SCIENTIFIC ABSTRACT FLIDLIDER, G.M. - FLINT, V.YE.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000413320016-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S1 1 03Y2,0
r
61/022/011/011/014
D~
Dynamic characteristics of ... D271 D306
l + (1 Be )pTe
o 1 + pT e (15)
v
where
k
8e (16)
For a full c~ linder 3 = 0.69 and for a flat disc 8 = 0.81. From
(12) and (15 time characteristics are obtained; for high frequen-
cies
a -VFt
1 Y-7- (17)
where
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S/103/61/022/011/011/014
Dynamic characteristics of D271/D306
(t) 2 t
"(t) = -10 and a t=
ti k (1+ 61p Te
+ 5J.) _T_
for low frequencies
V2(t) 1 - 2ee-T (18)
The boundary point between (17) and (18) is 3*(Tain)P40#5 andp ap-
proximately, tein = 0#465 T,# The characteristic of the clutch is a-
parabola of 0.5 order at high frequencies, and an exponential of
second order at low frequencies. Similar expressions are obtained
for the voltage supply case; time characteristic is of the type
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Dynamic characteristics of ... D271/D306
fet I -Ae Pit - BeP2 t
IT :--
(23)
When the clutch is switched off time characteristics can be.ob-
tained by subtracting (17) and ~18) from unity, kmplitude and phase
characteristics are obtained directly from (12 and (15) by substi-
tuting p = J&). Logarithmic characteristics are: for high frequen-
cies
20 1g [W1 [4 + 10 lgzaTJ
for low frequencies
(34)
20 19 [W2 (0)] = 10 lg[j + (1 13)2&)2 Tj- 10 lg(l +(02 T2) (35)
The bandwidth of the clutch as determined by the level of 10 - 14 M
is 4 - 10 units of relative frequency. The equations of the charac-
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)6127
0
S/103 22/011/011/014
17
Dynamic characteristics of D271/D306
teristics are also given for M = KMf' and n / 1. A complete engi-
neering calculation of a clutch is given in the appendix: The re-
luctance of the magnetic circuit is first found, then the equiva-
lent time constant and the cut-off frequency at 12 db level; from
the ratio of the control and equivalent time constants, the need
for forcing the control is determined. There are 5 figures and 8
references: 6 Soviet-bloc and 2 non-Soviet-bloc. The reference to
the English-language publication reads as follows: H. Hernev Journ.
of the Iron and Steel Institute, v. 172, XII9 1952t p. 4.
SUBMITTED: August 31, 1961
Card 9/9

TATUR, O.N... inzb. j FLIDLIDER M... inzh.
j
Dynamic obaracteriBtico of high-speed electromagnetic
clutches. Vast. elaktroprom. 34 no.7:13-20 31 163.
(MIRA 160)

IL'ICIIEV, Dmitrly Dmitriyevich; TATUR, Oleg Nikolayevich;
FLIDLIpp, stlye ED:-YSK-IY,
- -Pr~gpr~iy Maksovic1h. Frinimal uchas
.M.; ANOSOV, lu.0.4. red.j CHILIKIN, M.G., prof.. red.
[Systems with electromagnetic clutches) Sistemy s elektro-
magnitnymi muftami. Moskva, Energiia, 1965. 96 P.
(MIRA 180)

FLIEGM, Nandor
. '- ~ ~
Properties of Hungarian-4aade welding materials and description
of their fields of application. Elelm ipar 17 no.17t343-348
N163*
1. Gsepeli Femmu Elektrodagyara.

MEGER Nandor
Y
Pre8ant atate of welding material production in Hungary.
Gap 16 no. 3tlll-117 Mr 164.
1. Heal, Plectrode Factory of the C2spel Me-talworks.

U7 1,DPTA -' MICIA See 6 Vol 13 /7 Intprnal Led. 011 ~Q
3995. THE SYMPTOMS OF ALBERS-SCHONBERG DISEASE IN THE ORAL
CAVITY - Objawy choroby Albers-Schoenberga w Jamie ustnei - E11SjLe _rS
Klin. Chir. Stomatol. A.M.. Wroctaw - CZAS. STOMAT. 1957. 10/4 (195-202)
Illus. 12
A:tase of a 50-year-old man is described in whom the recurrent inflammation of
the jaw bones was finally traced to osteosclerosis fragilis generalisataorAlbers-
Schonberg disease. In addition the defects in the development of the jaw boneft
and dentition In 4 siblings affected 'by the disease are reported. Japa - Krakow

FLITII-CIIIR' Z.
Supplementary cquirment for cutting progressive wom-gears.
P. 314, (Strojirenska Vyroba) Vol- 5, no. 7, July, 1957, Praha, Czechoslovakia
SO: Monthly Index of East European Acessions (EEFAI) Vol. 6, No. 11 Novenber 1957

FLIECL, J.
"Breeding of plants to make them frost resistant."
VESTIIIK. Praha, Czechoslovakia.. Vol- 5, No. 7/8, 1958-
Monthly List of East European Accessions (EE~I), LC, Vol. 8, No. 9, September 1959.
Unclassified.

SOV/109-59-4-2-7/27
AUTHOR: Allpert, Ya.L., and -iiieiLL2At-
TITLE: Synthesia of the Shape of the Atmospherics and. the
Effective Parameters of the lower Portion of the
Ionosphere at Low Frequencies (Sintez formy
atmosferikov i effekbivnyye parametry nizhney chasti
ionosfery na nizkikh chastotakh)
PERIODICAL:Radiotekhnika i Elekbronika, 1959, Vol 4, Nr 29
pp 202-211 (USSR)
ABSTRACT: The article gives the results of a theoretical
evaluation of the shape of the atmospherics (produced
by lightning discharges), E(t,r),.and compares it with
the actual signals received from distances ranging from
500 to 3,000 ka from the source. The synthesis of the
atmospherics is defined as the determination of the
signal E(tr) at t1ze point of observation situated at a
distance r from the source. This is equivalent to the
evaluation of the Fourier integral:
00
E(t,r) g(W9r)Qo(W2O)e iWt dw (1)
27r S.
-X0
Card 1/4 where g is the electric or magnetic field over the
o. M

