SCIENTIFIC ABSTRACT KIRNICHANSKIY, I.V. - KIRNOZOV, F.F

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000722710015-6
• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

XIRNICHANSKIY, I.V. -'.
1 .1.
Ratimial treatment-of fractures of the femoral neck in elderly
and senile persons. Trudy Kioh,gosemed,inst. l2s8l-& 160.
(MIRA 16 W
1. Xafedra gospitallnoy khirurgii Kishinevskogo gooWarstvannogo
maditainakogo instituta.
(GERIATRICS) (FEMUR-FRACTURE)

XMIMANSurp I.V. - - - ~ ..
Imedimate late- wmdto of surgical treatamt in
obliteritive andarteritis aq senile gangrene, Trudy Xish*
goo.med4inst. l2s97.aO4 160. (KIRA 164)
1. Kafedra gospitaltnoy kbirurgii lishinevskogo gotudaratyermogo
meditainsko.go inatituta.
(GERIATRICS) (WERIES.-DISSAM) (GA4GRENE)

KMIIM, s. EK7=ing, s. I
Chemical method for determining vitamin A In feeds. Vitamirq
no.5t6l-73 159. (MMA 14211)
(VITAMIM-A) (MM-ABALYSIS)

v
Val g
IWO
49#

KIRNITSKIT , B., red. j MAGER, M., rel.
[cc)jjcjse manual for th~, :u,,! fj-3rli crow foreman]
t- -
K,Ao!iza agrononul"i shl a brigadi-rulul, K I.~hin-u, Editura
de Fartid a Komitetulul Chentral al fK al 'Xo1dovei 1 1964.
469 1). (In Xloldavianj fkvil"A 16-9)

KIRANITSHY, 13.T.
"The Peculiarities of the Utilization of a Perennial Grass Layer Under
the Conditions Prevailing in the Moldave)caya SSR." Cand Agr Sci, Moscow Agri-
cultural Acad imeni Timix7azev, Moscow, 1953- (RZhMol, No 2, Sep 5h)
Survey of Sceintific and Technical Dissertations Defended at USSR
Higher Educatiowl Institutions (10)
SO: Sum. No- 481o 5 may 55

rTMTSKIY, B.T., kaud. sell skDkhozywstvenrqkh uauk.
Alfalfa in the contml Urals. Zemledslie 6 uo.6:80-82 Jo 158,,
(Ural Nountaiu region) (MM llz6)

KIRHOS, D. P.
Kirpop, D' P "Some Particular Cases of the Forced YoveT--ont of the Fendulur. (cn tho
Seism.ograph).'" Trudy Selamichesko-o Instltutw A~ad. Nauk J.S.S.R., Lonln~;rad-~I:oscow,
11
No. 79, 1938, pp. 5-13.

KIRNOS, D. P.
Eirnos, D. P. "Fundanentals of the Theory ai, I the Calculation of OicillograFha. a
Trudy 3-iismologicliesll-.ogo Inotituto Akad.,',Iljuk S.S.S.R., Lenin-,4rsd-!oscvw, !;o. Up 1938p
pp. 1-91.

XIRNOS D. P.
%I%4k Neuk. 880#18or COOSA, 066fit" Vol X11, No
a-appmt- recently.released by Bois-
be.ookibo
moic'eilcal Inst' _A~ad: Sol USSM, nev type of eels.
wogMvb,vi+,h'gdI:vinawter type reglister for
-registering dleplicesent of crust dur ag wwth-
=keg :=a oliotrowgrietio t* extensawater for
..dote
Mining o'deformation of sollo Submitted
Jul/A,*-
SslsmOgra~h
Solonbeitrid ppm" us A4 11 and;-
A race
11 V. valhoralpy ~Soi USBRI 0"" last t pp

KIRX(61 PC and EWIWj D. A.
"Main Instruments Use& at the Seismic Stations of USSRO one of the reports
given at the 10th General Assembly of the International Union of Geodesy and Geophysics,
itome, 1954.
Rvaluation, B-86198 and 86204, 30 Jun 55

