SCIENTIFIC ABSTRACT SMIRNOVA, A.I. - SMIRNOVA, A.S.

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001651620008-2
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• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 24, 2000
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Chemical Abst.
V01- 48 No. 9
hay 10, 1954
itnalytical Chemistry
G. Bespalov andiX. 1. Smirnova. Afed. Pram. S.S.S.R.
1949, No. 0, 2G-8._-_A-7ffEUrdd-T& tlctg. fructose In the
presence of glucose, mannose, or galactose Is described,
Fructose, ia contrast to other monosaccharides, gives -a
greenish color with Na nitroprusside tinder certain condi-
tions. To 3 cu. nim. of sample of VH 3.4 add I m). of
freshly prepd. I % Na vitroprusside soln. and 10 drops of N.
alkali hydroxide. After 15 min. add 5 drops of coacd.
AcOH. After an addal, 20 min. the characteristic green.'
ish color develops fully. Two series of fructose-glucose
soins. were prepd. One series was acidified with AcOH and'
the other with HCI, with I drop of concd. HCI equal in.
H ion conca. to 77 drops of AcOH. The colors were meas-
ur-d 15 min. after ~he acidification. The resulting conen.-
absorption curves were almost parallel lines (in the range
2-10% fractose) with the HC1 series giving higher absorp-
tionsoflight: The It, tensity of the color varies so much that
a simple conivarator can be used. Eurilla Wayerle

BOGOMOIDV, A.1.5 SMIMICIVA, A.I.
Cataly',ic properties of natural clays containin
(.g h,,,rgrosc-p, c
-TC !:, R A
moistua-e. Trudy TN M no.174:54--60 161. 14:!2)
(Clay)
(Catalysis)

KIRYANOVA, Z.V.; a"ITRIYEV, M.V., doktor ekonom. nauk, prof., red.;
SASS-TISOVSKIY, B.A., doktor takhr.. nauk, prof., red.;
SMIRNOVA, A.I., ved. red.; YAZLOVSKAYA, E., tekhn. red.
[Ptoduction factors and means of lowering the cost of caustic
soda] Faktory formirovaniia i puti snizheniia sebestoimosti
kausticheskoi sody. Moskva, Vses. in-t nauchn. i tekhn.
informatsii, 1959. 96 p. (MIRA 15:6)
(Sodim hydroxide)

SMIMIOVA, A.I.
Mitorials on hydrochemical characteristics of the
Karadag area. Trudy Kpxad. biol. sta. no.160-15
(BLACK SEA-WATER-COMPOSITION)
Black Sea in the
160. OURA 13:9)

Ye-T. Li-IL"i-f:
A.S.(Trehubov-, EE - c. ,
11REG U B 0 V A j -
O.A.'Kysylenko) T
L L -
1.11 Kr.7.AY LOVA, O.i).[:.y-',haJlova, 6.15.1; D'i-HAS'~E'lliKC, A.l.;
,T
Oz, I.I.F.; K. Yu.!.L;~ k: A-I-Z-1-:BZRG,
- 11 llu R 1.
MPRKOV, V.I., red.
L A~r c c 11 s. e i. i c-.anual or, Trovince A--roklimatychnyi
De--zhsillh spvy-
-0
ciav b9' (V17iA 17:6)
1. ukl-aainc~. ";'i rvollinnya gluzhiZr.

49-5-5-3-5/19
A.Ta. ~-nd S--irnova, A.!.
TITLE: Clouds in the Stratosphere (Oblaka v stratosfere)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
11:5 i~r 37 pi) 337--31[G (USSR)
ABSTRACT: According, to KbLrr--ian (Ref.1), nacreous clouds at altitudes
0
Card 1/3
between 20 and 30 km are observed exclusively during the
wintez and predominantly in Scandinavia, Finland, Britain
and Alaska. Therefore the authors considered it of interest
to investi-ate a case in which nacreous clouds were observed
in the stratosDhere at a different time of the year and a
different latitude. At an altitude of 22.4 Im the authors
.-ho'-UoZ;-ra1)hed a cloud which was illuminated by the beam of a
projeotor (Fi,-.1) at 4.00 hrs of September 1', 1953 in the
Caucasus (410 44' latitude at an altitude of 1800 m above
sea level durin-- a windfree, dry but cool nig
C.: ht -when the sky
was perfectly clear. During the same day at 18.00 hours the
cloud was photographed again. Tile projector had a mirror of
150 cm diameter and a rating of 11.5 kW. The projected
beam was directed at 750 to the horizon and the exposures
viere taken at points spaced 9.6 -m a-Dart, usin- 3 identical
camr--ras7fitted with 1:1.1 objective lenses as well as with
'Hoollaston -prisms and filters. The data of the prisms and

