SCIENTIFIC ABSTRACT FR:ZAYTSEV, M.K. TO:ZAYTSEV, L.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001964100026-6
• Release Decision: RIF
• Original Classification: U
• Document Page Count: 99
• Document Creation Date: November 2, 2016
• Sequence Number: 26
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTR

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'~. A ~~fi~, ~v, M.1.
~1SSR,~9athc*n~t~,cs - ~~att:i.ces ~~~/~'~~g ~,~
auAggr~gate of (3rderz:r~,~s of az~ t~bo~.~.an (~rau~~," 2r~. ~". ~aytsev
t(sn~: -~Iata~C Nauk~, trot. ~~", Pdc~ 2(~3), ~~~; 135917
~,~..h.....~ r ,�-.,..
States that A. S. T~Ia:lttsev (~~prder~~d Gxoup.~,'~ Jx Ak -~ai~k SSSr~, S~;r,~P~9z~~r
Vol ~.,~, r7o 6, 1~73-~.~~.2,~ 19?~q) found the neCE~s.Sr~ry at~d suf'fa_oient cc~nditians ghat
~~` ra
an abstractly assign;~ed group lie able to be orderQd; ~~y theory of cardered
~;rc-ups is closely cn~~mected with the tYieoryr of reuolvabl~~ ,groups. ~;stublishQa
a sir-r~le sole fa~.r G. 13~.rkhoff ~ ~. problc~i 192 ~o f3rid all rrar;~.aPamorpYiic
arclerirgs of an Abe1.f.~an group wi.thc~ut tr~rs~.~~n pot~ses ink; ~: f:~.r,itc r~~~mher of
l;eneratrices ~Lattic.s Theory: p 227, 15~1~~). Sut~~~:i.tte~~ ~1 T1�v 52.
i
- ~.
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~l~'1'-1CMY~ ~'I~~r ~llelt;eeyevi~cM; ~'aD~]~AN, L.V,, xe~~.ktox; 7dl'1"~S~V~ Dt,~,~
xeG~viceen~; ~I~L'~~tx~~� ~'e.I-, ra�ts~r; M~YY~~,':"~��~ "~~``~~;
niche~aki, xed~~ktar
~Me~thade of c~~~culatin~ the cler~,nd fiyx dyes and chbxaiaal materi,Rle
by individual rattan mil~.e] Metodil~a godacheta ~otx~shnoat4 v kx~aai-
t~liakh i' l~hia~ichdeldkh ~ate~~ialakh tk~~a Atdelbchnu'kh kh~apc~~ta~
byroaxhnyl~ fat~x~~.k. Pod xea, ~.Q.Fodi~~l,zu~. Moakve,, tae. na~.chno_~
t+~~hn. isadwvo kfl.nietereta~a P~~c~ny~shiejnn,Ykh tavaxav ehf,z~oko~o ~c~t~xe-
(Dyed ~-.xul dysin,p+~-Gotton~
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ST~E'ANI~'S~IY, N.M, ; BR4btT~QVSLYY� L.~', ; i',~i~~, ~~,q. - ,AN'.i"gNOY, U. GE. ,
otv. red, r ;E'8S1Z1~8, A. S. , ~ av. zed� i~d-va; BIID.~KOY~, N.I. ,
t~'ghn. red.
~~Jni,form t;lme a~td pay standards I'or oonatxuatiab, Haoembly, and
r~mpair ope;ratiuanr im 196Qi] ~din~~e Wormy ~, ~aetsenki~ rya wtxai�-
teXinge, ~o,+~ntash~,,pa i re~~antna-at~roitea.1nye rabaty, 1960 g,
Koakva, (~o~a.i~d-vo ].it�~, po atxc-it., arkhit. i stroit.:nateriala~i,
Sbornik 28� ~~ssembliag the k~aist,ing and aanveying equ.ipmr~nt]
~o~ta~h poiluernno-tranepax~tnago oborudpvaniia. X0.2, Nan-~c~ontinuoud
equipment] Obornd0vanie prergvnaga deiatvi~,a. 1960. 186 p.
(x1;8 13:6)
1. 8~,issia 1;1923- U.5.5.8.) Qosuderetvennyy komitet I-o dell~m stroi~-
telsstva. 2. TBentral~noye normativno-iaslndovatel~sls.oy� b;q~uro
xinisterst~v~l stroite' ~stva �lektrOStanttlaiy SSSR (TsNIE- xS~S) (for
Brantkovsk,l.y, Zaytsev).
(W+9-ges) (Cranes, derrioke, etc.)
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~/a~1/~1 /aao,~a1 a/ac~~/o29
.~~ 17/B2a7
AUTi30f~~i: Bale2a.n, S. A. , 13eskov, ~. D. , Zaytsev, L. P..
