SCIENTIFIC ABSTRACT KUZNETSOV, A. P. - KUZNETSOV, A. R.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000928110017-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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KUZIIII~MOV, N. P. w"qlllinm-,nchin~q for hl-h cuttimp. Monlcva, jo~3. nauchno-tekhn.
iz,i-vo --mqhinoqtroit. llt-ry, 1949 83 'p. ' (T,71,chnolol-iin m-irhincstroerl'iR)
(51-37o4o)
TJI?15.K85

~ ~ - i 1~ 1-1 ~ : 7 : - ~ ~. i ~W0 W . I ZF
IMMMOV. A.P.. )mnUdat takhnichookikh nauk; TMONOV, 1#1., inshener.
Ourface defects anoaring on tin bronze following turning. Vest.mash. 33
no.11:56-58 1 153. (KUU 6:12)
(Bronze)

U z we-i-S OV A, R
TJU60.A34 TRUSURE ISLAND BOOK REVIM kID 854 - S
SKMOSTNYYS MSTODY OBRABOTKI I USWVIYA DALINEYSIOGO IKH RAVITITA (Speed
Cuttin of Metals and Conditions required for further Development of this
Methodl. Ta Akademiya, Nauk SSSR. Peredavoy opyt novatorov mashinoatroyeniya
(Progreasiv& Experiewe of laading Men In the Xachine-Blilding Industry) 1954.
Part 1: Skorostnyys metody mekhanicheakoy obrabotki metallov (High-Speed
Methods in Machining of Metals), pe 68-77e
The author briefly outlines the latest practical achievements in speed cutting
with hard alloyed tools of such parts as locomotive axles and ball-and-socket
joints for Buction dredges. He makes several suggestions for improvement and
further development of metal-cutting machine-tools, including V. N. Godyayevto
cutter, and advises further expansion of plant laboratory activities in
promoting now equipment and methods of metal proceasing.He thinks that the
Academy of Sciencesf institutes and local scientific research institutions
should help the laboratories in their work. The section on the mineral-ceramic
cutting construction, testing, and uaejof mineral-mramic cutters is presented
by the author in collaboration with A. I. Gusev, Engineer. Eight pictures and
diagramap and several GOST standards.
1A

USSR/Miscellaneous - Machin"o tools
Card 1/1 Pub. 103 16/23
Authors I Kuznetsov, A. P., and Tikhonov) I. I.
Title I Grinding and lapping of mineral-ceramic platc for tools
Periodical I
Abstract I
Inotitution
Submitted
Stan. i instr. 2p 35-36, Feb 1954
Various methods are introduced for the grinding and lapping of mineral-
ceramic, high temperature resistant platus used for machine tools. The
attachments used for the grineing are described. Drawings.
so***
'ji
U ME.*

KOZYNSOY A.P.; GOREWY, Y.H., inshener, redaktor; MUTTSOT, T.S..
, ; DIJGIXA, N.A., tekhalcheskiy redaktor.
(Drilling] Swerlanie. Pod red. T.K. Gorelova. Izd.2-e parer.
Moskva, Gos.nauchno-t9kbn.I%d-vn mashinostroitallnoi lit-ry,
1955. 45-p. (Nauchno-populiarnsia bibliotska raboebego
stanochnIka no.13) (HLRA 8:10)
(Drilling and boring)

MEMSOY.A.P.; TMONOV,A.I.
Screens for protection against shavings. Stan. i instr.
26 uo.5:13~-14 * '55. (MMA 8: 8)
(Nachinery-Safety appliances)

KUMET, V.T&.j KUZM, SOV, A,P.
Nknufacturing tools in school workshops# Politekh.obuch. no 121
58-61 D 158. (MIRA 111121
1. SradiWaya shko]A 16~473 Hoskvy,.
(*chino-shop praotice-3tudy and teaching)

PEL&GE I BOOK EXPLOITATION SOV/3912
Sverleniye (Drilling) 3rd ed. Moscow, Xashgiz, 1959. 46 P. (Series: Nanchno-
populyarnays, biblioteks. rabochogo-stanochnika, vyp. 14) 17,000 copies printed.
Ed.: V.M. Gorelov, Engineer; Executive Ed. (Ural4iberian Division, Mashgiz)-
'rJeAs Sarafannikova; Tech* Edo; NeAs Duginne
PURPOSE: This booklet is intended for machine-tool operators studying to im-
prove their skill&
COVERAGE: The book deals with characteristic features of the drilling process,
the construction and geometry of twist drills, and methods of sharpening and
inspection.of drillso The construction of drills for drilling deep'holes and
methods of coolent supp3,y and chip removal are discussed. No personalities sre
mentioned. There are no references.
TABLE OF CONTEN
Introduction
Card 1/2
3

Drilling SOV/3912
Operational Motion and Chips in Drilling 5
How the Drill was Perfected, 9
Twist Drill 12
Meamurement of Twist Drills 1T
Forces Acting on a Drill 20
Wear and Sharpening of,Twist Drills 24
Cutting'Speed 28
On Methodsof Improving the Productivity of.Drillins 30
High-Speed.Drilling 35
Deep,Drilling 38
Conclusion 46
AVAILABTZ: M~rarj, of Congress
2
2
Card
/

ANDREYEVI G.S., kand. tekhn. naukj- BOKUCHAVA,.-G.V., kand. tekbn. nauk,
dots.; BRAHMAN, L.A.j inzh.j BUDNfKOVA, A.Y... inzh.,,- GORDON,
M,B,f kand, tekhno naukq dots.; ZHAVORONKOV, V.N., inzh,;
KARZHAVINAf T.V.,, kand. tekhn. nauk; KORMKOVA, V.G.', inm.;
KORCHAKp S.N.p inzb.1 KWSHINO M.I.., kand. tekbn, naukq dotsol
KU2[ETSOV,_AoFo,, kand. tekbno nauk, doto.j XURAKIN., A,V.p inzb.1
IATrSHEV) VA., inshoj OLIKHOVSKIY, VoN*p insho; ORLOVy B*Mo)
kand. tekhn. niuki dots.; OSER, R.N.-, inshoj PODGQRKOVI,V.Vwp
inzb,; I SILIVESTROV., V.D.,, kand, tekbn. nauk [deceased
TIKH6NOVO VoM.p inzb.j TROITSWA., D.No, in2h.1 =I,IJKOV., Y.A.9
inzh.j IESNICHENKO, I.Ioj redo iad-val SOKOLOVA) ToF., tekbno
redol GORDE M Ap L.P.# tskbn, red,
[Wbricating and cooling fluids and their use in cutting metals)
Smazoohno-okhlazhdaiuahohie shidkosti pri rezanii metalloy i
tekhnika ikh primenenlia. Moskva, Gos. nauchno-tekbn. izd-vo
maohinostroit, 3.it-ry,, 1961. 291 p. (MIRA 151l)
(Metalvorking lubricants)

KIRILLOV, A.Ae, inshener, retseusent; BOGDANOV, A.T.,
(Assembling welded metal structures-, advanced training manual for
workers] Sb *orka, svarnykh metall1oheskikh konstruktail; uchabnoe po-
sobis dlia povyshenila. kyalifikatsil rabochikh. Sverdlovsk, Goo.
wmobno-tekbn. isd-vo mashinostroit. i sudoBtroit. lit-ry Dralo-Sibirskoe
otd-niel 1953. 147 P. (MM 7:6)
(Blectric welding) (Building, Iron and steel)

k~ZNETSOV,
Distribution of bottom fauna in Kronotakly Gulf. Trudl Inst.okean.
36slO5-122 159. (Kronotakiy Gulf-Marine fauna) (MIRA 1514)

