SCIENTIFIC ABSTRACT ANANOVA, L. A. - ANANYAN, S. A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000101310017-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 20, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

ACOESSAW KR: AP3013324 S/0O22/63/M6/0D5/bnq/b3.23
AUTHO~G i Arutyunyuns F. R.; AnanvvaL~t--~.q- Gri&or.-;an, N, 0.
TrZLE'-. MZhly directional Coronkov counter for rel~tiviatio particlea
SGURG~: AN ArrSSSR. 17.vestiaras Seriya fiz.-4utem, nauk# V& 16o nos 5P 1963P 11,9-,
123
TOPIC TAGS: Cerankov counter, relativistic Cerenkov counterp particle detector,,
charged particle detector
ABSTRACT: A highly directional Ceronk-ov counter has,been designed for relativistio
particles of threshold magnitude
Othres-h 2
using the principle of total reflection from the base of the radiator (detector) as.
wen as from the side wan surfacess The trapped radiation in the detector can
0t
then be used to date -~articlos with &,a > 0#995j which) in ter= of the angle Y
botween the normal to the radiator base and the incoming particle beam direction,
Card 1/2

ACCESSION NR: AP3013324
can be represented by j6' t~~sh
tlu~ Cos 7 ng-po
where n, - reflective index of the radiator# and n2,- the reflective index of the
media surTounding the rudiat'or. Orig. art. bass 2 equations and,2 figurese
:ASSOCIATION: none
SUBMITTED: 2alar63 DATE AOQ: 22Nov63 ENCLs 00
SUB CODE: PH NO REP SOVs: 001 003
OTHERs
card 2/2

SOURCE CODg.----UR/0252/66/043/002/0087/0090.1
ACC NRt AP'(005541
AUTHOR: A ~.Oyap R gan&yan, R. A.; Petrosyan. Zh. V.
na A.; Arut3, 04j I.
T'"Joint Radiation Laboratory of the
oRG: Physics Institutei(Fizicheskiy InstJ I
Academy of Sciences of & Armenian SSR and of the Yerevan State University (0b"ye-
dinennaya radiatsiomWa laboratoriyu Akademii nauk ArnVanskoy SSR i Yerevanskogo
gosudarstvennogo universitets)
TITLE: Transition radiation in oblique passage of electrons through aluminum films
SOURCE: AN ArmSSR. Doklady, v. 43, no. 2, 1966.. 87-90
TOPIC TAGS: metal film, aluminum, electron bombardment,, transition radiation, elec--
tric polarization, angular distribution
ABSTRACT: This is a continupLtion of earlier work (ZhETF Pis'ma v redaktsiyu v. 3,
193, 1966), dealing with normal incidence of electrons on films of different metals.
In the earlier investigation no radiation component polarized in the perpenducular
plane was observed in the case of aluminum. The present article contains the results
of an investigation of the transition radiation produced when electrons with energy
60 kev pass obliquely through films of aluminum of thickness 124 - 329 A. It is shown
that in the case of oblique incidence., a perpendicular radiation component appears,
the magnitude of vhich increases witb the angle as the a1tter rises from O'to 45%
The polarization of the radiation Is then no longer Unear and the plane in which the
mwdixum. intensity is observed does not coincide vith-the pl:.ae containing the normal
Card 1/2

ACC NRt AIP706554i.
to the surface of the film and the observation direction. The component polarized inj
the direction of observation also exhibits an anomalous behavior. The absolute value
of the perpendicular component is on the average one order of magnitude higher than
predicted by theory.. and the com'ponent in the obs tion direction is about half the
value predicted by the thoery. However, the angu!Tdependence agrees vith the theo-
retical distribution. It is proposed that the discrdpancy is due to the special
structure of the aluminum filmp but the lack of a thiory of transition radiation in
the case of inclined incidence of the particle in the crystal makes it impossible to
draw any final conclusions. This report was submitt4d by Corresponding member AN
ArmSSR M. L. Ter-Mikayelyan 20 AprEL 1966. Orig. az-i. has: 3 figures.
SUB CODE: 26,1# MM DATE: 60/ WM UF: 005/ OTH REF: 002
Card 2/2 i

ANANOVA, Ye. W.
"New Data on Sarmatian Vegetation In the lower Dnieper Area," Bot. Zhur., 2.7,
no. 2, 1952
PaleobotarW - Dnieper Valley

ANANOVA, TO.N.
Oszunda cinnamomea L. spores in the interglacial Kindel-Rise
deposits around the town of Likhrin. Dokl.AN SSSR 93 no.5:1089-
iogi Ap 154. (MLRA 7:4)
Predstayleno akademikom V.N.Sukaehevym.
(Likhvin-Spores, Yousil) (Spores. Yossil-Likhvin)

ANANOYA, TO.N.
~4-w
Now data on the flora and vegetation of the Pliocene. Dokl.Aff SiSR 96
no-3:625-628 My '54. (MM 7:6)
I.Predstavleno skademikou Y.N.Sakachavym.
(Volga Valley--Paloobotany) (Paloobotany--Volga Valley)

AUTHOR: 20-1-55/58
TITLE: The Pollen Morphology of Polygonum bistorta L.
(Morfologiya pylltay Polygonum bistorta L.)
Normally Developed and Underdeveloped Forms
Pormallno razvityye i nedorazvityye formX).
PERIODICAL: Doklady AN SSSR, 1958, Vol- 118, Nr 1, pp. 194-196 (USSR)
ABSTRACT: Among the fossil-Quaternary pollen the author found pollen-
grain& of a peculiar shape as if they had another, higher
stage of fossilization. They had indistinctly marked structural
elements (grooves, pores and so on), the thickness of "exines"
was badly visible and in most cases the sculpture or texture
wIas hardly marked. The surface usually shone like mother-of-
pearl. Such pollen was hard to draw, even to describe. In the
case of small grains the plant family sometimes even is un-
definable. Doubts rise whether this pollen was not re-deposited.
In the old-Quaternary inter-stadium sediments of the lower
Kama-river the author among others found pollen-grains which
remotely recall Polygonum with the aid of preparations of
samples she found out that this pollen belongs to an under-
developed forms of Polygonum bistorta. The morphological
Card 1/2 peculiarities of the pollen of this plant are described in

The Pollen Morphology of Polygonum bistorta L. 20-1-55/58
Normally Developed and Underdeveloped Forms
publications (references 1,2), but the underdeveloped pollen
was disregarded. The author gives a detailed description
together with representations of this pollen. It belongs
to the group Pf 3-grooved and 3-pored plants. It most
resembles the pollen of P. ellipticum. These descriptions
shall .!,xve the palinologists in the determination of genus
and species of the pollen.
There are I figure, and 2 references, 1 of which is Slavic.
PRESENTED: September 7, 1957, by V. N. Sukachev,
Acedpmician
SUBMITTED: August 4, 1957
AVAILABLE: Library of Congress
Card 2/2

AHAWVA, U.N.
"Periglacial" flora from lower Quaternary deposits of the
Kama Valley. Probl.bot. 4:92-128 159- (mIU 13:1)
(NAberexhM7e Ghelny region-Palynology)

3(5) SOV/20-126-2-37/59
AUTHOR: Ananova, Ye. N.

