SCIENTIFIC ABSTRACT L.V. DMITRIYENKO - A.A. DMITRIYEV

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000410510017-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

~S)/081/60/000/021/009/018
A005/AO01
The Activity and Structure of Iron Catalysts of the Ammonia Synthesis With Three
.and Four Activators
the specific activity of the iron catalyst but lead to a decrease in surface while
the amphoteric and weak acid refractory oxides decrease the specific activity but
increase the surface.
From the summary of the authors
Translator's note: This is the full translation of the original Russian abstract.
Card 2/2

SAMSONOV, G.V., DH jTM[LQJ,-Wv-*1-BIROTA. A.G. p SHESTERIKOVA, M.P.,
UVRENTIUVA, S.F.
Ph.valoochemical properties of albomycin [with Bummnry in English]
Biokhimiia 23 no.2:220-224 Mr-Ap '58 (MIRA 11:6)
1. Institut Vvsokomolekulyarnvkh soyedineniy AN SSSR i M:Limiko-
farmatsevtIcbeskiy Inatitut, Leningrad.
(AUTIBIOTICS,
albomycin, physicochem. properties (Rua))

YLAWLAUNIOVY I.; DMITRI)MNKO, M.
.
Every pilot should have perfect training. Grazhd. av. 21 no.9:12-14
S 164. (MA 17:10)
1. KomandirIbabarovskogo podrazdeMmiya reaktivnykh samoletov (for
Karamanov). 21. Zamestitell komandira po politicheskoy chasti Khab-axov-
skogo~podrazdbleniya reaktivnykh samoletov-(for Dmitriyenko).

GufGH31-1 1.0t. (Hurohii, 1.0.), doktor isotr.bAuk; MAKARENKO, L.L.; ZHUAVi0f, 91 *;
I DM-tTRIYENKO, M.F. [Driytriienko, 14..F.],, zhurnalist
-------------- -
History of names. Nauka i zhyttia 12 noi.1;17 Ja 163o (1-URA 1623)
1. Chlen-korrespondent AN Uler8SR (for Gurzhiy). 2. Direktor
Gooudarstveimyy istoricheskoy bibliotaki UkrS6R (Ior Makarenko).
3. Glavnyy bibliotekart Gosudarstvennoy igtoricheskoy biblioteki
UkrASR (for Zhevakhov).
. (Donets Basin-Names Jq Geographical)

GURZHIY, I. 0.[H=hii., 1. 0.1; MAKARMO ", L. L.; ZEEVAKHOV, P. %;
MaTRUMO, 14. F.[DjWtriienko, M. F.], zhurnalist
History of names. Nauka i zhyttia 12 no.2:33 F 163.
(MIM .16:4)
(Ukraine-Names, Geographical)

133-10-9/26
AUTHOR: Dmitriyenko, 14. G. and Sapko, A. I.
TITld],: Design Deficiences of Are Furnaces of the nCB Type.
(Konstraktivnye Nedostatki Dugovykh Pechey SeriiaCB)
PERIODICAL: Stall, 195?, No.10, pp. 902-904 (USSR).
ABSTRACT: The design of are furnaces of the ACB series (capacity
up to 30 tons), produced by "Ele kt rope ell" is outlined
and some of their design feature6 are criticised. It is
suggested that the segments and the roller tubes of
the furnace body rolling out device should be replaced
by a roll out trolley and to increase the design
reliability of all hydraulic drives. For large furnaces,
the use of swinging roofs is DrODOsed.
ASSOCIATION: Dneprospetsatal-" Works and Dnepropetrovsk Metal-
lurgical Institute. (Zavod Dneprospetsstall i
Dnepropetrovskiy MetallurgichesIdy Institut).
AVAILkBLE: Library of Congress
Cara 1/1

AUTHOR: Dmitriyenko, M.G.- Engineer 130-12-16/24
TITIE: Rapid Capital Repairs of Large-capacity Electric Furnaces
(Storostnyye kapitallnyye remonty elektropechey bol'shoy
yemkosti)
PERIODICAL: Metallurg, 195?, No.12, pp. 26 - 2? (USSR).
ABSTRACT: The relatively small capacity of charging-platform
cranes renders the removal of large electric furnaces during
rebuilding difficult. The method, described by the author,
was developed at the "Dneprospetmtall" Works and has reduced
idle time between the tapping of the cast heat to switching
on for the first of the new heats to 2.5 instead of the noizal
8 days. The method consists essentially in the wheeling of the
old furnace into the casting bay on a specially erected trestle
(Fig.3) for removal by the 125-ton a-anes available there, a
cross bar and braces being provided. A previously prepared new
shell with ra-mmed bottom is placed on the same trestle and
wheeled into position. There are 3 figures.
ASSOCIATION: "Dneprospetsstall" Works (Zavod "Dneprospetsstall")
AVAILABLB: Library of Uongress
uard 1/1

SOV/133-58-6-16/33
AUTHORS: I., Engineers
.,,,13apko, A
ITITLB: Mechaniqation of Labour-consuming Processes in the
Electric-amelting of Steel (Mlekhanizatsiya trudoyeir.-kikh
protsessov pri vplavke elektrostali)
PERIODICAL: Stall Nr 6 PP 525 - 529 (USSR).
t 1958'1~ 1
ABSTRACT: Mechanimation of the charging of slag-making materials,
fettling of electric furnaces and supply of oxygen into the
metal bath on the Dneprospetsstall Works is described. and
illustrated. It is pointed out that further work on improve-
ment of chargingand fettling machines for electric furnaces and
tuyere13 for blowing oxygen into the metal bath is necessary.
There ELre 4 figures.
ASSOCIATIONS: Zavod nDneprospetsstall" (Dneprospetsstall Works)
and Dnepropetrovskiy metallurgicheskiy institut
(Dnepropetrovsk Metallurgical Institute)
Card 1/1 1. Electric furnaces--Equipment 2. Electric furnaces--operation
3. Steel--Manufacture

DMITRIYENK0. M.G.- KUBIXOV, V.P.; ALEK8YUTOVICH,J.A.- WOLUYEV,
V.D,
"Im divided fastenings. Pat' i put.khoz. 4 no. 5:17-20
My 160. (MIRA 13:11)
1. Bachallnik distantaii puti, stantsiya Molodechno,
Belorusskoy dorcCl (for Dmitrlyenko). 2. Nachallnik distantaii
puti, stantsiya Dorogobuzb. lCalininskoy dorogi (for Kubikov).
3. Nitchallnik distantsit puti, staDteiya Moskva, Moskovskoy
dorogi (for Alekayutovich). 4. liachaltnik distantsiiv~uti,
stantsiya Ramenskoye. Moskovskoy dorogi (for Zaboluye
(241lr oads--Rai 19--lPa at e ni ng s)

TAYTS. Ye.M.. doktor tekh-a. nauk; ShIVARTS., S.A.p kand. tekhn.
naukjd--c.asedj.-, MIYSAKHZM !.B.p inzh.; GELIP-ER, M.L.,
inzh..-, DOJUM, G.A., inzh.-.
IZRAEi,lT, YeJI... :Lnzh.~ KULAKOV- N.K., inzh.,-. KUSMANSKIT,
B.,S., inzh.-~ MEYK30F, L.V.., inzh. [deceased]; LEONOV, A.S...
inzh..~, MARTS, G.A~p inzh.~ SHURMIAN, I.Ya.., inzho;
YATS610, N.Ya., -Lnzb.,!, BADIN, P.P.., inzh..,, KHANIN, I.M.,
doktor tekhn. naWc, prof., red.) KOZYREV, V.P., inzh.,
red., KUPEIIIAN, Pd,p inz~., redo LGALOV, K.I., inzh.,
red.; LEEYTES,, V.A,, Jnzh,, red,i iERNERP B.Z., inzb.,:red.3
POTAPOV., A.G., irizh.p red,r SHELKOV., A.K., red.
[By-product colce industry worker's handbook in six vo.-Lumes]
Spravc,chnik koksolchimika v shesti tomakh. Mosk-tra. Metal-
IiLrgiia. Vol-.2. 1,965. 288 p. (1-11RA 19:8)

DMITRIYANKO, R.K.
-
Buscalno's reaction in malaria. Izv. AN Kazakh.SSR. Ser.kraev.pat.
no#6:5-10 150. (XLRL 9:8)
MAIARIA) (URINE-ASALYSIS AND PATHOLWY)

I)KITRIYBM, N.K.; GROSUOU, I.M.
Achievements In tho control of pkraoitic diseaeou In Kazakhstan
during -the last ten years. Ned.paran.i paraz.bol. 26 no.6.-679-
684 H-11 157. (MIRA 13:4)
1. 1z Respablikanskoy sanitarno-opidemiologicheakov stanteii Mini-
sterstia zdravookhraneniya Kazakhokoy SSR.
(EL7 SM--PAUSITOLOGT)

ZHUMATON', Kh_'O.., prof.; DMITRIYENKO, N.K.
[Gharacteristics of the natural foci of tick-borne
encephalitis in Kazakhstan; report at a conference
devoted to diseases of tropical countries, September
1961, Tashkent] Osobennosti prirodnykh ochagov kleshche-
vogo entsefalita v Kazakhatane; doklad na konferentsii,
posviashchennoi bolezniam v stranakch s zharkim klimatom.,
sentiabr' 1961 g., Tashkent. Moskvap Medgiz, 1961. 7 p.
(MIRA 17:3)
1. Chlen-korrespondent AMN SSSR (for Zhumatov).

