SCIENTIFIC ABSTRACT ARKHANGELSKIY, V.N. - ARKHANGELSKIY, Y.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000102110003-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 6, 2000
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

RIM, N.A.0 vrach; VARIN, I.Ye,, vrach; ARKWGELISKIY V
N prof, j
TZBOTSKAYA.-ROSSELIS, Ye.H,, vrach; MMKIY, Y.G.,
dotsent
(Smolensk); UK=, M.L.,. dotsent; USTINOV, S.D.,
starshiy
prepodavatell gimnastiki
Health hints. Zdarovve 9 no.200-31 F 163. (MIRA 16:3)
(HYGIEB),

k7MMGU.SKIY, V. N.
"Neoplasm of the optic norveO.
Report to be submitted at The Second Congress of
the Suropean
Sooiety of Ophthalmology,, Vienna, Austria,, 7-13
Juxe 19640

ARK'WGEL'SKIY, V.N.,__prof.; BRYANTSEVA, M-K-;
DORYIDOETOVA, K.V.;
- BUNIN, A.Ya.p red.; LYUDKOVSKAYA, N.Lp tekhn.
red.
[Manual on eye diseases] Uchebnik glaznykh
boleznei. Pod
obshchei red. V.N.Arkhangellskogo. Hoskva,
14edgiz, 1963.
1963. 327 P. (MIRA 17:1)
1. Chlen-korrespondent MIN SSSR (for
Arkhangellskiy).

-ARMMGELISRUs V.N.,, prof.
Morphological basis of the change in the color of
the optic
disk in health and in pathology. Vest. oft. 76
no.5:39-49 -
S-0 163. (MIRA 171l)
1, Gla.2naya klinika I Hoskovskogo ordena lenina.
meditsinskogo
instituta, imeni I.M. Sechenova. Chlen-korre6pondent
AMR SSSR.

SIKHARULIDZE, I.A.p zaal. deyatell nauki, prof.,
otv. red.;
BERADZE, N.I., dots., otv. red.; ARKHANGgELLI�~V.N.,
prof,, red.; ABULADZE, V.A., red.; MliUVA, D.N.,
kand.
med. nauk, red.; BOGOSLOVSKIY, A.I., doktor biol.
nauk,
red.; BUNIN, A.Ya.,, kand. med. nauk, red.;
VILENKINA, A.,
doktor med. nauk, red.; VISHNEVSKIY, N.A., prof.,
red.;
ZARUBIN, G.S., nauchn. sotr., red.; ITSIKSON,
L.Ya., kand.
mede nauk, red.; KIIASNOV, 14.L., zasl, deyatell
nauki, prof.,
red.; MACHARASHVILI, P*D., zeal. vrach Gruz. SSR,
red.;
FUCHKOVSKAYA, N.A., prof., red.; RABKIN, Ye.B.,
prof., red.;
RSHZHECHITSKAYA, O.V., kand. med. nauk) red.;
ROSLAVTSEV,
A.V.p st. nauchn. sotr., red.; TARTAKOVSKAYA,
A.I., kand.
med. nauk, red.; FRADKIN, M.Ya.., prof., red.;
KHAYUTIN, S.M.,
prof., red.; CHERNYAKOVSKIY, G.Ya., kand. med.
naukp red.;
CHKONIYA, E.A., kand. med. nauk, red.; SHATILOVA,
T.A.j
doktor mod. nauk, red.; YAKOVLEV, A.A.,
nauchn.sotr., red.
[Materials of the Second All-Union Conference of
Ophthal-
mologists] Materialy Vsesoiuznoi konferentsii
oftallmolo-
gov. Tbilisip Respublikanskoe nauchn. ob-vo
oftallmologov
Gruz.SSR, 1961. 498 p. (111RA 18:1)
1. Vsesoyuznaya konferentsiya oftallmologov, 2d,
Tiflis, 1961.
2. Chlen-korrespondent ANN SSSR (for
Arkhangellskiy).

