FIELD EVAPORATION CHARGE STATE OF BORON IONS : A TEMPERATURE EFFECT STUDY A. Menand, C. Martin, J. Sarrau To cite this version: A. Menand, C. Martin, J. Sarrau. FIELD EVAPORATION CHARGE STATE OF BORON IONS : A TEMPERATURE EFFECT STUDY. Journal de Physique Colloques, 1984, 45 (C9), pp.C9-95-C9-98. <10.1051/jphyscol:1984917>. <jpa-00224395> HAL Id: jpa-00224395 https://hal.archives-ouvertes.fr/jpa-00224395 Submitted on 1 Jan 1984 HAL is a multi-disciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés. JOURNAL DE PHYSIQUE Colloque C9, supplgment au n012, Tome 45, dgcembre 1984 page C9-95 F I E L D E V A P O R A T I O N CHARGE S T A T E O F BORON I O N S : A TEMPERATURE E F F E C T STUDY A. Menand, C. Martin and J.M. Sarrau L a b o r a t o i r e d e Microscopic 1 o n i q u 2 , F a c u Z t d d e s S c i e n c e s d e Rouen, BP 6 7 , 7 6 1 3 0 M o n t - S a i n t - A i g n a n , F r a n c e Resume - - Une e t u d e d e l a c h a r g e d e s i o n s B o r e d v a p o r 6 s p a r e f f e t d e c h a m p , m e t e n e v i d e n c e u n e d i f f g r e n c e p o u r l e s Q t a t s d e c h a r g e d e s i o n s B 1 0 et B 1 l . C e t t e d i f f e r e n c e d d p e n d d e l a t e m p e r a t u r e d e l ' e c h a n t i l l o n . Une e x p l i c a t i o n d e cet e f f e t d f i a u d 6 p a r t d e s i o n s B b a s s e t e m p e r a t u r e p a r e f f e t t u n n e l i o n i q u e e s t donnee. A b s t r a c t - We h a v e o b s e r v e d the m a s s t o c h a r g e r a t i o o f f i e l d e v a p o r a t e d Boron i o n s . A d i f f e r e n c e b e t w e e n t h e c h a r g e s t a t e o f B I 0 and Bll i o n s i s o b s e r v e d . T h i s d i f f e r e n c e i s t e m p e r a t u r e d e p e n d e n t . An e x p l a n a t i o n i s g i v e n i n t e r m s o f i o n i c t u n n e l i n g d e s o r p t i o n o f Boron i o n s a t l o w t e m p e r a t u r e . 1, an i s o t o p i c variation in f i e l d evaporation A s i t h a s b e e n p r e v i o u s l y r e p o r t e d 11 c h a r g e s t a t e o f b o r o n ions h a s b e e n o b s e r v e d . T h e p r o p o r t i o n o f B I D i o n s f i e l d e v a p o r a t i n g a s d o u b l y c h a r g e d i o n s i s f o u n d t o be l e s s t h a n t h e c o r r e s p o n d i n g f i g u re f o r Bll i o n s . T h i s e f f e c t i s p r e d i c t e d b y t h e p o s t - i o n i s a t i o n m o d e l o f Haydock and Kingham 121. BI~ i o n s b e i n g less m a s s i v e t h a n BI~ i o n s t r a v e l f a s t e r and s o s p e n d l e s s t i m e i n the " p o s t - i o n i s a t i o n z o n e " i n w h i c h t h e t r a n s i t i o n f r o m B* t o B ~ ' i s e x p e c t e d t o o c c u r . T h e maximum o f d i f f e r e n c e b e t w e e n t h e p r o b a b i l i t i e s o f In p r a c t i c e t h e o b s e r p o s t - i o n i s a t i o n c a l c u l a t e d f o r B o r o n i o n s i s AP = 1.6 % 11 v e d d i f f e r e n c e AP i s much m o r e p r o n o u n c e d t h a n e x p e c t e d w i t h AP = 4.6 % 1. ex*, ex^ f o r e x p e r i m e n t a t 78 K. I I t h a s been a s s u m e d b y Menand and Kingham [ 1 t h a t t h i s d i s c r e p a n c y c o u l d b e e x p l a i nerZ i n t e r m s o f e v a p o r a t i o n o f b o r o n i o n s b y i o n i c t u n n e l i n g a t l o w t e m p e r a t u r e . T h e p u r p o s e o f t h i s p a p e r i s t o t e s t t h i s a s s u m p t i o n b y v a r y i n g the s a m p l e t e m p e rature. T h e e x p e r i m e n t s w e r e made w i t h were prepared from t a p e s o f 5 0 electropolishing in a solution a ToF a t o m p r o b e 13 w i t h a 3 0 a r e a . T i m i n g was b y m e a n s o f a t i m e o f 5 n s , low temperatures 1 s a m p l e s o f Fe Ni Mo B m e t a l l i c g l a s s , t h e s p e c i m e n s pm t h i c k n e s s and a b o u t 0 . 