SCIENTIFIC ABSTRACT LOBOCHIKHIN, V. M. - LOBODYUK, V. A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000930330001-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

30(l) SOV/99-59-2-6/12
AUTHOR: -Lobochikhin, V.M., Engineer
TITLE: Experimental Data on the Planning, Construction, and
Maintenance of Drilled Artesian Wells With a Water-
Yielding Crater Instead of a Filter (Opyt proyekti-
rovaniya, stroitel'stva i ekspluatatsii artezianskikh
burovykh kolodtsev s vodopriyemnoy voronkoy vmesto
fil'tra)
PERIODICAL: Gidrotekhnika i melioratsiya, 1959, Nr 2, pp 31-39
(USSR)
ABSTRACT: The author stresses the superiority of artesian wells
with water-yielding craters over those equipped with
filters. Every year, more than 500 artesian wells are
drilled in the Voronezhskaya, Kurskaya, Belgorodskaya,
and Lipetskaya oblasti, of which some 50% are equipped
with screen filters. As they have a very short ser-
vice life due to corrosion, clogging, and shortage of
spare filters, an improved type of artesian well with
Card 1/2 water-yielding craters, is making fast progress. The

SOV/99-59-2-6/12
Experimental Data on the Planning, Construction, and Y,~,iln~ernnce
of Drilled Artesian Wells With a Wate r-Yielding Crater Instead of
a Filter
best conditions under which they may be drilled are
the following: 1) the top of the water-bearing sand
must consist of crumble-proof rock; 2) the water-
bearing stratum must have a minimum pressure of 15 m.
In addition, the new wells have the following good
points: 1) on the average, construction costs are
down 200%; 2) the saving in metal for casing pipes
comes to 300`16; 3) drilling is carried out 300-400;^Ia
faster. There are 5 diagrams and 3 tables.
ASSOCIATION: Voronezhskaya ekspeditsiya "Rosgi rovodkhoz" (The Voro-
nezh Expedition "Rosgiprovodkhoz"~
Card 212

LOBOCHIMIN, T.M.
WAter supply on livestock farms of the Central Black Zart.a
Region. Vod.i aan.tekb. n0-3:17-21 Nr 160. (RIU 13:6)
(Central Black Barth ReGion-Water supply, Rural)

0 43 0 j), K, /1/1,
HOSIROY, Zinoviy Alekseyevich; MARTSINYUK,Ya.P. redaktor; SVESHNIKOV.O.A.,
kand.idat arkhitektury, redak-tor; WBOD.K.M.. inzhener, redaktor;
ZXFMXOVA,Ye.Te., tekhnicheskiy
[Carpenter*s and joiner's work] Plotnichnye i stoliarnye raboty.
Kiev, lzd-vo Akademii arkhitektury USSR, 1955. 349 P.
(Carpentry) (KLRA 9:1)

RODIONOV, V.14.; CHUDINOVSKIKII, A.V.; AIROKOL'SUYA, Zh.A.;
Inclusion of s35-methionine into blood proteins in irradiated
aninals following blood loss. Biul.ekep.biol. I med. 47
no.6:43-47 Je '59. (HIR& 12:8)
1. Iz Inntituta bioloeleheokoy I neditainakoy khinii (dir. -
deystvitel'nyy chlen MM SSSR V.1f.Orekhovich) MW SSSR, Moskva.
Prodstavlona 4eystvitellnym chienom A1411 SSSR V-71-Orakhovichem.
(1-0,11THIONINE. in blood,
blood protein uptake of radioandium-labeled
methionine In x-irradiated animals after hemorrh.
(Rus))
(1011101UMV,H, expor.
same)
(BiA)oD rRoTEms,
same)
(11OWTG141f RAYS, eff.
same)

RODIONOV, N.F.; LOBODA, A.I.
Study of dust in the air during the operation of excavators.
Sbor.nauch.trud.Kriv.fll.IGD AN URSR no.lsl7l-175 162.
(MIRA 16%4)
(Mine dusts) (Excavating machinery)

SHESTAKOV, M.M., inzh.; MIKRAYLOV, V.A.,, kand. tekhn. nauk;
LOBODA, A.I., inzh.; RODIONOV, N.F., inzh.
Construction and operation of automobile roads in Krivoy,
Rog Basin open-out mines. Met. i gornorud. prom. no-51
61-64 S-0 163. (KrRA 16al)
1. TSentrallrvy gornoobogatitellrqy kombinat, Krivoy Rog
(for Shestakov). 2. Krivovozhskiy filial Instituta gornogo
dela AN UkrSSR (for Mikhaylovp Loboda, Rodionov).

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coaftrowe 00 suel Prolhtim, 30

IODKOVSKIY, S.A., kand.tekhn.nauk; LOBODA, A.S., inzh.
Effect of calcium on the plastic properties of the E1765 alloys.
Metalloved. i term. obr; not* no,6:37-59 Je 161. (MIRA 14:6)
1. TSentralInyy nauchno-i7esledovatellskiy institut tekhnologii
mashinostroyeniya. (Nickel alloys--Metallography)
(Plasticity)

.Ii~ AUTHORS: Iodkovskiy, S.A., Novitskiy,
Kudellkin, V.P., Topilin, V.V.,
TITLE:
S,/765/611000/000/00VO03
Lobod Burylichev, Q'i 1. ,
V. K.,
Sidfryayev, N.A., Molev, D.S. N'.
The effect of the wall thickness of the mold on' the quality of nickcl-~ba5e-
alloy castings.
SOURCE: Slitok i svoystva stali; trudy V konferentaii po fiziko-khimichcsl,*m
osnovam proizvodstva stali. Moscow, Izd-vo AN SSSR, 1961, 47_~o,
TEXT: The paper describes an experimental investigation intended to impk-ove
the quality of large-size gas-turbine components. The investigation is concerr", d
with -the'fundamental defect of highly alloyed Ni-alloy castings, poured into o nary
molds with a vertical taper of 5% and a b/r ratio of 0.55-0.75, namely the prc#ence
of internal fissures of thermal origin. The investigation is directed toward the
elimination of one of the two possible causes of internal fissures, namely, the
stresses which arise as a result of the great difference in temperature (T) along the
cross-section of the casting during solidification and cooling. To counteract this
effect, the T gradient along the cross-section of the casting must be reduced.
Practical means for this purpose include either the reduction of the heat capacity
and the heat conductivity of the mold material, the heat rejection of the external
Card 112

The effect of the wall thickness of the mold .... S/765/61/000/000/002/003
surface of the mold, or a change of the mass of the mold itself (through the use of
molds with a reduced wall thickness). It was found that, for castings of the weight
range investigated (50-150 kg), the principal factor that determines the rates of their
solidification and cooling appears to be the mass of the mold itself. The thinner
mold heats up more rapidly than the ordinary thicker mold, and the T gradients are
substantially reduced. The investigation also covered the effect of an external theri-na:
insulation layer applied to an ordinary and a thin-walled mold on the macrostructure
of the castings and on their rate of cooling. A decrease of the wall thickness of a
rnold to a b/.r ratio of less than 0.30 results in a significant decrease of the mass of
the mold, a reduction of the rate of solidification of the casting, a reduction in the T
diffCrence between the periphery and the axis of the ingot, and, as an ultir~ate con-
sequence, in an absence in.,tho casting of any internal thermal fissures. There is no
appreciable change In macrostructure, but a casting poured into a thin-walled and
the rm ally- insulated mold is completely free of internal fissures. The experimental
thin-walled molds were used in actual production in the pouring of ~ighly-alloyed
Ni alloys in castings of 500, 700, and 750 kg, and resulted in the elimination of
internal fissures and in a reduction of the number of low-grade rejects as identified
by ultrasonic inspection. There are 7 figures and Z tables; no references.
Card Z/Z

