SCIENTIFIC ABSTRACT VESELOV, V.P. - VESELOVA, G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001859610017-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

OdtATION.. 416tie
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S/264/62/0001005/0021002
1008/1208
AUTHM Kudryashchev, L. I., Teranikov, A. V. and Vesclov V P.
TITLE- Inveiftigation of non-lincar problems in heat-conduction by means or electric models.
PERIODICAL: Referativnyy zhurnal, vosdushny transport, Svodnyy Tom. v. 5, 1962, 8, abstract
5A4:5. "Tr. Kuyby, sheviik aviats. in-t.", no. 12,1961, 13-34
TEXT: The article deils, mainly with the development of methods of simulation for the solution by means
of electronic models of non-linear problem; in heat- conduction and the investigation by these methods of
temperature fields in m,.-tallic bodies having variable properties.
(Abstracter's cote; Complete translation,)

t 1013-66 JD~W
ACC NR. AT60031CIO SOUROD CODE: trR/3181/63/000/015/0,'?95/0293'
AUTHOR: 4tldryas Lev, LwI* (1-t-ofessor; Doctor of technical sciences);
G-rekov, Aj.
ORG: None
V ?,,I tf
TITLE: Use of an EI-12 to solve problems,of unsteady state heat con-
duction- n metals with varyJng thermo In the
phyolcal properties,
presence of.convactive and 2;adiative heattransfer
-.-SOURCE: Kuybyshev. Aviatsiortinyy institu-t. Trudy, no. 15, pt. 2, 1963.
nauch o-te~,E-uTc-Ee-s-k~y--ko*aferentaiI po:vopronam -
Doklady=-ustovoy
mokhaniki -zhldkoeti I gaza (Reports~-of-tho Joint scientific-technical
.-conference on -problems of the mechanics of liquid and gas), 295-298
TOPIC TAGS: convective heat transfer, radiative heat transfer, heat
--conduotion,-metal, integr ated electronic device ~%.je Y101" %Owl
ABSTRACT: The article givee: the details of solutions using an elec
-tronic grid type integrator. The problem is stated in the following
:-manner. -The_symmetrioal problem- of- heat -conduction In-a sphere-re-
duces to the following system of equatio-ris in dimensionlessvariables,
Including the differentialheat conduaticn. equation
Card--- 1/2

3.6933-;M__
ACC NRs At6003100
Ps
Anil 0 1, P*> 0,
40-
iWe_
with"th-e.boundaiy condition,of the third order
80,
AAR > 0
(2);
and.,the initial:,condition
1; AA% 04P4 1; F(P-0. 0)
e ana g,of the-dimeusionless tempera-
ture-i F is the' Fourier number; W is theboundary of the sphercris a.
normil the GI)here; and
(EU Oif + ad' + ajP + all') e.; IY~+ -4e. 7 11
aj, as,,aj, a,
are variable pa:~&meters. -A table shows results of calculation based on
use of-an E1-12,igrid, iiLtmatorlocozapared to asolution using an IPT-
The r3sultd-agree=n i satisfactory manner. Orig. art. has:
9 formulas, -1-figure,-and Itable.-
UB CODEI:09A~* DATS: 001/ ORIGI.REF-. 01312-
IBM
-card 2/2

T6003099 SOUROE~OODE; UR/3181/63/000/015/b237/0293
AUTHOR; VeselovLV. P.; Temnikov, A.V.
ORG None
TITLE: Bleotronit) -simulation of heat transfer in a regenerative type'6~-/I'
heat exchanger
nstitul, Trudy, no. 15, Pt. 't 1963.
SOURCE: Kuybvsh r. Aviatsi2rim-1 2
Doklady kustovoy~nauohno-tekhnioheskoy konferenteii po voprosam
makhaniki zhidkontl I gazaj.Reports of the Joint-polenti cal
conf ~,renge _%A =LUeqe~ of th~ mechanics of liquid and -293
_gas- 1, 207
TOPIO TAGS:~ heat transfer heat exchanger,:electronic
simulation, ?axtQ& &M~V%kZoi
ABSTRACT;_ The, art 1cle-_ considers aregenerative type,heat exchanger of
----.the -most simple type.--- The mathematical problem of heat-tran&~fer in
such a regenerator reduces to the solution of the following two/partial
differential equations:-
0,
2),
Card JZ3;

L 16928-66
ACC NR~ JLT60f
resented'for~solutjon of thasa~equations on
'A mathematical method is p,
~an ana1og computer- Compwrisons of the-reaults of this simulation
method with analytical solutions are Shown in two figures. Ito Is
stated-that thoproposed m.3thod can be used also for Investigation of
'heat.t,ransfer In 4 fixed bad of particle material, blown through by
a stresLm of gaa, and for I-avestigation of the temperature of the heat
transfer meditua in counterourrent flow in a regenerator. The method
As-olaLmed to '09 sufficiently accurate;for engineering purposes.
Orig. art. has: 19 formulas and 4 figures.
--SUB -06PE; 2OjjsUBX- DATE: OD/ ORIG RBF. 008/ CJTH REP: 001,
cam

ACC NN 'AT7000387 SOURICE CODES UR/oooo/66/000/006/0452J6466'
AUTHOR: faidryashev, L. I.; Vesel(xv, V. P.
ORG: Khybyshev Aviition Institute (Kuybyshovskiy aviatsionnyy institut)
TITLE: Iwastigation of unsteady state heat conductivity processes and of complex heat
transfer by the methods of electrical modelling, and evaluation of the error
SOURCE: Teplo- i massoperenos, t. 6: Metody r"cheta. i modelirovaniya prots3r.--;ov
teplo- i massoobmena (Heat and mass transfer, v. 6. Yietho& of calculating and
modeling heat and'ziass transfer procosses). Minsk, Nauka, i tekhnika, 1966, 432.-466
TOPIC TAGS: heat conductivity, model theory, electronic simulation, conductive heat
~.,transfer
ABSTRACT., The mathematical relationship between the temperature, the time, and the
coordina:tes at a given point of a body, for a given physical phenomenon, is described
y the heat conductivity equation
ep (T) 7 (T). Ej =='di V* 17.(7) gr'ad Tj. (1)
Me law of interantion between the surrounding medium and the surface of the body :I,-
describod by bountlar.-yr conditionz; of the M type
Card 112,

ACC NRZ AT7000387
3a (7- Td + c" (74. 741). (2)
Jos
7he initis,l Condition is determined by-postulatio.-I
T- R)
(3)
The calculations presented show that the error in the results froza electrical
modelling in the solution of the non-linear problem of unsteady state heat transfer
with eomi*x non-linear boundary conditions does not exceed 5%. Orig. art. has:
45 formulaz and 4 figures,
SUB CODE:., 20/ SUEM DATE--~ o8j=66/ aRiG REF: 007

VESZ.,OV. V.S. ~kalinin. proyfizd Frofsoyuzov., d. 18-a, kv.16)
Surgical tact1*3 in t.,.-auma with extensive defects of the skin of the
fingers and hands. Veat. khir. 91 no.11:113-114 N 163. (MIRA 17:32)
% Iz khirurgicheskogo otdeleniya (zav. - A.A.Kuzfmenko) 4-y gorodskoy
bWnitsy (glavnyy vrach - O.M.Podkyuko) g. Kalinina.

M1,10V v
(:haractoristics or the trcatmint and tharapoutic. *.ACtie-3- ir. ft?,-Ite
cholecy!stitiA in elderly persona. Sov. rwd. 28 no.11%,17-61 ja 165.
'I "
,
-IM-k '18-.5)
1 1-ya kafedra khirurgii (zav. - zaslu?.hannyy dayntell nauk pro'
R:8.Aozsnov') TS'entralfrogo 'In3tItuta usovershenstvovaniYa 'vrruchey'
na azo bolfritay Jzfmi Boi.Mna (glavnyy vrneh - dotsent YII.G.
Antonov,) v Moskva.