TITLEi The Kashpirovka and Kreking Pliocene Plorae
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 128, Nr 2, PP 355-358
(Ussli)
ABSTRACT: 25 years ago, P. A. Nikitin found conifer pollen in exposures
near Syzran', Lower Povolzhlye (Volga region). He believed that
the pollen complex found pointed to a conifer- or taiga type of
the Pliocene phase (Ref 8, p 70). Nikitin assumes that accord-
ing to their stratigraphy these form3 correspond to the end of
Akchagyl, i.e. to the tai6a phase of the Ttentrallnaya
chernozemnaya oblast' (central black-earth region). The data,
although very rare, enabled Nikitin to draw a perfectly cor-
rect conclusion concerLng the basic character of vegetatior. in
the regior. investigated in a certain Pliocene stage. Since 1954
very valuable palinological material from Pliocene has been
collocted in layers in connection with an extended water
building activity. The Kinell strata in the region of
Samarskaya Luka (Samara bow of the Volga) were investigated by
Card 1/3 M. N. Grishchenko (Ref 4). P. I. Dorofeyev analyzed the seed

The Kashpirovka and Kreking Pliocene Florae SOV/20-126-2-37/59
florae of Povolzhlye (Volga region) and the lower Kama
(Refs 5-7). An image of the plant cover of the afore-mentioned
region during a longer Pliocene period nay be reconotructed on
the strength of this material, as well as its evolution and
successions. The author wants to complement here the know-
ledge of Pliocene flora and -vegetation on the strength of an
investigation of Plidcone deposits made in the environments of
Syzran' from 1950-ql- Material of M. G. Kipiani and A. D.
Kolbutov served this purpose. K a s h p i r o v k a
f I o r a t The complex consists of 88% tree pollen, 3;,4v herba-
ceous plants, 4 and 50/6 fern- and moss spores, respectively.
Spruce-trees of the section Eupicea predominate among the
pollen, followed by pine-trees of both subgenera. Tsuga, fir-
tree (Abies), and deciduous trees occur very rarely. The entire
pollen has the same degree of fossilization except the rear-
ranCed Mesozoic spores. K r e k i n g f 1 o r a : 85% of the
pollen belongo to tree specieu. Herbaceous plants and under-
shi* -ubs reach 10~, fern- and moss spores 3 and 21%, respectively.
The section Eupicea predominates here as well (55%), pine-tree
pollon play an important role-The pollen of Tsuea, fir-tree,
Card 2/3 elm, and several other trees is rare. The lists given and the

The Kashpirovka and Kreking Pliocene Florae SOV/20-128-2-37/59
percentage ratios of the pollen indicate distinctly enough the
taiga type of the wood. Nikitin's interpretation of the age of
the containing deposits is correct in general but needs one
correction: they do not belong to the end of Akchagyl, but
more probably to iLs lower part or even to the topmost parts of
Kinell. The roijults obtained by H- author agree well with the
data of A. A. Chiguryayeva for southern Predurallye (pre-
Ural region, Ref 9). There are 0 Soviet references.
PRESENTED: April 3, 1959, by V. N. Sukachev, Academician
SUBMITTEDi April 2,
Card 3/3

AWOVA, To
, N~.
Redeposited pollen cotplaxes. Bbal,HDIP. Otd.biol 65 U0.31
132-135 161-Jo 160. (MIRA 13t7)
(PALTHOLOOT)

ANANOVA Ye N
Pk3jynological data on the volume and lower boundary of the
Quaternary. Trudy Kam. chetv. per. 20t67-8~ 1624
kMIRA 16:1)
(&]~Ynology)

I ~l ~ ll~ , - ~/
f , . / , : e y r:l
I i 'r~. V ,

ANANOVA, Ya.V.; YEWLIYANOVA, O.S.
Use of the fluoresceni~-serological method for the detection of the microbe
of tularemia. Lab. de2,o no.1:35-39 164. (MIRA 17:4)
1. Laboratoriya tulviwemii otdela irfektsiy s prirodnoy ochagovostlyu
Instituta epidemiologii i mikrobiologii im. N.F.Gamalei ANN SM.

ACCESSION NH: AP4025079 S/0016/64/000/003/0092/Oo95
ATUTHOR: Ananova, Ye. V.; Saveillyeva., R, A.
TITLE: Possibility of F, tulexensis penetration through uninjured
3kin (preliminary report)
SOURCE: Zhurnal milwobiologii, epidemiologii i immunobiologiij
,;no& 3P 1961~p 92-95
TOPIC TAGS: F. tularansis., uninjured skin penetrations F. tularensis
i.noMhology, hair follicle, sobELCOOUS gland duets histological
.iinvestigation
';:ABSTRACT: Lateral body areas (if 13 guinea pigs-were sheared and 48
Ihrs later a 1 ml drop of an F. tular nsis culture containing a
.,billion microbes was applied to 1 CM9 of the sheared area to determine
.possibility of penetration through uninjured skin. Special procau-
-tions were taken to allow the 6-rop to dry thoroughly on the skin and
to avoid the possibility of being rubbed into the skin, During 0
the
following week histologioal investigations wero made of infeoted skin
areas in 22 guinea pigs displaying a reaction, Eleven of the 13 gui- 1
Card

CCESSION NR: AP4025079
Inea pigs had become infected and. died within 8 to 13 days. The other
;2 guinea pigs remained healthy as was confirmed by serological and
'allergy tests conducted a month after infection. Thus., the skin is
:not an absolute barrier for F. tularensis. Histological. investiga-
I
Itions indicate that microbes appear to penetrate through the hair
,follicles and sebacoous gland ductso Orig, art, has: None,
I!ASSOCIATION: Institut opidemiologii i mikrobiologii im. Gam'alei
MIN SSSR (Epidemiology and Microbiology Institute,,AMN SSSR)
SUBMITTED: 02-Tan63 ENCL: 00
SUB CODE: LS
2
NR REF SOV: 007
OTHER: 002

....... .
JK
L 6838-i-65 EEMCI)IM(b)
ACCESSION AF4039933 S/06A/W600/005/0024/0028
:AUTHOR*. Anshovaip Y19 Ve
-VITLE: Investigation of expDrimental tularemia pathogenesio
~SOURCE: Zhurnal m1.krobio1oSXi# epidemiologii,I immobiol6giip no o,. 50:
11964.- 24-28
TOPTC TAGS! tularconinj F. tularensis strain No. 503t F, tularensis
Schu strain, tularf-mia sentiltivity difference, tularemia psithogenesis'
F. tularensis norw-ctic va-ri.ety, F. tularensis palearetic variety,
,tularemia sensitivity of micej, tularemia senoltivit-4, of rats,
~tularemla sensitivity of osits
ABSTRACT: Thpee groups of imimals with different tularemia sensitivA4
ty were ir-focted -with virulgnt tularemia strains In a series of
experiments to compare pathogenesis In each grour. The ftrst group
consisted of white mice vita a high susceptibility and a a high
sensitivity to tularemia, the second group consisted of white rats
with a high cuseeptibility and a law seneitivity, to tularemiag arul
the third Sroup cc)nsistea of eats with a very low susceptibility a.-A
Icarj- 1/3. .... .. ....
OEM -1-77

----------
-ACCESSION NR: AP4039933
practically no sensitivity to tularemia Tularemia pathogenesis in
ihe second group was of greatost iWvoreat because the susceptibility
and sensitivity of the human organism is comparable to that of white
rats. Anima.ls wore Infected suboutanvounly with virulent F,
t,dlaronsls st-sin 11o. 503 (a palearctic varloty) or Schu sty-nin
(a nonarctic; -iariety) in a large dose contalnin~~ I billion bacteria
cells or a small dose containing 10 bacteria cells. Anima13 were
killed 19 2, 3 days or lator and material was prepared for morphologi-
cal investil-ations. The extent of the Infectious process was based
on the number Of tU"Laremia btetoria found In the lymph nodes, spleen.,
and liver. Findinga show theit tularemia infection differed clinically
and btkc'Uerio2og1ca3*L-y as wol-'. as pathomorphologioally in all three
groups infected witft a small dose of a tularemia virulent E.train. In
the first gronp (white mico):, tularemia infection induced by a small
dose was mostly of an exudat Lve-alte:r Fit Ive nature wbich indicates
that the organism is COMDletql-y defenseless in relation to virulent
t ul ar end a .--1n the second grDup (uftite rats), tularemia intection
'11jaduced by a small dose wa3 nostly of an exudative-prolifanative
-----'r~ature wittt-mar-ked protective reaotion in tisaues, With large dose
jinfection of the f Jr-st-iVidl- pacond-groupayl- the differences disappeared
6rd PA

L 6838-65
ACCESSION NR: AF4039933
and tularernia Infect-Ion developed at an accelerated rate with
predominantly exudative-alterative changes in the organs. In the
third 1-roup eats) Vaish was 1:nfected with only a large dose, the
tularemia infection process was of a benign nature with a vory
moderate inflltratio.,i of collidar elements. The P. tularencis
nonarctic variety (No. 503) p-7oduced more marked pathologic)al and
morphologiccl changas in all ;he animals regardIrS13 of f-,roiip. The
differont reactJvlty of the tivree groups is attributed to a different
call sensitIvity to the toxic action of F. tularensis. Orig. art.
- ---------------------------------------
baw Hone-
-1AS-SOCIATTON*,--- i--MilWobiolo'R Im* Gmnleyl
APT14 SSSR (Eyiderniology and Miz-,robiology Mnstitute U'UT SSSR
SUBIKITTEDo 05Feb64 ENC-A 00 SUB CODE; LS
VR RLY SOV: 009
OTHER: 002

