SCIENTIFIC ABSTRACT GRABOVSKIY, M.A. - GRABOVSKIY, YA.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

9, or
I @ dp@i&gk@Y,- W.* Y.-. m-'A"61, , .3"" :r.
Floating Bodies.
Floating of a bodv on the mwface of water. Fiz. v shkole no- 4,, 1952*
9. Monthl List of Russian Accessions, Library of Congress, November -100 Uncl.

11. A.
USSR/Geophys1cs:- Ferrites Sep/Oct 52
"Kagnetie Properties 6f Ferrites and Their Signif-
Icance in Geophysics)" M. A. Grabovskiy, Geophys
inst, AcadSci USM
I "Iz Ak N@uk SM' Ser Fiz" No 5, pp 41-46
Brief survey devoted to analysis of phys and struc-
Aural properties of ferrites--binary oxides formed
by Fe2O with.oxides of other divalent metals.
Author Lrives sozie@geophys conclusions on existemee
of ferrites in natural state. Indebted to A. G. Kal-
ashnikov. Received 14 Apr 52.
226T56

may/Jun 53
4 E0 Y,5 K A
"Thermo-residwl Magnetism of Mineral Rocks,," M. A. Grabovskiy,, Geopbp Inst, Aead Sci
USSR
Iz Ak Nauk SSSR, Ber Geofiz, No 3,, pp 215-224
Examdnes )from the modern vienoint of magnetization of ferromagnetics)the origin of
thermo-residual magnetization in ferrcmagnatic mineral rocks and also clarifies the caunee
of reversible magnetic polarity in acme rocks.

GRABOVSKIY , M. A.
USSR/Geophysics - Magnetite
Sep/Oct 53
"Variations of Yagnetic Properties of Magnetit6s Under the Action of Iargo Compressing
Stresses," M. A. Grabovskiy and E. I. Parkhomenko, Geophys Inst, Acad Sci USSR
1z Ak Nauk SSSA, Ser Geofiz, No 5, PP 405-417
Investigate the magnetic properties of magnetite samples subjected to uniaxial.
compression due to hydrostatic pressure. Relate results to present-day views on
ferromagnetism. Derive several geophys conclusions.
267T73

BAIIOVSKIY, M.A. (Moscow).
--mao
-II.-Lectrodymnic demonstrator-magnotometer. Fiz.v shkole 7 no.4.-60-64 133.
(MLOA 6;11)
(Yagnetomter)

FD 394
USSR/Geophysics Reverse thermoremanent magnetism
Card 1/1
Author Grabovskiy, M. A., and Pusbkov, A. N.
Title Problem of the origin of residual magnetization of reverse polarity in
minerals
Periodical Izv. AN SSSR., Ser. geofiz. 4, 320-330, Jul/Aug 1954
Abstract Experimentally demonstrate that the demagnetizing field from an induc-
tively magnetized ferromagnetic specimen is always less in absolute
magnitude than that strength of the external field that caused this
magnetization. Ferromagnetic specimens that have experienced thermo-
magnetization can acquire a demagnetizing field greater in absolute
magnitude than the external magnetic field. These conclusions enable
one, to explain the appearance of residual magnetization of reverse
polarity in certain minerals sometimes observed under natural conditions.
Thank 1. F. Paukov, senior laboratory assistant, for his aid.
Institution : Geophysics InstituteJ Acad Sci USSR
Submitted : August 18, 1953

C1
U&9R/Physice of the Earth Electric and Magnetic Field of the Esrth., 0-4
Abst Journal: Referat Zhur - Fizika, No 12, 1956,, 3639B.
Author: Grabovskiy, M. A.) Petrpva,, G. N., Isakova, L. I.
institution: Bone
Title: On the Occurrence of Thermal Residual Magnetization of Mountain
Rocks
Original
Periodical: Izy. AN SSSR, ser. geofiz., 1956, No 1, 56-60
Abstract: A description of an experimental investigation of thermal mag-
netization of ferromagnetie mountain rocks aqd the conditions for
the occurrence of residual ma etization Ir 'at all the stages of
the cooling of the rock. Magnetometric methods are used to measure
the magnetic properties of specimens of magnetite in the Ural,,
Kursk, and Angaro-niuk deposits,, and of pyrrotine and nickel.
For all the specimens, curves of the thermal magnetization Iit
are given, which show how the magnetization Tit increases in a
definite orienting field (an the order of the magnitude of the
Card V2

USSR/Physica of the Earth - Electric and liagnetic Field of the Earth, 0-4
Abet Tournalt Referat zhw - Fizika, No 12, 1956., 36398
Abstract: earth's field and above) vhOn t of the specigen drops from the Curie
point (tc) to the room temp@@rat-ure (t - 200). Investigation was made
of the residual part of the thermal magnetization Irt- it is shown,
that Irt occurs at values of t close to tc. The development,of the
thermal-residual magnetization in week fields occurs fundsamtally
as a result of irreversible magnetization processes. Particular at,
tention is paid to the determination of the stability of Irt and of
its.coercive force (thermal coercive force Hct). Plots are given
for the dependence of the Hct and '@c on the magnetizing magnetic
field. Ect le greater than Hc for the same specimen, and in the
region of weak fields it is much higher than the magnitude of the
field that "Uses a given the-noal magnetization. In this manner.,
Irt is magnetically stable. The high values of Ac and of Act for
many mountain rocke belps them retain their magnetization for many
geological periods and it is therefore of great significance to
paleamagnetism. Bibliography.. 10 titles.
Card 2/2

ORmvsxrr 0
Determination of the vertical component of a magnetic field for a
two-phase magnetic system after Its thermal magnetization. Izv.AN
SSSR.Ser.goofts.ne.2:157-164 IP 156. Oa" 9:7)
loAkeopmIya nauk SSSR, Goofisichookiy instituto
(Prospecting-Geophysical methods)

'USSR/Physics of the Birth Electric and Magnetic Field of the Earth, 0.4
Abst Journall Referat Zhur - Fiziks., No .12, 1956.9 36399
Author: Grabovskiy, M. A., Petrova,, G. N.
, %,-j-
Institutiont None ZTIIIV@4
Title: On the Stability of the Residual Magnetization of Mountain Rocks
Original
Periodical; Izv. AN 88SIR,, ser. g-.aiz.,, 1956, No 3, 2go-296
Abstract: Results ard, @'given of an experimental investigation on thermal-
residual magnetization and on thermal coercive force of spepens
Of etite, pyrrotine, and nickel. The different course or the
relative change in the mignetization and of coercive force for
normal magnetization and for thermal magnetization is established.
It is shown that the mountain rocks have a high magnetic stabilit 4"
to thermal magnetization., which gives a definite physical foundatibn
for development of paleamagnetic investigations.
Card V1

,qlro,N.A.
.2g.og
" w
Kagnetic anisotropy of rocks. lzv.AN SM.Ser.goofiz. no.4:47"2
Ap '56. (an 9: 8)
1. Akadenlya nauk SM. Geofisichaskiy Institut.
(24oks-Aagnstle properties)

a W.

&Rf)6OV6i,I-0Y, M-f@-
'PHASE I BOOK EIPLOZUTION 496
Akadaziya nauk SSSR. Xomitet po geodezii i geofizike
Nezhcb-inaroduaya, assotelatslya, gemagnetizza, i aer=(xdi; tezisy dakladar Aa
XI Gene--allnoy assembleye Mezhibinarodnogo geodezicheskogo i geofi2icbeskogo
soyuza (me naernatiowa As3oclation of Geonagne-tiez and Aeronomy; Abffbroeus
of the Reports at the XI Gezwr&3. Assembly of the Inte-a-nevional. Union of
Gecklesy and Geophyssics) Moscow, 1-7A-vo AN SSSR, 1957- 46 P- 1,500 coPies Pr-Tvteda
PURPME: Mxq-s booklet in irtended. for dissezinetion of abartracts of papers
pr-aseebed by the Soviet members of the International Association of
Ge,,mgmatIsm and AeronmW at, the XI General Assambly of the Liternational
Union of Geodesy and Geopbysicne
COVMVM: 7his booklet vith ftal English tran'slatlon follmdug the Rasslan text
prenez1ba abstramts of papers, mairtly on magnstics, telluric currents and
mirv.-se. presented by Soviet contribut6ra at the XX General Assembly of the
[e-mail] Union of Geodecy and Geaphyslase It vas published by the Mationall
CoemIt4t3a for Geodazy and GeopbysIcs of the Academy of Sciences of the UM.
Card 1P

The Zrtaraeblonal. Association (Coe.*)
TABU CF
COMM:
496
Me!--shn:Lk*vp A. G., Petr&m. 0. N., Grab No Flesults of an
Zxv.&Ugatlon of Magnetic Propext es of Rocks and Geological Bodies 5
Reeent@ laboratory Investigations showed the Terromeawtic rocks we
nonundio=ly maguetizede Peament mz@petlaz thou& distributed regularlyp
does not follow the direction of the magnetizing fieldo The article evaluates
stability and temperature Int'luencee on thermo-zagnetization. In discussing
the meqgnetla anisotropy the authors consider this property as typical, for
pblc rocks
Krasav-dkly, V. L Investigations of Aurarse and Zght Sky Glow in the MR 3.1
The reyort contains latest data on radiation In the upper atmospherso
HydrDayl radiation of night sky glow, twilight radiation of sodium and hydrogen
emission in the m--4w- intensity 2one of aurorae are discussed.
C-erd. 2/9

Mie International Association (Coat.) 496
Krasovskly, V. I* The Nature of PAdiation In the Uprar Atmosphere, 13
Radiation at 100 ka from this surface of the earth Is connected with the din-
sotiation and formation of molecules, Variatione of intensity of radiatIon
ar-- connected with temperature and presmue fluctuations in the upper atmosphere.
PrIzary and secondary radiation of aurorae and their nature are discussed*
See=dary radiation can originate aB a remat of recambination processes,, fo2za-
tion of an electric fieldj, end chemical reactions of primary ions and excited
prodacts.,
Shklovskly,, I. S. Elementary Processes in the Upper Atmosphere as Evidenced
by Radiation. 15
In eaUtion to common fluorescence originating in the selective absorption of
ultra-dolat solar radiation by atcas in the atmosphere with subsequent re-
raastion of *softer" quanta., processes of resonance fluorescence take place in
the upper atmosphere. With the detection of some lima in a tvilight arectrum an
estimate can be made of itz wmber of louan quanta In short vave radiation from
the Bun.
Cara 3/9

The Thrb-arnational Association (Cd6t.)
496
@roltakaqav Ve Ao Short-Perlod OscIllstions of the Barn's Electro-
magnetic Field- 18
Simultaneous studies of tellurle currents and magmetic: records facilitate the
study of short-period oscillatIonso ftperlments, installations for receiving
telluric currents, and the basic principles of A proposed classification system
for types of oscillations are discussedo The causal genetic relationship
between various types of oscillations and the most favorable relative position
of the Sarth and the sun In exciting such one"' ions vere formulatedo
DrJLatzkiy,, V, )6 Ibnoorphere Near the Polar Region.
21
Observations made from May 15j, 19% to Alpril 14,, 1955 on the drifting station
SP-3 Include vertical sounding of the staosphere on a ollding frequency*
During the period of -4n'- salar activity., the number of sun spots in the
vorking period was 8.3. Me vertical acnonent of the berth's magnetic field
clumged from 56,612@to 3,93.9 y . The geonagnetic disturbance was much saw' r
than in polar oiser*atorles furtber south, The behavior - of sow Ionospherle
layers is nearly the same an In moderate 2AWLtudes and shows the same depenaence on
the elevation of the s=o ionization of various la;yers is pronounded and triple
magneto-janic splitting vas observed rather frequently.
Card 4/9

