SCIENTIFIC ABSTRACT ROMANKEVICH, V.N. - ROMANKOV, P.G.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


ROMMUTICH, V.1%; SIDTAKIN, Y.G.
Inconstancy, of the electrical Parameters of selenium samples
containing bromine in relation to the duration of their
storage. Izv.vys.ucheb.zav.; fiz. no-3:180-184 160. (MFU 13:7)
1. Kiyevskiy politekhnicheskiy institut.
(Selenium--Electric properties)

SOV/139-5-8-6-4/229
AUTEO Romankeviph, V.N. and S,-Iiyahin, -,-.G,
'um 'tb Iodine
THU,: Elec ica roTerties of AmorDhous Selen-
V11
Impurity (Elektricheskiye svoystva amorfnogo selena s
primeslyu ioda)
Pi,,'t"CiODICA.b:Izvestiya Vysshilch Uchebnykii Zavedeuiy, Fizika,
1958, Nr 6, pp 25-32 (USSR)
ABSTRACT: The paper reports studies of the electrical coriduOlivity.
its temperature and frequency dependences and the thermo-
electric power of amorphous selenium with various
amounts of iodine, Pare amorphouz; selenium powder from
the factuoiT was used to prepare the samples,
The samples were prepared by applying a pressure of
30000 ai~m. This pressure vras used in order to obtai.~-
material whose density is equal to the densi~ of
amorphous selenium produced, by mel-t,-Ing (4,,2
Iodine was introduced in the form of -oowder which was
purified by several sublimations in vacuo,,, Eachsample
vias in the form of a Dlate 2.1 x 1.,l cm inarea and
0,15 - 0.2 cm thickness, Aquadag electrodes were used-
In addition to the series of samples prepared from
Card 116 powder, the aixt-hors also produced samples of pure

SOV/139-58-6-4/29
Electrical Properties of Amorphous Selenium with iodine impurit, y
amorphous se'Lendum and amorphous selenium with lodd-ne
by melting ir, evacuated ampoules, The electrical
conductivity of c of selenium without iodine was
measured using a d-,c, amplifier., The value of cv of
odine was found, employing the lisual
Samples with i
potentiometric method,. The tem-Derature dependence
of a was measured between 20 and 1000C3, The freque-cy
tanoe. at 1.04
deDendence of the electrical resis 108
was obtained, usin,,~-- the apparat-us shown schemaTic-aily
in Fig 2, This apparatus included a high-frequency
oscillator coupled by T to a circuit which included a
xralve (tube) voltmeterIKV). r-esistance of the samples
was deduced from their losses in a cauacitor C,. The
.thermoelectrit~- power of pure amorphous selenium was
measured using the apparatus shomm in Pig 3~; this
apparatus included a potentiometer and a ballistic
galvanometerGj ., The thermoelectric power of amor;Dhous-
selenium with'.Lodine was measured in the usual wayc. The
electrical conductivity of pure, selenium and selenium.
Card 2/6 with: 0.5, 1, 3 and 5% of i.odine at 200C is given

29
i,;le ctri~;a IProperf;ies of Amorphiaus Selerilui.,i with Iodine Impurity
t -pure
in Table 2. The elec rical ionductivity of
amorphous selenium was of the order of 10--12 ohm
a-1, 200C and rope rap'-dly Yn inUroduction of iodine,
reaching -10-0 ohm:-I =- when 551 of iodine was aclded~
Table 4 shows that the frequency of measurement, affects
strongly -~he val-up, of the resistance of the pure amorphous
selenlum and amorphous selenium with iodine. The
resistance of both pressed and melted samples decreases
,-ure dependence of
strongly with freqaenn-y, The temperat '.
the eleiztrical conductivity of amorphous selenium with
iodine is given in Ta bie. 5*, It is found that the
conductivity of selen.11-im witr, iodine increases fairly
rapidly with temperatu're, in r-ontrast to the
(-.onduc.-!:i,rity of crystallite hexagonal selenium, which
ri.ses only sligbtlly on. heating. It is dif f i"1 It to draw
final. conclusions from -t7he temperature dependenl-.e of tue
electrical conduct-ivity since crystallisation of
selenium cccurs 0_u.ri_P_F, t'L,--e process c-f measurement. The
room teapera-'Gure elec.".-rical conductivity was found to
be 10 to 1.00 times higher afi:ar a series of measurements
te per -f the e-eci-rical
a rd 3/6 of the mperat~.ire de- idence o T,

