SCIENTIFIC ABSTRACT LAPINA, M.I. - LAPINA, V.YU.
Document Type:
Collection:
Document Number (FOIA) /ESDN (CREST):
CIA-RDP86-00513R000928610020-3
Release Decision:
RIF
Original Classification:
S
Document Page Count:
99
Document Creation Date:
November 2, 2016
Document Release Date:
August 31, 2001
Sequence Number:
20
Case Number:
Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
File:
Attachment | Size |
---|---|
![]() | 3.67 MB |
Body:
M.I.; STRAKHOV, V.N.
New method for determining elements of the magnetio field
in the upper half-space from the given distribution of the
vertical component AZ on a plane. Izv. AN SSSR. Ser. goofiz.
no.3;317-335 Mr 162. (14IRA 15:2)
1. AN SSSR, limtitut fiziki Zemli.
(Magnetic prospecting)
IAPITA, M. I. Sep/Oct 53
LYSSWGeophysics - Seismic Geomagnetism
"Geomagnetism and Seismic Phenomena,n M. 1. Iapina Geophys Inst, Acad Sci USSR
Iz Ak Nauk SSSR, Ser Geofiz, No 5) PP393-404
Clarifies the present status of the problem of the relation between geomagnetic and seismic
phenormna. Proposes the following future investigations: (1) isolation of the micro-
variations of a geomagnetic field which are connected with processes in the earth's
crust, and elimination of the intensive ionospheric background; (2) study of
anomalous secular behavior in seismically active regions and in seismically quiescent
regions; (3) study of the extensive distribution of a geogmagnetic field as a function
of the tectonic and seismic peculiarities of a region.
267T72
i AP11VA, 1'rj,X,
MWIOPMOT, X.M.1 3MVITSIN, T.M.; ILAP =- -OL"W'"
I
All-Union interdepartmental conference on aerial surveying.
Izv.AN SSSR.Ser.goofit. no.3:415-416 Mr 157. NLRA 10:5)
(Aerial photogrammetr7)
AliTHORS: Devitsyn, V. M. and Lapina, M. 1. 49-10-'?/10
TITLE: On the accuracy of determining the depths of location of
disturbing masses studied on the.exam-ple of the magnetic
anomalies of Bashkiria. (0 tochnosti opredeleniya
glubin vozmushchayushchikh mass na primere magnitnykh
anomaliy Bashkirii).
PERIODICAL: Izvestiya'Akademii Nauk SSSR, Seriya Geofizicheskaya,
1957, NO-10, PP. 1266-1272 (USSR)
ABSTRACT: The authors studied the problem of calculating the depth
of disturbing masses on the basis of the magnetic anomalies
of Bashkiria, applying the most simple methods of calcula-
tion used in practice for the purpose of determining
the degree of agreement between the results of the
calculations and evaluating the accuracy of the calculated
depths. For the calculations the authors used a detailed
AT map of the respective section produced on the basis
of 1956 mapping work by Vniigeofizika, scale 1:200 000.
It is concluded that depth values of disturbing masses
calculated on the bas4s of a T magnetic anomaly maps,
using current simple methods of calculation, yield only
qualitative results. This is due to inadequate detail of
Card 1/2 the magnetic anomaly maps produced by aerial magnetic
-1 49-10-7/10
'Oji the accuracy of determining the depths of location of disturbing
masses studied on the example of the ma-gaetic anomalies of Bashkiria).
mapping and also by the over-simplified assumptions
relating to the physical and geological conditions on
which these methods are based. Use of such methods is
also difficult owing to the considerable influence of
some other factors.
There are 5 figures, I table and 10 references, 9 of which
are Slavic.
SUBMITTED: March 30, 1957.
ASSOCIMION: Ac.Sc~ U.3,5.R. Institute of Physics of the Earth.
(Akademiya Nauk SSSR Institut Fiziki Zemli).
AVAILA I Library of Congress
Card 2/2
A.
S~; LAFINA- M,I;; PUTROVA, G.N.; YALASHNIKOV, A.G.; MWALLOYA,
VIVO,
Ragnetinm of ores. lov. AN SSSR. Ser. geofiz. no.l.*141-143 A 158.
(Ores-Magnatic properties) (MIRA 11:3)
LA pINRI Nq
PHASE I BOOK EXPLOITATION SOV/5140
Kolyubakin, Vladimir Vasillyevich, and Margarita Ivanovna Lapina
Obzor sposobov resheniya pryamoy I obratnoy zadach magnitnoy
razvedki (Review of Methods for Solving Direct and Inverse
Problems of Magnetic Surveying) Moscow, Izd-vo AN SSSR, 196o.
362 p. (Series: Akademiya nauk SSSR. Institut fiziki-Zemli
imeni 0. Yu. Shmidta. Trudy, No. 13/180/) Errata printed on
the inside of back cover. 2,000 copies printed.
Resp. Ed.: A. 0. Kalashnikov,
Ed. of Publishing House: L.
S. 0. Markovich.
PURPOSE: This book Is intended
In research in magnetometry.
in the same field,
Doctor of Physics and Mathematics;
K. Nikolayeva; Tech. Ed.:
for scientists and engineers engaged
It may also be useful to advanced
COVERAGE: The book presents methods for solving direct and inverse
problems in magnetic surveying, for the case of uniformly mag-
netized bodies. The material presented has been assembied from
Car
Review of Methods (Cont.)
SOV/5140
both Soviet and non-Soviet literature up to and including 1956.
The book consists of three parts each of which is preceded by a
brief introduction giving a description and general statements
relating to the methods cited. The first part is devoted to the
direct problem of magnetic surveying. It considers analytical
(Chs. I and III) and graphical (Ch. II) methods for solving the
direct problem. The general methods for obtaining calculation
formulas for magnetic fields in the case of homogeneous mag-
netization are described in the introduction to the first part.
All formulas are cited without derivations. Bodies bounded by
surfaces of the second order are separately treated from the
bodies of a given form for which the solution of the direct
problem is presented. Throughout the book universally adopted
designations of bodies are used. Where necessary, a descrip-
tion of the distribution of the magnetic charges along the
body surface is given below the name of the body. The second
part contains material for solving the Inverse problem of mag-
netic surveying. Methods are considered for determining depth
and dimensions of a body which require preliminary assumptions
C a-rZ= ~,-
Review of, Methods (Cont. SOV/5140
regarding the shape of the body (Chs. I, II, III) and also
methods for which this condition is not necessary (Ch. IV).
Descriptions of these methods and general conditions for their
use are given in the introduction to the second part; each method
is given without any recommendations as to its application. The
third part is auxiliary and deals with calculations of the gravi-
tational and magnetic potential and its derivatives in the upper
h~lfspace and in the plane of observations. This material is also
presented Wthout a-dtqtement of the methods used in obtaining the
formulas. Single designations are Introduced in the book, the
-explanation of which is given at the beginning of the book in a
general list. 1n several sections some of the formulas are derived
by the authors. The following personalities are mentioned:
V. N. Strakhov (method of isolines), B. A. Andreyev (method of
limit distributions), T. N. Simonenko-Rose and A. P. Kazanskiy
(integral formulas), Yu. N. Grachev, V. F. Pyatnitskiy,
V. V. Kolyubakin, A. A. Logachev, L. Peters,, A. N. Timofeyev
(various forms of the method of tan ents). There are 476 ref-
erences: 275 Soviet, 123 English, 96 German, 9 French, I Swedish,
I Portug*ze, and 1 Hungarian.
KOLYUBAKIN, Vladimir Vasillyevich; LAPINA, N!~rgarita Ivanovna; KALASHKIKOV,
A,G., doktor fiziko-matez.nau I otv.rai4,; NIKOLAYEVAP--L.K... red.izd-va
MARKOVICHY S.G., tekhn.red,
[Review of methods for solving direct and inverse magnetic prosi.-
e(,-,.
'ing problems] Obsor sposobov resheniia priamoi i obratnoi zadach
p
magnitnoi razvedki. Moskva, Izd-vo Akad.nauk SSSR, 1960. 356 p.
