SCIENTIFIC ABSTRACT SMIRNOVA, N.P. - SMIRNOVA, O.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001651620020-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 24, 2000
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SCHASTNEV, P.N.; TEREKHOV, P.G.; red.; SAKHAROVA, N.V,
tekhn. red.
[General geography; textbook for t-eachers' schools] Obshchee
zemlevedenie; uchebnik dlia pedagogicheskikh uchilishch.
3. Izd., perer. Moskva, Uchpedgiz, 1954. 338 p. (MIRA 16:6)
(Physical geography)

SMIRNOVA, N.P.
The BuzuIuk-Kedveditsa watershed and the Yodyanaya Ravine. Trudy
lab. ozeroved. 9:150-156 1609 (MIRA 13:8)
(Bauluk Valley (Stalingrad Province)--Farm ponds)
(Medveditea Valley--Farm ponds)

SMIRNOVA, N.P.
Methods of field work in water and heat balance reseaxch and the
working up of data obtained. Trudy lab. ozeroved. 9:166-181 160.
(MIRA 13:8)
(Vyazovka District (Stalingrad Province)--Farm pondEi)
(Hydrometeorological research)

SMIRNOVA, N.F.
Heat balance of the Polivnoy Pond in the summer and fall of 1951-
1954. Trudy Lab. ozeroved. 9:203-237 160. (MIRA 13:8)
(VyazovkEL District (Stalingrad Province)-Farm ponds)
(Ifyd-rometeorology)

YEFREEOV, Yuriy Konstantinovich, geograf; 3-11210VA, N-P., red, izd-.,Vh~
14AZAROVA, A.S., tekhn. red. -- -
[In the name of nature's everlasting generosity] Vo imia vechnoi
shchedrosti prirody. Moskvap Izd-vo "Znanie," 1961. 31 p. (Vaesoiuz-
noe obshchestvo po rasprostranenliu politicheskikh i nauchnyl-r-h zna--
nii. Ser.12, Goologiia i eograftia, no.16) (MIRA I'W-11)
~Natural regouces)

SMIRNOVA, N.F.
Meteorological conditions during the field work of the expedi t4on
(1956-58). Trudy Lab. ozeroved. 12:25-34 '61. (WPA 15:3)
(Ladoaa Lake region--Meteorology)
0

S~URNOVA) N.P.
Radiational elements of the heat balance in the skerry region
of Lake Ladoga. Trudy Lab. ozeroved. 12:35-59 '61. 0AIFAL 15:3)
(Ladoga, Lake-Solar radiation)

SKERNOVAI 14.1%; ;M1-htWV. i,.Y~,.
Using aerial phoLo,7--ra.hy In studying vast deltas; based on the
example of the Ili lUver, Izv.Vses.,g-eog.ob-va, 93 no.5:4-18-4.22
S-0 t61. (1-MRA 14:10)
(Ili Valley-Aerial photography) (Deltlas)

S/020/61/136/003/014/027
B019 B056
AUTHORS: Izotova, A. F., Ogneva, T. A., and Smirnova, N. P.
TITLE: The Wind Profile in the Water-near Layer Above Lake Ladoga
PERIODICAL: Doklady Akademii nauk SSSR, 1961, Vol. 136, No. 3,
pp. 587-590
TEXT: From July 7 to August 16, 1959, the vertical wind velocity profile
above lake Ladoga, and its dependence upon the stratification temperature
was studied, and also the roughness of the wind was determined. The
observations were carried out by means of a remote anemometer with
electric contact which had been designed at the Glavnaya geofizicheskaya
observatoriya im. A. I. Voyeykova (Geophysical Main Observatory imeni
A. I. Voyeykov). These anemometers were installed on a mast on the south
side of the island Khankhipasi in altitudes of 6.15, 3.15, 1.65 and
0.75 m reckoned from the mast fundament. From the tape recordings the
values averaged for one hour were used for the analysis. These analyses
were carried out In consideration of the direction of the wind with and
Card 1/4

The Wind Profile in the Water-near Layer S/020/61/136/003/014/027
Above Lake Ladoga B019 B056
without taking the thermal stratification into account. The latter was
carried out with a temperature difference of AT between water and air.
The small size of the island warranted conditions that were not
influenced by land, as a comparison of the temperature measurements
carried out on the island Khankhipasi and near it shows. In Table 1 the
mean values of the vertical wind velocity profile and of the roughness
parameter with and without taking the thermal stratification into account,
were given. There are 3 figures, 1 table, and 7 references: 5 Soviet, 1
German, and 1 British.
ASSOCIATION: Laboratoriya Ozerovedeniya Akademii nauk SSSR (Laboratory
of Lake Science of the Academy of Sciences, USSR)
PRESENTED: June 18, 1960, by-D. V. Nalivkin, Academician
SUBMITTED: June 16, 1960
Card 2/4

T I rpynns
T
Cl S/02 61/136/003/014/027
Y

no
B019 B
056
1 1.15 3,15 1165 0,75

IOB-JOIOB

0103
10
TO
BC3 YqeTa
PAL CTf3THCPIfX.
2
2

:
l
2.
1
:l

'
:

