SCIENTIFIC ABSTRACT MUROMTSEV, G.S. - MUROMTSEV, G.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001135630003-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 13, 2001
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

1.-:URCI,ISKIY, Sa-,rva Nikol-rrevIl-ti, Leonid Fetrovicl.;
[ Unaergroizirl gas p I pfili inci f~ -)j, .'e -/ ' 71, j la;~rrT,&! a a. rmi--
tura podzerrrr,,kh M(~,skva, Stroiizdat., ii65.
70 p. (MIRA 1941 )

MUR-ONSKIT. Sayva-Bikolayevich; SHCHNGOLICV, K.M., red.; KHRISTZNKO. V.P..
red.izd-va; TOI16V, S.T., tokha.red.
Lfighting corrosion in hot water boilers for public baths] Borlba
a korroziel vodogreinykh kotlov ban'. Moskva. Izd-vo K-va kommun.
Ichoz.RSFSR. 1959. 86 p. (KIRA 13:9)
(Water heaters)

MMMSKI7, Nikolay Fedoravich; MUROMSKIY, Sawa Nikolayevich: VILENSKIr,
T.V.,, red.; IARIONOV, Gfe., tekbn. red.
[Safety engineering in small industrial steam boiler plants] Tekh-
n1ka bezopasnosti v ustanovkakh promyshlemxYkh parovykh kotlov me-
loi moshcbnosti. Moskva, Gas. energ. izd-vo, 1961. 230 p.
(MIRA 14:10)
(Boilers-Safety measures)

MUROMSKIY. S.N.; SOSNIN, Yu.P.; TYCHKOV, I.N.; KHMELINITSKIY, S.A.
Gas contact vater heaters and prospects for their use. Sbor.
nauch. rab. AKKH no.9:3-17 161. (KM 16:1)
(Water heaters)

MUROMSKIYJ, S., kand.tekhn.nauk
-------
The Soviet "Luch" electric stove. Zhil,-kom. khoz. 13 no,4z
28-29 Ap '63~ (MIRA 1685)
(Stoves, Electric)

ti-e
na s rM 'j zd a
18 C.)

KUR09SKIY. Yu.A.
Intra-arterial injection of blood under pressure in clinical practice.
fest.khir. 77 no.4:106-108 Ap '56. (xm 9:8)
1. Iz 1-y khtrurgicheskoy kliniki (zav.-prof. B.I.Linberg) Moskov-
skogo oblastnogo nauchao-iseledovatellskogo klinicheakogo inatituta.
Mosima. ul. Chkalova, d.34, kv. 17.
(IMSIONS, PMMNTARA
intra-arterial pressure inject. of blood)
(BLOOD TRANSMSION
intm-arterial pressure inject.)

MURONSKIY. Yu.A.
. ............
Causes for formation of bronchial fiotull following radical syirger7
In chronic Suppurative procenaes in the lungs (with summary in
linglish]. Khtrurgiia 33 no.6:54-62 Je '57. (MIRA 10:12)
1. 1z 1-y khirurgicheskoy kliniki (zav. - dotsent N.I.Makhov.
konsul'tant - zasluzhennyy deyatel' nauki prof. B.N.Linberg)
Moskovskogo oblastnogo nquchno-iseledovatellskogo klinicheskogo
insituta imeni M.F.Vladimirskogo (dir. P-M-Leonenko)
(BRONCHI. fistula
causes of from. in lung resection for suppurative processes)
(PLEUMONECTOKY. compl.
form. of bronchial fistulae)

MROMSKly, Yu.k.
oracoplasty of borachial fistulae folovinge pneumonectomV (with
summary in Finglish]. Khirurgiia 33 no.12:?4-80 D '57. (KLRA 11:2)
1. Iz 1-y khirurgicheakoy kliniki (zav. - dotsent N.I.Naftov,
konsulltent - zasluzhennyy deyatell nauki prof. B.N.Linberg)
Moskovakogo oblestnogo usuchne-is8ledovatellskogo klinicheskogo
instituts iment M.F.Bladimirskogo (dir. P.M.Leonanko)
(FUUMONCTORY, compl.
bronchial fistulae. thoracoplasty)
(IMOICHI. f istulas
after pneumonectosq, thoracoplasty)
(COIJAPSI THERAPY, in various dis.
throcoplasty in bronchial fistulae caused by pneumongcto=V)

KUROKSKIY, YuA., TSUMAY, V.G.
The acute abdomen syndrome in cases of traumatic retropearitoneal
hemorrhage (with summary in Inglish]. lhirurglia 34 no*7t49-57
Jl 158 (MIRA U:9)
le Is 1 khtrurgicheskago kliniki (sav. - dots, 1.1, Nalthov)
Koskovskogo oblastnogo nauchno-ionledovatellakogo klinicheskogo
institute Imeni K.F. Vladimirskogo (dir. P.K. Leonenko).
(ABDONSI, ACUTE. stilogy & pathogenesis
traum. retroperitoneal hemorrh. (Rus))
(MMOPKRITOM" SPACZ. hemorrhage
caused by trauma & causing acute abdom. (Rua))

MUROKSKIT. Tu.A.
Bronchial fistulae following pneumonectomy and their clinical
course [with summar7 in Inglish]. TestAtir. 82 no-1:69-76 Ja 159.
(KIRA 12:2)
1. Is 1-y khirurgicheakoy klinikL(zav. - dots. N.1. Kakhov, konsull-
tant - prof. B.3. Linberg) Moakovskogo oblastnogo nauchno-isoledovatell-
skogo klinicheskogo inatituta imeni N.Y. VlAdimirskogo.
Adres avtora: Koekva, 3-7a Neshchanskaya u1., d.61/2, Koakovskly ob-
lastuoy nauchno-issladovatellskiy klinicheakogo inatituta im. M.P.
Vladimirskogo. 1-ya khtrurgicheakeyn klinika.
(PE M 0NXCT W , compl.
bronchial fistula, progn. (Rua))
(BRONCHI, fistula
after pneumonectoaW, progn. (Rua))

~MOIMM, Yu. A., Cand Died Sci (diss) -- "Bronchial fistulas after lobecto-
mies and pneumonectomies". Moscov, 1960. 24 pp (Min Health RSFSR, Moscow
Med Stomatological Inst), 250 copies (KL, No 15, 196o, 14o)

MROMSKIY, ru.A. (Moakva,3-ya Keshchanskaya ul.,d.61/2, Moniki)
DiagnOBis and treatment of bronchoesophageal fistulae following
resection of the lungs. Grud. kbir. 2 n0-5:99-105 S-0 160.
(MM 16-5)
L Is 1-y khirurgicheskoy kliniki (zav. - dotsent N.I.Makhovo
Maskovskogo oblastnogo nauchno.~fesledovatsllskogo klinicheakogo
instituta imeni M.F.Vladimirskogo (dir.-kand.med.nauk P.M.Lemenko).
(FISTULA, BRONCHIAL) (ESOPHAGUS-DISEASKS) (LUNGs--suRrmy)

MUROMSKIY, Yuriy-Alekse evich;KAZIN, V.P., red.; PARAMINA, N.L.,
_t~Zin_. red.
[Bronchial fistulas following pulmonary resection] Bron-
khiallnye svishchi pasle rezektsii legkikh. Moskva, Med-
giz, 1963. 218 p. (mim 16:7)
(FISTULA, BRONCHIAL) (LUNGS--SURGERY)

MURGM1Y., lu.A., kand. mod. nauk; KOLEROVAP N.V.
GAwe of broncho-esophageal fistula following bilobectmy and
tharacoplasty. Vestn. reitt. i rad. 38 no-3:74-75 My-J* 163.
(MIRA 17:7)
1. Iz 1-y khirurgicheskay kliniki (zav. - prof. N.I. Makhov)
i rentganovskago otdelaniya (zav. - dotsent V.I. Petrov)
Moskovskogo oblastnogo nauchno-issladovatellskago klinicheakogo
institula imni M.F. Vladimirskogo (direktor - kand. mod. nauk
P.M. Lec-nenko).

