SCIENTIFIC ABSTRACT VVEDENSKAYA, M.V. - VVEDENSKIY, A.A.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

WEEi-p-l"13KAYA, 11. "1.
VVFF---iE-!:SKAYA., 14. V.; "Deternination of thiacyarzites In thc -arine w~ a metlro~!
of sUxlying the functiorzil state of the liver," Gorlk--*y, 1955. Glorlkiy
4 110 e
.)Late MedicnI Inst imeni S. MI, Kirov. (Disnertation for the Dei,,rCC- of C.-IrAl- t
of Medical Sciences)
paa Letonis' No. 47, 19 Nbvenber 1955. Irbscow.
SO. Lni2~L

VVEDENSKAYA, N.A.; IODKO, V.K#; XONDORSKAYA, N&Vo; LANDYREVAY N-S-;
---"~M=NA, L.A.; SDOW, P.G.; TABULMCH, V.K.
Bulletin of strong earthquakes In the U.S,S.R. In 1960.
Trudy Inst. fiz. Zem. 28 Vop. inzhe seism. no.8:61-76 163.
(MIRA 16:11)

".; DZHAITUZAKOV, K. D.; IODKO, V. K.; KONDORSKAYA, ff. V.;
LANDYREVAJ. N. S.; HISHARINA, L. A.; SULTANOVA, Z. Z.;
TSKWAYA.. A. D.; YURKMCH, 0, 1.
Bunetin of strong earthquakes in the U.S.S.R. in 1959. Trudy
Insto fix, Zeme not.2-2. Vop, insh. seism. no.7:3-24 162.
(MIRA 15tlO)
MmUquakes)

VVEDEIISKAYA, N, A,
General compilation of eeimic otatiotic3l data in oeiomic zoning
of Contral Asia. Trudy Inst. fiz. Zem. no.22. Vop. inzh. oeism.
no.7:25-45 -162. (MIRA 15:10)
(Soviet Central Aoia-Seiamology)

S/16 62/000/003/005/098
D228%)301
AUTHOR: Vvedenskaya, IT.A.
TITLE: ~The question of using instrumental data on strong Cen-
tral Asian earthquakes in seismic zoning
PERIODICAL:' Referativnyy zhurnal, Geofizika, no. 3, 1962, 13, ab-
stract 3A119 (Tr. In-ta fiz. Zemli, AN SSSR, no. 17
JsI7, 1961, 119-127)
TEXT: A method'is proposed for construction of theoretical earth-
quake isoscismals from the value of magnitude 14 with an account of
the regional geologic structure. A map is constructed for,the iso-
seisnals of Central Asian earthquakes with M,~4 1/2. It is s1rd%rni
that the character of the disposition of the force isoseismals de-
pends not only on the-focal depth, but also on the peculiarities
of thexegional g6ologic structure. /-Abstracter's note: Complete
tranalation,-7
Card 1/1

8151Y601000100810041031
D051 D113
AUT11ORt' Vvedenukayaq N.A.
TITLE: Contribution to the question of using data on micro-earthquakes
for problems of seismic zoning
SOURCEi Kkademiya nauk SSSR. Sovet po, soysmologii. Byulleten" no. 8,
Moscowq 1960.' Voprosy seyamicheskogo eayonirovainiya',3 60-66
TEXTs The author discusses the possibility of using data on observations of
micro-earthquakes for seismic zoning purposes. Ad tLis possibility depends
on the large-scale study of the complicated and varied association between
strong-iLnd-micro-earthqaakeel.it,.io stated that at present only very general
regularities' cin."~e discussed. -On a regional-basis the author describes
this association with respect to Central-Aoia, us*ng for this purpose graphs
and maps showing the epicenters of earthquakes and changes In seiomic acti-
vity foryarious 'se-ismically active zones.. An analysis of one of the maps
shows that areas where seismic activity is relatively more stable are char-
acterized by an increased number of micro-earthquakes. On the basis of an
analysis of -observations of mIcro-earthquaken in Central Asia for the 1950-
Card 1/2

S/5l9j6O/OOO/OO8/OO4/031
Contribution to the question... D051/D113
56 periodt it can be said that in areas where strong earthquakes previously
oaourred or occur tit present, the frequency of micro-earthquakes is relative-
ly higber. "Increatied technical 'accuracy has made.-more accurate the delinea-
tion of' seismic zones prone to strong earthquakes. Stationary seismic eta-
tiohs.aan be used for zones of stable as 'ismio,activity, highly-sensitive ones..~~
for unotable zones. 'The former can.be used for determining the epicenters
of'earthquakes with an error of only 15-20 km and observations made from
these stations car. be used for compiling 115#000,000 seismic ioning maps*
Observations of highly-sensitive stations can be used for larger scale seis-
mic =ing maps* The author discusses in detail the possIbility of using ob-
servations of micro-earthquakes for determining the recurrence of strong
earthquakes and the maximum intensity of individual,areas,'stating that still
more data is necessary for this possibility to be realized. The data of
these-observatione, however, coupled with geological datap can be success-
fully used for tbe delineation of individual oeismically-active zones. A.A.
Fogel' and I.V. Gorbunova are mentioned in connection with the compilation
of a seismic map. There are 5 figures and 2 Soviet-bloc references,
ASSOCIATION: Inutitut fiziki Zemli AN SSSR (Institute of Physics of the
Earth of the AS USSR)
Card 2/2

S/261g/64/000/033/0124/0143
.,ACCESSION NR; A14045972
',AUTHOR: Vvedenskayi~j Dzhanuzakov, K. D.; lodko, V. K.1 Kondorskaye, N. va;
Irk.'( -i J
rfavgdln~lclg; ~!s~prlnq, L. A.; ~natsakanyan, 0# K.; Ragimov. Sh. S.; Semenov,
G.
;-TITLE:' 13yulleten' sIPWIth',zemletryasenly SSSR (Bulletin of the Strong Earth-
quakes of the SSSR) for 1961
!SOURCE: AN SSSR. Institut fl;lki Zemll. Trudy*, no..33(200),'1964, Vopros
12 -1 3
~~inzhenernoy seysmologil'i (Problr-ms of earthquake engineering), no. 9 4
"TOPIC TACS: geophysics, selsm.4~,logy, earthquake, earthquake focus, earthquake
epicentet Ity seismicity
earthquake Intens
ABSTRACT: The " Bu I I et I n of the'Strong Earthquakes of the SSSW Is a periodic
annual summary which simultaneously summarizes all fnstrumental and noninstrumen-
tal data on the strong earthquakes (Ii > 4) occurring In the Soviet Unlon.The Dilletin
~-.contalns a catalogue of earthquakes (r~_eproduced In the paper for 1961 In the form
;:,of a lengthy table), a map of the epicenters and a brief description of the stron94
est earthquakes.-The catalogue Includes Instrumental data on the coordinates of
the epIcenter, focal depth, magnitude M and the time of occurrence of earthquakes,
taken from the Byulleten' setl seysmichesklkh . stantsh, SSSR (Bulletin of the Net-
~qoj~ %f Seismic Stations of the SSSR) arid,nonlnstrumentat data Information on
Car
r
mown

