SCIENTIFIC ABSTRACT KRYLOV, A. YA. - KRYLOV, B. S.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


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KRYIDV, A.,-YA.--,.
Kzzlovj A. Ya. - N. V. Baranovskaya, Yu. I. Silin - The Determination of Age by Means
or tile Argon Method of Sedimentary Rocks.
The Sixth Session of the Committee for Determining the Absolute Age of Geologic
Formations at the Department of GeoloRic -Geographical Sciences (COON) of the
USSR Academy of Sciences at Sverdiovisk in May 19157

HY i 'V,-- A.Yzi
"About the Employ/ment of the Argon Method In Weathered Gedimeratry Rocks."
report presented at the 7th Session of the Commission fGr Determination of the
Absolute Age of Geological Fomntlorin, at the Dept. Cecil ~,g I ~-a L -Geu;--,raph leal-
Sciences, AS US)SR, Moscow, 8-12 May 1958.

AUTHOR;
TITLE:
PERIODICAL:
ABSTRACT:
Card 1/3
Krylov, A. Ya. 7.-J9.3-2/15
Hadionotiyity of Various Rock Complaxeg of' the Ternkj Ala-Tau
Range (Radioaktivnoet' razlichnykh kotplakcoy porod khrebta
Terokey Ala-Tau)
Gookhiniya, 1956, Nr 3, pp, 19, - 1961 (USS:i)
The rocks of the investigated region can b? subdivided into
three great complexes: 1)Metamorphic rocks of Prott-rozoic and
Lower Paleozoic era; they are intruded in the Caledonian in-
trusion and apparently displacod or assimilatid by the latter
to a certain degree (symbol I.Q. 2) Caledonian intrusions of
,granitoids; by these the goochemical conditions of thin region
were changed fundamentally, they con.prise more thnn 50,p' of the
Toentraltnyy Tyanl,-Shan'. This group is subdivided into two
intrusions (Y2 and y3). 5) Cenozoic deposits; especially in the
2 2
basin of the Inayk--Xul1iKz). The two Caledonian intrusions are
shortly characterized. F~r each complex average sarplea were
produced from a greater number cf ntat;es; uraniur., and thoriun
were analyzed radiochemicalll , potaziaium by means of the dipicryl
aminate method by Z.Ya.Kolkor. The analygin was carried out

Radioactivity of Various Rock Complexes of the 7-58 3-2/15
TerskeY Ala-Tau Range
totally four times by two different analysta, A.14,14aricheva
and O.F.Korn. Complete analyses which had been carried out
in the All-Union ScientifAo and Renear,.,h Institute of Geolog'y
(vaesoyuznyy nauchno-innledovatellfikiy geologicheakiy institut)
and in the Kirghiz Geologicnl Institute (Kirgizakoye Geolupra-
Yleniye) are given for the characterization of the rock jroups.
The following final ocnclusiona can be drawn; 1) A considerable
quIantity of rudioelemento was introduced with the f;rartitc in-
trusion: uranium, thorium, and potassium. 2)%'Zran'Lte3 of the se-
cond Caledonian Intrusion (alaskaits granites) contain consi-
derably more radioactive elerents than the granites of the first
main intrusion (pirphyry-like granltsf; and granodioritan).
3) The variation coefficients (Y) of the contents of Investigated
radioelements are comparable for all. complexes and elements;
certain rules can, however. be foiind: a)In nedivientation rocks
v is uoually higher (except Y for thorium in M). b) In the gra-
nitua of the second section v for ur-Lniuyt arid thoriuu is con-
siderably higher than in the 4~rayiitej of the first Phase. 4)
The intruded rocks (1-1) and the Fr:inites of the firat intru3ion
Card 2/3 differ to a great extent in their chemical compos-ttion- 5) The

Radioactivity of Various Rock Com-plexes of the 7-50-3-2/15
TerskaY Ala-Tau Range
ASSOCIATION:
SUBMITTED:
chemical composition and radioactivity of the Cenozoic deposits
(Q lies approximatiYely in the middle between the rocks of the
metamorphic series and the granites. 6) According to results
so far available the given rules and the concentration of the
inyestiCc.ted elements apply approximatively to a greater region
of the Tyan'-Shan'. The work was carried out in the laboratory
of I.Ye. Starik. There are 4 tables and 9 references, 9 of which
are Soviet.
Radiyevyy institut im. V.G.KhlopinaAN SSSR, Lenin rad (Lenin-
grad)Inatitute of Radiux imeni V.G.Khlopin;AS USSR5
December 2o, 1957
1. Rook- Geology 2. Rock~"heml,,." -Lnalys'As
3. Rock- Radioactivity.
Card 3/3

KRYLOV, A.Ya.; 81W23, 1I.M.
Certain regularities in the migration of uranium In waters
of northwestern US.S.L Trady Radiev.inat.All SSSR. 8:262-273
'58. (MIRA 12:2)
(uranium)

U
I JT 10 R Krylov,
T I'll' 1. W Thv lgv of tt&e Nli-tnmorphia.,:i (,f *tic ttic:~-nt ;cdim1_,11LJ Of 11.114!
Northern Zor,(~ of Ty;)nl- 'ifian' kVrumya mot-.if~'.)rflzma
drevnikh ottozheniy .9(-.v(,rtioy Ty-inl- 'hnnyn)
Doklaay Akttdemij nro3k ITA3, Vol 1:1?, Nr i, pp W19-W)l
C.P_;:1H )
;t W~TRA CT- It' the ul-c )f a rock D9 dot,11-t-minsw by moatiti of the Argon Method,
th.. -~,c~o of the cry~italiizat lor r-inorals io estab-
I ~!~ti~id. Thp -.amp holds tro. for u ,tr~L
-mining the age of new
pottissilim minpraIr, r)rimariiy feldipar and mica, in a meta-
'norptlin rock. T1* the metamnr.ptii~:m tan complvtv rizid encumpaFised
ri hivg,~, rkit,,lor., it rinel, Lt- t,) it-to-t-mine the age of' tne
rn-~-,imnruniori nf tnt- rr)cV (it- -netatworptiic 1,evel") by the
Method. Y. 1. Vernal3Kiy nata procli.~,,med tnit ttic determi-
na I ion oL tho "metamorphic level" in th4- oldest croan-section
-3 f t it c
- enrthla crust 151 ,)** gre,,it t..itni!*icance ~Hc-fq 1,2). One
h r-;,i,)ns fn- dt*,er-iiri-.on of meta-
morpi:c tim:, ri-Intiorn, is ;r(.-driyzwya *.,iy% *,!i,:dle ~qia) (Ref
Curd Ln tititi ~jri!a otracturen hfive
092