DMITRIYENKO, N.K.
Virological study of Ixodes ticks collected in the v*inity of
Alma-Ata. Vop.virus. 7 no.6&7A2 N-D 162. (KIRA 1634)
1. Kazakhakaya respublikanskays, sanit;arno-epidemiologicheskaya
stant-3iya'i Kazakhskiy institut. epidemiologii, mikrobiologii
i giglyeny. (ALMA-ATA REGION-TICKS)

POLTORAXj, 0. M.; BORONINI, V. S.; R!ITRTYENKOj_N. ~.
Zstimation of the number of active contere by processing the
experimental data by the mathod-of the theory of ensemblea.
Vast. Moak. un, Sisr. 2s Khin. 16 [i.a.171, no.6:39-40
N-D 162,, (MIRA 16:1)
1. Kafedra fiziobeBkoy kbizdi Hookovskogo universiteta.
(Catalysis)

, 1. .; I '! - . - * ~l- '.. I '*;. y-, .1 1 Ll, p - F I.F."O" 1 i:. ,
Alit . . ~ t I - . - - A, jo , ~ lo v , I i nzho
, -~- ~` ~ I a
- - . -a erlt~ll 'pe?. tiz)TI CT 1 i,
e Lr,.l HM-81 c:llLl.er-loalpr,,i In
z% t; t-:: -,~ Ba s i n rd t, e s . I - i
SbOl-- '64.
(MBRA 18:9)

4;; ;To ;-i-;-i i we
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no
'PAO d Swell be awm Is w wil. S.
ymmov md 0. 1. Dinitrievu.. FVA*v (U. a. & R.)
.0a
2k aom-i7qwa),.&,,p,, .1 a tff,,,m a cmg.
24.5. 14A &w 4.9 NiMkqWvs. of abumbod ham
Per 100 g- a' -0 -we tAw 14
uantiti
h
1
31
-00
ft to
ave
.
q
milliequivs. of b-. The see. quantities of bam in the 09
ChtMorm wtm obt&iftd by ; UNKOW the orilghlal "a. .
t9- 26.1 -RHeqWvp. of bam, with o.05 N C1
'
'
INNAing out the
f H go*
exom o
C4
with d1std. 11,0.
A
1
=60

00 OW111
011 ww ewried out with 3 sampla of pods
13.68.6.1a and 2.63xnjjjrqQj".,jbsorbW bgm 4W the

000 qt
lant" "Lh4l was "041 to 0-M witflemily. Them mails
ITI'm tm&ttd with a 0
(12
N HCJ
00 .
,
IsAa. and the raidual acid
wasdtfaw. It -found thatthonxifty of the baws

00- Y!t~ in the dWaftt SWIN. It Is pointed out awt the
.

0
0
- higher the
of abegrbed H the swow is the MbWty
of the =0=
J

1
0
-
0 ~ 01k
ower the qumnity o(absadwd
twws the glom Ult IF*fity'cg tht H ions. rft Rutbm
*
th
I

0
0
r a
n
be
thl-OWitY factor should
-
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i m. SL A WALLUECICAL LITINATWE CLA$$0KA11C"
IF
I, x
U It AT 43 1 (vttj# (Itit Sit RIX It IT
0 0 0 0 : 9 a * 0 0 0
a 0 0 0 0 a 0
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see
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to,, b3.01
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1

1. KAEGTN, V. A.; VASTLIYFV, P. S.;
DVI,ITRIE'7KO, 0. T.
2. USSR (600)
"The Adsorption of Silver Salts on Mixed Gels of Silicic Acid.and Sezquioxides,"
Zhur. Fiz. Khim. 13, No. 12, 1939. Moscow Physico-Chemical Inst. Imeni L. Ya.
Karpov, Div. of Colloidal Chemistry. Received 7 Feb. 1939.
9. IN Report U-1615, 3 Jan. 1952.

00
so
00 sit'
0,0
00
so
wAnd a"
14C Ir
(U. IL 0. R.) 10,
JW# AL SHY-Mal- 41611flitlam W ASNOs took
40 11111114d Pb d POA OW BIN, iia vm t.- by the
Fftkllt it bM OW SPAW CWVQ wag obWmwd In I lw .uic
1111mift of do rmpamilat with alliali in in the titmOm of
PWO vMw. 72w eamt of the abw
ptim depctds
00 -
al the admorbad m1t. Ilills was verified by the
"IM fthe that churgW Ow moll. Mol. admwplion
tabu *m in ad! Alars. to t1w Oubmw Imlsorpikiet, an
al I 1w Odkizilo"
0. Moose
A!.!.% L A MITAILLU"ICAL LITIOATMIC CLASUPICATM
-90
-90
0
Vo
Vo
lee
.1 No-
00 d~
asio
see
fte
ZOO
moo
age
lee
too 0
too
ll~-AIP - 00 It A son ON96*16 of I V at 0 At a 3 1 V
0 * 000 * 0 0 0 0 0

Country : USSR
Category: Soil Science. Physical and Chemical Properties of Soil.
Abs Jour: RZhBiol., No 18, 1958, N082083
i
cornice has a dish'eter 6~ 4 cc. Then comes the thin-
walled part-,of the tube* with the thicImess of the
glass wall 0-2 0-3 mm, the diameter 5 MM, and the
length 35 mm. After that a smooth, tapered part
continues into a thick, glassed receptable 10 mm
high qnd with a diameter of 9 and 5 mm. The length
of the rece-.3tacle is 90 mm, the diameter 9 mm. The
receptacle is -nserted into a glass tube with a
diameter of 5-6 mm with a fused platinum contact.
The tube is filled up with chemically pure mercury.
Before it is used, the working part of the electrode
is made fat-frec with carbon tricbloride and washed
with a chromium mixture. The receptacle is filled
Card 2/3

DMITRENK09 0. 1.9 000 CHEM SC19 "MOLECULAR ABSORPTION
OF ELECTROLYTE$ AND WATER BY COLLOIDALLY DISPERSED DEPO-
SITION3 AND ZWK CONTROL OF THE COMPOSITION OF INTERMICELLAR
SOLUTIONS CONDITIONED BY IT, PART 1. ABSORPTION OF SOLUTES#
PART 2. ABSORPTION OF X~XK SOLVENT*" Moscowp 1960., (INST OF
OCEANOLOGY OF ACAD SMI USSR). (KLt P-619 200).
1

CLE I IRR j, Z.I.;. RASTORGU33V,, Yu.L.; SUDAKOV, P.Ye.; ANTIRaROV, M,.Ya.;
Prinimali uchastiye; 4PUTRIYEVIKO, O.M.; BOYABOVICH, V.A.
GNI automatic densitonster for liquids. Izv.vys.ucheb.,zav.;
neft' i gaz 5 no.2:109-116 162. WIRA 15:7)
1
1. Groznenskiy neftyanoy institut.
(Densitometers)
(Petroleum products-Density)

SOKOLOV, A.V.; VLASYUK, P.A.; GRINCHENNO, A.M.; GORBUNOV, N.I.;
PMTRIYENX0 k.; XONONOVAI, M.M.; MISHWTINp U.N.
Immediate tasks in studying soil fertility apd ways for its,
increase. Pochvovedenie no.1%8-20 Ja 163. (MIWL 16:2)
(Soil fertility)