GOV/ L --~S
Electrical Propertties of" Amori~hcus Seien-luia- wi-~~h In-dine T-I)Durlty
conductilrity, CcAParison of t-lae elecrric~a'L
c.oxnduc,-Ii-fity of selenlum samples prppared by pressing
and those prepared by melt-Lng ir, evacuated se a!-_ d
ampcules showed uhat tdiel:r iri-~Ial properties w-are of
t he s a me ord e rThe t h e rmc e. r r.1 C.,;, r. C,,~V _ r a V,,a S aS C,
puve q..-acrr4bciu; s ler~ium it was equal t. o
measured.; for SE'
1,1 utWdeg.. The. tc~mperature of tlie thermo-
electrin, -oower a vias obt-airie-d- fc."r sampleaof amrxrphous
selenium vitlb ]AX-dine., The. sligri c-,f the thavipo,~ le. et ri!:7,
power indicated flia~- pu.ve scl-~111-11j"-L az).d seli~11-ium~with
iodine havi, holg c-,DjjduC-tJ,?-Jty, -crvsul~.-s CA
measu-r.-emeti-f-, of th-10 !dte rmoe Irzcbr-i.,~ pciuver at va-rious
tempex-atures glver- -~.n Talbl,-:- 6- (Ii-n Wde-) ,vh-L--h
in~~ludes also the --ral-aes of the c~arrier density u
(i.n Table (-, shnlz~-~vs t-ti-at- ~--],ie of a are
1.1- to 2' times higher in armorohou-- s6lenium wlit--h i-odine,
thar. in crystalline seleniuui w-.L'v-','l siuilar amoarlr-s Of
iodine at the, same temperat.-.,xe-, Tab-le- 6 shows also that
tiae -Ialup of a decreases anu -h-rit, c--f n -Lncreases vith
Ca --rd 4 /6 temT)eratuxe- This Qi-e r.esults o1jt-ained by

C'.1
W
V/1' 59-58. - G - 1,129
-:electrical Propexties of Amorphous Seleni'um wir-h iodine !MT)Uirity
other authors. VFnen measurements of thermoelec"UrIc
power were repeated at room temperature after tests at
higher temperatures, the initial value of a was never
obtained.. The following conclusions are drawn by the
authors: (a) amorphous selenium is a semiconductor and
its properties are -retained when it crystallises because
the properIties of crystalline selenium are governed by
its short-range order, (b) if it is assumed that. in
--eneral, the Properties of crystalline and amorphous
selenium are similar, then the laminar structure of
selenium is confirmed by the observed frequenc-
y
dependence of its electrical resistance, weak binding
of the halogen impurity with the selenium lattice and
considerable decrease of resistance of selenium or, thE
addition of iodlne- There are 3 f1gures., 6 tables and
10 refere.-Lices of which 7 are SoViet, 2 are translations
Card 5/6

-Li/29
Electrical Properties of Amorphous Selenium with Iodine 1 m7p u r-
from English into Russian and I Dutchl,
ASS O'C' TATUI ON : Yayevskcly Politekhnlcheskly Iu3ti tut (Kiye
Pollytechnical Instit,.Ae)
8GBhd vD-. 29til IiIarc 1958
card 6/6

5=
ROMMICH, V. M.

A!Y~HOR: Romankevich, Ye, A. 20-3-27/46
TITLE: Orginic Matter in Bottom Sediment Columns From the North-West
Part of the Pacific (Fast of Kamchatka) (Organicheskoye veshchest-
vo v kolonkakh donnykh otlozheniy severo-zapadnoy cha3ti Tikhogo
okeana (k vostoku ot Kamchatki)).
PEHIOLICAL; Doklady All SSSR, 1957, Vol. 14.6, Nr 3, PP. 447-450 (USSR)
ABSTRACT: The clarification of the quantitative distribution of organic car-
bon (Corg) of the humic and bitumen substances, as well as of the
vegrt*tal pigments in the bulk of oceanic deposits.is of importance
foi- the detection of diagenesis proceases, the conversion of the
organic substance and the redistribution of individual components
of this substance in-the deposits. The author investigated 29 co-
lumns of these depositions, 2 to 12 m of length, taken from the
expeditionary vessel "Vityaz's, from the district near Kamc 'hatka,
the Komandoren- and Aleutian islands. These specimen come'from the,
continental slope, the deep-sea depressions and the bottom of the
ocean from a depth of 3 to 7,5 km. The luminescence method was
applied for this investigration. The sediments are formed of car-
bollateless (0 to 2d1o CaC03) loamy and aleurit-loamy muds. Their ,
top horizons contain a increased quantity Of Si02aut and are lo-
Card 1/3 amy or poor flinty diatomeous muds. The moisture content decreases