S/656/6i/uOO/OOO/O06/O07
D244/1)304
AUTHORS-. Muromskly Y Simanov,, Yu~P-, and Nemkova. O-G,
TITLE~- Investigating the Interaction of uranium and uranyl
phosphates with calcium oxide at high temperatures
SOURCE. Spitsyn, V.I., ed~ Issledovaniya v oblasti khImil
ura-via; sborn-1k statey (Moscow) 1961., 281 - 291
TEXT: To investigate the possibility of the interaction of U 3 (PO 4)4
and (UO 2)3 (PO' 4)2 with UaO at high temperatures the authors studied
the following processes; U 3 (PO 4)4 4 6CaO --~WO 2 + C'Ca3 (PO 4)2 Eq.
(1) in inert atmosphers; (UO 2)3 (PO 4)2 -+ 3CaO --- i-U308 ~- Ca-"(P04.)2 +
+ Y2 0 2(Eq. 2) and (U02)3(PO4)2 + 60a0 - 3CaUO4 + Ca 3(P6 4)2 (Eq~
)) in oxidizing atmospheres. The main method of analysis employed
in this work was X-ra tube of the E;CB (BSV) type with a copper
anode (without filters- The reaction between U 3 (PO 4)4 and CaO was
carried out by mixing the COMDOUntS in the ratio of 1 : 6 respecti-
Card 1/3

S/165 61/OuO/060/OU6/007
Investigating the interaction of D244%304
vely,~ The experiments were conducted in.nitroGer. The temperature
being increased in steps of 1000C oetween 400'-' and 10000C with hea-
ting for 4 hours. The X-ray analysis demonstrated that the interac-,
tion ot U3 (PO 4)4 with CaO begins between 400 and 50000c The reac-
tion products are U02 and Ca3(P04)2. The reaction proceeds as in 31.
1. To determine the influr-.,nce of temperature on the percentage con-
version of uranium phosphate into U02 the author conducted chemical
analysis of the reaction products obtained at 15000 and 100000- CaO
and Ca3 (P04)2 were dissolved in H01, U 3(PO 4). dissolved in H)P04
and the remaining UO in HNO, and then precipitated with NH and
2 3
weighed as U 30.0 The resulta of the chemical analysis also confirm
the correctness of Eq. 1, Reaction (2) was carried out by mixing 1
part of (U02)3 (PO 4)2 and 3 parts of CaO and heating in the atmosphe-
re of purified air between 3000 and 10000C in ste S of 1000~ In
each case the heating was cont'inued for 4 hours. Ke chemical and
X-ray analyses indicate that the products of the reaction wer,. ini-
Card 2/3

3/6)6/61/00u/000/006/007
Investigating the interaction of D244/D304
Lially Ca 5 (PO 4)2 and U0 The L-itter -:ias transLorriied above COO 0 C in-
to U_(_) The _-eacti.,~;n re,_-.ins oe-tween and 450"C_ To confirm the
.iorT.-,ation of' UOA between and tOOOC, -1 part of (UO ),PO and 75
1' 2 ) 4
parts of CaO were heatu., 6 hours bev-,,een 400~1 and 10b0OC in
steps of 11000. Analysis -e products indicated that the reaction
proceeds according to Eq vilth the formation Of CaU04. Interac-
tion of uranium oxides and c~lclum phosphates was also investigated
in order to demonstrate the irreversibility of the reactions stu-
died. Results of X-ray and chemical analysis indicated that tne re-
actions (1) and (2) are irreversible between 4000 and 10000C. The
authors conclude that at high .emperatures it ie possible to isola--
te uranium oxides or to obtain CaU04 fTOm (U02 _~ 4N2 3 4 4
),jo ) and U (PO )
in oxidizing atmospheres, The authors believe that these results
could be utilized in technological refining of uranium phoophate mi-
nerals. There are 6 figures, 8 tabl,33 and 6 references: 2 Soviet-
bloc and 4 non-Soviet-bloc. ehe reference to the English-language
publication reads as follows, J. Sch:,ayer and C. Boes, J. ~.mer~
Chem. Soc,, 76, 354, 1954c
Card 5/3

IMONTSIT. A.I.; SHABODAUX, I-?-
- .
weather-resistant coatlop based an coPOlPsn of wUWI chlorlde
with vlzWl acetate. Ukokram-mat-l lkh prlu no.5s28-21 160.
(NINA 13: 11)
(Protective oostinp ) (Ithylene)

MUROMTSEV, A.K.; ULANOVSKIY, I.B.; SHABODALOV, I.P.; KOROVIN, Yu.M.
Testing coatings for metal protection in fluctuating waterline' ones*
Trudy Izwt.fiz.L-h4-. 8:387-395 160. (MM :4)
(Protective coatirgc~-Testing)
(HuIls (Naval arc.'aitecture)-Corrosion)

BOGATYREV, P.M.; GADZHIYEVA, R.G.; MURZANEVA, Z.M.; MURCHTSEV A K -
KUTSEVAWVA, Ye.P.
Thirteenth technical exhibition organized by the Oil and Colour
Chemints' Association in England. TAkokras. mat. i ikh.
no.4:61-69 161. (MIRA 16:7"0
(Great Britain-Paint mate ria bs-Exhibi tions)

L 04965-67 DRUm LE~P I __ IJP(c) JDA - RIT
I~L
ACZ7'W ~,AXP&(A722
'_~~UkCedks UH/6j~~/a/000/001/0044/0046
1312
AUTHOlts Israllyantap To. D.; Muromtsev, A. K.
ORG i none
Epoxy:pitch
anticorrosion paints and primers for long-tam protection of sub-
TITLEs
merged pi-R-sof ships
S0U=1 lakokrasod~wM materialy i ikh primeneniye, no. 1,, 1966g 44-46
TOPIC TAGS$ paint# protective coatingg pitch materialp epoxy plastic
ABSTRAftl The article reports the results of tests of improved epoxy~pitch paints
(EK-1 EK-2# EK-5) with a high content of dry residue and :~;oxy-pitch zinc protective
primers. Particular attention was devoted to the behavior of the coatings under ca-
thodic protection conditions, when blisters appear on many types of coatings and
their adhesion to the metal in thus impaired. A32 the samples were tested in a 3%
N&Cl solution for adhesion to St.3 steel and f corrosion resistance. The best re-
allts were obtained with paint mad* from ED-59sin containing 8% of,curinK agent
(polyethylenepolyamine). 7he best sample of pa nt from E-40 resin had a 5% content u
curing agent. Compared to paints from U-59 paints from 3-40 dried fasterp retained
their effect for a longer period of timaj, had a greater hardnassq but their adhesion
to steel and elasticity were lower and their deposition produced a thinner coat
Two epwW-pitch protective primraq n-2 (from ZD.5) and PT-3 (from 5-40)9 were
Ca,d 1/2 ms 667.637.233-3".12.011.71

L 04965-67
ACC Nits
prepared. PT-29 containing 90f zinc dust (of the weight of the dry fills) had better
-proportion. The combination of protective pr-Uwrs and paints made with an epoxy-
pitch base was found to produce coatings with high anticorrosive characteristics. It
Is concluded that the adoption of spogr-pitch paints will insure IoWtem protection
of the Immersed pax-t of ships from corrosionp, icularly under cautafto Protection
, part
oonditions. Crig. art. hut 2 tables. 14
SUB COMI It/ 3UHK DATKs now/ ORIG Ws 004/ OM RM 007
141

