SCIENTIFIC ABSTRACT NIKONOROVA, A. I. - NIKONOV, A. P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001137220008-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: August 1, 2000
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SOV/137-58-8-17675
The Effect of Preliminary Plastic Deformation (cont. )
action of PD on the MT is a function not only of the degree of the PD, but of the
plastic-elastic properties of the initial phase as well.
1. Chrmium-irm-nikel &UM-4nalysis M. Sh.
2. Martensite-Transformations
3. HartenAte Deforeation
4. WUnsite-Temparaturs factors
Card 3/3

SOV/1-17-58,8 17676
Translation from: Referativnyy zhurnal, Metallurgiltio, 1958, Nr 8, p 211 (USSR)
AUTHORS: Maksimova, O.P.,A44.onorova-, A.I,__~
TITLE: On the Incubation Period in Martensite Tranoitormation (Ob
inkubutsionnom periode pri martensitnom pre--rashchenii)
?ERIODICAL- Sh. tr. In -t metalloved. i. fiz. metallo-, Tsent r. i. in -ta
chernoy metallurgii, 1958, Vol 5, pp 56-65
ABSTRACT: The authors describe the process of martens3le transforma
tion (MT) by considering it as a phase transition in a
component system. Unlike the usual phase transicrmations
which are characterized by a %-cry slow Ti;t,al ptejlrvs~ (JA;rinp
isothermal exposure followed by a gradual increase n raic
the transformation rate during isothermal MT ;s at a maximum
Inillillly and decreases subsequently as the time of exposure is
inc rea sed lioveNer, the process of isothermal MT proceeding
at an increasing rate may be observed during phase hardening,
as well as in the presence of very small degrees of supercooling.
In the alloy N23G), at a small degree of supercooling. isother-
mal MT is preceded by an incubation period, The phase nard-
Card I/Z ening of this alloy (with concurrent transformation of 10$0 of

SOV/ 117 - 58 - 8 - 17676
On the Incubation Period in Martensite Transformation
austenite) results in a condition in which the incubation period is apparent
throughout the entire interval of the mr. The duration of the incubation period
is at a minimum when the degree of supercooling corresponds to the maximum
rate of progress of the process. An incubation period daring the MT became
evident in the case of certain other alloys also. During investigations of the
Khl7N8 alloy it was established that the time of approach to the isotherm
located in the vicinity of the martensite point affects the rate of subsequent
isothermal MT. It is assumed that no significant temperature lag exists be-
tween the surface and the center of a specimen during its cooling.
1. Hnrtensite-Transformations M. Sh.
Card Z/z

117-59-6-IIZ68
Translation from: Referativnyy thurnal. Metallurgiya. 1958, Nr 6. p 300 (USSR)
AUTHORS: Maksimova, O.P., Golovchiner, Ya.M., Lyubov, B.Ya.,
TITLE: Fundamental Trends in Investigations of the Theory of Mar-
tensite Transformation (0snovnyye napravleftiy4 issledovahiy
v obigisti teorii martensitnykh prevrashcheniyj
A-
PERIODICAL: Sb. tr. In-t metalloved. i fiz. metallov Tsentr. n.-i. in-ta
chernoy metallurgii, Trans. Amer. Soc. Metals, 1957,
Nr 49, pp W-444. Discuss. 1958, Vol 5, pp 147-160
A13STRACT: Fundamental problems of the study of laws governing the
martensite transformation (MT), the effect of various factors
on it. and the control of the process of MT, also means and
methods for the investigation of MT are formulated. Biblio-
graphy- 80 references.
L. V.
I. Martensite-Analysis 2. Martensite-Theory 3, I*tals--Trans-
formations
Card 1/1

SOV/126-6-1-12/33
AUTHORS: Kurdy=ov, G. V., Maksimova, 0. P., JUknorova, A. I.,
Pavlenko, 75. D.,and Yaapollskiy, A. K.
TITLE: Influence of Preliminary Plastic Deformation on the
Kartensitic Transformation in the Alloy re-Cr-Ni
Miyanlye predvaritellnoy plasticheskoy deformateli
na martensitnoye prevrashcheniye v splave Fe-Cr-Ni)
PERIODICAL: Fizika Metallov I Metallovedenlye, 1958, Vol 6, Nr 1,
pp 95-105 (USSR)
ABSTRACT: The results are described or experiments carried out for
elucidating the finer reaturee of the influence of plastic
deformation and subsequent a=ealtrtG on the narteasite
transformation In Fe-Cr-Ni alloys of the type Kbl8N8.
The aim was to establish the activatiag effect of
deformation in such an alloy and to verify the validity
of the assumption of the activating W luence of stresses
on the martanaitic transformatioa or deformed austenite.
ror this it was necensary to study the character of
elir.;ination of the after effects of deformation with
gradually Increasing annealing temneratu-.,e; in view or
the possible super-position of diffusion processes onto
Card 1/8 the processes of stress elininatioa during annealing,

SOV/126-6-1-12/33
raflueace of Frellmittary Plastic Defomation on the L'artensitic
Transformation in the Alloy Fe-Cr-Ni
such Investigations could not be effected on steel,
If the assumption on the favourable influence of ntressen
on the martensitic transformation of deformed austenite
would be correctV the effect of activation should. be
eliminated in the case of heating In the range of
relatively low temperatures. Another aim of the
described work was to study the influence of deformation
on the Isothermal martensitic transformation for the
purpose of elucidating the ch-n-rReterintic features of
the changes in the kinetics caused by the Influence of
the activating and/or the braking effects of deformation,
Si-ce the activating influence of deformation can only
be detected in alloys with hiei elasticity values. it
was decided to carry out the erperiments on the alloy
KUM ~0:03% C, 18.10% Gr 8.1% MI) and the alloy
KhlM 0 0% C, 17.25% Gr: 9,16% Ni), both of which are
similar In composition and as re6ards the martensitic
point, On the alloy Khl8Y8 the inLfluence of defornation
and subsequent heating for obtaininF, martencitic
transformation durink; cooline wan Gtudif!d, whilet on the
Card 2/8 alloy Khl7N9 the influence of defornation on the Inothe.-Al

SOV/126-G-1-12/33
Influence of Preliminary Plastic Deformation on the Martenf3itiC
Transformation in the Alloy Fe-Cr-Ni
martenaitic transformation waa studied. InvestiKationa
were carried out on flat 3.5 x 5.5 x 25.5 mm npecimens
which after nanufqature were subjected to diffusion
annealing at 1150-0 for ton hours. The plastic deforma-
tioa was effected by compression by negns of a press
at room tempergture, at 100 and at 175 G. Deformation
at 100 and 175"'C was effected inside a special sleeve
fitted with a heater wending ; as a medium for enaurin&
the temperature of.100 C boiling water was used, whilst
deformation at 175 C was effected in Slycerine.
Evaluation of the change of the ability of the austenite
to become transformed into martensite was effected by
means of the thermo-magne8ic method by plotting the 0
curves of cooling ~o -196 C and subsequent heating to 20 C
with a speed of 10 C/min. Ao the basic criterion of the
stability of the austenite, the total transform'ition effect
was chosen which was obtained as a result of cooling and
heating. The change in the fine structure of the
austenite during the plastic defornation and during the
msxd 3/8 subsequent heating was investigated by the X-ray nethod

SOV/126-6-1-12/53
Influence of Preliminary Plastic Deformiation on the Uartensitic
Transformation In the Alloy Fe-Cr-Ifi
by measuring the width of the line (311). As a
characteristic of the state of the Gtructure of the
austenite (Type 11 stresses, dimensions of the blocks
and coherent scatterine), the magnitude of physical
widening of the (311) austoaite lines was chosea. Tn
Fig.1 the tran5formati8n of the austent.to into martenfi~ 1'~
during cooling to -19G C and eubsequent heating, to +20 C
Is graphed after various degrees of preliminary plastic
deformation at roon temperature for the alloy KhlBN3-,
in Fig.2 the same relatJon Is greLphed for the Ocase Of
deformiations taking place at lOVG and at 175 C, In
Fig.3 the change of the total effect of martensitic
tranefor-mation ac a function of the iegrec of
plastic deformetion Js graphed for various temperatures
of preliainary deformation for the alloy Kh!81;3. In
Fig.4 the influence of the annealing teaperature on the
transfo&mation of the defoged austenite during coolinr,
to -196 C an4 heating to 20 C 0is graphed for various
degrees of deformation at 100 C (alloy KblBN8). In Fig~5
Card 4/8 the change of the widening of the line (311) of the

SoV/126-6-1-12/33
Influence of Preliminary Plastic Deformation on the Martensitic
Transformation in the Alloy Fe-Cr-Ni
austenite of the total effect of martenaitic tranaforma-
tion (during cooling and during heating) and the change
of the martensitic point are graphed as functions of the
annealing temperature gor specimens of the KhlBNB alloy
deformed by 10% at 100 C. In Fig.6 the temperature
dependence of the Initial speed and the total effect of
isothermal martensitic transformation are graphed for
non-deformed and deformed (8 agd 17%) states for a
deformation temperature of 100 C (alloy Khl7N9). It was
found that depending on the conditions of deformation
and annealing, plastic deformation can have an activating
or a braking effect on the martensiLic transformation,
Small degrees of deformation activate the transformation,
i.e. widen the teiperaturu rar.Se of the transformation,
bring about an increase of the initial speed of the
isothermal transformation and of the total quant-it~ f-,f
the martensitic phase. Various changes In the fine
crystalline structure of the austanito may lead either
to easier formation of martensite nuclei during subsequent
Card 5/acooling or maj impede their formation. For small degrees

