F.:. ;7 C;
Disscr L.J. 1--jn: IVariation of the Solutions of' Ordlinkry Linc~,r 'JifforenUai t 1 ons
of the Third Order."
11 I-lay 49
Sci Res Inst of I-Lat'r-eimatics, '-osco-i- Jrd,n- Len4n 3tate V ~j,.ien~ -.V. Lor-cirio5ov.
oN
rz
KULIKOV, V.O.. in2h.; KRILIKO, M.M.0 inzh.; PRII&TSKIY, V.M.. inzh.;
ZUBKOV, A.P., irLzh.; prinimali uchstiye; MERSHCM , M.P.,
inzh.; CENT7MIKOV, Y.Ta.,,inzb.;.DUIMOV,.Y.S.,,inzh.;-TQLKQY,
VMMMI]p; S&FOHOVA, M.F., tek-bW
.,_,.tekhnik; YERSHOV, V.I.;
Using scale in steelmaking by the scrap and ore proces's.
Stall 20 no-8:708-710 Ag 160. (MIRA 13:7)
(Open-hearth process)
v kandidat meditsinskikh nauk; YEGOROVA, A.P.. kandidat medi-
E9LKW1"-L-v-1
taiaskikh nauk
Dynamics of the blood complement titer in radiation sickness
combined with other lessions. Voen.-med. zhur. no.4:27-30 AP 156.
(RADIATION SICKNWS) (COMPLEMENTS (IMKUNITY))
22034
3/17 61/000/001/010/010
2 7.6 D21 lYD306
AUTHOR: Volkov, I.P., Lieutenant Colonel of Medical Services
TITLE.- A device for studying the fatigue of flying personnel
PERIODICAL: Voyenno-meditsinskiy zhurnal.9 no. 1, 1961, 78
TEXTs The apparatus consists of a box with a metal lid; in the box
is a small electric battery and an electric lamp. One end of the
battery is connected to a metallic rod (5'mm long and 1.5 mm thick);
the other to the box's metal lid. One part of the lid is perforated
with holes of diameters ranging from 2 to 8 mm; on both sides of
the lid there are panels with non-consecutive numbers from 1 -25.
By touching them with the rod, the subject examined lights the
lamp, the time needed for finding consecutive numbers being recor-
ded by the examiner with a stop watch. The second part of the exer-
cise.~,Consists of inserting the rod into the holes on the lid, and
holding it there for 1 sec. The degree of fatigue as expressed by
the tremor of fingers is determined by the diameter of the hole in
Card 1/2
22034
3/17 61/000/001/010/010
A device for studying ... D211X306
which the rod begins to touch its sides, lighting the lamp. During
the teat the subject's arm is outstrethed and slightly bent at the
elbow. The author examined 780 airmen and 275 soldier for attentive-
ness and 400 airmen and 270 soldiers for fatigue. He found that, in
general, the airmen completed the first exercise in a shorter time
than the soldiers, mostly in less than 40 seconds. Such a time is
regarded as good; a time up to 50 sec is considered unsatisfactory;
men who needed a longer period of time were found to be either ill
or particularly tired. Fatigue is registered during the second exer-
cise when the tremor of fingers is so pronounced that it causes
closing of the circuit in holes of 4.5 mm or larger diameters. There
is 1 figure.
SUBMITTED& July, 1960
Card 2/2
Lr
G ID V t; I C, mb.i 'k k 0
T 111 L New TI-anslo,~aing Equipment at, Sea Forts (Novaya tokhnika
p ere'>-r LIZ 0 C anyj~ Ii rabot v morsk4kh portakh)
PERIODICAL: iekhanizatsiya Trudoyftkikh i I'ya,_'n4lykh ~HabCt, _19'_-8. Nir 4,
pp 28-30 (USSR)
14~B,ii2iltiGT: Loading and unloading operations at sea ports are not yet,
or only partly~ mechanized. This refers mostly to the hand-
ling of loose freight and goods in packets inside ship liolds
and railroad cars. The tsentralInyye proyektno-konstruktor-
skiye byuro (The Central Design-Construction Departments) of
the 14inisterstvomorskogo flota (Merchant marine I'vIinistry) are
developing new machines and mechanisms for the complex me-
chanization of loading operations at sea portu. 2he authors
give a detailed description of the following loading mecha-
nisms: 1) the PTS-1 coal loader, designed by Engineer IN.'I.
Sergell, with a capacity of 350 tons per hour; 2) the PTj-2
for the loading of ships with a capacity of 100 tons per
hour; 3) the PTS-4, designed by the TsPKB--4, for the loading
Card 112 of 50e/76 manganese ore; 4) the PTB-2, designed by the TsPH-3,
New 11'ransi-Dadl r.-,- Dul-lir-rient a " .~'ea Ports
lia-.5 8-4 1/23
for ti-,e loading of iron ore, bauxites, etc. into ship holds,
with a capacity of 150 tons per hour; 5) 'the TsPKB-3 designed
a scraper grab crane with a lifting capacity of 10 tons; 6)
the PSG-200, designed by the TsPKB-3, with a capacity of* P-00
tons per hour (the loader has been deoigned particularly for
the loading of manganese ore); 7) the bulldozer BUIT-1, desit--ned
by the TsPKB-4, for the scraping of loose freight in ship holds,
has a capacity of about 30 tons per hour; 8) the TsPKB-3 has
designed (T nitiator Engineer D.B. Spekbor) a fork lift with a
lifting height of 4.5 meters, to be used in ship holds; 9) for
use inside railroad cars, the TsPKB has designed a fork- lift
with a lifting height of 1.5 meters and a load capacity of
1.5 tons. There are 6 figures.
AVAILABLE: Library of Congress
Card: 2/2 1. Gargc~Handling-Equipment
VOLKOV, I.G., starshiy prepodavatell
I ~~~
Automatic portable gas analyzer for use on the "Donbass" cutter-
loader. Izv. vys. ucheb. zavo; gore zhuro 5 no.3:151-153 162.
(MIRA 15:7)
1. Khartkovskiy gornyy institute Rekomendovana kafedroy
gornoy elektrotekhniki Kharlkovsk.0go gornogo instituta.
(Coal mining machinery6--Electric equipment)
(Mine gases)
'USSR/ Engines .ring - Chain drives
Gard
1/1 Pub# 128 5/34
Aitthors tKasyanevich,, A. M., and Volkov.. 1. Gj.
-Titie IConcerning the quality, of noiseless chain-drives
Periodical :.Vast. mash. 12, 16-182 Dee 1954
Abstract xThe design of a new type of a noiseless gear chata-drive'with a link feed
of 19.05 mm, and a width of 94 mm Is discussed. Operational test results
of the above mentioned chain drive and its comparison with drives produced
by the Chain Factory are given. Ill ustrations; table.
Institution 3
Sutmitted, 9
TOLKOT, Ivan Georglyovich; GLIKIN, Boris Abramovich; MOLDTIfYY, Il'ya
Tevtlkhlyevlch; LIKHOTIIISKIY, Yalentin Sergeyevich; SPEKTOR,
David Borisovich; TAYMSKIT, Anatoliy Georgiyevich; SUMN, Ta.?.,
red.; MARTIROSOY, A.Te.. red.; YATLI. T.I., red.izd-va; LATRENOTA,
N.B., tekhn.red.
