DIFFUSION CLOUD-CHAMBER STUDY OF VERY SLOW MESONS. I. by C P Sargent; New York Columbia Univ; R Cornelius; M

By C P Sargent; New York Columbia Univ; R Cornelius; M Rinehart; L M Lederman; All authors

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1 I I 10 F i g u r e 15. I 1 20 I I I I 1 I 1 I 1 I 50 PERCENT LESS THAN I 1 80 1 I 90 I CL I 98 D i s t r i b u t i o n of t h e t o t a l a c t i v i t y by p a r t i c l e s i z e ( l e f t s c a l e ) a n d i n d i vidual particle activity (right scale), calculated assuming heterogen e o u s c o n d e n s a t i o n of 238Pu02 v a p o r u p o n a n i n e r t a e r o s o l . T h e c u r v e s h a v e q u a n t i t a t i v e m e e t i n g only f o r t h e s p e c i f i c v a p o r c o n c e n t r a t i o n s and a e r o s o l c h a r a c t e r i s t i c s d e s c r i b e d i n the text.

5 ) a t t h e peak f i r e b a l l t e m p e r a t u r e f o r a l t i t u d e h . T h i s tempera- t u r e w a s t a k e n t o be t h e a d i a b a t i c flame t e m p e r a t u r e for t h e S a t u r n V p r o p e l l a n t combination as c a l c u l a t e d by t h e ACE computer code(14), a t t h e ambient a i r pressure P(h). The d i f f u s i o n c o e f f i c i e n t D(h) w a s a s s m e d t o be i n v e r s e l y proportional t o P(h). Equation ( 5 . l )i g n o r e s c e r t a i n o t h e r a l t i t u d e - d e p e n d e n t f a c t o r s , h u t t h e y a r e r e l a t i v e l y iningr and t e n d t o compensate f o r each o t h e r (Appendix D ) .

3 ) - ( 2 . 5 ) e x a c t l y as b e f o r e . These r e l a t i o n s a r e based upon t h e assumption t h a t t h e v a p g r i z a t i o n r a t e i s d i f f u s i o n - l i m i t e d ; f o r t h e smaller p a r t i c l e s at t h e higher altitude:; t h i s c e a s e s t o he t r u e and a c o r r e c t i o n w a s a p p l i e d , u s i n g e q u a t i o n ( A - 5 ) in Appendix A. Results a r e shown as a f u n c t i o n o f a l t i t u d e f o r a v a r i e t y of particle sizes i n Fig.

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