ACCESSION NR: AT4o45972
the sen5ed Intensity of earthquakes, received from reports submitted by local in-'
habitants or from Investigations devoted to descriptions of the strongest earth-
quakes. With the exception of the Kurile:-Kamchatka zone, In the catalogue there
are data for all earthquakes with M >,4, and all earthquakes for which K was not
determined but which were recorded t;y- seismic stations of the general type.as'.
having epicentral distances greater than 1,000 km. Data for the Kurile-Kamchatka
Include all earthquakes with H > 5'. A map Is presented In the pape'r which
zone
shows the location of the epicenters7of the earthquakes listed In the catalogue;
_.,~_numbers on the map correspond to the numerical listing In the catalogue. In 1961
there ware 272 earthquakes in the SSSR with M > 4. Their distribution by regions
and Intensitl is tabulated in the original t-ext. Fig. I of the Enclosure shows
the value Y, ETh for Individual seismically active zones of the SSSR for 1961,
computed using the formula-19 E .-1).8 + 1.5 M. Fig. 2 of the EnWsure shows the.
'o_change with time of the deviation from the mean annual-volue'p, El 2 for four sels-'
micaW actlveoone!;. Along thi y-axis of the graph there i~ plotted the valuT
ME - (2 E ZYnean and along the x-axis - time (1946-1961)., The value (E
mean for each zone Is Indicated at the right of the graph., The authors go on to-
describe briefly, but Individually, the most Important seismic phenomena occurring,
In various regions oaf the SSSR In 1961. The annual publication of the Bulletin
was begun in 1956 and until 1961 It was printed In the Trudy* Instituta FIzikI
SSSR In the collection of articles Voprosy Inzhenernoy seysmologil
C1, cro I 1 4 r

ACCESSION NR-. AT4o4!;972
(Problems of Earthquake Engineering). Beginning with the Bulletin for 1962, the
report will be published In annual numbers of Zemletryaseniyp SSSR, which will be
a separate publication. Orig. art. has: 11 figures and 1-table.
ASSOCIATION: Insti.t.ut fIzIkI-ZemII AN SSSR (institute of-Phylles of'the Earth,
AN - SSSR)
SUBMITUD: 00 ENCU 03 SUB'CODE., ES
NO REF SOV: 004
.OTHER: OaO
Card 3/6

ENCLOSUREI 02
ACCESSION NI,: AT4045972 Flg. 2.
ova if~jv ""Pi
210
0. ljJ

/if
It-

R
RE

card

ACCUSION IfEt I AT045972 ZNCLOSUREj 03
Continuation of Fig. 2.

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opt

0
8 N a
h
Apo

,Erl/2
Change In JEI/2
an with
) An
time 1946.1961,: 'a'- Far East; b

Central Afla; c m
Eaucasus;
,cl- Baykal.
card 6/6

VVEDIENSIK,AYA, 11. A.
N. A. --- "Investir,,,tion of the Plutanic of
Central Asia." Sub 11 Jun.52,, Geop~rynics Innt, Acpd ~Sci lj=to
a i c mna t, i cmn t i ca I
(Dis-,, crta Lion for the Dof-rec of Cnndid-,ite -in Phy
Scicnces).
, - Vech(!rzinya Elos Janunry-Deccmber 19"2
50. kvn

VV V4 P_w ?" A Y A, V1. A "
USSR/aeophysice Seismology FD-11
Card 1/1 Pub..45-1/8
-Author Vvedenskaya, N. A,
Title t Procedures and results of generalization of the observations by
the uetvork of stationary seismic stations in Central Asia, 1950-53
Periodical t Izv. AN SSSR, ser. geofiz., No 6, 1954, pp 497-514
Abstract The author gives an account of observations of Central Asian seismic
stations. Using charts of epicenters she draws a conclusion about a
definite relationship between the distribution of earthquake centers
and the geological structure of a region. Establishes a dependence
in the distribution of centers of mild and severe earthquakes.
Institution : Gecphysics Institute, Acad. Sci. USSR
Submitted : May 4, '15954

USBR/Physics of the Earth - Seismoloa, 0-3
Abot Zcurnalg Referat Zhur - Fizika, No 12, 19561 36361
Authors Vvedenskaya, H. A.
Institutions None
'title: Concerning the Accl=acy of Determining the Position of the Focus
of an Earthquake Uning the Method of Intersections
Original
FeriodIcal: Tr..Gt3ofiz. in-ta .411 SSSHj 1955o No 30, 127-136
Abstracts A solution is obtained for the problem of estimating the accuracy
of determination of the foci of earthquakes using intersections de-
pending on the accuracy of reading the time difference in the ar-
rival of the longitudinal (P) and tranevereo (8) waves and the
relative positions of the stations. To derive the initial calcula-
tion equations, the method of the time fields Is used with the
followtug assumptiores the hodograph empl*yed is assumed accuratei
the idiamtification of the waves was correetly madej the medium
has a 3-layer composition -- granite, basalt., and ultrabasalt,
Card V3

USM/PlVsics of the Earth - Issionoloa.. 0-3
Abst Jcn=a1z Referat Zhur - Fizika, No 12, 1956, 36361
Abstract: with horizontal separation boundarieaj the propagation velocities
of the waves and the thicknesses of the layers used are in ac-
cardance with the data of Ye. A. Rozova for central Asiaj the
speed is assusted to vary linearly with depth in the ultrabaoalt.
For the majority of seismic statione, the error in the determina-
tion of the time t. - tp is approximately 41 sec. For earthquakes
with normal depth of focuB the accuracy of determining t1te position
of the epicenter and of the deptliof focus is greatest when Using
tbi difference tff - tp . The egcenter can also be sufficiently
accurately determined By Using ts* - tpi, but then considerable
errors are possiblo in the determtoatirm of the depth. When de-
termining the position of the epicenter of a deep earthquake, when
the time difference of the arrival of the "direct" waves P and S
Is used, It Is necessary to assign greater veight to the observa-
tions frcm relatively remote stationo., while observations of nearby
stations are emphasized in the determination of the depth of fQCus.
As t1uy number of stations is Increased, the observations of which
are uned, the errors in the determination of the position of the
focus diminish. Calculatioms have shown that undAr the most
Card 2/3

USSR/Pbysics of the Faarth - Seismology,, 0-3
Abst Jornmal: Referat Zhur - Fizika, No 12, 1956, 36361
Abstract: favorable placement of BtAtione located from 100 to 1,000 km avay
from the epicenter., t7he position of the epicenter can be determined
in the best case with ~b accurac of �10 km. In practically moot
cases the error is greater than 110 km and in :Lndividual*casee it
reaches 40-50 km. In the compilation of the maps of epicenters it
~s therefore necessary to estimate at least approximately the ac-
curacy of the deteinination of thepoidtion of the foci, since
othervise it will be difficult to conclude whether the particular
foci'of -the earthquakes belong to any definite geological struc-
tures.
Card 3/3

fVS I< A Yn.) N. A,
USSR/PJjyeics of the 4arth - Seismology, 0-3
Abst Joramalt Refazut Zhur - FizLka, No 12, J-56, 36363
Authors Vvedenskaya, N. A.
Institutico: None
Title: Concerning Reporting the Observations of the Stationary Seismics
stationfefof central As�a
Or:4;inal
Perio~ticals Tr. Geofiz. in-ts, AN BSSRY 1955, No 30, 137-141
Abstract: A description of the procedure for determining the foci of earth-
quakes vhen ccwpiling the bulletin of the stationary seismic stations
of Central Asia. 1%4--plotting of the epicenter maps -- the second
stage in theproceosing of the observations -- was discussed by the
author earlier (Referat Zhur - Fizikaj 1955, 18124). Tm Central Asia,
the Ustance between stations and epicenters does not exceed 600 km,
and u3uaUy is not less than 100 km. For these conditions it is
most :rational to determine the epicenters using the hyperbola or
interaection methods (based on the use of the hodograph). The methcd
Card 1/h,