BOV/126-6-1-12/3A
Influence of Preliminary Plastic Deformation oa the Martensitic'
Transformation in the Alloy Fe-Cr-Ni
or plastic deformation those structural changes will
occur to an IncreAsing extent which bring about the
formation of germinations. However, even at such
degrees of deformation changes occur in the austeaite
which impede transformation. With increasing degree of
deformation and also with increasing deformation
temperature, the changes In the structure which bring
about braking of the treaaformations increase in
importance. The changaiia the fine crystalline
structure. *tch ativate the transformationwe eliminated
at relatively low annealing temperatures at which the
width of interference linos does not yet change,, I.e, whj-lqt
there are s"Jill no Important changes In the mai;nitude of
the Type 11 distortions or In the dimensions of the
areas of coherent scattering. Changes in the structure
braking the formation of germinations we maintained
thereby; elimination of these takes place only at higher
temperatures corresponding to the region of decrease In
the degree of blurring of the lines. It is not possible
ard 6/ as yet to establish those details of the fine structure

SOV/126-6-1-12/33
Influence of-Preliminary Plastic Deformation on the Martensitic
Transformation in the Alloy Fe-Cr-Ki
which favour the formation of martensite germinations and
those which impede their formation. Comparison of the
results relating to the influence of plastic deformation
on the sarteasitic transformation in Fe-NI-Un and
Fe-Cr-Ni systems leads to the conclusion that the Intensity
of'the deformation caused changes of structural factors
depends on the elastic-plastic properties or the austenite,
The relation between the changes bringing about activation
and braking of the aartensitic transformations may differ
depending not only on the degree of deformation but also
on the elastic-plastic properties of the initial phase,
As a result of this an unequal character of the effects
of plastic deformation on the martensitic traiisformation
Card 7/8

SOII/126-6-1-12/53
Influence of Preliminar7 Plastic Deformation on the Martensitic
Tranaformation in the Alloy Fe-Cr-Ni
was observed in various oaterials.
There are 6 figures and 11 references, 9 of which are
Soviet, I German, 1 English,
ASSOCUTIOU: Taentrall W nauchno-iseledovatel'skiy inst-Itut
chernoy metallurgii (The Central Res"rah rhOltuto of
remAn Notanurcy)
SUBMITTED: March 21, 1957
Card 8/8 1. Chromium- Iron-nickel aljoya--Transformavians 2. Chmailm-
Iron-nickel alloys-Deforantion 3. Chromium-tron-rickel
alloys-I'leat tre&tment

7,5-0 0 9/180/60/000/02/014/028
9111/9152
AUTHORS: Zakher, LMep KakslMova 0 P NikonoroV& A
vl_ TWT'k".M-*T*'e*os
PlemYanatkova, I.K., aini Yax*r'l'vk1 - cow)
TITLZ: Study of the Austenite Stabilization Effect in Phase
PZRIODICAL: Izvestiya Akademli nauk SUR, OtdeleaJye tekhaicheakikh
naakp Kotallurglya I toplivo? 194-0,Nr 2, PP 93-100
+ KftA 01058R)
i~
ABSTRLOT; The authors suggest that the Important probilem of gamma-
phase stabilization should be to Include the
actloa of any factor which raises stability without
r;hanging the chemical composition of the austenite
(Refs 1-8). One of these is internal work hardening due
to the ma-tensite transformation Itsftlf (Hof 9), which has
been deso.:Ibed by Golovehiner. and Tu.D. Tyapkin, and by
Golovchiner and Landa (Ref 10). In superlavar alloy
Kaksimova and Golovchiner found a "super-stabilization"
effect for austenite with respect to the martensite
transformation In subsequent cooling, In the present work
the aim was to find: the Influence of varioys degrees of
Card
1/4 phase work hardening on gustenite stabili.tV kinetics of
isothermal transformtjo and the micro- and submicro-
A

69658
V180/60/000/02/014/028
till/X152
11tudy of the Austenito Eltabilization Kffect la Phase Work Hardening
atructur* of austenits; the rults governing the removal
of the efficts of this phenomenon during subsequent
annealing at gradually, increasing temperatures; the
changes In martensite trawformation, kinetics produced
by phase work hardening in contrast to those produced by
a different rort of effect, e.g. plastic deformation or
high-energy, particle irradiation. TWO types Of &110AY'
were used; Fe-Ki-Kn Q 8);
gLG3Y(and Fe-Cr-Ni (Xhl7K
their respectire, compositions teing 0.069 GM"; 23.1+59
8.4o% Ki; 3-3(79 4 Kn; -, 17-34% Cr. Thex4 had been
studied widely in connection with austenite stability and
fine crystal structure (Refs 5-7,~ 12). The inyastigation
involved thermomagnetio, X-ray, ttler.-pstractureVand
miarchardness methods.. The experlmenEU -conittions
chosen in the present work are represeated In Fig 1.
Phase work hardening was produced ty cooling to a low
temperature followed by heating In a tin bath to the
Card lowest temperature at which the reverse martensite
2A transition is completed; the heating conditions ensured
that a martensite mechanism governed the alpha to gamma

9/180/60/000/02/014/028
2111/9152
Study of the Anstenite Stabilization Effealt 1n Phase Work ffard*alng
transfo=atioa. Fie 3 give3 the influence oal degree of
phase wolrk hardening on the martenatte transformation on
subsequent coolingv while Pigs 4 &r-1 5 give for t1he
rxickel and the chromium allrivs. respectively, isothermal
martgnsite transformation cur-.es for the initial and
phase wo-:k-hardenel states. Figs 6 artz' '," give, for the
same allcys zespe,~-tl-,917, the inflaence of phase wr.).-k
hardening on the starting rate of the isothermal.
marteasite transformation (cur-s3 a) and on the overall
effect of the trans formation. In Fig 8 the influftnee of
annealing 111'emperature on the state rf N23G3 subjeot6d t.;
difforent degrees of phase vorK tardenIng is shown, while
Fig 9 3hows effects for nd7NO &I-Icy subleated to a 40%
pr-ase work hardeaing. Figs 10 and 1-1 show for the two
alloys, respectively, microstructures at different stages
of stabilization treatment and the nature of the
martensite formed in subsequent cooling. The w3rk
Card showed that for both alloys phase work hardoning depressas
3/4 the wtrue* martensite point and the temperature range of
the transformation, reduoing its initial rate; extornal /

69656
6/180/60/000/02/014/028
11DIII 52
SWdy of the Austenite liftbilization Effect in Phase Work Hardening
work hardening has different effects on the two alloys
(Ref 7). The observed changes in kinetics (similar to
those produced by stabilizing plastic deformation) can be
explained by. the relatively high tomperaturerequir*d for
the rovers* martensite transformation, which makes it
impossible to retain those changes In austonite fin*
structure which favour forma-tion of m&rtansite nualti.
Phase work hardening was found to produce oxt*nsion of
structural faults in adjacent austenits zon*v decrease in
marten-vite grain size andt to some extent, relative
stability or some austenite zones. rn general, the
changes produced are very stable (disappearing at 1100-
Card 1150 OC); their removal on raising the temp*raturo takes
IfA ~tlaa* in a stopwist mann,&r.
or@ are 11 figuret, 1 table and 15 references, of which
1I+ are goviet and I is English, J/
WBKITTED: JUY 30t 1959

NUONOROVAt A.I. (HoakviL)
KL*Gtt"qogr%*ic study of work perforimed at different
tSqM~ withLA tAe sam range of power, Glg* trWa I
prof. sab. 6 mi.W-13 VqI62. (HUA l6cS)
I., &stltat g1glyany truda L proressionallrqkh zabolevanly
ANN SM. (5=TROMrW-FAMY) (STP= (PMIOLOGT))

Ummugg X,Lo# kand. takhn. nauk; KIKQMgg".jjL, kand. tekhn. nauk;
CLADYSHETO S.A.j insh.; WU-n(3VAt UX.-t-Insh.1 SCOCLEVA, M.P.,
lash,
Stainless steel for thin-walled c4sttngs, Lit. prolzv. no.11i
3-5 9 165. OaKA M12)