1
66

-
- a
7
<
1
2
t ,
.
I
t
1
1
5 7
0 46
103 d T :- 4 , - - - - , .
< A T < 4 3.1 2.4 2.0 t 5 !1
3C3. BIOB
7 tie3 VlAeT4 Tep5l. CTPaTlf(oftK. ?.. 5 7.0 t.8 t:G J5 3.02
- .-n-BCB
A T < 2
2. Z
2.1
2.1
1,9
2
0.01)
a T > 3.0 2.4 2.0 1,7 10 t
2- < AT < 2.5 1.9 tj 1.4 12
CII-CCB- Be3 YqCTA lepm. mall"b"K.
* 2.7 2.1 t.S t.5 31 7.62
C-cc3- AT < 2
1 2 0
: 1.6 1.0 t.4 5 -
C3 4 T > 4 3
2 2.3 t.0 J.6 9 -
2- < ar < 4* 1 2,8 12,f 11.9 11.5 17 1
77 11 rpynar. ;7: III rpynn IV rpyn
BUCOTS. m

kv _
sucofa. m do
RWCOTS. m w c 2,1

6
15
15 1
3
65
75
10
0
15
-
J
3
1
65
0
75
6
15
15
3
t
55
0 75 0
I

. , . ,
N
. .
.
.
. 1 . . x

4 0 3 4 a 1 2 7 066 6.7 5.9 5.4 4,8 17 32
0 7
7 7.2 6.7 6 0 1 0.04 0.99
3 4 3 2
: 1
3:
2:7
19
0.06
5.8
5.&
5.2
4.5 4 0
05
:
7 7
:
7.2 6;7 6:0 1 0.05 oj5
A8 4.1 3 6 3 0 3 7.4 6.4 5.7 5.0 4
4.4 3.7 3:2 2:6 t0 - - -
4
1 1
1 1
3 1
1 30 1 6
0 5
5 1
0 1
4 8 0.72 7.9 7.4 6.2 6
0 2 0

4
:1
3 8
:
3 2
:
2
9
:
1 72 D 8
: 5 5
: 4 3
: 4 5
:
7 0.06
7.9
7.5
5.5
6:
0
1
0:14
049
4.2 3.A 2'0 2.5 7 7 0 6 0 5.3 4 5 3 -- - - - - - - -
4.3 ?._ 3.6 3.3 13 6:9 5:9 5.2 4:6 1 - -
A
OR 4 2
5: 3.4 2 7
3: 22
7 6.41 8.4
8
8 7.5
7
9 5.6
9
5 4.4
4
6 3
2 7.62 7.1

Card 3/ A 2
4 1
3 5 3.9
3 0 t
2 5 3 -- . . . .
4 :6 3:S 3:2 2:7 8 - 7.7 6.3 5.1 4.0 1

S/020J61/136/003/014/027 i
B019/B056
Legend to Tabl'e 1: 1) Direction of-wind. I1) S .outheast - south-south-east.1
south south-south-west - southwest. 12) West-northwest - east-southeast
east east-northeast. 13) Northwest - north-north-West - north - north-
northeast - northeast. II Without taking the thermal stratification into
account. III) Group I. a~ Altitude in meters. b) Measured value. 0)
Rotighnesij. IV), V), VI) groups 11, 111, and IV . VII) Mean value of
roughness. The measured values of group I correspond to wind conditions
at which, at a height of 0.75 m above the fundament of the mast, there is
a wind velocity of up to 2.1 M/sec. Under analogous conditions the? wind
velocity of group II is 2.1 - 3.9 m/sec, that of group 111 4.0 - 5.9 m/secf
while the-wind velocity of group IV amounts to more than 6 m/sec.
Card.4/4

ACCESSMI NR: AP4037557
S/0202/64/000/002/0027/0033
AUTHOR: Smirnovaj, N. P.
TITLC: The use of correlation analysis for decoding the wave pattern in recordings
of local earthquakes
SOMCE: PIT TurlanSSR. Izv. Seriya fizilco-tekhnicheskikh, khimicheskikb i
geologicheskikh nauk., no. 2J. 1964, 27-33.
TOPIC TAGS: correlation analysis earthquake recording, Enismic wave,
seismograph, seirmogram, earthquake
AMTRACT: The author investigated the wave pattern of longitudinal, canposite,
and transverse waves., as well as ,.-aves of a general nature, which were recorded
seismographically by the Izgant, Kepele and Vannovskoye stations during the
earthquake of 13 November 1961, and by the Sary*-Kull and Vannovskoye stations
during the 13 June 1961 earthquake. The method of corz lation analysis is based
on determining the correlation coefficient vhich is contained In the linear
dependence
5x 0 a+ bx
!-Card

.,%rC NRI AP7004556 SOURCE CODES UR/0202/66
AUMOR: Ly1cov, V. I.; SmirnoVa. 1j. P.
Oi.',G: Institute of Hi -he Earth re r~a4SR Ut
-AtmosPhq - (Inatit
_ftnd
fizlki Zcm1i I atmosfery AN Turlo~SSR) 1~4
TITLE: Value of the ratio of velocities of head waves from the.ro-oliorovicic
discontinuity k~L
SOURCE: AN Turkm"SR. Izvestlys. Serlya fiziko-teldinicheskikh, khimichaskikh I
geologichaskikh nnuk, no. 3, 1966, 33-37
TOPIC TAGSt earthquake, Wioroviclc d1l)COnt:11AUlty, Uppor mantle, selomogram
ABSTRAM . 1.)
observations were made with "ZvMJj1a" c-Lations with inLol-mcdiato
,magnetic recording and it has been ound Lh;tL they record local and near
earthquakes in the frequency range 1-5 cPr, with a good accurZLCY. Thia i
.ai-ticlo is concerned primarily i-rith the of tho ratio or
the velocities of the P and 5 head wavcs frora tlic 11-iollio.rovicic discontinu-
a-ity. It was found that in the Ashkhabad rcf;ion therri is an anisotropy
of about 10%; this factor must be taken into account lwfien constructing
travel-time curves and when detennining coordinates of the focus when
head waves from the Moho are used. Study of the behavior of the appar-
ent velocities and the coefficient Kb, (ratio of boundary velocities)
,,ade it possible to obtain the first data on the character of the Moho
at the southern margin of the Pred1copetdjr_skiY dounwarp. Since there
is an anisotropy in the Kb ratio it appears that the matter of the
upper mantle is -i-nore anisotropi.e for one of the typoo of rjrre3 (for
Card 1/2 UDC! 550.340