USSIt/Phyoice of tbAl EGrth - Beiazolov, 0-3
Abst journal: Reforat Zhur - Fizika., No 12, 1956., 36363
Abatract: of Intersection makes it possible to employ simultaneously ob-
servations frcm nearby and remote stations; its principal short-
coming Is the ne&I for study of the vayes of various types and
this means that V; is neceoeary to employ for all of Central
Asia one average hodograph (although the hodographs differ for
different epioevtTal regions). The waves that are the most de-
penclably identifi-nd are the F and T, or P and 9 at epi7central
distamces A. that are less than 170 km. Th6 travel times of the
and F waves are Wependent of the thickness of the earth's
crust and at A < 5d they depend little on the depth of the
foew, if the latter is lc~cated witb.Ln the earth's crust. Hodo-
graplas of F and Uwayes in different regions diffe ittle from
each other. This makes it possible to emplo, lerences the
obSW-VatiOnS of stations at A< 170 J= (the difference in travel
tine is less than 2 seconds). The dependable element of the
hodoipraph of Central Asia is the appeaent velocity of the P wave
(718-8-1 kolsec), diffracted by the lower surface of the earth's
,A*Ust. and arriving first at A > 200-250 km. Using the Instants
aT-vt'dch the P waves arTive at A*7 200 km, It is possible to
Card 2/4

USSR/Plwbics of the Earth - Sei8#409Y) 0-3
Abst Jciurnal: Referat Zhur - F12:�ka, No 12,-1956, 3063
Abstract: detexmine the epicenter by usljje,.-1~4e hyperbola method. Errors
causi!& by inaccurate knovledgem*t'th) velocity in the granite
laye:7 (from 5.5 Vr 6.0 IM/sec) vill. be insignificant. If one
employs observati'O'Ds of stations in which the times of arrival
of the first waves are close to each other, but which are lo-
cated an the opposite sides of the epicenter, and if the speed
Is tALken to be 5.8 kmisec. Under conditions prevailing in Central
Asia it is advantaf .eoiis to employ methods based on the assumption
that the hodograph'is a straight lina. The determi ation of the
depth of the focw of tha earthquake using the Vadati method is
possible mly for the small region in northern Tien Shan. The
use of waves of the type pP,, BP, and oS is possible in rare cases.
It Is. therefore possible to employ in practical cases only the
methcd of intersectips, which requires a knowledge of the exoct
W4*ra;hs for various depths of focvs. Tha depth is determined
with relative accuracy only for foci under the 6arth's crust. In
the presence of an FAve-mged hodograpb. for aU of Central Asia, it
is necessary to confine oneself to an approximate estimate of the
depth of focus. In the conclusion the author speaks of the
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USSR/Physics of the Earth - Seismology, C-L
Abst, Journal; Refetrat Zhur - Fizika, no 12, i956o 36363
Abstract: incompleteness of the datafgiven in the bulletins, and expresses
ideas concerning the trendb3 of development of more accurate
metbods for detennining the coordinates of the focus.
card 4/4

VVIDINIZLYA."..
Isolating the wave sP in records representing deep-seated earth-
,quokos in Central Asia. Trudy Goofiz.inst. no.36:25-34 056.
- (HLRA 9:8)
(S-oviet Central Asia--Seismometry)

SOVI 49 -58-11-13/18
AUTHOR: Vvedenskaya., N. A,.
TITILE, RdiationiW.-P 1xi Time, tht., Yae-atlane In Sidsszl,~ Ac-tivity
of Neighbouring Epicentric Regions (0 svyazi vo
vremeni mezhdu izmeneniyem. seysmicheskoy aktivnosti blizko
raspcilozhennykh epitsentral'nykh zon)
PERIODICAL: I:zvestiya Akademii Nauk SSSR.. Seriya Geofizicheskaya,
1958, Nr 11, PP 1394-1398 and 2 inserts (USSR)
AB,13TRACT: In order to establish a relationship between time and
variations of seismic activities in various epicentric
regions, an analysis of the earthquakes in Central Asia was
made between 1950 and 1955,, Six regions of the highest
activity were chogen (Fig.l) for which graphB were prepared,
showIng the total en6rgy of elastic. waves and the nuiebor of
ea.rt:aquakes oc^--,xr-ring in theoe regions during that time
(Fig~2)~ The graphs weTe based on the logarithmic, scale
acco.rding to the formula .1og 1-3 - 3.0 +- 1,7 M where E -
energy in ergs,, M - intensity, From all the selected
regions. only region IT was found to be suitable for detailed,
It was divided Into two areas (A and B in
investigatiq)i
Fig,l) and cumulat.ive graphs of the r-!Iastio wave energy
were made fo-r each of them, This type of graph is very
Card 1/4 useful but does not always give an exact picture. Therefore,

SOV/ 49-58,--11--13/18
MAbionship in I'Lua 11,;Avitu *1
of NeighbourJ-ng Epicentrie Region-o
both logarithmic and cumulative graphs were considered, The
analysis of graphs for two areas showed clearly that an in-
crease of seismic energy o-11 one ,,aused a decrease of the
other-, These examples are indicated in Fig,.3 by the arrows.
In order to define the relationship between the variations of
seismic activities in thA, differeat nreas situated still
nearer each other, a detailed analysis was made for the Garm
region. This region showed relatively high seismic activity
in 1930 to 1955,, with t-1-he epicenUres positioned more exactly,,
Fig.4 shows the map of tht% Garm region where the distribution
of the epicentres of weak eart'hquakes (M - 39 3.5 and 4) is
indicated together with the stronger earthquakes marked in
points. Based on this dis-tribution, four areas were distin-
guished which., duzing 1950-1955, ahowed the highest seismic
activity (Fig'4). The aharacter of variations for each of
these areas i; shown in Fig.,5.. whi~ch was prepared, taking
into account all the earthquakes of M.:1~3, It can be seen
Card 2/4

SUVI 4 ~~-58-11-13/18
Ri1%ti=9h1.p in Time tgWts-i-_t the in-StImde Aitivity crf
11,tai,eibexaring Epicentrie. RetlozA
from thisgraph that an Increase of seismic activity in one
area causes a decrease in the neighbouring areas. These
cases are indicated in Fig.5 as dotted lines, In some iso-
lated. cases where this relationship did not occur the ex-
plana.tion could be found in the special geological structure.
It WELS found that a generalisation. could be made that an
increase of activity of one epicentre always causes a de-
creaEie of others situated not further than 200-300 km away,
This did not apply to the strong earthquakes which only
caused some delay in. the accumulation of tension in the ad-
jacent areas. In order to verJ17 the result -s obtained., the
period of 1927-a'.949 for Central. Asia was investigated; but
due to the inadoquate observations during that period, a
detailed analysia could not be made, However, the
Card 3/4

SOVI 4'9-58-11-13/18
A'alAicraship in TU4
Vsjghb6ui1n9 Epit6ntric Rajdcn-v
inventigation did not contradict the results obtained for
the period 1950-1955~ There are 5 figures and no references.
ASSOCIATION: Akademiya nauk SSSP., Institute fiziki Zemli (Acad6M7 Of
Sciences USSR, Institute of Physics of the Earth)
SUBMITTED: June 26, 1957.
Cwrd 4/4

Vy~,D~F IODKO, II.K.; KONDORSKAYA, !,,'.V.;
L.A. ; flNATl;',AFJ-NYA.N) D.11,1. ; RAGINW, 5h.S.;
SM-171NOV, P.G.; T13,'LLVIC 7.11.
Bulle~ht ot powerful earLhouakes in tile U.S.S.R. during 1961.
.1rudy In:,L. fiz. Zc-m. no,33. Vop. irz~a. sci!jrn. no.9:121~-143

W= otv. red.; KOIIDORSKAYA, N.11. j, otv. rod.
(Earthquakes in the U.S.S.F. in 19621 Ze=letriaseniia v
SSSR r 1962 godu, Moskva, Nauka., 1964. 153 p.
(MJRA 18.-6)