DARDVSXIYI Ye.T.,, inzh.; VESFLOjxYA"j&
Testing.of MP-VTI aah coUectors. Yeploaziergetiks 11 no.3s
36-38 Mr 164. (MA 17t6)
1. YuAmoys otdoloni7o Gosudarstvennogo tresta po organisataii
i ratsionalizatsii ra.,roWkh elektrostantsiy i setay.

VMM. V.T.. TWIMSEW 113,
Interiwtional contacts of the Institute of the Peoples o1L Avia,
Vest. Ali SSSR 31 no.12:111-112 D t61. (MIRA 14:12)
(Russia--Relations (General) vith Asia)
(Asi& -Relations (Gleneral) with Russia)
(Oriental stxidies)

MS_EIU,Y,T.,insh.; DAROVSUY, U.T,p inzb.1 LOZINSKIY, R.P., lnzh.;
XHIRIN.t N.D., inzh.
Adjustuent and -feating of,type MP-VTL collectors with a
4p5OO =AlAmeter, Teploonargetika 9 no,,n-.41-45 N 162. (MIRA 15:10)
1. Yushnoye otdelemiye Gosudarotvepnogo treats po organizataii i
'ratsionalizataii ra:yonnykb,,elektrostantsiy i setay.
V17 ash)

FESIIMYX N.V. , i=h.,-, KBIRI.N., N.D.., inzb.; IDZINSKIY,, R.P.,, inzb.,
VESEWVI V.T., inzb,,
Studying the model of a wet ash collector witb a gas overfeed
systerit. Teploenergatika 9 no.1:11--34 A 162. (MIRA -14:22)
1. Yimhnoye otdeleniye Gosudaretvennogo tresta po organizataii
i ratsionaltzatsii elektrostantsiy.
.(Gasee-Purification)
(Electric power p1mto-Equipment and oupplieg)

V
I-Alk
191,90
71-v
too
V").
e4
Oi
lei
Ast
O&A- dB
ed
-vg -K
t
i
'D

Ul.; LINCHEVSKIT, F.Y.; MaRINA, V.I.
Thex mal eaterifivition of synthetic fatty acids under
preg-sure* Khimlx,*om. no.9-.558-560 Ag 162. (MIRA 15:9)
(Acids, Fatty) (Esterification)

USIMOV, V.Vo; SIPEYXVA, Z.V,
lAquid phase ratr, t~f pa-mffinitlc bydrr,~arbova
(synthine) tn thi diffusicn region. Zhu-r.Fr:tkj..kt,-"z. 38
nc.,9?2043---'2O,',8 3 I.S5, (MIRA, 18EIIN
1. Ve;aeoyuzW I prayelAnyy
Inatitu'; slntatlch,!,alk!kh zht roz.,mmitaboy.

W7
Rl
tz
5E ~

AUTHOR: Veselov, V4'V*
TITI;.?.-. Conical Chromatographic Coluinns (Konusoobraznyye
khromatogrEtfioheskiye kolonki).
PERIODICAL: Kh1miya i !?ekhnologiya Topliv i Maselp 1958t Nr-7-
pp. 66 - 70. (USSR).
ABSTRACT: Conical columns of small diameter are most suitable ftr
I
the analysis of small samples of benzene and kerosene
(UP to 0.5 ml). The boundary between the aromatic and
the saturated hydrocarbon has a conical shape - i.e. a
"conical effect" Rig.l) which could be seen by using
fluorescent dyes . Various experiments were carried out
to obtain information on the shape of the boundary bet'ween
aromatio,and saturated hydrocarbons in the column fo r.
chromatographic separation. Tho various types of column3
used are illustrated in Fig.2 and chromatograms of the
separation of mixtures of benzqne and pentane in cylindri-
cal (a) and slightly enlarged N oolumns are given in
Fig-3. The height of the layer of silica gol in both
columns,= 20 cm. "he efficiency and time roquired for
carrying out analyses for cylindrical and conical oolumns
was compared in order to test the advantages of the latte-Al
Card 1/2 Fig.4%. the ratio between the intermediate fraction and

Con:Lcal Chromatographic Columns, SOVI 65-59-7-11/12
the diameter of cylindrical chromatographle columns
(the diameter varied between 3.7 to 10.1 ram), Analof-ous
tests were carried out on conical columns, results of
which are g1ven in Table 1. It can be seen that the
constriction of the column decreases the intermediate
fraction. Fig.5 gives the dependence of the quantity
of the intermediate fraction on the time of wetting for
cylindrical. columns of varying diameter. This chroma-
tographic method is very simple, and can be used for
determining the course of processes. Fig:6: chromato-
grams of crudes and hydrogenates during, various stages
of hydrogenation. These analyses were carried out when
using oonicial chromatographic columns. The results given
in Table 2 are discussed. There are 2 Tablest 6 Figures,
7 Raferenoes: 3 English, 1 German and 3 Soviet.
-l'.-Benzdnes--Separation Kerosenemw-;.Separation Chromatographic-
analysis--Applications 4. Pentane--Separation
Card 2/2

TASILOV, Y.Vo; XURAM, li-V,;. ORICHKIN, D.B.; MWOT#XD, 0-7-
$man laboratory spray dryer. Masl.-zhir.prow. 24 no.5:33-
34 158. (Drying apparatus)

VIISEwV,jj.;,X,kTAYF,VA, I.S.-, OBRICHKIN, D.B.; POPOTA, N.V.
Production of surface-active and wasbing substances b7 sul.fonation
of the oxidation products from thoroughly hydrogoals6d. petroleum
fmations. Naal...zbir. prom, 24 no.10:19-22'-158. (ICRi 11:10)
1. Koskovskiy zavod "Slo2hny7e efiry.
(Washing powders) (Paraffins) ~Sulfonation)

VICSEWY, '4148WN
:Device for the raP14 chromatographic analysis of hydrocarbon nix-
tures. Izv.Sib,otd.Aff SSSR no.4:83-89 '59. (MIR& 12110)
1. Argarsk, TSentral4aya laboratoriya Kombinata Noa6.
(Hydrocarbons --Analysts ) (Chromatographic argilyals)

66954
,5-. 32 0 0 sov/63-59-8-11/17
AUTHORt Veselov, V.V.
TITLEt Determination of the Number and Position of Me-thyl
Groups in Paraffin Hydrocarbons I
PERIODICAL: Kh1miya i tekhnologlyn topliv i masel, 1959, Nr 8,
PP 49-56 (USSR)
ABSTRACT: Difficulties arise during the determination of the
chem�cal structure of Iso-paraffin hydrocarbons in
complex hydrocarbon mixtures (Ref 1). The degree of
branching is determined by defining the parachor and the
magneto-optical rotation. The author defined the
so-called "specific free surface energy" (Y20) which he
calculated by the formula:
Y20 ' 020
d20
4
Wh:re 020 Is the surface tension at the air boundary at
20 C and d2o the spec Iific weight. Graphs show the
dependence 9f the surface tension of paraffinic
hydrocarbons on the specific weight and refractive index
Card 1/3 (Fig 1) and the dependence of the specific weight on the

66954
SOV/65-59-8-11/17
Determination of the Number and Position of Methyl Groups in Paraffin
Hydrocarbons
refractive index of paraffin hydrocarbons (Fig 2).
Fig 3 shown the apparatus used for determining the
surface tension.1 The average number of methyl groups
in synthetic heptane and iso-octane mixtures was analysed
(Table 2). It was found that the surface tension of
n-paraffin hydrocarbons was a linear function of the
reciprocal value of the molecular weight (Fig 4).
lso;araffins~ such an 2--methyl butane, 2-methyl pentane
and 2-methyl hexaneg appear in this graph on a parallel
line to the n-pa,raffins; the same applies for
isoparaffins with 2 methyl groups (20--dimethyl hexane
and 293-dimethyl. pentane). The author concluded that
isoparaffins with a defined position of the methyl groups
have a different surface tension from n-paraffins of the
some molecular weight. This applies for all members of
the group. 7hey also calculated the value Ayao for the
limit of the spocific surface tension of n-paraffins.
The structurc of branching of various isoparafa!in groups
is given in Fig 5. Approximately equal results were
for various iaoparaffine
Card 2/3 obtained for the decrease of AY20