USSR / General Biology. General Hydrobiology.
fA
Abs Jour Ref Zhur - biologiya, No 4, 1959, No. 14479
=_ ov.-A--P,
Author _X ne1a
Inot Not given
Title The Feeding Fields of Floundern In the
Kronotakly Gulf
Orig Pub Rybn. kh-vo, 1958, No 1, 7-11
Abstract The study Is presented on the composition
and the size of the feedinS biomass of
benthos, taking Into account the feed's
composition as well as the general nature
of the nutrition of flounders (F) which are
the basic industrial benthos eating fishes of
the Gulf. In December-March, F of the
Kronotskiy gulf form a dense accumulation at
a depth of 200-300 M (the feeding biomass of
Card 1/2
B
USSR General BioloGy. General Hydrobiology.
Abs Jour Ref Zhur - BiOlOSiya, No 4, 1959, No. 14479
benthos is highest here). At this time of
the year, F do not feed and do not utilize
the rich feeding fields. In the fatteninS
period from May to September F stay in the
shallow waters Of the gulfs which are poor
In feeds.
Card 2/2
71

KUZNETSOV P,
. -P--At --
Distribution of bottom fauna in the coastal waters of the Kurile
Islands. Trudy Inst.okean. 3WA-2~8 159, NM 1534)
(Kurile Islands region-Marine fauna)
i
I
I *
,q I

KUZNETSOV, A. P.: Master Biol Sci (diss) -- "Benthic fauna of the Pacific wa-
ters near the Kamchatka and the northern Kurile Islands". Moscow, 1959. 16 pp
(Acad Sci USSR, Inst of oceanography), 120 copies (KL, No 11, 1959, 117)

SOMIDVA. K*No; MMNWSOT, -L.P.
Nature of feeding and role of the tropic factor in the distribution
of the sand dollar 31ohinarachnius Parma Lam. Sool. zhur. `9 no.8:
'j
1253-1256 Ag 160, (KM 13 t8)
1. Institute of Oceanology, U.S.S.R. Academy of Sciences, Moscovo
(Soviet Far &ot--Bea urchins)

KUZNETSOV, A.P*
Materials on the ecology of some forms of benthos occurring in large
maones i4fthe region of eastern Kamchatka and northern Kurile Inland
Trudy Inst.okean. 4605-97 161. (KERL 14:6)
(Pacific Ocean--Sea Urchins) (PaoU%o Ocean-Lamellibranchiata.)

KUZNETSOV, A.P.; SOKOLOVA, U.N.
Nature of feeding and distribution of Ophiopholis acuisats, (L.).
Trudy Inst.okeans 46j98-102 161, (KERA 14 6)
(Kurile Islando-Ophiuroidea)
"47

KUZI&TSOV A.P.
MeLteri&lo on quantitative eotimation of the bottom faung of the
Kamchatka Gulfs Trudy InDtookean. 463103-123 161. (KMA 14t6)
(Kamchatka Gulf-Benthoo)
ja

LUS., V.Yao; KUZNETSOV A.P.
Materialo on qWtitative eot ion of bottom fauna in the Xorf-
Karaginskiy arej (Bering Sea). ~ f Truo Instookean. 46:1216,-139 161,
144 (KM& 14#6)
(Nor:C Bay-Benthos) (Karaginskiy Gulf-Benthos)

XUZ111123OV, A P
Materials on the zoogeography of Paclfic waters near Kamchatka and
the northern Kurile Islands. Dokl. AN SSSP- 137 no.2:415-418 Mr 161.
(YJPA W-21)
1. Inotitut d1ccanologil, Ali 33~R. Predstavleno alcademikor. Ye.1%
Pavlovskim.
(Soviet Far East--4-:arine fauna)

KUZNETSOV, A.P.
------
Some characteristics of the structure and distribution of marina
biocenoses as examplified, by the biocenoses of the arsa of eastern
Kamchatka and northern Kurile Islands. Vop. ekol. 4%41-42 162.
(MIRA 151ll)
1. Institut okeanclogii AN SSSR, Moskva.
(Kamchatka--Marine ecology) (Kurile Islands-Marine ecology)

XUZNF.TSOV Alskaey Paylovichl FILAWVA, Z.A., oty, red.; MAKUSHDK,
Yu.V., tekhn. red.
[BotVim invertebrates of the Kamchatka waters of the Pacific
Ocen,n and the northern Kurile Islands] Fauna donnykh beeponyonooh-
mxh Prikamobatakikh vod Tikhogo okeana i severnykh Kurillskikh
ontrovoy. Moskva, Izd-yo AN SSSRq 1963j p. (MIRL 16tlO)
(Pacific Ooean--1ny*rtehXatse

KUZNETSOV. A.P., kand.biolog.nauk
Luminescence of water in the Atlantic. Friroda 52 no.10:102-104
163. (MIRA 16sl2)
1. Institut okeanologii AN SSSR, Moskva.

KUZNETSOV, A.P.
Distribution of the bottom fauna in the western part of the Bering
Sea by trophic zones and some general problems in trophic zonation.
Trudy Inst. okean. 69:9&-177 164. (MIRA 17:9)

PHASE I BOOK EXPLOITATION 770
Kuznetsov, Anatoliy Pavlovich
Sborka i svarka metallicheskikh konstruktsiy (Assembling and Welding
Metal Structures) 2d ed., rev. and enlo Moscow, Mashgiz, 1957.
12,000 copies printed.
Reviewer: Galaktionov, A*T. Candidate of Technical Sciences; Tech. Ed.:
Dugina, N.A.; Executive Ed. Ural-Siberian Division, Mashgiz:
Vakhonin, L.N., Engineer.
PURPOSE: The monograph is intended for assembly men and welders
interested in improving their qualifications and for inspectors
charged with checking the quality of assembly work and welding in
plants fabricating engineering metal structures.
COVERAGE: The basic processing and engineering problems arising in the
assembly and welding of metal structures are described. Materials
used in the fabrication of metal structures and types of structures
Car&~

Assembling and Welding Metal Structures 770
-are briefly treated. Manual,, semiautomatic and automatic metal
arc welding and the equipment used in these processes are discussed.
Considerable attention is given to preparation of metal structures
for welding., to deformations occurring in weldments, to welding
manipulators, roller beds and other fixtures and tools required for
efficient assembly and welding operations. Mechanization of assembly
work and welding., their quality control, and safety techniques are
also described. There are 28 Soviet references. No personalities
are mentioned.
TABLE OF CONTENTS:
Foreword
3
Ch. I. Materials for Fabrication of Metal Structures 4
1. Ferrous metals 4
2. Mechanical properties of steel 5
3. Effect of alloying elements and impurities on the
properties of steel 10
4. Marking oC steel 11
Card 2/ 11

NIKUL11i, Aleksandr Prokoplyevich, aborshchik metal-lokonstruktoiy; SMACOV,
M.P., Insh., retsensent; PINTUBOY. 1.K., inzh., red.; JTP~S-q!~-
A-P-. insh., red.; DUGINA, N.A., takhn.red.
C.Ifficient methods of ateembling metal structures] Proisvoditeltnys
prismy aborki metallokonstraktaii. Moskva. Gos.nauchno-tekhn.izd-vo
mashinostroit.lit-ry, 1958. 41 p. (MIRA 1213)
1. Uralmashzavod (for Malin).
(Building, Iron and steel)

GALAKTIOIqOVI A.T.; DENISOTI, ru.A.; KOPYTOV, G.T.; HASLOT, M.A.; WONOTV
I.F.; FETUNIVp I.V.; KOCHEVA I GeNq RZNMOT A.P., LUII=Ot
j
IT=. 8
N.M. IRAZIIOVp H.I.j SPZSHKOVq V.T.; STEPANOT, B. .1 ANOVS,
Mel kand. tekbn. nmkl SHELCHOVp B*Ye.j IMSHEVt G.P.; YRSIKOVp
X.A.0 dote., retsenment; BAKSHIq O*A., dots., retsezizentj BEREMINI
P.N.p dotoop retsenzent; PATSKIVICH9 I.R.,dota., retaentzent;
RUDAKOV# A.S.y doto,q retsenzentl FIZHBEYN, NeBol inah.9 reteen-
sent; KMWSTAM, L.Ya.9 4ah.p retsenzent; KRJJTIKEOVSKIY, V.G.p
inzh.9 red. BOBROVt Te.Ist kand, tekhn. naukp red. DUGINA9 N.A.9
tekhn. red*
(Welding handbook] Spravoobnik raboahego-ovarohuhika, Pod red.
V.V.Stepanova. Moskva, gos. mmuchno-tekhmizd-vo mashinontroit.
lit-ry, 1960. 640 p. (Welding) (KIRA 14t6)

