SCIENTIFIC ABSTRACT NAKOV, TR. - NALBANDYAN, A.B.

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December 31, 1967
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SCIENTIFIC ABSTRACT
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- NAKOV, Irr. Conditions fc:r a inlnlmal :3urface. '21'rud Fedag I~nit Plwdll, 1 no.l-.35-36 lo3. 1. Chair of Higher Al.-Obra, Higher Pedagogic Instititta, c Plo,r,liv. llead:Assistant Professor - - W o too 00 00 of 0 to 00 0 0 0 0 O e 0 0 0 6 0 -0 7W- 0000 0 0 O W ~~ 1 4 1 A AA f L f I 1 00 if It 13 14 IS 16 11 4 0 8 a' 14 a Is V a it A K L A X 6 A P 2 2 1 1 l ; 11) 11 V 11 IS ~, Is v is )OA, 41 Al i) "or* - - -. - - - - - -V Y MCC PP" is It 4 41 f I I j A oil &.R ?kfj fpvI*j 00 00 _046 410 A -00 The basic igneous real 01 nortneast Bolkash land and .00 the discovery in th.1m Of nickel and platinum. kuv- -00 nik. 7"441. Gfa, prPsmsing Srs~fe r ~. S. $0. 1173 )(,Wjl); Nfuts jdjrb. jUjotral. CW4. 1933, Ref"alt so 961A). -Old intrusiv" 'wag thwi Kopm consist 11 , diop,side imls. -qwfllitsr A"d 00 .10'ridmilt.. In J,,nx.% in w"wntine and ix-rulolitv prattandite and MaWtite. Ch"M mullit. chmmite .00 . show Ihr prrwt3er u~ Pi snd N! (1).12%). 8*0 so =OO ZOO 00 -0 41 ! zoo go 0 z;0 0 00 j t:o0 =40 10 00' SIVALLUPWAL LiTtRA1641 CLAWFKATIC" 1.7 t:0 0 0 49 u U AV 10 ' I ~ :coo 0 got 0 I I I a Od0 1 v As (1 9 V n A p rp Is 61 Is A x $9 ff It of I mmss M 1 0 0 0 0 .0 4 0 0 0 0 0 0 6 4 a 0 9 0 6 0 0 0 0 0 0 0 0 0 . 00*000100009090000*ea00000~~0*00000*0060040000 0. to 'OL40 _t__L_ A :0 1 - a, , N50 'Ken .1 a as "&:a" and KnJak-tam). M. Rtmlsov and N. N.Ummk- S. R. 67. *143 (11132); NAM" JdArb. mtosoal. Gotal, lqjj, Rvirrmle 1, UP., 711,-Anuly%" Ad vor.111,111111-full tmks Str ilw1whil 00 AS 9:0 00 w r0 0 0 U00 400 400 30 0 we 0 t:o 0 1~4 0 Aill-IL A 4111ALLIaltrMat UTINATtOl (tAWFOCAtION 1.00 1,00 W4*1) -6 as, 4.. as. ~w avoo W, a 0 chi ii- ft tt it 4w &C6 a %a plan 1141twn $,go 440 0 0 0 0 0 0 0 0 o 0 0 o o Co o 0 0 o o . o 0 0 0 0 0 a 0 o o 0 0, __ - - 0 o o * 0 0 C* o o 0 0 0 0 0 o 4 o 0 o o o 0 0 o 0i ie 0 0 9 0 0 * 0 0 0 & 0 0 & 6, 0 a 0 & 10 0 0 9 0 a 0 0 a 0 a 0 0 * 41 0 0 * 0 0 0 0 41 9 0 0 0 0 0 0 0 0 0 0 0 0 & 0 0 0 f 0 " " 0 0 0 0 0 a * e 0 41 * 0 e 0 0 0 0 4 1 t LN 01 AT N n c D to 6 Is x I a v 0 PQ -4 1-1-t 1-0 .4411-1 P. 611110PI, leg -90111NOIS011) 3111111VII1111 ictunlIV1341 IF ws T Use o 0' 00. go Pee 10 go go 700 ~4 00 'o.-Hif %11%) go '0.%t '6 31MA Offloel -1. 00 -1 " j '910~ M umpenJO2 PNV amnotolmly .100 w00 .It ell 14 I I "'I- 1- 7 A A Is to a a u st m w w 61 was( 9)(Fr ust 0 0-0 0 0 0-0 q 0-* 0 ---MU.0t 0 00 fees 0 0 * 0 0 0 0 0 ;040000*00000000 I to Iluumuld lite 21 12 a id n a p u u Wit hu ups., adjudro A -11 f It- It -1--l - V 1- AA- N M JDP U-4 IL- I I t Whandto near Kounred. S. 1, N'slinvink. He4koo, - Jlfldl. 1. 1 MIMS); Nelffl J11APh. MlIffift. Rtf~ U. 9 a 1437, 1110-The tirpmils air at the 4.1fich l1runnen, 7 L k"I, lrom IN clk 4k-Po%it4 of Kon"fad. rhcv coll%W of 41114111 vri". in olarnit, "I in the neirglINW. h,kwf 1.1 whit h the 9141"Ur IIM% IWVII 111MI'llt'll 10 AMIA III 0 and 4,M141111. topsy, Ililof It 4.. pvt it e, W.11frandor so 11.114 1111 rh&4-vliyyilr. rhe nso%o ini,miriAnt irimAto III wnitimasia I. *I the Quartolwrx. where it I, in cly4tal. muAlly 2-A anntfirnre 10 cm.. long. Ansly,it: Wth 7AXI, hIn( 111.341 and Pro 7.xle;. V, A. Sollwitod 00 v A I z - it ~1019` 11111 0 U A, so Ls 0 0 0 0 0:0 0 0 4 a 0 0 0 0 0 0 0 a 0 0 Is 0 a 4, 0 0 a 0 0 0 0 0 0 0 0 09 0 0 0 0 0 .00 so =6 0 ro 00 LAD 0 t:0 0 0 0 : : A :0 A 00 C 06 oil 00 0* 8 :0 a :: 0 -3 00 u ''I I a a At a 44:19 it, F- CA 11. 21-11 WS 7 oQ1 a I . ~ - 1. ~ VIOC1161% 4.0 0 0 o o 6 0 o 0 a o 0 0. sill u it job IOU mWe'la a) At 4;0 0 I. a 111A to Is.-@ . . - .101, 0 00 Koumd au4 Its an4alusits mitierstlisdon %'~ V : i 14akovaik. &r4l Go4. 11, 978 tKl(1tA;P;1; Xtutj Juhrk 0 0 'Mmeral.. Goof Rel' * 11 1919 Z14-fj; cl-Sbilmllov. C-1, - , C l i h 1 W; i -09 ,- oA?rr at Sultimill q 1 1% te t s 32, 4193 3wr deposit of Kounm of 2 lypes: a ortinfr-pylophyllitv. -00 avadidusite-quartsite contl. 0-80% andAllaiiie. and ib orti- -00 cile--chakepyrite(O~$%Cu)-qmrtzite. Fliamn.v(some 700 thin sections shows the andoluxite, -which ayffage% X&O 10-12%, to be umal y amervd. with trulamorphowd PorpbyTific farx. C. A. Sillx-rrutf Alm-ILA "TALLIP"KA.L LITENA114141 CLAIMPICATION 110juak"? wit OVVW as( .1 zoo go o clef SO* lose use too Via.. woo Ile U a A, 10 It 0 a to o 0 re- 0.- 0, 18TOG 0 N o 0 0 o 0 o o 0 0 0 o 0 0 0 0 aftL61 4d "I it, ad 0 01 a I or W I a 4 3 1 v 1W - on 0-9, 0, -0 0 a 00 0 t 0 0 0 I C 'POO 10046004 :0 0 0 0 0 0 0 of 0 0 0 c 0 0 0 0 0 0 0 11 is $0 14 is if If " a a IS It a lo, to of so so, or* .1 It-11 " I v 8, if P 9 8 1 1 v V, too'. .40 so 00 :-~* e9 , `~~ 00 so c so 1-00 go /M. ofiv,"1936. Nis. 22, 11 11.- This 0 ro, So Cu. &its. SON. Ail, mossit'll. A detailed K")I. mintfillilli,41 dewiplitm it givris. A. A. If. .0 0 -go z0 0 too ASP.SLA 61TAMMCKAL LIMATIAt CLAWFICATIC" 0 oil, &I -un Am in W., --4-4 �6 0 , III go a K n it 1 14 Aft I 1 3 not Do It 700~00 0 w 0 0 .00 0 0 O's 0 0 go 0so 0 0 0 0 0 0 0 0 0 00000660 0000 00 -9-0 --- - -- - ---- -- - - - - -- - -- -- --- - ----- - - - - - - Deposits in Kounrad, Its rocks and minerals Moskva, Izd-vo Akademii nauk SSSR, 1937. 176 p.0 20 platesl maps. (49-55367) QL'452. RqN28 9 6 0 0 0 a 0 0 0 9 0 0 0 0 0 0 0 0 : * 0 0 0 0 ,0 0 1) a 0 0 0 : : : : : 0 0 0 0 0 & 0 0 0 0 0 0 a 0 0 a 0 0 a 0 0 0 0 0 0 0 0 0 0 'h Oil` ft A# u ri". L, j, u n it p m tr 0 0 a, 41 11 0 1,1 it t. av it r% a w e go oo oo.,- go,, *or oo~ oo.'- 00-1 0 of 002 09 p 0 oo~ v 00 ' Aldal. qqwyp, . . UMINI)g-j" ' Pl 91 A. T Arl -1u go N '9 in got Ala-u V 00 of- go 00- go oo IN vv V- A A I t V 0 4 It U I r-I 5 1 so I o #I it -i 31 tv hrwa, Iq u re v it I? ~V it li 11 It U 11 tl I , I I f I & 0 0 0 0 0 - a 4 0 0 0 'a 0 0 00 0 0 a a 0 0 0 d, 0* -s 0 0 0 0 9 if WACC,44_4- [TO 9 Is It 1: 13 M it W It to .7 211 M D b J7 a to J; it 11 It J4 D 31, Y AV P 41 a a u A- 0 1 IL _J_ L. to I 2_1L -1 1 Jy N CC pp A t d ~pf. Umclotry quartsites and Their relation to olhpr Met, rnOfPhO6ed rocks N. 1-00 00 it, u, rot liu,41; If: 1 32. IIIII)Ile. 4"t low, IIIII.-faile I I;,. I'jO, Fr;f l'i .-go 09 a- "t Y quat I All". I'"., :.go 00 141.1e,i give lite txdvr a f"Illdli.,11 .4 VArim, ".1"'fulart . I 1111.11tille luilmou ululk, vitaimpt lawl Alit, of 1,11, ill,, -90 -00 11111"vitt. Lifillil... a 1.1101r, 'hbalt'. .00 L4,41111tv, mi-I hi'll'- .00 114.111.1 mW pl.-Il... Lowbtalor I"Ohm- =0 0 00 j ills Ill Ill,I Lit-vo, F. 11 RAIIIII1.11111 09 A! -:00 00 ld age see 00 .00 A 00 tie 0 t:0 0 wee so tj n AV i it x Of N 0 0 0''0 ~ 0 0 4 0 0 0 0 0 9 0 0 #!q 0 0 0 0 0 111,A 0 0 0 0 op 0 0 4 0 0 0 * 0 0 0:0 0 lip a 0 0 0 41 0 0 111,0 A A-A J C L &-s~ a 1 10 0 00 A A -A of CC too 0-11 f..'00, . Changes in mutton (its dudug storage, 1 i. S. );. R. 10, ncchni.- Afrilmiaw Ind, . Itmo.-Sto (I(gv,~j; Chimir & industrie 42; * , ullim Afhv , to +11 fat fm 0.5 days At -22 Sim"I at IN', tile (at st(xkl lip Gm 125 im"d Tw ' &% Alld h ld f , a ,jh tjay tr3orrs o hill the q. y -Jdl-W~tM. l."I (at mine that) 01.1.1yo. No. ring t i1 Ulenalot CLOWICAMN u x AT so u 0 ; ; ; ; ; ; i 9 0 0 i ; 0 : : : : : 9 & 0 0 m or a or u ' 0 A 0 00 I.Plal - no, _00 N. NAkui 1, 33 -1 nimlots ilq tillahly, I'M 414y. of PrIAM41c, to Lie e All A t it ad a a a 0 love C~_ Rem" of tbr" F"W sumni-am of 4madifted of tb* O"Win KAMMUM IA4 W ALWWW& N.1.NASQVM11t. C0111fibU11061310tcGCOkIcy ol of an Hxpedition to Cen- tral Kalsksla" III Ittlit-3- ii-m). Aced. Sd. EISS R.. Itple); Nhim. Relona.'ru-, 0 - 0-0 Ole-* 4-9-4 Y_A ~1_ I At 0 -00 4 0`0 *-*io 0 0 0 0 0 U IV El go 00 0 0 go Now data on the mineralogy ot the lateral rocks of py. - lite deposits in the Urals.N ui. 1'.R.S.S.. V;,. Abdiall) 9, 23111111111) D1.1,14mv. pylophyffirl" Polul, 11VTile dt'101.1(1 11C.If 014! COJIIJCt Witil gF.11111r. M. V. A I L WALLO~Gl'~&L LITINAT60t CL4111FICATIC* t1l" 11-t D -i' It 0 o 0 a, 0 a a 0 0 0 * 0 0 0 0 0 01,41 0 0 0 0 0 0 0 0-0 4 too -00 -00 - 00 ..00 'goo I I goo 0 0 0 a a 0 0 0 9 * 9 0 0 : : : :~'A :14- [it X it 9 11 )d IS NO I? X 0 4 At 41 43 46 Me@ L-ALLI-LI-ALAO 91 1166 ILI 11-111-tk- 211-44-10-114A2 A 1 0 0 1 a A a ,A Ax m_ .4 __0111V 0-1.11 A.F. fit ff a 1.1-6 If*,# I 00 A RsvWoo of the quattiZ64 minstain of Wait. N, t. -00 Nakoynik. -Ratatalka Nedr 12. No. 2. 