66954
sov/65-59-8-11/17
..DetermirLmtion of the Number and Position of Methyl Groups in Paraffin
Hydrocarihons
calculated on the basis of experimental data for the
surface tension and according to the formula deduced by
the author (Table 3);
69.2:3(do - d 0-930m (10)
20
wh ere do and d are the specific weight of n-paraffins
and isoparaffins of equal molecular weight and m the
number of side niethyl groups of the isoparaffirt. There
are 15 figures, 3 tables and 11 Soviet references.
Card 3/3

VISELOT, vor.; ORMCHKIN, D.B.; rOPOVA, II-V.
Cliromatographic method for determining the hydrocarbon content
of alcoholx obtained by the bjydrogenation of fatty acids. Iz-
S:Lb.of.-d.AIT SSSR iro.12:73-78 159. OURA 13:5i
(Chromatogr1aphic analreis) (Alcohols) (Hydrocarbons)

---- TIFMJ V.1~49 ORMWIs P.B., POMAt N.Y., SHMMIK09 0.7.
4droffning liquid., paraffins in order to obtain &lkvl-
&ry:l x1fonates and. to prepare raw proftets for oxidIation.
Trutly Voot,-SiMLAN SSSR no,26:135-140 159& (RDA 13t6)
. (Paraffins) (Oulfonic acids)

,_..YMiEWVr V.V,,j ORECMM, D.B.
Brodw.-tion of synthetic -tat -substitutes frozz the products of the
deep hydroganatian, Of petraleum.fractiona* Izv*Vs~ucbeb.zav*; khimi
lrbi-.-bekh. 3 no.6:1086-1090 160. (KIRA 14:4)
(Subatitute produota) (Petroleum--Refining)

VISEWT, T.T.; X&TILTATA, I.$.; ORWEXIN, DJL: POPOTA. N.V.
. Simplified model of a. machine for testing solutions of cleaning
, compourAs, Xhimsi teikhotopli masel .5 no.4s63-66 Ay 160.
(HIM 13; 6)
(Ciewang COMPOUAds-Testing)

VXSJILOV# V.V.; ORWHXIX, D.B.; PMVA# N.V.; SHIWMIW# O.F*
Prepwation of ll-quid peraffirm for oxidation, and sioraltanaous
--prc4uction of allyl aryl salfonates. MUmA tekh.tolpl.i msel
~-v 0
J. 13-8)

VIMOV, V,V,., lush.; KORTASHOV, A.L. lush.; OUGHKIN, D&B., inih.;
N.V., insh.
Ifflict of the conj;ent of nousulfur compounds on the quality
of irashing powderv. Xasl.-shir.prow. 26 n0-1113-15 JA, 160.
OURL 13:4)
(Clemining compounds)

D.B.; SMOTIKo, O.Y.
Hydrogenation of metbyl asters Of C7 -C9 acids on a zinc-chroziun
catalyst. 4hur.prikl.khis. 33 no.4:980-98) Ap 960.
(KERA 13:9)
Cleters) (Acids, Fatty) (4drogentition)

ACCIMION M- ,,IM4026723 8/0081/64/000/002/KO07/NO07
SPLTBCE: RM KhImIya' Abs. 2N32
AUTHOR: Veselov, V. V.; I111na, A. L
TITLE: Linear velocity of the air as a basic criterion during simulation of the process
of liquid-phase oxidation of pwraffin, hydrocarbons
CITED SOURCE: Tr. N. -1. in-t sintetich. zhirozameniteley I moyushchIkh sredstv, vy*p. 2,
1961, 19-25
TOX'C TAGS- paraffin, hydrocarbon, hydrocarbon, saturated hydrocarbon, hydrocarbon
oxidation, simulation, oxidation model, liquid phase oxidation, air flow
TRKNSLATION.- During simulation of the liquid-phase oxidation of paraffin hydrocarbons,
it was shown that the basic criterion Is the linear velocity of the air. The oxidation of
solid paraffin was carried out in the presence of Kn02 (0. 1% on the basin of Mn) on a
th various amounts of the product- 75, 1501, and 300 parts;
laboxatory colurnii charged wi
in all the cases the linear velocity was 0. 033 m/sec and the consumption of air was 2 liters/
min, The value of the specific consumption of air decreased with an Increase In the charge,
Card L/2

AMESSION NR: AR4025723
amolintIng to: 1600, 800, and 400 m3/ton - hour, respectively. R was shown that the
chan;e In the aold, other, tuid carbonyl numbers was the same in all casos, The end
product was alto the same. Therefore, the criterion chosen for simulation permits
complete reproduction of the results of oxidation with a 4-fold Increase In the load on the
column. Paraffin (solidification temp. - 61C) was oxidized In the presence of Mn02
(L 016 on the basis of Mn) at 105- 120C until the acid number attained 70 nig of KOH. One
serbaas of experiments was carried out at unifo;cm specific air consumption and various
linear velocities, the second at a uniform linear velocity but various flow-rates. At a
uniform. flow-rate of air, oxidation was retarded with a decrease In the scale of the process.
At a uniform linear velocity. oxidation proceeds almost at the same rate, although the flow-
rate of air Increases about 30 fold during the change from Industrial to laboratory condi-
tionn. The sinthine fraction (275-320C) was then subjected to oxidation It a N24:2~mixture
(3_47o02) on an industrial, experimental and laboratory column at 166-16-DC for 4 hours in
the presence of 4% 1133303 and a specific air consumption of 500 m3/ton - hour. It was shown
that when oxidation is carried out at a uniform specific air consumption, the depth of oxida-
tion which Is attainable in 4 hours Increases during transition from a amrill to a large scale.
Expi3riments rikade at close linear velocities showed practically the samu results.
DATE ACQ: 0SMar64 SUB COW"t OC ENCL: 00
T. 0gibina
Card 2/2

; I
VEME-0 ~V- -.1 SIPEYEVA, Z.T.
Effoot of diffusim difficulties cn the course of the oxi-lda-
tiort process of hydrocarb=o in the liquid phase. KhIm. J.
tekh. toplo i masel 9 no,3t22-26 Kr"64 (MM T7C7)

VRSRT.OV--X'V.j SlPffffA, Z.V.
lls=rcatlon of the diffunlon vad kinetic region in the :LlquM-
.phase oxidation of bydrocarbones Neft. i gaz. prom, no,4:52-54
O-D 164 (MIRA 1812)

VMELOVP V'.V., kand. tekhn. nauk; WOW, I.A. , kand. tekhn. nwk
, -., ~ . ". - I i
Wsys to reduce the production costa of hydrogen. KI-im. prom.
nc,.4t64-66 0-r, t64. (MIRA 1813)

K OPYTOV, V.F. p doktor tekhn. nauk, otv. red.; _)TASZj&jJY
kand, kh1m, nark., red.; YERMOV, A.Ye., kand. tekhn. nauk,
red.; TISHCHMO, A.T., kand. tekhn. nauk, red.; DASM!SYJY,
L.N., kand. te)14n. nauk, red.; CREGLIKOV, A.T.0 kand. tekhn.
nauk, red. SIG11, I.Yaep kand. tekhn. naukp red.;
SEMKOVSKAYAp P.T.p kand. tekkn. naukp red.1 YEREMMKO, A.S.,
kand. tekhn. naukp red.; DYBAN, Ye.P., kand. tekhn. naukp red.;
NEDOROV, V.I., kand. tekhn. nauk, red.; POLISKIY, N.I., kand.
ftz.-mat. nauk, red.
[Iransactions Df the Second Heat Engineering Conference of
Young Research Workers) Trudy vtoroi teplotekhnicheskoi kon-
A -
f
erentsii molodykh iosledovatelei. Kiev, Izd-vo AN USSR 1963
278 p. (MIRA 17:65
:1. Teplotekbnlcheskaya konferentsiya molodykh issledovateley,,
20 1963. 2. Chlen-korresponde-at AN Ukr-W. (for Kopytov).

