SCIENTIFIC ABSTRACT POPOV, I.G. - POPOV, I.N.
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CIA-RDP86-00513R001342310016-0
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S
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100
Document Creation Date:
January 3, 2017
Document Release Date:
August 1, 2000
Sequence Number:
16
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Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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ACC M: ;iT7011651. SOURCE C007-: UII/0000/66/000/000/0216'/0216
AUTHOR: I-opov, 1. G.
ORG: none
TIME: Aspects of rational nutrition of astronauts in fli-lit
SOURCE: International Astronautical Conc-'ress. 17th, I-ktdrid, 1966.
Daklady. no. 13. 1966. Nelcotovyyc aspekty rats i ona I I-.ioZ;o pitaniya
kosmonavtov v polete
TO?IC TAGS: human physiolo.-y, space nutrition, space food, di.-estive systerl,
biolo.-Ic metabolism
ABSTRACT:
Cosmonaut nutrit-Ion will be a relativ*elN,,, more Im-
portant environmental factor as spaceflight durations
C3
increase, considering the necessity of -waintaining himh
cD C-1
levels of work capacity and adaptability in cosmonauts.
The daily food requirements of co3raonauts for different
flight phases inusi first be determined. Tht, adequacy of
food standards established in the USSR and other countries
for professional groups with activities sitailar to those
of cosh.ionauts-was analyzed. Experience in feeding Ameri-
Ca,d 112
J.
ACC NR: A-17011651
can and Soviet costionauts and studYing their metabolism
was also considered. it is known Chat the overall nutri-
tional regime is important in maintaining homeostasis,
heat and water balance, and in determining the de-ree
of assii.Alation of nutrients. in this study the effect
of changes in the number and spacing of feedings and
in total food volume on functioning of the organism
were considered, Such factors as food variety, taste,
and physical condition of food recelved special atten-
tion. The importance of maintaining good appetite and
food palatability, and of promoting alimentary stimula-
tion of positive emotions (sic] was acknowledged. Vj'hen
food products to which man is accustcmed are used in
spaceflight nutrition, it will be necessary only to r.iain-
tain the alimentary system stereotype. But when closed
ecclogical systems are perfected, it will be necessary
to solve the complex problem of human enz-31matic adapta-
Cal studies of enzymatic
tion to the new food. Experiment . L,
adaptation of animals to new synthetic sources of fats
and proteins have indicated the complexity of this
proble,m. /_ATID ?RESS: 5098
SUB Coo-E. 06 / SUBM DATE; none
c.rcl 2/2
=W'---AP6015621
INVENTOR: Popov, I. G.
ORG: none
TITLE: High-pressure apparatus. Class 12, No. 181049
Z/Z/
SOURCE: Izobretentya, promyshlennyye obraztsy, tovarnyye znaki, no. 9, 1966, 15
TOPIC TAGS: pressure
A13STRACT: An Author Certificate has been issued for a high - pressurApparatus.
To simplify its manufacture, the chassis consists of welded plate domes with the
arched side facing the inside of the apparatus and fastened with longitudinal beams
and rings (see Fig. 1). Orig. art. has: I figure. [Translation] [NT]
SOURCE CODE: UR/0413/66/000.009/0015/oUlb
UDC: 66. 023. 083. 2
Card 1 / 2
L 43907-66
ACC NR- AP6015621
SUBM DATE: 17MarG4/
~:�VB CODE: 13/
Fig. 1. High-pressure apparatus.
I- Plate domes; 2-beams;
3- rings.
SIMIRIMV, A.D.; FOFOV, I.C,.Y red.; ISAYEA'.4, E.N., rea.
[Dynamic model of the interibranch bal-ince; a
book] Dinamicheskaia modell mezhoLrbslevogo be.-
lansa; uchebnoe posobie. Voskva, Ir,-t naro,in,-)t!o Oic.17.
1964. 111 p. (MLh.,. 1e.1)
S/12 62/000/003/042/052
D2 3 7 XD3 E2.
AUTHOR: Popov, I.G.