KUZXRTSOV, A.P.
Rigidity of the distributor box in the ZIL-151 automobile. Ayt.1
trakt.prom. no.7:11-13 J1 157. (MIRA 10:11)
1. Moskovskiy avtomakhanicheakiy Institut.
(Automobiles-Transmisaion devices)

XUzl;E?SOV, A. P., Cand Tech Sci - (dies) "Study of X8 hardness of the
elements of automobile gearboxes." Moo, 1958., 17 PP (Min of Higher
Muvation USSR, Moo Automechanical Inst, Chair~"Automobile ~-- " -A W),
120 copies (KL, 17-58, 108)

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j I.
AUTHORt Fallkevich, B.S., Doctor of Technical Sciences, Levin, 1,A.,
Condidate of Technical Sciences, and Kuznetsov, A.P., Can-
didate of Technical Sciences
TITLE: Some Problems in Gas- ,-Purbine Automobile Construction (Neko-
toryye voprosy gazoturbinnogo avtomobilestroyeniya)
PERIODICALt Avtomobile'naya promyuhlennost', 1959, Nr 2, pp 3-6 (USSR)
ABSTRACT: The "Automobile" Department at the Moscow Institute of
Automobile Engineering has started developing the theory of
the gas-turbine automobile in order to establish how best to
design and operate it. The article deals with the general
theory of gas-turbine power plants for automobiles and
describes the characteristic features of the current (USAf
England, France, Spain, and Italy) turbine-driven vehicles.
There are 6 graphs, 4 tables, 2 diagrams, and I Sovjet
reference.
ASSOCIATIONs Moskovskiy avtomekhanicheskiy institut (Moscow Institute
of Automobile Engineering)
Card 1/1
777-F-~-,_-"-,_-~~-*~

IPAL'XF,VICH. B.S.. doktor tokhn.nauk;--XUZUV.T~qnvv.,A-P., kand.tekhn.uad~_--
Traction properti 08 of a gas-turbine motor vehicle.
no-3:10-14 Mr 160.
1, M08kov8kI7 avtomekhanicheekiy Inetitut.
(Motor vehicles--Dynamics)
Avt.prom.
(MIRA 13:6)
~U

KUZNETSOV, A.P., kand.takhn.nauk
Effect of transmission parameters on dynamio rTopertion of
a gao-turbine motor vehicle. I2v.vy9.ucheb.z&v.j- mashinontr.
no.9-.62-70 161. (MIRA 14:12)
2. Moakovokly avitomekhanicheekiy in-titut,
(Motor vehiclem-Enginse(Compreosod-gao))

KUZNETSOVf A@ Pop kmdo tokbn. nauk; MORIN, Me Me, kand. tekhn. nauki
Rigidity calculati6n of motor-"hicle spur gear transmissions.
Isy. vya. ucheb. sav.1- masbinostr. no.7:235-243 162
(MIRA 16:3.1
1. Moskovskiy avtomakhani skly institut i Vaesayu2nn
zaoohny7 mashinostroitellrqy institute
(Motor vehicles-Transmission devices)

FESENKO, V.K.; KUZNETSOV
,~..,_kand. tekhns nauk
Road tests of the ZIL-127 motorbus with the TurboNAMI-053
gas-turbine engine. Avt. prom. 30 no.503-26 Yq 164.
(MIRA 17:9)
1. Gosudarstvennyy sovuznyy ordena Trudovogo Krasnogo
Znameni nauchno-issledovatellskiy avtomobillnyy i avtomotornyy.
institut i Mookovskiy avtomekhanicheekiy institut.
7,

CHAIKOVSKIYO V.F., kand.takhn.nauk, doteent; KUZNETSOVp A.P,,, inzh,
Low-temperature generators of cold. Trudy OTIPiKhP 12%22-32 162.
(MRA 171l)
1, Kafedra kholodillnykh mashin Odeaskogo tokhnologichaskogo inatituta
pishchavoy i kholodillnoy proqrshlennosti.
I '.
Is

M
CHAYKGVSKIY, v,rwp kand,takhn,nauk, dotisentl XVMMTSOV, ~ A.P., inzh.; LOS, p V.I.,
inzh.f CHMOX,.V.D., inzh.
Enthalpy-concentration diagram for the Freon 12 - Freon 22 mixture,
Trudy.-OTIPiKhP 1207-47 162. (MIRA 17:1)-
1. Kafedra kholodillnykh mashin Odesskogo tekhnologichaskogo instituta
pishchevoy i. kholodillnoy promyshlennosti.

XU=SOVr A. P.
*Refrigerant mixtures in compression refrigerating machines.ir
Report presented at the Ilth International Congress of Refrigeration,,
(III),, Municho What Germany, 27 Aug-4 Sep 63.

CHAYKOVSKIYS V.F., kand.te'kbn.nauk; ICUZNMOV, A.F.P inzhl
UtLlization of refrigerant mixtures in compression refrigerating, temoo
lboletekh, 40 nol.*9-3.1 J&-F ~639 (MM 16-V
lo .,9deoskiy takhnologicheakiy institut pishchevoy i kholodillnoy
POM-4-LO-blennosti. (Refrigerants)

KUZIETSMrP A.P., inzh.; GRANIK, Ch.B., inzh.
Nomograms of the working parameters of a low-temporaturo
two-refrigerant system refrigerating plant. Khol. tekh. i,
tekh. no.1:54-60 165. (MIRA 18:9)

KUZNEmovp A*Pop lnzho
Automatio refrigeration unit. Art.dor, 28 no,3tl3-14 Mr 165.
(NIRA l8s5)

KC_C~NRz ~6009632---(A)-- -SOURCE- CODE: UR/0413/66/000 /004100 24/0024
'AUTHOR: Chay~~kl V. F. LKuznets
Dankovskiy, V. B.
ORG: none
TITLE: A refrigeration unit which uses a two-component coolant. Class 17, No 178831
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki, no. 4, 1966, 24
TOPIC TAGS: refrigeration equipment, coolant, vapor ccndensation, gas compression,
,refrigerant gas
ABSTRACT: This Author's Certificate introduces a refrigeration unit which uses a two-
!component coolant. The device contains a compressor for the two-component vapor, a
iwater- or air-cooled condenser where the high-boiling component is liquified, a vapori-
Izing condenser for liquefaction of the low-boiling element by vaporization of the high-
~boiling component, a vaporizer for cold production and regenerated heat exchangers in
1which both components are recooled. The overall dimensions are reduced and the power
jindices are improved by using a booster at the ioput of the compressor for compressing
!the vapor of the low-boiling component.
UDC: 621.574.9-146.2
1/2

1--ccmpressor; 2--condenser; 3--vaporl zer
condenser; 4--vaporizer for cold production;
5--regenerative heat exchangers; 6-booster
L. AN-1
SUB CODE: 13/ SUBM DATE: 20Jul64/ ORIG REF: 0001
Cord 2/2
OTH RM 000.
:5,
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fi&

KUMT50V, A. 11.
KUZNETSOV, A. P.: "The vertical distribution of ozone in the atmo-
onhere.11 Moscow Order of Lenin and Order of Labor Red Banner
State U imeni M. V. Lomonosov. Physics Faculty. Moscow, 1956.
(Dissertation for the Degree of Candidate in Physicomathematical
Sciences.)
SO: Knizbnaya Letopis's No. 26p 1956

AUTHOR:-Kuznetsov, A. P.
49-9-6/13
TITLE. Observation of the vertical distribution of ozone in the
atmosphere. (Nabl deniye vertikallnogo raspredeleniya
ozona v atmosferT.
P12IODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1957, No.9, pp.1154-1163 (USSR)
ABSTRACT: A description is given of a photo-electric spectrophoto-
meter intended for measuring the vertical distribution of
the ozone in the atmosphere,which is essentially an
improved version of the well-known Dobson phot'o-electrie
spectrophotometer and was built by the Moscow State
Universiby (MGU). A photo of the spectrophotometer is
shown in Fig,l, p,1156. Fig.2 is a sketch of the optical
system. The results of the first observations by means of
this instrument (graphs Figs. 3-5) and the evaluation of
these results are given. In the included example the centre
of gravity of the ozone was located at an altitude of
22.8 km on August 2 and an altitude of 23.2 km on
August 17, 1955. Results calculated by other authors are
n1so given for comparison. Acknowledgments are made to
....netsov for his valuable advice, to V.A.Iozenas
--gistance in bUild-ing the instrument and to

