SCIENTIFIC ABSTRACT RUDAKOV, N. - RUDAKOV, V.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001445910012-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KOV. K. MIL
S,: r"U(SPNOV, A. -. RUAA YUCHIMIN. A.
Vichire mends stockings. Prom.koop , no.6:11 Je 157, OKRU
(Sewing machin.)

RUDAKOV, k.
Urgent problems. Prof.-tekhn.obr. 19 no-1115-6 N 162.
(MIRA 16:2)
1. Zamestitell nachallniku-Severo-Kazakhstanskogo oblastnogo
upravleniya professionallno-tekhnicheskogo obrazovaniya.
(North Kazakhstan Province--Farm mechanization-
Study and teaching)

V F.
7 iL~ fl~,~ ha k, L-n' -a -Sem-Falatirctr.~-
rEar.-S drins: -ishred s vetliu Serriorr)"
ChuE-,-ichn~-. ./ 'Kurzar.-Sh.-A-.1no'k 1-Ine; line wf.th Ser~-'~~-,-ol-
brarch (Trancro t ikh-)7-VO, Y)26, no. 5, 57-'E~O).
7.T'E
-t-liorrach Libr,
~.r of Congress
!e '-~viet Tra- :7uort~,4 am! Go-rv-.uni cations, B--
Reference De-partment, W' rh- lr)~32, Unclasri-r-2-ad
a

SKORIKY A.D.) inzh.-Inspektor; KANDAKOV, V.; SLYUNCHENKO, M.D., lnzh.;
SEDNEV, A.I., inzh. po tekhnike bezopasnosti (Nebit-Dag,
Turkmenskaya SSR); SHCHFRBAKOV, S., inzh.;,~~A~qV, N.A.
Readers' letters. Bezop. truda v prom. 8 no.11:53-54 N 164.
(MIRA 18:2)
1. Upravleniye Sredne-Volzhskogo okruga Gosudarstvennogo komiteta
pri Sovete Ministrov RSFSR po nadzoru za bezopasnym vedeniyem.
rabot v promyshlennosti i gornomu nadzoru (for Skorik).
2. Glavnyy mekhanik zavode Yacheistykh betonov, Tatarskaya ASSR
(for Kandakov). 3. Nachalinik proyektno-konstruktorskogo byuro
tresta Novovolynskugoll (for Slyunchenko). 4. Upravleniye
11vovskogo okruga Gosudarstvennogo komiteta pri Sovete Ministrov
UkrSSR po nadzoru za bezopasnym vedeniyem rabot Y promyshlennosti
i gornomu nadzoru (for Shcherbakov). 5. Amakinskaya ekspeditsiya
Yakutskogo geologicheskogo upravleniya (for Rudakov).

AKHMETOV, M.M., kand. tekhn. nauk: ANOSHKIN, V.V., gornyy inzh.;
DROZDOVSKIY, N.N., gornrl inz-h.; SHAMSTYMNOV, R.N., gornyy inzh.;
R~tjPAF,,Q-V,,A,F,, gornyy tekhnik, KNYA&-V, V.L., tekhnik
Results of testing electric detonators with a delay interval of
15 msec. Gor. zhur. no-5:3&-39 1W 165. (MIRA 18: 5)
1. Vsesoyuznyy nauchno-issledovatellskiy gornometallurgicheskiy
in3titut tsvetnykh metallov (11or all except Knyazev). 2. Lenino-
gorskly polimetallicheskly kombinat (for Knyazev).

Ime
RUDIUVT, 117. 1. Cand Tech Sci (diss) "Theoretical arA expeH ntal
study of the proGess cl' supercharging in quick-passage piston compressors."
Mos, 1958. 9 -9 (Min of Figher Eduor-tion US61R. Yos Hi6her Tech School im
E. Baivian LINTU), 110 copies
(KL, 13-56, 97)

4TAKOV, II.I.;,.ZAVIYALOV. S.N., takhn. red.,
CThearetical and exper~mentsl investigation of the com,3ressing
process in high-speed reciprocating compressors]. Teore'tteheskoe
I ekaperimentallnoe isslodovanie grotsesen nagnetaniia v
(Moscad.
bystrokhodnom porshnevom kompressore. Moakva, 1957. 117 P.
Nauchno-isaledovatellskaia la'boratoriis d,,rtgatelei. Trud~, no. 5).
(Air compressorU) IRA 11:7)

RUDAKOV, N.P., Cand BiD Sci (diss) "Application
of radioisotoDes Vr the study of~ absonotion lip
arid lnve_-~tigati_on of certain mineral ions in fish and
their marking.11 Len 1958, 15 PP. (All-Union Sci Ris
InsLof Lake and River Isher-i") 150 col)ies
(KL, 39-56, 108)
23

AUTHOR-~ Rudako-;-~ N. P., SOV/20-120-3-621/67
TITLE: A.~cum,..iletion and Lossas --f Calcium by Carp Fingerlings,
DependIng on the Conc-.entiation of Cale-lam Compounds in
~'ae S-~Trou-ndir4 Medlun, (.N~Lkople-niye i poteri kaltslya
-zegoletkam-' kaxpa v za-xislmostli ot kontsentratsii
kal".slyevykh soyedinenly v okruzhayushchey srede)
PERIODICAL.- Df~klady Akademii rvrAk SSSR, 1958, Vol. 120, Nr 3,
pp. 6~1-664 (USSR/
ABSTRACT3 As known, fishes az-. able to assimilate mineral substances
onl- from nutritlon but also from the surroundin-
medlum Immedliately (references I - 5). The marking wlth
isotopes has pro-;ed thig possibility for
~:a arid ph,:,ophoras 'references 6 - 9~. The quantitative
pdrt cf tha problem., however, rema--.-is 1-41.A.-le researched.
Tbis z9fers to the re'Lationsh.:;.p between th,~i absorptien
-~-f th-s. -u'--staa,~;6s and thair .~3ncentratlon ir, the
s~aLer-medlum, F--.z h-16 investigationsthe author used Ca45 I
the f----h were hybrid3 cf the carp with the cyprinus ~drpio
Card 1/4 L~ Th~-Y were divided Int.-, ~,wo groups, one of them was bred

Ac~cumulation and L-~~3ses of Calcium by Carp 3()V/20-120-3-62/67
Fingerlings, Depending,~n the Ccncentzation of
Calcium Comp,:~ands In the Slarr3unding Medium
water-with a high ~60 - '10 mg/liter) calcium content,
the ',-ther one, however, in calcium-poor water (5 - 7
mg/1-iter). A-,c-ording to this, the calcium content 4 n
ihe ash of the first group amounted to 29.12 ~ (not
decalcined fi,--h) and 18,7 % In the second group
(de~~alclned fish). For the Investigation of the calcium
abscrption. the fish were put into solutions of mixtures
of radioactive and normal calcium where they were kept
6 hours. It was proved that the fish absorb the
higher percentage rA calcium from diluted solutions than
from _-oncen~.rated solutions. Decalcined fish accumulate
t 4
total^ !.'aisiun 11,2 - 1..5 mes more intensively than the
ot.her,:3 (figure 11. The accumulation curve of calcium is
slm;.lar to the ad,.!.~)rption-lsotherm. In the second
,~-jcpeximental ser--e6 the losses of calcium after the
tranzfererlce cf the fish into non-radioactive water were
det:erm.,ned,, Aftar ha-i-ing teen. --'n xadioactjive water for seven,
1"-,e;u,-s they were kept In n3n-radlos--tive water for 24 hours.
Card 2/ 4 The calclum concentration amourzed to 10; 4U and 1100,0