F" 7
ACC-ESSION IMs ILP5015283 UR/Ir, 86/6 5 /OMAW/006 6/OOU
S..; Pechannikova, T.
AVTH6RSs Raniko-irskaya 19, 116., -DM1tr46h1*j1 ~jj
T ITLE IA method for obtaining 39,,_
No. 170655
SOMM' Byullaten' izobretonly i to:varnykb 7makovs, no. 9, 1965, 61':)
TOPIC TAM: resin, phenol,, formaldehyde) almdnum compound
ABSTRACT: This Author Certificate px*sents a method for obtaining phenolformal-
dehyde resins b7 condensing phenol with formaldehyde in the presence of an almi-
num salt. To obtain light resistant and heat resistant resins, aliminim StElfate
is used as the alminum-FM
,Jr
ASSOCIATION: Volgogradskiy nauchno-issedovatellski7 institut tekhrtologii
maBhinast (V d ScJanti~ic Resear-.h Institute of ~%chine C-onstruc-
royeniMi ~q~s~
tion EKLneeriA,,j1
SUMITFUs 17F61)64 MR C L 100 SUB COME -.OGJ 19
"0. R 000
ZF.Zov: '--000
Crd -V

TITLEZ Structure of LbMpl-forma qbV ra'subjected to thermal trentment
S01JRCE: Plasticbeskiye missy, no. 10, 1964, 13-16
TOM TAGS: phenol - formOdehyde, resin, triphenyl methane, theival treatment,
Infrared spectrum, phenollphthalein, ultraviDlet spectrum, resol resin, aurin,
fluorescein, polymer struuture, polymer.aging, resin coloration
-ABSTRACT: --TW ef fect.~of ~thermai~ treatment On phenol -formaldehyde resins was
inaut-WAIS-11-By inf Faredi ultraviolet and -visible light. The preparation of the
sample is described since, in':such_studies, the thickness of the resin films Must
remain almost unchanged at 1-151ji during the thermal treatment (agil~~Q the
surface of the samples must be open on one side. Infrared spectTa' were first
taken on the IIR-10 apparatus for resol resins In the region of 1100-1800 cm-1.
After the sample was slowly heated during the course of 1 hour and kept at 140-
1!,0C ior 1:5 min.j the thermally treated sample was again subjected to spectral
analysit ('1100-1800 cm-1) in order to detect the structural changes causing the
Card 1/3

AL Z471-661
ION HR:: AP4
ACCESS
i%oloration of The resin Ouring:ht:itinga 111k6 phenol content in the resin was also"
-lictermined-spectroscoOiceilly-t6-sttidy-ite-t~xidation during treatment with acid
and alkali. The spectral, analysis showed that chemical reactions, such as redox
:reactions.- lake pla-ce'during - the thermal ti-eatment of resins with the formation
of triphenyl -methane grofjips which are detected as a peak at 1655 cal-1. If for
a freshly synthesized,. revln,~: this peak appears weakly, it increases sharply after!
Ithe first heat treatment:.and-esPecially after the second. The presence of tri
phenyl methane groups is!also. formalde-
responsible for the coloration of phenol-~
V during~ entiiDgo- An the visible and-ultraviolet spectr; f t
--hydi. resi s b
iresinsi peaks characteriistic of these groups also appear. To check the data ob-
it,ained, spectra vere alsi:', recorded with-mo6el dye compounds such as aurin, fluor-~
escein and phl~nolphthaleln, which contain timilar groups. A comparison of tile
different spe4:tra for phi?nol, resins and the model" compounds permits one not only
1
to identify the groupings of the triphenyl methane type in therrmlly treated
1phenol-formaldehyde resi-ne, but also to determine their structure. In the specr
tre of phenotj treatment ~~inder-'affoieht -coliditio'na produced no di Her.ances in itd
'MaItcular.strticIture. , ThtlIm, ~ the -presente oT -free phenol in the resin must not be
considered as the vain camse of cot ration, "Thanks are due to 1,j.Nr_YeTSI~ I
a , ~h na
for taking thv spectra." Orig, Art6 has! 6 fiRures and 7 formulavo
card 2/3

C&IM 313

AP5026778 SOURCE (V.DE- UR/0286/65/000/017/00V/0067
INVENTOR: Kanlkovskaya, Ye._N.; Dmitriyenko,,S . S.; Pechennikova, T. I.
v~ 4+
Dfli-~O I ME" V.
Antibiotic properties of amniotic and allantoio fluide of the
chick embryo. Biul.ekop.biol.i med. 37 n0-1:59-61 Ja 154.
(MLRA 70)
1. Iz mediko-biologicheekogo Wela Inetituta skeperimentalluoy
meditsiny Akademii. meditsinskikli na-ak SSSR i kafedry embriologii
(taveduyushchiy - profesnor B.P.Tokin) Leningradskogo gc1sudarstven-
nogo ordena Lenina universiteta im. A.A.Zhdanova.
(Amniotic fluid) (Antibiotics)
The effect of the amniotia liquid ofahicken eggs on Glaucoma scintkllans was
investigated. The protistocidal effect of the liquid was found to increase strongly
on the 14th day ofthe eggs' incubation. t--'Kpts t4ith 14icroococcus lysocleikticus,
B. rTcoides, B. cai-votorum, B. phytophythorum, and B. prodigiosum showed that
al-lantoic liquid d!Ld not have any bactericidal effect, but seemed to stimulate
the growth of the bacteria. It is already known that. -alantoic liquid is a good
medium for the groiAh of pathogenic leptospirae, Str. viridans, Eberthella typhosa,
Aerobacte,:r aerogenes, Corynebacterium diphtheriae, and Brucella abortus.
In order to arrive at definite conclusions regarding the effects produced by
amniotic and allantoic liquids on mirroorganisms, expts with bacterLa pathogenic to
chickens -:hould be conducted.

.ANDONIYF,V, Y.L.; BAW4, V.&.; BAIMAJ71TAN, K.K.; BEWIN, V.D.; 'DIRYUKOV, I.K.;
BIRYM,"OT, S.M.; BLCKHIN, S.I.; BOROVOT, G.A.; BUIW, M.Z.; BUHAKOV,
N.A.; VARTSATZIR, B.A.; VOVK, G.M.; VORM0, B.A.; VOSHCHININ, A.P.;
GAUCTIONOV, V.D., kand. tekhn. nauk; GSWIN, Ye.M.; GILIDMOIAT,
Ya.D., kand. tekho. wmk-; GINZBUNG, M.M.; GLEBOV, P.S.; GODZS, B.G.;
GORBA131W, V.N.; GHZHIB, B.V.; GHWWWV, L.P., kand. a.-kh. nank;
GRCMINSWA, 1.74.; DOILOV, A.G.; DMITRIUV, I.G.; pjglNajWO,
DOBIMOTOV, D.M.; DUBIWIN, L.G.; DUNDMOV, M.D.; ZHOLIK.
A.P.; ZAMMIGH, D.K.; ZIKUW, Ye.V.; ZIM&SKOV, S.V.; ZTJBRIK, K.M.;
KAW97, I.F.; UMM, S.N.; )[CLWATIff, N~M#; KONAIM'SKITt V.T.;
KOSKNICO, V.P.; K(EWISTOT, D.V.; KOSTROV, I.H.; KOTLTIMSKIY, D.M.;
KRIV511IT. 11,No; 1UNNSOV, A,Ta.; TAGA"RIKOVi N.I.; LGWWV, V.G.;
LIM031M. V.P.; IW2UNOV. P.J.-, MOSMIGH, K.]?.-, MELPHICIMMO,
K.I.; MEMLIVIC11, I.R.; MIJIHAYWV, A.V., kand. tekhn. nauk;
MUMMA, R.N.; HATANSON, A.V.; NXITIN, M.V.; OUS, I.S.;
OGULINIK, d.R.; MUM, A.D.; 0SMXR, N.A*; FMOV, V.I.; FJMYMMIN,
G.A.. Prof.; PlYJUXOTA, Yej.; RAPOPORT, Ya.D.; RWIZ,N, W.P.;
ROZAKOV, M.P., lamd. biol. nauk; ROGHEGOV, A.G.; RUD10=, A.M.;
R'YBCEIEVSKIY, V.S.; SADCHIKOV, A.V.; SHMENTSOV, V.A.; Sl ' '0, P.M.;
SINU.VSKAYA, V.T.; SITAROVA. M.Nj; SOSNOVIKOV, K.S.; STAVITSKIY.
Ye.A,,; STOLYAROV, B.P. [deceased ; SUDZILOVSKIY. A.0.; SYRTS07A,
Ye.D.. kand. tekhn. nauk; FILIFFSKIY. V.P.; KWA TURIX. A.D.;
TSIS113VSKIY, P.M.; CHMWASOV, M.I.; CHIMUSHW, A.A.; CHUSOVITIN,
N.A.- MMTOPAL, A.O.; SH3KHM, P.A.; SHISHKO, G.A.; SHCHIMBM,
I.H.: 0GAL1, F.F.; YI&OBSON, A.G.; TAKUBOV, P.A., AIKEM3L'SKIY,
(Continued on next card)