ANANOVA, Ye.V.; SAVELIYEVA, R.A.
I. .......................................,
Possibility of the penetration of the pathogen of tularemia through
uninjurod skinj preliminary report. Zhur. mikrobiol., epid. i immun.
41 no.302-95 Mr 1:64. (MIRA 17:11)
I- Institut epidendologii i mikrobiologii imeni Gamalei AMN SSSR9

nj-, 1 ) /EVA 4 ) /FATA (b JX
2 9L _6~
Q ~ 11
N_.~; A P5 o ) 5 0 -16
S/0 10' A 5 A) 0 0/ 0 3 3 /006 5100 7 0
ATJ7.H OR Savellyava, R. A.; Ananova, Ye. V.
T 1-4. :,E Fatac,genesis of the pulm-onary form of experimental
tularemia
SOURCE: Zk-..u-,,nal mJkrobioloE,ii, epidemiologii i iminunobiologii,
no. 3, 1965.. 65-70, and toy third of insert facing p. .35
--OPIC, TAGS: guinei. pig, mouse, rat, tularemia, pulmonar,r tularemia.,
I I
,Lung., pathogenesis I
S 7RA' C T Tularer-a Infect Lon by aspiration and pathogenesis of the
C'~- -pi[.
_:_.-,c)r,.iuy :'orm of --.ularemia were invost. ated ir. guinea -,s, albino
... co, a,-,d 3LIbIL,-,o :-its In twa experlmorta_ th a first series
.3 a-. Lmal 3 w e r a a c e d ir, t o a s ne c a_-,b- e r 73
an i a
y V a. "1 53 3
bacterial syspenslan of a
was sprayed in the form of a fine mist (20-40 rLL bacterial suspension:
per hr). The numbar of baoteria in a suspended state at the start and
and of the expariment was eletermined b-j ai-I samples using a Krotov i
apparatus, A Petrie cup fIlled with 10 ml of a physiological solutlo~'_
Card

'L b29L2-65
ACCESSION NR': AP5001-M6
was plaead into the Krotov apparatus and 100 1 of air from the chariber~
was pa3sed throuCh tae fluid, Tho rosultinr, suspension was titerod
.1 41 nTr f~n v; -o c)f the SUSDon-
sl~~n and upon tnei.- death de';ormilnln~ z:-.a L,acLurial coils In
and tho7~oby 'in 10 1 of air). :n exparimental ser'Les
y forn, -,f z-,--a-r0.7!a studied in
7,athoE;enez,is of t~ie pulmv>nar-
r. v e g a ng P a L C, 0C an 5 0 f Un'-
n r)
a--4- ~n 4
~7 r a C n e 0r on cr~ al
P
later date the -Druccss assunzs a specific granulomatous nature wiTn I
Card 2/3

L 42942-65.
ACCESSION NR: AP5008016
,neerobiosis and necrosis in the grmulorms. Orig, art, hen: 1
fig-ire and I table.
~SS,-jr-iJkTTO'N'- Instu-11 tut opideniologil i milwobiologii in, W. F,
-ItE of Ep-'(~or'.LG- 7y 'nd Xiczrolblcic'
-C a t77Y
T:,,%T,T,: 00 SUB CODE: LS
r" v 6"
IV: oo6 OTHER: 000
Card 3/3

LESHCHANSKIr. ru..T., kando tekbno nauk; ANANSKIMp V.M., inzh.;
MMEVA,, O.N.-P inshi - - =NO
Electric pkkrametera of sand and clay in the range of centimeter
and decimeter radio waves. Trudy MPTI n0-10:49-57 162.
- (KRA 16t. 6)
(Soila-Slectric properties)
(Radio waves)

TITEMNILOVA-BAALYAN. D.N.; ANANUN, A.A. GASPARYAN, N.A.
**MW*MW*,*QM;
Susceptibility of tomatoes to fusarium wilt and mosaic disease in
the Armenian B.S.R. Izv.AN Arm.80.Biol.1 sellkhoz.nauki. 9
no.4:49-58 Ap 156. (XLU 9: 8)
1. Xafedra morfologii sistematiki rasteniy Yerevanskogo gasudar-
stvennogo universitets Imeni V.M. Molotove, i ArmTanskiy opornvy punkt
po ovoshchevadetvu Vuesoyuznogo na-uohno-iseledovatellskogo institute.
konserv,noy promyshlennosti.
(Armenia-Tomatoes-Diseases and pests)
(Tomato wilt)
(Mosaic disease)

ANANYAN. A.A.; YAGIAZARYAN. A.G.
1016
Iffect of fertilizers on the Increase in yield and dry matter content
of the tomatoes In the Armenian Lowland. Izv.AN Arm.SSR. Blol. I sell-
khos.nauki 9 no.8:91-99 Ag 156. (miaA 9:10)
1. Armyanskiy opornyy punkt Teesoyusnogo nauchno-iseledovatellskogo
instituta kouservuoy i ovoshcheaushilluoy promyshleanouti.
(ARIIINIA--TOKATCIBS) (YMILIZIRS AND KANMS)
6

USSR / General Biology. Genetics. B-5
Abe Jour : Ref Zhur - Biol.
j. No 12~ 1958, No 52448
Author : Armnyant A.-A,.-..
Inst Tot ~ von
Title New Torato Varieties Obtained by Vegetative and Vegetative-
Field Hybridization.
OriG Pub j%grobiologiya, 1957, No. 2, 58-64
Abstract The author grafted hybrid tomato plants (second generation
in the stage of two-leaf formation on stemiy. towto varie-
ties, resulting, according to the author, in the obtaining
of a stemiy variety of tonato with a high percentage of dry
mtter in the fruit. The author ascribes this result to n
corabination of effects of hybridization and grafting, rnd
calls such forns vegetative-field hybrids. -- S. Ya. Krayevoy.
Card 1/1
P-1

ANANYAN, A.A.
Kona. i ov. prom. 13 no,5:27-28 My '58.
(KIRA 11:5)
l.Arnyanakiy oporT*7 punkt po ovoshchavodetvu.
(Pepper--Varieties)

TNTERMIKOVA-IIARAYAN, D.N,,; ANANWT, A.A.; INGIAZARTA , A.G.; CASPARYAN, N.As
Iffect of organomineral fertilizers on the development of
fusarium wilt In tomatoes. Nauch.trudy Xrey.un. 64-993-104
1589 (MIR& 11:12)
1. Kafedra botaniki Terivanokogo gosudaretyennogo universiteta
I Armysmskiy opornyy punkt Vseaoyuznogo nauchno-inaledovatell-
skogo Institute, konservaoy I oveshcheaushillnoy promyshlennosti.
(Tomatoes-Fertilizers and manures) (Tomato wilt)

MANYAN, A. A.; TAROSOVA, Ts. 0.
Variability of the ainount of dry matter in tomatoes and the
methods for its incroass. Izv. AN Am. SSR. Biol. nauki 15 no.4:
19-27 Ap 162. (MIRA 15:7)
1. Opytno-selektsionnaya stantolya ovoshchevodstva Hinisterstva
sellskogo khozyayetva Armyanskoy SSR.
(TOMATOES-VARIETIES)
Liu

ANANYANp A.A.# kand.sel'skokhozyaystvennykh nauk
Developing tomato varieties for the canning industry. Agro-
biologiia, no.6s843--847 N-D 162. (KMA 16i1)
1. Opy~tno-selektsionnaya stantslya ovoshchevodstvat Armiyanskaya,
SSR.
(Amenia-Tomato breeding)

ANANYAN, A.A.; TAIDSOVA, Ye.O.; VAROSYPI4, R. Ye,
Change in the biochomloal indices of tomittoes as a result of
vegetative hybridirtition. 3:zv. AN Ax-m. &SR. Blol. nauki 2.4
no.965-44 S'63 (MIRA 1!.-7)

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to z the I= "h-Nrr f4fiml 1w1wrv" the A111%le, And oir
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Pt. A. and ANDR-1~',NOV) P. T.
"Study of Relative Tentperature, Thermal Conductivity, Specific Heat,
of Soils in Permafrost Areas and Electrical Conductivity of P;rnafrost,11
Vest. AS USSR, pp. 82-85) 19L6
Sr. Sci. Assoc., Igarka Frost Station, Inst. Pernafrost, AS USSR

