SCIENTIFIC ABSTRACT KLENOVA, M.V. - KLEPACH, P.T.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000723020007-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: December 30, 2016
• Document Release Date: June 19, 2000
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Marine geology work
S16141611000100810031004
D037/DI13
from 3,000 - 1#500 z and separate peaks are up to 19000 m high The North-
ern Atlantic ridge is also rugged with up to 4,800 m deep vall;ys. In the
bo.ttom configuration of the European basin between Europe and the Central
Atlantic ridgelthere are ridges with 600 m high and 3-5 - 4 km wide cones
from one of which fresh basalt was grabbed. These volcanic cones are upper
quaternary and recent formations. The European basin is deepest near the
shores of the Pyrenean peninsula. The study of sediment samples collected
in the north-eastern part of the Atlantic Ocoan will permit future Soviet
maps to be made more precise. The following classification of sediments
for navigation and soil charts has been established in the USSRs sand
with lose then 5% particles < 0.01 am)9ijilty sand (5-10,10S), sandy silt
M-30%)t silt (30-50%) and argillaceous a t ( >50% particles 4 O.Olms).
Fig. 1 shows the bottom sediment facies of the northern part of ta Atlantic
Ocean. A pre limin4ry investigation of cores has,shown that in their upper
layer (1-25 cm) the faoies shift considerably with time, the upper layer of
sandy silt or silt turning into a coarse sediment containing gravel and
pebbles. To the south of Newfoundland$ such a layer eAtends to a depth of
3,000 m and more. Above the submarine slopes the quantity of suspended
Card 2/5

8161416110001"1003
geology work D037/D113
solild mAGA'al increases.and -its mechanical cospositich changes In aAV,.
oluslon: the authors state that further practical and laboratory -fideat
will Mov the.goologlool,prooess*4 occurring in the Atlantl *0 Ocean," t41
morliaocurately def inad.. . The following persons participated'in the, ~w tOf.
the:--expeditions V#S. Sarasht'Ye-M, YMrinko# Sol. Olpyr Polo Yerofey
VAA1,,T6to*hzh*v-8hak0 A6V# llfin~ and T.K.'Xikoleyeva, A*Pj Kstal#81~,j
Vj1*-..".dUskhov'dmd V,Vo* Litvin are-als6 mentioned In the article'
3 figures and 14 referenoest .10 so,vist-bloo and 4'non-So~riot-bloco
glish4anguage refersdoes read is followas No Hillp Notes an the bai
m
i6,1 t of the '9,2. - At! i6& ~Deep_sss, Res, vol .39-19561 MOV, Ki
etr -char ant
n6vio 906haftl"2 composition of sediments as indicative of tha Conalt
iflepositiono congress. 'Report of the, 114
sit Sritfiin#~Stoi Sa"LO60904,
session Or ad a
2cord,:3/5-

Card'4/5 Pig. 1
- ~~ ~ ~v

Marine geology work
3/614J61/070/008/003/004
D037/DI13
Fig. 1. Bottom sediment facies of the northern part of tho Atlantic Ccean.
N facies of the upper level (1-25(ca)l
b facies of the underlying level 26-85 cm);
(1) outeropul
n
a
i:t;n clayl
d ibtution border of elastic fiolon;
4 facies of elastic sand and sandy siltj
5 carbonaesous elastic faciesl
6 carbonaceous facieel'
7 argillaosous facisel
8 volcanic faciest
191 large-fragmental facies,
Card 5/5

XMIOVAS NJ*
Origin of the r*Wf of the BMWU S" bottmo ToP*PQ9* JW*52S
165476 16le Od?A 24t6)
(VarenU Sea-0o"a-bottes)

KLENOVAj H.V.1 GERSHANOIICH9 D.Ye., red.isd-va; VOLKOVA, T.G.p tekbu.
.1 POLYAXOVA# T.Y.,, takhn. red.
(Sediments of the Arctic Basin; based on materials from the
drift of the icebreaker," O.Sedov.010sadki ArkUchsskogo bu-
seina po materialas dr*ifa Vp *G.Sedov.0 Noskvs, Izd-vo
Akad. nauk SSSR, 1962. 103 p. (HIM 16t2)
(Arctic regions-Deep-sea deposits)

EURIOVA stI47M; SOWVtYEV, Vladimir FUIppovich;
0 Iya A.Ukeandrovasl VIXMMO# Nina VAkamm;
KULAXOVA, lAdiya Bergeyma; XAMq Isgor GeorglyevIabj
RWMj Vladislay Gavrilovicb; MCMAKOVA, Nadezbda
Sergaymal ZEMKOVICH, V#Pop otv. red.1 LSWITZVp O*K.p
rod. Isd-va; UDYCMj L.P., rod. iad-im; GM'MXAj O.M.,p
tekba, redo
[Geology of the subsurface slope of the Caspian Soa]C*olo--
giabaskoe strosnU podvodnogo sklona Xaspliskogo moriae
LBYI M.V.Klenova L dr. Moskvat led-vo Aked. nauk SM9
. (KIRA 150)
19620 636 PO
(casplausea-Geology)
~Casplan Depression-Geology)

s/169/62/000/008/056/ogo
9202/E192
AUTHORSs Xlenovat M'Vot and Zenkeviche N,L,
TITLE: Geological works in the western part of the
North Atlantic
PERIODICALt Referativnyy zhurnals Geofizika; no,8, 1962, 4,
abstract 8 V-19. (Tr* Norsk. gidrofiz. in-ta. AN SSSRs
251 1962, 142-186),*
TEXTt The results obtained during the voyage of the Research
Vessel "M.Lomonosov" in the fields of marine geology according to
the IGY plan are given# The basic directions of the studies were V/
as followas the study of the sea topography and.tho geomorpho--
logical interpretation of the collected data, and the study of
suspended matter in the waters of the sea. During the entire
voyage of the ship, sampling oftho bottom with a direct type
impact tube and bottom scoop type "Okean" was carried outg together
with echo sounding and also sampling of the suspended matter.
The region of the studies was contained between approximately
450 and '100 N# The ground sampling was carried out predominantly
over the depth in excess of 4000 mo The topography and geological
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Geological works in the we Istern s/169/62/000/008/036/090
Z202/E192
structure of the region was described on the basis of the above
data. It was noted that the results of the studies of
"M.Lomonomov" in the vicinity of the eastern coast of N,America
are in full agreement with the data given by the American marine
geologists. The mechanical analysis of the sediments and analysis
of the composition of the aleuritic fraction carried out on the
ship gave quantitative charActerisation of the more Important
peculiarities of the sediments of the region studied, Mechani,,sl
analysis of the surface layer using microscopic method based on
the use of the graticule eye piece of Glagolev has shown that this
method may be fully utilimed to define quantitatively the
composition and designation of the sediment according to the
dynamic classification, The analysis of the matter contained in
the surface layer of the sediment together with the data obtained
from earlier voyages led to the compilation of a distribution
diagram of the mineral grains in the aleuritia fraction, which
confirmed the paramount importance of the scattering of mineral
material from the mainland in the process of sediment formation.
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Gcologica4 works in the western S/169/62/000/0o8/oWo9o
E202/E192
The biogenic components begin to play a noticeable.role,.in the
composition of the sediment only in those places where the
influence of the detrital material is no longer dominant, The
distribution within the sediments of various biogenic components
is closely connected with the-hydrological ionditions. The
decrease of the detrital componqnts in the a4euritic traction
down to 6*41,~ was observed only.in the region of the Central
Atlantic RidSe over a distance of Above-2000 miles from the nearest
(South American) land. In the eastern direction, irrespective of
the great distance from land, the quantity of the mineral groins
in the aleuritic fractions does not decrease.
42 rererences,
rAbstractor's notes Complete translationj-
Card 3/1