jMff yff, Vj~.... (continixed) Card 2.
Ye,A.,. retsenzent red.; AEM):N, A.N., retsenzent, rod.; BAIASHOT,
Yu.s.:- retsenzeni,$ roil.; BARLBANOV, VO.A., retBenzent, red.; BATUME,
P.D., retsenzent, red.; BORODIN, P.V., kand. tekhn. wxuk, retsenzent,
red.; VAIUTSKIY, I.I., kand. takhn.*n-quk, retsenizent, red.;
GRIGQ11'YZV;.V.M,~,,kand. tekhn. iauk, retsenzient, red.; GTJBIN, N.Y.,
retse-iment, red.; GUDAYW, ION., retsenzent, red.; YRRHOLOV. A. I.,
kand. tekhn. nauk, retsenzent, red.; KARAtTLOV, B.P., retsenzant,
red'; KRITSKIY,*S.N,, doktor tekhn.' uauk, retse'went, red.; LIM,
V.V,: retsenzent, red.; WKINv V. V, reteenzent, red.; WSKIN, Z.D.,
rets6iruent, rod.~ M&TRIROSOV# A.Kh., rieteensent, red.; MENDELET17,
D.H,11 retsenzent, red.; MMIEW, N.Y., doktor takhn. -nauk, retsenzerit,
red.; OB OV, S.S.' retsenzemt,* red.; FETRASHM), P.M., retsenzent,
red.; POLYAKOV, L.H., reitsenzent, red.; RUHYAMS]ff, A.M., retuenzout,
red. ~RYABCHIKOT. Ye.I., retsenzent, rea.; STLS~07, N.G., retsen-
zent: red.; TATAWIff, P.P., ratsenzen't, red.; TARANOVSKIY, S.V,,
prof., dokbor tel:hn. i3auk, retsenzent, red.; TT7TUTI, R.R., retsen-
zent. red.; FADOROV, 1b.N., retsenzent, red ; SMCVYAKOV, M.N.,
retse-azent, red.~, SMZ07, M.I., reteenzent: red.; ZHIUK, -'-Ya.
[deceased]. akadomik,'glavnyy red.; RUSSO, G.A., kaud. tekhn. nauk,
red.; FILIMONOV. N.A., red.; VOIKOV, LOW., red.; GRISHIN, M.N., red.;
ZHTIR3:N. V.D., prof., doktor te*khn. nauk, red.. KOSTRCfV, I.N., red.-,
LIM.GMU. V.P., red.-, M)MV3D11V, VON., kand. tekhu. t-m3k, red.;
HI)MYLOV, A.V., Icand. tekhu. nauk, red.; FSTRO7. G.D., red.; BAZIN,
N.V., red.; SGBOXXV, V.P., red.; FRUNGIR, B.P., red.; FRZYGOYM,
(Continued on next card)

ANDON'Y11V, V.L.... (continued) Gard 3.
Ye.F., red.; TSYFLAKOV, V.D. [deceased], red.; KaWLIMOV, P.M.,
telean. red.; G]WIN, lb.M., tekhn. red.; KACHZWVSKIY, N.V., tekhn.
red.
[Volga-Don; technical accoimt of the construction of the T.I. lenin
Volga.-Don Navigation (knal, the TSimlyansk Wdroelectrio Center,
and irrigation eyetem] Volgo-Don; tekhniaheskii otchet a stroitell-
stye Volgo-Donskogo mLdokhodnogo kawla imeni V.I. Umina, TSim2.-
lianElkOgO gidro'w3la i orositelinykh soortxzhanii, 1949-1952; v piati
tomakh. Mookwa, Gas. onerg. iod-vo. Vol.l. [General structural
deswAptions] Obahchee opioanie sooruzhenii. Glav. red. S.IA. Zhuk.
Ited. toma M.H. Grishin. 1957. 319 p. Vol.2. [Organization of can-
stmition. Specialized operations in hydraulic enginoering] Orga~
nizateiia etroitellstvn. Spetsiallnye gidrotakhnicheakie raboty.
(Continued on next card)

AmylyEv, (continued) Card 4.
Gia,jr. red. S.IA4 Zhuk. Red. tom I.N. Kostrov. 1958. 319 r,
(mm 11:9)
1. Aissia, (1923- - U.S.S.R.) Ministerstvo elektrostanteii. Bymro,
teldmicheskogo otcheta o stroitelletve Volgo-Dona. 2. Chlen-kor-
reffPondent; Almdemit nauk SSSII (for Akhutiu). 3. Day-stvitellnyy
chlen Akademii stroitallstva i arkhitektury SSSR (for Grishin,
Razin).
(Volga Don Caual-Hydraulic engineering)

DNITRIYMO, Yu.D., inzh.
Using floating bridges in lydraulic dredgirgoperations.
Yekh. stroi. 17 no,7:17 Jl 160. 04IU 13:7)
(Dredging)

DMITRIYENIM., Yu.D.
Crane for repairing dredging equipment. Mekh. stroi. 18 no.5:
23-24 My 161. (MIRA 1.4:7)
1. Glavspetspromstroy Ministerstva stroitellstva RSFSR.
(Dredging machine faintenance, and repair)
k

DMITRIYENKO, Yu I., inzh.; IVASHIN, V.M., inzh.; KUZNETSOV, V.P., inzh.;
')NSVK, M.F.,*inzh.; YAKOVLEV, N.A.,,inzh.
The "Lugansk Hour" competition in the mines of Luganskuiroll Combine.
Ugoll Ukr. 6 no.5s23-26 My 162. (MIRA 15111)
(Donets Basin-Coal mines and mining)
(Socialist competition) P

DMITRUM09 Tu.I.,, inzh.; IVASHIR, V.M., inzh.,- MATSYUK, M.F., inzh.;
G.G., inzh.; SMM-qOV, N.D., inzh.; YAKOVLEV, N.A., inzh.
.9
Msys of increasing the labor productivity of miners at 'the
mines of the "Luganskugoll" Combine. Sbakht. stroi. 8 no.2-
2-7 F 164. OIIRA 17:3)
I., Norma tivno-issledovatel I skaya stantsiya kombinata
lAiganskugolt (for all, except Yakovlev). 2. XLVMunarskiy
g-orno-metallurgicheskiy institut (for rakovler).

GULYAYEVA., A.M.; DMITRIYENKOO Yu..').; KUDERSKIY, L.A.
Resu:Its of the introduction of the Baikal whitefish in
Iialce Ukahozaro (southern Karelia). Zool. zhur. 42 no.6:
877-881 t6,y, (MIRA 16 17)
1. Karelian Department of -the State Research Institute of the
Lake and River Fishery Management, Petrozavodsk.
(Ukahozerop lake-Whitefishes)
(Fish introduction)

WIT4-v, A.
." r
261362
Milkhaylov, N. I Chenne6skiy, V. Za chistotu narksistskoleninskoy teorli v. statisti-
cheskoi literature. Vestnik statistiki, 1949', No. 2-, S. 57-61
SO,. LFrOPIS' NO. 34

:X'.1 -I ~' ~ L, I Y:" " , ..I .
-"trai-~!-htenin~: out, s;lortening, and simplifying statistical accountin,~.
Vez5t. 6tat. "c 3, 1952.