TITM: 1-n approximate calculation of lon- cylindrical slie-l'is
CD --
FIERIT ODIC i*11; Referatuivnyy zhurnal2 Nekhanika, no. 3, 1962, 12,
abstract 3V68 (Sb. Raschet prostranstv. konstrukt'siy
no. 6, M., Gosstroyizdat, 1961, 189 - 212)
T-'-.'XT: Assum-ints that in case of calculating lor.- Prismatic folded
systems and cylindrical shells (replacing them br folded syste--,s),
the method of V-Z. Irlasov (Stroiteilnaya mekhanika tonkostennych
obolochek (Structural ~,echanics of Thin-17alled Shells) M., 0-TT,
1036) is sufficient'-.1y confirmed by experiment and assuming that zhe
deformations of a spatial folded systen nearly coincide wit.h those
of axj-lin~lrical bar system, the method of solvingsdevelo-ped by the
author (Tsilindricheskiye sterzhnevyye sistuera-y (Cylindrical Bar
,stems) Gosstroyizdat, 1952), the author, in order to achieve
further simplification of t-he computation of long cylindric--l sheliz-
promses replacing spa-vial elements by s~patial bar systems. A se-
rie-s of comparative calculations by both metlods is performed and
Card 1/2
Cand ee ii L' c (;d 2
-oal Pits o t' 1~ r e Ior rn r~-~ a r aa.- a., 2~, up;
hii---her and S-c-aj-z
Lenin and of Labor Red -~-vjnnei- -,.' i r: i n
ies; price not ..~-iven; (KL, 21-6,,;, 125)
POPOV, I.I., otv. za vypusk; VORMIIKOVA, L.P., tekhn. red.
[Standard time and production norms for work in protective tree
planting and landscaping in railroad transportation] Tipovye
norny vremeni i vyrabotki na raboty po zashchitnym lesonasazhde-
niiam. i ozeleneniiu na zheleznodorozhnom transporte. Moskva,
Transzheldorizdat, 1961. 233 P. (MIRA 15:5)
1. Russia (1923- U.S.S.R.) Ministerstvo putey soobahcheniya.
Upravleniye truda, zarabotnoy platy i tekhniki bezopasnosti.
(Landscape gardening-Production standards)
(Roadside improverant) (Windbreaks, shelterbelts, etc.)
41
oal
YP
ril Q3 -1
f1c
0l
g S,
lei
CN""
YIN-,
Yj
3(j
up
Ii
f aph 7, L
Of
5r l..:,
,~5
s ,u
T.1
IL L
r u
TAG
KB
or T,
V
S B CI'S
G
fl aLd P
-.-i--ich jV0z--
A
F B sin (P (2 cos2t'- - Sin2,.P) 0 a_ncl, hence
b(P
t6 2TO = 2 for aa7:iI-rCUM f Thus: a..3 T-1
i,ecedes from P.1 alone AB the ros'Ll-oriii(I force F
corres-_)o-.,,din,, to (p = (po At ~~,roater
srows to a li
~i__-tances f diminishes, which can lead to ne-ative
1 0
values of f 1 - F and hence the falling of the aass
This is shovm L-,raphically in Fig.2. For small amplitudes of
oscillation and for angles (p close to a right an,-le the
~3
,restoring force cap- be considered quasi-elastuic. E-_-_--prr_-IsinS
the first equilibrium state of the system by the COTLditiOT!:
h h h
f P = f cos (p = f -0 = A A 0
P _V(h d?)-)
0 0 0
a.nd the restoring fo_-ce:
F f P A h0 + &I h 0
h +-,4h) 2 d 312 (h2 d3)3773-
Card 0
A S."Ort-Pez--iod Ver-ical 3
This ives w,)zro.-4imately:
d2_ h2
F ~~ A 0 1~h CAh
(ho +- d
i.e., F is quasi-elastic in this a-,-.,.roxiL'iatJor-.