2t)-3(lWrt- N-1rtf&qtf-ajjvomtrs a thorough rrfxamn. at the Salair 00 hfry quartzites whcnby he befievet (tZatakhstan) second I or neglected. com- gTmt (11jalstilles Ad either unrotim 00 metviAlly 1111p(wtant, Ole 111inerab woulti be discoveml. -00 00 W I _11110 00 00 1 woo .3 =oe ZOO Ood coo Oow coo coo 900 '400 moo izoo ;woo A 04TALLORGICA& LITINATtOOR CLASSOPKATION 9 UOO -Al Net) -A 141,345 .10 Oftv .341 GJA111*01 Arl I I -f,w 0 9 NO 5 A 'r it F 1 3 1 AT NO H 9 it rp It of It ff It IN KID " 1 14 dig 00000***Oeo*0000000000000000000000000000000e! ZOOOOO*10000000000000otooo4loooo000006000000000ij -W -all U=UR11% at9m, Ole 0 0 0 0 a 0 a 0 0 0 0 0 * 0.0 0 0 00 0 0 0 0 eve 0 00- 00000000090000000 00 --- I - I - s 11 .1 1114 -1 A- - it- to Is-* it n -11 14- A 0 loll" W-UP -4 it -4 to w 0 41 a stme 1 L I., J OIL 1 .1. .1-6 k i_ I -t 0 s- V ~A C-k Is ,L-------.----- -00 A F, .40 Go 41 F f ; 90 go A 7 66 so 0o -00 00 go A tivuW06" Jk* Mlowid faco~ 1444w~ and Bell. did J, iijv" Gitract"I In Chew. 1-114R.S.S. Inshes aft fit- zitur, 194,71ft"~Zlql~ 2M.-&vondary qtu 010matlacts. Le..changed effusiverorks Anvil as metasomt cwtaining. besides. quarts. pyrite. hematite. sevicite. too alunite, kanlinite. amialualle diaspont. corundHm. pro- 0 phyllite. Alunyhr. dumcwtwtr, awl talwS. Secondary anxit" are found mostly In Hast Nasakstan and 91-1 M IIA. 00 j lughe Caucasus, tlra!. and AIW numnlain & 00 see 00 goo 9 ISIS* lee WA A W 0 Ba~-j M! SL A WALL04KAL UttRATU411 CLASSIFICAT" too !talk GA-~140 44P *.v d5t too An A I a rw is 0 1 If It v A) fl7~ I, go to It at Ad It ft It It PC U It It W KAD A 1 14 9 :ie o 4 0 0 0 0 0 0 c 7 of n ~:.r %~,rieweAl 'by IT.L. vo3t. LOW I,- (Fritrol,).-7) 0,uznotuov, 25.A.) NAKOWNIK, N.I. The immersion method as applied to a petrographic microscope 2. izd. Moskvap Gos. Izd- vo geol. lit-ry, 1948. 34 p. (51-21081) QE433.N3 1948 Ajunits. I and relallons to cowtry rocks and or* Was N IT NAkovnik Zapisht Vsrsoyus. Mineral. minkral.) 77.55-4H(H148).- The crystallochem. fornsuLl is KAW50j)2(010j. with a IWliAI substilutlt;v of Sa for K. ()oelter dig-,injuishft the vokank gmesis of alunite. and a hydrotheraval type - in vrins, and a third type ch.Aracttrized by exogenic rc. actions of 11"Sof (froln Oxidized Fe-S, anti S) with count ry iock. In general, Munitc, 6 post.voicullic, jormell ulj(lcr low ""T conditions wilh pseudotnorphs after Ickilsilar. Alunile- 0 typical mineral of the epitherjual inelasotuatic forinAtion in secondAry quartzites, replacing especiAlly the higher silictrous alummolificutes. but not minerals with CA. Pet Alff (limestou". serpenduites, m.,r6. tic.). Llparitej. porphyritm. frachyles. and their tugs Anti brec- cU3 hire principallY affect-I by alunitization, basafts anti diAlusei only rjrrly changed to alunite, ultralsaic rock,, never. The dicutsiun of inure than 2(g) analyses sho%ji OLIt I[it lliglk-r it, the I%A%icity of the original rocks, jim. MOW, ii tile NZA) c0filtht Of the resulting alunile. Ande - sit" havc~% i-kti-itlfll-21oll: 1; thecurrespondini: NOO for p0fllI1YF1I" ii 0.4 it) 2.7: 1. and fordaci(es 0,7 to 4: 1 fav. 21.2: 1). Nearly pure K alunites, are derived from X-rich porphyries. trachytm, and rhyobtex (ratio 8: 1). The analyses of ulunite-beAnng rocks snow the prnlorni- nance of K alunites derived from high~ilica roelts. In cavities in darites, the r4tio K,():NA,O InAY evell be 12. 1, or 31: 1, tm*. Na alunite is never olnerml in vrins Insiliccoustocks. There is a distinct dtifference between the nwasommic silimilvi dillkUSStd Above and hydrothemml depogits of alunite on tile walN Of Cavities, foltred by HS01-conig. watrio In tile coontiy t1wits which ofirn transfer the alkali lons front .& d6lante. The optical iouxts. of K alunitc are characteristically different from thow of Na alunitc. anti A table i3 given which shows thc correlation of the KIO: Na.0 with ms for 20 simple%. %4 alunites IL&ve :4 bireftingencr of 0,00-5 to 0-012. K alunitc. of 0.01H to 0AW. The silicification of the country rack to qUArtX, C1341ccdony, or ojhtl during alunitizAtiou i3 highly significant. The paragentsis of SKh minerals with alunite is awled, with pyrite, of helliAtile anti rutile, anti in tuitior Atoll. by dimpotc, dickite, tuttyite, and 14. zVolitrib, selivile. Alorill.. tpillott. anti Pinill.ir minvtaln tire Awnt. Alunite tocks air ofien ac. rompanivel by vrins with minerAN of Ali, As, IIX, Sb, I'll, Zn, Cu. Fr, 'in, blo. Bi. KanliniLition and ptopylitiu. tion with alunitiLklion is olmervcd in ore deposits all over the world. In cryst. schists almnie 6 entirely absent, Al~ in Sr.6nitrs, grri~ns, skArn,,, and contArt hornfebes. W. Elul M~fAMGMUC CJ`T$tAIIIj&U40d With Coniltifill volumes '.4k )vf3j'k Zapiski l7sesoyms. Alsite,al. MIA. 4"/&.I %t, %I It'A . ti's mintral.) 78. 270 ie~ -2(totin.-rhe mech- anisot of tricummi.itic reactitnis Is chiefly ch;ir-Acterized !"v the inipregnatiots fit prefitisling minCrAl coniplettes hy a Iso,tilluille" soill. chiefly 14 majol-illie tallill. fir tit !it. VvItile w4teis. soln. ws,-,nding along channels and thniush. mit the capillAry sysitin of the solid frainewittli of the fix It. The typical IMMAII011 Of pseudomsiphs by them, trictiorij, "itiolevule for molecule." rep4cing the "hmt'* minerals is obcrvvl in sautisuritized feldip-Am nr III the :111111illit.11h)II anti it'lollilitizatloll of all-1.111111tr, Willi tl-i&rtx awl dlji%pore, the clLinge of hlothe to a 11111ril iggTrgitti; of wrivitc, rutitc, vind jqrfte. LisidgreWs ILIW (if "cou,lant volumes- for the host anti the fraction 1)rwltzt,t% is an im1wrtAnt principle- its petrography asid mc delitmit ,I u4sirs. P.Iftleu.Urly ints:mUng examples are Oven. mnotil; which the following are taken frints the hydro. thcrmAlly changed lava% of Kazaklislan: dirkile. reptscing Motile anti pliginctav, fillivig the cavilies of the liv... In !he first c~qe. rutile is simultantinuly forsticil with the IbCkitV, in the %CCOIld CIAMPIC free Si(h tryAll. 4% flU IrIZ. I'articuLaly instructive are the prallel oficiatalioni of the ,lickite P4rCCI4 in the layt-r structure of the origin al inica. Um protiounced are the orientation effeelti (it dickils: its p%cudomorphs after pUltiocl3sc. The pwudotnorlih, of al4nifeafter fek6par (with smile qu;irtz) are ch.LrActer6tiv lxvau.c of the absience of every influence of the repLuvil structure on the growth of the new prtxluct. although th - orighvil volume is entirely preierved and fill.-J. Aluni. sized tok-as AlwAys show the ofientatiott of JIM! Cfy%t.Lit pivillel to [he clc.&v-j4e plAne, like in the dickilt- I)-t:tttlrj- niorph-. W. Ellel ---- --- - ' M i -in the fir3 t gioup, 6 0 01 t. 8 for il eral facloo, en Oslo, and prictl6l Importance of Re0l, to 7 to 0 In the propylltind Zal'ttki Vsejoyur. I& l Mircrak A h 8 l . challged Ly prollylilha Han n re the 111CIAU offal fu 1111CAtu. (of- I - d % F h K I U b l ~j , ud gr. 0 rvm m ra 3, P&-P I .) (1954).