SCIENTIFIC ABSTRACT BLINOVA, M.V. - BLINOVA, Z. A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205520012-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 22, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

P Vo(Im- I. Ion W D).(,ar-boxyllo Acidu by Oxidatiull (,(66o
wji-Il wil-vic' Al-.1d. Comilitirt SOV/130-33-2-31 2
5/5
I 10110N: All-UnIon Scluritific Roucurch imaittite vor Putrochernical
Proccuueu (Vuesuyuznyy tiuLAcIiii,.i-.IL;-.jlcduvatellulcly
ItioUtut rieftelthimichc8lcildi pvuLUCLIUUV)
SUBMITTED: March 3, 11.111i(.j

MLDAVSKIY, B.L.; BLINOVA, M.V.
Thermal converoion of ouccinic. acid into
r,-ketopimelic acid.
Neftekhimiia 5 no.l-.108--llO Ja-F 165. (MRA 18:5)
. 1. Voesoyuznyy nauchno-iooledovatellskiy inotitut
neftekhimiche-
skikh protsessov. -

CHISTOV, A.D.; BA7ARNOVA, G.V.; H&K, N.D.: BIMIKOVA,
V.I.; BLINOVA M. Ta.;
KMNOVA, P.G.; XAKAROVA, N.D.; PRIPISTSOVA, K.D.;-
R-HOHOVA,-"-
7W. - ~--
TOLKACHEVA, Te.M.; TYUNUTEVA, V.V.; ZINGHENKO, V.S.,
red.izd~-va;
PAVLOVSEIT, A.A., tekhn.red.
[Foreign trade of the U.S.S.R. for 1918-1940;
statistical survey]
Vneshniaia torgovlia SSSR za 1918-1940 gg.;
statisticheskii obsor,
Moskva, Vneshtorgisdat, 1960. 1134 p. %*MIRA 13:10)
1. Russia (1923- U.S.S.R.) Glavnoys tamozbonnoye
upravlaniye.
2.~Otdel statistW Glavnogo taM02hennogo upravleniya
Hinisterstva
vneshney torgovli SSSR (f6r'all, except Zinchanko,
Pavlovskiy).
(Commercial statistics)

-BLINOVA~ N*I*;. GARAYMKAYAp LoS.
Atian of.the world, published in 1959; book format, Sbor.ist.po kart.
no.13369-78 161. (MM 15:5)
(Atlaoss)

PETRZHAKp K.A.; TOLMACHE;Vp G.M.; USHATSKIYp V#N.; BAK..
M*A.;
BLINOVA, N.I.; BUGORKOVp S.S.; MOSKALIKOVAp E.A.; OSIPGVA,
~'OV, Yu.G.; SOROKINA, A.V.; CHERNYSHEVA, L.P.;
SHIUAYEVA, L.V..
[Yieids of certain fragments in 'U215pU2111fand pU239
fis_ 235
sion by neutrons] Vykhody nekotorykh oskolkov pri delenii
U
U238 i FV9 neitronami. d"eleniia. Moskva, Glav. upr. po
is-
polizovaniiu atomnoi energiip 1960. 14 p. (MIRA, 17:2)

32986 ff
S/64 61/000/000/013/033
6 00 B1 04XB1 02
AUTHORS: Petrzhak, K. A. , Tolmachev, G. M. , Ushatskiy, V. N.
;~?~ . S., Moskalikova, E~ A_
o.., ~In Bugorkov, S
V . B.~,Petr~cv, Yu.'G., Sorokina, A. V.9
Chernyaheva, L, P., Shiryayeva, L. B.
TITLE: Yields of some fragments in the fission of U 235 ~ U2389 and
Pu 239 by fission neutrons
SOURCE: Krupchitskiy, P. Ao, ed. Neytronnaya fizikap Bbornik statey
Moscow, 1961, 217-223 89 95 99 ill 115
TEXT: The authors determined the yield of Sr , Zr , Mo . Ag Cd
and Bs.140 in the fission of U 235, U238 , and Pu 239 by fission
neutrons. A
U235-enriched uranium plate arranged .in the thermal column of a
heavy-water
reactor of the AS USSR served as neutron source. 300-mg tablets and
1-gg
targets were produced from each substance to be fissicned. The
fission
events were recorded in a fission chamber during the entire
irradiation
period (Fig. 1). The fission fragment yields were determined from
their
Card 1/j!

32986
S/641/61/000/000/013/033
Yields of some fragments in ... B104/B102
P-aotivity~ The absolute P-aotivity was measured by two standard
instruments with end-window countersi. These standard instruments
were
calibrated with preparations of the fission fragments "o be studied
which
had been applied to a collodium film. The absolute P-aotivity of the
standard preparations was determined either with a 4n-counter or
with an
end-window counter havinga idndow thickness of 0-005 + M01 mg/CM2..
Six
to eight measurements were made in three to four tablets (Fig. 3)~
The
determination error of the fragment yield was between 6 and 11V6. The
fragment yield is found to depend on the isotope mass number. There
are
3 figures, 3 tables, and 7 references: 3 Soviet and 4 non-Soviet~ The
four references to English-language publications read as follows;
Engelkemeir, D., Novey T., Schover D_ Radiochemical Studies; The
Fission
Products, Book 3? div. IV, vol. 99 1334 (1951)1 Radiochemical
Studies:
The Fission Produots. Book 3, div. IV, vol. 9, Appendix B, 2003
(1951);
Keller R., Steinberg E., Glendenin L.. Phys. Rev., 94, 4, 969 (1954);
Turkevich A., Niday J., Phys. Rev., 84, 1, 52, 71.
Card 2/j

29820
S/020/61/140/006/017/030
B103/B101
cp/ WOO
AUTHORSt Blinova, N. I., Solntsev, V. M., and Tolmachev, YU. M.
TITLEt Some particularities of the interaction between uranium mixed,'
oxide and acids
PERIODICA4:., Akademiya nauk SSSR. Doklady, v. 140, no. 6, 1961,
1314-1316
TFM t The authors studied the discrepancy between the initial and final
2+ 4+
UO2 1 U ion ratios on dissolution of uranium mixed oxide in acids
without oxidizers. This ratio is 20 on final solution, i~bereas in the
initial stage, mainly U(VI) is dissolved, so that the ratio U(VI) t
U(IV)
is much higher than 20. High-purity U 30. powder was dissolved in CO 2
atmosphere at constant temperatures (25 or 900C) in a) sulfuric,
.j W-b)Aperchlorio, and- c) aoetio acids. The solutions were anal zed
after
11)
100--min (H 2S04), 10 min (HO10 4), and 40 min (CH3coo U IV~ was
d.etermined
in the solution by titrating with XMnO 41 the total quantity of U by
Card 1/4

820
S702Y61/140/006/017/030
Some particularities of the interaction ... B103 B101
precipitation as ammonium diuranate and igniting to U30.. Ratios of
76 : I in a), 60 0 in b), and) 300 1 1 in a) were found for the
beginning
solution of U3OV After 2 hr, the ratio U(VI) 3 U(IV) in the solution
became I t-1 and remained constantp until dissolving was completed. A
precipitation is deposited in the final stage of dissolving, in which
the
ratio varies between 20 and 10. Once the ratio of lil is reached in the
solution as well as in the precipitation, the composition of the
precipitation does not change anymore. This is a dark, slightly violet
colored powder which becomes grey-green on drying in air, the ratio
U(VI) s U(IV) approximating 2tl..--A ratio of 10 is maintained for 48
hr in,
the powder, when the water is saturated with CO 2' 'When U30ais
dissolved
in HNO 3' a stable ratio of 21l is conserved in the powder during the
entire
time of-dissolving. It was foun a that the uranium atoms in U30a do not
play the same role. It is difficult to find a',different explanation
for ~e-
the varying..U(VI) s U(IV) ratios in the solution and in the
precipitate
during the,reaotion of U 0 with acids. It is presumed that U 0 which is
2 5
Card 2/4