CA
Displatomeat of moisture In flaxen loo" rocks under the
action of 44ectrobarnows. _ AI,, j,; wd. Zkup.
, LT Xvil
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14. Z"i fully IM Inobilt
up~
and availshic to plants. 1*0 test its Inobility. clectfo.
Wumis inks used, To the hases W a 04y priwo, 7.6 X
h X 44 cut., staur"Stvirl ttertmica vtrfc jamsed and it cur-
trill of W-135 V. and 6-1.1. Inillianip. .20 passed for 0 days.
The trinp. tit the vvisirr tit the prisin wa% - IX to -2.1 '
Unit 11M the Mundt! -11A 11) - I.M', 'I fir ittillil Ittolilure
colittut of the sainple wait 3S% tit vthich 441;,, wits Ire.
After the tapt. (lie inuistuic rnatent int-ir-sed front ;,17r
"'st to the itnudr to 65% ovitt to lite cathodr. I'lusli. 1110
it transported with pas, curtrut also In frozen wils. The
jw'ceu1Ajrr of liquid IljO in lite sample ultri the expt. was
2J% everyvilterit: only the it* s"turd to Ie tratiss-MvL
Presull'ahly there is an equilibrium ljet*ccn Ice and liquid
water Ahkh Is drid. by the surface forces.
(it liquid wa'lcr At a stout In the and Is too great the excess
If"Sts. SitnilaT results virte obtained at -0-2, and
the rate of clectrutisitiosis lncrrA~l with tefull,
The clay vot,sixtcl of after-nale dark and light layrts. and
the curt-ent towed alouc the layers. The dark layers con.
talned more (1A% aXitinil.3.3%) of thefine I)utticlcs(< 0.001
MM.) And had greater plasticity than light layers.
J. ). Ilikernistv

AUTHOR: Ananyan, A.A. V - 5 - 5 P -2- 55 /4 3
TITLE: The Application of Kinetic Conceptions Developed for Aqueous
Solutions of Electrolytes in Water Contained in Rocks
(Primeneniye kineticheskikh predstsvleniy, razvitykh dlya
vodn.vkh rastvorov elektrolitov v vode, soderzhashcheysya v
gornykh porodakh)
PERIODICAL: Byulleten' Mbs~ovskogo obshchestva ispytateley prirody -
Otdel geologicheskiy, 1958, Nr 2, PP 15F-159 (USSR)
ABSTRACT: In fine-dispersed rocks, the orientating interaction between
the active centers of the surface of mineral rock particles,
the molecules of water and the ions, exerts an influence on
the translation movement of the latter, deforming the tetra-
hedral water structure. In accordance with the theory of
activated jump particles of the liquid, the following formula
is mentioned by the author and explained in detail:
E
j - Joe - E +4 E and j - joe "RT
RT
where
j is the number of activated jumps of water molecules per
second;
Jo is a forexponential multiplier, approximately equal to the
Card 112 doubled frequency of oscillation of molecules around equi-

COV-5-5,-2-35/43
The Application of Kinetic Conceptions Developed for Aqueous Solutions of
Electrolytes in Water Contained in Rocks
librium state;
E is the activation energy for pure water;
AE is the change of the potential barrier by ions;
is the change of potential barriers iinder the influence of
active centers,
R is-the gaseous constant, and
T is the absolute temperature.
1. Rock-Moisture content 2. Water-TheorY 3. Mathematics
I+. Electrolytes-Properties
Card 2/2

SOVI 49-58-12-10/17
AUTHOR; __ Ananyan, A._-A.
TITLE: Effect of Moisture on the Electric Conductivity of Frozen
Rocks (Zavisimost' elektroprovodnosti merzlykh gornykh porod
ot vlazhnosti)
PERIODICAL: Izvestiya akademii nauk SSSR, Seriya geofizicheskaya,
1958, Nr 12, PP 1504-1509 (USSR)
ABSTRACT: An investigation was carriqd out on electric conductivity
as relatedto the moisture of'pulverized rocks remaining
frozen over the course of years. The results of observat-
ions are shown in the form of tables and graphs. Table 1
and Fig,l represent the data for the loam with the lower
plasticity level 23.3%i Table 2 and Fig.2 - 22%, loam.
Table 3 and Fig.3 - 29.2%, clay. Table 4 and Fig.4 - P-1%7
loam. Table 5 shows the quantity of not-frozen water in
the latter sample. The analysis of the data shows that the
lowest electrical conductivity of frozen loam occurs when
its moisture is equal to that of the lower plasticity level.
This was not so clearly expressed in the case of clay, where
Card 1/3

SOVI 4 9-58-12-10/17
Effect of Moisture on the Electric Conductivity of Frozen Rocks
experiments showed that at -0.30C the quantity of water is
usually higher than the moisture of the layer plasticity
level. Generally, it can be stated that the electric con-
ductivity increases with a decrease of the ice coefficient
and an increase of non-frozen water content in the pulverizecl
rocks. Actually, the water content of rocks should be con-
sidered as a solution of electrons (Refs.4 and 5). Therefore,
the dynamic properties of water molecules under the action of
an eleCt3.'iC field, should be determined. This can be ex-
pressed by Eq.(l), where j - the numbgr of "jumps" by the
water mo.!ecule, each equal to 5.9 x 10' per sec (Ref.8),
jo - a constant, equal to the double frequency of the mole-
cule vibration, (p - base of the natural0log, E - the active
energy of water = 4.6 k cal/mol. at +25 C- R - gas constant,
T - absolute temperature. The expression Zl) takes the forn
(2) in the case of rocks where some of the particles are
scattered with the molecules of water. The value of ~ in
Eq.(2) represents the coefficient of variability of the rock's
outer hard surface, which can be calculated from the funct-
ion ~ ~- f(m, 1), where m - mineral content of rock, 1 -
Card 2/3 distance between the rock's outer surface and a water molecule.

SOVI 49-58-12-10/17
Effect of Moisture on the Electric Conductivity of Frozen Rocks
It is evident that j> Jor , Therefore, 6j can be found
from the exprassion (3). This shows that the number of
active jumps of the water molecules contained in the rocks
is smaller than that in normal conditions. From this it can
be deduced that in the case when ice particles form a
barrier between the water molecules and the rock's hard
surfacel the number of active "Jumps" diminishes, which causes
a decrease in the electric conductivity to its certain
minimum value. There are 5 tables, 4 figures and 8 references,
of which 6 are Soviet, 1 English and 1 German.
ASSOCIATION: Vsesoyuznyy proyektno-izyskatellnyy i n.-i.institut
"Gidroproyekt" (A.11-Union Dcsigr.-Pla -,--ing and Scientifte Re-sen-xzh
Institute "Gidroproyekt")
SUBMITTED: January 10, 1958.
Card 3/3

AIUNTAN, A.A.
Using kinetic concepts of electrolytic aqueous solutions In
water contained In rocks. Biul. WIP. Otd. goal- 33 no.21
158-159 MrAp 1c:8,, (KRA 1W0)
(Water-Aralysim) (Rocks)
4-

AWMAN, A.A.
-*-" 1 ---,
Relationship between water and rocks In the light of concepts
on the structure of water. 11auch.dokl.vys.ahkoly; geol.-geog.
nauki no.2:14-17 '59- (HIRA 12:8)
1. Hoskovskiy universitet, geologicheakly faktilltat, kafedra
merzlotovedeniya.
(Water, UndergrouzA) (Rocks)

30)
AUTHORi
TITLE:
PERIODICALt
ABSTRACTs
Card 1/2
SOV/170-59-4-13/20
Ananyan,.-A.A.
Some Peculiarities of Interaction of Water With Rocks (Neko-
toryyo osobennosti Tzaimodeystviya vody a gornoy porodoy)
Inzhenerno-fizicheskiy zhurnal, 1959, Nr 4, PP 93-97 (USSR)
Water contained in rooks can often be considered as a solution
of electrolytes. The concept of the thermal motion of the
particles of a. liquid developed by Frenkel,Z-Ref 9-7, Samoylov
f-Ref 7-7 and others provides a new viewpoint for consider-
ing the problem of interaction between water and rocks. The
author generalizes Samoylov's method for the case of inter-
action of water molecules with active centers of the surface
of rook particles. As was shown by I.V. Popov Z_Ref 6-7 this
interaction iEs determined by the mineralogical composition, the
number and chexacter of the active centers of the surface, the
existence of ione in water, and the thickness of water film'
and separation between water molecules and ions on the one hand
and the activo centers of the surface of rook particles on the
other hand. The motion of moisture in thinly dispersed rooks
is considered under the influence of temperature gradientg
Y7