ACC UR, kt6012412 SQUW,.E CODES URPOWAVOW/WO/0329/0333
AUTHORSI Hikonorova, A. L; Sineonov, S. L.; Karabasova, L4 V.; DuWvaya,,_,G. Vq
I Sobolevaj,-W.-r-o
0 RG t no as
TITIZs Goofficiont of linear Wansion of imlustrial titaaim
SOURCZs Sove"hw4ye pa mst&Uokftin1Lj, matallovad4niyu I prim*neniyu tit-ans, i YVg*
splavoV, 6th, Havyye isslodoveniya titanov*h splayov (New'research on titanium
alloys); tmdy soveshchaniyaq Moscow, ltd-vo Hauka, 1965,, 329-333
TOPIC TAGS: expansion coefficient, titanium alloy, astal property / 7-11-1 ti*.Qn4A.U--4
alloy
AB3T?J4?s To determine the cause of the large scatter 1 65) of the
coefficient of linear expan3ion 0( ~,,otn c;ef ficien* and
-91 titanium alloys, the Piro&nq , V
texture of the corresponding were investigated on Wl-l'specizens. The
coefficient of linear egansiostl.
n was mesaured over the tw43erature interval of 20--
00C w1t-h a Matoaotor,, while the texture was doterainod by the x-ray method. Ue
coefficient of linear expansion was significantly affected by the texture, with Wirea
types of texture dafinable with certain values of the epansion coefficients LT0127
=,'I-valood textwe corresponded to (90-10.3) x 10-0 I/degros; no definable
texture corresponded to (8.5-9.2) x 10-9; &rA L*mj larce-grained

L4wg,kl-66
ACC NRs AT 412
4exture corresponded to (7-3-8.4) x 10-6 I/degroe. It was founa tuat repeated
forging r drawIft (W% eformation for cold working, 60-60% deforms%S~on with
f0
intermediate ~A 600C) would provide a fWly unifam tvctuvi*~ith a
60
coetfloient of linear ion of 8.5 t 0.5 x 10-0 1/d4sm, dii-g, art. hast 9
L
fig4res and I table.
TJB COM Up 13/ SUBM DAM OZDec65/ ORIO REFs 001/ OTH W t 003

ZWT(d)P.*4T(m2,/4'JP(c )/ZW A( d )/07/EVP( t
4WP i
ACC NRi Got, 'F N17: UP/0129/65/ooo/oio/mi6/(>oi6
Florvnnova F. f~-
<
Fu-,,rpt(L~ Metk,,,1lurgIcal Combinv.- (Xi-atiptakly met"illtirgichenkly kombinat)
Effect of the melting conditionn. on the quality of rolled K)UP(TYu steel
plates and bars
Vetallovedeniye I termichcokRya obrnbotka n-,~tnllov, no. 10, 1965, 16.0
71-7"IC TACO : steel , &tainlngn stoej, preciritafj ~L Wl' steel melting
-Qn,.jj, n1caluc rtn,"
stcel Qj2ingq plate rolling, bar rolling/Khl7N7Yu st-el 1~
FAC in 1960 the Kuznetsk Metallurgical Cr7n!Anoi,
production of MIT1117Yu
~.,i,ec4'.pitn.ti.on-),,ardenable steel plnter, C-L5 r-~i -Lnd round barz 100-110 = In
Initially the steel wrin m---ltPd fron, scra- I t
11 q a )riri:! arc fux-nace vith the
-"c of oxygen, but, the steel waa of lnro~rior I I ty 7-herefore, In 1963 the plant
8,'-) kg carbon 6teel scrap,
c,~,anFed. to the virgin-chftrge process, using 75 n
k;T, ircri cre, and 21 kg lime per ton. The virFin-ch%rge process yielded metal of
much bLt;vr quality, hot tears were elirvinatel completely, rejects owing to Unsatic-
frxturj chemice,1 composition were redue-ed fron ~-',.7'4 to 6%, ani the ingot consumption
vcis red,u,~vd from 3.11 t,,) 2.01 kg por kg, of fininhed pro!Iuct. Olabs ani billets are
conditioncd by rmcl7ining and heated for rolling to 12&D-13100C azid 1270-1280C, re- L
Keating to a lower temperature produced unoatisfartory results. I
TN*D1
art. hr.A, 2 figures.
C,
76 7

L 6482-641
z ACC NR, Ap,
I
I SL7,- CODE.-
1 ftlt$
1 Card- _Zjj~._
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2 /SWA P~C) J bl';U
ulo~ .6
ACC NRt AP$008863 SOURCE CODE.- UR/0128/65/OW/01110003/
AUTHOR: Oeokin M. It. (Candidate of technical sc1anc#P);.j1~onor=0-,'A----A-
(Candidtttq of technical sciences); Q,1adyatLey,__g,_&t (Engineer) Gtgjg~ x4j--L-
(Enginear); V& N. P. (Engineer)
ev~
ORG: nont
TITLk Stainless steel for thin-valled castings
SOURCE: Lit*ynoye zvodstvo, no. 11, 1965, 3-5
Prod
TOPIC TAGS: metal casting, martendite ateol, copper, corrosion resistance, tomporrID9t
au3t,anitlc fltnolt st-nel, stainlens at--ol/ rKh15ua)3r, atainleas nt-r!l, 35L atl~el
A B STRACT -, T'he steel used for thin-walled and intricate castings of parts of preci-
ubDn maiJklm:y and devices must display a filgh registnticc to attnosplipric corronion
wit'hout rqquLritir a prOLCCtiVO Co,itlng,, a natisfactury fluility, a high dtr.--4~niional
StIbility, adCqUF1tC phyajC0-M.(.-ch-inicvJ properties, and a satinfactory wiichinability.
011 the itnndord stninlega steels not one natisfies t1w entire Mrr. 4U'r Lhet;e rey) irement,4
Cr-111 a-isten[tic steels Nava a high COrrOCAOtl VAiStOnCC U-3t -1 4~w 11UWiLY, While
r.artenal.tic-rlaas steels have n low torroston rituintance but tin nsufficient fluidity.
Henca it is normally necessary to employ for these purposes 3"L steal despita the
highly -undesirable necensity of coating it electrache=Lcally with zllnc. Of the elemnL~-
-4.045.,-669.14,018.8
C.'d 1/2 -6 21. 7

ArC MR, AP6008863
enhancing the fluidity of stainless steels, Cu Is the tzo-st effective. In this con-
nection, tix ineltzi of the newly developed OKMM401, r-irtennitic stainless steel (up
to 0.081, C, 0.8X St, 0.77. Mn, 14.5-177, Cr, 3-47. Ni and 3-4% Ou) were teSLed for flu-
Idity, as v function of temr~eraLura and shape of metal. Tests of varloua intricate
thin-wallrd ('A.5 m thick) ca5tings confirmt-d the definitely aatirfnctory cAsting pro-
perties of this steel -- high fluidity and absence of hot cracking. Since Steels used
for thiti-1--alled And precision castingg also must satisfy hiLli requirementa With re-
spect to corrosion resistance In non-conted state, high dimcnsion4l st)bility; and
tiachinallility ~;theae properties were also investigated fC1rjKh15V4D3L! teel a com-
p:ired wit1.1 35,jt~steel. Findings: tho dimensional stabiliLy u~-&-E-N7,16h steel in such
that, after its air quenching fr(,m 1020%, 2-hr treatmitnt with cold at -70*C and 2-hr
ter-pering ot 600*C, this steel ruirains stable In tir-,e evnn In thp. presence of tenpe-
rarure fluctuations of from +150'C to -40*C. Compared with 35L Atual, O%J1l5?;44D3L steel
'displays superior strength properties (1.5-2 times higher) an well an superior cor-
-,rosion renistance and superior mixtitnability (30-140% higher). Viva 001111(031, steel
.inay be accepted as a replacement for 35L ateel.wh %ich praviously had to Le used for
L I
:this purpose. OrIg. art. has: 6 figures, 4 tables.
SUB CODE% 11, 13 SUBH DATE: none/ ORIC RM 00
212 "t,*

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3peatr%*9tonstric determinatton *f wthyl d -nmOtbyl&mt&t* In
potatoes* Chm amd Is no.5/6925-937 059o (=I M)
1, Voiskove Centralne Labovatcrium Sardtamo.-Higionleam,
Warname,
(dpmctrophoto~try) (Notby1naphthalerisacetic acid)
(Potatoes)

NUONOJWWl, K&ksyat GWIERTNUOKL, EmULA; KAIIIINSKI, Alfred
A masoma mooed for the determination of aur residus on the aurface
and insW sherry fr%Lts. A4t& pol. pharm. 18 no.6t465-01 161.
1. Z So"u Ba&nf- Srmmoi L Prsedolotaw Uzytku M I WoJakovego
Imstrtatu HIgisvq L Npidonialogli v Warsualo.
(DOT ohm) (MIT)

GWIE;ftTWIZW3tA,r Z.f KIKONUMg K.[ KOSLIlkli,
Studies on the.DDT rooldvam aborry
cherry fruit fly (F-hagolatis aorut
no.3t533-547 162.
K.f, LLS11, R.
fmit sprapd against ttio
L.). Roca auk "In roal 96

I , .~7 - ST J. ,
37YK"~'YK F. I nz.; ~ ~ A., ;-,*,.-,f . ';-, X. . -,-!r,. . . , . ~-,y ,
P I ----
pruIr .dr? M , prr;!'. -!r
Works ant R-:hl-vec fitm 'In piibllz r~yplnti-t f"17,-Wi *tl,14
period of thr, PcIlch Perplol's RepAbllcc. P-:- p-mat zul
15 no.41317-,347 1 ~,4 ~