-N. defines the prorpylites as a complex of uralitized, rom a owed atest t oclase. sai e C v, tj y plag tevicir of wpyntes hom linportwit art dcpCr~0, N. give-, chloritized, or albitizLd rocks, distinguished frmi tiva, diagrams which clcmanitrate the chern. di4nges occur- rocks, secondary quartzites and greenston" of ring in intermediate, and In basle rocks during, propylitiza- reglonal-inetamorphle nright. Propylites are hydrotherinpi tion, e-.1'Crilily for SO,, Algol, FCO, FLION"'C;10, h1go. 1 decompn, - arts of primary intermediate or hasic --ffu3ive g Na~0, X.O. CO., reSs, Cu. and An. In the ilifection from wlt . .1 , Ite, adutarla, uralite, or tu:tInalite, evidotro, = tile exterior to t1n: Inner zonns tho data for Slrh "tilt AII01 are rutile, catbonato, quartz, scricite, and pyrite. , They are intinult l d h h h t i d l d not c-sentlally vaxiahle. but CaO, M40. FcQ, and PeA '& -1 ili d l i t I d I U .- e y connec w e rot erina ore r t y posits of Au. Alf, Cu, Zn, Pb, As, Sh, Hg, IV, Mo, and sub- c- ent tt an Ls corit nuoug n crense v y, more nk dacitic rocLs than in those of pbbroidal k~p.~' Mi,() and ordinate Sn. Nj, Co. Pt, assocd. Irith veins of ankerite, calf K20 beliave reciprocally, with a max. III NlijD. a nAn. In tile, rhodocbrosite, quartz, PAc. Tile chem. rold mincral- K201 for the tPiflote-C111-110 7onM Parallel to the enrich- o0cal 4=pn. of propylites derived from andesitIL-dacitle or ment In Y-0 in the Inner une-i. 140. CO,, and sulfides are dintritic; rocks near the ore velas chnngc3 in a characteristic Incremed, and Cis and An cre parallel to the enrichment In zonalityAn the Inner zones, next to the ores tile quarU- tile voLitileg. SL Al, 11 are the lwt mobile Plement-3, more -eeridte assocn. prevails, while epidote, chloritc, and artino- mobile are Ca, Mg, Fc. Nfit, mont mobile Na. K, Cu. Au. lite are: typical minerals of exterior zone. Prnpylites de- and the vulatilescomingfromdee"Cated sources. Arough rived firom basic rocks (e.g. gabbros) show the type of list- parallelbui exints with tilt Ionic tadil of these elenlentN. veriltes, high in carbonates and scricite. often urith Cr-miLa. The rare and exceptional 'iydrothermal rock type of the The Inner zones am always smaller than tile extcr;,r mics. b~"_ ites (tinaftz-jau5covite aplite-j, without any K feld5par, ' This characterbstit-for the reactions (arnphilluh~, ,db,te!a e T dote) - (chl rit it RCO - ( i i + ) 0~c veins of Dcre;wvsk (Ural) is In ace^ respect5 in the Au k!s e f liti d o l th I ti t " a e e sex c te, P pyr , 5ttartz., sulfides),, with a gradual change of PH from 11 to 8 . nner zone orma ze r c o ons o ana ogous e propy W. Eitel J NAKCVNIK.N.I. Concerning articles in the collection 'Basic problems in the theory of mngmPtic deposits." Zap.Vses.m1n.ob-vA 84 no.2:237- 239 '55. (KLRA 8:10) (Rocks, Igneous) NAKOVNIK.N.I. T1-7z;w:T~ Classification and terminology of pyroclastic rocks. Zav.Yses.' min.ob-va 84 no (NUA :11) ' -3:381-385 155. % 8 (Volcanic ash, tuff, etc.) I . . ....... I- . . - - -4 NAKOVNIK. N. I. - ,,, Some observations on D.S. Korzhinsk-ii's work "Study of metasomatic processes.ffi Article reviewed by H.I. Nakovnik. Zap.Vaes.min.ob-va 85 no.4:597-603 156. (MLRA 10-2) (Metasomatism) (Korzhinskii. D.S.) NAKOVNIK, Njk CHETVERIKOV, S.D.. redaktor; NIHANOVA, GJ., .2bZ.jXgA=!ch: "'redaktor izdatalli-tv-a; KRYNOCHKINA, K.Y.. takhnicheakiy redaktor [Immers'ion method as applied to a patrographic microscope] Immersionnyi'metod v primenenti k patrograficheskim shlifam. Izd. 3-e.* Moskva, Goo.nauchno-tekha.izd-vo lit-ry po geol. i okhrane nedr, 1957. 40 p. (MLRA 10:8) (Petrographic microscope) N"OVNIK, IT.I. '! -7- ~__ - - New type of change zones adjacent to or& bodlov. Zap. VBes. min. ob-va 86 no.6:713-716 157. NTU 110) (Argillite) (Ore deposits) NAKOVIUK, 11. 1. Determining quantitative change of substances in h7drothermal metamorphism. Zap. Vass. min. ob-va 87 no.4:401-417 '58. (MIRA 12:1) l.Yeasoyuznyy geologicheskiy institut, Leningrad. (Rooks, Grystalline and metamorphic) WVSKIKH, V.vo; NAKOVIUK. N.I... MROVA, TO.V. New dumortierite-corundum-andalusite depooit in Kaza".stan. Zap. Vues. min. ob-va 88 no-5:521-532 159. (MIRA 13:2) 1,Vseso7uny7 nauchno-isFiladovatellokiy groologicheskiy inotitut, Leningrad. (Balkhash re&iou-Mineralogy) VOLOSTNYKH9 G.T. L~AK~VYIKV N.I. i_ROZENTSVIT9 A.O.; KLIMOVAq M.S. Remarks on IU.V. Nuzitsyn and G. V. Alelivandroy's article IMeta- somatic zoning in the oxgillization of granite-porph7ries near ore bodies." Geol. vu&~.mestorozh. no.6t9l-97 N-D 1 60. (Mira 14:3) 1, Voesoyuznyy geologicheskiy nauchno-issledovateliskiy institut, Leningrad. (Clay) (Nuzitsynp IU.V.) (Aleksandrovp G.V.) NAKCIVNIK, N.I. Study of kaolin minerals. Min.abor. no,,14:396-399 160. (raRA 1. Vsesdyuznyy nauchno-.issledovatel'skiy geologicheckiy inatibit, Leningrad. (Kaolin) 15;2) ~ "I . 4 ~_ NAKOVNIK, N.I.- History of the study of secondary quartzites. Izv. AN Arm.55H.- GeolA geog.nauki 14 no.4:73-84 161. (MIRA 14:9) 1. Vsesoyuznyy nauchno-issledovatellskiy geologicheskiy institut, Leningrad,,,_ (Quartzite) AVIKSON, Tu.A. . inzh.; WOZIN, N. I. . inzh. Drilling and punching openings in high-manganese austenitic steel. Sudoetroenie 29 no.2260-62 F 163. (MIRA 16.'2) (Shipfitting) (Manganese steel) NAKOVNIK, ~N.I. Vertical zoning of the products of Po3tuagnetic metasomatiam and the place.of the formation of secondary q'uaj*tzites,and propylites in it. Zap.Vses.min.ob-va 92 no-4:394-409 163,, (MA 17:2) NAKOVNIK, N.I.; KAZITSYN, Yu.V. Conference on the metasomatic alterations of wall rocks and their role in ore formation. Zapo Vises. min. ob-va 92 no.5:626-629 163. (MIRA 17-1) PAKOVIIIK, N.I.; TATARINOVI P.M., red. [Secondary quartzites of the U.S.S.R. aryl mineral deposits connected with them] Vtorichnye kvartsi-kir SSSR i sviazannye s nimi mestorozhdeniia po:Leznykh iskopaejVkh. Mos"ral Izd- vo I'lledra," 1964. 338 p. (MIRA 17:8) NAKOVNIK, N.I. Detemination, of the "subtraction-addition' of a substance during metasomatism and the lav of Lindgren. Zap. Voss, min* ob-va 93 no.1t110-113 164 (MIRA 18s2) Y~ a VIP ~bl!, P124;, Dde-VAUUOn nd v Pra"a a a kmgov (Co' V, dtjrACG7.~. ft&cts idth --t Ro so, 'Cl Ko. + zRj rLdr, Lius: and is uSec, 11, 00 per'ren'. + KCI + ICI kt, H ') d"s potentio-, I . ICid to t tram'. Rllphati, RUI&J, bnt, cetic hen ASSOlve(l In A M'XtllreQf dl water met-ically m :L,:etc ~'lf% phtha%to (35 Pt.). Lcl (0-4 N):j (CI %--l - . fL C. the cq;nr I, :E I prr cent. 7(-j 8707 S/191'60/000/01,0/01117/017 X Doi Bo6b B004 AUTHORS: Moshkin, P. A., Rubtsova, I. K., ZhJLLina, R. D., Nakrokhin_,h,~G 4111111100111~__ , Itenberj&, Sh. Id. TITLE: Alcoholysis of Some Di-ppf-C yanethyl E~terj, and Investigation of Products Ob tained PERIODICAL: Plasticheskiye massy, 1960, No. 10, pp. 60-6! TEXT: Proceeding from acrylonitrile the authors syrithE-sized the following compounds: di-OPI-cyanethyl)-sulfidej di-PPI-cirariethy! ether; furthermore, Pp'-cyanethyl ethers of ethylene-, diethylene- and tri- ethylene glycols and butanediols. By alecholysis by means of 2-ethyl hexanediol one obtains the 2-ethyl hexyl esters of oxadipropionio acid, 2,4-dioxahexane dicarboxylic acid-,1,6, 2,6-dioxaoctane dicarboxylic acid-1,8, 2,4,6-trioxaoctane dicarboxylic acid-11,8, 2,4,6 8--tetraoxa- decane dicarboxylic acid-1,10, and thiodipropionic acid. [Abstral-ter'3 Note: the conditions under which the alcoholysis wat3 performed are not indicated]. These esters were found to be resistant to frost down to -45 - -580C (determination by L. I. Burinova), and yielded, when mlxed Card 1/2 8707 Alcoholysis of Some Di-ppl-Cyanethyl Lz-vers, S/191/60/0GO/010/013/017 and Investigation of Products Obtained B004/BO6O with polyvinyl chloride resin in a ratio I : 1, plastics which satlsf-'ed the technological requirements. There are 3 tables and 4 rcferu.,-,ces: 3 Soviet and 1 US. Card 2/2 SHIBANOV, G.V.1 GINFUGH, G.1.