T 12411~-6.15 MJT(b) Pf -4/pad/
-1.zll S--L
P - 7P-u--~- JD/M1/JG/M&
ACCE.SSION NR: AT4046844 S/0000/64/000/000/0209/0215
AUTHOR: Iqdovskly, S.A., ICqdel1k1n, V.P...Lobod a, A. S.
TITLE: Effect of calcium on the plaaticity of nickel alloye
-.1 11
SOURCE: AN 99SR. auc I um, U)
_yay, Isslcdo
LUroblewc zharoMqchqy!Mjs2Ia
vaniya staley I oplavov (Studies on steC114 aiij-afl-o~F) --M-osc5*w-. Izd-vo Nauka, 1964,
TOPIC TAGS: nickel alloy, nickel alloy plpf ticity, alloy plasticity, calcium admixture,
are furnace, induction furnace
--kLISTRACT: It is very difficult to S-leform hcat:.resistant alloy's on a nickel base with
nd
-L-1,tp~,,:tkqn! 141EA&Leq4ni-.,~,t1urnlnum ti jitwdu~pV affloying elements. Even precise
bitching doeg not always result. In stable plaritic properties of the melts fti are furnaces.
,ir)wf-,Ver, in inductloa fiir-naces, fic rn(,-1t,,4 hnpro~,cd -m(' inore stablc proporties.
it llffer!~ in theso molts. Ln melts
ii lvosLigat,iuns have showi, that tho ralciurn ~;oritei
F-11111 Ifiductioll ful,1111C.'-s. the calcilun oontent varfe.,; from 0. to I). 012"l), whIle bi
,nelts froin are furnaf,es It varies between 0. 013 and 0 ~sven roaching fl. 020f7,.
The highler calcium content obtained 'In the arc turnace I's emlain(lr~ bv the reduction of
Card 1/4

L 12414,1155
ACCESSION UR: AT4046844
0
calcium oxide from the slag by aluminum or Ionized carbon at the are. Several articles
have beon published recently on the effect of small additions of rare earth and alkaline
earth elements. After a certain limit, an increase In the concentration of these elements
vieakens the grain boundaries. In Liho present study, test melt3 were made in are and
induction furnaces with the addition of 0. 01 - 0. 2% calcium. In the first series, the
calcium was added directly to the ladle before pouring. These tests showed that the Ut
alloys were forged properly only when the residual calcium content did not eKcced
0. 015'.,!. In the second series, the calcium %vas added to the furnace. The forging
capacity of the metal improved as the calcium was burnt out and the final calcium
content usually did not exceed 0. 015%. The curves in Fig. I of the Enclosure show
that increasing the calcium content to 0. 1-0. 27o increased the inpact toughness, with a
m aximurn at 1050- 1200C. In a laboratory are furnace of 0. 5 ton capacity, the Intro-
duced calcium resulted in a 0. 03% Ca content with a low plasticity of the alloy. During
Induction melting of the arc furnace melt, the content of alloying elements did not
change due to additional charging, but the Ca content was lowered from 0. 018-0. 020
to 0. 012-0. 014%. The article concludes that an Increase of the residual calcium in
cam 2/4

L 12414-65
ILCCE"MON NR: AT4040%44
Ni alloys, above 0. 01511 leads to lower plasUc propertlea. Part of thle Ca can be burnt
ci-,it in inducHon furnaces. IntrodueMon of U. 1% Ca with subsequent burning out leads
t'.) b-I.ter plastic propertico. 'nic best 141 alloys are therefore obtained in induction
I
I.Arnacoe, not in tire furnacee Orlq7. art, hae-, 3 f1puree, 4 tp-blo3 and 3 formulas.
I'TED-. 1G)Jim(M ENCL: 01 SUB CODE: MM
NO REF SOV: 000 001
c.,d 3/4

VOINOV I YeA. (Kiyuv,, Vorovoku-co 31u, kv.17); 1'.Ya.; L.'XIiGIII-'FKO,
M.P.; LOBCDA, I.P.
X-ray, radio and surgicai method for treating internally or ex-
ternally located cancer. Klin, khir. no.3:12-18 165.
(MIRA 18:8)
.1. Radio-khlrurgicheskiy otdol (zav. - zasluzhennyj doyatell nauki,
prof. I.T.Shevchenko) Kiyevskogo natichno-isoledovatellskogo rontgeno-
radiologichoskogo i onkologicheskogo instiLuta.

LOBODA, I. P., aspirant
Two observations of cysts of the pancreas. Nov. khir. arkh. no.2;
73-74 162, (MIRA 15:2)
1. Kiyevskiy naucbno-issledovatellski7 rentgeno-radiologicheskiy
i onkologicheskiy institut.
(PANCREAS-DISEASES) (CYSTS)

If"LCIA
LC i CL:,.J re cc rd Jumps 7.
vol. 11 , M. I-1c), July iq'~',
6'Fti,111 LTA FCLSFA.
I -1-CHINUCC-Y
~jarszawt,, Poland
So. -ast Luroi~eEin Accessicri, Vol. 5, 1-4'Co' 1 95t,

LOBODA, K.M.
......
Furniture manufacturers of the Ukraine improve their
production. Der.prom. 14 no.11:1-3 11 165.
(MIRA 18:11)

RDDIONOV, V.M.; ANTOKOLISKAYA, Zh.A.; CHUDINOVSKIKH, A.V.; -LCBODA, L.A.
Preparative method of electrophoretic separation of blood proteins
in starch gel. Lab.delo 6 no.1:23-25 Ja-Fe 160. (MIRA 13:4)
1. Iz institute. biologicheakoy i meditsinakoy khimil AMN SSSR,
Moskva.
(BLOOD 120TICINS) (UMTROPHORNSIS)

L 28441-66 EWT(m)/EWP(J)/T UP(c) WW/RM-
51
ACC NRt AP6017878 SOURCE CODE: UR/0061166TO00/005/ 2
r
AUTHOR: Kotlysievskiy, 1. L.1 &nine, A. S.; Shergina,_S. I.; Loboda,
ORG: Institute of Chemical Kinetics and Combustion, b-pak#A_~e2art-
5M
ment, Academy of Sciences SSSR (Inatitut khimicheskoy kinetiki i
goreniya Sibirskogo otdeleniy.a Akademii nauk SSSR)
TITLEs Highly unsaturated polymers. Communication 16. Polyacetylene
compounds, derivatives of di-, tri-phanylmethans and diphe'nYletRan
SOURCE: AN SSSR. Izv,estiya. Seriya khimicheskaya, no. 5, 1966,
902-908
TOPIC TAGS: organic semiconductor, semiconducting polymer, heat
resistant polymer, polyac*etylone, polyarylene . o1igomer
ABSTRACTt New highly unsaturated oligomers IV and VII (see below)
having alternating arylene and diacetylene oups in the backbone were
prepared which combine high heat resistanceKand solubility in some
organic solvents, It is noted that such oligomers are of practical
interest, dven if their electrical conductivity proves to be low, for
ouch applications as heat recistant dielectrics. Oligomers IV and VII
were prepared as follows: 1.5-

L 28"1-66
7878
0111COBt pol ell$
let,
CLTICO-
Hc=c
NON11,
PCIN GITICC13 A_CH
Alcla clisco. \.=/
Clisco-O L- CITIC011-0
(Vill)
Hceac
40
.-Lca-rd

L -28441-66
MAI 4141%1
Oligomers I and III
H(C=C-/,
_04 -CMC)"11 11 (C- N,
were prepared earlier. Owing to the presence of a methyl substituent,
oligomer IV, unlike 1, was almost fully soluble in pyridine. Oligomer
IV was obtained in the form of light-yellow films; it did not fuse up
to 500C.but darkened at 340C. Oligomer VII had apparently a tridimen -
sional network structure; a dark brown powder, it was much darker in
color than I and IV. VII gave a narrow intense EPR signal, indicating
the presence of conjugation despite the formal disruption of conjuga-
tion by the CH groups present between phenyl rings. A number of
monomers, mono-# di-, and triacetylene derivatives of diphenyl-methane
and -ethane were also prepared. [SM)
SUB CODEs 07/ SUBM DATEs 25Dec63/ ORIG REP: 002/ OTH REP: 001
ATD PRESS107,0,0-

LOBODA, L. F-, Doc---Mod Sci -- (diss) "LPilOP tic syndromes
Following Gunshot Wounds of the Cerebrum (Clinical Pictul'O and
Course in Late and Remote Periods)-" mos, 1957. 19 pp (Acad
I-led Sci USSR), 200 copies (KLj 49-57, 115)
- 57 -

d,),,- 1 11. ~' ~
VJ", ~Or t.,101-ilauk; LOI~ITA,
r I.Ilificw r:c)rtrol i.n rijc~imbprs. Khin. prom-
New fanvlni,je for pf"Wrio (MIRA 18:4)
[Lr,(r.] no,l :47)--';,l j',!- I-Ir '~,5.