(Reference book for sea harbor mechanizers] Spravochnik makhani-
zators morskogo ports. Moskva, Izd-vo "Morskoi transport,* 1959.
462 p. (MIRA 13:2)
(Harbors--Equipment and supplies)
(Cargo handling--Equipment and supplies)
~ IrMNINO
- -- - - - -- le-4,- i /t-e- ;- -j - -4--- -r-7 -- - - -
KUYAK, V.A.; VOIKOV, I.I., retsenzent; PIZMYANNIKOV, H.H., redaktor;
N3KRASOYk.--&.*T-.:-."tokhnicheskiy redaktor
[Kilns for annealing glass] Pechl dlia otzhiga stekla. Koskva,
Goo. nanchno-tekha. izd-vo legkoi promyzhlennosti, 1932. 152 p.
[Microfilm] (MLRA 7:10)
(Kilns) (Glass manufacture)
S/Oe 1,/6 210001004/0 19106 7
B1 491"Bl 01
AUTHORS: Ostroumov, E. A.t Volkov I I
TITLE- Separation of iron, aluminum, and chromium from manganese,
nickel, cobalt, and zinc with cinnamic acid
PERIODICAL: Referativnyy zhurnal. Khimiya, no. 4, 1962, 133, abstract
052 (Tr. In-ta okeanol. AN SSSR, v- 47, 1961, 150 - 158)
TEXT: The method of separating Pe, Al, and Cr from Mn, Ni, Co and Zn is
based on the precipitation of Fe3+, A13+ and Cr3+ with cinnamic acid with
2+ 2+ 2+ 2+
which they form insoluble salts while h1n , Ni , Co , and Zn form
soluble complex compounds. The most complete precipitation of Fe, Al, and
Cr occurs at PH 5.0 - 5.1- Coprecipitation of divalent elements is pre-
vented7by the addition of ammonium nhioride. To A=60 ml of the solution to
be analyzed containing about 0.1 g of the seaquioxides, 10 - 15 g of NH C1
4
are added, then a concentrated solution of NH OH is added until the appear-
4
ance of turbidity, which is cleared with 2 drops of HCI. The solution
Card 1/2
S/081/62/000/004/019/067
Separation of iron, aluminum, and ... B149/B101
is diluted with water to 80 - 90 ml, and heated to boiling. 20 -.n1 of 511-1
ammonium cinnamate (1) are added; the beaker is covered, the liquid is
gently boiled for 1 - 2 min and left on a boiling water bath for 1 - 1-5
hours, with occasional stirring. The precipitate is filtered, rinsed twice
with 20 - 25 ml portions of the following solutions 10 g ITH Cl dissolved
4
in hot water, mixed with 20 ml of 5% solution of I and diluted
with water to 100 ml, and finally with hot 4% solution of I; it is then
dried and calcined. This method is suitable for the analysis of marine
Terromanganese concretions. ~bstracterls note: Complete translation'
Gakd 2/2
VOIKOV,1.1.
Some aspects in,the development of climatology. Meteor.1 gldxol.
no-5:20-21 MY 53. ()(LU 13:9)
1. Upravleniye vodnykh putey "Glavvostok", Novosibirsk.
(Climatology)
VOIKOV. 1.I.! OSTROL'14DV, B.A.
Forms of sulfur compounds in silt waterR of andimonto oil the Black Sea.
Geokhimila no.4:337-345 '57. (HIRA 32:3)
1. Laboratnry of Marine Sediments of the Inatitute of Oceanolog7,
Academy of Sciences, U.S.S.R., Hoacowo
(Thiosulfates) (Black Sea--Silt)
OSTROUMOV, B.A.; TOLKOY, I.I.
Interconnection of phosphorus, vanadium and organic matter in the
Black Sea sediments Lwith summary in 3nglisbj. Geokhimiia AN
SSSR no.6:518-528 157. (MIRA 11:2)
1. Institut okeanologii AN SSSR, Moskva.
(Phosphorus) (Vanadium)
(Black Sea--Sedimentation and deposition)
AUTHORS I Volkov, I. I., Ostroumov, E. A. 20-114-4-47/63
-
---
TITLE: ------
Determination of Thiosulphates in Silt Waters of the Black
Sea Deposits (Opredeleniye tiosullfatoy v ilovykh vodakh os-
adkov'Chernogo morya)
BERIODICALt Dokladjl Akademii Nauk SSSRI 1957, Vol- 114, ;ir 4, PP- 853-855
(USSR
A,BSTRACT: In order to get a better idea of the diagenesis processes it
is necessary when studying the types of sulphur compounds in
aeacbposits, not only to investigate the solid phase, but to
determine also the types of sulfur compounds of the water by
which these deposits are drenched. In the Black Sea, in which
an intensive reduction process of the sulphates takes place,
there may also occur sulphites and thiosulphates, beside free
hydrogen sulfide and sulphates. The authors investigated, from
the expedition ship "Akademik S.Vavilov", at the below mention-
ed station, whether these-soluble compounds occur in the silt
waters of the deposits. A method for the determination of sul-
fites and thiosulfates in the presence of free hydrogen sulfide
C'_:; had been previously worked out by Kurtenaaker. Its applica-
bility to the Black Sea was to be checked. The shallow-water
Card 1/3 deposits here often do not contain any hydrogen sulfide. In
Determination of Thiosulphates in Silt Waters of the Black 2o-114-4-47/63
Sea Deposits
the Silt water of the deep-sea deposits it is often removed
during filtration in vacuum. Tests indicated that the con-
tent values of the thiosulfates obtained on this occasion are
unstible and vary considerably. This is due to the leaking
through into the filtration of small amounts of colloidal
sulphurous iron (hydrotoilite)o For that reason treatment
with zincarbonate suspehsion is undispensable. It removes the
free hydrogen -sulfide and the colloidal iron which is di-
sturbing in the determination of the thiosulfates. The exper-
iments showed that the silt waters in the Black Sea deposits
contain virtually no sulfites, at the most very minute traces
of them, whose amount lies within the limits of experimental
errors. But steady figures for the thiosulfates are obtained
in spite of their small amounts. They vary between from 010 to
10 mg/lit. The deep-sea deposits are richer in them than those.
:o of the shallow water. As is well-known one sulfur atom of
the thiosulfates is very mobilb and capable of reaction. There-
::--fore the thiosulfates can function as a peculiar type of
sulfur transmitters. In this respect the occurrence of thio-
sulfates may be of great interest in the study of diagerdical
Card 2/3 transformation of the Black Sea deposits. There are 1 table and
getermination of Thiosulphates in Silt Waters of the 2o--LU-44W163
11ack Sea Deposite
5 references, 4 of which areSoViet.