P.MU of lvalr;~- jm y Carp SOV/2O-'20-"-62/67
DeT).-1-n11'r.Lr :.:; tt.u of
Compo~-,nd~, in ifka-
mg The hIghes', of radi.,-.active calcium
in 3-.10.iona rilt,h a minimm, content of calcium.
in -) o s a s
An 'nLerrelaticnship Is proved for-the Ic
of 7ctal calcium. In dr-.,--a:LL1uA flah the losses of
rad~~ca~-tlje and total ca-;clum were considerably higher
than In them other.3 (figure 2). There are 2 fi-ures and
16. rk?ferenzag, 10 off which are 6oviet.
ASSOC'LATION;. V&a6oyuznyT nau:ln.~---'asledoi7ate4,.'akiy instl--.ut ozzernogo

yaq--ava (Al'-Union Sc-Pnf,f~c
IL zytnogij khoz- k -
fo-~ Iplm anti R-.I-;r!r F-'ifnerles)
PRESENTED, Febr-,:La-rj 10; 1918, 1-,y Ye. 14. Pa-,;-Iovskly, Meralter, Aaoademy of
USSR
SUBMITTiM. 1958
a r a /4

Accumulation and Losses of Calcium by Carp 3011/20-120-3-62/0
Fingerlinp, De7,end-_'rng on the Concentration of
Calcium Comuound3 in the Surr~Dunding Medium
1. Carp--Physiology 2. Calcium--Absorption 3. Carp--Absorptive properties
4. Calcium isotopes (Radioa6tive)--Applications
Card 4/4

S/169/62/000/011/057/077
D228/0307
AJTHOR: Rudakov, N.P.
Jsotopic affect when deter-mining prinary organic mat-
ter production in reservoirs by the radio-isotope
method
PERIODICA,: Referativnyy zhurnal, Geofizika, no. 11, 1962, 5,
abstract 11V32 (in collection: Fervichn. produlctsiya
morey i vnutr. vod, 11insk, 1961, 214-218)
TEXT: The C14,nzethod of determining the primary productio4-
of reservoirs is widely knoi-m at present. A series of corrections t
is introduced~ in the calculation proce(lure'- among them Vic isotopi6
affect correct ion appears to have the highest absolute magnitude.

n the thermodynam-
Isotopic effect phenomena arise from differences i
ic ana kinetic properties of isotopes. The kinetic, isotopic effect
has much more significance than the thermodynamic, so it must be
considered in tests with labelled atoms. At present, however, avail-
able methods f or calculating the kinetic isotopic effect constants
Card 1/2

7~ Bia gjA_eA0i --d t" ronnow
eys ye ri-eyt
SOURCE: An UkrSSR.' In .stitut f1ziol6 6
sti6n). Kiev -Mauk64a: dumia 1964,,'
izlucheniya (Biological effect of neutron radi
3o-42
Id TAGS- neut X ra dti- a, ct. cardiovascular'
OP ron radiation, y. radi on,-biologics -,effe
T
system, bematopoiesis, rat
neutronsAn!:bj61ojz c-
--ABSTRACT-,-- _c¶t~:L ff_'bf__ and
6t
'ar _Ati 46~(f T 1i
doses on the hematopoietic and c diovascular'systems' 200r,
200 rats 6ighed an average of 146 -9. - Irradiation -took ace in the^ horizontal~-
~pi
channel of a nuclear reactor. In the first series of tests, rats-irere expose 0-,
400-rad doses (reactor power, 4.0 Mw) of fast neutrons an'd.600--r,doses of_,x_rsys-_-
vith a radiation duration of 23.6 min. In,the second series$, animals were lirradiat
with: a fast neutron dose of 175 rad (reactor powers 8 Nw) An the third series
with 200 rad (10 NO, and in the fourth series, with 800.ri_-,The-morphological.-~con-

--5465M5

.66~�dION NR:---"
AT501495T- ENCI

i~eni ~-the periphe ral:~ blood
Table 1--'Morpho~ogicalcol

vne
s ixtrohs..~.
a

indices- nom
t~ day. 8t d hAiA ft day

Hemoglobin

1
8 14,4 jt-~ fA.6 Of 0

0
12 920% ---

137' ISO%-
130 76.8
1
4 .4
M 4646A -
5!9M
641
ytes j
-

t
~oc as
T
em 14820
6
0 7--
1262:, 772814
6 -
05 -06

-- 4474420-

0
6

r,
n ex . . ,
. 0.6

eticulocytes

6
R
18 49

9

Thrombocy-tes, 285000 16 203000 298M
3000'. l82000 314000 2�M::
Netitrophiles
Stabnucldar 139 - to-- 22 94- 126
'

333 A 1975 -2503

174
:
2161 -

'
~
3152 -

Eosinophiles, -

Br-sopb es

,

'
-46
1-107, - 152
0.:
0 0'. 0 134-:%:
_
0 -

1 29

1 -41ymphocytes
.
9722

18 1692
4
M
26W

-

Monocv+es
'
l 96
-1 M IM
lot W -M'
- 213

k
s cells
Tueri

78

9 78 -~:79 152.

M
-106 2 3

Ccird 3 5-

1
5)4650-6
L
AGMSIOR NR;,
M01 957
ei bio6d...:
Table 2. 6 og p ____'urrent--ofAhe periph
--of,rats- Arradiated, vJtji PP..

-indices,

6m
th- d _A,
12th'_ V
lfthicW_ i0th- ay

_d_

4th-
day

0 h-~ASY
t

90.0
150 82.2 7ZO
137 120-- - 64,2
- -
--
7
10
N1
8% 73,2
--.1
:'
.
2-
12
Hemoglobin
9,~A
M, I . g-
697 30000
,
g
40000 ,
'54
0 .
.
.g
AMA
.597
WO
7 U.5 9
-
669-'-
Erythroc
ytes 6 ~ 47 800
0 0
631
OW
' 641
-1,

Leukoc es
t
I 12390

6
0 2870-: 4933.

6
0
5
0 6788 7613

0
6 -
11512 12412
-06 -
-'06
2.1-

06

ndex
Color
. 1
, . --
-

eticulocytes
64

-*
6
.32 38

30
0 26
54

~
6
59

2

2 57

WhromboRnes

utro
es
e 274oo 0
4000
-23 -,
25900 50000 85M alum ..3:
p `

~Stabnuclear
Be
mentonuclear Ila
_
3
1 251-

1378 A
43
".; -J
144

,--
- 257

g
8
6
ar
-
W8. A294
8
462
6636

.Eosinophiles

80

9.. ~.' ;'_
68
61

32 t

26 289
3
'-
42.

asophiles

M 0 es
it
E

,

880

0
0

330 25S

0

3M
0 0

,
11 689

s
or
c;

82--
-63 L
146",
'
'189
-,_132-:11.

36
251

251

uerck's cello

If,
5
4 68
:139 180;

26
w

41~
a
C
rd

7:v 7'

ACCESSION MM-F
AT501495Y
" EN=URE

Table I Morphologi6alico~ftht--of- the -peii b .00d
_
'ys.
of ratB irradiated with '800-r,.X-mr"a

ndices
norm
t day
8th:. ddy
llah d*
dat 12, 2

d
~h qth`
3
, ~

76A%--~,
63.0%-
04,2v--
61.0%-
-49,J%_* 60.0

H obin
emogl
t
E
th
13,6
662W
128
6AU 10.5

MOM
5.3
32W

4W 0
rocy
ry
L--UKocytes I 14910 8W- 2680 -
.
,
., -fro IM

6 -:.6466 -
0
6 .:6m-
_
. -
$ 11300
-
._
O6_T_
C
olor Index 016 0.6
~ 0.4

1
21: ,
0,
~, M. .

