76-10-11/34
AUTHORSe
Antipinap T.V., Isayev, OsV.
TIT13i
The
Effect of the Composition of the Alumosilicate Catalysts
on the
Hydration of Diethyl Ether and Dehydration of Ethyl Al-
cohol
(Vliyaniye sostava alyumosilikatnykh katalizatorovx& re-
aktaii
Gidratatsii dietilovogo efira i dogidratataii etildvogo
Gpirta)
PERIODICALt
Zhurnal Fixioheakoy Xhimii, 19571 Vol- 31, Nr 10,
pp.2245-2252
(USSR)
ABSTRACTs
The dependence of the reaction
volocitie3 in the case of the
hydration of the diethyl other
and of the dehydration of the
ethyl alcohol on the
concentration of OH-groupa at the surface
of an alumosilicate
catalyst and on aluminum oxide wag investi-
gated here. The
kinetics of the hydration of other and of the
dehydration of
ethyl alcohol at alumodlicates of different com-
position and
at types treated with lye solution was investi-
gated at 400OC-
It is shown that the degree of the transformatkin
from other
into ethylene is lower in the cage of the ether-hyd-
ration-reaction by ev 1/3 than that of the transformation of
Card 1/2
alcohol into ethylene in the dehydration of the
alcohol. It was
76-10-11/34
The Zffect of the Composition of the Alumosilicate Catalysts
on the Hydration
of Diethyl Ether and Dehydration of Ethyl Alcohol
ASSOCUTIONt
SUBMITTEDe
AVAILLBLIs
found that in the hydration of other the ethylene separation
does not increase considerably with the reduction of the alu-
minum oxide pereentage, whereas it decreases linearly in the
dehydration of alcohol. There are 13 figureat 2 tables, 7
Slavio
references.
Moscow State UniYersity Imeni M,Y9 Lomonosoy
(Mookoyakiy goeudaretyennyy uniyeraitet imeni M.V. Lomonosova)
July 11, 1956
Library of Congress
Card 2/2
5(2)
cr_r~8-2-26/35
AUT11ORi Antipina, T.V. -101;P1' I
TITLEs Catalytic Activity of Alumosilicates Tr4-ated With Lye
Solution.
Report III (Kataliticheakaya aktivnont' alyumosilikatoy,
obrabotannykh ahcholochlyu. Coobshchonlye 111)
PERIODICALt Vestnik Yoskovakego Untv-.-,titeta.S-r",',
matematiki- mckhanikip
astronomii) fitiki, Wimii, 19-%8' N~ 2,pp 197-20~ (U33R)
ABSTRAM In the preceding papers [Hof 112 jthe author ahowod
that the
alkali treatment of the alumooilicates leads to a utrong ae-
crease of the ethylene development in the dehydration of the
ethyl alcohol. Now she investigates whether this phenomenon
is connected with a diminution of the specific surface. By
measurings of the catalytic activity and of the ,%urfacoa it
is proved that the phenomenon can be only explained by a
chemical alteration of the surface. Some further questions in
this connection are discussed. A method of V.T. Bykov LRof 41
was used* The author thanks Professor K#V. Topohiyeva for the
interest in her present paper.
There are 7 figures, 1 table, and 5 Soviet references.
Card 1/2
1011
Catalytic Activity of Alumosilicates Treated With 0
/5r-r%6-2-26/35
.1 1
Lye Solution. Ropoit III
ASSOCIATIOV's Kafedra fizioheskoy khimil (Chair of Physical
Chemistry)
SUBMITTEDi May 14# 1957
Card 2/2
"I,
All TIT ~)J%S IntipintL,T.V. andNorkina,R.S. 0 OV/ 5~1-4- 25/ 31
'21 T LE t ~stfil-t' A'"ToO." Aatii W' V: c. 2tiall Feroortaga
lu
A
m inium ~,ride (Katal5tif~hoskaya 6ktL-.ro.~11 alpmosilikatov
malym protment.-qm
PERIODICALz Vestnik !.,oskov --koKk>
ki~LIIUS 1958, N'.r 4,
ABSTRACT: iw.*,~ntigated ~.hr -,)f lix difforent
12 1 a
t A, 0 content.
11. is lh:wn thtt .!,;! kinetit-i-] :,-' ~o:q&-ral 1-.r, t~yl
&L-toh,,! is
x1..,3 equatitn cf A.V.Frvr~ 71 t? t) ~-,ange of
the alt~ohol in ethylene is mout irtmuilre fv.- R 5A Al ?0
content
of the ~ntslyaer. Fc.~! a arao-kirL. rf a-umera the
v lataly-i activity
dearoaaeLl
con-.-;int. It ia stated that
tt,e ne. ~W) ei~,fr.^v) A~-C:jk tne ril! ~,i t:-3i io alraller
Card 1/1
catalyliz- ActiNllt.~- 's t W ", t r,
Small Purc-~-ntago cf
than fo~,. ;l :(~v ~7~ "ir- q-ihoi-i V..,rk
for 1!0!'
A! SO C I A 'I 1CN! -.it or Ij- t AA i I f K 1
',,,A t nly
SUBME."CEDI :ulf-t
Card 2/2
50)
AUTHORS: Antipina.- Avdonina, Ye. N. SOV/76-33-1-32/45
T1TLEt The Influence of Boron Fluoride on the Catalytic Activity of
Aluminum Oxide and Alumosilicates (Vliyaniye ftorietogo bora
na katalitichonkulyu nktivnon't' nHsi alynnintya i alyumo-
ai I tka tov)
PERIODICALt Zhu rn-a i
(Us:~,O
ABSTRAM The 'Influence of boron fluoride on heterof;eneouc
processes was
investigated leas often than that on h6mogeneous procesoca
(Ref 1). lt is known that DF 3 chemiaorbs irreversibly on Al 20
alumosilicate, and silica (;e] (Ref 4). The dehydration
kinetics of alcohol and the crackinp, of are examined on
samples of aluminum oxide (Jn,1uoLri;i1 A111)0 and
alumosilicate catalyzers (n mixtur.- I ( '6 and
Sio .(.,t-OC boron
2 (00)), which were treated with 1~t ~
fluoride was adsorbed on the catalyzer in the.reactor (in
connection with a vacuum plant). The kinetic examinations were
Card 1/3 carried out by a method already described (Ref 5). The
results
"o 1111,111olice of 1,01-on "'Noritle oil the
:;UV/'76-33-1-32/45
Activity of Alwiinw Oxide and Alunovilicates
obtv-4inod ~-oro elnborntod by uoin~-. th(.- equation by A.
V. Front
(,Iiof 6). i'lic zid;orptiozi of PA,3iiwrearjes the activity
of
Al 0 (;.,ig 0. n () with '-driorbed - +ow
2 3 1 2 3 ".3 , .3 an incronaed
reaction velocity (it' the -.iurl'ac- rewctioii, i.,,& the
proportional qunntity -%~ si,owu nn lnercrir,(? from. f-4 -
0.049
to 0-r~ - 0.070 (Fig 2). The activatioii of' Al 203 and
alumooilicate by BF 3 for the cattilyciu of the dehydration
kinetics of ethanol is thouj;ht ao being caused by the
formation of a labile surface compound which in decomposed
by the reaction products. The crack tecto of cumeno took
place
at a temperature of 4000C and during a poriod of 30 minutes.
In this case, too, a sudden activity rice of the catalyzer,
caused by a BF 3 treatment, is seen 4). Thin is
especially true of aluminumoxido.
Card 2/3
The Influence of Boron Fluoride on the SCV/76-33-1-32/45
Catalytic Activity of Aluminum Oxide and Alumosilicates
The activating effect of BF 3 on alunocilicates wan alco
observed by A. P. Ballod in the laboratory oV the
Academician A, V. Topchiyev (~n-t nefti A". SSS!)(Inntitute
of Petroleum, Academy of Sciences, U.;SR), (report on
scientific research work of the Inctituto for the year 1955).
in conclusion, gratitude is exprev-sed to 11rofessor
K. V~ Topchlyeva. There are 8 fiCuren and 6 soviet
A6SOCIATIONt Moskovakiy gosudarstvennyy univeraitet, in.
