tbe The region from 55 feet to 130 feet is still imp®* vious but was apparently crushed since the drilling shows water return but no core return. It has not yet been feasible to detect this crushed region by sonic measurements even from inside the tunnel, so that detection by sonic means from above the surface is at least very difficult. Diagnostic kixperiments ie lif, Diagnostic experiments necessary for weapon development can be easily carried out underground. The yield can be measured be by shock arrival time measurements in the rock, analagous to the fireball measurements above ground. This wae done on Rainier and appears to be accurate to 10% even without a calibration, The radius of the radioactive debris or the armount of material melted might also be used if the medium is calibrated by a shot of known yield. The prompt diagnostics such as neutron and gamma ray measurements to give time interval or propagation burning data, streak camera work, etc., can be done better below than above ground since the shielding is free and one need only drill holes as desired. Radiochemistry has not been demonstrated to be satisfactory, since fractionation does occur, Howevcr, the use of hollow pipes leading into reception chambers from the cevice may give a substantial fraction of debris unfractionated, and may lead to satisfactory radiochemical diagnostics. Preliminary estimates indicate that a test operation can be 6 carried out more cheaply underground than on towers and balboons. The diagnostic stations could also be underground for clandestine tests (in fact they probably will be even if the tests are not hidden). Keeping underground tests secret will increase the costs by preventing » F f lity of proving a violation. epi meds ng aaa OM Reag the use of a single diagnostic bunker for many shots on the basis that more than one in a given vicinity increases suspicion and the possibi- It may mean that each shot must be ina completely different area, but this conclusion may be modified to some extent, because also natural earthquakes have aftershocks. In any event, such extra costs are associated with clandestine tests generally IV, ote u 7 SET perryan erden Bs PP Raa a al ee i : uy rather than underground tests specifically and are not likely to be more than a few million per shot, which is not a large percentage increase. Dependence of Seismic Signal on Yield and Medium On the basis of observations, it is believed that the amplitude of the earth motion from an underground explosion increases as the om A> ws t SECRET,- RESPRICPEDDATA” wee maT Spe im ges ig Le any rhe fe ba a eePETE ee fincenal: pot wy iid,a yon. at molten rock,

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