49-9-6/13
Observation of the vertical distribution of ozone in the atmosphere.
Ye. G. Natrusova and N. S. Strunina for their assistance
in carrying out the computations.
There are 8 figures and 13 references, 5 of which are Slavic,
SUBMITTED- December 8, 1956.
ASSOCIATION: Moscow State University imeni M. V. Lomonosov.
(Moskovskiy Gosuda--,stvennyy Universitet im. M.V.Lomonosova).
AVAILABLE: Library of Congrea3
Card 2/2
7777F

130) SOV/50-58-10-4/20
AUTHORS: Britayev, A. S., Tozenas., V. A., Kuznetsov, A. P.
TITLE: On the Relationship Between the Total Ozone Content and Meteoro-
logical Conditions (K vopro8u o svyazi obahchego soderzhaniya
ozona a moteorologicheakimi usloviyami)
PERIODICAL: Meteorologiya t gidroingiya, 1958, Nr 10; pp 24-29 (USSR)
ABSTRACT: The increasing interent in the problem MLntioned in the title, in
particular in connection with the International Geophysical Year,
is not -in accordance with the few data available on it. The most
usual methods of ozone determination (according to direct sunlight
and disperse light in the zenith) are limited by dull and cloudy
weather (Refs 1,3,4). The determination of an interrelation betimen
the ozone content and the synoptic processes requires continuous
ozone measurements for a number of days (Refs 5-8). This is only
possible in certain areas with a maximum of sunny days. In view of
these facts, the Tsentral'naya aerologicheskaya observatoriya
(Central Aerological Observatory) investigated the fluctuations
in the ozone content as mentioned in the title. As the most saitalie
area that of Nizhneye Povolzhtye (lower Volga region) was chosen.
The period between April 27 and June 8 (1957) corresponds to the
Card 113 highest seaoonal intensity of the ozone content (Refs 10).
gg-
gilig 's

SOV/50-58-10-4/20
On the Relationship Between the Total Ozone Content and Meteorological Conditions
A photoelectric speotrophotometer (according to Dobson, modified)
was designed by the Moakovakiy gosudarstvannyy univeraitet imeni
K. V. Lomonosova (Moscow State University imeni X. V. Lomonosov)
and used as main device for measurements. The total content of
ozone was determined according to formula (1), by means of formula (2).
Table I presents the average values obtained. Figure 1 gives these
values in oonnootion with atmospheric pressure on the earth's aur-
face and with the altitude of the tropopause. It may be seen from
it that the higher the tropopause the less ozone is contained in
the atmosphere, and vice verea. Furthermore, high ozone quantities
tend to occur during a low pressure on the earth's surface, this
dependence, however, being less pronounced than that on the tropo-
pause. The relation between temperature at an altitude of 2 m and
the ozone content is more difficult to be established. The results
obtained confirm the relationship between the processes in the
troposphere and in the lower stratosphere. It follows from it that
the variations of atmospheric conditions in lower layers are one of
the principal causes of the variations in the layers up to an alti-
tude of 20-25 km. These data are further indicative of the-fact
Card 2/3 that ozone is not being suddenly destroyed but within dozens of

SOV/50-58-10-4/20
On the Relationship Between the Total Ozone Content and Meteorological Conditions
hours. These rules suggested above are illustrated and explained
by examples in. dependence on some atmospheric processes in the
course of the observation period.-There are 1 figure, 1 table, and
-9 references, 5 of which are Soviet.
Card 3/3

33057
S/169/61/000/012/053/089
3, n~Z) D228/D305
AUTHORS: Britayev, A. B., and Kuznetsov, A. P.
TITLE- Vertical distribution of ozone
PBRIODICAL: Referativnyy zhurnal, Geofizilta, no. 12, 1961,
14-15, abstract 12B99 (Tr. Tsentr. aerol.
observ., 1959, no. 32, 28-35)
TEXT: The results are given for measurements of the overall
content and vertical distribution of ozone over the southern
part of the Union's European territory in Aprii-June, 1959,
rrom terrestial observations of direct solar radiation and of
UV-radiation scattered from the zenith of a clear sky. The
measurements were accomplished with the help of a photoelectric
spectrophotometer with a two-fold resolution or liglit by quartz
prisms assembled according to the scheme of Dobson. The tem-
peratureq pressureq and direction and velocity of the wind at
the surface were simultaneously measured by standard meteoro-
Card 1/4

33057
3/169/61/000/012/053/089
Vertical distribution... D228/D305
instruments, and the amount and form of the c1cudineos and op-,
tical phenomena in the atmosphere were also visually observed,
A thermoelectric actinometer was used to estinate the atmos-
phere's transparency. Air streams, the heights of the trop(::-
pause, and atmospheric fronts were established on the ,,round,--,
of the radioprobe data of neighboring stations and from mapp
of the baric topography. The meteorologic data were subjec-t-.1d
to processing and viere compared aith the overall content and
vertical distribution of ozone in the at-riosphere. Calculat-L,-_i~;
of the total content of ozone -.,ere made from the Bouger
the vertical distribution being computed by the method o'L' HeTz
and Dcbson with the arbitrar-~, division of 'he --trio- T-here
an,!
the layors 0 - 5 k!n, 5 - 20 6, 20 - 35 35" 50
abo-ve ~5)0 km,, The ozone content in the layer above 50) vlac,
assumed to equal zero, while in the low 5) km layer it wac cli-p
posed to be equal to, 1% per I km of the valite of its ovE~rall
content. The decrease in the air tempor!il.,,ire in the lay-Ir
Card 2/1"

33057
3/169/61/000/012/053/089
Vertical distribution... D228/D305
beneath the tropopause is revealed when the total ozone content
increases with the correlational relation equal to -- 0.54.
increase in the total ozone content is acconpanied by the N'.,arm-
ing of the air in the 4 km layer above the tropopause, the co-
efficient of correlation in this case comprising + 0.48. A low
tropopause corresponds to a high ozone content: the appearance
of extreme values for the height of the tropopuase almost alwayb
precedes by approximately one day the appearance of extreme
values for the total ozone content. The character of the verti-
cal distribution of ozone is related to its overall content:
as a rule, the higher the quantity of ozone in the atmosphere,,
the lower the center of gravity and the wider the ozone layer;
the curve of the vertical diatribution with a sharply expressed
maximum concentration and a comparatively high center of gravity,
on the contrary, corresponds to a low total content. The sink-
ing of air with a high ozone concentration into the atmospherels
lower layers occurs when the height of the center of gravity of
the ozone layer decreases simultaneously with the increase in
Card 3/4

33057
,/61/000/012/053/089
S/169
Vertical distribution... D228/D305
its total content. The ozone concent-ration in the ozonosDherelc
upper layers thereby somewhat decreases, but in the lower layers
it grovis substantially. CAbstracter's note: Complete trans-
C~
.Lation.2
Card 4/4

34501
S/169/62/000/002/028/072.
D228/D301
AUTHORS: Britayev, A. S. and A D
Ku!melsay,
TITLE: Some results of research on atmospheric ozone
PERIODIOAL: Referativnyy zhurnal, Geofizika, no. 2, 1962, 14, ab-
stract 2BI16 (Tr. Tsentr. acrol. no. 37,
1960, 3-4)
TEXT: The measurement method is described together with some re-
sults of research on variations of the total content and con-^en-
tration of ozone in connection with physical processes in the at-
mosphere. The observations on atmospheric ozone were made at the
Tsentralfna~a aerologicheskaya observatoriya (Central Aerologic
Observatory from 1957 by means of a Dobson-type photoelectric
spectrophotometer and an electrochemical analyzer designed at the
CAO. Measurements of the amount of ozone ondays with cloudy wea-
ther were accomplished by spectrometrically observing the light
scattered from the zenith of the cloudy sky. The magnitudes of the
total ozone content werey thereby, determined from transition dia-
Card 1/ 3