KCC'_NR-'AP700455j6
ngitudinal or transvorse), Gbscr-~,al- with llz~-
-I ~ L stat ions make
~_o I
it possible to detenLnino 'Uhc ratio of ve-locitico Ln ~kc C! '11-acy to 1%.
L
Such an accuracy is adecrual -e for using this paramc~ter not only as a
'kinematic criterion of waves, bii',~, also as a of thn- mediumo
On the other hand, use of scismogrcmis frora stations o'L the gencral
pL. prelinimaY7 analysis of a larre, quantity of, data._---,-
typo require
OrIg. art:. has: 2 figuren. [JPRS i 38,46Y
SUB CODEt 08 SUBM DATEI 15Lbv65 ORIG RM 002
2/2

SAFARGALIYEVy G.S.p kand. yurid.nauk;PALIGOV,NJ., akcad.; IiGGATYREV, A.S.;
AFAFASIYEV, A.V., prof.; BYKOV, B.A.; SHAKINATOVI V.F., kand. istor.
nauk; POKROVSKIY, S.N., akad.; SAVOSIKO, V.K., kand. istor. nwik;
NUSUPBEKOV, A.F.t kand. istor. nauk; BAISFEV, S.B., akad.; GOROKH-
VODATSKIYy I.S.9 kand. istor. nauk; AXIMTOVg A., kapd. istor. nauk;
RAKHIXOVy A.v kand. istor. nauk; PIVUI, N.F.; CHULANOV, G.Ch., doktor
ekonom. nauk; BOROVSKIY, V.A., kand. ekonom. nauk; SYDYKOV, A.S., kand.
pedagog. nauk; ZHANGELIDIN, T.y kand. filos. nauk; KARASAYEV, L.K.;
KAWAPIN, A.K.t kand. istor. nauk; BELENOV, M.D., kand. ekonom. nauk;
KARYNBAYEV, S.R., kand. mod. nauk; AKMWOV,
doktor filolog.nauk; SILICHENKO, M.S., doktor filolog. nauk; YERZA-
KOVICH, B.G., kamd. iskusstvovedcheskikh nauk; RYBAKOVA, N.; MUKHTA-
ROV, A.I.; BOGATENKOVA, L.I.; UNDAKBAYEV, B.; SIRANTOV, K.S.; SHVYD-
KO, Z.A., red.; MPIMTSOVA, L.B., red.; ZLOBIN, M.V., tekhn. red.
(The Soviet Kazakh Socialist Republic] Kazakhskaia Sovetskaia So-
tsialistichebkaia Respublika. Alma-Ata, Kazakhskoe gos. izd-vo,
1960. 477 p. (MIRA 14:6)
1. Akademiya nauk Kaz.SSR (for Fallgov, Pokrovskiy, Baishev)
2. Chlen-korrespondent Akademii nauk KazSSR (for Bykov, Smirnovaq
Sillchenko)
(Kazakhstan)

MI P, C, 11
r1
17-1 1
EM. ",- ~! r ~'. I . - 8, ~.'
come oyamuj.ps of ,!IV,
88-103

C a 11
AUTHORS: See Table of Contents
TITLE: A Dynamic Theory of the Propqg8tion of StFismic Waves
(Voprosy dinamicheskoy teorii rasprostraneniya
seysmicheskikh voln) First Collection (Sbor-ni"k 1)
PUB. DATA: Gosudarstvennoye nauchno-tekhnicheskoye izdatel'stvo
neftyanoy i gorno-toplivnoy literatury, Leningrad-
skoye otdeleniye, Leningrad, 1957, 386 pp., lgoo
copies.
ORIG. AGENCY: Ministerstvo neftyanoy Promyshlennosti SSSR.
.L.
Neuchno-issledovatel'skly institut geoflzicheskikh
metodov razvedki (NIIGR)
EDITORS: Editors: Polshkova, M. K. and Petrashen', G. I-;
Editor-in-Chief: Fedotova, M. I.; Tech. Ed..,
Gennadlyeva, I. M.- Corrector,- Segall, Z.G,
PURPOSE: This collection is intended for seismologists and
particularly exploration seismologists and senior
university and graduate students interested in geo-
physics and in the theories of elasticity and
Card 1/6 acoustics.

Call Nr: 1119002
A Dynamic Theory of the Propagation of Seismic Waves (Cont.)
lems In oil-bearing areas diminishes the efficiency of existing
techniques. Therefore a careful study of these articles may lead
to application of the dynamic theory described In interpret-
ing seismograms. The first 6rticle (pp. 7-69) by Petrashen'
discusses the most typical problems in wave propagation and the
method of their solution. Simplification of the final formulas
computed for the components of the fields of displacement is
the main consideration. The second article by Petrashen'
(pp. 70-163) describes the general quantitative theory of re-
flected and first-arrival waves. The third article, that by
Petrashen' and Manukhov, considers wave intensities and data on
the parameters required in composing theoretical seismograms.
The fourth and fifth articles examine the method of composing
such theoretical seismograms. The concluding articles examine
wave propagation in an elastic semi-space. No personalities are
mentioned; there are bibliographic references at the end of
each article.
Card 3/6