26 _:
.
0,
-
27 : 1
.
RetictElocytes 39
275,
25V *,
241 ~
_Agj~. ~'208 - 1
223: -
1
213 297
tes
Neutrophiles

'

9
48
40
W8

: ~, 246

tabnuclear
Segmentonuclear

191

o,

60

735, 68-
7
M

21

2,
0-
M

osin Dh les
'
Li
E
s
RI
494

0 -6

0 71

'0 12
0- 25

0
0
0
0
es.-
a
D
.
op
)cy-tes
L
ymphc
Monoc es IM

233 IN

0 4614

24 M

4' :M

5 AW

52

3

05';

TU i~s cells
275
26
1

,79
It

10 :492

Curd

9i 97
me ry-,.,--;
]TOPIC TAGS:. 1 dosimeter,.radiation.dosi t
-ge
M. b
-ABSTRACT - Gel f ons'iderable-.`-in
-dosimeter,s-are--o t4rest-to-ra iob 61ogists-_- ecausPF_'.`:'~,,_,.
of their tissue~equivalence Ii The -'author- has --studied t' _d
prepara. ion an testing-of.,
nitrate gel dosimeters in a mix6d-ga'jnma-n6utron.field.from-alnuclear r'actor-with
e
radiation dosages from 100 to 1060 rads. The-dosimeters were prepared from nitrate .s
of sodium, potassium and ammonium in-distill6d water~.and either gelatin-or agar:ag
plus glucose and alkali and were able to measure comb' d adiation.,.,.,
ine gamma-neutronx
only (not either one separately), Thp same, gel preparations were,u,sed'-to preparej-.,_.~,
0
phantoms for study of spatial distributi n ofradiation. Nitrate gel dosimetry'is~.
based on the conversion of.nitrate into nitrite in'a. water, containing mixture. _G61-
dosimeters have a.higher rate of n' --,than liquid dosimeterso the
itrate conversion

C
USSR/Plant Di-I-ease. Dise-ises of Cultivated' Plants 4- 3
Abs Jour Zhur-Biol., Nc 8, .19/58, 3/4-OJ63
Author lbadakov 0.
Inst Iiot driven
its Control r1
Title Grey Rot of Herip -Ind U (Seraya il'
ken-tra i merd bor'b,-[ s ney).
Ori - -Pub S. k1i. KirGizii, 1056, No 12, 1'7-21
A b s t rac t T~ie_ s~=-Dtoms of the dis-~ase, itus oh,7siolo-ical
--ff----,ct on t1le plant, the experi.,ments in which the
aj_~rest of -rovith and the small accumulation of fl-
ber in the sick plants are described. The Sreatest
,--ffectiveness in t1lie control of the disease is
achieved by the application of tetramethyltliiuran
disulfide. The sprayin_,r is conducted with a 5%6
)ension at ,ui c_,~menditure of 250 liters per
I-lectare. Tht r'orfll of expendituve of tiie Dr~~
,.vhen used -as a dust is l0kIg/hec tare. L paration
Card 1/1

U'S'SR/11[trit Dic;caE;OiJ oi' CultillatC(I 11311til.
Abs Jour : Ref ML- - Mole) 110 8, 1958, 34968
Author : Rudakov) 01,
Inst : -
Title : Gray Putrefaction of tbe Chfabo Hemp and Means. to Fig~it It.
Orig PLfb : S. Idi. Kirgisii, 1956, Ho 12, 17-21-
Abstract Described are the symptomc o-f the disease, physiological
effects on the plants, and c;.pc-_-imev_ts showing tha de-
crease of growth and insufficient filament acc=alation
in the diseased plants. ftti=l effects in the fid2t
against the disease are obtained by using tetramethylthiu-
ranatesulfide. Sprinkling is done with a 5% suspension,
calculating 250 liters per hectare, or ?,5% for 500 li-
tur per hectare. Amounts of the preparation to be used
in dusting 10 kg per ho-c"ai,c. Ghishcnkova
Card 1/1

KTDYNOV, M., nouchnyy sotrudnik; BATTRCHATEV, I.; LOPINA.-SHKNDRIK, M.D.;
KAIBAYEV, A.; IMANAKUNOI, B.; SULAYMANKULOV, K., kand.khim.nauk;
DUTSBEITALIYEVA, ff.; AKBAYXV, A'~; KAZ=, K.; GOLOVIN, F.I.;
BAKASOVA, Z.; KOVALXNOK, Z P.; SMUKRINA, N.P.; BUGIUBAYEV, A.B.,
Istarshiy prepodavatell; B.I;;TJLATOV, E.B., mladshiy nauchnvy
sotrudnik; FILIPPOV, N.A., mladshiy nauchnyy sotrudnik; XAMBETA-
KUNOV, T., aspirant; IM-UTIMOV, A., aspirant; TURMAMBETOV, S.,
mladshiy nauchnyy sotrudnik; KUKHAMEDZIYEV, M.M., nauchnyy sotrudnik;
KONURBAYEV, A.O.; PAK, L.V.; TOKTOSUNOV, A.;
K7IAKOVA, R.I.; ASRIRAKHMANOV, Sh., aspirant; ALYSHBAYEV, B.;
SULTANALITEV, A.; AKRMETOV, K.; POLONOVA, A.P.; NIKITINSKIY, Yu.I.;
SHAMBETOV, S.Sh.; DZHUMBAYEV, B.O., nauchnyy sotrudnik; DRUZHININ,.
I.G., red.; ANOKHINA, M.G., tekhn.red.
[Papers by junior scientists of the Acndemy of Sciences of the
Kirghiz S.S.R.) Trudy molodykh nauchnykh rabotnikov AN Kirgizskoi
SSR. Frunze, 1958. 411 p. (MIRA 12:j)
(Continued on next card)

M YNOV, M.---(continued) Card 2.
1. Akademiya nauk Kirgizskoy SSR, Ynmze. 2. Institut khimii AN
Kirg.SSR (for Kydvnov). 3. Kirgizskiy gosuderetvennyy universitet
(for Bugosyev). 4. Institut geologil AN Kirg.SSR (for Baybulatov).
5, Institut vadnogo khozyaystva i energetiki AN Kirg.S&R (for
Filippov). 6. Otdel fiziki i matematiki AN Kirg.SSR (for Rambetakunov,
Imanknlov). 7. Institut zoologii i parazitologii AN Kirg.SSR (for
Turmambetov). 8. Kirgizskiy meditsinskiy Institut (for Mukharoed21yev).
9. Otdel pochvovedeniya AN Kirg.SSR (Ashirakhmanov). 10. Institut
betaniki AN Kirg.SSR (for AlyBhboyev, Sultanaliyev, Akhmetov, Polonova,
Nikitinskiy). 11. Institut istorli All Kirg.SSR (for bzhumbayev).
(Science--Collections)

L i
Owtivated -':'itints.
6 r';-

A!--* K i r,,,, -3 ~j R3.9 5
lz

tiaz tlh~-~
-A-'a t-e-rap
aran!-tiskn -n~ Fc-tryris cinerat nij -a-
tft~At the Inttirr-alEitionn betwil-a thl~-t
faetilt:~tivc paarn--rite ;?clad the illoXrt plar~t
not to the intoy.1catior. of tli.;- cells
and the funq-11'Y's "Itilizatioll or zlip"ii Awl rIlL,1-11-,-

e 7"1 ev,-)IitlJvti of ilra dove- -,ert
opa
..-i I-l'ie produr-ed A- L rl
c ci, t dtc n -Jan ~t c-- f t- i -xit: 13 , :Ln fl,