~I:~LE; Chemical suxface purifico,t,ion of metal. procltic is by the het
rue thod~
PERI4D7:CAL: ReferF~tivnyy zhurnal. Khi~~iya, no. 10y 1961,, 285, abstract
1OVI19~~ (10119r~) ( "/Uah. zap./ I~Ioslc. ~vs. pecl. i.n-ttx i;n.
~rT. ~. T~enina", nO. 1 ~~, 19~7a, ~1 ~-61 }
TEXT: It is pointed out that the ,jet method far purifya.ng metal. surfaces,
which combines the chemical and r~lechanical effects of the taus til, solution,
rE:duce~~ the time necessary to purify metal products to between o;~e-tenth
ar:d on~~-fl.fteenth. Ccambi.ned fat and csustic; nz~acc~seea a~,e recorrmanded f'ar
b~~ass i~nd steel products. CAbstrs.cter's Hate: Complete tr~;xnsl~zt~.on. ~ ~
Caxd 1,/1
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3
# ~~CESSION ~tR: ~"~tA2~909
' of re arts war+g t~a~rated ~;a summa~~.~8 data an the geograpbi.cal eacp~larat9~an of tY-e
P
Caucasus a~~d o;~ ,~th~ Blacit Sea l~it~ by seismi.c,l grav~.metric, and by otheY means.
A five-yea~c pl~~~, o� geol~>gical~~~o~I~ysi.cal~geac:haai~a~. exploration ha,s bE3en dralfi.ed.
~t cansistos of 1~ ~ap~.cs;~ names of 'the pntenti~~1`~ ~.nvesti~ators~ and c;omp]~etian
dates. Qn~s of t~~e~,ma~n assignments is the rirai;t~.ng ~f gealagical~ tEecto~~ic,
struc~tura~. pa~,~o~alogi+~al~ pa~~at's-ctc-nic, axu~ ,~aa,ebstructural summ~~rieo~, maps,
~ ~ ~ Infarmati.on ~~se is tip
` + and profl:es. A17:' maps ,era to b~ c~awzt .to the same ~ic8'le.
be ob ~aine3 fr~or~ s~udies of refraotr!ed tiraaras, magneto=telluric soundfa~gs, andgostli~er
gaopl~~rsic~]. m~e~tl~,~. ThQ art~nca a~" xecaz~ct~.ng se~,smic phenomena ~~as ~stre ed
~t we,s reao,incted tlu~t '~braratarie's ft~r tl~ a+~u,~r of hh~~sa ~ axso'~sug~geat~ld.
prope~rtie~s of rags be E~stab~.ished. D7^i:Lting oaf deep
.The Ulcrad~ian Academy' of Sciences was ~a~ked to prepare r~rsults~yc`or~o'thaC aucaa~s
Cr3,mas.. ~ teni~x~~.ve date far dd~+auesia~a at pra~llm~,naxy
region teas sei;~ f~br the end of ~,Ql~.
ASSOCIATION: Wane
St1BMITTID ~~ C!~
StTB CO.UE t AS
Card 21h ..._........_ ..... .. ~.
DATE ~~: 48+R,pr61i EI~CL: d0
NQ REF 50q's OQO' OTHERs C~44
,;
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P i w � ~ q,
' ~ KPyF,mNpma.,. s ... r+..1�+r~.r ..�
. rH r.~�..v ... ..r r.~ sw+�
~c~;xo~l l~~x ,~~a2~9o9' e~atiaa~. sciences}
t1~HORs � z~~sav, L. P� ~Cand3.dt-te at pt~sico.-aath
~ h Mobile Session oP
t ~ outer ~untle of tha eaxt t
> > TrrL~ a In~resti,gati�an ~a~' tha crux
the Sc1.enGIB Council}
~piJ1~Es atd ~,>R. Qestnfk~ no. 2, l9btc: ~$~.1,~9
e ~,cg~ tectaaics~ -~PI~i~
` mantle, Cauc~agV~sp Cr,ia-ea~ g oP
TOPIC TAGS, a e,ari'~h crust, lace in Tbilisi a
r, Q~,tobar 31 November '3, ~.9~3 tl~ero taok p
�' AgSTI~tAGT: nuz`i.n,, r evaluat~.ng the praseni~ status off' i~o~seas.