USSR/Geophysics FArthquakes
Card 1/1
Author : Andreyev, S. S.
FD 350
Title : The method of equal surfaces in the interpretation of local earthquakes
Periodical : Izv. AN SSSR, Ser. geofiz. ~:, 153-159, Mar/Apr 1954
Abstract : Expounds two methods for interpretation of the record of local earthquakes
that are based on the application of time fields. The methods are illus-
trated by examples of treating the weak earthquakes recorded in southwestern
Turkmenia. Two references: Ye. F. Savareaskiy and D. P. Kirnos, Blementy
seysmologii i seysmometrii, Moscow/Leningrad, State kublishfiii'"gouse of
Technical Theoretical Literature, 1949; Yu. V. Riznichenko, "Geometric
seismice of laml r media," Trudy In-ta Teoretich. Geofiziki (Works of the
Institute of Theoretical Geophysics), Vol II, No 1, 1946.
Institution : Geophysics Institute, Acad Sci USSR
Submitted : January 6, 1954

KIRNOS, b.P.
SAVAMSKIY, Yovgeniy Yedorovich-, KIMS, Dmitriy 1?otrovich; ALIKSMW,
D.M.. radaktor; MURAMTA. N.Jas, VOWWelfffflely"Fadaktor.
(Blements of seismology wA saismonatry] Ilementy selemologit
notamometrit. Isd.2-e, parer. Mosive, Gos.Izd-vo takhniko-
toorst.Ilt-ry, 1935. 543 p. (MLRA 8:9)
(Seismology)

-Kruost D.P.; SAVARENSM, Te.F., professor. doktor fiziko-mitevatichaskikh
nauri redaktor:. SHUMN, N.V., redaktor; STMLWSXff, r.A., tekh-
niohankly redaktor.
Some problems of instrumental seismology. Trtdy Geofft.inst. no.27:
3-168 155.
(Selemometers) -
A"

1,~200) the time tl> 1.6 see but it can still
be < 1.6 see in the case of the wave P . Fig.6 shows an
Card 3/4

SOVI 49-58-12-2/17
On the Calculation of the True Value of the First Amplitude of Soil
Movement under the Action of Seismic Waves
example of the registration of the first longitudinal and
transverse waves for various stations. The relationship
between the intensity of earthquakes and the time t, could
not be established. Fig.8 shows the relation Ut - f(tj)
of aalitsylils galvanometric rogistration. , The relat-
ion ti = f(T W) for them is shown in Fig.g. There are 9
figures and 8 references; 3 of the references are Soviet, 3
are English and 2 German.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki Zemli
(Institute of Physics of the Earth)
SUBMITTED: August 30, 1957.
Card 4/4

~MITSIN, Boris Borisovich [deceased, 1862-1916]; PRUVODITZLZY, A.S., otv.
red.tomu; BOMMOTSLIT, V.F.9 profs# rod*; GOMMOT. G.P.. prof.. red.;
KIMOS, DI,~,1jroLl red.; SAVARMIT, Te.Y., prof., red,;
SAVARENdIY, Yo.l., prof., red.; VVZDEN=YJi, A.V., kand.fiz.-mat.
nauk. red.1 VISHIYAKOV, N.V., imnd.fiz.-matem.nauk. red.; LUITSKAU.
A.Ya., kand.fis.-matem.nank, red.; LIN=. N.A., kand.fis.-matem,
usuk, red.; FILIPPOV, L.P., kand.fis.-matem.nauk. red.; KHARIN, D.A.9
kand.fiz,-mntem,naukq red,; ALIKS37XV, D.M., red.izd-TO; KARTOVICH,
S.G., takhn.red.
(Selected works] Izbrannye trudy. Moskya, Izd-vo Akad.nauk SSSR.
Vol.l. [Physics] Piziks. 1960. 241 p. (MrRA 13:11)
I.Chlon-korrespondent AN SSSR (for Predvoditelov).
(Physics)

GOLITSYM. Boris Borisovich, skademik; BOXCHKOVSKIT, V.F., prof.. otv.red.II
toma; PRSDYODITAM, A.B., otv.red.1 tome; GORWMOV, G.P., profaq
red.g KIRNOS, D.P., prof,, red.; SAVAMSKIT, Te.F., profat red.;
VVNMNMATA, A.V., k9nd.nauk, red.; VEWTAKOV, N.V., kand.nauk,
red.; LEVITSKATA, A.T.. kand.nauk, red.; LINDM, N.A., kand,nauk,
red.; FILIMV, LqPq$ kand.nauk, red*; KRARIN, D.A., kand.nauk, red.;
ALMSIM, D.K., red.izd-va; KASHIRA, P.S., takhn.red.
[Selected works) Isbrannye trudy. Koakvs, Izd-vo Akad.nauk SSBR~
Vol.2. [Seismology] Saismologiia. 1960. 489 p. (KIRA 13;12)
1. Chlen-korrespondent AN SSSR (for Pradvoditelev).
(Seismology')