KASHEIIHLEBDV, I.F.; Wr-SKMVA, P.H.j KIKONOV, A.A,; OLZVMIKCV, G.B.;
PESTLOV, G.S.; SIKEWBOV, N.A.-i-TREYMp A.M.; TULrAKOV, B.V.,
Lash.; USTMTICR, B.P.; FUMAWT, A.V., rttseusmt; XIKIFO[IDV,
V.S., red.1 SAMTSKAYA, G.I., red.lzd-va; GALCUSAMU, V.I.,
takhm. red.
(munal on turpostiainel Spravochalks podsochka lasa. Pod ob-
abehal red. S.V.Ttiltakovs. vlaskva, Goolssbmlsdat, 1962. 334 p.
(MIRA 160)
(TurpentlaUg)

115pecialization and Concentration or Production In the 5ovkhozes
of Litvian SIR";
dlevertaUon for Ow dkigroe of Candidate of Economic Sciences
(rims.-ded L7 tke Ttmdri"mv AgriculturnX AoadwW, 1%2)
(ravoettym Timdr7anewskay S4$skektwcm*tvmww7 AkademiLj, Moscoug No. 20
1963p pp 232-236)

NIMOVe A.A.
Ultimate howt toads for steam-heated ow-foces of wriss
bitlers. IvAostrovate 24 so* 6t2l-Z5 Je 158., (KM Ills)
(Botlare, MartsO

MONOT, &.A., kand.tekhm.nauk
tvaluattag the operattowl reliability of evaporative beattaC
surfaces of wrise steam botlqrs, Sudostroesto 24 w.7:31-34
A 153. (MIA Ilig)
(Boilers. Marine)

91--QMV, L.A.
Characteristics of the last Clactation moralme In western SapUnd.
lev. Mar. I roll. f1l. AN SM no.2:62-74 158. (KIWA UC9)
1,0selogIchooldy Institut Zollekqp f1liala AN SSSR.
(Zapland-ftrain4a)

NIEDIDT, AA.
IRMIUVAtW a to t
~ . " .1 n 'twioglacial deposits of the western Ula
PONINGula- IST-Far, I roll-til-AN 5382 so-3:43-45 1 58.
(NIIA M12)
1. Geoldgicholkly Institut rel'skogo filial& -is SM.
(Zola Pentneula-4ooloff. Strmetural)

.30)
AUTHORSo Ylkonov, A. A.9 Cheremisinova, Ye. A. 30T1/20-125-3-43/54
TITLEt Recent Data on Late and Poatglacial Marine Basine in the
Western Part of the 'Ma Peninsula (Novyye dannyye o
pozdne- i poslelednikovykh morskikh basseynakh na zapade
KolOskogo poluostrova)
PERIODICALs Doklady Akademii nauk SSSRt 19581 Vol 10, Nr 3t PP 530-535
(USSR)
ABSTRACTs 11he recent land forms and the formation and distribution of
glacial deposits in the Kola peninstila, and likewise in the
other marginal areas of Fonnoscaltdi& 9 were determined in post-
glacial time by the combined effects of the shrinking ice nerer,
the iaostatic uplifts, and the fluctuations of the sea le791.
The multipurpose investigations of the previously very slightly
knownp western mainland part of the peninsula have clarified
several questions which concern the troblem mentiored in 'he
title and have supplemented previous data (RefR 1-5)- The;e
glacial sediments mentioned in the title are distributed in
depressions as bands 1 to 6 km wide, which extend from the most
Card 1/4 and southwest toward the east and northoest. At present th;~y are

R
I
ecent Data on Late and Postglacial klarine Basins sov/2 4 3/r
in the Vestern Part )f the Kole Peninsula
encompassed by the Lotta and Nota Rivers and their tributaries,
the Yauri-yoki and Girvas- 3 distinct cabjes can be reicv,-,1izPdi
1. banded clays 2. stratif-'#ii clays, clayey and sanly soilr
fine-grained sand and sandy soil.. These sediment =asses
belong to 2 complexes: Fortlandiya and FcIao.-rortlandiya
complext The lithelogic composition is described, and a li,it ~,f
the diatom complexes found (Table 1), wli(-)- arch charactf!ristlo
of the Portlanliya seaq is given. The assemblage contains f::r,,ns
of various ecologies and origir~ss 1. species of a
gretic-alpine naturaq which live in the shallow bank z-nqs cf
northern lakes and rivers. 2. Salt water and narine elezirt7,
coastal zone inhabitants. Grour I is nu=erically pr,?do=i!,,nrt.
The Portlandiya ara was alwat r1mah. "allen of
'7 r:,
plants aM the uniershrubs (dwarf bir-,h - P~etula nana - 46-11,
heather - Ericaceae - 6 - 7 5) are predomirant among the 1,,Yllei
assemblages. Also found werevoyawwd pollen (Artemisia) and
pollen from orach(Atriplex). 77he componition of the s,-:,,recj 'As
variedt 6o46 abundant green moss cany ferns IPclypodI-,t,-rAe) an~,
club-moss PInnts (Lycorodinceaq~- 7hi-q compos'itIon iniic'sxtea
sparsely forested or forestless lanin ivytrf birch tu:lfeq
Card 214 and a 17~nvering of grass and nose in the area. Salt water ~f the

Pacent Data on lAte -tnd PostClacial Urine Basins 50712C-12~11-1-43154
n the Wostern Part .' the Kole Peninsula
11 1
Portlandlya transgression gradually invadei the Clailal wate7z.
However, the salinification did not advance very far int:) the
narrow xnd long ocean bays. The arrival of melt water fnim the
glaciei also worked against salinfication (Ref 2).
occurred chiefly in bay areas near the shore from erosicn of
moraine materials and from materials brought by the glaoial
melt waters. The suspended materials In the glacial waters were
deposited in the central pp~rts of the bays. Fresh water 4!atDc
species increased after the retreat of the Fortlandiya s-se.
Folas complext The chiefly fire, Cray sani forms narrow
(up to I km wide) bands in the axial parts of the depreas'A:,na.
Their thickness attains 15-20 m. Table 2 contains a list of the
diatom assemblages. Among them are many marine salt-water
inhabLtantat littoral and upper sublittoral dwellors. The
Polas sea was not more than 40-45 m deep. In the western
sootiona# which were farthdot from the open so&, the
assemblages are composed almost entirely of fresh-water forms.
Tres, species are predominant among the pollen assemblages (66~)j
Card 3/4

Recent Data on Late tnd Postglacial Marine Basins SOV/2C_121_-3-4"'/'"'
in the Western Part : the -Wldr* Peninsula
and grasses and undorshrubs comprise 22f. of the assemblage.
The ollaate was far milder, and fir-birch forests extenied.
go further transgressions have 006ur"d in this regie)n. There
are 2 tables and 6 references# 4 of which are Soviet.
ASSOCIATION: Geologicheakiy inatitut Kollskogo filiala Akademii nauk SSSR
(Geological Institute of the WWAM Branch of the Acadez7 of
Sclencesy USSR)
PRESENTEDo June 28, 1958, by D. 7, Nalivkinq we
SUBMITTEDs June 269 1958
Card 4/4

XIMMT, &,A*
Foatwes of the structurli of *skars and problow In the
paleogeography of areas of late glaciation In the sonthorn
part of the rechengs district. lzv. rwar. 1 toll M. AN SSSR
no.1:47-58 159. (Niu 12tg)
legoolegicheekly Inetitut Eollskage filiala. AN SSS%.
(Kola ftninsvila-41ekar)

'.. suawr1w.A.Ap-,.-
Sm work an problem to 4~zaternary glaciation. Icv.1ar.1 1(411.fil.
AN IM no.3il54-155 159. Mu 11-.4)
I* GoologIchookly InstItut rol'skogo filial& All SSSR.
(glaciers)

3(5)
AUTHOR: ..'91konov, A, A. 90V/20-125..4-50/14
TITLE: The Restordion of Neotoctonice and the Pal*ogoography of the
Late Glacial Period by Means of the gpeirogento Spectrum in
the Continental Part of the Kola Peninsulas (Toestanovienlye
noot*ktoniki I palsogeoerafli poadnolednikovIya a ponashohlyu
epeyrogoalcheakogo spektra v materikovoy chastl Kol'skogo
poluostro*
PERIODICAL: Doklady Akade2it nauk SSSR, 1959, Vol 125, Nr 4, pp 666 - 86)
USSR)

ABSTRACT: The spectrum mentioned In the title reflects objectively the
Interacti6n,,of the isontatio movements of the eart'A.04 cruat,
of the vanishine Clacial envelope, and the postelacial watern.
Thue, the paleogeographloal milieu can be restored and the
raise governing the recent structure of the reglon clarified
(Refs 1-3, 6). The hitherto existinC data are completed b '-,
the spectrum constructed by the author according to the Lott&
(Lottinskaya) depree sion (Fie 1) for the continental ;cart c!
the Kola peninsula (Kollekly poluostrov). Purthe-...ore, it
facilitates a new Interpretation of several complicated -ro%-
Card 1/4 Isms of the postglaoial paloogeography of the western part of

