SCIENTIFIC ABSTRACT YEREMEYEV, N.V. - YEREMEYEV, V.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001962720007-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S/112/59/000/012/066/097
A052/AO01
Translat-ion from.- Referativnyy zhurnal, Elektrotekhnika, 1959, No. 12, p. 189,
# 25222
AWHOR.- Yeremeyev,- N.V.
TITLE: Automation of Rolling and Press Equipment
PERIODICAL.. Sb. statey. Ural'skiy z-d tyazh. mashlnostr.-1m-. S. Ordzhonikldz-e,
1958, No. 1, pp. 29-55
TEXT: An automatic control of rolling milAAand mechanism3' manufactured
by the plant has bean developed and partly realized for some years past. at the
Uralmashzavod. The following descriptions and circuits are giveni a) automatic
control of the blooming head part mechanisms; Ingot carrier, take in rolling
table, pusher, catch, swivel table and feeding rolling table; b) automatic con-
trol of the blooming working line mechanisms: rolling and working rolling tables,
base rolls, main drive and clamping appliance of the stand; c) clamping appliance
of the blooming mill; d) automatic control of the blooming cutting and finished
product disposal line mechanisms: shears, balance, stamping machine and pusherz
Card 1/2

S1 1 12/59/0W/0 12/066/0 -9 7
Automation of Rolling and Press Equipment A052/AO01
onto the chain conveyer; e) automatic control of plate mill 2800 mechanisms;
f) automatic control of cold rolling mill equipment for pipet of a vwjlng croba..
section; g) automatic control of forging and prevaing equIpment. 'Me work or
pulse automatic control. devices for rolling mills Is consWered, A list IV given
of automatic control devices which still have to be produced to widen the s.~ope
of rolling equipment automation. 71tere are 17 Illustrations.
V~YO.Kh.
Translator's note: This is the full translation of -the original Rusaian abstract,
Card 2/2

YERF~ N.V.
M;.V)
Plans hinge mechanisms simulating multiple-valued functicne of
a single argument. Vest. Mook. un. Ser.1 : mat.,, mokh.16
no.6:49-53 H--D 161. (MIRA 14:n)
1. Kafedra prWa aniki Hookovskogo universiteta.
*(l2MZ=ry--Models)
(Functions)

BORISENCK, I.T.; GENEROZOV) M.N.; YEREXIEYEV) F.V.; KARANYSHKII,
V.V.; KUZOVKXV, Is.T.; WHISE10K, I.T.;_KULIKOVSYAYAJ.F.V.J-'
SAVINOV, G.I., kanddiz.-rzt. naulc, doto. [decenced I
PIROGOV, I.Z.; Prinimali uchastiye: RALAYEVA, I.A.; DAWN,
BELYAYEVA, G.M.; DELYAKOV, V.I.; VELERS11TEY11, R.A.;
ZILARKOV, G.M.; KOHOLEVA, V.Ye.; LITVIV-SEDOY, M.Z.; POPOV,
A.I.; FRIVALOV, V.A.; STUKAIDVA, L.M.; CHISTYAKOV, A.I.;
SAVVIN, A.B., red.; CHISTYAKOVA, K.S., tekhn. red.
[Laboratory work. in theoretical and applied inechanics) Labo-
ratornyi praktil=_ po obshct4i i PL'ikladnoi rekhanike. No-
skva, Izd-vo mosk. univ. 1963. 233 p. WIRA 16:12)
1. Kafedra prikladnoy mckhaniki Moskovskogo gosudarstvennogo
universiteta (for Balayeva, Balakin, Belyayeva, Belyakov,
Velershteyn, Zharkov, Koroleva, Litvin-SqMoy, Popov, Privalov,
Stukalova, Chistyakov).
(Nechanics-Laboratory marmals)

MASLYAKOV, Vasiliy Nikolayovich; ARNSHTEYMp -0.E,# reteenzentj SURINKIN,
A.Djs retsenzent; SIUMPOV, V.H., rod.; YERU4EYEV, P.G,, red.;
FEDTAYEVA, H.A., red. lzd-va; RIDUAYA, L-v.',,"tekbn.' red.
(Raft towing]Buksirovka plotov. 14oskva,, Izd-vo "Rechnoi tran-
sport," 1962. 185 p. (MIRA 15:12)
(Towing) (Rafts)

-002--Y7
A 0

_L 25969-66
ACG VR: AP6005986 SOURCE COMI: UR/0256/65/000/008/0067/0069
AUTHOR: Y 7 0,
(Maio
V3
-ORG,
---None
TITIZ:.' A control device
S
0 1 P
URCE: Vestn k otivovozdushnoy oboronyq no. 8p 1965j 67-69
TOPIC TAGS: civil aviation,control circuit
ell
A]%TRA~T: An electric control device indicating the aircraft posi-
tion on an air route chart is described. The device was designed for
civil aviation aircraft and can fix the position with an accuracy of
1 to 8 minutes, The device is.used in connection with the route
chart on which indicating lamps can be placed along the air routes.,
The lights are of different colors for speeds of 350, 650 and 850 km/h
hri It was recommended that a 1:1000000-scale map be used for the
chart. The de'vice'is composed of a rectifier, yoltage dial switch)
voltage distributor, plug panels, signal system and indicating color-.,,,-.
ed lights.. Diodes of D-7 or DG-Ts types can be.used-for rectifiers.

ymsmv) P. F.
YEREMEYEV, P. P. -- "The Nutritional Value of Birch Leaves in the Feed-
ing of Oak Silkworms in Novosibirskaya Oblast.n Sub 12 Yay 52, Koscad State
Peda'~ogical Inst Imni V. I. Lenin. (Dissertation for the Degree of
Candidate in Biological Sciences).
SO: Vechernaya Moskva January-December 1952

US 2WCultivated Plants Grains M-4
Abs Jour : Ref Zhur - Biol.j. No 1., 19,c8,, ITo 1512
Author : P.P. Yeremevev
Inst Not--avm-
Tltle Me Effect of Microfertilizers and Industrial Waste Products
on Boosting the Yield and Accumulation of Sugars and Carotin
in Corn
Oi:lg Pub Tr. Novosibir. a.-kh. in-ta., 1956., 3-0~ 97-105
Abstract in the "V chkhoz" Lt-raIning farm
..7 of the lastitute and in the
Sovkhoz, of the zinc factory of Kem3rovskaya Oblast in 19562
the effect of the microelements on the development., yield and
accumulation of sugars and carotin in corn was studied. Me
experiments were carried out according to the plan: 1)Pc 2.5
centners per hectare; 2)P, + clinker (waste from the zinc
factory); 3)P, + microelements in the form of salts of Cu Zn.,
Mn., Li; 4) clinker; 5) microelements Cu, Zn, Ma, Li; 61
control. The best growth of corn was noted with the combination
of Pc clinker. Corn plant analyses in the tests of the in-
stitutes "ucbkhoz" have shown that in the combination MD~N03,
Card 1/2

VICUR/Culti-vated Plants .. Graina m-4
Abs'Jour : Ref Zhur - Biol.j, No 1, 1958., No 1512
P. and potassium-lithium wastes (K)., the volume of sugars
increased by 63%, in one the increased K by 54%, in the
combination of WO and microelements - by 42%. The con-
tent of carotene in he plants increased on the average 55%
in all sections fertilized with waste and microolements.
Most of the carotin accumulated during the period of lactic-
waxy ripeness; therefore, an early harvest of corn for the
silo is not expedient.
Card 2/2

MAKEYEII, kand. tAhn. muk; YERMYEV 11 V kand. Lukhri. ijiuk
Hard faclnp, the flanges of elecoric locomotive who-r-I
Jri ow,bon dinxide. ""var. ljrt)l,,,v. no.6:6-8 Jo 165.
(1,111RA 18:8)
I. Moskovokiy ordena Lenim i ordena Trudovogo Krasnogo Zriamen!
institut Inzhenerov zhe1eznodorozhnogo tritrispoi-La.