3/16 62/000/002/028/072
Some results of research D228YD301
grams, constructed from the data of simultaneous observations for
d~41'ect solar radiation and for radiation scattered from the zenith
of the cloudy sky on days with variable cloud. The use of this
method permitted the tracing of ozone variations in connection
with synoptic processes, whose passage in middle latitudes Is usu-
ally ac:oompanied by the formation of cloud. It is established that
starting from January of each year the ozone content oier Moscow
increases to reach maximum values in the spring -- in March-May --
thereafter decreasing to minimum values at the end of autumn and
beginning of winter. The average yearly value of the amount of
ozone above Moscow, calculated with allowance for the Vigru cc-
ef'ficients, comprises 0.347 cm, the variational range of the aver-
'3ge monthly values being about 0.13 cm; the maximum value (May
1957) was 0.434 cm, and the minimum (December 1958) was 0.273 cm.
As a result of statistically studying 110 cases of ozone obser-
vations at the time of airmass interchange it is established that
the passage of a warm front is often accompanied by a drop In the
quantity o'L' ozone In the atmosphere, while the passage of a cclid
front is frequently accompanied by the growth of the ozone concen-
Card 21',z,
01"
� W if

S/169/62/000/002/028/074-
Some results of research D228/D301
tration. The passage of an occluded front is either marked by no
variation whatsoever in the ozone concentration or else is accom-
panied by the increase or reduction of the total ozone content,
o-rer the point of observation. Together with changes in the ozone
quantity which are in agreement with Dobson's scheme, instances of
ozone fluctuations supplementing or contradicting it are noted re-
gularly. Cases of the weak rise in the amount of ozone beflind a
warm front and of the decrease in the total ozone content behind a
cold front were detected in particular. It is established that then
is a link between variations in the total ozone content and verti-
cal air-currents in the atmosphere: descending air-currents are an,
companied by in increase in the total ozone content, and vice--v-er-
sa. It is shown that variations in tile concentration of ozone In
the air near the ground surface usually coincide with those of the
total content, although instances are observed, too, where these
two quantities deviate from the coordinated course. 13) references.
Z-Abstracter's note: Complete translation.-7
Card. 3/3

33058
S/169/61/000/012/054/089
D228/D305
AUTHORS~ Yuzneteov, A,, P., and Britayev, A. S,
TITLE- Observations on the vertical distribution or
ozone over Moscow
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 12, 1961,
15, abstract 12BI00 (Tr. Tsentr, aerol. ob,,~erv.,
1960, no. 37, 8-12)
TEXT: The observational methods are stated together with
some resutts of investigating the vertical distribution of ozone
over Moscow. Observations were conducted with a photoelectric
apectrophotometer of the Dobson type which separates two light
rays with viavelenaths of 3114 and 3326 R and spectral intervais
of 10 and 14 R. The vertical distribution of ozone was calcu-:
lated from measuring the relative intensity of these two rays
Card 1/3

3305P,
S/169/61/000/012/054/039
Observations on the ... D228/D305
of ocatU)red light at Id.gh zenith angleo of tho sun ir accor-
dance with the moth,-_)d proposed by Walton. The amount cf ozolle
in the lower '12 km layer was assumed to equal 8.5% of the value
of its total content, determined from direct sunlight. The
expon;~ntiul decrease in the amount of ozone alt,;ttide ~,tas
p.ropoced for the layer above 36 km~ The absorption ccefliclent,~
of Vii , U, -" I
~er were used in -the calculated oolution of tl),~ . r b em;
the data an the denci ty of air to a height of 2'~; - 26 Kra viere
deteri:Iined froz tables of acrologic probin,~,, those for ereater
altitudes being taken from tables of' the standard atmosphecc.
As a re,Sult of the calculations, it is ehown th,111 the Introdu-.-
t-_on ol the new absorntion coefficients of of, +he
previou~;Iy usc,0 coefficients of Ni Tzi,-zE; anc Chung S.h.1--l'-plu
increases -the ozone concentration iiall the o_-onosphere s lF3.yera
by approximately one-.third, The patterns of tho connection of
the lotai quantity of' ozone with the elemi-2nis are
preserved. The number of cases when the o-7 t-he equa-
Card 2/3

33058
S/169/bl/000/012/054/089
Observations on the ... D228/D305
tions does not lead to definite reeults has increased. There-
fore, the perfection of methods for processing the materipl of
terrestrial spectrometric data and the more precise definition
of the coefficient of absorption continue to remain urgent
lems. The height of the ozone layer's center of gravity has
increased in comparison with previous data, which is evidently
explained by the new arbitrary subdivision of the atmosphere
into layers for -;.,hich the ozone concentration is being deter--
mined. Z-Abotracter's note: Complete tranalation.-7
Card 3/3

A. oo64-63 EnM/BD.V--AJFFT-G./ A"D/.PeD-.',1AP'G'C1Z0 Z*n--Pi-4/rPo-4/F-q-4--GW
ACCESSION TIR: AR3000341 8/00-',8/63/000/004/AO20/AO20
7'~
SQMCE: M. Mika, Abs. 4AI80
AUTIMR: -1ozenaa, V.J...j ra=ets A. P
TITM Photoelectric speclEMhotometei -for obsermt tion of atmoah2ric ozone
CITED BOMCE:- 6b. Atr=fern. ozon. M., Mosk. un-t, 1961, 14-17
TOPIC TAGS: spectrometers, sunlight,, photoelectric, ozone
TRANSIATION: A spectrophotcmeter is described,. ccns-tructed m the basis of a
double suartz mcnochromtoxjq(RD-1jMnd intended for the measirement of spectra
of sunlig)at scattered from the zenith. The mnochromtor, vith relative aperture
I.-MUM DISMRSICV EWa TO -] Angstrom per millImeter in them 3200
Angstrom rvgion$.~as 2 outpat alits which separates the regions of the spectra
near 3114 and 3324 Angstroms. The corresponding radiation fluxes are applied
alternately (with the aid of 90 CPS vibrator converter) to an FEU-19 racilation
receiver, the response of which is applied to a narrow band (approximately 5 CPS)
-Card 1/2
.................

L 10064-63
ACCESSION NR: AR3000341
amplifier. The intensity ratio of the tvo wave lengths is measured by a zPall
Mlethod using an optical vedge of BS-4 glass vith a deni3ity drop equal to two
units. The accuracy of measurement of the intensity ratio vith t:ae 2:enith.
distarice of the sun equal to, 60 is equal to 0.5%. The minimm fljxes
by the instrument in the 3100 Angstrom region are equal to 10 sup -14 W/Sq. cm.
sec. , =king it possible to start the measurements 10 minutes befare sunrl.-C-0- ana
terminate them 10 minutes after sunset. The spectrophotometer is mounted on a
carriae-, and can cperate lmder field ca2ditions. A. Alek:3andx0v
DATE ACQ: 1.4my63 ENCL: 00 SO CODE: PH
Card 2/2

S/169/63/000/002/014/127
D263/D307
AUTHORS: Kumetsovo A. ozerias, V. A,. and Britayevi A. S.
TITLE: Observations of the vertical distribution of ozone in
the atmosphere over Moscow
.PERIODIOAL: Referativnyy zhurnal, Geofizika, no. 2, 1963'P 137149
abstract 2B108 (In-colleo.tion; Atmoefern.--ozon, M.,
Hook. un-t, 1961o,55-60 (summary in Bng.))
TEXT: The method of calculation is described and some results are
quoted of observation vertical distribution of ozone in them
a of the
region of Moscow. The calculations were carried out from spectropho--(
tometxic observations of scattered Liv radiation from the sun, from
:the zenith of a cloudless sky,, by the method of Getts and Dobson.
'New coefficients for the absorption of light by ozone (after Virg)
were used in the calculations,.employing the arbitrary division of
;the atmosphere into five 12-km'concentric layers as suggested by
Walton. It was hence established that introduction of the new ab-
;a orption coefficients increased the calculated ozone concentrations!
'Card 1/2