`W, 1-39, -)')
,t' tit- f)t* ths-i Itncient ieditif-ritn (it' tti-, %nrttierti Zon#! it'
a r) I
twcyi ~,roqijck,i. Tn~- j,ju,#)rti tvjv,- !-,,, ioit-o r, Y;~-. ! i it Of 7natf~.riql
I'rc,x -.hLb mr-tfimurphic rockv ,V Nrr,.rth,-rv ','y!~W- Inarl in t-rder to
"ot i mine %Igq,L5 .7r., ttAf; nrt~,i -ir-! dufined
sjv~, cycle:l wilh 1.11, " j" ~! 4 ') ", Yfoljj..'t.
(RO' I). Trtroa;;h ,if
r i i c. r(; 3 Kit u r - , vt, h 0. 1 1-4j,
C ") v -
oI tvi ions t Tno age- v, at, rw-r?,-.. mi-N& ;~a,jor~ r/-j-,kfi I n
t!.- No 1, t I-, crn Tva ti wir. nrproxizmtely U.-) the noo!-
Cnleloni.-in old ro-kr: million. yeara.
Au i,ovL,, itt t, ! r,u ' rcco?ftr. I -.cckr were! met u-
uior:~n med to i7neioflon of tne i;ri i t'orm c-im-poR j * Iran diiring
C't I c~don in I i t I mf? 1, t the oarie timo moi;t of *.h- Lower RaIna--nic
roOKS 'Ncrf, made into schist!i and hornslones (rarely Fneisrl.
3) Th- grrinitoids of the firot. intriusive cycle (* '-)00 million
-7 in agii) ~iier-~ riot
...,ar sipnit'icut~tly metamorphosed d,ArIng later
"old
4.) The Hf!rc.,.-nian ana orogtny.,3 hn-v~, proa,.,c-l r~o
diisc-~-njl-lf- m.-trimni-pninm in tfjl~i rc~eion. ~-11 However, rito U~I-
froi-,) thi, sr,,ut.h.,rn :v,nc IJ,i-mir, --~-n-, by
C,t r d -,tich,~-rbakov) worp ',Ipine ngo.. This 7one roqltiir#~~I

Tn tif- 'Metrimnrphltin at' the *,nc,, ent - r-i imentri of' t h#, Northern Zone of
ft 11 t I EAT,
atudy . 6) Tne Argon Mf!fhod i,ivf.,.-; rathcr c,)rsintent resultzi
and may be unt~d to determine "mr-tnmorpnic levels" in time. The
parf!r Pa.,l cnrri~-d .)ut ;tt the Hbor%tory by 1. Ye. 3tarik, who
ulno l-,ok !irt in thir, work. Thc-rn arti 1 lubli- ana 9 Soviet
referencess.
9-,diycvyY ir.3l.itut in.. V. G. Khlopina ~kudemii nEluk 855R
4.1%i T n, is t p -1 ri,., isIC. volo.iii, -t' -h- -*,cudemy of
%I,ty 19-'18, by D. 1. ~;hchcrbukov, %cadomician
T
card

3(8)
AUTHQRS: Krylov, A. Ya., Atrashanok, L. Ya. So'V/7-59-3-5/13
TITLE: On the Forms of the Ocourrence of Uranium in Granites (0
formakh nakhozhdeniya urana v granitakh)
PERIODICAL: Gookhimiya, 1959, 11r 3, pp 246-251 (USSR)
ABSTRACT: For the purpose of obtaining data concerning the form in which
uranium occurs, samples of rocks and minerals were leached out
fe,r five days with a 0.2 N solution of Na CO Five groups
2 3*
of metam)rphosed graniti from the Tyan'-Shan' (Table 1) were
investigated. Table 2 shows the results obtained with individual
rsek-forming and a~,c?ssorial minerals. Minerals from pegmatite
Beams whi-,h also .,.ontain uraninite sh;~w individual behavior
(Table 3). The fcll:wing is. on the whole, found: 1. monazite,
zirconium, sphene, fluorite, and orphite during leaching-out
give off only a small part of their uranium. 2. Quartz and
feldspar give off a larger part nf their uranium content only
if also uraninito oocure in the rook. 3. The largest quantity
of uranium is lea,-.hed out of magnetite. A second leaching-out
in all. -.-ases resulte4 in naonsilerably lcwer values. In con-
Card 1/2 clusion It may be said that uranium ork-urs in granites an an
--- ----- --- *.

Or( ~he Forms of the Occurrenie of Uranium
in Granites
ASSOCIATION:
SUBMITTED:
SOV/7-59-3-5/13
oxide, a secondary minqral, or as an adsorbed .--ompound. The
authn::o thank 1. To. Starik for his advi:e and assistance.
There are 3 tables and 10 Soviet reforenef3s.
Radiyevyy institut 1m. V. G. Khlopina AN SSSR, Leningrad
(Radium Ins,itute imeni V. G. Khlopin AS USSR Leningrad)
October 28, 1957
Card 2/2

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43
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sli- ih
AS 4

3(0)
AUTHORSt __ _JU~Qlov, A. Ta., Silin, Yu. I., SO-1/20-124-3-47/67
Lovtsy-Ir ~,.V.
TITLE: Northern Zone of Tyan'-Shan'
The Age of the Granitoids in the
*
(Votrast granitoidov severnoy zAY Tyan'-Shanya)
4
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 124, Nr 3, pp 65o-66o
(USSR)
ABSTRACT: Previously published argon method determinations of the age of
the granitoids In the Northern Zone of Tyan'-Shan' (Refs 2-5)
are primarily concerned with the Torakey-Alatau mountain
range. Some of these ages were not well enough established
because the isotopic composition of the argon was not deter-
mined. Today the authors have more data for analygis, which as
before concerns the rocks themselves, not nonmineralic frac-
tiona. The work was carried out in the laboratory of
I. Ye. Starik. A few researchers consider that mica alone is
ouitablefor use in age determinations, for feldspar and
granitoids give much too young an age. Although in the
granitoids feldspar often surpasses mica in abundance - for
example mica is often lacking entirely - hundreds of age
Card 1/3 determinations have been already made directly from granites

The Age of the Granitoids in the Northern Zone of SOV/20-124-3-47/67
tyanf-Shan'
of the same mountain mansifa. The results are an a nile rather
close for granites of the same mountain masaifs nnd for grn-
nites of the name age from different massifs; the ages are
constant nnd compare well with one another. Table 1 shows
ages of rocks determined by the argon methods. In northernand
central Tyan '- Shan' predominantly Caledonian granitoids
(approximately 90 4) occur. ')acond In nbiindance are gray,
often porphyritic Granites and granitolds of Phase 1. The
ages of granites of Phase 2 (red alaskite-granites) often
lead to a misundoratanding in the age determination.
Hercynian granitoide are represented by alnekite-granite,
granosyenitef and eyenite. Although the specimens analyzed
by the authors are not, compared to other work, sufficiently
evaluated, they characterize to some extent the main scheme.
Above all, the rather close coincidence of ages for the
granitoids of each cycle should be stressed. At seen in table 1,
the extreme variations of average ages are at most +10 d..
Most do not exceed this variation by �3-5 ~. Thus, Three
intrusive cycles of the northern Tyan'-Shan' Zone can be
Card 2/3 defined with complete confidence. The granitoida of the same

The Igo of the Granitoide in the Northern Zone of
Tyan'-Shant
BOV/20-124-3-47/67
age can be closely enough paralleled with each other in
different structural zones. Granites of Cycle 1 ("Proterozoic"
or "Balairokiyell) were not well enough determined. Data is
lacking and also the rocks are somewhat alterod. Hence, the
age determined is perhaps too young. The ages of granitea of
the Caledonian cycle - approximately 340 million years - agree
well with many age determinations of metamorphic rocks of the
same area. There are 1 table and 5 Soviet references.
PRESENTEDt August 25, 1958, by D. I. Shcherbakov, Academician
SUBMITTEDt July 30, 1958
Card 3/3
-ill' 'M
Wg~
F-1
-RAV;