The Restoration of NeottCtonics and the Paleogeography SOT/2C-125-4-5:/7!
of the Late Glacial Period by Moans of the Epotrogento
Spoctrus In the Continental Part of the Kola Peninsula
the peninsula* The analyzes of the Dlatocaceae wore mostli
carried out by Y*e A. Cheremisinova,, the spore-pollen VOL-
lynes on the whole by.&* Me Lobedeva* No fauna, was founde ';'.c,
comparison of the height and the morphology of the levels ae
well an the stratigraphy of the sediments of the postglacial
waters made possible the synchronization of the levels of thc-
Lotta, depression with those of the Tuloma-gototerskaya depron-
sion the dating of which Is more prectoo (Rofs 1-3)., T'he tnttl
course of the torrace levels which second towards the wocat a:id
form a divergent bundle corresponds completely to the knoxn
rule on the highest elevation of the central parts of Fenno-
scandinaviso The specific property of the spectrum in luestivi
is its heterogeneity. It to expressed in the disturbances of
an *yen course of the levels which are accompanied by a silmul-
tansous variation of their morphology and their structure ftnd
by the vanishing ofthe upper level In the west@ 4 sections
can be separated In the spectrum which correspond to those in
the terrain: I - IT. In the Lotta, depression disjunctive Us-
Card 2A locations of the late-and postelactal period were found. Their

The Restoration of Neotoctonics and the Paleogoo- SOIF/20-125-4-50/74
graphy of the Late Glacial Period by Keane of the
Spelrogenic Spectrum In the Continental Part of the Kola Peninsula
elevation at that time took place with a different amplitude.
Such dislocations analogously dated by the archaeological neihod
have hitherto been known reliably only for the western part of
the Surman coast (Ref 6)e During the formation of all these
levels 1,h,g9F9e9d 5'd4 and d3 the waters spread durine an Iso-
static elevation of the terrain over the depression freed from
Lee as far as to the place whqre a c*rrosponding level had VL-
ntshe4. Her* the waters were stopped by the ice. Terminal mo-
raines and other traces of the activity of tha Ice lack for
this period. The character of the fluvio-Clacial formations at
the coast of the waters speaks In favor of an Ice which was
dead at that time. The Lee in the depression was apparently re-
duo*d mainly in consequence of the Influence of heat of the al-
jaoent sea. The discovery of & glacier marginal complet which
oresses the depression near the placa of the rapid vanishing Of
the mentioned coast level is In line with the conception can-
cernIng the *xIstence of the waters PortlandLa-Littorins, as well
as Pholas. Thus, the opinion concerninG the preserved activity
Card 3/4 of the ice during the late glacial period Is disprove4. On the

The Restoration or Nootectonics and the Palsogeography SOV/20-125-4-5-0/T4
of the Late Glacial Period by Keane of the EptiroGonic
Spectrum In the Continental Part of the Iola Peninsula
strength of the chronoloGy of Tanner (Hof 6) the PortlanflAa
transgression attained its maz1aus approximately 10#5C0 Yeft--s
ago. Thus, the elevation volocIty of the Lotta, depression
amounts In the west to 14 - 1.5 cahear, In the east 0.0 -
1.0 on/Year. There are I figure, and 6 references, 5 of which
are Soviet.
ASSOCUTION: Kol'skly filial Is. S. go Kirov& kkadocil nauk SUR (Kolft
Branch Iment S. X. Kirov of the Acalsay of Sciences, USSR)
PRZSZSTKD: November 21, 1958. by D. V. Nalivkin, lcadtmician
SUBMITTO: November 160 1950
Card 4/4

C""/
AUTRORSt Nikono ebedeva, R. M.
TITLEs A Contribation to the History of lAte-glacial
the Continental Part of the Kola Penin,;,.Ala
P---3ICDICALi Boklady Akidemii neuk SS'-R, 1~,59, Vol 128. ',,r
pp 140 - 151
ABSTRACTs The new material collected In the western c,ntirental par', of
the Kola peninsula does not agree vith the exi3ting sche~-C.'a
the Imte-glacial development of the reb-ion. The section ~f 'h,
late-glaciaL sediments on the bank of the Lotts river 50 '0'=
away from the mouth 1.9 interestin3 at.d instri=!Ave in thii
respect. The section was, cozp"led according to thret v,~ll
,;ompsrable oLA-cr~,ps arl may serve as directirF
otance tetween the oAt-crops amourAr to z " F AJ' g J
2 masses may be recogaized on the nt-.-enetti or
gical characteristics. The lower ono bh~sa a jira(-,~al
of the basin near the glacier removal of the coastal zonp- c~f
erosion), its stable exintence and subseq4ent flatteni:.g
simultaneous lose of the near the glqcier charactcr. The jp~,--
Card 113 mass characterized a flat basin with increased supply Qf 3an~llv

A Contribution to the H!story of Late-glacial L'srd9capea SOV/Zo-120-1
in the Continental Part of the Kola Penins-als.
material Puri undirturbc4 ccnditions of its accuLulati6n 7:
i.,.vestfgstion of ~~i:jtrns carricd oit by Y,~. A.
f1ras suct, ~i divi,,Iun of the sect'.on and
teriatics of the b~ieins and their A
accurcte c-...,;;srlaon of tKe pollt;n s~er_,.rn ~'etcr-L'An-6 tltn
material existing for thu Bsltl*c -.-ijon
thst the devf!loputnt course of plar.1s and :-,f
basin is 3i.Lilar to that oil the rc,7,lor. iLvcv
depos its of thv late glacial perlod of botb -I,, ;i~~i,e
tion froz the tAnlr% flora to a thcrxrphi,1;,,_ %oA-t.Ai-
was fourd. good -jgriiezert of t.1-le cnarsl, of
f Icra and al I. --,ts~ ~~ llow.i the f 01 ION it.g con,_l Ili
to the dlfferencP5 of Intit4de. Th. first i-ttt~;e ~,f d(.,ii
can be compared v-.th thk, 11n4 hi.-tr-ric zoii4r: ,f
("Allerod"), the recond with the 111rd zone ff~arli A~rlAf
the third with the Nth zone (preboreal ern). -Ahp fcurf-.
admit the asaj~;ptjon that the qeqAerce and rif 'hr
ment of the landacape In the regioLn cztendii,g
Jarents S ea -.. rr. V-ry a 4=11ar to V~e Sa' , ic 7:-,4 i-.-,
Card 2/3 w i t I i t h c c o r,tp p a e ( P. e , c ) q r, d Aa r I'i , f

A Contribution to the History of Late-glacial Landscapes SOV/2o-128-1-4o!~8
In the Continental Part of the Kola Peninsula
existence of a meridional z)nality along the eastern boundary
of the Scandinavian ice over and on the siailarity of the
plant history In North- and South-East Finland during the
late glacial time. The occurring differences are connected
with the latitude, the 44rUilrdying ( in any case before
"Allarod" ) and with the slower recess of the ice cover in
the North. There are 2 figures and 11 references, 4 of which
are Soviet.
ASSOCIATIONo Xollskly filial I=. S. M. Kirova Akederaii nauk SSSR (Kola
Branch Iment S. M. Kirov of the Academy of Solences, USSR)
PRESENTM Kay 12, 1959, by V. M. Sukachev, Academician
SUBMITTEDs May 12, 1959
Card 3/3

MIK011OV, L.L.
Stratigrapf7 of sediments and paleogeography of late-glacial aea
basins in the Latta Ekliression. Vop.gooswrf. t geol.os&d.pokr.-
Koll.poluost. U85-120 060. (KIRA 15:1)
(Kola FenInaul*--Deolof7, Stratirraph1c) Qaleoeeography)

Nrymv, A.h.
Stratigrraphy of moraines and glacial deposits in the western part
of the Kola Peninsula. Vop.geomorf. i ge-)l.oa&d.pokr.Kol'.polucst.
W21-135 160. (KIRA 15:1)
(Kola Peninsula--Geolory, Stratigraphic) (Drift)

huc,Nov, A.,k.
Developoent of the vegetation ard clinate in tbe. decreasinr. continer-
tal glacial deposits: review of Finnish literattreo 1927-1957.
Vop.geomorf. I reol.asad.pokr.W'.poluost. 1:180-187 160.
(KIRA 15:1)
(Fennoseandia--Vegetation ard climate)

ti.o r.:~trcat, c,`
of "=,xo,-SctrA
ia,
1:15c'-l'.3 ;Y-P
f.iro-Ai i-kadozii -L.-k
0,,c-,)-.) (:.ola cn'.

C-,10!*,_7 0: Lhe n
fronts. of t-lue oc,,.u! i,AvL,L.,A ir-.,~ crjvc,r. ~'*O 1. ki i no.2s3-
396 ."tr 161.
I* Kol'skly filial AI I)',.,.. Fr.-.(Lst,.-,rlqno
D.I.IhchsrLa~covjm.
(3CIndII2.*Vi.-
-oil C,)

ARXWq A.D, I AAXMp X.X.;.j"QKff4- AA.
OPGOW features of the histM of recent Claclation In the
northeastern part of Y*moecwWla,, lzv.AX SWR.Ser
no.205-W Xr-Ap 163. igNI40RAC*1694)
1. Goologicheekly Inatitut, gallabogo fiU&la AN SWR.
(ftwogcwWla-41acl&l epoch)

MosertaUem doftndled at tba Institufm of' G*ognpln*
for the aaadepla degree of Candidat? of Geograp"dcal Sciences:
4%gularitlee In th-9 Foiration Qtatemw7 (Anthropcgonle) FormtIons
in the West Kola Pqninsula (Basin of the Latta FiYer).*
Testalk AW Ifauk Ito. 4p 1963, pp. 119-245

NIKOKM..-A.Aw~ " - -
-,
NuTiml formtIons qnd the mtreat of the l"t ice shoot In
Uw norUmsatern paA of the.101a Pealneuls. Trudy Kost. chetv.
per. 210-14 *61e (KIRA 16 c 10)
1. gollskiy fiUal ALS SSSR.