Call Nr; 1119002
A Dynamic Theory of the Propagation of Seismic Waves (Cont.)
Ch. IV. Smirnova.--N-. -S..' Tsepelev, N. V. Berdennikova, N.I.
_
CoiftrF6-~It
ion of Theoretical Seismograms for Reflect-
ed, and First-Arrival Waves Propagated in Plane-
parallel Media. 213-248
No personalities are mentioned; there are 4
references, all USSR.
Ch. V. Malinovskaya, L. N. Composition of Theoretical
Seismograms 249-282
No personalities are mentioned; there are 5
references, all USSR.
Ch. VI. Manukhov, A. V. Exact Theoretical Seismograms for
Wave Propagation in an Elastic Semi-space _283-295
No personalities are mentioned; there are 3
references, all USSR.
Card 5/6

Call Nr: 1119002
A Dynamic Theory of the Propagation of Seismic Waves (cont.)
Ch. VII. Ogurtsov, K. I., Uspenskiy, I. N. and Yermilova, N.I.
Quantitative Investigations of Wave Propagation in
the Simplest of Elastic Media 296-365
No personalities are mentioned; there are 5
references, all USSR.
Ch. VIII. Some Explanations for the First Four Articles
of thjs Collection 366-386
AVAILABLE: Library of Congress
Card 6/6

32485
S/OAA/61/000/010/051/051
-7, Clil/C222
AUTHORS: Smirno and
-;-ermi lovva, N.I.
TITLE: On the construction of theoretical seismograms in 'the
neighborhood of the origins
PERIODICAL: Referativnyy zhurnal~ Matematika, no. 10, 1961, 57-58,
abstract 10 V 330. ("Vopr. dinamich. teorii rasprostr.
seysmich. voln.11 3. L., Leningr. un-t, 1959,16!-21,';)
TEXT: The authors describe a method for the construction of theoretical
seismograms of the reflected and the shook waves in the neighborhood of
the origin. The authors give an assembly of the calculation formillas and
discuss questions relating to the obtaining of the auxiliary functions
appearing in the formulas. The appendices I and 2 of the paper contain
tables. At first the functions
I (a.) I(a) a d3
I I fj a e dg e
Card lk~

-,I ;A5
.J/04 61/000/010/051/051
on the construction of theoretical C111YC222
4
are tabulated, where a = jai e and the branch of the root is
determined by the condition arg 5 -1,-- for (1 0 . These
8
functions satisfy the equation y"(a) + 2ayl(a) y(a) 0 for the
initial conditions
11(0) 1 .75)(1 i), 1(0) = F( 1 ~75)
3
1,' (0) --5) i) , I i (0) = 1 .25) -
""he table I contains values of 1,1(a)1 ps .9S vnilk~?s of
2
(a) T, + a.) a arg Ika) with rftree,
decimals for 1-9.1 0-00(0-01) 1.00 (0,10) 5.00 ThCI Tab,~- II cr,ntairis
values of
Card 2/t~

0, the construction of theoretical.
where
12485
F-,/044/61/ooo/010/051/051
Gill/C222
(T) ib (T)
W - I -t dw,
(D+ (,r, r) 2,. to F e'
I - L. (T) (T)
IV + (c, r) F eiw'c dca,
> 0.
F. - ~ I /'(c 1(Z)
1114
(C V, =--.) I e- Ir--- < 0,
I EO
(C if 0.
lbe
(C Y=-. < 0.
Card 3/ 4

3106 0/6 2/03 5/005/014/0 -.5
D~47/D307
Ye. V.
rova, Klytiahn4kova, G. G. and Szairn-ova,
ion, o.L -buteriL, o' crack-
tfie but;itte
nz~ -'ase!3 on a pnouprioric acid "'i'I'm ccltalytit
-,rikladnoy v. 35, no. 5, 1'~362,
C%rvicro ~'Or lilms Ot, i.haspi.ovic ac-I'd, based on na-
irxvvati6atod. The fil- .,~crL orcr;~trcd
or~ tne b,-.oe of 6round qU.'ArtZ of uand3 tr-,~ated -,,,Ith HF.
cavried out under constant flow conditions. ;,n
i:. prcsuure from atmosPher-ic to 40 - 50 a=. wao-found tv
lov,,cr efficiency of the polymerization proce.9s. A aer-193
sands were also prepured as carrIera to inveati-
t.' i ff c- c t u of impurities and of SpeQific grain ijurfacea. Re-
cxpreLijed as the yield of diisobutylene polymer as a por-
:/2

U/', "O-j 5/00.") 0 14/0 1
07
f~)j. C: 2. e L; 0 C;-. e - r- u r-
C t fi I
S "IU3 a r L h e e a c 0 a i m i -,; mi e v nd i 0 o
J~
vo (at atmosp'. t ea-
Q U,'! C; b .-.Lr-c
0" 75 for t"r,e roac-
C a i n p i i 'G ra L e
~I-e3h priospnoric cv~id for -.he
0.5 0 . 7;'~ 0-*
or j4r,~i- quantity per
fo-i, 50 hours -,xicier these conditions, t'-e uc-
oa quartz uccamc, comparable
y
---.du3-.r.4al catalyst (phosphoric acid on
s %-.,cre eaL;ier to re~e-
,-b,, sed cataiyot
'~~(:UCG'-3 t :1 1 ~'.!;,.d air or steam and bloa]"nz thtn
-i*.,--,Ot. Acid-rezistant sl~eal -eac tor
usod aa a
v d d not 2f-'ect I 1-i e reaction. There are 2 fijures.
r ~,. z; 3,,r z;'~ iy Losudarstvennyy universitet imeni II. G.
Oht;i,nyLi1r.evsko~o (Saratov S-,,-te Unlvaruit~y imeni .l. G.
Chcr.~y:~hevukiy
A2ril 10, 1961