ANDRIANOV, Aleksandr Alekseyevichi POTE)OL'IN, S.V., glavnyy red.;
HiTSUYU,, L.P.., zamestitell glavnogo red.; SHAXHNAROVICH, L.A.,
ro)d.; BMZIN, Y.P., red.; YEWOV V- V red.; GOLANDSKIY, D.B.,
red.; GOLIDTMAN V G., red A., red.; SHASHURA-, M.V.,
mdr; RIVKIN, G.M..; red.,~ F#IpRSO11, L.V., red.; SHMLEV,.I.T.
Ke'thods of analytic decomposition of caositerite and tin ores]
:tody analiticheskogo radozheidia kassiterits i rud olova.
~
Magadan, 1962. 14 p. (Magadan. Vassoiuznyi nauchno-issledo-
vatel'skii intitut zolota iredkikh metallov. Trudy Obogashchenie
I metallurgiia, no.53). WRA 160)
(C'"siterite-Analysis) (Tin ores-Analysis)

PJ~VIKIN, V-K-; POTWINx S-V-j i1myy'red.; MATSUrEV, L.P., zamBti-
tel' glavnogo red.; SHAWAROVICHp L.A., red.; BER IN, V,P..,
red.; GOU%WXIY, D.B., red.; GMIMWp
V.o., red.; IGNATWO, M.A., red.; SHASM, M.V., red.;
RI1ffJN, G.M., red.1 FIRSOV, L.V., red.; SHEPEW, I.T.j red.
[Ch!ounding and protective cutting-9ff in underground workings
of permafrost placer deposits.] Zazemleniia i zashchitnTe
otlcliucbeniia pri podzmmoi razrabotke mogoletnemerzlykh
rooaypei. Magadam., Vasa. nauebno-isel. in-t zolota i redkikh
metallor, 1962. 26 p. (Magadan, Vaesoium7i nauchno-iBaledo-
vaiAllskil instiiut zolota i redkikb metallov. Trudy, Gornoe
delo, no.40) (HIRA 16:6)
Kolym Valley-Electrio protection)
Kb3yma. -VaUey-PUcer deposits)
~

IWELOV V.V.; LISCHEVSKiy, F. T..; MORIlfti V. I.
Effect of the molocular veight eff bigWr fatty acids an their
capacity of being reduced to alcohols, Khiz. I tekh, topl, i
masel, 8 no.3111-15 Mr 163. (MIRA 164)
1, VNIISIXZh.
(Aeids~ Fatty) (Alcohols) (Raductionp Chesical)

PCTEMKIN, S.V., glav. red.; MA7SUIEV, L.P., zam. glav. red.;
PEFSMINt V.P., red.; - EWV. Y.--.# re ; GOLUMNITS
D.B,,p red.; GOLIDIMAN,-V.-G., i~--; IGNATENIO, M.l.p red.;
SHJ61;HURA, M.V., red.; RIVKIN, G.M., red.; FIRSOV, L.V.0
red.; SHAKHNAROVICH, L.A.,, red.; SHEPELEV, I.T., red.;
SHAAOVAj L.A.,, redi.
(Reports for 1961] Sbornik referatov %a 1961 god. Magadan,,
1962. 135 P. (Itti Trudy VNII-l) (KRA 1617)
1.'Kagadan. Vaesciyuznyy nauchno-iseledovatellskiy institut
solota i redkikh vietallov.
(Frozen grotmd) (Mining engineering) (Metallurgy)
(&dld:Lng materialB)

VESEIA)Vp IT.Y.; LINCIMVSKIY, F.Vo; MORINA.. Vol,
Transformations of higherr fatty acids during their reduction
process. Xhim. i tekh. topl. i masel 10 no.3tl9-22 Mr 165.
(MIRA 18:11)
L VveBoyumVy mauabno-losledovaUllakiy i prroyektnyy
inatitut sinteticheskikh shirom miteley.

VXSEUN, V,N*.; DOROIGIOVICH, V;.~-.
Reaction of methane with metal oxides. ZInw. prikl kbin.
38 no. lOs2292-2299: 0 165. NLU 28:12*
1, Submitted October 28,, 1963.

VISELOV V-.2-, inshener; KIRONOV, S.A., professor, doktor takhaichaskikh
lauroat Stalluskoy premii, redaktor; L02BUKOVA, Te.S.,
vedug"bcMy redaktar; MWIMOV, A.T.. takhaichaskly redaktor
[A collection of simmaries of research papers of theAll-Union
Scientift o Research Institute for Petroleum Construction ituring
1953] Sbornik anno-tataii nsuohno-iseledovatel'skikh rabot VNIIStroi-
nefti za 1953 g. float. VA.Veselov. Pod red. S.A.Mironeva. Moskva,
Goo. nauchno-takhas isd-vo meftlenol t gorno-toplivoot lit-ry,
1954. 1+7 p. (MIT& 10:3)
lo Moscow# TsespywiW nauchno-lealedovatellskiy Institut po
stroisel'stvu.
(Petroleum industry-Squipment and supplies)

IDASUIN, 11. 1.; VESELOV, V.Z.
Reimforced concrete reservoirs for underground storage of
gasoline Seft# khos, 36 no*3:68-?2 Mr 158. (MIRA 11:4)
iGasoline-Storage) (Reinforced concrete construction)
(Tanke)

AUMOR: Idashkin, S. I., anLd Veselov Z*
TZW; BeInforced. Concrette Tanks for Undergronad Gasoline Storage
(Zhelezobatonnyy rezervuar dlya podzemogo khraneniya b~nzina)
PERIODICAL: Nattyanoye khozynystvo, 1958., Nr 3. pp 68-72 (MBR)
ABSTRACT: Th.- article desel-ibeo experimental work in the development of gasoline-
*permeable concrete for underground storage tank construction in the
Saviet Union. The All-Vaion Scientific Research Institute for Construc-
tion in the Petroleun and Gas Industry (VItIlstroyneft') and the State
Batitute for tlu- Design and Planning oil' Pet-raleum Industry Establish-
ments in the Eastern Fegions (Giprovostokaeft) reCOM2eaded three kinds
of gasoline-Impeineable concrete from which experimontal tanks were
ca2structed. G. F. ChalIdn [Ref 21 has pub4shed experimental data on
a atorage tank ol! durable coarse-grain water-saturated concrete built in
tb-. area of Kuybyshev at Morkvasha. V. E. Leyrikha and Engineer
S. I. Ratner, published experimental data on a concrete storage tank
containing an aWition of calcium and sodium chlorides built at the
Pavelets tank fa3w (Pavelltsovskaya, neftebaza) (Ref 31. Professor
D. F. Kozyrev Wceased) suggested that gasoline -impermable concrete
can be produced by including im addition of ferric hydroxide.
Qwd 1/2

