RY toe ee ereae ate, NaGIN a meen YES ¢ Wy BELG wat rITUZ Yuu aAUrFDNASSS7 11323 15-UlUU-mn he Give. Arr 25 | 50 PH'T78 Zan UJIUU P 2521152 APR 78 UR? HM DOE/ERSP SNEwzTAK ATLL MI ot LSP 10 DCE LAS VEGAS NEVADA he TSee 3t fey _ UNCLAS NGWWD ge aya hoes Tentna PERSONAL FOR JON STEWART @AUCE ChUACK SENDSONL uw c. ty lay BJeOTs CoancLATIUN Of SGIL/IMP DATA REP: TeLECCN B. CHURCH ~ J. STEWART 242400 APR 78 1, SUBSEQUENT TO REFERENCED TELECON, PRELININARY TATA FROM TRE SOL! SAMPLE LAPORATORY HAVE SEEN RECEIVED WHICH SHEDS NEW LIGHT Cu SOLL/ vATA AND AEC OMMEND THAT Any IiEARLIER SOLELY ON CONCLUSIONS BASED dionUa JWoSANL eeEe eeee © Waiter kn berTH DISCUSSICAS CONCERNING DATA DiSCnePanCiEs BeDELAYED Fnnn ee et ee saint bapaescanen SET NEW DATA CAW BE TRANSMITTED /DELIVEREG JOTIL Tre TO NVO. THE NEW-IMP. DATA FROM ALICE INDICATES 4 RATIO CF WeWw/OLD OF 1. fe AVERAGED OVER SIK LOCATIONS THAT WERE REPEATED FROM Th SURVEYED. my 2. . The rnaATIO FROM FOUR CF THESE LOCATIONS IS GrlalNaAL 1.8 OR GAREATEX. FROM FOUR SOIL LOCATIONS ThE AVERAGE RATIO LucLUvIha A AND B CUMPOSITES IS 1.5, howEVEA SCKE A AND B COMPOSITES VARY AWIvELY CI owe CASE GREATER AN 2). mi oon we SUGGEST IT wCULD BE raz ATURE Tc benlVeCARY, rw IMP COMPARISONS. ThE SOIL/IMP RATIO IS 1.3 BASED CN TxO LCC- Y