(Akademiia nauk SSSR. Institute fisiki Zemli. Trudy., no.13)
(MM 14:5)
(Magnetic prospecting)
s/o49/6o/oo0/oo4/oio/Ol8
AUTHOR: Lapina, M.I. E032/E314
TITLE: Some R-e-s-uTTs-of a Study of Vertical Gradients of the
Magnetic Field in the Region of the Kursk Magnetic
Anomaly
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya
geofizicheskaya, 1960, No. 4, PP. 594-600 + 1 plate
TEXT: During 1954-1957, the Institute of-Physics of the Earth,
AS SSSR, carried out measurements of the magnetic field Z and
the vertical gradients of the field Z using the M-2 instru-
ment. The work was carried out by N.P. Vtorov, M.I. Lapina and VC
D.A. Student. It was directed by V.V. KolyjaUin. The value of
Z-was- me;-su ed with an error of up to 200 - 500 Y , the anomalies
being between 0.3 and 1.2 Oe, whilst the errors in Wah were
5 to 10 y/m -vith the corresponding anomalies of 50 to 700 Y/m
The data were used to evaluate the accuracy of the existing
methods of calculation of aZ/Oh by comparing the theoretical
and the observed values of 3Z/ah . Eight methods of calcu-
lation of aZ/ah were chosen, In methods I and II DZ/ah
was calculated according to Eq. (1), the integral being evaluated
numerically using the Tyapkin method (Ref. 3) (method I) and the
Cardl/3
s/o4g/60/000/004/olo/ol8
E032/E314
Some Results of a Study of Vertical Gradients of the Magnetic
Field in the Region of the Kursk Magnetic Anomaly
Strakhov method (unpublished, method II). In method III the
vertical gradient was calculated as described by Strakhov in
Ref. 2, while in method IV the gradient was calculated from
Eq. (2) of the present paper using a chart to calculate H from
the given distribution of Z . In method V use was made of
Eq. (3), in which all/ax was calculated from the H curve by
the least-squares method, using Strakhov's chart (unpublished).
In method VI, the gradients were calculated from Eqs. (4) and
(4a), in method VII from Eq. (5) (the Andreyev formula, Ref. 1)
and in method VIII from Eq. (6) (Strakhov formula). All the
calculations were concerned with the two-dimensional case, since
practically all the anomalies could be considered as two-
dimensional. Methods I to V give an accuracy of 10% when the
experimental accuracy for Z is 0.5 to 1%. Methods VI to
VIII give a 15 to 200/10 accuracy. Fig. I gives the measured
(dotted curve) and calculated (full curve) values of Wah
Fig. 2 gives a comparison of the observed and calculated
(methods I to V) aZ/ah In one case (Figs. 3, 4 and 5) the
Card 2/3
S/049/60/000/004/010/018
9g2 Ea~4
Some Results of a Study of Verf a~ adients of the Magnetic
Field in the Region of the Kursk Magnetic Anomaly
problem could not be considered as two-dimensional. Using
methods I and II in a three-dimensional treatment of the V/C
latter case, calculated values were found to be accurate to
within 10%, the measured values of Z being accurate to 0-501'0
to 195, There are 6 figures, 4 tables and 4 Soviet references.
ASSOCIATION: Akademiya nauk SSSR Institut fiziki Z6mli
(AS SSSR Institute of-Physics of the Earth)
SUBMITTED: July 9, 1959
Card 3/3
LAPII:A
the
e'd in ,in
U i no variations o e
mi~ -_-r--~Aic susceptibility of highly mapnetic rocks in 4-air
7,
rlaau~r,-a, locatior. Iz-,;. 111V SSII. Ser. geofiz. no. 3:41e-
I;t2 Mr 161. 0.1-D, 14:2)
1. ImAit-Ov. fj.~Ahi zeud-*L. j.11 SSSR.
1-roperties)
'j)BVITSY14, VOM.; LAPIIM, M.I.; SIME =4011, B.L.
Effect of inhomo zation.of a body of constant
.geneous.megneti
susceptibility on the results of magnetic anomaly interpretation
by,simple methods. Izv. UJ SSR. Ser. geofiz. no. 3:428-432
Mr 161. (JIIRA 14:2)
1. Institut fiziki Zemli AN SSSR.
(Shchigry Region-Magnetic prospecting)
KOPAYEV, V.V.; LAPINA, M.I.; RASPOPOVp O.M.
yariation method. of determining magnetic properties of highly
magnetic rocks. Izv. AN SSSIR. Ser. geofiz. no.9:1354-1362 S
l61. MRA 14:9)
1. Akademiya nauk SSSR, Institut fiziki Zemli; Leningradskiy
gosudarstvennyy universitet im. A.A.Zhdanovaj Kurskaya geofiziche-
skaya.ekspeditsiya.
(Zhigayevo region-Magnetic prospecting)
IAPINAp X.I.1 STRAKROV).Y.M.
New.method for calmaating the vertical derivatives of potential
fields in the qpper half'space; Izv.AN SSSR.Ser.keoflz~
no.4&561-577 Ap 163, (MA 16s4)
1'. Institut fiziki Zemli IN SSSR.
(Mapetism~ TerreBtr1al)
-
-
PR I K ti OT'K 0, F.
24 (T) ~-3 PHASE I BOOK MLOITATI
ON301/
1365
Mate rialy 2 Vamsoy=.2go saveshchani7a po spektroskopli. t. It
V41okulyarnaga spaktmls;~plys, (Papers or the 10th All-Union
Cc Vol. It WleculLr SpactrosooPY)
%6renoe on Spactnsocp7.
0
0v) lzd-vo Llvovskogo univ-ta, 195T. 499 p. 45
OD)coplea
EL
3
'
printed. (Sarlest Its; Vitychnyy abirayk* vrp.
/
/
Additional sjonsoring Agencys Akademlya nauk SM. Kozl&aly& PO
k
k
S
h
I
V
S
tros
opil. Rd.s later,
.L.; Tec
.
spe
araMk, T.
.)
Editorial Doardt 1A.4aterg U.S., koadetlo an (Rasp. Zd., Deaemad).
t
Weparont
B
S
Doctor at 6~slcal =4 MAthematical Sciences
.
,
.,
,
Fabelinskiy, X.L., Doctor of ftsioal and PAthomstical Sciences,
Y"-Iktz-%. V.A.. Doctor of Ph7nloal and Mathamtlottl Sciences,
KO V.Q., Candidate of Tso!=Acal Science*, PLayakly, S.M.,
=
r rhy lo4a jua mathecAtical 34jaz4as, Xllzovakly L.K.
I
Candidate of Physical arA MmitherAtical Sciences, Klliy&n*bU, V.3:,
Candidate, of 41 " M&th*vAtjova Sciences SM Glaubarman,
:10
a 1
1
N
m
6
timogs.
C '
A. Yo., andl of rhysleal and Kathematio
,a
card 1/30
Savinov# B.O. Use of Infrared Absorption Spectra in
Daterrdning the Characteristics of the Products of
vitamin I Synthesis 265
Belm X.U. Optical Method for the Determination or
the Cozoosition of Cavlexes in Solutions 26T
BOSOmOlov, S.O., M.P. Grobenshohlkova, and 1. Y&.
Llplavk. Analysis of Phenol-naphthalone Pdxturas
by NO&" of mtraviolet Absorption spectra 270
Zlalm X.X. and A.D. Siryu)" Oroup Determination
Of 6. N;hthaena Hyd"aarbons by Means of
Ultraviolet Absorption Spectra 2T2
SUbadach, A.M., V.?. PaherAtapta, ArA V.K. xhlahava.
Spectrwhotomatria Methods of Phass control in
Prooessing Acetic Anhydride 975
Noporent, B.S., K.P. Vasilevskly, and X.A
*
tative Absorptlbn b
Means of'
a
l
Vat
y
,
or
y
ap"
lr
t
lara"d Asalon
Card IBAO
51-3,13/14
AUTHORS: Neporent, B. So, Vasilevskiy, K. P., Lapina, R. A*
and Fursenkov, V. A.
.TITLE: A Vacuum Spectrometer with a Diffraction Grating for the
0 7-3/.t Spectral Region. (Vakuumnyy spektrometr a
difraktsionnoy reshetkoy dlya oblasti spektra 0.7-3/-6)
PERIODICAL: Optika i Spektrookopiya, 1957, Vol.III, Nr.3, pp.289-295.
(USSR)
ABSTRACT: This paper described apparatus of.high resolving power
for obtaining spectra in the region 097 -3 11 It consists
of a recording vacuum spectrometer with a diffraction
grating and a cell which light-is made to traverse many
times so that its path length in the vessel can be 180 m.