2 mm w i d t h , b y a n o d i c o f lv" % p e r c h l o r i c a c i d i n 2 - B u t o x y e t h a n o l . We u s e d cm f l i g h t l e n g t h w h i c h a l l o w s a l a r g e a n a l y s i s t h r e e c h a n n e l 4 0 0 MHz d i g i t a l c o u n t e r w i t h a d e a d was o b t a i n e d b y m e a n s o f a c r y o g e n e r a t o r . RESULTS AND DISCUSSION 1 - T......................................... emperature dependence o f i s o t o p i c e f f e c t T a b l e 1 g i v e s the r e s u l t s o b t a i n e d a t t e m p e r a t u r e v a l u e s r a n g i n g from 170 K t o 300 K : 2 0 3 0 4 b o r o n i o n s w e r e d e t e c t e d o f w h i c h 19.88 % w e r e B10 i n good a g r e e - 'UA CNRS 808 Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:1984917 JOURNAL DE PHYSIQUE C9-96 m e n t w i t h t h e i s o t o p i c r e l a t i v e a b u n d a n c e . T h e a v e r a g e p r o p o r t i o n o f B1 i n the d o u b l y c h a r g e d p e a k i s 19.46 % whereas t h e p r o p o r t i o n o f B10 in t h e s i n g l y c h a r g e d p e a k i s 20.41 %. T h e a v e r a g e d i f f e r e n c e AP i o n i s a t i o n o f B10 and B l l i s 1.5 %. Experiment I 2+ Blo Total 1 2224 Table 1 - exp between t h e p r o b a b i l i t i e s o f post- B:: 1 Number o f BZ+ 9204 B+ l o t B:; and B ; ~ i o n s o b s e r v e d i n s e v e n e x p e r i m e n t s o f Fe N i Mo B , a t t e m p e r a t u r e r a n g i n g f r o m 1 7 0 K t o 3 0 0 K . E a c h e x p e r i m e n t g i v e s a n 2+ 2+ 2+ e s t i m a t e o f t h e r e l a t i v e a b u n d a n c e O ~ , B and ! ~ B l l ( i . e ( B I O / Z B l o ) and 2+ ( B /ZB I ) and o f t h e d i f f e r e n c e i n t h e s e q u a n t i t i e s , Q I 11 11 exp T h e r e s u l t s o n t h e a b u n d a n c e o f s i n g l y and d o u b l y c h a r g e d i o n s o f t h e t w o i s o t o p e s o f b o r o n a t t e m p e r a t u r e b e t w e e n 20 K and 3 0 0 K a r e s u m m a r i s e d i n t a b l e 2 , t h e y show a s i g n i f i c a n t t e m p e r a t u r e e f f e c t . Temperature 2+ B1o B+ B2+ 11 B 11 2+ B 10 /ZB10 % 2+ BI1/XBll % 20 K 78 K 170-240 K 300 K 414 102 993 1231 627 108 985 827 1921 448 4034 5170 2028 404 3635 3429 39.8 48.6 50.2 59.8 48.6 52.6 52.6 60.1 Table 2 - 2+ Number o f B l o t 10 + AP e*p + + + + % 8.8 4 2.4 0.3 + 2+ B l O , B l l and B : ~ i o n s o b s e r v e d i n t h e e x p e r i m e n t s o n Fe N i M B f o r d i f f e r e n t t e m p e r a t u r e s l y i n g f r o m 20 K t o 3 0 0 K i s s m a l l 0.3-2.4 % w h i c h exp i s c o n s i s t e n t w i t h t h e p r e d i c t e d v a l u e o f 1 . 6 %, b u t a t l o w e r t e m p e r a t u r e AP exD i s l a r g e r , u p t o 8 . 8 % a t 20 K. These r e s u l t s s u p p o r t o u r a s s u m p t i o n of i o n i c t u n n e l i n g a t l o w t e m p e r a t u r e . T h e o c c u r e n c e o f i o n i c t u n n e l i n g means t h a t t h e l i g h t e r B10 i o n s w i l l b e m o r e e a s i l y f i e l d e v a p o r a t e d t h a n B1 S O t h e y may be I n the t e m p e r a t u r e r a n g e 170-300 K t h e d i f f e r e n c e AP .* evaporated a t f i e l d s t r e n g t h s l i g h t l y lower than Bll. T h a t i s , if B l l i o n s a r e o n l y e v a p o r a t e d a t the maximum o f t h e e l e c t r i c f i e l d p u l s e , B10 i o n s may b e e v a p o r a t e d when the f i e l d i s j u s t less t h a n i t s m a x i m a l v a l u e . As p o s t - i o n i s a t i o n p r o b a b i l i t i e s are s t r o n g l y dependent o n f i e l d s t r e n g t h 1 o n l y a 0.5 % d i f f e r e n c e i n e v a p o r a t i o n f i e l d s t r e n g t h i s r e q u i r e d t o g i v e .A 3 % d i f f e r e n c e i n p o s t - i o n i s a t i o n p r o b a - I I, bilities. 