diganic Matter in Bottom Sediment Column From the North-West Part 20-3-27/46
of the Pacific (Last of Kamchatka)
slowly from 0,2 to 0,5 m on the bottom-surface, in greater depths
it increases and attains, or exceeds the content on the surface
at various depths. The quantitative distribution of the organic
subs'Wice was very similar with all samples. The content of bi-
tunlinous matters 2S very Poor up from 0,8 to 1,3 m and is about
the saiae everywhere. The quantitj of both the bitumenland the
humic acids increases with the depth of the water. The orientat-
ion of the convertion processes of bitumen was disclosed by a
lui-ainescence-analysis: Both the oil- a-zid resin-cotent of bitumen
increased with the depth of the water, whereas the asphaltene W
content decreased. The content of green pigments decreases with
the de-ath. Since with all samples the horizon containing a MaX3.-
muni ofCorg, is also enriched witn clorophyll and Si02aut, it
be conclu ed that the diatomeous algas trere the main supplier of
tht! organic substancefor the depositions. A sediment-layer en-
riched with bitumen was discovered by means of the luminescence
analysis. Further examinations have shown that this layer also
cortains increased quantities of humic substances, pigments and
Corg- This horizon can serve as marking with the stratigraphical
arrangement of the sediments..There art! 2 figures, 1 table,and
Card 2/3 3 Slavic references.

0-,-~~-,nic Latter in Bottom S~diment Column From the T-Torth-West vart 20-3-27/46
of the: -COICII Ic (East of "umchatka)
As~~ OCI..,q, 101,
institute of Oceanology of ANI USSR (Institut oktanologii Aka.de-
uiii aAak liSSR)
P-R S- ENT D Julie 14, 19571 by S. I. IAironov, kcademician
S J -Bi,i ITT E.Ij Jmir,! 6, 1957
A A I LA 3 L H'. Libr-ar'y of Congress
Card 3/3

AUTHORt Y4~ A. 30V/20-124-6-34/55
TITLE-i Pig and of Vegetable Figments in the
Sedimc-ntg o~if the N-:-r+h-wes-;I-er-i Part of the Pacifi-,
East cf
~
Kaw~hatks (0 S~-s'+,q.Te ~ raspT adelebJA rasti-tel-'nykh pigmentov.
s4~venl~-zapadnoy chastj. T-ikhogo okea n~a IC
Kam,-qatk~.'
PERIODICAL~ DAI.ad- -1305- 308
Akad.emi-- na:,.ik SSS.R,. 19599 VsI 124, Nr 6 pp I
(ITS-SR

ABSTRAM, ts em'osAded 'n b-:)t'om sediments are presently
The pigmqn
o-~;:154de]~~Md as por: --:ne S-i rnes of o-*. A great significance
-Pily'rL
at-'--r--!Iuted +o-~he as indica-tors of the source
!na and c-~;-.id-'I.tions of bitiamen genesis in,

ks and o.CL (Refs Moreover
the chlorophyll-like
?
P-r,-ld-octo i-n The sediment are indi-.ative of the quantity of
Eza-?ily nouxishmeiit. fini:lusive of vitamins A and B)
-t.He fa-,)-na. The author has studied the.
pr-~b-,eir s-'nee 1955
(expedit4-)n ship "Vityaz""). This study was
4
-qe laborator.;:s of the Kafedra geologill 1
/4'
Card -sk-;payemy1ch. M,~akovskiy gosud.arstve
r-'3,3rY