MMOVAO M. V.
Suspended utter In Us Atlantic 00san as an indicator of the
structure of ths water layer. Trudy Inst. oksan. 561223-229
162, (MIRA 15tio)
(Atlantic Ocean-Vater-Ana2yets)
Aldl~
e Z4

XLEWOVAO M.V.j LAVROV$ V,M.j NIKOLAUVAp VA.
Distribution of the suspension in the Atlantic Own and Its
relation to the bottom topography. Dokl. AN &W I" no,,5s
1153-1155 JS 162, (XIRA 15j6)
1, Institut oksanologii AN SM Prodstarleno akadsaikom
MAhcharbakovyx jAt1anUo Ooesa-Zedise.utation avA deposition)
(Ocean bottom)

UXROVA,t MoV*
alassification of recent mrine deposits, OkeanoloWa 3,
noo3s527-537 163o (MMA 164)
(Deep-sea deimelts.-Massifloation)

KIIIXIA 0 N.V.
I'Ome rex'AtO of tho atudy 'of tiantic
ocean and tt~o s(nithern jArt of flo-
eldrofiz, AN URSE
~7

KIENOVA,-H,~Y.; IAVROV, V.M.1 YEROSHCHEV-SIIAK, V.A.; NIKOIAYEEVA, V.K.
Works on marine geology in the northern part of the Atlantic
Oceans Trudy Mors gidrofiz. inst. AN URSR 3006-115 164.
(MIRA 17t11)

ACC Nks AT7003622 OMM Ms tM/3090/66/000/015/0112/0117
AMOR: Xlonovas N.",
ORO: none
i7TLZ% New date on the geolqw or the Atlantic Ocean
SOURCE: AN WSH, MethduvedometyenrW geofixicheskly komitst. X raMel programW NO01
Okeanologlya., Gbornlk statey# no. 15, 1966. Okeanologicheaklys Issledovanlyag,
112-11T
TOPIC TAGS: hydrographic surveys ocean dynamics, ocean floor
topography 0 ocean property) S-rom if 004WOwy
ABSTRACT: This article covers the geological investigations on the r/v's "M.
Losonosov," "Equator$" and "Sedov" d=ing the Iffand IGC. An analysis vaa conducted
of the geological features of the ocean bottom. As a result of sonar soundings e.
smoothed plainss occasionally step-like* vere found at different levels In the
northern part of the ocean, Some of these vere related to submarine terraces of th
Barents Sea and other northern sees. The submerged wuntain region vas observed at
the continuation of the Farm lslands--~the Faros rises as vell as nev seamountes the
"Michael Liomonosoys" Professor Per*zUn#" "Academician Krylov#" and "Professor
Mesjazev" banks. In the Idd-Atlantle Iddge areas characterized by the alpine type
of relief vere observed Mjecent to ancient an". Gem probable volcanic Cow
card 1/3 VOCS none

were studied. The bottom relief of the Atlantic Ocean represents a system of inter-.:
sected submeridional and sublatitudinal structures which reflect the planetary
I
process of alternation of submerldional. and sublatitudinal movements. Just as in
other basins, the dependence of sediment thickness and the rate of sedimentation on
the bottom relief was found from cores. Maxima rate of sedimentation takes place at
the foot of the rises and hills and at the bus of the continental slope. The more
ancient rocks approach the surface of the rises and have been revealed under layers
of cores. As a result of slov sedimentation sman sediment thicknesses am typical
of the basins. The study of AWsleal composition on one-layer preparation from fresh
material on the research vessel resulted In the determination or the relative
Importance of rock-forming mineral and organic components. The following facles am
,distinguished: elastic$ clastic-calcareous# foreminiferal, coccolithophoral*
silicispongeouss and sediments of volcanic origin which were found chiefly in under
layers of cores. The altered remains of ItqAlarlopsis were found In sedimenta of
Brazilian and North American basins, This fact confirms the penetration of antarctic
waters Into the equatorial and northern parts of the Atlantic* The secharical.
analysis by microscopic method showed the relationship between the distribution of
sediments and bottom rellef, The detailed description and study of dry core cuts
revealed series of steps of carbonate and elastic sedimentation " well as
distinctive textural pecullw4ties# which are feebly marked In the cuts of moist ems.,
There were thin strata of relatively consl6grained meterialg slideq and hieroglyphic
textures connected vith the worm-boles# peculiarities of stratification planosq and r-
Card 2/2

., ACC NL ATTOO36N
3/3

3
SOURM C01011
AUTHORS Kle o,-X,-Vj Lavrovt V. M.1 NikolayevatiV. Ks
'~~_Rwa
ORGI none
TITLE: Peculiarity of suspended matter distribution In the Atlantic Ocean
41
SOVRCEt AN SSSR, Mezhduvedowtveunyy geofitichaskly kouLtat. X razdel programmy
MGC: Okeanologlys,Sbornik statty, no. 15. 1966. Okeanologichaskiya issledovanLY86
TOPIC TAGSt hydrographic surveyo ocean dynamics, ocean
propgrtyp ceanographyp oeeosa ikee)j' nrof4*G&A P'*L/.t k7r-SeAze#
WOA =4m'rolc! evogo.)
ABSTRACT: This article describes the research conducted by the r/v M. Lomonosou
during cruises carried out under the ICY and IGC program. Suspended matter was In-
vestigated using weight and microscopic analysis methods. Qualitative and 4u&ntitativd
analyses of suspended matter were wde. Substance composition and distribution were
used as indicators of water was" * In the northern part of the Atlantic Ocean. the
Arctic (Labrador) water was found to contain suspended matter with heightened coutdot
of diatoms above great depths and a mineral-diatomaceous suspension at the NewfouadaI4
Bank. Distribution and types of suspended matter are given for spring and fall on &!
diagram of the northern part of the Atlantic Ocean. The Atlantic Current waters colk-
tain detrital-uinetal particles in simpension; in the region of entry of Mediterranean
waters the matter in suspension in enriched by coccolites. The region of StA;arctic
I nnna