The International Association (Cont.) 496
Kalinin., Yu. D. Forecasting Secular GecrAgnatic Variations 25
Variation in annual values of geomagmetle elements is the sumptry effect of
changes in the geommoetic field caused by Internal agents ( 6-f ) and by
geoma etic activity ( S'@ ot ). The latter could be completely eliminated by
taking average values for 10-3.1 year cycles. The morphological examination of
such factors leads to the establishment of space-time relationablips. 7he effects
of internal forces In Eurasia are of a smooth, quasi-periodic character
lasting a few decades and the geomagnetic activity follows an eleven year eyele.
Tb1s makes it possible to forecast average values for a five year period vith
sufficient accuracy and to construct magnetic charts for the nearest epoch*
Nikollskiy, A. N. Disbrilutlon of Mognetic Disturbances in the Arctic
Region Near the Pole 30
Irregular changess in the magnetic field are the main indication of disturbances
in the high latitudes. The fam and amplitude of the daily rate of disturbances
are determined by-the effect of the earth's permanent magnetic field on the
inecaing jets of solar particles. The diurnal variations in high latitudes are
Card 5/9

The International Association (Cant.) 496
very emplex. Observations near the pole suggest the existence or a second
zone of Increased intensity and frequency of magnetic d1strubances close to 800
geomagnetic latitude. This in vell in accord with the studies of auroral and
Irmospheric disturbances and fits the theoretical findings of A3-4'nn.
Benlkovs, N. P. Alectric Current In MWetic Storm
Me regular caqpKwnts of world aftsetie and polar storm were studied in world-
vide observations frcu 1932-1933. 2he potentials of these fields vere camputed
and a system of polar.storu currents van reconstructed. An Increase in conductiv-
ity with depth van deternined and a break In It established'at 900-1200 ka., where
Gutenberg and Papetti-discovered a discontinuity for P-waveso_
I
Teller, A. Te. M@ydmen -ALUmUm In the tworal Spectrum 36
An in'restlgatlon of hydrogen radiation In the auroral. spectrum was conducted
at 640 of geonmtgnet1c latitude and In the neighbouring regions. 2he data
obtained concerns the bright besm flash and the afte phases. Prolonged
exposure spectogrOM (1-2 hours) in the region of 6,691!916001 bear Intense bands
of the first positive system of N2; there are no evident sips of R CL on the
photographs or adcrophotographs, yet In all seven spectra the presence of 9 d-
lines could be confi j .1
d 0=jten radjat@on is regularly observed in the after-
glov spectnm foll= developing aurora.,
card 619

Mw Thterniftonal AissociatIon (Cont.) 496
Zvoort- No No Magnetic Surveys at Sea in the Ship "ZLryaw. 38
I&& of mgwtic obserntions on the oceans after 1929 makes the study of
variations of the earthIs mgmetle field and the secular changes largely
conjectural. Mder observations made by the ships "Galileo" and "Carnegie'.
based on a 100 mile gr:Ld,, do not reflect regional magnetic an-ma"Jas related
to the structure or relief of the sea bottem. A pMosal has been made for
another smmy to be conducted by a laboratory ship. The specially built AbIp
*Zarya* vith a 600 t. displacement was supplied with everything necessary for a
mouth's voyagee The personnel consisted of 34 persons of vbich 9 vere research
vorkers. Mw instrnents used for measuring magnetic phenomena an: for wasuring
declination,, a 127 = optical goniametric compass and a rvW finding compass for
continuous recording and neasurezient of differences between the gyro-coursto and
the magnetic course for the Mwizontal camponeut,, two double magnetic compasses;
for wasuring R and Zj, a two-ecMonent magnetodynamic magnetometer and a
c T wSwtommiter with a self orientating indicator. *7Arya* already
som experlimental vork in the Baltic and the North Sea,, discovering a
considerable maber of anoinalfes. In the future it viU. make same observations
In several regions of the siWosed maximn secular movement, of magnetic elementse
Card TP

The MAernational Association (Ccut.) 496
POtakh"s Vo A& Solar InAron Mission Sources of Magwtic DisturbaseeB
and Aurcree 43
Mw author discusses the neutron theory explaining the relationship between -
salar activity and Processes Occurring on earth, the possible physical
PrO0108848 leadlM to the faMnation of a large Mulber of gsU&raW and the
WW*rl=At&l fludinp In this field,, and the detemination of velocities of
S02M P03MA'Allas by t1m intervals between phenowna oc==@U* on the a= and
an 4arthe
O.A. V. and Kebuladze, V. V. The Nature of Regional Telluric
Currents and Their Relation to Geology 44
Telluric currents have Interested scientists for a long time but the lack of
yetenatic studies and the irregular distribution of stations prevents
M
inite conclusions. Statistical examination of &round-the-clock observations
at the Dusheti station (Caucasus), led the authors to the opinion that the
potential difference in a telluric field can be divided into the constant and
the variable components. The latter depend on the Oin's diurnal, seasonal,
annual and secular variations as well as the time of occurrence of extremes
of these variations. At the same time, the meteorological factors and the type
Card 8/9

The Uternstional Association (Cont.)
496
of electrode grounding play an inportant part In the creation of a potential.
On zeylew analyzes telluric storm and dietrubances., their rates,, frequenales
and amplitudes. Parallelism of the horizontal component of the ma&etic and the
latltudlnal component of the telluric fields is fully established. The application
of ouch currents to the study of geological structures in Georgia seems to be
particularly successful in determing the depth of the crystalline basement.
ATAMIAM: Idbrary of Congress NM/bmd
9-2-58
Cord 9/9

AU.T.HORS; Grabovskly, X, A nd Yegorov
TITLE: -sa V. S.
ftsice saw, C409,1W, swriftlaft 53-44-7111
OveskolOk" demonstrats nnykh
MIODICAL: @ ccr
khi .Fizicbeakikh X io Opyt0v Po obshchow kurau fiziki),,
Usp4e auk, 1957, .4rft in
ABSTRACT., A device for
Vol- 63, Mr 4, pp. al3.8.U
Card 1/4
the demonstrati '
(USSR).
of a system Valling Board', on of the motion of the center of mass
oblique position .' This device
means of * One Of the ends of thisconsists of a board in
an electro board is held firmly by
without magnets while the other end slidea-
minationfrictiOns by means of ba I nearly
Of the Path J-1Z on a Blideway
on the System Of the center of - For the deter=
.9 which are in slight tou mass two brushes are fastened
Paper. One Of the brushes is fas ch with a vertical sheet of
systems the other so tened to the center of mass Of the
mewhat higher After
magnet the brush located in the center
line# and the brush I switching Off the electro.
ocated s of BASS will drayA. a straight
O'newhat higher will
(with the curvature directed towards the center of mass
a weight i dralw a curved line
br
tht is now in t Following
a fastened to the upper end of the board* The upper
ted it he center of mass.
was found that the upper brus When the experiment was repea-
now the lower brush h draws a straight line whereas
draws a curved line the curvature of wh!
Ich is
Soup C&"&-'6f
in Physics 53--"7/11
Card 2/4
directed tOwArds. the center of mass* The authors give some practical
directions as to the construction of this device. 2.
The resonance
of a motor suspended on a spring: In the case of resonance motors
are able to loosen their fundamentv These and similar phenomena can
be demonstrated
ca:L spring on aas follows: A small motor is fastened on a cylindri.
massive stand. On the axis of the motor at small
rod is asymmetrically fasteneds which eauses percussions@ of the
frequency of the motor. The first resonance at -. 85 rotations,per T
minute manifests itself by a periodical lifting and lowering of the :4
motor. The resonance frequency of the spring depends on the elastim 4.
city coefficient of the spring and on the mass of the motor. In the
case of the Second resonance, at about,17o rotations per minute, 4.
the motor oscillated round a vertical axis.
With an increase of the
number of rotations new frequencies Occur, With the highest frequen,
cy-standing osciUati6ns occur on the cylindrical spring but the
motor remains in its position. In large lecture halls it pis advisable
to project the shadow of the motor on to a screen, 3. The phenon
menon of acoustic resonance on Helmholtz resonators: Four Helmholtz
resonators of different size are arranged in such a manner that the
JA
holes are on the same level', In front of these holes four similar
paper turn-wheels are fastened. In front of the large openings of
the resonators a loudspeaker connected with a sound source is mowt-

S6=.-Cas*s of-Experlmata,D6wniitratdor"W,',~for.~.th6,)rawra1 Cawiw- 39>4-7/11
in Physics
ted. The turn-wheels which happen to be before the excited resona-
tor then rotate. The dimensions of the apparatus are given* 4*-
A small ball in a gas- or liquid jet: A glass;tubal one half of
which has a cross section that is about 16 timei as great as that
of the other, is connected by means of a rubber tube with a baUoon
which contains liqLAd carbon dioxide under high pressure. In the
wider part there Is a ball,, the diameter of which is smaller by
about IL - 1,5 mm than the inner diameter of the wider part of the
tube. The gas flows from the narrower into the wider part of the
tube.*Because of the decrease of pressure occurring on the wider
part, it is possible to turn the tube with its wider part directed
downwards without the ball falling out- 5. A ftut" ball: A tennis
ball caused to rotate by an oblique impact is surrounded by rather
compl-leated currents of air. ThereforeP a 11cut" ball may change
its direction during flight and may thus deceive the other tennis
partner. For the purpose of demonstrating this application of the
Magnus effect a special device is here described: A direct.current
motor of 25 watt power is vertically fastened to a massive stand,
On the motor axis a rubber tube is:fastened which is longer by
IL - 2 mm than the axis protruding from the rotor. On to the end
Card 3/4 of the rubber tube a celluloid table-tennis ball is fastened,-

Some C"eir,'6t4.BkpeJ?imefttall,beino6EItrations,.fo-rithd Gejiera1-'CdU-r:'9e, 53-4-7/11
in Pbysics
k small disk is pressed on to this ball. from above by means of two
cylindrical springs. When the motor rotates the ball ia taken along
by the rubber tubes and rotates with good regularity with the fre-
quency of the motor. The resting as well. as the rotating tennis ball
can be knocked out of its positiorrby means of a'spring. First, the
ba1IL is knocked out several times while the motor is not rotatingj
and in this case it practically always:flies: in the same direction.
However, in the case of a rapidly rotating motor, it flies in anow
tber-direction.
There are 16 figures.
AUILABLE: Library of Congress.
Card W4

