By R. Koch (Auth.)

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**Example text**

555(100) (n, p)Be j from C 32 (n, a)Be none BERYLLIUM τ» % λ ~12 Be (or, ny)C Z =4 Determination of Be by d i r e c t counting of 4„ 4 Mev p r o m p t y Y s; B, AI, Mg, and other elements interfere. G9 0 3 Excitation function from 0. 8 Mev to 5. 0 Mev; E . 75 Mev; E = 1 . 75) = 0. 15 b ; 7 th P σ ( 5 . 4 b. 9 8 Be 7 (v,n)Be la H6 T2 Non-destructive determination of Be in o r e s by d i r e c t counting of photo-neutrons using an 124 "»-1 curie Sb s o u r c e with a sensitivity of 1 ppm; B, Cd, and other neutron a b s o r b e r s m a y interfere.

4 Mev to 4. 1 Mev; E t h = 1. 27 Mev; E^ > 4 Mev; σ ( 2 . 4 ) = 95 mb; cr(4. 1) = 0. 16 b. , 7 7 Li (p, n)Be 10 Possible interference from B 7 9 7 (p? or)Be ; from Be (p, t)Be . & 7 JLi (d, n)Be 10 7 9 7 Possible interference from B (d, cm)Be ; from Be (d, 2n)Be at E > 5 Mev; possible interference from 10 7 9 7 secondary reactions: B (p, ar)Be ; Be (p, t)Be . JLi(d, t) Possible interference from Be(d, t); from other (d, t) reactions; possible interference from secondary 2 3 3 3 reactions: H (n, γ)Η ; He (n, p)H ; other (n, t) or (p, t) reactions.

A (n, v)A Determination of age of K minerals by analysis for radiogenic A 11 41 41 flux = 1 x 10 ; K (n, p)A >60 mb S741 ; sensitivity = 3 x 10 μg; interferes and requires pre-irradiation separation of A from matrix. Determination of age of meteorites by comparison to K activation. (n, γ)Α 40 A Possible interference from Ca 41 (n, γ)Α Α36(η,γ)Α37 l x 10- 3 fjg. |A 4 °(n,Y)A 4 1 2 x 10" 5 Hg. B6 (n, at)A 41 Possible interference from K with a Ca matrix. 41 (n, p)A M43 S74 Determination of A in drinking water.