SMIRNOVA, N.S.
Calculation of wave fields in the vicinity of aencdes. Pt. 1.
Vop. din. teor. raspr. seism. voln no.6:30-59 162. (bffRA 16:7)
(S4ASMIC waves)

VC)T 7Tj IT
ey
f C,
11c)
-a)
'i"zros -ic,-,-Ona-se~enlya sw az i
c al ric e s
r t F -'rlc 09
,Iti ~-.:)rjg,
port fo t
re
1-4 G

sl,UBI,IGVA, 11.
tITI.e t,;!~e~
otanicall COng, E, 3-12 AujL 6-
01~
p'-s ,jssl~

MIK1,111HEV, KHOMAZAK, A.I.; 11,01~HFIM03f)1-
SMIRNOVA, il,s.;
DL3r)rder.- in circulaLory regu1-aI,.--,-,-,n
atherosclerosis in 4-)gs. Trudy Innit .-I~n- I okrper. ka!
AN Grw- SSR 8:1.81- 186 163. k"'.:RA
1. Ukralnskiy institut
N. I
, D.,33tra-zheska, Klyev.

L 16174-66 EWT(m)/EWP(J)/T. WWIJWAWRM
ACC NR: AP5025348 SOURCE CODE: UR/0366/65/001/010/1868A8n
AUTHOR% Chapplya, A. S.; Zhisdyuk, B. I.; 11~rzhenko, L. M.;
Golub, G. I.; Ponbdia-Y-ey, A. A.
ORG. Saratov State University Imi. N. G. Chern shev (Saratovaidy gosudarstvennyy.
univereirer-
TITLE: P drogenatio of aromatic amin"I on ruthenium catalysts
SOURCE: Zhurnal organicheskoy khimiip v. 1, no* 10p 1965P 1868-1871
TOPIC TAGS: hydrogenation, aromatic nitro compound., primary aromatic amine,
catalysio, aniline, ruthenium
ABSTRACT.*' Aniline and m- and p-phenylenediamine (I) were hydrogenated In liquid
phase on Ru catalysts at 100-1700 to give cyclohexane analogs. All of the RU
catalysts testel gave satisfactory results, however, the rate of hydrogenation
decreased in the order Ru02>Ru-C7Ru-siliea gel. The p)cesence of an additional
Card 1/2 UDCi 542-541 s 547-551/3 546-96

L 16174-66
ACC NR: AP5025348
on the aromatic rinSl slowed down the reaction. Hydro-
amino or nitro group
genation of I at 80 atm. H-Pressure occurred faster in polar solvents
(H20, MsOH
than in solvents of lower polarity (EtOR, PrOH, n-amyl alcohol, or dioxane). In a,..
typical experiment, the catalyst was placed in a rotating autoclave, the aromatic
in a 3-10-fold amount of solvent, the autoclave pressurized with
amino added
electrolytic H to 110 atm. ani histed In an electric oven. After the H absorption:
was fini-,$,ed, the catalyst was filtered offq the solvent eliminated,, an] the
residue distilled in vacuo. The hy&-ogenation of I is highly ster4ospecific and
yields almost exclusively trans-1,4--iiaminocyclohexans. Orig. art. has: 2
fi gures and 1 table.
SUB CODE: o7 Sam DATz: 09Nov64/ -jM!GiWs OM/~~AOTR "M 1 005"
Card 2/2

m p t4 (I vA FONOW-RE-Vi A~A-
:lyl-ogenatioa some, aromatic a!:~j-ds and thv-r J,~,rivatsves
ruthenillm 4atalysts,, Znuf. org, Y=m, I
1;g 165.

T

-52535
NR: AT6012710
CESSION
AC

and 8 figures*

ASSOCIATION: nms

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NO REP. K(YV* 00511

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PIN S S S.

J C!" CI
"ilie Chemistry and Metabolism of Carbohycb-ates in An!lw-l and Plant Orgardsms.
CnnferQrice ir, Moscow. January 28 to T=.LLQ-ry 30 1958.

AT4MO06 S/2789/63/000/051/0014/0019
ACCESSION NR:
AUTHOR: Gayvoronskiy, 1. 1.; Krasnovskaya, L. I.; Seregin, Yu. A.; Smirnova, N. V.;
TITLE: The problem of the temperature limits of applicability of the method of
artificial modification using solid carbon dioxide
'~-jRCE: Tsentrallnaya aerologicheskaya observatorlya. Trudy*, no. 51, 1963, 14-19
lurit, IMUZ: meteorology, weather modification, fog, cloud, fog modification,
cloud modification, solid carbon dioxide,.Ice crystal, cloud seeding, dry Ice,
supercooled cloud, Ice formation
ABSTRAM Information on the temperature limits of effectiveness of solid carbon
dioxide as a reagent for the artificial modification of the phase state 6f super-
cooled fogs and clouds is contradictory, as demonstrated a review of the Soviet and
THIs article therefore reports on theoreticarl
western literature on this subject.
and experimental investigations to resolve this question. The authors used the
i! theory of homogeneous condensation in saturated vapor to study the generation of
ice crystal nuclei at different temperatures. A previously derived formula (L. 1.
Krutskaya, Trudy TsAO, No. 19, 1958) Is cited which gives the rate of formation of
nuclei of the new phase at the time of introduction of solid carbon dioxide tnto a
leugercooled cloud; this formula was used in computing the quantity of nuclei of the:
or