Author. D-yakov. C.P., Candidate of Physical. 301155-58-2-34/35
zathass,tical Sciences
fxnxs Survey of Papers Need by Set-tizt. of zosco.
University at go Jai-Imla Corcreas ca dor Physics it !:Agnetic
Materials (Obzor dokl&4*v uchonykz -ovLo-cgo unt-mitata
" watsayusacm, soveahchamit go fixtke saCT@ttaykh mt.rimlov)
PZILXODICALs Testnik Zookovmkogo Univerniteta.Seriya -tesetikl, mokhmalk.1,
astronooll, flamt, Wait, 195a. Or 2,pp 247-250 (USSR)
ABSTRACTs From December 6 - 11,1957 there took place the fourth Union
Congress an physics of magnetic sauriAls in L*nitgr*A. (The
firmt two meetings took place 1946 and 1951 in Sverdlovsk,
the third sooting1956 in Mesta*). The congress was organizol
by a Academy of Sciences of the USSR, Department of Physical-
Mathematical Scionamot Scientific Council on P`uAdamental
Problems, of Magnetism, Institute for Semiconductors of the
Ac"en7 of ScL@ues& USSR and Committee for Wagnettra. There
"" more them 300 participators, 59 lectures wors' Civono
smug them the following lectures of the representatives of
the Moscow state University .
1. [e-mail] R.T. Tolasnim, To.?. Xtritsynat Lecturer @Oa the
-yeleatty of T -ettc Rev'r'sl of the Forromn-ne tits". -
2, Toleanin, To.T. Xj@r2.h_A91na. Axs1st&nt
-on Magnetic Viscosity of TorritW.
3. Prof .... r IT.Y. T.I.snl. %.G. Shlahka., Aspirant
'Urfact of Wagattic Viscosity on the Frequency CbArocterlatica
of forrix.s..
4- K-T._P-@jtymz, Lecturer 'Variations of Structure and Anti-
forrommignatic Properties of It 3rel.
k
XaAA_qj&k2vv11y, Lecturer, S.Ta. Dr@a_dak&yso Junior Scitnts"t,
Assistant `91&-ttlc Pro;orttes of Arloctropic Stonom'.
6. G.P. Dlyskov, Lecturer @KLdoatamtriction Properties of
Sicar'y Alloys".
7- ?"teaser To.l. No
E4,opskiy, L.T. Sobol.v, Assistant
02lectris Properties of S14n-PorritesO.
a. senior Scientific Assistant, A.P, Pstsanov.
Aspirant @Nsgaatlc Propertlas and Structuro of Isaganese
Baran - Alloys'.
9. 1.&. smal-ko" Senior Scientific Assistant, B.F. Aalo.
Properties or Ferrites-.
10. N.A. 3-sm-fir- Sclw.tL-fli A,
'Prop
Lecturer, ortloo of %'r., 04 - I!C F.2,4
11. N.A. S.cl-ka, ad T..T. rqtaako. Zrigineer @proportlea of
IFerrite* 1A th: Rleh-Pr ,quo@.cy asr4*4.
12. Professor I.P@Ile2cv. X.M. Vo2'.hovA.1v:tuNr, T.A.
Tolkina, Lecturer, &ad it.&. z^@P Ive, J%rlar Scientific
AssVetant -PerrItes V.th Ccc;ensw-ton Point".
13. 1.?. Dole'. T-7. -RIAL.Z.,vs, -zl.c-rt. and
Calvanozagtotl- Propettl6a of the Torrltes*.
14. V.A. Tiz.fej-z, J,vl-r Cc-nT:f-Ic lrlsiotln-, A.T.
7@Produc-lzn @f cf Ftrritas@.
15. ProfWiscr X.r. Belov, I.T. Pti-ko. Zuaior !@clectiftc
Asstst-t '04 of ftrro@dtotic
A'IOJs Star the Lt$ol.t. Zwr@ of -.:=;tratjra%
The p*rtlcl;atcr- of the @#!tr4 visited a 1%toralory if ttA
--tllt@%@ a' r-tcord-t4r# of th- Action:, cf :zlor. *a a I a
IT c r t,
(P-1.*4cr .A. :ro.-.kty).
-to --- @-Wl-zl-A ty Pr;! .... I ::.V.
nz,-,
- .h
-.@nzres. j.L&=.t4 far
195e.
X.C-11: ..A *,.., X.t.h-,
?or--4r&.r-et1: @Forr4l*z) - .1@ rnla.
tt4 Por.-entti@4 ar.! !,art.

SOV/49-58-8-4/17
.,AUTHORS: Grabovskiy, M.A. and Brodskaya, S.Yu.
TITLE: Vormal Magnetii@`Ftion and Thermb-magnetisation of
Anisotropic Rocks (Normallnoye namagnichivaniye i termo-
namagnichivaniye anizotropnykh gornykh porod)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya Geofizicheskaya,
19581 vr 81 pp 9?? - 988 (USSR)
ABSTRACT: The results are described of laboratory investigations of
normal magnetisation and thermo-magnetisation of rocks
possessing a pronounced magnetic anisotropy and also of
investigations of the magnetic stability of such rocks
for two types of mgnetisation. The measurements were
effected magnetometrically on a vertical, ast@tic thermo-
magnetometer with a sensitivity of 1.94 x 10- Gauss/mm.
Magnetically-isotropic 10 x 10 x 100 mm specimens of
thinly-layered. iron-mica magnetite quartz from the Kursk
magnetic anomaly were investigated. One series of
specimens were cut parallel to the direction of layering,
the other perpendicular to that direction. Prior to
thermo-magnetiaation I the intensity of maEnetuic saturation
Is was determined for all the specimens in-a closed
Cardl/6 circuit; Is characterises the quantity of magnetite

SOV/49-58-8-4/17
Magnetisation and Thermo-magnetisation of Anisotropic Rocks
in th6 specimen. For the magnetic investigations, the
specimens were selected in such a way that the
"longitudinal" and the "transverse" specimens had equal
values I S . in cases in which this could not be
accurately fulfilled, specimens were chosen with somewhat
higher values of I S . The specimen was placed into one
of the coils of the thermo-magnetometer and, prior to
heating, the normal magnetisation curve at room tempera-
ture and the curve of residual magnetisation I were
r
measured and the magnetic stability of the residual
magnetisation in various fields was evaluated. For
evaluating the-stability, the following three magnitudes
were used: the coercive force H cac I the dc field
required for reducin the residual magnetisatio@n to zero
0
when recording H @thellestroying field) and HI
0 C)ac
which reduces the residual magnetisation to zero (the ac
I'demagnetising" field). The investigated speciEeu was .
heated in a furnace to a temperature 50 to 100 C above
Oard2/6 the Curie point at which it was held for a certain time

SOV/49-58-8-4/17
o-magne-tisation of Anisotropic Rocks
Normal Magnetisation and Therm U
and then cooled to room temperature inside a certain
magnetic field. The cooling was effected sue6essively in
orienting fields of the following 8 intensities;
0.5, 2, 5, 10, 15, 25, 50 and 100 Oe. During the process
of cooling, the magnetisation of the specimen I t was
measured at intermediate temperatures whereby the last
value of I was determined at room temperature. Then
the orientatins field was removed and at room temperature
the thermo-residual magnetisation and the thermo-
coercive force were measured and, following that, the
stability of the thermo-residual maenetisation of the
specimens was evaluated. For eliminating relatively
laPge changes in the magnetic properties of the investi-
gated specimens caused by the heating, the average values
of the normal magnetir@ation at roomtemperature prior to
and after heating were taken. The magnetic character-
istics relatine to the specimens cut in the direction of
the layers are denoted in the text and in Lhe graphs by
the index it , whilst those relatin., to the transverse
specimens are denoted by the index = . The measured
uard3/6 results are reproduced in the graphs, Figures 1-14. It

SOV/49-58-8-4/17
Normal Magnetisation and Thermo-rzgnetisation of Anisotropic Rocks
was found that if the layers of the disturbing, layered,
ferromagnetic body are distributed in the direction
perpendicular to the vector of the total magnetic field,
then (due to the large de-maEnetisation factor) the body
will hardly be magnetised at all in the direction of the
field; the vector of the inductive and the residual
magnetisation will be very small. The magnetic anomaly
will manifest itself very little, in spite of the high
percentage of magnetite content of the rock. If the
same body (or a similar body with an equal content of
magnetite) is located in the direction of the vector
of the total magnetic field, the inductive and residual
magnetisation will increase considerably, which will bring.
about an increase in the intensity of the magnetic anomaly.
This is the picture of the process of magnetisation of anan-
isotropic, layered rock if the formation of the ferro-
magnetic rock takes place without the effect of temperature.
If it is assumed that the rock formation takes place under
conditions of thermo-magnetisation, the decrease of the
temperature from the Curie point to the temperature at
which the body is at present will cause an intensive
Card4/6

SOV/49-58-8-4/17
Diormal Magnetisation and Thermo-magnetisation of Anisotropic Rocks
increase in the magnetisation both-Parallel and transverse
to the layering, as aRn be seen from the described
experimentaJ, results. Consequently, in this case, the
residual maf;netisation will manifest itself also in the
direction porpendicular to the layering if the layers
were in the direction transverse to the magnetising field
during a relatively intensive magnetisation in the longi-
tudinal direction of the layers. Therefore, it can be
assumed that the total magnetisation of the rock will be
in an oblique direction, in which case it is to be
anticipated that the disturbing body will form a more
complex magnetic field. The magnetic stability of the
rocks cannot be expressed by a single parameter but by
several, each of whicb is linked with the geological
conditions of formation of the residual magnetisation.
Thermo-magnetisation of anisotropic rocks brings about a
considerable increase in the mgnetic values. This
increase of the magnetisation in the transverse direction
of the ferromagnetic layers during thermo-magnetisation
can be so intensive that it can exceed the residual
Card5/6 magnetisation of the anisotropic rock along the lagers

SOV/49-58-8-4/17
Normal Magnetisation and Thermo-magnetisation of Anisotropic Rocks
produced by isothermal magnetisation. This brings about a
relatively complex distribution of the residual magnetis-
ation in the anisotropic rock and, consequently, complicate5
,the magnetic field above the disturbing body.
There are 14 figures and 12 references, 1 of which is
English and 11 Soviet.
ASSOCIATION: Akademija nauk SSSR Institut fiziki Zemli
(Ac-Se-USSR,Institute of Terrestrial Physics)
SUBMITTED: May 282 1957
Uard6/6 I. Rock--Magnetic properties

052U 71

.9(3.9). 24(1)
AUTIWR# Sakolows, Ye.3.9 Candidate of Technical Sciences
TTTLN, A 3-iontiti- C--f*@--- -0 the k"lle-ti-ft or Ult---4 in the
Investigation, of Matter
FW6VjCjLs lov..Uys, e7..hM chebrkh saadenty, Itd1.t.khnlk%,. 1959, Yet
2, W, 3, P 336
ADSrRACTs rrum'Fobroary 10-14. 1950. the 3-*.th Scientift. Conference
the Application, or Ultrimmand to, the f %letter
go.e convemood in Mosove at the U..k-.kiy ObI.at'..7 p.&C.9ib se-
kly InstituL& Inset MAC. Kmpok*7 (Uoscow Oblast PedsCogical Imatt-
totta, tonsil N.r- Trupshaq.). About 800 - imastruct.r. free W-o-.
Lowlag-4, Xm.ay.-!L, Kameas, Stalingrad and scientists from the
;e
icipt*d in the cents-
Oarsman Democratic Republic and Poland pa
essm vork. More than 80 papers were read at the couter 6
=:*Th

conferences 1 -14
r
following mactions vers org=izod at this
--ii.s, t.@bmtri.l application, or ultrasound research -thads,
propagation of ultrasound In solid bodies, dan@omatmtlsm of

i
tical pbsoomems. in ..beat. and -... At the firet. pt*-"7
::"
I
Curd 1/3 the paper or v.r. Soadrow "a read *Physical Principles of T

Lou at Low-A=plituds Molecular A-tic... B.D.
Indryawto,r, read his paper "be Appli;atim or Ultrasound In Is-
4-t'7'- Th. p-,, - ser. .ad at the pI ... ry
4 Vo,e Vi.:@ rate. is Rarorl am...;
@
7
z.=s
z:..."ic Republic, @Ultrsscxila Zmoott,
%I- at Bills. Got -M It.Vortvatives-1 V. 1- , Pol"d, -Th.