ARKHANGELISKIY, V.N., prof.
Physiology and pathology of the vitreous body. Trudy 1-go
MMI
32:7-27 164. (MIRA 1815)
1. Zaveduyushchiy kafedroy glaznykh bolezney 1-go
Moskovskngo
meditsinskogo instituta imeni Sechenova.
Chlen-korrespondent
AMN SSSR.

ARULOGILI SKIT. V.N., RZYTLINGXR, S.A.
,
%-- __-It"'-- -lospheric balloons for studying the
atmosphere. Meteor*
Automatic stra
i gidrol no.11:47-50 N 956 (HUtA 10:1)
(Balloons, Sounhng)

AUTHORSs
Arkhangel'skiy, V. N. Sukhotskiy, Ye. I. 5o-58-5-14/2o
TITLEt
A
Now Standard Atmosphere (Novaya standartnaya atmosfera)
PERIODICALs
Meteorologiya i Gidrologiya, 1958, Nr 5, PP- 55-58 (USSR)
ABSTRACTt
The
authors report on the results of the work done by the

committee
organized in 1953 in the Weather Bureau and the

Directory for
Geophysical Research of the Research Center of

Kambridzh (Cambridge,
USA) of the VVS. In 1956 the elaboration

of the above-mentioned
atmosphere up to an altitude of 30o km

was concluded. The fundamental
quantities of the now atmosphere

are represented in figure I and
tables I and 2. The advantages

of the new atmosphere, as compared to
those of 1947, are enum-

erated. The Directory at present is engaged
in working out de-

tailed tables of this atmosphere which shall soon
be edited.

The contents of the tables will correspond to the standard

atmosphere of the International Civil Aviation Organization

. (ICAO)
which was accepted as an international standard. At

the end some
explanations of the standard atmosphere of 1956

and the pertinent
tables (edited in England) are given.

There are 3 figuresp 2 tablesq
Card i/I

1. Atmosphere--Standards

ARKWGILISKIY, Y.T.
-
with galvanometric
SSR 2:195-201 56.
for frequerey characteristic@
recording. Trudy Inst.f.izA
(Seismology)
of seismographs
geofiz.Alf Turk.
(KLRA 10:3)

ARKHANGELISKIT, V.T.
*M,-- seismic inclinometer with galvano-
metric recording. Trud7 Inst. fiz. i geofix. AN Turk. SSR
4:3-8 158.
(MIRA 11:9)
(Saismotetry)

87966
S/049/60/600/010/002/014
E133/E414
AUTHOR: Arkh""lls-kiv. V'.T.
TITLE: On the Theory of a Long-Period Vertical Seismometer
PERIODICAL: Izvostiya Akadenii nauk SSSR, Seriya geofizicheskaya,
ig6o, No,109 P001432-1441 -
TEXT: The author uses the term "neismonoter" to denote that part
of the seismograph which detects earthquakes as distinct from.the
recording apparatus, There has been considerable recent Interest
in long-period seismic waves, A typical seismomet*r pendulum in
the USSR has a period -12.5 sec. To study long-period waves, it
in necessary to lengthen this to at least 30 see. This can be
done fairly easily for horizontal seismographs, but vertical
seismographs become unstable even for periods as short as 15 to
20 see, The instability occur* because of a strong dependence of
the period on the equilibrium position of the.pondulum and on the
amplitude of the oscillations. The author sets up the
differential equation for the motion of a vertical seismograph
pendulum 9"
Card 1/8 Ke a M(Q)

87966
s/o49/6o/ooo/olO/002/0l4
E133/B414
On the Theory or a Long-Period Vertical Seismonster
for a typical seismograph (cr Pisa). Retaining the first rour
terms in the Maclaurin expansion or M(Q), he arrives at the
differential equation (10) for 9 which has the solution
0 a A sin (nt, + f#) (11)
where n in dorined by
M, (0) M. (0) MW (0) (12)
K + zM, (U) 0+ _UAF_(TJ
The angular frequency (no) as 0-40 in given by
Card 2/4