This apparatus is suitable for recording of spectra of
rarefied or weakly absorbing gases at temperatures from
room temperature to 10000. The optical part of the
apparatus is shown in Fig*l. Fig.2 shows the general
view of the apparatus with the control panel. The cell
used in this apparatus follows in its construction Ref.
14 and 15. The diffraction grating used is of echelette
Card 1/3 type, 150 x 150 mm, with 300 lines per millimetre. This
51-3-13/14
A Vacuum Spectrometer with a Diffraction Grating for the 0.7.-i
Spectral Region,
grating reflects 75% of the incident light at 2/j-,
55% at 1.5 )u and 60% 'at 2.3 The monochromiLter used
follows Ref.16. The spectroire;er is placed in a vacuum
chamber (0.1 mm Hg). The signal falls on a PbS
photoresistance and is amplified. For this purpose
the incident light is modulated by a perforated disc at
550 c/o frequency. This apparitus makes it possible to
resolve spectra down to 0.1 cm- Fig.4 shows radiational
lines of water vapours near 3900 cm-1 obtained usijg the
apparatus described. The flit width was 0.06-cm- and
lines approximately 0.1 cm- distant from ea:ch ofher are
resolved. This means that the resolving power of the -
instrument reaches 40 000, and this corresponds to 45 000
resolving power of the diffraction grating. Fig.5 shows
absorption spectra of water vapours near 2.7,/.j- obtaineId
using path lengths of 8.8 (broken curve) and 120.8
(continuous curve) metres respectively~ When the
container used was of quartzabsorption and emission of
Card.2/3 carbon dioxide could be measured with this.apparatus.
A Vacuum Spectrometer with a Diffraction Grating for the 0.7-3
'Spectral Region.
The authors thank F. Me Gerasimov for supplying the
diffraction grating used. There are 5 figures, and
17 references,, 1 of which is Slavic.
SUBMITTED: 15 January, 1957.
AVAILA-BLE: Library of Congress
Card 3/3
. DRAIKIN, L.A.; TVARADZE, L.R.; !--kEj-mj A-
Coking of Tkibulli coals In-the" I~arkov rxperimBntal Plant.
Trudy Inst.prikl.khim.i elektrAhim,AN Gruz,SSR,3sl8q-193
1620 (WRA 1631)
(Kharkov-Coal-Carbonization)
MKITAiik)VA2 P.D.; LAPINA.. N.r.
Life span of suailik fleas Neoppylln 6etosa Wagn~ and Ceratothylluo
t--so,uorum wagn. under natural conditions~ Zool. zhur. 44 no.6.'883-
887 165. (MTRA 18-10)
1. Institut "Mikrob", Saratov.
PORAY-KOSff ITS, A.Ye. [deceased]; FMAY-KOMITS, B.A.; LAPINA., N.G.
Rasearch in the field of tautomerle compounds. Part 19. Tautomerism
of dipyrazolonyl-m-nitrophenylmethane. Zhur.ob.khim-25 no.8:1604-
1609 Ag 155. (KWA 9:2)
1.Leningradekly tekhnologichaskiy institut imeni Lensoveta.
(Methane) (Isomerism)
USSR / Soil Soionoe e Biology of Soils J-3
Abs Jour. Ref., Zhur Biologiya.. No 17, 1958., No, 77400
Lapinao H. K.- Kasstochkin, V. I.
:Author
Inst Institute Z~tel Reserves AS UM
Title Ion Exchange and the Structure of Humto Acids
Orig Pub :.Pochvovedeniye, 1957, No.9, 28-32
Abstract Investigation of the IE absorption spectra of humic, acids
and humates of Na, Ca and Ba.tbat were separated from
.different coals confirmed the -molecular machantem of ion
-e xchanIgo in'the alkaline solutions,of'binaies'. Alkaline
humates are genuine molecular solutions vh1ch consist
of individual arcmt1c lattices vith lateral radicals vhich
carry car'boxylic groups in ion fom. With the formation
of Ba- or Ca-humates, an exchange reaction vithNs. or H
takes place; the formation is possible of complexes of two
and more molecules of humio acids connected through a cation:
Card 1/2
LAPINAP N.M.
So that children could have a good posts Sov*profsoluzy 17 U0.12:
38 Je 161. 1415)
1. Starshiy Instruktor sektora po rabote aredi uchasheheyaya,
molodezhi i detey kullturno-massovogo otdo2a Vaesoyuzno teentrallnogo
soveta profsoyuz6.
(Pioneers (Co=inist youth)) (Canping)
LAPINA, N. N.
"Biostratigrapby and Brachiopods of the Lower Carboniferous
(Vizey) and Middle Carboniferous Deposits of the Molotov Cis-Urals."
Cand Geol-Min Sci, All Union Sci-Res Inst of Geological Prospecting
for Petroleum Leningrad., 1954. (RZhGeol,, Nov 54)
Survey of Scientific and Technical DissertEtions Defended at USSR
Higher Educational Institutions (11)
SO: Sum. No.521., 2 Jun 55
2210Y. N.A.; UP
Bottom depoelts in the region covered by the "Worth Pole 24 drifting
stntion. Izv.AV SSSR. Ser.geol. 21 no*7:3-16 Jl 156,
(HLRA 9:10)
li, Gls"o7e Upravlaniya Severnogo z ,or Bk6go pati, Ark-tichaskly na-
ujphnq-issledovatellskl~ inotitdt,..LenIuU&d*
bottom)
~ ep I A),Ij IV, Al,
Loin, N.N.
Mw.ngs in the porosity and gas permeability of rocks belov freezing
point& Trudy Nauch,-Issl, inst, geol, Arkt. 89.-189-200 156.
(Rocks-Permeability) (MIRA Iltl)
SOV/ 124-58-5-5605
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 5, p 99 (USSR)
AUTHORS, Lap avinova, A. 1.
TIT LE: The Study of the Permeability Coefficient of Sand at Subfreezing
Temperatures (Izucheniye koeffitsiyenta fill tratsii peska pri
otritsatell noy temperature)
PERIODICAL: Byul. nauchno-tekhn. inform. M-vo geol. i okhrany nedr
SSSR, 1957, Nr 3 (8), pp 28-29
ABSTRACT: Bibliographic entry
1. Sand--Physical properties
2. Sand,--Temperature factors
Card 1/1
LAPIX&, N.11.
-
processen taking place in soilo 'under freezing point.
-I-- Inform. biul. NIIGA no.2:34-39 158. (MU 12:10)
(Soil chemistry)
LAPINA N.N.
Conditions governing gas and water migration in sandstones below
freezing temperatures. Trudy IIIIGA 67:177-217 158.
(MIRA 12: 10)
(Rocks--Permeability) (Porosity)
MLOV, N.A.; IAPIIIA, N.N.
Bottom sediments in the central part of the Arctic Ocean.
Trudy nauch.-isal. 1nst. geol. Arkt.,85:go-n6 '58.
(MIRA 12:8)
(Arctic Ocean--Sediments (Geology))
B#,loir, N'. T,avina, N. N. SV
ir, X 1"a -, a ~-: P. n i. ra j F_, - a i or rhe iio t Din -: 9d i rt;~, n ~ a 2 o~*
zn c rc t. i c :~c ea n i!&:2 n tia ii isvv., ~E, -,!1a t - F_Lka. ts _,). sic nnyl-r.
-,.,eana)
Vokiady AkadeLn-, nauk Nr I
U,
q, Strali~~`i(ML.ion c~ tiie rcL~c Dasin as mentioned Jn the t2r.;e
wai; aescrirjeii J'or tne f-;rst -time by members -,i ine expeditions
t i-'cien-
' Lne !~rkLicheskiy nauenno-iosledovatell-kiy insli,-u~
o
ti-fic Research -1nst.--, Late for tne Arctic Re,7ion 3n tne years
from " 948 to 114-)4 . N. A . Bel c)v succeeded, nowever, oziiv in 19s,:~
in (-akirig a 412 cm nign cojumn from a depti, of j 044 w for the
fir8t time during the mentioned expedition aboard thta ice-
breaker 'IF. Litke" north of and Frans Josef,. _.and
(!'-'hpitsbergen, Zemlya Frantsa !oFjl*a) (Fig 1). The obtaiijed re.-
sulTs confirmed the entire scheme of' stratification which had
been found already in euriier invieziLipations iRpi'3 1,5). On th(.
strength of the stratification of tfic sediments ana of tne
radium content the absolute age may be determined and the cor-
Card 1/5 relation can be carried otit betveen tne3e sediments and k. 1.