ANAMN, A.A.
RolAtion betwem the time of freezing and the amount of watnr
contained in finely dispersed soils. VenteMookouneSor.biol.,
pachv., goal., geog. 14 no.2:171-180 159. (KRA l3t4)
1. Kafedra mortlotovedoniya Monkovskogo goo. univoruiteta.
(Soil freezing)

ANANYAN, A.A.
)-echanism of ice separatioa in frozen soils during electroosmosis.
Vast. gook. un.S er.m at., mekh.,astronrfiz.. kh1m. 14 no.4:149-151
159. (MIRA 1):?)
1. Kafedra merzlotovedeniya Hoskovskogo universiteta.
(Frozen ground)
Cm VdEg11

A~k"A
Nffeot of the.structure of water and %hermal motion. if molecuLas on
ice fromation. in freezing and frozen rooks. lest.mo8k.an'. Bar. biol.
pochv., geol,, geog. 14 no.4:175-187 159. (HIRA 13:6)
1. Tafedra merzlot;ovedeniva Hoskovskogo universiteta.
Orrazen ground)

AWANYAN, A. A., Doe Geol-Min Sei';-- (diss) "Phase transitions in
water and electroconductivity in freezing and frozen rock." Mos-
cow, 1960. 26 pp; (Moscow State Univ im M. V. Lomonosov, Geology
Faculty); 150 copies; price not given; list of author's works on
pp 25-26; (KL, 17-60, 143)

ANLNYAN, A,.A,.; MULIN, V.V.
Second layer of frozen rooks in the Salekhard region. Trudy
Inst.mersl.AN SSSR 16:141-149 160. (HIRA 13:4)
(Salekbard region--Frozen ground)
I

ANANYAN, A.A. kand.geol-.-miner.nauk
Studying processes of moisture migratiorL and the formation of
segregational ice in freezing and frozen rocks. Trudy Gidroproekta
3:121-148 160. (KM 13:7)
1. Otdel inzhonetruoy geologii Vsosoyuznogo proyektno-izyskat4I'skogo
i nauchno-iasled.ovatel'skogo institute " Idroproyekt" imeni S,Ya.
Zhuka.
(Sail freezing)

AUTEOR:
TITLE:
PERIODICAL:
Ananyan, A. A.
- -----------
Blec'troconductance of
ture. in the R. Igarka
Referativnyy zhurnal,
stract 6A3ES (Merzlotn.
206-215)
S/169/62/000/006/006/093
D228/11304
frozen rocks of a natural strue-
area
Geofizika, no. 6, 1962, 8, ab-
issled., no. 1, M., MIGU, 1961,
TEXT: The eletrocondue-,ance of rocks of a natural structure that
have been frozen for maiV years was investigated in specimens from
prospecting shafts and wells. The measurements %here made at tempe-
ratures from -0.3 to +1.200 by means of a Kohlrausch bridge, with
the use of alternating o=rent. The phase composition of water in
the frozen rocks was determined in an isothermic colorimeter. El-.:
ectroconductance values were obtained for clays, loams, sandy
loams, and sand3 with different textures and various inclusions.
It is shown that the electroconductance of frozen rocXs is princi-
-pally governed by the degree of dispersion of rocks and by their
Card 1/2

S/1 69/62/000/006/009/093
70 0 D228/D304
;L-UTHORS: Ananyan, A. A. and Dobrovollskiy, V. P.
Electroconductance of frozen rocks of a natural struc-
ture in the R. Salekhard area
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 6, 19062, 8, ab-
stract 6A39 (V sb. Merzlotn. issled., no. 1, M. YIGU,
19061, 216-226)
TEXT: Laboratory determinations were made for the electroconduc-
t1ance of specimens of frozen rocks of a natural structure and mois-
c,ure. Comparison of the data of measurements, ol5tained with -the
application of alternating and direct current. shows that they
-j~actic nce
ally coincide. It is estabIl'shed tha-u 16he electroconducta,
of loose frozen rocks is largely determined by the water's *phase
composition. In the freezing of rocks the electroconductance.de-
creases suddenly. It is noted that rocks of a similar genesis are
characterized by approximately identical electroconductivity va-
lues. /-Abstracter's note: Complete translation._7
ri
Card 1/1
1C

AMMAN, A.A.; DPDROVOLtSKIYj, V.P.
Electric conductivity of frozen ground. Geol. i geofiz. no.3:96-103
161. (MIRA 14: 5)
1. Moskovskiy gosudarotvennyy universitet.
(Frozen ground-Blectric properties)

ANANUN. A, A.
Relftlonobip between the liquid water oontent of finely
dispersed frozen ground and the water properties of suoh jlftid.
Merzl. issl.. no.11184-189 161. (MIRA 1621)
(hozen ground)

ANANYANP A. A.
Speetfte electric conductivitY of frozen ground of natural
structure from the Igarka region. Merzl, isal. no.18208-215
063, (MIRA 16ti)
(Igarka region-Frozen ground-Blectric properties)

i
ANANYAN, A. A.; DOIBROVOLISKIT, V. P.
SpealfIcy slectrio conduotivity of frozen ground of natural
struottwe from the Salekbiwd region* Moral, isel, no.It216-226
161o (MIRA 16:1)
(Salekhard region-Frozen ground-Blectric properties)

MUNAN, A.A,
Studying the depth of the freezing and thawing of rocks
under natural oonditions using an electric frostdepth
metar. Merzl. isal. no-3.-118-126 '63. (MIRA 17: 6)

ANA."YANY A.A.;
Change in biochemical charact,ers of tomatc-cr as a of
complex '~ntvrvarict4LI hybridizution. 17.v. AN Arm. SSR. Biol.
m%uki 18 no.1:47-53 Ja 165. WIRA 1815)
1. Arnkywiskaya ovoshchiictyu opytno-selektsionrviya sUintsiya.
I

AMUN, A. K.
Application of the bcundary layer theory to the determination of the
lose of pressure in cgen-source transition sections. Izv.AN Arm.
SSR.Ser.YKNT 1 no-7:551-572 148. (MM 9t8)
1. GidroalektricheelaWe, laboratoriya vodno-energatichookogo instituta
Akademii nail Armysnokoy SSR.
(Boundary layer) (Fluid dynamics)

AKLNW, A. K.
Transverse circulation during the deflection of turbulent flow in
circular &nd rectangular conduits. Izv.AN Arm.M.Ser.]MT nauk 6
no.1:43-54 Ja-F '53. (KLU 9:8)
1. Voduo-energetichaskiy inatitut AN Arngnmekoy SM.
(Aydraulice)

AN A

S S 1M. Jan A. K squaltil" of bubsbal now a tho
MIS
~
U
I~OUA cl, a enter d
ZZ), Dww~. ~. ash
(
(N.S.) 93. 4, W- GM, Dec. IM.
AutlAox i0ta-kv tbo peublem by means of sucetfAvo approxi-
wationp for (1) tbe truavetse t4vulatory flow, and (2) change in
MaUt vtloolly (*tdI*A"doc to the trwisverse flow. Botliare
for steady vjqjo, ke~, fin OwAtIons (at from thet beginning of the
kand.
For tkis pur~om, be "tes 4~o vquatkm of motion in tUo
JAM"Iromeko-Mirw1k (OM Ito cylindrical oDordInateN with
variable tuiLuleut vWoolty cosiffielont. Then, In first aplinjod-
rantion, divegaditig higher Invetw posvers of &-nd radius and
*
'
cbanps or the main velocitlen and of turbulent viscosity co~
clent, M deduces the AgerentlAl equatlon (4th-order) for%~
trionryierse flow fpnellpR. Ile givps*ebounda:ycondWo4%44h
*

b~d by ihn
" ~p4 my !~o problem ruy to~ M
rpgarj to s"A joctlop v
GaleAln itiriallonal inothod.
Then, atio disregartling higher Inverve po%vrs of bend radius
and changes In turbulent v1pooeity-coafficient diptribution, he
deducca Ow differentin). equation (2nd-order) for the inAln veloc-
Ity changep, to be --olved by ltemtion.
Author vlalrax hnvirrg obtained PoNtiona for eircukr and rec-
tangulor erpm w,-cliolot iind aliptoximste Poluflonsi for trnpP.10lddl
ant! tFumpslar r"" fx-rfions, and having checked them by ex-
perimental krivitsurements, with rnrod agreernenL &)nw. n-fe-r-
PrICOS R" given to books wid lialot". In lluambin, toy xamn tuabor
and t3theri.