1-1. V. Lonolio!~Ova
(Moscow State University imeni M. V. Lomonosov)
SU1314IT I'LD: July 9, 1957
Card 3/3
S/195/60/001/003/013/013
B0021BO56
AUTHORS: Topchiyeva, K. V.,_Wjpj-naA__Z-_Y~, Li Khe-suyan'
TITLE. The Effect of the Structural Porosity of Catalysts on
Their
Activity and the Kinetic Parameters of the Course of the
Cracking Reaction
PERIODICAL: Kinetika i kataliz, 1960, Vol. 1P No. 3, PP 471 -
477
TEXT: The effect of the sizeof poreo of an alumino silicate
catalyst on
the crwking reaction of cumene between 350 and 5000C was
studied. A
catalyst of the following composition was used: 12% A120 3
and 88% SiO21
The various sizes of pores between 12 and 115 A were obtained
by re-
placing the intermicellar water to a different degree by
isobutyl alcohol.
Isoamyl alcohol or cumene. Moreover, an industrially produced
catalyst and
a catalyst of the type Gudri (Goodry?) were studied., The
structure of the
samples was calculated from the adsorption isotherm of
methanol vapor at
200C. The kinetic of the cracking reaction of cumene between
350 and 4750C
Card 1/2
The Effect of the Structural Porosity of
8/195/60/001/003/013/013
Catalysts on Their Activity and the Kinetic D002/B050
Patameters of the Course of the Cracking
Reaction . ~/
is described very well by the following equation by A~ V.
Frost;
V ln(1/1-y) - a 4. Pv y. v Is the volume rate of the addition
ol the'
initial m-iter a n mmoles7g~hj y is the degree of reaction; a
in the
apparent reaction rate constant in mmoles/g-hj 0 is a constant
equal to
unity. log a is a linear function of l/Tj the transition from
the kinetic
range to the diffusion range is manifested by a break of the
curve This
correspondd to a considerable chant;e of the activation enerey
There are
9 figures. 2 tables and 15 references.; 13 Soviet,
ASSOCIATION: Mookovskly gosudarstvennyy universitet (Moscow
State
University)
SUBMtTTED: March 23, 1960
Card 21"
3/109160/000/002/002/006/XX
B017/BO67
AUTHORS: Topdiiyeva, K. V., Antipina, T. V., and Khe-guyan' V
TITLE: Effect of the Pore Radius and Other Structural
Characteristics of Oxidic Catalysts on the Parameters of
the Course of Heterogeneous Catalyti~: Proceseps.
Communication 1. Productio! of Aluminum Silicate
Catalysts With Different Structural Characteristics
PERIODICAL: Vestnik Moskovskogo universiteta. Serlya 2,
khtmiya, 1960,
No. 2, pp. 13 - 21
TEXT: Aluminum silicate catelystalof equal chemical
composition but
different structural chaiacteristi a were produced in
experimental
series. The adsorption- and structural properties of the
catalysts were
studied in dependence on the degree of displacement of
Intermicellar
water by isobutyl alcohol and cumene. Intermicellar water
was displaced
by isobutyl, alcohol and oumene, in the apparatus shown In
Fig.l. Aluminum
silicate catalysts of the composition 12~ Al 203 and 88~ SiO
2 were
Card 1/3
Effect of the Pore Radius and Other
S/109/60/000/002/002/008/XX
Structural Characteristics of Oxidic B017/Bo67
Catalysts on the Parameters of the Course of Heterogeneous
Catalytic
Processes. Communication 1. Production of Aluminum Silicate
Catalysts
With Different Structural Characteristics
produced by the method of GrozNl,,rL (Groznyy Scientific
Research Institute).
The structural characteristics of aluminum silicate
catalysts are gl7v-en
in a Table. Two series of catalysts wore produced: 1) Series
with the
intermicellar water being displaced by butyl alcohol at 35,
51, 81, 95,
97, and 100%1 2) series with the intermicellar water being
displaced by
cumene at 34, 63, 90, and 96~. The adsorptive properties and
structural
characteristics of the catalysts produced were calculated
from the iso-
therms of adsorption of methyl alcohol vapor at 200C. Figs.
2 and 4
graphically show the adsorption Isotherms of methyl alcohol
vapor, the
distribution of pore volumes and pore radii, and the
dependence of the
structural characteristics on the degree of displacement of
water in
the catalysts of the first series. Figs. 5-7 show the same
Curves for
the*catalysts of the second series, in which water was
displaced by
cumene. It was observed that the chemical nature and
properties of the
organic solvents, which displace the water from the
catalysts, influ-
ence the structure of the catalysts. An aluminum silicate
catalyst with
Card 2/3
ARTIPINA, T.V.
Irfect of changes in the chemical nature of
on its catalytic activity. Vest. Hook un.
ji-Aa 6o.
L, lafedre. fishiahoskoy khimli Mookovskogo
I (Alumina)
the aluminum oxide surface
Ser, 2t Khim- 15 no.413-11
(MIRA 1319)
aniversitsta.
TOPCIIIYEVA, K.V.; AhVIIINAO T.V~; Ll KIIE-SULIN,; LEONTIYEV, Ye.A.
Formation of the porous atructuro of aluninosilicate catalysto
subjected to the action of surface-active agonts. Yin.i kat.
2 no.6:887-893 11-D 161. (MIRA 14:12)
1. Hookovskiy gosudar3tvonnyy univoroitet imoni M.V. Lomonosovap
kh W choskly fakulltot.
(Alum1noollicatoo)
(Surface-active agents)
I- AnIPIKAO T,V.-j- CIMHEDNIX, Ye,Mo (Moskva)
Surface chemical compounds of boron fluoride on &1umimm oxide am
their role in catalysis* Part 2, Zhur. fiz. khin. 35 no. 0836-
U1 AP 161. (MIRA 1415)
1. Moskovskiy gosudaretvannyy universitet,
(Boron fluoride) (Alumina) (Catalysis)
S/062/62/000/010/00 3/003
B144/BI86
AU NIORS: Nesmeyanov, A. N., Kritskaya, 1. 1., and Antipina, T.
V.
TITLE: Application of adsorption chromatoGraphy when working
with
ferrocene derivatives
PERIODICAL: Akademiya nauk SSSR. Izvestiy,%. Otdeleniye
khimicheskikh
nauk, no. 10, 1962, 1777 - 1703,
TEXT: The formation of keto groups on the central C atom was
observed when
chromatographinf, ferrocenes (P). More detailed studies were
made of this
phenomenon in aralkyl-PI, FICH 2Ar, and in ferrocenyl
carbinols, FICII(OH)R
(H being Ar, Alk), chromatographed on "chromatographic" AlI)O,
(FOC7 2962-54
U 0 ST 2, 9 6 2 - 5 4p 11 6. 7 - 7 1 It 2 0 3,~', by weibht)
and on and kOk (KSM)
xilica gal in air. The acidity of the adoorbento was determined
by It. A.
Benesils method (J. Amer. Chem. Soc- 78, 5490 (1956)). Al 20
3:aralkyl-Fl
yielded a distinct amount of keto derivatives; bonzyl-FI, for
example,
yielded -15'p" benzoyl-FI uftor 92 hre contact at room
temperature. Alkyl-FO
Card 1/3
S/062/62/000/010/003/003
Application of adsorptioneb. B144 B166
became oxidizad only in tritces, if at all. 4ith a contact time
of
120 - 200 hre, the ferroconyl aryl carbinola FICH(OH)C 611 50
F, ~'CIIOIOC 611 5) 29
and FICH(OH)CH3 yi elded respectively 92, 76.8, and 34)~-
Dehydration a.
~Iuo C in an N 2strean increased the catalytic activity of Al
20 3* The
degree of oxidation decreased.when Al 203 had boun exposed to
air or CO 2
for a considerable time, but reducing the contact tire of
FIC112 C 6115from
90 to 4 hre increased the FICOC 6H5 yield from 13 to 72,,. when
air or 02
wus blown throurh,.he adsorption column. There was no oxidation
when Al 0
2 3
was treated with alkali. 41hon Fe had not been separated from
310 2'
oxidation of alkyl and aralkyl-PI and of diferroconyl othanea
easily
occurred, forminj: forricinium cations of F1 derivatives with
electron-donor
cubstiltuents. Forrocanyl carbinols weru dieproportionated and
otherifiod.