ASSOCIATION: Black Sea Experimental Scient1flo-Research Station of the
Institute of OCean06MVWof the AS USSR (Chermomaskays, eks-
perimentallnaya nauchno-issledovateltakaya stantsiya Instituts,
okeanologii Akademii nauk SSSR)
PRESENTEDt December 18, 1956 by N. M. Strakhov, Member, Academy of
Sciences, USSR
SUBMITTEDk December 12, 1956
Card 3/3
V /~_O V T; 27
jAUTHORS: Volkov, 1. 1., and Ostroumov, E. A., 2o-4.-32/51
TITLE: Concretions of Iron Sulphide in Black Sea Deposits (Konkretsii
sullfida zheleza v otlozheniyakh Chernogo morya)
PERIODICAL: Doklady AN SSSR, 1957, Vol. 116, Nr 4, pp. 645-648 (USSR)
ABSTRACT: Already in 189o colloidal iron sulphide was found in the Black
Sea deposits and the possibility of a formation of pjrites which
was contained in it in form of tiny pellets was assumed. Also at
that time concretions of pyrites of a length of 12 mui and a
breadth of 0,5 mm were found there for the first time. Beside
90,80 pyrites they consist of a small qhantity of silicates
which apparently are of the deposit itself. A further reference
review shows the presence of mellnicovit, hydrotroilite, and
marcasite also in the old Black Sea deposits. Transitions bet-
ween the two latter minerals occur, too. The research of these
transitions and of the process could throw a light on one of the
questions of the autogenous mineral formation of the bottom of
the sea. In summer 1956 a pillar of the ground of a length of 6m
was taken in a depth of 540 m by the expedition ship "Akademik
S. Vavilov" from one of the stations beside the cape Kodor
(42054',0 north latitude, 40054',8 east longitude). It was clayey
Card 1/2 mud, grey coloring with bluish tinge and with single intermedia-
Concretions of Iron Sulphide in Black Sea Deposits.
2o-4-32/51
te layers and stains colored black by hydrotroilite. The an.-a-1-y-
sis carried out showed that the concretions consist or, the whole
of iron sulphide. The latter contains considerable quantities of
iron sulphide which can be decomposed by hydrochloric acid (ap-
parently melluicovit) and small quantities of pyrites(marcasite).
Apparently the accumulations of colloidal hydrotroilite form
change into smearing semi-solid lumps. In the case of a further
dehyd-ration and consolidation begins, as it can be assumed, the
addition of the second sulphur atom under formation of the meta-
stable form of iron sulphide-mellnicovit which in the further
course changes into marcasite and pyrites. Thus it can be assumed
with a certain degree of conviction that the found concretions
are a transition form in the transformation of hydrotroilite into
pyrites(marcasite). There are 1 figure, and 1A. references, 12 of
which are Slavic.
ASSOCIATION: Institute for Oceanology AN USSR (Institut okeanologii Akademii
Nauk SSSR)
PRESENTED: May 6, 1957, by 11. M. Strakhov, academician
SUBMITTED: May 3, 1957
AVAILABLE: Library of Congress
Card 2/2
;-) PHASE I BOOK EXPLOITATION 846
A
U.S.S.R. I-linisterstvo geologli i okhrany nedr
Metody opredleniya radioaktivnykh elementov v minerallnom syr1ye
(Methods of Determining Radioactive Elements in Mineral Raw
Materials) Moscow, Gosgeoltekhizdat, 1958. 68 P- 3,000 copies
printed.
Compilers: Sochevanov, V.G. and Titov, V.I.; Ed.: Krasnova, N.E.
Tech. Ed.: Averkiyeva, T.A.
PURPOSE: This book is for those engaged in geochemical prospecting
for radlaactlve ores.
COVERAGE: The chemical determination of radioactive substances in min-
erals and rock formations is described in this publication. Chemical
treatment of materials in preparation for radiometric analysis is
also included. The proposed methods are considered to be the most
Card 1/4
Methods of Determining Radioactive Elements (Cont.) 846
reliable for geochemical research. Methods are presented in the
form of separate procedure instructions with the inclusion of:
principle of the method, elimination of interfering factors,
application limits, necessary reagents, procedure of analysis.
Specifications for high purity reagents are given whenever neces-
sary. There is a bibliography with 26 references, 17 of which are
Soviet, 4 English, 3 German, 1 Czech, and 1 Swiss.
TABLE OF CONTENTS:
Preface
URANIUM
3
Titov, V.I., Volkov, I.I. Colorimetric Determination of Uranium
by the Trilon-Phosphate Method 4
Zvenigorodskaya, V.M., Rudina, L.P. Colorimetric Determination of
Uranium by Means of the Fluoride Method 12
Card 2/ 4
Methods of Determining Radioactive Elements (Cont.) 840'
Zvenigorodskaya, V-M., Vasilevskaya, L.S., Deykina, T.V. Colorl-
metric Determination of Uranium in Phosphorites 16
Brodskaya, V-M., Lanskoy, G.A., Sochevanov, V.G. Photocolorimetric
Determination of Uranium in Rock (Indirect Method) 24
Vasillyev, P.I., Podvallnaya, R.L. Method of Luminescence for the
Determination of Uranium With Preliminary Separation by Means of
Titanium Phosphate 27
IONIUM
Bocharova, A.P., Malyshev, V.I. Determination of the Ratio of
Ionium Content to Uranium Content in Ores and Minerals 35
RADIUM
Sochevanov, V.G., Martynova, L.T. Method for Rapid Dissolution of
Card 3/4
Methods of Determining Radioactive Elements (Cont.) ~46
Rock for the Determination of Radium and Thorium X by the
Emission Method
Chaykin, P.I., Gumbor, K.K., Zarezkina, A.K. Simplified Separation
of Radium Isotope~s from Samples UP to 3 g
Chaykin, P.I., Gumbor, K.K., Zarezkina, A.K. Separation of Radium
Isotopes from Samples From 3 to 20 g
THORIUM
Ostroymov, E.A., Astanina, A.A. Determination of Thorium by the
Weightand Colorimetric methods
Bibliography
AVAILABLE: Library of Congress
47
D
51
54
68
TM/nah
Card 4/4 12-10-58
5(2)
AUTHORS: Volkov, I. I., Ostro"Lmov, ---. L. SO 11/75-1 ~- 2 (sometimes 'Less) the process of 1-vidrotroilite
pyri4tization proceeds ra-oi(~ly and is already almost fully completed
in the topmost ground horizons. '-Then the ratio of free S to sul-f-id-
ic S is 1, hy(f..rotroilitc chnnges very slowly into pyrite, the
derrree of nyritIzation is vcry small, and in this case hydrotroilite
Card 2/3
S/169/62/000/010/055/071
Regularities of D220/D307
will be the prevalent --'c -1---,ifidc forn in thc ground-. At the same
tinx, si-ace the amount o.7 "_1 in the -round dc-)e-nds on the free
.1-12'- corritc-rit, it can 'c irafcrred- that H2'__~ is not just the source of
all the reduced forns of L compoundS, 'out is. also in its ourn way
'the regulator o.-E all subsccuc-Lit proccsses of sulfur-compound dia-
srenesis in -he -round o_-~' the sea. 17 references.
r__Zstracter"s ln~ote: Complete tr`anslation,2
Card 3/3
D228/D307
U T H 0 RS Ostroumov, E. A. and K~~_Ikn I~ I.
,-.1 -r n, T -.-- :Z
reparation of iron, alu.-,qinum and chromium from manga-
nese, nick-el, cobalt and zinc by means of cinnamic
acid
P 0 D T C;LL: Re _1:'_-_-a t4
ivnyy zhurnal, Geofizika, no. 5, 19062, 7, ab-
s.Vract 5V50 (Tr. in-t-a okeanol. "IN, SSSR, 47, 19061,
150-158)
t4 on of
TEXT: A new method has been developed for the separa -L iron,
a7ur-1-Inum, and c.h.romium from manganese, nickel, cobalt and zinc by
-eans o' c4nna-mic acid. On heating ammonium cinnamate iron, alumi-
L - -
rium and cl-l-romium nrecipitate quan-Uitatively from a weakly acid so-
lut _4 Ont w-'-1-le manganeze, nick-el, cobalt and zinc reniain in solution.