60V/20- 122-1-32144
New Data on the -itratificrtion of' the Bottom c:edimenTation of the Arctic
Ocean Basin
Moskvitinov's and S. A. Yakovlev's schemes for the Quarternary
on the conLinent. They are: 1 ") Recent deposits from present
time unL.41 9 000 - 110 000 years ago. 2) Finiglacial, or the
fourth new glaciation in Europe and the Sartanskaya glaciation
in !,ioeria (Sibirl): 9 0QO - * 10 000 an(2 as far as 16 C100 -
1-1 000 years ago. 3) Sediments of' the heat period 16 000 -
17 000 to 20 000 years old. 4) Deposits from the cold period
of the Ostashkovskoye or third neyt glaciation in Europe and the
second stage of the Zyryanskoye giaciation in 8ibir, are 20 000
to 30 000 - 32 000 years ola. 6 The sediments of the next cold
period which obviously corresponds to the Kalininskoye or sec-
ond new glaciation in Europe and the first stage of' Zyryanskoye
glaciation in Sibirl are 50 000 - 52 000 to 6-i 000 - '70 o0r)
years o)d. 7) The sedimentation of the deposits underneath
which date from the heat period took place during the boreal
encroachment (Mikulinskiy period), e.g. 65 000 - 70 000 to
110 000 years ago. 8) The sediments which are below the men-
zioned ones were already deposited during the Moskovskoye or
Csru ~1'3 first nt_A glaciat3.on in Europe and the Tazovskoye in -ibirl
I
':0V 1, 0
-122-1-52/4j
Nev., Data on t~e !~7,tratificaLion of the Pottum -~euimentatiur, of tnif ;-re-Lic
Ocieein Basin
netween 110 000 and '1:;') 000 - 1'~*) y~,,rs qpo. 411 Those strata
,r he- vricv, ~.X ':ir- Middle
were formea durinp tne I-
', i. o, Til v eF7
r:, ae,(,, wi !:a r. inning
':' nr f. re fig
o, c,-) tld )i.,*, ?,).l a ure and
ASSOC I,.~T., ON: i i:~. geo I oi~i -I k iki -rctic Ins ti-
r C L j C 0 p. y
P R E, 3 E Irl 6, rjy 1~. la. kcademy of Sciences,
SUBMITTED. 2-l", 19-16
Card 3/3
~ (0)
AUTHOR: Lapina.-N. N. SOV/20-1271-3-42/5-A
TITLE.- New Data on the Stratigraphy of the Carboniferous at the Mouth
of the Lena River (Novyye dannyye po stratigrafii kartona
ustlya r. Leny)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 3t PP 528-529
(USSR)
ABSTRACTt In the northern Kharaulakh mountains brachiopods were cillac-ted
from sediments which correspmd to,the upper parts of th6
Visean and Namurian Stages, as well as the Middle Carbor--~f--.-
(collected by Ye. 1A. Lyutkevich and V. D. Nikiforova). T-,i::~,--gh
identifications of the collection of A. A. Mezhvilk 1-
carried out by A. P. Rotay, the impression originated th,-,.-, .-.77ay
Tournaisian and Visean sediments (Lower Carboniferous) in
these mountains. The author has-a brachiopod fauna from thass
mountains which indicates the development of the upper part of
the Visean and the Namurian. The Middle Carboniferous secllimnent~-~
(thickness of 800 m), grouped as the,Tiksinskaya suite by A. A.
Mezhvilk (Ref 1), lie-directly over the jCrestyakhskaya.
conglomerate. The fauna of this conglomerate includes the span
Card 1/3 of time from Silurian to the Lower Carboniferous. The opinion
New Data-on the Stratigraphy of the Carboniferous BOV/20-123-3-42/54
at the Mouth of the Lena River
that these sediments belong to the Middle Carboniferous stems
from F. N. Chetnyshev (1883, after collections by E. V. Toll'
and A. AO'Bunge). This standpointp.disputed by many
investigators,now begins to win more and more general acceptance.
The chief basis for the diverging ihtiarP;O_t&.tjkQAO is the
insignilCioant similarity between this fauna and the well known
Middle Carboniferous fdund of the western areas of distribution
(Ural, Donbass, Podmoskovlye 'Moscow Basin). It is likewise
dissimilar.to the fauna lying directly over it in the
Kharaulakhski3emountains and to the fauna of the contemporary
deposits of the neighboring Arctic regions (Novaya Zemlyat
Taymyr). By comparison the author has discovered a similarity
with the brachiopod fauna of the lower part of the North
American Pennsylvanian System. Nevertheless, some elements of
the European fauna are also present. Characteristic is the lack
of the widely distributed Middle Carboniferous group of the
Choristites. Consequentlyq the Tikeinskiybraoh:Lopod complex
Card 2/3
New Data on theStratigraphy of the Carboniferous SOV/20-123-3-42/54
at the-Mouth of the Lena River
belongs in its entirety to the Middle Carboniferous, perhaps
with the exception of the uppermost parts, which could be
placed in the Upper Carboniferous, There are 3 Soviet references.
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy geologo-razvedochnyy
neftyanoy institut (All-Union Petrbieuvi-lwtltuti for S_d*jen:1.jfjc
Re"arch-and Geologic Prospecting)
PRESENTED: June 28, 1958, by D. V. Nalivkin,-.Ao"am;~cian
SUBMITTED: June 26, 1958
Card 3/3
TAP I NA, N. H.
Mineralogical provinces established on the basis of recent bottom
deposits in the Arctic ocean. TrudY NIIGA 107:42-50 159 (KIU 13--3)
(Arctic Ocean-Deep-ses, deposits)
3(5)
AWHORS:
TITLE;
SOV/20-128-2-40/59
Lapina, N. N., Troshina, M. K.
The Carboniferous of the North of the Bol'shezemel'skaya Tundra
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 128, Nr 2, PP 366-366
(USSR)
ABS TRAM The occurrence of considerably bituminous rocks in Upper
Devonian and Lower Carboniferous strata was detected first by
G. A. Chernov (Hof 1) in 1940, then by D. K. Aleksandrov (1941),
as well as by B. I. Tarbayev and V. A. Urman (1954) in the
region of Sin'kin Nos on the Talata river east of the afore-
mentioned tundra. A strong bitumen smell and bitumen inclusions
were characteristic of the petroleum manifestations. The above
exposure was investigated in 1958 by M. K. Trochina, and the
fauna (foraminifers, anthozoans, braohiopods, gastropods) was
collected in one layer after the other. Investigation of this
fauna first suggested a new scheme on a biostratigraphic basis
instead of on the hitherto lithological one. The T o u r -
n a i a i a n s t a g e is represented by carbonate rocks
which on the whole are very similar to those of the Famennian.
Card 1/4 The lower boundary of the Tournaisian is therefore drawn only
SOV120-128-2-40159
The Carboniferous of the North of the Bollshezemellskaya Tundra
with certain restrictions. T h e 1 o w e r s t a g e o f
t h e L o w e r T o u r n a i a i a n is represented by
alternating light- and yellowish-grey, fine- and medium-grained
limestones and dark-grey, fine-stra"IL'fied dolomites. An impact
causes a slight smell of H 2S and of'_~'~~nllight petroleum frac-
tions. The fauna was determined by L. F. Grozdilova, N. S.
Lebedeva, and A. V. Durkina. The lower stage is 120 m thick.