29a2O.
5/020J61/140/006/017/030
Some particularities of the interaction ... B103/B101
pos:ibly a compound of U(V) forms in the final stage of U 308
solution
in acids. Probablyq U(V) disproportions to U(VI) and U(IV) in a
ratio of
10, when it-is dissolved in acids. It might be possible, however,
~that
U205 is not a comDound of U(V), but for instance UO 3' UO2. When it
is
dissolved in acids, a ratio of U(VI) s U(IV) w 10 will result. In
this
case, U308 should have a composition of say UO 3' UO 3' UO 2. UO
3*U205 is
suggested, until the structure of U 308 is finally cleared up. Tbe U
308
formed reactsq however9 much slower with acids than the initial U 0
3 a
molecule. It is presumed that the peculiar course of the reaction
described is characteristic of many chemical compounds; oxides,
sulfides,
and further compounds (basic and double salts) of metals, the atoms
of
which show different valences, will react, presumably, sometimes in
an
analogous way. Papers by Vikt. I. Spitsyn, G. M. Resmeyanovaq Ye. A.
or
Kanevskiy (ZhNn,5., 1938 (1960)) and by G. M. Nesmeyanova, G. M.
Alkhaza-hvili (Atomnaya energiya, A, 330 (1960)) are mentioned.
There ar~
3 tables and 6 references$ 4 Soviet and 2 non-Soviet.
Card 3/4

29820
S/02q/61/14o/oo6/ol7/030
*4artioularities of the interaction... B103/BlOl
ASSOCIATIONt Radiyevyy institut im. V. G. Khlopina Akademii nauk SSSR
(Radium Institute imeni V. G. Khlopin AS USSR)
PRESENTEDt May 24, 1961,by A. A. Grinberg, Academician
SUBMITTED: may 18, 1961
Card 4/4

BUINOVA, N.L.; TOLMACHKV,, YU.Ne
Problem of the equivalence of uranium atoms in uranous-uremile
oxide. Radiokhimia, 4 no,4:447-451 (MIRA 15:11)
(Uranium oxide)

XJNOVA., N.L.; ROMANOV., G.A.; SOLINTSEV, V.M.; TODUCIM7, Yu.M.
Nwetic properties of U205o Dokle AN OM 347 no*5#1112-M3
V t62, (KM 1602)
1. Radiyern, inetitutime TOO. Iblopina, AN SSSR~ Predstavleno
a.kademikom A*Ae Qqnbergome
(Uranium oxides-Mapetic properties)

/Va-P(b 4',
L L972- U L
ACCFSSION N_R: AP4043855 'T 'Esp"G 8/0186/64/0D6/004)'0463/0466
-Blinova, N. 1-:;,, Kurbatov, V. V.; Solntsev, V. I.A.
TME: A roentgenometric study lot the system U sub 3 0 sub 8 U sub 2 0
sub 5
~A ~A 11641 463-466 ------
e--~dv ruct
U r.a d at urei-xray
TOPIC TAOS nitm oxide, oxi Ys a dif ra va
lattimeonstant, rbombic lattice, uranium pentoxide
h' b di- ng U0 in sulfuric acid or!
ABSTRACT- nle authors prepared U20 eit er y Soo V1 3
by reducing with hydrogen at 390C, and then determined Re lattice
constants
U308
by x-rav diffraction analysis during the reoxidation of U 0 to U10
They found
?t5l 8*
that3 as ",'20~ Is sat~.,ratcd with oxygen, only the U,O:: crv~ A 1r,
-b-
served in all the inter-mediate stages, and stable ~iffrac *, I ?T)
ice
of the U 0 latt. appear only after reachingg an empir ica !
3 8
The entire range of compositions from U 0 to U 0 is thu 8 Vinua
cemparison of the x-ray diffraction patie5rns 1A the authors to
conclodi-, in up-
position to the hypothesis of Milne (Am. Miner., 36, 5-0, 417, a;-.,'
that the U 0 lattice is a deformed U 0 lattice. On the bas~ir, or
hc~mulogy, thc
3 8 2 5
~wd' 1/2

most likely structure for the U 0 lattice Is a rhombic structure,
Produced by the
gradua I penetra t ion 4im oxysen. 24,a --into- the, U,U. unit Ce I I
a "ThL authors thank
:14 TolmA ev
.ku. Auibi-- orig, art. has: 2 tables and
Frak , eh for h s Va
A A e advice."
igure.
ASSOCIATIM None
SUMMED: 18Jan64 E14CL: 00 SUB CODE: IC, OP
M REF SOV- 004 OTHER: 012
:,Caro

BLINOVA,,-~,kp- ,,- -- -
Productivity of bits and econorde efficiency of rotar7
drilling.
Trudy VNIIBT no.6sI50-161 162 ' (MM 16:6)
(Boring)
I.

SHMV, S.I., obahchiy red. JJVQVAVofivJw, otv.red.; IVAIIOV, Yu.M.,
red.
kart; IGNATINKO, A.B., red.kart; 11OLISNAOVA, I.G., red.kart;
LIUMA, S.K.. red.kart; PZNTSON. Ye.E., red.kart; P3BFILYEVA.
N.A., red.kart; SERGAYEVA, S.I., red.6rt-, SHIRNOVA, A.L., red;-7----
kart; KHOLODOK, V.D., red.kart; ~amAN, Ye.M., red.kart; KUZNNSOVA.
O.L., tekhn.red.; LIFSHITS, N.I., tekhn.red.; SMICHU, A.T..
takhn.red.
['World atlas] Atlas mira. Moskva, Glav.upr.goodes. i kartografii
Ma SM, 1959. 324 pe (MIRA 12:12)
(Atlases)

:3~
4
U;
I
- ;R - .

IHOLIN, A.I.; PLINOTAO Moo "ably nauabnyy votrudaik.
Using the neutron-panw-ray method for determining the position of
oil-water c.ontact in forvAtions penetrated by the well. Trudy M
no.15t213-221 153* Mu 9: 8)
(Oil well logglM, Radiation)
I

PHASE I BOOK EXPLOITATION 749
Barsukev, Oleg Aleksandrovich; Zlinova, Nina Mikhaylevna;
Vybornykh,
Sergey Fedorovich; Gulinp
Yur-i-y-ITe-R-s-a-na-r-o-vi-c-h--,---D-a-RMT6v, Vladimir
Nikolayevich; Larionov, Vyacheslav Vasillyevich; Rholin,
Arkadly
Ivanovich
Radloaktivnyye metody issledovaniya neftyanykh i gazovykh
skvazhin
(Radioactive Methods for Exploring Oil and Gas Wells) Moscow,
Gostoptekhizdat, 1958* 314 P- 5,000 copies printed.
Reviewers: Tarkhov, A.G., Doctor of Physical and Mathematical
Sciences,
Professor, Department of Ore Geophysics of the Sverdlovsk
Mining
Institute im.eni V.V. Vakhrusheva; Executive Ed.: Shorokhova,
L.I.;
Tech. Ed.: Polosina, A.S.
PURPOSE: The book was authorized as a textbook by the Ministry
of
Higher Education for students of geological and geophysical
sections
at petroleum vuzes. It is also intended as a handbook for
geologists
and geophysicists dealing with the theory and techniques of
modern
radioactive methods of oil well exploration.,
Card 1/10