ThUHWHV Pq
.~r Yjq4k4EUkph; MAnYEV, Mikhail Grigorlyevich; BEUSTOVOY,
I -- 00 0. inzh.red.: KHITROV. P.A., tekhn.red.
[Hard facing and strenethening bands in locomotives; practices of
loading depots] Naplavka i uprGchnenie bandazhei lokomotivoy;
opyt peredovykh depo. Moslgva, Goso transp. zhel-dor. izd-vo.
1958. 46 p. (MIRA 11:4)
(Hard facing) (Car wheels)

7)
MEM --~:Ml;
. I,~il ,
-x- of wom Imomotive part.a.
A~ ':~~
i tcpJ.. tiaga 5 no,. -~2- ::-r ; -1- 0 k X-
I. lloor:Ov:j'T-iy inz-1,11"l-A Inzlicn(irov zlieleznodorozhnog..)
(for I'ladvillaill- do-v Perarva
doroGi (f-~r 'Justov-0;V
(nallroads- -n ~,, .air z',,cpi--aT-.ij,mont amt sup,lics)
(Locomoti'les)

YEREHEYEV, P.V., kand.tekhn.nauk; MAKEYEV, M.G., kand.tekhn.nauk
'.
Design and performance of the universal automatic head for the
weaving are welding in the building up of parts for the rolling
stock. Trudy MIN no.160157-75 162. WMA l6t2)
(Electric velding-Equipment, and supplies)
4

YERMCM, P.v.; mompov, i.i.; Fir.,fuq; v.~,.
Expertmontal pipelinirg of a ges ar.--j oil mi;r*.,:re frm t~4 Zz--aikul
fi;1144 to the central Jack plant. Nefteprcm. delo no.1205 f630
fv!qA 17~-4)
1. N3ft~apromyslovaye upravlenlye "3,jnzh&-teftI".

CHESNOKOVj B.V.,-,
DecrystalUzation of sefamict pyrochlor* muler niLt=l couUtions.
Dokl. AN SSSR 146 no.3t683--665 S 162e (MIRA 15:10)
1. Severdlovskiy gornyy institut im. V.V.Vakhrusheya. Predstavleno
akademikom H.V.Belovyiu
(Cryst&Uization) (*tmiat state) (Pyroeblors)

YERrrWEV, S.V.;ISTOMINA, R.F., nauchnyy notrudnik
Collective farm is raising standards of agriculture. Zenledelie
7 no.11:35-37 H '59 (MLU 13:3)
1. Prednedntell kolkhoza Imeni Sverdlova, Bogdnnovichokogo rayona,
Sverdlovskoy oblasti (for Yeremeyev). 2. Urallskly nauchno-issladovatell-
skiy inotitut sellskogo khozyaystva (for Istomina).
(Bogdanovich District-Agriculture)

LU-SM/Kedicine Veterinary, Foot- Sep 53
and-Mouth Disease
"Experience in the Application of Citrate-Phenolized
Blood of Ani-1s That Have Recovered From the Foot-
and-Xouth Disease," Vet PhysicianaLt. Z. Yeremeyev,
I I
2~. V - ICrasnenkov
Vete-Jr-riya, Vol 30, Wo 9, pp 26-27
Treated blood of Pni-Is recovered from foot-and-
mouth disease with citrate and pbenol. Found that
ail-inistration of blood treated in this manner -oro-
tected adult cattle and calves against infection
270372
with foot-ancl-mouth disease, and alleviated symptoms
in these FtriTngls which-caught the d13ease, notvith-
standing the fact that the infection was compliclii4
by tuberculosis and brucellosis.
2TOM

Tzumzrjv, T.
t 1!,47 1
4,,Wij~
At.the COWS88 Of Turkmen Trade Unlou.
no 4:4z-45 ip 158. Say' ProfBOIU2.v 6
(Turkmanistan__Trade
unlons) (MINA 11;5)

YEREMYEV, T.
- - fe~ ..... .-Y
In Cuba. Sov. profooiuzr 7 no,14:56-59 J1 159-
(KRA 12: 10)
I.Rukovoditell Sovetskoy profsoymnoy delegatell v Kube.
(Cuba-Politics and gover=ent)

IMIalEYEV) T.
Concern for the people is first and foremost, Sov. profsoiuzy
17 no.13:13-15 :1 161. (MIRA 14:7)
L ZaveduyaAchiy zhilishchne-bytoVym otdelcm-Veexoy~4zzqj~
tsentrallnogo soveta profesoionalfnykh aoyuzov,
(State farms)
(Restaurantoo lunchrooms, etc.-Auditing and inspection)
(Trade unions)

YLWWYNY,__nSof oy y IXTSOVA,
J~si,jlp_!i~h; POTASHNIKOV, Fedor Petrovich; KM
N,I,, red.; takha.red.
[Problems in housing and public services; collection of resolutions
and instructions] 7.hilishchno-bytowye voprony; abornik postan,ovlenii
i instruktaii. Koskva, Izd-vo VT9SPS Profizdat, 1960. 2
(NDU 3:12)
(Housing) (service industries) (Retail trade)

- . IV - -
,. ~. YT" - v a 1 .4. r, 1 tocf:~! -- - - --- - - -- - - - - -
1'l-1-11 . . I
'r. ZAI -~ r- ~,-. Z~ -P." c , c
& - . - . , A@ - ,.
'A -1, K " zic,3227 Mr 164,
(MA 18:8)

5/755/61/000/003/024/027
kiJTHORS: Beskorovannyy, N.M., Yeremeyev, V.A., tTomashpollskiy, Yu.-,!Ka.
TITLE: The diffusion mobility of lithium in iron and, steels.
SOURCE: Moscow. Inzhenerno-fiziclieskiy institut. ~4atallurgiya i metall4ve-
deniya chistykh metallov. no.3. 1961, 233jZ48.
TEXT: The paper describes an experimental deterr6ination of the diffusi9p
processes of the corrosionally highly aggressive Li in structural materials.
less-than-l-bec half-life of radioactive Li and Li9 discouraged their use; fence,
the flame -photometry method outlined by N. S. Polucktov (In Metody analiza pl, foto-
metrii plameni - Methods of name -photometric analysis. Moscow, Goskhimizdat,
1959). This method constitutes a non -photographic spectral method in whichra
photoelement and a galvonometer are used to record the radiation of the speciinlen.
The readily excited Li line 6708 .9 with an excitation potentiAl of 1.9 cv was found
convenient for the present study. A straight-line variation of radjation intensity
versus Li concentration was found for concentrations up to 5 - 10" wt. 70. A sche-
matic view of the equipment setup for the determination of the Li in the flame is
shown and explained, including the aerosol generator, a large-particle and droplet
catcher, a mixer, and an acetylene-air burner, a monochromator (6708a
Card 1/3

The diflusion mobility of lithium in iron and steels. S/755/61/000/003/024/027
photoelectronic multipli9r, azXd a range - shunt- equipped light-beam galvanometer
with a sensitivity of 10- -10-'J a/mm, The te~st specimens were cylinders 12-16-Mr-11
diam, 30-35 mm high. Annealed specimens were placed in tcehnical-Fe beakers
whichWere filled with Li in a vacuum equipment and placed in stainless-steel con-
tainers which were sealed in an arc furnace in an Ar atmosphere and held atT = 600,
800, and 1,0000C, After diffusion soaking the Li was leached out with water. A
0.05-0.1-mm layer was taken off the cylindrical surface (after removal of a possibly
Li-contaminated face layer of sufficient thickness), dissolved in a HNO 3- HC1
mixture, and analyzed. At any one T a maximum Li content occurs not at the
surface, but at some depth (of the order of 1 mm), at a value and at a depth which
increase with C content in the steel. Intense surface-grain disintegration is ob-
served (photos). The diffusion mobility of Li in steels is found to be appreciable,
an in y-Fe. The presence of
comparable with that of C. It is greater in a-Fe th,
C deepens the penetration of the Li. Li corrosion reduces the microhardness of
technical Fe and of the ferrite in C steels, possibly in part by microscopic -pore
formation. Such structural changes occur only in regions in which the Li diffusion
is substantial. The Li penetration proceeds preferably along the grain boundaries
which are ordinarily enriched with impurities such as C, S, etc. Thus it is con-
firmed, as was stated by the senior author et al. (in no.2 of the present sbornik,
Atomizdat, 1960) that S inclusions serve as focal p-o"Ints- of corrosion. The even
Card 2/3