S/16 63/000/002/014/127
of the vertical D263%P307
:by -1/3, whilst the nature of the relation of this quantity to m
teorological elements remained--unchanged.-During--the-calculation of-'----
o 'distribUtion-With
zon6 _heiight the number of cases where solution
~
.of equation8,did not correspond to determined results was increased.'
:Height of the maximum ozone layer was calculated as higher than
suggested by previous data,'whiah may probably be due to the new
arbitrary subdivision of the atmosphere into layers. Z-Abstracter's
note: Complete tranglation.-7
lCard 2./2

D263 D307
AUTHORS: Britayev, A. S.,and Kuznetsov, A.
TITLE; On the connection of atmospheric ozone with meteoro-
logical conditions
PERIODICAL; Referativnyy zhUrnal, Geofizika, no. 2, 1963, 15-16y
'abstract 2B117 (In collection; Atmoafern. ozon, 14.,
Moak. un-tj 1961l 170-175 (summary in Eng.))
TEXT; The relations between the variation of the overall ozone
content and oscillations of the tropopause layer, air, temperature,,
and vertical currents in the tropoophere are studied by statisti-
cal analysis. It is shown that, for the region of Moscow, the cor-
relat-i-on coefficient between ozone variations and the temperature
of the 3 km layer under the.tropopause is -0.54, and that between
the ozone variations and'the temperature of the 4 km layer above
the tropopause it is 0.48. The descending currents of air, deter-
m1ned at the 1.5 and 3 km layers by the divergence of wind velocity
-~-and at.heights of 3 to 28 km,by the rotation rates of vanes of
Card 3/?

3/16%63/000/002/022/127
On the connection of ... D263 D307
radiosondes is, as expected,accom-panied by an increase in the
overall concentration of ozone, whilst the aucending currents are
accompanied by a decrease in the ozone content. The beat agreements
between the variations of these two quantities are found when data
concerning the vertical aerial currents above 16 km are used; on
the other hand, ozone variations are occasionally in agreement with
the sign of the aerial current also in the troposphere. According
to the authors, this may be due to the fact that in certain synop-
tic situations, such as in regions of cyclones and anticyclones,
vertical currents of the same direction may cover a large part of
the troposphore and extend intlo the stratosphere, reaching the
ozone-rich layer. During the summer and winter months variations
in the overall ozone content are related more closely to the ver-
tical movements of air than io,the horizontal transport. In inter-
mediate periods, on the other hand, and particularly in the spring,
the influence of advection and large scale turbulence plays the
predominant part. Appea.-ance of the spring maximum*in the overall
ozon
e concentration is conneo'ted chiefly with advection, and ver-
--~-tical movements of the air are then practically unconnected with
e fluctuations.
ozon _,Abstracter's note: Complete translation:-7
-Card -2/2~
7-

YAKOVIEVA, A.V.; KUDRYAVTSEVA, L.A.; BRITAYEV) A.S.; GERASEV, V.F.;
KACHALOV, V.P.; KUZNETSCIV) A.P.; PAVLEIJKO, II.A.; JOZENAS, V.A.
Spectrometric investigation of the ozone layer up to the
altitude of'60 km. Isk.sput.Zem. no.14:57-68 162.
.~ (MIRA 15:11)
(ozone)
(Atmosphere, Upper-Rocket obeervations)

L 296346 IWWEWTUVFSM-310~~CAJ~~d TT/GS/GW
CESSION URI. -AT502356T- UR/0000/65/000/060/0017/0088
AIMORfs Lebe41nskiy, 'A.~ I., Krasnopoltakiy, V. A;; Kuznetsov, A. P .-Ioxenas'i Vs A,
UIL'
TITLE.-% nv6stigition of terrestrialatmospheric radiation In the-visible And: tra-
violet re?
Iva- yojikike kotimicheskolto prostren~t"#
1565. safe On on arents
-d _ovanlya kodmiche-s-ico--go---prostrani;tva-tspace--tesearen)-;-trudy.-komfor:=Ii-,
scow, Izd-vo Kauka, 1965, 77-88
TOPIC TAGS: atmospheric radiation, visible radiation, IR radiation, UV,radiation.
instrumentation satellite, satellite data'analysis,.radiation measure=ent, airglow/
Cosmos 45 savillite
ABSTRACT: Measurements of airelaw and scattered solar UV radiition were made by'
smog 1964. Scattered UV radiation was measured by a UV spectrophotometeril-
(range, 2250-31001; resolution, 15 X; field of vision, 20 km in width).operating
only on the day side of the Earth. Airglow was measured by a colorimeter (field of
vision, 120 km in width) operating only on the night side. For switching t~e. instn
ments , -and. fixing 'an.: -the underlying- -surface, . a-'6ebsor --which -4assured
illumina tion ' at .. 0, 6' 85 was - used. ...The volorimeter carried... four.'%(.
filters 'on`,4. common,~' -Axis _-.V0'unted along a disk. one filter
Card 113

L 2963-66
'ACCESSION NR:'_-AT_50235_67_
zodiacal light was relatively small. A comparison of these readings,(averaged) with'
:the results of ground observations at 3200-4000 X lead to the conclusion that night,
sky radiation at 2500-3000 is small and at 3200-4000 X does not exceed star glow
and zodiacal light. Measurements at 1700-2500 X indicated that no night sky radia-
tion exists In this region. Thus, results of measurements over the e9tire wavelength
range (1700-4000 A) confirmed the absence in the night sky of high-energy excitation
processes. Orig. art. hael 7 figures. EJP]
ASSOCIATION: none
SUBMITTED: 02Sep65 ENCL, 00 SUB CODE: as #qA
0 REF SOV: 004 OTHER: 008 ATD PRESS:
_Cq"L_3 3

L C`963-J~6
ACCESSION NR: AT5023567
screened out UV radiation-, its long-wave houndary was near 6000 The
second was used to investigate wavelengths at 2500 to 4000 X*, and two uarrow-band fil-
oters with passbands of 100 X filtered emission at 5577 ~ and 3914 A, respectively.
An IR spect ropho tome ter recorded thermal radiation concitrrently with Lite operation
of the other two instruments. A correlation was found to e%ist betweell readings uf
-it ozone band. A correlation of
:the UV and IR spa cL ropho tome tern in the 9.65
,ties was also disclosed near the long-wave boundary of the UV spectrum at X ~, 3000
'and in the readings of the illumination sensor. These readings depended strongly on
cloudiness because the albedo of clouds in thp red zone is' subs tantially greater than
:the albedo of the Earth's surface and of the clear atmosphere. The correlation con-
Sirms that at X > 3000 A, the noticeable part of atmospheric radiationis due to.tropo-
spheric dispersion and reflection occurring below the basic mass :ii the ozone layer.
,Conclusions were also reached on local$ diurnal, and latitudinal, variations of air-
1glowi A difficulty arose in the evaluation because of the depepdence -of the readings
:on cloud cover. In,making the measurements in space, it was necessary to Include re-
flections of airglow from the atmosphere and glow of astronomical origin in addition
to airglow itself# Consequently, results varied with atmospheric conditions by as
Puch as a factor of two, with the minimum occurring during cloudless weather and the
maximum during total cloudiness. The correlation'of readings of one light filter
~'(5577 A) with the others indicated that the share 'of illumination from the 9tarij and
ic
ard 2/3

--- L 23449.-66 FSS-2/EWT(l) TT/GW
ACC NR: AP6011690 SOURCE CODE: UR/0203/66/006/002/0185/0189
AIMIOR: Krasno2ol'skiy, V. A.; Lebedinskiy, A. I
ORG: Moscow State University, Institute of Nucle4j_ghyq~qg (Moskovskiy gosudarstven-
nyy universitet Institut yadernoy fiziki)
TITLE: Measurementa of the ultraviolet spectrum of. the earth made by the satellite
"Kosmos-65"
SOURCE: Geomagnetizm i aeronomiya, v. 6, no. 2, 1966, 185-189
TOPIC TAGS: solar ultraviolet radiation, ultraviolet spectrophotometer, diffractional
monochromator, ozone concentration, spectral brightness, radiation intensity
ABSTRACT: Solar ultraviol et radiation'keflected from the terrestrial atmosphere was
measured with an ultraviolet _spectrophotometewunted on the artificial satellite
"Kosmos-65 -" The spectrophotometer used was a.double diffractional monochromator
operating in the spectral range of 2250-3070 A'* 2500 spectra were obtained during
the flights. Spectra were recorded on motion-picture films. The distribution of
energy In the violet spectrum changes with the zenithal distance of the sun and the
geographical latitude. Local peculiarities caused by the ozone concentration appear.
Longer waves in the ultraviolet range penetrate deeper Into the atmosphere and in-
crease the albedo intensity. Two kinds of spectra were obtained on cloudless days
UDC: 523.72:629.192