MM-ITMW, A. 14.
"Experiment for Division of the OcPan SpRcs Into Zonps." Sub 8 Mar ')I,
Inst of Ocnmrnloa, Ac:sd Scl USSR.
Discertationr precented for srlorco and aneincerine, degrees In 'Aos-!0w
durlng 1951.
SO: Sum. No. 4430, q 14v 55

KUROKTSU, A.K.
Deepest seem areas. Geog. v shkole no.3:62 IV-Js 153, (IMU 6:6)
(fteific Ocean-Desp-sea sounding)
1 1 11,21 11111 i dm-L~Iujj

U56h/Geopaysics - Oceans Nar/Apr 53
It's-
"Classification 6f the Subdivisions of World Ocean WER CTIM
A. M. Muromstev
V-s
Iz %m Geog9W Ob, Vol 85, No 2, pp 154-161
Lists classification of subdivisions as follows: 1) world ocean; 2) oceans; 3) regional
oceans; 4) seas, inland (closed and semiclosed), adjacent 10 and interisland; 5) regional
seas; 6) gulfs; 7) bays; 8) straits. States this is the first attempt made to classify
and regionalize oceans by hydrological syrbols.

- . X - C- f i -, /r 11 /f-
^1 1//F i0 /~~F /,/' 1`1 ' ' " ' - ' k' A ' 6 1 -,`- ;i v / c- tt-
RAMOT, Vasiliy Stratonikovich; :UI~WMZV. Aleksey Kikhaylovich; MAL-
ZIN, A.G., redaktor; KAN, . '.,- 'i'Wo- # A.K., tekhni-
cheskly redaktor.
[Oceanography] Okeanagrafiia. Moskva. lzd-vo OKorskoi traumport.0
1954. 165 p. (KLU 7:12)
(oceanography)

KURCxT,qz.v,.Al~ksey gikhaylovich; PRIOBRAZHENSKIY. TU.V., redsk-tor; FIAUK.
N.Ya., tokhaicheakiy redaktor
(The ocean] Kirovoi okean. leningrad. Gidrometeorologichaskoe izd-vo,
1956. 85 p. '%MLRA 9:10)
(ocean)

IN"I U "'B ~ MTS E V ~ H I M,
USSR/Physics of the Hydrosphere - General Problems, N-1
Abst journal: Referat Zhur - Flzika, No 12, 1956, 36225
Author: Vuromtsev, A. V.
Institution: None
Title: Application of Tntersect!ng Hydrological Surfaces In Deep-Water
Investigations
Original
Periodical: Meteorol. I gidrologlya, 1956, No 2, 44-45
Abstracts The author proposes to employ the method of intersecting hydro-
logical surfaces In the processing of hydrological data (tempera-
ture, salinity, or density) in deep-water investigations. This
method shows simultaneously the hortiontal and vertical distribu-
tion of the hydrological elements and makes It possible to make a
fuller 3-dimensional study of theIr distribution In space. It
permits a more accurate study of the character of water exchange
and heat exchange betw-en various layers of the ocean and to solve
other problems related to the study of streams. The author states
Card 1/2

USSR/oWsice of the ffrLro"here - General Prob low, N-1
Abst Journal$ Referat Zhur - FiziJm, No 12, 1956, 36225
Abstract: that the Method of intersecting hydrological surfaces in conjunc-
tion with the T-S curves may facilitate to a considerable extent
the study of the schedules of oceans and seas.
Card 2/2

MUROKTS11V A,H,
New map showing the salinity contest In the surface of the
Northern Pacific Ocean. Keteor.i gidrol.no.6:36-38 Je '56.
(Pacific Ocean--Salinity) (MMA 9:9)

Kmolesly. A.M. (Moskva)
.- -
The greatest depths of the Southern Hemisphere. Pr1roda 45 no.5:
90-91 My 156. (MLRA 9:8)
1. Gosudaretyennyy okeanograficheskiy Institut.
(ocean)

HUROMTSIV. A.M.
-0 RININNINNOW
Now maps showing the salinity content and the
surface of the Pacific Ocean. Hateor.i gidrol.
157.
density in the
no.4:15-19 Ap --
(MLRA 10:5)
(Pacific Ocean--Salinity)

KURCKTSAV, A.K.
NM"ft%
sanographic knowls4ge about the Pacific Oce&16 Pstsor. i Adrol.
no,5:21-21 Ky 157.
(Kza& lorey
(Pacific Ocean--Oceanography)

rs-,E tl 4, 14 -,
kUTHORS; Yushchak, A. A., and Mli-romts ev,_ A. - M.- 5o 11-819
TITLE: Progress of Soviet Oceanography (Uspekhi sovetskoy okeanografil).
PERIODICAL: Meteorologiya i Gidrologiya, 1957, Nr 11, pp. 6o-67 (USSR).
ABSTRACT: In 1921 the floating sea institute was established. The function of
a methodical center for wide research works in the field of oceano-
graphy was taken over by the State Oceanographic Institute, which
was founded in 1943.
At present there are about 2o special research ships, more than 30
local sea-research institutes of different offices and about 5oo sea-
hydrometeorological stations. In 1947 regular hydrometeorological
and biological research in the Atlantic part of the antarctic region
as well as in the Northern part of the Atlantic ocean, and on the
Norwegian and Greenland parts of the ocean were started. Since 1951
oceanographic complex observations are carried out by the liVityazill
research ship of the Institute for Oceanology in the North-Western
part of the Pacific ocean.
Since 1955 ocoanographic complex resparch is -),it In the ant-
axctic region by meanB of the diesel-electric ~;hip "0b" and -iinre-
auti.ma 1-957 in the Northern ittlantic on the shLps "Loma nos ov 11,
Card 1/h "Sevastopol.'$' and !'Ekvator". At present the hydrostatic floating

Progress of Soviet oceanography.
50-:1 ~1/9
wave-graph of Ya. 0. Vilenskiy and B. Kh. Glukhe-,rakiyls belng im-
troduced to research practice; it showed good results in operation
at ship condition. For temperatore observations water-depth tilting-
thermometers are used.
In the first stage of development oceanographic observations on la-
kes were mainly directed to the collection and accw-Ulation of data
on temperature, saltiness, density and chemical elements of s-awater.
Furthermore also hydrologic special pTnt-ures were taken togt__,er
with observations not only of essential hydrologic and hydrochemical
elements but mainly also obqervations of streams and vortires. Great
use has been made of special observations of i.;efieldsp these obser-
vations were carried out by airplanes and shi4o. At present a far
reaching mechanized treatment of the data of Eurface-hydrometeoroID-
gic observations of ships as well as of data o.-i I'lood. differences
of the position is being carried out. In the next time a?L observa-
tions of the a ea.,hydromete oro logic system will bt~ chpnged to mecha-
nized methods.
Of great importance for the study of Lakes and oceans are the works
which develop the theoretic basis of various branches of science of
oceanography. The enumeration of these works from 1917 -1955 follows-
The informations and ideas published by the State Institute for
Card 2A oceanography are to be mentiored in (,onnection with the methods of