"it=
t the Molecular IrAnowatic Theory of rose& to the prob-
I.
t
:.
Of 1k, .1th a Limited A.,,Iit.d.-; X.X,.A:X!ux. -the TI-ry
at 2ua-h6II-t7p- Salta-, and . -p- of Professor P. Kocher, Pat-
and. Rms"mh in the field of ultrasound wavo propagation in It-
q.14. - the subject or the p.;." of D.B. IW&Y--t.@. S.A@ list-
I", O.A. V.U. Zml@-amavj. T.U. TA.,r,-
"
O
g
@
ras,t.
.
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I
irkstch, L.F. Yotosbcb jim,N.L. Oryulthetava, L@d
N.A. Golossom-The paper J*IvtlY produced oy D.a. Kndryavt-, V.P.,

7
li
N"Arow, 9.1 X- h - end V.P. Tak-lev va, levot.d to the co.-
:
.4deratim i pr
b
l
in the development of oolocular acaustic4.
Dr. R*Lbrd d.lie.r-d . report - the dyn"j. qultl- of the
state or strongly i-c coa liquids . Th. ultr=c oscillations
Card 213 o.r. subject of the Ireport. of To.W. Dystrov, L.N. Trotim-, A.t.

Rynasawe, L.B. Pir-Immilkaw, L.P. L.P..41c, P.L. lk.hLo, I.L. Char-
shmake and t@.". Th. report of L.A. A.T.
-d *the,. dealt vith the applic.ti- of ultrasound In ,Id-
sw.
.
tag. In the actions of .'-ti. re ... r.h the paper. at

"
the r.21-Ing ..the- or d, T.Lorl."
.
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:

N eith put .. ..... .
rt
d.
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Upir and ..
A.D. Th ..
Lag .th.d. or ol-Ity -4 ah-ption of eltra.van4. Th. props-
Asti" of ultrasound to solid bodies -. the ..bj.zt of the report.
f 1-0. Morklow, Y.S. Cb.rk-his, L.A. Y.U-Ise, A.I. Dr.kl., A.K.
*
U.t,.y- and others. to the -tica dealing Itb -ocotic.l d--
stratlon at school& &" vuem, the folloviog reports vort deliver-
Gov.sly and Tp.1w, DomanstrLtion
.d. F,
or tnsma Doommatration at
"
Somod-I I.N. Ir A.0%StIc R"i-.L*r far Docamet-ti.%
Cmr4 3/3 Purp as annual conference convened at IMPT ah-d the ris-
lag =*".& in problems. of applyUS ultro.own4 to the
uns or setter. The onsober of particip=tn and the onobar of Ash-
mumamot April 13, 1969 jo.t. 1. ri.1.9 steadily.

22(l)
r,
G(Al /4 59- 3-41/53
AUTHOR: Grabovskiy ML. A.
'17rbblom Of thE! "Dead Loop"
TITLE: Imen - oil @he
PERIODICAL: Fizika v shkole, 'Ir 3, pp 93-95 (USSR)
ABSTRACT! The author propo-os a new rnethod to approach the
"t@
iead loop" in physics lessons.
problem of the
Nearly all ph ir.-Ji-cs u'-orkbooks contain the following
problem: rroma which height must a carriage roll down
an incl-ne-d tli,-it it will describe the "dead
loop" Without falliji-, frora the highest poiht? Often
@Llie problem ic solveci b,r explaining the phenomenon
L,@@ (bic to force. The author, however,
tak-;:; anothor nr-p@@c@@-tr-,h tjhich can be summarized as
folioz,,S: the of an object along the "dead
loop" can be conoidar@@,d as the movement of a body
fluur, .,;ith initir@i speed at an angle against the ho-
L)
Card 1/2 rinon, bnt comrlic-i-tod by the uninterrupted action

SOV/47-59-3-41/53
Comment on 'Uhe Problem of t1it, "De.-id Loop"
of Lho doformod ori it, i.o. as the case of a
1;0@@-"- 111,0vin(7 an a;3ALned way. Tbe author neg-
ieo.to, fric-.ion. For experiments, UD.(.,refore, he
rll@coca,uwnds Wio of special carriages, the
mass of which io mainly concentrated in the body,
whereas tha riass of the wheels can be neglected.
There are 5 dincrarns.
ASSOCIATION; YGU, 1.'Io-,kva (LGu, J.@Oscovl)
Card 2/2

8/049/60/000/03/016/019
AUTHORS i Brodslays. 8.1u. and QrQM":g 1131/2691
TITLB-. One of the Causes of.Dlicropancy Between the Vector of Reasnent
Magnetization of. Rackm and the Direction of the Magnetizing Field
PUIODICU ilivestila Akedwil asuk SSSR. Serlys geofisicheskaya, 1960, Ir 3,
PP 4,90-494 (USSR)
ABSTRAM The authors were inytatigating the direction of preswt or past
magnetizing field I Ja'relatlon to the ramnent magnetization I.
in rocks. Their method -of investiVation is illustrated in
Figs ls 2 and 3, They found that the Tootor of roment napetIm
In the anisotropic rooks alsays diff ared frca tbat of the magnetizing
field. In the case ihere the present magnetizing field was found
to be perpendicular to the rock: stratification, the vector@ of
remnqnt magnetizatica of rock: samples, more parallel to the rook
stratification, alth(ugh they might be In two opposite directions
Card 1/2

8/049/60/000/03/016/019
213"691
One of the Causes of Discrepancy B*Wem the V*ctor of Ramnent Magnetization
of Rocks and the Direction of the Magnetizing Field
(Fig 4). It was fommid tb^+. the discrepancy between the two
vectors I and In In the anisotrepic rocks could also occur during
magnetization in low t4aperstares. Aeknowledynents are expressed
to NJ, Talklik for his assistance. There are 4 figures, 2 tables
and 17 references, 10 of ihich are Soviet, 5 English and 2 French.
ASSOCUT1(N4Wtwiy& nauk SSSR. institut fisiki zomil (Academy of Sciences USSR,
Institute of Physics of the Barth)
SUWTMs July 22. 1959
Card 2/2

GRAWVSKIY. M.A.: KLMNIN, H.V.; US&GIN, S.I.
Description of the physics auditoriums and the laborator7
for pbysics demonstrations at Moscow State University. Usp.
,fix.nauk 71 no-3:515--524 JI 160. (MM 13:7)
(Moscow--Physice-Study and teaching)
41

S/05 60/071/004/005/005/XX
Boo6yBo67
AUTHORS: Grabovskiy, M. A. and.Yegorov, V. S.
TITLE: Some Experiments on the Topio "Rotational Motion"
PERIODICAL: Uspekhi fizichaskikh nauk, 1960, Vol. 71, No. 4, pp. 677-680
TEXT: The authors describe some demonstration experiments for physics
classes of demonstrating some rules governing the rotational motion.
The first device which is described is a cylindrical double spiral which
is perpendicularly fitted onto a stand and which can rotate about its
longitudinal axis. The instrument shown in Fig. 1 (photograph) is
1.1 m high, and the distance between the two-windings is 55 mm. The two
spirals form rails on which a metal or wooden sphere may roll. The
uppermost part which is called the "accelerating part" is designed in
such a way that the sphere is supported by the lower rail; as soon as
the speed of the sphere is high enough it rolls downward on the rails
which are nowlying on the waj,? of the cylinder ("perpendicular part of
the winding") (see Fig. 2). With this device a demonstration of the
rolling of the sphere on the perpendicular winding with braked rotation
Card 1/2

.GRAWVSKIY. M.A.: ZRZE=O. O.N..; SKODORODKIN, Tu.P.
Possible use of magnetic powder in studying the com-
position of Iron ores. Isv.41 SSSR.Ser.geofix. no-7:
970-973 J1 160- (KIU 13'- 7)
1. Akadenlya nauk SSSR, Institut fiziki leall.
(Iron ores-PAgnatic properties)
(Ores-Sampling and estimation)

B/053/60/071/03/05/008
B0061BO63
AUTHORS3 Grabovski4, M. A99 Malining M. V I usaginj S. 1.
TITLEs The Lecture Rooms and the Demonstration Rooms for Physics
of Moscow State University
PEhIODICALs Uspekhi fizichoskikh nauk, 1960, Vol- 71, No. 3, PP- 515-524
TEXT: The article gives a description of the lecture rooms and the de-
monstration rooms InAhe new building of the fizicheskiy fakulftet-MGU
(Department of Physics of Moscow State University) and briefly deals with
the teaching and research program. The new building stands on the, Lenin
2
Hills and covers an area of 28,000 m . Its front has a length of 228 m.
On the sides of the main entrance th 'ere are two statues representing'@he
famous Russian physicists A. G. Stoletov and P. N. Lebedev. Besides
numerous laboratories, rooms for practical work, and a library, the
building has three large physical ledture rooms and demonstration rooms.
Elevation and ground plan of these rooms are shown in Figs. 1 and 2. The
central auditorium is 21.6 m long, 18 m wide, and 11.4 m high. The two
Card 1/2

The Lecture Rooms and the Demonstration Rooms S/053/60/071/03/05/008
for Physics of Moscow-State University B006/BO63
2
side walls have six windows each, with a total area of 83 m The equipment
;.:f the rooms is described in detail. Fig. 3 shows the two desks, the black-
board, and the projection screen. The doors open into the demonstration
rooms. The central auaitorium has 530 seats, and the two side rooms (north
and south) 300 each. A partial view of one of the demonstration rooms is
shown in Fig. 4. The apparatus and objects for demonstration were collected
and arranged by N. A. Lyubimovq A. G. Stoletov, N. A. Umov, I. F. Usagin,
S. I. Vavilov, G. S. Landsberg, V. G.Tikhonov, M. V. Kolbanov,
A. B. Mlodzeyevskiy et al. At present, the demonstration rooms h ve 1795
instruments. The building also contains a workshop covering 30 m . The final
part of the present paper is devoted to problems of organization, teaching,
and teaching methods at the demonstration rooms which are administered by
the kafedra obshchey fiziki (,Chair of General Physics).'The curriculum
includes courses, lectures, and practical training. The following persons
are mentioned in this connections A. B. Mlodzeyevskiy (deceased),
M. A. Grabovskiy, S. I. Usagin, Prof essors.K. P. Yakovlev, K. F. Teodorchik,
S. E. Khaykin, S. G. Kalashnikov, V. I. Iveronova, S. P. Strelkov,
R. V. Telesnin, I. K. Kikoin, and I. A. Yakovlev. There are 4 figures.
Card 2/2