AF(Ri IN, K.B.; BURTSEV, K.I.; BYSTROV, S.N.; VnMTS, G.B.; 'ICDIlvV, G.G., VCRONIN,
A.B.; GSVLIGH, A.S.; GRYAZHO'V, U.S.; GUDIM, A.F.; GUSYATINSKIY, M.A.;
DVCIRIN, B.S.; DIDENKO, V.Te.; DMITRIM, H.H.; DCUM, M.M.; DaROGOBID,
G.M.; ZHDANOV, G.I.; ZAGCIRULIKO, A.I.; ZELMD.TSXIY, A.G.; IVASHCHENKO,
Ta.U.; KAFTAN, S.I.; XVASHA, A.B.; KIRRYEV, A.D.; KLISHEVSKIT, G.S.;
KOZYREV, V.P.; KOLOBOV, V.N.; LGAIAN, K.I.; IFITTES, V.A.; LFJUM, B.Z.;
LTgAW&A.; LUBINETS, I.A.; MARDRYKIM, I.I.; MUSTAPIN, P.A.; NWIIRCVSKIY,
fW..; NEFEDOV, V.A.; OBUKH(YVSKIY, Ya.M.; PRRTSY.V, M.A., PETROV, I.D.;
PODCIROMIANSKIY, M.O.; POPOV, A.P.; RAK, A.I.; REVYAKIN, A.A.; ROZHK07,
A.P.; ROMGAUZ, D.A.; SAZCKOV', S.A.; SIGALOV, H.B., STC14AKRIN, Ta.B.;
TARASOV, S.A.; FILnPOV, B.S.; FRIDMAN, U.K.; FRISHBERG, V.D.: KHARIKOV-
SKrY, K.V., KHOLOPTSAV. V.P.; TSARHV, M.N.; TSOGLrN, W.M.; CHERNYY, I.I.
CHMOK, V.T.; SHWXOV, A.K.
Sa=il Berimovich Bnm o.Koks i khim.ne.6:64 156. (MLRA g::Lo)
(Brmms, Samiil Berisevich, 1910-1956)

SOV/68-59-3-17/23
AUTiMR: Loboda, N S.,
TI12LE: Some New Forms of Acid. Resisting Coatings (Nov-&e vidy
kislotoupornykh pokrytiy)
, pp 58-59 (USSR)
PERIODICAL:Koks i Khimiya, 1959.9 Nr 3.
ABSTRACT: Smeiyanskiy Aazhine Building Works started the production
o:r enamel tubes and apparatus, the applicability of which,
for operation in corrosive media at 80-900C, is discussed.
ASSOCIATION:Dnepropetrovskiy Sovnarkhoz (Dnepropetrovsk Sovnarkhoz)
Card 1/1

AUTHOR: Loboda, N.S. SOV68-59-5-10/25
TITLE: Development of the Chemical Industry in the
Dnepropetrovsk Economic Region (Razvitiye khimicheskoy
promyshlennosti v Dnepropetrovskom ekonomichegkom rayone)
PERIODICALs Koks i khimiyal 1959, Nr 5, pp 28-29 (USSR)
ABSTRACT: In the Dnepropetrovsk Sovnarkhoz a common directorate of
the metallurgical and chemical industry was established.
In this way the coking and the chemical industries are
under the same direction, which has had a positive
influence on the development of these two industries.
Special stress was put on the utilisation of local raw
materials and coking by-products in the production of
plastics and synthetic fibres, A brief outline of
proposed developments is given. Main points: research
work on the production of thermo setting resins from raw
and higher phenols; production of new plasticisers from
naphthalene, toluene and formaldehyde; production of
plastics from acetomphthene, anthracene and phenanthrene
with formaldehyde by the condensation and oxidation and
Card 1/2 hydrogenation methods; production of ditolymethane;
studies of electrochemical oxidation of benzene;

SOV/68-59-5-10/25
Development of the Chemical Industry in the Dnepropetrovsk Economic
Region
the production of terephthalic acid etc; production of
furfural from agricultural waste (experimental
installation is erected); a plant for the production of
chlorine is being designed; hydrochloric acid, produced
as a by-product in chlorination of saturated hydro-
carbons, will be used for the extraction of manganese
from tailings of manganese ore for subsequent production
of manganese free from carbon; a plant for the
production of ammonia from hydrogen from coke oven gas
Card 2/2 and nitrogen from the oxygen plant with subsequent
manufacture of liquid fertilisers is being considered.
ASSOCIATION: Dnepropetrovsk Sovnarkhoz

PLIT, I.G.j KUZNETSOV, Ye.G.; LOBODA, N,S~; SHEVC1k,11KO, A,I,
Investigation of the process of hydrogen sulfide removal from
coke-oven gas by potassium solution3 in a scrubber with a
pulverizing-atunizing plate, Koks i khim. no.10:42-.47 0 161~
(MIRA 15:1)
1. Dnepropetrovskiy khiaiko-tekhnologicheskiy institut (for
Plit). 2. Stalinskiy sovnarkhoz (for Kuznetsov). 3. Dnepro-
petrovokiy solmarldioz (for Loboda). 4. Yasinovskiy koksokhimi-
cheskiy zarrad (for Shevchenko).
(Hydrogen gulfit7e)
(Gas purification)
(Scrubber (Chemical technology))

LOBODA,, H.S.
Coke and coal chemicals in the Dnieper Economic Region.
Koko i khim. no.1:3-5 164. (MIRA 17:2)
1. Zamestitell nachalinika upravleniya chernoy metallurgii
Pridneprovskogo soveta, narodnogo khozyaystva.

1!. Y(..
Lcl-,O(I.l 11- ye- "Thel !--e-ep of and
9, 194", r,.3'
";0. 13, l9tM
11-3566, 11' I'larch 53, (Letopis '71tur al Inykli

USSR / Farm Animals. Sheep and Goats. Q-3
Abs Jour Ref Zhur - Biol., No 10., 1958, No 45213
Author Lobodat N. Ic...
Inst Not Uv~en -
Title The High-Producing Flock of the Kirgiz Fine-Wool Breed of
Sheep.
Orig Pub Ovtsevodstvo, 1957, No. lo, 16-aD
Abstract The article gives the characteristics of the Kirghiz
fine-wool breed of sheep which was obtained through a
complex three-breed crossing (Fat-rumped X Precoce X Caucasian)
and through a further improvement by the Askaniyr- breed.
The ewes are characterized by n high productivity and belong
to the wool-meat type. The average live weight of rams is
115.2 kg., their wool yield is 12.4 kg. (6.2 Ig. of pure
fiber), and the perforarmce of ewes is 65.2 kg. and 5.3 kg.
(2.83 kg.), respectively. Me wool is of staple structure,
Card 1/2
20

LOBODA, P.P., inzh.
Effect of low-frequency mechanical vibrations on the rate
of dissolving. Pishch. prom. no.2:140-145 165.
(MIRA 18:11)
1. Kiyevskiy tekhnologicheskiy institut pishchevoy promysh-
lennosti.

-T
AUTHORS:Kvachevt E',N. and Loboda, S.I. (Engineers) 100-4-12/16
TITLE: Mechanism for the prestressing of reinforcement of uniform
profile by hydraulic method. (Ustanovka dlya uprochneniya
armatury periodicheskogo profilya s gidravlicheskim
privodom).
PERIODICAL: "Mekhanizatsiza Stroitel'stva" (Mechanisation of
ConsTFU-Rion), vo.L.J.4. No.4, pp'.26-27 (USSR).
ABSTRACT: This mechanism for tensioning of the reinforcement allows
the operator to observe the progress of tensioning and the
cessation of the cold flow of steel'. The process is discon-
tinued automatically when the predetermined stress is
reached. The apparatus consists of rolled steel joists
which form the base, which has fixed to one side adjustable
anchors and to the other side enhydraulic cylinder with a
detachable grip ing mechanism. The latter comprises a base
plate, 170 x l;8 x 14 mmy with a 60 mm aperture, in which
the body of the mechanism is fixed. The gripping cones are
made of steel Mark Y-7. The hydraulic cylindervN-183. is
used; it operates at a pressure of 40 to 50 kg/cm2. The
hydraulic actiou.is brought into play through a suction
1/2 unit which consists of: a hydraulic pumptnIP12, which is
identical to the one used in the excavator ?-5059, an oil

Mechanism for the prestressin of reinforcement of uniform
profile by hydraulic method. ~Cont.) loo-4-12/16
tank, an hYdraulic distributor similar to the one used for
the automatic.loader J13A-4000 A diagram of tinsioning of
steel Mark Ct.5 shows that the cold flow ceases when a
2 to 2`5% elongation has been reached and further elonga-
tion tLes place by increased tensioning. The hydraulic
cylinder allows tensioning up to a length of 60 mm (original
length of the bar = 11 m) which corr 'esponds to 5.5% of the
original length. Steel rods Mark Ct.5 and 25rc with a dia-
meter of up to 18 mm were tensioned. The capacity is 70 to
80 r'ods per hour. This work is carried out Py one opera-
tive. The weight of the apparatus is 600 kg. The follow-
ing points are criticised: bulkiness, complicated designv
2/2 unreliable control of tensioning and the early wear of the
screw adjustment.
There are 3 figures.
AVAILABLE:

YICEIGIN, A.F., dotsent; LOBODA, P.A., inzh.; SALTAIC"N, A.D., inzh.; Yilj~Y'A,
V.D., dotsent
Experimental desit:.n of the cutter of a stoping cutter-loader. Izv.
vys. ucheb. zav.; gor. zhur. no.1.1:91-94 161. O"IRA 15;1)
1. Karagandinskiy politekbnicheskiy institut. Hekomendovana kafedroy
g,3rnykh mashin i rudnichnoCo transporta.
(14ining machinery)

WBODA, T.; ONOYKO, I.
Operation of motorbuses and taxicabs under public control. nvt.-
transp. 40 no.2:8-9 F '62. (KIRA 15:2)
1. Ukrainskiy respublikanskiy sovet profsoyuzov.
(Motorbusu.;) (Taxicabs)

LOBODA, V.,,general-mayor
'__ ~-O~fficers in the development of the armed forces of the U.S.S.R.
Voen.vbet. 37 no.2:12-21 Y '58. (MIRA 11:2)
(Russia--Armed forces)

KOZHEVNIKOVY S.N.; SKICHNO, F.Ya., kand.tekhn.nauk; LENSM, A.N.v inzh.;
_,~BODA,_V.M.,_Jnzh.; BOLISHAKOV, V.I., inzh.
Determination of optima conditions of reduction mil-I operations.
Trudy Inst.chera.met.AN URSR 16:70-477 162. (MIRA 15:12)
(Rolling mills-Electromechanical analogies)

LOBODA, V.M., inzh.; CIIUDNOVSKIY, V.S., inzh.
Electromagnetic drive for the cut-missing mechanism of
flying shears. Mekh. i avtom. proizv. 19 no.5:27 My 165.
(MIRA 18:11)

LUGPIISKIY, N.I.; IMQAA,-,-Yu.I.-- .
Coqverdon of unithiol in the body. FarmA taks. 23 no-4:349-355
~I-Ag 160. (MIRL 142-3)
1. Ukrainskiy nauchno-iseledovatellskiy sanitarno-khimichookiy
institut.
(UNITHIOL)

1. LOBODA%V, N.S., KVACHADZE,Ni.I.
2. USSR "(600)
4. Roads - Maintenance and Repair
7. Winter plane for automobile log roads.
Alg'
Les.prom. 12. A 1952
9. Mnnt& List of Russian Accessions, Library of Congress, March, 1953.Unclassified.

WBOD&W, Marcell ingo
Using rheology for studying bitumen behavior. Rev transport 10
no.9&402-41Z S163
I

1. LCTOIN, P.
2. USSR ((a-,)
4. ?etroleu-q industry
7. Inorcvina the u-e of c.-ectric ,:)ower in the oetroleurp. industi-f. Za ekon. T'Xit. no. 4.
152.
9. Monthly List of Russian Accessions, Library of Congress, February 1953. Unclassified.

IVANOV, Nikolay Vasillyevich-, MALYUTIN. Kilkolay Kuztmich; PUYSUMAN, Abram
Llvovich; BURSUTAYN, I.I., retsenzent; LO DIA .&Y, retsenzent-
MOROZOT, A.N.. retsenzent; LYUBOVICH, fuu~.B-1.11M :Mrt okoaomiche;klkh
nauk, radaktor; TMIN, A.T.. tedaktor izdatellstya; UVAROVA, AJ.9
takhnicheekly redaktor.
[Supply of materials and equipment In machinery manufacturing] Material,-
no-takhnichaskoe snabzhenie v mashinestroatii. Moskva, Ges.nauchno-
takhn.izd-vo mashinostroit.lit-ry, 1956. 275 P. (MIRA 10:4)
(Machinery Industry)

_2 I
A i 1 2. , . i
13
J-A
Ig v
to
fat- A Ali 1~ozl 6
nil 141 - .1 4 L
An -
s R -

PHASE I BOOK ZOWITATION SOV/4316
SOV/2-S -97
Leningrad. Glarnsys, geofizicheskiLya observatoriya
Voprosy atmosfernogo, elektrichestva (Problems in Atmospheric Electricity)
Leningrad.. Gidrometeoizdat.. 1960. 115 P. (Series: Its: Trudy'v vyp. 9T)
Errata slip inserted. lpOOO copies printed.
Sponsoring Agency: UM. Glavnoye upravleniye gidrometeorologicheskoy sluzhby.
Ed. (Title page): IX Moyanitov., Candidate of Physics and Mathematics;
Ed. (Inside book): T.V. Ushakova; Tech, Ed.: N.V. Volkov.
PURPOSE: This publication is intended for meteorologists and scientists concerned
with the problem of atmospheric electricity. The book can also be used by
graduate students at hydrometeorological institutes and by university students
studying physics of the atmosphere.
COVERAGE: This issue of the Transactions of the Main Geophysical Observatory
im. A.I. Voyeykov.contains works = problems in atmospheric electricity
written from 1954 to 1958. Individual articles deal with the electrical phenomena
associated with thunderstorms,, clouds, rains, and fogs. Observational techniques
Card 1,4

?robless in Atmospberic Electricity
MV/4316
and instruments used are described, No personalities am mentioned. References
accompany indivi&,-l articles.
TAZZ OF CONTMMt
Inyanitov., I.M. Changes in the Atmospheric Electrical
Field Dmljqg Solar Eclipses 3
Imyanitov,, I.M. Use of Data, on the Electrical Fields in Thick
CwmLUW and Nimbus Clouds by Aircraft to Avoid Storm Areas 5
Tmyanitov., IA.., and V.V. Mikbalovskaya,, Lavestigation of Cbarges
of Precipitation Particles in the Free Atmosphere 16
.Lobodin, T.V, Some Results of the Investigation of the Electrical
Field Above Oceans 34
Lochp B.F. Diurnal Variation of the Number of Thunder Discharges 39
Kolokolov., V.P.., and K.A. Samenov. Measurement of Rain Charges in
VoYeYkovo in 1958 43
Card 2/ 4

Problems in Atmospheric Electricity SM/4316
Makhotkin., L,G, Changes in the Charges of Dmpkto During
ZVaporation 48
Makhotkin., L,G.,, and V.A, Solovtyev. Electrical Charges of
Droplets in Fogs and Clouds 51
Xakhotkin., L.G. and V.A. Solovtyev. Electrical Characteristics
of the Atmosphere During Fogs 63
Izergin., A,N. Irwestigation of Components of Vertical Electric
Current to the Ground 87
Tammet.9 Kh, F..9 and Z,V,, Sepper. On the Tbeory of an Electrostatic
Fluxmeter 97
Filippov, A. Kh. Investigation of a Galvanic Bath for Model
Measurements in t&e Research on Atmospheric Electricity 101
Card 3/4

Problems in Atmospheric Klectricity SOV/4316
Filippor., A. Kh,., and A.L Tyatrin, Simplified Recording of
the Potential Gradient of the Atmospheric Zlectrical Field 104
Furman, A.M, Distribution of Light end Medium Xons in the
Atmosphere According to Their Mobility and Concentration lo6
AVAILAM: Librwy of Congress
Card 4/4
JA/dvm/m"
lo-14-6o
M

AUTHORSt Imyanitov, I. M.,'Lob-od qj._T. V..-
451o6
8/531/62/000/136/001/007
A052/A1O1
TlTLEs I.nvestigation of the electric structure of shower- and thunder-
clouds
3OURCE: Leningrad. Glavnaya goofiziohookaya observatoriya, Trudy.
no. 136, 1962. Atmosfernoye alaktrichostvot 3 - 20
TEXTs The results of more than a hundred measurements of electric
field distribution near peaks of and underneath shower- and thunderclouds
are discussed. The investigation aimed,on the one hand at collecting data
about the electric structure of shower- and thunderalouds and, on the
other hand., at obtaining material necessary for refining the methods of
these measurements. It was carried out by means of aircraft- in the far-
eastern regions during Auguet-September 1959 by the State Scientific-
Research Institute of Civil Aviation in cooperation with the Main Geophy-
sical observatory im. A.'I. Voyeykov, Central Aerologioal Observatory and
Central Institute of Weather Forecasts. Compared with the other principal
Card 1/3