tic represc3itai
shows a photo~;rap~a a-nd Fi-.1 -a Sclf-2-eme
tant Tuagnetic fieldl
the correspondin--~17 'a~J]PEXU-t-'AS- The cons 0 8 cm. A4--a ca
is created b7 -1 ma~=c-t wi,-',,h dimensions 4- Y. 5 :~:
di'stance 0.5 W1 from its SUrfLace is the counterbalan-3ed
tized iron rod of len,-th 00 i*-im and crcsc-
ei~d of a we,':C.~J'T '~-U-Jje
section 0.5 C7. The rod is fastened alon- the radJus c~f
-L lict r .1
-,er Or aluminj.= disc vJ1 otatez about a
circular cop,
the end of the rod in t'-,%-e ma~;netic
horizontal axis. o~ rotation. TL1e -od
U
field xas 11.5 (--n ~'-"s -L
the having a relative UC
disc represent
Card 4/7
30V-49-58-6-8/12
3~10rt-Period Ver~ical Seismo~-ra~;~i with 1,,~at--netic Restoring Force.
U
10-5kr./m2
L-he axis of the disc of K 3 x
The system
,~,'~,jtitutes a seismogra-t,)h with direct
optical re '-,,~istration
-lie C~ I I
len-til of the optics:,! lover beii-, A = 100 cn, ) a-rid a
i-,a~--Iiification Vo'- 90. This apiaratus was first tested in
the Seisometric Laboratory of the Institute of Physics o-
the Earth, Ac. of Sciences, USSR. A trace of the oscillation
L
is given in Fi-.L~, where the upper curve gives the oscillations
C,
of the seismograph platform with different periods. and the
loviez- Gives the oscillations of the seismograph wiih a natural
period T = 0.5 see. Without addibuional damDing and in con-
ditions close to resonance,, the max-imum magn1fication was
ap:prox-imatelY 500. Da-aping was noticed in ordinary Dscilla-
tions owing to the dampin,- action of the magnetic field. The
natural oscillations of tile pendulum without additional damp-
ing are given in Fig-5. Two cases were taken:(a) period of
C3
pendulum T 0.09 see, damping D 0.029 , correspond-
.Lng to a marnification e\j 1600 , (b) Tj 0.44 sec, dau-in~~.
Di = 0.065 and
characteristics
Card 5/7 .~~2.ven in FiZ.G.
maxim-um, iiia,~~Iif icat ion 700
Trie frequency
of the seismograph for these two cas~-S are
These are calculated from the fori.,iula:
g
M
Ng-'Y Y't"N
- -- --,. -- *1-
Nv 'I
NvA
S,
in-
kj
-period Verti-cal Sei
A Short where u1 Tw /T
U =- ------ 2 2
I -V (1 _ 1,1)2 + 4D1 U
;he arrivint-D v"anves of
of the periods of 0.,
the rat io h and D is tile d of tile pendulum
seismOgraP 1 jairror attached to the
,js-t.rption i - bi a Ij ste:ri-1p, a t3us a
Optical reo Tjsill,- an ord't-nar-,[ re~;- -p-pa~a the
the disc. of the recordin; dru;', --prisms
e
horizontal axis of rotati:)n :)ssed, totally ref"Cting
li,ht is reflected bi tWO Ir( I llati_on can be alter--
'Jj 2he Veriod of natural oscl maSnet This t--,7PF-
(Fis .7 the distance 0 the constant
by varyinu
C,ard
3 0 V - 12
.A
sei_s:nD-za-,)h seeMs suitable for u0e w-L"Wh stror.~;, close c-a~-th-
res and 4 Soviet referen-ces.
z Tiiere are 7 f'isl~_
au., 333R, I-stit-u~~ Fizi':i ZI,--nii, Tsentral'-
kkademiya ii,
~1~a seysaiiches'-aya sban~sija (Acvde.,V of
Sciences USSR Institute of Physics )f the Eart-h. Central
Seismic Station "Si-aferoDoll")
SUNIAITTED: Alay 28, 195?.