-, OBRAUS01, A.T.; MATHOS, Yu.Sh.; SKUE, G~1.; NAROKEP, V.B.; ITEMERG, Sh.M.; RUHRAGUICH, Kh.D. Oxidation of methanol to formaldehyde on oxide catalysts. Kh1m. prom. 41 no.2-17-19 F 165. (MIRA 18.4) NAKRCRYIN, D.G.; SHIBANOV, G.V.1 GINFVICH, G.I.; OWAZTSOV, A.I.; MATRODS, lii.Sh.; SKTF--, G.I.; NAKRCK.HIN, V.B.; ITENIERG, Sh.M.; RASHIRACKNIGH, Kh.D. Oxidation or iriethanol. to formaldehyde on oxido catalysts. Kh1m. Proni. 41 no.2:17-19 F 165. (MIRA 18:4) NIPUIIWUI.~11.11 ~'i. NAKROPIN, 0. - - Instrument of aggression. Voen.vest. 34 no.io:94-96 o '54. (KIRA 10:10) (United States--Politics and government) 107-57-2-63/56 AUTHOR: Nakropin, 0. 1ITLE: A Voice of Instigators (Golos podstrekateley) PERIODICAL. Aadio, 1957, Nr 2, pp 59-60' (USSR) ABSTRACT: A review of activities of "Itadio Free Europe" is presented. A group.of American magnates founaod the "Crusade for Freedom" organization in 1949, which quickly built a network of radio stations in Western Europe. "Padio Free Europe" operates 29 radio stationsg that transmit 20 hours a day to Poland, Czechoslovakiap and Hungary, and 8 to 10 hours a day to Rumania and Bulgaria. Its headquarters are in Munich, and the total per- sonnel number 1,200, of whom 120 are American citizens. S. Mikhallskiy, a Pole, and former employee of the Munich radio center, related in the Polish press that Hans Fisher, Chief of the Security Division of "Radio Free Europe", made it clear that obtaining a permanent job there depends on good relations with the Security Division and with the American Intelligence. The West German magazine "Spiegel" commented that "Radio Free Europe" can speak with the voice of a private organization, and still be taken as the official voice of the USA. The'role of "Radio Free Europe" in ihe Hungarian r-prising of 1956 is discussed in the article, and a number of West European publications are quoted in this connection. Card 1/2 Card 2/2 AP60317 29-----g-o'uR'C-E~-C-OD'P.'-7--Ul~'/0-1*36-/"6-6'/006/00!~/-0-078-10080-----' ACC NRI AUTHOR: Polin, 1, Va; Hakaimov, Ve Mo; Darmograyl Ve Ve ORG; none TITLE: Results of experiments on deoxidation of titanium SOURCE: Tsvetnyye metally, no. 9, 1966, 78-80 TOPIC TAGS% titanium alloy, titanium zirconium alloy, titanium gadolinium alloy, titanium yttrium alloy, titanium dcoxidation, metal Property,3 OXVGFA) j --11?C0AJ1UM (VA-~7n/A.01A.)6 17440c1 j 13At-OLI e0/nP0'5j'7'0't) ABSTRACT: The possibility of lowering the oxygen content in vacuum arci meltod titanium by alloying with zirconium, gadolinium or yttrium has -I been investigated. Commercial-grade titanium with addition of the above: alloying elements was double melted in a vacuum of 0.012-0.1 mm Hg into 5 kg ingots 130 mm in diameter. It was found that zirconium lowers! considerably the oxygen content. For instance, while unalloyed commercial-grade titanium contained 0.102Z oxygen, an alloy with 1.5-2.5% Zr contained only 0,055-0o075% oxygen. . ResuIts of experiments with yttrium and gadolinium were inconclusive due to the Card 12 UDCj 669,295.046.55 ACC NR.- AP6031729 ,very small number of tests conducted. It was concluded that it rs possible to deoxidize titanium by alloying it with zirconium. Orig. lart. has% 3 figures and 3 tables, ISUB CODE: l1/ SUBM DATE: none/ ORIG REFs 001/ OTH REF: 001 KC14AROV, P.V.;-NAKTINAS, Ye.M 01.1., Fluorine, chlorine, and boron as elements--ird jeatorS 4r., gecchsmfc~al prospecting. Geol. rud. mestorozh. 7 no.3:65-74 My-Je 165. (MIRA 18:7) 1. In-titut geologii rudnykh mestorozhdeniyj petrografiip mineralogii i geokhimii AN SSSR. BUSEV, AJ; XAKU, A. [Nacu, A.]; Prinimals. uchastiyet DZERZHINSKAYA, L.S. Use of mercaptopropionic acid derivatives in analytical ohomiatry, Report No*13 Extraction-photometric determination of palladium with p-anisi~ide-l-mercaptopropionic and p-toluidide-l-mercaptopropionic acids. Zhur.anal.khim. 18 no.4:500-506 Ap 163. (MIRA 16t6) 1. M.V.Lomonosov Moscow State University. (Palladium-Analysis) (Proionic acid) BUSEV, A.I.; NAKII. A. - - - - - Eytraction-photometric determination of palladium by means of thionalide. Zhur. anal.khim. 18 no.12:1479-1482 D 063. (MM 17:4) 1. Moskovskiy gosudarstvannyy universitet imeni Lomonosova. IUSEVP A.I.; FaJDZIT, G.P.,- NAKU, A. Use of 1-mercaptoprovionic acid in analytical chem-listry. Report No.4: Extraction-photonetric determination of molybdenum in steels with p-phenetidide-l-mercaptopropionic acid. Zhur. anal. khim. 19 no.6:767-769 164- WIRA 18: 3) 1e Moskovskiy gosudarstvennyy univer.,ftet imeni Lomonosova. SAVUL, M acad.. BOTEZ K. [Botez, C. I IONESI Y L.J, OLARU , D. P ;IA'KIJ.9 A. [1-lacu, A.] Chemism of the rocks of the Palegogene Flysch transient facies, developed in the Moldovita Valley (Northern Moldavia) for the Co, Ni, Mn, Cu, Pb, Zn elements* Rev geol geog Rum 7 no. 2; 217-244 163. BUSEV, A.I.; NAKU, A. Use of 1-mercaptopropionic acid derivativas in analytical chemistrj. Report No.2; Photometric determination of palladium witi; r-phenetidide-l-mereaptopropionic acid. Zhur.anal.khim. 18 no.10:1233-1238 0 163. (MM 16:12) 1. Moscow State University. 'A DUSEV, A.I.j., II.A.KU, A.; RUM2T, G~P~ Us,i of af~id dsrlvat-lv,~B in anhly-.tcbl cherdBtry. Report No.3il-ML~rcaptoproplonlc acid anl sm,:s of its anilides as reagente for the ex-tiaction-photometric del.cri-al-nation of' m,-)lyWc)nu.,n. Zhur. anal. khim. 19 no.3? 33'7--3-'5 '614. (M-TRA 17::9) 1. Moskovskiy gasudarstlrEnn)-y tirilvernitet, imeni Lomonosova. ACCESSION NR: AP4019509 S/0075/64/019/003/0337/0345, AUTHORS: Busev, A. I.; Naku, A.; Rudzit, G, P, TITLE: Use of 1-mercaptopropionic acid derivatives in analytical chemistry. Communication 3: 1-merca topropionic acid 4nd some of its anilides as reagents for extracUon-photometric determination of: molybdenum !.SOURCE: Zhurnal analiticheskoy khimii, v. 19, no. 3, 1964, 337-345 TOPIC TAGS: molybdenum, determination, extraction, photometric extraction determination, m'ercaptopropionic acidl mercaptopropionic acid derivative, phenetidide, anisididef touidide, analytical chemistry, quantitative analysis ABSTRACT: A study was made of the interaction of Mo( V) and Mo(VI) i ions with 1-mercaptopropionic acid (i) and some of its derivativest o- and p-phenetidide, o- and p-anisidide, o- and p-toluidide-l- morcaptopropionic acid. It was ostablished that I and its p- phenetidide interact with Mo(V) and Mo(VI) ions in tho-ratio of 2:1 (In'fig. 1: thetangent of the angle of inclination numerically Card V6 ACCESSION NR: AP4019509 equals the number of moles of reagent interacting with one mole of Mo). The compounds of molybdenum with p-phenetidide-l-mercaptopro- pionic acid (II) are most readily extracted with a 1:1 mixture of isoamyl alcohol and benzene, and the compounds with I are extracted with a 1:1 mixture of isoamyl-alcohol and chloroform, when1diphenyl- guanidinium or benzylthiuronium cations are present in the aqueous phase. During extractibn one diphenylguanidinium or benzylthiuronium cation is added to a complex anion of Mo(V) with I and--two cations are added to a complex Mo(VI) anion (fig. 2). Extraction-photometric methods were developed for the determination of molybdenum with I and with II in the presence of other elements. A sample containing molybdenum is treated with a solution of I and benzylthiuronium chloride, extracted with 1:1 isoamyl, alcbhol:chloroform solutions and the optical density is measured and compared with a calibrated graph. It was found that: Cr, Ti, Co, Ni, Zn, Al sulfate and nitrate ions,.do not