U p p e r T o u r n a i s i a n 1 o w e r s t a g e . The
fauna is bound here to the upper part. The anthozoans were de-
termined by Yu. N. Rogozov. Bitumens are found in strongly
cleft calcareous layer. The lower stage is 100 m, the entire
Tournaisian stage 220 m thick. The V i B e a n s t a g e is
230-235 m thick. The sediments of the T u 1 1 s k o -
A I e k s i n s, k i y c o m p I e x belonging to this stage
rest without any visible interruption upon the above lower
stage (thickness 110-115 m). The upper boundary of the
Aleksinskiy horizon is drawn at the interfaces between the
crystalline limestones (without macrofauna) and an organogenic-
Card 2/4 elastic silicified limestone of the Mikhaylovskiy horizon. The
BOV/20-126-2-40/59
The Carboniferous of the North of the Bollahezemellskaya Tundra
rocks have a slight petroleum smell. M i k h a y 1 o v s k i y
h o r i z o n (80 m) has its upper boundary in the roof of a
massive limestone (3 M thick) with flint. The V e n e v s k i y
h o r i z o n (40 m) has abundant fauna. Bitumens are found in
the shells and cavities of the limestone. S e r p u k h o v -
a k i y 1 o w e r a t a g e (70 m). Their topmost layers
which correspond to the Protvinskiy horizon are sugar-like,
coarse-grained limestones which occur north-west of the Talata
river and on the coast of the Barents Sea. No fauna was found
in them. They are separated from the exposures of the under-
lying limestones by an interruption 40 m. thick which is covered
with grass. The latter contain-' fauna. The cross section in-
vestigated here is thus extremely similar to those of the Lower
Carboniferous of the Podmoskovnyy basin and North-Ural.
Only the terrigenous mass between the Tournaislan and Visean of
the Russian platform lacks here and is replaced b,', carbonate
sediments which most probably belong to the Tullskiy age.
There is 1 Soviet reference.
Card 3/4
SOV/20-128-2-40/59
The Carboniferous of the Korth of the Bollshezemellskaya Tundra
ASSOCIATION: Vsesoyuznyy neftyanoy nauchno-iseledovatellskiy geologo-
razvedoohnyy ini3titut (All-Union Scientific Research Institute
of Geological Petroleum Prospecting)
PRESENTED: May 4, 1959t by D. V. Nalivkin, Academician
SUBMITTEDt April 29, 1959
Card 4/4
PHASE I BOOK EXPLOITATIOV SOV/5331
International Geological Congress. 21st, Copenhagen, 1960.
Morskaya goologlya (Karine Geology) Moscow, Izd-va AN SSSR, 1960.
205 1p. 2~500 copies printed. (Soriess Doklody novatakikh
geo2ogov, problems 10)
Editorial Board: P. L. Dezrukov, Reap. Ed.; A. V. Zhivago, V. P. z'
Zenkovich and 0. D. Vdintsav; Ed. of Publishing Houvoi V. S.
Sheyaman; Tech. Ed.: V. Karpov.
PURP=S This book In Intended for geologists and oceanographers.
COVERAGEs The book contains 18 articles reprocentinC the reports
given by Soviet geologists at the 2lat. International acolozAcal
Congress. Individual article* deal with the bottom topoC:rcphy.
sedimentation, and tectonics of oceans (Ventern Pacific and
Southern Indian), an well ad the gcomorphalo~ and tectonics of
the Black and Cagian Seas and Soviet sectors of the Wltlo.
An English r4ouz.3 accompanied each artiola. He Porconalittea
N It , 1. Ta Mkhallta!a, 0 B. VdIntoov, 1. D.
or
Licl_rv;~, ~nd Iloprochn_9y. RaruMo
V_Q_- ~gitions or_ a !YEh-rs_ Crust Under
'.tion. 0 er
Sci=ic-xioustic dn oyr a L
Seas and Oceans
a;
Sold-,,a Kh M 3tratigr hy t& a.1d the PalcoS,ioaraph,7
on
r -2
g frart;Ntorn Pacific and tha' Par Eastern Sean of the
V= According to Sea-Bottom Foraminifers 59
L'LsIt A Formation of Sediments In the Southern
19ftd-A'a-lan Voeans 69
M
and IT. A Belov Bottom Sedimentation Can-
1NON: %-he Artk-
Gotehu,qy, V. P,,,and Ta. P. Neproohnov. Bottom Gcomarphology
and Tectonic Frob cma or the Black Sea 94
lolov7ey V P L S ako 0. Y_AZapova. Relief and
a .1. t ;;.uro or i.Xa, =d
n Southern Cadpinri-S-Fl' 105
vloh D To Recent Shelf Deposits in the Marginal
0
Pr 216
ja!jova. M. V. The Geology of the Barents Sea 223
Gorshkova, T. 1. Sediments In the Nortragian San 132
To v . H_ V. Study of the Diagenesis of Some Kerins
R=n t 0 240
Zornkovich V. P.x 0. K. Leantlyov, and To. N. Nevooekly The
iW=4~-~J-cr-tho the
Development of the Coastal Zone of Soviet Seas 254
A
lbulatov, ~._A_ V. L. Do gyrov, and V P Zankovich. Song
troama Along 164
P A, Xs plin,tand V. S. Medvedov.
;N.Notv~.Vria,'c 1,1110-vLem-cn ton," ashorea-Th he 0 ~2-2 ~tr- 275
Isontlyev, 0. K. Typed and Formation or 14&ocna on Recent
Sea"oroo 288
C"d-4,is
I
1._'_%
01-1
METEV, V.A.; L&PINA, N.N.
Stratigraphy and brachiopods of Carboniferom deposits on the
eastern slope of the Arctic Urals. Tnidy VNIGRI no-154:142-166
16o. (MIRA 13:9)
(Shchuchlye Valley~Brachiopoda, Fossil)
(Paleontology, Stratigraphic)
B=Vv N.A.; LAMNAY N.N.; SAKS~ V.N., red.; DROZHZHINA, L.P., tekbn.
red
[bottom sediments of the Arctic Sea basin ] DonWe otlo2ale-
niia Arktichaskogo basseina. Pod red, V.H.Saksa. Leningrady
lzd-vo "Morskoi transport," 1961. 151 P. (MIRA 15:5)
1. Chlen-korrespondent Akademii nauk SSSR (for Saks).
(Arctic regions-Deep-sea deposits)
BEIAN., N.A.;. UPINA, N.N.
Wenty-five yeap of geDlogieal studies of ibe bottom of.the
Arctic Ocean. ProbX.Arkt.i Antarkt. no,nt97-104 162.
(KMA 16s2)
(Arctic Ocean-Ocean B.Sc.'
LAPINA, N.N.
Stratigrapby and Brachiopoda of the Lover Carboniferous sediments
in the nortbeastern part of the Siberian Platform In the Olenek
basin. Trudy VITIGRI no.196.Paleont.ebor. no.3:107-123 162*
(MM M: 4)
(Olenek Vaiiey~-Geology, Stratigraphic)
(Olenek VaUey-Brachiopoda, Fossil)
LAPINA, N.N.
Brachiopoda of Krestyakh eonglomerates from the lens, estuary.
Trudy VNIGRI no.196. Paleont.9 . no.3.?125-149 962.
,r (MIRL 16:4)
(Lena Valley-Brachiopoda, Fossil)
LAPINAi N.N.
Stratigraphy of the Lower Carboniferous deposits of the Siberian
Platform.- Dokl.,AN SSSR 148 no.5026&-1171 F, 163. (KM 16:3)
1. Vsesoyuznyy neftyanoy nauchno-issledovatel'skiy geologorazvedochnyy
institut. P-redstavleno akademikom D.V.Nallvkinym,
(Siberian.Platfoi ..,,eology, Stratigraphic)
LAPINA Nina Nikolayevna; KULIKOVI M.V p red.; IONINA, I.N., vedushchiy red.;
A.B.I. te~~;.red.
[Brachippods of Carboniferous sediments in the Ural Mountain
portion of Perm Province) Brakhiopody kamennougollnykh otlozhenii
Permskogo Peiurallia. Leningrad, Gostoptekhizdat, 1957. 132 p.
(Leningrad. Vsesoiuznyi neftianoi nauchno-issledovatellskii
geologorazvedochnyi institut, Trudy, no.108). I (MIRA 16:8)
(Perm Province-Brachiopoda, Fossil)
LkPIMA, N.N.
Using ultrasonics in the
for mechanical analysis.
245-252 164.
preparation of sand-clay sedinants
Uch. zap. NIIGA. Reg. geol. no.4;
(MIRA 18:12)
7AHAXEIDVMTA, Aleksandra Grigorlyevna; LAPI #ina Tladimirovua;
XHMBLITSKIY. B.N.-j redektor; NEL"W2. talstva;
~IKRONOVA, Ye.A., tekhnicheskiy rodaktor
[Plann-ing and analyzing cost of ship repairs in shops of the
Ministry of the Merchant Marine] PUniruvanis L analiz sebes'toimosti
:udoremonta,na zavo'dakh Ministerstva morskogo flota. Moskva. Izd-vo
Morskoi transport," 1956. 125 P. .. (MIRA 10:7)
(Ships--Ma into nance a ad repair)
ZAKMOVSrATA, A., kand,ekou.nauk; LAPINA, Nove
Inproving the planning andmeounting system in the ship repair enter-
prises. Mor.flot 19 no-9 S '59. (MIRA 12:11)
1. lachallnik sektora okonomiki prompredpriyatiy TSeutralluogo uanchno-
tsaledovatellskogo instituta morskogo flota (for Zamakhovskaya). 2.