The diffusion mobility of lithium in iron and steels. T/755/61/000/003/oz4)027
more consequential modifications~ in the austenitic and porlitic structure as aasult
of the Li-produced C leaching are pictured and interprc&,d. In round figures the
corros ion- affected Li-saturated structure has one-half ~he depth of the decp4f Li
penetration, G steels soaked in liquid U undergo signiftcant volumetric incroilisels;
their density decreases with increasing C content in the ~steel. This must be 'asttri-
buted to the iormation of low-density phases, such as LizC? et al. The high-~T for-
mation, of low-density phases is accompanied by significant plastic deformatioAs,
whereupon cooling results in crack-formation (photo). Tn addition to the chanoe in
microhardness, the strength and the plasticity of C ate a are impaired by Lj~Xcnc-
tration, especially in high-C steels and at high T. Thu'61, e.g., steels 45 andf7O
acquire the properties, of low-grade pig iron at T 800_1,0000C, an crnbrittlerv~pnt
that must be attributed to intense microporosity formation, There are 18 figures,
3 tables, and 6 references (4 Russian-language Soviet, I presumably Russia4-
language Chinese, and 1 Englis ,h4anguage). The participation of E. A. korepanov,
L. M. Ozerov, and M. V. Teregulov in the work is acknowledged.
ASSOCIATION: MIFI (Moscow Engineerink Physics Institute).
Card 3/3

�__ACC_NR___,jj6_03_
6018 (A) SOURCE CODE; UR/0125/66/000/010/0057/0058
j
AUTHOR: Subbotovskiy, V. P.; Yeremeyev, V. B.
ORG: Electric Welding Institute im. Ye. 0. Paton, AH.U1jcrSSR (Institut elektroavarki
AN UkrSSR)
TITLE: Continuous multilayer facing under flux without slag removal
SOURCE: Avtomatichankaya vvarkA, tio. 10, 1966, 57-58
TOPIC TAGS: metal facing, mechanized facing, continuous facing, multilayer facing,
Metal deposition, slag, olectrodeposition
ABSTRACT: A method of block-sequence, mechanized, multilayer metal facing without
slag removal is described. In this method, the face metal deposition is achieved
by continuous reciprocal motion of a consumable electrode under a flux along the
weld axis with the electrode forward travel (a,) always greater than the backward
travel (ad. To ensure a constant cross section along the entire length of the
facing surface, the relationship a - a,(n - 1)1(n + 1), where n is the number of
the deposited facing layers, shoul3 be strictly maintained. Facing by moving the
electrode instead of the workpiece produced better bead formation at electrode
travel speeds well above 40 m/hr. The metal deposition rate (Vd) depends on the
electrode travel speed (vt) and is expressed by the formula vd /n, where n is
the number of deposited layers. Block-sequence facing require: VhIgh-meting fluxes
with.low electric conductivity. The best results were obtained with AN-28 flux, a
1/2
: 621.

lam
ACC NR, APOSOI
sound poreless three-layer facing was deposited at a speed of 40 m/hr. Orig. art.
has: 3 figures.
SUB CODE: 13/ 'SUBM DATE: 14jun66/
Ca;d* 2/2

PA156T21-
USSR/Engineering - PoVei Plants., BleCtric sov 49
Currents, Electric -
Direct
"Locating Damage in DC Circuits at Electric Power
Stations and Substations," V. D. Yeremeyev., A. K.
VAnn, Engineers, 3 PP
"Elek Stants" No 11
At present, faults on DC circuits are located by
"breaking down!' and checking damaged line with a
megger. Describes own method which can be used
without switching off current. (Editor notes,
method needs further improvement and operatio~ai
check.) Includes f1ve diagrW.

KOZI-Ov, V.A.. inzhener; YXRZKVYXV, V.D.. Whener.
Use of cut-off svitches for aut 06~VIV'Izvitchimg-ln of reserve
capacity. Ilaktrlchastvo no.6:73-77 is 154. (MLRA 7:7)
1e Leningradskaya kabellsayn set'.
(Xiectric evitchgear)

S100611511000101110021002
DOWD113
AUTHORSs Batrakov, Yu. G., Yeremoyov, V. D. and Savinov, L. B~
TITLEs Investigations and practical use of the NL-3 level
PERIODICAL% Geodeziya, i kartografiya, no. 11, 1961, 29-32
TEXT: The article deals with investigations and the practical use of the
HA-3 (NL-3) level. Investigations were conducted by the Department of
Geodesy of the Moskovski institut inzhenerov zemlaustroystva, (Moscow Insti-
1~ and the Central Establishment of the Vsesoyuznaya
tute'of Survey Engineers
kontora Sellkhozaerosllyemka (All-Union Office for the Aerial Surveying of
Rural Areas). The device has an optical altimeter built in the telescope
which consists of a reticule of altimetric hachuren protected by etched
glass. The image of these hachures can be seen in the left part of the vis-
ual' field of the telescope on a silvered strip; the image of the staff2 of
the middle'hachure of the graticule and the two anallactic hachurea can be
seen in the right part. The position of the altimetric hachure in the vis-
ual field of the telescope depends on the inclination angle of the direc-
tional ray. The functioning of the level depends on the point-to-point
Card 1/2

S/00 611000101110021002
Investigations and practical use of D054~DI13
correapondQnce of the altimetric hachure with the middle horizontal hair of
the graticule at the horizontal position of the directional axis of the
telescope. The authors describe the functioning of the NL-3 device which
waa used in stereotopographic surveying in the Smolenskaya Oblastt and in
the Moldavskaya SSR in 1960 and compare the results obtained -,rilth the re-
s*ts obtained by geometrical levelling. The NL--3 level can be used for
altituainal field observations, for stereotopographic surveying, and for
compiling a vertical control network for an aerophotographic survey. The
NL-3 level is also recommended for operations in regions with broken C~on-
formation, as well as for surveying roads, transmission lines, pipelines,
etc. The disadvantage of the device is that the prism for observ.ME; the
spirit level bulb is fixed at such a distance from the lens rinr. that it is
impossible to observe the bulb when taking the readings from st.affs.
Scientist A. N. Kolmogorov is mentioned in the article. There
are 2 tables.
card 2/2

yinnm' V.P.
Szg~~nificance of mito-genetic irradintion for peptide synthesis
in the liver (with summary in English]. Blul.eksp.biol. i med.
45 no.5:6n-64 Ky 158 (MIRA 11:6)
1. Iz kabineta mitogeneza, (2&Ve - prof. A.A. Gurevich) Instituta
normallnoy i patologicheakoy fiziologii (dir. - deystvitellnyy
chlen AKK SSSR V.N. Chernigovskiy) AMN SSSR, Moskva. Prodstavlana
daystvitel'nym chlenom AMN SSSR V.N. Chernigovskim.
(LIVE, methboliam
peptide synthesis. mitogenatiC Analysis of selective
scattering of ultraviolet radiations in hungry animals
(Run))
(PEPTIIMS, metabolism
liver synthesis. mitogenatic analysis of selective
scattering of ultraviolet rnya in hungry nnimnle
(Rua))
OITRAVIOLET RAYS, effects.
on liver peptide synthesis, mitogonetic analysis
of selective scattering of rays in hungAry animals
(Rua))
(HUNGIM, experimental
eff. of ultraviolet rnys on liver naptide synthesis
in hungary animals ~Itogenetic nnnlysts of selective
scattering of ultraviolet rays Otun))

rMMFjYEV. V. F.
Analysis of the mechanism of degradation mitogenic irradiation
[with summary in English) . Biul.ekep.biol. i mad. 45 no.6:95-100
Je 158 (KIRA 11:8)
1. Is kabinsta mitogenesa (sav. - prof. A.A. Gurvich) Institute.
normallnoy i pntologicheakoy fisiologii (dir. - deyetvitellnyy
chlen AK11 SSSR V.N. Chernigovskiy) ANN SSSR, Moskva. Prodstavlena
deyetvitellnym chlenom AKN SSSR V.N. ChernigovHkim.
(LIVER, physiology.
energy degrndntiqn mitogento Irradintion (Rua))
(TUPERATURE, effects,
liver energy degrmdation mitogeuic irradintion (Rua))
(MMUT.
same (Rua))