SOV/109-59-4-2-7/27
Synthesis of the Shape of the Atmospherics and the Effective
Parameters of the Lower Portion of the Ionosphere at Low Frequencies
earth surface, having a frequency w, which is produced
by a dipole of unit intensity; this is defined by Eq (2).
The function % is the spectral density of the radiation
source, which is defined by Eq (3)~ As was shown earlier
by the authors (Ref 1 and 4).,the. function Qo can be
defined by a svandard source whose amplitude and phase
components are given by Eq (3a). The wave numbers kSn
and other parameters of Eq (2) can be evaluated
approximately (Ref 3) by employing Eq (4) where h denotes
the height of the ionosphere, N is the electron
concentration in the ionosphere and -4 is the number of
electron collisions. In these equations it is assumed
that the waves are propagated in a wa"'eride. formed by
the earth surface and the ionosphere (R f 3). The above
equations were lased to evaluate NI-49 Soll S02~and p as a
function of frequency. Results are shown in able 1.
On the basis of Eq (1) and Eq Oa)', the received signal
can be written in the form of Eq (8) or as Ea (9).
Since t-he sub-integral fun-,tion of Eq (9) can be written
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S07/1003-59-4-2-7/27
Synthesis of the Shape of ths Atmospherics and the Effective
Parameters of the Lower Portion of the Ionosphere at Low Frequencies
the received signal oan be vepresented by the series of
Eq (11). Eq (101) and (11) can be employed to evaluate
the signal E(t,r). The recorded signals and the
theoretical approximations are shown in Fig 2r A and 4.
The analysis-of the signals is illustrated in Fig 5,
where the full auinxes --orrespond to the theoretical
values, while the dashed curves were obtained from the
analysis of the measurements. From the measurements and
the theory,., it is concluded. that in 30-60% of the cases
observr-,d, the shape of the received signals corresponds
4-
to the tfieoreI-;-ical model,. From -this it follows 'hat for
most cases, 'the theory of the ionosphere proposed by the
authors (Ref 3) is -Icrrect. Tt was also foun-d that for
the propagation distances of over 2.000-3,000 km. tihe
theoretical signals seldom coiniAcLe with the shape of
Card 3/4 the received atmospheri--s. The causes of this discrepancy