T.he composition ol- cominounds, by cinnamic acid with trJva-
ent, ii--on, aluminun, and -u chromium under precip-itation
irivai en _L U
Co,nditions, has been, determined. Iron is deposited as a mf-xture o--:'
-I -
~wo basic salts', nd -a'e has a variable composition.
~U. a- .he nrecipiu U
.A.I=inum, and chromium precipitate as basic salts of constant com-
Card 1/2
S/16 62/000/005/0-519/093
Separation of iron D228y,-)307
nosition. The basic cinnamate salts of iron, aluminum, and chromium
-;reci-o-itate in a dense form and are readily filtered and washed.
- u
-;L'he sor-otion of divalent metals (Mn, Ni, Co and Zn) remaining in
solution by t-he basic-3altl reoidue is rio ne"ligible thatu- the oe-
Paration io achieved in a sin-le stage. The preuence of sulfates
and nitrates causes no interfere-Lce. The method is applicable for
analysis of a number of te cIrraical and natural objects, contain-
4nc- the indicated rrieta-ls, especially in the analysis of m '
.i.- 6 --- - U arine
iron-manganese concretions. 9 references. Z-Abstracter's note:
Complete translation.-7
Card 2/2
VOLKOV, I.I.
Rree hydrogen sulfide and some of its co=vers-LCJ-- FzC4=c'LS fn
sediments of the Black Sea. Trudy Inst. okean. 50:2r,-67 161.
(MIM 15.1)
(Black Sea--Hydrogen sulfide)
VOLKOV, -
r-
Iron sulfides, theIr interrelationships and trans forr-a- U ons in
sediments of the Black Sea. Trudy Inst. okean. 50;68-92 161.
(MIRA 15: 1)
(Black Sea--Iron sulfides)
08THOUMOV, OA -.,; VOIZOVY 1,1;,; POMINAil L~S~
Distribution of different forms of sulfur ccrnpounds in bottom
sediments of the Black Sea. Trudy Inst. okean. 50:G13-129 161~
(MIRA 15:1)
(Black Sea--Sulfur compounds)
OSTROUMOV) E.A.;,_YOLKOV, I.I..
Use of cinnamic acid in analytical chemistry. Report No.2:
Separation of titaniijm, zirconium, and thorium from manganese,
nickel, cobalt, and zinc. Zhur.anal.khim. 17 no.4:461-465
J1 162. OffRA 1518)
1. Institute of Oceanology, Academy of Sciences, U.S.S.R., Moscow.
(Metals-Analysis) (Ginnamic acid)
VOLKOV, I.I.
State of hydrogen sulfAqa in the water and sediments of the Black
Sea. Trudy Inst. okean. 54:39-46 162. (MIRA 16:6)
(Black Sea--Hydrogen sulfioe)
OSTROUMOV, E.A.; VOLKOV, I.I.
Separation of titanium, zirconium, and thorium from manganese,
nickel, cobalt, and zinc by using cinnamic acid. Trudy Inst. okean.
54!170-181 162. (MIRA 16:6)
(Metals--Analysis) (Ginnamic acid)
VOLKOVS I.I.
Distribution of hydrogen sulfide along the vertioal of sed.1-
ments in the Black Sea. Lit. i pol. iskop. no.1:125-130 163.
(AURA 17:3)
1. Institut okeanologii A14 SSSR.
ON m-- NO WIN- - - ow
OSTROLTWV, E.A.;-VDLKOV, 1.1.
Sulfates in marine ooze. Idt. i pol. iskop. no-3:91-102 163.
(MIRA 17; 1)
1. Institut okcanologii AN SSSR.
5/075/63/oi8/ooi/oo4/oio
E07l/E452
AUTHORS:
rj-TLE,.
Ostroumov,
The use of
Communication
from mangan4se,
PERIODICAL: Zhurnal analiticheskoy kh1mii, v.18, no.1, 1963, 52-57
TEXT: A new method for
gallium by cinnam1c acid
manganese, nickel, cobalt
ci.nnamate quantitatively
acid solutions on heating,
zinc remain in the solution.
of a mixture of-two basic
filtered and washed. Sorption
zinc (remaining in the solution)
salts is small, so that the
precipitation. Sulphates
experimental procedure is
2 figures and 4 tables.
E.A., Volkov, I.I.
cinnamic acid in analytical
3. The separation
nickel, cobalt
quantitative precipitation
which permits
and zinc was
precipitates indium
while manganese,
The precipitate
salts of gallium
of manganese,
by the
separation
and nitrates
described in
chemistry
of indium and gallium
and zinc
of indium and
their separation from
developed. Ammonium
and gallium from weak
nickel, cobalt and
formed,consisting
and indium, is easily
nickel, cobalt and
pveclpltate oE bas�c
can be done by a single
do not interfere. The
detail. There are
Card 1/2
S/075/63/018/001/004/010
The use of cinnamic acid ... . E071/E452
ASSOCIATION: Institut okeanologii AN SSSR, Moskva
(Institute of Oceanology AS USSR, 16foscow)
SUBMITTED: May 16, 1962
Card 2/2
OSTROUMOV, E.A.; VOLKOV, I.I.
Ginnamic acid in analytical. chemistry. Report NO.4- ro--terminati-on
of beryllium and its separation from manganese, nickel, cobalt,
and zinc. Zhur. anal.khim. 18 no.12:1452-1456 D 163.
(MIERA 17:4)
1. Institut okeanologii AN SSSR, Moskva.
L 02103-67 EWT(1)/EWT(m)/EWP(i)/ETI-.-.-.-IJP(c) - JD/JG/Gw
i ACC NRt AP7002373 SOURCE CODE: UR/002-0/66/167/W5/1143,/1146
AUTHOR: Pilipchuk, M. F.; Vo1ko_Y,__T,,_L,,._
ORG: Black Sea q-Zcp~~rim n'al Scientific Research Station. Institute of Oceanolo
-AN--$~SSI~-COh-ei;~o-i~or3l~aya eksperimentaltnaya nauchno-issledavateltskaya stantsiya
Instituta okeanoloaii AN SSSR) enum"'I recent black
TITLE: Distribution of molybd _aoj~ sediments
SOURCE: AN SSSR. Doklady,,v. 167, i~'o- 5, 1966, 1143-li46
TOPIC TAGS: oceanography, molybdenum compound
.ABSTiUCT: *Very little data are available on the content of molybdenum in
sea sediments. This paper gives data on the distribution of molybdenum,
in the recent sediments of the Black Sea. -Samples were collected on a
voyage of the "Akademik Vavilov",I""200 samples were collected at 192
stations,, relatively uniformly covering the area of the Black Sea. The.