GUFTICH, A.A.; VZa-=V-,~ LIPKIND, M.A.
Mitogenic irradiation of the neuromuncitlar system as a method for the
analysis of its molecular substrate. Report No.3: Regulat6ry effect
of spinal centers on the molecular substrate of muscles in animals
or various ages and t1w,role of the regulation in muscle metabolism.
Biul. eksp. biol. i mod. 51 no.407-61 Ap 161. (MIRA 14:8)
1. Iz kabineta mitogeneza (zav. A.A.Gurvich) Instituta normallnoy
i patologichookoy riziologii (dir. - doyotvitollnyy chlon AM SSSH
V.T.Pirinym. (SPINAL CQW) (MUSLCE) (CELL DIVISION (BIOLOGY))

Analysis of the mechanism of mitogenic irradiation of the liver
in mice with implaAted cancerous tumors. Biu.1. ekap. biol. i mod.
51 no.41102-106 lp 161. (MIRA 3J.: 8)
1. Iz kabinets, mitogenoza (zav. - 'prof* A.A.Gurvich) Inotituta
normallnoy i pa~ologicheokoy fiziologii (dir. - doy'stvitelinyy
chlon A1,91 SSSR V.V.Parin) AIAN SSSRp Moskva. Predstavlona akadomik=
V.N.Chornigovskim.
(LIUR) (CANCER) (CELL DIVISION (BIOLOGY))

YEREWYEV, V.F.
List of amendments made in "Fundamental rules govornIng Qz
production of DlWOO, D25,000 1:50jOOO and 1:1001WO topo-
graphic maps" published -'n the Journal "Geodazia i kartografiia"
No-3p 1956. Good. i kart. no-1149-52 Ja 164.
Remarks on the calculation of leveling altitudes In foreign countries.
Ibid.t52-60 WIRA 17: 9)

L 3740-66 Ehrr(i)
ACCESSION 1IRs kp5o27640 CZ/0023/63/009/002/0128/013~
AUTHOR: T_erem (Doctor)
~TITIZ: Method of computing the disturbing potential, plumb-line deflections aAd
oStokesl constants on the basis of Molodenskiy1s integral equation for the
t ial the the Detb
disturbing po ent [This paper was presented at Symposium on Mi-
h LobAL
Figure of the Eart _q~t -6
natio a of the.
:SOURCES Studia geophysica at geodaetical, V. 9, no. 2, 1965"t'128-137
MPXG WIS t geRde integral equationg Rgity
al)Pro .2 04to 5' *earth 9mvity, graTimtry,
XiMation 4q)
Abs, tra,~t Authoi t a Enalish jummary Modified
-`.pents formulas for the expres _T1 ThO aiiiclo pro.;
siOn of corrections Of Stokes' ap-
of the disturbing
and potentialg plumb-line deflections'-
the coofficielits of expansion of the 4isturbing potential in
tOrms of spherical harmonic$,,
Plumb-line defle- -When used for the computation of
otLong.in any terrain-oonditions, those formul
bure a relative as au-~
accuracy of~tjjq order-of-tho Earth's flatteni-
ng
Oo,b.e.twoon-thi giVen and'&
_~Qurront point Is croat
or,,/
Card

,dkiii6i-iil i-erraini--ci-onditions inside 'the central zone, the appli-,;
-cation of Molodenskiyfs equation for the disturbing potential
ogother with the equation for the sinf:le layer density is ne-
Pessaryo The projections of the elementary areas onto the refer-
may be formed by arcs of meridiansp parallels and
4iagonals of' the corresponding trapezia. Besides the gravity
anomalies and Stokes# approximation values of the disturbing po-
,tentiall the mean slope of the Earth's surface and the mean square,
value of that slope must be known for the olementary.area,,in_ques-
tion..-IOrig. art. had I figure and :L5 formulaa.
ASSOCIATION o Teentral I v7 nouohno-iseled, inat e- t.,odesii aeroe"Yemki L kartografii,, - -
Moacow- - (Central Scientifie RealoarW Institute of Cloodesyt -Photogra=etry ag
-Cartogmph
1GUMITTED1 060at65- ENCLI 00 SUB-00DEs ES# MA.
NO M SOV* 002 OTMI W1 JPHS
Card A/2

_Mwa~x _1~
fL 3024-66 E*67(1) Gw
ACCESSION IfRt AP5026870 CZ106;!316510061009100OV6623-'-"'--'-'-
~2_
AUTHOR., YereinMev, V, F.
TITLE: Problem of determining norava heights
BOURCEl DWI& goop4slca et geodattical v.9, no.11, -.1961";, 1-3
TOPIC TAGS: geodetic aury yl. trimplation
(V
-6.fticli - a&hli~ s Russian su=ary J-: -?o as for
P6 rmU are'diii4ed
;~computlng normal heightsj their differences, and the theoretical errors of clo-
!.sure in levelling lines; for mbuntainous regions these formulas can ensura an
accuracy in the order of I =. fLeco=endatlons are made with respect to comput-,
:ing the heights of point's inside the Earth's crust. It is pointed out that Vig-1
inal'B system of heights is not connected witb the problem of determining the to--
ital height of points 6n the tarth's physical surface., above the reference ellip-
:sold. Vlgnalla system of heights is not identical with the system of normal
heights. ContrAry to getieral belief) the method proposed by Rune for detcrmln-',
iling heights is Act identAcal with the method of determining normal heights. Them,
results obtaine4 in compthationo according to Rune's formula depend on the path
kof levelling. Inaccuracleo are pointed out in the works of Bok= emd Chojnickiol 1--
Orig. art, ban I figureq 34 formulan, and I table.
Card 1/2

r m M,
jb"RVICHP ASAO;__~MR V, V. F.
Yitogenatio radiation an .hemilumiresc&rce. Intorrelation
betwd9n fluorencence procanses and thoic similcur to phou-
phoreszence in living eystems. Tnidy WIP. Otd.. biol.
21 t 1 Id 5-141 16 5. (MIRA 18 j 6)

Y
3795-66 EWT(1) G,1
ACCESSION NR: AT5023299 UR/2547/65/000/157/0069/0084
AUTHOR; Yeremyev, V. F
TITLE: The determination of normal altitudes
SOURCE: Moscow. Tsentrallnyy naucluio-isoledovatellsldy institut geodez% aeros"yemid
I kartografil.- Trudy, no. 157, 1965. Isaledovanlya po geodezicheekoy gravimetril (Re-
search on geodetic gravimetry), 69-84
TOPIC TAGS: ggodesy, geodetic survey, Earth Planet, measurement
ABSTRACT: In view of the interest accorded in the SSSR and abroad to the theory of -
Mologensidy concerning the determination of the external gravitational field and the shape
of the Earth, the present author Investigated thoroughly some of the earlier derivations.
The largest term omitted in the Taylor series expansion of the perturbing potential used
by Molodenskly Is equal to-~ U (119 Hq)/j B. A B, where U Is the normal potential, D
the approximate value of the geodesic latitude, 11 B the difference between the triie value of
the geodesic latitude and B, and 1% the normal attitude. Even withA D = 01. 6 this term is
Hq. Formulas for the calculation of normal altitudes, normal altitude
less than 10
Card 1/3 uDc: 528.373