S/61 61/000/016/002/005
D055YD114
AUTHORS: Kirnos, D. P.1 Rulov, B. G.; Kharin, D. A.
TITLE: The VEGIK seismograph, designed for engineering seismology work
and the registration of near earthquakes
SOURCE: Akademiya nauk SSSR. Institut fiziki Zemli. Trudy, no. 16 (183),
moscow, 1961. Voprosy inzhenernoy seysmologii, no. J, 32-56
TEXT: This is a description of thcB3rot(VEGIK) seismograph, elements
of its theory, methods of determining its constants and examples of the use
of the device in engineering seismology and the recording of weak local earth
tremors. The main purpose of the seismograph was the study of the seismic
effects of explosions, but the device has also found wide application in re-
lated fieldso It has galvanometric registration and magnetic attenuation
and may be used for recording horizontal and vertical vibrations. The dia-
gram of the seismic receiver is shown in fi& 1. Vibrations are recorded
with the aid of rK_vI (GK-VI) or GK VII "alvanometers, small mirror Calve-
nometers or ordinary loops In ongineerin,-Olismology nOFk.-9 (POB-9), n09-12
(POB-12) and nOrrl4M (H-7;0) EPOB-14M (N-70 ) oscillographs or other
Card 1/3

S/619/61/000/016/002/005
The VEGIK seismograph so* D055/DlI4
maCnetoolectric oscillographo are used. For recordinG earth tremors the
ordinary Pe -II (RS-II) registering apparatus iG used with a higher moving
speed of the photo-paper of 120-240 mm/min. When the seismograph is oper-
atinr, at 1-50 c/s there are no parasitic resonances. Formulae are discussed
for calculating displacement, rates of movement of objects and acceleration
durinG vibrations in the ground or buildings. Basic and simplified -,.cth4T'd3
of determining the constants of the VEGIK seiamograph are examined. Acct,,unts
are Given of how the VEGIK seismograph was used to observe vibrations during
unPlerGround explosions with the purpose of ascertairtinC safe distances for
enGineerinG installations from mass industrial explosionsg to study vibra-
tions in reinforced-concrete dams and in turbo-generators, and to record
earth tremors. There are 18 figureaq 1 table and 12 Soviet references*
Card 2/3

The VEGIK seismograph ...
LeGond:
I pendulum
2 steel plates forming
ax's of rotation of pon-
dulum
3 - pendulum supports
4 - ateel ocrew apring
'5 - screw regulating pen-
dulum's equilibrium
6 - device regulating angle
of the spring
7 - ligbt plexiglaso cylin-
der wound with two coils of
thin enameled copper wire
8 - permanent magnet with a
coil in the cylindrical air
gap
316151/611000101610011005
D055/Dll4
3
7
0

1j S
Card 3/3 Fig.l. Diagram of the VEGIK seismograph

S/049/61/000/005/004/013
D218/D306
AUTHORS: Arkhangellskiy, V.T., Kirnos, D.P., Popov, Igist
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 on 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 wdvea with periods between 20 and 300 sec. The instru-
ment is a modification of a vart'.aal seismograph designed 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 1/,4-.,

S/04 61/000/005/004/013
Preliminary observations of ... D218YD306
employed is illustrated achematicallyin Fig. 1. The reduced length
of this arrangement is 11 = 0.742 m and the moment of inertia is
2
K 0.381 kg.m . The flat spring is made of elinvar which has a
po8itive 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 60 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
frame is K2 = 8.63 x 10-7 kg.m 2. 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 Kay 22, 1960. Waves
with periods up to 480 sec 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 Engli8h-language publications read as
Card 2/K_

loi/049/61/000/005/004/613
Preliminary oboervations of D218/D306
follows: 11. Bonioff, F. Press, Progress report on lone, period
seiumographo. Geophyu. J. Roy. At3tr. Soc., 1, no. 3 (1958); N.
'-'winL
- ?,,, 1. Press, Purther study of atmoopheric prououre fluctuations
recorded on ticismographe. Trans. Amer. Goophys. Union, 34, (1953);
F. Vrouo, 11. Ewing, F. Lehner, A long period sciumograph system.
Trans. Amer. Geophys. Union, 39, no. 1 (1958); N. ';",winr, W. Jar-
detzky, P. Press, Elastic waves in layered media (1957 -
AOSOCIAMON: Akademiya nauk SSSR, Institut fiziki zemli (Academy
of Sciences USSR, Institute of Physics of the Larth)
SiBMITTED: December 17, 1960
Card 3,/4~