:Me content in this sea varies greatly: from 2 to 78-io-4% mo03- Cem-
parison of this figure with data for the Sea of Okhotsk shows that tho
quantity of Mo in the Black Sea is approximately an order of magaitude
:greater. The cortent varies from one type of bottom material to
another. Two maps accompanying the text show the distribution of
molybdenum in the different types of Black Sea sediments (in %); those
patterns are interpretod in relation to bottom composition and entry
..Of water into the sea from the,riverse Relationship to.sea.currents
also is considered. This paper was-presented by Academician N. M. Strakhov
24 December 1965. Orig. arte has: 2 figures and 1 table. 1JPRS: 37,7101
.SUB CODE: 08 / SUBM DATE: 20Dec65 /' ORIG REF: '007 / OTFf REF: 001
UDC
Card 1 1 not 551-464-38
on
30 (N)
AUTHOR: Pilipchuk, M. F.; Volkov, 1. 1.
ORG: Black Sea
SOURCE CODE: UR/0020/66/167/002/0430/0433
--Z-~.~
Academy of ~ i gs,SSSR (Chernomorskaya eksperimentallnaya nauchno-issledovatell-
skaya stantsiya Instituta okeanologii Akademii nauk SSSR)
TITLE: Tungsten in recent sediments of the Black Sea
SOURCE: AN SSSR. Doklady, v. 167, no. 2, 1966: 430-433
TOPIC TAGS: tungsten, sea water, ocean dynami s . ocean property
ABSTRACT: The object of the study was to determine the pattern of distribution of
tungsten in recent sediments of the Black Sea. To this end, 192 samples of bottom
sediments obtained at 192 stations were analyzed. The stations were uniformly distri
buted over the water area of the Black Sea and encompassed various types of samples.
The data showed the tungsten content in the surface layer of the sediments to range
rather widely: from 1.2.10 3 to 16.1-10 3% based on W03- In natural material, the
highest tungsten content is found in aleurites. In carbonate-free matter, calcareous
argillaceous sediments, which are free from the diluting effect of carbonates, $bowed
,the highest tungsten content. High tungsten concentrations are observed in both the
sandy material of coastal areas and finely dispersed argillaceous material of the cen
Card 1/2
UDC: 551.464.38
L 24olo-66
rT6C-NR, AP6010430
tral. regions of the basin. Haps of tungsten distribution were compiled. It is con-
cluded that in the course of sedimentation, the behavior of tungsten in the Black Sea
is controlled by processes of mechanical differentiation of the material. The distri.
bution of tungsten depends on the modes of its migration and on the hydrodynamics of
the sea. Tungsten associated with coarse material is deposited primarily in the coast.
al zones; tungsten associated with finely dispersed suspensions and Fe, Mn, Al and Si
gels migrates according to the principles of hydrodynamics and deposits in fine sedi-
ments of the pelagic zones of the sea. The paper was presented by Academician N. M.
Strakhovo on 24 December 1965. Orig. art. has! 2 figures, I table.
SUB CODE: SUBM DATE., 20Dec65/ ORIG REr: ooe/ OTH REF: 002
J Card 2/2
A0-' HR: Al-'701211,2-9 S,).Ui-1,GE' CODEt UR/0075/66/021100.9,'10,'-O,'1057
AUTHOR: Ostrounov, E. A.; Volkov, 1. 1.
ORG: Institute of Oceanology, AN SSSR (Institut okeanologii AN SSSR)
TITLE: Use of cinnamic acid In analytical chemistry. Report 8. Precipitation
of rare earth elements and Yttrium and their separation from manganese, nickel,
cobalt, zinc, calcium, and magnesium
SOURCE: Zhurnal analiticheskoy khimit, v. 21, no. 9, 1966, 1050-1057
TOPIC TAGS: cinnamic acid, chemical precipitation, chemical separation,
rare earth element, yttriu-m
SUB CODE: 07,11
ABSTRACT: To separate metals of the third analytical group, the authors used
ammonium cinnamate., which quantitatively precipitates, upon heating, from
weakly acidic solutions Fe, Al, Cr, Ti, Zr, Th,' In, Ga, Be, U, and Sc, while
Mn, Ni, Co, and Zn remain in solution and can thus be readily separated. The
only slightly soluble compounds thus formed in most cases are crystalline basic
cinnamate salts.
Solutions of the nitrates of rare earth elements and yttrium were preparedo
beginning with the purest oxides verified by spectral analysis. The oxides were
dissolved in concentrated HN03 with heating and the excess of the latter was
Card 1/ 2 UDC% 543.70
ACC NR- Al-701242-9
:removed by evaporation over a water bath. The .residue was dissolved in water
'and brought to the required volume. A solution of Ce(III) was prepared from
chemically pure cerium nitrate. -.The titers of the solutions were established
by evaporation in platinum dishes of precisely measured volume with subsequent
calcining of the residue to the oxide. The concentration of the solutions was
about 1 mg of oxide per'ml.
It was found that rare earth elements and yttrium are quantitatively pre-
cipitated by ammonium cinnamate from weakly acidic solutions with PH 3-5
upon heating. The final pH value of the solution ---5-4. The precipitates are
'crystalline and correspond in composition to the normal cinnamate salts
R(C6H5CR-CHCOO) where R = rare earth element.~ Ypon calcining, these compounds
are conv;rted 2t1o.oxides..The authors thank N. V.-Lizunov, in whose laboratory
were carried out the spectral analysis of oxides of the rare earth elements and
the determination of calclum.and magnesium In them. They also thank G. M.
for the
Varshal, In whose laboratory was carried out the chromographic analysis
determination of the composition of the sum of rare earth elements. Orig. art.
has: 7 tables. Lj_P RS t40,4227
ACC NR- Apno8604 SOURCE CODE: UR/0075/6?/022/001/0030/0033
AUTHOR: Oc;troumov, E. A.;
ORG: Ocoanology Institute, AN SSSR, Mloscow (Ins-titut okpanologii Ail 53311)
TIME; Use of cinnmaic acid in analytical chemistry. RcDoet, No. 9. Cinn,,-metes- of
rare earth elements and yttrium as a gravimotric form-
SOURCE: Zhurnal analiticheskoy khimii, v. 22, no. 1, 1967, 30-33
TOPIC TAGS: rare earth compqund, yttriwd compound, cinnamic acid, gravinetric
analysis
ABSTRACT: Conditions- were determined under which rare earth elenents and yttrium
are precipitated by ammonium,cinnamate on heating in the form of neutral salts of
constant composition corresponding to the formula R(C6H5CH:CHCOO)' , where R is the
3
rare earth element or yttrium, no basic salts being formed. This is accomplished by
adding the reagent quickly (a"..onium cinn.-umate solution containing about 5~- cirnardo
acid) in substantial amounts with good stirring in order to have a sufficient initial
concentration of reagent to counteract hydrolysis. 'Ibe presence of ammonium salts in
the solution does not affect the 6omioosition of the DreclDitato. 'rho method Dem"its
the determination of very small amounts of rare earth elem'ents and yttrium, since the
cinnamate weighed has a fairly large molecular weight. The method can be used for
analyzing special alloys where the rare earths are not* in a mix-ture, but enter into
Cocd 1/2 UDC: .70
ACC "NRt
the commosition of the alloy. It is -particularly convenient for determining praseo-
dymiun. and terbium, which. on heating yield Mixed oxides of frequently indeterminate
composition. Orig. art. has:.1 table.