3 (5)
AUTHORS: Starikp 1. Ye., Corresponding Member SOV/20-126-1-39/62
AS USSR, Ravich, M. G.j KF-10-Vo~: -YR.,
Bilin, Yu. I.
TITLE: On the Absolute Ago of the Rocks of the East-Antarctic Platform
(0b absolyutnom vozrasto porod Vostochno-Antarkti-cheakoy plat-
formy)
PERIODICAL; Doklady Akadomii nauk SSSR, 1959, 'Vol :126, Ur 1, PP 144 - 146
(USSR)
ABSTRACT: In the present paper the first determination results of the
rocks mentioned in the title, mainly of Precambrian aget are
discussed. For this purpose the collection of the Sovet Oka a
antarkticheakaya.ekspeditsiya (Soviet Antarctic Expedition~
1956-58 was used. It was colleoted during the prospecting of a
coastal strip of almost 5000 km length (Refs 1,2). The invest-
igated region has the structure of a 3-stage plateau which is
in many a respect analogous to the other Godvanskiye platfome
All three stages are characterized in short. No Mesozoic sedi-
ments have hitharto been found in the region of the mentioned
plateau..Conozoio sediments are only represented by covers of
Card 1/4 basic effusives among which leucite basalta predominate. The
5-,

On the Absolute Age of the Rooks of the East-Antarctic SOV/20-126-1-39/62
Platform
first 40 determinations of the absolute age by means of the
argon method made more proclee ideas possible concerning the
structure of the aforesaid plateau. Several results were aur-
prising and their geological interpretation meets with serio-28
difficulties (Table 1). The highest age, 1- 0- 1020-1270 Mil-
lion years were obtained at first for the oases Langerosot,
Grirson, Bangerp and Obruchev, i. e. for leucocratic granites
and pegmatites. The aGe of the weakly migmatitic (Banger oasis
andother regions of the crystalline basement) rocks fluctuates
between 940 and 1050 million years. So-called poly-migmatites
which are 700-730 nillion years old occur at the same time at
several places, especially in the Ban5er oasis. Thus two migma-
titization stages can be separated; a an ea.-lier one which
occurred more than 1000 million years ago, and b) a late one
- more than 700 million jears ago. Thus the migmatitization of
the oldest masses of the eastorn Antarctic belongs to the Pro-
terozoic. A packet of eneissoo in the region of the Einavort
bay and the Ville= elevation is for the time being the only
exception. Weakly migmatitized biotite-gneisses are here 425-
Card 2/4 485 million years old. Thin agrees almost with the age of the

On the Absolute Age -of the Rocks of the East-Antarctic 507/20-126-1-39/62
Platform
here occurring porphyroblastic graniton. The age of the green
achints and mica phyllitee (middle stage of the plateau) flue-
tuatea between 400 and 500 million years. This corresponds to
Sinisian and Lower Cambrian, The Rapakivi granites in the ex-
A. reme east of.the investigatod region has approximately the
same age. The most recent granitoide are the subalkaline bio-
tite-hornblendo varieties. They ara Caledonian, with an age of
305-315 million yeara. The age of the abbro-dolerits from a
stratiform intrusion within the Bikon ~Beakon) series (1T0
million years old) agrees rather well with the geological po-
eition (Lower Tria ate). The same holds in the case of Terti-
ary loucite-granit: (nountain Gauss) which is approximately
20 million years old. The age determinations of the ment!oned
rocks confirm on the whole the authors' assumption concerning
the 3-stage structure of the plateau. The old Gerling constant
Ak 6.02"10-11 year-1 which in much used in the USSR was used
for the determination. The data are only temporary and prcbabl;r
Card 3/4

Or, ihe Absolute Age of the Books of the Baot Antarctic S07120-126-1-3(V62
Platform
somewhat too low. There Are 1 table and 3 Soviet references.
ASSOCIATION: Radiyovyy institut im. V. G. Khlopina Akademii na-A SSSR
(Radium Institute imoni V. G. Khlopin of the Academy of
Sciences USSR). Nauchno-iseledovatollskiy institut geologii
Arktiki iScientific Research Institute of the Ceology cf the
Antarctic)
SUBMITTED: January 191 1959
Card 4/4

ATRASIIENOK L. Ya.; AVDZEYKO G.V.; KRYLOY_, Ta. SILIN Yu, I.
.9 2 1!__~ J,
Aboolute age of the Monastyri type graniteo of Kalba, GeoMimlla
no.3;278-279 160. (KEU 34: 5)
1. Radiyevyy institut imeni V. G. Khlopina AN WSR, Leningrad.
Wba Range-Granite)
Geological time)
~
g,~, t

RAVICH, M.G., doktor geol.-minar.nuuk; KRY14)V, A.Ya., nauchW sotrudnik
gion of the Hawson 'Station.
Abooluto age of rocks in the ra.- Inform.
biul. Sov. antark. ekap, no.19:8-9 160, (MIRA 13:9)
1. fiduohno-issledovatellskiy institut geologii Arktiki i Radiyevyy
Institut im.Khlopina.
(Hawson station region, Antarctica-Charnockites)

RAVICH, M.G., doktor 1;ool.-mineral.nauk; KRYLOV, A.Ta., nauchnyy votrudnik
Absolute age of rocks in the eastern part of the mour-tains of Qum
Maud land. Inform. biule Soy* antark. skeP. n0-20.15-17 160.
(MIRA 13:9)
1. Nauoho-looledovatel'skly Institut geologli Arktiki I Redlyevyy
institut AN.
(Quen Maud IwA--Rooks, Igneous)
(Geological time)

KRYLOV, Yu.1,
Using the argon method for determining the age of clastic
nedimentary rocks. Izv.AH SSSR.Ser.geol. 25 no.1:56-66 Ja
'6o. (MIRA 13:8)
1. Hadiyevy7 institut iment Y.G.Iihlopina AN SSER, laniagrad.
(A'gon) (Rocks, Sedimentary)

sTARIK, I.Te. - RAVICH, x.G,.- -raTwy. A.Ta. I STLIN, Ta. I.; ATRASHXDDK, L.TA.;
0 1. 1 -.1- - ~ I
IDVTSM, A. V.
Recent data on the absolute age of rocks in eastern Antarctica. Dokl-
AN BSSR 134 no.6:1421-1423 0 160. (HIRA 13tlO)
1. Radlyevyy institut im. V.G.Idopina Akademli nauk SSSR- 2. Chlen-
korrespondent.AN SSSR (for Starik).
(Aiitarctic regions-Rocks) (Geological time)

fd-'.YLOV~ A..Ya,!-,- LL31TSYN, A.P,; SILIN, Yu.I. (Silirw, J.I.1
Sipificance of the argon - potmalum ratio In oceanic silt. Izv.
All SSSR.Ser.gool. no.3:87-100 Hr 161. (MIRA 15:2)
1. RadiyeM inotitut AN =R, Leuingrad i Institut okeanologii
All SSSR, Moskva.
(Ocean bottom-Deep-sea deposits)
(Geological time)
-77

STARIK, I.Ye.; SILIN, Yu.I.
Absolute age of base rocks in the eastern part of the Ruo:jian
Platform, Biul,Kom,po opreabo~vozr,geolofom. no.4:64-65 161.
(MIRLA 15:1)
(Russian Platform-Rocks.. Crystalline and metamorphic)
(Geological timo)
S~,
PIK q~
4~01t 7K
EF, d~~ ~i,

I.Ye.; BARANOVSXAYA, F.V.; ZIUROVA, V.V.; BYLOV, A.Ya.
Determin* age of magnetites b7 the helium method. Diul.
Kom.po oft.abo.vozr.geol.form. no-4:151-159 161. (MIRA 15:1)
(Geological time)
(Magnotiton)

VISTELIUS, A.B.j KIffIDV, A.Ya.
Absolute Age.of the clastic part of sandy silt deposits in the
southwestern part of Centrea Asia* DokleANSSSR 138 noe2:422-425
W .161. (KERA 3415)
le lAbomtorlya aerometoday Akademil rAuk SWR i Radlyeny institut
in. Mahlopina Akadenii nauk SSSR, Prodstavlano almdemikon D,V,
Nalivkir4u.
(Turkmnistan-Goologys Stratigmphia)