GRKWVSKIY, M.A.; YEGOROT, V.S.
4 few experimquts In rotary motion. Usp.fiz.nauk 71 no.4:
677-68o Ag 6o. (HIM 13:8)
- (Rotating bodies)

GRABOVSKIY, M.A.; ZHMWNKO, O.N.-, SKOVORODKIM, Yu.P.
Possibility of the use of magnetic powders in the investigation of
pyrrhotite ores. Izv.AN SSSR.Ser.geofiz. no.5:737-743 Yq 161.
(.KM 14:4)
1. Akademiya nauk SSSR, Institut fiziki Zemli.
(Pyrrhotite--Magnetic properties) (Mineralogy, Determinative)

BRODSKAYA, SJU.; MIABOVSKIY, N.A.
Study of magnetizatigp processes in one-component and two-component
ferromagnetio systems# Izv, AN SSSR. Ser. geofiz. no.811158-1170
Ag 161. (MM 14-7)
1. Akademiya nauk SSSR, Institut fiziki Zemli.
(Forromagnatism)

BRODSKAYA, S.Yu.j GRABOVSKIY2 M.A.
Magnetic stability of single-component and two-component
artificial systems, Izv. AN SSSR. Ser. geofiz. wol:54=66
Ja 762. (MIRA 115:2)
1. AN SSSRV Institut fiziki Zemll.
(Rocka-41agnetic properties)

GOABOVSKII, M.A.; ZHEMNKO, P.N.
r-------------
Using the magnetic pattern method for studying ore minerala.
Geol.rud.mestorq$h. .5 no.109-104 -Ta-F 163. (MMA 16-. 3)
1. Musey semlevedenlya Moskovskogo gosudarstvennogo universiteta
i kafedra obahchey fisiki fizicheskogo fakullteta Moskovskogo
gosudarstvannogo-univerniteta.
(Mineralogy, Determinative)

IVERONOVA, V.I., prof., red.;.XAR4
@ _.Q
M.A., dots., red.;
KONONKOVI A.F., kand. fiz.-mate. nauk,' red.; MAIDV, N.N.p
prof., red.; TELESHIN, RaV.) prof., red.; USAGIN, S.I.,
at. prepod.p red.; YAKOVLEV, K.P., prof., red.; YAKOVLEV,
I.A., prof., red.
[Methodology and technique of lecture demonstrations in
physics; transactions] Metodika i tekhnika lektsionrqkh
demonstratsii po, fizike; sbornik trudov. Moskva, Izd-vo
Mosk. univ., 1964. 280 p. (MIRA 17:5)
1. Mezhv-uzovskaya konferentsiya po demonstra-
t.siyam po kursu obshchey fiziki. Isi.

air -ural P,
Dorn. , aLruchrre of mat pyrrhotL
M@URCE;- IVUZ. FitUa. ma. 4, IM4. 27- 34
;rO-PIC T.4,aS. demiain atru-cftre. pyrThvtMe, cry-.3tal
JA.A,'1i-RACIA* Results eve given -,i of deazwn by the
I-.ttc-.-Ak,jIc-t figure-5 -yn crysX=25 cf notunil pvy-rhr-.t4mcI 17, 1 e
4,Q _A I y -1
urvrj a4-re o-baAiryed on vA-, t 7 4

jgl;wl r4imi
VOL6" tit
fir-,-re@s A,f
A r
1L am , "@=-, .--
7 @340-
"i Zvi,

7-7

GRABOVSKIYI_.@@,A@tj. ZHERDINKO., O.N.
Domain structure of the pyrrhotites of different genesis. Geol-
rud. mestorozho 6 no.300-97- My--Je 164 (MIRA 18A)
1. Muzey zemlevedeniya Nloskovskogo gosudars'Orennogo imiversitetu
i Kafedry obshchey flziki fizicheskogo fakullteta Moskovskoga
gosudarstvennogo universiteta.

ORABOVSKIYp N,A.; GREMU, R,Kh.; METALINIKOV, A.P.
Some geomorphological characteristics of the bottom relief of the
Atlantic Ocean along the 30th meridian from the Arctic Circle to
the Tropic of Capricorn. Okeanologiia 1 no-5:860-865 '61.
(MUU 15:3)
1. Kalingradskoye otdeleniye Morskogo gidrofizicheskogo instituta,
AN SSSR.
(Atlantic Ocean--Submarine topography)
X

GRABOVSKIY, N.A.
Geomorphological characteristics of the bottom relief in the north-
eastern Atlantic. Okeanologiia 2 no.1:92-97 162. (MIRA 15:2)
1. Kaliningradskoye otdeleniye Morskogo gidrofizicheskogo instituta.
(Atlantic Ocean--Submarine topography)

L 28508-66 EWT(1) GW
ACC HR:
-SOURCE - CODE: - --UR/0213/66/
.006/ F, 021
QW/M 51 9
AUTHOR: Graoovsk&2 N* As
ORG.- Kaliningrad Department of the InBtitute of Oceanographyt Ali 85SR
(Kalinrngrads5yj oiaeienlyeinstNuta okeanologii AN SSSR)
TITLE: Bottomi geomorphology in the region of the Newfoundland Grand Banks
SOURCE: Okeanologiyu, v. 6. no. 2# 1966p 285-293
TOPIC TAGS: 6c.ean floor topograpby, geomorphology, geopkysios, research ship,
ocean current
ABSTRACT: A goomorphic description is given of the relief of the Atlantic floor
in the 'Newfoundland region, as shown on maps prepared by the author. These are
based on a new bathymetric map of the nortwest Atlantic prepared by a group from
, AN SSS.R from data of
the Kaliningrad Department of the Institute of Oceano ran4y
marine navigation maps) domestic ctz@d -forolgn (18 8-1962). and also from recent data
of expeditionary ships.k Geologic structure is interpreted on the basis of geo-
physical studies, but the geomorphology also strongly reflects those structures,
The main divisions are the underwater margin of the continent (to 200 m), the tran-
sitional zone (200-4500 m), and the ocean platform (4500-5000 in and deeDer).. In
the marginal zone, the relief-producing agents are wave actionj tidal currentsp
and bottom currents# The transitional zone ranges from. 75 km in width at the south
C-A

p.,.polkovniky kand. voyennylch nauk
GRABO'VSKIY,,,.".-. - 180)
n. znan. 41 no.6s36-37 le t65. (MIRA
Mvigation on dry land- Voe

RISMAN, M*B* (Rysman M.B.1; BAKALOR, 14. Yu.,- SHKOLINIKOVA,, N.B. [Shkoll-
nykova, N.13.1 V A. (Hrabrvstkyip P.A.1
; -qm]R-M@p _ ?@@ -
Fusion sealing of seams and cuts on articles made from n7lon
fabrics, Leh. proirt,. no.201-52 Ap-Je'64 (MU 17 -.7)

G bO V S -K\@e)
1.
Meteorological Alint.
Vol. 5 No, 1
Jan- 1954
Aqueous Vapor aiul
Hydrometeors
5.1-217
Grnbovskil. P. 1. (horad), 0 ProleModdall stmoder"kk hj&r k$WMjL
-ricin 0A ntmn' )re i"@nsafion ni
r KkU -Pri-114, Moscow, No. IM41, Jan,
refq. flung1rian trans. Ift- lddjdr.ds, 57 (1).32-34, Jan./Feb. 19M D
Autijor nintle, a critical survey of hypotheses on the origin of condensation jiuclei an
0 an
I
111AI Ike "InAi milwirtaut cause may be. wa water spraying Into the air. Transfer cj ch
imiq filln Ilic atmosphere by spraying at least IS-10'- tons per annum. Back trander by,
prrripitation in form of,ccmdeusation nuclei only 1.4.1(P tons. Water low ofomns by Way.
il@g kill.)JIt I%(,( then .1 byevaporation. Subjedlreadings:I.CandensattansudeI 2.Sft-.
l1nPnucleI 3.Selts@t4r., I.Gelldri,Sindor(trant.).~-A.A.

GRABOVSKIY, P.m.
Accelerated diaghosis of acate dysenterv,by-the-mothod.of fluorescent
antibidies. Lab.delo 7 no-9:38@-42 S 161. (MIRA 14:10)
1. Kafedra mikrobiologii (zav. - prof. M.N.Fisher) Loningradskogo
sanitarno-gigiyenicheskogo meditsinskogo Wtttuta.
(DYSMERY-DIAGNOS IS) (ANTIGFM AND ANTIBODIES)
(FLUORESCENCE)

GRABOVSKIY, P.M.
Serological diagnosis of acute dysentery bymeans of a fluorescent
antAbody method. Zhur.ITikrobiol,oid,i immun. 32 no.2:3-6 F'161.
(MM 1A:6)
1, Iz kafedry mikrobiologii.Leningradskogo sanitaxno-gigiyeniche-
skogo moditainakogo inatituta.
(DYSENT-M-)

GRABOVSKIY, P.M.
Speciricity and sensitivl*Py of "he Indirect fluoreacent antibody
I
nx-thod. Trudy LSGMI 66t-120-123 62.
Use of fluorescent sera in the diagnosis of acute dysentery.
Ibid.:124-12')
Study of paraetraino of' intestinal microflora by the indirect
fluorescent antibody m, thc/d. lbid.i130-134 (MA 17-14)
.@afedra ir-lkrobiologii Leningradskogo sanitarno-4glycnicheskogo
meditsinskoge, instituta (zav. kafadroy - prof. M.N,Fisher),

P.P.. red.; WXIMTTY, YevGo, tek@nored,
health in the Ukrainian S-8.1a; a statistical mauuall
Zdravookhronente-v USSR:,statistichookii spravochnik. Kiev, Go*.
md.isd-vo UM, 1957. 139 P- (MIRA 11:4)
1, Ukraine. Ukrainskoye nauchno-issledovatelokcqe byuro
sanitarnoy statistiki.