SOV/109-59-4-2-7/27
Synthesis of the Shape of the Atmospherics and the Effective
Parameters of the Lower Portion of the Ionosphere at Low Frequencies
are not, as yet, understood. There are 5 figures,
2 tables and 9 references of which 5 are Soviet,
3 English and 1 German.
ASSOCIATION:N.-i. in-t Zemnogo Magnetizaa, Ionosfery i
RasprostraneniyaRadiovoin (Scientific Research
Institute of the Earth Magnetism, Ionosphere and
Radiowave Propagation)
SUBMITTED: 14th August, 1957
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AUTHOR: Fligell, D.S.
TITLE- Synthesis of the form of atmospherics
SOURCE: Akademiya nauk SSSR. Institut zemnogo magnetizma,
ionosfery i rasprostraneniya radiovoln. Trudy, no.17
(27), Moscow? 1960, Rasprostraneniye radiovoln i
ionosfera. 27-49 -*
TEXT. A brief preliminary description of the present work was
reported by Ya.L. Allpert and the present author in Ref.8
(Radiotekhnika i elektronilia, V.4, 202, 1959) and by Ya.L. Allpert
in Ref.9 (Usp. fizich. nauk, v.60, 369, 1956). A more detailed
account is given in the present paper. The research is said to be
similar to that reported by J. Wait (Ref-71 N.B.S. Report 5513,
September 3, 1957). It is stated that Wait's work became known to
the present author only after the present research had been
completed, although a preliminary account was published prior to
the publication of Ref-7. The author has computed atmospherics at
various distances from the source, taking into account the
necessary number of modes and the dependence of the effective
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conductivity of the ionosphere on frequency. The computed and
observed forms of the signals are compared, and it is shown that
this comparison is capable of producing information about the
effective conductivity of the ionosphere. Although the method is
in principle suitable for practical purposes, it is stressed that
its accuracy can only be estimated by direct measurements of the
effective parameters of the ionosphere. The analysis.is based on
the following considerations. The form of the signal received at
a distance r from the source can be computed by evaluating the
Fourier integral
+00
E(t,,r) = 1 g(w,r)Q 004,0)e iWt dw (1)
25% _~
OD
where 2
g(w,r) = B(w,r)e -iQ(W,r) = i29Tk
h
00
S2H (2) (krS )P(C
n 0 n n
n--0
(2)
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is the electric or magnetic field of frequency w above the
earth's surface, and
Q 0) A 0) IYOO", 0) (3)
is the spectral density of the radiation emitted by the source in
its immediate neighbourhood. It is shown that the problem can be
reduced (approximately) to the evaluation of an integral of the
form
co
E(t,r) B(w,r) A (w,O) cos (wt + y) dw (7)
U7- ~ 0
0
Fig.14 shoirs,a typical comparison between an observed (a) and
calculated ( ) atmospheric for r = 1000 km. It is found that the
calculated atmospherics are nearly identical with the observed
atmospherics in 40-60% of cases, which must mean that the effective
parameters of the ionosphere which are assumed in the calculation
must be very nearly the same as the actual parameters. There is
some evidence of a discrepancy between the theoretical and the
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Synthesis of the form of atmospherics E032/E114
experimental forms of the atmospherics at larger distances r.
It is stated that this will require further analysis.
Acknowledgments are expressed to Ya.L. Allpert for directing this
work, to S.V. Borodina for advice, and to V.I. Krayushkina for
assistance in the calculations and in setting up tables and graphs.
There are 24 figures, 8 tables and 12 references: 6 Soviet-bloc and
6 non-Soviet-bloc. The four most recent English language
rieferances read as follows:
Ref.5.- J. Barlowq G. Frey, J. Newman, J.' Franklin Inst., v.258,
187, 1954.
Ref.6: K. Budden, Philos. Hag., Y.42, 1-19, 1951.
Ref.7i as in text above.
Ref.12s L. Lieberman, Jo Appla Physo, v.27, 1473, 1477, 1956.
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4- .
0
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?,Woo S/57o/6o/ooo/ol7/004/012
& ~/a 0 E032/E114
AUTHORS, Borodina, S.V., Kalinin, Yu.K., Mikhaylova, G.A.,
and Fligell, D.S.
TITILE.- A review of the present state of research into the
propagation of ultra-long electromagnetic waves
SOURCE: Akademiya nauk SSSR. Institut zemnogo magnetizma,
ionosfery i rasprostraneniya radiovoln. Trudy,
no.17(27). Moscowq 196o. Rasprostraneniye radiovoln
i ionosfera. 130-172
TEXT: Long and ultra-long electromagnetic waves are defined
as those with wavelengths between 3 -.5 and some tens of
thousands of kilometres. Part I of this paper is concerned with
a review of the theory of propagation of ultra-long radio waves,
beginning with G.N. Watson's paper (Ref.1: The transmission of
electric waves round the earth. Proc. Roy. Sot., v.95, 546, igig).
It is indicated how the various equations formulated to describe
the propagation of electromagnetic waves in the earth-uniform-
ionospheric wave-guide can be evaluated. This is followed by a
summary of the methods which can be used to take into account the
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finite conductivity and the spherical shape of the earth. A review
is then given of attempts at the synthesis of atmospherics, among
them the theories of Fligelt (present Symposium, 27-49) and
J.R, Wait (Ref,18: The propagation on very low frequencies to great
distances. NBS Report v.5513, September 3, 1957)-
Part II is concerned with the experimental studies of the
propagation of long and ultra-long radio waves. Experimental work
on the amplitude and phase of these waves as functions of distance
and time is summarised. Direct measurements of the field-strength
and the diurnal variations in the propagation of the GBR signal
are reviewed. An account is also given of the results obtained
by indirect methods, e.g. lightning discharges, analysis of the
spectrum of atmospherics by the tuned rece�ver method and studies
of the tails of atmospherics. It is concluded that the
experimental study of the propagation of long and ultra-long radio
waves has confirmed the basic idea of the wave-guide theory of
propagation. Direct measurement of the field-strength at 3000 km
from the source showed that interference effects are present up to
r = 1000-2000 km and are due to the large number of modes taking
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part in the propagation. As the distance increases some of the
modes are attenuated and the field amplitude falls off
exponentially but remains relatively large. Direct measurements
of the frequency stability of the GBR signal showed that the
daytime stability at r = 5000 km is 10-9 over a period of several
months and 10-10 over a day or two. At the antipodes, the
frequency stability is of the order of 10-9 per hour. Indirect
measurements confirm the results of direct field measurements but
in a wider frequency range, namely, 500 cps - 50 kc/s. Analysis
of the waveform of atmospherics showed that the wave-guide formed
by the earth and the finite-conductivity ionosphere,has certain
selective properties. At 7 - 15 kc/s and 100-200 c.p.s. there is
energy transmission with minimum attenuation. At 2 - 3 kc/s there
is maximum absorption. The attenuation at 10 kc/s is greater by
10 db than at 2 - 3 kc/s. The ratio of the maxima in the spectrum
of atmospherics on 10 kc/s and 100 c.p.s. varies with distance.
At 500 km the maximum on 10 kc/s is 20 - 30% larger than on
100 c.p.s., while at 2000 km this difference disappears altogether.
The signal level on 7 - 15 kc/9 is subject to appreciable diurnal
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and seasonal variations. During daytime the signal level is lower
than at night; during summer it is higher than in winter. The
spectral region 40 - 200 c.p.s. exhibits small diurnal variations
showing good propagation conditions both during daytime and at
night. However, it appears that the difficulties encountered in
the design of transmitting antennas on these frequencies cannot be
overcoma, The phase velocity in the frequency range I - 20 kc/s
varies irregularly in the neighbourhood of c. In the frequency
range 10 - 20 kc/s, the average phase velocity is practically
independent of frequency and differs from c by fractions of a
percent. As the frequency is reduced the phase velocity becomes
appreciably greater than c, for example, at 2 kc/s the phase
Yelocity differs by 10% from c. As the distance is increased
from 1000 to 3000 km, the differences from c are appreciably
reduced and are equal to a few tenths of a percent. The effective
parameters of the lower ionosphere have been determined for larger
distances where the zero mode predominates. The experimental
values obtained for the ratio of the electron concentration to the
collision frequency are found to be in good agreement with the
theory of Ya.L. Allpert and S.V. Borodina (Ref.19- present
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A review of the present state of ... S/5RAO/000/017/004/012
E032/EI14
Symposium, 3-26) right down to 3 - 4 kc/s. Thus, direct and
indirect studies have shown the propagation of ultra-long radio
waves to distances of 3000 to 5000 km as relatively stable during
daytime but somewhat less stable at night. The propagation of
.-adio waves with frequencies below 1 kc/s has not as yet been
adequately studied either theoretically or experimentally. Direct
measurements of the phase velocity as a function of distance and
of the effect of the earth;s magnetic field on the propagation of
ultra-long radio waves is of major practical interest. It is
stated that there are no published results in this field.
Acknowledgments are expressed to Ya.L. Allpert for advice and
to Yu.G. Ishchuk and G.M. Sosnovskaya for assistance during the
writing of this paper.
There are 23 figures, 5 tables and 107 references: 10 Soviet-bloc,
I Russian translation from a non-Soviet-bloc publication , and
96 non-Soviet-bloc. The four most recent English language
references read as follows:
Ref-71: A.D. Watt, B.L. Maxwell. observations on some low-frequency
propagation paths in arctic areas. Trans. IRE v.AP-6,
no-3, 308, 1958.
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Ref.81: J. Tantry. Automatic atmospherics-waveform recorder.
Indian J. Phys, v-32, 367, 1958.
Ref.84: J. Chapman. The waveforms of atmospherics and the
propagation of very low frequency radio waves.
J. Atm. Terr. Phys., v.11, no.3/4, 223, 1957.
Ref.101: F. Hepburn. Atmospherics with very low frequency
components below I kc/s.
J. Atm. Terr. Phys., v.10, 266, 1957.
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AUTHORS: Borodina, S.V., Kalinin, Yu.K,, Mikhaylova, G.A. and
Fligell, D.S.
TITLE% A Review of the Present State of Research into the
Propagation of Very Low Frequency Electromagnetic Waves
PERIODICAL: Izvestiya vysshikh uchebnykh zavedeniy, Radiofizika,
1960, Vol 3, Nr 1, Pp 5-32 (USSR)
ABSTRACT: This is a review paper treating both theoretical and
experimental problems., In the first part a rel,iew is
given of calculations on the propagation of electro-
magnetic waves taking into account irregularities in the
\4/ ionosphere, the finite conductivity and the spheroidicity
of the earth. In the second part a review is given of
experimental studies in the frequency range 10 cps to
50 Kc/s. Above 3 Kc/s there is good agreement between
experimental and theoretical data, It is pointed out
that it is necessary to develop a general theory of
propagation of very low frequency electromagnetic waves
Card 1/2 taking into account both the spheroidicity and the finite.
gmamwj
A- R
f 12.tst.'A"~ tli*L
a

69410
s/i4i./60/003/01/001/020
EOVE414
A Review of the Present State of Research into the Propagation of
Very Low Frequency Electromagnetic Waves
conductivity of the earth, particularly above 3 kc/s.
The review is based on 109 published papers,
Acknowledgement is made to Ya.L.Allpert, Yu.G~Ishchuk
and G.M.Sosnovskaya for their help, There are 14 figures,
and 2 tables and 109 references, 11 of which are Soviet
and 98 Western,.
ASSOCIATION:Institut zemnogo magnetizma, ionosfery i rasprostraneniya
radiovoln AN SSSR .(Institute of Terrestial MaSn2_tj--%m_,
Ionosphere and the Propagation of Radio Waves, AS USSR)
SUBMITTED: September 19p 1959
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&
0119
-0,
V'-

FLIGELI . D.S.
Properties of the coefficients of refraction, attenuation and the
coefficient of passing through the ionosphere at low and
ultralow frequencies* Geomag, i aer, 2 no-5:886-903 S-0 162.
WIRA 15 i 10)
1. Institut zemnogo magnetizma., ionosfery i rasprostraneniya
radiovoln AN SSSR. .
(Ionospheric radio wave propagation)