~7pM
S/049/60/000/010/002/014
E133/E414
the Theory of a LangoPtriod Vertical Seismometer
.Writing this in terms of the corresponding period (TO)
tq*(18) now becomes
3 At, (0) To, Oo- M- (0) T"
24nsjr (14a)
Who tits torms Ivisi44 tht brackots are.snall, Eq.(14&) can bv
!written *a
At' (0) Ts AP (0) 71
TO+ a+ (15a)
or T a To'+ AIT. A2T.
!Card 3/8--

87966
5/049/60/000/010/002/014
E133/E414
'On the"Thoory of a LonS-Period Vertical Seismom*ter'
iFor M"(0) > 09 the effect of the 61T. term is to decrease the
;upper halt of the oscillation and creams the lower half. Ibis
:term in proportional to 9 and Tr if M It, (0) >0, the
.effect of the 42T. term is to Increase the amplitude an the
:squar* of 9 Next, the author considers the pendulum
~parameters on which M"(O) and M110(0) depend. He finds that
:M11(0) a 0 for either of the conditions
too (a + &/b
'or (24)
coo (01 a b/ai
Soismometer arrangements which satisfy these requirements are
shown in Fij,5. The values of M111(0), which correspond to the.
two cases illustrate,4 are given by
Card 418

S/04 9/4 000/010/002/014

9133/9414

On the Theory of a Long-Period
Vertical Seisnometer

2 &,)
A1'w(O)=a'O 1+ (24'a)

(24b)
M (0) bsc
+ (246)

S.

t

However, in practie*,
these arrangements give periods which
are-"

only of the order of
two seconds. In order to increase
the,periodi

of free oscillations,
Richardson (Ref,2) has suggested the
use of a,

0
second spring which.oboys the relationship: ati + Ol -a
180%

2

It is found that the
period can be increasedby altering the
To I

length of the second
spring, It is also possible to make

45jLTO a 0
and to decrease the dependence of period on

amplitude. However,
oicing
to the constructional complications

introduced, a second
spring is
seldom used. The author next
21

consider* the use of
a single spring of
taro initial length

0). He finds
that, in this case, the period hardly
changes

Card

87966
S/049/6010001010/002/014
2133/E414
On the Theory of a Long'Poriod'Vertical Seismometer
even for'larse oscillations. The initial length is defined a.*
2
.z T
47x2
40
5
The period of free oscillations is given by
A
2' (34)
X~ Y-tg 50
9
This equation shows that the period can be increased if I
X/mRo in increased or It a + F tends to 90% The latter
C As of no practical importance-as the period then tends to
infinity, It is found that small changes in the equilibrium 55
position of the pendulum do not affect the-period. The author
concludes that the best practical approach is to us* a suspension
Card 6/6

gem-
87966
S/049/60/000/010/002/014
E133/E414
On the Theory of'&'Long-Period'Vertical Saismometer
10
spring of zero initial length. There should be various possible
attachment points for the springand the upper point of
attachment should be easily movable, both in the direction of the
b-coordinat* and in a directift perpendicular to this and to the,-.
axis of rotation (Fig.50- It is suggested that for ease of
construction oither * a SZ 0, 90* (Fig.5b) or
M 01 a V 9 (Fig.5c) should be used, The spring should be
made of a material wit1v low coefficient of expansion. The
apparatus should not be affected by pressure changes, I.e. the
20 disposition of volume about the axis'of rotation should be
symmetrical. There are 5 figures and 7 references: 2 Soviet.
and 5 non-Soviot.
ASSOCIATION: Akademiya nauk SSSR Institut fiziki zenli
25 Academy of Sciences USSR Institute of Physics of
the Earth)
SUBMITTZD: May 18, 1960
Card 7/8 - --

S/04 61/000/005/004/013
D218YD306
jangel's dy
AUTHORS: Arkl Kirnos, D.P., Popov, 101.1
&nd 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, ~70-675
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 SizfRropoll. The authors briefly
report
on a prototype vertical seismograph which was designed for
detect-
ing seismic waves with periods between 20 and 300 sec. The
instru-
ment is a modification of a vertical 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, Ber. geofiz., no. 10, 1960). The
pendulum
Card 114