-- ------- -
PAKQjj,-Q.L..; WHASHOVA, A.A., otv. red.; LEVITUS, B.I., red. izd-va;
YRU D
ABOKHIINA, M.G., tekhn. red.
[A fungus parasite of the dodderv its cultivation and use] Grib-
noi parazit povilikit ego vyrashchivanie i primenenie. Fr~unze,
izd-vo AV Kirgizskoi SSR, 1961. 65 P. (MIRA 14:6)
(Dodde~-Diseases and pests) (Fungi$ Phy-topathogenic)

pl~~Tlmu- T - I
C-.
U33?/Goncral and Spocial Zoolor?y. I,-,lsoct3. Injurious In-
socts and Ticks, Posts of Fruit and Borry Crops.
lJos Jour: Rof 71hur - Biol., No 11, .1958, Ho 49649
Autlior Rudakov 0,L.
1.1nd :-ar!11Ato).0'--Y' A'S Kin'jz
MI.
TA10 Funr-i '.,Thich Davolop in tho Thoracon of tho 11ppl-,
Troo i4otll
Or ir: aib Tr. In-ta z--ol. i -parazitol. !il-S Kir,-.S32
1, 1956,
vv~)' 5, 175-18o
Abntr.--.ct This is a description of fun,~;i found in tho thor-
acos, w-rL. collz.;ctccll ia tho o,::;rl -3
L 44 y spri-w-
of 1955-1956 in tho-ard'ons of th- val)-ay of tho
Rivor Chu (Kir~--iziay: Tarichium Iparasito
sp. - a
of th:) larvao; Honillan lipolytica.an:ft Sporo-
tri--hu-.-.. sp. - apparontly, parasit-as of larvau; tho
part plaYod by Pirolla r-ialinclla, Zy-~osaccharoLiy-
Card 1/2
59

RUDAKOV, O.L.; POSPELOV, A.G., red.; ANOKHINA, M.G., tekha.red.
[Biology and conditions favoring parasitism in fungi of the
genus Botrytiol Biologiia i usloviis para21tizma gribov rods
botritis. Frunze, Akad.nauk Kirgizskoi 1959. 188 p.
(MIRA 12:11)
(Fungi, Phytopethogenic)

~~, , ~;:"-,~ F'..- ; ... 4. 1

RUDAKOV, O.L.
Fungi developing in caterpillar cases of the apple moth. Trudy Ins t.
zool.i paraz.AX Kir.SSR no.5:175-180 156. (KIRA 10:5)
(Chu Valley~--Pungi) (Apple-Disease and pests)
(Insects, Injurious and beneficial-Biological control)

RUDAKOV., 0._.L., kand. biolog. nauk
Biologicalmethod for controlling dodder. Zashch. rast. ot vmd.
i bol. 6 no.6:23-24 Je 161. (MIRA 16:4)
(Dodder-Biological control)
(Altenaria)

RUDAKOV, P., arkhltektor
Apartment-t7pe old-age homes. Zhil. strol. no.2:27-31 '59-
(WRA 12:6)
(Old-age homes)

ACC NRt AP6029880 SOURCE CODE: UR/0413/66/000/015/0043/0043
INV~11~70R: Akhmetzyanov, K. G.; Petrovichev, V. I.- Rudakov R. F. J/
ORG: none
TITLE: A waveguidep
device for concentrating an S11F electric field in a piezoelectric~~
sample. Class 21, No. 1814298 (announced by the Moscow Engineering Physics Institute
(Moskovskiy inzhenerno-fizicheskiy institut)]
SOURCE: Izobret prom obraz rov zn, no. 15, 1966, 43
TOPIC TAGS: rectangular waveguide, high voltage line, piezoelectric crystal
ABSTRACT: This Author Certificate presents a waveguide device for concentrating an
SHP electric field in a piezoelectric sample. To achieve a strong field within the
Fig. 1. Waveguide device
;H I - Shorted rectangular waveguide; 2 - coaxial
f, J,,;o 14 stub; 3 - flat capacitor; 4 - central conductor,
of the coaxial stub; 5 spark gap; 6 ceramic'
'Ij-
rod.
n
I Cor UDC: 621.372,855.4: 621.372.88

A~C
AP6029880
samplea coaxial stub (see Fig. 1), connected to the broad side of a rectangular wave..!.
guide, has a broken center conductor that forms a spark gap within the-waveguide;
the broken ends of the center conductor are joined together with a ceramic rod. A
piezoelectric sample is placed between a flat capacitor formed by the center conductor
and the broad side of the waveguide. Orig. art. has: 1 figure.
SUB CODE: 09/ SUBM DATE: 1%ar65 ATD PRESS: 5069
-Card 2/2 blg

KOSONOGOV, L.F. (Voronezh, u1. Pravaya Sukonovka, d.12, kv.6)j RMAKOV, S.A.
Fixation of the anesthesia apparatus to the operating table
for the centralized feeding of oxygen into the operating room.
Grud. khir. 2 no.4:125-126 JI-Ag.160. (MIW, 15:6)
1. Iz kafedry goopitallnoy khirurgii (zav. - prof. V.F.
Radushkovich) Voronezhakoge go instituta.
(AISSTHESIOLOGY)

RUDAKOV S. G.
Ancient volcanism in the Soviet Carpath!.ans. Dokl. AN SSSR 255
no. 2-340-U2 Mr 164. (MIP.A 17:5)
1. Moskovskiy gosudarstvennyy universitet im. 14. V. Lomonosova.
Predstavleno alrademikam V. S. Sobolevym.

-1U'-PHORS:Ly,,a-;jshev, L. 1-A. and Rudakov, S 11
TTT=, In B'.--perimental S-tudy DJ-1-9.~acnlar Reflection o--,- Sound
by Fini'te Thin Rods in I at er (ElKsperimertal'noye issladov-
aniyo nezer'vzallnogo otrazheniya zvuk-:1 tonkini or-ranichenny.~~i
sbcrzhny-m-i v vode)
FE.LIIODICAL: &!:;.)stiches!,,iy Zhurnal, 195,8, Vol 4, Nr 3, pp 283-285
(USSR)
ABSTRACT: Results of an experimental study of non-s-pecular
reflection of sound by thin finite rods in water are repor-
';ed. Elle rods vrere madle of alurainium. steel and brass. A
coa---)arison is made between the experimental data and the
theoretical predictions -iven in Ref.l. It is shoum that
non-specular reflection of sound by such rods is due to
ion.,-it'udinal and bending vibrations of rods, and the ex-
periEientally observed intensity distributions are satis-
factorily described by the theory of Ref.l. Ther,':~ are 4
.Card 1/2

SOV-46-4-3-11/18
An Ex-cerizn-3ntal T.-udy of Non-&,-,ecular Reflection of Sound by
Finite Th-':n Rods in 1,7cqter
tz,ra-~-.ns and 1 Soviet reference.
ASSOCIATIO111: institut AIT SSSR, ',,Ioskva (Acoustics"-
!~s'l-i-bute of the Soviet Academy of Sciences, Moscow)
BUT.JTTED: ~,L,3!cli 2r, 1W').
1. Sound--Reflection 2. Water--Acoustic properties 3. Rods--Acoustic
properties
."-,rd 2/2

CaLegory USOR/AcoujUo,; - Sound vibrationr, and waves J-2
Ab3 Jour Ref Zhur - Fizika, No 1, 1957, No 2103
Author Lyamshev. L.M., Rudakov, S.N.
Inst Acoustics Inst., Ac`ad~~nces USSR
Title : Reflection of Sound by Thick Bounded Plates in Liquid
,Orig Pub : Akust. Zh., 1956, 2, No 2, 228-230
Abst.-ract: Report on an investigation of the reflection of sound from thick bounded
brass, steel and aluminum plates in water, in a direction opposite to that
of the incident wave. Non-mirrorlike reflections were observed in directions
that do not agree with those of previously-known reflections. By "non-mir-
rorlike reflections" are meant strong anomalous sound scattering in a direc-
tion opposite that of the incident-Wves (cf, for example, Ref. Zhur. Fiz.
1956, 26537, for details).
It was established that the non-mirrorlike reflection of sound is obaerved
every time that the phase velocity of the incident sound wave in the liquid
along the plate becomes equal to the velocity of one of the normal waves in
the plate (in the elastic layer).
Card 1/1