ACC
AT7003623
imixing is characterized by suspended vatter of mixed,composltion with heightened
content of diatom and coccolit". The weight amount of suspended matter approximates 1
0.5 mg/l in autumn and about 1.1 mg/l in spring. The vertical distribution of sus- 1:
pended particles confirm the importance of bottom morphology for all marine proc"SOV
lAbove seamountoi, ridges, and rites, the content of suspended matter incre"es from
surface.to bottom. On slop" an increased amount of matter in suspension is observed
at depths of about 3000 a. At depths of about 800-1000 m the suspended particles
nearly vanish; In the upper layers they increase again but do not exceed the content
of bottom layers. In foothill ion" the distribution of suspended particles is
homogeneous from surface to bottom and amounts to tenths of mg/l. The study of sus-
pended matter reveals concrete relations between hydrological regime, relief, and the
distribution of sedisentse The investigation of suspended matter mot be continued
in order to specify the peculiarity of water moveodnt and to study the chealcal and
mineralogical composition of suspended matter " Initial material for bottom deposits#
A section from the English Channel to norids, shows the transparency, particle size.
and vertical distribution of suspended matter in the Atlantic Oc"n. Orig* art* h"s
3 figures and 2 tables. (DA).
SUB CODSs 08/ SUBM DATISS none/, ORIG RIF: 0091
2/2
1, Card

ACd'NC_AT76_0362
SOURCE CODES UR/
Avnm Klenova, m. V,; S&V611yevap P.
..................
IORC: none
TITLE: Sediment saps of the North Atlantic
66/000/0151012410130
SOURCE: AN $$SR. Methduvedomstvennyy goofitichaskiy komitet. X razdal programmy
Sbor'nik statcyg no. 151 19660 Okesnologichaskiye Issledovanlya,
MGG: Okeanologiyas
124-130
TOPIC TAGS: hydrographic survey* ocean currentg ocean dynamics, o0an props)RI
'ABSTRACT: An evaluation Is given of the sediment maps for the Atlantic Ocean, The
first map was compiled by Murray and Renard (1891) and is still used with some modift-
cation in handbooks and textbooks; it shows the distribution of terrigenous deposits
("blue" mud) and pelagic deposits (globigerina, radiolarian, diatom, pteropod ooxe,
and red clay). Similar designations are given on a map compiled by P. L. Betrukov
(1961). The sediment map of the Naval Atlas (1952) was prepared on a different basis.
In the Naval Atlas chart and the Great Soviet Encyclopedia, the navigation classifi-
cation was based on the content of polite fraction 50% of this grade*
p: foraali
Some components of substance composition are also shown on the ma Wera,
concretions, stonesp shells, corals, ate. The chart Is based on the Idea of sediment
UDC: none
ACC'AR" AT700-3'624
t,
I
disperelen an a primary property of bottom deposits. During IGY and ICC investiga-
tions the chart was revised. DeterPination of CaC0 showed that carbonate sediments
are distributed -more widely than was shown on Murray's and Correns' charts. Content
of CaCO In the surface layer to connected with the polite fraction content, but the
former incre"es'more rapidlyjaince C&CO In mud sediments is formed by Coccolitho-
phoridae, individual coccoliths, carbonate detritus, and pelitic carbonate, while
foraminiphera enriches only more coarse fractions. When elutriating in water, the
carbonate particles disintegrate and the results of the analysis correspond neither
to the visual description of sediments, nor to their physical properties and deposi-
tion conditions. The microscopic slave analysis gives more reliable results, but
further investigations are necessary for working out a method which would permit
the reflection of the distribution of sediment tipee In conforalty with conditions of
deposit and properties, The article includes three diagram of ac"n floor s6il types
of the northern Atlantic Ocean, Ori&~ art, has: 3.figur" and I table. JBAJ
SUB CODE: 08/~ SUBM DATIs
none/ ORIC Rat
010/ OTH REF: 009/

AXOPOT. Ll-: MYATUAYAt Yo.A.: MMOTA. 8.1.
Ow
Capsella bursa pastorls as a bImA aosedation, larm,j toks. 28
no.lA348 Ja-l 155. (XLU a I?)
1, tafedra farmakologil (sav, doteent I.I.Akopov) SmarkwAskago
pleditsinskago instituta Iment t,P.F&ylova,
(PUMSO
Oaps*lla bursa'pastorlso off. on blood coagulation)
(BLM CQAWWtOgs effects of drugs on.
Capsolla 'bursa pastorls)

KUJIDVA, Vera: YANTIS, Alfred
Antidotes to methyl alcohol poisoning, Cook# oftbe 13 wall
71-77 Yeb 570
I* Ocni a nourochirurgicks. klialks VIA J. Dr. P, v Rradel
Iralovo.
(ALCOWL XKM It.
.ntld.ts. (;or)

KLMp XLUsjXUCK0YA, Teral POCUZZA, Zdawki JWp Zboat
Ploarders of v1slon In orpmol" 2mdma of the chiasmatic cook*
orth. 17 nQO4/5$241,--,W 12'16L,
Ukarsks faknlt& lar2ovj~ daiversity v BMci Kmlovs, Imtodra
amibo 2skantwip prodnosta prof. Mr. M. Ulm.
0MC NW dis"ses) (VISION)
M MCOPZASW patb*2)
M

KLnAA, Milool _KL.:-.IIOVA 9 Vera; PIUXHAZKA v wenek; JUAN, Josef
Disorders of vision in GxPGn8ivG lesions Of the ch4gs2fitic region,
aborn. ved. prac. lak. fak. Karlov. univ. (11rad Twi) 4 no.2sn9-137
161.
1. Ocni klinika dno ta prof. Mr. H. Klima.
(CipTIJ (WWH MXKASM physiol.)
(Vial 1)

KLOWA, Vera
Contribution to Uw tr"toent of conjunctivitis. Sborn. vedo praos leks
fak. Karlov. uniye (Brad Kral) 5 no.107-92 162.
lo Ocni klWkal prednosta of Mr. M. Klima.
(COHnNOTMTIS) rMLIM) , (ACRIDINES)

MIKUTUN, A.I. vraah&. UMWA,--,V.A.o meditainalmys sestra.
Magorsakov on lhe poouliaritlas of care for nental pattentso
Ked.mastm 18 A6.9140-0 a 059. (MM 12:11)
(NORSAXW# SZWI MORMCK, 1854-1900)
(pMausic IMIM)

HIMMOV, A.X. 9 vmobl KLMMAj V*A.,p wditsinsimp sestra
Charaoterlatics for cue of pationts vith mdo-&"* pIT* pwbosis.
Mod. sestra 20'nods44-49 Ag 161. (min 14S 10)
(MANIC-DEPMSIU PSYCHOM) -

KIXMICSO Iwo
Conduct of social Insurance In Bowsy County, MmIm n w*788-9
n 161,
1. Ssakosemosti Tanadalambistoositami 105yout Somogy mgyGI
Alkospontjanak vesetojoe
Muory6-Insuramet Social))
9wagarp-Trado unions)
i

RAZUMIKHINP Nikolay VasillyevIch, Frialswa uchastiye KLF2;OVITSKIT
N.P,j MROVSXJffAs T,Ip red*
...ON.
[Experimental studies of the evolution of the roundness
of rack fragments) naperimentalOrqe Ireledovanila evo-
hutsil okatannosti ablomkoy Comykh porod. LonitAradj
Leningr. unt-voj 1965. 65 p. (MIRA 18s12)

KMOVSKAYAt K. 1.
"On the Pathoanatomical Changes in fatal 4ectrotrmirA." Cani Had Scip
Uningrad State Medical Pediatrics Instp L*ntnpvdp 1954. (KL, No 5. Jan 53)
Survey of Scientific and Technical Dissertations Defended at USSR Higber
Educational Institutions (12)
SOs Stm. No, 556,, 24 Jun 55
!Up