IT-MGOV-r-PN. [V"iuhov,, P.M.); GONCHAROV, K.S. bloncharov, K.S.1;
M.23;,Tiyp V.S.
Man~facturingo(- and p-sources for the graduation of dosi-
metric apparatus. Lllc~. fiz. zhur. 6 no.2t284 Mr-4p 161.
(IORA 14.6)
1. Fl.ziko-tekhnichoskiy institut AN TISSR.
Alpba rayl) I
~
Beta rays suroment)
(Radiation-Mea

S/619/61/000/017/001/002
B' 239/D302
AUTHORS: Medvedev, S.V., Bune, V.I.9 Viredenakaya, N.A., Gay8kiy,
V.N. Kirillova, I.V., Nerses~_,T,_f--L., Rii-A-1-c-henko,
Yu.1f.2. Savarenskiyj B.F. and SOrBkiy, il.A.
TITLEs Instructions for regional seil=0106iCal summaries
SOURCB8 Akademi a nauk SSSR. Institut fiziki Z.emli. Trudy no.
17 (1M Moscow 1961. Voprosy inzhenernoy seysmologii
no. 5, 128-145
TEXT: These instructions were confirmed by the director of the
Institute of Geophysics AN SSSR, M.A. Sadovskiy, on Pebruary 27,
1961. Their objective is clearly to secure a uniform system of
recording all seismological data pertinent to building construc-
tion, obtained in future in the USSR. The instructions are divi-
ded into six parts, containing 64 numbered articles, the follow.-
ing being an indication of the scope of each part: 1) General
Card 113

Instructions for regional ... S/619/61/000/017/001/002
Section. This defines the purpose and scope of the work. The
seismological map of the USSR established in 1957 is being kept
up to date by continuing observations. Its scale is 1 1 5.000,000.
The maD is tc be used to make seiaiaolo6ical forecasts both for
the epi-central zone and for the whole earth's surface. 2) Instru-
mental data on earthquakes. This is defined as data obtained
now from both fixed and expeditionary stations as opposed to the
study of past earthquakes. Uethods of olassification by magnitude,
precision of epicentral location and frequency of recurrence
are defined. 3) Engineering seiBmology. Under this heading is
defined the format of an atlas of strong earthquake with isoseis-
mals. This should be on a scale of lt 1,000,000. It is alao
hoped. to include data on. the energy density distribution of the
frequency spectra. 4) Seismogeological data. Since some regulari-
ty is discernible in the distribution of shocks, a 11seismotek-
tonic" map should be a possibility. This would be particularly
helpful in regions where seismological data up to this time are
Card 2/3

S/6191'61/000/017/001/002
Instructions for regional vo. D2394)302
Bpa,ose. Gravitational data could also be useful here. 5) Proce-
dtires f or mak".ng seismological summary rjaps and their dccumen-.
-vation. These'are to be of two types, corresponding to 1 and 3.
above., i.e. seismological maps and maps of iscseismals shcNing
energy and attenuation ohara~.;teristics of the region. The way
in which thesi:,, should be prepared is described in considerable
detail, togetiaer with some guidance about what is envisaged for
the seismolektonic maps. 6) Arrangem,ent, duration of -and parti-
r;ipants inlhs fulfilmant of the project. The names and addres-
ses of the participating institutions for each reGion are
0'4venrthe end of the first term will be at the -end of 1962.
The map is expected from the AN SSSR (AS USSR) in 1963. There
are 60 Soiiet-bloc referenceo
Ca:-d 3/3

lit
'a go
P. 'o
.48
A

VVIMSMYL-ILA.; KOMRSKAYA, N.V.
Bulletin of strong earthquakes recorded in the U.S.S.R. in
1956. Trud~r Inst.fiz.zem. no.5:3-19 139.
(MIR& 13; 6)
(lbrthquakes)

vv=HN3xkuo _-HAKO
Time relation of changes in the seiaxic activit7 of near epicentral
zones. Izv.AN SS67R.Ser.goofiz. no.11:1394-1398 K 158.
.(MIRA 11:12)
lo-LO SSSRjInatitut fiziki Zemli.
(BarthcpuLkes)
I

UMNSKAYS, N.A.; YOGILI,-A.A. [deceased]
I Kap shoving the epicenters of northern Tien Shan. Blul. Sov. po
seis-m. no*3:106-117 157. (MIRA 11:5)
(Tien Shan-Seismology-4taps)

Vil,65,01F,P5k4M *A.
49-58-2-7/18
AUTHOR: Predenskaya IT.A.
TIM: On Utilising Observations with Instruments of Weak- Earth-
quakes during Seismic Zoning (Ob ispolIzovanii instrmmer-
tal'ny1ch nablyudeniy nad slabyrii zemletryaseniyami pri
seysmicheskom rayonirovanii)
PERIODICAL: Izvestiya Alcademii Nauk S3SR, Sariya Goof
19513, Nr 2, pp.210-224 (USSR)
ABSTRACT: On the basis of analysis of observations of turbulent
seia-mic stations of earthquakos in Central Asia between
1950 and 1955 an attempt is made to establish the relation
between the distribution of tremors of weak and stronn-
ear-,;hquakes and to solve the problem on the possibilitly of
utilising the territorial distribution of weak earthquakes
in i3eismic zoning. Analysis of this data as well as the
data ol stron--er earthquakes during earlier periods ---?Id of
results Published by other Soviet authors leads to tne con-
clusion that -there is a territorial linlk be-tween t'he dis-
triloution of t'he Loei of weak earthqualces during recent
yea:cs wit-h the distribution of foci of stronG, earthquakos
u
ove:r lon-ar -oeoiods. This pe:vmits utilising datua collect-ed
Card 1/2

V FE D F_ IVS K P3
60-36-3110
AUTHOR: Vvedenskaya, N. A.
TITLE: Separation of sF Waves in the.Recordings of Deep Earth-
quakes in Central Asia (Vydeleniye volny oF na'zapisyakh
glubokikh zemletryaseniy Sredney Azii)
PERIODICAL: Trudy Geofizicheskogo institutal AN SSSR, 1956, Nr 36,
pp. 25-34 (USSR)
ABSTRACT: The author discusses the isolation of a reflected-
diffracted sP wave in the recordings of deep earthquakes
with small epicentral distances, and shows the possibil-
ity and expediency of using an sP wave in determining
the depth of an earthquake focus. D. P. Kirnos' apparatus
was used in Interpreting the kinetic and dynamic charac-
terlstics of waves. There are 7 figures, 1 table, and 6
references of which 5 are Russian and 1 English.
AVAILABLE: Library of Congress
Card 1/1

IVVVNNSKAYA, N. A.
Usitig the data of waak earthquakes Ln probleas associated witb
the establishment of seismic regiont. Biul, Sov. po saiRm.
no.8:60766 160. (MIRA 13:10)
1. Institut fiziki Zemli AN 3SSR,
(seismology)

USSR*&thematics - Pedagogyo Olympiad Jal/Aug 52
"Mthematical Life in the.USSR-. 14th Moscow
School Mathematical Olympiad," B. N. Delone, X. D.
Vvedenskays.
"Uspekh Matemat Wauk" Vol vn, No 4 (50), Pp 180-
184
'April 51 the Yoscov.Msth Soc together with the
Moscow State U and Moscow City Div of Pub Educ con
ducted.sub~ect olympiad of students of middle
schools in Moscow (7-10 classes). Lectures were
'heard from: Prof kus'h^-irhp Act Mem,
Acad.Ped Sci FWSRI Prof V. A. Yefremovich; Prof
225T69
Kosmq~~Mldy, Corr Mem., A2~~dt_Sci;
Prof A. P. Yusbkevich; A. A.'Xronrod, Dr. Phys-
Math Sci; Prof_!._,.Q_Ge3_itota, Corr Mem, -Acad-Sci
WM; Prof P. X. Rashevskly; Prof A. Ta. Xhinchin,
Corr Mei., Acaa Sci USSR; Prof Ya. S. Dubno'v; Prof
A _'M. Lopshits; Prbf L. A. Lyustec-nik, Corr Mem
A;ad Sci USSR; Prof A. G. Kurosb,, Prof V. V. Nemy-
takiy; Prof P. S. Aleksandrov, Corr Mem,_Acad_Sci_
M-;,. Prof A-.-T-. 7h, Act'iiem, Acad-re&
Acij~; pl~Ci-iim_13ii of docents and csndidates~
Zzemples of problems given the students are shown.
Statistical results of solns.broken down by clas-
ses of students.
2=69