SUBJECT USSR PHYSICS CARD 1 2 PA - 1477
ii~UTHOR LiAMSEV, L.M. I RUDAKOV, S. N.
TITLE The Reflection of Sound by a Thin Rod in Water.
PERIODICkL Dokl.Akad.11auk, 110, fasc. 1, 48-51 (19561
Issued: 11 / 19_~T reviewed: 11 / 11956
In the case of some angles of incidence a strong reflection in the opposite
direction of incidence of the wave is observed ( #?non-mirrorlike reflection").
The assumption that this reflection is caused by diffraction- and longitudinal
waves in the rod was confirmed by experiments.
The device used for the examination of this reflection consisted of a trough
with sound-absorbing walls which was filled with water, a generator for ultra-
sonic impulses, a quartz vibrator, a reception amplifier, and,an impulse
oscilloscope. The duration of impulse amounted to 30 /A-see and the repetition
frequency of the impulses was 50 c. The rods had a thickness of less than 1 mm
and were 1110 mm lone, the distance between them and the vibrator was -150 em.
Tjje angle of rotation was measured with an accuracy of 0,2 0 and the relative
error when measuring the amplitude of the reflected wave does not exceed IOCA.
The polar diagrams of the reflection of some copper-, aluminium-, and steel
rods are shown in diagrams. The angles of non-mirrorlike reflection correspond-
ing to rods of different materials are given. In the case of brass rods of
0,79 mm thickness such a reflection does not occur.
Next, the problem of the scattering of a plane sound wave by a thin rcd sub-

Doki.Akad.Nauk, 110. fasc.1, 48-51 (1956) CARD 2 / 2 PA - 1477
n~erded in a liquid is investigated in consideration of the shearing oscillations
and longitudinal oscillations of the rod. The correipondint differential
equation is given. lion-mirrorlike reflection occurs at the critical angle of
C/Cx. lion-mirrorlike reflection by infinitely long rods is due to the
effect produced by free longitudinal waves (or shearing waves) which are re-
flected by the boundaries of the rod. If the above mentioned condition is satuis-
fied, spatlal resonance occurs if the amplitude of the longitudinal or shearing
os-~;illations excited by the exterior field of sound increases considerably. In
-qe case of an infinitely long rod and spatial resonance the amplitude of the
scattered field can be considerably higher than the scattering amplitude in the
case of a vertical incidence of a plane sound wave.
Losses in the interior of the material of the rod exercise an important influence
on the scattering of sound in the case of sufficiently thin rods. The sharp de-,
oreape of the amplitude of non-mirrorlike reflection due t.o longitudinal waves
is, in the case of steel rods, connected with the nonstationarity of the
oscillations of the rod.
INSTITUTION: Institute for Acoustics of the Acad,~my of Science in the USSR.,

LYAMSIIEV, LM.; A~DAKOV. S.N.
Sound emission from plates and shells in water. Akust. zhur.
7 no.3:380083 161. (MIRA 14:9)
1. Akusticheskiy institut AN SSSR, Moskva,
(Elastic plates and shells) (Underwater acoustics)

ROCHEV, N.N., glav. red.; VAVIIDV,-'P.P., red.; VERTEL", E.L., red.; GORELIK,
A.I., red.; GUZMAN) I.S., red.; KUZMSOV, G.R., red.; YMVEDEV, G.A.,
red.; MODYANOV, Ya.V.j, red.; PANTEIEYEVA, A.A., red.; POLYAKOV, V.V.,
red.; POFOV,.S.A.,, red.; FOPGVA, S.M., red.; RHEVSKIY, S.S.., red.;--R7:-
--.DAKOV,..S.V., red.;,SYUTKIN, A.F., red.; USOV, A.I., red.; USTINGVA, I.K.3
P.T., red.; CHEBYKIN, N.P., red.; MEZENTSEV, S.A., red.;
MOROZOV, V.S., red.; OPLESNIEN, I.I., tekhn, red.
[Forty years of the Kori A.S.S.R., 1921-1961; studies on the cultural
and economic development of the Komi Republic140 let Komi ASSR, 1921-
1961; ocherki o razvitii ekonomiki i kulltury Komi Respubliki. syktyvkar,
Komi knizhnoe izd-vo., 1961. 154 P- (MIRA 14:11)
(Komi A.S.S.R.-Economic conditions) (Komi A.S.S.R.-Culture)

814oil
S/020/60/132/06/23/066
B014/BO07
AUTHORSj Gringauz, K. I.p Rudakov, V. A.
TITLEs Measurement of(~ftectron Concentration 'in the Ionosphere
According to the Rotation of the Polarization Plane of Radio
Waves Emitted by Rockets
PERIODICALs Doklady Akademii nauk SSSR, 1960, Vol. 132, No. 6,
Pp- 1311 1313
TEXT: In the present paper4he results of measurements are given, which,
were obtained by means of a*%geophysical rocket of the AS USSR on
August 27, 1958 eaching an altitude of more than 450 km. The rocket was
stabilized in the three directions of rotation. Formula (1) describes the
rotation of the polarization plane of the radio wave during its propaga-
.tion in the terrestrial magnetic field. Formula (2) is developed,,which
permits determination of the electron concentration in the ionosphere in
the case of a vertical, free, completely stabilized flight of the rocket.
Details of the antenna construction are discussed; 24,,48, and 144 Mc/s
were transmitted. Fig, I showo uscillograms of the signal levels of the
Card 1/2

81401
Measurement of Electron Concentration in the S/02Y60/132/06/23/068
Ionosphere According to the Rotation of the B014 B007
Polarization Plane of Radio Waves Emitted by Rockets
three wavelengths as examples. Fig. 2 shows the electron concentration
calculated along with the recording of the rotation of the polarization
plane of the 48-Me/s wave from formula (2). The differences between the
result obtained here and that of an experiment carried out on February 21,
1958 are discussed. There are 2 figures and 2 Soviet references.
PRESENTED: March 14, 1960, by A. N. Shchukin, Academician
SUBMITTEDs March 9, 1960
Card 2/2

1 25985
17, 7/0 0 s/56o/61/ooo/oo6/003/010
E032/Ell4
AUTHORSt Gringauz, X.I., Rudakov, V.A., and Kaporskiy, A.V.
TITLEt Apparatui for rocket ~meazurementz of free electron
concentration in the ionosphere
PERIODICALs Akadqmiya nauk SSSR. Iskusstvennyye sputniki Zemli.
No. 6. Moscow, 1961. PP. 33-47
TEXTi The present paper gives a brief description of the
radio apparatus which is being used to study the electron
concentration as a function of height in the ionosphere. The
apparatus is designed so that it can be mounted on a vertically
launched geophysical rocket of the Academy of Sciences USSR
(K.1. Gringauz. DokI. AN SSSR V.120, 1234, 1958,- Sb.IfIskusstvennyye
sputniki Zemlit, No.1, izd-vo AN SSSR, 1958, p.62, Ref.l:
K.I. Gringauz, V.A. Rudakov, Dokl. AN-SSSR, V-132, 1311, 196o,
Ref.2). The apparatus incorporates radio transmitters and trans-
mitting antennas set up on the rocket, receiving antennas on the
earth's surface, receiver-phasometric devices, and recording and
auxiliary apparatus. The method of measurement, the choice of the
frequencles and the results which have been obtained are reported
Card 1/ 8

2598-5
Apparatus for rocket measurements .... s/56o/61/ooo/oo6/003/010
E032/E114
by the present authors in Ref.4 (page 48 of the present issue).
The experiment consists in the determination of the phase difference
between the signal transmitted from the rocket and detected at two
different points on the earth's surface. The phase difference
occurs because of the dispersion of radio waves in the Ionosphere.
Between 1954 and 1958 the frequencies employed wer fl 144 mc/a
and f2 = 48 Me/a. Since 1958 a further frequency f3 24 Mc/s
has been used. The phase difference between vibra:ionB of
differing frequency is defined as &(P = Yl - PT29 where fl = Pf2
and p < 1, i.e. the phase difference reduced to the higher
frequency. The average electron concentration ne can then be
calculated from:
n = k electron-cm-3
a 23t Lh
wheret &(~ is the phase difference corresponding to an altitude
change of Ah (the phase difference is in radians and the altitude
change in meters). The coefficient k was 2.25 x 107 for the
frequencies f1.2 and 0-515 x 1o7 for fl 13. The recorded signals
can be used to measure the rotation of the plane of polarization of
the received radio waves. With a completely stabilized rocket the
Card 2/ 8