This ruaction depended on the acidity of SiO54
1,11-di-(a-hydroxy benzyl)-F'
was not disproportionated, but yielded 5516 of the internal
ether besides
small ounts of F(COC6H5)2 and ferrocinium cations. Polyaryl
methyl
Card 2;F5
Application of adsorption...
S/062/62/000/010/003/003
B140186
carbinols yielded other under the same conditions. Benzhydrol
for example,
gave 41A of dibenzhydryl ether. The oxidations described are
important
especially for chromatographing small amounts. The conditions
and results
of 41 experiments are given in a table. Thera is i table.
ASSOCIATION: Institut elementoorgunichookikh soyodineniy
Akademji nauk
SSSR (Institute of Elemental Organic Compounds of the Academy
of Sciences USSR). Mo8kovakiy' gosudarstvonnyy universitet
im. M. V. Lomonoeova .(Moscow State University imeni M. V.
Lomonosov)
SUBMITTED: March 26, 1962
Card 3/3
NESMEYANLN, A.N.; KRITSKAYA, I.I.; ANTIPMA, T.V.
Use of adsorptica chromatogMhy In workAng with ferrocens
derivaUveso
Isve'AN =H*Otd*khim,,n&uk no.lOd777-1$
,#3 0 162. (NIRA 15tlO)
lo Institut elementoorganicheakikli soyedinsuiy AN SSR i
Moskovskiy
gosudarstvennyy universitat ime H.Y.Loozonosova*
Verrocene) (Chromatographic analysis)
V.A.; ANTIPINA, T*Ve
Kinstia of cumno cracking on aluminum oxide
activated with
boron fluorlde. Kin* i kat, 4 no+-595-600 Jl-Ag 163,
MRA 161l1)
1. Moskovskiy gosudarstvennyy universitet imeni
Lomom)sova, khi-
mich&skir fakulltst.
CHENNOV, V.A I ~NTIIIINA T.V.
Adsorption of benzene and mothsnol on fluorinm,*d
Fklum1wir. oxile,
Vest.?V)ok.un.Ser.2iKhlm. 20 no.3:23,17 MY-JP 065.
(MIRA 180)
1. Morkovskiy univoraltet, kftfodra fitichmskey WmIlI,
CHFMOV, V,A*j ANTIPIRA, T.Vs
Aluminum fluoride as a catalyst for cracking of
hydrocarbano.
Xine i kat, 6 nos 6al134-U15 N-D 165 (MIRA 19ti)
1. Moskovskiy goorALretvmnyy universitat imeni
Imononova,
khtmicheekly fakulftete Submitted December 19,
1964,
SWAYNTA. Te.S.; RtMU. T.M.; DMATKOTA, A.T.; DOLGAMIOY,T.I.,
starshiy
nauchn" notrudnik; ANTIPINA, T.I.; ROGOYBKATA, Ts.O., red.;
SlRalTV, A,V,,
[Agrooliantio referenoe book on Pskov Provinool Agroklinnti-
chaskii spravochnik po Pokovskoi oblasti. Leningrad,
Gidromateor,
lid-vot 1959. 138 P- (KIRA l3t2)
1. Leningrad. Oldromtoorologichookaya observatorlys. 2.
Nachallnik
sektore agrometprognosoy Severo-Upednogo upravlonlys gidromet-
lushby (for Deryatkova). 3. Institut geografii AN SSSR (for
Dolga-
:
hov).
(Pskov Provinoo-Crope and ollwte)
POPOVAr L.A.p insh.; ANTHIPA V I '; GIUMiOV, A.N. , starshiy
inzh.; PERSHINAv
M.P.t tekhn,; TMNIT414~9+-Aoq starnhly takhn.i ZARINApYe.S.;
TUULYA-
MSTSp KhJust inthsl XMIIA, L*A.t starehly insh.; KUZNETSOVq
I.V,O red,j
KYPRIp T.F"j red.1 SVITINAj A.A., red.; XOISEYEV, I.N.,
red.j FIAUM.M.Ye.9
tekbn, red:
I
[Hydrological yearbook Gidrologicheskil ezhogodnik.
lieningradv Gidroveteor.
iso-vo. 1957, Volel.lftsin of the Baltie Sea] Bassein
BaltUskogo,
moriao Nos*0-3. (Basins of the Oulf of Finland and the Oulf
of Riga from
the Russian-Finnish frontier to the northern watershed of
the Salaca
River] Basseiny Finokbgo i Rizhokogo zalivov ot
gosudarstvonnoi granitay
a Finliandi9i do severnogo vodorazdela r.Salatsa. Pod red.
I.V.Kuznetoova
i T.F.Sipro.-1961- 460 ' (MIRA 140)
(Baltio Sea region-HydFo-logy) (Kama Valley-Hydrology)
L 31810-66 E 4A" ( I
-/0
ACC NR. SOUkF~ CODS j U~ 6~~1661oj61603764~5-11
AUL1101i Blitnyuk, No Kai Kolomiyotal A, Fee, KvAoha, Za Nol
Lovokaya, Go Sol PF
Antipina-1- Ta~# '97
0"(',-. All-Union Scientific it -osoarch Institute of
Phyt9yathology (VaoaoyumVy
TITLI,t DiallWl phouj~iltos and
SOURC~-': Zhurnal obshchoy Idilmil, v. 36, no. 3, 1966, 475-)00
TOPTC 'AGS: orranic 1-4iot-,phorus compouivA, chortical reaction
kinetics, toxicity,
plant injiiry, ohartical :%)rnthosia, ester. Azootropic rLixturo
A'56T,', Nt' i'% It vas foui-A that dial',qrl phosphltnz- ary.1
nonoa31vlpho5p%:1nitqs are
pr'o~"Vicocl -In hi'711 yloiiis (al.Kmt quantitativo)
ImInly,,irlont of th.) torporAttiro
ot Which Atho reagents are mixod. and degree of removal of
hyxiroi-en chloride
fro--a Ui oreaction zone, by boiling the reaction mass,
cont.ninint, the reaction
prodticts of Alcohol,,% idth phosphorus trichlorldo or
dichlorophosphinos, An
astorification catalyst (such As sulfuric acid or
p-toluenostilronic acii),
and A Solvent. with atootropic distilIntion of --tor. A
preliminary ostimate
WAS nAde of the herbicidaVactivity or sone or the tqn compotuids
uynthosized. I
in the tosts the abovoground portion of the plants (the kidney
benn An rA
ty-dical dicot and the oat an A typical monocot) WAS sprayed with
mulsions of,
IUBOYO V.V.; ANTIPMA, TeJ.; CMIMMt, N.N.
Temperature dependence of the mWnetostriction of
certain ordering alloys* love vyea ucheb, sav; fit.
no.149,51 163, (MIA 1695)
1. Lqbyohevskiy Industriallayy institut imani
Kuybyphovao
(Hapatoatriction) (Alloys)
1
41
- --
--VOROBIYICV,--B.-L~-.-ANTIPINA,-Z.A.,-rodiiktb7r--,-Al=SANMo
v-, V.10, tekhnicheekly
redaktor -
(Transfer pictures (decalcomania)] Pereyodnys toobrathentia
(dekslikomanita). Moskva. Oos. Isd-vo "Iskusetwo,* 1952. 106
p.
[Microfilm] (KLRA 7tlO)
(Decalcomania)
NADZWIN, Th.; ANTIPOV. A.
% --womstim
Through the Island of Java. Tokrug eve%& no.8:25-32 Ag
053. (Iff-RA, 617)
(Jays,-Daeoriptlon and travel)
- ARPIPOV, A.,jDaster
We use dismountablo dumping trays. Stroltell
no.50-19 Ur '59.
(141RA 1218)
1. Torkhno-P~rshainakty sayod thelosobatenrqkh
konstruktaly I
dotaloy. Sver4lovskogo noynarkhoza,
(Loading oind unloading)
AIMPOV, A.0 genorAl-mayor aviatail
Laninist oontrol. in action. Takh. i vooruzh.
no.3:4-5 Mr '(~4.