ReVioWer (A)Bcms fnilx~rtanfv of the tramcitetwi fljw problern
fi]rhydrgul engineering. He c6-AM gilt hor'e dedu" inim and
qiPtencim In formulAs are L)I)o-
~ound them correct. wame incon.
Ire4ihical mlstnkcs fiot Ocuting the rwultq. A logleal extendon
of Lho subject would be: equations for furthcr approximatiotit,
for BtMV state. and gorne atudy of the nowteady fLlkte (at
entrance and exit of bend), N. Krlvwheip, Arl~ntina

LWANt G*A#
Remrks on A,K-Ai&"4u Is artiole uVater flow capacity of double
level epillwkys.;w Isv. AN Arm* SSR Ser. ]MT nmik 7 no.2:85-89
Mr-Ap 1549 (KWA 8:3)
le Armyanmkiy usuohno-Issledoyattliskiy i-astitut g1drotakhnW
i maliorateii,
(Spillways)

ANANYAN.A.K.
Answer to G.A.Ambartsumants article "Remarks on A.K.Ananian's
article on "Gapacity of double-level water overflow spillways'
Izv. AN Arm SSR. Ser PHET nauk 8 no-3:121-124 My-je '55.
OWA 8: 11)
1. Vodno-eneirgeticheakiy institut Akademii nauk Armyanskoy SSR
(Spillways) (Ambartsuman4G.A,)

"ARYAN, A.Lr!,-
Distribution of turbidity In flow with transverse circulation* Dokle
AN SSSR 109 no,2:275-278 J1 156* (XLRA 9:10)
1. Vodno-eneripticheekly institut Akademii nauk ArVanskoy SSR. Pred-
itavleno akademikom A.I. Nekrasovym.
(Hydrodyumics)

PRASE I BOOK EXPLOITATION 655
Ananyan, Antik KALrpovich
Dvizheniye zhidkosti na povorote vodovoda (Fluid Flow at the Bend of a Pipe)
Yerevan, Izd-yo AN Armynnskoy SSR, 1957. 361 p. 1,000 coplee printed.
Sponsoring agency: Akademiya nauk ArT*,anskoy SSR. Vodno-energeticheakiy institut.
Resp, Ed.: Hkhitaryan, A. M.; Tach. Ed-% Kaplanyan, M. A.
PURPOSE: Me book is intended for workers, technicians and engineers concerned
with hydromechanics and hydraulics, and also for students of these subjects in
institutes and universities.
COVERAGE: The author gives the hydrodynamic solution to the problem of deteradn-
ing longitudinal-tranaw~rse and vtlocity fields around the bead of a pipe of
any shape.. for pressure and nonpressure systems. He also compares the results
of theoretical studies with data from experiments by a number of researchers,
including himself. In particular he describes basic methods for investigating
the motion of liquids around the bend of a pipe. He states that the problem
of transverse circulation, which is a part of this motion, may be solved
Card 119

Fluid Flow at the Bead of a Pipe 655
by averaged equations of the turbulent-flow motion around the bend, and by the
boundary conditions of integration. He gives basic methods of analysis of the
equations obtained and shows the possibility of solution of this problem by
the variation methods of mathematical physics. He gives final computation
formulas which determine transverse circulation in pipes of various cross sec-
tions (circular, rectangular and triangular), for various diagrams of longLtud-
inal-velocity distribution above the bend. The solution of the problem of
longitudinal-velocity distribution within the bend is also given. The author
presents an approximate theory of development of transverse circulation within
the bend, and of its damping below the bend. Ib compares the results of an
analysis based on this theory with experimental data obtained by workers of
the VEnI (VoIno-energeticheskiy inatitut-Water-energy Institute) and by other
researchers. In conclusionhe gives the solution of some pmctical problems
obtained on the basis of application of the transverse circulation theory
elaborated by the VEnI, including distribution of turbidity in a flow with
transverse circulation, transverse-circulation in a divided flow (applicable
to damless srater intakes), and analysis of pressure losses around the bend of
a pipe. Me author thanks M. 1. Ter-Astnatsaturyan, A. S. Melkonyan, I. G.
Khristostva-.mn, 14. N. Mailyan and A. N. Tar-Oganesyan, Chief Engineer, An*rans-
koye otdeleniye Gidroenergoproyekta (Armenian Branch of the All-Union Trwit
for the Design and Planning of Hydroelectric Pover Plants and Hydroelectric
Card 2/9

Fluid Flow at the Band of a Pipe 655
Developments) for their help in preparing the book. There are 90 references.,
of which 80 are Soviet (including 4 translations), 7 English, 2 German and
1 ftwash.
TAKE OF CONTEM:
Preface 5
Ch. I. Basic Equations for Investigation of Tarbulent-Flow Motion Around the
Bend of a Pipe
1. Equations of motion of a continuous medium expressed by tension 9
2. Rypotbesis on supplementary turbulent tension 12
3. Basic asWcts of the statistical theory of turbulence 19
4. Coefficient of turbulent viscosity (physical analysis) 24
5- Equation of motion of averaged turbulent flow expressed in
cylindrical coordinates 27
6. Origin of transverse circulation at the bead of a flow 31
7- Formulation of problem of turbulent-flow motion around the bend
of a pipe 33
8. Derivation of equation of turbulent-flow motion around the bend
of a pipe 35
9. longitudinal-velocity distribution 44
Card 3/9

Fluid Flov at the Bend of a Pipe 655
10. Computation formulas for the coefficient of viscous turbulence 48
11. Boundar;r layer in a turbulent flow 54
12. Boundarr conditions of integration of equation of fluid motion
around the bend of a pipe 6o
13. Longitulinal-velocity distribution at the bend of a pipe 66
14. Investigation of transverse circulation at the bend of a pipe
in the second approximation 71
15- Boundary conditions for the solution of the problem in the second
approximation 75
Ch. II. Solution of Problem of Motion of Uquid Around the Bend of a Pipe
16. Basic methods of solution of equation of motion of turbulent flow at
the bend of a pipe 83
17- Equation of motion at the bend of a pipe expressed in polar
coordimates 96
18. General solution of transverse circulation problem for a pipe 99
19. Computing method of solution of transverse circulation problem
at the bend of a pipe 101
20. Solutica of transverse-circulation problem for a pipe with vari-
able coefficient of turbulent viscosity and logarithmic diagram
of longitudinal-velocity distribution 104
Caxd 4/9

Fluid Flow at the Bend of a Pipe
655
21. Solution of transverse-circulation problem for a pipe vith averaged
value of turbulent-viscosity coefficient 117
a. Solution of equation of motion around the bend of a Dipe by use
of logarithmic diagram of transverse-velocity distribution 3-19
b. Solution of transverse-circulation problem for a pipe by use of
elliptical diagram of longitudinal-velocity distribution 124
c. Solution of the transverse-circulation problem for a pipe by use
of parabolic diagram of longitudinal velocity distribution
(according to Bazin) 12T
22. Influence of various accepted laws for coefficient of viscous
turbulence on results of solution of transverse circulation problem 130
23. Influence of various laws of longitudinal-velocity distribution on
results of solution of transverse-circulation problem 138
24. Investigation of transverse-velocity fields for smooth and rough
surfaces 142
25- Origin of formation of double transverse circulation in a pressure
pipe (pbysical analysis) 143
Conclusions 144
Card 5/9

Fluid Flow at the Bend of a Pipe
655
26. Solution of the transverse-circulation problem for a pipe of rect-
angular cross-section with variable coefficient of turbulent
viscositr 145
27. Solution of transverse-circulation problem for a pipe of rect-
angular cross section with a constant-value coefficient of
turbulent viscosity 161
a. Solution of transverse-circulation problem by use of parabolic
diaLV= of longitudinal-velocity distribution (according
to :%zin) -
b. Solution of transverse circulation problem by use of elliptic
diagram of longitudinal-velocity distribution 170
c. Solution of the transverse-circulation problem by use of
loEpirithmic diagram of longitudinal-velocity distribution 175
28. Comparison of results of solution of problem, obtained for a pipe
of rectmigular cross section 185
29. Solution of transverse-circulation problem for a pipe of triangular
cross section 190
card 619