interfere; in the presence of large amounts of vanadate andle (III) ascorbic acid should be added; Cu ions lower the accurac f the determination; and very large.amounts of W make determinatiWdifficult, but with smaller amounto# the optical Card...2/6.. ACCESSION NR: AP4019509 density may be measured at 350-365 and at 430 millimicrons. A similar determination may be made with II, using 1:1 isoamyl, alcohol:benzene solution for extraction and measurin the optical density at 360 millimicrons. It was found that: Cr fIII), Ti, Co, Nil Znj Ali Fe and V do not affect this determination; Cu lowers the accuracy; and W in a 100:1 ratio to Mo has no effect. I does present an odor problem; II has no odor.. Orig. art. has: 2 tables, 5 figures and 6 formulas*' ASSOCIATION: Moskovskiy gosndarstvenny*y universitet, im. M. V. Lomovosova, (Moscow State University) SUBMITTEDs 27jun63 DATE ACQ: 31Mar64 ENCL: 03 SUB CODE: CH NR REF SOV: 006 OTHERV.004 Card 3/6 ACCEssiox Has AP4019609 INCLDSUMI 01 .3 H0441 f ig.I Determining the composition of the compound of Mo(V) with 1-mercaptoproplonic acid (1),,' p-phenotidide-l-me'rcaptoproplonic acid (2) a~d compounds of Mo(VI) with 1-marcaptoproplonic acid ~3) and p~-phenettdlde mercaptoproplonio acid (4) Card 4/6 .ACCESSION MRs AP4019509 fig. 2 Relationship of IgK to Ig [Rjin extraction of diphenylguanidinium and benzy1thiur- onium salts of mol)b'denum compounds with 1-mercapto-propionic acid (1-4) and with thioglycolic acid (5, 6) 1-diphenylguanidinium salt of Mo, (V); 2-benzylthiuronium salt of Mo (V); 3-diphenylguanidinium eUt of Mo (VI); 4-benzy1thiuronium salt of Mo (VI); 6-diphenyl- guanidinium s~xlt of Mo (V); 6-dipheny1guanidinium nalt of Mo, M) Card 5/6 ACCESSION NRs AP4010509 jwu)svas.03 t gel. fig. 3 Calibrated graphs I-determinatiOn of molybdenum pphonetidide-i-mercaptopropionic acid (360milli- microns); 2-5. determination of molybdenum 1-morcaptopropionic acid: 2-350, 3-365, 4-380, 5-430 millimicrons Card 616 NAYU) A.G., Cand Yed -c-', -- (diss) I'linle of %plQA4l'lu infection in the all-) c ;1-.9c of schizophr~,nj.a.ll Kishinev, 1958, 15 PP (Kishinev State 4-'..!ed Inst) 250 copies (KL, 29-58, 137) - 123 - MOLOIGIOV2 A.N.; NAKU2 A.G. [Nacu, A.G.) --------- Rheumatic amentia, Zdravookhranenie 2 no-4:14-18 Jl-As, 159. (MIRA A: 6) 1. Iz kafedry psikhiatrii (zav. - prof. A.N.Holokhov) Kishinevskogo meditsinsko o instituta. SOMATIC FEVER) (MENTAL ILLNESS) NAKU, 102ristodor [Naku, C. I., Inzh. (Rwiumskaya Narodnava Reapublika) i Corrosion of the alloyed digester shpll and methods for its control. Bum. prom. [38] no.6:16-18 Je 163. (MM 1617) (Autoclaves-POorrosion) (Woodpalp industry-Equipment and supplies) NAKU) N.F.; SHO'YKHET, R.N. I-- Nonspecific pyelonephritis in renal tuberculosis. Zdravookhra- nenie 6 no.507-40 S-0163 WIRA 16t12) 1. Iz urologicheskoy klinili (zav. - doktor med. nauk S.D. Goligorskiy) Kishinevskogo meditsinskogo institutao NAKU, N.F. Three cases of conser7ative surgery in secondary renal hemorrhages. T Irudy Kish. gos. med. inst. 24:234-236 264 (MIRA 18tl) 1. Urologicheskays, klinika Kishinevokogo gosudarstvennogo medi- tsinskogo instituta. KMCIKU, K.; MIHO, K.; ~4LK~~Tj, M. 5 cases of keratoacanthoma. Bul,Univ,Shtet.Tirane no.3/4t74-80 163- 1. Klinika e Demato-venerollogjise (Slief Doc. K. Kercikm), Universitetit Sliteteror te Tiranos. KERCIKU, K.; HAKUCI, M. Results of the treatment of psoriasis with aminopterin. Bul. univ. shtet. Tirane [14jek] 2:72-75 '63. 1. Katedra e dermato-venerologjise (Shef Doc. K.Kereiku) Uni- versitetit Shteteror te Tiranes. KERCIKUP K.; NAKUCI, M. - Results of the treatment of psoriasis with wriinopterin. Bul. univ. shtet. Tirane [Mjek) 2:72-75 163. 1. Katedra e denaato-venerologjise. Universitetit Shteteror te Tir--nes.(shef doe. K. Kerciku). BAKULI, V.N., kando te".n. nauk- ZAKHARENKO, I.F., Imnd. tekhn. nauk; BABIGH, M,M*, kand, takim. naukl. iNAKUL,-' I''.S., kaM. tekhn. nauk; DIJBITS&AYA, I.S., kand. tekhn. nai~c Haxd-alloy taps. Mashinostroitell no.12:15-16 D 165. (MIRA M12) NAKUrNYY, D.D., ENG. Electric Power Plants - Moscow Activities of inventors and rationalizers of the Yoscow Regional Power System Administration. Rab. energ., 1., No. 2j, 1951. 2 9. Monthl List of Russian Accessions, Library of Congress) October 1951, Uncl. AUTHOR: Nakutnyy, D.D., Engineer SOV-91-58-11-10120 TITLE; The CentralizeT-S4ply of Hydrogen to Generators (Tsentral- izovannoye snabzheniye vodorodom generatorov) PERIODICALs Ehergetik, 1958', Nr 11, pp 21-22 (USSR) ABSTRACT: In order to improve the exploitation of the hydrogen cool- ing of electric machines, Engineers G.D. Vullman and V.S. Ivanov, of the Mosenergo TETejhave realised a new system for the centralized supply of hydrogen to the generators of power-stations. This consiste4of installing a recept- acle with a capacity of 10 cutiof hydrogen at a pressure of 10 atm. near the machine room. Next to the receplable, a building with a gas ramp for discharging the hydrogen balloons into the receptacle was erected. Gas pipes con- Card 1/2 nected the receptacle with each generator. -A detailed The Centralized Supply of Hydrogen to Generators SOV-91-56-11-10/20 description is given. This system has proved to be satis- factory. Engineer S.A. Mandrykin also took part in the design. There are 2 diagrams. Card 2/2 1. Generators--Equipment 2. Hydrogen--Applications NAKUTNIY.,-D.h.,-inzh. Damage of disconnecting devices installed between the outlets and the cable assembly of the generator. Energetik 9 no.6: 16-17 Je 161,, (MIRA 16:7) (Electric power distribution) (Riectric owitchgear) V- Ya *1141q-N;ZON -Vw/h~gineerinez Theory of elasticity Ord IA Pub. 22 7/44 Authors Nalanzon, V. Ya. Title On a change:of a boundary condition of the flat problem in the theory of elasticity 27-29, Sep 1., 1954 Periodical Dok,,,AN L&~R 98A Ali Ot.rdct -1: The so-called flat (two-dimensional) problem of the theory of elasticity, solution of whi .Ch usually has been reduced to finding two functions satisfying the boundary condition of Muskhelishvili, can be solved by a slight change in the boundary condition., namely., by expressing the variable.unlmowns in parametric forms of periodic functions-, Graphs-, Institution Presented tor :,.Academician Muskhelishvili, June.1, 19% NALBODW I-e~ B., inzh., nauchnyy sotrudnik 1 11 Mechanization of the removal. of rubbish from construction. Zhi-I.-kom. khoz. 11 no.12:15-16 D 161. (MIRA 16:.U) 1. LerdngradskAy nauchno-issledovatel'skiy institut, Akadendi komnunallnogo 1zhozyuyatva. LANTSOV, V.A., kand.tekhn.nauk; NALBJkNDOV,.B.A,, inzh. Using chain save in the major repair of buildings. Stroi.i dor. mash. 7 no.lot22-23 0 162. OURA 15:11) (Chain save) (Apartment houses--Yaintenance and repair) -- -- NALBANDOV$-B.,t-inzh. I- ~- N Over-all mechanization of the removal of construction rubbish. Stroitell 8 no.5:28, 3 of cover My 162. (MIM 15:7) (Refuse and refuse diopooal) (&Mding) TIALBAI E2~~~ ~ turly of the mwating vrr~,Pgs Of rACHMS '13 3 1 1 :_i . 6 v the. mnjar repair of buildino. N3im~. trudi ~FT~4 no. IA~P-^-105 162. fl-UP", -';17; XU.BANMV, G. Z. Application of secondary methods by means of Intensive water flooding of oil zanda at the Krannokamak oil field. Neft.khoz. 32 no.8:31-32 Ag 154. (MLRA 7:8) (Krasnokamsk--Oll field flooding) (Oil field flooding-- Krasnokamsk) 11118-66 ACC NRt AP6007728 SOURCE CODE: UR/6413/66/000/003/0155/01 --1 and AUTHORS. Mayevskiy, A* G*;, -Nalb ovp.,V,~Ae~ ORG: none TlTLE: Caterpillar drive for heavy machines. Class 84, No. 178753 SOURCE: Izobreteniya) promyshlemyye obraztsy, tovarnyye znaki) no, 3,, 1966) 155 'TOPIC TAGS: tracked vehicle, ve~iole component ABSTRACT: This Author Certificate presents a caterpillar drive for heavy machines., particularly excavators, including a lower frame and caterpillar carriages. To improve maneuverability and to decrease power requirements during turning, the lower frame is equipped with, a pivot, plate which can rotate in the horizontal direction and which is connected with the carriages so that it can operate vertically with the help of a lifting device (see Fig, 1)# As an additional foaturo, the lifting devices (hydraulic cylinders) are rigidly connected to the lower frame and are pinned to the 2, Fig. 