Progress of Soviet Oceanography.
5o-~/q
research, as well as the monography of Snezhinskiyi, 4., "Practi-
cal Oceanography,' 1951 and the collections of the essays on methods
published by the Institute for oceanology which generalize research
data of the 'Tityas'll ship. The works menti,-ned above give an idea
on the general trend of develapment in oceanography.
The Uivestigation of wind vortices developed simultaneously ei-piri-
cally and theoretically. The enumeration of these research work5
folloNs.
The investigation of the strears represents a special problem which
is currently being investigated. The probleqLq nf convective flows
on the monsoon fields were investigated by Shuleykin. Zhe problems
of the influence of wind and ground relief un streams are investi-
gated by V. B. Stockman. He also started to use the method of full
streams in the study of the dynamics of deep sea,
Of great practical importance is the problem of the positioa of law
kes and oceans. The classification as well as the methods of prac-
tical calculation of flood characteristics worked out by A. I. Dun
vanin, represent a great value. He suggested a method for tLe com-
position of floods with constant effects in a table which is based
on the characteristics of floods according to astronomic characte-
Card 3/4 ristics. He also worked out the methods for simplified harmonic

Progress of SovietOceanography.
5c - 1 1 -8/9
analysis of short time observations. The works of Go So Ivanov, No
I. Belskiy and others which were directed to the investigations of
the Leningrad flooding, investigated the synoptic and hydrologic
connection which made it possible to improve the prognoses of this
phenomenon.
AVA.ILABLE: Library of Congress.
1. Oceanography-Development-USSR
Card 4/4

AUTHOR: Kuromtsev. A. X. 20-5-16/48
TITLE: Types of the Annual Temperature %riations in %a Surface Layer
of the Ocean (Tipi godovogo khoda temperatury vody v
paverkhnostnom sloye okeana).
PERIODICAL: Doklady AN SSSR, 1957, Vol. 116, Nr 5, PP. 776-779 (USSR)
ABSTRACT: The data of observation collected in the Oceanographic State
Institute ( Gosudarstvennyy okeanograficheskiy institut)
make possible the determination of a differe-)ce in the
annual course of temperature in the various depth of the
surface layers of the ocean. The annual variabiiity of the
temperature in some areas does not only depend on the
radiation balance of the given part of the oceat. Also au,.h
dynamic factors as the adequation and the rising currents
which carry water from great depth to the surface of the
ocean influence essentially this phenomenon. The periodic
and constant adequation of the water masses the temperature
characteristics of which had been formed under different
climatic conditions influence the annual course mainly in
the 1'over part of the surface layer but in certain areas
Card 1/3 the annual adequation can be noticed in all the surface

Types of the Ann 10
ual Temperature Variatims in the Surface Layer 20-5-16 48
of the Ocean.
layer. The rise of the water from great depth to the surface
of the ocean shows its influence first at the lower boundary
of the surface layer and then gradually covers the whole
surface layer. Depending on the influence of the just
mentioned dynamic factors three types of annual courses of
the water temperature in the surface layer of the ocean can
be distinguished:
1.) The radiation dependent annual course of temperature is
essentially dependent on the processes of the convective
turbulent mixing.
2.) The radiation advective annual course of temperature is
dependent on processes of the convective turbulent
mixing as well as on the entering of water masses with
unequal temperature into various depth of the surface
layer.
3.) The radiation advective annual course of temperature
with the rising of water from the depth is dependent
on convective turbulent mixing processes, on the
horizontal entering of warm and cold water masses as
well an on the vertical rise of relatively cold water
Card 2/3 masses. These different types of temperature courses

MUROMTSEV, Alekswj Mikhej lovich (State Oceanographic Inst) for Doe GjroZ ~;ci
on the basis of disserktion defended 23 Dec 58 in Council of Central Inst of
Forecasts, entitled "Basic features of the hydrology of the Pacific Ooean."
(MMSSO USSR, 1-61, 25)
.*218-

MUROI(TSIVO Alakasy Mikhayloviah; RIMOVITS, L.Y., otvatstvenW redo;
rot;; NrJK)]MWO. Z-1., red.; TWINUCY, O*G.9
takhn. red,
(prinelp&I hydrological features of the Pacific Ocean] OSUOTWS
cherty gidrologii Tikhogo okeana. Ieningrad, Gidrometeor. izd-vo,
1958. 629 p._ __JAppendix 2; atlas of vertical profiles and maps
indicating te"raturs, salinity, density, and oVgen content]
Pril(khoule 2; atlas vertikal'tWkh rexrezov i kDA temperatury,
solenosti, plotnosti i sodarzhaniia kisloroda. 1958. 124 p.
(Pacific Ocean) (MIRA 11:8)

AUTHORs Muromtsev, A.M. SOV-10-518-4-3/28
TITLE. The Scheme of the G~_nral Cir~.uiation of Vaters in the
Pacific OcEan (Shhemzi obs',.chey tsirkulyatsi, vod Tikhogo
okeana)
PERIODICAL: Izvestiya Lkademi-_ nauk SSSR - Seriya geor-raficheskaya,
1958. Nr 4, pp 24-~2 (USSR)
ABSTRACT~ This article is a detailed study of the general circula-
tion of Pacific waters. The currents of the surface
layer are characterized by a closed anticyclonal circular
motion in the subtropical and tropical zones and by a
minor 3yclcnal circular motion in the northern arid very
southern latitudes. After detailed oceanographical in-
vestigations of the currents at various depths in the
Pacific,, the author comes to the conclusion that the circu-
lation of the bottom waters is the same as the circulation
of waters at minor depths. The scheme of the general cir-
culation of the Pacific waters shows that the main source
supplying the waters is situated in the very southern lati-
tudes. From there the waters circulate into the various
Card 1/2 depths of the southern part of the ocean and then enter the

SOV-10-56-4-3/28
The Scheme of the General Circulation of Naters in the Pacific Ocean
northern part in the form of deep and bottom currents,
finally penetrating into the Okhotsk and Bering Sea.
There, the deep waters, as well as the intermediate and
sub-surface waters, are continuously transformedi they
are raiged in a cyclonal circular motion to the surface
and return in the form of surface waters. They then sink
into the deep layers of the corresponding convergent zones
and are absorbed by the upper deep current and taken to the
south., where they are carried into the Atlantic with the
general eastward movement. Thus the general circuiation
of the waters of the Pacific ocean is closed at the same
point in the southern latitudes from which it started.
There are 6 chartg, 1 diagram and 8 references, 6 of which
are English and 2 German.
ASSOCIATION., Gosudarstvenriyy okeanog-raficheskiy institut (State Oceano--
graphic Institute)
1. Oceariography 2. Ocean currents--Pacific Ocean
Card 2/2

'UV 301 50-5d-6-3/24
A HOR: Hurom
TITLE: The Oceanographic Investigation of the Indian Ocean
(Okeanograficheskaya izuchennost' Indiysko6o okeana)
PERIODICAL: Meteorologiya i gidroiogiya, 1958, Nr b, pp. 1,1-18 (USSR)
ABSTRACT: The author gives a historical survey of these investigations
carried out in 1772 - 1957. The inve3tigations covered
almost the whole area of this ocean with a rather dense
network of deep-sea stations (Fig 1). All data known are
at present collected in a catalogue by the State Oceano-
graphic Institute (Gosudarstverinyy okeanograficheskiy
institut). The present data of observations made in the
Indiz.~n Ocean are far behind those in the pacific nd even
further behind those maue in the Atlantic Ocean. The author
is, however, of opinion that it is not correct that the
Indian Ocean has been less investigated than the two otners.
This may apply to some detailed problems and regional
characteristics only. Because of u favorable distribution
of the deep-sea observations with regard to are" and deit,)
Card 1/2 in spite of their relatively smaller number they supply

The UceanOKraphic Investigation of the Indian Ucean S(F/50-5a-6-5/24
complete spatial characteristics. The continuation of the
investigation of Lhe Indian Ocean in the same wav as has
hitherto been folloved %iil probably not supply much new
knowledge. It would be better to direct the observations
to the collection of material on the variability of the
hydrological and hydrochemical element-~; in the courae of
time, Eta in done oloewhore. The diutricta of tho gulf of
Aden and the gulf of Oman with their respective straights
are of special interest where the hydrological characteristics
of the waters are formed which fill all deptns of the
ocean. The author hL~d already eariier mentioned the
organization of such observations (Ref 1). There ure
I figure and 1 reference, 1 of which is Soviet.
1. Oceanography--Indian Ocean
Card 2/2

