SCIENTIFIC ABSTRACT MOLOTOV, B. V. - MOLYAKOV, D.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001135110005-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 13, 2001
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SIDOROV9 O.M.1 MMOTOVo B.V.
. C
CbJective method for the fintion of additional traces of a gunshot.
9W.-med.ekspert. 3 no.4s_%-56 O-D 160. (KML 13911)
1, Dywo Glavnqy ffudebnowDditsinakey sk"rtisy (rw;th,, - prof.
SA.Sidorow) Ministerstva zdravookhraneniya Kazakhakoy SM,
(PROrOGRAM, RAII STIC)

8IDOFLOYt SM.; MOLOTOTr B.T.
$'.,udy of lesions inflicted with bltmt objects with a ra=ded
awfaceo Sud,med. eksperte 6 no*4t5.L-53 06-D'63 (MIRA 1602)
1. B~uro, Glaynoy sudebn=editainakoy ekspe&,Izy (nachaltn1k;
prore SM. Sidorar) Hinistaratym zdrarookhraneniya K&z5M

FRMOV, re.r.r SIVOKHINA, N.B.; DDMIM, L.P.; KOCHLrTOVI, K.X.F MDLOTDV',
N.A..:
PrdlIminarjr method or evaluating the accuracjr of calculating
petrole= reserves by- the volume method. Trudy,* VNII no.3608-56
t62. (ICRA 15M)
(Petroleum geology)

MMMT, N. D.
2. USA (600)
4. Flax
T. Fractico of a leading flax factatTe Tekste proms 121, noe 101, 1952,
9. Monthly List of Russian Accessions, Library of Congress, Jawlar)rv J953. Unclassified.

31[LYA,PIMP YO.G.; FibWE0K, N.V.
St-j-dying the possibtl;ty of ravxml grapi-.Itn wlte-.
an ,-h content of up-to 0.2% in electric engirat.-Ir-F.
TSvet. net. 37 no.1103-91 N f64. (KIRA 18W

HDIVWV I, S. V.
*Th& Int4rn&ttojma And r,49al Regime af the Baltic Straits,,w S*r. gosudamtva
i prave, 90.5, pp 61-63, 1950

XOL=,, Mtor,.Tiaofeyevich. inth.; MATAIMCM. I*T#, kandotekhn.nauko
CUrVy red.
[Xfftclent utIlIzatLon of automotive transportation an collective
farug] RatelonaVae vftoryetannis avtotranaportu v kolhospalch.
ryiv. 1959. 33 P. (faverystTo d1la poshyreants polityahnykh I
naukovykh zaan' URSR. Sar.6, no.21) (KDU. 13:2)
(Collective farns) (Transportation, Automotive)

14OLMYLt L.A.
G=trol of bloodmwking dipteraw, in Gmsan-Wl IY-atricts,
Zdrar. Turk. 7 w,443-44 Ap'63. (MIRA l6s6)
1. rs Turkmanskoy reqmblikmnakoy sanitarno idemioUei-
chaskoy stantaii. (glaynyy vrach - T,l*=-evl-
(GASAN-Mr DISTRICT-DIPTEU-EEMMINATICK)

yttit- ~~-!Tde 6- wvt-Um
of tba UlbAd
At $.*station, in diffarent parl
Collected
IKO taipc 145- L", -d c-
- ~ Tepftfivn e . de 4.erje:Au m -idle, Picaml.d4e, T
Lyganid ae. cor-f-Hal, P(-)-tatfjml-dzn' and cydnid-'Sa~ TV,') Species o"', the genw
plettrU am aaw to ordor~a-j. rofiv-dcluz St!71. and 0mcAl
r Oto
avft-cfmC Jak. we-re wnon& tha i arrer ispe4-its f --nm~, the leFlarel. The w1laetican

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ACC NRt AP603411Z
SOURCE CODE9 UR/03581661035100510538/0539
AUTHOXt Molotov&, L, A,
ORGt DeparCment of HoLogyv Turkmen Kedical Institute (Kafedra
biologiL Turkmenskogo vieditaLaskogo inaticuta)
TITLEt Sensitivity of Lasect Larvae to trLchLorouecaphos-3
SOURC2: HaUtsinakaya parazLeologLya L parazLtarayre boletra, V. 'so
no. 5, 19660 539-539
TOPIC TAGS: peat control, peat coutrol maithad,
insect )
ABSTRACT: The effecctyaness of trichLoramataphos-3 against dipteran
larvae was determined. The cescs were performed in October, 1964 unaer
field conditions in the Turkmen Republic. The breeding grounds of
these inseccs, mostly mosquito species. were in &lov flowin& screams 4
or 5 cm beLow che water surface. The test areas were treatLd with 0.051
tc O.JZ mixtures of trichLocametaphos-3 and with hexachLoracycLohexane
to compare results. WLthLn two days larvae were absent fran alL eecC
areas although pupae were found La the hexach2orocyclahexane created
2 UDCt 615.779*3-G9Z*Z59:595.77-l34.Z

area, Repeated cests ahowed that 90% kills were obtained wLth the use
of these quantLcLes of trLchloracietaphos-3o- JW.A'. Sol
SUB CODEs 06/ SUBM OAM 12Jaa65/ 0
Card 2 12

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MMOMPL, D.T.; TABIL"'ff, rim.r.
Vagultu,;e of ,he velocitr ratio of Ionggitu&iaal and trans-
verse wav.: in rocks. Report No.l. Izv.AX S=-Ser.geofiz.
n0-7:930-945 J1 l6o. (KIU 13:7)
1. Akademlya nank SSM, InatittA fizild Zealle
(Seismic prospectinC)

86314
s/o4q/60jO0OjOO7/GO5/O0q/XX
Et9l/E381
AUTHORSt Kovalev, 0.1, and Molotova, L.n
TITLEs An Impulse Borehole Device for the Excitation of.
Elastic Waves Of Various Types
PERIODICAL: Izvestiya Akademit nauk SSSRI Sertya geoftzt-
cheskaya, 1960.No-7,pp. 959 - 969 + 2 plates
'r.
TEXT: A patented Lvfce (Author's Certificate No. .124648)
Cor the excitation in deep boreholes of transverse's-eismic
waves by impulses has been developed for the purposes of
examining the physical properties of rocks, determining the
absorption coefficients of longitudinal and transverse waves,
studying the form and peculiarities of an impulse in the
immediate vicinity of the impact and the excitation of trans-
verse waves In seismic exploratton with the help of transverse
rerlected waves. The device in a mechanical axciter in which
a heavy ram, under the action of a spring, hits a slug which
is in close contact with the rock. The device consists
of a borehole cartridge unit, a suspension rod system, an
Card 1/k

56:14,
s/o4g/60/000/007/005/009/XX
E191/E381
An Impulse Borehole Device for the Excitation of Elastic
Waves of Various Types
operatLng head and a supporting cover at the top of the
borehole. The borehole cartridge unit consists of a body-,
an impact head and a casing. The steel body of the impcet
head contains the impact mechanism and the wtnding-up and
release mechanisms. The impact mechanism has a heavy ract
placed in the cylindrical channel of the body pressed against
the slat by a stiff steel spring. The slug is mounted on the
body through a rubber damper. The wtndLng-up of the ram is
performed by the winding mechanism and compresses the spring.
When the ram is released, it presses the slug against the
rock whilst the casing taken the reaction. The suspensif)n
rod units, made of duralumin, each consist of 5 bars and have
& length of 2 at. The corresponding bars are connected when
further suspension rod units are added, The operating head
controls the operation of the cartridge by pressing the slug
against the borehole watt, winding up and releasing the ram
through the 3 bars in each rspension rod unit. The weight
Card 2/4

MM4
s/ok9/60/000/007/0Q5/00q/XX
E191mal
An Impulse Borehole Device for the Excitation of Etastic
Waves of Various Types
or the borehole cartridge and operating head is 9.5 kg and
the weight of each rod unit is 5 kg. The depth of suspension
can be increased to about 50 m. The elastic energy released
at each impact is about 10 - 20 times Less than the
explosion energy of a single detonator. It is stated that
the energy of the device could be increased ten-fotd. Field
tests with the new device are described. The pulse shape,
although ccmplex, has a simple amplitude-frequency spectrum
and does not depend on the depth or point of impact nor on
the type of wave. The directionality has been round to be near
th* theoretical for a source of the type of a concentrated
force. The amplitude spectra of the SH wave excited by the
impact are shown in Fig. 5. It is advisable to place the
device at some depth inside the borehole. Comparing the
frequency spectra of explosion and impact-excitrd vibrations,
it is shown that the difference Is small. Some results of
studying the physical properties of' rocks with the new device
Card 3/4

&5nl
s/o4g/60/000/007/005/009/XX
E191/E38l
An Impulse Borehole Device for the Excitation of Elastic
Waves of Various Types
are illustrated. The effect or the device is the excitation
of P, SV and SH type waves. The velocities of these waves
as rar as a few dozen metres can be mea,.tured and the
coefficient of absorpttou determined. It was found
for example, that In dry and slightly humid Loess type
formations the velocities of the above waves do not depend
on the direction.
There are 11 figures, I table and 18 references: 14 Soviet
and 4 non-Soviet.
ASSOCIATIONt Akademiya nauk SSSR Institut fiziki Zemli
(Academy of Sciences USSR Insitute of Physics
"Ethi-EA11b)-
SUBMITTEDs November 3, 1959'
Card 4/4

86206
46 3/01+9160/000/008/001/015
9201/9191
AUTHORSt Molotoya, h.,V., and Vaslllyoy Yvtj.
TITLE: The Ratro-o-r-th~ongitudinal and'jr.ULs_yer_gr._W%Yg
Velocities in Rocks. Il.
PERIODICAL: Izvestiya Akademii aauk SSSR7 Seriya geofizicheskayag
19609 No. 8, pp.1097-1116
TUT: In Part I of this work (Ref.1) the authors reviewed
methods of measuring the ratio vp/vg in rocks (vp is the velocity
of longitudinal waves, va is the velocity of transverse waves).
The present paper gives a comprehensive review of published
experimeatal values of vp/vS obtained bT various workers using
various methods. The frequencies at which the vp/va ratio was
obtained varied fron a few c/s to tens of Kals. Consequently the
authors considered first how the values of rp/vS in heterogeneous
media are affected by the test frequency. It was found that In
two-component heterogeneous cadia (Figs 1-4) the r%tIo vp v,a
varies nonmonotonically with the frequency of harmonic vibrations.
This ratio oscillates about a value vp,,/vS., which represents
Card 1/3

1.w
86206
s/ol+,7/60/000/008/001/015
9201/H191
The R&tio of the Longitudinal and Transverse Wave Velocitias In
Rocks . H.
the case of infinite frequency. The differences betvean the vp/vS
values at lov frequencies and at high frequencies are small In
the majority of cases; the same is true of the vp/vS maxima or
minima at intdrmediate frequencies. Consequently the authors
assumed that, in the first approximationg the ratio VP/VS is
independent of the test frequency. Values of vp (col.2)9 the
depth at which measurements were carried out, H (col-3), "Plvs
(col.10, Poisson's ratio a (col.5'), the locality of measurement
(col.6), the method of measurement (col 7) and the cited
literature (col.8) are listed In Table i for 176 rock materials.
The values of vp, vp/vS. a, for several metA-ls, glass, wood,
plastics, ate. are listed in Table 2. The ratii vP/vS of rocks Is
plotted as a function of vpl va and H in Figs 5, and 7
res ectively. The results quoted in tables and figures show that
V73 In crystalline and metamorphic rocks lay between 1.7 and 1.9.
The ratio vp/vi; In sedimentary rocks varied wlt.'iln much wider
Card 2/3

86206
S/049/601000/008/001/015
E201/E191
The Ratio of the Longitudinal and Transverse Wave Velocities In
Rocks. II.
limits$ There was a definite relat.'onship between the
limits of the vp/vS values of sedimentary rock-!~ and vp, vS ani H
for the same rocks (Figs 5-7). In dry weathered rocks with small
vp the values of vp/vS were smallc 1.5-1.8, The range or values of
vp/vS was alao small in sedimentary rocks with the longitudinal wave
velocity greater than 3000 m/see. icknowledgements are made to the
authors' colleagues for their advice and to..I.V, Aleksiny who
carried out the calculations.
There are 7 figures, 2 tables and 74 referencest 33 Soviet,
29 'English, 5 German, 3 Japanese, I Italian and 3 translations.
ASSOCIATIONt Akademiya nauk SSSR, Institut fiz1ki zemli
(Physics of the Earth In5tUU-tA4-"-U-OSH)
SUBKITTED: November 9, 1959
Card 3/3

MCLOTOVIt L.V.; IVMVL, T.G.; TENUILS, S.A.
Saisale method Of PrOspectlag in the orystel2im basement of the
Valga-Ural region. Geofix.razved. ndr-70~-191 162. (KM 15 t 7)
(Tolgar-Mml region-Seismic pro"ating),

HOIDTOVAt L.T.
R&tia Of the longitudinal W tmnswrodl wmvv velocitiot
in tarripnous: rocks, rzy. Aff SSSR. Ser. goofiv. to.,IZt
1769-1779 D 163. (MVI 17t1)
1. rwtitut fisiki ZexU AX SSSR.

MOLOTUVA, L.V.
Absorption of ultrasonic waires In granites. Thrudy Imat. fit.
Zem. no.3OtU-87 '63. (FIRA 17:4)

"JiDTOVA.-J-11Y.
Dependence of the frequency speitra of stvismic waves on the
conditiong of the explosion. Part 1. ltv. AN SSSR. Ser. geofts.
no.12cl753-1766 1) 164.
Dependence of the frequency opqctra of seismic wav"s on the
conditions or the explision. Part 2. lbid.tl767-1773 (MIRA 11:3)
1, Institat fizikl Zaali AN SSSR.

ACC NRi AP6005936 SMCE CODEt UR/0387/65/000/010/0057/0062
AUTHOR: Molqtoya, L. V.,. Flitr.",
............
ORat institute of P sics of the'Earth. Academy of Sciences SSSR (Institut RZIki
Zemll Akaemli -na;~i
TITLE: Displacements in an elastic medium cauaed by a plastic wave
SOME: AN SSSR. Izvestiya. Mike Uall, no. 10, 1965, 57-62
a 4L
TOPIC TAGS: seismic wave, elastLcAvwe, wave mechanics
ABSTRACTs The 3uthors consider elastic oscillations on the external surface of a
sphore with a radius %ialch increases according to a given law (with the velocity -of
the longitudinal waves at the initial moment and then gralually decreasing In speed).
The constant normal stresses on the surface of the sphere are given. The roving sphe-
rical nurface simulates a plastic wave front. The rediated elastic wnve is studied as
a function of the form of the hodograph for the plastic %ive, AnalytLcAl expressions
am derived for displacements in the sUatic wave assuming an Invariable stress at
the Interface between the elastic and plastic regions. The theoretical results are
ewpared with the solution given by Snarpe (J. A. Sharpe, "The Production of Elastic
Waves by Explosion Pres3ures", Geophys., 7, No 2, 1942). It Is shown thst there is
a difference between tha forms of displacements U, and V?. (where the Index I indicates!;--
UDC% 534.14s550.834