S/531/62/000/136/001/007
Investigation of the electric structure *too* A052/A101
methods of studying the electric maorostructure of shower- and thunder-
clouds) the aircraft method) while maintaining their positive features,
eliminates many of their shortcomings. An aircraft flying at a high
speed enables to make measurements in a time much shorter than that neces-
sary for.the de'velopment of a cloud, Consecutive measurements near the
same cloud enable one to determine the transformation of its electric
structure. A special equipment can be installed on board-a *ircraft, per-
mitting the full allowance for the distortions of measured fields caused
by the.airoraft. By making several flights at different distances from a
.cloud or by'making measurements by means of iseveral planes at a time, the
di.fficulties'faoed it ground- measurements in determining the magnitude and
distribution of.main charges of a cloud can be overcome. By measuring
hrom'an airoraft,the changes of the field connected with lightning
.atrikes and fol*low'ing at the same time.the oloudg the transformation of
its electric 13-truoture oan.be. studied in detail. The application of planes
enables one to eliminate-distortions introduced by the surface free char-
ges, and also a considerable number of cloud# can be investigated in a
relatively short period of times Another important advantage of the-air-
Card 2/3,

B/53lj62/000/136/ool/007
Investigation of the electric structures## A052/AlOi
craft method is the possibility of obtaining synchronous data relating
both to the. topography of clouds and to the, aerological characteristics of
.atmosphere by means of radart airborne meteorographs and other devices.
The application of high-altitude high-speed planes like TY -104 (TU-104)
widens the potentialities of the aircraft method and gives better.results
than those obtained by using transport planes like JIM-2 (L1-2) and HJI -14
(11,10- On.the other hand the aircraft measurements do not provide
reliable-information on the mesostructure of electric charges, and probab-
ly only a combination of aircraft and sounding methods will enable one to
study bot-h ms,oro- and.mesostruoture of thunderclouds. The airborne equip-
ment for measuring the field intensity is described; the field intensity
pickup is adjusted so that the field produced by the plane's own charge
will-not ~ffeot the indications of the device. The investigation has
shown that clouds in 50% cases carry a considerable excess charge of about
2 coulomb. This charge is located 6 - 7 km obove the earth surface and
the "mirror" effect (the opposite charges of raindrops and the surface
field) may be ascribed to the action of this charge. The polarized clouds
observed are charged to 60% positively and to 40% negatively. There are
9 figures and 4 tables.
Card 3/3

AUTHORt LDbodin, T. V_
TITLE: Snowstorm electricity
45!08
8/53 62/000/136/005/007
A052~AIOI
SOUROEt Leningrad. -Glavnaya geofizicheskaya obeervatoriya. Trudy.
no. 136, 1992. Atmosfernoye elektrichestvo, 62 - 76
TEXTt Snowstorms are accompanied by complex and very intensive elec-
tric proceoses taking place at the collision, desttuotion and friction of
ice crystali,. The absence of commonly accepted methods, of a reliable
inertia-less equipment and of comprehensive measurements of atmospheric
electric characteristics has led to a state that at present the snowstorm
electricity is insufficiently investitipted. The. article gives average
monthly atmosphere electric potent
I ~vLl gradients, volume charges and point
discharge currents during snowstorms and drifts. It is based on observa-
tions madeat the Mirnyy observatory (Antarctica) in the period January 1958
- January 1959. For measuring the atmosphere electric potential gradient
the electrostatic fluxmeter of rro-type (UGO - the Main Geophysical
Card 1/5

Snowstorm electricity
3/531/62/000/136/005/007
A052/A101
Observatory) was used. The measurements have shown that the sign and
value of the gradient depend on a number of meteorological characteristics.
The highest values are observed during storms without a snowfall and the
lowest during snowdrifts. The recorded extreme values ares E min
9 . '104 V/M' E 2.3 - 104 v1m. The value and sign.of the gradient
max I
during snowstorms and drifts depends on the wind velocityq the amount,
temperature and physical state of the driven snow. The gradient increases
with the wind velocity, reaches maximum values at v - 19 m/sec, then de-
cieases rapidly and reaches zero at v - 25 m/sec and maximum negative
values at v\ 25 m/sec. The gradient is proportional to the amount of the
driven snow/up to v - 19 m/sec and a change of the amount of snow of
~.5 g/m sec corresponds to the gradient change of 1 v/m. The gradient
increases with the decrease of temperature, reaching maximum values be.-
tween - 200 and - 250C- It decreases with a further decrease of tempera-
ture reaching negative values at temperatures lower than - 290C. The
connection between the gradient during snowstorms and the visibility is
described by the equation E - A - BlgS, where E is the gradient in v/m,
Card 2/5

Snowstorm electricity A052/A101
S tIL(.' vi.-jibility in m, A - 4,500, B - 900. For measuring volume charges
the Imyanitov's method was used. As n. recording device an electrostatic
fluxiiieter was used, with a metal grid placed I m over the earth. The mean
volume charg-e value is determined by tivi L- , where p is
for"qula 2Ah
volume charge, E is potential gradient and h is the height of tile grid
over the earth. Calculations show that in the middle and lorter parts of
the meter layer about 30V6 of all volwirie charges are concentrated. To
study the noise level conditioned by icrz; crystals hitting a metal surface
(e.6. antenna) a 3 x 5 m metal rotary .3urface was installed connected
by means of a coaxial cable with the input of a d.c. amplifier (20 cycles
to 25 kilocyclea-pase-band). The recorded noise level at wind velocity
of 12 - 22 m/sec was 0.3 - I mv per 1 cl,12. Point discharge currents were
weasured by a device developed tit the Mr~in Geophysical Observatory im.
A. 1. Voycykova. The height of the point was 10 M. An electronic poten-
tiometer was used for recording. At a constant wind velocity the point 0 ..,
discharge current increases at) Lhe tconparature decreases frow 0 to - 20 C,
At te i;ipera Lure s from - 20 to - ~~50C it 11;19 small values of either uign
and the maximum values correspourl to tenperatures below - 290C. The
Card 5/5

S155116210 ))/!36/0'35/rjO7
Snowstorm electricity A052/A101
dependence of the point discharge current on the wind velocLty is de
scribed by the equation i - i0 [1 + th/'(v - 23~ 1 where 1 13 the point
discharge current in ~J-a, io - 1411a, v i~ the wind velocity In m/aec and
,4- 0.1. At v>19 m1sec there i's no diotinct relationship between the
point discharge current at 10 m height and the potential gradient at the
earth. There is no clear-cut relationship either between the point die-
charge current and volume charges in the lower meter layer. Both these
values increase with the wind velocity up to 16 M/sec and then change in
opposite directions. However, within 21 - 25 m/seo range these values can-
have even opposite signs which is connected with the concentrations of
negative charges in the lower meter layer. The following dependences of
~he height of negative volume charge distribution (x), potential gradient
At the earth (E.) and the maximum positive potential gradient (Ez) are
established. x increases from a few cm to 10 - 15 m as the wind velocity
increases,_E and E increase as the wind velocity increases to 19 M/800'
within 19 ~5' m/seaz range Eydecreases and E. increases, at over 25 m/sec'
Ey assumes negative values and E. increases to a certain limit determined
by the maximum carrying capacity of the snowstorm. In most cases during
snowstorms a generation of positively charged particles takes place; the.
Card 4/5

Snowstorm electricity
8/531/62/000/136/005/007
A052/A101
atmosphere receives a positive charge and the earth surface is charged
negatively~ On the other hand,the conclusion can be drawn from the ob-
servations of point discharge currents that due to them the earth during
snowstorms loses the negative charge. Thus during snowstorms a separation
mechanism supplies the negative charge to the earth and corona currents
take it away. To determine the difference between charge and discharge
currents, is not possible as yet. However, it can be taken for granted
that the vast stretches of tip Arctic and Antarctic are the regions of earth
charging. There are 7 figures and 7 tables.
Card 5/5

DffMTOT, I.M.; IDBODINO T.V.
Study of the electric structure of shower and thunderstorm cloWs.
T-=dY GGO no.1360-20 162. (MIU l5t12)
Utmospherie electricity)

LOBODINp--T.V.
Ilectricity of enowstorms. Trudy GGO no.336:62--77 162. (MM 15:12)
(Antarctic regions-Show-Mectric propertim)