AUTHORi Dmitriyev, A., Engineer SOV-4758-10-31/39
-
TITLE: The Harmony of Elementary Particles (Carmoniya elementarnykh
chastits)
PERIODICAL: Znaniye - sila, 1958, Nr 10, PP 33 - 35 (USSR)
ABSTRACT: The discoveries of Rutherford, Einstein, Fermi, Snyder and
Heisenberg are explained in simplified form. There are
5 caricatures.
Card 1/1

r#4ITRIYICV A, I
- -, L-
Dump semitrailer. Biul. tekh. Inform. po stroi. 5 no.5:27
MY '59. WEA 12:8)
(D=p trucks)

DHITRIYIKV, A.
Sov.profacivsy 5 no-8:39-JW Ag '57. (HIBA 10: 8)
-'~n'lRrofgritporg vtorogo formovochnogo konveyyara chugunolitaynogo
tilekha No.1 Chelyabinakage traktornogo zavoda.
(Chelyabinsk--Tractor industry)

'01fY 4, /,~
DMITRITU A
"M-1- - ijLWAW~--;
New tire houses and water reserroire on collective farma. Pbzh. delo
1; no.l.*15 A 158, (14nu 11,a)
(Irazakhatan-Collective farmB-71res and fire prevention)

DMITRIYEV, A., mladehi7 nauchny7 so,-rudnilc
--- ,--l--------
International merchant mal-'~-n conferences; freight carts. 14or.flot 19
rAQ.l:A0--4? Ja 159. (IGRA 12:3)
1. Ilauchno-iosledovatel"i3kiy kon"yunkturriyy inatitut Ministerstva
vnealiney torgovIi SSSR.
(Merchant marine-Congresues)

SOKOLOV., L,j, m:Ladshiy nauchnYY sotrudnik; AZIZOV, M.; ZHURAVLEVA, A.,
mladshiy nauchVy ootrdftik; _WTR4EV 0 A., mUdBhiy
nauchnyy sotrudnik
Justification of the architectural and structural type of
a universal dry-cargo whip with 3,000-4,000-ton deadweight.
Mor. flot 23 no.8:29-32 Ag 163. (MIU 16111)
1. TSentrallnyy nauchno-iseladavateliskiy institut morskogo
flota.' 2. Starshiy inzh. TSentrallnogo naucbno-issietdovatell-
skogo inatituta morskogo flota (for Azizov).

DMITRIYZV, A., kand.tekhn.Pauk
Now construction elements of brick apartment houses. Zhil. stroi.
no.12:28-29 160. ' (MIRA 13-11)
Okxrope, Weatern-Building, Brick)

~.,%utj3507 3 SOURCE CODE: UR/0160/66/000/008/P,049/BO49
AUTHOR: Dmitriyev, A. A.
I TITLE: Consideration on the influence of a large city of the Moscow type on the
turbulence coefficient in the lower troposphere
SOURCE: Ref. zh. Geofizika, Abs. 8B356
REF SOURCE: Sb. Klimat bollshogo goroda. M.. Mosk. un-t. 1965, 136-151
I TOPIC TAGS: troposphere, atmospheric turbulence, air pollution
ABSTRACT: Equations are derived for the transfer of impurities, taking into
consideration convective anabatic and catabatic movements. The analysis of i
solutions presented in the study shows that a high degree of roughness as well as i
a great warmup of the anabatic convective streams. over large cities must cause
an increase of the turbulence coefficient over them. It is only in the thin surface
layer, situated inside the "displacement layer", that mixing can be weaker than in
the surrounding fields. Sufficiently large concentrations of smoke and gases can
accumulate in these thin layers and at all levels of urban build-up, if strong
surface inversions exist. The dynamic turbulence merely produces a more uniform-
112 UDC: 551. 511

ACC NR: AR6035073
mixing of smoke under the inversion. During thermal convection, the dust and
smoke cap over the cit will be higher than in the surrounding area. This is
y
accentuated by a regulated ascent of the type of breeze circulation which
corresponds to the theoretically expected lowering of pressure of the order of
1 mb in the city. 1. Kravchenko. [Translation of abstract] [GC]
SUB CODE: 04, 13, .08/
212
Card

los(-coa !1--dro-m.--ticro)-o;:l!,al Inst., ~-194it-)-
'OT" 7-a'.", ~r -'o `11-~ cluilst-;Oll of
icta, ion u
u L
C~Tccttliv~ at-lon,
I, r. ~.To;fraf. i ~.aofiz-, ','0. 1-t, !~'114-

DDI,ITRIYEV., A. A. Prof PA 237T64
USSR/Geophysics -.Earth's Albeao Dee 52
"Problem Concerning Procedure Followed in the Study
of the Reflective Properties of the Earth's Surface;'
Prof A. A. Dimitriyev, Dr Phys-Math Sci
"Meteorol I Gidrol" No 12, pp 25-26
Comments on S.I. Sivkov's article (ibid. No 8,
1951) which evaluates the accuracy of procedures
for observing the albedo by use of BerezkInIs for-
mula. Conc~ludes that Berezkin's and his own for-
mula give similar results.
23TT64

ACC _NK. t-61-~Bbi~4-01~Ici3-6:~/66/002/008/089VO8997-,
AUTHOR: Dmitriyev, A. A.; Yenaich T. V.
ORG: Moscow State University (Moskovskiy gosudarstvennyy universitet)
TITLE: SimuLition of the problem of determining the temperatures of rivers from a
satellite
SOURCE: AN SSSR. Izvestigya. Fizika atmoafery i okeana) v. 2, no. -8, 1966~ 897-899
TOPIC TAGS: radiation measurement, temperature measurement, q2onnaissance satellite,,
ABSTRACT: The authors make use of EC method for determinfig the radiation intensity
measured with a wide-angle receiver (Dokl. AN SSSE v. 147, no, 5, 1962 and in Aktino- I
xetriya i opt:Lka atmosfery [Actinometry and Atmospheric Optics], Nauka, 1964) to per-'
form an experiment in which they measured the brightness of a narrow white strip
against a uniform dark background, using a radiation receiver having a photocell with
a. field of view of somewhat larger diameter than the width of the strip. The purpose!
of the experizaent was to simulate the reading of a radiation receiver mounted on a
satellite and measuring the thermal radiation from a river whose width is narrower
than the angle subtended by the radiation receiver. The measured brightness distribu-~l
tion turned out to have a bell-shaped rather than a true rectangular form, and thd~-
authors calculate' the true brightness of the strip from the measured one by a pro~,~
cedure based on the earlier work. The method is based essentially on comparing tho-:
coefficients of the Fourier expansion of the true (rectangular) and smoothed (beli-~,,.
Card 2/2 LTDC: 551-521.2

L 46957-66
FACC 14-AF363oo88
0
shaped) distributions. The accuracy of the method is better than 4% a if the
., nd
measurement error does not exceed 1%, the temperature of the river (which is related
with the brigIrtness by the Stefan-Boltzmann law) can be determined within loc. Orig.I
art. has: 2 f.-Igures, 10 formulas, and 2 tables. (0211
SUB CODE: 20/ Sum DATz: 3Djan66/ ORIG REF: 003/ ATD PRESS: 5089
Card

S/020/62/147/005/014/032
B1121B102
AUTHOR: A. A.
TITLE: ~Radiation intensity distribution measured by a wide-aperture
detector
PERIODICAL: Ak.ademiya nauk SSSR.- Doklady, v. 1.47, no. 5, 1962x 1061-1062
TEXT: The sought intensity distribution I(~) is determined from the
measured intensity f(if) by the integral relation
K(V-9)1(T)dg.
4p-ca
The coefficie,nts of the Fourier expansions
c0
(V) + Y, A, cos mp; (2)
2
00
,K (%p �0- + I a,, cos n -.1 (V (3)
to
Card 1/2 n-1

S/02 62/147/005/014/032
Radiation intensity distribut'~"on...- B1 12YB102
Do
+ an cos tnq) +mn M(P. (4)
2 Z
are interrelated by
2(oA,,
an co (5)
[sin (mixla) + n) W, sin (m;tlo)*- n) col
I mnl(a + n+ -,M/(0 - r.
M=U
00 2o)B, (6)
a [s1n(ma/(0+n)(L) sin(mitho-n)(o
mzt/w + n+ mAlri) - n
A particular case is illustrated by a figure.
ASSOCIATION: Universitet druzhby narodov im. Patrisa Lumumby (University
of the Friendship of Nations imeni :Patri a Lutuumba)
PK-SENTED: July 11, 1962, lky 1. V. Obreimov, Academician
SUBMITTED: June 16, 1962
4
Card 2/2 ;

MUTRMV.- A.1%.
ArtMaial, influezice on the clinate of large and small regiong;
using the example of the coast of the lake Ineyk-Kul". Zzv. AN
SSSR, %rogeoge Y;0*1:45-1+9 Ta-T 163. (MM-A 16:2)
1. 'Upi-verbitet druzhby narodav tm~ Patrisa TAmumby.
' (Isayk-Kult region-Climate) I
I(Imk-Kull regicm-Windbrbakev Phelterbeltap etc*)

Pffn=j A.ji~.
Distribation of radiation intensity measured with a
aperture receiver. Dokl. AN SSSR,147 no-5:1061-106-7
1. UnIversitat druilby narodov Jin. Patrisa Iammby.
akadenikcm I.Ts. Olweimovpi.
(Radiom-ster)
wide-
D 162s
(VIIRA 16 t2)
Predstarleno