Radioactive Methods for Exploring (Cont.) 749
covERAGE: The authors stress the physical prineiples of
radiometry
of oil and gas wells, describe the operation of radiometric
instru-
ments and measuring procedures, and interpret the obtained
data.
In 1953, the authors working at the Laborutoriya
Radioaktivnykh
Metodov Issledovaniya Skvazhin (Laboratory of Radioactive Oil
Well
Logging) of the Moscow Petroleum Institute were the first to
solve
one of the most important problems, i.e., the use of
radioactive
methods to determine the location of oilfield water in eased
wells.
The authops developed the radioactive isotope method and the
special modifications of neutron methods for well surveying
which
have been used extensively by industry since 1954 in the
explora-
tion of petroleum resources. A method using sodium activation
to
establish the location of oilfield water was developed in
1954 at
the Petroleum Institute of the USSR Academy of Sciences.
N.M. Blinov wrote chapter I; V.N. Dakhnov, the introduction
and
chapters II, V, and VII; A.I. Kholin, chapter III; O.M.
Arutinov,
O.A. Barsukov, Ya. Ya. Gorskiy, and V.V. Larionov, chapter IV;
V.V. Larionov and A.I. Kholin, chapter VI; Yu.A. Gulin and
I.I. Felldman, chapter VII; O.A. Barsukov and K.A. Barsukov,
chapter VIII; O.A. Barsukov, chapter IX; O.A. Barsukov and
A.I. Kholin, chapter X; and S.F. Wbornykh, chapter XI. There
are
66 references scattered through the book, 37 of which are
Soviet,
and the rest English. The book contains 21 tables and 146
drawings.
Card 2/10

Radioactive Methods for Exploring (Cont.) 749
TABLE OF CONTENTS:
Introduction
3
Ch. I. Physical Principles of Well Radiometry 10
1. Radioactivity and the law of radioactive decay 10
2. Radioactive radiation and their characteristics 18
3. Brief data on the structure of the atomic nucleus 22
4. Artificial transformation of elements and nuclear
reactions 23
5. Neutron sources 27
6. Interaction of particles with matter 30
Ch. II. Radioactive Characteristics of Rocks 47
7. Natural radioactivity 47
8. Neutron characteristics of rocks 59
9. Induced radioactivity of rocks 66
Card 3/10

Radioactive Methods for Exploring (Cont.) 749
Ch. III. Methods of.Well Radiometry

69
10.
General data and
classification
of methods of well

radiometry

69
11.
Method of
natural radioactivity
of rocks
71
12.
Method of tagged atoms
(isotope
method)
73
13-
Method of scattered gamma radiation

78
14.
Neutron-neutron method (method of neutron density)

15.
Neutron-gamma method

16.
Method of induced activity

83
17.
Spectrometry of gamma radiation
in wells
85
Ch. IV. Radiometric Instruments 88
18. General data and specifications to be met by radio-
metric instruments 88
19. Gamma-ray indicators 89
20. First radiometric well instrument 95
21. MNI one-channel instruments for operation on a
triple-core cable 96
22. Two-channel instruments (1955 NGGK-55 model) for
operation on a single-core cable 100
23. Auxiliary instruments and equipment for radiometric
surveys ill
Card 4/10

Radioactive Methods for Exploring (Cont.) 749
24. Testing instruments for the absence of the interrelation
of channels and for linearity ill
25. Procedure of measurements In wells 113
26. Selection of conditions of measurement 115
27. Quality control of measurement 119
28. New models of radiometric instruments 120
Ch. V. Theoretical Principles of the Gamma method of Well
Surveying 137
Ch. VI. Interpretation of Results of Measurements by the Natural
Radioactivity Method 151
29. Calculation of fluctuation distortions 151
30. Distortions of gamma-method diagrams connected with
measurement procedures and operation of the instruments 156
31. Adapting gamma-method readings to uniform well conditions 158
32. Establishing the boundaries and determining the thick-
ness of layers according to intensity curves of natural
gamma radiation 16q
Card 5A0

Radioactive Methods for Exploring (Cont.) 749
33. Evaluation of relative intensity of gamma radiation 172
34. Qualitative evaluation of radioactivity of minerals 176
35. Correlation of well profiles according to intensity
curves of natural gamma radiation 177
36. Lithological disintegration of well profiles 180
37- Use of gamma-method data in studying collector
characteristics of rocks 183
Ch. VIII. Intepretation of Diagrams of the Scattered Gamma-

radiation Method
183
38.
Principles of the theory of the
scattered gamma-

radiation method
183
39.
Elimination of the
influence of changes in the density

of the drilling solution
191
40.
Evaluation of the density of rocks
193
41.
Evaluation of the
porosity of rocks
195
42.
Making more precise the lithological,
characteristics

of the well profile
196
43.
Depth of prospecting
method of scattered gamma radiation

.
and the collar influence
199
44.
Height determination of cement elevation
200
Card 611 o

'Radioactive Methods for Exploring (Conte) 749
Ch. VIII. Principles of the Theory of Neutron-Neutron and Neutron-
Gamma Methods in Well Surveying 203
45. Distribution of neutrons emitted by the point source of
thermal neutrons In an infinite homogeneous medium 203
46. Distribution of thermal neutrons in rocks of varying
water content in the case of a fast neutron source 207
47. Distribution of neutron-gamma radiation in a homogeneous
medium 222
48. Distribution of neutrons in media of varying neutron
properties 225
Ch. IX. Interpretation of Diagrams of Neutoron-Neutron and
Neutron-Gamma Methods 239
49. Evaluation of diameter influence, types of well filling
and bracing 239
50. Determination of correction, taking into account the
indicator length 247
Card 7/10

Radioactive Methods for Exploring (Cont.) 749
51. Lithological breaking-up of rocks and the correlation
of well profiles according to neutron-surveying methods 250
52. Method of determining porosity 254
Ch. X.
Use of Neutron Methods for Breaking-Up Oil and Water

Saturation Collectors
26o
53.
Physical principles of breaking-up
oil-bearing and

water-bearing layers by neutron methodo
261
54.
Analytical evaluation of the difference in the intensity

of
neutron-gamma radiation in water- and :oil-bearing

layers
262
5~-
Measurement procedures
266
5 -
Interpretation of measurement
data
269
57.
Breaking-up of oil-and water saturation collectors
by

the spectrometric method
271
58.
Breaking-up of oil-and water
saturation collectors by

the neutron-neutron method
273
Card 8/1o

Radioactive Methods for Exploring (cont.) 749

Ch. XI*
Procedure and Diagram Interpretation by the Tagged Atom

Method
276
59-
Selection of radioactive Isotopes and technique
in

preparing activated liquid,
276
6o.
Some general directions
on conducting well surveys by

the tagged atom method
279
61.
Determination of absorptive layers and piping between

layers
in working and pressurized wells
283.
62.
Determination of
damaged spots in the column and zone

losses in clay solution
circulation in the drilled well
290
63.
Determination of the
height of cement elevation in back

of the column and of the
thickness of the cement ring
291
64.
Testing the hydraulic
break of the layers
295
65.
Making more precise the depths in
perforating the eased

columns
301
Card 9/1o

'Radioactive Methods for Exploring (cont.) 749
66. Basic trends in the future development of the isotope
method 302
Ch. XII. Use of Radioactive Methods in Exploring and Surveying
Other Natural Resources 304
AVAILABLE: Library of Congress
Card .10/10 IS/jmr
11-26-58

CHALOV, N.V.; LAPPO-DANILEVSICIY, Yu.K.; GORYAGHIKII, Ye.F.;
BLINOVA, N*N.;
ZHDANOVA,, L.A.
Chemicomechanical degradation of linters in the presence of
sulfuric acid. Sbor.trud.NIIGS 12:87-98 164.
(MIRA 18:3)

'6'Ll'vo VR At, - F.
USSR / Cultivated Plants. Fodders. m-4
Abs Jour#.-:Ref::ZhuT-B1q-;..,, No ,6.0 .1958, 25096
Author:
.. Kaplupqvskly, S,J.,j
Inst "Askaniya--N6Vd'1 ihstitute-i"of-Hybridization and
Acclimatization of Livestock
Title Experimental:,,ISowing.of Corn at the "Askaniya-Nova"
Institute.-
Orig Pub:. sb ~'~Kukur"u;zi -'. - V`:' 19 5 5, ~~g 'vyp 61 m., Sel
k,h-ogiz,
1956, lio-114
Abstract: The "Askaniya-Nova" Institute of Hybridization and
Acclimatization of Livestock conducted in 1955 a
series of experiments t.o study the agrotechny of
corn raising for green feed and grain. The highest
green stuff yield with two harvests came from square-
pocket planting (50 X 50) with 4 plants per bunch.
Good results were also shown by mixed sowings of
Card 1/2
89