session off' the Slriance C~ounc3.1. ;for the ad~~acent
ec-7.o ica~. structure and ~vo~.uf:ion ' a� a ra ~ n$ ~ thi$ area ar~d o~rganized~
an tale C g ro am o~. axpl
n.ce caun Over l~fl repreaer-tatives o~~ aieatifi.c Y~ese-arc
The ('.ounc~:l also warltiadc:il. a ~ ~ ted,. alt t;he ple~-ry' ,
a regxona.~ sci�e in~u~tr~a~, orga~a~at~oz~ �~ar ~. p
institut3.uns, cc+~.lsges, a~ with a detailed analys~.a o~ tha csurrea~
sassions papers were diascussed d�al~~ - an the evolution of the 8truaturi~1 el~ ons
'data, an t:l~e t+ac#~an~+ca a;~ the Caucas , s ruse
~ . ~ qC~ the distribui;ian a~ ,earpution~th teo~le,~a~ ~tructuxe
of the ea,~th '~r+ eirties of ranks. ~el~arate aapeats ~' ~
;the physical ;p ~'Q t territor;Ges warn dealt with ~ detail. A ,Large nucubes
in the Caucasus and ad~acen
Cdr~~2 -
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ACCF~SxOtJ tt~>< A1'SQ4~IG~9~
' roltttod to the otudy of noiemlo proratiaEto. 9�hn r3aealon in MhidaatN~d >ma rapot"teq'
. ~ JJ,�--~,,. L{4 ~:~"E~+Yi candidate o~ ~phyn ica-uk'tLhomo-t:t~:lkl aaioneoa. Tt rltur! ~~ frith ,
tl~a t~n}~vr a.~' M. A. Sautavek.ty ~uh+~ ctt-narilaod tttn p;l~t~lntnn cif oart~hqurtks: nr_ntttin~�
1C,._~. t~n~~i~i~~ttav and 11.., A. pzntx};~!av pra:~~ontc~d new irs.~nruwtian on t11o tloai- c+truott~~
c-C 'WaaCnrtt 'I'urkmt~nia~an, Via, ti� "~nt_t�t~nv dnnorlhrac~ tha ~nnoral. atruatura:l. hiatOry'
of tho l~lpi.c~n-Jtizynlny~nn mobi~o 'bolt gtld t.ho nd~ncoat trenaition zono~ 1� N�
Gvrhit~nikov ro[xyrt.od to Lho I'zodidltua tho raauJ.ts o~ ttic~ Teahkont aeaeion s~
wtt1r,11 V,,,V_..~,ilnlouagv xmoaontnd tho papc-r. '+~nrth nruat en~a tha upp~~p+antl�{'v[
contSno:ita.� A., 5~,~tt~Fl~,nah:iy: diaau~uod thn ctrl~itl, of natural aullur. ~1~11,,_._._,
i~inlnkltav dol3cribad tttn ntutellagenia peouliari.t~.ou etad typos oT tho Uabok orot~�
ri. !;. Vol'1'laon, Y, a,l_G~.r!ttvv~tni end A,._~,.YSx~oYakl~+ analyzed the applicatiota
cif'~r~octicml~Yal enud ~00}~3~Yo._ioa.l mvthoda to e~1Qre~tion�~'yThe Preaidium of tho
AGn,denr,~ oC~ J3ainnaaa ~A ap~rrvv~o~`tho ~~io~ oP th~+ q~pa~t~uoont of 16~a~rth e4l.a>QOOa,
~r~~aontod i6a r~~u1u'~io~~ tta~ uxparel~lrt~d its ~rai~itwd~ to ,Ap~td+~a~a AR P.
yi~to~radavt the aeo~cloteuc~- opt w,u~ Deparlatian
i of ~l.nclc~r mol.tin~ in tt-e ~noun'r,aina of Cantral Asia, 6f spoeinl interost gran the
~ileiaunsian o1' tho ftt~uttro i'at.n +)� tho Ax~nl Son, 'C'wr) c~ppoaito opiniane woro pxa- i
aonted: V. L, ShrLl.~~ts ~tatod that i.ncroanod vino nl" rivor wators �or irrigation ~
wi.?.1 cacao a CO^1glete dryinC ut? of tho aaa, L. G', f)rxnin-Sark_ovskiy drove attontioA f ' '
to the x'oCE~ilt x�:i.sa o!C the watorr Zovol j.n the aoa, cxplQining it by the peculiar- '
' it'.ioa of wata~� s;r:~na~:~iration b;V dLffare~nt t;{paa cri' vogatation. F,_l?..Aav~it~r
hati~evor, oa:pl~-it~ed tho pnt~ndox by' tho rrator auppl.y at tho river souroes at the
I'.asa;i.r-Altai, and 'l.'~ata~-Shnn~ di�vid�. Tho rasults o3.' tho thrvo sessions care '
' aucr~rizod by Acude>.~:ia3.an I. P, Gorae.inmv. Acadc-mician A. L. Yanahin reported ~ ~
on tho nu~~tn eeASion ~~~' the Furth Scionc;os lMpArtniont in Alm-Ata. R. A, Oorukc~yero~, I
A, K. t~ayY:ix1~~, C,, F'. L~~npichov, and L._,d. Aflxoahnichonko reported on tkie st,ruo~ur~s~1; ~
ani~ me"a.tlcr~;onic~mnFrp:tttg of oantern ICa~,ukli~tnn.....~, 8.:~i.l.3nakiy dieouseed 44~
problet~a~ ix~ thooreti~anl and eaperimentcil miuoral~. ~' A. K, Ka,yupov spoke on the ~ n4
ro:lntion oi' onda~ene mettslloge-~r to tho deep atr:toture of the crust, Y. P. _
No?~~k?xntGk~,yy reported on ~.ron ~a-nd ~nga:neae d~lpooito ~t l~saY}a,etan, 7~;_ ~.