GRA.BOVSKIYP P.P. (YJyev)
Some characteristics of health statistics in the People's Republic
of Bulgatia. Sovl.zch-av. 20,no.3-ls94-96 161. (RIM 14.12)
1. Iz.Otdela organiz4taii zdravookhraneniya Ukrainskogo nauchno-
issledovateliskogo instituta kowunal Inoy gigiyeny.
(BU14LUA-PUBLIG HEALTH-'-STATISTIC9)

GRABOVSKIYY P.P. (Kiyev)
Validity of selection in the processing of data on disease incidence.
Gig. i san. 26 no.8:93-96 Ag t6l. (MI-RA 15:4)
(DISEASES-REPORTING)

GIRABOVSKIY, P.P. (Kiyev)
Nev data on the method of studying population morbidity,- materials
of the Fourth Session of the Semashko Institute of Public Health
Organization and-Medica.1 History. Vrach. delo 4:126-127 Ap 162.
(W-A 15- 5)
(M-DICAL STATISTICS)

RZANSKAYA, A.M.; GRABDVSUY.. P.P. (Kiyev)
--l- --- i-.- -,
Some problems of rural public health service .' 'n the ALUarim
People's Republic. Vrach. delo no.9:122-124 S;63.
lum 16tio)
1. Otdel organizataii zdravookhraneniya (--ave - CI.M.Zelezinakaya)
Ukrainskogo nauch-no-issledovateliskogo instituta kcamunallnoy
gigiyeny. (BULGARU-PUBLIC HEALTH, RURAL)

meteorological Abet.. 4 351-574.1

@ol. 4 No. 2 ,

Gr, iL_L_I.p Mirovoi okean kak ietochnik atmos
Feb. 1953@. fernykh isder kondensataii.'- [The @world ocean as a source
AOeous Vapor.and of condeneationnuelgi, Akademiia Nauk SSSA, Izvestiiaq
Hydrometeore @eof#jchgakaa, 206-74, 1952. 2 figs. P 5-t-affe-s;
36 eqo. DLO-The various hypotheses concerned with the
origin of atmospheric condensation nuclei namely Us
continental, cosmic and marine hypotheses are discussed
critically.- A thorough analysis is made of th@ marine
hypothesis which attributea the origin of atmospheric
condensation nuclei to the action of wind upon the sea
surface and the resulting spray formation. An
approximate calculation of the annual ammount of salt
entering the atmosphere from the sea surface in made and
the quantity of chlorides removed from the atmosphere
in the form of condensation nuclei of precipitatioix is
estImated. Conclusive evidence is presented indicating
thl It spray from sea water plays a fundamental role in
M'salt balance of the earth and is the source of
condensation nuclei. Subject Headinget 1. Condensation
nuclei 2. Sea spray 3. Chloride content of air.-I
2:kA"&)

Waabinxof th*chlorides tT-im the 4tm rspherc by metcor-
Olopall 7171-AFF. 1.
7
(IMIJ.-It LS PTOVE4 mathtrllatl@:ajty 11,at irom 16-3 1. of
air ",=t" out try a ',O-ntg. min drnp faLuig frazu the height
of I km. caly 0.012 cc. is actu@llv --ui,t Ni fmc d -hlGri&s.
Two nethods of cR!cns. are used: otteimolvinggmVitational
ccuplation of aeroA with the niun drop. the other, coagu-
latkmt caused by the Browitfim mmticn. These "Ims Are
ba-sec an (be MhurliptiO115 thtLt t Ile Mfl.'@J (ii icn@nl t hrejugh-
out I km. tayer of air is 10*.cm. @4 amd tim m-itznt A cto-A
:4 taica as satd. soln. of MaCl. Orly aerosol pirtides with
radius> 10-4 zm. man be- efflcieudy -L-shr-3 out hy pietecrl-
A P K,,,!o@,v

-3Rk30-vSKId;, R.
GraboypzIcii-, R.
"Proce3s of atmospheric nucleation." P. 32.
(Idoiaras. Vol. 57, no. 1, Jan./Feb. 1953, Budapost.)
SO: i-:Inth1v LiA of East Suronean Vol, 2, No. 9, Library of Congress, September
1953, Uncl.

GR,A-F.CVSKIY, R. I., MIDTIATIYEll, K. Ya., and SELEEZILOVA, Ye. S.
AM__@@Ww
"Pavel l1kolayevich Tverskcy, 11 Meteorol. i gidrologiya, E0 1, 1953, PP 59-60
Cn the occasion of the 60th birthday of the well kno-"M Soviet meteorologist and
geophysicist, Prof. P. N. Tverskoy, Doctor of Physicomathematical -Sciences and head
of the Chair of the Physics of the Atmosphere in Leningrad University. WhGeol,
1.
-io 5, 1954)
SO: Sum. No 568, 6 Jul 55

: If I
- )"ein of ;,tin@ngpimsdc , . .. - 1 " C ,,I
.L &A rnv=--T,@z 7Z @
- I- I R- 'A' I
@-, -I,,--- X
.I.i. "

3*7
Gt-.ihn%-,W, 1; -Ob obt 41.1akav-4-Millcisf,pirny"
1@ 6:1
(if clum!"i Ow n flUir tk-.mrilx.@ pqiA'.@Wv t., 1 11 1 1 1" ,1 'd i 1!@ I It,,
311til"O involvitig the rciafluv@iihip 'i pri-,mm'I d1i 'i ... . ..... ... ltrjti-, -d
plicric chttlrld'@ with the cut"'Ponding- increa-, iti "!@. j"I
a 111tiv,11g, Sliffne att.'I'dwil to lit airplaile. lltiot 44-% i. t- i - @!t
all'113'6 (if t@'I Ofariec (yint-elt iruric-It out I'v thc alitil"ir .11 Iliz. ni, r-it'. 'd
IA. 8 Xj@ sim"Pa nt the C'..Titral Avr@,,Itq K'st,-c it 1-1111'riOu (1111
gic@1104-,''rv'@tlffv
01,63 Ingnitt'-, alic: vii nignare refir"-fi-th'. li'l
!wr-,icvq
vorde-ari'm lit, t., it fit&l;'
am! 6z'@ I -P@iz
z4wamy
C.07 J NY)O-If-0

TVERSKOY, P.N., redaktor; TIASOVA, Tu.T.,
redaktorl FIAUK. M.Ya., tokhnicheakiy redaktor
(Condensation nuclei In the atmosphere] Atmosfernye ladre dondensatelt.
Pod red..P.N.Tyerokcigo. Laningrado Gidrometeorologichookoe izd-vo,
1956. 163 p. (KWA 1,0,: 1)
(Atmospheric nucleation)

GRABOVSKIY, R. I.
T- ' -- ,-- .--
- Atmospheric condensation nuclei. (In Russian).
Len'lngrad,, Gidrometeoizdat,, 1956., 364 P-j 43 figs., num., tables, bibl.

GRABOVSKIY, Rostislav Ivanovich; IVANOV, I.A.,, red..
-1 -., -, - 1. 1 -1 ..... .@. 4:- - ! @ I ;-- - -
[PIWsics course for agricultural institutes] Kurs fiziki
dlia sel'skokhoziaistvennykh institutov. Moskva,, Vysshaia
shkola, 1963. 525 P. (MIRA 17:6)

IGRABOVSK ,A._bnd.tekh;a.naWc; JOFFINAI E.M,, starshiy inzh.;
NOVIKOVA, A.I., naadshiy nauchnyy sotrudnik; SKOMMOVA, V.M.,
mladshiy nauchnyy sotrudnik
Intensification of -the clarification of sulfite liquors in the
causticizing shops of sulfate pulp factorie's. Trudy LTITSBP
no.11:73-182 162. * (MIRA 16:10)

I lisle ?I UJINAMPAmill))l AID xxv mg mixg a) U41 "evre
Y -1 AA 00 CC PP U I d. s -A, go
f5 VV S
O
P11
Test* of the villictianked PrOP-08% at P
klyskif and H. 14ma. .1141-1-1i.f
""Mm lft@(. Fz,11V4t-.1vR11I I'F- ( I'MM3.
.1 jj.f'ftjja &t. jVfjj"h lft@t 1'.IfW, I tqLj I
-

: ,'A. A
tail. N.. 4. .41
ll
t
d
t
a
0 1-
at
iog
mn, llrili,h avid CwTvirween slan'
Ch- 111mw

'
4
0
r
4

oil
zoo

e*
-4 Ipw
ti
Ai. It . 't si h A I H,. I
"oo

ti
I
-
-
-
' 1
, IF I
h
@ -
S V tie
A
-
;00
% '
1@

u s It it it "
It '
0 4
vir 8
I
i
as
4
T
I : a
n 1
11
1114.
0 0 a 0 0 0 0 0 0 0 0 o 0 * 0 0 We 0 0
0 0 0 0 0 0 0 0 0 6.0 4 We 0 0 0 41 41 0 0 0 0 oi

a u is is I? is of it N a it n v W"m
11 H"a eu .40 -101,
1. 11P go u
1_1 j M 0 cc 99 U
lit jw mIt"
IN
00 c
00
Do
a Ui
00
-,! "
-----------------------------------------
a I, u 0 m is m v a o a a 4
I -f k A 4
B ""Amy*
%m d Vwww cum CSAS. PLANC
:
0: ledwy pro"
0 31 jij I
00,21 111
00
os
A S I L & MOTALLON"AL LITERAltdo CLAHVICAT"
*7-'-":L--- =7:::: 4
00
Lo 0
a**
0
1,00
ivoo
'00
A 0
u I AV 4) is I a tw 0 1 w so 5 fia a 3 6 1
0 o :1* 0, 0 0 10 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
-To 0

I N 11 v m ]d is m 11 111 Do a 41 a 43 a goo
I 1 0 Is 11 13 it M, 11 11 11 1" it,
A I-L-A-A-L A m L-A-A. 0 1 3, VP 911 1 1
00 so
00 .00
uduzative 01 lop brimbes in paper mclux".
00 9 v P4. 1-1,
ItWerialmi (Cestral Nd. Rww(h
4@4
Imil. Pdpff Ind. Traps.) 1933, No, 4, NV
Sulfate Pulphip 44 gralvvint twit"ch" vj,+1, a P.@l emda. -00
V4 Wimpping PatwT atul. whr" 14,401"J"441w MmOml .00
of palwt. likew
.00
00 &
moo
00,3
oo
oq '00
o4b i:j
06 '00
-- 'KA
'00
!AO
LITIMATUNE CLASUPICATION UO
"all too
4ir qmv 441 ak q..
t
u IV 10 All; PA t I a W
to I , 1% P
-01 Y-90,0121010y, it
0 0!404*000600000060900

0 0 0 0 0 0 0 0 0 0 6 0 0 Wo 0.0: 0 0 o It 0 6 0 0 0
is If mIs 16 it 4 it, n a Ifa U" "'04 41 ou 66 one
Ott 0
.6'et."'t
----- -- - --
it]
00 C
.00
00
z: P. V. svmmbw um I
-V7 ma P,
SO a IDA.
ifapd" 16^'No. 2. U-ST.-A p. lips new
w Surva Ile
40 6.1m W'. waity with 116. 4
0-nd jslqmk@. = 9= Mwf was obtalmd
in dw bb. bg *AM 11" bIA144cotbed "te pulp of me*
fillinut 40
"s bwimm md 46 framemetar" by 'b %
C
-3 Wds md bwor Ada-
Z9
ice*
Iv
see
1A4
t:o 0
Do'
be
00 0
.4'sil Ui
u 00 is:$ goo
0 fO' 19 0 K 6 4 Of Ill IT It C9 It Of 1140 4 1 l"4 AM L Ia w 0 W In 0
0@0 0 * 0 0 0 0 0 0 & * 0 4 0 a 0 0
:!0 0 0 as 0000000000000
-15TS:0 : 0 0 10000000000000000006:0*000000000000000::i

i*0 000*000 00*0 K 1. .
tio 00*00000000000 IV-1-75-0-IN @--. 1 0 0 0 d 0 0 0
03 5 6 1 1 1 a if ti U Is Is It IF It it a ]I a a to a v A x 11 32 a 38 Is a 0 a IN 0 14 a a a 4
06' JL 8 C 0 1 9 L- a 2 1 1 IS L-,A- . . .1-
, 0 1 z id as cr, go off, I , J . A
A.0 06018% C&2(6%
FOOCISSI-S Afto P.CPWICS '%W.
00 J,
=*dMom. Tedowiladeol part. v iT and
ov. Two&d. .-Its test.
V. Munt Aycock '.
00 Buna"g Prime. Makridai 19M. No. 3. 3-O.-Refined
tai , obta W the productim of spatite by
0
notatke of belite-a the depopits, when treated an a
COMM. th 2 N H for I hr. in the cold by the .00
M"bod of ShumMov (C. A. U. M819, MOO) yiekled 17-
I too of dry, Wgb-rwk belit tadinpl
1=11i.33 tower otendard=ZI). tg.
X
00 13.5% At^. The pro- list! congmunpumn of HISO, is at S gas
rate of 0.9 ton of 1 111901 Our I too of tailings. The
00 '3 sabstitation of = oulfitte fiquor for econ-AWSO.).
40 an eq@W bam is uted *quay good P 900
resigill. The promW=wW== in a* Aug paper
00 with the addo. of I Alg(00.). decreased to 769'0 of so*
00 the viormal most be wolknoil by hday practice. The
km ccate of loetallation wol operittlot; of sepbelite exin.
with HAOt fully compel to for the high cad of trans- r.0 0
Partation of t"Ings mW 119SO.. wW renders the wv of 0
nelthelite comm"C"Y feasible. Ch". alluse
too
too
0
"o
------ boo
AIII-SLA INITALUINGICAL U11014710119 CLAWFICAITION
boo
it OONIIIV
lotusj "to P,, 4dr- fill 11 Ovt t@
100119 --Ir I I-- -.- -.-- 66"i, - -'W' ,
It is I I v ed o a a I to 0 'j a 1 3 1 9
* S ; a It * It it I't "t "W 6 1 'Is
0 & 0 0 0 0 0 0 0 0 0 VO 0 0 0 0 0 * 0 0 0 0 0 9 0 0 0 0 9
*it 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 19,0 0 0 q 0 0 o o 0 o 0 q 0 6 0