149-58-3-5/19
Clouds in the Stratosphe--re.
of the filter are given. The results obtained by photo-
,-raDhi-ng by means of polarised light', are compared with
D CD 0
aerological data and weather chart data. Polarisation data
permit expressing certain assumptions on the nature and
ainiension of the particles composing the cloud which was
photog a-o ed. The case of a laminated turopopause is con-
,r _h
Sidered2 the fo--r-i!),ation of which was followed by means of
probing with a -projector. Th;i results of probing of the
U
stratospht--re by the projector beam are in good qualitative
agreement with visual observations made in England (Refs.G
and 8), and also with observations of a complex tropo-pause
under anti-cyclone conditions (Refs.9 and 10). The data
obtained by 'he authors of this paper on the stratosphere
cloud (altitude, vertical thickness, transparence, average
particle dimensions, refraction index of the particles)
lead to the assumption that t'h- cloud pho-tographed by the
authors in the Caucasus and the nacreous cloud are of
exactly the same nature in spite of the fact that the latter
has not been observed in the Caucasus re-ion. There are 12
Card 2/3

49-58-3-5/19
Clouds in the 3tratosphere.
fi-ures and 10 references, 6 Englishl 2 Russian and 2
0
German.
ASSOCIATION: Institute of Physics of the Atmosphere, Academy of
Sciences, USSR Olkademiya nau:~: SSSR, Institut fiziki atmos-
fery)
SUBMITTED: January 31, 1957.
AVAILABLE: Library of Congress.
Card 3/3

49-58-5-5/15
7
AUTHORS.- A. Ya, . V,11, Zolotavina.. Polozcva '-_N. and
TITLZT~ Determination of the A-11i,,iosDheric- Stratification and Products
of C.Dnderasation by BearchliGht Mebh-~od (Stratifikatusiya
atm-osfery i obrazovaniye produktov kondensatsli po danz4
7m
prazhek't-rornc1crc zondirovaniya)
.D
PERIODICAL: I2:17estiya. Akademii Yiau'K SSSR. Seriya Geofizicheskaya.
1-9158, Nr 5 pp 617-624 (USSR)
ABSTRACT-. Th.e 1:tin layeve of semi,-transDarent clo-ads are often seen
to b6 fofmed at about 18 000 m high, The cbservation,7 es-~;ab-
lished the fact thhaL these clouds are produced when the tropo-
p,al;se is steadily lifted with a simultaneous cooiing
1 4
a~. Uhe c-lould layer. It was observ--d in Great Britain that
this D112romenon is a,:companied by a lowering of the upper
layers over the antii~~yclones, The dynamic press-oxe appears
to be the main factor in the production of water condensation,
Its intensity can be affected by speed of rising air and an
inflow of moisti-Lve from the surrounding areas, As the water
condensation in tiie atmosphere greatly affects light scatter
I)roperties ol" the air it is evident that the problem of
Card 1/5

L~9-58-5-5/15
Determination of the Atmospheric 'Stratification and Products of
Candensation by Searchlight IMethod.
optical methods of observation becomes important. Of the
methods of application, the searchlight proved to be one of
the most precise, This work gives an account of an optical
sonding through the atmosphere carried out for four consecu-
tive nights in lJoscovi region in conjunction with the aero-
logical data and synoptic charts, The resulting observat-
ions are presented in the form of graphs showing various
aspects of light scatter, temperature distribution and polar-
isation, Fi-J gives the intensity of light scatter of the
beam as measured at various heights through a blue filter.
Fig.2 represents the thermoisoplets for the period of exper-
imenting. Fig.3 shows a degree of polarisation of the light
scatter for various heights, It is interesting to see how
0
the height of "he light spot was rising during the first
three nights. It rose from 2-3 km to the region of the
tropopause by the second night and showed a height of 22-
25 km during the third night. The measurements at 22-25 km
were carried out also with a photographic camera. It should
be noted that while the scatter intensity was changing at
higher levels., it remained constant at about 8 im. The
oserved data agrees with the theoretical calculations of
Card 2A ci