Tile Compos-* F~ad DI s t~ ~ln c.f Veqetq-I~-'--e P-'~ajTie ilts SOV/20-124-6-34/55
-ii the Sed-imen~s ~;f Pa-.:t of the Pac-Ifiog East of Kami:thatka
4
urdirersite-t i,Cha-..r ef G-e-Ilogy and Geochemistry of the Fossil
r--G-Is :)f M-,s:2ow S4-ats Ur1-!-.rersI.ty) and -the Vsesoyuznyy nauch.10-
j:szledo-~Ya Tel' skiy L7.eL,-,-!-~g-.-...-razvedoch-oyy neft-yanoy institut
(AlL-Un:Lo-.i Petr:,Ie-m Research Institnte for
Su.rvey). The pigments were extracted fr-~,m sediments
of nia-~ui-a-. moist'Ir.-z cl-nten-. with a~,etone and alcohol ac:etone.:
The avaounts --f chl.-~rophyli and phaeo.)phytiln were determined on
a phot-meter wlthouz separation. The qualitat-i"We
c-,~-rjtent- of t1hia pigments and the carotene content were
as~ert-a'.aad by chrematog
_~raphy on paper. A total of 66
quan.t`'ta~i-re deterzinat--ocns of 3hlorophyli and carotene were
:arr~,P-d. --;vkt. Th-~ ws-re determined in the uppermost,
sediment layer% a- and d-,. chlorophyll, phaeophytill
'.apparen-,.Ly a;, oar.,Aane, lutelin, fucoxanthin.. All of these
P�,gmelrks ~With Fhe ex,-eption of Dhaecphytin) are charasteri-stic
of the -;)j.gme,-at systv-m of living dilatoms,. By
Ih'q +-he Promin-~---IT r~- --~ the diatoms in the formation of
L
:,rean~n, si--stanc?s 3f "no bot~~om sediments in this reE:Lon Is
prc--e,,;~ 11-1a~.tered OCCULrS in the depths from 130 to
fn 'L~P-7 6'.)* '- I - phyt-In
00 M 00rd-na.'r-n amc-ints compared with phaeo- L
Card 2/4 Frodu~,t -,~f the first oxi'dation stage).

The Compos-)'.-tio-ri a-rd- of Velgetable Pigments SOV,/20-124-6-54/55
~-i the Sedimen~.s c--r i~- 14,i,.rthwes,Lern Paxt of the Pac4fic,-. E
a-st of Kamchatka
Theref----, the o-rgan4c substance wae oxidized during the
'tse--
-.nk:!.rk- ~f the Par~icleB as w--~!! aa 3.n. the sed-4ment I f.
F-,~-)m the mwa tFI-P :+
I . IS eirpare-Ilt that the highest pigment
are z:, be f-.;und in fine grained muds on the
DTA Pm' C ".1. 5,1 -e 119-.Lt:17e).Y
near the coa t (500-4200 m deep)
q a 4. n t h e -Z, s I&S - ic- nof the :-ontinental shelf (30-200 m deep)
the pigmear ront-~-a-~ 4-9, h.igh~ The phaeophytin and
~~arolsne :~on+enr sinks to rain-imum values in the deep sea
ba!s.-.re m' a--ad the -~,-~ean bays (depths of 4600-5600m).
M
Ih.Lt~ inay at."~-r--'buted t.:) t1ne impover-,shment of i)lankton in
T-Zese wh-;sh -s -.r2s--wTd as the chief source of the
th"
kzmcs nt -s .. Al s-,~ a+ zlhe trarsition from fine sand to I~Lleurol-
ard .'.-~~-vey wad, 'ae~~e -c-a-ralle-A T*-~-, the increasing depths,
and' f-nri aa inc~,easingiy small percentage .
t)f -,-hs i~,rganic substan,,e. The: piginents, a.re destroyed during the
5-aking ,,f the pa-,-*~i~ea~ Stabler humin and remnant organJIC
ma~i.~-~al.- a-.~avilat-2 on the bottom (Ref 9). Tab-, 'e I shows the
phac--,phyt.w'.~% conrten-s in the basai parts of the cores. The
of +he ae-diment has a de~iisive effect on the
preser--;-&.t-J,-,n bhe plgment~~,

The Compositit)n and Distribution of Vegetable Pigments SOV/1420-12~,1-6-34/55
in the Sediments of the Northwestern Part of the Pacific,. East of Kamchatka
If oxidation conditions during the sedimentation of
prevaL
1.5 - 2 m of.sed1ment, only small amounts of phaeophytin can
be -transformed ii1to the fossil state, compared with its
orig4nal content in the uppermost sediment layer. There are
I figure, 1 tableo and 10 references, 6 of which are Soviet.:
ASSOCIATION:. Institut okeanolcgii- Akademii n-auk SSSR
(Institute of Oceanography of the Academy of Sciences, USSR)
PRESENTED: November 4,. 1958, by S. I. Mironov, Academician
SUBMITTEDi No-vember 4, 10,58
Card 4/4

