critic a lity b e nc hma rk o f the mo lte n sa lt re a c
play

Critic a lity b e nc hma rk o f the Mo lte n Sa lt Re a c to r E - PowerPoint PPT Presentation

Critic a lity b e nc hma rk o f the Mo lte n Sa lt Re a c to r E xpe rime nt Ma ssimilia no F ra to ni | Unive rsity o f Ca lifo rnia , Be rke le y Mo lte n Sa lt Re a c to r Wo rksho p 2017 | K e y T e c hno lo g y a nd Sa fe ty I ssue s


  1. Critic a lity b e nc hma rk o f the Mo lte n Sa lt Re a c to r E xpe rime nt Ma ssimilia no F ra to ni | Unive rsity o f Ca lifo rnia , Be rke le y Mo lte n Sa lt Re a c to r Wo rksho p 2017 | K e y T e c hno lo g y a nd Sa fe ty I ssue s fo r MSRs Oc to b e r 3, 2017

  2. A pe e r-re vie we d re a c to r physic s b e nc hma rk fo r mo lte n sa lt te c hno lo g ie s is unde r de ve lo pme nt ¡ DOE NE a wa rde d a n NE UP to UC Be rke le y, in c o lla b o ra tio n with ORNL a nd the Gre no b le I nstitute o f T e c hno lo g y (F ra nc e ), to c re a te a n MSRE b e nc hma rk (Oc to b e r 2016) ¡ T he ta rg e t is to c re a te a b e nc hma rk fo r the I nte rna tio na l Re a c to r Physic s Be nc hma rk E xpe rime nt E va lua tio n Pro je c t (I RPhE P) ha ndb o o k ¡ pe e r-re vie we d se t o f re a c to r physic s-re la te d inte g ra l da ta ¡ use d b y re a c to r de sig ne rs to va lida te a na lytic a l to o ls fo r a dva nc e d re a c to rs ¡ use d b y sa fe ty a na lysts to e sta b lish the sa fe ty b a sis fo r o pe ra tio n o f a dva nc e d re a c to rs

  3. T he b e nc hma rk is b a se d o n a se rie s o f sta rt-up ze ro -po we r e xpe rime nts (June 1965) ¡ An initia l c ritic a lity e xp e rime nt me a sure d the minimum a mo unt o f 235 U ne e d e d to re a c h c ritic a lity ¡ Me a sure me nts o f the d iffe re ntia l wo rth o f o ne c o ntro l ro d a s a func tio n o f p o sitio n with sta tio na ry a nd c irc ula ting sa lt ¡ Me a sure me nts o f the inte g ra l wo rth o f va rio us c o ntro l ro d c o nfig ura tio ns ¡ Critic a lity c o nfig ura tio ns o b ta ine d c ha ng ing 235 U c o nc e ntra tio n a nd c o ntro l ro d p o sitio ns; ¡ Me a sure me nts with sta tio na ry a nd c irc ula ting sa lt c o nd itio ns ¡ Me a sure me nt o f the who le c o re iso the rma l te mp e ra ture re a c tivity c o e ffic ie nt ¡ Me a sure me nt o f the p re ssure re a c tivity c o e ffic ie nt

  4. T he b e nc hma rk is b a se d o n a se rie s o f sta rt-up ze ro -po we r e xpe rime nts (June 1965) ¡ An initia l c ritic a lity e xp e rime nt me a sure d the minimum a mo unt o f 235 U ne e d e d to re a c h c ritic a lity ¡ Me a sure me nts o f the d iffe re ntia l wo rth o f o ne c o ntro l ro d a s a func tio n o f p o sitio n with sta tio na ry a nd c irc ula ting sa lt ¡ Me a sure me nts o f the inte g ra l wo rth o f va rio us c o ntro l ro d c o nfig ura tio ns ¡ Critic a lity c o nfig ura tio ns o b ta ine d c ha ng ing 235 U c o nc e ntra tio n a nd c o ntro l ro d p o sitio ns; ¡ Me a sure me nts with sta tio na ry a nd c irc ula ting sa lt c o nd itio ns ¡ Me a sure me nt o f the who le c o re iso the rma l te mp e ra ture re a c tivity c o e ffic ie nt ¡ Me a sure me nt o f the p re ssure re a c tivity c o e ffic ie nt

  5. Cre a ting a b e nc hma rk c o nsists o f two ma in ta sks ¡ Cre a te b e nc hma rk spe c ific a tio ns ¡ Re trie ve da ta a nd re la te d unc e rta inty ¡ Ma ke a ssumptio ns a s ne e de d ¡ T e st the b e nc hma rk ¡ Cre a te a nd run o ne o r mo re c o mputa tio na l mo de ls ¡ Asse ss unc e rta intie s

  6. F ue l g e o me try

  7. T o p c o mpo ne nts

  8. Co ntro l ro ds a nd sa mple b a ske ts

  9. Oute r c o re c o mpo ne nts

  10. Co re mo de l H o rizo ntal c ro ss se c tio n o f the MS RE mo de l

  11. Do we l se c tio n o f g ra phite la ttic e H o rizo ntal c ro ss se c tio n o f the do we l se c tio n o f the graphite lattic e

  12. T a pe r re g io n H o rizo ntal c ro ss se c tio n o f the tape r re gio n

  13. Co ntro l ro ds a nd sa mple b a ske ts H o rizo ntal c ro ss se c tio n o f the c o ntro l ro ds and sample baske ts