25985
s/56o/6l/ooo/oo6/003/0l0
Apparatus for rocket measurements ... E032/Ell4
radiation of the plane of polarization is due only to the Faraday
effect. The electron concentration can then be determined from:
n = M 0 electron-cm-3 (2)
e 2 ITE HB Ah
where: 0 is the rotation of the plane of polarization; HB is the
verticalcomponent of the geomagnetle field In oersted; Ah Is the
path (in km) traversed by the rocket while the plane of polarization
is rotated through 0; M is a constgnt whose value for fl,2,3
was 56 x 1o6, 6.2 x 106 and 1.55 x 10 respectively. In all
these measurements it is necessary to know the coordinates of the
rocket as functions of time, and hence the recording of the phase
and amplitude of the signals must be accompanied by the recording
of the time. The apparatus employed in these measurements was
developed during 1954-1958 and the present paper describes its
latest form. The transmitters mounted on the rocket produce
coherent vibrations on the three frequene.',.es fl, f2 and f3. There
is a separate output for each frequency with a symmetric load of
100 ohm. The power at the outputs is 15, 8 and 3 watt respectively.
A block diagram of the transmitting system is shown in Fig.l.
Card 3/8

25983
Apparatus for rocket measurements .... S/56o/61/obo/006/003/010
E032/Ell4
The coherence of the oscillations is ensured because they are
obtained as a result of successive multiplications of the frequency
of the common master oscillator. The master oscillator is quartz-
stabilized and is placed in a thermostat. The HT supplies are
fully transistorized. The transmitting antennas are in the form
of symmetric linear vibrators set up in the upper part of the
rocket. The frequencies fl and f2 are radiated from a common
antenna while a separate vibrator is employed for f3' The
apparatus on the earth's surface is designed to perform the
following functions: a) measure the phase difference between fl
and f2, and fl and f3; b) measure the amplitude of the high-
frequency waves at the inputs of the receivers (a minimum of five
microvolts is required); c) record on a 35 mm film the two phase
differences, the corresponding amplitudes and suitably scaled time
markers. The three frequencies are received by separate antennas.
Two photographs are included which show the appearance of the
antennas. The receiving apparatus has the form of a three-channel
superheterodyne device capable of carrying out the simultaneous
detection and measurement of the phase differences. In each
channel there is double frequency conversion which is carried out
card 4/8

25895
S/56o/61/ooo/006/003/010
Appar'atus for measurements ... E032/E114
with the aid of suitable.mixers. The si nals at.the output of the
three channels have the same frequency (94 Me/s). The working
bandwidth of the three channels fl,.f2 and'f3 is 40, 25 and 15 kc/5.11
The signals are recorded.on a 35,1nm film using two methods. The
first method makes use of loop oscillograph Mao -2 (MPO-2) which
shows the interference-frequency current and also the currents which
depend on the voltages at the input to the receiving device. Thle
speed of the film is 100 mm/sec. Typical records are shown in
Fig-7. The second method of recording the phase difference makes,
use of Lissajous figpres produced on the screen of a,cathode ray
tube. Further details are given in Ref.47(pAge 48 of the present:
issue). Acknowledgments are expressed to A.N. Gridin for ad'~~ce
and assis-.'snce.
There are 11 figures and 5 Soviet references.
SUBMITTED: April 2, 196o
Card 5/8

25986
c7, C?/O 0 S/56o/6i/ooo/oo6/oo4/oio
E032/E114
AUTHORS: Gringauzo K.I., and Rudakov, V.A.
-T-e~c
TITLE: Measurements of the e tron concentration in the
ionosphere up to 420-470 km, carried out during IGY
using radio waves,emitted from geophysical rockets of
the Academy of Sciences, USSR
PERIODICAL: Akademiya nauk SSSR. Iskusstvennyye sputniki Zemli.
No. 6. Moscow, 1961. pp. 48-62
TEXT: The systematic study of the electron concentration in
the ionosphere as a function of altitude was begun in the Soviet
Union in 1954. The experiments were carried out with the aid of
vertically launched geophysical rockets. The resultB were first
reported by K.I. Gringauz (Ref.1; Dokl. AN SSSR, V.120, 1234, 1958',
Sb. "Iskusstvennyye sputniki Zemlill No.1 izd-vo AN SSSR, ig.58,
p.62) and K.I. Gringauz and V.A. Rudakov (Ref.21 Dokl. AN SSSR,
V-132, 1311, ig6o), and were '?reproduced" by H. Friedman (Ref.3-1
Proc. IRE, V-47, 272, 1959). The apparatus employed is described
by the present authors and A.V. Kaporskiy in Ref.4 (page 33 of the
present issue). The present paper is concerned with some problems
Card l/ 10

25986
Measurements of the electron .... S/56o/6l/ooo/oo6/oo4/olo
E032/E114
which are encountered in dispersion and Faraday effect measurements,
an.used in the determination of the electron concentration. An
account is also given of the experimental results obtained in 1958
with three geophysical rockets launched to a height of 450-470 km.
These measurements were carried out at different times of day and
year and have thus provided information about the electron
concentration in the region of the ionosphere which includes the
so-called outer ionosphere (above the maximum of the F layers and
quite inaccessible by the normal.radiosonde methods). All the
measurements were carried out above the same geographical point and
the same method was used throughout. The velocity of propagat on
of radio waves in the ionosphere is a function of frequency and to
a considerable degree depends on the concentration of free
electrons ne- Hence dispersion methods can be used to determine
ne. The dispersion can be conveniently measured by the radio
interference method due to Mandellshtam and Papaleksi (Ref.61 M - L,
Gostekhizdat, 1945, "Recent investigations on the dispersion of
radio waves along the earth surface"). The method was first used
by Papaleksi in 1936 during the solar eclipse. It Is designated
by the present authors as the I'dispersion interferometer method".
Card 2/ 10

25986
Measurements of the electron .... s/56061/000/006/oO/olo
E032/Ell4
In this method, coherent radio waves with frequencies -fl and f2
are emitted from a point A (fl = Pf2 where p = m/n '>'l and
m and n are integers). The radio waves are detected at a porint B
and the phase difference between them is determined. The phase
difference is reduced to the higher frequency, i.e. ayc-yl - py2.
The phase difference is given byt
27EPf2 L n1(t)dt L n2
0
where L is the distance between A and B, and the integration is
carried out along the path from the transmitting to the receiving
Antenna; nl(t) and n2(4) are the refractive indices for fl and f2
respectively. For sufficiently short radio waves it may be
assumed thata 2
n ( f I - ne
2TEmf2
where ne is the electron concentration and f is the frequency.
Substituting Eq.(2) into Eq.(3) it is found that:
Card 3/ 10
- - - - - - - --- - -

25986
s/56o/6!/Ooo/oO6/004/010
Measurements of the electron ..... E032/E114
&P e2 (p2 - I ) L n (4)df K L n (f) dC (3)
cmf2 p e ~ e
0 0
If it is assumed that ne and L are functions of time (i.e. the
point A Is moving relatively to B) then during a time bkt
during which A is displaced through &L the change in the phase
difference at B is given byi
L+,AL L
K n (f)df +( S -Ln f) d pith b(p, + (4),
e at e
L 0
The recorded increase in the phase difference consists of two
components, namely, one ' due to the increase in, the path L,
which depends on the electron concentration in this region, and
another' A 40 &f N -r which depends on the total number of electrons
in the coiumn between the observer and the beginning of the section
6L. When the point A is fixed, as for example in the case of
Card lo