49-58-5-5/15
Deterlfqinat-ion of the Atmos-oheric Su"'-abificration and Products of
Condensation by Searchlic;-ht I`Aethod~
I-)
the an,,-l(,, of scatter.as it is shown on Fig.4,. where the
theoretical curve is being plo-tted to-ether with the
0
observed ones, The graph of temperature isoplets indicates
a definite lowering ofL' temperature at the observed heights.
0
The surface synoptic charts are shown on Fis-5. It sliould
0
also be noted that the degroe of polarisation in the lower
C~ -0
atmosphere lies always in the range of light scatter 135-159
as sho--~~-n o-q Fig.6; t1ais was pre-Dared from the data obtained
on many occasions for different localities, The degree of
accuracy of the measurements is someuhat lower for heights
above 15 km, due to the star light interfering with the
searchlight, The tests with a green filter showed that it
Laakes measurrin- more dIfficult owin- to the absorDtion of
some of the light intensity. Fig.? shows an example of the
results obtained through it. Entirely different results were
CD . u
obtained on another occasion off sonding the atmosphere. Fig.8
shlows the re3Ul'V-S Of searchlight measurements made every 3.5
C~
hours for two consecutive nights, The degree of polarisation
is sHovin, on Fi-=,9, The curves are rather smac'uh, giving
Card 3/5

49-58-5-5/15
Determination of the Atlmosz;heric Stratification and Products of
Condensation by Searchlight Method~
evidence of no layers of an increased scatter, This proved
Uhat the upper atmosphere up to 15 km was homogeneous, Fi.-.10
represents the temperature distribution for that period, The
syno-pti-. charts are shown on Fig.12, The following can be
derivea from the experiments: 1. Mhere the synoptic situation
represents a high with the pressure 1030 mb at its centre and
a sufficiently developed low to the North, while the upper
atmosphere is of a uniform condition., the searchlight method
will show a slight decrease of light scatter intensity owing
Uo very sinall dimensions of free particles in the air
(aerosol 0,10, 2. In the case of a vertical decrease of
temperature the light scatter e:%poses the particles of an
increased size due to water condensation. 3. The products of
condensaticn in such a case at heights of 14-23 km axe in
the shape of water droplets of 1.5~t diameter. This method
also makes possible an exact determination of the -relation-
ship of condensation products -in the stratosphere to the
vertical movement of the air at certain synoptic situations,
thus contributing to observations of the least known sDhere
Card 4/5

49-58-5-5/15
Determination of 'he AtmosDheric Stratification and 1~roducts of
i
Condensation by Searchlight- Method.
of the upper air. There
2 of whicl a-re Soviet,) 2
ASSOCIATION-. Akademiya nauk
(Academi of Sciences.,
AtmosDh-,2re).
SUBMITTED! TanUar-
31 i9c
SSSR,
USSR,
are 13 figures and 12 references,
German ando 8 English,
Inst-itut Fiziki atmcsfery
Institute of Physics of t1le
2. Searchlights-ApplicaLiozis
Card 5/5

SIMONOY, Ts.P.; SALEPOYA, A.I.; SMIRNOVA, A.I.; MTSOYA, Te.M.; MIKHATLCYA,
A.D.; T91"1110YA, K.A.; MORN,' T'F ; GUK, Tu.I.; 141KOLAYEYA, Z.A.;
AYZENBXRG, M.M.; MIKHAYLOYA, K:L:; ROGOVSKAYA, Ye.G., red.;
VOIKOV, N.Y., tekhn.red.
[4,roclimatic reference book on Nikolayev Province] Agroklima-
tichaskii spravochnik po Nikolaevskoi oblasti. Leningrad, Gidro-
meteor.izd-vo, 1959. 103 P. (MIRA 13:2)
1. Kiyev. Gidrometeorologicheakaya observatoriya. 2. Nachaltnik
otdela agrometeorologii Kiyevskoy gidrometueorologicheskoy observa-
torii (for Salepova).
(Nikolayev Province-Crops and climate)