A(;(;:Z3ION THU A21013137 s/b2o3/64/bo4/bol/bo41/bo53
AUTHORS: Fligell, Do So; Adleva, Go
MU: Properties of the 'coefficients of refraction, extinction,, and transmission
I
of the ionosphere at low and ultra-ldw frequences at night
S(YJHCE: Geomagnetizm i aeronomiya, v. 4, no, 1. 1964,, 41-53
TUPIC TACIS: refraction, refractive index,, extinctiop, extinction coefficient,,
transmission, transmission coefficient,, ionosphere, low frequency,, ultra low
frequency
ABSERACT: The authors present the results of computing the index of refraction
(n), the extinction coefficient (x), the transmission coefficient (S.),, and the
average phase velocity (vd in the range of 1-100 000 cycles for a model of the
nigl-rt ionosphere. They have shown that these values gradually change with increase
in the angle 9 between the wave normal and the earth's magnetic field vector until
the angle reaches appr6ximately 600. At a frequency of 100 000 cycles and a
height of 3000 km n and x begin to change markedly at 9;6 760. At lower frequen-
cies the angular dependence does not become noticeable until higher angles. At
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ACCESSION NHt APhO13137
frequencies of only 1-100 cycles, n and x remain praotical3j unchanged.on increase
in 9,.-The coefficient of transmission decreases with increase in 9, A very sharp
increase begins at 9 > 600. At low angles the waves pass through the night
ionospl-.Gro with pracitically no loss for frequencies ranging frop one to almost
100 000 cycles. "We consider it our duty to express our thank& to Ya, L, Allpert
for suc-resting, this topic and for his guidance in the work." Orig. art* hut 10
figures and 3 tables,
ASSOCIATIONs Institut zemnogo magnetizma ionosfery* i raorostrananiya radiovolzi
AN SSSR (Ins4itute of Terrestrial Magnetism., Ionosphere, and Propagation of Radio
Waves AN SSSR)
SUTNITTED: O6Dec62 -DATE ACQ: O2Mar64* EML 1 00
SUB CODEt AS, PH
NO RU SOV: 004
OTHER t 001
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L 17778-66 kNT(4)/E-wT-(i)LE~~-qk)m-2/-FgpJwA(h~. RBIWIWS~2_
[AM-1 ~.M06663 SOURCE CODE: UR/0203/66/006/OOli6697/0
AUTHOR:
ORG: , I
AN SSSF
SSSR)
Guseva, E. G..; Fligell, D. S.
~titute of Terrestrial Magnetism,
W eand jo
Sm I= hu bF
Institut zemnogo magnetizaa, ionosfery i rasprostraneniya radiovoln AN
TITLE: Calculations of low-frequency electEgaaaetic wave Eropagation in"an Earth-
ionosphe waveguide
SOURCE:* Geomagnetizm i aeronomiya, v. 6, no. 1, 1966, 97-104
TOPIC TAGS: geomagnetism, electromagnetic wave propagation, waveguide
:,ABSTRACT: Theoretical calculations of the amplitude and phase velocity for low-fre
quency electromagnetic waves in the 1-30-kc region near the surface of the Earth
for plane and Spherical Earth-Ionosphere waveguides are compared with experimental
data. Curves for the phase velocity as a function of frequency show nearly identi-
cal forms for both the plane and spherical waveguide approximations. However, in a
~plane waveguide vlo is always.greater than 1 (where V is phase velocity and c is
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the speed of light) and approaches v&y.aaymptotically with an increase in fre-
!quency. In the spherical waveguidesv/d gradually decreases with frequencp be-
icoming equal to and then less than .unity. Curves for VIc as a function of distance
;calculated for the'plane approximation show that the phase velocity is close to the
1speed of light and changes irregularly with distance. Experimental and theoretical
Idata are compared.for -the average phase velocity as a function of frequency. These
!curves show good agreement for'calculated and empirical values of VIc down to fre-
lquencies of 5-6 kc. There is a considerable divergence between theoretical and ex-
perimental data at frequencies below 3-4 kc. Curves for the amplitude spectra of
Ahe electric field component at various distances from the source show general
agreement between experimental and theoretical data at frequencies above 2-;-3 kc. Th(
theoretical spectra are somewhat wider and shifted toward the high-frequency sides
which may be due to improper selection of parameters. A comparison of data for
field amplitudes shows good agreement.up to distances of 3000 km. This satisfac'-
tory coincidence is ne arly t he same for the plane and the spherical approxim 'ations.
,The data show that sphericity has little effect on calculations of electromagnetic
Iwave propagation at low frequenciesjso that the simpler formulas'of the plane ap-
:proximation may be used,, The results also show that the magnetic field has little
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ACC NR: AP6006663
effect at frequencies of 16-30 kc. In conclusionsthe authors thank Ya. L. Allpe!rt
who proposed the topic and. guided the work. Orig. art. has: 8,figures, 1 table,~
-and 6 formulas. (141
SUB CODE: /7, 0,9. SUBH DATE: 02Dec64/ ORIG REF: 007/ OTH REF: 008
ATD PRESS:

ACCESSION NRs AR4033682 8/0189/64/000/002/033/033.
SOURCE: Refs zh# Geofiso, Abso 2AI72
!AUrdORs Fligell, M. Do"
iTITLEs Radio wave absorption in the ionosphere as indicated by data for Wirwjy,.
station
CITED SOURGEg Doklo Nauohns aimposiuma po iononfers, 1960; Rostov-na-Donup
Rostovsk, un-t, 1961, 54-61
ITOPIC TAGS% radio wave, radio wave absorption, ionospherej, ionospheric radio wave
'Absorption, solar activity, magnetic activity
!MINSLATION: The article describes the results of measurements of absorption (L) b~
the pulse method at Uirnr in the period July 1957-Decombor 1968 (working frequen-
go//
lcioz 1.9, 2.2 and 2.6 8). The diurnal viriation of L in approximated well by
P~-.Uula (005 Where n changes from 0*2 at the equinox to 2*0 in winters The
tr6nd of moan monthly values of midday values L is'similar to that at Dikson Island
and ha:; no obvious relationship to oos A relationship is noted betnen varia.
tiozz L and solar and magnetpio activitya The observed values L were used to compute
1 2

t~e~w~, 4-

It
S/203/61/001/005/027/028
A006/A101
AUTHORS: Ben'kova, N.P., Turbin, R.I., Fligel'... M.D..
TITLE: Solar radiobursts at 28 Megacycle frequency on July 12, 1961
PERIODICAL: Geomagnetizm I aeronomiya, v. 1, no. 5, ig6i, 842 - 84,3
TEXT: Cosmic radio-emission at 28 Megacycle frequency is reguarly recorded
at the ionospheric department of IZMIRAN for the purpose of studying ionospheric
absorption. An analysis of the recordings showed -that in some cases chromospheric
flares caused a greater intensity of signals) which was particularly high during
the chromospheric flare on July 12, 1961. The data recorded show that the chromo-
spheric flare,-was accompanied by radiobursts of types II and IV which were strong-
ly different as to time and nature, During bursts of type II and IV, the r-dio-
radiation Intensity increased in the centimeter, meter and 30 Megacycle range (10
meters). This fact does not confirm the concept that the spectrum of type II
bursts rapidly decreases with reduced frequency. The different nature of radio-
radiation during II and IV type bursts confirms E.I. Mogilevskiy's hypothesis on
different mechanisms of generation: plasma, oscillations in the solar atmosphere
Card 1/2