'a 1 1 lower frame; 2 2 carriages; 3 - pivot plate; 4 - raising mechanism. UDCs Gird 1L2 621-879.48t629.11.012.57 ITALRANDYAN, A.A. Eliminating the formation of ~ce locks in railroad tank cars transporting liquefied gases. Gaz. prom. 4 no.7:28 JI 159. (MRA 12:10) (Liquefiod gasoo--Tranaportation) ' I"J. Lasidleav mW tin-frito opaque $lam (or well Ilk* matt nialtilkil.- A. A, 4NAtNAWfWAw4S&k X#Tjw. 8. Nit. 1, 19, 19811 Muir anti tolouresi iqhujue 1114iiev are virry SUIIAIjk Pit ltleartt. with Sno, 64 all f1wifirt. &A"Ity tit III OW11 So Cphi. necesititatt% the lite of sultalituipt, s, g, Sit, 11, Ce. As. F and tr elidi. In 1%47 it Ruto-tark rewstirb In-lituto ,dovirl,-lied the f,41,mmil otl4olve fkatift for III(,#, etc. MA& tit Moscow and tither tiny* (in p V.1AW*-I,ikW C I If.Zr In thrw 11vitand I arroitout 111MI I,Y thrdl, It CION . F it. Colemanito (C4,11.0"All o tit hytitot-irvicito 4(a.Sigiltoo,61110). An socFeaw of 41kiiii content bryontl 3 mol. and of 11,0% obirve 04 wealcruis the opaclAcatkot and cauws erasing. 10 obtam tire nt%ediiary Icl.^4 and tit lower the in p. a or"All amount tit TOO. which Us 4 high rrfriictive Index 12.3- 2 0). i_4 added to the, glass. Up to 114 TKI, in the fill lowrts thr, m, p. of the AlAte, by 2W C. MWI iRCMAO's the Alosi; by We ; to 6,14fition, TIO. Intea-Allev the I import. a pleavict isarm trino 44) the KtAse. As a substitute for C Is. IV urml (If"Wi0j. The opacifyitirl cil4vt of this in Immd on the co-existence 11 2 ph&" having diffmat refractivi; ta4scirs and solubilities. The tipacificaticin Increases with increasing difference licticti-it the indices of the c, ond gtair. The indictit tit normal glazes very twtwvvn 1-3 anti 1 -6. whereas M, 1 '40 'it I has so In.lex of 1-83, SnO it 204 anti thAt -1 Sb,O, Is 2 6. Zen During coating, ASO relrat-i 1K), with an Itolex of 24 (1.#,. higher than that of SnOj. With ;J;, anti &0 dixectl" In the glitzo at the fusion temp. but separate out agaia during vociling. ~nvnbrr merit of ZrSiQ, is He low coett. of thermal expansion. rxpts. have shown that tho frill 1 14 e@ at* critisiderably oil ~SujK1".to raw ones of the "tit! COM The a4ditim of 53T Zoo and 10-15% YJ, Ann A Simultaneous MIuction Tsios llnplov~ the Kkvts anti 0 h I, addiiij.,ticification., T e best opscif)mp vilect tia achieved when 8-40% of Zff"'Uj toth"frit. nils-10% to the. lwttb~ Tho to p. of lite Ala" I* WSW-I.fX)OI C., the owd -1 linear thermal 0 asItoo of its eq.timum comp. 13 3.37 Y 1". the whilimem tin - anti the glims At stubt.1tutt,' 7& for lilt clids., cilcrrZ~;ite. hydn~ borarst 1 .1 tit were used. Z^iO,. owinit tit its chem. inertness. is not #iMble'loc I lit cotoor shades: thew frits were theretwe used without Zr%10# with on incrvas" coat I of 110 Thiv rnlucrit the tit It. of Irils it- I.W01- 1,0501 C. And i,f rlitars 1 40-- E, file latter W a low viscotaty on.1 a good gl,.o. on the bosi:i of lite at~ve frits, by the addition to the mill botch tit pigments and fn-glAZV C-1101111% IL palette of glazes of var-ious Wit colotiris was olittained. The tit p, was 940"ANX)l C.. the coed. of linear thermal exiiiiisiun 4-77 v 10-4. and gloss 71r~ F Prelimimiry expts. have shown that NalIUVO can he used as C~emical Abst. Vol. 48 No- 6 .Mar. 25t 1954 Glass, Clay Products, Refractories, and Enameled Metals Firing of N1va;j1b~1tVpAqug AlrlijWlum 214 a. 0v 4. Q. Tu an. and A. A. yan. Steklo i Kera-its. 10, No-. T;-rS:W (19 -11rolonged hording at I haprovcs the surface and luster of boro-Zr glaze, but opacity and whiteness are Impaired. Prolonged holding during cooling Impairs the surface A1ld-CJjUS1:S CTyOtJ;.-.. OptinJU111. heat Cycle Includes holding at 1000* for OX-1 hr. and cooling in a short period (up to I hr.). Microscopic study revenla that opacity is caused by Zr, accumulation of fine-grained needle-like crystals of unknown origin, and quartz. H. Z. Kainich --T,- .T7 - -. - -. -.-- - - --- - -- - - --- - - -- - --- ---- - -- -- -- - - - - - --- -- - - -- - ---- - -- -- - - - - - - - --- - Dissertation: "Investip.ation of the rcssitility of lmprovirE~. the ',unlity of :FuLdlule, , Cpaq e Zirconiw-, Glaze." Can6 Tech -ci, Yosco," of Lenin EQron-Gont,aininU u - - - - ChemicotechnoloEical Inst ij-.~cni D. i. ll,'en6eleyev, 7 Jim 54. Vecherrryay-a '.0skva, I'OE:Cow., 27 MaY 54. SO: "SUIP-81+1 26 Nov 1954 a 0 0 0 o 0 o o o o o 0 o * 0 0 0 * * * * ' 0 03 1 1 1 1 a I a 037A -A 11-C-11 It I C I U 11 m is $6 it Is Is JI a A As a j I 90 4 00 - -- , - O!OCIIjill A.* 0 ;oo I fr. 1, The owAwJm of the uppw WWt m4 ON son ,,A. Naillawya "040 tu OcIrl 8i I 1 W3 go , - a SerjAm'. 4. 7 t ~( ctiI 6d w j; u 4 N to widowd a detanistfun 61, 1 1 dUnkddwd br I Or 0 Atum (Ormd dsctlim " bdavW in on Al VUW AM that dm UPP T1 of ale ps. not of the Surliam ressure dr,, ction of f d =W 00 A 0' un " a tte p p&ws tbrwgb is mia. and rimes shmOv III pmmnv Undt. I 00 4 r4 1 i : 1 B l l 9 4 0 4 0 0 0 0 0 a 0 0 0 a 0 V U U U 4 ft U son $,1 0084140 --A- I's- % - I , . a -&- I ------- - 0 ice Fill. nw I is ItAr Is a lon .00 Ay, MOO jwr it =00 GO 0 no 000 X60 we* ~ k IWO& 00 0 101b u n -0 A I- Al A I I ad 0 o w 1 mr so s a 4 3 2 IF -- I dn", :fe 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 10 0 0 0 0 0 0 * 0 0 G G - G 0 a 0 0 0 0 0 0 0 a 0 I IN 11 u u SO it 1 1) IN It IS a IN 8 i_ 4_4 A,-,, 'L -14 A C_jk~A_j a 0 1 L JL--JL P. 4 L-1 At IL -&-I- 00 Of dw A. KO"hwove snd phpik. Z. 4, 7w-m 1 Tho activs. tw y Is CAW. for 11W "wo- It + of -oil + 0 9 w OS , a. compared with setnenov-, VUILW 0, 9 (d . 0 0 0 00 w 0 0 S L a AIIALLUOIGICAL 1.111111AU41 CtASSWICA111001 NJ -4 - G 4 -b U-S Jw__* ou-41--w-d-co -,a I , 'i" -I I *00 ~00 .00 .00 ago =00 0 :a: 0 Co 0 4900 x0o woo =00 too* 1100 log ZA Aft I S I Od 0 0 0 1 Ir, 90, 9 a 4 3 1 1 U IS Al 10 AS' , ; ; t, &' t', ; M' K ',tK a Ccpsa 1'9~~nl '114 0 0 g *1* 0 0 0 0 0 0 0 0 0 41 0 g 0 0 0 41 0 0 0 0 0 0 004 000 0 0 P, 01 "A U, I _JII A 64 a --11 - ll 1 s O 4 i o + .00 so, A. Ndhoodpa. Ads a 27= I N)* the "6cti= a4 the dieckM ki an so thm OAM ow. The 0 ' 0 0 -b3f tbw dbcbwge catums an upiaoiim, ' se l ad sm at ,, temp. *" bdow 3D0 a twp~. of ks Men MOO. Tu Ckda kmb is ee l s 7U --Wk ftuA be pmvioWy acdwMaS & win bek tbm reafts can be oht= V. H. RatkOLAM 013 : goo 0, see w. I :00 M N not not -Alf.SLA ~VAILIMII~CAL IWINATM4CLASUFKAT a** V U of 1111464 mv all 41401041 6161114waft Ili ;r 'N v R-W -I Mai 5 AT 00 01; 0 ;G 0 so 000 so 0 a goo 000 see 0 Of I x It a U w " 14 1/ a a a )d A A 0 x x 11 u 13 w 4 16 11 x A 61 Q u 0AJDO A A p It AL I a L A AL A_ FL A-1- --JL M? U t 0 A Ad" 7 Yo 0 Low" betiggen hydWn Ud o so 7 R. A. Bimn aml A Nalbowls- Ada PhysiOXAS'N. 5--see c- .4. 31 41"u, S. 0. 43 nobw NI. W. it. SOO =0* 0 13 0 ass 01 ]41 goo -0 0 *ITALLL106KAL L111MAI L41 CtASPFKAIPCr koo 1914.1 It avv oat I I I Fi- - U 8w 00 t a C, it 4 1 IIA N it 91 3 S 0 i~ at 0 1 0 0 * 0 0 0 0 0 * 0 111 0 * 0 o 0 0 0 * 0 0 0 o 0 0 00 ~00 0 0 0 00000000 *0 :10"0 0 4p q 0 4 o 0 o * 0 0 060 so t$ k to pI.-U f, 11 11 =U.1111! ", -a-? 91411 ~ -- 00 -00 00 A 00 000 1.00 09 -00 go Lmw Mmk at r*kgm betwom hyttrope -00 0 0-znm- A. Boos md-A- 0 rX~4WMAX.