ACCESSION NR: AT4o4ooo6
inew phase formed under different conditions. It is shown that the generation of
I i
~nuclei of ice crystals in a cold chamber and in the atmosphere changes in conformi-
ty to different laws. For example, at a temperature of. -4C the effectiveness of
'C02 in a cold chamber is two orders of magnitude less than at -10C. In natural
iclouds, when granules of C02 are seeded from an aircraft, the generation of Ice
;crystal nuclei remains quite intense to -IC. As a-result, the production of-6
le down
large number of ice crystal nuclei in supercooled clouds and fogs is possib
,to temperatures of several tens of degrees below zero. However, to obtain the same
..,effect on the microstructure at a higher temperature, it is necessary to have a
';higher concentration of propagating crystals. At hightemperatures the width of the'
ozone forming from one pass of the aircraft will be smaller than at lower tempera-
;Itures. Various specific experiments and groups of experiments are described in
:detail. The following were the general conditions: vertical thickness of clouds
fogs - 100 to 1,000 m; air temperature at upper cloud boundary - +0-5 to -4.9C;!
Itemperaturd at lower boundary - 0 to -8.IC; wind veloci.ty In the cloud or fog layer,
not in excess of 3 m/sec. The experiments revealed that It Is possibli to inodify~-_
j.(disperse) clouds and fogs at temperatures as low as -2C. The experiments were
made at Alma Ata, Frunze and Dzhambul and made It possible to keep the airports at
Nthose cities free of fogs-and low clouds. it Is noted that further work must be
'done to determine the influence of wind on artificial modification of fogs and
ds and the modification of clouds and fogs associated with frontal processes.
':2/3

ACCESSION NR: AT40ooo6
Orig. art. has: 9 formulas, I figure and 3 tables.
ASSOCIATION: Tsentrallnaya aerologicheskaya observatoriya (Central Aerological
Observatory)
SUBMITTED: 00 ENCL:' 00
SUB CODE: ES NO REF SOV: 001 OTHER: dk'2
Illy
Car.d.i 3/3

KIRPICHNIKOV, M.E.; LEBEDEV, D.V.; SMIRNOVA, N.V.
".. -_: ,
Aleksandr Allfonsovich Grosageim, 1888-1948. Moskva, Izd-vo Akad.nauk SSSR,
1953. 127 p. (MLRA 6:11)
(Gorsegeim, Aleksandr Allfonsovich, 1888-1948)
(Bibliography--Grosageim, Aleksandr Allfon3ovich, 1888-1948)
(Groasgeim. Aleksandr Allfonsovich, 1888-1948--Bibliography)
(Caucasus--Botany) (Botany--Caucasus)

.i
CHERLUKIIIII., A.Yo.) inzh., red.; ASHKENAZI, E.L., red.; YEFUEI~GVA, V.K.,
red.; IVAEOV, N.F., red.; MUST40BRODSWIA, L.L., red.;
YOSHENTSEXA, I.I.I. red.; KHABDITI, Me., red.; BELIGHTI., V.I.,
r.qladshiy red.; KOMAIROVA, Ye.B., mladshiy red.- S',-'IH11GV4 N 1;
r,ladshiv red.; Klkff:-IGVA, I.I., mladshl4y red.; BRUDNO, K-.F-.)
tekhn. red.; KOLEE-SNIKOVA, A.P., tekhn. red.
[English-Russian technical dictionary].Anglo-russkii politokJmi-
cheskii slovarl. Moskva, Glav. red. inostr. nauclmo-tekhn.
slo-varei Fizrpatgiza, 1962. 663 p. (111RA .15: 11)
(English language--Dictionai-ies-liussian)
(TechnoloQr-Dicti-onaries)

SMIRNOVA, N.V.
I
Scientific activity ofIthe Botany Department of the Krivoy Rog State
Pedagogical Irstitute. Bot.shur.[Ukr.] 11 no.1:116 154. (MMA 8:7)
(Krivoy Rog-Botany-Study and teaching)

,Ibs Jour Pipf Zhljr Biol., No 211 ).9583 95392
Auth~_-r Khrobtov, N.S., Smirilova, N.V.
Inst Burynt -Mongol State Agricultural Experimental Station
Title IrriLPti,Dn Syster. and the Influence (,,:C Different 'TyjjC.3
band doses of fertilizers on Irrigatod Meadows.
Orig Pub Tr. Bury-at-Mong. gos. ,.)pytn. st., 1957, vYp.. 2,
65-80
P,bstract No abstract.
Carl 1/1 E N D
122b

ARENDARUK. A.P.; BUDOVSKIY. R.1.; GOTTIKH, B.P.; KARPEYSKIY. M.Ya.
KUDRYASHOV, L.I.; SKOLDINOV, A.F.; SMIRNOVA, N.V.; KHORLIN, A.Ya.
KOCHETKOV, U.K.
Dihydrosarcomycin and related compounds. Part.le- Zhur.ob.khim.
27 no-5:1312-1318 MY '57. (MTRA 10:8)
I.Institut farmakologii i khimioterapii Akademii meditsinskikh
nauk SSSR.
(Antibiotics)

-.ffJIITDARUIL', A.P., SMOLIN, D.D., SK
SMIRIIOVA,jT,-Y-,-, [OLDINOV, A.P.
Esters of lf-(Rrylalkyl)-i~-phenylisonipecotic acid. Medprom.12 no.7
31-35 Jl 158 (MIRA 11:8)
1. Institut farmakologii i khimioterapii AMN SSSR.
(NIPYGOTIC ACID)