25986
S/56o/61/000/006/004/010
Measurements of the electron E032/E114
the 1936 measurements during the solar eclipse, the first component
is absent and the measured phase difference yields the average rate
of change in the second component. If the point A is a rocket
launched in the vertical direction, then a similar situation occurs
at the apex of the trajectory where the vertical velocity changes
11 ign and passes through zero. This method therefore yields the
integral electron concentration. In addition to the dispersion
effects the electron concentration can also be measured from the
rotation of the plane of polarization of the radio waves emitted
from a vertically launched rocket. The rotatlon angle & can be
evaluated froms
L+ LS L
e 1 H n (f) de 6)
27tc2m2 f2 L e
L
where: HL is the vertical component of the magnetic field and f
is the frequency which is sufficiently high for the absorption.in
the ionosphere to be small and the refractive indices of the two
components to approach unity (A.N. Shchukin. "Physical Principles
Card 51 10

25986
Measurements of the electron .... s/56o/61/000/006/004/010
E032/Ell4
of the Dispersion of Radiowaves in the Ionosphere". M.,
Svyazlizdat, 19110). Fig.1 shows a part of the.record obtained for
the three frequencie 8 fai= 24, f2 = 48.and f, = 144 mc/s. This
figure shows a plot Of n (microvolts) at the inputs of the
receiver connected to antennas with the same polarization. The
0 ^.jl/f2 relationship is said to be clear from this figure so that
the recorded periodic changes must have been due to the Faraday
effect. It follows from Eq.(6) that if e 'it then assuming HL
to be known and replacing AL by A h the average electron
concentration can be calculated froma
2 7t 2c2m2f2 1 (7)
e3 h HB
The quantity h is determined from the times ti and t2 which
correspond on the record to two neighbouring polarization minima,
since the coordinates of the rocket are known at eachinstant of
is
time. The interval of altitudes over which the average of ne
taken can be reduced by using two receiving devices with .
independent antennas having mutually perpendicular polarization.
.Card 6/10

.25986
S/56o/6i/ooo/oo6/oo4/Ol0
Mdasurements of the electron ... 4 . 1 1.11
E032/Ell4.
Fig-3 shows the electron concentration as a function of height Ckm).
The curves were obtained by the dispersion interferometer method.
Curve 1 was obtained on February 21, 1958 at 11 hr 40 min;
Curve 2 on August 27. 1958 at 8 hr,06 min; Curve 3 on October 311
1958 at 15 hr 54 min'. Fi'.4 shows a sirfiilar curve obtained on
August 27, 1958 with the aid of the Faraday effect. The. poillts
1, 2, 3 and 4 have the following meanings: I - identical data at
two points of reception; 2 - data at a third point; 3 - identical
data at three points; 4 - curve obtained by the dispersion method
(at the samq time). It is concluded that all the results fully
confirm the fact that the ionosphere has a single main maximum in~
the electron concentrations which occurs at about 300 km,,.and that
the belief that there is a sharply defined E layer was due to the
inadequate data which have been available so far. Acknowledgments
are expressed to S.M. Rytov for assistance an-d advice.,
There are 6 figures and 18 references% 12 Soviet and 6 non-Soviet.
The four most recent English language references read as follows:
Ref-3: H. Friedman, Proc. IRE, V-47, 272', 1959.
Ref.10,. J.C. Seddon, J.E. Jackson. IGY World date center A.
Experimental results of the U.S. Rbcket program for the IGY.
Card 7/ lo

s/56o/61/ooo/oo6/004/OlO
Measurements of the electron .....
E032/E114
to I July 1958. National Academy of Sciences, Washington,
No. 1, 1958, p. 14o.
J
Ref.14: J.A. Ratcliffe. The Physics of the Ionosphere, published
by the Physical Soc., London, 1956, p.89.
Ref.15: J.V. Evans. Prod. Phys. Soc., 69B, 953, 1956.
.z3i,BMITTED: April 29, 1960
Fig.1 too
50

3 3 3k 18
S/560/61/000/010/016/016
D299/D302
AUTHOR-, Rudakov, V. A
TITLE,, Results of measuring electron concentration
in the ionosphere up to 200 km altitude
carried out by rockets in 1959 and 1960
SOURCE. Akademiya nauk SSSR. Iskusstvennyye sputniki
Zemli. no. 10. Moscow, 1961, 102-103
TEXT-. In recent years, the altitude dependence ne (h) of
free-electron. concentration in the ionosphere has been studied
by rockets launched on behalf of the Academy of Sciences of the
USSR, Thereby, a dispersion radiointerferometer was used,
operating on frequencies of 144, 48 and 24 megacycles. The
electron concentration was determined from the phase difference,
of the coherent oscillations emitted from the rocket and re-
corded on earth, whereby the frequency-pairs 144 and 48, and
Card(!03

3 3 3 1
S/56 61/000/010/016/016
Results of measuring.-
144 and 24 megacycles were used. Below, the n e (h)-distribution
is considered, as determined in 1959-1960. The results obtained
by rocket measurements are more reliable than those obtained by
terrestrial radio-probes and can be used for developing methods
of correction for the latter. A figure shows the ne (h)-
distribution curves obtained on July -14 and 22, 1959, and on
June 15, 1960. All the launchings took place at the same site
in the mIddle zone of the European part of the USSR. The launch-
ings were accompanied by simultaneous radioprobing by iono-
spheric stations, The n e(h)-distribution obtained from the
rocket experiments (including those conducted prior to 1959)
lead to the conclusion that the electron concentration increases
almost monotonically in ihe ionosphere (in sunlight) up to
-900 km with small maxima at altitudes of 105, 115 and 125 km.
An exception is the n e(h)-distribution obtained with weak sun-
light; in this case, the electron concentration is small (of the
Card 2/3

33318
S/56 611000101010141016
Results of measuring~_ D299YD302
order of I _Z_ 2 ~ 104 electron cm-3) and ch,-mges little
increasing altitude up to 180 190 km, where it begins to
increase considerably. There are 1 figure and 3 Soviet-bloc
references.
SUBMITTED: April 189 1961
Card 3/3

1-04 4 A 5 -67 EXV )/FCC
~R. AP6018922 ri/o 86-
iEC SOURCE CODE: URA
AUTHOR: Grinrauz, K. I.; Kravtsov, Yu. A.; Rudakov, V. A.;Rytov, S. M.
i ORG: Radloengineering Institute, AN SSSR (Radlotekhnicheskiy institut AN SSSR)
TITLE: Once more about the feasibility of local electron concentratio determination by the
dispersion method using artificial Earth* satellites and about the new Ionization maxima In the
Ionosphere
SOURCE: Gcomagnettzm I aeronomiya, v. 6, no. 3, 1966, 568-580
TOPIC TAGS: ionospheric electron density, ionospheric physics, Ionospheric disturbance,
Ionospheric radio wave, satellite data analysis, geophysic rocket
ABSTRACT: This Is the continuation of an earlier debate between the present authors and Ya.
L. Allperl el al, (see, e.g., Geomagn. I aeronomiya, 1 1965, 6, No 4, 766) concerning the
feasibility of local electron concentration determination by the dispersion method using arti-
ficial Earth's satellites. The authors show once more that the electron concentration deter-
mination using such a method leads to inaccurate results because of the presence within the
Ionosphere of horizontal Ionization gradients as well as because of the nonstationary character
Card 1 2 UDC, 550.388:629.198.3

