/ramana.html">BRM article</a>
7)Preliminary yield reults
<a href="http://www.barc.ernet.in/webpages/milestones/drs_02.html]http://www.barc.ernet.in/webpages/milestones/drs_02.html
8)Yield estimation of Indian nuclear tests of 1998 - S. K. SIKKA,FALGUNI ROY, G. J. NAIR Seismology Division, Bhabha Atomic Research Centre, Mumbai 400 085, India9)The specific yields of Pokhran 2 were measured by the methods mentioned <a href="http://tejas.serc.iisc.ernet.in/currsci ... f">here</a>:"Further,the ratios of neutron activation products to fission products for the thermo-nuclear
and fission test of 11 May 1998 were also found to be in quantitative agreement with that expected from their radiochemical yields. BARC has also performed simulation studies of the
close-in acceleration values and surface features by finite difference and finite element codes (unpublished). These studies also corroborate the estimated yield of POK2."
the yield of a nuclear explosion can be determined with a reasonable accuracy from the close-in acceleration and velocity measurements. Com-parison of the close-in seismic data pertaining to POK2 with the available global data from similar geophysical environment gives an yield value close to 58 kt for these explosions (see Figure 10)3 . Recent radiochemical analysis of samples from post-shot logging of POK2 32 has confirmed the authenticity of the estimated seismic yields
of POK2 explosions. The radiochemical yield for the thermonuclear device has been obtained as 50 ± 10 kt. A preliminary estimate of the radiochemical yield of the fission device, is 13 ± 3 kt (ref. 33). These studies have further substantiated that the fusion component was in accord with computer simulations.
[URL=http://www.iisc.ernet.in/~currsci/jul102001/72.pdf]http://www.iisc.ernet.in/~currsci/jul102001/72.pdf</a>
The principal difference in the yield estimate of Sikka et al.1 and others is in the value of a: Sikka et al use 4.04 on the assumption that the yield of the first Indian test (18 May 1974 referred to below as 740518) was 13 kt, Wallace 6 uses 4.45 on the assumption that a for Pokhran is the same as that of eastern Kazakhstan.