SUB CODEz 0?/ SUB14 DATE: 13yaY65/ 0,RIG REF: 002
Card 212
SEWLTIYANOV, V.F.; VJLKGII I .-r -
Redistritrut'on of iron and mangranese in -he
1. 1
processes in the bottGn sed_-,nent-- of the exidation zone in the
Black Sea. Lit. i pal. iskcp. no.4:72-81, Jl-Ag 265.
(141RA 18.9)
1. Chernomciikaya eksperimental7naya nauchno-issledq;Latel'ska-ya
stantsiya Imstitul;ta okeanologii ANT SSSR, Gelendzhi4,~,-.'
vo allev, 1. 1.
VOLKOVj 1. 1.:' "Some problems of linear matrical transformations".
Moscow, 1955. Moscow State U imer-i M. V. Lononosov. (Dissertation for
the Degree of Candidate of PfffSICOKkTHDIATICAL SCIENCES)
SO: Knizhnaya Letopis' No 51, 10 December 1955
Some problems involved in linear matrix transformations.
Dokl.AN SSSR 106 no.4:591-594 F '56. OMRA 9:6)
1.Xoskovskiy goaud&rBtvennjy7 universitat imani M.Y.Lomono-
soya. Predstavleno akademikom P.B.Alskeandrovym.
(matrices) (Series)
68010
1,6tTt SOV/155-58-6-11/36
AUTHOR: Volkov, I.I.
-TITLE: On the Compatibility of two Summation Methods
PERIODICALs Nauchnyye doklady vysshey shkoly. Fiziko-matematicheskiye nauki,
1958, Nr 6 Pp 71-80 (USSR)
ABSTRACTs Definition s The (real) sequence fSn ~ is called summable by the
(real) matrix A -(a mn ) to the value s, where s can be finite as
we-11 as infinite and of fixed sign, if
00
T__
lim aMnan
Theorem I : Let A and B be regular methods described by the non-
negativ~e matrices A - (a M.) and B (b mn ) with finite linea.
If each A-summable sequence is B-summable, then the methods A and
B are compatible for all sequences.
Card 1/2 Theorem 2 considers the summability to + oo.
68010
On the Compatibility of two Summation Methods SOV/155-58-6-11/36
There are 5 references, 1 of which is Soviet, 1 French, 1 Polish,
and 2 English.
ASSOCIATION: Moskovskiy institut mekhanizatsii i elektrifikatsii sol'skogo
khozy,tystva (7.7osco-w Institute for 71(-cbnni.7it1nr and ';'Inctri.-
fication of A.frriculture)
SUBIid!~-!c~GD: ~Juiie 10, 1957 (Uspekhi matematicheskikh nauk)
October 24, 1958 (Nauchnyye doklady vysshey shkoly. Fiziko-
matematicheskiye nauki)
Card 2/2
1.1,
,~.y /I,, ei I ,
_2 :-:
VOLKOV, I.I. (Mosl~va)
transformations. Mat. abor. 44 no.1:85-112 Ja 158.
(MIRA 1l.-2)
(Matrices)
VOLMV, I.I. dotsent, Imnd.fiziko-matematicheskikh nauk
K,
.."WO ~~~ng the method (G,O~-) to the sumnation of divergent series.
pplyi
Trudy HIMESK9 4 no.1:137-14,6 159. (MTRA
(Seriesi-mvergent)
VOLKOV, I.I.
Summability factors for Cesaro's methods of complex order. Usp,-
mat.nauk 17 no.1:161-168 Ja-F--,'62. (YdRA- 15:3)
(Series, Divergent)
OSTROUMOV,, E.A.; VOLKCVv I.I.
Sulfates in the bottom sediments of the Black Sea. Trudy Inst. okean.
67t92-100 164- (MIRA 17:12)
Separation of indium and gallium from manganeoeq nioke15 cobalt and
zinc with the help of cinnamic acid, ".bidetl4l-150
A new method of gravimetric determina,-,ion of beryllium and its separation
from manganese, nickel, cobalt and zinc with the help of cinnamic acid.
lbid.:151-156
VOLKOV, I.I.
Forma ti on regulari tie. s P-yi cr MPG z i 4-.~L rf Z. ll'i I i" r~: Ile a
in the deposits of Lhe fjl,,ek Trucly InaL. oketm. 67.*101-3-34, '64-
(MIRA 1-7:1-2)
VOLKOV, I.I.; OSTROHMOV, E.A.
Cinnamic acid in analytical chemistry. Report No.7: Separation of
titanium from irnn, aluminum.. chromium, and other elements. Zhur.anal.
khim. 19 no.10.,1223-1227 164. (MIRA 17:122)
1. Institute of Oceanology, U.S.S.R. Academy of Sciencen, Moscow.
9~ USSR/Engineering - Combustion, Coals )bY 52
C-4
1H
(11~ "Combustion of Anthracite Dust and Its Mixture
CV With Lean Coal," A. N. Lebedev, Cand Tech Sci,
1. 1. Volkov, Jr Sci Worker, and M. A. Yefremov,
Engr, Combustion Lab, TETs, Mosenergo (Steam-
Elac Power Sta, Moscow Regibnal Elec Power Ad-
min)
"IZ V-s Teplotekh Inst" 11o 5) PP 17-20
Describes expts for combustion of Donets anthra-
cite dust in pure state and mixed with lean
coal, in shielded furnace with corner burners
and 'without any ignition belt. by 2-stage method
developed at VTI. ExPtl data obtained permit es-
tablishing Optimum distribution of air required
in each stage Of combusti-on process. Boiler fur-
nace of TETs under operating conditions was used
for expts.
231T39
0
~rnr,InF~rr- , A. NI. - VOT,MT I. 1.T. : 77, Mlr'~")V, IV. -'-~ -
Coal, Pulverized
r" I '?! 12.
tlur-~nr nuiverized coal and its t~-.in (-.oa--. T7 '71-T 21 NO. ~'
- ; - V. -
C- ---: -
,;,onthly List of russian Accessions, l,i.!)rar7,r of '~on7ress, October 17~12. ~IV
RCKADINI, V.F., DT-.; VCLYCV, I.!., Enr-
Ccmbus t--;c,.n
Feat economy of schemes with interrupted cycle. Izv. VTI 21 No. 8, 1952
9. Monthly List of Russian Accessions, Library of Congress, December 19,5& Unclassified.
1. VOLKOV, I. I., Eng.
2. USSR (600)
4. Coal, Pulverized
7. Determining the grain structure of coal dust produced in vertical sbaft mills.
Izv. VTI 21 no. 10, 1952
9. Monthly List of Russian Accessions, Library of Congress, January -1953. Unclassified.
9WT(1)/EWT(m)/EWP(t)/EKP(b) IJP(c)
L 146 1
ACC NR: AP6004395 CAI) SOURCE CODE:
AUTHOR: Sevastlyanov, V. .; Volkov, I. I.