Solarradiobursts at 28 Megacycle frequency ...
S/203/61/001/W5/027/028
A006/A101
in the case of type II bursts, and synchrotronous radiation of relativistic elec-
trons in the case of type IV bursts. There are 1 figure and 2 Soviet-bloc ref-
erences,
ASSOCIATION: Institut zemnogo magnetizma, ionosfery i rasprostraneniya radiovoln
AN SSSR (Institute of Terrestrial Magnetism'. Ionosphere and Propa-z_...,~
gation of Radiowaves, AS USSR)
SUBMITTED: September 11, 1961
Card 2/2

S/203/61/001/005/024/028
A006/.4101
AUMIHORSt Ben'kova, N.P.,_.KligeV , M.
TITLE: Ionospheric disturbances on November 10-17, ig6o
PERIODICAL: Geomagnetizm I aeronomiya, v. 1, no. 5, 1961, 832 - 835
TEXT: Data obtained on magneto-ionospheric disturbances in July 1959 were
compared with disturbances of November 1960 and conclusions were drawn on the
spectrum of geoeffective radiation of the Sun and the nature of disturbances.
The distribution of absorption in the ionosphere from data of 26 stations is re-
presented In graphs, which show also changes in the average hourly values of the
H-component of the geomagnetic field in Moscow, the moments of chromospheric
flares and the-sudden commencement of magnetic storms. It was found that chromo-
spheric flares, accompanied by a higher intensity of cosmic radiation, entailed
absorption of the III order which was oaused by particles with an energy of se-
Y
veral dozens of megaelectron volt. In spite of the high geoefficiency of the
flares on November 10 and 11 (Ultraviolet radiation, radio radiation and corpus-
cular streams) fast and cosmic particles were apparently not generated in them
(qith an energy of ten megaelectron volt and more). When analyzing the intensity
Card 1/2

Ionospheric disturbances ...
S/203/61/001/005/024/028
A006/A101
of corpuscular radiation of these flares an attempt was made of evaluating the
southern boundaries of the penetration zone of corpuscles from the magnitude of
Dst variations of the geomagnetic field. For the active periDi of November 12,
c5 values calculated varied from 53 to 600, whilst the actual boundary of polar
~bisorption attained 460, There are 2 figures, 1 table and 4 references: 2
Soviet-bloc and 2 non-Soviet-bloc.
ASSOCIA.TION: institut zemnogo magnetizma, ionosfery i rasprostrareniy~L radiovoln
AN SSSR (Institute of Terrestrial Magnetism, Ionosphere and Propa-
gation of Radiowaves, AS USSR)
SUBMITIED: August 1, 1961
Card 2/2

S120316210OZ100610071020.
AOO1/A1O1
AUTHOR: Fligel',~M. D.
TITLE: Geographical distribution of Ionospheric absorption
PERIODICAL: GeomagnetAsm and aeronomiya, v. 2, no. 6J.1962, 1091 1094
TEXT: In a previous study of the author, Collection "Ionosferny'ye Issle-
dovaniya" (Ionospheric investigations), no. 10,*AS USSR, 1962, 5, he analyzed
absorption data for 2-Md radiowaves during low magnetic activity periods in
summers 1957 and 1958 and derived a formula expressing absorption as a sum of
t4o components; one of them is.conditioned by the undulatory part of the solar
radiation; the second part, of apparently corpuscu *lar.nature, is somehow re-
lated to geomagnetic latitude. The author reproduces this formula and presents
the values of empirical coefficients entering It. The present article gives
formulae for describing spatial distribution,of absorption for the winter and
the equinox 1957 - 1958. Thus the proposed empiripal. formulae make it possible
to calculate geographical distribution of absorption for 2 Mc radlowaves and.
three seasons, winter, summer, equinox, during t~e'periods of high solar (R~---*50)
Card 1/2

S/203/62/002/006/007/020
Geographical distribution of... AOO1/A1O1
and low magnetic activity. An important conclusion has been drawn that the
structure of the formula propo6ed'turned out to be correct, although there are
some differences due to seasonk variations. The empirical approximation formulae.
represent rather well experimental data, which is seen from the graph given irk
the article. There are 2 tabled'indl figure.
ASSOCIATION: Institut zemnogo magnetizma, ionosfery.'i rasprostraneniya radiovoln.
AN SSSR (Institute of Terrestrial Magnetism, Ionosphere and'Radio-
wave Propagation, AS USSR)
SUFMITTED: June 23, 1962
Card 2/2

AUTHORS:
Bukin, G. V.,Fligel', M. D.
44453
S/203/62/OM/006/009/020
A001A101
TITLE: Winter anomaly in the E-layer of the ionosphere
PERIODICAL: Geomagnetizm I aeronomiya, v. 2, no. 6, 1962, 1103 11o6
TECT: There is a peculiar feature, known as winter anomaly, in the sea-
sonal variation of absorption, which consists iri the following: absorption level
is higher in winter than In summer, the zenith angle of the Sun being the same..
It is assumed usually that this anomaly is due to sporadic formations in the
lower ionosphere. The authors put forward another-hypothesis to explain the
winter anomaly from the viewpoint of the conventional ionization equation. Ana-
lyzing the expressions for ion formation rate I in winter and summer, they came
to the conclusion that electronic concentration is higher in winter than-in
summer at the same value of the zenith angle of the Sun ydue to different rates
of X variation in different seasons. It follows thereof that winter anomaly must
exist in*the seasonal variation of critical frequencies of every regular layer.
Experimental data from 50 stations all over the world were.analyzed and it was
Card 1/2 J
5~ '11
xz-~n 05'~!