KLIMKO, V.T.; PROTOPOFOW,., T.V.; SMIR11,10VA, N.V.; SKUDINOV, A.F.
Funct~.onal derivatives of rAloncdiald6hyda- and their reactionz!.
Part 12! Preparation of Ikox-yacroleins. Zhur.ob.khim. 32
no.9:2961-2966 S 16-9. (miru
1. Institut farmakologii i khimioterapii AMI SSSR.
(Acrolein)

GROMOV, I.M.; GUREYEV, A.A.; NOVIKOV, G.A.; SOKOLOV, I.I.; STRELKOV,
P.P.; CHAFSKIY, K.K.; PAVICVSKIY, Ye.N., akademik, glav.
red.; BY)RiOVSKIY, B.Ye., red.; MONCHADSKIY, A.S., red.;
SKARLATO, O.A., red.; SHTAKELIBERG, A.A., red.; SMIRMOVA,
N.V., red.; SMIRNOVA, A.V., tekhn. red.
(Mammals of the U.S.S.R.] Mlekopitaiushchie fauny SSSR.
Sost. I.M.Gromov i dr, Moskva, Izd-To AN SSSR. Pts.1-2. 1963.
(MIRA 16:9)
1. Akademiya nauk SSSR. Zoologicheskiy institut.
(Mammals)

3M PHASE I BOOK EXPLOITATION SOV/1880
Leningrad. Glavnaya geofizicheskaya, observatoriya
Mikroklimat severnoy chasti Kazakhskogo melkosopochnika (Microclimate
of the Northern Part of the Kazakh Hummocky Region) Leningrad,
Gidrometeoizdat, 1958. 207 P. Errata slip inserted. 800 copies
printed.
Sponsoring Agency: Glavnoye upravleniye gidrometeorologicheskoy sluzhby
pri Sovete Ministrov SSSR.
Ed. (Title page): I.A. Golltsberg, Doctor of Geographical Sciences;
Ed. (Inside book): V.D. Pisarevskaya; Tech. Ed.: N.V. Volkov,
PURPOSE: This book is intended for meteorologists, agronomists, workers
on collective farms, and the interested layman.
COVERAGE: This book provides a climatic description of the Kazakh
"Melkosopochnik" (hummocky region). It lists the results of studies
C ard l/-0,-

Microclimate of the Northern Part (Cont.) SOV/1880
made on the microclimate of the region. Individual chapters deal
with the physical phenomena underlying and shaping the microclimatic
features, and the effect the latter have upon the region's agri-
culture. The work was prepared by members of the GGO and the
KazNIGMI. A map on the recurrence of drought was drawn Lip by
Doctor of Agricultural Sciences A.M. Alpatlyev and scientific worker
A.I. Trofimova of the Vsesoyuznyy institut rasteniyevodstva. Ye.I.
Kuznetsova worked on data dealing with the temperature of the active
slopes of Li Pkhill En and the changes in prevailing air currents
brought about under the influence of relief. The chart showing
the amount of precipitation during the warm period of the year was
drawn up by L.P. Kuznetsova under the direction of Doctor of Geo-
grahpical Sciences O.A. Drozdov (GGO). There are 89 references of
which 81 are Soviet, 6 German, 1 French, and 1 English.
TABLE OF CONTENTS:
Foreword
C ard 2/8--

Microcilmate of the Northern Part (Cont.) SOV/-1880
Ch. I. Methods of Conducting Investigations
The Organization of Microclimatic Investigations In the Kazakh
Hummocky Region (I.A. Golltsberg) 5
The Methods of Field Observations of the,Combined GGO Expe-
dition and the Description of the Working Locality
(T.A. Golubova) 6
Weather Characteristics During the Period of the Expedition's
Activities,(N.Vi. Smirmova) 11
Ch..II. A Brief Characterization of the Climate of a Wann Period
I. . (N.V. Sm-irnova)
The Physi-c-a-T-G-eographic Properties of the Region 16
Conditions of the Development of Climate and the Characteris-
tics of Its Individual Elements 17
Ch. III. The Mechanism of the Formation of Microclimatic Dif-
ferences Under the Conditions of a Dissected Relief
The Radiation Regime of Slopes (Ye.P. Barashkova and T.A.
Golubova) 34
Card

Microclimate of the Northern Part (Cont.) sov/1880
Determining the Temperature of the Active Surface of Slopes
(Li'Pkhill En) 42
Wind Conditions and Their Effect on Thermal Variations
(Ye.N. Romanova) 45
The Kicroaerologic Features of the Cold Air Flow Over a
Slope (P.A. Vorontsov) 63
The Microaerologic Features of the structure of Nocturual
Inversions (P.A. Vorontsov) 70
Ch. IV. The Microclimatic Peculiarities of the Thermal Cycle
and of the Humidity of Air Under the Conditions of a
Dissected Relief
Soil Temperature (Ye.P. Arldiipova) 79
Air Temperature (M.Ya. Glebova) 94
The 24-Hour Cycle of Air Temperature (Z.A. Mishchenko) 117
The Relative Humidity of,Air (M.Ya. Glebova) 128
Ch. V. Main Features of the Adverse Conditions of a Vege-
tation Period
Drought and Dry Winds (I.A, Golltsberg) 134
Card 4/V

Microclimate of the Northern Part (Cont.) SOV/1880
The Recurrence of Rainless Periods (A.D. Gedeonov) 137
Frosts (I.A. Goltsberg) 140
Ch. VI. The Effect of the Relief of the Hummocky Region on
the Agrometeorological Conditions of Growth and De-
velopment of Agricultural Crops and Natural Herbs
Agrometeorological Conditions of Growth and Development of
Plants (A.P. Fedoseyev and G.G. Beloborodova) 149
The Effect of Thermal Periodicity on the Growth and Develop-
ment of Grain Crops (Z.A. Mishchenko) 165
Ch'. VII. The Agroclimatic Features (I.A. Golltsberg)
The Requirements of Agricultural Crops From Climatic Factors 170
Agroclimatic Featuresof a Vegetation Period for the Area of
the Kolkhoz im. Kirov, Aryk-Balykskiy rayon, Kokchetavskaya
oblast' 176
Bibliography 183
Card 5A7