Omlia 1,1:0
1. Zwootitell nachalItLika politichoskogo upravierdya
Wlcrusskogo
voyennogo okruga.
us is 0 a
10-1.0 0, 114-j -4-1
$-1- 8 1 - 0 as
let- 4"D 041 fools%
wa
bill
PAid 0 c 10
eaql Ail Seep" *Wlellp 91111 a" "A As".#
Iql 44!44 "Ulm (in (W PO MM III *M" Aq " %VI
0`1 a" 041 Ul 11 -qv= .41
a' "a 11%).114 0101 aRI P Wa "aawy at-al it so
'1 0101 M."M 464 POIS&AWO JO A"P"p in Paul
son gt=- M -1 P " 'I"- "P4-4
a 'am "11104 so "ISAM IM 049 1101116011 103uw 00
Zwll UVO 01 F"FWW P" r PUM 0 I"IM 01 to
so- 14w^" &MOO19.6 4141 P" RIPM 0114014WAP 80" W11
o. M 9g Io -on- 40111 Is (M) VM*0111HWIMN%l
~) Is 19111 P" wul" P *1114111" "1 " (a)
=%Xturfl p, 648 111$& OH311114
441 1" 1"&s .111M "Plao "I Olk"WIP, 190
M" 101cillmu v awil"ald A 00
q)
Mq $11 P" sow" "W=P, "W"M
so.
so.
to
066446
A.A,, Inzh.; WNW, V.G., kawl.teklin.niuk; MIESHCHENU),
A.F.,
kani.tokhn.nauk
Methods of calibrating propeller shafts. Sudostroanie 29
no.10s
64-66 0 163. (MIRA 1602)
r., :t: ruL
Y: r
yu ......
ANTIFOY, A.I., kandidat tekhalcheskikh nauk.
Xffect of lightweight passage@ on resistance to seepao In
foundation
eoile. Oldr.stroi. 25 no.9t48-51 0 156. (Km 9111)
(Hydraulio ongineariftg) (Boll mechanics)
SOV/98-r)9- I o- 10/20
10(i)
AUT11ORs v A.I. Candidate or Technical Scienre.4
WWUOMI
TITLEs The Selection of ft Itational Subterranean Contour for
Concrete Dams
on Sand Foundations
PERIODICALt Gi (trot ekhn i cheskoye atroitel'stvog 19599 Nr
10, pp .16-40 (USSR)
AJISTRACTs The article gives a brief account of a method
developed for the
cnIculation of subterranean contours or concrete
constructions;
this is normally a very complex question, but the inethod
detcrib-
ed here enables such problems as the weight of the
construction,
the coefficient of resistance to dislAncemont, coefficient
(if ero-
sion, filtration pressureq pressure on the rrest of the
spillway,
cost, etc.9 to be solved simultaneously. Tit? filtration
count?r--
pressure V . 0)
where p1. 61-2-3 is the area of the provisional lay~out of the
counterpressure in the form of a trianglej is the volumetric
weight or the water, Oe is the coefficient perrection or the
filtration counterpressure lay-out (taken to be 1.50). The
rela-
Card 1/4 tion between V and Lite size of the subterranean
contour is expres-
SOy/98-59-10-10/20
The Selection or n Rational Subterranenu Contour for Concrete
Dams on Sand Foun-
dations
sed thust nl1(1 + 0) S 1.5 (2)
where 11 ic the pressure on the buildingt I in the length of
the
comtilever, B is the width of the dam, and n is the ordinate
of
filtration counterpressure directly behind the channel. The
coef-
ficient of the dam's safe resistance to diRplacement in
determined
according to the formula K W tG - W - W1 f, (3)
C 1; N
where EG in the sum of the forces acting downwards( W in the
sus-
pending forcef EN is the sum of the moving forces htrizontal),
and f Is the coefficient of erosion of the concrete in the
founda-
tion. The depth of impervious deposits (T) should not be less
than
that dictnted by the formula S f 4 0.4 when 1 >/ 3, where S
in the
length of the channel and b in half the breadth of the dam
baset
Including the front part. By using Professor Ye.A. Zamarin's
nomo-
Card 21/4 grnph, shown in fig.21 we find the length of the
channel S to be
SOV/98-59-10-10/20
The Selection of a Rational Subterranean Contour for Concrete
Damn on Sand Foun-
dation&
and the length of the front part of the dam to be L - b
n
blo S1 in the case of small-scale work the use of Professor
P.F.
Fillehakov's tables in recommended (Ref.5). From the compact
graph,
providing data concerning all the factors affecting the
subterra-
nean contour and their cost, the most suitable ce~bination may
be
chosen for all kinds of dame. Two sample calculations are
given in
the text# one with drainage, one without, and table 2 contains
ft
list of the pressures combining to form the quantity n and the.
formulae for their calculation. By inserting the value of the
act-
ing forces into formula (3), we find n to be
K
+K A +K A A V 'I( EN+N., (7)
2 3 4 5 0 7 - I - f
0.7511(l + D) 12
Card 3/4 The cost of the variations In given in table 3, while
fig.3 shows
SOV/98-39-10-10/20
The Selection A' it Rational Svibterrwienn Contour for
Concrete Dams on Sand Foun-
dntians
the combined graph for the different variations of the
dimensions
and cost. The conclusions drawn are that the method described
pro-
vides for greater rationalization and economy in all kinds of
dams,
but that In class I and 11 projects it should be supported by
more
careful calculations. There Ore 3 tables, .1 graphs, I
diagram, and
5 Soviet referencesio
Card 4/4
ANTIPOV, A.I., kand.tekhA.nauk
Determining basic dimensions of
ground profiles. Oidr.strol,
(Dams)
buttress dams with flat under-
30 no,7127-30 JI 160*
(MM 13:7)
ANTIFOY, A.M.
OW"
Conical vibrator sifter with production capacity of
15 cubic
motors per hour. late. I Isobr. predl. v stroi.
no,7026-29 153.
OloveO (Band) . (MLRA 7ilO)
wt
"
III If I fit
v '"p 41A.-Mill -
600cows &40
CA
APPARAIIIS FOR PIVRIFTIVO "3t2, VAPORS, AND
LIQIADS. P. go Irsahow *ad
A. K. Aajjpvw* INese lI#TTO. Doe. 4.
1911. Coastruetton details
met
0*
00,1
0see
00
w
w
860
1, 9
00,
oo
0
9
~16
g
400
1
off
"
0
2
goo
&$o tt a 04tattwSatat Imefilwat ct6twFICAVOR
see
goo
-j~
u a " 0
goo
0 0
ANTIPOV; A.N.
Complications arising in deep drilling beyond the
Arctic Circle.
Neft,khoze 43 noo4t63-66 Ap 165. (MIRA 1814)
YIVCIRAFOVp Oeorgly Konstantinovichp prof*, doktor
tekh&,rAukj IOSIIZVSK11p
Ley lzralUvichp kand.takhassauk, dotoWl ALWANDROV, Anatour
Vasillyevich, k".tekhz.nauk.. dotsent; D6W;4Xj Nikoiq
NikoUqevioh, kwA.tokhn.n&uk# dotsent; I Up Genrikh
Mikhvqlovich, iazb.; CHIRKOVv Vladilon Favladch, Lush*
FrInimall uchastiyet RTBIWp V.,D.j Lash.; ANTIMT,
KMOFANOV, Yu.Mej, inzbo,, rateementl KARM~I--i',A,, inzh.v
rbd*l UMMO, L*A,p takhnoreds
of the reinforcement
[Prestressed bridge girders with stratOM
before the concrete is placed] 'no napriashemWe
balochrVe proletiWe stroenila mostov a napriasheniem armatury
do betoniroyaniia. Mookvap Vass.isdatellsko-polUT.obPedinonis
H-va putei ooobahcheniia, 1962, 282 p6 - (KtRA 15t4)
I* Daystvitel'My chlon Akademli stroltelletva i arkhitektur7
Sam (for Yovgrafov).