Reinforced Concwte Tanks (Cmni-,.)
93-58-16117
Va, H. Vesel(w., R. V. Dabronkaya., T. A. Yesl*wm., 0. V. Prokof Iyeva, and
R* S, Mato opwried aut labcrat=7 experiments with this kind of cement and
the results are show4 in Table& 1-2. FIg. 1 presents the plan and cross
section of a storage tmul near Moscow biLilt of concrete with a eerric
hydroxide w1dition. Ple. ;2 GhtYw a machine designed by Engineer
G. XAlani~!kxa3ko pulling ci:-culax rt-Anforcements onto the =pex-L-mtal taak. Ole
coMletea storage tank vas tested undjor industrial conditiono'by the All-
Union ScientIfic Pes,3arch :r4atitute foz the Processing of Petroleum and Gas
and for the 3-1~uction of Si7irlbb-st'je 14qidd Fuel (Vlr=IP) under the direction of
N. N. Konstazitinov. The t&.a-*4-s &-texrIna(I that than wz practically no
Sa.0031ne 1039; due to evapoxe;Uon, no Sasoline seepage,, and no deterioration in
gasoline prcVerbiea. The axlthors coaclude that the laboratory and field results
make it yossible to --3ccmnead the, use of ferric bydroadde additions in the con-
structim of -eLi-forced-ccrnerete storage tnnk . Xxperimnts
are bel'ag coullucted in wder to dete-ri-Ine whetlier layers of gunite ccataining
ferwla bYdroztde applied to storrage tezks of conventional Portland cenent can
make t!L-- taulw gasoline Im3permable. There axe 2 figures, 2 tables., qnd 4 Soviet
references.
AVAMMS: Library of Congress
Card 2/2