NIWA, A.Ye.,, AVXRBM. T.D .;-~~ILP~.;'.:MATUSLiVjc% V.S.;
SHqHXIKUMVA, N.V.; HASHKIROVA, Te *- R.
Woodesing of waste thiosul-fate liquore produced in the removal
of hydrogen sulfide from gages. Koko i khim. no.12:40-4 160..
(MMA 13:12)
I-* trralfskiy Muchno-issledotatel'skiy khimichaskiy iustitut.(for
Bashkirova).
(sewage-jawif ication) (Sodium thiosulfate)

AVM:LBM,, T.D.; APAK.UOV, I.A.; MAXDUROVAI 0,V,; BAKINA., N.PoLBLDWA,
___Ior,; BURU, A.Ao; AVDEYEVA, love
Removal of sulfur from wastegases of copper and sulfur plants
by the method of afterburning. Xhim.prom. no-4:281-288 Ap 162.
OUR& 15:5)
1. Urallskly nauchno-issledovateltakiy Irbirnicheskiy institut i
MDdnMorskiy madno-sernyy kombinat.
(Gases-Purification) (Sulfur oxides)

MATUSEVICHP L.N.; BUNOVA, N.P.
Crystallization of salts from aqueous
temperatures. Zhur. priklo khim, 37
solutions at different
no. 4%71(~-716 Ap 164.
(MIRA 17:5)

MATUSEVII'~'By L.N.; BLINOVA, ILP,
1.3ohydric crystallization at the varIcnis
cooling rates of
solutions. Zhur. prik".. khim. 37
no.10:231CP-2311, 0 164.
(14TRA

Mn I BOd EMMIUMal SCV/5721
Vsesoy,u;zo,*a astrcmetricbeakaya Loafcrentsiya.
Trudy 14-y AstrcmetricheaRoy koaferantsil SSM, Klyev, 27-30 maim 1958
g.
tiran-sactions of the 14th Actrc-matrical Conference of the USMO~Neld
in Kiyov
27-30 May 1958) Mosemr, Izd-vo AN SZZSH, 1960. 440 2. Erratz clip
Inserted.
1000 copies printed.
Sp6nsoring Agency: Akmd=iya nauk B832. Glavnaya astronomichesWe.
dbeervutoriya
(Pu3l-ovo).
Resp. Ed,: 14. S. Zverev, Corresponding Me=bcr~ Academy of Sciences
USSR; Ed. of
Publishing House: 11. K. Zqrchik; Tech. Ed.: R. A. Zr-m=Weva.
PMOSE, The book is- Intended for antro:i6mors and astroybvoicists,
particulv.]~ly
those Interested in astrmotrical research.
CUTEME: This publication.precento the Transactionsiof the 14th
Astr=etrical
Conference of the USSR, hold in Kiyev 27-.7,0 May 1958. It includes
27-reports
and 55 scientific papers presented at the planary'mecting or the
Coarcrence
Ca=d

Transactions of the l4t~ Astrometrical (Cont.) BOOM
and &t the special sectional meetings. An,appendix contains t1he
resolutions
adopted by the Conference, the composition of the.committees) the
agenda, and
th,.~ list of ~axticij%ants at the Con2erence. A brief summary in
English Is
given at the end of each article. References-foUaw individual article3.
The Presidium of the Astrametrical Committee (Chairman M. S. Zverev),
vhich
supervised th: pre~aratlon of tbla publication, expresses thasiks to the
wnmbara of th secretariat. V. M. Vasillyev, 1. G. Kollchlaakiy, A. B.
One-
gina,, and Xh., 1. Pbtter.
TABLE OP CalTMMi
Pareword
Address by A. A. Mikhqlav,;CbeIrmau of the Astronomical Council ~r the
i Academy of Sciences USSR T
REPORMS OF THk ASM010MICAL CMarM AM SUBOMM-IMS
wowmai CO ASTRMUMCAL WMM PMMM By vmjous nqsTjTmaiS
Carl 2YL16

T--svsAticas of the 14th Ast-r=etrical (Cant.) OV/5721
Vasillyev V. Mep
k and Do Do Polo:hentsLy Application of Punch-
Oira 9&-~:hlues for Calculations Made W the Time Service at the
MsIn Astroncutleal ObBervatory .
Yealpovs, M. I., azd D. V. Zagrabia. Solution of the Pmblem of
('=,alling a Catalogue of Right Asceasioas of 358 Stars, Uoing
Zua:h-4sxd Machinea
Yeeiro-m, H. E. The Cs1culation of Memerides of Apparent Right
Ascenslzcs of stwo in the Time Service Progm
Khrashchev, L. 1. A Comps--ison of Rrrcra in Tine Determination
M&IO With Dirfermt Mtroamical InstrMents
i
328
332
335
337
leilfrIkP G.. P.J. AO At TO-3hilina, and No Be Blinova. One Caas of the
i 30
Deterzinstion of rom*ltuda
Aear."Iyevs, P. M. The Effeat of ifind on the Results of the Astro-
nomical Determination of TIms
345
cact t*::6

BLINOVA, N.V.; SOVZ, I.Ye.
investigation of the Pioht's three-mirror telescope. Sbor.st.LITHO
no.4701-97 -159. (MM 16: 10)

PETROV, N.Tu.; BLINOVA, N.Y.. red.; SHCHEDRIZIA. II.L., tekhn.red.
E ~Ietorical and legal sketch] Sovety narodnogo
khosiatetva; istoriko-pravovoi ocherk. Moskva, Gos. icd-vo iurid.
lit-ry. 1958. 83 P. (MIRA 12:1)
(Russia--Economic policy)
F

i
LAZARET, Boris Mikhaylovich; BLIkOVA
._ vw-~,-_,~z-~' _7d.1 BTKOVA, Vj., tekha,red,
[Anforcing the obserfance of prices and regulations in
Sovitit ,
commerce] KontroV sa sobliudenism teen i pravil
sovetzkol.
torgovli. Moskva, Gos.isd-vo iurid.lit-ryg 1959. 82 P.
- (MIRA 12:6)
(Retail trade) (Price regulation)

XOSLOVA, Tokaterina Iv.anovna; UKANSKITj Ya.l., dotsent,
otv,.red,;
BLIITOTAq I V. red.; LUMA, Tel** takhnorod,
[Soviet construction; textbook for a specialized course]
Sovetskoe stroitelletvo; uchebuos posoble po spatskurau.
Noskrat I~wwo vyssbego Vereduago spatelalinogo obrasovanlia
RSM* 1960, 150 pe* (vm A 14:12)
(Constructien Induetry)

KALININ~ G.S., dote.; GONCHAROV, A,F*j dotsvp otvq red*j. BLIIOVAj
N.V*.q
red.
[The Soviet state and law in the law in the period of the
consolidation of'Soviet rule# October 1917-Ju2y 19181 Sovet-
skoe gosudarstvo A pravo v period uprocheniia Sovetskoi vlastis,
oktiabrl 1917 - iiull 1916 gg,,-, lektsii dlia studentov VIUZI-
Moskvas Vses. iurld. zaochnyi in-t- 'No-l- 1960. 88 p.
(MIRA 15:1)
(Russia-m-Politiesand government)
(Russia-~-Revo'Lutionj, 1917-1921)

BMIOVA , N. Ye.
"The Carbon Dioxide and Oxygen Content of Venous Blood in Rickets
Cases,, 7op.
Ped. i Okhtan later. i Det., 16, No.6, 1948
Chair, Pediatric FacuIty and Chair Biochenistry, Leningrad
Pediatric I-led. 1nst.