UM/Mathematico Elliptic Equations 1 Aug 53
"A-Boundar'y-Value.Problem for Elliptic Equations That
Degenerate on the Boundary of the Region," D.
Vvedenskaya
DAB*SSSR,, Vol 91, No 4., PP 711-714
-Acknowledges guidance.of her teacher 0. A. Oleynik.
.Zab&blishes theorems,on tbO existen-ze) continuity
and boundednees of the solutions to the foliowing eqs:
L (u) ymu~,~uvv+au ibu tcu z 0, L-,Jul M Y% +u 4
jbu +cu = 0 ;,Witg the, boundary conditionsyll-Uff=
a
U'~~"'Au- f (x,y) on G, u(x,O) F(x) on-,-/G/(Pi) ; here
V
272T64
&,btc-,A are functio'ni.of x,y and uV 5.s the derivative
alone-, 'the. direction, Y(Xy).. ttesentud by Acad 1. 0.
PiArevokly 6 Jun 53.

1461 nL~jjA
Mathematics - Comp)titions - Moscow
Fifteenth mathematical olympics for schools in Moscow. Usp. mat& nauk 7 no- 4, 1952.
q

RASIMVSKIT, P.E.; VVZIENSWA* N.D.; KOROLIE7, B.H.
I?if teenth mathematical ol~vplad for t1ut schools of Moscow. Usp.mat.zauk.
8 no.4:,193-197 Jl-~Ag 053. jMLRA 6-8)
(Moscow-Kathematics) (MathematicB-Moscow)

0t T tepon.
;0
9 l
14 (1953).

"alpnj~ pf the fw-n
au , gill

, AU,+&(Z. Or Y)U -0.
Y :;+~ +C(r
!
-C
-q 4" ay

+ - Ou, +6(r. Y4 , 4-C It viti - Cl.
-I,
are -oi-~ sid.. rril m a doinain D in the ialf -plane y > 6. l*hr
voeffi,tevtf ar,~ a-&, cm~ I art A I yric tvi h -.6 0. m > Gj The
,+)~~,-d , ar, ~tfi f-rm ng oic 6,)ujidar, ( D are ii"-urred to
-(insist ~f -vrrwww t,t ,he x axis and ertm. arcs r In the
tipper i\all ~diztne .-ti~hug on thew selments. For such a
10main the boundiLry (riAlitions

A Y Y) F.

f
w)-,rc , H A d!r(-x LIW~ makrng ~111 aCtite an Cie With thO InteflOr
f,~---Tiai to r A 90, and Max (A (9, y)--C(x, y)) v Is similar to the behavior of dg/dO. The posai-
bility of smooth solutions An.the whole range 0 s 3 s 2v is questioned. The nature
of a singularity of the solutions obtained for the windward side of the cone-at
--0 - w is -analyzed W:-.- Orig 0 arto-haer 3 figures-O 12 - formulas and 1 table.- ____ -[All]
SUB CODE:- 20/ SUM DATE: -28Dec64/ ORIC REP:~ 003/ OTH REP: 003/, ATD-PRESS:
4
-1--card ___'2/2
7- 1~
M-M

SOURCE CODE: UR/0421/66/000/005/0036/0040
AUTHOR: Vvedeaskaya, N. D. (Moscow)
ORGI&
TITLE: A note on three-dimensional laminar boundary layer on a blunt body
SOURCE: AN 888R. Izvestiya. Mekhanika zhidkosti I galas nof 59 1966, 36-ho
TOPXC TAGSs supersonic aerodynodas, laminar boundw7 layers'Navier stokes equations
Prandtl boundary layer, ideal gas flow I .44iA1rVmc1
deal
'ABSTRACT. Prandtl's laminar boundary laye In a stesAy suRersonic flov of an I
gad'past a blunt-nosed con at an angle or attack is considered in order to elucidate
the behavior of the solutions of three-dimensional Prandtl equations. The eqiations
are derived on the assumption that all flow paelameters in the boundary layer change
slowly in directions tangential to the surfaceVof thet body. Thus, the existence of
discontinuities in thi solutions of Prana=s equations points to the fact that those
equations do not ade9justely describe the flow in the whole boundary layer. The solu-
tion is sought by a Vinite-difference method. The pticuliarities of the solutions for
the lea side of the balf-plane 0.- w, where 0 Is the angular coordinate, are Investi-
gated. The results of numerical calculations of the flow past a-spherically blunted'
I C"d 1/2

scone at X 4, To n 3000 m const, 200, a - 50, wid~Cp 0.014 Lre given. graphs
and discussed., Orig. ixt. has: 5 figures and 8fontulas.
.SUB CODE-v 20/ SWX DAM 28Fab66/ ORI(; P"I 005

VVEDENSKAYAI N. N.
.1 "Application of the ?,(,ethcd of the End Differences for the Ccnstructi(;-n !:...P
Generalized Solut:Lon5 of Nonlinear Equations."
dissertation defended for the degree of Cand. of Phys-Math. Scl. at the Inst. of
Mathematics im V. A. Steklov.,
Defense of Dissertations (Jan-jul 1957)
Section of IIhynIc%1 Math. Scl,
Vest. AN SSSR, v. 27, No. 12, 1957, pp. 108-9

VVEDENSKAYAO N. P.
Cand. Tech... Sci.
Dissertation; "Experimental Investigation of the Process of Yfichining
Splined Shafts with Hob Cutters of Various Types."
3 Oct. 49
Moscow Order of Labor Red Banner Higher Technical School
imeni 11. E. Br~ujran
v
so m0
S U Yn 7 1

KLOKOV, V. G. , VVEDE-MMAYA, IT, P,
"The Formation of Re" Side Ant,,Ies In Villinp Slotting Toolso. Stanki I Instrumont, 10,
No.. 7, 1939, 1-floscow Tool Plant, Znrinear.
Report U-1505. 4 Oct 1951-

3/563/62/000/00.~1/004/004
DC41/1)113
L.X., and Vvedenskayat N.P. Candidates of Technical
Sharnenint, and honinr of tools provided with hard-alloy plates
diaTond wheels
usin,f,
;-..T., C." Gosulartvenn777 I-o-Itot Zovettt IUnintrov SSSR no ai, -.o:natizatqiJ.
i 'V.,3.esoyuznyy nauchno-insledlovatellskiy
in.itrument:-I-nyy institut. Moscow, Mapbrizo 1961. o va Y.:
tekhnolo,,.jy-A izp-ofovIeniya Instrumenta, 131-139
T.-. -he -ontains thf, rest,,lts of invertip-ationi carr~~Pd f;u~ b VNII
Y
ri"n, di'-)r1ovid whe~!Ia manuracturei at Uf-li.Ch3kiy cha~7ovoy ltavnd (Uplich
Clock Plant) and NITalma7. 11,~ Well az nn qnaly:-,iz of non-Ooviet e ta on dia-
mon,! -hoels. Thie purpo3e of the study w:ti to obtair. the optimur workin7 con_
ditions anl -r!(IUi.TIInc.-nt r-quirc-montn for r%tionally usini- diamond and
to devolop a pro,-rpm "or f,. s(,r.,i-aijtvatIc machint. slisrp-n-
Card 1/4