P/035/60/000/W3/00e/006
AOrjolAW6
AUTHORSt Mindowics, Jerzy# Doctor of Baginoerlng,-Assistant Prof*ssorl
Klenowioz, Zbigniew, Master of Engineering
T1=3 Examination of Hunt Preventing Properties of lubricants by Means of
Static Water Drop Corrosion Test
PWOMCALt PriegIfid Meahatom, 1960, No. 23, pp. 694 - 698
TEM The article describes the static water drop corrosion test developed
by the Research Laborator7 of the US Navy In 2949. Further, a nuidw of lubricants
produced in Poland were tested with the above method and results we described.
The best,anti-oorrosion proportion showed the aviation lubricant Type SP-1, a rifle
grease and the anti-oorrosion lubricant Typo LT. The worst wore technical vas*11ne,
spindle-oil 2, TDK lubricant and aviation oil Type HS 20. Further, the authors
describe the advantages of the static water drop corrosion test and suggest this
method for being adapted in Poland. Thor* we 5 tables, I photograph and I figure.
ASSOCIATIONt Politsohnika Odafinka (Odafisk Polytechnic)
Card 1/1
IN

XWSXIY, A.Yo; TURAMs N#A,l TSUMEV; A,I.j GARANINAt L.F.p
~-fied
(The city of Gorkiyj a conolso mnwa] Gorod Gorskil; kratkil
spravoobnik. Gortkiis Gortkovadmo krdshnoe isd-vo. 1963.
2 53 (MIRA 17s4)

MRAS, :,r*d,l ROIGASt Eop redo; LWI, Is, red.; ~412AIM4-A&4-
redo
[TrUbomoniasis of the urogenital tract; a collection of
"Clail Trikhomonas urogenitallnogo trakta; sborn1k at&-
tei. Tanins AN Estonskoi &U,, 1963. 213 p. (P.IRA l7s6)

TOM, TuAh,(Teras# J.1t red.; LW I A red.) PIMj Kh-0-
(pibl,, H.1p rod.1 TALU09M; I:T:tT&1lx*isUr, 9.1, red.j
TAMBO L.X.(Jfirxu . 1.). red.1 - MIT I S , -uc redal
BVASTOYANOV# As# rW*; p X,p tekbne redo
f1westiptions in microbiology] Issledovwdia po mikrobiologil.
TA114rrn. Volalo 1961. 221 p. (K= 15 s 6)
1, Resti NSV Teaduste Akedesulas ZkgppriM=taaage ja X144n4l4s*
Reditaiini Instituut,
(MICAL 141CROBIOLOM)
MOVIE"

BOGOVSMp Pavel Alsksandrovi h ELZMW# X.S., red.; SEVASTITANOV, A.,
",,:I
redo; TOCMSMj X.0 to
[Carcinogenic effect of products of Estonian oil slale] Kantserogen-
nos doistvie produktov pereraboth estonskago sl&ntea T&Mmip Akad,
nauk Estonskol. M, 1961, 349p III, V. ?mIRA W12)
(EMONU,-.41L SHAT (CARCINOMS)

HAKWO2 Paul' KhanSOV10h; KLENS11T, K.S., red.
(Seasonal quantitative dynam1cs of soil becter3a "
factors determining It) SezonWa kollebootvannata dinatike
pochvenzWkh baktarit I faktory, obuslaylivalushchle ea.
Tallin, All Istanskal &,;R, In-t ek"rlxantallnol biol 09111,
1964. 234 P# (MIRA 1911)

KLF,NTS;W,Rt Imres Cand Agr Sci -- (dies) V 6cadwe
in the 7seea Fr-0~74IViMj" Mos, 1958, lb pp (Mos Orfler of
Lenin Agr Acad im K.A. TimiryazeU) 110 coiiies (KL# ?3-5b, 109)
99 -

kzl"is O-f labor involved in the repair of equlpwnt In
metanurgical productione Sots. trud 8 no,12:93-1W D,;61.
(KM 17
Numm or 0 IN

Adrenaline and adroalinelike substances in the blood in pe is
uloer.,Yraobe delo no*$s3&-4l A6163. (KMA 16V
1. Xafedra khirurgii No.1 (%&v. - prof. V.I. Akimm) Kiyevsko-
go inatituta umovershenstymnlya Ymbey,
(ADMMAUM IN M BCDT) (MTIC M.CEIL)

na-MRIN. M.
7668. KLMUSHIN, X. -- n& trelevochnom traktore (Ruesk" traktorista gynov.
lospromMosa. lit, tapts' X. S, Urvsklna). Molotov, Xn, Isd., 1954, 24 s.
20 ca. 3.000 eks. 301.-(55A2i8_)p_ 634.992.5:656.13st(47.813)
Xontrollnyye sadanty4L I ustodlebaskire ukazanlya po kursu *T*khnol*6i"
metallov I dereva",, -Sm. 7630
SO: Inis latuals', Vol. 7, 1955

NURABHDV,p Y,6,70- strict IW&4 Veterinary rwtor),
Veterinary Doctor of an Zxperimental Model haul Noiaorsh District.. Winin
Oblast').
"The vork of Yeterinary.speei"ta at an experimental model fam..."
VeterinarlYa.- Vol. 39s no- 30 ~Much 10 13.
R

jLUZX OVp V,,Dj SOROXM, To,I,l VIMMMA9 rI,M,; ]MtWlXAP
.0. XHOXHLAN# A*8*
-SLV JOL
ft-ddiwor of aotinWain belonging to the fluorescent *.of I
A.atinmycatess .Sr*V Inst, aicrobiol. no,6sl93-201 19.0
(KIPA ]AS-1)
1; Teem ft"~WisslodovatsX!skiy insti~ut antibiotikow,
M*Okva.
(ACTINKYWALIS) (ACTINOMT

lAVMWA,, 10.D.1 KPAVC=Ut X,A.j 17MPIMO CIV.
Nature of the onsymatio activity *f lysosyms lxyoAl SSSA Otdo
k"navk no.4029 IP 161. (XMA UW
Is Imstitut, organiabookoy kbiaLU Ins X,D,Zellnekogo AN SM,

P;
News UMPMt Ao A*
Dusertaticas Cbmaw An Abe cautent at, I*id" in the blood mama
patimu idth arurloaciamix WA wpertocu due&"
In treatmat vith lwitbU
Dum: Cad Ned fti
AcM *d Scl WR
PafAj&ZC;-e Date, P2"es 1956, Yloscow
&mftet ftliboys 14t":W Ip No 4T., 190

IUVCHSMKOS N.A.1 XLBOPM* Q.Tj ~UVMWAq To.D.
StWy of the oatalyU"Ily &*Uve oonterm of lywqm, DWa.
AN SUR 1" no.isn&221 W 162. (xMiL 1515)
le inatitut organi4bookoy WWI La. V*D*Zolizakop AN SM.
PredstavUno akaftnikon BoAslasmaklas
NPOSYM) (C&ta4vis)