Nachallnik planavo-ekonomicheakogo otdela Kanonerkogo zavoda (for Lapina).
(Shipping-Wittenance and repair)
SHRABSET M.J. dots.; CHFRJ[%SOY-TSY3IZOV, A.,starshiy prepodavatelf- MILYUKOV,M.;
prepodavatell; BORISOV, B.,inzh.-ekonomist; LWU&, N.
wEconomics of transportation by aeaw by S-F.Koriakin, I.L.Bernobtein,
W.F.3911inskii. Reviewed by I. Shrabahtein and others. Mor.flot 20
no.lo:46-48 o 6o. (MIRA 13:10)
Odesakiy institat iuzhenerov morskogo flota (for Shrabshteyn,
Gherkesov--mTSybizov, Milyukov). 2. Nachallnik Planovogo otdela
Baltiyskogo parokhodstva (for Borisov). 3. Nachallnik Planovo-
~ekonomicheukogo otdela Kanonersko.vo zavoda (for Lapica).
(Shipping)
(Korlaklui S.7.) (Bernshtein, I.I.) (Illineklil, IU.7.)
KRAVCHIKp Feliks IvanovichjKAWOMy I#Lov retaenzent;_w___mA,-Nff-7
retsenzent; DZFJCLaWCYVp T.L.,, naucbW red*'; SHAMMIOVA, VJf.f
red.,- MISHKOVA,, L.M.., tekhn. red.
(Planning and organization of the repair of ships] Planirovanie
i organizataila remonta audov. Laningradp Goo.soiumoe izd-vo
oudostroit. prorqshl.f 1961. 158 p. (MIU 3.512)
(Ships"ftMaintenance and repair)
/wpmw
AUTHORIs Ivanov, S.I., Shalinets, B.I., Xyshlyayev, A.M. 47-6-36/37
TITLEj A Conference on the Method of Teaching Physice(Konforentaiya
p0 metodike fiziki)
PERIODICALs Pi zika. v Shkole, 1957, 6, Page 93 (USSR)
ABSTRACTs A scientific conference on the method of teaching physics
took place at the Moskva-Oblast' Pedagogical institute with
and the Moscow Oblast' and
teachers from the city of Mosoow
.
representatives of the Moscow, Stalingrad, Krasnodar
Mariyskiy [in,Yoshkar-014, YsbardincP-Bft1kELrskiy, Tula, Yaroslavl,
Berdichev, and Shuys, Pedagogical institutes, the Institut of Psychology
APB and the Kaluga Oblast' Institute for the Improvement'
of Teachers.'
The following reports were heard and discusseds S.I.
Ivanov - "The Methods of Methodi.cal Researches", O.N.Lapina. -
"The Rise and Development of Concepts of Temperaiure Zn_d-14i, n-
tity of Heat".(at-the 7-class school), Ye.Xh. Lyatker -
"The Rise and Development (at the pre-school age and the
7-class school) of Basic Concepts in the Tield of Electri-
city", T. Ya. Ishkova - "The Rise and Development (during
the pre-school age and at the 7-class school) of Concepts
Card 1/2 of Magnetism", A.V. Selenginskiy - "On the Development of
MAGININA, X.P.1 LAPINA R.A. BLINOV, V.A.; GUDVILOVICH, I.V.
New "carbozoline" softeners. Tekst.prom.22 no.3:6" Mr 162,
(MIRA 15:3)
1. Nauchno-issledovatellskiy institut organichaskilch poluproduktov-
i krasiteley (NIOPiK).
(Textile finishing)
I A Y A 9 0 It U AM 111 OR IS 0 V IS It
*a
00
00 3
fit
V a 14 a so m a to V .1 U I *.to
of Cotant from kyosetramine. M. N.
~:Iy
v
-00
pmmt and N. A. llrrbmzhem%ki%
insl U. A. 1
h
twi. arad: id. Cksiv iti. math. not., .1;4FPV
~ -00
ekim. 1936. Wo-IRWin Gcnftn IVW).-A new proce-
(late for the. prtpa. of Cstm lly the
attion of carboxylic no"cortmepwolow 6 given which runs
%moothly at the III. V. at alotoWk !No or K with good
yjrldt attvItAch pnm4ts OniWatlorsis of cocaine front
h
i
h
d
i
A
0
tte an
m" t
roug
tiop
mor
hy.1cyam e and odm
tn4vtoone. Tiopim oplidimod by simply twat ing hyrotcy- zoo
arnior ohh 1110. X. Addimill
7 re 9
-1
AIR-ILA WITALA, L;Itrr.AL 1.1111PATURS CLASSAFKATION I I--- At*
slow 111.1403A.. %jow 110.11.
"noo-i igloo.) .10 Q"V a.(
4241)10.4 111&1111 o" a.. M
T- V--p- 0 Poo
-T- 1, 1 T i An a 4 ad 0 or ; 0 a 0 .1 0 1
is 0 a of '410 It A
1111 0 0 0 o 0 o 0 6 o 0 o
0 Wo
.I MUCH. K.G.; IAPIn, R.A.
. . Poretherification of dialkylaminomethvlalkyl others. Zhur.ob.khim. 23 no.g:
1512-1518 S '53-- (wRA 6;io)
1. GosudaretvenW Nauchno-iseledovatellskiy institut organicheakikh polupro-
duktov i krasiteley im. X.Te.Voroshilova. (Ethers)
LAPINA, R. A.
"Use of Dialkylaminometbylalkyl Esters in the Synthesis of Levelers." Ilin. Higl-er
Education USSR, Moscow Order of le-nin Ghe-.rical Techrzlogy Inst imeni D. I.
Mendeleyev, Yoscow, 1954. (Dissertation for the Degree of Candidate. in Techrdcal
Sciences)
SO- Knizhnaya letopis', 116. 22, 1955. PP 93-105
MIZUCH. K.G.'; JAPIML, RA.
Reactivity oi dialkylaminomethylall7l others and of compounds with
inilar cinfiguration. Zhur.ob.khin. 26 no.3:839-842 Mr 136.
(NM 9:8)
lauchno-iseledovatellskly institut organichaskikh poluproduktoy
i krasiteley inent K.Te. Voroshilova.
(Ethers)
~-Ir, Of d3l 1 IW4 or com-
and R.
b
C
J. Gen. Clem. U.S.S.R. 26, W-9(I9W(H?.rg-
If It tion).-See C-A. 50. 147644,
XRYUKOVAI A.S.;.LAPINA,--&,Au kand.tekhn.nauk,- MIZUCH, K.G.)
kand.-
khimicheokikh nauk
Finishing preparations with a base of dimethylolalkyltriazone.
Tekst.prom. 22 no.9tl6-19 3 162. (MM 15.9)
1. Sotrudniki Nauchno-iseledovatellskogo instituta organicheskikh
poluproduktov i krasiteley.
(Textile finishing)
MYUKOVA, A.S.; IAPINA.. R.A., kand,tekhnonauk; MIZUCH,, K.G.,, kand.khim.nauk
Finish preparations vith a dimethylolalkyltriazone base. Tekst.
pro=. 22 no.8:62-64 Ag 162. (440A 25:8)
1. Sotrudniki Nauchno.-isoledovatellskogo instituta organicheskikh
poluproduktqy i krasiteley (XIOM).
' (Textile finishing) (Tri-ey-in no)
LAP14Aj-7*gOvy uchitelinitsa
Independent work of students in chemistry lessons. Xhim. -i sbkole
18 no.31:61-66 My-je 163. (APtA 16:9)
I* Shkola-internat No.1, Kostroma.
(ChemisU7-Studv and teaching)
ti
YARUSOVA, 11-6. - ULIVANOVA. V.M.; IAPINA.. S ~A..
,Physiological effect of substances with vitamin P activity. Vol).
pit. 16 no-5:66-75 S-0 '57. (MIRA 11:3)
1. Iz otdela vitaminov S,i P (zav. - prof. N.S.Yarusova) Gosudarstven-
nogo nauchno-isoledovateliskogo inetituta vitaminologii Ministerstva
zdavookhraneniya SSSR, MoB1-.va.