1. Seismographs--operation 2, Magnetic fields--Appliqation 3. Seism
mographs--Analysis
Card 7/7
87968
S/049/60/000/010/004/014
E133/E414
AUTHOR-. 4W"*P4&' Aw-
TITLE, The Dispersion of Long.-Ppriod Love Waves in the
Continental and Ocean Crust Along the Great Circle
Indonesia-Crimea
PERIODICAL; Izvestiya Akademii nauk SSSR, Seriya geofizicheakaya,
ig6o, No,io, pp,.1458.-1462
TEXT- Seismic waves have been recorded on a long-period,
horizontal, electrodynamic seismograph at the Crimea. The
characteristic periods of the pendulum and galvanometer are
60 see and 36 see respectively, The seismograph magnification is
shown in Curve 1, Figj; (this is a plot of magnification M
against period in see). The apparatus was stabilized as suggested
in Ref,10, Love waves of periods up to 74 see were recorded from
the earthquake of 1958, August 12 (19 h 25 a 05 s ),, The azimuth
of the earthquake,as measured from the station, was 90* + 2'-
Two groups of Love waves were noted, one 41 win and the other
112 win, after the first P-waves arrived, The first group tame
Card 1/6
87968
s/o49/6o/ooo/o1O/004/Ol4
El33/E4l4
The Dispersion of Long-Period Love Wavem in the Continental and
Ocean Crust Along the Great Circle Indonesia-Crimea
across the Eurasian continent (10300 km) and the second across the
Pacific and Atlantic (29700 ka). The dispersion of the Love waves
was studied by methods mentioned in Ref.2,3 and 11, A sample
recording is given in Fig.2, The group velocity of the first set
of waves lay in the range 3.32 to 4,03 km/sec, that of the second
set from 4.13 to 4.29 km/sec. A table is given of the velocities
and periods of the waves, The track of the waves is given in
Fig,3 and the experimental (dotted) and theoretical (continuous)
dispersion curves are compared in Fig,4, in which the group
velocity (ka/sec) is plotted against the period (set)~ Curve I is
a good approximation for the Eurasian continent for an upper layer
of thickness 40 km and wave velocity 3,5 k/s on top of a lower
layer with wave velocity 4,5 k/9. the ratio of the densities of
the two layers being 1.28, Curve 4 approximates waves travelling
two-thirds of the way through the ocean crust (with a layer depth
of 15 ka) and one-third through continental crust (layer of 40 ko),
Card 2/6
87968
S/049/60/000/010/004/oi4
E133/E414
The Dix persion of Long-Period Love Waves in the Continental and
10cean Crust Along the Great Circle Indonesia-Crimea
40
A
Bd
:15
NO
C
I I J#S
l7epaoO 140,fmw 7.rex
.55
I Our, t. tIRMOTIM 1BPUKTOj)11M1H1k AnHmionepx*,
-romajoro coficmurpa(pa (1) n cono-
omjoro ropiaou
Mane"1111 0 " irre CTSH A ropwouunbu
corlexorpa$", T'IM, Crit (2) Oro
87968
s/o4g/60/000/010/004/014
E133/E414
The Dispersion of Long-Period Love Waves in the Continental and
Ocean Crust Alonx the Great Circle Indonesia-Crimea
Card 5/6
Onr. 3.: Tpa~ca 8011H __ gyra Gontworo Hy yra, npoxaAamir qcpe3 z)rmgcnTp
UnqeCRY10 cTaflixuio (c) H auTnaunqeuTp.
A, - 92*,A A. - 267'.6
87968
E133/E,A4
The Dispersion of Long-Period Love Waves -,.n the Continental and
Ocean Crust Alons the Careat Circle Indone4zia-Crimea
0
4 .......... 15::~A
~A
at
tz
40
--nerumf 10,411bl- r rifir-
Onr. 4. ConomBneEme w~nepnmemanmmx itpuBux Ancriepcim
rpynnomi exopom Boan Amna (A - A, B - D) c Teopennecimmu xpn-
Buy" Allcuepull (1-3); 4 - xomGmmpommm Teopenmema xpimm Ann
Card 6/( ------- nTOPO&I TIMCC-
S/049/61/000/005/004/013
D218/D306
AUTHORS: Arkhangellskiy, V.T., Kirnos, D.P., Popov, 1.1.9
and Solovyev, V.N.