KRAVCMXXOj X.A.1 Ktg"At O.T.1 XXVSRVMs To.D.
Isolation aM d*uatino of th* proftets of lywosyne nodLfied
by lodcavetle &old@ Biakb4=41& 30 no. 31534--%2 MY-40 #6
WRA 19113
Is betitut orgulebookoy kMaii immi Selinskogo AN SON4
140sk"O

VladimirowA;
KRAVCHENKO, Nikolay Alekservith; KLEOPMAj,,G'.- otv. red. j
KAVERZMAj Te,D.0 doktor khlm* n9uko
SIMMKOl E,I* , red,
(Hatual for the chrovAtOgruPhic analysis of amino acids
on colums] RukOvOdq+.,vo po khrmAtografichaskotu Anauxu
aminokislot n& koloaakh. Vloskvap Naukap 19649 69
(141RA 182*

F7JVClTENXV, N.A.; U"PIM G-V-; KAVk,v'--`vW~A YA U
0 4 .
Study of the reavtIon of ci.-t*)ry-mrthylv ton of lyioryro, wil-h
iod,lacetic &-31d, ldclKbl:--A.Ist -10 no.1119~--202 J'a-? 1-6!.,
(VIIA lh6)
1. inatitut organlohesKny- r~';Z)Rs
MO-4kVa.

KRAVCHENKOp N.A.1 KtEOPINA GG-V~~; XAVERZNEVAO Te.D.
- w "ej ~. ~ I
w
Study of .an aetive conter of lysotyme by thI carboxyzethylation
method, BiokhWia 30 no*4013-720 Jl-Ag 6% (KrPA isle)
1. Inatitut organichaskoy khImil Imeni N.D. Zelinskogo AN SSW#
Moskva$

KtEOPINA-G.V.j KRAVCHEHKO, N.A.1 KAVERZNEVA, Ya.D.
Role of C--amlno groups of lysins in lynozym. 1xv. AN SSSR. Ser.
khim. no.5030-838 165. (MIRA ISO)
1. Institut organichaskoy Wait ix,,N.D.Zol-inskogo AN SSM*
-1 il -

SOCHAVAs Vs; KLEOPOVI I.
"Problems In the geography -of the Far East.* PAwiewed b7 V.Sochavo,
I.Kleopova ltv# Vass. goo'. ob-va 93 no.6t54&548 N-D 961, ~'
(~au 15:1)
(Soviet far last-Geograft)

S/120/62/000/004/003/047
zl94/E420
AUTHOASS oo Login, S,P,, Okorokov,,I.S.1
Nov*
TITLE: operation or the supply system for a proton
synchrotron of 7 GeV during th4 starting period
PERIODICAL: Pribory i tokhnika 'eksp*rimenta,. no.4, 1962,. 33-36
TEXT: ' The article describes-early operating experience with
the magnet supply system, the performarico and construction of
which are described in the present journal (27-33 - preceding
abstract). The equipment usually works continuously for up to
5 days per week followed by a regular weekly shut-down.. In.
6 months it-has operated for a total of 2200 houirs. The faults
that have occurred resulted only from defects in the control
circuits, mainly in the ignitron firing control arrangements.'
A few backfires occurred because the valve temperature conditions
,were not right, mooIt backfires occurred under inverter conditions
for which the beat lead angle was about 400. The different
kinds or rauit, their causes and the steps that were taken to put
them right are described. The stabilization of the primary
rectified voltage is described and the operation ofthe control
Card 1/2

5/12o/62/ooo/oo4/005/047
Operation of the supply system oe, E194/E420
reactors which govern the transition from rectifier to inverter
conditions is examined. Performance of the equipment is
illustrated by oscillograms, There are 5 figures,
ASSOCIATIONt Institut teoreticheskoy i eksperimentallnoy fiziki
GKAE (Institute of Theoretical and Experimental
Physics GKAE)
SUBMITTED: April 11, 1962
Card 2/2

S/120/62/000/004/038/047
9073/9382
AUTHORS i Kleopov, I~F* and Lazarev, 14,V.
TITLEs System of current supply for the maSnetic-moasuroments
bench
PERIODICALs Pribory i tekhnika ekspertmenta, no. 4. 1962.
203 -:2o6
TEXT: The systom dexcribre~ produces once every 30 seconds
an autonintic sequence of current cycleb in five series-connected
ma4netic blocks (L a 0.15 henries, Hy u 0.11 ohm) which
simulate the cycle~of the main'curr'ent supply system of the
accelerator. The current in a cycle increases at an initial'
rate or 1 670 A/see. reaching its peak after about.1.8 seconds
and fallIng to reach zero after 3 seewds. The current for th*
magnets or the test-banch is provided by d.c. generators. At
the initial instant the blocks are switched onto a stabilized
voltage U1, which ensures a given rate of current increase.
For coropensating the voltage losses caused 'by the resistance of
the circuits the voltage is increased continuously to the value
U2 etarting at a suitable time after switching on. When the
Card 1/11

5/120/62/000/004/038/047
System of current supply E073/9382
current in the system reaches Its full amplitude the polarity of,
the voltage in reversed so.that a now value of t~e voltage U 3 Is
reached, corresponding to the given rate of decrease or the current
strength. When the current drops to zero, the magneto are switched
off from the supply :ystem and the circuit returns to its initial
state. Two series-c nnected 230 V, 1950 A generators, with two
sanchronous motors of 6501k'W -each are used as current sources. Two
threo-phose,thyratron rec tifierm food the serits-excitation windin!rs
of the generators. The block schematic of the supply circuit is
given in Fig. 3. Forspeeding-up, the reversal of the output
voltage of the generators, their excitation windings are switcb*d
onto a voltage of opposite polarity when the current aprroaches its
full amplitude vnlue. The switching'is effected by a low-curront.
fastrelay,connected'into the grid circuit of the thyratron
rectifiers, which are connected in parallel in oppoiition to each
other, whereby the-control circuit excludes the possibility of
their operating si ltaneousily., The current cycle in the magnntic
Mu
Card 2/4

System of current supply so,
Eig. 31
C,
OF P
Re 6w
Card 4/4 D(:,Av4PIIfi#v Pa,
S/120/62/000/004/038/04?
E073/9382

4( )76h
9/120/62/000/004/045/o47
zo39/x420
AUTHORSt Sokolovskiyj V,Vs, Radkovich, I.A.2 Golldin, L#L$j
Xleopovj 10F., Xulskov, P.M., Lusin, V.No,
44wz&-r*-v-jskiy, I#A,, Okorokov, I*So, Talyzin, A.N.,
Trakhachav, G.V.
TITLEt The effect of changes in the r~glme of the proton
synchrotron supply-syttems an the magnetic
characteristics of the blocks
PERIODICALt Pribory i tokhnika oksperimenta, no#4, 1962, 240-244
TEXT: Measurements are made of the effect on the field and
gradient in the C and X-blocks at a level of 90 Sauss when the-
final smoothing condensers are e1ther disconnectled or connected
symmetrically or non-symmotrically4 in addition, the came when
the final smoothing condensors.&re in circuit but the primary4
smoothing condensers are reduced to one quarter of their usual
value is examined, The offset of a shunting thyratron and
resistance is also*investiS&ted. Changes in the value of the
field cikused by any of the abovedo, not exceed + 0,6% while the
difference between blocks is about + I%# The ;ffect of those
Card 1/2