AUTHOR; MuromtBev, A. M:__ SOV/50-58-11-10/25
TITLE: New Maps Showing Distribution of Salt Content on the Surface of
the Indian Ocean (Novyye karty raspredeleniya solenosti na
poverkhnosti Indiyskogo okeana)
PERIODICAL: Meteorologiya i gidrologiya, 1956, Nr 11, PP 35-37 (USSR)
ABSTRACT: As is well known, salt content is one of the main characteristics
of sea water. All changes of its quantity are caused by a change
in the volume of the sea water which depends on the.addition or
consumption of fresh water. Inasmuch as all fluctuations of the
water balance component of fresh water take place on the sur-
face, all changes in salt content are also observed on the sur-
face, from where they are propagated to various depths by verti-
cal circulation. For this reason, the distribution of salt con-
tent on the surface is important to an understanding of the
respective regularities in various depths. In the depths salt
content remains largely constant which is an indirect proof of
currents within the masses of water. Our knowledge of the dis-
tribution of salt content on the surface of the ocean is a very
limited one. Until now, however, it has not been tried even once
Card 115 to complete the existing older maps in the light of the new data

SOY/50-58-11-10/25
New Maps Showing Distribution of Salt Content of the Surface of the Indian
Ocean
available. This task has now been possible due to material
available at the GOIN (Gosudarstvennyy okeanograficheskiy
inatitut = State Oceanographic Institute). This material was
obtained by observations made during 1873 and 1957. It forms
part of the investigation carried out by the GOIN on the hydro-
logical conditions of the oceans. The observed seasonal fluctua-
tions of salt content made it necessary to systematize the ob-
servations strictly according to the seasons and to compile
maps only on this basis. This holds especially for the Indian
Ocean. Figure 1 shows a salt-content map for summer, figure 2
for winter. These now maps not only show more precise data but,
for the first t Pe, specify the distribution of salt content
south of the 20 parallel, southsrn latitude. For the first
time it was proved that south of the 600 suuthern latitude salt
content increases owing to ice formation (up to 34.65 0/00).
Furthermore, the zone of higher salt content in subtropical
latitudea was considerably restricted. The greateB~ differences
in the now maps are 9hown in latitudes north of 20 . Here a zono
Card 2/3 of reduced salt content (36.3 to 36.5 O/oo) along the 10th

3OV/50-58-11-10/25
New Maps Showing Distribution of Salt Content of the Surface of the Indian
Ocean
parallel southern latitude is especially striking. Here is also
a zone of maximum precipitations. The new representation of salt
content in the Arabian Sea and in the Bay of Bengal as well as
in the adjacent parts of the Indian Ocean rellect clearly
moneoon-dependent conditions of these areas. Finally, the salt-
content (Listribution in +he Red Sea and in the Persian Gulf are
set forth for the respective seasons. The highest values
03.42 c/oo) were obtained at the Northern spot of the Gulf of
Suez, These high values are directly connected with the penetra-
tion of water from the Great Salt Lake (salt content 50 o/00)
thro"gh the Suez Canal. The Shatt al Arab contributes to a de-
crease of salt content of the Persian Gulf down to 30.0 to
350/oo only within a small zone in the North, immediately before
the estuary. Several miles to the south, values of 39.0 O/oo and
40-53 O/oo (in winter) are recorded. Only some observations made
in the last.years were not taken into account. Today, the Indian
Ocean is the only large sea from which characteristic dtta on
the distribution of salt content of the entire surface can be
Card 3/3 obtained in summer and winter. There are 2 figures.

3(5')
AUTHOR: SOV/20-123-6-16/50
TITLE: The Density of Water on the Surface of the Indian Ocean
(Plotnost' vody na poverkhnosti Indiyakogo okeana)
.eERIODICIAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 6, pp 1014-1017
(USSR)
AISTRACT: The author first reports in short on the history of the subject
investigated in the present paper. The results of the -
obser-li-ations carried out in expeditions and other voyages in the
Indian Ocean are now collected in the Gosudarstvennyy
okeanograficheskiy Institut (State Oceanographic Institute).
This material made it possible to work out a map for these
density distributions over the whole surface of the Indian
Ocean in summer and in winter. 535 and 1125 data were used for
the working oilt of the summer and winter map. For these maps
the scale I : 5,000,000 was used. Notwithstanding the
different data for summer and winter, the corresponding maps
are of similar quality. These new maps show the real density
distribution and they satisfactorily show the characteristic
features of the monsoon in the northern part of the Indian
Card 1/3 Ocean and the seasonal variations of the density in its southern

The Density of 'Water on 'the Surface SOV/20-1 23-6-16/5 0
of the Indian Ocean
part.The maps ulso give the characteristic features of the
density distribution in the Red Sea and in the Persian Gulf.
The minimuir density value within the course of a year was
observed ir. the north-east part of the Indian Ocean. In winter,
however, "in the season of the north-east monsoon) the water of
low density is conveyed towards west, and it is observed north
of the equator, at 550 east longitude . In the north-%-.,Qofern
part of the Indian Ocean and in the Arabian Sea, the density
increases considerably. Between the equator and 100 of southern
latitude, the Indian Ocean is subdivided by a zone of lower
density which in the east is united to the zones of lowest
densities. The development of such a zone is connected with the
general distillation and with the high temperature of the ~7ater
in the vouthern subequatorial waters. North of 100 of south
latitude, density distribution is very irregular, but south of
this latitude it becomes more regular. The Red Sea and the
Persian Gulf have exceptional properties not only within t1he
Indian Ocean, but also among all oceans of the world.
Card 2,,3

KURMSIT. Alekae Mikhaylovioh. Prinimala uchastiye SMIOTA. Ye.M..
-- - Y
Ljo, prof., doirtor geograf.nauk, zasluzhennyy
dayatell nauki, nauchnyy red.; PROTOPOPOT, T.S., red.;
SMOVZYCRIK, A.A.. tekhn.red.
(Basic hydrological features of the Indian Ocean] 09novnye
cherty g1drologii Indiiskogo okeana. Leningrad. Gidrometeor.
izd-vo, 1959. 435 P. (KIRA 13:2)
(Indian Ocean-Hydrology)

14MONTSE7. A.M.
Nomenclature of principal forms of tne bottom relief of
the Pacific Ocean. Trudy GOIN no.46:86-94 159. (MM 13:6)
(Pacific Ocean--Submarine topography--Nomenclature)

S/05 61/000/005/002/003
D235YD301
AUTHORS: Lagumin, B.L., Muromtsev2 A.M., and Yushchak, A.A.
TITLE: In memory of Nikolay Nikolayevich Zubov -- engineer-
rear admiral, honored scientist and tecbnician of the
RSFSR, honorary member of the All-Union GeoErap:iic
Society, doctor of geographic sciences, professor
PERIOD.CAL: -.,-7eteorologiya i gidrologiya, no. 5, 1961, 59-60
TEXT: This is a brief survey of the life and work of Nikolay Niko-
layevich Zubov, one of the founders of the science of c:~eanogra-
phy. Before 'Jorld 'ar I, Zubov graduated in 1910 from the Naval
Academy (Hydrograp~ic Division), and in 1912 he attended at the
Geophysical Institute at Bergen in Norway an oceanographic course.
Until 1928, Zubov was mainly concerned with naval tactical re-
search. From 1928 to 1948 he was directly concerned with establish-
ing the directorate of the Hvdrometeorological Survey. During this
Card 1/3