ACC NR: AR7004108 SOURCE CODE: UR/0169/66/000/012/V029/V0330
AUTUOR: Romankevich Ye. A.
TITLE : Distribution and structure of organic matter in the surface layer and thick-
ness of sediments in Pacific Ocean area
SOURCE: Ref.. zh. Geofizika,. Abs. 12VI75
REF SOURCE: Sb. 2-y Mezhdunar. okeano'gr. kongress, 1966. Tezisy dokl. M.
Nauka, 1966, 329-330
TOPIC TAGS: . oceanography, hydrolysis, organic substance, precipitation,
bituminizing substance, humic acid
ABSTRACT: On the basis of more than 2000 determinations of organic substances,
an oceanographic chart was prepared showing the distribution of these substances
in the surface layer of certain sediments in the Pacific Ocean area. The nature of
changes in the quantity of organic substances in the sediment is also explained. The
conipositional variability of organic substances (such as readily hydrolyzed and
bituminized substances as well as humic acids) was investigated in relationship to
their remoteness from the dry land in Central Pacific Ocean area. [KP]
ODE. 08/ IrEranslation of abstract7
UDC: 551.-464-.7:551. 35_(265/2G)

ROMANKEVICH, Ye.A.; PETROV, N.V.

Papers R'bltud for INA Nctle 31cism. Congrasa, Nonald P.-I 1 .21 A-c-
6 Sep MI.
Zzstt~-ta of C-elarr - "Me5024W deprea5lOns &nd troneha
f .44, As-&--- %T;* and tbetr postUo. In the syatct~ttcs of tlatcolt
0, a, (S~-Iza
Ywscc~ 3- ma UnIvers' ty, ?nysjc%! razujtT - -7h. pr=--ray
of &rA.Lficial mdlcactif-rity In up;er 1.7ers
of the ccessol
~- ~l T. 0., ztbatr of Forestryt Tht ArXicultursl. Acadt=Y i=ent K. A.
~VlJilijWZ-r~- ~Forts- ll~ restarth an.1 mithcdz of fire ccntml.* (Station V,D)
'R ~,tx . A, Z=I-Ittt of Oc.snol.Q, ani
-rPbQ-!zj;L!s.! R=AZT-19 of reprodaztL.n nod of fl.-flah
In nf PNoMe" (3-:11cl Itt.r)
t- of O-nncl~rj of the hori-ont-1
turbe.le-vt I. the Paaci^t. Oe=" V11.0)
O~e& In the Cccr.Aphtml
"I.ar -
di.trit-trttra of r_yt.G flb.2 in the Pacific O~enri* 71E.C)
of Go I ,- M. h~ri%-, I. the
0 ~I7
r=-,hatnn" (5*-.
ereta,ct
y . "Thi ;rv-sats of mccnt aqdt-
lnv.1 tle cf Occn.lor
r-, Ica in -be -ttern ;drt of t o ej-W..rt-4 -e I,, t" Puift.'
(Secucz *.,=.--..)
Institute uf Eorth 1~4etcn ,-1 0. Yu. 3doi4t
~Tl~e sel=ic =ditlcna Ll the acrth~lvt-.- cutl7i.IC sZeft
If t~l beaLn* (S-ttoa VIT.C.2)
of Oeeencl.Cy In
P.:- of -!~4 Pwific" (Section TUX) 7
Zzs---.V~te of Z~--c7 'Thi -'b1 ~~ .1 the Dering 1~nd
tL. polrt
"am.
zoa-tut. of
in th- C!' the earth Wt of thi Pwific be- (Section 711.0
TM Stott UnivereLty, F-Ulty U.~
de,--ce for -M.- coxrstt, Owu,)" lu*tlon M.3-0
ILA -A., :nCtitirte a' Ccolocy - 'On t~w a-AblUty md
If C-oneato I. the rr- of the fteLfIc Oceen
dprea.lca* (:--et.Lcz 'r-C)
?A=. T. ;~ m,,? Zallltu.. of
Oc~lc rq7uL~[-Hga U--inL;Yrd- to repr-ucticn vid
da"le,Q. t In the mr-Own% pert Of the rezirlt,
of Cce~lcl~a - "Oreante smb.tmce In
'art of the Poetlic,
:~-,-t.te f Zarth M7:ita 1-Mi 0. Y- 3c.'=It
t~-!- in -e -3-ero ~-'. of
d!.p fc-3.0arth,
f n.lxt e~~a-t`
VnLler.tt~-- ~,, F-4ty - '-.he
--tt na-le in-let Ao a
1
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.ta 1, LlervLty, My,l,al
Uca
neth.d C~r vli-el= (See' I.. VTI.C.2)
of 0-01.a - "Thi dl.lrtl,,tj., or b.tt~~
(~C~f the F-jfjc ned L-a z~ for
the -.A!:AZLa4 ~t
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:c=At.-.z z: the in "~ =J oce-v*
on I n of o
Ta -~ t th
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of F.re-lf~r% .1 Y-l.tw
of -Jqj~lle -d 1. the
il.st- ~:t (a-ct,- llrx)
:n5tLta.- f
im-l 0. 5th-idt
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0,11 e 1-- "See,1 4
Studie. of
A-t&r-- za- ~Stt-,-a
'YX=-. :;. :;.. Zr
5 cf Ce~-nnol~r~ - "Y~thedz 'or deep
V-~Z- re rtsulta ~f th.-Ir epilLcoticn In the
?~I- .3 - ,.he et.- =d a.
-C C--~ (Seetten