C-4
Acid-Un brium In np* and losic ceollitim in
dMm. RVI-turavi.. ..d X-K-Bliocim (Unin.
"d redist. Inst.). 110prosy pedial. i OkArday Mattf-
140m i Defitto 18. No. 1, 9-14(IWO).-In septic cam tbt
lotal Illood Cos was 5 Vol. I- below SIMItal in most In.
ktancr-.4. Oxygrif
ctuilent w&4 thailufly Intel 7.2-7.3 vW. Irt, a I A UOMIAI
8.3%- vubstances are I ghtly
normal In Isnost MOVIC71.
toik mwnallcl= al."Ibac Plasma. Cs lly in twic
,'but individual vurlmlons are Veal Cl
rR*s in eryttat.
O.M.K.

~od and their reactions in toxk
and "P "m 1. Kattanskayn and N
Moved Pediat. lost.). V pf-Y pedgel-l.",
i Ddstw 18. No.
I y
.)m IS The level of Ilm enlymes and the
type of IvArtion it-
Opolibe it, 11miruirial, of I"ilk air
11111virm
III mpitc. mod toxic tutditims. III the
(1411irt, low levels
of lipase and valmlism we cluumcictibise,
with..
We cultance-nicut o( lipulysis an
irritation by ntilk ail-
tuinistrallo".. In toxic comitious it
higher vatalAw with
Icu 1(mvtbtg *( liliam is foundi &nil the
milk teactkm is
sTn"ally SICK. In chlittren With
"ItT11411"l. 4.0114filiatir,
lipaw MR) ard law an IOW, VAIAIAW ill
FUSISCr high, 41111
the "Alk trat.2% is T"We, G. M. KiW4,411oft

WIULINA, S.K.; ANANIIKA, N.V.,;.BL
Dynamics of some'bio6hemical indiesoja-children-during an
interparoxyamal period of theumatle ftver. Vopokh.mat. i
dot. 8 no.2t22-27 F163. (IEEPk 16#7)
1. Iz kafedry fakulltetskoy pediatril, (zav.- '4aystvitellnyy
chlen OW SSSR.,zasluzhannyy dayatell nauki prof. M.Maslov
Edeceasedl Leniviradekogo pediatrichookogo maditainskogo in-
stituta.
(RHEUMATIC FEM) (BLOOD-ANALYSES AND GHEMTRY)

SAPIR) A.D.: BIRYUKOV, N~D.; HATAL-NIKOV) S.G.; MOLOVA, Z.M.;-
NkINA, V.R.; SHUVANOVA, N.V.; KRASIMNINNIM)VA, Ye.F.;
Exchange of experience* Zav.lab. 28 no.6:670-671 162.
OMIRA 15:5)
1. Chelyabinskiy metalltrgicheskiy zavod (for Sapir).
2. Institut neorganicheskoy khimii Sibirskogo otdeleniya
AN SSSR (for Biryukor). 3. Moskovskiy khimiko--tokhno.-
logiohe,skiy institut imond Merdeleyeva (for Katallni-kovy
Frolova).
(Chemistxy, Analytical)

'MoA., red.; B.MOV4jS.Yai., red*; KRASNCV, A.I., takhn.red.
[Problam~ in the.economice.of the agriculture of the.Chuvash
A.S S.R.; a collection of artiolemil-Voprosy a.konomiki
sel'skogo
khoilaistva.0huvashokol-ASSR,; oborhik statei. Pod red. K.A.
Andreevs, Chebokeary, 0huvashakoe gos.isd-vo, 1957. 242 pi
(MM 12:6)
1,Chabokeary Chuvashakiy nauchno-issledovatel'ski'y
institut 'literatury. istorii i skonomiki.
(Cbuvashia--i~riculture-Jeonomic aspects)
SON

T.
The use of comparisons in a 5th class program. Geog. v shkole no.2:36-39
Mr-AP '53. (MLRA 6;5)
(Geography-Study and teaching)
q4II I
j1,~Lu II i I I I 11 LT -LIIJI UI

8LINOVA~ T. A.
BLINOVAJ T. A. -- "Effects of Low Concentrations of
Benzenej Styrene, and
Alpha-Methyl Strene on the Blood Under Chronic Experim-
ental Conditions." 4Dissertations For Degrees In Science
and Engineering Defended at USSR Higher Educational
Institutions)(29) Min Public Health RSFSR, Lenengrad
Sanitary-Hygienic Inst, Leningrad, 1955
SO: Knizhnaya Letopis' No 29, 16 July 1955
For the Degree of Candidate in Medical Sciences

BLINOVA V.~416PLOTHIKOWA. N.V.; VOLROV, N.M.; SYSOYNTA, A.V.; AVDRYEV,
P.P.:
W N. Kh.A.; RODIRA. ?.M.; GUSLTA. L.L.; KAMENSUY. V.1., red.;
BYKOV. A.M., tekha.red.
(Economy of Tambov Province; a statistical manual] Narodnoe khoziai-
stvo Tambovskoi oblaBti; stati ticheskii sbornik. [Tambov] 12d-vo
"Tambovelmia pravda.0 1957. 1; pe (MIRA 11:3)
1. Tabmovskaya oblast'. Statistichaskoye upravlenlye. 2. Statisti-
cheekoye upravlonlye Tambovskoy oblasti (for all except Kamenskiy,
Bykov). 3, Nachallnik Statisticheakogo upravleniya (for lamenakiy)
(Tambov Province--Statistics)

/7)
137-1958-3-4882
1~ranslation from: Referativnyy zhurnal, Metallurgiya, 1q58,
Nr 3, p 61 (USSR)
AUTHORS: Lidov, V. P., Blinova, V. A.
TITLE: Experience in Smelting Lead-copper Matte With Sodium
Sulfide
(Opyt plavki svintsovo-mednogo shteyna s sernistyrn natriyem)
PERIODICAL: Sb. nauchn. tr. Gos. n.-i. in-t tsvetn. met.,
1957, Nr 13,
pp 232-234
ABSTRACT:
Card 1/2
The shaft smelting of Pb-Cu matte was carried out under
industrial conditions. The matte was composed of 19.2 percent
Pb and 13.4 percent of Cu, with an addition of converter slag
(composed of 2.4 percent Pb, 1.3 percent Cu, 14 percent ZnO,
36.8 percent FeO, 28. 8 percent SiOZ , 10. 61 percent CaO, and
6.54 percent A1203), some industrial sodium sulfide (approxi-
mately 70 percent NaZS) , and some Fe- scrap; the charge
ingredients, namely: the matte, the converter slag, the sodium
sulfide, and the Fe scrap, constituted, respectively, 57
percent,
35.3 percent, 6.2 percent, and 1.5 percent of the charge. In
com-
parison with the smelting of an analogous charge, but without
the
addition of Na?S, the weight relationship Cu:Pb in the matte
ob-
tained increased from 1.9 - 2.6 to 3.8 (5.4 percent of Pb
instead

8
137-1958-3-4882
.Fxperience in Smelting Lead-copper Matte With Sodium Sulfide
of 10.4 - 14.4 percent) ; Pb content in the waste slag was
reduced
from 0.9 - 1.7 to 0.7 percent. Cu content in the matte
diminished
from approximately 27 percent to 20.7 percent.
Ye. Z.
Card Z/2

ZHILIMKIY, Ye.S., zasluzhennyy vrach RSFSR; EYDELISHTEYN, S.I.,, kand.
med.nauk; Prininali uchastiye: AGRONIK, S.Ye., vrach- BLINOVA
V A. vrach; GOSPODIROVA, N.Y.., vracb; MARAIKINA,, V.N., vrach;
-iiWhYEVAP X.I., vrach,
.0
Importance of nicrobi ogical analysis in the treatment O:r,;-)
otorhinolaryngologica diseases with antibiotic aerosolS4
Sbor.nauch.-prak.rab.Poliklin.in.F.E.Dserzh. no.23152-162 161
(MIRA 3.68Z
(OTORHINOIARYNGOLOGY) (ANTIBIOTICS) (AEROSOL THMAPr)

m
BLINOVA-,-V.A.; ZHILINSKIY, Ye.S. [deceased]
Prevention of side reactions in antibiotic therapy. Antibiotiki
9 no.7:667-669 Jl 164. (MIRA 18:3)
1. Poliklinika imeni Dzerzhinskogo (glavnyy vrach I.G.
Karakozov),
Moskva.