(Bridges, Concrete) (Prestressed concrete)
YEVGRAFOV, G.K., prof.1 ANTIPOV, A.S., inah.
oper'----~- --
Results of the ation o prestressed concrete bridges Put#
i put.khos. 7 no.1200-31 163. iMIRA 16t12)
KIIILlN5KlY, F.A.; LMSHFV, I.P.; LFbi;PMEU, 6.i~.;
SFAMil"OVA,
N.D.; DORIZO, A.F.; TEM-OVAYA, K.G.; AHMOV, A.S*j
obahchestv. rod.; MAK, Yu.M., toklin. red,
(Gorynchiy Klyuchl Gorlachli k1luche ltdo2,, 18pre i
dop. [By) F.A.KiAlinskli i dr. Krannodarsko
Krasnodarvkoe
knizhnoe izd-vo, 1963. 84 p. (MlHA l7t2)
1. Glavnyy vrach vanntoriya No.", hurorta Garyachly
K4uch)
Kavkaz (for Lobodenko). 2. 'Anntorly No.1 Kurortn
Goulxhly
Klyuch, Knvkuz (for
Sliavkwi(va#Tornov~)ytt).3#ZarastitalI glaviiugo
vracha po maditninakoy chastl sanatoriya No.,' hurorta
tioryachiy
Kly-uch, Kavkaz (for Dorizo).
IOSILWSKIT, L*I*, kandttekhnonauk, doteenti ANTIFOV, A.S.,
Inzh.
Results of testing reinforced boundles vith NXIIII& anchor
shoes for
pulsating loads. Trudy KIIT no#126t68-8) 160. (HIIU 13: 10)
(01rders-Testing)
ANTIPOV, A.P., otv.red,; XALAGMUKOV, Y.P., takha.red.
[Traffic regulations for care and pedestrians on
streets of
cities and communities, and on highways of Moscow
Province]
Pravila dvishemija transports i peshekhodov po uliteam
gorodov, naselemVkh puxktov i dorogam Momkovskoi
oblesti.
Koakvn, Izd-vo *Koskovskais provda," 1959. 94 p. (MIRA
12:10)
1. Moscow (Province). Otdal Gosaytoinspektaii i
bezopasnosti,
dvishanlys.
(Moscow Province--Traffic regulations)
CdAoi. ;11.,. 'tae I Ity Timof eyev ich ; AIC POV Androy
Yoe I lizemIch [ as :eased)
W3A40Y. Ifiktor Ivanovi-.h; ITM =-!!ent; 5U4-Vi~. TO.64.,
WVAW~PV., r4ioktor
JustalliM and servicinj se-uUhing and hackling devices
In flex
%t,d temp MLIIGI Ustroletvo i obolushivents
mial'no-tropolInykh t
~wjeleprirotovktollzWkh agragatow l1nosayodov I
oonlkozsv~uy.
4c,s'iya. Goo muahno-telchn.l.-A-vo H-va logkot
)rL-.;iydhl. ~;L-h. 1957.
.19 p.
(tiax (Tot t I 1-i i i -A ry)
SXXXMXNXO, N.A., doktor takha. "uIc: YURMY, V.N., insh.;
SIMLIKOVSKIT,
L.W., kand. tekhas nauk: ANTIPOT. A.Y., insh.
'Thermal calculation of boiler unitag(standard method).
Roviewed
by CA. Sessa4nka and othores Toploonergettko 5 no, 5:92-94 W
158.
(MIRA llt7)
I* Moskovskiy suargetichaskiy Institut,
(Boilers-Tablem, calculations. etc.)
ZANWIlt 79.1 ANTIFOV# B.1 XMSANOV, Sol KOLOKOLOVAq Hol M=j P.;
SWILINIMA, NWTOV, T. p takhn.rod.
(city or Orel) Oorod Orel. Orelp Orlovskoe knishnoe izd-vot
1958. 122 ps (KLU 1416)
(Orel-4seaription)
ANTIPOVO B.
The general plan of Omsk. N& stroi.Ros. 3 no.9tlS-19
S 162*
(MIM l5sl2)
1. Glay"y arkhitektor Ouka.
(Omsk-City planning)
ANTIAN, B. A.
Antlp~ 11. A IfInvestIFation of Um wit,!!r nai,no-tic.
Fell it oblata
;-M-PsAds of rotAtion arvJ slort. CY111;"iers in 'a,
-miforzdy
alternate fLeld," Trlidy Sib. fi:~.-tmWhn. in-ta) Issie
p. ~321-31
SU: U-521il, 17 Deco-nber (Leto;As 'Vim-nal ln~;kh
Staf'01~') ~O* '~~51 11,9101)
ANTIPOV, B.V.
Paeudomyxoma of the peritoneum. Trudy mol. nauch. notr.
MCNIKI
noell222-224 199 (MIRA 16oll)
1. Is pato-corfologicheakogo otdola (rukovoditel* prof.
S.D.
Vaynberg) Moakovakogo oblastnogo
nauebno-lealedovatollakogo
klinicheakogo inatitu+A imeni Vladimir8kogo,
AMTIPOVf B.A,; ZUYXV, Wee I. EUMILN=O. P.N#; SONCHIXg
T.Ke; YZMSHIN.
'~'- - T.A.
2ransparenoy of a horizontal atmospheric layer In the
range from
0.7 to 14 . Part lt Squipment ard measurement methods*
Ivy.
Yy%.ucheb.say,;fIs& no.2t103-110 1609 (HIMA 13t8)
1. Sibirskly fisiko-takhniohaskiy institut pri Tomakom
gosuniversitste
In. V*V.11uybyvh*Ya.
(Atmosphere--Optical properties)
82331
(3.9000 s/i5q/6o/ooo/oVoll/05
3/
AUTHORSt Antilov, B.A.1 ZuYev. VJV , faaasnenko, E.F.,
Sonchik,--.
Y ana- 1Fe3yuskqn_,_"6
TITLE: Transparency of the Horizontal Layer of the Atmosphere
\Vin the Range or M.7-14 u. Part Lle Dependence of the
Total Transparency of the Atmosphere in the Range
0-7-14 0 on the Thickness of the Precipitated Layer of
Water
PERIODICAL: Izvestiya vysshikh uchebnykh zavedoniy, Fizika,
1960, Nr 3, pp 72 - 75 (USSR)
ABSTRACTt The authors made an attempt to determine an
empirical
relation between the magnitude of the reduced signal V
(magnitude of the signal multiplied by a factor
42 /Sj:- Li being the distance between the emitter and
the receivor, Sj heing the area of the emitter)
and the air humidity which would show satisfactory
agreement with experimental results obtained by the
authors. As sources of infra-red radiation, four
special emitters were used which were heated to 500 OC14",
and placed at a distance of 1210, 3494, 6645 and 9855 m
Cardl/4 from the receiving equipment. The experimental set-up,
82331
S/139/60/000/03/011/045
Transparency of the Horizontal Layer ofEM/11MI04sphere in the
Range
of 0.7-14 p. Part 11. Dependence of the Total Transparency of
the Atmosphere in tits Range 0.7-14 p on the Thickness of the
Precipitated Layer of Water
tits method of carrying out the experiments and the
processing of the results were the same as those
described in an earlier communication (same journal,
No 2, pp 105-110). The air humidity and the intensity
of the signals were determined simultaneously. The
partial pressure of water vapours was determined directly
and then the thickness of the precipitated water layer
wL was calculated, where w - the thickness of the
precipitated layer of water in mm for I km and L - the
distance in km between the emitter and a receiver.