-(Ac?A 190 Phyalmomm. U-P-8s., lim -W).-Ths .00 anal sot 1611011 FA n0i y W Probaim, of) A;'tb=; ;;;K7kI-I&thamy Of zoo K"aw ad in Whoe"PIS0001dwn p In mrsim to tm Sam= the tbaty =1 PnNPM Of A. in acemd. 7 ZOO MUD AM &VvWz (A., 1931, In both casm p ~k ibe p&rU&I pr,,m, Of 14 + rem-ud show* ib, .1.4". woo ""On P And thlP % OMPOWdon -f A-frm if -0 1'. L Soo use !!0 0 tie 0 SL A 04ETALLLHMICAL LMNATLMRI CLASWICATION t1so N1 JD~ - -- -- -- glow 61.151 1. roe 148400 Mir o.W 009 433jaialt flim 4K AT so 0 -Y j A i v rij b it v i v m i a a 5 i7r- u 'a a, 11, MAQ 4 1 o' 0 so 0 0 0 0 0 0 : 46 0 0 0 0 40 10 0 0000400*0000*009069664 0 00 0*000040000.0000000*00*4000000000004;00*01 0 0 41 to 0 00 see 04o0 a oo -110000000*00040000 0 0 0 0 ,W~O, 00 , , 1, to Is x it a I list to 90111113tS441 Is If is Is x it a a U IS so A % W Slows) UU met* a I A, 1. - N . l, I - I J, -1 1-1 1 :O'A III, A I - I ~2 _Y 1-1. .7 A~ PA N Rt U I A I g S J- "*iolow I'S tle a A C 0. II-IIIIS A- -4 0 0 COL--- 00 0 Lawor limit of CM ceactim of hydMen witk o -00 :0 tp A. ifiron aod A. Nalbandyan. J. 11bys. C". . S. -W V N, k.) 9. lots Ut given for the Watt .00 0 -itum -4 ignition of Hl-4)i mix1p. in quartz and 11yrri, v~l. with wA without the addn. of A at 4K5 5-#U*. in If 11yrrs the Inell lias has no efitcl on The lower limit. but In quarl It, t he lower limit Is made lawer in artmitlomm wit b I + couxt. For vatims tttixt,., pffs.ih) co 0 (I -rolo- W-0.95 0 (whe" -j 14 the mol. Ira- 00 111 '40, th It and 0 Atoms are a-uni"t to N - U hawr as IM-livr ctntels for the frarlimi. F. 11, k, too *0 see 00 -Oo 0 d goo Als-ILA OCTALLUNCKAL LITtNATWl CLASUPKATICOO A it- ~-r. U00 too 044" 11"41114 42.1n, It ISJ40i iiiiii ciW Q~; iii 0 _T'_ j AV a 3 1 9 1- __ U : Al 151,* ; r 1~ nT I An I t 0 0 0 a I It At f Or 0 * 111 0* 0, 0 0 o o * 0 o 0 o 0, 0 0 0 0:0 0 0 4 0 0 4 , 0 0 0 0 0 0 0 0 0 0 01 0 : 0 o; 0 0 0 0 0 0 0 4 0 0 0 0 0 0 0 0 0 010 0 0 0 0 0 0 0 0 0 & 0 0 4 o 4 o o GIA 0 006 a 0 0 a a_ 0 0- 0 00 0 0 0 a 0 0 0 0 0 0 0 00 0 -J,_14 1 10 1 V I M a 9P_U+J-1 J_ a Mtochemical oxidation of drogen. it -00 Ff 4XI ; ,valban I W (IM97(in English).-the vclmity of the phol,whem. -00 oxidation of It at pressures of 1-311 unn. irradiAted by light of 1300-IM A. is givrn by u - (rJ/0JI61,41 .40 it C-V) 11 - (-II1,134pd) (J. 401j.fmfl, w1wre intensity of illuminatilm, 0 - probdInlits, of chain -0 rupture. d - diam. and I - length of rvactiun vrs,-I, .4 /' - apd. k - abustrption coeff. for 0, 4 - % (3 1,, 14 )4), x 00 8 1,,-.no. of collissionm undergone by 11, before rviletinn with .00 ne. J. (ix). J.(sx) are Bessel functiom of 0 and Its order. The mechanism of the zone birrivition prin-e-i is; v LN + is, - 0' + 0: 0 + Its + bt - Hit) + iM, -any A A 00 su,C); 0 + Ot + (h - Lh + (h; 0 + will VON. Thr Inobability of the reaction 0 + 11 Is III Thr quan. 06 tons YkId Is 2 moll. a U.0 + (h v (JoUnIum Abo'llmil. N * believes that no chains ure r(PrIned, but thar. NMI exited and normal atorms act as activ,- centerm. F. It. Rathmann A ze 0 U Rt a.&, ft. C, 6-A '%v% r I& A #11CUU1161CAL LITI44TUNI CL&SAIFICATION Aid 11441 #)will slo"I s 14110411 Nit 0" oat MW aw a., lit 7 - 0 0 - v I U 9 AV go M sIr r 11- M t S N 04 0 0 4 1 If 61 9 a 0 : b .61 WOKK matt 410 14 ang: 0 0 0 0 0 0 00 *1& 0 0 0 0 0 0 0 0 10-- all Oll 11 111 t O 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0, g -A..? 2 -A- A.-U. rim I L cc, t " m AS is 0 m 0 a I _d_j r 10 0 At u it a 0 0 &-A- 0 0 0 go # I St of cwbn dWO&s. A. D. P, see ck". (U. S. s. U.) 14, kriSdiated by fight fi 3% j R =00 -31 7 f VIMIll t. C , + 1 A- cf. s Ls depo4ted do the waUs wid the 47 so a m 0 prtxwe In the madiz vrswl decreaw. 0 atom as well 00 C as activc eta- as The '18, 1. IfM f CS i + i OO on o on reg 1 Sm. tuat 1 S, 1111911" klwvr lesvilm. on IrtmadiAllon. V. If. 1"1 x*4 boo 1::l lid.fL. slIALLUAGICAL 1.11INATWIl CLAISIPICAVION 41- Sir. 141,43 it Gh q4t U SS AV 0 S; 6 4, ft ff IS C9 a it 9 4 An I I a 14 a IS IN I Af III I La In f I ~ a a 3 a d(lo, 1 0 0 0 0 # 0 4 0 0 0 0 0 0 : o 0 Is * 0 0 0 0 N 0 * to a 0 0 e 0 0 0 0 0 t Goo 0 40 6 0 0 0 0 6 0 0 0 fe 0 0 : : Srl OF uhrtam in MUTS' womok. & 2=1ndignitto ad SK" Jan (C-Mpl. rend. A"d. Sci. Ir.Rj,S" 1041. U. I fill 14,4), 1114. Il. In Aw I Pit itY fit the surlAip rrmtuin malit-4 irty rAllhi filling ne,~ he 1-met lonlit 4,1 9 situr Ignition Is jjjhII,jj,l 1.y fill) ntane,,Il,t ignitin" in tho AR %r%wl ti~j 1, I Ira*" I Willi incrF,4511IR tetill, Irsifn 32 Illin. at A714' 1., 17 I Ill- 1101111,01% 1101 all indn' lion 1.4.11M will, It .1m wa., "MI In. ormilm If,,, I.... 11 ill' 11-4.1,lg , .111111 al 011161 6.11111 1 It,- ~h"Jjjje.. ,I If,, tioll litin JjfVVr.Ijt tile U111%.j 111111t If MALBANDYAN, A. B. - ------ "The Kinetics of Hydrogen Oxidation in the Regton of Low-Temperature IgAiticn, I. Dependence of Induction Period on Pressure and Temperature, II. Influence of ,11 Admixtures Acta. Phys., No. 6, 19441, tPl*;22, NOW I'll jet *4401 be at* A f- L-1 04 f-00 :ra 0 A 00 The effect of a AC "ifeco on the expl"ion limite of a cf. C..J. J7. 411411 Ile stiuly ig file vilthrdots of 11-0 nilits. III As ve-eb is conflatiM, The luwa expit"W limit was detd. 0 In Ilyrr% vm4els cents. As wims a( varimi %is", This i, :0 1 nit 6 higher when the wire It prer"t and is ithifted by 11IM104114 If &91ft-11 tGWArd higher tempst.g $be ithill 11 '09 o: IrrAter the lgfmtrr the wire diam, The great effect of As .00 j 1114M." of .111011 amt I% altdNited III 1hr high prIxImbility W A. 1ivf.vIIl,.W-"I the fil,.141 %]lofmv. :0 If "'1199 0 :0 00 .09 '00 1:0 0 If !,ego OOA Ogi~q :.I 4o;f I 1J.- -IAI Vo 0 An 1 1 a 41 0 3 0 as o a 0 0 a 0 a oil It .0 *0 Ve 0 0 a 0 0 411 0 0 0 0 0 0 0 0 9 0 0 111 0 0 0 0 0 0 0 0 0 0 0 0 0 0 ei The kinetics of hyd'RE14 olldsuon in the region ot tow- fel""Agluff IgnItlM A. Dependence of fUdugt on P on. pressure Rua temperature. 4. 13, Nall~lnfivall. AcIaPh vicachh". U.R.R.S. 10, 493-W09i'l) (its Lngli.411). ~1193cYon the mechAnIsin of H oxidalinn %siggested by Lewis and Elbe (Combiwion P14mes and PzpInsion of Gciies. CambrIdge, IW4) and on Seotenov ,s * met hod of partial stationary conen. (Chemical Kinclks and Chnits Rfactidns; C.A. 29. 17064), a formula for the dclicudenre of the Induction pcr!cKI upon-prtsmirc: and tcnip. inside the peninsula 61 low-tenip. Ignition of 2111 + 03 was derived. . Expt. shows this forntida. to be well satisfied an a mlbi the n? the ViOut 23,OM Col. to the activation energy of cha n-btanching reaction It + 01 - Off + 0, which ultimately dets. the over-all rcoetion rate as well aq the tetnp.dependenczttfttictippcrliinit. Therntcoflloxifla- tion was Investigated as a function of the contpn. I)[ the "c milt. I]Npt. and thenry aft shown to lie I W I I 407- 7. hirreement, It. Effect of admixtures. 16fd 2 The effect of water and 13 on the cxpIrAInn limits nnd the kinetics of It oxidation with'In the region of low-temp. Ignition were Investigated. . 11,0 vapor bt shown to Imi-cr the upper limit -one to displace the Ignition Peninsula the Upper expirsinn thillit shifthli the region of -,elf- towards higher temps. HiOlsftittliersitoutitonctoiitlic ignition towards higher IC 'he kinetics of; upper limit as an Inert gas, jtq efficiency being six tillics as 2143 + 02 Ignition. III .11frast. to Ilo'!'Ct"Mols. exert a! large as that of It. and to have no cflcct on the tenip. tie- direct actian on the branching reaction H , 0,-011+1 ndence (it (fie parameter ip chararteri4sr, the veleycity of Os rtsidting In chnnge.1 III the tem - dence of ip.; r, Oxidation. Tracci of 11111 the 11-0 mixt. greatly lowei, kjttin It. Slagle 111111" 1)% ilia "M ilu njon)SPAIII it N11 Jill Jim is A if -W-64-41,C& A 11- L-11 I IF Is A j L 1. 