KRYLOV, A.Ya.; VOROIJOY P.S.- SUM. YVI.I.
- P
Absolute age of the cry9taJlIn& basement of eaztern Antarctica.
DoU. All SSSR 143 no.D184-167 Mr 162. (MIRA 15:2)
1. Radiyevyy institut im. V.G.Khlopina All SSSR. Predetavlena,
akademikom D*I.Shcherbakoy-ym.
(Antarctic reglone-Geologyl, Stra:tigraphic)

T ~M
RLVICHO M. G.; IMLOY, A. Ia.; SOLOVITEV, D. S.; SILIN, Yu. 1.
Absolute age of rocks of the central part of the mountains In
Queen Maud Land (eastern' Antartica). Dokl. AN &M 147 no.6t
1433-1436 D 162. (MIRA 16:1)
le Nauchno-imalsdovatel'shy inetitut geologii Arktiki i
Radiyevyy institut in. V. G. Xhlopina. AN SSSR. Predatavieno
akademikom D. L Shaherbakowym.
(Queen Maud Land-Petrolocy)

SILIN, Tu.I.; SHNIP# O.A.
Reoent data on the age of bummtrogko of westem Central
Amia, Dol~. AM MR US no.3s665-667 Ja 163. (HIRA 16 s2)
1, PredstivIeno skadstalkom D.I. fteberbakoy1m,
(Soviet Central Asia-Rooket Ipeous)

-
m
t
A.Yn. KRILOV YU.I. Sn'Iff. (USSR)
"Argon-method of age determinition in marine geology tuid paleogeography."
Report presented at the Conference on Chemistry of the Earth's Crust,
Moscow, 14-19 Mar 63.

KIULOV I A. Ya.
Calculating thr- stressed otate of' gravity dams on a rock base. Report
No.2. Trudy GISt no.44t6.22 163. (KRA 17tll)

AVRASHOV,, A.S.; XRYLOVj A.Ya.1 SILIN, Yu.I.
Now data on the ap of granitoid Intrusives in the central
Pamirso Dokle AN BUR 153 no.5sll36-n39 D 163.
(MMA 17: 1)
1. Bredotavlano akademikom D.I. Shoherbakovym.

AYMNI)IMIYEV, A.A.; FEREUVATOV, V.X.; SHIVA."OV, 11.111.;
I.A.IjjLtj~PV~
[Student's manual of calculations and diagrms In 3tructural
mechanics] Posobie dlia studontov po vypo1ncniiu raschatno-
grafichoAlkh rnWt po i3troltellnol mokhaniko. Gorlid-it
Inzhonerno-stroit. in-ta in. V.P.Ghkalova. Pt.42. 1.96 p.
7~,."N ~P,

KRYLOV, A.Ya. (Gorlkiy)
Calculating the stressed state of a gravity dam with a large
opening. Pryk1. mckh. 10 no.3024-336 164. (MIRA 17:6)
1, GorIkovskly lnzhonerno-stroltellnyy Institut.

KRASILIZINA11KOV, A.A.; LRLL0Vj A.1,YAl,YrlJf!N, O.A.
Age of certain granitolds and pulsses Ln the northem PaTt Of
SpItabargen. Dok.. AN S-SR 159 no.,4a796-798 D 164 (MIRA 1811)
1. flauchno-lasledovateltakiy lnstJtut geologli IL-ktikl. Pred-
starleno akademikom P.I.Shcberlwtkoryms

L GW
ACC NRi AP6014232 SOURCE CODE: UR/0213/60060/002/026110C.66
AUTHOR: Bezrukov, P. L.; Krylov$ A. Ya.; Cherrnreheya. V. 1. /3
ORG: Institute of Oceanology, AN 868H (Institut okeanologii AN SSSR); Radium Insti-
tute (Radiyevyy institut)
TITLE: Petrography and the absolute age of the basalts on
SOURCE: Okeanologiya, v. 6, no. 2, 1966, 261-266
TOPIC TAGS: ocean property, oceanographic expedition, oceanographic ship, basalt,
petrography
ABSTRACT: Volcanic rock from the bottom of the Indian Ocean was sampled during the
1959-1962 cruise of the research vessel "Vityazl". Petrographic study of the samples
has shown that in the most cases the rocks were olivine and nonolivine basalts and
basalt glass (hyalobasalts). Chemical analysis indicated that the part of the samples
is low-potassium tholeitic basalt, and the other part is alkaline basalt. The K-
argon method was used to determine the absolute age of four rockt samples from two
stations in the southern part of the Ocean. Their age appeared to be about 60 million
yr, corresponding to kwPaleogene (Eocene). Orig. art. has: 1 figure and 2 tables.
[Based on authors' abstract.) [NT]
SUB CODE: 081 BUBM DATE: 12Jan66/ ORIG IW: OOT/ M REF1 oo6/
Card 1/1 UDC! 552.2/331A(267)

ATRASHENOK, L.Ya.; ATRASMOK, P.V., AVDZFYKO, G.V.; IMYLOV, A.Ya.;
LOVTSYIJS, A.V. ,
Isotopic composition of lead of the northern Tien Shan. Radiokbimlia
5 no.W60-164 163. (MIRA 16slO)

ATRASHOOK, L.Ya.; -KRYIAV, A.Ya.
Radloactiva equilibrium In rocks of eastern Antarctica.
Radiokhimila 5 no.W70-172 163. WRA 16110)

KRYLU, A.Ya.
Evolution of radloactlyity 4M of general chemical composition of
rocks in the Tien Shan northern zone. Rndickhimlia 5 no.2t
173-182 161. (MA 16:10)

87987
4?$17000 S/144/60/000/01'L/001/008
E031/E255
AUTHORS-, Ugodchikov, A.. G., Doctor of Technical Sciences and
A. Ya., Post-graduate Student
TITLEt The Electrical Simulation of the Conformal Trans-
formation of Semi-infinite Domains
PERIODICAL, Izvestiya Vysshikh Uchobnykh Zavedeniy,
Elektromekhanika, 1960, No, 11, PP, 31-35
TEXT-. The problem frequently arises of establishing a
correspondence between the points of the unit circle and the
points of the boundary of some semi-infinite domain S., To do
this it is convenient to transform the domain S with boundary L 0
into an enclosed simply-connected domain S, with boundary Ll by
an inversion. It then remains to find the transformation between
S, and the unit circle.. The establishment of a correspondence
between points on the boundary of the circle and those of Ll, and
the construction of a polynqmial giving the conformal mapping of
the circle on to a domain Sj which is very close to the domain Sl,
can be achieved with the aid of electrical simulation (Ref. 2).
However, the function effecting the mapping of the unit circle on
to S' (which is very close to 5) can be simplified by the
Card 112

87982
S/144/60/000/011/001/008
E031/E255
The Electrical Simulation of the Conformal Transformation of
Semi-infinite Domains
observation that in two-dimensional problems in the theory of
elasticity (where the problem under discussion arises most '
frequently), the boundary Lo assumes the particular shape that the
ends which tend to infinity do so in directions parallel to the
real axis. Thus the t ansformation consists of -the sum of a term
of the form C-1/(l +j ) and a power series in is tile
complex variable in the plane of the unit circle). TheiW ef f ic-
ients of the power series are obtained by putting"t = e ,
expressing the coefficients as cxk + i0k, and separating the real
and imaginary parts. Tile results of a simple application of the
theory are given. There are 2 figures and 4 Soviet references,
ASSOCIATIONg Kafedra stroitelinoy mekhaniki, Gor'kovskiy
inzhenerno-stroitel','nyy institut
(Department of Construction Mechanics. Gorkiy
Construction Engineering Institute)
SUBMITTEDi September 19, 1960
Card 212
Id &M Effiftz MAYA

UGCIDGIIIKOV, A.G. (Gor-kiy)j IWLOV, A.Ya. (Gorlkiy)
Calculating stresses near inspootion galleries in hydrotechnical
installations. Inzh.zhur. I no-41140,165 161. (HTIA 15 s4)
(Hydraulic ongineoring)
-z-

A. TA, KUTIMEIMOV A M 3:-PXB-- IM nTw-- I - C) I
i.; UUCIxH1K I', A.G. (Gorlky)
410n the solution of some plant problems of applied elasticity with the aid of
electrical simulation of conformal ma,, ping".
report presented at the 2nd All-Union Congress on Theoretical and Applied
Mechanics~ Moscow, 29 Jan 5 Feb 64.