L 3795-66
ACCESSION NR: ATS023299
differences, and theoreti-cal closing errors of leveling polygons have been derived assuring
an accuracy within one millimeter in mountainous terrain. Methods are also proposed for i
the calculation of depths In the Interior of the Earth. Ju the discussion based on 25 re-
ferences the author shows that the Vignal system of altitudes (Jean Vignal, Ove Simonsen,
1Identito des corrections de pesanteur appliquees aux altitudes dans les pays de I'Europe de
IfEst et en France, Reprodult par Robert Authonsen, Copenhague, 1962) to not connected to
the problem of the determination of the total height of points on the physical surface of the
Earth above the reference ellipsoid, 1. e., Vignal system of altitudes is not Identical with
termination as
the- system of hormal heights. Ukewlse, the method for altitude de proposedl
by 0. Rune (VeroeffentUchungen des Finnischen geodaetischen Institutes, 1949, N 36, 227-
f the
al attit
de d
te
mination
As a
atte
of fact
ith that
the
231
ti
l
t Id
i
o
norm
u
e
r
.
m
r
en
ca
w
s no
,
)
results of the computations according to Rune's formulas depend on the path of the
appropriate leveling line. The author also points out some inaccuracies in articles
CrItIcIzin as, 2 figures, and I table.
ASSOCIATION: Tsentrallnyy nauchno-lasledovatellaldy institut geodezil, aeros" yem1d,

. Aerial Photo-
I kartografti, Moscow entral Solentific-Research Institute of Geode
i jrrRhIc Survey an1LqM!SU h
_V Y
[Card 2/3

1,3265-66 D ri,
;ACCESSION HR: AT5023296 UR/2547/65/000/157/0003/0046
5 2 8,2 1 s 5 3 1,.2 6
IAUTHOR: Yeremeyev, V. F.; Yurkina, H I.
TITLE: Computation methods based on Holodenakiy's ~nt~egral uaiion
for the disturbing potential
SOURCE: Hoscow. Tsentraltnyy nauchno-isoledovatel'skiy' institut
geodezLi, aeros"yemki i kartografii. Trudy# no. 157, 1965. Iseledo-1
vaniya po goodezicheekoy gravimetrii (Research on geodetic gravimetry)j
3-46.
TOPIC TAGS: ggSde tte 1~jjr ~Ilgravity computationt disturbin'g
potential, gravity anomalyg gravity potential
BSTRACT: The HolodenskI7 method of deriving the Integral equation
,A
for the dinturbing 'Potential T ig used to obtain the expression for
Card 1/4

3265-46
ACCESSION NR: AT5023296
the T-derivatlve along a-tangent T to the earth's surfacet
2
sec2 a
sec a T)
I-- 71~ &
-2
dg r.
where ris the distance between the fixed station and the station
being observed, g is the gravity measurement, y is its normal, V is
the normal to the reference surfaceg a is the angle of tilt of the A
surface S with respect to the reference surface, and Tis the value
of T at the station being observed# This formula can be used to
express the deflection of the vertical on the physical surface of
Ithe earth in terms'of gravity anomalies and the disturbing potential.!
IMethods are presented forthe computat.Lon.of the disturbing potential'
Card 2/4

ACCESSION HR: AT5023296
deflection of the vertical-, and thd Stokes constants (in spherical I
functions). - Stok as approximations are derived, and corrections to
them are calculated by representing the physical surface of the earths'
as sides of a polyhedron; the projections of the aides on the refer-
ence spharo.ara spherical triangles. The heights of the sides are
determined by the formula
h a~B + bX + c'~
where e and X are the polar distance and longitude, respectively,
and a, b, and c are coefficients determined from h at the angles of
the aides. Three formulas are,derLved for expressing the disturbing
potential and deflection of the vertical in the case where the dis-
tance between the fixed station and the station being observed ex-
ceeds 300 km, or where the terrain In the vicinity of the station
being observed is relatively flat. Investigations carried out on a
model of the earth constructed in the form of a cone situated on the
reference plane indicate that the Stokes approximation of the die-,
turbiug potentLalq using the first,6f thd above formulas, does not
Card 3 /4

326~-66
ACCESSION NRs ATS023296
improve the accuracy of the Vening-Heinest formula for the area
in a mountainous region. Orig, art. hasi 71 formulas and 8
figures. IER)
ASSOCIATIONS Teentrallnyy nauchno-isoledovatellakiy Institut geodeziig
eroallyemki', i~ kirtograf ii, -'.Ho scow-, (Central-Sc Lintif L6 Research In&
a
tute of Geodesy, Aerial Surveying, and'-,-
SUB CODE~~ ES
SUBMITTED: 'ENCL4, 00 -
NO REP SOV% 007, OTHER: -000 ATD PRESSI
Card 4 /4

TERMEYEV, V,F,
OF-terminaticn of norwl altitudea. Trudy TSNIIGAIK no.157t69-U 165,
(MIRA 38tlO)

v tI tt (1 11 go It Ad Z~ J* It x 101, Wald* %1t loossol QS1 " d r4a
I I L 0 - 1-1 - C-L,
A JL. T -
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olf salt4soldc "Tity a (is Ultraviolet "d 41
so ff 7"-- (10 r-Wast 01"N' F i
detcvtorv whow bra-l-
tmt=o 2M A. awl hanth up to 297f) anti ' MO A.
in CMbrJOG SPV#CtM U( %OM TCgCtAlolt tvils.
Loor-intemity radhalon a JL 2800-3610 A. prodtkv%
milogen"ic vNerts In ymqt detertan in co"itim- of
tW:IW (eke, fillitt or dayllight) Illumination, but nA in
00 41 the doock, &Wh W04 k"111111 Aff 1we'"I Ill tkcl I'&
Anti dAY1!qfjl' WI the tullfrmcr Of-wlvvl It not 401611111.
able to gnu. IL A.
Zee
01111
zoo
Joe
00
CO 0
ASo
40
fee
-.s too
77.
t
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U U AV 00 11~0; 01 ft U it it er K&O n Ila *still -1.9 -1
9~e ; 0 to
0 0 00900's
964
0

"Use of the Modeling Method for the InvestiCation of Formulas DeterminivE the
Shape of the Earth." Sub 27'Apr 51, Moscow Inst of Engineers of Geodesy, Aerial
Photography, and Cartography, Ministry of Higher Education USSR -Cr Can(/. Fe'ei,. sc"
Dissertations presented for science and engineering degrees in Moscow during 1951.
SO: Sum. No. 480, 9 May 55

"Tho (if 1,'Xrur~ #Duo to t'~,-- D.1*.!ok,,L'u-i (,X th,, D:t~~,
I P.')
In mountainous regionr, the deflection of thq vertical may U~ co..-. uted ,., i t-
quadratic error of 1" .2 to 111 -5, lowerino the accuracy, of trian'-Ulation, ;1--~
with plane regions. Thereforo lincar interrX)Iatl-n of thu coom.11i ate.-, of t1l.-- (Ir'-flect"on. of
tho vertical. 1.-, n ot to1rratcd. WhA, tr, Nor',1955) SO: Sula.;b. 713, 9 !.'()v 55

TJOUIKBIWO Vero; YURKIIAt Xvie
Applieation of dynastic heights, Sborest.po geod.no.M23-38 '53*
(Altitudes-Measurement) (NLRL 10:2)

YXROMYRY,I-
Tables for calculating the deflectirja of the vertical line on the
physical surface of the Barth and the height of a quasIgeold.
Trudy TSNIIGAIK no.121:3-16 157. (MIRA 10:10)
(Geodesy--Tables, etc.)