Fluid Flow at the: Bend of a Pipe -
655
30- Iongitudinal velocity distribution in the bend of a pipe
a. Pbyuical analysis of pattern of longitudinal-velocity
distribution around the bend of a pipe
b. Theoretical study of changs of-longitudinal-velocity field
along the length of the pipe
c. longitudinal-velocity distribution around the bend of a pipe
of circular cross section
Ch. III. Transverse Development of Circulation at the Bend of a Pipe and
Its Damping Belov the Bend
Introduction
31. Damping of transverse circulation in a viscous liquid in
rectilinear section of a wide pipe
32. Increase of transverse-circulation along length of bend of a pipe
Ch. IV. Experitrental Study of Fluid Motion Around the Bend of a Pipe
33. Basic problems of investigation
34. The author's installation and method of investigation
35- Ijongitudinal-velocity distribution according to the author's
experiments
Card 7/9
203
-
207
209
221
223
234
242
243
249

Fluid Flow at the Bend of a Pipe 655
36. Transverse-velocity distribution at the bend of a pipe 255
37. Experimental investigation of damping of transverse circulation
along the length of a straight pipe 269
Ch. V. Application of the 7heory Developed to the Solution of Some Practical
Problems
3htroduction
38. Basic equations of motion of a heterogenoua liquid -
39. Turbidity distribution in a flow with transverse circulation 289
40. Boundary conditions (turbidity near bottom) of integration of
differential equation of a haterogenous flow motion 296
41. Methods of solution of equations of motion of a heterogenous flow in
axially symmetric problems 3o2
42. General diagram of divided flow 305
Cale 8/9

Fluid Flow at t1a Bend of a Pipe 655
43. InvestioLtion, of steamlines,in divided flow (first
OpProxiiation) 305
44. MnvstipxLticn of boundar7 streamlin in a divided flow (second
apwoximtion) 327
45- Analysis of transverse circulation in a drainpipe when flow is
divided 332
46. Pressure losses in turbulent-flow motion at the bend of a pipe 335
47. Buie equations for investigation of pressure losses around
the bend of a pipe 339
48. Analysis of losses around the bend of a pipe of circular cross
section 341
Bibliography 352
AVAnA=: Idbrary of Congress (2C1T4.A6T)
Card 9/9 TS/fal
lo-14-58

ANANTAN, A.K.
Approximate solution of the problem of lateral circulation caused
by curved flow in water conduits of triangular cross section.
Izv.AN Arm.SSR.Ser.te)ch.nauk 10 no.3:3-20 157. (MIRA 10:10)
1. Vodno-onergetichaskiy institut AN A anskoy SSR.
(HydrodynAmic'a

ANANTAN, A.K.
Problem of Lake Sevan has to be solved in a nev vay. Izv. AN Arm.
SSR. Ser. tekh. nauk 10 no.5:9-14 '57. (MIR& 11:1)
1. Voduo-onergaticheakiy institut AN ArmSSR.
(Sevan, Iake-Hydmulle engineering)

10(4) BOT/95-59-7-21/22
AUTHORs Rosinoor, S.T., Chairman
TZT1Ns Conference on Scientific Research in the Yield of
Aydromobanlow
PRRICE11CAL: GIdrotakhoLobaskoye stroltel'stva, 1959, Nr 7, pp
62-65 (USSR) T.T. Dlovaiz
Can-
,
d1dat. of Technical :~clomaom EVIL d fmg-tioer
'
he FYdrau-
X.Z_J0=ujEjalw forro-Concreto (VIIII), "-
"lle Fractionation of latural Send In the preparation
of Concrete.* At the "salon an equipment the fol-
loving papers were r*&ds ZugLnsor S.M. MiLundla
Cazd 4/6 (Oidroproyert)i -'&=h ZotenMrs%
Zaglowerp jA._JLaroa_ (21sm-tag and Design Office of
-- --,the Rydromechanlam3lon Trust of the Ministry of the
1 Nov Designs of Bucket-Rotor Typos of Slain-
=
1
on StUIPEOWt Z.D._SQZiAR=JU6 Candidate Of
Technical Sciences (ZG11 of the Leademy of Sciences
of the USSR), Engineer It. I-XazLknr-(The Lead-Ml
nIng2rust), and Candidate of TocKli-
tbo 14&dlng of Heavy-YEAterLals Into pressurized Wa-
ter Com4ults*; The "salon on transport contained
papers "ad by the following: X.T laz or.
amber of the Acade:7 of
BaRs -The Movement Of Alluvia, and Related 2robleasA
Prof voctor of Technical Saltness
(VZM* and R-11.
_A&;EgXLm. Candidate or an . (the Lasti-
tute of snorgetlas of the Academy Of Sciences Of
the LrjwnLan 3SR)i 'The Kinmatlom of Turbulent
Stromm.; Prof. r. 1. rr-k-l-, Doctor of Technical
Sciences (K "az lzq_~ tat* University)s *A
Card 5/6 Xethod for Battling tim novesmut of Alluris'; N.A.
k2likanoz- corresponding amsber of the Load&V of
Sciences of the USSR: 'The Th*orstloal and Fr"ti-
Cal Value of the Grayltational Thoar7 of Alluvia*;
jzA.-ILUA. Candidate of Technical 3olonamas 'Laos
of Pressur* and Hydraulic Resistance in I-Arg*-DIa.
motor Tubes% Canddate of Techni-
cal Sciences (VN11TS). 2.1. irelov (70DGSO), and
L,~~wr (1GD of AcadiiY of Sciences of the
GSSR)t *ExperfWants In Water Supply in Condult Tu-
bes of Various Diameters': T~3~jng=jq VandIdato
or Technical SOI*Dcost *Resistance in Hough open
Riverbado.1
ASSOCIATIONs (Comforono* Organixing Committee) Ortkcaltet po
pror*denlyu

ANANYAN,-A. I.
Some problems dealing vith the theory of the stream bed process.
Izv.AJI Arm.SSR. Ser.tekh.nauk 13 no.2:3-12 660.
(XIR& 13:8)
1. Institut energetikl I gIdravlikI AN ArnMskoy SSR.
(Rivers)

ANANIYAN, A.K. _doktor t ekhn. nauk, prof.; BEK41AIDIARCIEV,, B.I.,
nauk; ZIUMGORTSYAD, V.11., kand. tokhn. nauk;
CHITCWAIJ, A.I., kand. sellkhoz. nauk; YEDIGARYAN, Z.P.,
mlad. i2auchrory sotr.; SATIAN, M.A., kand. geol.-Mineral.
nauk; PAYRAZYAN, V.V., mladshiy nauchrory sotr.; VEBER, V.V.,
prof.; NAZARYAN, A.G., kand. tekhn. nauk; POKHSRAIffAN, M.S.,
mladsh-:Ly nauchrqy sotr.; TER-ASTVATSATRYPII$ M.I., mladshiy
nauclu-j.yy sotr.; VELIKOOV, M.A.j VEUKANOV, M.A.., otv. red.;
SHTIBEII, R.A., red. izd-va; KAPLANYAN, M.A., teklin. red.
[Results of complex research on the Sevan problem) Rezulltaty
kompleksnylEb issledovanii po Sevanskoi probleme. Erevan,
Izd-vo Ali Armianskod. SSR. V01.2. [Channel processes] Ruslovye
protsetisy. 1962. 255 p. (MIRA 15:7)
1. Akademiya nauk Armyanskoy SSR, Yerivan. Institut vodnykh
problem. 2. Chlen-korrespondent Akaderii nauk SSSR (for
Velikanov).
(Sevan Lake region-Hydrology)

ANANYAN A.K doktor tekhn.nauk, prof.
.;I- -- .4-- #
Using models to study channel processes during continuous lower-
ing of the index of the river's level of erosion. Gidr. stroi.
33 no.11:37-39 N 162. (MRA 16:1)
(Erosion) (Hydraulic models)
il
:1