JD/aW
UR/0020/66/166/003/0701/0704
ORG: Black Sea Exnerimental Scientific Research -5-~ation .__Ins:titute
Academy of Sciencoks,-05A (Chernomorskaya eksperimentallnaya nauchno-issledovatel'-
skaya stantsiya Instituta okeanologii Akademil nauk SSSR)
TITIX: Chemical composition of iron-j~~anese concretions from the Black sea
3~1 IVI
.SOURCE: AN SSSR. Doklady, v. 166, no. 3, 1966, 701-704
TOPIC TAGS; iron oxide, manganese compound, =am-wa=r 0-V% oA
ABSTRACT: The chemical composition of concretions '~akcen from the sea bottom at 15
stations an the Black Sea coast near the Crimea was analyzed. The bulk of the con-
cretions consists of iron and manganese oxides in variable concentrations. The re/
/Mn ratio changes frQR 1.45 to 28.6. A definite inverse portion is observ d between
the content of iron and that of manganese. Iron is present only in the trivalent
state, and its content ranges from 26.08 to 52.27% (in terms of Fe203); manganese is
present in the divalent state, and its content ranges frcm 1.83 to 18.02% (in terms
UDC: 550.41
Card 1/2
L 14692-66
ACC NR: AP6004395
of.MnO). The active oxygen concentration varies from 0.17 to 3.35%. Substantial
amounts of SiO2, A1203, and CAC03 were found. The elements present are divided into
three groups: (1) Ni, Co, Cu, Mo, and P, which are characterized by a high geo-
chemical mobility; (2) Ti, Zr, and Cr, which have a low geochemical mobility; (3)
V and W, intermediate between the first two groups in mobility. It is concluded
that the iron-manganese concretions in present-day bottom sediments are diagenetic
formations resulting from the drawing together, of authigenic oxidized forms of man-
ganese and-iron and of elements combined with these components of the sea bottom.
The paper was presented by Academician N. M. Strakhov on 13 October 1965. Orig.
art has: 1 figure, 1 table.
SUB CODE: 0.830-1/ SUBM DATE: lOOct65/ ORIG REP: 004/ OTH REF: 000
43 Oc'
Card 2/2
VOLKOVY I.I.
Linear transformations df directionally diverging sequences.
DokI. All SSSR 165 no-4:71+2-74.4 D 165.
(1,aPA 18:12)
1. 14oskovsk-iy institut inzhenerov sellskokhozyaystvennogo
proizvod5tva. Submitted April 15, 1965.
OSTROUMOV,, E.A.; VOLKOV, 1,1,.
PrecipitMtkion of uranium and its separation from
nickel, cobalt, and zinc by means of cinnamic acid. T~nudy
Inst. okean. 79,69-74 '65.
Precipitation oC ecandium and !I's separation from manganes&,
nickel., ccballt, and zinc by means of cinnamic acid.
I b id . ,~ 7 5- 80
Separaticn. of tiltanium from :irrn, aluminim, chromium, and
other elements Iq-
y means of cinnamic acid. lb~ld.~81-86
'M7F?~. 18. S)
3 t r
iyti ca
ta f;l (a s-c an f rom. mangnntz~Se, nicKei,
t, arj ~q - 11.073
(,~ . Rl
IT
;'n t t t Li e, I T) 0 11 .7, S R , M va
OSTROUMOV., E.A.; VOLKOV, I.I.
Use of cinnamic acid in analytical chemistry. Report N'O.5:
Precipitation of uranium and its separation from manganese,
nickel, cobalt, and zinc. Zhur. anal. khim. 19 no.2:216-
220 t64. (MIRA 17:9)
1. Institut okeanologii AN SSSR, Moskva.
(-VOL&O[, ij~
High quality cellulose for viscose fiber. Bum.prom. 36 no.3;11-12
mr 61. (IMIRA 14 4)
1. Direktor Klinskor kombinata.
(cellulose (Rayon)
CHERIIETSKIY, U.S., kancl. t,~ik,,n. nuiTk; R.A.;
7 T
nt~ .; IOLKO"I
LE;YZF.RO'E',,f';';y .. -- '. ) - -
Datorifilrintlic"u, oV txlf-~avi arici cscoricjri!-~ vmil c-es of th,! (iperlIti.On
of a 200 M-w. 'UI-C)e'll LISILti~fy a cont-rol
L T] .1
no.7.-20--2 10 _ 1 C.14. (MIRA 17:8)
1. Vcf-soy-u2,nyy
VOLXOV, I.M.
~ --
Downstream formation of an abrupt wave during discharge into an empt7
channel. Izv.AH Xazakh.=.Ser.energ.no.l1:34-6l '56. (MLRL 10:2)
(Fluid Onamice)
vMKOV, I.K.
An agricultural exhibition at school. Bet. v shkole no-3:83-84
MY-Je '54. (tffRA 7:7)
1. Direktor chernowashokoy semiletney shkoly Sharangskogo rayo-
na, Kirovskoy oblasti. (Agricultural exhibiti*ns)
Z~Z~ ~,~ ~LIA~k-7.~.,Z."40~i~.,~Y4,~,---,.-A - . . - -- - -
VOLKOV . I.M.
Calcula+~ng the motion of the outflow wave in a dry flume.
Trudy Inst.onor AN Kazakh.SSR 3:74-108 161. (MRA 14:22)
%Ullid dynamics)
NOVIKOV, I.T.; NEPOROZHNIY, P.S.; GANICHEV, I.A.; LAVRENENKO, K.D.;
FINOGENOVY Ya.I.; AIEKSANDROV, D.Ya.; SERDYUKOV, N.P.;
KUDRYAVTSEV, L.H.; PETROV, A.N.; BANNIK, V.P.; V-QLMY,!-.B.I_
MELINIKOV, B.V.; STAROSTIN, I.A.; BUBNOVSKIY,.G.A.; SUVORIN,
F*Ia.; GRITSAY, B.I.; SKUPKOV, A.A.; BAMSHTEYN, Ye.B.-j TURCHIN,
'N.Yao I
IUrii Nikolaevich Pongillskii; obituary. Energ. stroi.
no.27t99 162. (MIRA 15:9)
(Pongillskii, IUrii Nikolaevich, 1925-1962)
3(6). 14(10) SOV/ 112-59-4-6669
Translation from: Referativuyy zhurnal. Elektrotekhxxika, 1959, Nr 4, p 41 (USSR)
AUTHOR: ILq ~ov 1. M.
TITLE: Reviewing the Results of Investigations of Release-Wave Travel Over a
Dry Channel
PERIODICAL: Tr. In-ta energ. AS Kazakhskaya SSR, 1958, Vol 1, pp 3-18
ABSTRACT: The history of studying transient-wave traveling in an open channel is
described, and theoretical investigations of wave travel over a dry channel
made by Engineer N. M. Bernadskiy are reported; laboratory investigations
conducted by several institutes are reported. Formulae are presented.
Bibliography: 63 items.
Card I I I
17ormation and Motion of a Wave ----on' in a Lry, 7iver Be,%"
Dr Tech Sci, Leningrad Inst of 'Water Tzrans:~ortu Fnz"inec-rs, lenin-
grad, 1954. (PiYWJekh, Oct 54)
Survey of Scientific and Technical Dissertations Defended at
USSR Higher Fducatiorial Institutions (10)
S 0: Sm. - 11o - 481., 5 1,11ay 5 5
SOV/ 124-58-8-8756
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 8, p 60 (USSR)
AUTHOR: Volkov, I.M.