YRUMM, V 7 YURKINA, M. I.
~Computlug effect of for zones on the height of the quasigeold
and on the deflection of the vertical. Trudy TSNIIGAIK no.121:1?-24
'57- (MIRA 10:10)
(Geodesy)

Timign-a-M V
Design of squared transparent sheate for calculating the height of
the quasigeoid. and the deflection of the vertical by means of the
Stokes and Wening-Neines forculas. Trudy TSNIIGAIK no.121:43-75 '57.
(MIRA 10:10)
(Geodesy)

YXRZKIFM , V.P.
,
Formulas and tables for covqmtIng geodetic coordinates by molodenskillo
method. Trudy TSNIIGIIK no.121:77-104 157. (MIRA 10:10)
(Geodesy)

YBRIMMY1 Y.F. -,,, - ~'~ I- ~ -, ~ - I -I
--, :,
A method for solving an inverse geodetic problem on large distances
by means of computing the coordinates of the 'meann point of geodetic
line. Trudy TSNIIGAIX no.121:105-112 157. (MIRA 10:10)
(Geodesy)

&T F-- V; V, k~
AUTHORS: Scientific Collaborators of the Ts1,UIGAiK: 6-58-4-14/18
luxicina, II.I. , Fedosov, F.I.
Uspenskiy, YL.S., Meshchanskiy, F.L.
TITLE: Letter to the Editor (Pislmo v reaaktsiyu)
PERIODICAL, Geoaeziya i Kartografiya, 1958, Nr 4, pp. 66-66 (USSR)
ABSTRACT: It is pointed out that different tables published for the same
quantities. which differ only by the distribution of the material,
by the reduction of the number of figures of tabulated amounts,
and by the modification of the intervals between them are being
published by various persons who describe themselves as authors
and o1nim authors' rights. It is demanded that this state of
affairs be ended and that in no case these persons, viho merely
carry out some modifications of existing tables, be allowed to
claim authorship. The calculation of tables must be
entrusted to the care of organizations, so that the costs of
editiona would be reduced.
AVAILABLE: Library of Congress
Card 1/1 1. Tables- Material distributica

3W SOV16-59 4--16/2o
AUTHORS: Yurkina, 111. 1.. Can-lidate of Technical Sciences,
Yeremeye- V. F., Canlidate of Technical Sciences,
vlakarov, N. P., Candidate of Physical and Mathematical Sciences
TITLE. On a Result of the 11th General Assembly of the International
Union of Geodesy and Geophysics in Toronto (0b odnom itoge
XI Generallnoy assamblei MCGS v Toronto)
PERIODICAL: Geodezj'ya i kartografiya, 1559, 1Tr 4, PP 59-62 (USSR)
ABSTRACT: At the meeting of the International Gravimetric Commission
in Paris in 1956; M. S. MolodenBkiy delivered a short report
on his method of determining the figure of the real earth.
Special attention -was then paid to this communication. It
eliminated the need of a regulation. In this cace, the accura-
cy of determining the figure and dimensions of the earth only
depends on the donaity and complotenes3 of the gravimetric,
astronomic and geodetic surveys on the physical earth's sur-
face. The only condition required for 'jolodenskiy's method
is t*hat the earth's surface has no acute angles, i.e. that
a certain tanGential. surface can be laid on each point of
the same. Many countries have already provided their areas
Card 1/3 with a gravimetric sur-ey with one point to every 10 km2. With

SOV/6-59-4-.16/2o
On a Result of the 11th General Assembly of the International Union of
Geodesy and Geophyaios in Toronto
the use of gravinnetria surveys of such accuracy and density,
and of the theory by Molodenakiy,tho deflections from the
vertical, for instance: can be determined with an accuracy
of up to 011.1. According to the theory by Stokes such accuracy
can only be attained, by camryipg out the present gravimetric
surveys not on the earth's surface but on a regulated Geoid
which is, however, physically impossible. As, however, the
elements of the external. gravitation field, and particularly
the deflections from the vertical, are necessary to solve
different geodeiio tasks, attempts were carried out abroad
t,~ improve the old traditional way basing on Stokes' theory
in order that the accuracy of the conclusions should corres-
pond to the accura.-.;y of the survey. Such iin"attempt is re-
presented by a suggestion made by Graf -Hunter -_~t the 11th
Assembly of the International Union of Geodesy and Geophysics
in September 1957- Ile suggested to consider the gravitational
anomalies to be'm9ni'aured in points on the physical earth's
surface. Crt -Hu:xter lid, however, not consider the changes
in the defleotiona from the vertical, nor did he put forward
Card 2/3 methods of considering these changes. As can be seen from

SOV/6-59--4-16/20
On a Result of the 11th General Aaoa=bly of the International Union Of
Geodesy and Geophysics in Toronto
the paper by A, A. Izotov (Ref 3), the A2aembly did not
recognize the importanec of ee report '-)y 1.11. S. Molodenakiy
though.it had been submitted to it. In this connection, the
fault in Izotov'r, ',1 nointed out. He asserts that
Graf-Hunter is In w1th Molodenskiylo method
but out,'.-Gatu to 1"ho prublem in a different way. Also
the assertion by Izotov (Goodoziya i kartografiya, 1950, Ur 7)
that Molodenskiy suggests a formula of the Stokes type gene-
ralizod by him in not corroct~ The known Stokes'formula is
obtained as a epecial case of Molodenskiyts theory. Finally,
the-authors of the present paper express their astonishment
at the fnbt that the Assembly approved the method by
r: i, : f. IT Tlvnv~~ ia corresponding to the requirements of Stokest
theorem. .Vhere are 4 references, 2 of which are Soviet.
Card 3/3

MOLOIUCNSKIY, Mikhail Bergeyevich; TUMM", Vladimir Fedorovich;
TURKINA, Mariya Ivanova;
?.A., red.izd-va; ROXAMVA, T.T., takhn.red.
(Methods for studying the exterior gravitational field and
the figure of the earth] Metody Izuchenlis, vneshnego gravitatsion-
nogo polis. i figury zemli, Kookys., Isd-vo geodes. lit-ry, 1960,
151 p. (Leningrad. TSentrallnyi nauchno-iseledovatellskii
institut geodesli aerosOemki i kartogr&fii. Trudy, no.131).
(HIM 13:6)
(31arth-Figare) (Gravity)

VJ_
PUSE I BOOK EUWITATION SOV/4291
MY/42-S-131
rjolodenskLy.. Mikhail Sergeyevich., Vladimir Fedorovich Yere yev.0 and
Mariya, Ivanovns, Yurkins,
Metody izueheniya vneshnego gravitatsionnogo polya i figm-y zenli (Methods of
Studying the Outer Gravitational Field and the Figure of the Earth).,
Moscow,, Geodazizdat,, 1960, 250 P, Series: INbscov. Tsentrallnyy nauabno-
issledovatelfskiy institut geodeziij, aeros"yemki i kartografil. Trudy., vyp, 131)
Additional Sponsoring Agency: USSR. Glarnoye upravleniye geodezii i kartografil.
Ed,: N,P, Makarov; Ed. of Publishing Ebusel T.A. Shonarova; Tech. Ed.:
V.V, Romanova.
PURPOSE: The book is intended for geodesistop ma-veyorep and cartographers. It
may also be used by students of geodesy and cartography.
COVERUM: This issue of the Transactions of the Central Scientific Research Insti-
tute of Geodesy.. Aerial Surveyp and Cartography deals with methods of investi-
gating the outer gravitational field in a system of coordinates applicable to the
entire Earth, The aathors analyze the possibilities of a geometric methodpi.e.,

Methods of Studying the Outer Gravitational Field (Cont.) SOV/4291
combination of precise linear and angular measurements (triamgulation, astre-
nonic dete-rdnation of latitudes., longitudes and, azimzths and trigon tric
levellin ). Authors give methods for the determination of anomalies of the
gravitational field and metbods of mmxerical integration and the possible errors
in grav-bmtric conclusions. Chapters I to VII are based mainly on the work of
H.S. Mo:Lodenskiy,, and Chapter VIII on the work of V.F. Yeremayev. The aathora
thank I,D. Zhongolovich# L,P. N111 n and N.P. Makarov. There are 13.1
references; 83 Soviet., 12 Englisho 10 German., 4 French, 1 Italian,, and 1 Czech.
TAME OF CORrOUS:
Introduction 3
Foreword (Tn German) 8
Ch, I, Geometrical Ylethod for the Study of the Figure of
the Phymical Surface of the Barth 14
1e Principles of the method 14
2. Geodetic system of coordinates 15
3* Differential formilas for the tramsformation of coordinates
into a now system 20
4o Geodetic constructions usiM straight lines 24
csv&:Vr--