S12031621002100610091020
Winter anomaly in the E-layer of the ionosphore AOO1A1O1
found'that'for the most stationt foEwin ..~ roI'~sum- Moreover, winter anomaly was
analyzed for the stations in Moscow and Yuzlino-Sakhal'insk for the periods of
maximum-and minimum solar activity; its existence wa:s established in both. No
correlation was f6und between 6&x1ma of 11 (average monthly number of sunspots).
and foE. Formulae are given to d6termine the values bf I and oc,(effective re-
combination coefficient) from the*magnitude of winter *anomaly. These values
proved to be close to those known from the literature sources. There is compara-
tively smail scatter of the values in different months. There are 2 tables and
I figure.
ASSOCIATION: Institut zemnogo magnetizma, ionosfery i rasprostraneniya radiovoln
AN SSSR (Institute of Terrestrial Magnetis6i Ionosphere and Radio-
wave Propagation, AS'USSR)
SUBMITTED: June 20, 1962
61RRN

FLIGELI M.D,,
Nature of the winter anomaly in ub~;ov GeOmaJ7.
i aero 3 no,4:703-706 J.1-Ag 163, t, 16:21~
1. Institut zemnogo magnetizma, ionosfery i rasprostranyniya
radiovoln, AN SSSR,
4 ~Wt
M~

FLIGELIMAN, F.M., inzh.
Use of phosphate enamels for aluminum enameling. Trudy KIIHeattopproma
no.17s208-220 062. (Nnamel and enameling) (Aluminum) (MM 160)

FLIGZI','.%IANq F.14.j inzh.
Enameling isteel wlthaut prkning. Maubtiostrmiie ne.6979-80
N-D 164 (KIRA 18.-2)

,-, zu." : 'N.
Qvl~ogenetl,, and commarfitivot ansto-itrel data on *'he nf
.ho subutpntla nip-.q, Trvi. - -i ~ 11 1 . .
I y GoS,Inpt. Do i7u(,I-. ~-i-Fi 149,
(?,F.A 114) , 4:.,; "
II i .. 1 ~):,) I

KHTSHOVA, N. A;FLIG'SLIK&N, P. K;AK&TOV, M. Y.
U-1~~~-.~~.id,.a?~f.*,.':,-~-,-,r--,~E -
Treatment with dibasol of the residual stage of poliosWelitin.
Zh. nevropat. palkhtat., Kooky& 52 no.4:42 Apr 1952.(qLML 22:2)
1. Of the Scientific-Research Institute iment, T. I. Turner (D1-
roctor -- M. N. Goncharov).

KHILKOVA, Lidiya Stepanovnal ptichnitsa; FLIGELIMAN, S., red.; WZHDAYYJNA,V.,
tekhn. red.
[I will raise 6000 ducks] Vyrashchu 6000 utok. Kalinin, Ka-lininskoe
knizhnoe izd-vo, 1960. 15 P. (MIM 14:12)
1. Kolkhoz nVelikiy putl" Sonkovakogo rayona (for Khilkova).
(Ducks)
10-0
WRY
MEN ~~:l

VISHNYAKOVA, Ye.S.# inzh.; WCANTSEVA, N.F.p inzh.; BORONICIEV, G.A.,
inzh.,- PITINOVA, L.V., inzh.; FETRUNT11, N.I., inzh.,- YZESNDI,
I.M.p Inzh.; AIIDIWEVA, L.P., inzh.; BISTOWNICII, G.V., inzb.;
RYABININAq A.Lp inzh,; MOSIMIN, V.S., red. gazety; ROMKOV,
A.I.j otv. red.; YUNITSKIY, V.P.p red.; FLIGELIMAII, S.M., red.;
ROZEDAYKINA, V.9 tekhn. red.
[Kalinin Artificial Fiber Combine]Kalininskii korbinat iaWs-
tvonnogo vololma. Kalininp Kal-ininskoe Inizhnoe izd-vo,, 1960.
92 p. (MIRA 15:8)
1. Knlininskiy kombinat iskusstvennogo volokna (for all except
Koinkov, Yimitskiy, Fligellman, Rozhdaykina).
(Kalinin--Textile fibers, Synthetic)

Station for filling sprayers with poison solutions. Zashch. rast.
ot vred. i bol. 8 no.D29-30 A 163. (MIRA 160)
14 Vedushchiy inzh. Zaporozhakogo filiala Vsesoyuznogo institute.
elektrifikatsii sellskogo khozvaystva.
(Spraying and dusting-Equipment)
MM,

FLIGER) N.Ya.; BAZDYREV, A.A.
Mechanized station for preparation of poisonous chemical
solutions. Sbor. nauch.-tekli. inform. po elektr. gellkhoz.
no.16/17:76-80 164. (MIRA 18:11)

FLIGER, N.Ya.
Electric vulcanizing apparatus with automatic regulation
of temperature. Sbor. nauch.-tekh. inform. po elektr.
aellkhoz. no.16/17t8l-84 164. (MIRA 18:11)

-.FLIQER,-Nj4*,,[r:Liher# N*IA~lp inzh.
Electric vulcanizing apparatus with automatic temperature
control. Y44. #11. hoop. 12 no.12t6-7 D 161.
(MIRA 17: :L)

FLIGER., N.Ya. [Fliher, ILIA.], inzh.
Device for the ZID-4.5 engine. Makh. sill. hosp. 13 no.4:26 Ap
162. - (MMA 170)

AUTHOR: Fliginnkiy, A.S. gineer 00V/91-58-3-14/128
TITLE: A Self-Synchronizing Type Synchronoscope for Switching-In
Low Capacity Generators (Sinkhronoskop dlya v1-1yucheniya
generatorov maloy moshchnosti sposobom samosinkhronizatsii)
Exchange of Experience (Obmen opytom)
PERIODICAL: Energetik, 1958, Nr 3, pp 20-21 (USSR)
ABSTRACT: The problem was to find a simple, yet effective method to
control the frequency difference between the operating ge-
nerator and the one to be started and synchronized with the
first. The author tells how he solved the problem, describing
and illustrating the technical and operational characteristics
of his own sYnchronoscope based on self-synchronization. His
synchronoscope can work on 220 or 12 V.
There are 2 circuit diagrams and 1 diagram.
Card 1/1

e v
Certificate intrjducp5z .1
.-T-ilketen' izcbr'c-teniY i tovarnykh znalcov,
-rear; suspension, C a n,4 ar, u r1 i V,~
7'
ir Author' s

5017859
Vsesovuznyy nauchno-is~:Iedov ate i

T .)jlj ti F. - AP5017859
ENCLOSURE!
I '--locking speed --ducer; 2-drive for the locking ~;peed reducer
Ca~d 3 3
A 2~1

FLIKf E.P., inzh.
Precision of the manufacture of the Cardan joint parts
of farm machinery. Trudy VISKHOMA no-44:3-16 164,
(MIRA 18: 2a)

FLjA, GAFANCNI,"fl, A.A. .
IncreaAng the reliability of the Cardnn Joints of agricultural
machinery. Trakt. i sellkhozmsh. no.11;35-38 N 165.
(WRA 18:12)
1. VBosoyuzW nauchno-issledovatmll~ikiy Irmtitut sel'skokic-
zyaystvennogo mashinoutroyenlya.