TITLE: Formation of a Translatory Bore Wave in a Tail Water Upon a
Release of Water into a Dry River Bed (Obrazovaniye voiny
popuska v nizhnem b'yefe pri izlive v sukhoye ruslo)
PERIODICAL: (KazSSR Gylyrn Akad. khabarlary) Izv. AN KazSSR, Ser.
energ., 1956, Nr 11, pp 34-61
ABSTRACT: Its subject being the translatory bore wave heading a flow
of water released into an initially dry tail-water basin, this
paper deals with the formation of said wave as of the instant
that the water crosses the barrage and starts to enter the
basin. The author has conducted detailed experiments on the
formation of this type of translatory wave, using for the pur-
pose a rectangular trough fitted with a removable block-off
partition; tests were made with and without lateral contraction.
In the performance of his experiments he employs motion-
picture photography, grid coordinates, and graduated measur-
ing rods. From an analysis of his motion-picture frames he
Card 1/Z determines the depths at the abscissa of the block-off partition,
SOV/124-58-8-8756
Formation of a Translatory Bore Wave in a Tail Water (cont.)
the mass flow at that location, and the propagation rates and contours of the
aforementioned translatory bore wave. By using in some of the experiments
small spheres suspended in the water he is able to determine the velocities
at various points of the wave as well. Included in the article are extensive
data on the measurements the author rnade during the experiments, also
formulae and graphs embodying the results of his analysis of the proposals
that he makes for determining the water-discharge rate involved and the
depth at the nominal location of the barrage. Bibliography: 10 references.
V.A. Arkhangel'skiy
Card 2/2
S/115/62/000/007/003/008
E194/E455
AUTHOR: Volkov
TITLE: The measurement of stresses and small displacements
by means of frequency pick-ups
PERIODICAL: Izineritellnaya tekhnika, no.7, 1962, 14-16
TEXT: The usual resistance strain gauges have the disadvantage
that they can only be used once. A device is described for the
repeated static and dynamic measurement of stresses and small
strains; it is use~d in an oil-field to transmit,by radio,
teledynamograms of well-bottom pumps. The device consists of a
displacement pick-up and a frequency meter whose output is read
directly or by oscillograph. The pick-up is a-LC-Senerator based
on a germanium transistor; its circuit inductance varies in
proportion to the strain at its base, so altering the generated
frequency. The meter, which measures this alteration,'has a
phase-shift train whose input and output voltages are applied to a
phase discriminator which converts the phase displacement to a~
d.c. vd1tage for reading directly as strain. Construction of the
various parts is described and.the circuit diagram ia Siven. The
Card 1/2
S/115/62/000/007/003/008
The measurement of stresses ... E194/E455
range of frequency change is + 5%; a change in pick-up ambient
temperature of 15*C alters 'Che output reading by 1%. The
sensitivity of the pick-up is 10 c/s per micron, so that
displacements of 0.1 to 0.05 microns upwards can be measured.
Its sensitivity can be widely altered by adjusting the gap in the
magnetic circuit of the inductance or by altering the.
capacitance in the resonance circuit. There are 3 figures.
Card 2/2
VOI,KOV, I.N.
Using frequency pickups in =-easuz-ingrr stresses and minor
displacements. Izm.teldi. no.7:14-16 JI t62. (IMERA 15:6)
(Strain gauges)
VOLKOV: I. N.
Radiotelemetric dynamograph with frequenc7 t--dmduaers. Izv.
vys. ucheb. zav.; neft' i gaz 4 no.9-.73-78 161. (miRA 14:1-2)
-1, Taganrogskiy radiotekhnicheskiy institut.
-L
,(Remote control)
.Mr"ll -'Pum'ps)
ACCESSION NR: AP4039390 S/0144/64/000/005/0616/0620
AUTHOR: Volkov, Imert Nikolayevich (Aspirant) -
TITLE; Investigation of a frequency-sensitive pickup
SOURCE: IVUZ. Elektromakhanika, no. 5, 1964, 616-620
TOPIC TAGS: electromeasuring device, electromechanical converter,
magnet coil, transducer, thermistor, testing device
ABSTRACT: The article reports the results of an analysis of a pickup
used by the Department of Automation and Telemechanics of Taganrog-
skiy radiotekhnicheskiy institut to plot '(via a-radio channel) dy-
namic performance curves of deep pump installations. The purpose of
the analysis was to determine the variation of the frequency of the,
electric oscillations with the inductance of the,pickup resonant cir-
cuit (or with the plunger displacement) and the 4~liminate the non-
linearities in this variation, to find a method for temperature com-
pensation of the frequency and amplitude drift, and to determine the
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ACCESSION NR: AP4039390
feedback coefficient necessary for proper operation. The pickup is
regarded as a controlled electric oscillator and the conditions for
its stationary operation are derived. The amplitude balance coildi-
-tions yield the required feedback coefficient, while the phase bal-
ance yields the operating frequency. The nonlinearity in inductance
vs. frequency curve is compensated by a nonlinearity in the-induc-
tance vs. displacement curve, making the overall pickup characteris-
tic linear. Temperature'compensation is by means of a thermistor
connected in parallel with the resistance in the connection'circuit.
The same thermistor compensates for both the frequency and amplitude
drift. Orig. art. has: 7 figures and 4 formulas.
ASSOCIATION: NoAe
~SUBMITTED:. 05Apr62 DATE ACQ: 19Jun64 F_NCL: 00
SUB CODE: EE NR REP SOV: 003 OTHER.- 000
Card
VOLKOV, Imert Nikolayevich, aspirant
Study of a frequency transducer. --,z-,i. vy3. uzheb. zav.;
elektromekh. 7 no.5:616-620 164. (Hit"A -L-t:,))
1. Kafedra avtomatiki i telemekhaniki radiotekh-
nicheskogo instituta.
VOLKOV,.I.P.
Reducing Ymm breakage in weaving. TekBt.proin. 21 no.7.43-44
JI 161. (MMA 14:8)
1. Glavnyy inzhener pryadil3no-tkatskoy fabriki Imeni Vagzhanova.
(Weaving) (Textile machinery)
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A'-'- NKI AP6000174j,-/ UR/0148/65/000/009/009810102
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AUTHOR: Zalesakiy, V. I.; Volkovp~i, P&
ORG: Moscow Institute of Steel and'Ailoys
'j
(Moskovskiy institut stali i splavov)
TITLE: Study of the deformiation of metal during_!!~tti~npvunder conditions of vi-
bration loading , 17,
SOURCE: IVUZ. Chernaya metallurgiya, no. 9, 1965, 98-102
TOPIC TAGS: vibration stress, cyclic load, metal, plastic deformation, cold forging
ABSTRACT: This investigation was based on the use of a hydraulic vibrator with ge-
neraticn of h ulic pulsations by means of a screw pump, mounted In a vertical hy-
draulic presstwin a 200-ton squeeze (Fig. 1). The vibrator's cylinder is mounted
on the press bolster. Attached to the mobile press cross-bar is a platen with a dy-
namometer for measuring the deformation stress. For hot upsetting a heated upset
punch is attached below the dynamometer. A water-cooled fitting to protect the dyna-
mometer from overheating is installed between the punch and the dynamometer. Mounted
on the vibrator piston is the upset die. In the tests, cylindrical specimens of lead
with various diameter-to-height ratios (D IH = 0.65, 1.54, 3) were cold-upset, at
various vibration frequencies. The vibrado0loading stress as a function of degree
of dr--ormation during upsetting is presented in Fig. 2. Similar experiments were
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UDC: 621.735:539.374