T 'N
43 4 4 ~',_ 66
ACCt4R__Zjjj0
AP60
in the equatorial zone: the typical spectrum and the spectrum of maximum intensity.
The first consists of the usual-spectra of tropical zones and the second seldom
occurs. The intensity of radiation reflected by the atmosphere depends upon the
quantity of ozone in a vertical column of the atmosphere. Spectra of the terrestrial
atmisphere and the sun obtained under the same solution conditions have great
structural similarity. The decrease in intensity in the atmospheric spectrum
occurring with decrease in wavelength is greater than in the nolar spectrum. The
authors thank 'Yu. V. Yaremenko, V. It Malin and_H,_DA__Ug_t for their great help with
this experiment. Orig. art. has: 4 figures, I table, and I formula. [EG]
SUB CODE: 04/ SUBM DATE: 24Nov65/ ORIG REF: 003/ OTH REF; 009/ ATD PRESS:
Card 212

MAZALOV, Yovgenly Vasillyevich; LAVRIKOV., Yu.A.; KUZUETSOV, A.F.
(Alone the paths of technical progress; from the work
of the Leningrad party organization, 1951-1961) Na pu-
tlakh tekhnichoskogo progressa; iz opyta. raboty lenln-
gradskoi pcrtiinoi organizatsii, 1951-1961 gg. Lenin-
gtad, Lenizdat, 1962. 480 p. (MIRA 17:10)
g

0ZHEVOV, A.P.
'
',f - A;.
-r-,
Preparing chlorides an a continuous production lJne. Avt.
dor. 27 no.4t28 Ap 164. (MIRA 17%9)

BRITAIW# A.S.; ZUZNETS2Y,.,.A.P.
Atmoapherlo oxone and some meteorological processen, Trudy TSAO
no,45s22-31 162, (MIRA 16:10)

.KUZNETSOV, A.P., kand. tekhn. naukv dotsent
Problems In the precision machining of heavy shafts."Trudy GPI
17 no.4:41-48 161. (KMA 16 112)

KUZNETSOVy A.P.p oty. red.; MALIKCYV, H.F., zasluzbenrqy deyatell nauki I
prof.t red,; BARIIICV, V.A.t doktor tekhn, naukt prof,f
red.; IZONOV9 B.M.f redo; MALIKOV, S.F.9 kand, tekhn. nauk, red.
KOLICE M 0, G.N., red.
[Hundred,years of the state weights and measures ser7ice in the
U.S.S.R.] Sto let gosudarstve=oi sluzbby mer i vesov v 'SSSR.
Moskva, Gos. izd-vo tekbniko-teoret. lit-x7, 1945. 376 p. (SSSR.
GosudarutveraVe standarty) (MIRA 14:7)
1. Russia(1923- U.S.S.R.) Komitet standartov, mer i izmeritell-
zWkh pr.4borov. 2, Fredeedatell Komiteta po delam. mer i izmeritell-
rorkh priborov pri Sovete Naroftkh Komissarov SSSR (for Kuznetaov)
3. Chlen Komiteta po delam mar i izmeritellnykh priborov pri Sovete
Narodnykh Komissarov SSSR (for Leonov)
(Weights and measures)

1~
I ." I I ."- ~ - - . - . . - -

i
i

~-,trcdun!ng tho ''tig gr~rdr,-r
ekon, 1 nf orm. Gon.natiobs - s lr.-~, 1,. nal~(
ALP (MTHA 13,8416)

KOLCOOV, A.A.; DEZ41DOV, G. Ye.1 KUZNETSOV,, We
Appanutus for the removal of tartar with the aid of ultraacnio
waves. Trudy VNIIMLO-no.3t79-86 163 (MIRA 18:2)

KUZNETSOV, A. P.
KU7NETSOVq A. P. --"Peculiarities of the Summation Phenomena in the Presence
of a Stal.-le Focus of Eycitation in the Cerebral Cortes." Inst. of Experimental
Medicine of the Acad. 1YAeg.Sci. USSR9 Lenir rads 1955. (Dissertation for
the Degree of Candidate in Hedical Scienceal
SO: Knizhnaya Letopial, "o. 35, 1955

VYSOTSKIY# B.V.; PALM, F.s.; KUZNMOY, A.P.
Onme animls as suppTwulzi reservoirs of pathogenic Z,eptoopira
natural-conaitious. Zhur, mikrob1oli'epJC,. j -1mi
lie -Ag 158.
(NM. IM01
I* Is Vladivostokskogo institlita epidemiologlig' pikrobiologil I
gigiyezv.
(IMOSPIRM33, transm.
by wild animals (Ram))
(AXIMAIS, die.
leptospirosis, transm. by wild anirals (#t4))
~U'
ff

KOLOSOV, A.A.; DEMIDOV, G.Ye.;,_KUZNETSOV, A.P. ,
Apparatus for removing dental calculus by means of ultrasonics.
Med. From. 17 no.9:53-58 S163. (MIRA 17-5)
1. Vsesoyaznyy nauenno-issledovatellskiy institut maditsinskikh
instrumentov i oborudovaniya.

S/193,/60/000/012/017/018
AO04/AOO1
AUTHOR: Kuznetsov, A. P.
TITLE: New Technical Equipment and Technology at the Chelyabinsk Sovnarkhoz
Plants
PERIODICAL- Byulleten' tekhniko-ekonomicheskoy informatsii, 1960, No.12,pp.66-67
TEXT: The author reports that a number of resolutions have been passed by
the Chelyabinsk Sovnarkhoz concerning the fulfilment of the Seven-Year Plan. He
points out that ultrasonic tooling becomes of increasing importafi~ae at the Sovnar-
khoz plants. The widespread use of ultrasonic equipment In various fields of in-
dustry results in great technical and economic effects. In 1960 the Troitskly
stankostroitellnyy zavod (Troitsk Machine Tool Plant) will produce 100 ultrasonic
machines for the tooling of brittle and hard materials, and 25 ultrasonic welding
apparatus. A number of shops of this plant have been rebuilt and reequipped,
which will enable the plant to increase the output of h1gh-quality ultrasonic
equipment during the next years. A special team consisting of workers of a number
of Sovnarkhoz Administrations, of the Chelyabinskly tr&ktorrvy zavod (Chelyabinsk
Tractor Plant) and the Chelyabinskly kuznec*.,mo-pre_-sovyy zavod (Chelyabinsk Plant
Card 1/2

3/193/60/000/012/017/018
AOo4/Aool
New Technical Equipment and Technolcgy at the Chelyabinsk Sovnarkhoz Plants
of Forging and Pressing Equipment), was created by the Sovnarkhoz to resolve
problems in connection with the widespread use of the seamless die-forging process
by the Shcherbakov method. The inventor of this method, Shcherbakov, and workers
of the Nauchno-isaledovateltskiy institut tekhnologii mashinostroyeniya (Scienti-
fic Research Institute for Technology of Mechanical Engineering) also participate
In the team. The research work carried out by the Tsentrallnyy nauchno-issledo-
vatel'skiy institut chernoy metallurgii (Central Scientific Research Ifistitute of
Ferrous Metallurgy), Zlatoustovskly metallurgicheskiy zavod (Zlatoust Metallurgical
Plant) and Chelyahinsk Sovnarkhoz, in the field of refining electrosteel'in the
ladle by liquid synthetic slag showed the possibility of obtaining high-criality
steel by this process. This refining process 443 to be lntrc4uced in some of the
Chelyabinsk Soynarkhoz plants In the course of 1961 and 1962,\
Card 2/2

t I A L I A A :I

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chargrM Meg& Ta theory, it la most wvmwjg~ uu hmve & it alAe
f4 qM
7- tni, n[alke 9vatern on tb,- engine, which wi-II change Aepen ling ir -~e speed . d I ad
L:~- . v q I en of
of operation. it s advisabie tu increabt U-.,~
h - .-_ -- -f , cl r ar-
type by dividing the air cleaner in)D two aections, w." 1he firqt Qfnrra n the eane
ranged rationally in front of the empressor and the second element located between the
~omxpreugor and the intake ovIlector.:
PR ENC L 00
A