IEMIEV~ A. A., (Bu1',aJxdnskOy Ice-Crusted Growid Sta.)
SP: "The classificatiori of 9L-Lzed frost building on uires."
LO: Russia.
RE: In t!)e present paper a scheme for the classification of glazed frost and silver thaw on
wires is offered3 constructed according to morpholoCical indications. The connection
between the procesict of the forming, of deposits and their structure is established,
Threa genetic groups are introduced: glazed frost$ ice-dropfrost, sublimate, Glazed
frost arises at tho sprea-dint of drops being, in contact with the wire. Ice-dropsfrost
forrw.d from drops 'instantly freezing at contact* It is marked the dependence of the
appearance of one: of the both mentioned forms of sediments on the cluiracter of the
heat balance. There m.V be hydrodynamically explained as well the brancy structure
of the ice-dropsfrast; the increase of the role of the surface frict.1on forces in
comparison with thc mass inertial forces causes the tendency of smaller drops to
f3-o-,.T round obstacles better than larger particles do. Drops accidentally failing
upon the rough surfaces of the vires and freezing form the bases of the branches
(Fig. 12) of the ice-dropsfrostj. on the peripheral particles of which the probability
for a contact with new drops is the greatest. It seems natural to Q-pect a greater
spatial development; (branchity) for smallerdimensions of drops and smal].er wind velo-
cities. The t1drd group contains the forms of sediments of sublimate: origin.
I
SO::Acad. of Sci. of USSR. Vol X. 11.1is 281107, 1946

y
VNITRAT!, A.
"Evaluat.ion of the Precision of 0'.')senrations of Sleet: (Wo:7ks of 3'atc~' 10 --- ~-,
NO 3, .1947)
SO: M U21)2, 22 So) 1952

J
DMMIP3101, It. A.
"Deposits of iloa-~--.rro".t on I'll-res in Connection thc o'
surface (Worko ol the S'Jitc- (.-(!oph-~sical Oboi~!rvatory, No
SO: ~ U23,~1'12, 22 Sep l),52

DMITIZI W, A. A
"An App:,.-oac*:-. towa:-d ~.he Problem of the of Cro3s-,S~ction o--I DepoCit-- fr-~m
Mi - I -
Su,ourcoole-J Fo,- of SuDencled Droplet[; A~ Ji. s o -:' t h e S ~ a 4, e
,Ieopliysical. Obse:7vatory, No 3, 1,)47)
~ U-23-/2, 22 Son- 1)52

DMTRIYEV, A. A.,
"COnnection Between Monsoon Pressure and Temperature Oscillations and
Solar Activity," Met i Gidr.Dl., No 5) 1949
NLRA, oct 52

42860. Z~T (1)1FCC';_, _11
*

T ACC~~SUON
40~ ~r AR4 4537
SOU 2, Geo iz
tki
-AIR HOR:
1 ~Vev.!*
1tri -A

TIT [~&ieniificati~

CIT O Mid , ir. Arkt.; f~
tok c -TAGS - I wind velocity,
..Clr tulatio'n,j drif ting statj
TM 4,SLATION'.~'-_ This,~ipvestij

PW

0 .. I I

DMITRUIT, A. A. REMIWV, G. A.
"About microclimatical differences of temperatures in Yriscow in connection
with some radiational factors."
report presented at the Atmospheric Radiation Symp, Lerdngrad, 5-12 Aug 64.

M
:L
2 5 ~~5 5 T (1) cc: Ow.
-AI404879-9 125VOOO/0169/083
ACCINS1014.14R.
A.
asin
TIM i Wir-41 ntensification in certain ravions of the Arctic a
7
SOUTICIE: Arktii'lics1dy i,antirltichoskiyiiu*tuclino-is y institut. Trudy*j V,
255,: T.M.' Sbornik Ltatey povopros-am dolgorrochny*Wi prognozov pogody* d1ya Arktild
:-(Coftectiomofarticles on.-the- problems of long~-rango weather fo:recasting for the Arctic),
16C
wea
--,------~%TOPTC TAGS, arctic nic',6oyol6gy,.iNvirid.,-volocity, ther forecasting, lorg-rango weather
forecasting
ABSTRACT: NVind obse-i-vations a. the drifting stations SP-4, SP-5, SP-G and SP-7 ha~,e
ed. for cases of -wind: int6isiffeations with a velocity (if 10 rn/sec or irora in the
been analyz
sumiaer-autumn per;Aod of 1954-1960 in the polar and oastorn regions of th,,- Arctic.
A total of 1, 505 obse rvation periods. weie andlyzed.- 495 cases of wind intensific,,vtion worc
note d (duration of -wind intensification was for one observation p3riod or moro). T'here
weriam 244 such cases in the region near Aie pole (129 in summer and 115 in auturna) and
251 cases inths eastern region (133 in cummer and 118 in auturnn). It was foundl that wind
ar 3!

AC CESSION NP.: AT4048799
velocities.'exceeding 10, m/sec* are.,rarely observed in'the central part ofthe Arctic basin
dul-big Ahe navi
gation season (only 7.5m of all observations in 7 years from June through
October). Most strong Nyinds.have.velocitics of 10-12 m/sec; winds with a force of 1. 3
m/sec' have! a frequency maodmum in the autumn months. The greatest number of xvind
intensifications was observed in October (10. 6%). The maximum of inteasifications of
xvind in the region near the pole is observed When there is a C form of circulation, but
in Che easte-m region the maximum is associated with an E form. The eastern Arctic is
stormier thim the central Arctic. During the entier period mentioned tho greatest number
of wind intensifications occurred When there were type )Gb, XM and XVa processes and
no intensifications were observediduring type Mb processes. The greatkist number of
stablie Nvind intensifications Was observed during types Xlb, XIlb and X'11b and none -were
observed during processes of tn)es 111b and Xb. In most cases the zone of xvind inwnsi-
fication is the leading and southern parts of cyclones; these, penetrating into the high
latitudes with at-jacent anticyclores, give riEe to wind intensifications. Ili all cases t1le
deve*.1opment of it strong wind isassociated ivith an increase of intensity of pressure
sysU.ms deterinf-Ab3g, the zone of intensification in comparison with standard mean pressure
-values. Vile moJel charts i4hich have been compiled for almost all types can be used in
forecasting work by comparing Qem.,%vith thet predicted pressure fields determined by the
imethad used at the twkticheskiy I Antarktich5aldy InsUtut (Arctic and AnLarctic Mstitute).
CA:rd 2/3

L 38149-66 E11T(1)/FCC GIJ
ACC NR: .AT6012779 (N
AUTHOR: Dmitriyev, A. A.
ORG: none
SOURCE CODE: UR/2561/65/000/021/0049/0055
4
TITLE: Southeastern winds of hurricane velocity in Pevek and some possibilities of
controlling them
SOURCE. Leningrad. Arktiche.,,k~y._iantaikticheskiv,-,nauchno---i-s-s-le-.do-va.tel.'sk.iy
institut. Problemy Arktiki i Antarktiki, no. 21, , 49-55
TOPIC TAGS: wind velocity, wind direction, atmospheric wind field, electric power
source
ABSTMCT: The mechanism of the formation of the "Yuzhak" (the local name for the
winds), means of predicting it, and the prevention of damage from it were investi-
gated in 1963 on the basis of earlier investigations,'(Shapayev, Tolstikov, and
Farmosova). The port of Pevek (located in the Chaunskaya Bay of the East-Siberian
Sea) is frequently the victim of yuzhaks. Observations of the yuzhaks were made
using airborne surveys and the Bernoulli formula
Card 1/2 UDC: 551.555.3(98)

L 38149-66
ACC HR: AT6012779
p + ConSt.
2
where P is the pressure, p is the air density, and V is the wind velocity. The
data show that the Southeastern air flow from the Anadyrskiy Range turns t(Y'qard the
Southwest and upon reaching the Pevekskiy Range, strikes the village of Pevek and
then gradually loses raomentura. The appearance and the velocity of wind of yuzhak
type depends on the curvature of trajectory of the air flow. The maximum velocities
of the winds are observed at 100-500 m altitude with a progressive velocity decrease
from 500 m - 5 km altitude. It is suggested that by creating a pass between the two
valleys, the strong Southeastern wind may be partially deflected from the village of
Pevek and the damage to Fevek can be considerably minimized. The author also specu-
lates on the possibility of harnessing the yuzhak for the production'of electric
power. Orig. art. has: 4 figures, 1 formula.
SUB CODE: 04~ SUBM DATE- 070ct641 ORIG REF. 003/ OTH REF: 000
Card 212Mil~_

DMITRITEV. A. it.
"Influence of Continents and Oceans on the Circulation of the Atmosphere.'
Sub 18 Nov 47, Central Inst of Weather Porseasting
Dissertations presented for degrees in science and engineering In
Moscov in 1947
SO: Sum No.. 457, 18 Apr 55

I-! SOV/49-59-10-5/19
.AUTHOR: Dmitriyev, A. A.
TITLU1-, on he question of the Velocity of Cosmic Dust FallinG
From the Upper Layers of the Atmosphere
PERIODICALi Izvestiya Akademii naulr. SSSR Seriya geofizicheskaya
.L959, Nr 10, -p 1468-1472 (USSR5
P
ABSTRACT: The process of fall is illustrated in Fig 1, The motion
of fine particles of cosmic origin at heights 80-110 km
is considered as turbulent. The specific concentraT-1-oli-
~L Of the particles can be defined by Eas (1a,6). The
Irelocity of fall of the particles of radius a can be
obtained from Eq (2) where X - mean free path
(Eq (3)), jo density of particle, A + 19 Tj - air
viscosity, mean velocity of miolecules. The
constant magnitude of p V (Eq (4)) is derived from
Eqs (2) and (3). The coefficient of turbulence at
1.00 km Aig is taken from Booker (Ref 10) as
K ;Z, 107cO/sec. The formula (1) can also be written
as E~2(5) and its solution can be given as Eqs (12)
and 5). The conditions described by the latter
Card 1/2 formula are illustrated in Fig 2, which shows the

SOV/49-59-10-5/lQ,
On the Question of the Velocity of Cosmic Dust Falling From the
Upper Layers of the Atmosphere
distribution of a volume concentration at the
stationaryconditions. There are 2 figures and 13
references 9 of which are Soviet and 4 English.
ASSOCIATION: Akademiya nauk SSSR. Institut Prikladnoy geofiziki
IIAcademy of Sciences USSR. Institute of Api)lied
G e 0 pry-S i C s
SUBMITTED; September 5,1958
Card 2/2

DMITRIYEV, A.A.
TranEmission of the perturbations of wind speeds in the upper
atmosphere to the tropopause level. Astron.sbor no.3/4.-.109-
U3 1:60. (VIIRA 14:11)
1. Institut prikladnoy geofiziki AN SSSR.
(Atmospheric turbulence)

87975
S/049/60/000/010/011/014
E133/E4i4
AUTHORS: Jbitriyax- A.A., Mishina, M.I., Mikirov, A.Ye. and
Cherenkova. -T-e-7.P.
TITLE: The Influence of Cosmic Dust on Certain Solar
Radiation Characteristics in the Atmosphere
PERIODICAL: I2,vestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1960, No.10, PP.1518-1528
TEXT: Kalitin has shown that there is a small decrease in the
measured solar radiation correlated with the date of the
Perseids (Ref.1). Zacharov found that the minimum measured value
occurred three days after the maximum of the Perseid stream but
that the time depended'on the wavelength used (Ref..2).
Giovanelli (Ref.3) calculated the size and number of the particles
responsible, and information on these data has also been obtained
from radar (Ref.5) and rocket (Rnf.6) observations as well as from
-collection of magnetic material (Ref.7) and work on the zodiacal
light. It seems likely that the dust in the troposphere derives
Card I/

87975
S/049/60/000/010/011/014
E133/E414
The Influence of Cosmic Dust on Certain Solar Radiation
Characteristics in the Atmosphere
from the Earth, whereas that in the stratosphere is of ijiterplanetEvy
origin, An equation is derived giving the distribution of dust
with height ii:t the presence of convection (Eq.(7) ), This formula
is considerably more complicated than the exponential expression
which holds in the absence of convection. A lower limit for the
number of dust particles in the stratosphere is then derived.
assuming that tropospheric'convection does not extend into the
stratosphere. It is found that the mass of particles entering the
Earth's atmosphere is 5.5 x lo-15 gm/cM2 sec. The authors next
consider the effect of the dust content on the solar halo and, in
this connection derive an equation to represent it, Fig:1 is
obtained from this equation and consists of a plot of halo
brightness against height for various wavelengths, (The
observations were made from an aircraft.) The atmospheric
transmission coefficient is closely connected with halo brightness,
but effects in the lower atmosphere can be sufficiently large to
blot out effects in the upper atmosphere, From data obtained in
r--A 2/ 61

87975
s/o4q/6o/ooo/oio/oil/oi4
E133/E4i4
The Influence of Cosmic Duit on Certain Solar Radiation
Characteristics in the Atmosphere
the period 15133 to 1955, it is found that the intensity of solar
radiation seems to oscillate with a period of 5 to 7 days as
well as having minima during meteor showers. It is shown that
there is a I:Lnear correlation between the intensity of short
wavelength solar radiation and the number of meteors per hour
found by radar observations, A correlation was also found
between oscillations in solar radiation and radio-echo
observations, although maxima and minima of the two curves were
displaced. The authors finally calCUlAte the ratio of the
intensity of light scattered by meteoritic dust to that scattered
by air molecules at varying heights, The results are shown in
Fig.6 for different angles of scattering and different elapsed
times after the initial influx of the particle stream. It was
found that the ratio had a constant maximum At 87 km for all
angles of scattering near the level of the noctilucent clouds
(Fig,7). 11bere are 7 figures, I table and 20 references:
7 Soviet anti 13 non-Soviet.
Card 3/9
2/

87975,
S/049/60/000/010/011/014
E133/E414
The Influence of Cosmic Dust on Certain Solar Radiation
Characteristics in the Atmosphere
ASSOCIATION: Akademiya i2auk SSSR Institut prikladnoy geofiziki
(Academy of Sciences USSR Institute of Applied
Geophysics)
SUBMITTED: December 25, 1959
Card 4/�

Di,iITRIY,,'Vt A.A.
--
Repr,)oentLtivity of air temperat-.ire observations in case of a
nonu~ndfomz undcrlyLng surface. Izv. All SSSR. Ser. geolfiz.
no. 202CC-333 F 161. (MML ll+:2)
1. Instuitut priUadnoy goefiziki AN SSSR.
(At,mospheric temperature)

-3, roO-D
S/170/61/004/011/014/020
B108/B138
AUTHOR: Dmitriyev, A. A.
TITLE: Thermodynamic determination of entropy in a gravitational
field
PERIODICAL: Inzhenerno-fizicheekiy zhurnal, v- 4, no. 11, 1961, 114-116
TEXT: The appIlication of the general formulae for entropy may in certain
cases lead to contradictions with theory. In meteorology, for instance,
the specific entropy of perfectly dry air is given by ip = c in G
p To
where T(1000/P)AR/c . P denotes pressure, T the absolute tempera-
p
ture. For the following ealculationso the atmosphere is assumed to con-
sist of f-,,jo strata with potential.temperatures 19 * and (9 antl with mass
1 2
m and m, per oquare centimeter. The total entropy of an atmospheric
1 91 0
2 in in w2
column with a cross section of 1 dm is then S =mj9p ~_00 +m2op 100
This ,relation. obviously does not depend on which of the strat-a has the
higher potential temperature. However, when gravity is allowed for, it
Card 1/3

S/170/61/'004/011/014/020
Thermodynamic determination of B108/B138
Must be the upper stratum which has the higher temperature.. If this is
not so they will change place. The entropy of this new state would be
higher. In order to account for gravity, the relation
dE + APdv + Aydx .
ds - T has to be used. y is the generalized force, x
the. generalized PELth. dE denotes the change in internal energy. Assuming
gravity to be constant with increasing altitude, the entropy of a two-
stratum atmospheric column must be-
-AIvp
S M1 YJ + Ms TS P, +
Ag 10, Ph P. (10)
PC) ARIc " P" 'A
P.
where P is the isobaric'-8urface be twee-n~,th6 -two strata, P the pressure
h 8
on the Earth's surface. It is easy to stj that the entropy reaches.a
Fj P T _ P
ma*ximum of S ' - I (c in -~ ARln when the temperature T is
T 9 p T 0 P0
Card 2/3

2891
S/17 61/004/011/014/020
1
Thermodynamic determination of B1087B 38
constant and equal to T. throughout the atmosphere. There are 2 Soviet
references.
ASSOCIATION: Ins,,itut prikladnoy geofiziki AN SSSR, g. Idoskva. (Institute
of Applied Geophysics AS USSR, Moscow)
SUBMITTED: February 14, 1961
Card 3/3