I,IKCVOVOA.A.; VOSTPUKHINA, T.M.
Quatemary stre.tigraphy in tho r-rthem part of the Kola
Peninsula. Dokl. All SSSR 158 no.ltIO4-lCf7 S-C*64
(MRA 17t8)
1. Geologicheskiy inct-Itut Kollskogo filiala imni. S.M.Kirova
All SWR. Predstavelno akademikom A.A. G7~gorlysv-ym.

HIKOIZOV, Lndre L2 kmayevich; BISKE, G.S.,, Ioht,-,r ge,,gr. riavk,
Frk~-,-Oxl -- -
(Developmat or the Quatomazy relief and palcogeography
in the western part of the Kole Peninsula] Ratvitie rellefs,
I paleagGografits, antropogena n& sapade Nol'skogo polu-
ostrova. Maskyag Ncukap 1964. 181 p. (41RA 18.3)

71011FRinyllp L.P.g SAFROSOVp V-S-; \ETYAN,
GFXDLER, V.Te.1 CHMMOV, V.S.; YtTEMIN, 9-1-; KOCAN, H.S.; YAW,7117'
K,N.; LANGE, O.K.; KABANW. G.K.; KIMNEMU, X.I.; SAINAMTKA, :.K.;
SKIRPOVA, T.N.; VEMTACHALAPATIO V.; KASIAKOVA. S.I.; BEIDMOVA, Z.D.;
YAKUBOVSKATA, T.A.1 YURM, A.L.1 RYPAKOVA, M.O.; MR07AM, V.G.;
PARASH# H.S.; FCqARFV, V.I.; MIKOfjOV,_A,,4.
ActIvity of the Geoloetcal Sections of the Viscow Naturilistil
Soclety. Rid. MOIP. Otd. geol. 39 no.6tP7-151 N-11' 164.
(MMA

N! Ec"Nov, A.A.; Vi r.. I.
=,-ath remains In
t-an".

SIM111070 Mt.
stmUtpaphy 6,rl
f ala fenltmAla. To*$* i
iF

-94
Roseent and Iresout tectonic mov~nts of the earth's cmat
in the KoIA Ptylimula wd adjaaent amas. 1&v. AN =R. Ser.
go". moAtAO-47 " 165. (MIRA 18:11)
1. Zvatitut fitild Uali AN SSSR,,

TMOTO LI. v "Uftt; KLILICMMO V.I. 0 ComWy insh.; KUCM,,-A.r.,,
gorW Lmho; CHMMUTO V.I. g lmovy lash.; Smst SeDop
pmr.; KILUCMV, A.P.9 dat4snt; DIMOv ImSe# gozujy imbe
ftWml respowe to A.A. Shaming A.M. Belemkil ad A.T.
OkWals artioU OPLllar mstWs of ad-4 flat dipping seem
witbmt imderminim the ai" vaUs ia dmlopwut wwkimp.0
U011 Mro 6 no.206-U F 162. (KMA 15 c 2)
1. ma"Obut"Guy ?aitekbaLob"kly institut (for Tyusnow).
2, Trost lanUbvll fcr Dudko). 3. Dowtakly nuchno-
looladentellskLy ugoltzqy imtLtat (fW Kiricho6o). /,, Gas-
udsmationgy la~tLtat po proyaktirava:dym shakhtmoCa stroitelf-
atm hommumcalfacy ProrawbUmmotl (for Mikonav), 5. Ukmin.-
ady ffllf-l Tmoo7umCo nauchno-Loolodaratollskogo markmba7dor-
Olgap imtLtuts (for Chormayov), 6, V4&kovWdy CoraWy institut
(tw Swing Mynah").
(Cola min" Wd staLle)
(shmint 41suldir A.M.) (GalH j A.V.)

KIWVOT. &.a.
;~M, -" -- ~ I,
Potthocetionle mni trf-atmAnt of ehnler,;. Tot.1 dokl.konf.lrk.geiv.
mmeh.-tsel.prottvachurs.inst. no.1:7q-30 155. (MINA 11 :1)
1. X4etavakly gosudarstiennyy nnuchno-imaledovetollakty
arativachmiWy Institut.
(CMIZRA, ASIATIC)

T rN r ,I -,,x,
F'I"TC)'k 'Jf~c Vo _1
J~ 17 ?
al 0,
2058. NIKONOV A.G. Rostov -on-Don, U.S. S. R. The pathogenesis and
Lreat-m-e-Wr-5f cholera (Ruasian text) ZbUKROEILOL. 1256, No.5
(32-39) Tables 2
firnall doses of V. cholerae were introduced into the gallbladder of guinea-pf 98. As
a result of rapid multiplicallon of the vibrIon in the gallbladder and small Intestine.
the animals died In 6 to T days. Experiments carried out on rabbitz and guinea-
pirs showed that antigenic products of the vibrios are absorbed from the biltarr
system into the blood. The less marked the cholecystitts, the more Intense is the
absorption. Removal of the gallbladder. before guine-&-pigs were infected into the
common bile duct, lessened the toxaemla and prolonged life. In a series of expe-
riments gulnea-pigs were infected by Injection of vibrios Into the duodenum. In
some of the animals the common bile duct was ligatured before Infection. These
experiments showed that V. cholerae can make their way Into the bile both hae=-
(Nenousty and enterogenously via the common bile duct. Ligature of this duct
stimulated multiplicat.ion of the vibrios in the Intestine. On the baste oC his results
&PA of supporting data from the literature, the author considers that the bill
system Is a second focus of multiplication of cholera vibrios and, that the PeAs,79tent
carrier state In cholera to s, biltary carrier state. In the treatment of cholera It Is
aseentW to use preWatiorm able to anko their war, Into the btliary system.
Chakhaya - Moscow

51JOCIPOV, A.G.
=OqthovZ~ ~
Is and diagnosis of prolovged aftrrytmg of Vlb~rla cows*
In comwalasconts, Shur.o1krobloLoold, I lown. no.1:41-4? Js 118.
(KMA 11:4)
1. In losimhWo-na-Dom nauchno-lealadovmtol'skoCo Institute
Klmisterstva sdromooftraywmiya GSSR.
(M&MA. transalgalon.
carrime by amvelfacents Olus)

VIKOVIV, A.G.: TXTSXMA, T,L; HIBIOTA, P.V*; NICKMI, Ka.
Cultivation of TibrIa co~ in the svKII Enteettm of cminma pigs.
Mw. aikroblol. spido lbom. 29 n0-12-01-53 D 158. 0 (MM 12:1)
I., to InIkovskogo-na Dom vAuchno-inslodovatallskogo, protivochmnaea
Institata Kintaterstva adravooidwwwal7a =SR.
(TUMO COM, cultures,
an Isolated loops of Kuimw Pic Small LatestLao (Rug))
(LVMTIM SULY11
cultLvatlou of librio, comma in lactated loop* of latestLas
from gmlzoa p%s (ats))

A.4.4,,Uouzm~ X.G.;
-0.K
Molera tecterlooWe thur.ulkrabloteeptA. I Imn. 30 w.1:"6
Ja 1519. (KM 12: 3)
L Is lostevskage-sa-Dom amehao-looledavatel'skoo prativoehumi.-
wCe inatituta Nialsteretwa adravoolbromenlya CSSZ.
(Tmlo =me
(BAC"RIOMA
of Tibria coma (fts))

PIANKINA., Z.A,.j,NVMMVt L.G.t SAUIWt R,K*' KOTLYMVis, Fel-
Control of cb*Iom in Afghanistan. Zhar.nikrobiol. epid.1
immm. 32 no.IWO-U, D 161. ISCII)
i, rz protivochu-mijYM uchrnhdeniy HInIsterstra, zdravook"nenlya
SSSRI
(AMHAJUSTAN-CHOLEUp ASUTIC-PREVENTIVE INOCULATION)

MO"U , z.L. j, ii I KOCROV , L.G. ; %taA.T.UV1; , R-.V. I KUITIWL~, UIL . .~-- 1.
Cholera control In Afghanistmn. Cesk. ep-'dex. U no.1:65-69 J&
,62.
1. laborator Ypoce virulantaich infskci ministerstya sdravotnietvi
SM.
(GROL&M prev. & control)

NIKOM, A.G. (d*coamd)L.,GOHlTENr. , I.I.; KMITSKATA, N.V.; GOLIDMM,
W.3.1 wmwwm=ATA, T.D.
C*U-Pratmo bmtori Jn gqprimntal conditions In vivo. Aoport
I wee 1. zbw. mi;;:92hwtv4 I ilmmm. -40 so. SoMS5 Ag !63.
(KIRA M9)
is- I$ 0?4etov'skogo inatituta spideadologit, alkrobioCit I giCiyany.