S/12o/62/000/004/045/047
The affect of changes 9039/z420
circuit changes-on the rate of growth of the field covers the
range, +3.2 to -8,3% and for thit,differ*nce between blocks
+.5,2 to -6.9%. Changes of the working range without altering the
circuit produce significantly smaller effects than are produced by
circuit changes, e.g. changes in the average field of separate
blocks are 0.2 to 0.3% while the difference between their fields
changes only by 0,02 to 0605%. The introduction of an auxiliary
control an the value of the residual field noticeably increases
the accuracy of the resultst i*ee error reduced to less than a
half its previous value. There or* 3 figures and 4 tables.
ASSOCIATIONSS Institut t*oreticheskoy i skoperimentallnoy fixiki
GKAE (Institut* of Theoretical and Experimental
Physics GKAE)
Nauchno-imaledovatellskiy institut elaktrafisichaskoy
apparatury M & (Scientific-Research Institute of
Cloctrophysical Apparatus GKAE)
SUBMITTEDi April 11, 1962
Card 2/2
;?

S/120/62/000/004/030/047
2140/Z420
AUTHORSI Kulakov, P.M., KAfdash, A.A.. 9obQVAkoV, A.306
Spevakovs, P.M., GDA'din, L*Lol Xloop4v# t#F#*
Koahkarov.
Sharnov, 0.1.
TITM The system for magnetic field the
proton synabrotron.
PERIODICA1.1 Pribory i tokhniki Oksperiments, n0.4, 1962, 158-16?
TEXTs The magnetic field configuration In the strong-fosused
7 GeV machine is adjusted by a series of correction systems . I
permitting the betatron oscillation frequen4y to be controlled
and resonance disturbances at the orbit to be ellminate4. The
system used tar field correction As described together with the
system for switching and exalting the windings, with experimental
data on their attest an the %oan. The windings permit
adjustment of the magnetic field detay Index. the azimuthal
asywAstry of the field. ecopensation of tho.nonlinoar distortion
or the ifield with saturation, correction of the position of the
neutral plane &ad the "ttereates between the focusing and
Card 1/2.

5/120/62/000/00%/0)0/0%7
The system for magnetic field S140/2420
dofetusing groups at blocks. There are two sets at those
windings, the "gradient" and the Ononlinear* windings an the
nAgnetic Palo surface facing the chamber. Measured date
presented in the atti:16 Indicate the effectiveness or the
corrections In stabilizing the betatron frequency. flow*ver, it
to considered that further adjustments will be made In the course
of the work.. There are 15 figures.
ASSOCIATION$$ Institut t*orstitheakey I sksperimentallney tisikk
GKAZ (Institute at Theoretical and Uperimental
Physics GXAZ)
Wauchno-Issladevatelfskly Institut eloktrarinicheskoy
apparatury ML42 (Solontitia R*aearch Institute for
gleatrophysical Apparatus QXAR)
SUBHITT&Dt March 294 1962
Card 2/2

3/120/62/000/oot/047/047
2039^420
AUTHORSs Vlodimirokly, Y.Vs, 4614dift. L.L., Pligin. U.5.,
Yeselov, M,A,, Talysint A.X., Taras6vi TOOK*$
Kashkarov, O.ao.'L&pitakiy 'N&., 11arabash. LAs
Peopov, X.F4 Lobodev, Poi Kux'sin, A A..
In Ono4ovsklyt K.X.o Uvarov,*V.A.,
Vedoplyanov, r*A.
TITLEs Adjustment or tha.~aceleratton rogivas of the 7 GeV
proton synchrotron
PZRIODICALt Pribory I tokhnika skeporinonta, no.4, 1962, 246-255
TEXTs In order to establish the optimum parameters for
programming the control frequency the Intensity$ positlin,
and frequency and amplitude of transversi oscillation of the beam
Is measured in three ststeal (1) during the first r*volutlonj
(2) with a tirgule,tiftS beam and (3) with acceleration.
for measurements 6n the first roValution long afterglow
scintillation screens are used which are either observed visually
or by means of a television camera# The *croons are placed to
the soations between magnet blockal 1~ In the InItI&L part and
,rIn -tAo final port at the dmober.' - Win aho4oft .0at'thoorbit do** not
7~- ---,7,

3/120/62/000/004/047/0'k?
A4justm*nt of the acceleration 9039/t420
deviate by more than loS tot from the axis during the first
revolution. Circulating boom* without acceleration are obtained
which continu*,for 20 to 30 revs. The circulating current to
determined by means of a flight tube and the transverse
oscillation frequency with an electrostatic probe with doubl
vertical and harlsontal plates#, he
3clatillation screens In I*
form or & grld with 85% transmission are used to show the boom
position and diameter for 5 to 10 revs. The beam diameter is
shown to be about 4 eta under normal OoDdItIons. zavest1gations
are carried out on the optimum form of the frequensy- Slao
roUtl6st fat holding the boom in orbit. The width or the trapping
r;gt:: 1:,t 3 Kc/s for an Initial frequenoy of ?50 Ke/s vhith
a rv w r with theoretical estismtes# Preliminary adjustment
Permitted the ottainment or 6.2 4ov protons and after adjusts*%%
7.2 Gov protons were obtained an Oatober 3~, 1961 The usual
Intensity on a normal eyelo Its* In the range J~ %; 5 X 109.
There are 7 figures and & tablea
ASSOCIATIONt Institut toorstithookoy L eksperimontallnoy tialki.
UA& (Institute of Theoretical and txperlmontal
LUO physiss out)
rJ11;J01 April 11, 1962

VLADIMIRSKIYP V.V.; GOWDIN, L.L.; PLIGIN, TU.S.; VEXI", P.A.;
TALTUR, A.M.; TARAMVj Te.K.1 KOSHKAW, D.G.; LAPIMIT,
Yu.Ta.j RMaM, L.Z.1 MEEDEV, P.I.;
KOZIMIN, A.A.; RATALIN, V.A.1 ONMVSKIY, K.K.; UVAROV, V.A.;
VODOPITANOV, F.A.
Adjuntment of acceleration In the 7 bay. protc- syrichrotron.
Prib. I takh, eksp* 7 no, 4s248-255 jl,-Ag '(2. (PIRA 16%4)
1. Institut toorsticheakoy i eksperimentallnoy flaiki Gosu-
darstvennogo kcattota po Ispollsovaniyu atomnoy energit 5.11M.