41611916118141 w 11 1& f, is R .0 V n a )d A M 17 aIt U Is Id 0 IF w x x A 41 41 4ar4-
M, If Q I A @ 1 9 Il, t- I I I OA 0 " LO It
4 k
Kolbods ad 41 pw ow the
Pop 1001P6
1". BummAnd Fma. AtOW6" 190, No. 1, 1".-
00
of the mdb" of Aims t , of pop"
with WWW" Itints" 1@w tin I in of paw top
*0
with w6ciest darms of vater- and mk4apermability.
Elm impregnalbin wkb molm. of bitumm Is wimirral ods
*0 (prefuramy in awn is the Most satimls"Gry. Mists. of
aqwpwisdbk~maodegaivetbetwmnwAts. Ttw
00 .00
sea in to the I" of paw. Arm 2540 bitunta to
U410% :r=* 2%,
la beg imprepated b a mist. at
1000 in The mim NUNN at a rate of 63 M./min. with
@the dryieg rolls bated with stem at 2.8 aim. premye. r*0
About 3&-W% of the akt. of the wt. of And papa is
00 commomw is the procesm of Impragmadom. (m the papm
of md. the bat pactical remits woo obtaimed with the
too
Lumpregintloo of beg paper of OD g./sq. a. with On sk-
penvembility an gxxedkW 180 sq. ca. Vorion proce-
for isovelfivatim ad 9 ad am
dacrPird. Few be opdd popw-"g oullaimm. 0.
0.10&. bid.
I
e%prosive rimlaimm for the lmoqxw ation and stump of
-,99
votfi%" mattflaN poilkiskily ftilillm- *"it NeCl W ION.
I A Ia S t A 611ALLURGICAL LITERATI*( CLA$SjflCATfGN A
.36
t Was% S."#) -zo
A .1 -j An 1 001 0 1 IF 14 9 a 13 IF I
it m @10 A
u of 91 t? 1, 1.0 14 K It 11 0 tt It
: 0 o *.#, a * o o 0 0 0 0 0 0 9 9 0 0 0 0 0 9 0
0 000 00 0000 0 : : : 1*' 0 0 a 00 0 0 9 * 0 96 0000 0 :

I I 41t@f,wi#u' ll it d t is " x I it n a i. it v ji it r, v a w w e u o w ss
s L a L_ r__A J_ A_k a it U v i L -A I AA 14 (C IV, it
A
NNMILPWI Mp hopervion to Wat" and ale by-,
-
114 vft soulskas of b1twoess and aft

7 @Ar
b
"
d V
ki
;=:
V
r
so
ov
a
an
manskil.
z
.
. Va
als"Sh2fillat Prom
1faferwo0i
. .
ION, Not. 3-4, the lah, rxpts. the hest rc-
rAft in the prodwdon and un of Mable coacd, coubions
00
-
4 1 &W pusift weve obtained by the uw of hon:
0 to 10% of coin, stearin (asixts. of strark- ancl palmit6c
so wich) &a an emaWring agent, Vat of Mee envulsions
tx*wwMt dat"ard the ntcvh
mwilet of the requiting
**,1 .
W
b
h
M
1
bIl
1 conswera
IMAM
lu
l)p
111prrmtA
ity to
;Opw,
k is b
I
k
t
th
th
f
k
Th
t
0, xwom
wa
e.
e
o a
wer
an
a
o
mpov
p" dkwOy treated with bitutnen essuWarts stsbillred
with mimmal oils (avtol). No particular advantips In
f
W i
i
PaPW W"V RO
n treat
qa@ft O
ng PUIP for hnper.
meability as cam with a idtallar treatment o( Witted
goo
paW. In Um cows.-wale ezpts. the best resalts In the

preva. wd use of eandolons were obtained with tM aid of '00
the Hurell homogeedw. The biturnea4taolin etnulvineus
"VT 001"0 )ut may prove to be prac-
t
k
oe
t
*l
weawe of thv* town tt"t. No patticuW diff"Itles r

Chan, 111dow
I Zee
u's 0'
so
so
12*7koif CLASSWICA71CM
A' I I-1, stjA@WIGKAk kil t ts
is 16 t i
b u ti A* to is L 54 a w I w so 0 :t I
0 H a it It 0 it or it x $9 of tt rt It M i@w 1 ^3
40 : 0 : : : :;! 0 0 so 0 0 0 0 0 *0 0 0 : : :* : ::is 40411141141 000 0 0 a 0 6 ei
0 f*000000000000 0 411404141404110 ***6646661A

0000*0:0000
0 r _-- ill c
0000*0 9000 69
ID 11

8 C
9 1
'
is M 0 4 1? 0 a a 11 a a &I A a
a U
4
a O.-C

A- 11 _C-
f S X-1
A
A-M F, Q LIP 11
1 1,
.
.
.t
"Pt#0
JP9 a & I jj

I @ to
_
'. _ - , " I -- __ --_
- ,
JWW of the kind at Wood (Pia
exit4ft) go itike tuaity of 1P for cablo Papers.
V, Variltumskil. Tsaftal. X-A.-
00 -1ma. Pawaskovi Pr@. Alatorialmi 1033, No.
S. jf@ lb.-ftriwe and pint and mixts. of 'd 3% 51truct and
230% phtar *ad equal parts of sitnitm &ad pine were C1141110d
-90
in a 26-1. autoclave in 4CP- r-tai-n an,l pjjjp@d with 4
volt. of onin, (5070 bLick liquor of a definite tr-inpu.).
r* N
q
d
l
Oll (

,Me
ca
c
.w
a
N&01(. IN DWS and 7 5
(toiullmiiiitt from 4 fit,.
i
741 Irw I suit 2 Iw
L
.
an4 40 min. to 5 fitc) with Wwings at U111, mut GOV.
4 43
39
1 @e
f
.
.
or 4pruce.
tip yields were 41.4 -;; 2%.
lZe

j for
P
difficultly Pulped than 41nruce, giving 1-1.1170 l"wer ytehl,
er unit of tht
the
i
ld
i
f
d

r.
tte
e
. o
c of the greater
p
y
p
of the!'
const,
l
m
h
Tl
6 zoo
;J' .
e
icr
.
.
gfeater
autocla vecapacity
pr,Trtiv@ of pine pulp are
c rnft h
Th
.
pi
Sulfate Pultm of Pruev Art'i
I ruce
t= Of
f sp
tZ
4f .
g
l4wor thek mitts. mn be uwd for the prmhwiion.4,abl@
see
popm, thnush antler equal coralitions of Niping pint
MY" a harder prtAuct than does Spruce. Chat. Burt,
zoo
ARTALLUICKAL UJINAIV41 CLatsviciijoco
a"- j'@'_jj t 7 @. '7-
Flit
U 0 AT 10 It
o 0
00000 66000 09000 * 00 0 a
zoo
moo
009
too,
"J"' WOO
4on alwall'a
0 0 0 0 0 0 0
0
0 0 010 o 0 0 a 0
0 0 0 9 * 0 0 0 411

-GRABOVSKIYp V.A., kand.tekhn.nauk; NAWSTNIKOV, I.V., kand.tekhn.nauk
.Effect of pressure differences in the diffuser on the 6shing of
sulfate pulp. Trudy LTITSBP no.8:105-108 161. (MIRA 16:9)
(Woodpulp)

ALMKSBTW, A.A., Inzhener, redaktor; ASHKINAZI, K.M., doktor tekhni-
cheekikh nauk. redaktar; GRABOTSKIT Y.A. kandidat takhnichookikh
-- Mdlda,;,
nauk, redaktor: ODRBAUHM, takhnichaskikh nauk.
redaktor; IVANOT, S.N.. kandidat tekhnicheakikh nauk, redaktor;
LAPIN, P.S., kandidat tekhniaheekikh nauk, redaktor;
N.N., doktor tekhnicheakikh nauk, redaktor; FUZIEW, S.A.,
kandidat tekhnicbeekikh nauk, redaktor; JUU IN, N.V., kand-ldat
takhnicheakilifi nauk, redaktor; ILTATI, D.M., kandidat tekhnJL-
cbeeiikh nauk, redaktor; SHAPIRD, A.D.. immAidat tekhnicbeakikb
nank, rodaktor:XLIASFIBXRG, M.G., kandidat tekhnicheakikh natlic.
redaktor; KR=AEDVA, A.V., redaktor; VOLKHOnM. R.S.. tekhni-
cheskiy redaktor.
[Paper maker's handbook] Spravochnik bumzhnika (tekhnologs)
Moskva, Goolesbumisdat. Val. 1 1955. 790 P. (HIJU 8:10)
(Paper Industry)

6 VSKLY Y".14,
A X5273V, A.A., inzhiners rodaktor;ASHXINAZZ, X.M., doktor takhnichaski'911
nouko redaktor- ffRARQffjQr'j..", kandidat takhatcloskikh nauk,
redaktor; GORBACHIIT@ AJL-@- @n@t takhnichoskikh nauk, redaktor:
IVANOY,, S.N.g kandidat takhnichookikh nauk, radaktor; LARIN, F.S.,
kandidat tekhnichaskikh amuk. redaktor; NEMIN. N.N.. doktor tekhni-
chaskikh nauk. redaktor; PUZYRAT, S.A.. kandidat telchficheakikh nank,
redaktor: RYUKHIN, N.V.. kandidat tekhnicheakikh nauk, redaktor;
FLYATI. D.M., kandidat takhnichaskikh nauk, redaktor; SHAP20, A.D.,
kandidat takhnicheek1kh nauk, redaktor; ELIAS , M.G., kandidat
tekhnibheakikh neuk, redaktor'; UMYAKOVA, A.Y.# redaktor tzdatelletva;
XARASIKO K.P.,,tekhnicheekiy redaktor
[Paper makerge handbook] Spravochulk bmmxhnike (takhnologe). Kookwa,
Gonleebuxizdatjol.Z., book 1. 1956. 458 p. (MLRA 10:2)
1.3aningrad TSentralOnyy nsuchno-tseledovatellskiy tustitut tmellyuloz-
noy L bumechnoy promyshlennosti (Paper industry)