VASEWV Yelpidifor k1skasy
,~~ch; XUZNETSOVA, OlIgs, Nikolayevna;
~~~~DVSUU, L.P... red.; GORDKWVA, S.S.,, takhn. red.
(Latoratory manual on soology]Praktikum po soologii. Moskva
Gas. isd-vo "Vysshda ahkolap" 1962. 248 p. (MIRA 16tl~
(Zoology-La*boratory manuals)

BELYAYEVt V.B,I, inzh.; VESELDV, Ya.A., l.nzh.
Prevontion of incr mW Tibration of bearIngs durIng the start
of gionerators. Eli~k. sta 36 no.406 Ap 165. (KIRA 18t6)

VISELOV, Ye.A., profi; VSr4tKIKH,, A.S., prof.; DENISOV, N.L., prof.;
li.p., Prof.; LAS70CIMZ, prof.; ALLU=M,
T.A.p dots.; MSSARABUV, V.I., dots.; KAT- IN, 'f.loj[ dotS.;
SOKOIDV, A.K.,, dots.; ZAVARSKIY, A.I.p red.; DEMA, V.M."
takbn. red,
(Animal husbandry and veterinary bygiene] Zbivotnoyodstvo i
zoogigiena, [By) E.A.Veselov i dr. Izd.2., perer. i dop.
Moskva, Sellkhozizdat, 1963. 451 p. (MIRA 17:2)

VESELOV., Yelividifor Alekseyevich-I doktor biol. naukj prof.j
SHU9~OVA, -I.B., reU-.; FAIMIM, I.B.., red.; ATROS."CM.-KO,
Lje,l tekhn, red,
(Evolution of aninals and plants]Evollutsila zhivotxvkh i ra-
stenli. Moskva, 3zd-vo uZnanies" 1962. 47 p. (Harodrqi uni-
versitet kulltury: Estestvennonauchnyi fakulltet, no.9)
(IAJRA 15:10)
(Evolution)

- -- VE SFILOV-Yew---A. -- - ---- - - -- - -
Mbr., Leningrad State Kedical Pediatrics Institute - 1947.
"Lasting Survival of' Fish in Air," Dolk. AN, 58, No. 7, 1947 1

VESELOV, YE. A.
Fishes
Influence of varioug factors on the oamotio pressure of blood of fresh-water fish. Uch.
zap* Kars - Fine unt., 3, 1948*
Month List of Ruasian Accessionsy Library of Congresvp October 1952., UNCLASSIFIED.

--Hm - fo~giditggjlekseyevich,
- OURWBITSUTON.F.,
Darwinism;
iv%,hebnik dlia
no-pedagog.
4,51 p.
professor; RrMOVA.N.T., reetaktor:
takhnicbAiskiy redaktor
textbook for pedagogical Institateal Darvinism;
pedagogichookildi institutovs Moskva, Gov. ucheb-
izd-vo Hinisterstva proeveshcheniia RSM, 1955.
(KULk 9:4)
(Evolution)

USILOV, Yelpidifor Alaksayevich; 210KIYA, A.L.. red.; TATURA. 0.L,,
Darwinism; textbook for pedagogical institutes) Darvin1m;
uobabnik dlia pe(tagogichookikh inatitutovo Isdo3se Ispr, i dopo
Moskva, Gos.uch9bno-pedmgog.izd-vo V.-va proov.RSFSR, 1960. 503 p.
(H IM 13: 10)
(1volution)

L 349666-66 zm~;m, ~,t v - 2
tACC MR: AR6000i305
SOUR03 CODE: VR/0169/65/00O/009/B044/B045
~SOURCE: Ref. 71k. Geofizika, Abs. 9B325
~AUTHOR: Veselov Ye. P.
ITITLE: Strong vinds on the Nhite Sea
CITED SOURCE: S~b. rabot po regional'n. sinopti)-e, no. 9, 1964, 14n-47
.:TOPIC TAGS: weather forecasting, wind, atrmpheric pressure, storm
TRANSLATION: n,.e paper is a report on the use of the physical relationships between
wind, pressure field and local physical and geographic conditions for wind forecasts
'in the White Sea. region. Statistic analysis of data for 1953-1957 wirs used as the 1.~:;
~material for studying storm winds (>10 m/sec) on the White Sea. Theve am- an aver-
.age of 78-87 stcormy days In tile northeni section of the White Sea, wIdle the average
in the inlets is 12 to 15 sto:rmy days. Storms are more prevalent in the western
half of the region 06-64% of the total). ~.In some regions, there is Inore frequently
an Intensification of southea-ft winds. In all regions of the White Sea, southwest
winds am observed more frequently In the summer and northwest winds in the winter.
Card-1/2 UDC: 551.55 + 551 .509.52

L 39666-66
I-ACC HR: AR60001305
.~The storms are caused by western (Atlantic), northern (dipping), southern and east-
,ern (anomalous) cyclones. The methods for forecasting storm winds were improved by
busing V. R. Dub(!ntsovts idea IF r calculating the wind velocity from maps for the fu-
ture distribution of atmospheric pressure. A curve was plotted for forecasting the
.actual wind ca="!kApo m/sec (where k--calca, cc is the velocity of the gradient wind,
:and Apo is the pressure increment in millibafs per 300 km). Values for Apo in mb/300
~km were laid off along the x-axis of this graph, while values of ca in m/sec were
laid off along the y-axis. Sloping straight lines drawn every 0 .05 units correspond
.to the various values ofk. it check of the me-thod showed that the M03t reliable
;forecasts (86-9$%) are obtained at all points of the Dvinskaya and Onezhskaya Bays,
;as well as in ftzen', Gridino and Kovda. The least reliable forecasts. (70-80%) are
:observed in the northern section of the Sea.
I
':SUB CODE: 08
;Card

ACC NR- AT6032991
SOURCE CODE: UR/2546/66/000/149/0102/0107
AUTHOR: Vesel.ov, Ye. P.
ORG:
TITLE: Calcu%ation of wind velofty at the earth's surface
SOURCE: Moscow Tsentral'n,ry institut prognozov. Trudy, no. 149, 3.966. Rezul'taty
ispytaniy raz:Lichnykh sposobov kratkosrochnykh prognozov pogody (Rnsults of analyses
of various short-range weather forecasting methods), 102-107
TOP19 TAGS: inicrometeorolol;y, weather forecasting, wind spend
W~"J) .~4,ZH Vt&_zt)
ABSTRACT: A method is presented for calculating wind velocities at: a point on the
-;urface with the baric gradient, rising winds near fronts, and chauges in the pres-
sure and wind fields in timoi taken into account. The equations of the geostrophic.
wind Cgs and -the gradient vind Cgr (in the form proposed by Brent) were employed
as the initia1 equations fo:r calculating wind velocities at Kanin Tios on the 16aite
Sea coast. Expressing the :radius of curvature r in km, apo/an z Ap,/An in mb/300 km,
Cgs and Cgr ta m/sec, at laiciiudes between 65 and 70* N, latitude:
.-C 2AP
go 0
or
Card 1/4

ACC NRj AT6032!991
Cgr 2ApO 30(ap,)2/r (2)
Since equation. (1) is simpler to use and is sufficiently accuratea the equation for-
the true-wind velocity., witb-friction taken into account, can be written
Ctr a 2KApo, (3)
where K is thc ratic. of the velocity of the true wind to that of the geostrophic
wind. This Uctor takes implicit account of friction and other physicogeographi.c
factors. An attmept was made to use a differential approach in determining the
average valuee; of K, using the Kanin Nos Hydrometeorological Station F1___1 an examples
.It was assumeil that the pressure gradient at a point usually varies ih' time as a .
result of the movements and evol6tion of baric formations. The different nature of'-.,
mutual adaptations of pressure and wind fields in tha*atmosphere was also taken '
into account. A. M. Obukhov has shown that when the true wind differs considerably
from the geostrophic wind, atmospheric waves are generated,.which move at the speed--
of sound, and the pressure field adapts itself to the wind field as these waves are
dispersed. This adaptation occurs at the middle barotropic atmospheric level if
the initial radius of the disturbance is small compared with the conditions of.the
horizontal scale L, equal to 2000-3000 km for nontropical latitudes, and -commen-
surate with the radii of cycaones, anticyclones, and other large-scale disturbances.
Similar results have been obtained for three-dimensional allwsphereii by. 1. A.'Kibel
A. S. Monin, AL. H. Obukhov,~Chleng Ch'ing-chun. An order td clarify the nature of

ACC NRiAT6032991
adaptation of the atmospheric pressure and wind fields, values of the true wind
velocities at the surface and the baric gradient at Kanin Nos were compared for
300 synoptic situations. It turned out that the Wind and pressure fields coin-
cided in 50% of the cases, the wind adapted to the pressure field in 32% of the
c.ases, and presaure adapted to the.wind field in'only 18% of the cases. Compari-'..
son of these adaptations and -the radii of the cyclones and anticyclones.
showed coincidence of fie:6da or adaptation of winds to the pressure field
when the radii exceeded 500 lui. Adaptation 'of pressure to the wind field was
observed for radii under 500 lun. It was found that X decreases when the pres-
sure gradient and the wind velocity increase. When the pressure and wind velocity
fields coincide, the windvelocity calculated by formula (3) almost coincided with
the true wind velocity. A study was made in calculating the frontal strengthening
of winds. For chis purpose, analyses were made of 477 instances of the passage
of cold and war;a fronts,occluded fronts, and the warm and cold branches of quasi-
stationary fron!:s over Kanin Nos. Frontal strengthening of winds was noticeable only
when the baric gradients were small. In these cases, K was larger than during
front-free periods (from 0.90--2.20) and wind velocities were higher, on the average,
by 2 m/sec. TabulateA data indicated that in working with actual charts, the dif-
ferential approach to selectilig the coefficients improved calcula-tion accuracy by*
11-16%; use of coefficients ithich took account of the effect of fronts yielded a
6% improvement when the baric gradient was increasing and 1OZ when it was decrpasings
It was concluded that one could be guided by the following rules: 1) During the
passage of disturbances with radii of more than 500 km, 'wind velocity calculated for,j-
Card**3/4

ACC NR- AT6032991
a given point at time t should be expected in the period from t to t + 6 hr;