4'
Sharp(min and honing of 0 /D!13
inf- and honinr cmttsr~,, nrovidi~d vrl~th hard-alln- pl%tes by -f-ann of diamord
wheels. Diamond -xni7eln vilth thr, i~rit sizes -re recomnerided by th4?
NIIalma~. 08-39-1-57 nor,-. 'or honinr tools with hay~-!Mcy
,~ , C. k (I
M-10 /v;4 )4~28 (-M?O)j fJ14 (IM14), and P110
(V10); -ftheeln with FrIt s.Lzes of 150 i-nd 2.~G -1hould b,~ used for ~,n
- - -~r rAD-r -~nll
8-gtb clas3 finirh Its i, 2769-5~' (GOST 2789-59), M40, M2---,~,
I VLF I
M14 for ',--llth finish ant]. VAO for 12-13th clans finish. V31! lin-i C;-
.aine-d .. finish of VIO vrith wheels havin:- grit ni7.ei of 100 and I'io, -7 -1
follovir!j,v diamond conrertration valal-r, ii-avr, been accepted in induttrial
prac-I ice:a 100-1,9 con ~-,nlvratior corresuc-i-Inr, to a diamond contont of
0 878 m =3; 50-:' connQntration correspoi..,.inf to a diamond con!--:n* of
0:4179 ZI/m--,J- an-i 5 -` on r-- pondinr to a dianond content of
r-,cr::---md3 th. se
at xht, witri
0. 21.9 T!~ - c;~- .
q,
t
lined, aince excenniv, TAJ.~:! Z, 'fir -IJ)Qfj 1 -4~-,
Card 2/4

Sharpening and honing of s##
S/568/61/000/002/004/004
DOWD113
any bond. Thereforep the cross feed and longitudinal feed are chosen within
a narrow range of values. NIIalmaz recommends a cross feed of 0-05 to 0.1
mm/double pass and a longitudinal food of 0-75 m/win. VNII recommends that
the diamond wheels be fastened like the abrasivo wheels. The following per-
centago coolant composition is recommended by the NlIalmaz norms trisodium
phosphate - 0.60; vaseline oil - 0.05; borax - 0-30; calcined soda, 0.25;
sodium nitrite - 0.10; water - 98.70. It is pointed out that Soviet machine-
tools for sharpeningand honing tools by means of diamond wheels should be
built, For the clock and instrument making industries, the C 194 (S194)
machine tool should be used as basic design modelq and the 3P64 OA64)
marhine tool for the medium-sine machine-building industry. Machine-tools
for diamond sharponing and honing should have the following specificationst
a cross feed of OAl to 0.2 mm/double pass, a shaft wobble of not more than
0.01 mmf a critical speed of 30 to 50 M/0009 and a longitudinal feed of 0*20 V/
to 0.60 m/min. A special installation (Fig. 5) is used for electromechanical
sharpening. 'Thelatter reduces the diamond wear by 75%, There are 1 tablef
5 figures, and 1 Soviet-bloc reference.
Card 3/4

Sharpohing and honing of
S/56-/Ifl/000/002/004/004
j
B0417DI'13
Fig- 5- Device for electro-
mechanical sharpening.
Legend:
I - tank;
2 - brushes;
.3- insulation;
4 - disk;
5 - diamond grain on the disk;
6 - instrument to be sharpened;
7 - nozzle;
0 - rectifier.
:Card 4/4

3/121/631/000/0 1 10CY7101 4
A0O4/A126
AUTHORSi Degtjarenko, N.S., Vvedennkaya, N.11.
TITLE: Tool grinding by reans of diamond wheels with bakelite and retallic
hinders
PERIODICAL; StankI iinstrument, no. 1, 1963# 26 - 30
TEXT% The authors report on Investigationr. of elastic grinding by means
of diamond wheelt; with bakelite and metallic binders carried cnjt by VkT In con-
nection with resoarch work on the automation and mechanivation of the grinding
and dressing of outting tools with sintered carbide bits. As a result of these
studies it wa's found thatthe elastic tool grinding with diamond wheels with
bakelits binder makes it possible to increase the efficiency by a factor of 5 In
comparison to gr;Lnding with rigid clamping of the tool. Optimum grJnding condi-
tions are obtained at a wheel speed of 30 Wsec and a preasure of 3.0 kg/cn?, If
wheels of A6 grain size W*A 5G% concentration are used-on machining areas of up
to 0033 cm2. Diamond wheels with metallic binder of A5 - A6 grain size admit
pressures In -the range of froin 7.3 11 kg/cfR2. To reduce clogging of the wheel
Card ~1/2

6/221/63/000/001/007/014
To~l grin'dIng by means of &aAwawt whae2v with ..... A00VA126
Surface, wheels of 100% coneentrailon are rooommaded4 Under optinim conditions
.of elastio grindlng, diAmWd wheelsvith metallic binders are 4- 5 times more
efficient than those with bakelite hinder, while the same surface finish is ob-
talned. For me6anizlng " automating tool-grinding processes, the elastic
grinding with diamond wheels with bakwlIte or notalUe blyide.r is considerably
more efficient than the present tochnoloo of Crinding wIth diamond Wheels, while
a surface finish of at least class 9 cm be attalned. The model B 3 -80 (V3-80)
grinder for-the dAamond grinding of 'cutting tools bags been 4esikned according to
the principle'of elastlic griTkling. There are 9 figures.

FETROSYAN.. L.K.., kand.tokhn.naukj kand.tekhn.nauk
Grinding and lapping metal-cutting tools equipped vith hard-
alloy tips by diamond wheels. Nov.tel:h.izg.instr. no.2:131-
139 161. (IffU 15:8)
(Grinding and polishing)

S/121/61/000/003/004/oo6
D04O/Dll2
AUTHORS: Petrosyan, L.K., and Vvedenskaya, N.P.
TITLE: Sharpening and lapping carbide tools with diamond wheels
PERIODICAL: Stanki i instrument, no-3, 1961, 28-31
TEXTs The article contains the results of experimental investigations made
at VNII in order to establish optimum techological conditions for sharpening
and lapping carbide tools with diamond wheels. References are made to fo-
reign practide,-inclucling that of the Norton Company in the U.S. It is
stated that the latest foreign trend is to use porous metal binders and a
maximum wheel speed of 90 m/sec# and that in the USSR the application of
diamond tool grinding in industry could result in high losses in view of tho
narrow permissible feed limits*in diamond grinding and the consequences of
wheel wobbling and improper dressing. The available Soviet tool grinders
are not suitable for the use of diamond wheels. New grinding machine*de-
signs will be developed during 1961, and modernized universal grinders may
be used for the purpose meanwhile. The experimental data are given in as-
tail and illustrated by graphs; recommendations for grinding and lapping
Card 1/2

S/121/61/000/003/004/006
Sharpening and lapping carbide tools ..... D040/bll2
three carbide gradesp ~-~2 (VK2), -'-15K6 (Tl5K6) and 73OK4 (T30W are con-
tained in a tab'.ee The following recommendations are made-.use of the
organic7'.* l(Bl) b-Inder; different grain size(according to state standard
numbers) for difforent carbide grades; different diamond concentrations bet-
ween 25 and 100%; 1-2 liter/min coolant consumption; 0.01 mm cross feed of
wheel per double run for all grades, in grinding and lapping; the use of
paste consisting of two portions of vaselime to one portion of paraffin as a
coolant in grinding VK2 and T15K6 carbide or lapping VK2 -xith wheels with a
50% diamond concentration. The following problems have yec to be solved
before diamond whoels of Soviet make can ba used in in(~,_=Lryt 1) Pilot units
of diamond grinding and lapping machines for carbides have to be producedl
2) The production technology of carbide tools with the use of diamond wheels
must be standardiised (i.e. curface preparation for diamond grinding, allow-
ancen, otoo)l 3) Production of diamond wheels on metallic binders must be
started, for such wheels have a lower diamond consumption and higher produc-
tivity than wheelo on organic binders. There are 7 figures, 1 table and 2
Soviet references.
Card 2/2