-m
BRI)NIUV,Ilyux-v7a Muchkayevich; VII&INKIN, II.Ya.. I)rof., retSen2ent;
NAZAREVSKIT, G.A.. uchitall, retsonzent;_RPRA uchi tel I.
ff,114
retsenzent; OBUKHOVSKAYA. U.N., uchitell, retiahzent; MOLCHANOV,
M.P., red.; KREYS, I.G., takhn.red.

2

LOMISADE, Yu.14. [Lomsadze, IU.M.]; KRIVSKIY, I.Yu. [Kryv51kyl,
ROMANKO,..G.D. (Romanko, H.U.]
POSS4bility of specific interaction L-etween, r; -states in the quantum
field theory of the probability amplitude. Ukr. fiz. zhur. 8
no.12:1,111-1312 P 163. (MIRA 17;4)
1. Migorodskly gosudarstvennyy universitet.

ACCESSION MRs AP4010405 3/018 5/6 3/009/022/1304/1322
AUTHOR: Lomsadze, Yu. M.i "Valky*y, 11. Yu.;.Ramanko. G. D.
TInSt On the possibility of a apealfla Interaction betomen the-B-states in the
quantized probability amplitude field theory
SOURM Ukrayinalky0y fit. zhurnal, r. 8, no. 12, 1963, 1303-1312
TOPIC TAGSt quantized field, probability amplitudes quantum mechanics, quantum
theory. quentum, E-state, 0-state, $-matrix, 3-operator, wave function, interaction
Hamiltonian, Hamiltonian
ABSTRAM This article Is.& continuation of work by the authors in developing the
quantized amplitude probability field theory. It Is shown that two types of
interaction Hamiltoniana exist In the framework of that theorys Those of the first
type, corresponding to absence of interaction among the 3-states entering into
G-states, with any arbitrary degree I a 1, 2, 3,.... of the internal chaotic states
for characteristics of processes usually observed experimentally# lead to the same
results as conventional quantized field theory and therefore cannot determine the
value of the universal constant I realized in nature* Those of the second type#
which have no analogy In quantized field.theory and.uhloh correspond to the
Card 1/2

.ACCESSION NRt 04010405
occurrence of a specific Interaction among the R-statee belonging to one 0-state,
in addition to Interaction of the first type, lead to physical effects wbich depend
on the degree I of the internal chaotic state of the particles 1 that degree can in'
principle be experimentally determined* Since the effects are small, they can be
observed only after a substantial increase In experimental precision* It probably
will be easiest to detect thea In processes of particle decoy* The authors are
cordially grateful toProfessor Ve Le Donch-Bruyevyooh for valued stimulating
remarks and also to Yeo Vo Kyoryoohuk and Sh. Sh. Kazinets' for aid In making
certain caloulationse Orige arte has& 21 formlase
ASSOCIATIONs Uzhgorodsky*y dershunivereyotot (Ushgorod State,univeIraity)
SUBMITTEDs 031ay63 DATE ACQt 2OJanG4 ENCLi 00
-SUB CODEs NS xo Rzr soys ooe 07=o 003
Card V2