ODINGO I.A. [decenvedli NIKCNI~JV A.G.; T.-
I Z~~
Efrect of tempering on the critical brittlomess tAx,.erature rf
cyclically loaded car6-,n fiteol. Dr)kl. AN 161 M.3071-579
Kr 165. (KIRA 113 1 /.)
1. Institut metallurgil im. A.A.Mykovs. 2. Chlen-korresix,ndent
AN SSSR (for OJIng).

1~nl 1110 A. rl
N"
'I , I Vrl xy.
Ilbr.,, Inst. lletal,, in. A. A. Paykov,, Dept. Tech, Scl., Acal. Scl.., -cl949-.
"Interaction of Magnesitn" Ith Carbor, Uonozide,ft Ix. Ak. Nauk S!:SR, Otdel. Teckh.
Nauk, No. 10v 1949;
"S,~roun Diseases and Passiv,! Imunity," (bk.), 1949.

USSP/Metals Cadmium Jam
'On the Interaction of Cadmium With Carbon Oxidoe.0 D. H. Chizbikov. Corr gem.
Aced Set USSR, To. 1. Missanov. A. 0. likonov, last JkUalurgr Isoul A. A. Balkovo
Acad Sal USSR
*Iz Ak ITAuk $90, Otd*I Tekh Iauk8 Wo 1. pp 68-73
Showed that Od to not oxidized with 0 oxides at tamp above its bp (7680). OzIdILtIon
with 00 occurs below 3500 and oxidation with 00 Is noticeable on4 near Cd mp
(3296). Low ratos of oxidation of Zn and (14 with 0 oxides sweat possilillity
of fractional condensailon of vapors of Za and CId fro= their aixt with 00 in obtaining
total by dietillatlon.
184T93

Iff KOW7, A.G.
NIKOMV, A. G.s *Investigation of the effect of alloying ele-
ments on the quality of senaligas rolled railroad uhaelow. Moos
cow, 1955. Aced Set MSP. last of Motallurgy Insal A. A. Say-
kov, kad Set USSP. (Dissertattone for the D*Cr*e of Candidate
of Technic"I Sciences)
SOt KalzbMs-19toplet, No. 52, 24 December, 1955. KDffcow.

. ~ iT , ! d e~ ; . ,:- :-, - - - --, !
""~3 ""' C' CC ~~"fl 1 at' I' - ~1:3:-* 1~ :'0 1 ' : - '; G A - - : .
-2 "~: - .1. --~C - I . - !,~ le -,t a C.~ 111 0 ,-4z ~ r ~, .1
a p,-ipr-,r oub-nitted for of C)A~
'T-12 Oc-t 57
C-3,700355

SOV/1 37- 57- 11--1264 1
Translationit rom: Refer at ivnyy zhurna I, Metal I urgiva, I q57, Nr 11, p288(USSR)
AUTHORS- Bardin. 1. P. , Nikonov, A.G. Pir-khtisovich, L. L.
-----------
TITLE- The Hardenability of Wheel Steel Due to Sliding Friction
(Issledovaniye zakalivayemosti kolesnoy stali pri trenii
skoll zheniva)
PERIODICAL: Tr. In ta metallurgii. AN SSSR, IQ57, Nr 1. pp 114-119
ABSTRACT: A new method is described for testing the resistance of steel
against the formation of chipped-out hollows on the rolling
surface of railway wheels (W) through braking action. The
reproduction of the hitrdened layer (HL) on the surface prior
to the formation of the chipped-out hollows was accomplished
under laboratory conditions on a special machine in which the
specimen (S) of steel tested was fixed in a stationary position
while the local heating %vas accomplished by the friction of a
rotating W 1000 mm in diam with the rim machined in the shape
of the railhead profile. The hardness on the rolling surface of
the W was HB = 500, i. e. , equal to tht hardness of the rail.
The length of the S tested was equal to the width of the rim of
Card 1/3 the W, their width was 60 and thickness 40 mm. 5 were carefully

SOV/1 )7-57 -1 1-ZZ641
The Hardenability of Wheel Steel Due to Sliding Friction
ground on four sides, washed with gasoline and fitted intn the grinding slot of
a yoke, which was made of a piece of W rim, and fastened with a wedge. This
ensured heat elimination at about the same rate as in the rim of a full-sca!e W.
Thereupon the rail-shaped W was set into rotation and, when the surface of
W reached a constant linear speed (60 km/hour), the S was pressed to the W
with a force regulated by the safety valve of the hydraulic transmission, and
kept in this position for a specified period of time. To decrease the sticking
of metal onto the surface of the W during its slipping on the S it was wetted
with machine oil. Upon the expiration of the time of holding the specimen
under pressure, the valve on the hydraulic transmission was switched over
and the S was moved away from the W. The experiments were carried out on
S of carbon steel with 0. 59c/. C, holding at a constant pressure of IZ50 kg
during 1, 5,and 8 sec, and at different loadings (750, 1000, IZ50, and 1500 kg)
for a constant duration of 5 sec. In addition, S of 7 grades of wheel steel were
lested After the tests the structure was investigated, microhardness was
measured over the section of the S, and the HL was analyzed by X-ray di(frac-
tion. The evaluation of the resistance of the W against the formation of
chipped-out hollows through the braking action was made according to the
hardness and the thickness of the HL. Tests were also performed on the
forMdtion of HL at low temperature (-600C) in order to ascertain the effect
Card 2/3

SOV/1 17-57 -1 1-Z264)
The Hardenability of Wheel Steel Due to Sliding Friction
of the temperature of the S on the thickness and hardness of the HL, and also
the tendency towards the formation of cracks without the application of mech-
conical action. The results of the investigations are adduced and recommenda-
tions are made on the manufacture of inte p, rally -rolled W, resistant to the
formation of chipped out hollows through braking action,
L, G
Card 3/3

3 t,
C, 1- 01
Translation from: Refo%ratitnyy zhurna.. Mefal'iurgaya~ 1958, Nr ', p 168 (USSR~
AUTHOR411 Guseva L. N, NiRorov. A.G.
TITLE; Use of X-ray Structural Ana~ysis for Investigation of Marden-
ability of Wheel Steel in Sliding Friction ~'Primerieniye rent-
genostrukturnogo analiza dlya issledovaniva zakalivayemosti
kolesinoy stal.,' pri trenii skc,'zheniva~
PERIODICAL, Tr. In-ta metallurgi;- AN SSSR.1957 Nr 1, pp lzn-12.1
ABSTRACT: One of the most common dc,~ectq on the rortact surface of
railroad wheels it; the '";at spot fiue 'o hraking act4on. The fcrm-
ation of flat spots is the result tf excessiye heating at the point
of contact between the wheel ard th,! rail when moving with
brakes lociced. the heating be-rg followed by subsequent rapid
escape of heat within the r,.m, In the heat.ng zone. a hard and
brittle work-hardened rrust up tr, 3 mm in thickness, that is
discolored an the wheei contivues . 'n us", '.0mes into being. !n
order to reproduce the hardened laver "orming at the sur'ace of
a wheel under sliding Iriction !or purposes of laboratory repre-
duction and investigatien a spncia' machine was deg4gned. De-
Card I/Z termination of hardenAbi.'.i~y urder varicus ccnditoris o' heat

Use of X-ray Structural Ana!yvip (ront.
treatment was performed by eva luating the shift of lira! (0 111 or comparing
the width of x-ray iines 1,1101 - f0ttl of the test specimens of carbon and
wheel steel against the width o4 the iines of standard specim,~-ns 'S1 of carbon
teel hardened to martensite, and by measuring the microhardness of the
urface of the S. It was found that in the S of wheel steel o-. the various chem-
:
ical compositions investigated, and in the area of the flat spots due to brak-
ing, products of austenite transformation are present due to rap-d cooling at
close to the critical rate. The tendency of the steel of the grades investigated
to harden under Londitions of sliding fric-tion variC9 And may be determined
by the width of the interference lines (110', - (011 '. The S revealing the great-
est hardness also p-esented the greatest expansion of the lines (011). The
width of the x-ray lines obtained ir the S ol wheel steel investigated and S
from zones with flat spots due to braking on an operational wheel were greater
than the width of lines of hardened standard S, which is due to the change in
the structure of the crystal lattice arlAing out of the special conditions of
hardening.
1. 2, X_z,t-1-APPA1t'!atV A Porit N, T~
trenta,ent
Card Z/Z

A6THOR. SGrencen, S. V., We-zber of the i4~ Jkralnian 50. 1-~f iirn
35E
TITLE: A Vesting of the French Socistj of Lletallurj;lsts
(Sesslya, Frazatauzakogo obahchestya metallurGov)
PERIODICAL: Vectnik AN SSSR, 19150, Vol. 20, Ir 1, pp. 107-10a (USSR)
ABSTRACT: The mectinG took place in Paris from October 7 - 11,
1957- Problems of riaterial fat1j;ue were discussed, with
French, English, Italian, Russian, A.,--erican and Swedish
scientists taking part. The processes In fatigued steel
were determined by means of asseurecente of the magnetic
resistance. Problems of fatigue with Increased ;Znaeratures
were discussed. Experiments with motor elements, auto-
-chassis and riveted airplane constructions wero discussed.
The Soviet scientists reported on fatIGu* probleas:
S. V. Serensen (Fatigue of cast Iran In Connection with the
Character of State of Strome and Structure),
G. V. Uzhik (On the Influence of the Concentration of
Tensional Stress on Fatigue),
A. G. Nikonov (On the FatIgue Phenos*na in RollinC with
- Slidin,~r),
C u r.1 1 1/2 1. A. Oding (On the Structure Theory of Creepini-.).