IC/I ~-'// W
.:' .11 )
VrXMMKA,YA, X.Te.; TOU)SYAMN, G.D.; MASIDVA, A.I.; RUNSOVA, N.A.
"mm-WeAwl
Organization of occupations for tuberculous patients. Probl. tuterk.,
Kooky,& No,6163-66 Nov-Deo 31. (CIML 2134)
1o 0 Irzannodar Scientif lc-Re search Institute of Tuberculosis (Director
Prof@ A.L. Samoylovich)o

im-nn. 40 17.6)
1. 1z !nstAI.,ut.,j I

VVEDMKArA; 0.1.
"The viralenco factor (H-orubstance) and the protective antibodies
(M-antibodies) in streptococcal infections.*
Report BubmitlAd to the Intl Congress for Microbiology
Montrealj Carutda. 19-25 ;;9 1962

LYAMPERT, I..H.j VV NSKAYA, 0. 1. -
Content of M-substance an one of the indexes of the virulence
of streptooocoi of the A group isolated during acme strepto-
coccal infections, Zhur. mikrobiol,l spid. i immun. 32 no.8t
43-48 Ag 161. (MIRA 15:7)
1, Iz Institute, epidemiologii i mikrobiologii imeni Gamalei
AM9 SSSR.
(STFXPTOCOCCAL INFECTIONS)

LYAMPERT, I.M.j VVEDENSKAYA, 0.1.
On tb~ question of obtaining the M-oubetance possessing antigenic
properties from group A streptococci. J. hyg. epidem. 6 no.4:442-
449 1152.
1. Gwaaleya Institute of Epidemiology and Microbiology, Academy of
Modical Sciences of USSR, Moscow. I
(ST.FXPTbCOCCUS) (ANTIGENS)

KOVAIZVA, Ye.V.; SHISHOVA, Ye.M.; VVEDEIISKAYA, 0.1.
Role of streptococci In thes pathogenesis of rhawcatic
fever. Vop. revm. 3 n0.4:3-8 G-D "3. (MIRA 17:2)
1. Iz kafedry dotskikh bolezney (zair. -doystvitollnyy chlen
AMI SSSR prof. Yu.F. Dombrovskaya) I Moskovskogo ordcna Lenina
meditsinskogo instituta imeni I.M. Sechenova i iz otdola streptokok-
kovykh infektsiy (zav. - doktor rued. nauk I.M. Lyampert) Instituta
epidemiologii i milcrobiologii imeni E.F. Gamalei (dir. - prof. P.A.
Versbi-lova) AM .53SR,

VVEDENSKAYA, 0., 1. Cand !.led Sci -- (diss) "kitibodles for various antiZen
0-4L I C-
components of hemolytin, strelitococoh in anti streptooocew sermiss Mm, Isr,8.
9 vp (Acad Med Sci USSR. Inst of Epidennioloai wid Microbioloar L-1 Honored
Acedemiainn N. F. Gamaley), 200 copies (KL, 13-58, 100)
-98-

VVEDENSKAYA, 0. L
Detem. ination of H-antigens in antistreptococcal sera. Zhur.
o1krobiol.epid. I immun.28 no.12:15-20 D '57. (MDU 11:4)
1. Iz Institutn epidemiologii I mikrobiologii iment, GAmRlei AMY SSSX.
(STREPTOCTIOCUS, immunolog7,
K-antigens in nnti-streptoc. Immune serA (RUB)
(DOWUNS SHRUMS,
isame)

VVEMSKAYA,_.R.,I.
Antigen characteristics of autoclaved cultures of group A otrep-
tococei and oup antibodies in irmmine antistreptococcal eerums.
lab. delo;8 ri.e.91 no.1239-44 Ja 163, (MIRA 16:5)
1, Otdal straptokokkovych infaktsiy (zav. I.M.Lyampert) Insti-
tuta apidemologii i mikrobiologii imearN.r.r-m-lei (direktor
prpf. P.A Vershilova) AMN SSSR.
iSTHMOCOCCUS) (APTIGEFS AND ANTIBODIES)

IMARMO. T.A.; VVKMSXAYA. T.Teo
OWWRENWNR
Exhaustive splitting of brown-coal humle acids by metallic sodium
In 11(rald, ammonia. Do)d. AN SSSR 109 no.2:322-324 il #56.
1. Inaltut geryuchikh iskopayemykh
akndenikou A.Y. Topchiyevymo
(flumic naid)
(KW 9: 10)
Akademii nauk SSSR.Fradstiavleno
(Lignite)

1~ . .
I.,

. 1 1. ~ i - . . , , . ~ 11 . - ~ ~~ -I--- -, ;, ~. , . ~ . . I . , - . . - 11
: .. . I I -- - . 'z- - I '. . - . . . - - I ..: - I -", - ! !- - -
a . 900" - . - I I
FM
flm' "m

6) ~M, EIISXATA. T
KWARn T, A J-BI)
BELICOVA) . A,
Humic Acid
Interaction of humic acids of mineral carbons with metallic sodium in liquid a=onia.
Dokl. AN SSSR 86 no. 3, 1952.
9. Monthly List of Ibissian Accessions, Library of Cotigress, December 1952. Unclassified.

JO
41,
tiy
sad leftwk via ty~l
caorane imcdo%e, A. Vs. - Komkv. 1C. A. Asdriaow.'
L- S. Ute&bent, suid T. E. Vredt Lko~ ly A ka.
N4*k S.SS.R. 89, MIT= -Pawmmoe of
dIO 0.9750, at* 1.4061, was (wtionated bF p 11, 40u1 I'o'
Ca 1. sotn' at 231 Oman With to 4 & The
oamrAic preuarts were detil. In tolutme by US' deal-
-CoOty (111) Were Wcd. by
is WW K, ArA the Intrinsic VL
using the e4tmtlamn of lfuW'ns (CJ 36 5(076* - 17 09,
R
TDI d
114
0
0-6, --P)ef; q - v opec4Ar/4)atco - 0; V./Clo- /q/ +
jvlks, iowfithl tite I and 2subscriptstefertosal, ,at and
somte, nwatic pres-
resp., c - onco., d m density, r - e
I The follwLig mtilts an reported (frutcm no).,* -
yle COU i#ezcy, M. K. resp., giv tn):- 1.
14.3%, etasth- 1.200,000, MOO, 0.479, OM; 2, M570,
Plastic, 4M.000, 0.10. 0.475, 643; 3. 30.6%,; very glotk
144 000.0-4A 0.07, OM, 4,15.4%, vitmo liquid 7 000:
0.456. 0.40, - The uafnttIonztM sample had a woli wt. of,
74r In totuene &A in CC4. Tte rel:";on 1wtween IVI
was 11 --12.16 X 10-4MO.". Being vC in kluene,
If
the m2ter4l larotly linear. but the vwiame in j shm",
that the fractions difftr samr, in structure, and the swAlltr
values *f K indicate th~tt the fta4diOnS at t(jWT(
mot, wt. are
mom branched. 11te velues of It are smAller th4o those
obtained by Scott 'C-4 41 637i) wul mom in ac"id with
thom expected by it "I', for Vis0oul liquMs Xftd PkLSAIC
mAterials. John flowo.kAti-

BELICULs
Humic Acid
Interaction of hunic acids of mineral carbons with
metallic sodium in liquid ammonia. Dckl. All SSSR
86 no. 3, 1952
9. Monthl List of Russian Accessions, Library of Congress, December '2
195~ Uncl.