  14. Sa mple b a ske ts

  15. Co ntro l ro ds

  16. Overall model

  17. T he b e nc hma rk mo de l wa s te ste d o n the first MSRE c ritic a lity e xpe rime nt ¡ F ue l sa lt c o mpo sitio n 65L iF -29.2Be F 2 -5ZrF 4 -0.8UF 4 (99.99% fo r 7 L i e nric hme nt). ue l sa lt d e nsity 145.3 ± 1.0 lb / ft 3 (2.3275 ± 0.0160 g / c m 3 ) ¡ F ¡ Ma ss fra c tio n o f 235 U in the sa lt is 1.408 ± 0.007 wt% ¡ Co re te mpe ra ture 1,181°F (638°C) ¡ One ro d wa s inse rte d a t 46.6 in. po sitio n, o the r two ro d s a t the ir uppe r limits k eff Case 100(C-E )/ E Be nc hmar k 1.0 - Calc ulate d 1.01276 ± 0.000098 1.276 (SE RPE NT 2, E NDF / B-VI I .1 c ro ss se c tio ns)

  18. Gra phite de nsity is the ma jo r so urc e o f unc e rta intie s o n k e ff | D k| × 10 - 5 Ite m Nomina l a nd bounding va lue s (1.87 ± 0.02) g / c m 3 349 Gra phite de nsity (2.3275 ± 0.0160) g / c m 3 83 F ue l sa lt de nsity (1.408 ± 0.007) wt% 235 U ma ss fra c tion in the sa lt 61 (8.7745 ± 0.0200) g / c m 3 9 INOR- 8 de nsity (166.446 ± 1) c m 19 Gra phite c ore he ig ht (70.168 ± 0.2) c m 13 Gra phite c ore ra dius (1.016 ± 0.127) c m 100 F ue l c ha nne l width (3.048 ± 0.127) c m F ue l c ha nne l le ng th 42 (0.01 ± 0.001) a t. % 6 L 174 i e nric hme nt (0.00008 ± 0.000008) wt. % 18 Boron c onc e ntra tion in g ra phite 39.687 c m (1 s = 4 c m) Outle t pipe he ig ht 31 0.819 c m (1 s = 0.08 c m) 29 Distributor thic kne ss re mo ve o ne I NOR-8 pla te 16 Sa mple ba ske t she ll dime nsion 0.06% (C ma ss fra c tio n), 0.08% 10 INOR- 8 c omposition T ota l (root me a n squa re ) 422

  19. he la rg e st se nsitivity c o e ffic ie nts fo r k e ff fro m c ro ss T se c tio n da ta unc e rta intie s a re fo r C a nd 235 U Nuc lide T ota l E la stic sc a tte ring Disa ppe a ra nc e F ission -0.0286 0.0000 -0.0286 - L i- 6 0.0040 0.0165 -0.0139 - L i- 7 0.0251 0.0283 -0.0033 - Be - 9 0.0014 0.0018 -0.0006 - Zr- 90 -0.0060 0.0005 -0.0066 - Zr- 91 Zr- 92 -0.0007 0.0008 -0.0016 - Zr- 94 -0.0002 0.0001 -0.0005 - Zr- 96 -0.0006 0.0002 -0.0008 - F - 19 0.0749 0.0705 -0.0105 - C- na t 0.5212 0.3970 -0.018 - B- 10 -0.0064 0.0000 -0.0064 - 0.2386 0.0003 -0.1386 0.3768 U- 235 -0.0857 0.0056 -0.0921 0.0006 U- 238

  20. Co nc lusio ns ¡ A se t o f b e nc hma rks b a se d o n the MSRE is unde r de ve lo pme nt ¡ T he e va lua tio ns will inc lude multiple b e nc hma rks fo llo wing the ze ro -po we r e xpe rime nts c a mpa ig n o f June 1965 ¡ A dra ft b e nc hma rk o f the first c ritic a lity o b ta ine d va rying 235 U c o nc e ntra tio n with ste a dy sa lt is unde r re vie w fo r inc lusio n in the Re a c to r Physic s Be nc hma rk E xpe rime nt E va lua tio n Pro je c t (I RPhE P) Ha ndb o o k ¡ I f yo u a re inte re ste d in the dra ft b e nc hma rk e ma il us: ma xfra to ni@ b e rke le y.e du

  21. Ac kno wle dg e me nts I nte rna l E xte rna l E va lua to rs re vie we r re vie we r Adrie n Bida ud L uka Sno j Da n She n Ge rmina I la s Je ff Po we rs Gre no b le Jo ze f Ste fa n UC Be rke le y ORNL ORNL I nstitute o f I nstitute , T e c hno lo g y, Slo ve nia F ra nc e

  22. Re fe re nc e s [1] Princ e , B. E ., Ba ll, S. J., E ng e l, J. R., Ha ub e nre ic h P. N., a nd K e rlin, T .W. Ze ro -Po we r Physic s E xpe rime nts o n the Mo lte n-Sa lt Re a c to r E xpe rime nt ORNL -4233, Oa k Ridg e Na tio na l L a b o ra to ry, Oa k Ridg e , T e nne sse e (1968) [2] Ro b e rtso n, R. C. MSRE De sig n a nd Ope ra tio ns Re po rt Pa rt I : De sc riptio n o f Re a c to r De sig n ORNL -T M-0728, Oa k Ridg e Na tio na l L a b o ra to ry, Oa k Ridg e , T e nne sse e (1965) [3] Brig g s, R. B. Mo lte n-Sa lt Re a c to r Pro g ra m Se mia nnua l Pro g re ss Re po rt ORNL -3626, Oa k Ridg e Na tio na l L a b o ra to ry, Oa k Ridg e , T e nne sse e (1964)

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend