SCIENTIFIC ABSTRACT TATARSKIY, N.V. - TATARSKIY, V.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001755110012-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

TATAMIY, N.V..
lAte reoults in thoraeopluty. Probl.tub. 38 no.6s47-51 160,
(KMA 13 t32)
L rsrtuberkule=ogo otdoloniya (zav. - kand.med.nauk N.V.'
Tatarskiy), klinicheskogo otdola (z4v* - prof. M.I. Mivilivitska7a)
leningradekogo inatituta eksperti4 trudoopoi3obnosti i orga-
nizatoii truda invalidov (dir. - knnd-medamlk PoA. Mokkavq&iy).
(CHEST--SURGEU)

TA7tKIy"!N.v.
lpt~rmvibce Conferenod 64 bI "Of Medical Dis-
P" . VO,
aWlity. IcPbrtiae and Rehabilitation of JAVdIdg Mmabled by
PdlmonarY Tuberculosis. Probl. tub. 4:L,tv,,%824~3 963
(HIRA j7z4)

TATARSKIY; N.V. ~And.med.nauk (Leningrad, V.O.Gavanskaya_ul., d.6,,kv.15)
Late results of thoracoplasty in tuberculous empyema. Vest.
khir. 90 no.305-41 14063. OHIRA 16:10)
1. Iz tul)erkaleznogo atdeleniya. (zav. - N.V.Tatarskiy) k3.i-
nicheskogo otdela (zav. - prof. II.I.Khvilivitslcaya) Lenin-
gradskogo instituta ekspertizy trudosposobnosci i organizatsil
truda invalidov (dir. - kand.med.nauk F.A.Makkaveyakiy).
(EMPYEM) (TUWWULOSIS)
(CMST--SURGERY)

L/t,yot
956T 's 0
(aasy2m)
~ *A * S g MSUVIVr,

0 9 0 0
10 Is
o 11 w is I? it 12 a 30 At 14 v a
a A a I It I I I I Y. _L, AA 0 CC 0
A

"A
V. J). Tatarswi. vm.
-
-
7m'. '034,
rvq
677 s4mkr;7
AL V. c
Ia.

,3

of u

AD It v u m 0 0 wife it 4161.4re
It . I R-11-1 'k J. 8 a
'I'M"'
wt%
wh
coo
do*
Igo*
90, 'a' too
Ijd.j ~4' 4 1.
V IF Ilk
0 Ad 14 a It $9, K n 1 09 MID it 1 :14 An I Ia 00 a a 1 9 81
oil 00 40 0 0 0 oo* so 0
re 0 0 0 fe, 0 ~Ldi go it 0 00-0 0 0 w 0 0 Ole 0 -00
000000

calam P .. A..ocpm atw pyl-4114. it. A, Plot -
m1b Vs&pcjjI.b#go Alin
,ik,v Simi V. 0. Ta 75. 234-A
__ 11%.
,ral, 06j I i's Stu- 111vilu.
(IM).-The P- -11 jti,, ~Jgjcss ~A.in
b0figna of the 'I"S, M"nr pyrite, Alid
te, or(lintrii1%. with
'hirdy purr -110m, I.Ypicl u2uumliluc 1011116 -.1
.6,1 in the lower I T c . .511 cwtvr.l.. the
g,ylissisite, NssmWs- I .
A. with OW
,-Tystab we pcvVmj cm. Sisk. i IV the crPtlis. frotla the
jt)10). Thef-atc kkmill Lake of
WMA.1 LAke. San' I Calif. ic Ond tid* from Ilse
%cmiss, MA the synthirt cl
1ISS4101113, pjucm. The tcallp. cosAital. of She say-
LetAussic Nxk my have been 0% in a ins
lummite crystu. 0 by evalin with :u upper $tA"-
brine. Or at higher teray'S" 1, %1~ cac(N--
ility umit of 40% above which pit N X W -. Fitel
2H,0. is f--d-

TAIMS=K, V. B-
UM knei-SIA Jul/Aus/aep 48
Bitumen
Analysis, Microoooplo
*The Forms of Bitumen Deposits in Carbonate Books
ae'Rovealed Under the Microsuaps," V. B. Tatarskly,
Active Ma%Aoad 801 USM,, 7 PP
"Zaplekl V-S Mineral Obshoh" Part T7, No 3
:Resulte of microscopic studies of carbonate rocks
fcwm Khaudag and Uch-kizyl. Describes the mor-
ph*13W and method for obseriing bitumens in
x1crosections and presents some of the data
.obtained by these studies.

1. TATARSTHY, V.
,2. ljss-,i (6,.)")
4. Physics ~Dathe Atics
CvTstrallo-Ogti(,~S 'Irli 17r.-ersici-, a 'iubnt,-,.nco,,
V. -3. T!~.tarski:r. (L-nin-,trd, Press of the Lemn4r-ld ITniv:- -sity ir-.ieni A. A. '""'Idano-79
.0). -."nvie%ed by 7~. Ye. Vedenel,mva, Sov,
1911, 1;
1WHOport U- 3091, !6 Jan. 19.5), Urclassified.

30755. TATARVSKI , It. B.
__L
I
Ob okrashannoy poloske bekke. (Iz inostr. diteratury). Zapiski Vsesoyuz.
mineral, o-va, 2-ya seriya, 1949, vYp. 3, s. 233-3h.

\Do'o'omi 'Afion,,ro' fod'. It T IA A
hd,.nq)v 511.ile Un Le"ifir 1)44 ~ylfd. NaNk
S.S.S.R. 69. ch4lise of dulmlitic
sedimenu to limestone is describrd from Bukhara. iu fh~
rocks of the Taclibik drprcsbitm~ The ptvk-ciA i~ a typical
WdAM MW6011: CAC(h..%I8C(A I COO. - XJC(h 1
NISS4)'. Fpsomite, with i. Ofirn Obwr~cll
fm the burf4rvn(d~hAoniitizM rwks.
.rhe petrogriphk, eharuw of the ltttx--. 6 utpwrvetl in all
franwilkx1a front ,j btXjjjujjjX intertAlAtittii t4 oak-ite in fine.
tr1r.t. dolomite. to the complete replArrinent M the Later
bV A C1Md*-Cf`ySt.. USUAlly JXWOU~ Aral C4VCT1tOt&% IiHWtt%W
.11h MWAskmial rcliLt W4:lgt*kmii of &AA)ujife. IhAtihomi-
vAti,"s i* alu known from I'AAcowiv rArk.% of N[wrta. hi
:
he Kutun and IlAu region. Often it has 1xvn dc-A-rib"I
.IS the reverse prortsa. i.e. a4 the rhattgr of 1h3womic t,-
folumitv. but the dctzd~J rnki~vj,ic ou,16% f,I dw iv ical
"Carlin" Otructures f2cluelm every

;0000 0 606 -e
14
00
00
T-- T T
- MWOTOW-WO-16'r I Well
46
0 N 0 if 14 t is V Is 0 41 0 a a
'1_1 4W i-t
TherwAlgrams ot addar" Of Ali-r-sit Md k"KLIL V. P.
Q 40 1 VANOVA A" V. It. TATARP1911 Pv*WyAk4d. Noxk.Y.S.S.R..
7
3 121341-Q (MSW-:&Z-pTn of washed k3olin. dolomite. and

0* dolomite with admixtures of 15. 30. rill. and M"* Lialin were
l IG*
h
t
din
l
b
t
i
l b
i
it ru
r
ou
a
ra
it
n.. ata
eat
j m
ng t urvn were obtained
by the differtutial method. using a Kuroakov pyrometer. The
first dolmnitc stop was within the interval of")* to rj)*C. NO
substantial or regular drop In temperature of decomionhion of
the dolomite was wited; an The Mirary, the admixture of large

040 amounts of kaolin was the cause (or mom rise in tempefature of

*0 decompnxillonof the dolomite. The second endathermal stop of
dolomite, corresponding I* the dissociation Of Cacoo, was more
00 intembe Than the, fint for the original sample. Hven a small

0
0
~ admixture of kaolin. however, strongly reduced the intensity

Of W
1 i compared with the first stop. This is apparently the result of
1 the supemosition of the endotbermal reaction (decomposition of
go a CaC%) and the notberimal peak of kaofin-the lomlatints of'
00 S mullite. The start of the dissociation of CaW~ Is substantially

0
00 lowered only for considerable admixtures of kaolin; the t-ml a6a

T occurs earlier in mixtures with a large content of kaolin. Large
anumnis of kaolin act inosily ac a filler. diluting the carbonate
and reducing the partial pressure of Ms. The filler hail prac.
t"lly rKjr&ct on the first stop. Admixture ofdol,nnite has no

I
J e
flert an the starting temperature of dissociution of kaolin, the
I rod temperature of this reaction depends on the amount of kaolin
in the mititurr. 111.K.
!0 1-1--.- - -- --- ~
.04
1-06
-00
-40
.00
#00
811111
- - - . 1 1. - -
L, %0.1L4 _61TALLWfICAL LITINAIWI CLASSOPKAT" 9-2- -1.
-=7=.
1-4n59% 70-7 IWI&S810-41
coo
coo
see
4111111411
see
rjo 0
goo
11001
140
AID 0
100 0
too
U Al 10 Al a of 0 a a I IF a I a a 3 1 T
0 0 0 0 lot
0o 0064111
0 0 0 0 0 0 0 0-0-0 0 0 0 0 0 0 11111 0 0 0 0 4 0 0 0 0 000 0

TATARSKIYj V. B.
"Methods of Deteinining Rock-Forming Cartonate M'inerajB.," (Metody Opredeleniya
Porodoobrazuyu. Shchikh Karbonatnykh Ydneralov), Release #53, 1952.
This book contains works of the A3.1-Union Petroleum Scientific Research
Geological-Prospecting Institute (UNIGRI)
UBC014 - D 163o98, 14 jan 55

TATARSKIY--V.B., EiiAhorl---SMJBNIKOV-A-V--A4it-vit-e-lf-ny-y--chlon-Cr"iW-e-rl,-
. 0 1 . a 9
Oft"OMMMM ft
V.B.Tatarskilla law of the ellipsoid ('Grystallo-optics and the immersion
method of Identifying matter.' V.B.Tatarskil. 14mieved by A.V.Shubnikov).
Zap.Vses.uIn.ob-v& 82 no.3:235 053. (XLRA 6:11)
(Crystallograpbr) (Tatarskii, V.B.)

------------
TATARMY, V.B.
Table for identifying forms of cleavage, AIW. s7stem, and smon7
of minerals In Imersion. Zop.Tese.min.ob-va 82 no.4:283-285 PON
(ML 7tl')
1. Beystvitillay chlen Vassoy-Asnogo Mineralogicheskogo obehahostva.
(CMtallograph.v)

SARAWKINA, Galina Mikhaylovr.&; K&LARET, L.A., redaktor, TATARSKIT#-V-~Bw,
redaktor; BODOLAGINA, S.Do, tekhaicheakiy redaktor. ' wbkv&%ftftMWAwA
(The Yedorciv mthod) Yedarovskii metod. LeningrvA, Izd-To lsniz~-
gradskogo vniverelteta, 1954. 134 p. (KEPA 8:5 )
(Crystallograpby)

gy

15-57-5-6677
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 5,
P 143 USSR)
AUTHOR: ratarskiy, V. B.
TITLE: 'Origin of Petroleum in the Bukhara Stage fK- probleme
,7enezisa nefti (Proiskhozhdeniye nefti bukharskogo
yarusaf
PERIODICAL: 'test. Leningr. un-ta, 1954, Nr 7, PP 181-187
ABSTRACT: Bibliographic entry
Card 1/1

TATAR KIY, V.B. I d,eystvitelln" chlen.
Aa observaition on the law of the ellipsoid. Z*p.Vm*t.vIn.ob-va
83 no.1:7f')*-79 154. (XLRA 7;3)
1. Leningiadskiy Gosudaretvennyy iniversitet in, A.A.Zhdanova,
Kafedra k3-istallografii. (Crystallography)

'PATARIU4, VjLal~y Borisovich; IVANOV, A.S., redaktor; IONIRL, I.N.,
vedUMMUy* redaktor; GZNADITEVA, I.M., takhnichookly redaktor.
[Microscoldc determination of carbonates of the calcite and ara-
gonite group] Mikrookopicheelcoe opredelenie karbonatov grupp
kalltsita i aragonitas LeninUad, Gosenauchn-tekhu.izd-vo neftia-
noi i gorito-toplivnoi lit-ry. Leningradskoe otd-nie, 1955.61 p.
(Carbonates (Mineralog7)) OCMI 8:3)

TATARSKIY, V.S.
a$
Relation between refraction Wiese of trigonal. carbonatos. Uch.zap.
Len.un no.'188:117-128 135. (mm 9:8)
(Refraction) (Carbonate* (Nineralo&7))

TATARSKIY,V.B.
' ' ' ' . ~ ~
- " '-, - '.t~
Petrographic types, comparison, and formative conditions of the
Bokhara stage in the Tajik Depression. UchezapeLensun* no*189:
90-105 '55. (KLRA 8:12)
(Tajik Depression--Geology, Stratigraphlo)

TATARSKIY, V*B.;. FRANK-KAHMMSKIY, V.A.
Osip Markom-ich Ansheles; on the occasion of his 70th birthday.
Vest.Len.wt. 10 no.10:117-122 0 155. (Mm 9:1)
(Ansheles. Osip Markovich, 1885-)

TATARSKIT. Y.B..
- www~ MW
Determination of the number of plagioclase by Immersion method.
Z&p.Vs~e.mIn.ob-v& 85 no.2:204-208 156. (MLRA 9:9)
(Feldspar)

FRAM~-XAKOWSKJY, V.A.; BURAKOVA, T.N.; NARDOT, T.T.;
PWWTq T.G.; XONDRATIMA, V.V.; KAMNTSIV, I,Yo.,- CHIWYSIWA,
V.P.; ALMMYNYA, M.P.; ARTSYBASHZVA, T.F.; BAWOVSKAYA, N.I.;
BUSSM, I.V.; V , I.A.; GNEVUSHEY, M.A.; GOYKO, Ye.A.;
KOMKOV, A.I.-, KOTOVICH. V.A.; LITVINSKAYL. G.P.: MIXHHY3VA. I.V.:
MOK17H7SKIY, V.A.; PSTROVA, L.V.; POPOV, G.M.; SAFRONOTA, G.P.;
SOBOLIITAI V.Ve; STUIODT, H.Np; TUGARIWOVAg V,Ge; SHAFROOVSKITl Iel,;
SHT=3HRT, A*A*; TANULOV9 K9P*
0.1f. Anshelee; obituary. Vest. IOU 12 no.18:152-154 157. (HrRA 11:3)
(Ansheles, Calp Markovich, 1885-1957)

RIGORIYEV, D.P.; BONSHTEDT-KUPLZTSUYA, B.M.; GRITSAYINW, G.S.; MINK&M,
V.I. [deceased]; TATABSKIT,
Prom the Go=ission of Now Minerals of the All-Union Mineralogl-
cal Society. Zap. Voss. sLin. ob-va 86 no.2:315-316 157.
(KLRA 10:6)
lo Predeedatell Leningadskogo gornogo institute, (for Grigorlyev
and Hikhayev). 2. Institut geologii rudnykh mestorozhdanty, petro-
grafii, mineralogii i geokhimii Akademil. nauk SSSR, Moskva (for
Bonshtedt-Kupletskaya and Oritsayenko). 3. Leningrad-skly gosudar-
etvannyy univerBitet (for Tatarskiy).
(Mineralogical societies)

RUXHIN, Lev Bcrisovich. prof., doktor geolago-mineralogicheskikh nauk,
red.; SJKRDYUCBENKO,, D.P., prof,, doktor goologo-mineralogicheakikh
Tit _1~ gUgLLch, prof., doktor goologo-
nauk, red.: TA=IT4-- -8 WAq
miners log it-heskikh natai-,r~-d.-, XALIIIKO, M.K.. kandidat geologo-
mineralogicheskikh neuk, red.; RENGARTAN. N.V.. kandidat geologo-
minere,logiabookikh nauk, red.; RUSAKOVA. L.Ta., vedushchty red.;
TASHCHURUIVSKAYA, A.B., tekhnsreds
[Reference manual on the petrography of sedimentary rocks,- two
volumes] Spravochnoe rukovodstvo po petrogrefit osadochTWkh porod;
v dvuk:h tomakho Leningredo Goo. nauchno-tekhn ~ Izd-vo neft, i gorno-
toplivnoi lit-ry, Leningr. otd-nie. Vol.le [Conditions of formation,
characteristics and minerals of sedimentary rooks] Uslovtta obraso-
vaniiii evoietva i mineraly osadocbnykh porod. 1958. 485 P. Vol.2.
[Sedineatary rocks] Osadochoye porody, 1958. 519 P. (MIRA 11:2)
(Rocks, Sedimentary)

SOV/136-58-10-14/27
AUTHORS: Kompaniyets, M.F. ank_T~.tarskiy, V.B.
TITLE: On the Mechanism of the-Formation of Grains by Technical
AluirLinium Hydroxide (0 mekhanizme obrazovaniya zeren
tekhmicheskoy gidrookisi alyuminiya)
PERIODICAL: Tsvetnyye Metally, 1958, Nr 10, pp 6? - 69 (USSR)
ABSTRACT: The author examined specimens of technical aluminium hyd-
roxide from the Ural' Aluminium Works and the Tikhvir
AluzLina Works with the aid of a polarising microscope,
using thin sections. They conclude that the material con-
sists mainly of spheroidal aggregates which are for the
mos", part coarsely arystallised. The aggregates show
chaxacteriRtic growth directions from a common centre -
thej are not crystal aggregates formed by collision;
occasionally two-centre aggregates are found. The struc-
ture of the technical hydroxide suggests that although
thej are made up of separate single crystals, this is the
result of their having grown from a poly-crystalline
nucleus and not of reaction during collision between
ind,9pendently growing crystals. The hydroxide crystals
are mostly deformed, the degree of deformation being less
Card.1/2 for the large grains than for crystals in the small and

SOV/136-58-10-14/27
On the Mecbanlam of the Formation of Grains by Technical Aluminium
Hydroxide
mediujn fractions: the latter thus have a higher internal
and surface energy. The hydroxide structure was found to
be non-uniform, with deleterious intra-crystalline inclusions
of mother-liquor.
There are 2 figures and 5 references, 4 of which are Soviet
and 1 German.
ASSOCIATIONS: Urallskiy alyuminiyevyy zavod (Ural Aluminium Works)
and leningradskiy gosudarstvennyy universitet
(Leningrad Stati University)
Card 2/2 1

SOV/?0-3-5-23/24
AUTHORS: Shafrimovskiy, I.I., Stulov, N.N., Tatarskiy V.B.
and Frank-Kamenetskiy, V.A.
TITIZ: Certain Observations in Connection with the Article of
Academician N.V. Belov "On a Co'U'rse of Geometrical
Crystallography for Physicists" (Neskollko zamechaniy
po povodu stat'i Akad. N.V. Belova "0 kurse geometricheskoy
kristallografti dlya fizikov")
PMODICAL: Krii3tallografiya, 1958, Vol 3, Nr 5, pp 637-638 (USSR)
ABSTRACT: Complaints by Leningrad mineralogists against the
exce8131ve physical bias by Belov in his article.
There are 4 references, 2 of which are Soviet and
2 Genian.
ASSOCIATION: Leningradskiy gornyy institut-LeningradBkiy
goE)udarstvenxtyy universitet.
(Leningrad Mining Institute and Leningrad State
University)
SUBMITTED: May 2~1, 1958
Card 1/1

TATARSK -, VITALIY BORISOVICH
t'Determination and Study of Crystals by the Immersion Method!
A report presented t.t Symposium of the International Union Conference of Cx-ystallography
Lenningrad 21-27 W 1959
SO: B 3,135, 471 28 JUlY 1959

- -- - - -- - I
TATAR91119. X6---
homenclature and classification of carbonates according to the
S120 of grains. Vest. LOU 14 no.24.-5-10 '59. (MIRA 12:12)
(Carbonates (Mineralogr)-Classification)

ICM, Boris Vaniaminoviob; Prinimeli uchs9tiye:_TATARSKIr, T.B., prof.;
FFLTJ=-I# S.Ta., starBhiy nauchnyy sotra-dxxi-k-,-lTSKlff-.Ylr-l-.
nauchnj~ sotrudnik; SVER=YA, O.T., mledshiy nauchnyy sotrudnik;
RAVMMI!, A.A., red.; SEMINA, G.A., red.; WILIM, 're,Ta,t
tekhn.red.
[Rafra(stometric methods in chemistry] Refraktometricheskie matody
khimli. Leningrad, Goe.nauchno-tekhn.lzd-vo khim.lit-ry, 196o.
382 P. (mIRA 14:2)
1. Len.Ingradskiy universitet (for Taterskiy). 2. Institut vysoko-
moleku'-Iyarnykh soyedineniy AN SSSR (for Frenkell). 3. Institut
khimli silikatov AN SSSR (for Ryokin).
(Rafractometry)

TATARKIT, T.B.
Numbe:r of accidental oriented crystals required for principal
refractive indices. Up. Toes. min. ob-va 89 no.it94-96 160.
(MIRA 13:10)
(Refractive index) (Crystals)

KUKHARENKOI Aleksandr Aleksandrovichi
_jAjA&%Uj.& V.B.. red.; POSPELOVA,
A*M*, rod. izd-4a; GUROVA, O.A.,, tekbn. red.
(Minerology of placer deposits] Mineralogiia rossypeil. Moskva,
Goso na-ttcbno-tekbn. izd-vo 3it-ry po geologii i okhrane nedr,.1961.
316 p. (MIRA 14'11)
(Minerology)

TARUMOVA,, N.N.i; KUKHAREUKO., A,,A.;-TATARSKIrl V.B., red.; GOLIDBERG,
R.Ya.,, r;id. izd-va; GUROVAI 0--K. -Itaim ~-' -
[Atlas o:r placer minerals) Atlas minerahm ross7pel. MDBkva, GoB.
naucbno--I-,ekhn. izd-vo lit-ry po geo'l. i okhrane nedr, 1961. 435 p.
(MIRA 14tU)
(Minerals)

TATARSKIY, V.B.,
Index of refraction of biaxial crystals in the articles on mineralopy.
Zap.Vses.min.Ob-va go no.4:486-488 '(1. (MIRA 14:9)
1. LenLngradskiy gosudarstvennyy universitet.
(Mineralogy, Deterr ifi4ti*ie)

GRIGORIIEV,, D.F.; BONSIITEDT-KUPLFTSKAYAl E.M.; BORNaWl-STARY-MVICH,
I.D.; GFITSAYENKO, G.S.; TATARSKIY, V.B.; FRANK-KAMENETSKIY, V.A.
To 9,11 mdneralogisto of the Soviet Union. Zap.Vaea min.ob-va 90
no.5:6(Y,1-608 161. iMIRA 14:10)
1. Fradsedatell Komisaii po novym mineralam Vaesoyuznogo mineral-
ogiches):ogo obahchastva (for Grigorlyev). 2. Komimaiya po novym
mineraIjun Vassoyuznogo mineralogicheakogo obahche3tva (for all).
(Mineralogical sociatiao)

TATARSKIY, V.B. _
Reduction of goniometric data on crystals to a single principal
meridian, Zap.Vses.min.ob-va 90 no.6:691-695 161. (MIRA 15:2)
(Crystallography) (Goniometry)

TATARSKIYi V.B.
mIN-8 and Mp-6 polarizillg microseopels. ZaP* Vses- inin- 'b-va
92,no.!;:6o8-612 163. (MIRA 17:1)

SHAFRANOVSKIY, I.I.; BELOV, Me; BOMp G.B.; GRIGORIYEVp D.P,;
STUMV, N.N.; MOKIYEVSKIYt V.A.; TATARS&Y V BO;
,.
HIBEffEVA, I.V.; DOLIVO-DOBROVOLMA, GOH.
Gew~gii Mikhallovich Popovj obituary. Zap. Vees. min. ob-va
92 n:).5:613-615 163. (MIRA .17:1)

TATARSKIY9 V.B.
Note an S.Sh.Gendelev's article "Face morpMology of yttrium ferrate
cryataln." Kristallografha 9 no.1;132 Ja-F 164- WRA 1733)

ACCESSIM NR% AP4039"
V
AUTHOR: B.
TITLE: The lack of any example of optically active crystals with planes of
symmetry
SOURCE: Kristallograflyap Yo 9,p no. 3p 1964P 451-454
TOPIC TAGS: optical activity.. symmetry plane,, polarization planes enantiomorphium
ABSTRACT: Using vmmetrx phenomena and giving no regard to position of elements in;
;a crystalp it is easily shown that rotation of the polarization plane is incompati-i
:ble with the existence of an inversion center and of the axes '3 and 7; in the crys-
;tal. It is also-olementary to prove that rotation is impossible for the direction
normal to the symmetry plane and for any direction lying in the plans. However, 1
these analyses do not forbid optical activity Li directions obliquely inclined tZ a-
and L There are thus 15,classes of crystals in which rotation of the polarization~
,plane appears possibles 11 onantiomorphia and four others# represented ~y M) 2=p
and ~26. Of the last four, only the class a has a representative claimed by,
~-ord-"- 1/2
S/0070/64/bO9/003/0451/04A

nt Ao3944
.:investigators actually to show rotation of the polarization plane. This represent-'
ative is the organic polymer (C9H.1204)2., but the author finds-no satisfying
Jevidence.of thiss believing that no actual crystal of this .class has been found to
~;rotate the polarJzation plane. He points outp also, that most of the other claims
for optical activity in the remaining 3.1 enantiomorphic groups, are based on improper
interpretation of' optical figures,, the presence of defects,. twinnings other imper- ,
fections in cryal.-Jx, or to the iradequacy of the optical system of the microscope.~
Thus., though theoretically possible# experimental evidence of'optital activity is
lacking, Orige iirt. hass. 11igure.
ASSOCIATIONt L6Wtngradskiy'gosudarstYermM univeraitet in* At A, Zhdauova
:'(Leningrad State UniversitY)
SDUMIXTIOUS 3.oJwi63 ENCU 00:
'-SUB CODE: SSj 01.) NO REF SM 002 OTHERs 012,
2/2

TATAR IYI VitgIly _r;L, (), i., red.
SK B,) 5pN~~qh; KUK!Y-t*llK
[Cx7stal optics and the immers-lon tellAxid for atulyingi
Kristallooptika i imeralowli raet-~d iLsledovanllft Mi-
neralov. Moskva, Nedraq 1965, 305 p,, (MERA 16.12)

YANOV, E.N.; STRAKHOV, N.M.; KRASHENNIKOV, G.F.; ARUSTAMOV, A.A.; GEYSLER,
A.N.; GRAMBERG, I.S.; LIBROVICH, V.L.; MDGIAYLOV, B.M.; NEKRASOVA,
0.1.; PISARCHIX, Ya.K.; POLOVINKINA, Yu.I.; T _L2".
SHUMENKOP S.I,
Reviews and diacuavions. Lit. i pol. Iskop. no.6185-89 and 91-119
N-D 165, (MIRA 18:12)
1. Vaesoyuznyy nauchno-issledovateliskiy geologicheskiy inatitut,
Lening-ad. (for Yanov). 2. Geologicheakiy institut AN SSSR,
Moskva. Submitted July 12) 1965 (for Strakhov). 3. Moskovskiy
gosudarstvennyy universitat (for Kraahennikov). 4. Kazakhakiy
nauchno-issledovatellakiy institut minerallnogo ayrlyap g.
Alma-Ata (for Arustamov),

ALYAVDINP V.P.; BONSHTEDT-KL~KXTSKAYA, E.M.; GODLEVSKIY, M.N., doktor geol.-
mineral.nauk; KOMKOV# A.I.; KUHARRITKO A.A.. prof.; SALIDAU, E.P.;
SMOL'I'ANINOVA, R.N.; BMRMAN-ST&t"1CF1f I.D.; TATARSKIT, V.B.,
prof,; FRANK--KAMENETSKIY, V.A.
From the Commission on New Mineruls of the Minerological
Sociel,y of the U.S,S.R, Zap,VseB.min.ob-va 94 no-5055-
565 165- (MIRA 18ill)
1. Kouissiya po novyu mineral= Vsesoyuznogo mineralogicheakogo
obshchestva. 2. PredaAdatell Komisaii po novym mineralam
Vses(r.ruznogo mineralogi-.-heskogo obshchestva (for Frank-
Kmenotskiy). 3. Zamestitell predsedatelya Kcmissii po novym
mineralam, Vsesoyuznogo mineralogicheskogo obshchestva (for
Bonsh-tedt-Kupletskaya). 4. Sekretarl Komissii po novym
mineralam Vsesoyuznogo mineralogicheakogo obshchestva (for
Sallditu).

.4
Taw"
V. L On the fluctutions oi
turbtdonF meMu= Jrvestiya Akad. Nauk SSSP- SM
--I Geofiz. 19S3, 2S2-258 (1953). (Rusdan)
This paper considers the question of fluctuations of phs.
so
:of sound received by two microphones situated in a turbu-,,
MathematIC&I ROVLOW8
Ilent.medium. The mean auadratic fluctuations of the di.ffer-
Vole 15 No. 2 ence of phases is computed for an arbitrary relation between
Feb, 1954 'a quantitative base and the distance traversed by the
sound in the turbulent medium. Treatment of the question
MochaniCS
is carried out within the framework of geometrical acoustics. V..
Author's SUMMar

N. , I 7t
k~ "Inlrl~l it, dclzoi mc 'A tvr~ng qf
lou'-0 wAvvi fur the C~w 'tt .'OrOnlc M
an rr=r,,pr--wbl-. hqwd ln'"[;pi" lhC CEnCuA
fo~Tr. of lh~ u--It;etlrg :1-4--alr - Arw dC'CMj7l for j(
ar, cxprctsion knx~cd illw r~imula R,ipp
CM Ci Eric SphCrICAl CourdimIn or the tvqm. ond I
tf~ K;li~ lk~AOCICFIZIR. Df '1-!C 01:47agO
pnAaiton ure Th, inal~vi c,( ihi% 1-?,tnairer~n_
Q-, "!t" -a,
of

To -F a v,,- \1 V,
USSR
optics to pcoblems rif the Vqpgattm of walrev throuM
a =dun dontuduill by "t rtfractive Wet
tldatlM V. 1. TATAIMIL A. OkWf, lf4w. lkv
No. 1 (7) 6" (191.13) In Russian.
3 OlMal w1wd (Abstr. 1513 (1952A is used (of
obtaln!ag a moro gencM criterion cmuling the coin-
cidence of waw-fluixt(Ons, mutting from the "uttom
of the two fanUmental equations involwd. It lv-
tMwn that conMans A 4 1, and AL -C P (where i A
6 the krigh of th,~ propagated w.-Nv, I h the a."
sim of fithorrvigen6lics, wd L is the path of wave
in ft lao=Fmcaus tmdfum) are suaki-rit W
miurIng the coincidence of badl IN amplitudes Nr4
in Ond Wmic taftitfort.
r' &ACIOAA4

TATAMIY 1. 26" -
USISR/Physicr; Sound Scattering 11 MaY 53
"S(;attering of Sound in Turbulent Flow," V. A.
Krusillnikov andt~V. I. Utarekiy'~'.tci-Res Inot of
Plusics, Moscow State U
DAN SSSR, Vol 90, No 2., pp 159-162
Analyzes scattering of soumd as sum of scattering by
pulsations of flow and.by thermal inhomogeneity.
Assumes that scattering of sound is responsible for
damping of infrasound In the atmosphere. Presented
by Acad M. A. Leontovich 16 Mar 53.
26oT89

TjnATA,",_C nlVa , V. T
USSR/Geophysics - Conference
Card 1/1 : Pub k4 -lo/1-1
Author : KiriLlov, F.
Title : Chronicles. Conference of young scientists of the Geophysics Institute.,
Academy of Scientists of the USSR
Periodical : IzV. AN SSSR, Ser. geofiz., 495-496, Sep-Oct 1954
Abstract : May 17-20., 1954,, the Geophysics Institute held a conference at which
junior scientific workers participated with 18 reports; eg.g. Ye. A.
Lyubimova (heating of the Earth), S. L. Solov'yev (intensity of
earthquakes in Turkmenia. 1912-1951), S. A. Fedotov (wave hodographs),
Yu. .1. Vasillyev (use of amplitude data in seismic prospecting), 0. G.'
Shamina (elastic impulses during collapse of rocks in earthquakes),
0. 1. Silayevix (velocity of propagation of elastic waves in granite,
marble, etc.), V. I. Tatarskiy (propagation of waves in medium with
random weak inhomogeneity of refraction coefficient), L. P. Zaytsev
(reflection of waves from boundary). A. S. Chaplygina (measuring the
themobaric field in the atmosphere by statistical treatment of empiric
data).
Institution
Submitted

_1-7=SION NR: API;033-164 S/0056/64/046/004/1399/1412
AUIHOR: -,Zq FS-Ve, L.
TITLE: Propagation of eiectror~netic waves in a medium with strong dielectric-
ccnstant fluctuations
SOURCE: ZK. ekspa,% i teor. fiz., v. 46, no. 4. 1964, 1399-1411
TOPIC TAGS: dieleatric constant, electranagnetic radiatim, electycxmgnetic
scat-tering, electrcmiagnetic wave diffraction, correlation, longitudinal wave,
rwaltiple scattering
-1 ETF, v.
ABSTRACT: The restats of an earlier paper (with M. Ye. Gertsenshtey., Zh'_
44, 676, 1963), where the scalar wave equation was considered for the case ka> 1 is also consider-
ed, bL~d a more consistent treatment is given of the field fluctuations. The analy-
sis is restriated to a monochromatic source proporticnal to exp(iwt), and it is
assumed that the me(lium has unity perreability, wro conductivityl and a dielectric
Card
1/2

ACCESSION NR: AP40.112164
consitant which is a randan functicn of the coordinate. For ka c< I the result
reduces to a variatim of the propagation constant and to the appearance of longi-
t~dinal waves. Fcr ka >> 1, the additional attenuation of the average field does
not reduct to a change in k. The mean square field fluctuaticn is also computed
for ka %ce 1 and is found to be smaller than the value obtained in the first-appro-
ximaticn perturbation theory if multiple scattering is taken into account. In
view of the inaccuracy of perturbation theory when it canes to strong fluctuations
of the dielectric mastant in the wdiun, the diagram technique of field theory is
emplbyed. Orig. art. has: 11 figures and 36 formulas.
4SSOCIATION; Instit-xt fiziki atmosfery* Akademii nauk SSSR (Institute of the
Physics of the At=.;b~, Academy of Sciences SSSR)
SUBM=: 140at63 DAM ACQ: 07~~4 ENCL: 00
SUB CODE: AS9 EM NR IEF SOV: 001 GIM: 002
Cord 2/2

Name TATARSKIYO V. I.
Dissertation Microhaterogeneities of a temperature
field and fluctuattion phenomena during
the propagation of waves in the
atmosphere
Degree Cnnd Phys-Math Sci
Defended At Inst Physics of the Atmosphere Acad Sci
USSR
Publication Date, Plaze 1956, Moscow
Source Knizhnaya Letopis' Ko 5j 1957

- - ___ - TAT-ARSM, __ V. 1. - - __ -- - - - - ___ ____ ___ - -___ - - - ____I
"Amplitude and Phase Fluctuations in a Plane Wave Propagated in a Turbulent
Medium with Slowly Varying Characteristics."
paper presented at the 4th All-Union Conf. on Acoustics, Moscow, 26 may - JQ Jun 58.

Y. GT CHI'A.,_ T* rM'M V !-and -T-ZVArD,--L* R.
"Experimental Study of Twinkling crf a Light Source Situated an the Lartki 'a
Surface."
Conf. on
paper present-ed at the 4th All-Union MMKM Acoustics, mosr-ow, 26 MaY - 8 Jun 5)

- - T.AkTALRUSKIv V I ~A.I; jil;6E,
IJ_ _ L, . 6
Ilwave Scattering by Randoin lie terogene i ties of the Refraction Inclex In the
Fresnel Diffraction Approximation". I
report presented at the All-Union Conference on Statistical Radio Physics,
Gortkiy, 111-18 October 1958- (Izv. vyssh uchev zaved-Radiotekh., vol. 2,
No! 1, pp 1.21-227) COMPLETE card under SIFOROV., V. I.)

3(7) SOV/33-35-4-11/25
AUTHORSs Tatarskiy,V.1.9 Gurvich,A.S.,Kallistratova, M.A., Terenti-
Yeva'.L.V.
TITLEt ~?he Influence of Meteorological Conditions on the Intensity
of Light Scintillation Near the Surface of the Earth (0 vii-
:ranii meteorologichaskikh usloviy na IntensivnoBtl mertusaniya
oveta, v prizomnom slays atmosfery)
PERIODICALs iketronomicheskiy zhurnal,1958, Vol 35, Nr 4, pp 623-626(USSR)
ABSTRACTs The authors report on the experimental investigation of the
dependence of scintillation of a source on the earth on the
meteorological conditions. The observations have been carried
out in autumn 1956 by an astrophysical expedition of the In-
stitute for Atmospheric Physics, Academy of Scienoe USSR. It
was stated that the intensity of scintillation and the ver-
tical gradient of the mean temperature strongly correlate
(correlation coefficient 0.92) which shows a good coincidence
with the theoretic4l results of the authors. The investi-
gations have a provisional character and are to be continued,
Card 1/2

The Influence of Meteorological Conditions on the SOY/33-35-4-11/25
Intensity of Light Scintillation Near the Surface of the Earth
There are 1 figure, and 14 references, 6 of which are Soviet,
5 American, and 3 English.
ASSOCIATIONtInstitut fiziki atmoafery AN SSSR (Institute of Atmospherical
Pb7sics AS USSR)
SUBMITTEDs May 25, 1957
Card 2/2

AUTHOR: TOcirnklY, V. 1,
TITLE: On the of Wayes in a Loca".y 1,jotrorio and Turbulont
Medium Witt Oradually Changing Characteri.k;tics (0 rasprostrfnen!-i
vo.~.u v lokallno izotropnoy turbulzininoy arede a
yushchimij,ya kharakter'Astikami)
PERIODTCAL: Poklady lkidemli nuuk ISM, 1958, V01- 12o, Nr 2,
pp. 289 - 292 (USSR)
ABSTRACT: A rumbc-.-i~ ot' .1fictcrz rudL be laken into a-.count in the
of the of the. amplitude and of the phase of -jrr.V":!
which are prc~pnpated im a real atmosphere (or in the ortvaO:
Thf! inten3ity of tmrbulencs~can be different Ln the differt;nf.
do-wains the jet. (Thus, for example, the intensity tf th;-
tavi-u--n~.,e ~f the atmo6phere depends upon altizud*~.). In dcma--*n5
which are 1~krge as compared with the dimensions ?f che tarbulence
~ttc f ( V, 9= D -r"" , 71' ) ae
-egi Dn the atructural func. n -- Ef(rl')- 2 1 2
---1P ---:p
sul-pc-?-~od to leprend. only upon I r1-r21 -In the sp-i~:7ial .a2c In
Card 1/-k qucation the structural function can be represented by a spec:tr-al

On the Propagation of Waves in a Locally Isotropic SOV/2o-12o-2-17/63
and Turbulent Medium With-Gradually Changing Characteristics
expe-nsion. The flUctuations of the refraction index n
can be
i
represented in the form of a stochastic Fourier (Purlye) -Stleltjes
(Stilltlyes) integral. It is possible to repreeent the corre-
lation furretion of the-logarithm of the wave amplitude in the
plane x-L by means of a two-dirnensicnal Fourier (Farlye) trans-
formation of the function P.0C)(which Is defined in this paper).
1.
.
The author then investigates the case - which is of practical.
importance - in which the fluctuations of the refraction index
are described by the "two-thirds" law. The contribution made by
the inhomogeneities to the fluctuations of the amplitude is in-
dependent of the coordinates of these inhomogeneities, it in-
creases, howe,,rer, with their distance from the pcint of observatim.
The formulae deduced in this paper can be used for the purpose
of explaining peculiarities of the scintillation (mertsanye) of
the stars. The "flickering" (drozhanye) of the imagos of the stars
in the isotope3 is cause-J primarily by the lower layers uf the
atmospheret but scintillati:)n is mainly due to the upper lay,-r.q,
Card 214 m
These conclusions ,well agree with astronomical obsarvation3.

24(4), 3M SOV/2o-123-4-22/53
AUTHORS: Gurvich, A. 5.1 Tatarskiy, V. I., Tevang, L. R.
TITLE: 2xperimental Investigation of the Statistical Characteristics
t)f the Scintillation of a Terrestrial Source of Ligl-t
(Ekspei-imentallnoye issledovaniye statistichoskikh kbA---ak-
teristik mertsaniya nazemnogo istochnika sveta)
PERIODICAL: Doklady Akademi-i nauk SSSR, 1958, Vol 123, Nr 4, pp 655-658
(USSR)
ABSTRACT: If the fluctuation of the refraction index n of a medium
obeys the '12/3-law"
4% j 2 2 21F3
Q r C
[n (-r* + ) - n ( nQ3 4
and the conditions X < 1 (1 A L