KLRXDVo le.P.1 EMPMO I-L-
Carboniferous stmUxmpb7 of the northwestern SIberlAm Platfom
M&tJM= no# 32s73-79 160, (MM U13)
(Siberian Plalforw-WO109yo StratigmPhle)

MWFOVO 1A,
wmmft---~
In the Institute of Vis ClaogrsplW of Siberia and the Far Ust,
DAls lust* geog, Sib, i Dal', Yost, no,lt68-72 062, .
(KMA 17s 8)

UMPOV I#L.; VORODIM.. XV.
OGeograpUcal, problem of TaJmU&o* Uviewed by I.L.10"pcwt VIT,
Voroitev, Iwo Voss# geolto Obwm 94 no,N263-263 162.
(Ukutia-46ograpbr)

Devvlopment and distribution of gold mirting l9k the hr I&A
before the %wolutici. and during the first years of the Soviet
regimes Sib* pogo aboro noeW06-214 163, (KaU 161 n)

ximpov 1. LO
An Interosting practice of the Chukchl Geographical Mussuso
Inv* Voes, pogsob-va 96 no. WA&U9 Mr-Ap 164,, (MIRA 1715)

otm, red,
[Geological Comdtteej, IF&'-19291 hIstOrY Of thO P01097
or Russia) Geolegichaskli kot.itet 1882-1929 Istorlia
genlogil, v hossit. Moskvnp Paukas 1964. 173 p.

in p. 11,7 *7779
~*cnV-!--., Lint ~~r
Au--~-:7,to 1^191,

lables of varcentile increane in gore pOSSibIlItter or Aotarr-InLnZ
pircentilo incrensis. p. 4541 LL412 Vol. 7Z, o'io. ~/10, Sept./A;ct.
19541 zek"bi Yugoslavin)
SO: Lonthly List of -Zust 4uror6an Accessllono, -0$
Unal,

Frepitney of the transition period. ;3. 3.
ZAgreb, Vol, 79j ro. 112, Jan./Feb. 11j55.
30; X,-~nthly List of Mat Zkzropean Accevu!onv, (EZAL), LCI Vol. 4, no. 10, Oct.
Uncle

KLIPAC,o D.
tWAC,, Da Affect of odatlotoo on development of fir trees. p., 2310

KLEPACp D.
Methods of determination or forewt growthl preliain=7 research an
gr&Ab of the British o4k, po 60). SUMARSH LIST. (Drustvo sumarskib
insonjera i tahnicam ?MR AWslavijs) Zagreb, Vol, 79p no, UA2 MY/Dec.
19556
SO. FA8t European Accessions List Vol. 50 no. 9 September# 1956

YUGOSLAVIA / Forestry, Dendrology. K-2
Abs Jour: Ref Zhur-Biol., No 6, 1958, 24879.
Author :_Klep4c_, Dusan.
Inst i 11oz glveff-."----~
Title s The Study of the Growth of Spruce by Diameter at
the Het ht of the Cluster in the Most Widespread
(forestl Combinations of the Gorski Kotar Province.
Orig Pub: Glasnik sumake pokuse, 1956, 12, 225-256.
Abstracti Investigation was conducted in plantings of Western
Croatia, not far from the Adriatic Seacoast, The
growth of the spruce in the calcium (CS) and clay-
humus soils (CHS) was compared, In both cases*
the types of plantings are described in detail.
Card 1/3
YUGOSLAVIA / Forestry, Dendrology. K-2
Abe Jourt Ref Zhur-Biol., No 6, 19580 24879.
Abstracti In the plantings of CS, the spruce, beechp maplep
elm prevail; plantations on CHS are mainly compoced
of spruce, For determination of the average an-
nual Growth by diameter at the height of the clus-
ter, the following equations were derivedi for
spruce planjings on CS mr a 4.66574-0.41163 1/d -
0.00031 1/&~; for spruce plantings on CHS m m
~31-931420 - o.u60540 d + 0.004160 dl: - 0 ' 7U36
0MFi. 0.43236 + 0.12581 d - 0.0087 d2, where mr
signi e9 the growth in mm, d - the diameter of
the trunk at the height of the cluster In cm.
Mathematical processing of the data showed that in
CS the average annual growth constantly increases;
in CHS it attains a maximum by the diameter of the
spruce at 65-7u em.; In the first case, the speed
of growth is expressed hyperbolically; in the
Card 2/3
29

IhnotAonal relation beUmn annul S rowth in Yo2mme and diameters of trunks of f1r
trees in t Id mod forests p. I
SUMM19LIM?s Zagmbp Val sot Noi. 1/29 Jan./Feb. p 1956
801 Zast Nuvp*an Aocessions Usto Vol go No* lot Octes 1,956

XLEPAC, D,
Using frwpency curves of tree numbers in the d": cription of staMs. P. 357.
(Saoijallaticko Zenjoddstwos Vol, boo no, 11112 Noy,/14co 1956,)
SOt Pbnthly jAst of last lumpean Accessions (UAL) LC# Val. 6p no, Ip W7 1957, Uncle

KWACq D.
Research an the thicimas of the bark of the most important bals in Croatia, p,91s
(SUMMKI um. Vol. Olt No*' 3A# Y"o/Apre 1957s Beograd, Yugoslavia)
50t Monthly Liat of last Ibropean Accossions (MAL) LC# Vol* 6# No, 10p Octobw 1957e Unelt

KUMC D.
rawtimal relation b"vow thicira" of the bark and di=eter of the trw* In car
major docidnow ti"as P* 2%#
Periodical# SUNUM LM.
Vale 820 no. 7/6j, July/Aug, 19%
AWCULTM
SO: Mont-My LIst of East Muvpom Amessieft (MM) LC
Vale as, no,
ApaU 2959,, Urmle
7777777

KLEPAC D.
m ~~
Determ1ning losses In the Increment of stands caused by gypey notba
(Umantria AUM) -
SUMMKI LIST (Sumarsko drustow Urvatsks) Zagrebp Tupslawls,
Vol. 83o no. Ot Aug./Sept- 1959
Montbly list of Seat Impsan Accesslon (MAI) LC Vol. 9. no. 2, 1960
Uncle

-SUCPAC Do
PIAVE p M.
Determining the volume of Increment according to the control method at the
"riment lots In the L1povIjwd forest r*gion. p, 257.
SU)MKI L33T (Suparsko drustov Wwatske) Zapebg Yugoslavia
Vol. 830 no. 8/9# Aug./L.. 19,9
Ponthly list of last Impean Aca"Nion (SM) 14 Vol. 9,, no. 2p 1960
Unol

nEPAC;D.
for"t plaming wW saWment, Rd so Toug 8 no#3/4o"
Jo--Ig'63.
lo ftsariski takultatp MW#b.
g
-.4
i~w i"I bm
el-11

FUXARAK, WTO J,j WSTROVIZO S.1 KLEPAr,,,,._D.; LMICEX, Z.; ZHIJANAC, D.j
SEVNIK# Fs; ZAGAR9 B.1 KIXLAVZIC# J,j KNEZt A.; PIPMO R.; FUNKLt L.1
MTLICICj A.1 ZUMMO L.1 "V0# Ft.
Revo1w of periodicals; silviculture. b-al sc Youg 9 ro.4/5i244-
145 Ag-O 164.