(VITAMIN P. effects,
on various phyciol. funct. in animals (Rus))
YA1WSOVA. N.S.; LAPINA. S.A.
Biological test for vitamin P active substances in a Lecoq diet
[with summary in English]. Voppit. 18 no.1:45-49 Ja-F 159.
(MIRA 12:2)
1. .1z otdela vitaminov C I P (zav. - prof. H.S. Yarusova) Gooudarst-
vennogo nauchno-iseledoiatellskogo instituta vitaminologii Minister-
stva zdravookhranoniva 9SSR, Moskva.
(DIETSO
Lecoq diet, determ. of vitamin P (Rua))
(VITA-MIN P, determ,
in Lea,-,, diet (Ru7s))
YARUSOVAI N.S.-; DERGACHEV, I.S.; SELIVANOVA, VA; LAPJIU, S.A.
Physiological effect of vitamin P-like-substances. Vit. res. i ikh
isp. no-.4:92-97 159. (XJ?A 34:22)
Institut vitaminologii Ministerstva zdravookhraneniya SSSR.,
Moskva.
(VITA14IIZ-P)
YAMSOVA~ H.S.; BEREZOVSKAYAj,.'W.Nq LAPINA., S.A.; TIKOTSKAYAj, K.M.
The technique of biological detemination of vitanin F-lilm Substances.
Vit. res. i ikh isp.- no.4:179-183 159. (MIRA 14:12)
1. Indtitut vitaminologii Ministerstvazdravookhraneniya SSSR, Moskva.
(VITAMI!4S-P) (BIOLOGICAL ASSAY)
BF,RE2.OV$KkYA,, N.N.,- TSEWINAp A.Ya.; IAPINAj,,
Interrelations between vitamins C and P. Vop. pit. 21 no.5.
26-31 S-0 162. 041RA 17:5)
1. Iz otdela vitaminov C i P (zav. - prof. N.S. Yarusova)
Gosudarstvennogo z,-auchno-issledovatellskogo instituta vitaminologii.
Ml.nisterstva zdravookhranen--*ya Moskva.
5/244/63/022/001/001/001
A004/A126
00
AJ& Tseytina, A. Ya., Lapina, S. A., A~kadlyevskiy, A. A.'
TITLE: Effects of noise on the C-vitamin metabolism of test animals
PERIODICAL: Voprosy_pitaniya,no. 1, 1963, 78 - 83
TEM The authors studied the effect of noise of 110 db intensity and
1'250 cps frequency on the C-vitamin metabolism-in guinea pigs ihat were sub-
J;cted to this noise for intermittent periods of 4 hours. The entire test series
covered a period of 21 days. The tests were carried out on male guinea pigs,
weighing 500 g each, that were fed on the ordinary-diet of hay, oats, carrots
and bran. During the first 13 days of the tests, the animals received a daily
dose of 25 mg of vitamin C each, this amount 1~eing'increiased up to 100 mg during
the following 8 days. The tests proved that noise stimulation resultedin the
reduction of the ascorbic level in adrenal glands and in a decreased urinary ex-
cretion of vitamin C. This was particularly clearly revealed when the animals
were receiving daily doses of 100 mg of ascorbic acid. It was also found that
the amount of urine excreted'by the test animals over the 4-hour period.deareasecL
There are 4 figures and 2 table.sv
Card 1/2
S/244/63/022
/001/ODI/001
Effects of noise on the... Aoo4/Al26
~'ASSOCIA~IONS:
Vitamin C and P Department (Head Prof. N. S. Yarusova) of the
nauchno-issledovatel'bkiy institut yitaminologii,(Scientific Re-
search Institutel6f Vitaminology); Noi6e and Vibration Labor'atory
(Head - A. A. Arkacl!yevskiy, Candidate of,Medidal Sciences) of.
:Nauehno-issledovafeltskiy institut Siglyeny i sanitarii im. P. F.
Erisman (Scientifi!o Research Institute'of Hygiene and Sanitation
lim. F. P., Erism=)~ Moscow
IAPINA, S.A.; YARUSOVA, N.S.
Effect of vitarnin P on the vitamin C level in human milk.
Vop. pit. 22 no.4:48-52 Jl-Ag 163.
(MIRA 17:10)
1. Iz otdela vitaminov C i P (zav. - prof. N.S. Yarusova)
Goeudarstvennogo nauchno-issledovatellskogo instituta. vita-
minologii. Ministerstva. zdravookhraneniya SSSR, Moskva.
TSEYTINA, A.Ya.; LAFMiA, S.A.
arfect of 4tamin-F (ratin) an the cholestarol 6oitent in the
blood ear= and the level of ascorbic acid-in th& organs of
experimental Animals. Vop. pit. 23 no.1:6749 JTw-F 164.
(MIRA 17&8)
1. Iz laboratorii vitaminov C i F (zav. - prof. N.S. Yarusova)
Naucbno-isaledovatellskogo instituta, vitaminologii Ministerstva
zdravookhrananiya SSSR,, Moskva.
ALIYEV., D.A.; AGAYEVA, Z.G.; LAPINA, S.D.; TAGIYEVA, G.T.
Apparent and bulk densities of petroleum coke. Nefteper. i
neftekhim. no. 3:24-25 164. AMIRA 17:5)
1. Bakinskiy zavod "Neftegaz".
ALIYEV, D.A.; LAPINA, S.D.
Thermal depolymerization of an alkali polymer of pyrolysis production.
Nefteper, I neftekhim. no.7:16-19 164. MRA 17-11)
1, Bakinskiy zavod "Neftegaz".
SULTANOVI 7.f,.; ALIYEV, D.A.; 1-1,Pll,!A, S.D.
ln3--Rsing Lhe reserves of tar, the stc-.e.- i
a.!.hless coke. Nefteper. I reftekh-im.. nr,-IC-25-~7 I f~l, ,
(illfVi 1-7: 12)
1 i
. Baknskiy zavod "lief tegaz".
KOGAN, X. H. S
Activity of a cardiorheumatologiral center for the prevention
and therapy of rhemnatic fever. Terap.arkh- 31 no.7*25-32
J1 159. (HIRK 12:11)
1. Iz gorodekoy klinicheakoy bollnitsy iment N.I.Pirogova,
Moskva.
(RHMJWIC FSVER prevention & control)
LLPINA, S.M. (Moskva)
Luminescence of the urine In cases of cancerous neoplasms.
Klin. med. 35 no-1:118-119 Ja 157 (MT-RA 10:4)
1. Iz propedevtiobaskoy terapevticheskoy kliniki (zav. kafedroy-
chlen-korrespondent AM SSSR prof. V.Kb. Vasilenko) I Moskovskogo
ordena tenina meditainakogo inatituta imeni I.M. Sechenova.
(NEOPLASMS, urine in
luminescence)
GLADKOV, I.A., doktor ekon. nauk; KOSSOY, A.I., kand. ekon. nauk;
VIDONOV, S.S., nauchn. Botr.; SAY-CYLOVA, I.D.., nauclm. sotr.;
GORLWOV, E.P., kand. ekor. nauk; I-IAYEVSKIY, IN., doktor
ekonor. nauk;CHE-BOTAREV,V.A., kand. ekon. nauk; KAMUSHER,
L.N., nauchn. sotr.; STROYEVA, Z.B., nauchn. sotr.; FOMINA,
L.V., nauchn. sotr.; VOROBIYEV, Yu.F., kand. ekon. nauk;
KRAYEV, M.A., doktor ekon. nauk; KAPLINSKIY, Ye.M.., kand.
ekon. nauk; LAP3~4,,JS.,.Ij., nauchn. sotr.; YAKOVTSFVSKIY, V.N.,
kand. ekon. nauk; OHLOV ', B.P.) kand. ekon. nauk; DIKHTYAR,
G.A., doktor ekon. nauk [deceased]; PLOTNIKOV, K.N.j
MALIKOVA, A.I., nauchn. sotr.; TOVI-',OSYAN, M.Ye., red.i7A-va;
POLYAKOVA, T.V., tekhn. red.
[Socialist national econony of the U.S.S.R. in 1933 t4p 191+01
Sotsialisticheskoe narodnoe khoziaistvo SSSR v 1933-1940 gg.