FLIKKER9 R. (Omsk)
1- ~-
Let's simplify planning methods. Sov. torg. 35 no.2:47-48 F 161.
(MIRA .14:3)
(Retail trade-Accounting)

I '. ".
Metals
Efforts to conserve metal. at the A. A. Zhdanov plant "Krasnoe SoruWvo." Vest, mash. 32 No.
4, 1952.
9. Monthl List of Russian Accessions, Library of Congress, October _Iqck Uncl.
~ay

lnzh.
Interrelation b~-twe-e~nthe carr7ing cable and the contact'vire and
deriving the state equation for chain suspension systems. Trudy MIIT
no-118:5-15 '58- (MIRA 12:2)
(Blectria railroads-Wirea and wiring)

FLUM ~&
.&,,,.inzh.
- - 7W
Bffect of wire beating In contact networks on their strength.
Trudy MUT ne.104:288-297 '59. (14IRk 1229)
wiring)'
(Folectric
rallroads-Wires
and

kkim
!~~Y~ inzh.
Effect of the beating of the carrying cable on the paraneters
of contact suspension. Trudy MIIT no.122:91-102 159.
(YLM 13: 5 )
(Electric railroads--Wires and wiring)

FLINK,, MoV*,,Inzhe
Temperature dependence of the point of inflection of the sag curve
of a freely suspinded wire. Trudy MIIT no.l":208-211.162.
(KM 15:10)
(Electric lines--Overhead)

FLINK,ju.4,. dotsent, kand.takhn.nauk; FRAYrr-LO, A.V. dotsi-nt kand.tek-tin.
.9
nauk; ENGELIS, G.G., lnzh.
Design of semicompensated circuit suspensilms with spring wires.
Trudy WIT no.199:120-129 165. (MIRA 18:8)

FLINSKY, Jan inz
State and development of repair services of rai2xoad whic:1es.
Doprava 7 no.1:8-11 165.
1. Deputy Minister of Transportation.

red.
[ShInthesis and PkYsic&I properties of dimiond; biblio-
graphical index, 1934-19611 .5intez i fizic~eckie svoistva
alraza; bibliograficheskii ukazatell 10/34-196.1. ':o;-,kva,
lzd--vo "hauka"' 1965. 119 p.
1. Akademiya nauk- SSSR. Sektor seti spetsialInykh bibliotek.

FLINT, V.Ye., kand. biolog. nauk (Moskva)
Keeping snakes in captivity. Pr1roda 52 no.8:114-U5 Ag 163.
(MIRA 16:9)
(Snakes)

7
. a ~~4T, V. Ye.
2. U3,31 (600)
4. Cage Birds - Feeding and feeding stuffs
7. Feeding insectivorous birds in winter. 'Est. v slmlole no. 6, 1952.
9. Monthly List of Russian Accessions, Library of Congress, February -1953. Unclassified.

FLINT, V.Te.
- ~-! --l - ~ ~,
Experimental study of the activity of a brood eider. Zool.zhur.
33 no.1:159-161 Ja-F 154. (MLRA 7:2)
1. Biologo-pochvennyy nauchno-iseledovatel'Bkiy inatitut Moskov-
skogo goauaarstvannogo universitata im. M.V.Lomonosova.
(Eider)

KMOMT.UVA, T.L.; FLINT, V.Ye.
Xseping fish in a homemade aquarium. Priroda 43 n0-7:127-128
ji 154. (KLU 7:7)
(Aquariums)
R
Mn
PY %o',
:j

V-YO-;SJIILOVA-KRASsoyA
- .".M- S.A.
Method of observing a flock of titmice. Zool.2hur. 34 no.6:1386-1388
H-D 155- (KLRA 9:1)
I.Blologo-pochvennyy fakulitet Roakovskogo gosudaretvennogo
universitsta imeni H.V.Lomonosova.
(Titmice)

USER/Bioloey - Ecoloa
Card 1/1 Pab. 86 25/37
Authors s Flint, V. Ye.
Title 1 Daily activity of birds in the littoral zone
Periodical i Priroda 44/4,Ppage 113j. Apr 1955
Abstract t The daily,cycle of activity is found to consist of alternating
periods of activ-1ty and rest. The rhythm of this cycle depends on
the influence of different factors - temperature, length of daylight
hours and conditions of the weather, For birds depending on the
littoral zone for sustenance the cycle was foxn-Bd to depend on the
rise and fall of the tides. Three references: 2 Soviet and 1
Amrican (1938 1949).
Institution
Mmitted t .....

FLrNT,V.Ye.
The biology of the common eider. Biul.MOIP. Otd. biol. 60 no.4:
53-62 Jl-Ag'55- (MLRA 8:12)
OYUCKS)

FLIBT. V.Ye.; SYRON, X.R.
Affect of droughts an the distribution Of swine rodents in difftmt
habitats in northern lasakhatem. Biul.MOIP. Otd.biol. 61 no.6:122-123
N,.D 15 6. (141a 10:8)
(KMTAMAY PROVIIES-MICS)

AUTHOR: Flint, V.Te,,, (00=4 26-12-27/49
TITLEt The Eider Duck and the Eider Down Industry (Gaga i promysel
gagachlyego pukha)
1/6
PERIODICAL: Priroda, 1957,4No 12, pp 99-101 (USSR)
ABSTRACT: The eider duck, Somateris. mollissima, is the only one among
all other eider varieties that gave rise to the eider down in-
dustry. The ducks inhabit the coasts of the North Atlantic
and the northern parts of the Pacific and Arctic Oceans. As
typical sea ducks, they thrive in stony shallow waters, build-
ing their nests on rocky or wooded islands. Their worst
enemies are big sea gulls and grey crows. Their downs are ex-
tensively used by people inhabiting arctic regions. They are
well protected in Iceland and their number there is growing
every year. In the beginning of the 19th century Russia was
the greatest exporter of eider downs in the world. The number
of eider ducks has decreased since then, and in many parts in
the USSR they have disappeared completely. In 1930 hunting of
eider ducks was forbidden and a series of reservations establish-
ed on several islands in the Barents Sea and in the gulf of
Kandalaksha in the White Sea. These bird sanctuaries and care-
Card 1/2 ful study of the duck's biology have lead to substantial re-

The Eider Duck and the Eider Down Industry 26-12-27/49
sults. In 1930 Only 475-5 kg of eider downs were delivered at
the state trading posts. By 1957 the amount had risen to over
3,000 kilos. The best way to increase the number of ducks is
to establish special farms where the birds would be well pro-
tected and could build their nests undisturbed.
There are 3 figures.
AVAILABLE: Library of Congress
Card 2/2

FLINT, V.Ye,
._--St-r-U-00.ture of the area of distribution and settlement types of some
suine rodents in northern 11unkhatan [with summary in Rnglish]'
Biul.KOIP9 Otd. biol. 63 no.617-22 N-D 158 (MIRA 12:1)
(SUSTANAT PROVINC39-MICE)

FLINT,, V. Ye., Candidate Biol Sci (diss) -- "The zoological principles of epi-
demiological prospecting (Experiment in evaluating the epizootiological signi-
ficance of an area, on the axample of tularemia in Kustanay Oblast)". Moscow,
1959. 19 pp (Acad Med Sci USSR, Inst of Epidemiology and Microbiology im
Gamaleya),, 200 copies (KL,, go 25, 1959, 131)