3/05 61/000/005/002/0"03
In memory of N.N. Zubov ... D235 YD301
period he managed to bring about the establishment of the first
Department of Oceanology in the world at the Moscow Hydrometeoro-
logical Institute, where he was active for many years. The authors
point out Zubov's wide range of scientific interests. His works
include mono raphs and textbooks, suen as, for example iMorskiye
vody i 11dy ~Sea 'ffater and Ice), Lldy arktiki (Arctic Ice) and
Dinamicheskaya okeanologiya (Dynamic Oceanology), historic-.0,reogra-
phic treatises of which the most impclrtant is the fundamental book
Otechestvennyye moreplavateli-issledovateli okeanov i morey (Pa-
triotic Seafarers - Investigators of Oceans and Seas), popular-
science articles and books and also sp,-~ial manuals for research
oceanologists Z-Abstractor's note: No dates or place of publica-
tion of any works mentioned in this article are gi,.,re In the
last five years of his life 20 works wero published FY-Zubov, in-
cluding well-known treatises such as Osnovy ucheniya o prolivakK
(The Basis of the Study of Straits)q Okeanologicheskiye tablitsy
(Oceanologic Tables), Uplotneniye pri smeshenii vod raznoy tempe-
Card 2/3

3/050/61/000/005/00-2/005
In memory of N.N. Zubov ... D235/D301
ratury i solenosti (Condensation during the Mixing of Waters of
Differing Temperature and Sclinity~ jbstractor's note: The date
of N.N. Zubov's death is iot given/.
Card 3/3

MUROMTSEV, A.M.
Wdrology or the Red Sea. Dokl. AN SSSI 134 no.6:1443-1446 0 160.
(MIRA 13:10)
1. GosudaxstvenWy okeangrafichookiy institat. Predstavleno akademikom
A.A.Grigorlyevym.
(Had Sea-Hydrolog7)

9MO14TSEV, A6#K.
Rydrological conditions of the Suez C-inal. Dokl.AM SSSR 135 no.I:
179-191 n o6o. (NEU 13:11)
1. Gosudarstven4y okeanograficheskiy institut. Predstavleno
akademikom A.A..Grigorlyevym.
(Suez Canal--Hydrology)

MUROMTSEV, A.M.
Development of maritime hydrometeorological ress-rch in the
U.S.S.R. following Lenin's decree of March 10, 1921. Okean-
ologiia 1 no.3:375-381 161. (MIRA 16:11)
1. Gosudarstvennyy okeanograficheskiy institut.

"-MUROMTSEVO A.M.
I,-
Hydrology of the Suez Canalp the Red Sea., and the Gulf of
Aden. Meteor i Cidrol. no.2:42-45 F 162. (MIRA 15:2)
isuez c
Red S ~gy)
==:l0
Zen, Gulf of-Hydrology)

MUROMTSEV., A.M.; MAKEHOV, Yu.V., kand. geogr. nauk, otv. red.
[Atlas of the temperature, salinity and density of water
in the Pacific Ocean] Atlas temperatury, solenosti i plot-
nosti vody Tikhogo okeana. Moskva, Izd-vo AN SSSA, 1963.
120 p. (MIRA 16z12)
(Pacific Ocean--Oceanography)

SKLYAROV, V.M., otv. red.; GRIBANOV, N.N.9 red.; MU4WTSLT,,,A.M.,
red.; POGOSYAN, Kh.P.p red.; PROTOPOPOV, V.S., red.; RUDNEV,
G.V.J. red.; SOKOLOV, A.A., red.; SOLOVIYEV, V.A., red.;
USMOIT19 R.F., red.; ZHDANOVA, L.P., red.; RUSAKOVA, G.Ya.,
red.; CHEPELKINA, L.A., red.; KOLESOVA, Z.M., tekhn.red.
[Man and the elements; hydrometeorologic desk calendar for
1964] Chelovek i stikhiia; nastollrori gidrometeorologicheskii
kalendarl 1964. Leningrad, Gidrometeorologicheskoe izd-vo,
1963. 154 P. (MIRA 17:2)

,M0OMTSEV,..A.M.; ARKHIPOVA, Ye.G.; MAKEROV, Yu.V.; KHARITONOV,
D.G.; DOBROVOLISKAYA, L.N.; POTAYCHUK, M.S.; VORONOVA,
S.P.; BELOV, V.P.; RZHEPLITISKIY, G.V., nauchn. red.;
ROSHCHINA, V.V., red.; ZARKH, I.M., tekhn. red.
[Basic characteristics of the hydrology of the Atlantic
Ocean] OsnovrWe cherty gidrologii Atlanticheskogo Okeana.
Pod red. A.M.Muromtseva. Moskva, Gidrometeoizdat, 1963.
835 P. _[Atlas of vertical cross sections and maps of
temperature, salinity, density and o)q-gen con.position] Fri-
lozhenie no.2. Atlas vertikallrqkh razrezov i kart tempera-
tury, solenosti, plotnosti i soderzhaniia kisloroda. 182 p.
(MIRA 17:3)
1. Moscow. Gosudarstvemiyy okeanograficheskiy institut.

MAKEROV, Yu-V.; SUKHOVA, la.m.; MUAWTSEV A
j._.Zg&
Daily oscillationj of hydrologic characteri-ticB in the northern
part of the Pacific Ocean. Trudy GOIN no.77:57-82 '6z,.
(MIRA 18:1)

14UROKTSBV. A.S.
-rAk" __ -
QI~P '
1.1
Geologic%d ature of the Lvov Dept-3ssion. Geol.abor.[LVOV]
no.1:39-43 154. (KW 10:1)
1. Vansayusnyy nauchno-isalodavRtellskiy gologo-razvedochnyy
neftyRnoy institut. LIvov.
(Zwov Province--Geology. StructurRi)

T
KLITOCHIM. I.F.; KUROKTSZT. A.S.; BARANOT, I.G.; KARTYNOV, A.A.
Oil-and gas-bearivg prospects of the eastern part of the Dnieper-
Donato lowland. Gqo~. m9ftI I no.9:-1-7 & 157. OMRA lotg)
(Duiplmr Lowland-4%troleum geolW)
mniqper Lowland-.Gas. Natural-4eclogy)
(Donato Basin-Ntroleum geology)
(Donato Bhein-fts, Natural-Geology)

MUROMTSIV, A. S.
- ; ,
Tectonics and structural features of the Carpathian 4spression.
Gaol. sbor. [Lvov) no.516:552-556 '58. (MINA 12-10)
1.Ukrainsko7e otdaleniya Voeso7uzwgo nauchno-looledovatellskogo
goologo-razvedochnogo neftyanogo instituta, L'TOV.
(Carpathian Mountains-Geoloa. Structural)

V au E
.4 A
16
,I
gJ33 A -
0 0
30
&141 p Z
A.3 A
zi
-all J, 3 a 33
13
22
i!N1 41 ~l 11 i ~1~
-x I

34RONTSEW, A. ZAV I YALOV, V.H.
Mconomic effectiveness of oil and gas prospecting in the
Dnieper-Donets Lowland and northwestern margins of the Donets
Basin. Geol. nefti i gaza 4 no. 3:6-10 Kr 160. (KIRA 13:12)
1. Ukrainakiy nauchno-issledovatellskiy goologo-razvedochnyy
institut.
(Dnieper-Donets lAwland--Petroleum geology)
(Dnieper-Donets Imland-Aras, Natural--Geoloa)

KJILOKT"V, A. S.
Oleaknya kev well. Trudy, Ybila.Ul no.24:147-199 160.
(KIU 13: 7)
Iffov Proviace--Petrolnum geology)
Iwov Province-"s.f(atural-Geology)
~