BLINOVA, V.L.; XRAVTSOVAs, V.I.
.Drainage map in the glacier atlas of Moimt Elbrus. Inform.abor.
0 rab.Geog-ofak.Mosk.goa.un.po Me2hdunar. geofiz.godu noM93-iO2
162o (KMA 16 z 2)
(Elbrus, Mount-Glaciero)
(Elbrus, Mount-Drainage-Hapo)

BUNOVA., V.L.
Studying the discharge of-the Gara-Bashi River using the
4drochemica method,, Informsebor.o
rab.Geog.Fak.Molk*gopeun~
po MeWunarigeofizigodu no.9tlO3-n6 162. (KMA 16$2)
Gara-BELshi. River-Runoff)

3LI!n!t,.Y.U.p,I~IHIDOV, A.A*; IOLIN. Ys.S.-. MAKUSHKIN, Ya.G.:
MYZIN. L.M.-,
PHIWAKOV, H.P.; POMILIO, A.I.; BOROVIX, Z.G.; YBYREMOV, I.A.;
KOPAYGCRODSKIY. A.Be; HARIWOVI A.M.; NWOROSHKOVA, 0.1.;
POKROVSKIY,
A.F.; ROIIANOVSKIY, A.A.; RASSADNIKOV, Ye.l., red.; SAVELIYXV,
V.Io,
red.; FRIDKIN, A.Mo, tekhn.redi
[Electric power in the Uxale during the pact 40 years] Inergetilm
Urela za 40 let- Moskva, Goa, energ, ixd-vo, 1958. 141 p.
(KIRk 11:5)
(Ural mountain region-Electric power)

BLIHDVI V.N. inzh.; WZILISKIT. V.B., insh.
Gas relay protection of transformers in pover system. Blek.sta. 29
no.6:87 Je 158. (MIIU 11:9)
(Blectrio transformers) (Bleatric relays)

BLINOVA, VeNe.inzh.-. KOZNLISZIY, V.Be.inshe
Automatic unloading of electric power lines In Ural power
eystems, Blekatae' 29 noo'11:51-34 N 158*' (MM n: 12)
- (Ural Nomtain region-31ectric power distribution)

BLINOVA, Ye.I.
Materials on the distribution of bottom vegetation in the.region
of the White Sea Biological-Station of the Moscow State Univer-
sity.. Trudy Belomorobiol.sta.MU lt22-34 162. (MML 16tl)
1. Kafedra nlzshikh rasteniy Moskovskogo gosudarstvennogo
universiteta.
(white Se"lgae) (White Sea-Benthos)

XMOVAp le,I,, (Murmansk)
Wgraso i~ the Barent a Sea* Pri-roft 51 no*12:105 V 162,
(MIM 3.5112)
(BiLrento Sea.Eel*pzt)

BLI140VAl Ye. I.
Distribution-and quantitative indices of commercial algae
of the Murmansk sublittoral (Barents Sea). Rast. res. I
no. 4083-w590 1,65 (MIRA- 19 %1)
1. Vsesoyuznyy nauabno-issladovatellskiy institut morskolp
rybnogo khozyaystva, i okeanografii, Moskva. Submittect
July 20,
1965.

Vertical distribution and quantitative evaluation of
macrophytes
of Aynovy Islands (the Barents Sea). Trudy K4BI no-8:41-55
165.
Epiphytes of Laminaria of the Murmansk Coast of the Barents
Sea.
lbid.:56-62, (H= 19: 1)
1. Vsesoyuznyy nauchno-issledovateliskiy institut morskogo
rybnogo
khozyaystva i okeanografiio laboratoriya kormovoy bazy.

KOZHINI L.I.,, prof.~ glav. red.; ABAKLJMOV, V.A.,
zam. glav.
red.; BLIYOVA, Ye.N. red.; BYROV,, V.P., red.;
S.G., red.;
POWLYAK~ S.I., red.,- VELICHKO, Ye.bt., red.
(Papers of young scholars] Trudy molodykh uchenykh.
I-loskva2 Pishchevaia promyshlennost', 1964. 261 p.
1. Moscow. Vsesoyuznyy nauchno-issledovatellskiy
institut
morskogo rybnogo khozyaystva i okeanografii.
Vsesoyuznyy
nauchno-issladovatellskiy institut morskogo rybnogo
kho-
zyaystva i okeanografii,, Moskva (for Abakurpov,
Blinova,
Bykov).

BIZENOVA., Ye. N.
*A'Hydrod~na~cal Thebx7,of Pressure an'd-Temperature Waves and of
Centers of
Atmosphere Action," Dokl,,-AN S=p 39,, Noe7s 1943
Chief$ Geophysics ObservatAry

'zp

77'
AL
c7i,
4t

lution 0i the n=-hut;~f
f otlans on
-fir

ZI A10 Vl~r
'3(7)
N,
PHASE I BOOK EXPLOITATION SOV/1837
Akademlya nauk SSSR. Institut fiziki atmosfery
Raboty po dinamicheskoy m~teorologii (Works on Dynamic
Meteorology)
Moscow, Izd-vo AN SSSRs-1958. 186 p. (Series: Its% Trudy, vyp. 2)
1,500 copies printed.
Resp. Ed.: I.A. Kibell, Corresponding Member, USSR Academy of
Sciences; Ed. of Publishing House: K.P. durov.
PURPOSE: The istue of the Instituten'Trudy[Transactions) is
intended for scientists and research workers engaged in weather
forecasting and climatology.
COVERAGE: This collection of articles represents the results of
12 studies in dynamic meteorology, carried out from 1951
through 1954. They treat weather forecasting techniques using
the methods of dynamic meteorology as well as general
theoretical questions in the study of climate. All authors,
Card l/ 4

Works on Dynamic Meteorology SOV/1837
except N.I. Buleyev and A.D. Christyakov, are associated with
the Geofizlcheakly Institut (Geophysical Institute of the
Academy of Sciences). A.D. Christyakov and N.I. Buleyev are'
associated with the TsentralInyy Institut prognozov (Central
Institute of Forecasts), OUGMS. References accompany each
article.
TABLE OF CONTENTS:
Foreword
3
_Djinov;a,_Y&j. The Theory of the Annual Rate of Non-zonal
Circulation of the Earth's Atmosphere 5
Obukhov, A.M., and A.S. Chaplygina. Change In the Barle
Yield in the Middle Troposphere 23
Monin, A.S. Transformations of Energy in the Zonal Circu- -
lation ofthe Atmosphere, 50
Card 2/4

Works on Dynamic Meteorology SOV/1837
_jj1jngx&,_Y&,N. The Effect.of Non-linear-Terms in the Equations
of Thermohydrodynamics When Solving a Problem Dealing With
the Long-range Forecast of Meteorologic Elements 54
Buleyev, N.I... and G.I. Marchuk. The Dynamics of the Large-
scale Atmospheric Processes 66
Blinova, Ye.N.J. and G.I. Marchuk. The,Theory of the Annual
It-at-e--of-R-111urely zonal circulation 105
Marchuk, G.I. The Annual Rate of the Circulation Index 114
Marchuk, G.I. The Large-scale Thermohydrodynamic Processes
in the Baroclifiic Atmosphere . 119
Marchuk, G.I., and N.M. Kireyeva. The Problem of Expansion
By Small Parameter of the Solutions of Equation Systems
in Hydrothermodynamics.as Related to Atmospheric Processes 142
Card 3/4