KRYWIV,-B.-j Onrshiy nauchnyy sotrudnik
Nonpackaged transport-ttion of cabinet-type furniture. Sov.
torg, 35 no,10145-47 0 161, (KMA 14:32)
1. Wentralln" nauchno-isoledovatelleddy institut t"Y i
upakovki,
(PUrniture-Packing for shipment)

M.1ho"10vt S., -io~.Ujr Lqkhh. W10 AIMOT, D.j khrd. tAXh-,.. nALk, MUKHA,
Jn2h,
V., kPind. toklin. ti A u k Y U. , 4
'improved meLhM of sealing jlo!nts or large-panel biAlding" in
w Intoir 411, stroI, no.9M-25 10. 18,11)

KRXLOV# P.; SaMINS V.
Solution of the prot4on ofpeak hours in urban bus service. Avt.trazwp.
na.'011-13 Ag 1620 (MIRA 1634)
le Orlovokaya avWtraneportnaya kontora I Nauchno-issladdvateltakiy
institut avtomobillnogo transporta.
(Notorbus lines)
E'.
77

KRYWV. B. A,
IKRYWV. B. A. lFeaturse of the organization of concrete work under vinter
conditions using frooza-metting concrete". Wscow, 1955. Min Higher
Educatiob USM. Moscow order of labor Red Banner Construction Engineering
IpA imeni V. VO X bysheyp (Dissertation for the Degree of CAndidate of
(Technical Sci*nc*18.
Sol wIbW lWall k- 46t 12 Movimber 1955, Weclow
PLT,,,~,g ap

HIRONOT, B.A.,,doktor takhnichoolrikh nauk. professor. r*d&kt*r:-ELUXX..-
3 , kandidat tekhnicheskikh nank, redaktor; RROAK. S.A., redaktor
--j-,AA
zda tallstva; PMOK, X.M., tekhnicheskiy redaktor
[Papers delivered at the International Congress on Winter Concreting]
11sterisly Nesbdunardonolo kongreass po stansau betonirovantin, Pod
red. B.A.Kironova i B.A.Xrylo,*. Moskvs, Gos.lsd-vo lit-ry po
stroit. i orkbit., 1956. 125 p. (KIRA 10:7)
1. Symposium on Tberory and Practice of Winter Concreting.
copenha on, 1956.
f0oncrets construction~-Cold weather conditions)
T

IRTLOV, B.
Useful manual for rural builders. Sell.strol. 12 no,90 of cover
3 157. (Bibliography--Building) (MIRA 10:10)

MIRDNOV, S.A., dolctor takhn. nauk; XR~~., kand.tekhn.nauk.
Cond-ate and reinforced concrete construction under winter
conditions. lovetekh. I pared. op. v stroi. 19 no.12:6-9
D '57. (MIU 1111)
(concrete constructlon-Cold weather conditions)

KRYLOT, D.A., kandidat takhnichookikh nauk; DiNIMY, N.N., kandidat
*4-IK.,,,.wt~nicheskikh nauk.
Using concretes with chloride salt additives on the experimental
construction yard of the Kakhovka Hydroelectric Power Station.
Strot. prom. 35 no.103-37 Ja '57. (KLRA 10:2)
1. Mookovskiy insbanerno-stroitellrqy institut imeni
V.V. Kuybysh"va.
(Kakhovim Hydroelectric Power Station)
(Concrete)

/7
UKHOV, B.S., prof., doktor telft.nauk [deceased]; TOROBITNT, V.A.. prof.$
doktor takhn.nauk, seslushannyy deyatell nauki i takhniki; TZOOROV,
Tu.A., prof., doktor iskusstvovedchaskikh nauk; STRAMENZOV, A.Te.,
prof., doktor takhn.nank; SIROTKIN, V.P., prof., doktor tekhn.nauk;
TOROPOT, A.S., dotsent, kand.takhn.nauk; KRYLOY, B.A., kand.takhn.
naukj GWYM, A.K.# kand.takhn.nauki O9tOtOM1r*,'-M.S., dotsent.
kand.arkhitertury, insh.-nrkhttektor: POGODIN-ALXKSSTEV, G.I., prof.,
daktor takhn.nauk, obahchly red.-,-NAYMOT, N.A., doteent, kan4.takhn.
nauk, nauchnyy red.#, KOKOSHKO, A.G., red.: 11AUMOT. K.M., takhn.red.
[Industrial and residential construction; textbook for higher party
11 chools) Promyshlennoo I grazhdanskoe stroitalletvo; uchebnoe poso-
tie dlia vysshikh pnrtiinykh shkol. Moskva, 1959. 434 PO
(MIRA 1):2)
1. Kommunistichaskaya partiya Sovetakogo soyuza. Vysshaya partiynays
ahkols. 2. Chlon-korrespondent Akndemii stroltelletva i arkhitak-
tury (for Strawntov). 3. Rukovoditell kafedry promyshlonnogo prois-
vodstva I stroltalletva Vysehey pnrtiynoy shkoly pri TSentrallnom
komitete Kommunistichaskoy partii Sovetakogo soyuza (for Fogodin-
Alaksayev.)
(Construction industry) (City planning)
ii7-

BMWZOVSKIY, B.I., insh.; KELYLOV, S.A., kand.takhn.nauk, nauohnyy red.;
GKVWWTA, U.K., takhn.red,
[Some charecteristion of construction under conditions of the
Par North]' Nakotorys osobannooti stroitalletva v uslovilakh
Krainego Severe. Xoakva, Gonjad-vo lit-ry po stroit.. arkhit.
I stroit.materialam, 1960. 126 p. JMIRA 14t4)
(Russia. Northern-Building-Cold weather conditions)

KEYWM, L.I., inzh.; VOLYRTSEV, V.A.; LUIOUCV, V.A., retsenzent;
SHELKOVNIKOV, S.G.p reteenzent; )MLOV..B.A....kand. tekhn.
nauko nauchnyy red.; SHIROKOVA, G.M., red.izd-va; b0l"OVNEV,
N.K., tekhn. red.
(Construction of high reinforced concrete structureslStroitell-
stvo vysotrWkh zhelezobetoraWkh sooruzhanii. Moskva, Gosstroi-
izdat 1962. 278 p. (MIRA 15:12)
Neinforced concrete construction)
2

MIRONOV, S.A., prof.j KRYLOV, B.A kand.-tskJin.nauk; UKROV, Ye.N., inzh.
Hardening of concrete with an addition of potash in freezing
weather. Bet. i zhel.-bet. 8 no.3-1:483-487 N 162. (KIRA 15;11)
1. Chlen-4orrespondent Akademii stroltelistva i &rkhitektury
SSSR (for Hironov).
(Concrete oonat-ruction-Cold-weather conditions)
(Potash)

KRYLOV, B.A., kand. teklin. nauk
Cooling of mortar and concrete during the aealing Of
joints in frost. Trudy NIIZHB no.321123-136 163.
(mrRA 17t1)