2) If the raditia of.-the disturbances is less than 500 kM, the.calculated wind
velocity should be expected In the period from t-tot- 6 hr,---3) When frontal
effect6 are anticipated (with small Apo), 2 m1see should be added to the calculata~~
values of windwelocity. IWA-501
SUB CODE: 04/ SUBM DATE:..-adne/ ORIG REFs 008/. 0TH RHF9 003/
2~
TV
Corel -4/4

ACC NR' AR6035231 SOURCE CODE: UR/0169166/000/009/BO22/BO22
AUTHOR: Veselov, Ye. P.
TITLE- Computation of wind velocity at the Earth's surface
SOURCE; Ref, zh. Geofiztka, Abe, OB158
REF SOURCE: Tr. Tsentr. in-ta prognozov, vyp. 149, 1966, 102-107
TOPIC TAGS: wind velocity, boundary layer, surface boundary layer, baric
gradient, wind field, weather foravasting, wind gradient, wind pressure
ABSTRACT: A method is described for computing the velocity of the wind at a
given point in the surface boundary layer. The method takes into account the baric
gradient, frontal wind increase, and variations in field pressure and wind with
time., (Based on author's abstract) (BPI
SUB CODE: 20/
-WC1 "I*.

ACC NRt AT603299JI. 'SOURC27 CODE: UR/2546/66/000/149/0102/0107
AUTHOR: Veselov, Ye. P.
ORG: Y141a
'TITLE: Cal6ulation,of wind velco,_*y at the earth's surface
SOURCE: Tsentral'nyy institu 't prognozov. Trudy, no. 149, 1966. Rezul'taty
,ispytaniy razlichnykh sposobov kratko-srochnykh prognozov pogody (Results of analyses
.of various short-range weather fQrecasti:ng methods), 102-107
TOPIQ TAGS: micrometeorology, weather forecasti ng, wind
T"
'ABSTRACT:. A me.th.od is presenteZ*for calculating wind velocities at a point on the
!;urfage with the baric gradient, rising 'winds near fronts, and changes in the pres-
sure And'wind fidlds in time taken into account. The equations of.the geostrophic
Find C., and the gradient wind Cgr (in the .form proposed by Brent) were employed
.as the initial equations for calculating wind velocities at Kanin Nos on.the-White
Sea coast. Expressing the radius of curvature. r in km, apo/3n -- Apo/An in mb/300 km,
C an&C' in m/sec, at latitu4:es between 65 and 70* N. latitude:
gs gr
C - 2Ap
gs 0
or'
(1)

AT6032991
24p0 30(ap,)2/r (2)
Cgr
Since equation (1) is simpler to use and is Eufficiently acturate, the equation for
the true-wind velocity,'with-friction taken into account, can be written
Ctr - 2KApo, (3)
where Kis the ratic. of the velocity of the.true wi-Ad to that of the geostrophic
wind. This fictor takes implicit account of friction and other physicogeographic
factors. An attmept was made to use a differential approach in determining the
avetage values of K, using the Xanin Nos Hydrometeorological Station as an example.
Tt was assumed that the pressure gradient at a point usually varies in time as a
result of the movements and evol-ation of baric formations. The different nature of
mutual adaptations of pressure and wind fields in the 'atmosphere was also taken
into account. A. M. Obukhov has shown that when the true wind differs considerably
from the geostrophic wind, atmospheric waves are generated, which move at the speed
of sound,, and the pressure-field adapts itself to the wind field as these waves-are
dispersed., This adaptation occurs at the middle barotropic atmospheric level if
the initial radius of the disturbance is small compared with the conditions of the
horizontal scale L, equal to 2000-3000 km fornontropical latitudes, and commen-
surate with the radii of cyclones, anticyclones, and other large-scale disturbances.
Similar results have been obtained for three-dimensional atmospheres by I. A. Kibel,.
A. S. Monin, A. M. Obukhov, Chleng Ch'ing-chun. Tn order t6 clarify the nature of
Card 2/4

ACC NRt AT6032991
i adaptation of the atmospheric pressure and wind fields, values of the true.wind
velorcitics at the 'surface and the 6aric gradient at Kanin Nos were compared for
3.00 siynoptic-situations. It turned out that the wind and pressure fields coin-
cided in 50% of the cases, the wind adapted to the pressure field -in :52% of thAe
cases, and pressure adapted to the wind field in only 18% of the cases. Co-.,,pari-.
's'on'of*these adaptations and the. radii of the cyclones and anticyclones
sh6wed coincidence of fields or adaptation of winds to the pressure fiel
d
when the radii exceeded 500 kn,. Adaptation of pressure to'the wind.field was
I observed for radii under 500 km. It was found that K decreases when the pres-
sure gradient and the wind velocity increase. When the pressure and wind velocity
fields'colincidth, the wind'velocity calculated by formula (3) almost coincided with
the true wind velocity. A study was made in calculating the frontal str n theni
e 8 ng
of winds. For this purpose, analyses were made of 477 instances of the passage
of cold and warm fronts,occluded fror%ts, and che warm and cold branches of quasi-
stationary fronts over Kanin Nos. Frontal stxengthening of winds was noticeable only!
when the baric gradients were small. In these cases, K was larger than during
,front-free periodp (from 0.90-2.20) and wind velocities were higher, on the average,,*
by.2 m/sec. Tabulated data indicated that in working with actual charts, the di.-:- I
ferential approach to selecting the coefficients improved calculation accuracy by 1
11-16%; use of coefficienis which took account of the effect of fronts yielded a
'6% improvement when the baric gradient was increasing and 10% when it was decreasing.
1". was concluded that ctne could ':)e guided by the following rules: 1) During the
passage of disturbances with radii of more than 500 km, wind velocity calculated for
Card 3/4

ACC NR. AT6032991
a given point at time t should be expected in the period from t to t " 6 hr;
2) If the radius ol the disturbances is less than 500 km, the.calculated wind
velocity should be expected in the period from t to t - 6 hr; 3) When frontal
effects are anticipated (with small. Ap ), 2 m/sec should be added to the calculated
values of windvelocity. JWA-50) 0
SUB CODE: 04/ SUIRX DATE: nonef ORIG REF: 0081 OTH REF; 003/

-- vrkszLov,,Tu,..
,Wwwmwwftwm~m..-wAw
History of camemil. IUU. takh. 2 n0.9:64-66 a 157. (KLU 10:9)
(Camram)

vmzov, YU.
YOUILSO "ga)*tpr. .4ov,foto 20_no*3 160
I - - (KiRk 13:7)
(Photograpiw-MMipment and supplies)
(VoTtap rega3ators)

NIKOIAUNNO) S.S.~ inzh..-, IESIKOV, A.S., in?,h.; Wfo"MY, A.R.,
Deepening the shalt of the Kocilmtern Mine. -hak-ht. stroi.
6 ncw.7:2C).-2.1+ Jl 162. (1-a',:;A 15:7)
1. 3WlitoproLlux-choskoyc upravleniye No.2 treata :t)assshakhto-
prohhodk,- (for li'llolayenko). 2. KrIvorozhskiy fili-
Uk-rhiml.~;,-,o nauchno-issledovateltskogo instituta org.,~aizattdi
i n-IokhvmJzatsii ui,a'~Ltnogo rtroitellstva (for Yes Ikov, 3otsldy,
veselov).
(Krivoy Rog Basin--Shaft sinking)

84580
8/006/60/000/010/002/008
B012/BO54
AUTHORs VeBelov, Yu. F.
TITLEt Consideration of the Effect of the Daily Aberration in the
Method of Equal Altitudes
'IV
PERIODICAW % Goodeziya i kartografiya, 1960, No. 10, pp. 18 - 20
TEXTt For determining the astronomical coordinates at triangulation
points of the let order, the specification for triangulations of the lst,./
2nd, 3rd, and 4.th orders admits, besides other methods, also the method of
equal altitudes suggested by A. V. Mazayev. When evaluating observations
made by this mothod, it is, therefore, necessary to take account of all
corrections by which the effect of various external factors is eliminated.
A. V. MazayeV suggested formulas to consider the following correctionst
Al i - corrections necessary because of the level, and Al v - corrections
necessary on apcount of\%Btar acceleration. The author describes the effect
of the daily aberration in determining--'a-s-tronomical coordinates by the
method of equal altitudes. The zenith distance error csk - 6z due to the
Card 1/3

84580
Consideration of the Effect of the Daily 8/006J60/000/010/002/008
Aberration in the Method of Equal Altitudes B012/BO54
effect of the Uily aberration can be determined from the triangle akol
(Fig. 1)t 6z 0".32 coo T sin A coo z (1). This is the error of the
calculated zenith distance z B due to the neglect of the efrect of the
daily aberration in Mazayev's method. The error 6z is of the same order of
magnitude as Al V. To take account of the effect of the daily aberration,
it is, therefore, necessary to add hl . 6z to the free terms in the
a
observational equations. Thus, the free terms of the observational
equations are obtained from formula Mt 1 - 10 + Ali + 41T + Al a + Alf'
With the aid of Fig. 2, the author describes a method of determining the
effect of 6z or; the coordinates of the neutral point to be determined.
For control, he made calculations taking account of the 6z corrections.
These calculations showed that a systematic difference of +08,015 exists
in the longit0les computed. It is pointed out ihat in deriving the final
longitude of the neutral point the mean longitude obtdttadC&.corrvcted by
the correction necessary because of the personal equation pf the