VAIIIIII D.Ye... ispolnyayushchiy obyazannosti dotsenta; ROMAN'K0, M.D

GRACideNj V.V., Geroy Sotsializiticheskogo Truda; ROMANKO, M.D.
On the YalinovIra Village Collective Farm. Zashch. rast. ot
vred. i bol. 7 no.l:/+-7 162. (MIRA, 15:6)
1. PredsedatelIkolkhosa mmUKalinovki Khomutovka (for Grachev).
2. GlavnTj ar.,,rono-.i kolkhoza sela im-Linovki, Khoumtovk-a (for
Romanko).
(Khomutovka District-Plants, Protection of)

R-Im
ROIGUITKOJI M.Ye.; ASIPOVICH, A.N., inzh.
Use of tracklaying cranes for current repair work. Pat.' i put.khoz*
7 no.8:26 163. 0-liFu 16:9)
1. Nachallnik putevoy mashinnoy stantsii No.22, stantsiya Kalachins-
kaya, Zapadno-Sibirskoy dorogi (for Romanlko). 2. Stantsiya Kala-
chinskaya, Zapadno--Sibirskoy dorogi (for Asipovich).
(Railroads-Tracklaying machinery)

A(AVCRONKO, N.M.; ROMANKO, P.G.
Basic trends ol" the scient4fie studies It, the field of mass
transfer processes of chemical technology. Khim. prom. 41
no.2.,1-4 F f65. (MIRA 18:4)

further experimental and clinical studies of the effects of the
preparation farcoven (with surmary in Ahglish. p.61-621. Probl.
gemst. i perel. krovi 3 no.1:21-24 J&-Y 158, (KIRA 11:3)
1. Is laborstorit sukhikh preparatov krovi (zav* - prof.
Bogomolova) I gematologichaskoy kliniki (sav. - prof. 5.1. Sherven)
Uningradekogo ordene Trudovogo Krasnogo Znamenl 'nauchno-iseledovatell-
skogo instituts pereliventys kroyl (dir. - dotsent A.D.Belyakovo
anuchiVy rt*ovoditall chlon-korrespondent AKH SSSR prof. A.M.Filatov),
(MV, therapeutic use.
saccherste.. anemia (Rue))
(AINKIA, therapy,
iron saccharate (Rue))

S -a
EXCMPT.,% MEDICA-ec.6 Vol 21, or.M~:d. Jan 195
a
353. PARENTERAL TREATMENT OF HYPERCHROMIC ANAEMIAS WITH
FERCOVEN. (PRELIMINARY REPORT). (Russian text) - Romanko, T. A.
KLIN. MED. (Moak.) 1957, 35/1 (5--63)
Fercoven. an Fe compound containing saccharose and cobalt gluconate. was
administered during 17 days to 34 patients suffering from various hypochromic
anaemias (posthaemorrhagic anaemia, Fe deficiency anaemia). A total of (on an
average) 1700 mg. Fe was given per patient. A reticulocyte response and an in-
crease of the blood values was obtained in all patiints; 12 transient side reactions
were encountered. Siurala - Helsinki

ROKANKO, T.A.,(Leningrad)
Parenteral infusion of forkoven in the treatment of hypochromic
anemia of varied etiology; first report. Klin. med. 35
no.1:57-63 Ja '57 MRA io:4)
1. Iz gematologicheskoy kliniki (zav.-prof. S.I. Sherman) i
laboratorii sukhikh preparatov (zav.-doktor meditainskikh nauk
L. G. Bogomolovaj Laningradskogo nauchno-issladavatellskogo instituta
perelivaniya krovi (dir.-dotsent A.D. Belyakov, nauchnyy
rukoyoditell-chlen-korrespondent AMN SSSR prof. A.N. Filaroy)
(ANFMIA, HYPOCHROMIC, ther.
gluconic acid cobalt & sucrose iron prep.)
.(GLUCONATES, ther. use
gluconic acid cobalt & sucrose iron prep. in
hypochromic anemia)
(COBALT, ther. use
same)
(SUCROSE, ther. use
sucrose iron & gluconic acid cobalt prep. in
hypochromic anemia)
(IRON, ther. use
same)