;.A,,, loktort-3khn, nalik, prof.) ML(M. B,,&,, kand. t*khn.
ne Uk
Inoreane of the strength of concrete during frost and ~during
Ito subsegijant hardening at above freezing temperatures. Bet.
I zhelo-bat. 9 no.11:495-.501 N 163, 04MA 17cl)

MIRONOVt S.A., doktor Whn. nauk, pr:)f.lt KFLYLOV. P.A., kand. takhn. nauk
0
I - ..' I
Una of gas concrete In Sweden. Strol. mat. 10 no.2 38-39
F t64. (mlRA 171s6)

KRILOVI B.A., kand. L(Ahn. rinuk; ~:OPY'A",*, V.D.,
Heat treatment of urb.,lAe..Strcl. mat. -11f) S 16"',

KRyLoV~ 13.F.; laWMVI A.P.
Automatic charging of materials on the alntering conveyer belt
eyatem. Biul. TSIIC104 no.3:36-37 161. (KRA 14:12)
1. Cherepovetakiy meta.Uurgb:hOskiy zavod.
(Sintering-Equipment and oupplies)

MASSEN, V.A.j MILOSLAVSKIY, I.L.; PAVLOV, S.P.; POGODILOV, M.N.; SHEVELEV,
A.Ye.; KUNITSA, S.S.; YAKOVLF.V, V.G.; CHESNOKOV, V.K.; KRYLOV,
B.F.; SHINHANOVICH, B.A.; YAITSKOV, S.A.
Proposals awarded prizes at the 16th All-Union Contest for
Electric Power Economies. Prom.energ. 17 no.lOsl2-14 0
162. (MIRA 150)
(Technological innovations--Competitions)
Aq

Ka!g4,4.p., inzh.j LEZHNKV# A.P., lnzh.
Voltage reguAAtion in low-power 220-380 volt lines. Prom
energ. 18 no.5:22 MY 163. (MIRA 16:6i
(Electric power distribution)

IIARKHO14OVSKIY, I.D.; GRIBANOVO P.F.; LISITSYN, F.P.; KHYLOVp B.G.,
Btarahiy nauchnyy sotrudnik
Research Institute:of Containers and Packaging starts talking
about containers. Izobr. i rate. no.8:8-10 Ag '61. (MMA 14:9)
1, ZavoduywheUy laboratoriyey standartizataii i normalizataii
TSentralluogo nauchno-issledovatel'skogo instituta. tary i upakovki
Uor Parkhomovskiy). 2. Zaveduyu3hchiy laboratoriyey t,.Lry i
upakovki iz polimernykh i kombinirovannykh materialov TSentrallnogo
nauchno-issladavatellskogo institute. tary i upakovki (for
Gribwwv). 3. Vedushchiy konstruktor Spetsiallnogo konatruk-
torskogo bpro Tgentralinogo nauchno-issledovatellskogo instituta,
tary i upakovki (for Gribanov). 4. Laboratoriya ekonomiki
TSentrallno o nauchno-issladovateltakogo instituta tary i upakovki
(for Krylovj.
(Containers)
W_
J:

YEGOROVV B. N.; KRYII)V, B. G.
Double malting of triatearin. Zhur. fiz. khim. 37 no. 3:67-,-,-
676 Mr 163. (MIRA 17:5)
1. Tnntitut obiffichoy I neorganichookoy khimil Imeni Kurnakova,,

MYLOVY i)X.
More e,.onoml.c methodo for. packing Nrniture. Der, prom. 10
no.705 JI 161. (14IRA 107)
1. TSentrallnyy nauchno-issledovatellskiy institut tary i
upakovki,
(Furniture) (PackagIng)

. 1.1- ". --, kI.--l,4,l,,, .
~ - " r- ~,, - - I --- 111-1-- - - - -~_- )k . . - % -,, ~ " 11- " ., ,-~
KRYbDV# B.C.; MIZINA, I.N., red.; PEMENKO, V.M., teklm. red.
[Packing of furniture) Upakovka raboll. MoL;kvn, TSontr.
in-t tekhn. informatsil, i ekon. issled. po lesnoi, bumazhnol
i derevoobrabatyv. promyshl., 1962. 31 P. (VIRA 17W

RAVICHj G,B.; YEGOROVp B.N*; KRTLOVV B,Go
Po:~mrphism of higher monoaoid trlglperldes studied by means
of an volumetrio microdilatomer with an automatic recording
device. Izv.AN SSSR#Otd.khim.nauk no.3481-487 Mr 163.
(MMA 16W
1. Institut obehahey L neorganichaskoy khindi im. N.S.Kurnakova
AN SSSR.
(Glycerides) (Pblymorphism)
I~N

YEGOROV, B.N.; RAVICH, G.B,; KRYDOV, B.G.
Phase transition of the second kind In 2,4,6-trinitrophenol.
Dokl. AN SSSR 152.no.2t370-371 8 163. (MIRA l6sU)
1. Institut obahchey I neorganicheskoy khimii in. X,S. Kurnakova,
AN SSSR. Predstavleno akademikom I.V. Tananayevym.

Sloe 11631000100310051056
B1441BI86
AUTHORS: KrIlovo Be Koo Kalmanovekiyq V. I.
TITLE: Technique for identifying the results of chromatographic
analysis using a mass spectrometer
M(IODICAL: Reforativnyy shurnal. Khimiya, no. 3, 1963, 119, abstract
3G34 (Tr. po khimli I kh1m. tekhnol. (Gor1kiy)p no*4# t961p
747-752)
TEXT: The mass opectrometer ~IA1305 (U1 1305) (RZhKhim, 19599 no- 5,
15666) was adapted for identifying chromatographically separated components
of guseoua mixtures. Mase-spectrometric analysis was conducted by freezing
out tho fractions as well as by continuously admitting to the mass
spectrometer the gasea leaving the chromatographic column. In the first
case components with a concentration of 0.5 - 1~. in the initial mixture
could be analyzedg in the second case those with up to 3% concentration.
The volume of the sample Introduced into the chromatograph was 10 - 30mlo
The continuous admission of gases in viscous state was effected using a
Cu capillary tube 15 cm in length and 0.3 mm in diameter, to the end of
which a glans capillary 10 - 15 am in length and 0.03 - 0.05 am in
Card 1/2

s/Wi 63/000/OD5/0051/036
Technique for identifying the results ... B144X3186
diameter was soldered. Electron patturns are given of the continuous
c angd--o-f-th-e--a-otel-era%it4g--yaltage~-in-the-masc~--spee-trome-ter-for the
scanning of the mass spectra. The technique was checked on a mixture of
C and C hydrocarbons. lete translation
3 4 LAbstracterlo note: Comp
14

Kpagy, F. 1'.
Zur ciner arteit von lutz: = Die aLlIgemeine losung Aer Ilf f e rent lal-gleichung U-S-W-=
Sitzunesber. Payer. Akai. Math. Natur4. Abt. (1926) Kazan, lZv. riz. - Matem. O-VA (3)
5 (1931), 85-89.
Opredeleniye gruppy sisteW Gaussa. Kazan', Izv. fiz. - matem. O-VA (3), 9 (1937),
13-30.
Postroyenlye kAnonichaskikh lntegrall-nykh matrits sistemy GAussa. Kazan', Izv.
FIZ. - MRtem. 0-"VA Mt 12 (1940), 92-117.
SC: Mathematics in the USSR, 1917-1947
FAited by Kuroch, A. G.t
Flarkwevichg A. 1.
Rashevskly, F. X.
Moncow-Leningrnd, 1948
"M~"N