YURKEIA, E.I.; MAKAROV, R.P.; yERRT,-y8v v.F.
Present state of theories applied to the study of the earth's
phy.5ical surface. Trudy T.;IIIIGAIK no-139,45-59 160,
(MIRA 14:7)
(Earth.-Figure)

S/006/62/000/005/002/002
D054/Dll3
AUTHORS: Yurkina, M.I. and
TITLE: Three-dimensional geodesy
PERIODICAL: Geodeziya i kartografiya, no. 5, 1962j 63-71
TEXT: The theory o.- f determining the Earth's shape by geodetic
measurements on its surface, proposed and substantiated in 1945 by M.S.
11olodenskiy, gives a full, practically realizable solution to all problems
of three-dimensional geodesy. Whereas Western geodeeists are still dis-
.cussing these problems, Soviet geodesists have been accurately working out
problems of three-dimensional geodesy since the beginning of the 1950's.
Idolodenskiyls theory, little known and insufficiently understood abroad,
was exposed in his works published in 1945 and 1948 and in the following
articlesi (1) "Izueheniye figury Zemli geometricheskim (astronomo-geode-
zicheskim) metodom" ("The study of the Earth's shape by a geometric (astro-
nomic-geodetic) method"), Sbornik statey GUGK 1949, no 27, and reprinted in
the Trudy TeNIIGAiK, 1950, no 75; (2) "Novyy meted resheniya geodeziche-
Card 1/2

Three-dimensional geodesy S/006/62/000/005/002/002
D054/D113
skikh zadach" ("A new method of solving geodetical problema"), Trudy
TnNIIGAiK, 1954, no 103. Problems of throe-dimensional geodesy were dis-
cuesed at the Toronto and Helsinki assemblies of tho IGGA hold In 1.957 and
1960, respoctively, as well as at the 1959 Vonibe Sympouium duvoLnd exclu-
sively to r)r,,)bloms of three-dimensional geodesy. Theories exponed Lherf,-
by several specialists including Brigadier Martin Hotin, Director of 0-.i(.,r-
seas Surveying in England, and Antonio Marussi, Director of the InsLitute
of Geodesy and Topography at Trieste University, only repoated the findings
and formulai published long ago by Molodonskiy. H. Dufour, Levallais, TI.A.
Hirvonan, 2yorhammar, todemueller, Vignal, C.F. Baeschlin, Kobold and
Hunzikor are mentioned.
Card 2/2

s/547/62/00o/145/001/002
E032/E414
AUTHORS: Molodenskiy, N.S., YereTeyev, V.F., Yurkina, M.I.
TITLE: An estimate of the accuracy of Stokes's series and
some attempts to improve his theory
SOURCE: Moscow. Teentrallnyy nauchno-inaledovatellskiy
institut goodexii, aeros"yemki i kartografii. Trudy.'
no.145. 1962. Iseledovaniyalp6 geodezicheskoy
gravimetrii, 3~21
TEXT: It is pointed out that because the regularization of the
Earth cannot be carried out with sufficient accuracy, the accuracy
of Stokes's series may be appreciably lower-than the nominal
accuracy. For high order harmonies there in no simple relation
between the coefficients of expansions-representing anomalies
defined on the Earth's surface and the Stokes constants
characterizing the external gravi ,tational field. This effect in
pow investigated with a model in the shape of,& sphere girded
along the equator by a toroidal belt half buried in the sphereand
covered-by lateral conical surfaces in order to reduce the angle
with the sphere to ~6bout 10% Varioun methods of expanding the
disturbing'potential are then tried and numerical values for the
Card 1/3

5/547/62/00o/145/001/002
An estimate of the accuracy ... E032/E414
expansion coefficients are tabulated. The expansion
coefficients Are computed (1) for the given distribution*of
anomalous masses, (2) by formally referring,the quasigeoidal
heights at points on the model's surface to the reference sphere
and (3) by formally referring the gravitational anomalies to the
sphere and applying the Stokes series. Marked discrepancies are
found between the numerical values obtained for these
coefficients in the three cases, and it is concluded that these
discrepancies can only be explained by high harmonics in the
formal expansions for.the anomalies and the heights of points on
the physical surface. The present results are in full
agreement with earlier calculations of quasigeoidal and geoidal
heights at the equator and the pole. The error in the integral
Stokes formula at the pole of the model, i.e. well away from the
region with large gravitational anomalies and large slopes,
turns out to be greater than the possible departure of the
quasigeoid from Listing's geoid. It is concluded that,current
practical methods of computing the coefficients in the expansion
for the disturbing potential from gravity measurements are
inadeqUate. In order to achieve acceptable accuracy the theory
CArd 2/3

S/547/62/000/145/001/002
An estimate of the accuracy E032/E414
of the external gravitational field and the shape'of the Earth's
physical surface must be used. A asirvey is then made of the
various theoretical treatments available in the literature. It is
shown that the methods of S.N. Gromov (Vestnik Leningradskogo
universiteta' no.19, 1956, 174-185: no.19, 1957, 145-152:
Uch. zap. LGU, no-273, 1958, 208-249) and of R.A Hiryonen
(Sarja A. III Geologica-Geographica, 5~,.Helsinki, 1960) cannot
lead to an improvement in Stokes's theory, whereas the method due
to Arne Bjerhammar (Series A III, Geologica- Geographica, 1961, 61)
leads to the same accuracy as Stokes's formula. The authors also
disagree with the model of J. de Graaff-HUnter which is said to
lead to the same difficulties as the application of Stokes's theory
to the real Earth. Finally, the integral equation for the
disturbing potential developed by J.J. Levallois (Bull. Geod., 1958,
N50) and Bjerhammar is shown to be subject to an error of the order
of the slope of the Earth's physical surface at the point under
investigation. This error may reach up to 40%.
There are 5 figures and 7 tables.
Card 3/3

MOLODERSKRY 14.S.j 'YERE24ZYgN,..-V.F.; YURKINA, M.I.
Problem of transversal shift in triangulation. Good, i kart. ne.6:3-5
jo 163o (MIRA 16:9)
(Triangulation)

BROVAR, V.V.; YEREWYEV, V.F.; MAKAROV, N.P.; PELLINEN, L.P.; SHIMBIREV, B.P.;
YURKIMA-M.'I.-
p
Determining the external gravitational field and the Iligure of the
earth. Geod. i kart. no.10:74-76 0 163. (MIRA 16:12)

Y I ('R K I NA , N
,uracy of
tje &cc
-orcmicaj-F,-,jvlr-,Ptric 2e*.,eiing.
,~urftcy of a3troncmical and a5tt
Good. i ~-~ajq. no.8:76-V Ag 16-11'.

YEREMEYEV, V.F.
On the problem of determining normal heights. Studin goophya
9 no.lil-13 165,
1. Central Research Institilte of Geodesy, Photogrammetry and
Cartography, Moscow, Verkhnyaya Pervomayskaya E-264, U.S.S.R.
Submitted March 14, 1964.

FOZD6,-M, ~ M.; TARNUISK ri,, V. I.; MIFREYVI, V. r.
Prospecti for applyirg of rrwap
to-dard aalo,,.ul!Aion rf in irmtalwc,r'K!.ve. by
Izv. vya. ucheb. m-x6; chorn. met. 8 no.1l.-.62-(P '65-
(MTRA 1.801)
1. Urallakiy politekhnioheskiy imititut.