S/169/62/000/002/014/072
D228/D304
AUTHORS: Kirno-s. D. P. and Rykov, A. V.
TITLE: Special rapid-action seismic apparatus for announcing
tsunami
PERIODICAL: Referativnyy zhurnalg Geofiz.4ka, no. 2, 1962, 111-12;
abstract 2A76 ~Byul. Soveta po seysmol. AN SSSR, no.
90 1961, 56-66)
TEXT: Versions of the apparatus for the rapid (3 - 4 min) determi-
nation of the epicenters of catastrophic earthquakes (YS017.)--f
UBOPE-1) equipment and the epicenters of earthquakes (YE013 -Z
MOPE-2) equipment~ have been developed. Each contrivance con-
sists of two instruments: one azimuthograph shows the direction to
the epicenter, while the other indicates the magnitude of the epi-
central distance and the force of the earthquake. The UB0PE-1 az4--
muthograph includes two mutually-perpendicular horizontal pendu-
lums, and the UBOPE-2 azimuthograph is a pendulum with two degrees
of freedom. The pon connected to the pendulums regiaters the line
Card 1/ 3

3/16 62/000/002/014/072
Special rapid-action ... D228YD301
of azimuth on a smoked paper or plate, and a special optical ap-
liance projects it onto a mat screen with a scale. A 83rW K
EGIK) vibrograph is used for synonymously determining the direc-
N
tion. In the UBOPE-2 the recording is made on luminescent paper
with a post-luminescence of 30 min, which corresponds to the time
of one revolution of the recorder drum. The magnification of the L100-010
UBOPE-1 and UBOPE-2 azimuthographs equals 25 and 500 respectively.-,
Two mutually-perpendicular horizontal CMP-3 (SMR--3) seismographs
(a magnification of 2 and a natural oscillation period of 3 see)
are used in the UBOPE-1 to determine the epicentral distance and
the earthquake force. An astatic pendulum with two degrees of free-
dom, whose movement is resolved into two mutually-perpendicular
directions, is used in the UBOPE-2 (the system's magnification is
50, the period of natural oscillations being 4 see.). There is an
optical device which allows the difference in the arrival time of
the transverse and the longitudinal wave, and the oscillation am-
plitude, to be read off without removing the tape. The analysis of
two tsunami earthquakes recorded by the UBOPF,-l testifies to the
Card 2/3

S/ 16 9,A) 2/000/002/014/0-7 4"
"26/D301
Opecial rnpid-action ... D-
dooinibility of decrouning the oenvitivity of fthe SMR-3 seismo- 7
graph by 4- to 5-fold. /-Abotructerla note: Complete tranalation.-/
Card 3/3

5/6) ()/b I /Coopi,)/100 I /C P1
AUTHORS: Ych Shill-Alan, Kirnos, D.P., SolovOyev, V.N.
C~_~
T I TIX: A simplified recording unit for in%trumental %,.Nb-;crvations iri elli,etizial
zones of' strong earthquakes
SOURCI": Akademiya nauk SSSR. Tnstitut fiziki -crati. Trudy, no. 19 (1~6),
Moscow, 1961,SeysuLicheskiye pribory, 5-11
authors describe an YAP(U.AR) recording unit for making time rer-~rdjngs
0. v;~rious seismic processes in the epicentral =ones of strong earth,,tuak-es. It i<
auLouwtically started at the beginning of an earthquake and stops after cric ViAnute.
the average period of a local carth,uake. It consumes power only %dien recardine,
and is always ready for operation. It consists of the following units, mounted on
a single base: (1) three accelerometers, veiocity meters, or seismometers of the
same design as those used in the CP30 (SiUJI) device developed by the IF-', AS
USSR for recordings at Soviet seismic stations; (.;) a special recorder with a ftl.m
or photographic PiLper; (J) a starting scismoscopc in the fort: of a verticai pendu-
lum with two degrees of freedom. Calculation of the chart iveti
Card 1/.3