7-~ -- I M .1 1 -1 - -
. - IM -~ 1~ - :
1~ Is " -I .
.- - i

SUVO;=Ap Lidiya IllW obnaIKAWIRM Leo nid Nikolayevich; VAW-ABIMMOT.,
rod.; KUPACH, Jj red.1 SHUNSIAXA, M.0 tokhne redo
rinowledge wA know-bov; collection of artioles on the economics of
socialist agriculture] bat' 1, umet'S sbornik statei po ekonomike
sotsialistiahelde,,jo sellskoga, khosisistva, MosWa. lad-vo TaK MUM
"Holodaia gyardum 4 1961, W P. (MIU UtIM
(Agriculturo-Sconmic aspoets)

OURBYICHt A.M.; SUIRZfMWj Z.I.; KWAM E.J.; RUSIMOVs, ILY, karA..
takhn. asuk, retsensenti GALAHOVAp M.S.# Insh., red.;
UVAROVA# A.F.# tokbn. red.
(Fuel system an diesel locomotives and motorships with
D100 and D50 safineal Topllvnaia apparaturs toplowosnykh I
mOovykh dvigatilet Up& DIOO i D50. Moskyaq Mashgis, 1963.
2D3 ps (MIRA 1615)
(Diesel loacwtives-Fuel system)
(Motorships-Fuel system)

All electrical technicians should belong to factory groupq of the scientific Tech-
nical Society for Electrical Rr4imeriM,
P. 1. (ELEXTROTECIMIX) (Praha, Czachoslavakia) Vol. 13. no. 1. Jan. 1958
30. Monthly Index of Zast &wopean Accession (EW) W Vol, 7, No. 5, May 1958

SAUXON, T, d-r,IEWAO, Z. d-r,
Second cass, of Me2korsoon-Rosenthal syndrome. god. arb.. Sarajevo
12 n0-3173-" may-Ifthe 157. 0
lo Dispanser a& kome Westi u Imajaluoi. Sof: d-r T. Salmmon I
0djelonjo v& tho. grlo I moo Opets bolnice u Banjalwl. $sh dwr
IMM, IMIA4 paalyols
Wo2kersson-losonUal
("YMO die*
Ms

KUZ'HnOVp I.Lj red,; KLEPACH, N,Ya.o red.j SLASTENENKO, V.A.,
red*1 TREFILOV, VXj-k6d*-j VORONINAI N.# md.
(socialist production conectivej Sotsiallsticheskii prols-
vodstvenmyl konektiv. Moskva, 1964. 230 p.
(MIRA 180)
I*.-Moacove Akademiya obsbehestyamVkh nauk.

EaACH, PO T*t Water Tech Sol (diss) -- "TM$ttfptlon of the process of
Injecting liquid fuel Into a locomotive engine In amll doseo. Mar1kay, 19580
17 pp (Min Transportation tMq lbarlkov Inat of Railroad Tzensport TWInsers
In S, M. Kirov), 150 coplao (KLO Ito 1"9p 126)

GURVICH, A.N,, kandetakhn.001*1 EMACII, P-T-v Inab.
rual system perforissail of a diesel wiss OWAUAC Oft 4011
amounts of hel, Stake I tepl, %tap 2 00*9139-42 a 158.
(Diesel saghos-4asting) MRA 11120)

SOV/115758-5-15/36
AUTHOR: Klepacho P
TITLE; U30 or Wire Pick-Ups ror Measurements in the Fuel
Systems of Compres3orless Engines (Primeneniye provo-
lochnykh datchikov pri limereniyakh v toplivnykh
sistemakh beskompressornykh dvigateley)
PERIODICAL: lzmeritelinayn tokhnika, 1058, Nr 5v PP 32-34 (USSR)
ABSTRACT: The author deals with the use of wire pick-ups for
measuring rapidly changing pressures and the rise of
the jet needle in the fuel systems of internal com-
bustion engines. The paper contains diagrams and
photographs of equipment used to study the fuel system
of a D-50 engineo as well as some results of the measur-
Ing operations. For measuring pressurcs in the feed.
pipe, the wire pick-ups were glued to the bottom of a
canister installed In the body because of the bottom's
high frequency or natural or free oscillations. Of
especial interest Is the question of determining the
Card 1/4 free.oscillations of a resllient~element (here# the

V
SOV/115-5&5-15/36
Use of Wire Pick-Ups for Measurements in the Fuel Systems of
Compressorless Engines
canister bottom). Two forces are operative when there
is free oscillation of a free plate. 1) The plate's
elasticit -(-Kx); 2) Force of inertia of the platets
mass (-m Le 'A,
dt.r ). The formula for the plaite's movement
dt
is: M ALL 'T kx a 0. The canister bottom to which
dtr- I
one or two pi,ck-ups are glued, receives the pressure,
arising in the feed-pipe and is deformed. The wire
pick-up is correspondingly deformed and thus changes
its resistance. The problem of temperate compensation
of the resistance measuring bridge when using this
device was successfully solved. Good results were also
achieved$ by using a device based on the Ts HIDIs 1955p
design. The device has an additional horizontal beam,
via which the force of the-rod - connected with the jet
needle - is -transfermvd to the working beam. 'hire-pick-
ups are glued to the latter. The measured pressure
Card 2/4 process in the pipe of a fuel system consists of a

Use of Wire Pick-Ups for Measurements In the Fuel Systems of
Compressorless Engines
constant and a variable component. To measure these
processes, the amplitude modulation method Is used, by
which processes with a frequency 10%-15% that of the
ap source - with which the measuring bridge Is fed
can be measured. Ac amplifiers with a carrier fre-
quency of 5 and 50 ke were used with an UPO-2 oscillo-
graph and type I loop. Pressure oscillograms were
prepared with a fuel pump shaft revs Z70 rpm, a fuel
feed of 1.266 g per cycle and a clearance in the dis-
charge collar of the valve of 0.2 mm. Pressure was
recorded with the same device, using an amplifier with
the carrier frequency of 50 ke shaft revs 370 rpm and
fuel feed 0.101 g per cycle. ibe wire pick-up can be
regarded as universal since It can measure the pressure
in the engine's cylinder, the fuel system and the
collectorsp rise of the jot needle, shifts, angular
velocities or rotating parts etc. The measuring
method worked out by the author was checked by invest-
Card 3/4 igating the fuel systems of D50 and 71- en&ines and is

SOV/115-5&5-15/36
Us& of Wire Pick-Ups for Measurements in the Fuel Systems of
Compressoriess Engines
used in investigating the fuel equipment of the 2D-100
-engine under Industrial conditions. For testingg
amplifiers with a carrier frequency of L5-50 kilocyles
are utilized. There are 3 diagrams, 5 graphs and 6
Soviet references.
Card 4/4

CWMW# AP. , 4oktor taktmoneak, prof,: =N=o -doteento land, tothnonauk;
KLVI tokhri.nauk; Sm
00=~~nd
Invest1gating the perf ormnoo of the fuel system of 2DIOO diesel
loconotive engine at low too". Ibrudy IMIT no.35A-12 160.
(Mosel ousinse-nal systems) (MIRA 13 t 10)

CIUR S, A.P., doktor tokhnnauk, Irot-1 MBWZD, S-L, kand-tsidwAsuko
dotment; ILZMACS. P.?.. kwA.tekhn.z&uk: StMZ 2.1.0 insh.
Investigating the deforsotions of the fol lujoator b"y of the 2DIOD
euxine, 2rudr ]MIT no-35150-54 160. (MINA 13zlO)
(Diesel sagints-ftel systems)