For detecting the relation between the air humidity
and the magnitude of the signal only those measurements
were taken into consideration which were carried out
in the absence of any visible clouding of the atmosphere
(mint, haze, fog, rain).Cra total of 811 determinations
~6nly 140 complied with this condition. The experiments
Card2/4 were carried out during various days in March, April,
4-'*
- - 6-2-33131 -- - - - - - -- - - - - - -
S/139/60/000/03/011/045
Transparency or the Horizontal Layer ofEM/fUlosphere in the Range
of 0.7-14 ji. Part 11. Dependence of the Total Transparency of
the Atmosphere in the Range 0.7-14 'o on the Thickness of the
Precipitation Layer of Water
July, August, September, October and November, 1958
and encompassed a wide range of variation of air humidity;
the value of w varied between 0.7 and 17 mm/km and
the wL values varied between 0.8 and 167 mm. It was
found that the magnitude of the reduced signal V is
not a linear function of *4WL-7' (see plot, Figure 1)
but it appears that the dependence can be better
expressed by a linear dependence of Ig V an V -WL
The following empirical relation was derived by the
authors for the reduced signal V
V a VO e - b ~fw-L (2)
whereby V. is the magnitude of the reduced signal
in the absence of water vapours in the air, b is a
constant equalling in the given case 0.2319. Curves
calculated according to this equation are in good
Cand3/4
1, f ~' ~ -
S/169/62/000/008/032/090
82-02VE392
AUTI'O*.13: Ant ipo I
Zuyov, V.Yo. , 'AZohhanen!~o, P.N. ,
S iTi i1z, It. and Fedyushin, A.A.
TITLE: and cortain results of studies or korizontal
tr.inn )aroncy of the ati-iusphere' to long-wave
raklia~ioll
M.11OD1CAL: ;lefurativnyy z)iurnal, Gpofizilha, 110. 19Gz' 31,
"butract 0132.32- M, tho
sfarn. optilca' (Actinom, otry and atmosplieric o tics),
Lanin~;rad, Gidromoteoizdat, 1961, 2-48 - 251)
Tl~;--,r: The effect of t-nateorolo-icai conditions ol, the
tranu-
.)nrency I' Cie atmosphare to 1011'~;- ave radiation (0-7 - 14
over of 1.2, 3.5, 6.6 and 9.9 ]an was studied. n't
notallic radicktors with alactrical heatinU were used a,4 -~ok
re
cc;
of raLUation. A vacuum thermo-ale;aent with a vibro-converter
a ;~c~kstiriw- aniplifier 23AM
na' 0 (231,M) served as a receiver.
A4c rocciv(~r was anced it, tiie rocus or a parabolic rairror.
3i::-ulta;-,eoualy ..*it*,i tho inoasure;aents at .111 four
poitits Ule
ciateorolo~;ical conditions wore also :-aensurod, ViZ.
tem.;)erature (f
Card 1/2
s1 169/6 2/ooo/oo%04/03 2/ogo
Metaod.,~ and cortain results .... E2oL,/El-)9-,,
the zli;-, :mllidit", wind and intollnity of -)I-Cci:dtatC- T% e
retjtlltz-~ "; Cle in Lae for..% %)A~
radiatiua curves vs. (Ustance. The seasonal relation wit:%
attelluntioll wlicA coillcidC3 with talc Periou or lli-%Ont
absolki'le 11111-aidity wall f0tuid. A m'.mrp attenuatioji of
ro(liation
was obaerved u,) to 3.5 lua durin-t- the winter period, tLicii it
decrcasm*., while the auia--.-.cr period a sharp attenuatioil
was observod up to 665 Ian -
Abstracter's noto: Co.-aploto translntion.-,
89693
S/139/61/000/001/001/018
E032/414
AUTHORSt ---Antipov B,A,, Zuyev, V.Ye., Kakhanenko, P.N.,
Sonchik! VA, and Fedyushin, A.A.
TITLE., Transparency of the Horizontal Layer of the Atmosphere
in the Region 0.7 to 14-0- 111. Dependence of the
Total Transmission of the Atmosphere in the Region
0.7 to 14), on the Thickness of the Precipitated Layer
of Water
PERIODICAL: Izvestiya vy9shikh uchobnykh zavedeniy, Fizika,
1961, No.1, pp.17-19
TEXTz In previous papers (Refs.1 and 2) the present authors
described an apparatus and a method of measurement of the
transparency of the atmospheric layer next to the earth surface
in
the region 0.7 to 14 0 and for distances between 1.21 and 9.86
km
The experimental material obtained was also reported. In the
present paper additional data recently obtained are reported.
As an approximation, the magnitude of the transmitted signal was
described in Ref.2 by the exponential law
V a vos -a -44' -L (I)
Card 1/4
89693
S/139/61/000/ool/ooi/olB
Transparency of the Horizontal ... E032/9414
where w in the thickness of the precipitated water in mm per km,
L in the distance traversed by the radiation in km, a in a
constant and. V, is the intensity in the absence of the absorbing
medium. Eq (I was obtained empirically and gave a sufficiently
good representation of the experimental results. This expression
accounts for the absorption of the infrared radiation by water
vapour only and does not take into account absorption by carbon
dioxide or effects due to atmospheric turbidity. The criterion
for the applicability of Eq.(l) is the linear dependence between
1S v and AqwL. The now data now reported are also well
represented by Sq.(l) right up to wL a 90 mm. However,12P
greater values of wL, the dependence between lg v and VW-L is no
longer linear and in order to describe all the experimental data
the following formula was employed
V = c + k
1 + wL
(2)
where c and k are constants. This expression is also purely
empirical and the criterion for its applicability is a linear
Card 2/4
89693
S/139/61/000/001/001/018
Transparency or the Horizontal ... E032/z414
relation between v a~d (1 + wL)-l. Vig.2 shows the dependence
or v on wL. During the measurements the sensitivity or the
receiving apparatus was controlled by a 6 watt lamp at a distance
of 5 M from the detector, It was found that the signal due to
the lamp was very.dep*ndent on the humidity or the air. It is
therefore pointed out that the use of a standard'source at a short
distance from the receiver may introduce errors unless
%corrections for the humidity are introduced. There are 2 figures
Aand 2 Soviet references.
ASSOCIATIONt Sibirskiy fiziko-tokhnicheakiy institut pri Tomskom
gosuniversitete imeni V.V.Kuybysheva
(Siberian Physicotechnical Institute of the Tomsk
State University imeni V.V.Kuybyshev)
.ISUBMITTEDs' February 13, 1960
Card 3/4
89693
S/139/61/000/001/001/018
Transparency of the Horizontal ... E032/E414
0
. v
Jv
- - 0
Fig.2.
a
.N
0
0
m
Card 4/4
- W1
Pme. I
.',3 v /FC C / -;'.-.C i - If G
1, ','7,R A15( 111 UTR, C-3 2 14
A V Y Kii
Y'.
TTTI.F: ';-IV A ppar a I. US for m~-a our i )g a tmospher I c
t ranip.ir cncy in the ~nitaz eki re-
-c fo r V,
r ,v r, -I n, f
pi-
"ll 0 f,1
n i r a i od r ad int i or s ozin or opt. r a t ing with n i i
or t ured co the,
mmodnlijclon ficy,wi ev of Itho radi; t ion source . 7he c,",
o, ho aarruv-hand am-
COffj ~43
ACCESSION NR: ATUIL1177
;)l if I C., can be cormccted to an e I --c t r,iv- ic
co~nriit.,r imln,,., the circult of the WS-2
3evel"Pe" t,,r a n,i i oT,o); ph o r i c
ve r - - s w,i t
u z a
I z lko i khn i clh- ft-*~ z I -Ij pr i T,,-rn ikon gosudar s
tvenu)u.-
7 , c. ik S T a t v 1 niv --i r t
sTal-IT rE,); 2 5 N ov 1 -4
NO REF SOV: 000 OTI I ER: 000
cnrd 2/3
Ti.: .' N.V., 'n'~ .
x,tkini- firl.(A structures of 1,1116A woolle ;'
v.6 i ~ ~ I , - ' " ' - - '
P-14 tp 104. , ~l I ;' , :' . -) ~
A17-11POVo B*V*
Pathomorphological examination of the Hdry* arreated
beart under
conditions of experimental artificial circulation.
Arkho pat. 22
no. 6t67-72 160. (VIIRA 14il)
(PERFUSTON MW (HEMT))
1 1, - .
ANmov.-ILY.i GALTkIERIN, Yu.M.; Yr"WWOVA, 1:J1.;
P.1U~;TGRONIN, S.Aj
SM1RJ;OV8 YO.Ye.
Restoration of cardiac activity aftor prolonged arrest and
anemia
of the heart in a surgically prepared experiments Vast,
khir. 85
no. 7:9-17 Je 160, (MIRA 14i1)
(HEART FAILURE)
ANTIPOvf B. V.; GAWPERIN, Yu. M. (Moskva, ul.