Works.on Dynamic Meteorology SOV/1837
Christyakov, A.D. Forecasting Temperature and Wind in the
Upp6r Troposphere and the Lower Stratosphere 16o
Kogan, S.Ya. The Short-range Forecast of Pressure Field in
the Central Troposphere.With the Aid of the Linear
Fridman's Equation 167
Kogan, S.Ya. The Solution of a Non-linear Problem Related
to the Short-range Forecast of Pressure Field - 177
AVAILABLE: Library of Congress
MM/Jmr
6-15-59
Card 4/4

UTI~ 0 R S Bli nova, Ye. N. , Corresponding Member AS USSR SOV/2o-1
2o-2-15/63
Be ouso;~,.. Z.
T I T Non-Lineur Nor.-Steady Problem of the Determination of the
Planetary
Flow Pattern at t'-u Midlevel of the AtiTion-nhare (NelineyrLaya
nestat-
sionv_rnaya zadacha opr(-deleniya poley davltiriya planetarnogo
aiasshtaba ne- srednem urovne atmosfary)
P _--~ R I C, D 1 C17.1: Dokiady Ak~idemii naulk 0121>R, 1958, Vol.
120, Nr 2,
pp. 281 - 284
ABST' CT- In 194*3 one of the authors ol~' this -oauer recommended a
hve.:~o-
dynamic method for the lone-term forecLt~;t of pressure fields and
t'. e f ow lines ijt atmospheric midleve' . An equation 'or the
vortex (a simplified e6t.111tion by A.A.Fri&man) and one of the
'Ailer .(.!,'yler) equations' were used for solvinE this problem.
This.
P-im was achieved by a linearization of the equations with resgect.
to west-east tr--nst'er. The solution of the non-linear nrobl ~m
of loni;-terrn weati.erforecast by the methods of hydrodynazie -s was
facilltated by electronic computers. The most oirriple solution
is obtained for the midlevel ~f'tha atTosnhere. Some variants of
Card 1/3 such a solution sui.-.-ested in-1954. 1~ this PaDer the
methods

Non-Linear Non-S,:ee_dy Problem of IthG Deterirdnation of the
SIGjV/2o-12o-2-15/63
Flanethry Flow Pattern at the Midleval of the Attriosp .nore
and some-resuits of the application of one of these vari-n.t.s
are d4scussed. The equation for the floxy function can be used
as th; initial equftion, as was done p*reviously:
+ (f,A41)+2 LJ 0, where a and&ddenote
,at a 2sin ak 0
the rad.iv,.s and the anCular velocity respectively of the earth.
.Further, the equation
2 /2
1 - COSY 2 a -- -1
at 2 0 0 ln 1 _ cos. DY, AV)+2c4a 0sin a'
Ans.0
'holds.
:dg'dA
Let the function lp be known. The forecast of the values of %v
can be achieved by means of time steps in the computation.
CowDutation is discussed in short. The authors also make a few
suggestions for the performance of this computation by means of
Card 2/3 electronic computers. The problem under discussion was
carried

Von~-Linear Non-Steady Problem of the Determination of
BOV/20-12o-2-15/63
~l anetary Flow Pattern at the Midlevel of the Atmosphere
out with the BECM (Bollshaya elektronnaya schetnaya mashins: All,
SSSR)(great.electronic computer of the AS USSR). Examples con-'
cerning the forecast of the absolute topography of the 700 millibar
siirface covering periods of up to 10 days are computed. One of
these examples is illustrated by three-figures. There are 3
figures and Soviet refirences.
ASSCCIATION:Tsentral1nyy institut prognozov (Central Institute of
Weather
Forecast)
-SUBMITTED: February 14, 1958
1. Planetary-atmospheres-Theory 2. Weather forecasting
3. Mathematics--Applieations
C;Lrd 3/3

AUTHOR:
Blinoj!~~. Corresponding S011/20-123-3-46/54

Academy of
Sciences, USSR
TITLE:
On the Problem of the Forecasting of the Smoothed
Values of the

Meteorological Elements at the Mean Level.of.the
Atmosphere

(K voprosu o prognoze sglazhennykh
znacheniymeteorologicheskikh

elementov na srednem urovne atmosfery)
PERIODICAL:
Doklady Akademii nauk SSSR, 195Bt Vol 123, Nr 3, pp 440-442

(USSR)
ABSTRACT:
The field of the current function Y on the mean level
of the

atmosphere may be calculated by means of the transport equjation

of thp absolute curl

+ 2 CJ 0
(

w aA -a e
t a21 sine

0

a
denotes the radius of the Earth; c4 -the angular velocity of

,
0
the Earth's revolutionj th*e complement of'the latitude;

;k- the
longitude (which increases from West to East) of the

place; t the time.
Moreover it holds that

Card 0
(sin 2

~
)

sin 6)
14
2
sin

On tfie Problem of the Forecasting of the Smoothed SOV/20-123-3-i6/54
Values of the Meteorological Elements at the Mean Level of the
Atmosphere
The motion on the mean level of the atmosphere is assumed to be
turbulent and the author endeavors to find a summarizing
statistical description of this motion by means of the first
equation. This investigation is carried out according to a
method developed by L. V. Keller (Ref 1). The first equation
contains only one function y (e,Alt) and the author seeks the
smoothed values rr (6p;jjt) of this function. The deviations from
the smoothed values are denoted by y' (0,A,t) so that
TIMIAlt) 7 T(()I;k,t) Smoothing is then applied
to the firs equation. The equation deduced in this way (besides
the sought function contains the 2 smoothed quantities
'a w which may be expressed by the
C)
moments of correlation (moment avyazi). Calculations are
discussed step by step and the final expression is given
explicitly. Smoothing may be carried out by various methods.
Card 2/3

.On the Problem of the Forecasting.of the Smoothed
SOV/20-123-3-16/54
Valuetwof the Moteorologieal,Elements at the Mean Level of the
Atmosphere
If it is carried out by averaging over a circle of latitude,
a system of equations is obtained the solution of which can
immediately give the forecast of the circulation index.
There is I Soviet reference.
ASSOCIATION: Institut prikladnoy geofiziki Akademii nauk SSSR
(Institute of Applied Geophysics of the Academy of Sciences, USSR)
SUBMITTED: August 6, 1958
Card 3/3

-3
AUTHOR:
TITLE:
PERIODICAL-
28413
S/169/61/ooo/Oo7/o73/1o4
Aoo6/Aic)i
Blinova, Ye.N.
On the theory of a long-range waather forecast by taking into
accomt
vertical velocities and fluctuations of the tropopause level
Referativnyy zhurnal. Geofizika, no. 7, 1961, 69-70, abstract 7B431
(V sb. "Vopr. dinamich. meteorol.", Moscow, AN SSSR, 1960, 12_2D)
TEXT: The present study solves the problem of a long-range
pressure and
temperature forecast with the attempt of taking into account the
effect of verti-
cal velocities and fluctuations of the.tropopause level. Initial
values are:
the equation of the tropopause and conditions on it in spherical
coordinates,
written down for the tropopause altitude g OR ~Lq t). the equation
of continuity
in spheric coordinates integrated over.Z from 0:)to taking into
account
the condition on the tropopause the equations of motion along axes
Q,?, and the
barometric formula. In the equations of motions those terms are
neglected which
contain the component of velocity along the radius. It is
considered that the
motion of the atmosphere consists of a purely zonal circulation
and its distur-
bances. The velocity of the basic motion is represented through
the angular ve-
Card 1/ 3