f Sai~}rkov made a quantitative mraluation of arteeifu~ vstere in tJ~e artselan beefnn,, f'
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s
~ AC~CFSiIpN I~1'ta APSacx~~9$
St;eta C,onJ.opiE;nl Cotnmi.ttus :i~:}R. gEStn~bliah~ ~liroct rol.ntion:r pith the ay~vs
acnclo>s:ios wrap tho ilucnocli.nto F;r~al of tho trip. 7'1~Ey :~ym}yoaitun on soic~r;r~laG;~` (h81d
~, i 1.11 Tnn-tkont~ wan ra;portpd an hY td. A. 5adov:+kiy� Tho problems in L111;, ,.'o1.d rraro i
{ r}'Iyritlo~l i.irtq Llir.oo ,;rrun9t 1.) intornrcl. ni,ruatc~~e o,f thc- oartli'3 Grin' ,nd
:~ ;3~3di.mont;n�ry mr~ntlo ravoa.lod by dntn obtninnd hY difforont bronahc,s of tho };oo-
i r~~~i.oncol ;2~ rolaticln amen}; diC�orvnt c~arthgcanka nourcou; 3) protection of the ~
Tt are:; raaummondod that
Iu:,c;,a:lcitian oncl tuatinnnJ ccono~~y from enrh.}-c}un'.ce ciatrtn(;e.
r~ EipOG~,rtJ. tif~rViGe clnalin w,i.tlt t.ho ~3~:rt}u.Ttuikcr f.~~rnan,a t3 pa At~l;nn.l.znd. Anliirrve-
menta of t,}~o aympoaiiun ou h;~dra7.n~ czlaxo rAportod by lt, bl. A}t}imoclgafin. D. I.
` Kcadelin (1�Snccco~t Ua.l.voroity ~ proenntscl a paper on rho drain;ago and renot'ral of
I;rounaj we.tgr. U. lwl. Akh~~ednafin spoke hn the at,ady of nrtoa�tan braaina in
t ita~~k}as+tem. TZ.� A..,KonEennr:ln (Uzb~ls ipstituto, of ltyrlr~X~Cy._a1~d. ~~~nopring_Geo?,OI~Y~
' diaanusvc! tUA prlnaipn'1 ~,rola],om.~+ of t}~aorotiGal, hydrolc,6~Y� ~b�..s~ Sa.ciykGv
} ~ (Acnd+a~r of ~oi.ancEiu, Knzakla &Slt) opoka~ nn t~ha ~ovpagv affaot of wador~~a 4d _~~ `. -
krrinsa acid :lta mentr,ing in tlxr~ interprEStation of era-t'azmation Prooeaaoa.
' I+fav~.y,.anar ~e3vnted an vngi~aaering-geological slap of the acid Ctzbakiatan. ~~.~1s .. _..
~,_~~'C~Afurov diaouseAd ;lrrigatiaa prinoip].eo and thel foraoaef; of ~rdrogeod~runia
''~'jirocoepgl~ t~.t�ng pleas in tl~a irrigai;p~l ar�aa. !,~_L~Yonahia apoita on utilisation
` ` of t1t'tt1Et.:.dA asters. !~. A. '1�aytavio} reao~-snda-d the organ~~st~iobse~ai aialisad
I E-�rriae :f'or the pa~~bleame ~'~ ,s+'oiwa wa-tere. Thu dao~Ph
:-.~,
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

,� ~ _.
...
' f
y
~~,,,-i~%~SZON lit, npg0t1~49g s/ao3o/f~/�p/oo3/o~zs/axs+~,
~i
A.UTHOIt~ ~ ~/~,i14l;~'~1415>Y,w~,e, ?. (Aor+dflmf.ni.an) f C,~eran impv~,-_I. ~, (1loademioian); ,~,r ~~
Xan~h.in~ A.. 1;,. (Aau~'l,anlainn); 5hnhorUnkav~__p%..