A Uestln6 of th.- ?re-nch Societ7 of !:ettllur..-iatv 1-1 -25,133
AVATLABLE: Library of Co:i,;reoo
I.. Ket&Uurgy-France
Card 212

fig
fig
ts
oil is
Ills

NIXOIMV#! A,Gq HIMSOVICH., L.L.
Vkwel budale wm. Trudy rust. mt. no./,:250-253 t60,
(Car wb"lo-Testinc) (KIFA IA: 5)
Q%ebodma wear)

3 /; 48/60/rxX,,/O I Wo I P- /C I
A I (it 1AW
AVMORSt Pinkhusovich, L.L.; Nikonov, A#Go
TITLEs The Effect of the Quenching Method an Wear Resistance and on the
Fatigue Crumbling of Rolled Seamless Wheels
PERIODICALs Izvestlya vysshIkh uchobnykh zaveid@nly. Chernala retallurgila, 1960,
No- 10, PPo 126 - 131
TEXT$ Rolled RR wheals are quenched in the USSR In a horizontal position
by water Jets directed an the rolling surface from tangentlaUy placed pipeso
This method has been compared with the U.S. method of quenching wheels In vorti-
c&1 position by rotation with & wheel rim portion submerged In water (Refe. 5 -
The test wheels were af standard steel w1th 0.53% Cs 0.69% Kn; 0.27% Sit 0.020
P and 0.02% S. The hardness and the mechanical properties of wheels hardened by
the U.S. method were better. they had pe4Lrlltlc structure through the work por-
tIon and higher wear resistance In comparative tests on a 1A Amsl*r test machine.
In fatIgus crumbling tests on the samis Assler machine, speotmens taken at 12 and
30 = dIstance from the surface of the wheels treated the U.S. way withstood
690,000 and 875,000 cycles, compared with 630,000 and 660,000 cycles withstood by/
Card 1/2

31/148/60/OW/010/012/018
A1611A030
The Itfoot of the ColonotAng Method on W4ar Resistance " tto Fatigue Crumbling
of Rolltd Seamless Wheels
spoelmens from same spots treated In the Sovlet-way. The higher crumbling resist-
ance Is explOned by the different metal structure having a higher resistance to
cracks formation. The oanalusion was made that wheels quenched In a vertical
position by periodical submersion of a portion of the rim Into a rinning water
will have higher resistanci to wear and fatigue crumbling. There are 5 figures,
2 tetbles and 8 references$ 5 Soviet wA 3 English.
ASSOCIATIMs InatItut metallurgil Im. A.A. Baykova AN SWR (Institute or metal-
lurgy im. A.A. Baykov of the Academy of Sciences USSR)
SUBMITTEDs November 26, 1959
Ca rd Z/2

NIKVONOV, k.G.; KLEF.AnoV, G.14
Measuring surface texperatures during sliding friction* 1xv. y7jr.
ucbeb. &&-f.; chom. mt. no.2S122-1Z6 061. (KIRL, 14: 11)
1. Institut vittallurgii ix. AA;Iqkcma.
(Surfaces Mchnalogy)-festing)
(Car wheels-Ttatint)

ngooov. A.G.L nmmsmcH, L.L.
la"atIpting trIaL bat4hes of Iwa-alloy idml-gra& steel, Truo
lost* mto no,1100-96 162, (KERA 16s 5)
(Chrosim-"" um steel-Teat$M)
1 7
imo

S/62oj6z/145/006/013/024
3164/B101
AUTHORSs Oding, 1. A.# Corre3ponding Member AS USSR, Nikonov, A. G.,
and Marlyanovskays, T. S.
TITLEs Effect of cyclical loading on the cold-brittleness threshold
in carbon steel
P&RIODICALs Akadeoiya nauk SSSR. Doklady, v. 143, no. 6, 1962,
1332-1335
TEXTs The effect of the duration of cyclical loads on the critical
temperature for failure of carbon steel containing 0.60% of C and 0.68%
of Un was examined. This critical point was determined from the chang*
in Impact strength that occurred within the temperature rang* -60 to
+600C. Round specimens were subjected to fatigue by cyclIcal loading and
then to Charpy impact tests. The critic I temperature for failur;,:teadily
inoreases with the dur-%tion of loading, ;ros -50*C Initially to - C
after 30#10 3 cyolest +300C after 60-103 cycles, and to +50 0C after
150-103 cycles, ExamInation of the fractures of the specimens showed no
Card 1/2

510201621143100610151024
Effect of cyclical loading on the ... B160101
macroscopic cracks after relatively short durations of loading
(30-60-103 cycles), but cracks of considerable size were noted after
150-10 3 cycles. These, however, do not affect the position of the cold-
brittleness threshold. An explanatiou of the Increased entrittlement way
be sought In the theory of dislocations, It being supposed that the
loading produces stresses In the steel, which cause dialocational these
accumulate at obstacles so that heavy local stresses arise, which lead
to fracture. There are 4 figures.
ASSOCIATIONs Institut metallurgii Im. A. A. Baykova (Institute of
Metallurgy luent, A. A. Baykov)
SUBMITTEDs Ncomber 29, 1961
Card 2/2

mrxa,, r.A. (Keikra) ldecea"dj, wamov, t.a. (xasimog xacracysmA. T.,8.
(Nftkra)
U"Ces of rail mt&2 properties in serviam candItLons. Inv. AN SUN.
Note i gore delo no*51101-107 5-0 064o (KIM Isti)

-PRIDL19TSEVO K.V,j KAZARMOVSKIT, D.S.1 DAXILOV, V.9.1 VUSER, P.A.1
PIKONOVI A,G*j 51KOVO Nor@
leatherval treatmat of ralls. Stall 25 no.4058-361 Ap 065.
(MIRA Mill)

V) -.M 6wasvdm~-,
Fit I

SKARUIDWAYA, T.A. [6ka-,zhYnOka, T.U.); NIEONOVV Al.l.
DIvJsIon of a lnwer member of the tuffaceout-sellrenta-y and
effuslye rocks of the Beloterka Iron-ore region. Geol. zhur.
24 noo4t86-91 164. WIPA 180)
1. Institut geologtcheakIkh nauk AN Lkr,S.R I Elnepropetrovskays
ekspeditelya Mtrainskogo nauchno-lasledovatellekogo gornorudnaga
Inatituta.

YOPOLEV, K.A.1 ICZKGWII# A.].
InprovIng the work of tra-ak machtnery stittlons. "ut' 1. pit. KYox,
9 no.lOg22-23 165. (KIRA 18il0i,
1, Rachallnik putevoy mashinnoy stantsli No.47 stantslya
Orenburg, Tushao-Urallskoy doraCt (for Korolevi. 2. Glaynyy
makhanik putevoy mashinnoy stantoll Ko.47p stantsiyok Orentnirg,
fushno-Urallskoy dorogl (for Mikonov).

114Q 2 I.T.
, _N-QRQY f A __,.4 ORIDU p L. K. ; TSAM F
Unit for measuring the jmrf&c* raughbass Of Pinion Umth.
rm. t4kh. no. 5 c 24 Kr, 160. (sear cuttlvg) (KV-L 24: 5)
41

Smary Imarvatlou of tka @***ague. Tr%U Stal.wd.1sate
21:117-145 157 (KIIU life)
1. Is Wodry Cletalogli I embriologil (wav. dots. LT. Sharaw)
'Stalluabodskoga Coaudoirstvannoga moditsinakoga tneltuts, to.
Abuall lbu-Slao.
(Mcmom- nimyA? low)

9 IZO j!LAOL XTadzhikskaya 55R. C.Stalinabad. u1. Uziwl C.13a, kv.211
Sensory innerv tion of Intramural urvo gtaglia of this esophoots
In dogs. Arkh. arvat. rist. I sabr. 36 no.5:96-99 IV 159. (IMPA 12:7)
1. Kafedra gtstologtl I sabriologil (gav. - 4otsent 1.1. sharov)
Staltnaba4skage meditstaskoCa InatUxta ismi Aviteewq,
(NNOMM. Innorr.
Intrawiral n*rvo ganglia, sensory Innorv. In doKs (Ima))

If _LIKOWff k-P.1 PASSOOIRk, L.'.;, ETIM-iX, L.Te.
mray . k. V.1
first confennee of amtcalstc,, histqlogUts, and mbryclog"tS of
Untral Asia &rA rasakhet&n. Arkh. w*t. gist. L embr. 40 no.Zelll-
115 IF 161. (HISTOLOGY-MGRESSES) (MI RL 149 5)