s/t, I ."Ib I /Uco/1' I'L; i(')9
!ILI 59/P 11
simplified recording unit for
Latiora to ry test$ of a workLng mode I of t Ile dcv1%,e showed ~h-"r I It is %ta I ted
by an earthquake of a predeteindned intensity. If no eaj thquake %.,I tho given in
tensity talces place. the unit can renain teakiv for for UJI C': I Il-edr;
G) the uniroiiii tape speed of about IC mjr/sec 'P; reach.,A 0.03 - C.0, e, dle' tho.
i_-rrival of a sci!,vuc wave, wh0e the luminaire laiiip li!zht, up even socnei ; (')
seismic- re(~eivel-" with oplical and gakanclmeti i,_ rekoidint, svstvi-~~ ell CHIC (he lint:
to photol-raphik-ally rekord various clements of !around iiiovcrient,~ Jtotne eatthqual,~--i
with an intensity of more than 3 points; (4) powel is Supplied ft--!l .1 (1 V '10 ..'
100-v dry battery and is consumed only during tile leconline prorec (421 tile lill't
is sufficiently simple, reliable anti cheap, and can theiefore be in I-Ale-
scale scismometric observatiurv- of stretv-, eerthquakes Th,-AW(Al, -ul,jCSMiAM)
scismoscope -type devices are menticned as dimple arld ch"'LP 'W%i I11CA ill
seismic observations. There are 3 figurer. and 5 references: 2 Siv;et .01,- ani
3 non-Stiviet-bloc. Tile three references to Enz1i5h-1a(l4ua:ze publ!~,iz_ons reid a!:
fo I lows: N.H. fleck, Civil N 1, 1~44_1 F P, Ulr-Wl Pr~
Caru :W3

'3/6 1 -)/t'1/'Q'uo'O I il ~ "C" -)
Do 3 ()/1) 11 .
A simplified recording unit for
of Scism., work by U.S. CGS western U.S. during 1941. 1101. Sei-m. ot' ~,M.
34, 1944; R. Takahasi. The SMAC strong motion acceleroaraph and other late5:t
instnir-its for measuri*,.g earthquakeE and building vibrations. Pror. of %%Orid
Conference on Earthquake Engineering, June 1956.
V~
Card 3/,i

AUTHOR
TITLE:
PERIODICAL
Kirnos, D. Rand Solov'yeN. N.
S12631621MMI 1/0081022
1007i 1207
Seismograph for optical recording of strong, destructive earthquakes
Rcfc(ativnyy zhurnal. o(det'nyy vypusk. 32. limcradnaya teklinika, no 11. 1962, 22,
abstract 32.11.164. "Tr. In-ta fiz. Zemli. AN SSSR", no. 19 (186). 1961, 25-36
TEXT ~ Soviet and foreign devices for recording vilitations of soil and structures during strong earthquakes
are critically examined and it is shown that certain deficiencies in the method of measurcmcrit-rccording do
not permit these devices to be used as standard recorders at socismographic stations. Description is given or a
new type of seismograph designed by the Institut Fiijki Zcmli AN SSSR (Institute of Geophysics of the
AS of the USSR), having an improved automatic recording system. The seismograph records different
components of acceleration, velocity and displacement of soil. The sensing device of the seismograph is
an elastic pendulum made or an aluminum plate located in the air gap of a permanent magrict and fastened
to a steel wire that forms the rotation axis of the pendulum. The latter is provided with a flat miffor for
beaming the light of a special lamp thrcugh a focusing lcns, to the photographic paper fixed to a rotating
drum. The rotational speed or the drum driven by a spring gear is 5 or 10 mmlsec. An electrical, b3itcry-fed
device ensures connection or disconnection of the seismograph at the beginning of an earthquake and the
end of recording. There arc 6 figurcs and 7 references.
(Abstracter',. rinte - Complete translation.
Card 1/1

3/61~/61/000/019/015/0201
D039/D112
AUTHORS: Kirnos, D.P.; Moskvina, A.G.; Shebalin, N.V.
TITLE: On the selection of rational methods of determining the
constants of electrodynamio seismographs
SOURCE: Akademiya nauk SSSR. Inatitut fiziki Zemli. Trudy, no. 19 (166).
Moscow, 1961,Seysmichaskiye pkibory, 91-112
TEXT: Rational methods of determining the constants T142, Dl, D2, 0'2
and V of the pendulum-galvanometer system of an electromagnetic seismograph
are proposed. These constants entirely determine the form of the frequency
and phase response and are accepted at Soviet seismic stations as the basi~,-
constants of seismographs. The period of free oscillations of the galvano-
meter T2 can be determined by a seconds timer with an error of not more than
1%, when the oscillation periods of the frame of the galvanometer are short
it is recommended to determine T2 by recording the free oscillations of the
frame on hotographio ,,r. The pendulum period T, was found for the e6K
(SVK) I B& (VSKh) ndp NOW (VEGIK) seismographs. The measurement of
Card 1/4

S/61 61/000/019/015/019
On the selection ... D039YD112
TI should be done at Cr2 4 0.1 and at P,< 10-3. Since dirpot visual
determination of T, at ffl,