~~ti,~~i~d~rai.a~mn~~;,9ndav~~k~.y., M. A. (Cor>�a~pnnd~nt; m�mbor AN 99$8 j~~A~i 11~~~
(li,cadomioi.an APi~K~~~SR~f.?~rtoov~gl,,~p. (Carrdldate of pl~greiaa~nathematt.oal
~ ncionoas) f Ovch~r~nj ~!:av~. _~.+_. ,
f~:TL~t Ik-valop~oant of on~rth r~aiencen in CantrA~. Aei.a and in fta~akbetan (Results
I o!' a fiolcl trip off' i;ho Dopartm~ant of Earth soien~coe)
1 souRC~t nN~ s,SSR. vi,et~xilc, no. 3, 1969, x.28-150
~ i ()P;~C 7'AG's t g~yoaot;lvity, ~ooeh�mi~tty i 6paohronological pi`ablem~ geochraaolo~r~, .
E:;ffodony, 1390~'j~PhY, Boolo~iae~ aurvo;~~, solo , gsomognatlem, gAOphyeioa7. prog~
' pt3ctinB, I;oaphyaioa:l reaaarch, Reaphyclios �~~~;, ti~�
N~TMG'I' : T1~o Pros ilium o~ the Aopdet~- oP 5aieiaaee, SRSR henxd tha roport�~df
arade~nicil~i~ A. P. Yir~o;;'radavy aaorata~,y of the 1?epartment of earth Scienoeo, at
~lao e~:ac~~.~~o held oti ~anuaar~ 1.5. xhe ~tpeake~r grnr~entsd the rueu).te of tlta daperr~~ ,
I tm~nt~s trap (Oot, ).~ll, 14G4)r organised try the Aoadema.ed of Soienoea a~�
R,az.~kt~utaxa~ Kirghi~ti.~a~ Tedahikiatau~ 't`ur~enia'tas~~ and Qetrerrciltat~i anld the
Card I/5 _._~ _.-. , _.....~_._w ~.......~..__~.. ......__.. _. _ _...._.._._...._~..........,.___
j r
1 ~
~i~:.,
�-,r--~-
I1
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

a
AOCCSS l OM Nti: AP40k391~1~ -
4
I
i
i Propagating with the veiacity of S-waves in a half-space has been recorded ex e~ri-
mentally on twro�dimensianal models. i;ert~in (dynamic pecullaritl+es al~ p
rate head wav~as are analtyxed; they a~~e essantlat 1 lower tt~e degen~a�
j with a direct R-wave and their amplitude is c+xnparabie tort~heeamy in cvnaparisan
r direct" Ppl~~vave and a Rayleigh wave. Cc-mparisan of theoretical computa~~ionsFaa
experimental data shows good agreement. between velocity of propagation aind the ire�
dominant period for a degenerate head wave propagating with the veiocit~ of S- ~
waves, In the models i1: was possible to record a '~sio~" interfering d~:generate
head wave;, that is, a w~rlve propagating in the layer with the veiocit of trans-
verse waves in the underlying half-space. This wave was detecte~f clearly when
there was a certain optimal relation b
length (h/' 0�~ etween the thickness of the layer and wave-
+ d )� In this case the thickness of the layer in ccxnparis~nn with
wavelength was such that: there wa '
"slow" de ene,at~~ s an rnterference effect and the amplitude of the!
9 head wave increased :sharply In a certain frequency range. ~n f
the Gase of otlher values of h/~ (0,3 and 0.4) no "Sioy,~t wave Was reCdlyda~i on the
seismograms. 'this apparently can be attributed to the fact that the ifntrrferen ~
I effect is manifested only in a narrow range of h/7~values. The cs
! observed travel�>rime cur+ves of the t's1G-w" wavy yirtUaii coincidehe Thaithe rnd .,
ce i ve tue ,~~ ~�Z~ ke/s a;greas wei i . wt thi tha e~spQrtmmntat q l o et i
~ freeqquency oaf this wave which is 6 + ~ kc~s;. at rnata �~ #~h~ d~min~~lc
i ahead wavo area observed ~ i n the mQ~iei s."" ~~ No `;rapid" interfering de enera~te
f o d ~/3 .~,_~.._. Q ig. att. has. 2.2 formulas anld
.._.~,~..~.~ 2.,_
......_...,,. ..a..~_ _._....,..,,._... -.
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

i
ACCES3"1ON NR. AP~O439p~-
AUTtitlR: i:aytsev, L. P,, .Parkh~amenko, '1. S.
S~p{i~t.9/bf}IOfJO/Op8~ i f'~~/ 11 ~ !