KRTLOV, B.L*____
Determination of a group of regular.systans of uniform linear
equations with differential commutative substitutions of the
second order. Trudy W 20:92-111 148. (XLRA IOW
(Differential equations. Linear)

IRTLOY, B.L.
1 .1
Finite solution of Rismann's problem for Gauss' systems. Trudy KAI
31:203-441 156. (KI2A 10:5)
(Differential equations)
(Katrices) (Punotional'analysis)

KRYIA)V, B.L. (Uzan')
Singleness of the solution of Riemannian problem. Trudy UI 43 j13--28
159- (XIU 14 11)
(Yunotiono)

Rk,
KRTLOV0 B.L.; TEVGRAFOVA, L.N., oty. za vyp.
(Fundamentals of operational calculus] Osnovy operatslob-
nogo Ischislenlia; uchabnos posobie dlia aviatsionnykh
institutov. Izd.2., parer. Kazan', Kazanskii aviatsion-
nyl In-t, 1961. 50 P. (MIRA 16;11)
(Calculus, Operational)

KRILOV, B.L.
(Fundamentals of th& fi*U ikmry; -taxtbock for,aviation
institutes) Oenovy teorli pdliaj uchobsoe ppooble dlia
aviatsionnykb institutoy. Kazan', Kazanakii aviatslonrgi
In-t, 1962. 109 p. (MIRA 170)

KRYLUV, B.R., irizh.; LEZIMIKV, A.11., Inzix.
Mechanized procedsing of oscillograms. Pr=. energ. 18 no.9s
12-14 S 163. (KDtA 16 10)

4100b/010
,000/00
S/1" 135 13.5.
SOZ7 JOV 3.0 JS
raeta
P'.5 0
we .(.IC d ot-,rabotltft
of
of
i'1tJJt%Y
'C C)IIS COP a crokc0nis
t5u!4 ,, . torTAIG ot V*" 3.3.6
, 1core 3. A to or
to _Y0 r jol, b'31'%A 804 t Jill
VC(le"i d C' ir I% J~
0 1,6-53 _1.0114 to too
I- e "TAt ditA91 't 011 5010
(je ~0'1 tt 101, efee
for C 0, 115 ttla 0 J6 k1sivi, erkis
50"o ~Cde x bad i, (I out '&V0 C, j~va very
tx1d 151AOVI 0 d V10
rr'~le is f ibres c, I, r Ir toe otfled e WJ1316
were %Jae Ilt 5 If c,
or A. O'er .4cre iller 'ra
T I., b e 0 "to diOS' 5 -
0,1-101"IlAry a"') t r inle 1 3,05 a VI it feet 01%
Ck"l, I JLM3- C Is 13 in 0.)Lvo it ick lolt of froo 1) 1
t3.t str tj-ver the i" t ilue to 0bo. 4 ILo 0. k~T
u5 cdo j., 1. d f A:kI croLtuir '4 "
too , AlAd for t 1% i.11 boorO teoxv 11.0-yo % J.Jo ItC.
O~j re treso cer for room koe UL Itse CL
Act%., t
r . I'1 S - 0, 0 r-
to " e cal'~ af tox b5 . aout I.Ybek bet, V 0002-1~ "2'*
of t1 to
t br ti.09; c- 3-C ICA -JVbV6- d 0.
no -be OL 'art 'Sins n 9L
did VTe to %4ere 43r0 Ild a COlAtak
e4 VCIa 8
11,11
V"nd 00 Yf too
ad
ter a,
Taa
er
'Ca c
PN' r d
Susceptibility of Welded Joints
w S/l21/62/o(j0/0()1,/008/010
ith tile fol-lowilla hyarog, L'027/F.135
soaking: it conterit., w
1'9 mm thio-005' ()'01()l 0-015, 0 ere "'Plred by therma
Ck were bt * 030 and 0. 050j,,.
no filler 'tt Welded Using ar i Strips 1.~') to
Tile metal. The arc 9
'9",';c()I)t 'bility specimens were lgon -Procedure with
content to crncking increaa5 HIM Wide and 6o min Iong.
- The time for cracking varie ed with increasing IlYdr~gen
6 to 40 days. All the alloys d with Ily(Irogell contel
in tile we,, ' I a
led joint3 At 0,05-91101'foc coarse It from
hydride could be ob 010' 4cicular
C080"Ved in t 9 112 dark inclugiolls of. Structure
titanium hYdrido lie VTI,
hYdride Uld be foun titanium
VT5 and OT4 al
finely di n TiA13Snii loys. No
otributed in tile w le titanium
distributed atiray from th.. Ile, i -TI
to be resPonsibl, _I tn t_re elded joint and coal.sely
Cted zone.
titaniu for crackil r n
of h y the fol "ydrO9Cn a
In allo s 19 tinder Constant bending. I
Yd'O,gez, can occur atlowing Ppears
Of hydride can occur; roo P Opceernateu,res 1) with
diffusion
2) hydmrtem 'asociatteldle precipitation
the phases. Precipitatioll ogen can be redistributed between
Of hyd,ide at
along certain crystal grain boundaries and
ductility. 'OgraPhic directions causes loss of
Card 2/3 Cracking in due to$ i) the above mentioned loss of

rilywvU_~ ~S. I insh.
Iffect of 4h temperatures on peat insulating boards in tho
process of drying. Torf, prom@ 39 noA19-21 162. (MIRA 16o1)
1. Ivanovskiy onergetichaskiy institut imeni V.I.Lenina.
I (Pnt--Drying)
~(InoWAting materials)
77 7777~~

KRTWV,___PfOftj~-jnzh.j SOROKIN,v A.IP.p doktor tokbn*nauk, prof, (decoased]
Conourning the movement of cotton particles in a gas flove
lzv*vpeucbebezav*; energ. 6 no.lsl3.1-134 Ja 163. (MA 16:2)
lo lvanovskiy anorgatioheakiy institut imeni V.I. lanina.
(Muid dynamics) (Ou dynamics)

KRnOV, B.S., PYATACHKOV, B.I.; ROMANOVA, T.M.; SKRYABIN, Ye.l.
Drying of insulation slabs made from peat. Torf.pron. 40 nc-5:
25-28 163. (MIRA 16t8)
1. Ivanovskiy energeticheskiy institut imeni V.I.Lenina.
(Peat-Drying) (Insulating materials)

iO,,YLUVp B.S. (Io-~aingrad); HIMAYLUV A.S. (Uningrad)
kXfect of hydrogen on the tendency of titanium alloyo to delayed
cracking. Izv. All S,jit. Utd. tok1j. nauk. 3-it. i gor. delo
J"F 163. (Uiit 16.3)
(Titanium alloys-Hydrogon content)
10
iz:!K

ACCESSION NR: AT4oO7O34 S/2598/63/000/0)0/0)44/0150
AUTHOR: Mlkhaylov, A. S..; Kry*lov, 04 S.
TITLE: Effect of hydrogen on the tendency of titanium alloys to delayed fracture
SOURCE: AN SSSR. Institut metailurgli. Titan I yego splavy*, no. 10, 1963.
Issledovaniya titanovy*kh splavov, 144-150
TOPIC TAGS: titanium alloy, VT-5-1 titanium alloy, TIM sub 4 Sn sub 6 Cu sub
2 alloy, OT-4 titanium alloy, VT-4 titanium filloy, OT-4-2 titanium alloy, ATA
titanium alloy, VT-6 titanium alloy, VT-14 titanium alloy, titanium alloy strength,
titanium alloy ductility, titanium alloy delayed cracking, titanium alloy hydro-
gen content, titanium alloy weld strength, titanium alloy weld ductility, wold.
delayed fracture
ABSTRACT: The present work was carried out because no data are available on the
tendency to delayed cracking In TI alloys. Delayed cracking was studied on un-
welded and welded specimens by the method of prolonged bending. Three modifica-
tions of this method were tested. in the first the bending produced stresses In
the external fibers of the specimen equal to 0.6 times the modulus of elasticity
during bending. In the 2 other modifications, the Intiial bending produced stres-
ses In the external fibers equal to 0.5 times the modulus of elasticity, the
Card 1/2