L 0444!5~67
ACC NR; AP6018922
of the ionosphere. In addition,, the unreliability of the results of Allpert et al. Is caused also
by an inaccurate method used during the processing of experimental data. [Publishing Editor's
note: no further articles concerning this discussion will be published.] 1-orig. art. has:
9 formulas and 4 tables.
SUB CODE: OB/ SUBM DATE: 270ct65/ ORIG REF; 023/ (YrH REF: 015
Card

the. Of L
"rnflauT 0l a
Ko er o '.2'

L 2800-66 EWT(l)/FCG/&JA(h) RB/GS/M~WS -4
ACCESSION NR: AT5023578 UR/0000/65/000/000/0168/0177
AUTHOR: Gorozhankin, B. N.; Rudakov, V. A.
TITLE: Ionospheric investigations using rockets and artificial satellites in 1960-
1964
;SOURCE: Vsesovuznava kantereTitAiya-aqjialtv-kqsmichg�Xog2_prostranstva. Moscow,
1965. Issledovaniya kosmicheskogo prostranstva (Space research); trudy konferentsii.1,
Moscow, Izd-vo Nauka, 1965, 168-177
.TOPIC TAGS: artificial earth satellite, meteorologic rocket% ionosphere, ion con-
;centration, ionospheric electron deni3ity, satellite.data analysis
1ABSTRACT: In this short survey, the authors study measurements o0e1eqla~qn, --- and-iQn-
concentration in the lqjlqqp
he-re up to altitudes of approximately 2000 km. Specific
data obtained from various experiments are given, and trends are described in the
development of methods for making measurements of this type. The various methods
,for measurin n and n- are divided into two main groups: 1) probe methods, where
9 e 21
!the sensing element is In direct contact with the ambient atmosphere and 2)'radio
methods~where the information is transmitted over considerable distances. Data
Card 1/2

L 00560-66 ErWT(l)/FCC/EWi(h) Gw~.
'ACCESSION NRI "AP5021'006 '--,--------"--'----.--.----'--~-'--UR/0203/65/bo5/004/0762/076
6;
550-388.2s621-391-81
'AUTHORS: Grinpuzq K. Kr teov ~Yu. A~. Ry-toff, S -.M.
VITLE: On the possibility of determining local electron concentrations using the
.;dispersion method with the help of artificial satellitemand on a new ionization
maximum in the ionosphere
ZOURCE: Geomasnetizm. i aeronomiyat v. 59 no. 4i 1965, 762-766
'TOPIC TAGSt electron concentration, ioniza-bionp artificial satellite,,ionospheres.,
fDoppler shift, F layer
!ABSTRACT, In order to determine whether dispersion methods for measuring No in the
ionosphere by means of artificial satellites are valid, the various, gradient terms
-0 X/7bXV -6 Ifl-byp and 7b K/ ~ t must be investigated to determine if they are signi-
ficant in comparison with No$ These various gradient terms that appear in the
expression for the difference in Doppler shift between frqquencies &)I and ej2 are.
given.by
ON V ON -ON.
Vs I ids
al Nd,, sdz.
td COS (PC, sin (pa ow ay
So COS IPO OV
Card

00 0
ACCESSION NRs AP5021006
A detailed analysis is made to show that the terms 116P/ 610a." COS ax](f. + j. I Cos 1pe)
zc/cos q0. A similar state-.
(Mlal)dS~ are not necessarily small in comparison to No
ment# with even more assurance, can be made about the unsteady term (8N 88) d8
To demonstrate this, an altitude versus density curve (see Fig. 1 on the Enclosure)
is ahown. Here the maximum in N is above the maximum region of the F-layer if one
.1bases the data on the local dispersion methodl neglecting the gradient terms7solid
curve in Fig. 1). Radio-probe methodsp on the other handp support only the lower
g. 1), For this reason and because dispersion meaeur
curve (dotted curve on Pi ements
far from the earth are unreliable# the authors do not agree with the local concen-
omagn. i
tration data reported by previous authors (e.g., Ya. L. Allpert, Ge
aeronomiya, 1964, 4, No. 3, 479)-, Orige art. hass 4 formulas and 2 figures.
ASSOCIATIONt Radioteklmicheskiy institut, AN SSSR-(Radio Technology~InBtitUt8p AN
SSSR)
SUBMITTEDi OlFeb65 ENGL: 01 SUB COM GP, Mi
NO REF BOV: 013 OTHM t Oil

BDS/LW (V)/ZZG--2/ZS (V)/EP (t
L 1"76-43
)-2 FTG/ARW
g~6 /,a 't , Au n
C/A
SD
ACCES
H& E AP3000990 8
100
AUTHOR: Gdalevich, G. L.; Gringauz, K.. I.; Rudakov, V. A.; Ry*to S. M,.~
TITLE: Effect of the ion A= the, -position finding of space rockets ZR"eport,
of the Thirteenth Inte ational Astronautical Conxress held in VarnaSeptember
196_2T
SOURCE: Radiotekhnika i elektronika, v..8, no. 6j 19639 942-949
TOPIC TAGS; &pace rocket, effect of ionosphere
ABSTRACT: Some ideas are set forth about calculating the errors caused bythe
ionosphere in.determining coordinates*'Yand. speed of space rocketsby radio means.
Assuming a geometrical-optics approximation and measurements at frequencies over
5 X 10 sup 7 cps, fomulas are derived for the lonosphere-caused errors in deter-
mining range, elevation, and speed of rockets. ~The rocket is assumed to be in
outer space, and errors due to the troposphere and interplanetar7 plasma are
neglected. Approximation of the real altitude distribution of electron concentra-
tions is discussed for purposes of evaluating the above errors. Western and Soviet
data on electron concentrations are compared. Orig. art. has: .9 formulas and 6
figures,
Card 141
---------------- --------------

I ta
C-4
rA.

LIBOFUDOV, A.P.; HIGULIN, V.I.; Z1TDTiUS, M.D.; RUDAKOV, V.F.; KOTOV, K.I.;
HAK, A.M.; TISYMBALYUK, V.Yu.; FILIMONOV, V.V.
Service of the lining and cooling equipment of a blast furnace
in the smelting of ferromanganese. Metallurg 10 no.10:12-14
0 165. (MIRA .18: 10)
1. Zavod im. Petrovskogo.

RUDAKOV, V.I.; ZIL'BERSHOT, B.S.
Making reinforced concrete pressureless socked pipes in vi-
brating forms. Suggested by Y.I.Rudakov, B.B.Zillberahot. Rats.
i izobr.predl. v stroi. no-10:11-13 159. (MIRA 12:11)
1. Po vztterialam trasta TSentroopetastroy Ministerstva stroitell-
stva RSFSR.
(Vibrators) (Pipe, Concrete)

RUITikKeV, ll.r",;
iat ve .e ory.
I.,tc,tiluds of selactinC; a raultij,la answer trom an nisoc i !- m
NTI na.6.27-36 ',64. (,THA 17:9)
.A

RUldiAD.,"E, Alckvandr Konstantinovich; LW_D-,M_v_Xuni=in_Fedorovich;
DR0191XIOVA, Ye.11., red.; INIARAKAS'OVA L.P., tekhn.
y -
YELAGIN, A.S., tekhn. red.
[IndustiPes of the southern Urals] Industriia IUzh
(,O-o Uralla.
MosIcva, Sovetskaia llossiia, 1962. 141 p. 15;7)
(Ural Mountain region--Industries)

-ISE
RUDAWV, V-I-, Inzh.
Piezometric meter for level measurement in closed tanks. Zlek.sta.
29 no.8:82-83 Ag 158- (MIRA 11:11)
(Tanks--Measurement)

RUDIAKOV, V. 1.
Neftianye kalorizat~_rnye dvigateli. moskva, Gos. izd-vo sellichoz. lit-ry,
1950. 15~5 D. diagrs.
Semi-Diesel oil engines.
DA DLC: TJ790.R8
SO: Ylanufacturing and Mechanical Engineering in the "oviet Union, Library
of Congress, 1953.