'AL a - F 2 a 'I I . W T I L-1 --- l- M 14 cc OR _u Io A -11 0 0 Jut 0 A ost 0 4-0 f1pulot to " J O IMP S V Pirmurs limit of an explMve .0 0 mixture of SH, + td f& an Fe vMel its W awe Od in .00 0 a Sios Vaud. on other hand. the lower lormure WWt is &A Fw ve-d Is > in W, ThU -990% that The fictive cestres; of the *0 :0 a -tion viorst cattily on met&llbc thag on nowr,&%ft =00 Md-411111, ThO temp.-d"ilm" Of the IQ"* Uttaft U glvn by a P41118-7I Ar 14 !- C. R, It. . 000 40. r4lo 00 000 4111ALLOWAIL LITIMAIL1011 CLAISIFICATICII At. -I L A D u t. to, 03 too tio 1, it ot a u n It n it it a 0 o o 0 e 0 0 0 0 0 0 o 0 o 0 4 0 0 0 0 0 0 0 0,01 0 0 0 0 0 41 0 0 0 roe 00 .4,11% s" a., 'to too cc mLo n iiios 4,14 4 9 0 010 0 0 0 0 0 0 0 0 0 0 0 0 0 0 41 a *1 0 0 0 411 0 0 111 A a C a t F a I a L I#- r--2 A -1 V 1 11 1-1 M ft cc up it W, 1 0 S I -0 0 K"M Lt IkMeWft 41itIOR he lain at lowlanywature 00 A 1,00 0 'I V rh I . A. Nalbandjact (Acid x MAN, 11-R.S.S., 1943. W, 31-11).-Fxperlmentat data for the kinetics of oxidaticia of He itt a Rumixtit vessel wathed with It 00 oil solutioll of XCI wW In a stainless steel vessel do not Indicate any 00 of Matetion rate on the conditit-a of the vessel walls. de .,. of ilia lower limiting pressure In the tamer cam is Occounted (orbyansuming tfieprobabilltyaldestruction of the active centres an the walls of a vessel covered with it layer of KCI to be 5 =0 a the probability of destruction on clean walls. (Cf. A.. 1943. 1. 1 dg.) S. It W 0 2 ve 0 z Ize .0 =9j : &so 00 U MITILLMICAL UYINATURI CLAISIO'KAMN tt** 0 see it Oil U 91 AT W) All,, r, it OW of "limit pit% Is eg 14to A I 0 0 0 0 0 O's 0 0 0 0 0 0 * 0 0 a 0 a 0 a CO 0 16~044 0 0 0 0 0.0 0 0 0 0 0 * 0 0 * 0 0 0 a 0 O,0 0 oi~ W10 a I a o'$ *09 P DOC I t%C% A 00,4 a of 019111"" systems. CorDpf,rf%d,drA4,Mf. 11 Ou"r-5-V5 46, 107-00946); Poklay A "d. t%'4xb S.S.S.R. 9 46, II3-i6(IQ*).--Th* specilic effect d dw vulume of 00S the asegm or traparom pgoducts of an explosive reaction, go the rats of detonation tras favestipted. A scries of **JI caprritnents were patormed will; rub d I aptcak" a-P,! tuns which had oduos in adilsor the NAW OW, final stases.- ~ (1) rA'XCI(Z+ P,.%. - 3.GXCJ + 9.511.0 + 4ZOSA. and (2) KCXX + 2M - KCI + A40o. Time o Of exploolvit corrsito of the two "PAIM " mixtures - to doid. by nuasuring the compremlons cl a lead column Ob- bdoed by employing a modilled Ifess method artil a No. 8 CAPSUIV detonator, In 3 nins using the VAIX- lure XCA + 11c0i the diamcfer of charge, wt. of Aup in g.., mud comfir" al! the lead Mumn In into. was, 0060 resp,: 40. Wt 0; M 240 0 7 * and 77.5, 49). 15.1. By 8: 8 the $plain KEK ~ i4 I.; it. am diameters and 400-11 weights of eJarp am above rod & mixturc density of 0.96 JLLJ S./cc. " emp" with 044 Above, the "opective cam- orc2sions of the kad colutaw were 6,40. 10.73, AM 21 A% 006 The KaO4 am Al juixturs, Fives a Y"Ivvly repo". Wltb 60 g. ~d~tbo ' sadem" tolsture ii-O --a ......... ..... af-KCX). sta At a ccutpreacim d I&W im. 6 obtaicted go compared wit b IfAY Mut. prodate-4. by LU wxw qm AtIff td the MIRAUSO KC10o AM PM, Irtick 0" 40 1- 4 ma pradmu. Kn9wimento to determine Um = oftbodetmadmaAdlWitelocity ei carrit4otatia tubes of diffoat dkmtftrs. In the case of bAk Paless mix- turcs, the Moulin wsa stable wben tub" ter than III an. In diam. vat used. For Ow 9 and FCSI inixt. the detacation YtWdtY stessured by the 11-utricht melbod In a tube X1 tom, ki diam, was I ITO m4s it.. In a tube 27 tam. Is diam., 1270 tn.jw~; for the K(30j and Al mixt. the 4efoooJoa vtkcity in a tube 21 Mo. In dism. was 1300 m./oce, and In a tube 40 mus. is diaxi., 1370 M-/soc. Rapts.to-ktatia voi.of pocamexploswo prod- uctsforthe KCKN ~x4 Al systernwere maids to a Postal bomb In which a premed liad w4de detowar was oW,Akb wea, ad ad alecUlcully. The gaftous val. was 1=4 to be In. s1guificant, sW wati Jo4A4 to c== 46% carboo-4at"is cocapas. Howevet. at= s, Iable put of the es- plosim work of boCs gask=tcm k expended I" a temp. much higher than dic crit for KCIt it follows dot substance sbmW bo! In the vapor state during a considerable portion of the explaDion process and consequendy believe Me 4 AlLs. Hyto'llds vat. of vapor b -11 cocipared to that given off by tho usual cxpWv". Allattcutputopro. duce stable detonation in systems ykiding scitliti, gas am vapors C!rn ~! bigb tempo were futile. Ph Y ASA.ILA ARIALLWGXAL UTUATURE CLAMPICATIN NOWAY MOV9 M&? CRT 999 as"" am OtffT Lis z 1 F q - I - -P a I ff 0, ; 00 It V Of a 9t 09 1! - PC It K~00 A T 1A I I bd 0 4 0 0 0 0 0 6 0 0 0 4 0 0 0 0 :119 .6 0 610 6 0 6 0 0 0 0 0 0 411 0 0 0 0 2 0-0-0-0 0 010 o 0 O-C 009006 0 0 0 .1, 0 0 0010-4-0 a- 0 0 0 0 0 0 0 0 0 0 0 0 00 .00 .00 "of .00 800 =so 4*0 too Coo ago 111949 Ifo* 0 0 0 ips st 0 of 0 0 goo 0 0 0 . . 1 . U U s 14 It a 0 a 41 a At it dZ 0 t ~-j I oCK %tilt 1.4 #40#90t.tt 1.041 .1411i_ Expetimectut deteltuaination at the probability of the di f i 90 sappearaws, o fict ve centers. A.-U.-NallaudyAll 0 : Fend. acdd. sti. I klady w1kad. so MA SAS.H. 47. 208 t)(19151-The C4 p 0 Of nk-fill wife Into glatim, or quarts vi-sorls inafitirdly lite lowvr ituitloil Until of conitku.111)k filkliti ,3j1c-/S z 1/a , rlw vitillefis"i dryckliml by SrIllellow Md. is, :11mul). -1/1"In (d1a) wherf, p lit the lirvilmat, at tht u . : lutirr limit fit cololluololl. it 14 lite 41111111. 44 tile rt.1c e, y 0 lims .1 Illedifilil. of The wile, luill /I a coll4t. tie. l l th l d f tie 0 li ing fill e Icillp., was colli tine or the mist. lit jil, join- (h at 406'. '1 lit lowrr linilt lit lplitholf In 111111. of lit Without a wile was U 911b l"In ; for wire iff distill . . . 0.2 ctn.. 4.20 mm.; 0.1 tin.. 3.80 mm.; (11.015 cm., 1 1 I&C tin 3.10 Mot. it. ( COO Igoe 1:9 0 W10,111fill CLASWCATICK use go -4.1 J.Jnv It[ tonat's Islas,) at Qs I got a I I I j II silill " 4.. m V I U S 41 to is All I 1 0 Rd 0 M 8 '1 W of -3 a a 2 0 1 of or $0 at It a IT it it Is No 0 0 0 6 0 a 0 0 0 0 UALiM'DIJAN.', A. fJ.- Measurement- of tile Cod, ecoru*aruatton 'of t varjou. 1011i`esolryl a der;rminat on 0 t 0 4. 11, Nail aram vital itkut ~. M. Shubia (I V. q.1. U.S.S.R1, hInsrow). J. FAY5. C pol, ZU, tu-ill-oak "'IV III Atl5sialn).--The lowest i R tilt toint pressure p It 11rhiell C Ild) 2 112 + Os can be ig-; nited at.,140* Is 1.05 and 7 mam, -jig ill glass vessels ilki 6.50 alld 131 call. dirun. . I'llament.4 of othcr solids, "' ' raise P. The greatest increabe wro ob i0.1 Cut. Ill dimil. I', served lVith ZnCr3Oj alld grapilitc; both give p tillit. in a vessel tbat, alone, gave p - 0.53 at 490% Au, NV, Ill, and staltilms steel show sinaller incaar,.=-, of p. rIZ rakpil p at 4,10* front 0.04 to 2.3 1, ;laid uIllareated qua -quartz rinsed ivith Ill? rai%.:d p to 1.48. KCI dirt tioLifIcCt ,,p,jat,,6tV I larcause of rapid cv3pat. I'll [uld (above 390 ) Pt it y ell tile colijbilstioll of Ill so tilat p could Iva be measurcd. Frout the expil. P villni-r. the coLff. v of Te- 1 combination of It tatoms at varimt% surfaices, call IK: ca ZIICrt(Ji and graphite have 1 .0 tit AM', Ali Wills at 4-10 *, Pt OAW~ At W. , W Wim), m. 0.0029 at .110*, jultle.1ted (piartz 00M) at -110% quartz Till,`(l Wit 11 11 V 1).(XxrJ nt -110 % and pyrex glalsq washed The pirtsmirrebi tile PrSst'll" of Farrillhite ivai detil. niso sit 5M, Suld .5,58 ; frail, tiles(.- value- the ettergy of netivatirlit of flat- reaoialn if + 02 - 011 + 0 9-1)1-cars to be 17,8") rnl. Froui thp hir; elase 40f tile upper limit of izilitb)II will, telop. lx,t jvecII;jI()* and IV in n glass vessel w.-mlied svith KlIt.61 solo. file ar(i- vation entirgy (if 18,M) cal. 1% computed. All tile nlvovc~ results njorce %%rith Ixtrienov's theory (C.A. 38,