T1T1.E:. pe~gener~ate Mead waves in the c;~se of a thin is cr~ i In
Y Y ~ can a ha l ~~wspace
S~URG14: AN SSSR. lxves~tlya. Serlya g~.of'ixich~slcaya, nar $ 1 b~ ~ ~, ~
9 , i i~,~ 1 Ib1
7OP1C TAGS: seisntologY- seismic head wave, ,yQl`smic brave seismic; t.~s~ve a
s e i sm l c mode i i ng, 9eaPhy;s i cs - { r oi~ag~a t i c-r~,
ABSTRACT: This paper is a continuation of a study of degenerate head u~;a
was undertaken earlier b)- onQ of the authors ~[,. P. ~t-tyts~~v (xv, ves wf~ich
D AN ~:i~f\, ~~rr
geofi,q., Nc>. $, i~bp; A ~~oiovnoy Volne potferkhnastnoBo tips, Vo rasgkt~;� -f ''
teori i rasx~rostr~aneniya ;;~eysmleheskikh voln No, p Y ~ inarnicheskoy
! retical studies discusset~l the axis! 1 s, ' ~~ lzd~v~t 1,Gt1, 1~~~}a These the,o.~
in a medium consisting of= two liquidyan+~~tworel,astipcohatf~~s~acescwd oscillations
continuity. Anew f=orm of oscillations caned ;~ de enerat~:ph itft a plane dis~-
This new paper i s a theoret 1 ca l and exp00%11/G01fCE'~
D218~D,~08
surer and geotharn~y, (;eachronolo~rical ;fpP ,
oi' ir-terna.t procer~~se:~, geoma~;netxsm, rompasite sti cliesfyat-Et~t_~,i,~~~:aes
pora~~y mov~aaments, com~;,osito stud,iles of voloanolo ~ni,z.rr~
~aunding ~.nd mc~~n+~to-tell.ur.tc m~thc~r}~- tat' cittzrl. ~.t1Cyt}i{,e~ ~.sei;rrrra,c
tari~sy. x`~iE~ f'i,rc~ t ~rc:sslot'- of tlr~r~ y' ~" r~x th ~; a t~.,
~9~~~ and ws,r~ conc.c~rne~d with thra coord~~nation o;~~ace �r' }',~'bruax~~�
' :number of a.natitut;es for which �the Cour-ci1 is rer~ onsi of the 1Ftrge
oecond session tod;kc pli3ae towarc}s the elnd of .May and i tsemain~ t,zra
pose was to diseus'~ scientific ~7ra~octs for thc~ ~~ext pew f ~
~inaludin~ ~3d3~ 1n ~tomE- cases ii, was decided to held s ccia~~~r;+,
ctinat:tng oonferenc~~s (paleontolc, P 1 cnor-
E;xoge~letic processes ~~ neotectonics, ge0morpha].af;,y and
n-iner~-Io ' he problem of the tsunami e., physic�rhem:E~~a1
E;'y and peta.olog~y at li~rge depths in the es,rth'e crust)�
Among the m~7at imp,:-rtant meetinCe which took 1 ,
plenary sesr~fan of �che Council on the p:roblentpofcthenfa~~c:nstir- t}j~;
of eax~thquab~c~s, a i~,eminar on the physie~~l properties of ranks ~~
high x~ressure~-, a saympar~ium on the c~rrd~yr
and a conference on paleomagnetit~m. pZtrinhnote try of volcs.nir, rcleks
perio+i of ac~tivi ty of the Council was le-rgely con~yerned ewi th gor an
Card 2,/3 ~ ~.
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

r. i
~/a3~/~~/'ooo/o~ ~!~Q~/crc~,
Ao~~i~ox: s~~ov~>t~
~r yy ~} ;~Sr.~A., ~�cyrr~~Y~-~+ti~~in~ Pie~r-t-r~~~ ~.>.t' t?,ICS
Vi)J~E, ~,nd ~gytBE~lt} ~r ~'.
'~~.__.........~ ............_.._,.....e........_._..~..
TITL~s The etructt~a^e and E-volutian 'of the earth ,gig
a composf to problett-
ryl ~, , ~.
yL~t.i bit~~.c-t~;icta~i.~l~i.~~lcJi.ttf; t~~;~ric fr~~irr~ oxyrliticiry
%C7iiCt't,i.t? ;t'c''Clli~~;`+ 1~~; t:}iit:l{t7t,l.+:i icy ~'~ r! ~vlit.ti ~Eyt;; c;c~tytr,:t~t ();1' ~'1'ir.