A.A.; ~-~j',LLFOVA, A.I.; 51-~IRMVA, A.I.; 5YRTSC-VA, Ye.N.;
GUK, Yu.l.; NIKOIAYEW, Z.A.;
~G , '~I'K~-AYILZV A , K. L. ; U 'ST,'AKOV A , T.V. , red .
Lf'-'-,r,7rGclimatolo-,ical ratinual for Strdino Province] Agrokli-
spravuelmik po Stalinskoi. oblasti. Lenin rad,
1~159. 101 P. li:eS
1. Ukraine. Upra-vleniye girdrometeorologicheskoy --lwhby.
- Nae"I.allnik Otdela agrumeteorolaCii Kiyovskay -idro-
2
observatorii (for salepoval

SIMOE1011 Ya.F.; SALEPOVA, A.I., SYRTSOVA, Ye.M.;
y $
ABOVICH, F.B.; AYZRIBERG, M.M.; MIKHAYLOVA, K.L.; USHAKOVA,
T.V., red.; SERGEYEV, A.N., tekhn. red.
[Handbook on agricultural CliLatology in Zaporozhlye Province]
Agroklimaticheskii spravochnik po Zaporozhskoi oblasti. Le-
ningrad, Gidrometeoizdat, 1959. 111 P. (MIRA 17:4)
1. Ukraine. Upravleniye gidron.eteorologicheskoy sluzhby.

SMIRIIOVA, A.I.
Waste removal device for a mobile-carriage circular saw. Sbor.vnedr.
rats.pred. v les. i meb.prom. no.2:56-57 159. (MIRA 13:8)
1. Mobelinaya fabrika tresta "Lengorles.N
(Circular saws)

I SMIT-UTOVA, A. I.
Utilization of glued plywood wastes. Sbor.vnedr.rats.pred. v les.
i meb.prom. no.2:121-122 159. (MIR& 13:8)
1. Mebel1naya fabr1ka tresta "Iengorles."
(rlywood industry)

SMIRITOVA, A. I.
Improved hand cart for hauling cabinet-type furniture-inside.the sUop.
Sbor.vnedr.rats.pred. v.les..i mebiprom. no."2:130-131 1119. (MIRA 13:8)
1. Mebellnaya fabrika tresta Olengorles.ff
(Furniture industry-Aluipment and supplies)
(Hand trucks)

USSR/4141edicine - ALetino mycosia Sep 48
Medicine - Penicillin
"Mild Cases of Actinomycosis Treated With a Com-
bi.-L- tion of Penicillin and Iodine," A. I.
Smirnora, First Burg Clinic, MONIKI, I p
"Sov Mad" No 9
Subject affliction is one of most difficult to
treat effectively. Reports results of penicillin-
iodine therapy which appears to be more effective
than methods now in use.
24/49T61

XONY111HINA, I.A.: ODREYETh, V.I.- IYSTRYAKOVA, L.V., KUS'IINOVA,G.A.:
S?IIR;','OVA, A. 1.
Clinical characteriz-,tics of dysentery in young children. Pediatriia
no.2:Mr-Ap '55. (MLRA 8:8)
1. Iz kafadry infetskonnykh holezney-tLdetey (zav.-prof. M.G. Duni-
levich) Loningradskogo pedintrichaskvgo meditainakogo instituta
(dir.-Prof. IT.'. Shutova) i Detakoy infektsionnoy bollnitay Lenin-
skogo rayona-(glavW vrach A.,H. Belyayeva)
(DYSENTMY, BACILI~M, in infant and child)

SHUMKIN, B.N., SMI"~..A .,~_,,,r.DAjjjLOV, A.I.
the Acader-Y of Medicine of the U.S.S.R. held in Astrakhan
Sess;on Of -
on th- ns. Vest.AW SSSR 13 nO'9:
e problem of intestinal o-f infectio
65-74 158 (INTIESTI-IMS-DISBASES) (mm 11:10)

SH04KIN, B.N., dots., SMMOVA, A.I.. DANILOVO A.I.
Astrakhan session of the Academy of Medicine of the U.S.S.R.
on the pro'hlem of intestinal infections. Vest*AMN SSS
a R 13
no-10:7L" 158 (MIRA 11:10)
(=ST =-DISEASES)

0 0 0 0 0 0 0 w- w ww
0 0 a 0 0 0 0 9 0 IS 0 0

Preparation of butadient from pstudabutylene (2-
butent). B. P. Fedorov, .1, 1. &Ilirtluva and P, A. :.so
: S