FLINT, V.Ye..;.- ZE14SKAYA, A.A.; SIDGROV, V.Ye.
Role of ecological bird groups in the feeding of the tick-
Ixodes persulcatue. Zool.zhar. 38 no.3:476-480 Nr '59-
(MIRA 12:4)
1. Department of Infections of Natural Nidality, Institute of
3pideniology and Microbiology, Academy of Kedical Sciences of
the U.S.S.R. (Moscow).
(Sikhote-Alin' Range--Ticks as carriers of disease)
(ParaoiteB--Birds)

FLINT, V.Ye.
-.Wwww- M-00"PA-Sm ~-
Materials on the fauna of Tuva and outlook for Its stud7- Bi!17.-
Otd. biol. 64 no.2:123-326 Mr-Ap '59. (MIRA 12:10)
(Arzin District--Zoology)

FLINT, V.Ye.
Materials on the biolog7 of the steppe birch mouse (Sicista subtilis
Fell.) Zool.zhur. 39 no.6-.942-946 Te 16o. (HIRA 13-7)
10 Institute of,lpidemiology and Microbiology, M.S,14 Academy of
Medical Sciences., Moscow.
(Kustanny Province--Birch mouse)

,-I-IINT', V.Ye.
Zoological principles underlying epidemioloeca.1 Bur7eys. Zhur.
o~. biol. 2.1 no*5:353-360 S-0 160. (MIRA 13:9)
1. Gamaleya Institute of Epidemiology and Microbiologyp Moscow*
(KUSTAKAY PROVINCE-TULAREMIA)
(RODENTS AS CARRIERS OF DISEASE)

FLINT, V.Ye.
The lizard Ikemias kessleri Strauch, 1876 as a species hitherto
unknown in the fauna of the U9S.S*R* Zool* zhur. 39 no.8:1264
Ag 16o. (XIRA 13:8)
11 Institute of lpidemiology and Mikrobiology, U.S.S.R. Academy of
Medical Sciences, Mosoov.
(Tava Autonomous Province-Lizards)

4LINT--VQYe---- -- -- -
9 0 --,
Biology of the hamster Phodo
,pus roborovskii Satunin, Biul, WjF~
Otd* biol. 65 no.5igg-IM S-0 160, (KLU .13:12)
(.TUVA AUT.ONOMOUS PRdVINCE-HAMTERS)

FLIRT, Y.1a.4-OKILUNC=, B.P., otv.red.; STAKHURSKIT, A.Ye., red.;
BEGICHEVA, M.N., tekha.red.
[Trapping equipment] Orudiia lova shivotnykh. Moskva, Izd-vo
"Detskii mir," 1961. 1 fold. (Prilothenie k shurnalu OIUnyi
tekhnik,* no.7(97)) (KIRA 14:3)
1, ftentrallneys stantal yunykh tekhnikov, Moscow.
(2npp

FLINTt V.Ye.; GOLOT4111, A-N.
Role of the Tannu-01a Range as a zoogeographical barrier and the
origin of the desert-steppe fauna of Tuva. Zool. zhur- 40
no.4:556-567 Ap 161, (MIRA -14:3)
1, Institute of Epidemiology and Microbiologyp U.S.S.R. Academy
of Medical Sciences (Moscow).
(Tuva Autonomous Province Zoogeography)

FLINT, V.Ye.
Hypocollud ampelinus Bp.v a nev genus and species of birds in the
fauna of the U.S.S.R4, Biul., MOIP. Otd. biol. 66 no.1:127~129 Ja-F
161-4 (TEDME.N VALLET-SHRIUZ) (HIPA 140)

FLIET, V.Ye.- GOLOVKINJ, A.N.
Comparative ecological survey of the hamsters of Tuva. Biul. MOIF.
Otd. biol. 66 no-5:57-77 S-0 161. (MIRA 14:10)
(TUVA AUTONOMOUS PROVINCE-MI-ISTEFS)

(AUGUNOV, Yu.D., SAFIYAKOVA, V.M.; KUDRYASH)VA, N.I.; FLINT, V.Ye.;
Ryzfnwvf ~.V.; MALITSEV., Me
Testiqg the effect of a mixture of automobile exhaust gases
andinsecticide dust for the formation of a protective zone
in a focus of cutaneous leishmaniasis. Vop.kraev.paraz.
Turk.SSR 3:153-156 162, (MIRA 16:4)
1. Inst~tut epidemiologii i mikrobiologii imeni N.F.Gamal,6ya,
Moskvfi Okruihnoy gospitall pogran;Lchnykh voyak Tmkmenskogo
okruga jSAND FLIM-EXTERMINATION) (GERBUS-.&TEMINATION)

CHUGUNOV, Yu.D.; FLINT, V.Ye.; MALITSEV, M.I.; KATKOV.. Y.M.; SIDOROV, N.F.
Experiment in mapping the habitat of the greater gerbil vithin
the foci of cutaneous leishmaniasis in southern Turkmenistan.
Vop.kraev.paraz.Turk.SSR 3:157-160 162. (MIRA 16:4)
t
1. Institut epidemJ~logii i mi-krobiologii imeni N.F.Gamaleya,,
Moskva i Okruzhnoy gospitall pogranichnykh voysk Turkmenskogo
okruga. (TURKMNISTAN-~ERBUS AS CARRIM OF DISME)
(TURXWNISTAN-DELHI BOIL)

nINT, T.Ye.
Ornithofauna of Tuva. Ornitologiia no.5sl44-146 162,
(Tuva A.S.S..R.-Birds) (MIRA 16:2)

FLINTj V.Ye.; CHUGUNOVV Yu.D.
YAterials onthe distribution of some birds of Turkmenia.
Ornitologiis, no.5tl75-176 162. (MM l6s2)
(Turkmenistan-Birds)

, FLINT V.Ye.
Hypocolius ampolinua in the U.S.S.R. Ornitologiia no.4:186-188 962.
(MUU 16:4)
(Turkmenistan-Hypooolius)

FLINT., V,Ye.; KRIVOSHMVp V.G~
Changes in the ornithofauna of the Izmaylovo Park during the
last 25 years. Ornitologiia no.5000-308 162. (MM 16s2)
(Moscov-Birds)

CHUGLIFOV, Yu.D,; FLINT, Me.; SAFIYANOVAO V.M.; KUDRYASHOVA, NJ*
Protection of humans fraa infection with zoonotic cutaneous
leishmaniasis in populated pointo of southern Turkmenistan.
Report No.l. Med.paraz.i paraz.bol. no.1:39-43 162. (MIRA 15t5)
1. Iz otdela bolezney s prirodnoy oobagovostlyu Instituta epi-
demiologii i mikrobiolo~ii imeni N.F. Gamalei AMT SSSR (zav. -
prof. P.A. Petrishchova). ---
(DEUrI BOIL) (TURDENISTAN-ANDWS AS CARRIERS OF DISEASE)