2 - Constant f i e l d s t e n g t h s t u d y ............................ W e h a v e p r e p a r e d a s p e c i m e n w i t h a v e r y narrow t a p e r a n g l e w h i c h m e a n t t h a t t h e d e s o r p t i o n f i e l d r e m a i n e d c o n s t a n t ( w i t h t h e t i p v o l t a g e h e l d c o n s t a n t ) d u r i n g the d e s o r p t i o n o f many a t o m s . T h e s t e a d i n e s s o f t h e t i p r a d i u s was v e r i f i e d b y the meas u r e m e n t o f B I V b e f o r e and a f t e r e a c h e x p e r i m e n t . W i t h t h i s s p e c i m e n we h a v e p e r formed e x p e r i m e n t s w i t h i n c r e a s i n g t e m p e r a t u r e ( b y s w i t c h i n g o f f the c r y o g e n i c r e f r i g e r a t o r ) . So during t h e course o f t h e experiment, and,as t h e evaporated i o n s w e r e d e t e c t e d , the t i p t e m p e r a t u r e was s l o w l y i n c r e a s i n g . F i g u r e 1 g i v e s t h e cumu- a t i v e number o f B ~ i+o n s v e r s u s t h e t o t a l number o f Boron d e t e c t e d i o n s , the c o r r e s ponding temperatures a r e a l s o i n d i c a t e d . F i g . 1 - C u m u l a t i v e number o f B observed 2+ ions o b s e r v e d a g a i n s t t h e t o t a l number o f B i o n s T h e s h a r p s l o p e c h a n g e w i t h i n 140 K i s the r e s u l t o f an i n t e r e s t i n g a r t e f a c t . For t e m p e r a t u r e s u n d e r 140 K the e v a p o r a t i o n r a t e was i n c r e a s i n g v e r y s l o w l y and t h e to 4. but near a v e r a g e number o f d e t e c t e d i o n s p e r p u l s e n l y g n g f r o m 5. 140 K the e v a p o r a t i o n r a t e i n c r e a s e d s u d d e n l y n > 3 , t h r e e Boron ions os m o r e w e r e produced f o r e a c h p u l s e b u t o b v i o u s l y o n l y 3 ions c o u l d b e s t o r e d i n t h e t h r e e c h a n n e l s d i g i t a l c o u n t e r . In t h i s s a t u r a t e d r e g i m e d o u b l y c h a r g e d i o n s a p p e a r more a b u n d a n t b e c a u s e t h e y r e a c h the d e t e c t o r f i r s t . T h i s s u d d e n i n c r e a s e i n t h e e v a p o r a t i o n r a t e i s i n t e r p r e t e d a s a c h a n g e i n the e v a p o r a t i o n p r o c e s s from a n e s s e n t i a l l y t u n n e l i n g d e s o r p t i o n o f b o r o n i o n s , t o a n e s s e n t i a l l y t h e r m a l l y a c t i v a t e d e v a p o r a t i o n . T h e t r a n s i t i o n t e m p e r a t u r e T w i l l be 140 5 K. + i s p a r t i c u l a r l y i n t e r e s t i n g t o n o t i c e the s t e a d i n e s s o f the c h a r g e r a t i o 2+ /CB a t l o w and a t h i g h t e m p e r a t u r e ( e x c e p t e d i n the s a t u r a t e d z o n e 140-165 K I . T h i s i s a n e v i d e n c e f o r the p o s t - i o n i s a t i o n model o f Kingham, t h e c h a r g e s t a t e It B o f b o r o n i o n s i s a f u n c t j o n o f f i e l d and n o t o f t e m p e r a t u r e Acknowledgements T h e a u t h o r s w i s h t o t h a n k D r D. R. Kingham f o r f r u i t f u l d i s c u s s i o n s and v a l u a b l e comments. JOURNAL DE PHYSIQUE REFERENCES If I A. MENAND and D. R. KINGHAM J. Phys. D : Appl. Phys., 1 7 ( 1 9 8 4 ) 203 12 1 R. HAYDOCK and D. R. KINGHAM P h y s . Rev. Lett., ( 1 9 8 0 ) 1520 13 1 C. MARTIN, D. BLAWTTE and J. M . Rev. P h y s . A p p l . , ( 1 9 8 4 ) 27 44 19 SARRAU
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