1 ,~ !~ ' i'ftLC~l~.1J/ C:f)Itll;i)1'tC,'C1
tivKii:c:r is 1U~~~, tutC.l i~,Y ~a;;~/c tiv}tc~:y t1,cj ~~rF~otirii C> w~~tcz' itl 1.~1C: catycrc:tc i5 'l;~ l;g/rn`l
,,, s~ o .~
ttivi~n ~>, c,osa,;i; z'atio ryf i)]/ll~, = lt~`~'), iti~:yn7.rrlY~m rcUltt~l,ian in a}7iclciin,; tnxCkne~s
titiG to tlye ~.i~raciitic~tl ofi i~ar~an to l7caavy co.~icz'ctc 1'~r~r arc�fillcc3 car~~c~cte vriih a
VaUt7l'L'iriC ~4veight bf 3~Oi~) ~4g/11~~ is 3rJo (when ttie ratio between i;he dasagcs is
~~ liar = 1.0"'z}. Thus, tl"re addition of boz~ary is not ee:anor.~tically advantageous,
in~:u :it r~:s~.>,lts in wryly a small savings in cotyc:rGte. Exaeptian:~ are reinfor~:ed
' ~-----
l ~� C n
Card 1
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

1. Altl~~i
acc r~R~ ~__..~_.._...~,~__......._... __
~..~ '
of from witi~,~aut tb� addition of t~ydrvgen i~t not expedient. ':CrhQ aufihc~~s axe clcel~ly indebted to
V. S, i~isel~ev for hie help in tJie calcultttionl of ttie buildup i'�~cto~,e of int~~rmediat� neutronEi- an
~ V~ia~nae' ev and V M~ATaxarov for' eking availal~l~a the calibrn,ted high-miner amd
interrtiediat~~~-ener~- neutrcl.n detectors, (~a~i art. has. 7 forn~ula.e 2 fi ~ ''
g� - ~e$, and 3 tables.:
SUB CODE: 1$/ SUBM D~-.TE: 29dun6~/ OIZIO III;F; A04/ t)TI-l itEi'; Oql '

Cart!_ 2!'2 ~
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

_ _
~~ .ACC IVRs A.Fti013725 ~ ~,~ SOUI~.CE COLE: ~ UIt/008'9/fi~6/020/1304/0323/032?!M __.~ ._
~ `- ,.
AUThtOR: I5T~ek-ev. H. S.; Ma1'koy, V.wV.; Komochkov~~''~i� Ni:.:i__ Zev~I,._N. ~~,r
f+.e1 1
ORG: none
TITLE: Th,a~ passage of hit~i energy neutrons throu4~- iron-water mixtures
SOURCE: Atomx-aya ener~~tya, v. 20, na. ~i, 1n 66, .323-3Z7
TOPIC TAGS: neutron shi:lding, neutron diffusion, neutron detector, neutron flux
~y
AI3STRAC'I': 't`he accumulation of slow neutrons ~~ ~ 1 MeV~ during the passage of high energy
n~:utrons ti~rou~;Z iron and iron-vuntex� mixt:-ros wr:s clc:terxtitned c.~porimrnts~lly ntid tl~eoroticul-
ly. A set o,f 20 mm thick l~180 x ,)SO mm stE,el plate~~ was placed into a 1000 x 1000 x 2000 inm
metal cont~-inor locatod ~ tl~e synclaracyclot~.�on cltambu~.� of thu OIYaI. t~oncrete blacks shield-~
cd the de~rilce from scatter+~d radiation. Neutrons were generated by 170, 250, 300, X80, and
GGO NteV p~,otons. The palter presents the characteristics of the three detectors used, the
attenuations of the neutron ;flux g~~neratcd by' high enf;rgy protons, rho relaxation length of high
ene~�t~Y r)�ul,rtfns (for v~-rlo~us c~nc~rgic~r~ cff p~rinanry ta~otons rind clliffering c;r~nccntar:tiainR ref wr~tc~:r~,
the buildup factors of i~atexmedi:-te neutrons, and th.e thicwiess of iron-water shielding of vary
ing hydrogen content fora 200-fold attenuation. An- analysis of the results shows that the use
Card
UT~C: 621, t)~IS .512.45
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

q~^T~~.~~~ ~ ~.~ rw -~ .~ ~_~~r^T^L-~ w = T^T^z ~-T'~ fi [~Z~Z~Y~:~:~
~~~~~~
~~~~~~.~ f~12/fl~~
~/~~~1
B~o~/~10~
p C~ {~ -
,~s
~~,f j~~~~.~rit~tkrS
f ~ ~~ ~ 7,`~t:Y ~',.t ~~ 1~_ ,~~ ~ l1 � ~ ~~ t7,t3uGl: UTi~ '.art r;Orlf,~ t3
~ ;~t,t~;n'aa~tx�; n~~ ~ 1~~E,~, ,
~ a ~i.l. h `' "`V
~ ~ 12 ~ fli e ~~ r r, ~ ` ~,deT.~ ` ,
~S:LTLL� ener~i~~'' ~ nr; thro~l(~ ~c~r1-Y~. Y
p,t,~~�ln�~~~~~ s ~~,c.,l. Ia~>.b�r~~ for
,;r~ ~"LCI~~a ~F:i,at "riF3'arT'gn ~ ~ ~~f the ,r~b�~ryti{,r.y
g k ~ ~- ,
loaae~t ~' G.l ~ cLri~�irx~.y T
:iit'Y tihe gy'~.chro , kh ~ caa-� ~,h
~iie �~riten to y~a,cle ~a,r ~��c`ir , ~ y , tyl.>!,;i c)1
~~-~X~ ; ,ztl,:~ed �n rj7'~ TXu~T.c, ~nrr.c.