Vorovakogo, d. 26, kv. 14)
Use of direct cardiac imemage for artificial blood
circulation
(experlmental-morphological data). Grud. kh1r.
no.5152-58 '61.
(MIRA 15:2)
1. Is nauchno-ekMmrimentallnogo t patomorfologichookogo
oldela,
(say. - prof. S. B. Vaynberg) Moskovskogo oblartnogo
nauchno-
isoledovatelIekogo klinicheekogo Inatituta imeni M. F.
Vladimirskogo (dirt - saslushenM vrach RSFSR P. M.
Leonenko)
(tMART1 FAILURE) (RESUSCITATION)
.,ANTIPOV, B.V.; GALIM-RIN, Yu.M.; Y-.;P,',:AKOVA,
N.M.; PEMIZ ToliGN Il;, s.A.;
SHM1OV, Ye.ye.
i;ffOct Of Cw-dIOP109ic subetances " artificial blood
circulation rol,-inos on tho routoration of hoart
activity
after prolonged tuiemia. Grud. kh1r. 2 no.4:106-113
JI-Ag
160. (MIZA 15:6)
1. Adres avtorov: 111-loakvu, 3-7a Vioalliclum3kaya,
d*61/2p
Moskovskiy oblantnoy nauchno-isslodovatallikily
)d1nicheskiy
institut inoni M.F. VladimtrskoGo.
. (UMID-ClUGULATIOU, AFTIFICIALN
(MWIT FAILURE) (CAMIAC RESUSCITATION) (CMI0V&;CUIAR.
AGEIMS)
VA)N-BFJIGP SOB* [deceased]; YUDINp Yu*091 ANTIPOVt B.V.
e`"~
Leukemold reactions in tumor-like, diveaves. o klin Pate
no.2t257.-262 t6l MIRA 6tl2)
1. Is paU logamorfologichookog;o otdola (save - prof* SOB*
Vaynberg [decessed)) Moskovskogo oblastnogo nauchno-lealodo-
vatellskogo kEmiaheskogo, inatit-dta. ineni Vladimirskogo.
h
, I
'N"ROV, 13.1%; N.M. (Moskva)
Interrelations of local and general factors in the
pathogenesis
of a dynamic obstruction of the Intestines In
peritonitis. Ar)di.
pat. 27 no.304-60 165. (KIRA 18:5)
1. Nauchno-looledovatellekly Inatitut morfologil
choloveka (dir. -
chlen-korrespondont AM SSSR prof. A.P. Avtsyn) ON
SSSR I 14oskov-
skiy oblastnoy rutuchno-lasledovatellskiy
klinIcheskiy institut
Iment Vladimirskogo (dir. P.H. TAonenko).
I I f
164,
v n
~/ 01- . (I
A,NTIPCVI , 3.A. HAI0KVj laul P.A. KWAM.
Girookopichaskis aviatsionnyis pribory, Moskma,, 19/,0,
Title tr.t Gyroscopic aircraft instruments.
Nor
0
SOs Aeronautical Sciences and Aviation in the Soviet
Union, Library of
Congress, 1955
ANTIPOT, 0.1.
-Bitumens In traps of the Siberian Platform. Boy. geol.
n0.61:144-146
157. (XIM 11W
1. Ikepeditsiya Ministerstys, geologii I okhrarW nedr, g.
Rudnogorsk.
(Siberian Platform-4itumen)
AUTHbRi Antipov, G.I.
TITLE: Prospocting Characteristil.,-s c" Iron Ore
Argara-Ilim Region (Poiskovy~e prizziaki
mostorozhieniy v Ingaro.-Ilimskom reyonp)
PERIODICALi Razvedka i okhrana nodr, 1958, ':r 7, PP
7 -
Depcsitq 1r the
-zhq1ezroru3nykh
1-4 (1L!,1,3R)
ABSTRAM The author describes various characteriattos which
could
help to locale more iron ore deposits In the Angara-Ilim
re-
gion. This region, atill Insufficiently explored, has only
2 Iron ore depoitte which could be of commercial
Importance,
There are indicationa that more iron ore depogito can be
found. In the last century, geologists discovered the con-
nection of deposits with tectonic breaks and their location
ovar the trappean intrusions, At n later date, other geo-
logists (B.N. Artewyev, S,A. Doktorovich-Grebnitakly) con-
firmed those findinge, -the author claegiflies these
charac-
terintica in separate groupst 1) lithologic-stratigraphic,
characteristics - alfrost all depositi of the region are
cor-
nocteA with tuff breccia, Those fcrmationa are of pyro-
clastic origin and, in contact with the ore bodips, they
be-
camo skarnnd; 2) structural-tectonic charactoris%ice - all
Card 112 knowr are deposits are located on large fields
formed by
Prospecting Characteristics of Iron Ore Depopits 'In the
Argara-llim Pegion.
uniform mar!-argilscoous formations anti tire ipposited lkrri-
zontally. In thi inmedints vicinity of the ore deposits
these formations %r9 3lightly dislocated and broken Into
separats blo:ks. The complicated structure of these hori-
zontal layera indicates the poseibility of ore depositst
mineralogle chareotorInttca - encloo-_~rg rocks are trana-
formod into skarna in contact. with the ore bod%,. The larp-
or the body, the larppr thf~ skarned surroundingst 4) geo-
morphologic charecter'.!3tic% - tht Anga7s-llim region is an
ancient plateau cut by large rivers, so that trap and mag-
netite ore bodies alone form protruding bald mountains
which must be studied carefully in cases whore theoe ore
depobits are covered by a layer of alluvial sediments, they
still form bed-like ,rotrAi4ione, wiich can be discovered in
early spring or auttimn after ',he leaves have been she4.
There are 6 Soviet references
AZZ"CIATMI.- Vinisterstvo geologii I ckhrany notIr SSSR
(11.1ristry of Geo-
loey and Conservati on of !.An~~:!i.'. lie ^,urcas of the
USUR)t
I. Geology--USSR ~. Geopilysival Prcv;j;,~Ctln~ D.
4. Iron orn,,~.-.-Econo-rde aspects
Card 712
AVT1"V. 0.1.; IVASHCHRWO. N.A. (deceased]:
XORABZLINIXOYA, T.T,,*
16~_TUINv
M#Xo, dotsont; X=XT5OT# G.A., dotsent; PIKARIN,
P.M.; ROSUANOT, O.T.. dotsent; W%WOV, L.G.; CHEWIM51r,
G.D., red*; TXALICH# S.Map red.; XMIN, B.S.,
red.ind-va;
GUROTA, O.A., takhn6red.
[Angers-Ilin Iron ore deposits of trap formation In
the southern
Siberion Platform] Angaro.-Illmskie sholexorudnys
mestoroshdonita
trappovol formtsil iushnoi chasti Sibirskoi platformy.
Koskya,
Gos.nauchno-takhn.lid-vo 11t-ry po geol. I okhrane
nedr, 1960.
R3 P. (MIRA 13:10)
1. Russia (1923- U.S.S.Ro) Ministerstyo geologil I
okhrany nedr.
2. Geologi Irkutskogo geologicheakogo uprnvlonlya (for
Antipove
Iveshelonko, Korabelinikova, Pekarin, Strakhov). 3.
Irkutskiy
gornometallurgichaskiy Institut (for Kosyt;in,
Roolyukov). 4. Ir-
kutskiy gotudaretyannyy universitat (for Kutnotsov).
5. Glayn"
insh. Irkutskogo goologichaskogo upravleniya (for
Tkalich),
(Angers-Ilim, region--Iron ores)
AN?IPOT, 1.
- ,-,
Device on a cardignu-stitch knitting machine for
reducing yarn,
Prom.koop. uoel2t24 D 156o (XLRA IW)
1, Direktor fabriki no.22.
(Knitting machines--Attachments)
AIITIPOVj 1.
On the threshold of 1962. MeBt.prom.i khud.promyo. 2
no.1:14-16
Ja 161. (MIRL 1414)
1. Direktor Hookovskoy shveyno-galantereynoy fnbriki
Vo. 2.