4/863/62/000/000/002/008
D2Q7/D308
A
AREHOW Dmitrivev. A Bonchkovskaya, T.V. and Byzova, N.L.
TITLE: Estimates of the parameters for modeling of atmos-
pheric circulation in rotating liquid-filled con-
tainers
S OU RC Z 'Vodclirovaniye yavleniy v atmosfere i gidr' os fere;
trudy Ile n,oy. me zhduve doYnstvennoy konferentsii 22-26
noyabrya 3.960 g. Moscow, Izd-vo Ali SSSR, 1962, 20-31
Mcf: The purpose of this paper.is: 1) to select the para-
meters (dimensions and geometrical forms of containers, temperature
0 0 tion in the atmos here so
drop) for modeling of large-scale circula
that they satisfy the,requirements of similarity; 2) to estimate
the effective viscosity coefficient in such models; 3) to find whe-
ther it is possible to establish vertical temperature (or density)
stratification in a model, similar to the typical stratification in
the atnosphere; 4) to forTmIate some problems which can 'De attached
by modeling mettiods. The following conclusions and results are re-
Card 1/2

3/86-5/62/000/000/1002/008
Estimates of the parametet,,s~- D207/D308
ported; 1) It is recommended that the container should be a body of
revolution: a sphcre, a paraboloid or a'cylinder with a flat :)ase.
The suggeste 'd dimensions of containers are given in mathei-ilatical
relationships. By heating one part of the container base and cool-
ing another, horizontal temperature gradients of 1.0 deg cm can be
obtained. A water-filled container (up to 75 cm. in dimensions)
should rotate at about 0.1 rev/sec in order to simulate atmospheric
circulation. 2) Zaq. ef f active viscosity in water-f illed rotating
cylinders is 0.1 cia"/sec. 3) Vertical temperature stratification
can be obtained.by using two heaters. one above the container and
the other below it. .4) Modeling can bemused for studying radioac-
tive fallout, possible control of the weather, effects of cities,
large faetories o'37 water reservoirs on the weather etc. There are
4 figures.
ASSOCIATION: Institut prilcladnoy geofiziki, AN SSSR (Institute
of 'pplied Geophysics, AS 'USSR)
Card 2/2

S/863/62/000/000/002/008
D2Q7/D308
AWHORS: Dmitriyev, A.A., Bonchlcovskaya, T.V. and Byzova, N.L.
TITLE: Estimates of the parameters for modeling of atmos-
pheric circulation in rotating liquid-filled con-
tainers
SOURCE: llodclirovaniye yavieniy v atmosfere i gidr*osfere;
trudy Pervoy mezhduvedoinstvennoy 1conferentsii 22-26
noyabrya 1.960 g. Moscow, Izd-vo All SSSR, 1962, 20-31
TEXf: The purpose of this paper.is: 1) to select the para-
meters (dimensions and geometrical forms of containers, temperature
.drop) for modeling of large-scale circulation in the atmosphere so
that they satisfy the,recpiirements of similarity; 2) to estimate
the effective viscosity-coefficient in such models; 3) to find whe-
ther it is possible to establish vertical temperature (or density)
stratification in a model, similar to the typical stratification in
the atmosphere; 4) to forimilate some problems which can be attacked
by modeling methods. The following conclusions and results are re-
Card 1/2

S/863/62/000/000/002/008
Estimates of the parametett ... D207/D308
ported; 1) It is recommended that the container should L-se a body of
revolution: a sphere, a par-aboloid or a *cylinder with a flat ~)ase.
The suggested dimensions of containers are given in mathematical
relationships. By heating one part of the container base and cool-
ing another, horizontal tet
,vperature gradients of 1.0 deg/cm can be
obtained. .1 water-filled container (up to 75 cm in dimensions)
should rotate at about 0.1 rev/sec in order to simulate atmospheric
circulation. - 2) The effective viscosity in water-filled rotating
cylinders is 0.1 Cm2/sec. .3) Vertical temperature stratification
can be obtained-by using two heaters: one above the contaitler and
the other below it. .4) Modeling can be. used for studying radioac-
tive fallout, possible control of the weather, effects of cities,
large factories oir water reservoirs on the weather etc. There are
4 figures.
ASSOCIATION: Institut prikladnoy geofiziki, AN SSSR (Institute
of Applied Geophysics, AS USSR)
Card 2/2

DWITRIYEV, A.A., otv. red.:; BYZOVA, N.L., otv. red., KRAVCHENKO, N.M.,
rW.-Iz-d.'=lra; NIKOIXYEVA, L.K., red. iad-va; POLYAKOVA, T.V.,
tekhni red,
[Studying the boundary layer of the atmosphere from a 300-
meter weather towe:r]Izuehenie pogranichnogo sloia atmoaferr a
300-Teetinvoi bashni. Wskva, Izd-vo Akad. nauk SSSR, 1963. 158 P.
(MIRA 160.)
1. Akaeleiniya nauk 13SSR. Institut prikladnoy fiziki.
(Atmosphere)

BULINSKATA, Nataliya Aleksandrovnal DMITRIYEV, A.A., doktor fiziko-
matenukticheskikh nauk, otv. re&.-;B N.N., red. izd-va;
MAKIINT, Ye.V., tekbn, red.
2
[-Atlaa-of the b4rometric characteristics of cyclones and anti-
cyclones; cyclones and anticycl.ones as climatic and weatheir
indices, based on materLil-from synoptic charts for the 14,~'-year
veriod from 1943 to 19571-Atlas baricheskikh kharakteristik
tsilclonov i antitsiklonov; tsiklony i antitsiklony kak
pokazateli klimata i pogody po materialam sinopticheskikh
kart ZEL 15 let 8 1943 po 1957 g. ~bskva, Izd-vo Akad. net*
SSSR, 1.963- 193 P. (MIRA 16:6)
(Cyclones)

. ..............
ACCESSION N11: AP4003730
AUTHOR: Dmitriyev, A.A.
S/0293/63/001/002/0221/0226
TITLE: Two dimensional problem of'reconstructing the true brightness index
from a smoothed measurid data plot
SOURCE: KosmLeheskiye issledovrtniyn, v. 1, no. 2, 1963, 221-226
TOPIC TAGS: brightness index, true brightness index, spaceborne optical
observation,. spaceborne camera-, spaceborne atmosphere photography, spaceborne
atmosphere observation, spaceborne earth photography, spaceborne earth obser-
vation, spaceborne optical system, brightness index computation, photography
aboard artificial satellite
ABSTR.kT: The author has previously analyzed the one-dimensional problem of
reconstructir4,,''the true brightness index from a smoothed measured data plot.
'However, in the analysis of atmospheric-optical observit:Wns from satellites,
it is only poasible to use a one-dimensional approach ip special cases. The
information'is more frequently two-dimensional in character, as in the case of
the distribution of a cloud cover on successive-orbits when the radiation
Aetector is pointed downward. It is shown that the true brightness index can
Cor4_1

1;'
I
ACCESSION NR: A24003730
be reconstructed from a smoothed measured data plot, both in the case of a
pi-shaped fuirztion of the distribution of instrument sensitivity in a.Particular:
range of solid angles and in the case of a function rapidly decreasing' Jn value
fr.= the point of sighting. Specific cases of computation of the true field of-
brightness for a two-di=ensional case are cited. The numerical examples show
tLte necessity for taking into account nonuniformities in the field of bright-
ness and the nonuniformity in the characteristic of sensitilvity of the de'tector
in the case of observations of the distrigution of the radiant flux from non-
homogeneous surfaces when wide-angle apparatus is used. In order to introduce
corrections, it is necessary to know the distribution of the sensitivity of
the detector as a function of the angular distance to the point of sighting
and the results of change of the smoothed brightness as a function of' both
angular coordinrttes. Only in the case of slowly changing fields of brightness
and a rapid dec-rease in the sensitivity of the detector with increasJIM& dis-
tance from the point of,sighting do the smoothed and true brightness have, sim-t
ilar values. Orig. art. has: 1 figure and 31 formulas.
Card 2/3

ACCESSION NR: AP4003730
ASSOCIATIO14; None
-ENCL: 00
OTOR: 000
St"MaTTED: lOJan63 DATE ACQ: 26D--c63
SM CODE: Pil NO REP SOV: 001

- - - - - -- - - - -

DMITRIYEV, A.A., prof.
- I I - w .
Dynamics of the atmosphere; an international symposilso.
Priroda 54 no.12:67-71 D 165. (MIRk 18:12)
1. Moskovvkiy gosudarBtvennyy universitet i-ri. Lomonosova.