1.* KO.ROLFIV,. A... YA.',- ANrFYANOV,* K: A-.',' Trr-SqFIA,* L: S." r7nFNSKAYA'
T. Eg
2. USSR (6oo)
4. High molecular weight compounds
7. Molecular weight and characteristic viscosity of fractions of
polydimetlqlsiloxane, Dokl. AN SSSR 69 No. 1, 1953
9. Monthly List of Ru.sslan Accessions, Library of Congress, May 1953. Unclassified.

1. Xollofxv, A. Ya.,z I. ; VVE'DE-3XIYA, T. Ye
2, USSR (600)
4. Siloxanes
7. Molecular weight and characteristic viscosity of fractions of polydimethylsiloxane.
Dokl. All SSM 119, No. 1, 1953.
9. Monthly.List of Russian Accessions, Library of Congress, May 1953. Unclassified.
KuXW,R8NKo, i,.A.; Yvicaw-run, T.Te.
Water soluble acids of solid mineral fuels. Pochvovedanie
no.12.:51-58 D 159. (HIM 13: 4)
1. Inotitut goryuchikh iskopayerqkh Akademii nauk SSSR,
(Peat) (qoal) (Acids, Organic)

)IMRAREM, T.A.; VVEDEFSKf~TAA
Complete decomposition of hunic acids by metallic sodium In liquid
a=o:aia. Xhim.i tekh. topl, no*6:25-34 Je 156. (W-RA 9 19)
.1
1,1natitut goryuchikh isk avemukh Akademii nauk SSSR.
(Humic acicli

4 1 6
SodUm
Interaction of humic aclils of mineral carbons with metallic sodium in liquid mmnia.
Dokl. AN sssR 86, no. 3;, 1952.
9. Monthly List of Russian Accession!, Library of Congress, Decembtr 1952. UnclessifitkI.

MMUUN09 T.A. (Moskva); VVEDENSKAYA T.Ye. (Mosk-va);
=j
GRIGORIYEVA, Ye.A. (Ko-oWa-T; -6AVELOYLY, A.S. (Moskva)
Obtaining of organic acids from weathered.coal. Izv,
AN SSSR,, Otdo tekh. nauko Met, i tople no,03.43-249
JI-Ag 161. (MnA 24:8)
(Organic compounds)
(Coal)

VMMSKAYAp T.Ys. 4.
Oxidation by oxygen in an alkaline isedium of veatbsrtd
coal in varioue otages of metamorphism. Trudy IGI 21:3-15
10. (MIRA 16t 3-1)

ITEDE-E-SKIYA, V. IN.
Vved-7ns,kava. v. N. ,ft,,jto7ati, rcr-rc, of C,irrent -Itrenr`h 7,rd Time I- ():~Ivarlv
Frcmsses." info rmat s I c, rn-.,,,r tek?lrdci.--;',i f- .- 1 4 1 1
1953, Er: V, Fall-M 214-27, Y . - .1 y 7;^~,,mflk M-fprr-nc;~ Tck,-,!cs'., ra~t;a 1

1 STANKOV, S.; TROFTMOV, V.; VVEPEYM=,-A.;. STIRIDOV, A., inzh. vodnogo
transporta; CHERNOV,-g-.-, inzh. vodnogo transporta
Improve the management of the consDlidated inland waterway
network. Rech. transp. 24 no.10:1-3 165. (MIRA 18:12)
1. Nachallnik Glavnogo upravleniya rechnogo flota pri Sovete
Ministrov KazSSR (for Stankov). 2. Na.challnik Kamskogo rechnogo
parokhodstva. (for Trofimov). 1. Nachs.11nik Severnogo rechnogo
parokb.odstva (for Vvedenakiy).

D.WILEVSIKIY, Tiktor Tasillyevioh, akademik; SrAPUKHOT. T.I., prof..
doktor geol.-mineralog.nauk, retsenzent; PRUDBUSUT, G.A.,
prof., doktor skon.nauk. retsenzent; VVEDEN -, -.-$.,,Prof*$
%TT -A A
doktor ietor.nauko retsenzent; WUMIKOT, e.A., red.; ARXH"-
MIMIATA, H.S,, red,izd-va; YATUSMYN, Ye.B., tekhn.red.
(Russian gold; history of its disoovery. and mining up to the
middle of the 19th century] Rusakoe soloto; istoriia otkrytiia
i dobyohi do serediny XIX v. KoBkva, Gos.nauohno-tekhn.izd-vo
lit-ry po chernoi i tovetnoi motallurgli, 1959. 380 p
NIRA 13:3)
1. AN USSR (for Danilevskiy). 2.lChlon.-korrespondent AN SSSR (for
Prudenakiy). (Gold mines and mining)

4
TVIMENSKIY, Aleltsey Alekseyevich.
%Wm-
[Electricity in oux life] glaktrichost7o v nashei zhisni.
Moskva, Goo. izd-vo tekhniko-tooret. lit-ry, 195). 63 p iMA 7:3)
(Nauchno-populi.arnaia biblioteka, vyp. 16).
(Electricity)

1 0 4 a it U U W is if is x of v a a x a A1111 ON us issralre of au a OC
a I A -A A - I -A. 11 -J-k- P --V I j
A 00
J, 00
91b
T_
00 J. G". Chm. (it. S. 14. RTI 11); d A. 25, =11-A study was made .-so
7
Wit
00 9 ot the tf,; of white P Into red whit, in the liqukl state, at temps.
"locity of trim,form so
175-MOV. Impurities In wWe P catodyte the tranx(orma0m bt-tween 17&0 and ZVI%
00 therefore the white P was camfully pvfiW by distn. in roetw. in the Interval 175- 00
6; :0 2W the velocity coast. K Increases with time. the more in the lower W temp,. which
Indicates that the reaction is outoestalytic at them tempq. Above 2M' the trangfor.
matinet folilims the law of nwousmol. revirtiori. showletit a litonjenrotil; (non catalytic)
reaction anti K rrinsins rmst. frestdiew of the length of time from the sidn 1`164 Is .00
vlarly true for tenips. sbutc.I(W. At highrr truilm jelsorr 4.1W) the rracli,vi
ty becomes much higher and The transformation It accomi*njnl by a smaig see
=
so is evolution of best, the truip, ii" to 52LV-W)* and the prewrt reaches 42 min, At '00
still high" tevills, Or reactlin slows elown. This prculiar lehavlor Is attritmtrit to
00 the matener In the sawlaus Niaw of several kinds of molt of while 11 that rallidly reach 4*0
a state of ev"Ale equil. and tralet to form particks of felt Il- It L MAIN-OSKY
00 '00
sew a**
.0 of 01910004 an Rv Nuft A
:~o o 4 0-1 0 0 0 0 o * 0 0 o o
~o o 0 0 0 q o o o 0 0 0 o 0 o
Ice 0
'00
00
boo
61146 i* 4.v its
so
p 0
UO n I a a; a * a I W is a 4 3 "1 9 00114
0 0
o 0 Zo 0 0 0 0 0 0 0 0 0 6 0 0 0 0 0 a 0
~o o a 0 0 o o o 0 o o 0 o 0 0 0 o 0 Z

a V -Irv
,~4v' itV
49, 0 0 0 0 ,-i ],!Mrs A a 6
it 1A
o411 0 it w is, _A -j_ 1, As
a
- L_ .riot 1441t.ts-
* A
A
CIO/
0
far to do I
U.
sea TINS *w%dds 4d As C
I cetrjys bf 44 sots.
A, & V tM3 "m with rl
&0& %7 bir It
see
f via, W, Witt affill,
I'llicittiffill I .00
ee'l "j" the C.S."
v
fle
of 'IT, ;;,
04 11 -lls;R
I N
of tot,. Cl god
100, so
00 8~ 00
t9
to
CV-
c:4
&So-$L
0'0 ILL 0 0
u it 1416 1;
K 7'% 0 0 0 9