BARANOVj I.G.; VITEIJKO, V.A.; ZAVIYALOV, V.M.; MUROMTSEV, A.S.
Possible reservos of oil and gas in the Dnieper-Donets Lailand,
Geol. nefti i gaza 5 no.7.-17-19 JIL 961. (MLV- 14: '-)
1. Ukrainskiy nauchno-issladovatel4skiy goologorazvedochnyy
institut.
(Dnieper-Donets Lowland-Petroleum geology)
(Dnieper-Donets Lowland-Gas, Natural--Geology)

MMOMrSF,Vt A.S.
G" pysers, Priroda 50 w.IsSD-81 Ja 16le (MIU 34sl)
1. Mcrainskly 3mmehno-looladovatellskly goo2agorasvodocbMy
institutt Levowe (G". Natural)

flIHO f~sqv
ZAV-YAi,OV, S.Yq.
Means for increasIng the efficlency of c!l a-nd gas
prospecting operatlons in ui-e Dnieper-Donets Lowhind.
Trudy UkrN-JGRI no. 7 j 9-16 163. (V.IRI, jc),~J)

AWiRYVHKFVlr,H, N.1'.; MITROMTSEV, A.",; PPRKHOMOVSK:f, C'~A.
Methods of genloglra-
I and ge~qnhyaical Froapp-Ing in
Dnieper--Donets Lowland, T:-udy UkrW.GRI no,71l7-24 lb".
Om,iRk 19-,I)

117.

IMAMARENKO, V.N.; MUROMTSEV, A.S.; PARKHOMOVSKIY, O.A.
Series of geological and geophysical prospecting operations
for oil and gas in the Soviet Union and the efficle-fly of
these operations. Neft. i gaz. prom, no.2:3-6 Af4Je 164
,MIRA 17:9)

ZAVIYALOV, V.M.;, MUROMTSEV. A.S.; PALIY, A.M.; CHEKALYUK, E.B.; CHERPAK, S.Te.
Possibilities for increasing the efficienc7 oi prospecting in the
eastern part of the Ukrainian oil- and gas-bearing basin, Goal,
nefti i gaze 9 noo2s2O-2/+ F 165.
(MIRA 18:4)
1. IGiGGI AN UkrSSRj Glavnoye upravleniye geologii i okhrany nedr
pri Sovete Ministrov UkrSSRv Ukrainskiy nauchno-issledovatellskiy
geologorazvedochnyy institut i trest Poltavaneftegazrazvedka.

MUROMISEV, Als.
Gonaitions gmmrning the formaticn of the e=ercial hy-d.-cmrbon
pools in the Carpathina piedmont fault. Trudy UkrYIGRI no.5.-91-96
163, (MIRA 180)

PHASE I BOOK EXPLOITATION SOV/4362
Baz', Grigoriy Averkovich, Gennadiy Petrovich Muromtsev, Aleksandr Nikolayevich
Rainkin, losif Konstanti-n-ov-fc-h--Tr-e-g-uE,-i-uid--]K-iril-1 Andreyevich Tsikunov
Raschat impul'snykh skhem (Design of Pulse Circuits) Moscow, Voyenizdat, 1960.
237 p. No. of copies printed not given.
Ed. ~Tltlle page): V.G. Milenin, Candidate of Technical Sciences, Docent; Ed. (In-
side book)t M.I. Podguzov; Tech. Ed.: A.N. Mednikova.
PURPOSEt This textbook is intended for the specialist radlo engineer who is
asstim6d to be acquainted with the theories of the calculated circuits.
COVERAGE: The authors make an attempt to systematize engineering calculations
of basic pulse circuits, and, as a basis for calculationsouse the gra~hic-
analytical method. Sections 1 and 3 of Chapter I and Section 1 of Chapter 11
were written by K.A. Tsikunov; Section 2 of Chapter I and also Section 3 of
Chapter II by G.P. Muromtsev; Section 2 of Chapter II, and Chapter 1II by
G.A. Bazl; Sections 4 and 5 of Chapter 11 by A.N. Rainkin; Chapter IV by
I.K. Tregub. Design of the phantastron circuit was done by V.Yu. Bulybenko.
There are 24 references, all Soviet.
Ca="#5=-

BAZI Grigoriy Averkovich; MURGU99V, Gennndy Petrovich; R!dNKIN,
A-'eksandr Nikolake-v~ich; TREGUB, Iosff-K--o-ns-t-a-nt-IFe-v-i-ch;
TSIKUNGV, Kirill Andreyevich; Prinimal ucbastiye BULYBMOo
V.Yu.; MIMIN, V.G., dote., kand. tekhn. nauk, red.;
PODGUZOV, M.I., red.; IWIIKOVA, A.N.,, tekbn. red.
[Design of pulse networks] Raschat impul*sz7kh skhem. [By)
G.A.Bal i dr. Izd.2., do~. i perer. Moskva, Voen. izd-vo
IJI-va obor, SSSR, 1962. 267 p. (MIRA 15:3)
(Pulse circuits)

XCC-k- --
IAM6018987 Monograph UR
Milenin, Vladimir Girgorlyevich; Bazt, Grigoriy Averkovich; Bulybenko,
Viktor YUrlyevich; Muromtsevs,"Agnp Petrovlchi. Osipov, Vladimir
Pavlovich; Rainkins Aleksandi Nikola.ev"f6hj- ~jab, Iosif
Konstantinovich
Principles of pulse techniques (Osnovy impul'snoy tekhniki) Moscow,
Voyenizdat N-va obore SSSH, 1966, 389 Ps illuses biblio, 45,000
copies printed.
.TOPIC TAGS: pulse coding, pulse counter, pulse generator, pulse
shaper, logic circuit, tunnel diode
PURPOSE AND COVERAOEs This is a textbook on pulse technology for-.
students attending military schools of higher education. Circuits
and methods employed in numerous fields of radio electronics are
described and analyzed. In addition to the usual problems of pulse
technology,. comparatively novel problems related to computer technology
and the use of semiconductor devices are covered.-Emphasis is placed
on the physical aspect of the phenomena.
TABLES OF CONTENTS:
Introduction -- 3

ACC NIhAM6018987
Section I. Pulse Shaping
Ch. I. Pulse ShapIng by Means of Linear Electrical Circuits -- 5
1. Electric pulses and their characteristics -- 5
2.. Brief information on linear electrical circuits -- 10
3. Differentiating circuits -- 15
4, Integrating circuits -- 31
5. Shaping lines ---35
6. Stages with an impact excitation circuit -- 52
Ch. IL Pulse Shaping by Means of Nonlinear Electrical Circuits 61
1. Nonlinear circuits and their characteristics - 61
2. General information on amplitude limiters - 63
3. Diode limiters -- 67
4. Limiters-amplifers - 72
5. Effect of separation-capacitor voltage an limiting level
(quiescent point creep) - T9'
Section II, Pulse Generation
Ch. III. Multivibrators -- 84
z/ 6

-----------
ACC NR- AM6018987
1. General information on relaxation oscillation generators -- 84
2. Multivibrator characteristics -- 87
3. Physical processes in multivibrators -- 88
4. Dependence of pulse shapes and multivibrator oscillation periods
on circuit parameters -- 93
5. Frequency stability of multivibrator oscillations and methods of
improving it -- 99
Ch. IV. Blocking Oscillators -- 103
1. General information -- 103
2. Basic equations of a blocking osiellator -- 105
3. Dynamic characteristics of blocing oscillator currents 107
Conditions for self-excitation of blocking oscillators 110
5: Physical processes in a blocking oscillator
6. Blocking oscillator pulse parameters -- 120
7. Practical circuits of blocking oscillators -- 125
8. Special features of blocking oscillator operation during the
generation of nanosecond pulses -- 132
Ch. V. Trigger Circuits 135
1. General information 135
2. RC trigger circuit with cathode coupling 135
: -,I j