20582
9,31,5-0 s/109/6i/oo6/002/014/023
7, L// )~v E14o/E435
AUTHORS: Lobov, G.D. and Yeremeyev, V.I.
TITLE: Certain Effects Accompanying Detection in Gas Discharge
PERIODICAL: Radiotekhnika i elektronika, 1961, Vol.6, No.2,
pp.286-291
TEXT: An experimental verification is given of tfie hypothesis
that microwave detection in gas discharge devices is accompanied
by variation of both the discharge current and the magnitude of
glow of the gas. Curves of various discharge parameters along
the length of a special tube indicate that the maximum pulse
detection coincides with the maximum of excitation, with these
maxima occurring at the negative glow. The regions of maximum
recombination intensity and of excitation do not coincide, giving
maxima of the corresponding parameters in different locations in
the gas discharge. The experimental results show agreement
between the phenomena of detection and of variation of glow
intensity. A qualitative explanation of the results can be based
on the assumption that the microwave power varies the electron
energy, Three physical phenomena in the tube are considered to be
related to the detection process. These are the variation of the
Card 1/2

20582
S/109/61/006/002/014/023
Certain Effects ... E140/E435
recombination factor, of the number of excited atoms and the
number of collisions leading to excitation. These phenomena
influence the discharge current and hence the detection process.
There are 8 figures and 4 references: 2 Soviet and 2 non-Soviet.
ASSOCIATION: Moskovskiy energeticheskiy inatitut
Kafedra teoreticheskikh oanov radiotekhniki
(Moscow Power Engineering Institute, Department of
Basic Theory of Radioengineering)
SUBMITTED: may 6, ig6o
Card 2/2

ymmw. V.M.
v9s"MOM-F.- ~
My experience In pr,,--ofresding mRD compilations. Sbor.3t.no kart.
no.6-53-57 '54. (MLRA 10:9)
Onrtography) (Proofreading)

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U111KNMOV, V.P.
Additional data on the study of ths neointruslons of Adsharia. Trudy Inst.
Geol. Nauk No.89, Petrograf. Ser. No.28. 62-77 148.
(CA 47 no.22:12154 153)

.A3,50949). -QLurtx4lk)rik-% with riths-r wArty grAnit",
A I by di.[MWS And CtAltACt fiCtMAIJOUS Of dif-
I txvur jmW.t the Lowtr .&od NNI-11v Caju.
I- Ex. t 7 Y7i-.s the highly Invulilorphic kllh*itv, .4
the Central Tuvi, priticipillY in the wilk-Y, -,( fiv,-r-
Nfettzhi I asul Usigmit. Extrinivr quAnt. lnkfu~lpps%
And n'ylk-Al mudic, ( U.-. .I,, I.,- list highly hy.
h6licAmActer of the hornfvlw~, slcun~. tic, which or.
routki the app4rent gritsitc4moritc 1whoisch. polk-ul-arly
in the rvSke of SmwuuvkA, The riv, U
the intruivvs shows A chem. trAti-ifumt- fr4mit grmsitr
to 4wbaw. Awl Abms how illl4.l3.,!v th, 4,1,r r-k. ws~t,
4b*iJUdAtCd Alkl hytifidiWI. It I- ~V~ll I.W1141,1V (ILAt 00
m"w-grained quarts4liotitcs are hylmbe ill th,ir dwita
awl lictrov4plue CILLt4cut.

Rv-AF-~ov,
ptjrvt!~'~, b,
lu
sceol't.
the
.V-s
711
cbrm.

131WKSYNY, V.P.
Problem of the character of contact changes in clay @halos. (In:
Akademiia nauk SSBR. Vopromy petrografii i mineralogil. Kooky&,
19530 Vol. 1, P-113-118) (MMA 7t4)
(Clay) (Shale)

YEaVMYXV. V.P.; SHMYGINA, L.D.
Claqs and clVer soils in the central region of Taya lutonsmous
Province- Trudy Inst.geol.nauk ne.165:31-" 135. (MLRA 9:4)
1 (Kva Autonomous Province-Clay)

V~ KIM$ VOPO -
i, V and nonmetallic ore deposits of south-
k pvtrwraph
,.11111141~i
.N"0*44" -.VWA""s -
eastern and western ftya. Trudy IGM no.101108-142 137,
(Tuva Autonomous Province-Petrology) (Kin litO

- ---- --YEBJMYBV, V.P. - ------
Tan, TrwV IONK no,17s23-33 157. (xin n:6)
(ftm Autonomous Prov-ince-Agalmtolite)

YRUMYEVI V.P.
......................
Petrograph7 and nonmetallic minerals in the eastern part of the
central Kamchatka Range 2rwW IG3K no,17slO7-242 157.(KM lit6)
4amchatka-Petrolog7)

3(5)
AUTHOR: Yeremeyev, V._P
SOV/11-59-10-9/16
TITLE: On Potassium Metasomatosis in Granites of the South-Western
Tuva
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geologicheskaya, 1959,
No. lo, pp loo-lo6 (ussa)
ABSTRACT: Numerous intrusions of granites and granitoids of various com-
position and age are observed in the south-western part of
Tuva, forming the so-called TqknnuolliAdy oomplex# Red-colored
granites in the region of the Agar, -Dag-Tayga mountain ridge
are u'sually situated near the plutonic tectonic faults, in
contact with enclosing Cambrian dynamometamorphized achists.
The red color of granites in some places change to pink. Mi-
croscopic studies showed that in the central red parts of the
intrusionj the feldspar part of the granite, especially the
latticed microcline,wan to a large extent pelitized and the
plagioclast - much less. In places of contact with the Cam-
brian rockal the granites are cataclysed and are represented
Card 1/3 by plaglogranites. On the whole, the intrusion was formed

SOV/11-59-10-9/i6
On Potassium Metasomatosis in Granites of the South-Weatern Tuva
from plagiogranites, but the plagioclaot was replaced by the
microline. Results of chemical analyses of these rocks are
given in table 3. All analyses were made in the laboratory
of the Institute of Geology of Ore Deposits, Petrography, Min-
eralogy and Geochemistry of the AS USSR, by M.G. Zamurayeva,
O.P. Oetrogorskaya and D.N. Knyazeva. The same processes of
replacement of the plagioclast by the latticed microline are
observed in other intrusions of the region, near the Tea-Khem
and Ulor Rivers. Granites from the Yamalyg mountain range
situated 15 km from the mentioned faulted zone sharply differ
from the above granites. They are of light-grey color and
the microscopic study disclosed the presence of quartz with
resorbed microline and plagioclast crystals. In some places
plagioclast crystal concentrations alternate with large parts
of secondary latticed microcline, forming a porphyric struc-
ture (figura 4)- Small allotriomorphic recorbod plagioclastic
relics are observed In certain parto of the microclino atruc-
ture. The author thinks that the microclinization of Tuva
Card 2/3 granites is associated with the late pootmngiintic alkaline

SOV/11-59-10-9/16
On Potassium Metasomatosis in Granites of the South-Western Tuva
solutions which by their action caused the metasomatic re-
placement of the plagioclast by the microclineo The same
magmatic hearth from which the granites were formed was also
the source of those alkaline solutions. Such a theory was al-
rd'ady proposed by G.D. Afanaslyev and D.S. Korzhinskiy. There
are 3 photographs, 2 tables, 1 map, 6 Soviet references.
ASSOCIATION: Institut geologii rudnykh mostorozhdeniy, petrografii, miner-
alogii i geokhimii All SSSR (Institute of Geology of 'Jineral
Deposits, Petrography 14ineralogy and Geochemistry of the AS
USSR)
SU34ITTED: February 24,, 1959
Card 3/3

~l TIRTAYNV. VP.-. AMMIKOV, B.Ta.,- PETROV, V,P, I SOKOLOVA, L.A.
~
Genesis and distribution of chrynotile-asbastoo deposits as a
form of contact effect exorted by granitoide on ultrabasic rocks.
Trudy IGIN no-31:19-35 159. NIRA 12'- 7)
(Asbestos)

YEUKUN I V. P.
rakskoys eb
Petrography and genesis of the Aktov rysotile-asbestos
deposit. Trudy, IaF,14 no.31:68-111 159. (HIM 12 '- 7)
(Tuva,Aiitonomous Province--Asbestos)

t:_ YEFamn"vf--.!JP---
Genesis of the Chazadyr hornblonde minera-lization (veBtern Tava).
Trudy IGEM no.47:43-52 160. (MIRA .14:5)
(Chamadyr region (Tuva Auton=ous Province)-Hornblends)