26413 S/169/61/00o/007/073/104
On the theory ... A006/A101
locity of air motion in respect to the earth. If the pressure on the
tropopause
is equal to zero, the barometric formula serves to obtain the value of
pressure
at a purely zonal circulation and deviation from pressure. The
equation of mo-
tion along axis 9 and the equation of pressure at a purely zonal
circulation pre-
determines the altitude of the tropopause. Linearization of the
conditibn on
the-tropopause and of the equation of motion yields a formula for
determining
the elements of disturbance of velocity and pressure components.
Instead of the
disturbances of components it-Is convenient to take their products by
the alti-
tude of the tropopause, which are then replaced by the derivatives,
with respect
to the axes, of some functions T and Three equations are obtained to
deter-
mine T, q/ and g '. To integrate the obtained system of equations, the
Haff
method is employed. The solution is sought for in the form of a
product of two
functions one of which depends only on the latitude, and the other one
on the
longitude and time. To determine the unknown functions a uniform
system of con-
ventional differential equations is obtained. If the solutions are
searched in
the form of series in associated Legendre polynomials, an infinite
system of al-
gebraile equations for 'm is obtained after eliminating the functions
~ m(e) and
Y m(B). Using the presence of a small parameter,in the system to be
solved, the
solution of equations may be represented by expansion in a series in
powers of
Card 2/ 3

On the theory ...
26413
8/169/61/000/007/0"/104
A006/AlO1
this parameter. Assuming the altitude of the tropopause over
the pole to the
equal to infinity, terms with small parameters vanish.
Representing the solu-
tion of the problem by series In spherical functions, the
value P is eliminated
and already solved equations of long-range weather forecast
are obtained. Taking
this solution as an initial one (as the first approximation)
the solution of the
actual problem is represented with an accuracy up to the
magnitude of first order
in respect to the small parameter. The final solution for
71, and is ob-
tained in the form of the sum of associated Legendre
polynomials with different
coefficients, determined from boundary and initial data. As
initial data the
author used the diEtribution of pressure for the northern
hemisphere at the ini-
tial moment-. When finding the distribution of vertical
vilooities,, the following
formula is taken as a basis:
z (vp sin Q + v
s -in 0 . 6 0 ?1
VQ and Vkare excluded by means of It and 99by the af re
entioned method. Using
the values found for F and tP an expression for vertical
velocities is obtained.
The formula obtained for the forecast of the field of
vertical velocities is si-
milar to formulae for pressure forecast. N. Chuzavkova
[Abstracter's note: Complete translation]
Card

BLINOVA, Ye.N.
Hydrodynamicall investigation of nonstationary atm:)spheric processes
on a planetary scale. Dokl. A14 S-SSR 140 no.2:354-357 S '61.
MRA 14:9)
1. Ob"yed3nennyy meteorologicheskiy vychislitel'nyy tsentr AN SSSR
i Gidrometeorologich6skoy sluzhby SSSR. Chlen-korrespondent AN SSSR-
(Geopbysics) (Atmospbere)

LMMOVAp Yee N.
Three-dimensional problem eond#rnixg the forecasting Of
flaUsned values of meteorological elements,, Dokl-i AN SSSR
ul *no.6-.13554359 D 162, (KM 16:1)
I* VychislitellmV meteorologioheskiy teentr. Chlen-korrespondent
AN SM.
(Weather forecasting)

ACCLSSION;NR: AP4014029 S/0049/64/000/001/03.10/0323
AUTHOR3 Blinova,, Ye.,N
T.ITLE.- The'status and immediate objective of the hydrodynamic theory
of climate
:and of long range weather prediction Cpresentod at the Symposium on
Numerical
Methods of.1deather Prediotion,, Hoscow., 24 Juno. 19627
-110-123
SOURCE: AN SSSR. Izv. Seriya geofizicheskaya,, no, 1., 1964,,
-TOPIC TAGS: hydrodynamic theory,, hydrodynamic climate theoryj,
weather predictionp
,.Weather forecasting, long-range weather prediction., long-range
foreeastings
boundary value problem, thermodynamics
.ABVLRA.CT: The author gives a brief survey of modern hydrodynamical
methods of
short- and long-range forecasting. Basic -trends in developing a
theory of climate
arA of long-range forecasting are discussed. ~Previous works on the
hydrodynamical
theory of cl~maie have developed a theory that permits one,, for a
given config-
uration of,continents and oceans and for a given influx of solar
heat,, to deter-
minethe basic features of climatio distribution of tomparatme,
pressure, and wind,-
(in which th4fe is a yearly period) by'solving the boundary value
problem of
"Cbrd 1/2

ACCESSION NR: AA014029
thermodynamics, This theory may now be refined and, at the same
time,, generalized
for the problem of long-range weather forecasting in which processes
with a yearly
period are not'distinguished but,are examined 'together with
nonperiodic processes
(depending on initial data). Beg:~=ing with velocity functions that
neglect
previous quasigeostrophic or quasisolenoidal movements) the author
derives expres- I
sions for the various parameters required in my adequate climatic
theory to
permit lor4,'-range forecasting, Work of this kind should mpke it
possible not only
.to extend the forecasting interval and to improve the quality of the
predictions,,
but it z4ould aid in solving the basic questions on hydrodynamics and
thermody---l
namics of atmospheric movements on a planetary scale. Ands in
particular, it
should aid in solving problem associated with the goal of controlling
climate,
Orig. art, has:! 23 for=aas.
USSOCIATION: Vy*chislitellnM motoorologichoskiy tsentr (Meorological
Computing~,
,Center)
iSUBIMTEDi 19Jul63 DATE AGQ: 14Feb64
ENCLs 00 1
NO Ra Spv: o:L6 -OTHER: 00
SUB CODE: AS
Card 2/2

BLISM O.N.
DetermiTting the initial wind and prossure fields from the distribation
of temperatures and the vertical motions of air, Dokl. AN WSR 149
"11064024-826 -ApI (MMA 160)
1, Vyohislitellnyy meteorologicheakiy teentr, Chlen-korrespondent
AN SSSR.
(Atmospheric pressure) (Vends)

BLINOVAj_ Yq.N., otv.red.; NIKOIAYEVA, L.X., red.izd-vaj VOLKOVAj
tekbn. red.; HAKUNI, Ye,V., takhn. red.
[Hydrodynamic long-range weather forecasting) Gidrodinami-
cheskii dolgosrochrqi prognoz pogody. Moskva, Izd-vo
"Nauka," 1964. 105 p. (MIRA 17-.2)
1. Akademiya nauk SSSR., Ob"yedinenzWy moteorologichaskiy
vychislitel'My tsentr. 2. Chlen-korrespondent AN SSSR (for
Blinova).

Ail
4CIMSSION -MR: AT4034671 S/000of"1000/0000005/0018
..AUTHOR: 81 inova. Ye. N.
'~:!-TJTLE: The hydrodynamic theory of climate and long-range weather
forecasting
~SOURCE:. -AN SSSR. Ob"yedinenny*y meteorologicheskly vy*chIsIIteI'ny*y
tsentre
amic ldhg-range weather'
.7'Gidrod.inamicheskly dolgosrochny*y prognoz pogod)* (Hydrodyn
forecasting). Moscow, Izd-vo' "Hauke," 1964, 5-18
TOPIC TAGS: meteorology, weather forecasting. long-range weather
forecasting$
climate, climatology, climate theory-
ABSTPACT: In earlier studies (Ookl.,AN SSSRO 140, No. 2, 1961; Ookl. AN
SSSR, 140,
No* 3. 1961) the author reduced-the problem of long-range forecasting
of meteoro-
.1''logical elements to the solution of a system of differential
equations describing
not only aperiodic.processes, but also processes possessing an annual
period (cII_
matic processes). On the basis of this Initial work the author now has
proposed a
specific scheme for solution of the derived system of differential
equations. The
paper begins with a general consideration of the problem., followed by
a detailed
solution of the equations and selection of numerical values of the
parameters In
the problem. The forecasting problem Is solvedlin time steps. All
equations In
Ithe problem are written so that an implicit system Is obtained
relative to th
.2

BLINOVA, Ye,N,
State and prospects of the development of the hydrodynamic
theory.
of climate and long-range weather forecasting. Trudy MMTs
no.2:
3- 20 164 (Mila 1881.)

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