Moskva, Izd-vo AN SSSR, 1963. 665 p. (MIRA 16:12)
1. Akademiya nauk SSSR. Institut ekonomiki. 2. Sektor istorli
narodnogo khozyaystva Instituta ekonomiki All SSSR (for
Stroyeva, Fomina, Kaplinskiy, Lapina). 3. Chlen-korrespondent
All SSSR tfor Plotnikov).
(Russia-Economic conditions)
TSITOVICH, I. K.; LAPINA,. T. A.
Use of cation exchangers In the form of salts for removing
foreign anions in the determination of nitrates. Zhur. VKHO 7
no.5:579-580 162. (MIRA 15:10)
1. Kubanakiy sellskokhozyaystvenW institut.
(Nitrates) (Ion exchange)
TSITOVICH, I.K.; LAPINA, T.A.
State of the trani3itio:, elf-ze-at:j o1' the fourth Period in gul-furic
and phosphoric acid solutions. Izv. vys. ucheb. zav,; khim. i
khim. takh. 6 no.3:370-376 1063. MIRA 16:8)
1. Kubanskiy sellskokhozyayetvennyy institut, kafedra
neorganicheskoy i analiticheskoy khim-ii.
. (Transition metals) (Ion exchangers)
TSITOVICHP I.K.; LAPINA, T.A.; Prinin-2a uchastiye.- NIKITINA, N.G.
Absorption of cations of heavy metals by anion exchangers
from aqueous solutions. Zhur. VKHO-8 no-5:597-598 163.
(MIRA 17:3)
1. Kubanskiy sel'skokhozyaystvennyy institut.
IAPINA, T.V.
Oxidation-reduction regimen in tissues of greenhouse plants during
the year. Nauk. zap. 1yiv. un. 16 no.20:113-119 157 (KIRA 13:3)
(Greenhouse plants) (Oxidases)
(Ascorbic acid)
IAPINAt T.V.
Water balance of tozatoes grown in a greenhouse. Visnyk Xyiv.
un. no.2. Ser.bdLol. nq~ls5q-67 159. (MM 16:4)
(TOMATOES) ' (PIANTS--WATER RE4UIREMENTS)
(GREENHOLIBE PIANTS)
__IAPINA.p T.V. .
Adaptive reaction--of the photosynthetic apparatuB of pUnts to
the decrease in light intensity, Viwqk Kyiv,un. no.j. Ser b1ol.
no.249-54 158. (MM 16;4
(PHOTOSYNTHESIS) (CHLOROPHYLL)
I
LAFIVA.. T.V.
Characteristics of the pigment system in leaves of green-
house tomatoes. Visnyk. J~y~* un, no*4* Ser.bio3.* noo2z
28-33161, '400~__ (MM 16:6)
(CHLOROPHYLL) (TaUTOBS) (OMMMSE PLANTS)
S11151611000100110031007
B129/B201
AUTHORS: Gordov..,A. H.., lzrailov, K. S., Kandybap V. V., Kirenkov,
1. 1., Kovalevskiy, V. A., la ) E. A. Kinkellshtey-nj
A_J__R=3 I
V. Ye.,, and Ergardt, N. N.
TITIZ: Comprehensive metroligical studies for developing methods and
apparatus for exact measurements of high temperatures
FERIODMAL: lzmeritellnaya tekhnika, no. 1, 1961, 22425
TM: The ever-increasing demands made by industry on the accuracy and
range of measurements of high temperatures make it necessary to reorganize
the entire metrological system in the field of measurements of high tempera-
tures and the development of new standard and model devices on the Uasis of
the latest achievements in the construction of precision instruments. In
this connection, fhe VNIIJ4 imeni D. 1. Mendeleyeva and KHGIIaP developed a
program for the performance of comprehensive metrological studies for the
establishment of new stangards and high-precision master instruments for tem-
peratures of up to 10,000 C. This metrological research work was completed
in 1960. The studies were made in four fundamental directions: Thermometry
S11151611000100110031007
B129/B20l
Comprehensive metrological ...
of gases, thermoelectric pyrometry, optical visual pyrometry., objective
pyrometry (photoelectric and radiation pyrometry). Now temperature scales
in the field of high temperatures were established on the basis of new
methods of objective spectropyrometry. The optical pyrometers used for
measuring high temperatures arF not sufficiently accurate* Thus, the admis-
sible error In measurement of the optical pyrometersMiIP(OPPIR) is up to
+ 150C at 1.,0000C.. and up-to 30 C at 210000C. It is evident that this is
Tnsufficient for mny purposes and for scientific research work. In con-
nection with the abofe problem., i.e.., direct temperature measurement of high
accuracy, the optical precision pyrorietersMq -51 (EON51) and-On _h8 (0P-48)
spectropyrometers of the typesOQ-57 (IKP-57) andWK(SPK),, and new optical
devices of the type M (Urp) were developed and introduced. The interna-
tional temperature scale ,n7s used with maximun accuracy for the new instru-
ments at the Vsesoyuznyy nauchno-issledovatellskiy institut metrologii im.
0. 1. Mendeleyeva (All-Union Scientific Research Institute of Metrology
imeni D. 1. Mendeleyev) and at the institutes of the Komitet standartov,
mer I izmeritellnykh priborov (Committee on Standards., Aeasures.,a nd
measuring Instruments) The new pyrometers are widely used or scientific
search work. There ;re 59 references: 49 Soviet-bloc and 9 non-'boviet-
ice.
f
Card? 2,
K4=VKO* V.V.p professor; ZORIN, A.N,; KOROBOVA, T,B.; XRASMININNIKOVA, A,I.;
LAPINA, T.Y.;. SMINOVA, Te.l.;- SUKRACHEY. N.0.; MMUMV, S.B.
[Practical work in general biology for medi oal, schools] Praktikum po
obshchei biologii dlia madvasov. Koskra, Nedgis, 1933- 294 p. (MLHA 7--l)
(Biology)
SHAPIRDt APINA V G
New colorimetric method for -the determination of iron in wine. Vinodelle i
linoj~iiAaiifvo - S O'S.S.Re' 13, No.3, 22-'5 '53. 6: 3)
(CA: 47*-i6.'ft:11651 i33)
l.. Odessa Ned. Inst.
U Is 6 It
J760~ A mew wloftdrie miethod lar Mernflulng
Comm in wine, INL Ya. I.Shlaplm ~Rfl V, C- I-Apina
Wir-Mie f -)!-4-t-47g-F-o7sTto---.ITSYR,~:)Iilgiliilloifii&
'ne Cv in ZL simph.- is ptd.. vith --N aAC~ in the
I H'S04 and Jo ignitcd ppt. is dim4ved
*fr:ktn '61 1~46 .-by* iTtm,
-with Ai. ~41' soln. and tjr filtrate is e~polhtw to
drynefs with DO =j tcatal tov~vkvve animnium
salts; the residne-is dissolved in a definite vol. of
water. 77icCuis-tbrndrierminedc-DIDTirrettically;
tb& yr-How cobnT vbi~ deN t1pps on the additi6z Of
I percent. guniaz]-and.0-6 per cent-aq. Mi. m1n.
iB=eAWUft1.'
the intens3ty of the Colour, is propoitional to 1"t Cu
C=t=t; the coloat Avvelops fully in 25.mia. Tb*
"mction cu Also 1;a md .-W dctort Cu; the vmi-
tiVity 6 004 p& Of C4) jTr r0L Otbtl =04111C
U11sinit'dba. Y-th'y ar~n PreuAlf In axa,~Mvts 300 in
ZARATaUt T.V.; LAPIKAO V.V.; MMUUv -R.A.
Indium distribution in casolteriters, sphalerites and chalcopyrite
from the tin are deposit in Lifudzin. Gookhiniia no.2-.156-161 f6l,
(MIRA 14:3)
1. Daltnevoistoobnyy fi3lal Sibirskogo otdolmiya -a Smt
Vladivostok.
(Lifudziri rbgion-Tin ores)
(Indjum)
LIL?INA$ V. Yu. . . . -.- . .1 . . - I..I .---I . .. I... .'
25482 .LA PINA.V. YU. K voprosu o viiyanii parazitov na dinamiku 191,P-, vyp. 4, B. 329-
34. - Bibliogr: s 334.
30; Letopis' Zhurnal Statey$ No, 30, Moscow, 1948