ACCESSION NR: AT4007034
stress being increased every 24 hours by 0.1 mm in the second modification and by
0.2 mm In the third. 'rho second and third modifications proved more sensitive.
The relationship between delayed cracking and the H content was Investigated after,
vacuum annealing, when the H content dropped below 0.002%, and after saturation
with H up to 0-005-0-03%. Saturation with H was carried out by the thermodiffusion
method at 700C. It was proved that an increase In the H content may cause delayed
cracking. The resistance to cracking of the welded specimens was generally lower
than that of the basic alloy. Only In the VT-14 and T-4 alloys was this resis-
tance higher for the welded specimens than for the basic metal. All alloys test-
ed of the a and a + 13 structures showed delayed cracking above a critical H con-
tent, depending on the presence of the hydride phase of Ti. It was found that de-
layed cracking of the alloys VT-5-1, TiAI14SA6CuZ, OTA and VT-14, used for wald-
ed construction, can be predicted by reducing the H content of these alloys be-
low 0.015%. Orig. art'. has: 2 figures and 3 tables.
ASSOCIATION: INSTITUT METALLURGII AN SSSR (Institute of Metallurgy AN SSSR)
SUBMITTED: 00
ED * '
SU'M'L
L
ODE_ 14L
SUB CODE: ML
SUa
Card 2/2
DATE ACQ: 270ec63
NO REF SOV: 002
ENCL: 00
OTHER: 003

ACCZSSION MRs AT4007037 8/2390/63/000/010/0139/0167
AUTHORi-_ 1~7~ I Be so
lov
TITL& Kinetic# of ;Vdrogen evolution from titanium and its alloys in a
vacuum
SOURCM AN SSSR. Institut metallurSti. Titan L yego splavy*, no. lOj 1963,
Ilsoledovaniya titanovy*kh splavov, 159-167
TOPIC TAGS: titanium alloy, titanium, solid state degassing, solid titanium
degassing, hydrogen evolution, vacuum degavoinS, titanium alloy degassing,
VT-l alloy degassing, OT-4 alloy degassing, degassing
ABSTRACT: Hydrogen outgassing of c arcially pure titanium and of titanium
alloy OT-4 in a vacuum wto investigated at temperatures fra~A 600 to 1000C. Test
specimens measuring lOmmJ, 1.5 x 10 x 19 mm, and 3.0 x 10 z 19 mm were heated to
700C and suffused with hydrogen at four concentrations: 0.015%, 0.030%, 0.050%
and 0.100% Specimens vote transferred to an environmental chamber which was
evacuated i0 5 x 10-41 mm HS, and exposed at 600, 650, 700, 750, 800k 900 and IOOOC
until outgassing ceased. Above 650C. hydrogen evolves briskly at a rate IncressinS
1/2

ACCESSION NR: AT4007037
with teWerature, and also increasing directly in relation to origLnal hydrogen
content. Cc-Ni electroplating or oxide conversion coating markedly decrease$
the degassing rate. Neither specimen sisal up to 10 mm thick, nor distribution
of hydrogen affect the deposing rate. Orig. art. has: 4 photcmicrographas 1
schematic, and 14 graphs.
ASSMIATIONs UstLtut metallureLL AN SSSR (Metallurgical Institute AN SSSR)
SUBMITUDs 00 DATE AOQt 27Dec63 WMI 00
SUB 00DE t MM 50 RSIF GOVt 000 OTRZRt 000
CWd 2/2
5,
Z~

KRYLOV, B.S.
Some replaritias in con"ative drying of insulating peat slaba. Inah,-
fiz. zhur. 7 no.203-37 F 164. (MIRA 17s2)
1. Energetichaskiy institut imeni Lenin[, Ivanovo.
VI

MIKFAM071 A.S.- ' Ov B S.
Effect of hydrogen on the tendawy of titani= allo..-s tomrd delayed
crackinge Titan i ego splavy no.10il/.4-148 '63* (14IRA 17:1)

KRYLOV, B.S.
,
Kalposition of the thyroid gland. Test.khir. 77 no.3:115 Kr 156.
(XLRk 9:7)
1. Is kliniki bolesney ukha, gorla I nos& (nachallnik professor
VA.Voyachek) Voyeano-meditsinskoy ordena Lenin& akademit imeni
S.K.Kirova.
(TMOID OLM--ABUCRITIW AND DIMMIMS-DISRAS )

IRYWV, B.S. ManinvaA)
Now modif loot ton of tympanoplasty us Ing a f Iola (with BUMMS27 in IngliGhl
Vaot.oto-rin, 21 no.IsI13-116 Jap-7 159 (MIRA 12:1)
1. lz kliniki bolazne7 ukhai gorls, i nos& (nach. - zaslyshanm
dayntell nauki profe XeLe Mi lov) Voa7nno-meditalnskc7 xkadamii Im.
S*Xo lirovai
(TWANIG KWR=o surge
non-free ty-mpanoplAntyt modified technio (Rus))
TVI,-16 il~'~~,11--~1111.

KRYLOV,.B.S.
Use of cortisone in lo-yngoplasty. Vaototorin. no*5:35-41 162o
(MIRA 15:9)
1. Is kafedry bolezney ukhaq gorla, i mosa (nach. - zaaluzbennyy
dayntell nauki prof. K.L. Khilov) Voyanno-meditaimkoy ordena
Ionina akademil, imeni SoM. Kirovap laningrad.
(CORTISONE) (LARrNX-SURGEMY)

. ~i.~ .. -~ -1 ,T
. . ~ E., -~~ 1 1: 1
. . - - - -- - - -- -V
...... KRYLOVY BIS,
Kinetics of hydrogen liberation in v*Auum from titanium materials.
Titan i ego OPlaVt n&.101159-167 163. (MIRA 171l)

KRYLO
V , insh.
Heat and mass tmnxfer in convective drying peat insulating
plates* Izve vyno Ucheb. zav.; energ. 7 no.2:64-68 F 164.
(MIRA 1713)
1. Ivanovskiy energeticheakAy inatitut imeni V.I. Lamina.
Predstavlena kafedroy promyshlennoy teplotekhniki.

KRYLOV, B.S.; PYATACIIKOV,, B.I.; ROVANOVA, T.M.
Principal factors bearing on the drying or peat-insulating slabs.
Inzh.-fiz. zhur. no.10:56-61 0 164.
(MIRA 171ll)
1. Energeticheskiy Institut imeni bonina, Ivanovo.

B lkrnmik mud. allizIlb.",
Improving the orgqnlzation of otorhlnojbr;~ngOjO4jf,
_ :3C-TVJSe to Q,
irm-A rorces of the no.()~T-94 161'. e
(M.MA 18,, i)
J1,

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I . r . j - :--t ~-~ ~ ~ I ~ : -
. - - - - I -..- .1 ". I . .-I ~ .1 - 1~ , 11 1 . - ---
- I --" ~ . --- ,, .1. - I . I c- T- ---
KRYLOV; B*S.,, kand, mod. nvLulx,, podpolkovnik meditsinskory sluzhby
Early restorative surgery in otorhinolarpgological lesions.
Vocne-med. zhur. no*3:50-52 165. (MIRA 18ill)