ACC NR3AM0"018907
3 Variants of RC trigger circuits -_ 149
I): Rheostat trigger circuits (triggers) -- 158
Ch. 111. Sawtooth Voltage Generators -- 164
1. General information -- 164
2. Pulse characteristics of sawtooth shaped voltage -- 165
3. Sawtooth voltage generator with a resistor in the capacitor
charv,ing circuit -- 168
J;. Ways of linearizing sawtooth shaped voltage -- 174
5. Sawtooth voltage generator with a pentode in,the- capacitor
charging circuit -- 179
6. Sawtooth voltage generators with a positive voltage feedback
183
7. Sawtooth voltage generator with a negative voltage feedback 7
Ch. VII. Pulse Circuits Using Semiconductor Devices - 206
1. Special features of transistor operation under pulse regLmes--.
-- 2o6
2. Limiters-amplifiers -- 213 L
3. Mult1vibrators -- 217
4. Trigger circuits -- 226
5. Triggers -- 235
6. Blocking oscillators -- 253
C,,d 4/6

ACC NR- AM6018987
7- Sawtooth voltage generators - 262
Section III. Pulse Control
Ch. VIII. Pulse Frequency Dividezz -- 278
1. General Information and principles of operation -- 2T8
2. Stability conditions for frequency division operation -- 281
3. Frequency dividers using relaxation oscillation generators with
external triggering - 284
4o Step-by~-step frequency divider-,-- 288
Ch. IX. Pulse Counters -- 293
1. General information on pulse counters -- 293
2. Number systems -- 294
3. Pulse counters using trigger cells -- 296
4. Pulse counters using ferrites - 303
5. Sub3tracting and reversible counters - 314
6. Counters with through carry - 316
7. Pulse counters using decatrons -- 318
B. Pulse repetition frequency motors - 323
Ch. X. 'Digital Computer Circuit& - 326

CC NR& A616018987
1. L,~)gical circuits ~26
2. Dynamic triggers 345
3. Circuits using tranefluxors 354
4. Circuits using tunnel diodes 360
Ch. XI. Pulse Time Delay 364
1. " Oenera~ information 364
2. Pulse delay by means of lines 367
3. Delay by means of electronic circuits 378
Bibliography - 386
SUB CODE: 09/ SUBM DATE: 2lJan66/ ORIO REP:^042/ OTH REP: 002/
6/6

KURCKT"V, G.S.
Products of microbiological activity In sell and their role In re-
leasing P205 from phosphorites. Agrobieleglia no.1:96-103 AL-7 '57.
(MML 10:4)
1. Rookovskeye stdoloviye Isetituta, sel'skokhosyaystvanney mikroble-
legil.
(Sail micro-organisms) (Phoophornim)

Country : USSR
Category : Soil Science. Biology of Soils~
Abs Jo-ir : RzhBiol,, No 69 1959, No 24628
Author : 14uromtsev, G. S,
Inst
Title : Cjnce?ning the Products of the Soil-Elicroir-
gant.cms' Activity in the Nobilization of P205
Pho s-,-Ahor it es.
Orig Pub : Agrobiologiya, 1957, No. 11, 96-103
Abstract : The solution of Ca phosphates by soil bacte-
ria in connection with a change of the pH me-
dium and the reproduction intensity of the
microbe culture was investigated by the au-
thor In a semisynthette glucose-aspartic me-
dium wit'h 0.02 corn extract and with fluopa-
tite as P. source of P. A dira-t dependence
between The change of the pH medium and the
Card 1/4

Various methods for studying dissolution of calcium phosphates by
micro-organisms [with summary in Inglishl. Mikrobiologiia 26 no.2:
172-178 Kr-Ap 057. (KIRA 10:10)
1. Hookovskoys ot1oloniye Vaesoyuznogo nouchno-iseledovetallskogo
institute sellskokhom7systyennoy mikrobiologii.
(RACTUIA. metab.
calcium phosphate dissolution. store. methods (Rug))
(PROSPHATIS, setab.
calcium phosphate dissolution by bact., determ. methods
(Rug))

MUROMTSEEV, 'a. S. Cmidl ?,iol Sci -- I(disl; ."hifisollitinn 0, (!~._Icillm P,ros;yr-.s
in Connection vii-rh the u, lif'e-of root ~,:. ! :~nil rai,~ronrCFnjs-s."
SlIns , 19,5) .. 1 ~ p.) -'Ito 3 -'+- ~ I ~ - 4 .j - I. .I .. .. IV '00 COT i F, - , "' , " - 7 , , ,L1 )
.1 1 , ~ I . ) . - 1, 1
a16-

MFDMTSEV, G.S.
--A Ir
-Y. , - - -., i~,b 44 -T.- - L*LC -qr Wij6 14~6 water-.*
i~ :ixwd rq jgp I
insolu.I;i~~ calcium phosphates. Agrobiologlia no.5:9-14 S-0
58. (MIRA 11:11)
(Soil micro-organisms) (Phosphates)

MUROMTSM, G.S.
Chemistry of dissolving calcium phosphate by mold fungus
Aspergillus niger. DokI.Akad.%o9j'khoz. 24 no.10:19-23 '59.
(KIU 13:2)
1. Vsesoyusnyy nauchno-Issledowatel'skiy inatitut udobreniy
agropochvovedenlys. Predstavlens akademikom P.A.Baranovym.
(Phosphates) (Aspergillus)

MURCKTSLV, G.S.
Results of the investigation of the production and use of
gibberellin. Trudy Inst. mikrobiol. no~U *308-317 161.
(KM 16tll)
1. Tsesoyumyy nauchno-issledovateltskiy institut udobreniy
.' agropochvovedeniya.

KUZNETSOVt 8.0 kand.seltakokhozyaystvennykhnaukl_MMMTSE_VO_G.t kand.biolog-
ichesklkh "Allk.
Gibberllim and possiblities for its usage. Zemledelie 23 no.23:91-92
Nr 161. (Gibberellin) (MIRA 14:3)

PEN IKOVj L.A.; BLOKHINA, V.V., red.; DEMA, V.M'p
tekbn. rad.
(Gibberenins]Gibberelliny. Moskva, Sellkhozizdat, 1962.
230 P. (MIRA 15:11)
(Gibberellin)

MURONTSEVO G.S~ '9TYUK, MAI
"tolorimtric determination of gibberellic acid In the culture
fluid of Fusarium moniliforse. Izv.AN SSSR.Ser.biol. no.6:
825-831 N-D 162. (KRA l6sl)
1, Vaesoyuznyy nauchno-loaledovateliskiy Institut udobreniy I
agropachvovedeniya. (GIBBERELLIC ACID)(COIDRnwrRY)

MUROMTSLj- G.S.; RUSANOVA, N.V.
Quantitative determination of gibberellins based on the grwth rowt1an
of peas of the G-1 Pioneer varietya Fizi'-le rast. 9 to-5:626-629 162*
(MIRA 15:10)
1. All-Union Scientific Research Institute of Fertilizers and
Agronomical Soil Sciences, MDscov.
(Gibberellin)

KHMMEV, G.S.
UNWOUins of highez planta. Usp.sovr.biol. 54 no.1:90-101
Jl-Ag t62. (KW 15:11)
(GIBEEKIM)

MMMTEV, G. S. .
- ----------
The gibberellins of higher plants. Analele biol 17 no.2:100-112 Mr-
Ap f 63.