(Moscow-Clothing industry)
M~
LLDSHS. Georgly Vladialrovich; C.IMNTSHRY. V.L.
re4aktor; BOBURO , Te.56, takhnichoskiy redaktor
[A production and financial plan for long hauls by railroads]
Proievodstvanno-finansov7t. plan distantell putt# Moskya, Gose transpe
thel-dor* iad-yo, 1956, 47 P (KLRI 100)
(Ps ilroads-Kanagems N)
)dvT-IP,0Y,1*A*.
Operation costs should be reduced. Putt i put. khoz.
no.4:31-3,1
Ap 159. (MIRA 13:3)
(Railroade-Cost of operation)
7R-IT,.V,-F
APTUPOV, I.A., insh.
All divisions can and nut be profitable. Put' put.khoz. 4
no.2:3-5 7 160, (HIRA 1):5)
(PAI Iroads- News went )
AKMVP I.A.1 inshe
Constantly imroase the labor productivity,, Put' i
putkhose 7 noel&
10-11 163 * (HIPA 160)
(Ra.UroadA-IAbor productivity)
ANTIPOV, I,A,s inzhe
Now devolopenonts in tho detorminat,lon of labor
productivity. Put,
i put.khoz. 8 no.301-32 16/to OMRA 17%3)
1
Al,'T I I OV, 1vun Azitipovich; HADKIIIII,
Alekastidr HodionovIch; SOAKA,
XAM11 Grigorlyovich; I '-L'~KOVA, Lots'., red,
F
(D.-oriordes, organization and plunning of
ruilroad tra,,-k
aL,onotq) Flonomika) organitataila I
plunlrovanle putevego
khozininstva. Monkvrip Transport, 1964. 2~6 1~.
(VUBA 17:9)
ANTIPOV# L9A*j lnth,l LEZHEPEKOV, B.S., inth.1
STAVTSRV, B.N., irsh.
Stleation of parameters for working unitts of a
motor grader.
Strol. i dor. mash. 8 not-12t4-5 D163 (14IRA 170)
SAGATOVSKIY, V.N.1 Ah"rIPOVI, 1.0. (Tmsk)
Correlation of the concepts *cause.* condition,* Ostiologyg
and Opatbogenesis." Vest. AMN SSM 21 no.104-40 166.
(HVU 1911)
"~-,PVIYKV, P.Yo.-O. VTIPOVP
I.K.
Change in the group composition of humus or gray and
light-gray
forest soll.3 unler the influenco of cultivation.
Nanch. doV-1. vys.
shkoly; biol. nriuki no.1089-1,93 164. (MIRA 17t4)
1. Hekowndovnna kafedroy pcx!hvnvrA--nty1t Wskovikogo
gowidarstver-
nogo 11hiversitotrk im. M.Mnnonosova.
KUROCIIKINO V.M.; ANTIPOVO lAt otv,,;*d.; ORWVAt I.A.0
red.; KORKINA, A.I.;,
takhn6r*d*
(Standard UNSM-2 programs of the Computer Center of the
Academy of
Sciences of the U.S.S.P41 Standartnye programV BBSM-2
Vychislitelf-
nogo tsentra AN SSSR, Moskva, Vychislitellnyi tsentr AN
SWR,, 1963,
11 P. (Akademiia nauk SSSR. Vychislitallnyi tsentr,
Standar" I
tipovye programmy BESM-2, no*6)o (MlRA 160)
ANTIPOV, I.N.; PODrERYUGIN, V.D., otv.fed.; ORLOVA,
I.A., red.
(Use of gimpson's method in solving a definite
integral] Vychislanie
oprodelannogo integrale. metodam Simpson&. Moskva,
Vychislitelinyl
tsentr AN S-SSRO 1964. 9 p. (Akadsaiia nauk SSSR.
Vychislitellnyi
tsentr. Standartnya I tipovye programmy BESM-2, no.9).
(KRA 17W
BORISOVA, E,P,l ANTIPOV,.J.P., otv.red.
(Subprogram of the iteration method for solving a
general problem
in linear programming) Podprogramma iteratsionnogo
metoda resheniia
obahchel sadachi Uneinogo programmiroyanila. Moskva,
1964. 40 p.
(Akademila nauk SSSR. Vyohislitellnyi tsentr,
StRndartnya prograz-
my BESM-2, no.8). (MIRA 17W
- 4^- - I
FOGMEK, I.A.; ANTUOV I N., Otv.rnl., 131.,
- . . It-, A _ -
X01KNAO A.!., t,1)khn.r#,I.
[PrORram fcr cnIcul-tive oigt~nvnIlien nnti
fAgo?nvvC",.CT-n ol .4
symmetrical mqtri) 1. Y-rorrunmk nobntvvnnykh _nnr n
1' .4
i sobntvonny~h ve~torov I!o:1v%q1i 10it)4.
23 p. (Andomita nsilik .3..',M. Vy-i .J's1j1kIIny',
~-nontr. . t
tipovye projtrs~Ay no. -! "
I n , . ,
U'l.)Y,ANOVA# T.Mj; AMIFUV# I.N.; CHIBraMp V.V.t otr.
redo
[I.Work at the control deek of tits BESM-~.'
computerl programmer's
hatAbookaj Rabot& m pulltm =H-2; posobie dlia
pro(-a=istov,
Moakvap 1965. 31 P. (Akademila nauk SSSR. Vychislitel
nyi teentr.
StarAartnr i tIpovyv progra=y Bel;M.Q,, no.10) (MIPA
Ists)
ACC NRt ")-~003062 SOUICS-COD:;:-U 00?3/67/033/=~1~014/0016
V
AUTH01: 13olotsklyt D. P.; Antiloov, I, N.; Krylyuk, N, V.
ORG! Chornovtsy State University (Chornovitskiy gosudarstvonnyy
universitot)
TITLSI Synthesis of single crystals and study of the SbI3-BiI3
system by using the
1 fusibility and electrical resistance mothods
SGURCE., Lkrainskiy khimichoskly thurnal, v. 33, no. 11 1967, 14-16
TOPIC TAGGS: single crystal growing* antimony conowand$ bismuth
compound, lodido,
resistivity
ABSMICTI SbIj and DIII single crystali were ioronarod from
snectrosconically Duro Sb
and BI And iodine by the Bridgman method in a vertical furnace
with throe tommoraturo
zones. 'I"he melting point diagrara of the Sb13-ftI3 system vas
studied by plotting
heating &n$ cooling curves. The diagram obtained (see Fig. 1)
showed the 3ystom to be
characterized by a tomploto solubility in both the liquid and
solid state. The do-
pandonce of the log of the resistivity on the reciprocal
tomDerature -das found to be
iinoar In SbI single crystals. The pro3ance or BiI3 changes this
function con-
pletalyt and ?he latter keeps changin'g with increasing Bi13
content. An isotherm of
the resistivity of the SbI3;BiI3 system at 1000C showed a peak at
20 mole % KI3; this
is attributed to a certain rderirig of the structure. Orig. art.
hast 5 figures.
Card 1/2,
ACC NRs AP,7oo8o62
i
Fi g. 1
t, %, ,
.-k
1.
i
SUB CODSt 0?/ SUBM DATSI Z)Jan65/ ORIG RSF:' 007/ OTH REF: 001
a
j .
4
ANTIPOV, 1. T. Cand Teoh Sol -- (dine) ",We ~Ilverosl method
of th?
d=v ~t
of serl&IARUvRmW photorraphs of 55 M fooAl A
on a lilOpOscales" Moo, 1957. 25 pp (Yin of Higher FAjontion
115"IR. Mon
Inst or Enrgineers of Geodesy, Aerial Motography, and
Cartogre. j.,hy), 100 coplese
(KLI 6-50, 1.00)
AWNPOT9 lotel "pirant
Processing of aerial photographic pictures by mans of
transformation
of projected bundles of rays, Trudy HIIGAIX
no,29tlO9-144 157.
(141RA 110)
1,Xafedra fotogrammetrit Moskovskogo institute,
Inshenerov geodesil
aerofotoogyawki I kartografil.
(Aerial photograimtry)