ACCESSION NIL: AT4015619 S/2972/63/000/005/0089/0099
AUTHOR: Lobodin, T. V.
TITLE: Results of electric measurements in the atmosphere over the oceans
and in Antarctica.
SOURCE: AN SSS1t.-Mezhduvcdomstvenny*-y geofizicheakiy komiter,. II razdel pro-
.-rraiwny* MGG: Noteorologiya. Sbornik statey, no. 5, 1963. Meteorolo3icheakiya
isaledovaniya (Meteorological research), aq-99
TOPIC TAGS: atmospheric electricity, unitary variation, meteorology, Antarctica,
atmospheric potential gradient, thunderstorm
ABSTIUCT: The Main Geophysical Observatory investigated the characteristics of
atmospheric electricity over the oceans and in Antarctica during the Interna-
tional Geophysical Year. The studies in ocean areas were made aboard the re-
search vessels "Kooperatsiyall, "0b" and "Mikhail Kalinin".' The results of
investi.gation of the unitary variation of the potential gradient, shown in
Fig. 1 of Enclosure, confirm the conclusions drawn from investigations made
by the Carnegie Institution 40 years ago. The alight difference in the time
of onset of extremal values of field voltage of the measurements made in 1957-
and 1915~-1921 is due to the redistribution of thunderstorm activity over
Jr,11 1/7 1 L~,, . . -

ACCESSION %t: AT4015619
the entire globe. The effect of diurnal-variations and meteorological elements
(air temperature, relative humidity, wind velocity) on the distortion of the
unitary wave is insignificant and for practical purposes can7be neglected. Ra-
malcrishnan's experimental data (Indian J. Meteorol. and Geophysics, 1955,
p-171) are used to calculate the changes of world area covered by thunderstorms
during a 24-hour period and the changes of this area for the Carnegie Institution
observations; these changes are shown in Fig. 2 of Enclosure. Changes of unitary
variation are caused by thunderstorm activity. Measurements of electric charac-
teristics in Antarctica gave the dependence of the potential gradient on wind
velocity during the wind transport of snow, diurnal changes of the potential
-radient and annual changes in volume charge, as shown in Figures 3 and 4 of
Enclosure. Orig. art. has:,10 figures and 2 for=las.
ASSOCIATION: Glavnaya geofixicheakaya observatoriya (Main Geophysical Obser-
vatory)
Cord 2/7

ACCESSION MRS AT4024451 S/3010/63/000/013/0034/0037
AUTHORI Lobodin, T. V.
TITLE: Reasons for the annual variation of the potential gradient In the atmos-
pheric electric field
SOURCES AN 3113R. Mezhduvedmstvenny*y gooflalchaskly komitat. Geofizicheakly
byulleten', nos 13t 1963, 34-37
TOPIC TAGS: meteorology, atmospheric electricity, atmospheric potential gradlefit,
atmospheric unitary variation
ABSTRACT: A new attempt Is made to explain the annual variation In the strength
of the atmospheric electric field. At present, the diurnal unitary variation of
E Is attributed to the Influenie of thunderstorm activity, and It has been sug-
gested that the annual unitary variation has the same cause. This has been studied
by the author, who used Remakrishnan's data (Ind. J. Meteors, Geoph., 1, 1950.
The area of the globe occupied by -thunderstorms by season was determined; Fig. I
of the Enclosure coWares the annual variation E (curve 1) and the area on the
eairth occupied by thunderstorm (curve 2), Curves I and 2 not only are not paral-
at' but are In entiphase. Thunderstorm activity therefore does not"determine the
I Farlation 9 and probebty Is not the only factor maintaining a positive
Cfttannua N
1/3
.mffiffiaww~~

ACCESSION NR: AT4024451
charge of the earth. Possible causes can be local variations In the electrical
-conOuctivity ~L and volume chargep of the atmosphere; It Is demonstrated, how-
ever, that neither of these factors can be responsible. The literature is reviewed
In an effort to explain thd phenomenon; particular attention Is given to the sys-
tem of generation of volume' charges and the structure of clouds of different gener&
It Is noted that In the past Investigators have failed to take Into account that
thunderstorm clouds are not all positively charged at the top and negatively charg-
ed at the bottom. The author does not solve the problem; the principal contribu-
tion Is emphasis on the fact that the thunderstorm mechanism Is not s9lely respon-
s Ible for the unitary variation, nor are local variations In X and Orig, arts
has: I figure and I formula.
ASSOCIATION: MEZHOUVEDOMMENW*Y GEOFIZI HESXIY KOMITET AN SSSR (Interdepartmen-
tal Geophysical Comisittes, An aWR)
SUBMITTED: 00 DATE ACQ: 16Apr64 ENCL: 01
SUB CODE-. No REF SOW: Oil. OTHER: 009
Card- 2/3-

A=UIOK MRs AT4024451
so.. P
77"
Fig. Annuat variation of potential gradient (1) and of area
-occupied by thunderstorms on earth (2).
19MCL406URZ t Ol
Cdrd*
;pe,

ACCESSION NR: AT4011514 5/2531/63/000/146/0036/0038
AUTHOAs Lobodint !_,-V,,-
TITLE: The variation of the atmospheric electrical potential gradient at Mirny*y
SOURCE: Leningrad. G)avn. geofiz. observatorlya. Trudyfi, no. 146, 1963.
Atmosfernoye elektrichestvo, 36-38
TOPIC TAGS: meteorology, atmospheric electricity, atmospheric potential gradient,
antarctic meteorology, wind profile, temperature profile
ABSTRACT: The author gives the results of observations of the variation of the
atmospheric electrical potential gradient E made at the South Pole observatory at
Mirny'4y during the IGY (1958). These observations embraced a total of 81 days.
The E readings were made on an electrostatic fluxmeter, designed in the Glavnaya
.&eofizicheskaya observatoriya (Main Geophysical Observatory), with tape recording
by means of an automatic electronic potentiometer. The uniform and even floor
surface, the absence of open qroun~ and radioactive contamination of the soil in
Antarctica explain why an essentia! role in the diurnal variations of the potential
gradient is played by unitary changes, the wind and temperature configuration,
cloud formationsand precip'itation. Curves are given to illustra'te the variations
of E for the different 6nths of the year. The diurnal behavior of E for the year
Card 1 /1&' -
' al?

ACCESSION NR: AT40iI514
was obtained by a weighted summingof all Vie monthly curves, with all curves round-
.ed off according to a sliding-hourly-average formula. Diurnal variations of tem-
perature, relative humidityand wind velocity for 81 days are tabulated. A general
curve for the May-October period is also shown. All the curves show a clearly ex-
pressed maximum at 1800-2000 hours and an indistinct minimum at 0600-1200 hours
Greenwich time. The coincidence of the sum curve of unitary variation with
curves obtained by the author in over-ocean readings confirms the shift in the on-
set of minimal E values toward.0700-1100 hours, In comparison with previously ob-
tained data. Recalling that it has been claimed that a redistribution in thunder-
storm activity over the world is taking place, the author notes that, If this
hypothesis be true, then the correlation factor ki of E variations, obtained"over
the oceans in 1957-1959 and at Mirny*y, should be greater than the correlation
factor k2 , derived in readings over the oceans in the 1016 - 1921 period and at
Mirny*y. Calculations for these factors give the following results: ki a 86%.
ki = 81%; thus, it may be affirmed that at the present time the unitary variation
o E has, in fact, somewhat changFd. The close values for the amplitudes of the
unitary variation of E for the oceans.and the polar regions of the northern and
southern hemispheres (on the average -'44 volts/meter) Indicate, In the opinion
of the author, a stable d1urna) change In the factor* which determine the presence
of a unitary variation of E. It should be noted that close amplitude values for
the unitary E variation are obtained only for a large number of observation days.
Card 2~/"

ACCESSION NR: ATW1514
This may have soine relation to the constancy of the yearly-average diurnal
amplitudes of areas of thunderstorm activity around the world. Original article
has; I table and I figure.
ASSOCIATION: Glavnaya geofizicheskaya observatorlya, Leningrad (Main Geophysical
anservatory)
SUBMITTED: 00 DATE ACQ: 20Feb64 ENCL: 01
SUB CODE: AS NO REF SOV: 005 OTHER; oo4
Card ~ VV3

ACCES.SiON NR: AT4024452 S/3010/63/000/013/0038/0040
AUTHOR: Lob di,n, T- V-
TITLE: Relationship between the strength of the electric field in the atmosphere
and auroras
0
SOURCE: AN SSSR. MezhduvedoTtvenny*y geofizicheskiy komitet. Geofizicheskiy
byulleteni, no. 13, 1963, 38-4o
TOPIC TAGS; meteorology, atmospheric electricity, atmospheric electric field,
aurora, atmospheric phenomenon, atmospheric unitary variation, atmospheric volume
charge
ABSTRACT: Observations on the strength of the atmospheric electric field were
made in Antarctica in 1958*using an electrostatic fluxmeter. Diurnal and annual
unitary variations of E were determined and the behavior of the electric field
during auroras was studied. The conclusions concerning the relationship between
auroras and the electric field are based on 81 hours of continuous observations.
Study of the relationship required a comparison of observations made in the Arctic
and Antarctic. It was found that when there is an increase of E during auroras in
Antarctica there is a corresponding decrease of E in the Arctic; auroras behave
as a positive volume charge in the southern hemisphere and as a negative volume
Card 1/3