observer. It in shown that the effect of the daily aberration can be con-
sidered directly in the firtal calculationi of longitude by adding a
Card 2/3

84580
Consideration of the Effect of the Daily S10061601000101010021008
Aberration in the Method of Equal Altitudes B012/BO54
constant correction 6X to the approximate value 26 of the longitude. This
0
constant correation can be calculated from formula (5), and will have the
above-mentioned value of +0 -015* irrespective of the latitude. In
determining tho personal ec.uation at thet main longitudinal point, 61 is
coAtalned in tho personal e~,uation. Therefore, the personal equation is an
algebraic sum of the effective personal equation of the observer and the
correction 61 necessary beoause of the offect of the daily aberration. In
conclusion, it is stated that it is not necessary to introduce the
correction req,aired becaus-a of the daily aberration in the individual
results of the longitudinal determination, but that the same is considered
in the final derivation of the longitude by the correction necessary
because of the personal eq,aation. There are 2 figures.
Card 3/3

I . P.JAW~j VESEUVO WOO
-- --.. I ~ 1-7~~.'.-: - I
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VESEIaV,-YU. V.,j SIZEMVAO G. A.
,
Ron the opidemiology &ad clinic of Omsk hemorrbagic fever.2
report submitted at the 13-th All-Union Congress of HygJenists, Epidemiologists
and Infectionistss 1959.

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bp/RD/JKT/GD/JXT
Xt-66--~-699-5
ACC NRi
SOURCE CODE: UR/0000/66/ooo/000/0035/005.1
AUTHOR: Nefedor. Yu. A~ipimov B. V.- VA-selova., A. A,; Zaloguyev, S. N.,
Zhuravlov, V. V.; Iseyev L.'R.; Komarov, 177. N.; Kartacy, A. N.; 1- enko. G. T.;
Levinshiy, S. V~.
ORG: none
TITLE: The aerc-ion composition of the air of hermetic chambera-and its influence on
the human organism
SOURCE:--Kgkferentsiya po kosmicheskoy biolo ii i meditsine-.--19641 Materialy.
Moscow, Inst. medi16 !1
TOPIC TAGS: aeroionization, human physiology', life support system, space physiology
ABSTRACT: A number of previous studies have indicated that while aeroions are of
minor consequence, chronic exposure to them can lead to substantial changes in the
functional condition of the organism. To further study this factor, five experiments
of 20 days duration were conducted on 25 male volunteers from a laboratory (not
named). The firist experiment was for control purposes to obtain hygienic, chemical,
and,physiological data. The density of ions in this experiment ranged from
50-2000 pairs o:! ions/cm3- The second, third, and fourth experiments entailed
exposure to positive, negative, and bipolar ions generated by "Shteynbok" radioactive
ionizers. Ion concentration in the respiratory zone was 700-900 thousand ions/cm3
Card 1/8

L 45965-66
ACC NRI AT6030695
CU-:O. 9
2000. ==ro - Heavy ions.
Light.;- Ions
Charge exchange
CU unipolarity
coefficient
CU-1.1
*A-coef fl
logo NO
NY
U j 4 4
1, 1 2 3 5 f 7 9
Fig. 1. Aerion composition during a 10-day experiment
L_qord 2&_

ACC NN AT603)695
Control I
Control II
Negative
Positive
Bipolar
de-ionization
070
AV 1 2 J 8 7 8 .9 /0 /1 12 /3 AS Is /I Af IS 20 1 5 10= D
ays
3-(tfPrq During Aftemr
'aa - * I
Fig. 2. Pulse dyn cs during -voxious experimental regimens

L
45965-66
ACC NR, 4TO19695
120
f f j
Control Negative - h-A Positive lonsIBipolar lom Ddonization-
3. 'P-u1bi--Viriation.s. dur.i.ngbicycle ergometer tests
4

L 45965-66
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170
fir
ISO
140 .

120 -.

1,70 Qj
T3 Ij

~g
-
No)
0
55 'OvI3 5 f 3 f re/3 .7,/j
3 5 /3 j P
Control -NegitAve loric, Ttaitive.Ionh Xpdbijor,61- Dedonizatioirl
Fig 4. Changes in systolic pressure during
exercise on a bicycle ergometer (mean values)

L 45965-66
ACC NR, AT60306515
K-Control
Fig.5. Comparative characteristics
-0 neural
Go
+ processes in various experimental
regimens control)
a - Character of reactivity curves;
b - changes in the coefficient of
reactivity to light (yhiVe) and to
% opening the-~ies '(stripA).
,b)
40,
29.
-14
6/8

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ACC NRI AT6030( 5
150
;/4,17
130
0
/Z6
10
1 80
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Cont
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-

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1 %
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2

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! S
'# 6*18 3 f /I is ZO 3 7 o f J 0/4-3 7d

e
Pef6r efo: ~efdre

Aft'er, Before

A t
iefore
After-
qs~
Fig. 6. Changes in the sensitivity of central (E
and peripheral (L3) components of the visual anayozer
(mean values): 1 - EO; 2 - L3
[Card 7/8

L 45965-66
ACC NR. AT
during experimi?ntation. Allowing that the natural exposure dose for the lungs is
12-87 mrem/week (Givinteev, 1960), it was calculated that I g of lung receives
0.33-1010 pairs of ions pbr day. If, in the respirato medium, there were 500
3 -1
pairs of light ions/cm and 5000 pairs of heavy ions/cm , then 0.7-1010 light and
7-1010 heavy pairs of ions would reach the lungs of a man during a day. In these
experiments, the average subject received ivpproximately 1011 pairs of light ions
per day. In the fifth experiment, the chfanber was de-ionized using a system of
filters and srecial ion traps. However, complete de-ionization could not be
achieved and the density was 50-60 pairs of ions/cm3. Some results of these
experiments are shown in Figs. 1-6. The results of the experiment generally showed
increased muscular working capacity, external respiration, and an incre&sed level
of gas exchange during exercise in the experiment with negative aeroionization.
Partial norma:,ization of some indices occurred during the respiration of negative
aeroions. Holrever, fcr a number of indices, a noizalizing effect was also noted in
response to the respiration of positive and bipolar ions. Nonetheless, the general
-trend of the majority of shifts noted during experimentation lends credence to the
proposition that prolonged exposure to positive ions or a de-ionized air leads to
some changes Jeleterious to human health. It is possible thataneflvdle approach to
this problem 'would be to combine negative ions with positive or bipolar ions. The
establishment of optimum aeroion regimens requires additional research. Orig. art.
has: 7 figures. [CD]
SUB CODE: 06/ SUBM DAM 14Apr66/ oRiG REF: On/ ATD PRESS: 5o86
8/8 as

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LEBEDEVI K.P,;- *4ELOVA, A.I.; IEFIMOVA, M.N.
Foundry and technological properties of INMtoZhA 62-1-2-1-1 allope
Lit, proizve no, 4:40-41 p 610 (MMA 14:4)

4 T~-Tq
YE~F-
LZMIZV, K.P., kand.tekhn.nauk; VIKHOREVA. T.N., inzh.; V3CS1WVA, A.I.,
inzh.
Improved technology of casting brass propellers. I&t.proizv.
no.8:7-10 Ag 157, (MIRk 10:10)
(Brass founding)
(Pror,-llers)

rMCI A T 1-j',;-!!l
"ES 61 VIA, A.
Utilization of chips :.rcm norforrous allrys. Lit. proizv. ':o. 2, ISI,'~3.
;onthlv Listof RIISSiRn Acces2ions, Library of C~mgress
June 1953. 137"CL,

- -- --l- - -, A
I I - - - ~
. VESELOVA 3, A. L ; MAY ZEL I p Ye, I.
Sodiwi silicate mixtures for copper alloy founding, Lit. proizv
no.6--34-36 Je 16 2. (Sand,, Fbwdrv) (Founding) (MIRA 1;:6)

VEMLOVA, A._14,
L-11, v2pel and fi, P', Pariyovskaya, "Orientation of Data on Disew:,r3s of
flemp,ff 2019moo VOICkn9j. no. 5, 1935, pp. 41,46 73.8 Z12
SO: Sira Si 90-53t1l"? Doc 1953

USSR / Plant 1heeases. Diseases of Cultivated Plants N-3
Abs. -Jour Bef Zhur - Biol..4 No 6., March 195T, Mi 22987
Author Jes1JQnj-A.JL-
Title The C%ief' Apple Diseases During Stor-age and Meir Early
Diagaosit.
Orig Pab Sb. rabot In-ta prikl. zool. i fitopatol., 1956, No 4., 136-146
Abstract A detalleid picture is presented of external apple diseases
in storage caused by different vectors: Monilla ruet gna
Pars., Wnicilliw glauc~m,, Botrytis cinereal oeos r' ym
gractige ram Berk., Sk ro skis malor-im Peck., Ehizopus ni LqCFM
Ehr. It is indicated that apples in storage are mostly
subject to infecti on by P. glauc=. Me results are presented
of the study of temperature influence on mycelium development
in fruit tissues and sporogeuo-lis formations of M. fructigTna.,,
B. cineziLa. P. Glaucum. Observat-lons showed the absence of ~h
spore fo.*.ming process of M. fructigena. B. cimerea~ Asper 11-as
and Muco:v at 52 % relative humidity. Also the relationship of
fruit stUrage to time of picking is ir-dicated.
Card 1/1

A ~636,lov'a tiElabora ion of Diagnostical Chiracterisluics for Identification
of Polyphagaus and Sp!icializzcd Sj-,ecie3 and for D~ter-minatir-ri of Form-,y of raz-ari=psl
Itovi Ilauchno-rssledoltatal-IsPI'l Rabot Vsanolunopo-Instituta Zaphchlty Pastanll za
1235 Goda, 1936, pp. 11.94-496. 423.92 L541
00 gli~a Sl 90 53, '15 Doe 1953

VIISMTAO A.P. (Vyborg)
Technic of treating rubber gloves In diffpanoary practice. Ned.sestra
18 no.12:42 159. (MIRA 13-3)
(SURGICAL INSTRUMINTS AIM APPARATUS--STXRILIZATION)

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