ALEKS&YU, A.A.,inzheasr, redakton. ASHKENAZI, K.M.,doktor
takWebeekikh nad@- redaktor; GRUAB V kandidat Inkhnicheskikh
N.91an1dat t6 chaskikh nauk, redaktor;
nauk. redaktor; GORBAC.".V, A
IVANOV. S,N..kandidat te@ghnicheskikh nauk, redaktor; LARIN, P.S.,
ksudldat takhaichesiAh nauk,redaktor.-AMPSNIII, N.H.,doktor
tskhnicheskikh nauk, redaktor; PUZYREV, S.A.,kandidat
t*khaichookikh nauk, redaktor; RYUKRIN, N.T.,kandidat
takhaichoskikh nauk, redaktor; MATE, D.M.,kandidat takhnichookikh
nauk,'.rejAktor;.-SHAP.IRO,-..A.D..,kandidat takhaichookikh nauk, redaktor;
ALIASHM , K.G.,kandidat tskhnitheakikh nauk, redaktor,-PUZYRNY.
S.A..redaktor; PYUKHIN, N.V. redaktor; KHUDYAKOVA. A.V.,redaktor
iidatelletva; KARASIK, N.P.t;khnicheskty redaktor
[Paper maker's manual] Spravochnik bumazhnike, takhnalogs. Moskva,
Gooloobumizdat. Vol. 2. book 2. 1957. 433 p. (MLRA 10:4)
1 leningrad. TSentra'lInyy nauchno-issledovatellskiy institut,
tsellyulozn0y i b11mA%hnov promyshlenaosti.
(Paper industry).

GRABOVSKIY, V.A., dote.; NANIMIKOV, I.V., iuzh.; YARCTSKIT, B.A.
Rapid washing of sulfate pulp in diffusers. Bum. prom. 33 no.4:
16-18 Ap 158. (XIU 1114)
1. Lieningradskly takhnologichookly institut (for Grabovskiy.
Namestnikow). 2. Svotogorskiy tsellyulozno-buns hW7 kombinat
(for Tarotekly).
(Woodpulp) (Diffusers)

GRABOVSKIT. V-,Aj , dote.; RAMISTNIKOV, I-V-, inzh.
MAM"
]Cffect of certain factors on the washing of sulfate pulp in
diffuser tanks. Bum.pro"- 34 no.6:2-4 Je '59.
(MIRA 12:10)
1. LeningradsKy tel-chnnlogicheakiy institut teellyulosm-bumsh-
noy prorTablennosti. (WO04pulp)

BARANOTP NikolaY Aleksandrovich; GORBOVSKIY, Boris Grigorlyevich; SOLYUSj,
N.G.9 reteenzent[deceased]; DENISOV9 Yu.A.-, reteenzent; GPJJ30VSKIr,
V.A., red.j PROTANSIUU9 I#Vej red. izd-va; VOLOKHONSKAYA-qL-.T.-p-
rR, izd-va; VDOVINA, V.M.v tekhm. red.
[Technology and autmption of cellulose production] Tek6ologiia
i av'tmatizqtsiia taelliuloznogo proizvodst7a. Moskva, Goslesbum-
izdat, 1961 471 PO' (MIRA 14:6)
?Cellulose) (Au4cmation)

ALEL3=9 A*A&t inzhv redj ASMMAZI, K.M.; doktor tekhn.nauk, red.j
MUOVSKIY, V.A.j_kand.tekhn*naukq red*; GORBACIIEVy A.Nej kand*tekhn.
TIAII , red-e-JIMOV9 S.N., Iaqrd.tekbn.nauk, red.; IARM, P.S., kmd.
tekbnonauky red,; NEPWINp NoNap doktor tekbn.nauky red.; FUznw,
S.A.v kand.tekhn.naukp red.; RYUKRIN, N.V., kand.tekhn.nauk, red.;
FLYATEp D.M., kand.te)dmnaukp red,; SHLPIR02 A.D.9 kand.tekbn.naukp
red.; ELI HBMG9 M.G., doktor tekbn.nauk, red,; KHMAKOVA, A.V.,
red.izd-va; SIDELINIKCYVA, L.A., red.izd-va; LOBANKOVAq R.Ye.9 tekbn.red.
(Manual for paper industry tecbniciaxw] Spravochnik bumazhnika; (tekbno-
loga). Moskvat Goolesbumizdat. Volo3. 1961. 719 p. (MIRA 34:6)
1. Leningrad. TSentrallmyy nauchno-issledovatellskiy institut
toellyUoznoy i bumazbnoy promyshlennosti.
;,(Paper products)

ALEKSEYEV, A.A., lnzh., red.; VIYUKOV, I.Ye., kand. tekhn. nauk,
red.; GRABOVSKIY, V.A.# kand. tekhn. nauk,, red.; ZHITKOV,
A. V. *' Mald!'.@ f6ik rauk-j@red.; NAUMOV, V.V., kand. ekon.
nauk., red.; NEPENIN, Yu.N.p kand. tekhn. nauk., red.;
PUZYREV, S.A., kand. tekhn. nauk,, red.; RYUJG1IN, N.V.p
kand. tekhn. nauk, red.; SHAPIRO, A.D., kand. tekhn. nauk,
red.; ELIASHBERG, N.G., doktor teklm. nauk, red.
[Handbook for the papermaker in three volumes] Spravochnik
bumazhnika v trekh tomakh. Moskva., Izd-vo "Lesnaia pro-
myshlennost'." Vol.l. Izd.2.1 persr. i dop. 1964. 840 p.
(MIRA 17:8)
1. Moscow. Vaesoyuzryy nauchno-issledovatellskiy institut
tsellyulozno-bumazhnoy promyshlennosti.

GRABOVSKIY, V.A.; LYAN VEN-GHT
Balance of oilletc acid In the ;L,,ulfite oooking oC reed pulp and
desillconization of black liquor. Trudy L-TITSBP na.1210232-4W
164. (MIRA Z818)

30-58-4-17/44
AUTHORSt Gn@@bovs 1. Professorl Kolesnikov, A. G., ?rofessorl
Tvanov, A. A.. or of Physical and Mathematical Sciences
9
TITLEt Rd search Done During the Expedition of. the "Mikhail LomDnosov"
di@jionnyye issledovaniya na sudne "Mikhail Lomonosov")
*AflyMce in the Atlantic (Gidrofizicheskiye raboty v
Atlanticheskom okeane)
PERIODICALt Vestnik Akademii Nauk SSSR,1958 @4,'@-l Nr 4, pp. 86-90 (USSR)
ABSTRACTt The present investigations of oceans and seas show that their
most essential processes are dependent on the thermal and
dynamic interaction of the ocean and the atmosphere, There-
forethe main interest is directed to the investigation of the
heat exchange processes between atmosphere and oceang to the
distribution of heat in quantities of water as well as to the
formation of streams and waves. Then the authors report in de-
tail on the future research within the frame of the program
of the International Geophysical Year. According to a decision
of the Committee for the execution of the works of the MGG
the investigations in the North Atlantic are to be carried
Card 1/3 out by the scientific research ships "Mikhail Lotionosov"

30-58-4-17/44
Research Done During-the Expedition of the 'HikhailLomonOsolg". Hydrophysics in the
Atlantic
(Figure 1) 9 "Ekvator" and "Sevastopol". The "Mikhail Lomo-
nosovif was built in the "Neptun" ship yards in Rostok (DDR),
it has a displacement of 6000 t and can also be used for
works in ice. Its deck was made longer and a landing place
for helicopters was inecrporated. The ship has special de-
vices and equipment, among others a deep-sea hoist for
anchoring down to 15000 mg 8 hydrologic hoists of the "Okearil'-
-type down to 4000 m, 3 echosonic fathometer automatic re-
corders dowrM2000 m. 1 echosonic fathometer of the "Lodarl'-
-type for vertical and horizontal probing. Then a workshop
for experiments and 16 laboratory rooms are installed aboard
the ship. The average speed of the ship is 13 knots and it
has an operating range of about '11000 miles. The maiden
voyage was made for testing the equipment of the ship (Fi-
gure 2). But also a number of works of general kind were
carried out. Also a group of German scientists under the
direction of Doctor E. Bruns took part in this expedition.
The second voyage is shown in Pigure 3 and is supposed to
include the collaboration of all three ships. The main oceano-
graphic work of this voyage will be carried out according to
the plan by the 11GG, which is further detailed. The"Mikhail
Card 2/3 Lomonosov" started on this voyage which will last 4 months

30- 58-4-17/414
Research DoneDuring.the Expedition on the 'Mikhail Lomnosov." Hydrophysics in the
Atlantic
on February 25, 1958o There are 3 figures.
1. Oceanography-Atlantic Ocean 2. Oceanography-
Instrumentation
Card 3/3

HRABOV.'3'KYI, I/ Volodymyr Klymentievych
[Cooperation mid mt1tual, aid among all members of society
are forms of the productive relations in socialism]Spiv-
robitnytstvo ta. vzaiemodopomoha vsikh pratsivnykiv sus-
pillstva - forma vyrobnychykh vidnosyn sotsialimu. Kyiv,
Vyd. Kyivslkoho univ., 1961. 60 p. (MIRA 16:4)
(Cormnunism)

Sh-WILOVSKY, Nikolay Nikoja@yevichj YARMOLIOUK, Geor'g;y
Grigor Iyevich;
ADQ=SM i tali k ich
7,,Pro of 'Yev
FRUSOV) Mikhail AntipovIeb
(Fiddy current methods for production parameter controig
principles of theory and design] Metod vikht-ev-,vkh tokov'
dlia kontrolia proizvodaLvennykh pa-Lireatlrov-. o3nov%v teorij
I
i rasCheta. [B)rl N.N.Shimilovskii i dr. Frunze, Izd-v-.,.)
"Ilim," 1964. 20/6 p. (MIRA 11@0)

ACC NR-. AP70124n
SOURC& CODE: Ult/0367/67/005/001/0123/0128
-AUTHOR: Gareyev, F. A. Gareovo F. A.; Graboirskly,,-.Ya. Grabowski,, Ya.;
Valinkin, B. N.
"y
ORG: Joint Institute for Nuclear Research (Ob edinennyy Institut yad*rnylgh'
Issledovanly)
TITLE: Diffraction effect In the Angular distribution of transfer r0ae on
ti
ducts
ro
p
SOURCE: Vadernaya flzlka, v. 5 no. 1, 1967, 123-128
TOPIC TAGS: angular distribution, nuclear collision
.11:, SUB CODEt 20
ABSTRACT. The diffraction effect In the angular distribution of transfer
reaction products has been treated. Its relation to the parameters charac-
terizing collisions between nuclei Is established. It Is qualitatively ex-
plained why an asyvpetry exists In the half-i4idths of the stripping and pick-
u reaction product energy 9 ectrum Orig. art# hast. 3 figures and 10 formulas.
Based on authors' Eng, Abs PRS:- 40,3967
t 55 ci
Cord