vrer� a ti. ina~itu c�ncretPa ~ x,, 1, ~/
,t~;a titutc ~}~ etii t {;tile f. i ~rrr-ic ~(
concr~' ,,, eairlc;n'tto ~;c 3 �int xn.s ~ ~.n~~,r~f ~ t;udti f tiu x
blE~m Qb ~ r c~:C the for Qr. 3~ were�~' ,neutron
x.r. � r r ~blem.y cle �nly rznd ~ � ~i ~~cm on fi~>F
~ bcen ma oc c7.�tr t1 r�;_Lc..
~1 ~. ~n,~ 2n C
~;Iuci�~'r had j.l ? i1~hr ~ ~~
,uch atud~,es ti.r.:a ~ 2 � ~`~ + the ay the n the en~'r~~
(~.angi n
conrx~ete P ~~,s tha1luaed ~ t',y in the c t&nt cross ~eCt1~ c�ncrei~,e ?~~ ~ ~`~
.~ 'the sam ~cti,va.
bQini:~ t;he ~ ,fev ~,nc1 ~ c;�ns �f intens}t,~ ent.s
frorl ~p drop ~ eY.;;erim
ir-ed 'Phe ~,ul;hora intens'i~'~ t > the
has e. n tial law ~ the
ti~-T� aiderec~.~, At E ex~�nen re~uGP`'
re con to doll�w Ern thick:nea5 wrich
r;3,nl, t tlae
w,~e f ou:nd tion tea
cm thick ~asumP
re~~uted, tha
___.
Ga:cd 1 ~~~ .
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138001964100026-6

!"

r
... l
~ .�:
', affoxdecl by various typ+~ws of aonerel;e. The reaotor ooneldered has a '
graphite moderator, a r~afleator, andl a coa~crete external shield. Fox
aompuxation, the laaowa +~~bsorption ox~os8 se+otions for fast and inter
mediate neutron's for thi~~ elements px~eeent ;ln the oonaxeta were u�
Tt f o~lc~we ~'~o~ 'fie ooma~~utat~,aa~e tb~~t the ~daet le Animal fox � ed.
shield of an ordia~r otalnarete with 2304 ~m~. ~'or the hee,v~r con
! crate (~4~Op4 ;kg~q/~ ~ th� ooet is min.l,mal ~~~n the watex conte;ct is i~he,
enaallegt;, au~d ;~o~r a oonc;~xete Stith a higher deneitg the mi~.m~u~m aoet
fie when the ~wa~~e;r oonteti,t ~, s at i to maximum. The- authar� aye Brat�-~
ful to A,.M~ ;~oxaaacoa~s~sy for ~.ut�re~t, and p~raotioal advioo." Oxi,g.
arty has: g ;~'i~~raa and ~ tables.
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At~CESS~~~ ~~: ,9,Y~4122fi2.
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AUTHOR~-s B.roder, 1~.L. ~~ Zaytse~', L.N.. 8y+~ohev~ 8.$.; Tu~olu~cov, ,~.M.t
~...... _ - . ,. _ , ~_.,., , 1
TITLE: Bffect of wate~~~ oontent in oonorete on the thiol~ess of the
reaotor eh2eld and ite aoet~.
SOURaE ~, ~tomnaya ener~s;ipa, v.16, n,o.1, ~ !~~, 26-32
ToPIQ 9`AGS: r~aala~or oh~l~ld ~ biological reaotor proteotion, reactor
eh~.e~.d aost~ r~ea~tor shield ~ate~~ oonoe~ntxation, optimal x~eaotor
proteot~an
AES~RA{~x: The purpose of the ~ree~~nt work is to determine #fhe eco~
nomical aspect oaf the :l,noreas~,ag ancouat o,~ hater in oonorete- at'or !
''reaotor� shield:~.bgs. ~a~~oreasi th~~ water ooutent in ooaore~;e inorea-
see its hydrage~, ao~oa~~~tr~tson whi~~h ef~`eot~.rrely~ reduoes thE~ leakage
o~ fast: ahd intermedia'~~e neutrons t~eoauee of the large oros~r eeotso�
o~ hydrogen, for fast ay~~d Intermediate neutrons. Various twee of . oon-
orate ~;ree~, fox reaotor shield~.ngs stave hy~drog�n oonoe~ttrati~~n, ttithA~-
' the 12~` range. The au~f;hors have o~-z~puted th� bsologioal pr~~teotlon .
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