TITLE: Preliminary observations of long-period seismic waves
at the Simferopol' station
PERIODICAL: Akademiya nauk SSSR. Izvestiya. Seriya geofiziches-
kaya, no. 5, 1961, 670-675
TEXT: This paper was first read at a seminar or. surface waves
which was held in the Department of Seismology and Seismic Service
on October 1 - 5, 1960, at Simferopol'. The authors briefly report
on a prototype vertical seismograph which was designed for detect-
ing seismic waves with periods between 20 and 300 see. The instru-
ment is a modification of a vertical seismograph deaigned in 1959
in the Department of Seismology of the Institute of Physics of the
Earth AS USSR. The modification was carried out in accordance with
the recommendations given by the first of the present authors
(Ref. 6: Izv. AN SSSR, ser. geofiz., no. 10, 1960). The pendulum
Card
S/04 61/000/005/004/013
Preliminary observations of ... D218YD306
employed is illustrated schematicallyin Fig. 1. The reduced length
of this arrangement is 1 1 = 0.742 m and the moment of inertia is
2
Ki = 0.381 kg.m . The flat spring is made of elinvar which has a
positive temperature coefficient of frequency (22 x 10-6 ). The
long-period galvanometer was made at the Seismometric Laboratory
of the Department of Seismology and Seismic Service, Institute of
Physics of the Earth, AS USSR. The period of the galvanometer may
be adjusted to between 80 and 130 seconds. Its current constant is
2.2 x 10- 10 amp/mm at one meter, and its electromagnetic damping
constant is 72 ohms. The moment of inertia of the galvanometer
7 2
frame is K 2= 8.63 x 10- kg.m . The seismograph has been used to
record long-period surface Rayleigh waves with periods in excess
of 30 sec. Interesting results are said to have been obtained for
Rayleigh waves due to the Chile earthquake of May 22, 1960. Waves
with periods up to 480 see were recorded. There are 5 figures,
1 table and 8 references: 3 Soviet-bloc and 5 non-Soviet-bloc. The
4 most recent references to English-language publications read as
Card 2/16
S/049/61/000/001/000-/008
D226/D306
AUTHORS: Popov, I.I., and Solov1yev, S.L.
TITLE: Conference on the seismic zoning of the Crimea
PERIODICAL: Akademiya nauk 88SR. Seriya geofizicheakaya. Izvestiya,
no. 1, 1961, 120 - 121
TEXT: A conference on Crimean seismology and seismic zoning took
place at Simferopol' on October 6 - 8, 1960, the participants being
the Seysmicheskiy sovet AN SSSR (Seismologic Council of the AS
USSR), the "Simferopol'" Tsentral1naya seysmicheskaya stantsiya
instituta fiziki zemli AIT SSSR (Central Seismic Station of the In-~j
stitute of Physics of the Earth, AS USSR)p and the Crimean ~branch
of the Nauchno-tekhnicheskoye obshchestvo stroyindustrii (Scien-
tific-Technical Society of the Building Industry). The aim of the
conference was: 1) To attract the attention of both local and other
experts to the study of Crimean earthquakes; 2) To remind builders
of the need for providing for earthquakeproof buildings in ha~ar-
Card 1/4
3/049/61/000/001/006/008
Conference on the seismic ... D226/D306
dous seismic zones; 3) To familiarize the participants from vari-
ou8 institutions with work being carried out on the theme of the
conference. It was opened by S-V. Sosnitskiy, the assistant chair-
man of the Crimean Regional '111~xecutive Committee, and E.F. Savaren-
skiy, chairman of the Seismologic Council AS U188R. Seismologic pa-
pers were heard on the first C, ay. T.I. Poi)ov ("Siml'oror,oll" Seis-
mic Station) spoke of the history and prcsent state of t1fie study
of Crimean earthouakes and -cave some basic facts about earth-uakes.