ACCESSION NR: AT4024452
in the northern hemisphere. Fig. I of the Enclosure shows the change of E during
auroras at Mirny*y. A problem arises because the amplitudes of the diurnal and
annual unitary variations are approximately the same as the change of E at the
time of auroras. Corrections therefore must be made to compensate for this factor,
although no correctionfor the annual unitary variation is required if the value of
E at the t;me of auroras is compared with the values several hours before their on-
set and after their disappearance. The importance of this correction is shown in
Fig. I of the Enclosure. The world maximum of the unitary variation coincides ap-
proximately with the maximum frequency of occurrence of auroras; therefore, the
maximum correction is for hours with auroras; It Is shown that the correction for
unitary variation of E is about 607. of the change of E. An accompanying table
gives numerical values of the corrections for diurnal unitary variation E. Orig.
art. has: I formula, I figure and I table.
ASSOCIATION: MEZKDUVEDOMSTVENNY*Y GEOFIZICHESKIY KOMITET AN SSSR (Interdepartment-
al Geophysical Committee)
SUBMITTED: 00 DATE ACQ: 16Apr&4 ENCL: 01
SUB CODE: &S I
140 REF SOV: oo6 OTHER: 004
Card 2/3

1TZ
ACCESSION NR: AT4024452 ENCLOSM: o,
0
Fig. 1. Change in strength of th atmospheric electric field during auroras.
I - without correction for diurnaT unitary.variation; 2- with correction for
unitary variation taken into account. (Abscissa time In hours before and after
the aurora.)
Card 3/3

IMYAIIITOV, I.M.; LOBODUI, T.V.
Inhomogeneity zoneig in th-unlieralouds. Trudy C40 no.157:3-8
164

LOBODIN, T.V.
Relation between the unitary variation in the atmospheric
electric potential gradient and thunderstorms. Geofiz.
biul. no.15:49-51 165. (MIRA 18:11)

-1.4' h Z~ T,
9 5 "P.
_T7 r .7 n ~I-F'
AUTHOR: Lobod1n, T. V.
T~i,;'.am-e v a ri at ions in t he 11 - t ill (III ri ~l i
Leningrad. Glavnaya
At mosf~-, moye elekt richestvo (Atmosphe r i c e I ect. rc i
ridust r [a) rad Ii., int 1- 1-
P, q q'R,~ CT In an investigation of industrial radin interference wi',h part f-uldr
-it tenr ion to the long wave ' ength reg i nn .t ~ 14, au t: r ~,i i: 17 p Iqin r,; f i r. I d
'M (peak or mean square) r'inwe a
i-,-LerslLy recorder with a 3 mv/n-3n vi
9 t~~ Tile 2 10 (-,Y,.Ie red i nt r f- r, ~i fr-7 1 1: 1~ i~ -
M. r-Tre 1, 3 il t '3 t i )T1 :t
i- hT i ck factories , an
ss~j 1 :,.- of all the testG 1-ie ""'. th! nh~- f 'm !I.!,-
E- - E, I,` I ~-
where S Is In meters. Orig. art. has: 4 formilas, I figure, and I Lable. 08
Card 1/2

AT5019935
00
7
2/2

~e Star
(MIRA 181S)

ACC NR, AT7001921 SOURCE CODE: UR/3010/6610001017/0059/0062
AUTHOR: Lobodin, T. V.
ORG: none
TITLE: Change in amplitudes of leaders of lightning discharges with distance
SOURCE: AN SSSR. Mezhduvedomstvennyy geofizicheskiy komitet. Geofizicheakiy
byulleten', no. 17, 1966, 59-62
TOPIC TAGS: lightning, electric discharge, discharge amplitude
ABSTRACT: On the basis of experimental data the author determines the character of
the change of the amplitude values of a leader with distance. Construction of the
curves of the rdtlo of the lightning discharge amplitude to the maximal amplitude of'
the leader preceding a given discharge and to the average amplitude of all leaders
of this discharge revealed that they read parallel to one another. This indicated
a proportionality between the amplitude of the discharge and the maximal and average
amplitudes of" the leader. This ratio was found to increase with distance to the dis-
charge. This indicated that the attenuation of the amplitude of the discharge is
less than the amplitude of the leader. The difference in the attenuation of the
discharge and leader amplitudes Increased with distance. The maximal and average
312
amplitudes of the'leader6 decreased"with distance in,proportion to r- . An ad-
vantage of determining the leader amplitude as a function of distance with respect
Card t i-)

ACC NRs AT7001921
to the discharge and leader ratio Is that It is free from errors associated vith the'
calibration and operating stability of the equipment employed. A check of the
character of the decrease of the leader amplitude with distance by two other method
yielded a good agreement of results, vhich indicated the absence of systematic
errors in the calculations and measurements, Orig. art. hast 2 figures.
SUB ODDS: 04/ SUNK DATEs none
2/2

TFSLYA, A.G.; LOBODIN, V.A.
Introducing a filter sampler. Razved. i rikh. nefi-r uc,.,!:
51,.-56 F 164. %MIRA 17:8)
1. Vaesoyuznyy nauchno-issledovateltakiy institut gidrageologii
i inzhenernoy geologii (for Teslya). 2. Krannodarskaya kom-
pleksnaya geologicheekaya ekspeditslya (for Lobodin).

_3
L 38155-66 EVIT (d
ACC NRi AP6025640 SOURCE CODE: UR/0413/66/000/013/0092/0092
INVENMR: Gryts'kiv, 1. V.; Litvinov, I. .; Lobodin,_V. M.
ORG: none 10
TITLE: Airplane cloud-trans2arency meter. Class 42, No. 183440
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki, no. 13, 1966, 92
TOPIC TAGS: airborne photoelectric detection, aircraft guidance equipment, aircraft
flight instrument
ABSTRACT: An Author Certificate has been issued for an airplane cloud-transparency
meter consisting of a light-beam modulator spun by an electric motor, an optical
Fig. 1. Airplane cloud-transparency meter
I - Main illuminator; 2 - additional
illuminator; 3 - photoresistance; 4
photocurrent amplifier; 5 - detector;
6 - direct-current amplifier; 7
electric motor; 8 - modulator.

:7~
X
A
_VZ
~.r V:
a 95
AC NR, AP6025640
ecording devices and a power supply
tem, a reflectors a measuring photocells a r nts of a certain parameters in
Sys In order to obtain direct measureme Lght beam from which is
(see Fig- l)- r circuit is an additional illuminators the lj amplifier to the
the illuminato -or connected through a photocurrent maintains a
detected by a photoresist Lnput which, through the power amplifiers Orig- art
fre-quency-Vhase-detector I ator's electric motor.
constant rotational speed of the light-beam-modul KTI
has: 1 figure j7/ SUBM DATE: 21AVr65/ ATD pRESS:
SUB CODE: %09-
2 / 2 f!~~

MWAMW
LOBODIN, V.P.
tors. 1=-tekh. no.51-46 14Y 160 IMIRA 14:5)
Testing quart2 o0cilla.
r
(oacillatorep ryst&l,-Testing)

LOBODYUqjjEjR;-O A. F. and FEDOROVSKIY, J,. A.
I ..' Use of Ileterogenic Serums in Bloodshed
the 14edical In 4 n -orjjIISt
"An Experiment on es." Trudy VFIII Svezda rhirurgov USSR (Ukre, -a ~, -
and other Surgical Diseas ,
Soviet Republic), Fiev, 1955-

V i I;-
'ov, r- r
C1.7
j;c. 2

A.F.
MOROVSKIY, A.A.. professor (Kiyev. ul. Kudryavskayn, Be, kv.l).,
WBODTOBINO-A-Z.. doteent
Some results and prospects for the use of BK-8 blood substitute for
transfusions in a surgical clinic. Novekhirearkh. no.2:3-6 Mr-Ap '57.
(MLRA 10:8)
1. Kafedra khirargii pediatrichookogo fakulteta (zav. - prof. A.A.
Yedorovskiy) Kiyevskogo maditainBkogo institute
(BIM PIASKA SUBSTITUTZS)

ZMEN, N.H. I dots'; IMODyUcE no=, A-F-, dots*
- -1 - - - . - Ilhirurgll, 35 no.1:145 Ja 3590
Professor A.A. Iledorovskii. (14IRA 12:2)
(BIOGRAMIIM I
Yedorovskii, Alakeei A (Rug))

-I-OBODYUK, L.A.
Therapautin effect of small doses of antireticular c7totoxin
serum in Influenzal 2esions of the retina and the optic nor-;e.
Trudy 1-,,~o MMI 32s97-106 164. (MIRA 1815)

UI-LWSKIY, M.A.; TRESHCHRISKIY, A.I.;LOBODYUK, M.S. (Kiyev).
Use of protamine sulfate in surgery with artificail blood
ciraulation. Vrach. delo no.112133 N163 (KM 16:12)
1. Kl:Lnika torakallnoy khirurgii (zav.-chlen-korrespondent
AMN-SWR, prof. N.M.Amosov) Ukrainskogo ,:.jtituta tuberka-
leza i grudnoy khirurgii.