KURANOVA, I.P.; S~ffRNOVA, N.V.
Preparatton of Phiodogramicidin S. Izv. AIN SSSR. Otl.khim.na-.xk
no.6:1148 Je 163. (MIRA 16:7)
1. Instittit kristallografii AN S3SR.
(Antibiotici)

CAYVOISKIY, 1. 1.; KRASNOVSKAYA, L. I.; SEREGIN, Yu. A.; SMIRBOVA,
V.
U
Temperature limits of the applicability of the method of
artificial reaction using solid carbonic acid. Trudy TSAO
no. 51:14-19 63. (MIRA 17:5)

S'. i I :-ulro V-k, 11. V.
"Type of Cement and the Influ61" e of Cementation Upon the Collector Itroperties
of SandZI ~Iocrksff
Tr. Vses. Neftegazovogr, n.-i. in-ta, No 4, 12-53--IL6, 19-54
The author considers the problem of the influence of textural types of
cerient ani percentage composition of cement upon the collector properties of
fine-grain quartz sandstones of the productive horizons of the gas deposits
In the West Ukraine. He selecto the principal and intermediate textural types
with uniform and iv-;nuniform. distribution of cement among the grains.
(RZhGeol, No 6, 1954)
SO: Sum. 492, 12 May 55

SMIRNOVAO N.V.
-Z',
Now data obtained from comparing cross sections of the Ugersko
series in the Carpathian Mountain region. Trudy TNII no.11:65-83
157. (MLRA JO.-11)
(Carpathian Mountain region--Petroleum geology)

3(5)
SOV/9-59-7-7/15
AUTHOR Smimova, N.V.
,T-ITLE 2 Cement Types and Their Effect on Permeability 'of Sandy Rocks
FERIODICALt Geologiya nefti i gaza, 1959, Nr 7,pp 33 - 39 (U-SSR)
ABSTRACT: Collecting properties of oi-I and gas bearing sand horizons are often
subjected to changes due to the different degrees of cementation of
rocks. The regularity of such changes can be established by in-
vestigating the cements of collecting rocks. Until +.be present a
summary composed by M.S. Shvetsov on cement charac--~eristics had served
as a basis for work with elastic rocks. The author of the present
art�cle carried out a detailed subdivision of cement types according
to correlations between the cement and the grains. There are two
groups,i.e. uniform and non-uniform cements. The first group includes
t
the pellicular, contact, porous,incomplete porous and basal types. Non-
uniform cements are divided into two subsections including mixed and
clotted types. Characteristics of the different cement types are given
in a -table and are illustrated by diagrams and microphotos. The effect
of the cement content on the porosity and permeability of sandstone was
Card 1/2 investigated and it was stated that regular inversely proportional

Cement Types and Their Effect on Permeability of Sandy Rocks SOV/9-59-7-7/15
correlations between permeabilA~ and content of cement could be deter-
mined only within each of the aforementioned groups and not in general.
Data obtained proved that the cement content in sandy gas and oil
collectors can vary from the fraction of a per cent to 4~~, according
to the type of cement. Sandstone and aleurolites with basal, basal-
porous, porous-basal and porous cementscannot form collectors. All other
types analyzed can serve as.oil and gas collectors. It is concluded that
the described investigation of cement types permits to estimate the
collecting indicators of sandy and aleurolite rocks and explains regu-
larities kn their change.
There are: 1 table, 2 diagrams, 1 set of microphotos, 1 graph and 2
Soviet references.
ASSOCIATIONt Instimut geologii i razrabotki goryuchikh iskopayemykh AN SSSR (Institute
of' Geolog~ and Exploitation of Minerkl Fuels of AS USSR)
Card 2/2

SMIRNOVA, N.Y.
Types of cements in sandstones and siltstones. Trudy Iast. gpol.
i razrab. gor. iskop. 1:247-259 6o. (MIR4 14::L)
(RockB. Sedimentary)

SMIRNOVA, N.V.
Relationship between silification and the reservoir properties
of,Devanian sandstones in the Volga-Ural region. Geol. nefti
i gaza 5 no.7:38-42 J1 161. (MIRA 14:9)
1. Institut geologii i razrabotki goryuchikh iskopayemykh.
(Volga-Ural region-Oil, sands-Permeabi-lity)
(Porosity) (Quartz)

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SMIR140VA, N.V.
"On the Ronction of' Ketene With the Amiduf5 of Carboxylic Acids. " TheSis for degree of Cand,
Chemical Sci. Sub 2F Jun 50, Moscow Order of Lenin State U Imeni M. V. LomonoBov
SummarY 71, 4 Se. .-;2, Dissertations Presented for Degrees in Science and Engineering in
Moscow in 11050. Frcm Vechergaya Moskva) Jan-Dec. 1950

USSR/Chemistry TrisayInitrogen I Jun 52
"Preparation ot Compounds of the Triacy;Lnitro-
gen Type," N.V. Smirnova, A.P. Skoidinov., K.A.
Koches~aov, Corr Nem, Acad of Sci SSSRJO All-
Union Sci Res Cham-Phar Inst imeni S. Ordzhoni-
kidze'
"Dok Ak Nauk SSSR" Vol 84, No 4, PP 737-740
Ketene reacts with amides in the presence of
F-I