IGMHYAN, S.S.* akademikl.ANANW,_~.K-,_doktor tekhn.nauk., prof.
I*V.Egiazarov; on hio aeventieth birthday* Elektrichestvo no.3:94
Mr 163. (MIRA 164)
It Akademik-sekretarl Akademii nauk Armyanskoy SSR (for Nkrtchyan)o
(Egiazarov,, Ivan Vasillevich,, 1893-)

ANANYAN, A.K.; BEK-MARMARGHEV, B.I.; 22AMAGORTSYAN, V.N.; MKIIITARYAN, A.M.
Using Soyiet-produced surface-active agents for reducing the
evaporation from water surface ih reservoirs. Izv.AN Arm.SSR.
Ser.tekh.nauk 16 no.2/3:U7-128 163. OCRA 16:9)
(Surface-active agents) (Evaporation)
-~!- ~- 1, 77777F_o ~, -
~, t - -

ANARY1,111 A.K.
Yetbods for designing the structures of the Sevan-Razdansk
series of hydroelectric power stations with dacressed flow
during the Onter. Izv. AN Arm. SSR. Ser. takh. nauk 18
no.30-15 '65. (MIRA 180)

--AANUN.-4.J"4 13GOTAU. V.L.
Geothermal studies in Armenia. Izv.AH Arx.SSR Ser geol.1 geog.
nauk v. 11 no.4:23-36 158. RIRA 12:1)
1. Inatitut geologichookikh nauk AN ArmSSR.
(Armenia-Springo)

ANANTAH. A.L.; UPWiTAJI, P.M.
Metumorphism of mineral waters and the possibility of mineraliza-
tion within the Dzhermuk region. Izv.AN Arm.SSR Ser geol.11fogo
nauk Y. 11 no.4:83-88 '38. (MiRk 12:
1. Institut eeologicheakikh nauk AN ArmSSR.
(Dzhermuk region--Mineral waters)
21~

KHACHATURTAN, S.A., glevnyy red.; ANANYAN, A.L., red.; KAPLANYAN,
P.M., redo; PBTROSYAN, R.A., iEdst.
red.; AZIZBEKYAN, L.A., tekhn.red.
(Proceedings of the 7irst Conference of Young Scientists of the
Geological Institutes of the Academies of Science of Georgia.
Azerbaijan, and Armenia] Trudy Pervoi Zakavkasskoi konferentsil
molodylch nauchnykh sotrudnikov geologichaskikh inatitutov Akademii
nauk Gruzinakoi, Azarbaidzhanskoi i Armianskoi SSR. Erevan,
Izd-vo Akad.nauk Armianskoi SSR, 1959. 202 p. (MIRA 13:8)
1. Zalawkazeknya konferentsiya molodykh nouchnykh sotrudnikov
goologicheakikh inBtitutov akedemiy nauk Gruzinskoy, Azerbay-
dzhanskoy i Armyonskoy SSR, let. 2. AN ArmSSR (for Koplanyan),
(Geol ogy--Congre sees)

ANAKfAll. A.L.
Rartb temperature neasuromonto at Dzbermuk, Dokl.AN Arm.SSR 28
no.1:27-29 '159. OGRA 12:7)
1. Institut geologichookik-b nauk AN AraSSR. Prodatavlono
alcadsmikom AN ArmSSR I.G.Magaklynnom.
(Dzbermuk --Barth temperature)

ARANYAN, A.L.
Some travertine formations in the upper Arpa and Vorotan Valleys.
Izv. AN Arm. SSR. Geol. i geog, nauki 13 no-3/4:89-99 160.
(MIRA 13:9)
(Transcaucasia-Water, Underground)
j

rol.-AaC. to t, a
c-f hot r,
Sov- 3 no. 5
Cai-l', 1.1+:2)
r ans
any koy I..

BABAYAN? M..;~1AKMAZYANp K.TS.; ANANYAN, E.S.
Aqueous alkali cleavage or 1,5-dia=onium salts containing a mul-
tiple bond in the 2.3-position of the common group. Dokl. AN Arm.
SSR 38 no.3s157-162 164. (MIRA 17t6)

RhEAYANV A,T,; TAKSMAN, K,TS.; ANANIAN, B.S.
Axines and numon4un compounds. Part 28t Alkaline decomposition
of 1,5-di-(trialkyl am7sonium)-2-pentenes. liv. AN Arm; SSR.
Xhis. nauki 18 no.3s262-268 *65. (MIRA 18211)
1, Inetitut organicheakoy khimii AN ArmSSR. Submitted July 21,
1864.

ANANTAN, Grach4A Tigranovich
(Soda Solonchaks of the Arazdayan Semidesert and the pos-
sibilities of their leaching] LSodovye solonchaki Arazda-
ianskoi polupustyni i vozmozhnosti ikh proqrvki. Erevan,
Armianskoe gos.seltkhoz.izd-vol 1962. 61 p. [In Armenian]
(MIRA 1714)

Rl RiKOSYAN, A.Vo "t!
f:: T, f
M-T RA C.)
, i~,

Y " 17 1~ 1 T . - , , - , ,
?.,I' j KO N Y AN, ;,.h. z,
11 , - . 4 . , - , 0, . ;
I f fil,,t cil pli medi-am cn the develop-.ent tif ec~-IcF' fz~-na ~f
Azotobactor chroococcum. Vol). mikrobio:.
kr"F-tv 18:3)

-ANANY.- N -)--S.- A.
Anar;ya ,S. A. "Contemporpry problem of the immunology and laborr-tory
diagnosis of mosquito fever". Voprosy med. virusologii, Issue 2, 1949, P. 301-
14., - Biblio, 1 21 items.
SO: U-30423 11 March 53, (Letopia Ishurnal 'nykh Statey, No. io, 1949).

nn 5q
~Ledicize' - Virus Diseases
n
The Problem of Active Immunization Against Pa-
patacci Fever. 1. Adaptation of the Virus of Pa-
patacci Fever to-Laboratory Animals," S. A.
Ananyan, Inst of Virology imeni D. I. Ivanovskiy
"Mur Mikrobiol, Epidemiol, i Imminobiol" go 1,
VP 32 -40
The virus of papatacci,fever can be successfully
cultivated in white mici. Guinea pigs are sus-
ceptible,to the disease. A symptom-free infec-
tion is produced-in white rats and rabbits. The
disease in these apinals is specific: the
241T12
modified strains from these animals produce com-
plement fixation with serum from recovered human
patients and specific antisers.-from infected animalit.
The virus that has been modified by passage throu&
exptl animals creates immunity in animals vbich have
bad.the disease. Vaccines prepdfrom some lab strains
of the virus proved to be non-pat4ogenic and at the
same time immmogenic in humans. ' The strains of ,
virus obtained can be cultivated on chicken embryos.,
are filterable through "Rublev" filters Noaa I and 2,,
are resistant to temps down to minus 700 and to
drying at low temps. They do not stand heat: heat-
Ing at 560 weakens them considerably within 10 min
and kills them in 30 min.
241T12..
>4

USSR Jan ~ 93
Ft/iLedicine - VirL= Diseases
"The Problem of Active T-nization Against Paps-
tacci Fever. 11. Specific Prophylaxis By Neans of
Live Vaccine," S. A. Ananyan, lust of Virology
imeni D. 1. Ivanovskiy
"Zhur Mikrobiol, Epidemiol, i Immunobiol" No 1,
pp 40-48
Tests carried out in 1951 in various parts of the
USSR showed that dry live vaccine lowers the inci-
dence of papatacci fever 2.5-3-5. If the disease is
contracted notwithstanding the inoculation, the
period during which the patient has a raised temp
241T13
is shortened considerably, or any increase of temp,
eliminated entirely. During 1951, observations
vare made on 69,000 persons inoculated with live
vaccine.
241T13

ANANYAJI, Serik Arshakcivna
Academic degree of Doctor of Medical Sdiences, based on her defense,
24 December 1954, in the Council of the Department of Hygiene,
Microbiology, and Epidemiology, Acad Med Sci USSR, of her
dissertation entitled: "Mosquito Fever (Disease of the 'Papatachal
(Etiology, Epidemiology, Clinic, Prophylaxis)."
Academic degree and/or title: Doctor of Sciences
SO: Decisions of VAK., List no. 16, 2 Jul"55, Byulleten' I-IVO SSSR, No. 15,
Aug 56, Moscow, pp 5-24, Uncl. JPRS;~Y-537