],'07A!,~' V.A. ( Kiyev 1 er,, cllatilr-., ."I, kV - t-
-cc -17! :V:
I - .. ... , -' ,
,111,TAYUDW .3.1. 1 d,~ G C',
va"y -'-"J/-(~
U.9p of a C'..al"ber ~n
Grud. kl-iz-. 6 nc,.6:3-1(j 10,
1. Otdel biokibernetiki (2,av. - chler-l-orreslondent Alal S E-:') i
11.11. Amosov) Instituta klb~~rnptil-i (direrktcr
T)
Glushkov) AN Ilki-S'..., Kiyev.

S/601/61/000/013/015/017
IYYO D207/D302
A jT I, OH S LabUdguk- V, A. and Khandros, L. G.
T 1T L The form of martensitic crystals and the orientation of
phase boundaries in the copper-aluminum-nickel and cop-
per-aluminum manganese alloys
6 0 "U- -a 0 Ej Akademiya nauk Ukrayinalkoyi RSR. Instytut metalofyzy-
ky. Sburnik nauchnykh rabot, no. 13, 1961. Vuproay fi,
zilk-4 metallov i me tall oved eniya, 147-157
17"~'~`2: "'he authors determined the form and orientation of marten-
itic inclusions in Cu + 14.45 Al + 4.7co Ni and Cu + 14.4c0 Al +
s
Lui i
+ 3c' 1.'" alloys. Alloy monocrystals were cut into rectangular pla-
.es o_F'1-5 x 3 mm cross-section, quenched from 9000C and polished
at- 60 - 700C. This lu-reatment produced large martensitic grains
hich were examined with a)0,< r- 0 (RXSO) x-ray camera, using No ra-
diation and the Laue back-reflection technique. Martensitic grains
ivere wedge-shaped in Cu-Al-Ni monocrystals and their ImidribI
Card 1/2

S/601/61/000/013/0115:/017
T."lie for,.,i o-IL' martensitic ... D207/D302
p,anes were close to ,110),; the planes of the Grain boundarieu
usually coincided with -uh'e '331~, plane, but there were often large
devi,itions from this orientation. In Ca-Al-TvIn monocrystals the ha-
bit planes of martensitic ;,rairis had poles concentrated around a
0 4
Point which was 5 - 60 Of arc from the P33). plane. The conside-
rable scatter of the habit-plane poles was due to stresses during
crystal -rowth. There are 9 figures, 4 tables and 11 references:
ID
10 '"oviet-bloc and 1 non-Soviet-bloc. The reference t) the B'ng-
lish-languaae publication reads as follows: L. C. Chang and T. A.
'lead, Trans. A111-M, 139, (Jan., 1951).
.1 L
S'LlaK.1"ITTED: September 12, 1960
v
klard 2/2

KURDYUMOV, G.V.; LOBODYUK, V.A.; LHANDROS, L.G.
Form of marten6ite crystals and the orientation of the interphase
boundaries in the alloy Cu-Al-Ni. Kristallografiia 6 no.2:210-217
Mr-Ap '61. (MIRA 14:9)
1. Institut metallofiziki AN USSII.
(Martensite crystals) (Phase rule and equilibrium)
(Copper-aluminum-nickel alloys)

S/126/62/014/001/013/018
Xlll/E135
AUTHORSt Lobodyuk, V.A., and Khandros, L.G.
TITLE: Changes in the state of the 0-phase during*
martensitic transformation in a Cu-Al-Ni alloy
PERIODICAL: Fizika metallov i metallovedeniye, v.14, no.1, 1962,
133-133
TEM In previous work one of the authors reported on
fragmentation and recombination of crystals during martensite
transformation and heating. In the present work the behaviour of
a.;ingl* 0-phase grain in a Cu-Al-Ni alloy with 14.4% Al and
4 % Ni (according to the melting charge composition) has been
studied,*u.,,.ing the Laue back-reflection method. Patternf; ivere
obtained from a given martensite crystal during forward and
reverse transformations,~ the camera being provided with a small
heater. The final 0-phaso crystal consisted of six fragments at
a certain angle to each other, Further slight heating led to
rotation of these fragments into their original-positions4 The
fact that heating by only 10-12 *C is sufficient for restoring
Card 1/~

Changes in the state of the S/126/62/014/001/013/018
Z111/Z135
the original 0-1crystal indicates that the l'ow-angl*.bo'undaries
between fraSmente move easily~
'there are 3 figures.
ASSOCIATION: Institut metallofiziki AN USSR
(Institute of Physics of Metals, AS Ukr.SSR)
SUBMITTEDs January 19,* 1962
Card 2/2

LOBODYUK, V.A.; KIIANDUOS, L.G.
Crystallogeometric correlations in the Cu-Sn alloy. Sbor. nauch.
rab. Inst. motallofiz. AN URSR no.17:170-173 163. (MIRA 17:3)

LOBODYUK, V.A.; KHMIDROS, L.G.
Reorientation of the lattice of the martenBite, phase during
transfomation. Dokl. AN SSSR 153 no-4:8(Y7-809 D 163.
(MIRA 17:1)
1. Institut metallofiziki AN UkrSSR. Predstavleno akademikom
G.V. Kurdyumovym.

LOBODYUK, V.A.; KBANDROS, L.G.
Changes in the state of crystals of the initial and m&rtanaite phases
during direct and reverse transformations. Fiz. met. i metalloTed. 18
no.3:409-415 a' 164. (MIRA 17:11)
1. Institut metallofiziki AN UkrSSR.

LOBODYUK, V.A.; KIIXJDft(JS, L.G.
Determination of a macroscopic shift during mrtensits trune-
formationa in GU-Al-Ni alloyr. Fiz. met. i matidloved. 17 no.6:
936-938 Je 164. (MIRA 17:8)
1. Institut metallofiziki AN UkrSSR.

'b -W
551 65 /L A(C) Pi-L/Pad
!JP(c)- JDO/P
~xcmzim im: AE5=7516 M1/0!2G'/64/018/WM057]V0579
3,9
AUMORI-LobokfE, V.. Ael Khandroi, L. G. 3F
TI'ra: Raoriontrztion o! gammOMrthamo cryst dur4-- mrtMite transformtion.
SOURCE: ka matallov i motallovedenlye, Vol. 18, no. 4, 1964v 573-579
TOPIC V.GSt martinraitic ctooll crystal,, physical notcUurcy
.Abstract: In the-- j9.2:)-1 irabsformation' proce.ss 1x4 a Cu-Al-N1 alloy, wed&-,
ing and mutual Interce-ation of cartenaite crystals are observed as well as
the fora"tion of vedge-shaped layers on previoucly forced cryatala. It was
established by the laack refl=tion Laue cethod that reorientation of the
;;crystal lattice takes place in all there carea , Vie whole proccGG takes
place in reverse order during heatlnZ,;
For carrying out the experftents, a M-Al-111 alloy war. chosen (-ih.4~-
p.1; 4.74p IX, in the charge). The Ingot wi`57eaeaTcd Car 10 blcu= at 6900C
a=d re-etangular spzcim=z Oi6-0.8 = thiez v=e cut off. 7-- lorder to optain
large' -zavtans ite phase crystals, the sampl&-avere - 'Innealed in a -microffurnace,
after u ttinor deftrmation, for .12 hours at 8,900~~ 7hey were t%-=- quenched
in a 10% aqueous solution of NaCl, ground and polished at 600 (cb=,;a the
81'
_N
__l ~,2 ~Z,
Z~