KTJZ~ A.R.; MOVASTYRSKATA, M.S.; PAVLOV, S.A.
000
ionization coating of fabrics with latex films.
no-7:25-27 Jl 158.
(Rubber coating) (Leather, Artificial)
Leg.prom. 18
(MIRA 11:9)

BOV/138-59-4-5/2.6
Lyudvig, P., Monastyrskayag M.S.9 Pavlov, S.A#
TITLE: The Ionic Deposition of Carboxylate latexes, Communication
2: Increasing the Thermal Stability of Films Prepared from
Carboxylate latexes ( K Toprosw ob otlozhenii karboksilat-
nykh lateksov. Soobshcheniye 2, PovAheniyi termostoykosti
plenok, wluabtym~lh' iz karbokeilatnYkh lateksov)
PERIODICAL: Kauchuk i Rezina, 1959, Nr 49 pp 17-19 (USSR)
ABSTRACT:The first part was published in "Kauchuk i Rezina", 1959, Nr 1
Experiments were carried out on increasing the thermal
stability"of carboxyl groups containing latex films by
ionic deposition, The following factors were determined
for films made from SKS-5-30 latex: dependence of the tensile
strength on the time of vulcanisationg relaxation curves
and equilibrium moduli at 100011o elongation ( Figures 1 and 2)o
The vulcanisation temperature was 100 C PH 6.79 20%5
magnesium chloride was used as a vulcanisation agent.
Experiments showed that the tensile strength increased on
raising the vulcanisation temperature. Films made of latex
SKS-5-30 with polymethyl acrylate were also tested as the
introduction of polyacrylates increases the adhesion-of
carboxylate latex films to fibres (Figures 3, 4 and 5).*
Card 1/2 Optimum strength was obtained v&en 20%, of either polymthyl
777777777

SOV/138-59-4-5/26
The -Icniic Deposition of Carboxylate Latexas. Communication 2$
Increasing the Thermal Stability of Films Prepared from Carboxylate
Latexes
acrylate or polymethyl methacrylate emulsions were added to
the latex. Investigations on the action of calcium ion as
coagulating and:vuleanising agent showed that calcium
chloride can be used for this purpose. Films with the
largest degree of thermal stability were obtained by adding
melamine-formaldehyde resins to the SKS-5-30 latex and
vulcanising the product in the presence of magnesium ;Onso
'1~he reaction mixture was heated for 30 minutes at 100 0 and
subjected to vulcanisation for one hour at pH of 8.1; 201,60
magnesium chloride solution was used as a vulcanising agent
Results obtained duilng these exTeriments are discussed and
given in the form of graphs (Figures 6 and ?). The strength
of films was considerably increased when using SKS-5-30 in
conjunction with melamine-formaldehyde resins; optimum
results were obtained when 2o,% of the resin was used. The
vulcanisates show considerable relative elongation even when
30% of the resin is added to the polymer.
There are ? figures and 4 Soviet references.
ASSOCIATION: Moskovkiy tekb3lo1bgicbeakiy in~,titut legkoy prcmyshlezw.,~.
Card 2/2 -nosti (Moscow Technological institute of Light Industry)

KMNETBOT-A.B.d MOITASTYRSKATA, M.S.; PAVIOV, S-A-
wwwwwwwommmo- I
Problem of ion deposits of carboxylate latices. Report No.l:
Preparation of fabrics coated irith carbox7late latex by the method
of ion deposition. Kauch. i rez. 1.8 n0-1:13-15 Ja '59.
C (MIRA 3-2:1)
1.MoskovskiV takhnologichookiy institut legkoy prom7shlennosti.
(Rubber coatings) (Ion e;change)

PAVIAN, N.N.,, inzh.; inzh.j PMUZOV, G.A.0 doktor tekhn.
nauk,, prof'..
Complexometry of trivalent chromium. Report No.l. Izv. vys.
ucheb, zEtv,j tekh, leg. prom. no. 1:54,59 160. (MIRIL 140)
1, Moskovskiy tekbno3ogJLcheakiy institut legkoy prwWshlennosti.
Rekwandovana kafedroy neorganichaskoy i analitichoskoy kh4m4i.
(Chromium,Analyois)

PAnOV. N#N,, inzh.; JWKl3TSOVj_A.R.,lnzh..- ARBUZOV, G.A., doktor
takhn.nauk. prof.
Oomplaxometric analyais of trivalant chromium. Report No. 2. Izv. vys.
ucheb. zav.; takh. lag. prom. no.2:55-61 l6o. (MINA 13:11)
Koskovskiy.' -,ioglaheekty institut legicoy promysb1sunosti.
-.3~kcasadova~1"..ri~04ray aisorpatobaskoy I analitiebaskoy khtall.

PAVLOV, N.N. assistant; KUZNETSOV, A.R.,_~ssistent; ARBUZOV, G.A., doktor
tekhn.nauk, prof.
Quantitative analysis of chromium (III) in the solutions and films
of high polymers. Nauch.trudy MTILP no.18:0d-47 '60. (MIRA 15-2)
1. Kafedra neorganicheskoy i ana2Aticheskoy khimii Moskovskogo
tekhnologicheskogo instituta legkoy promyshlennosti.
(Chromium--Analysis) (Polymers)

PAVLOV, N.N., insh.; KUZNETSOVt A.R.8 inzh.; ARBUZOVY O.A.0 prof.9 doktor
--tekhn.nauk
Studying the stability of aluminum (III) complex compounds. Izv.
vys,ucheb*zav6; tekh.leg.prom. no.2t22-28 161. (MIRA 14:5)
1. Moekovskiy tekhnologichp'ekiy institut legkoy promyshlennoati.
Rekomendovans, kafedroy neo~ganicheekoy i analiticheskoy khimii.
(Aluminum compounds)

SIOBI1621000101210571063
B158/B101
AUTHOR:
Aj. R.
TITLE. Production of films by ionic deposition
PERIODICAL: Referativnyy zhurnal. Khimiya, no. 12, 1*962, 612, abstraot
12F276 (Nauohn, tr. Moak* tekhnolt in-t legkoy -prom-stil
n06 19, 1961, 31-314)
TEXT:' A description is given of a device for the preparation of films of~
various latexes (L) by ionic deposition on (cloth, paper)bases. Pilms
are obtained on a previously wetted fixative and a dried undersurface
placed on a horizontal glass plate under conditions similar to a
suggested technological process. A fixed amount of L is uniformly spread,
over the surface of the sample with the aid of a special device. The
thickness of the films is regulated by the time of deposition and the
amount of L. To reduce shrinkage, the films are removed,from the
undersurface before vulcanization. In this case they are poured in a
form wfth caprone fabric used as undersurface. The fabric pressed into
horizontal.form is impregnated with fixative, dried and a given amount
Card'1/2

S/081 62/000/012/057/06~
Production of films by ionic B15aXB101
of L spread evenly on it. Water formed during syneresid is removed from
the surface of the film by heating'with an infra-red lamp. The film is
dried for 3-4 min at 90-950C, after which it is easily removed from the
undersurface. [Abstracter's note: Complete translation
!3 0
Card 2/2

KUZNETSOV, A.R., assistent; FAVLOVp N.N., kand.khimicheskikh nauk, assistent
Chelatometry of barium solutions. Nauch.trudy MTILP no.23:
62-66 161. (MIRA 15%9)
1, Kafedra noorganioheakoy i analitioheakoy khimii Moskovskogo
tekhnologichaskogo instituta legkoy promyshlennostf.
(Barium) (Cholatometry)
R- rN