25546-66
ACC Mgt AP6005836
displacements caused by the action of the plastic wave, and the Index 2 Indicates dis-
plAcaments calmlated In conformity with Sharpe's theory). The effect on the plastic
wave side is an increme In the duration of V, as compared with U2 due toa lose
abrupt'arrival. This neans. that the absolute value of the amplitude spectrum S1 goes
further into the low fiequency mnge than $2. The "perimantal data IndicAs &,i OR-
tr4waly rapid attenuation of plastic waves with distarce from the source. It is tug-
gested t*.at further studies In this field should nct be 1imIt*dL_tO~_imstan"tr*ss----
at the Dlastio-wave-fr=t-tince~-tkl*-condi-ti n a not agree with experimental date.
conclusion the authors con5idar it their pleasant ditty to thank
and for discussion of this work. Orig. art. hast 2 figures, 14 0
So CODES- 6/ SUBN DATES 1OMa-65/- __OPJG Ws 006/ OTH Fat 002

_-L-14k1a;~iL __L'XFf' - i
ACC t4Rc AP6010063 SOURCE CODE: UR/0387/66/00103/0033/0043
iAWHOR: Gurvich, 1. 1. (Goctor of technical sciences); Kolotova. L. V.; Lavyant, V. R.
ORG: hoscow Geological-Mining Institute Imeni S. Ordzhonikidze (Haskovskiy geologarax
vedochniy institut); Mizhnevolzhsky InstLtute of Geology and GeopLysicat Academy of
~
Sciences, SSSR (Mich olthakiy institut geologit L geofiziki Akademiya nauk ZSSR);
iInstitute of Earth D2sicst Academy of Science . GSSR (Institut fitiki Zenli Akademiya
'iFa_u_k_S_S_YRU
ITITLE: Experimental amplitude characteristics of explosions
SOURCE: AN SSSR. Izvestiya. rizika Zemli, no. 3, 1966, 33-43
TOPIC TAGS: longitudinal wave, explosive charge. sound wave, seismic wavi~
lee,
ABSTRACT: Alcomparison was made between experimental and theoretical aml2litude charac
teristics of Uplosion nuclei In sand-clay deposits. -she theoretical -analysis was bas
~_d on the theory of spherical emission of longitudinal waves.* Selemological sections
of underground JAyers down to 60 m are shown, giving the relative velocities of pres-
sure waves (v ) and sound waves W.) as a function of the respective layar compositione
P
(sand, clay, soil or sandstone) and the positioning of the e"losion nucleus below the
earth. Model spectra of asismic wave reflections are shown w1th the corresponding am-
plitude spectra (amplitude an a function of freauency--from 0 to 60 cps), for charges
UDC: 550.83Li
1/2

ACC NR: AP6010063
weighing from 0.1 to 6.5 kg. Characteristic parameters for conditions in the vicinity L.
I
of the charge nuclei axe tabulated for the different selsmic aections with charge
depths to 35 m and charge weights to 500 kg. These parameters 'were: the ratio
(V /V ) ; tosAv where k is the radial ooefficient of the nucleus of the explosion,
a P a
obtained from the formula
RckQ11,j
where R to the radius and 9 Is the weight of charge. The frequency coefficient of the
nucleus g was about 40 sec 'kg~3 for damp sand-clay deposits. The values for (119/11P ) a
ranged fixn 0.3 to 0.7, as determined from the amplitude curves. These were system&-
tically higher than W a /aP)Iwhich were detemined directly fron seismic e_xploslons.
Both theoretical and experimental values of K agreed clostlr and ranged from 1.14 to
3A m-kg VZ. Orig, am. hagi 7 f1gurest 2 tablesg 7 fomulat,
SUB CODC: 08/ SUBM DATE: OlJtm6S/ ORIG REF: 010/ am Fzr: ooj-
2/2

AP60-29666, SOURCE CODEt UR.1038.7'1fi6fQ0Q/QQa[OQ36/Q046
AUTHORt Malotavay L. V,
ORGI rastLtuto of Physt-cs of the Eart!~, Aeadej!y of Sciences SSSFt
(InxtLtut ftsikt Zemlit
TITLEr Velocity dispersion of body waves in terrigenous deposits
SOURM AN SSSR, lavettLydo FULks ZemlL, no. 8, 1966, 16-46
TOPIC TAGSt SeEgmic waveIpoep-g*&&"jr h*d:r-~. reek e"otie~,_
%&WCd-.c: wfvs! 'ropagatton. saldaf c
AESTRACTc di