S.V. 1.*Tedvedev (Institute of Physics of the _~'arth AS USQ1R) outlined
the chief aims of furt'lier viork on making a no--,,e accurate scheme
for the seismic zoning of the peninsula. 0.1. Yurkevich (Seismic
Department AS UkrSSR) spoke on the seismic zoning of TransiCarpa-
thia -- the second seismic region of Ue Ukraine, in particular on
the use of multiple-leveling data in seismic zoning. A mat of
earthquake epicenters in the Black Sea basin was pi-esentea by A.Ya.
Levit'ska (In;titute of Physics of the Earth, AS USSR). Z.I. Arono-
vich ("Simferopol"' Seismic Station) reported in detail on the
energetics of Crimean earthquakes. The second day of the conferen-
Card 2/4
S/049/61/000/001/006/008
Conference on the seismic ... D226/D306
ce was devoted to building problems. Papers were heard by V.P.
Umants ("Simferopol"' Branch of 'Giprograd'), O.Z. Ioffe of TreBt
"Yaltastroy" (Yalta Building Trust) and V.N. Timofeyev (Yalta
Branch of 'Giprogradt) on the state of planning and construction
of buildings for seimic areas of the Crimea as was the information
of B.K. Karapetyan on the work of the Armyanskiy institut stroyma-
terialov i sooruzheniy (Armenian Institute of Building Materials
and Construction) on problems of earthquakeproof construction and
engineering seismology. Papers by G.A. Lychagin, Krymskaya geolo-
gicheskaya komplekanaya ekspeditsiya (Crimean Geological Expedi-
tion Group) on Ceology of the Crimean Peninsula and M.V. Muratov,
Moskovskiy _eologorazvedochnyy institut (Moscow Geological Proq-
pecting Ins titute) on Crimean neotectoniesp and also reports by
V.B. Sollogub (Geologic Institute, AS UkrS'-R) on the study of crus-
tal structure in southern areas of the Ukraine and A.A. Shimkus,
Black Sea Station of the Institut okeanologii AN SSSR (Oceanologic
Institute, AS USSR) on the study of crustal structure in the Black
Sea basin, were heard on the last day. The conference adopted a
Card 3/4
ORESHKIN, P. T.; DEVYATKU1, V. A.; POPOV, 1. 1.
Thermal diffusicn. currents and the thormooloctr(,mative force
in industrial refractories at Ugh temporaturos. Izv. vyEl. uCh(.1b,
gav,; chern. met. 7 no.6.*181,,-190 16~1. (MMA 17.7)
1. Sibirskly motallurgit~,honkly hitititoiL.
POPOV, I. I.
Experimental Reserch in Formation by -eJa,-es oil 5table Profiles of -'bstream
Faces of Earth Dams and Reservoir Shores.
renort presented at the 7th International Conference on Coastal Engineering,
The Fague, 21-27 Aug., 1960.
All-Union Sci. Res. Institute of lbjdrotechnics iri. B.E. VEDEN'MEV.
POPOV) I.I.-, VORONIN, P.A.; MATYUNIN, V.S.
Ylpthod of testing in mines of coal aining explosives for a
ten4,ency to burn out. Vzryv. delo no.52/9:217-221 163.
(KRA 17:12)
1. Makeyevskiy nauchno-issledovatellskiy institut po bezopasnosti
truda v gornoy promyshlennosti.
POPOV, I.A., inzh.
Autonomous aEynchrono!-,s generator with excitation Lfrom variable
condensers. Elektrotekhnika 35 no.11:41-44 if f64.
(MIPA 18:6)
P":)Pov, I.., . -7 - ~;
the M,
prom. 18 no.3:29 165.
Vakhtanskiy kanifoll-io-eksuraktsionnyy zavod.
ACC Mt AT7011649 SOURCE CODZ: UR/0000/66/000/000/0001/0009
AUTHOR: Akulinichev, I. T.; Zhdanov, A. 11,; Popov, 1. 1.
0%G: none
TITLE: Problems of bioteleiaetry during prolonged spacefli.ghts
SOURCE-,: International Astronautical Congress. 17th, Madrid, 1966. D31