3 '~ 5 )
AUTHORS:
T IT LE:
PERIODICAL:
ABSTRACT:
Card 1/3
Barkhatov, B. P.,Miklukho-Maklay, A.D.V SOV/20-125-6-37/61'
Romanlko,_Te..J~.-t Tairov, E. Z.
New Data Concerning Permian Deposits of the J,-orth- Pamiru (flovyye
dannyye o permskikh otlozheniyakh Severnogo Pamira)
Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 6, pp 1303-1306
(USSR)
Permian deposits characterized by their fauna predominate in
the northern and south-eastern structural-facial zone of Pamir
(Ref 1). The stratigraphy of~the Permian deposits in thesouth-
east of Pamir could be precisely defined in the last years.,by
investigations of the Upravleniye geologii i okhrany nedr.pri
Sovete Ministrov SSSH (Administration of Geology and Protection
of Mineral Resources the Council of Ministers of the USSR)
as well as of Leningradskiy universitet (Leningrad University)-
New Permian exposures were found in addition. The separation,
of the individual zones is indicated (Refs 1,4,5) (see Scheme
in Fig 1). On the strength of a tectonic and paleontological
analysis the authors draw the conclusion that the stratigraphic
position of the so-called "Violet" suite (earlier ascribed to
the ctntral part of the Lower Permian by Y. 1. Shabalkin) has.

New Data Concerning Permian Deposits of Northern Pamir SOV/20-125-6-37/61
to be revised, The "violet" suite, wldch contains Upper.Permian
fauna in the conglomerate, is obviously bound to have.a strati-
graphically higher position; it is, however, as well possible
that these deposits belong to the Mesozoic (Jurassic, and.even
Cretaceous)_, The detection of Lower Permian fauna in the rocks
of the northern metamorohic zone of Pamir indicates the uniform-
ity in the geological development of the entire northern.zone
during the Paleozoic and Mesozoic or at least up to the Upper.-
Permian. The southern boundary of maximum downwarpings in the
Upper Paleozoic is distinctly marked; it is in accordance with
the southern boundary of the Darvaz-Sarykol lower zone, Thus,
the development of the northern branch of the Pamir geosyncline
in the Upper Paleozoic was better determined. There are I
figure and 5 Soviet references.
ASSOCIATION. Leningradskiy gosudarstvennyy universitet im. A. A. Zhd anova
(Leningrad State University imeni A. A. Zhdanov) Upravleniye
geologii i okhrany nedr pri Sovete MinistrovTadzb-v-~ska,~-- S5--R
(Administration of Geology and Protection of Mineral Resources
o" the Council. of Ministers of the Ta~aeiL-~:SSR)
Card 2/3

S,/191/62/000/009/004/012
B101/B144
AUTHORS. LIvov, B. S., Panferov, K. V., Romanenko-z,-I--G-,-,_ - -----
Shpakovskaya, Ye. 1.
TITLt;. Chanyes in the physicomechanical properties of glass-reinforced.~,
polyester plastics.due to water
PEMODICAL: Plasticheskiye irLassy, no. 9,,1962, 16 - 18
TEXT: Lon6er immersion in water had the following effect on the physico-
mechanical properties of glass-reinforced plastics (GRP) which contained
35-40~ 411-1 (PN-1) polyester resin as binder: (1) Reduction of tensile
strc.-nj.-,tb and,bending strength depended on the type of glass filler. After
6 months' immersion in water, the tensile strength (in % of the initial
value) for GRP with rope glass fabric was 62-5,.withr-I (T-1.) plain weave
glass fabric 68.0, with staple glass fiber 55-9; the bending strength
dropped to 44.0, 66-5, and 35-1, respectively. (2) When T-1 glass fabric,
was treated with the organosilicon rbc-g (GVS-9).Preparation the tensile
strength of GRP after 40 days' immersion in water dropped by only 7.6,
the bending strength by 15-6%, while the corresponding values for GRP with
Card 1/2

st/191/62/000/009/004/012
Changes in the physicomechanical ... B101/B144
untreated ,-la3s fabric viere 12-5 and 61.8. (3) Result of the comparison
bo tween PN-1 resin and 9+6-1 (VFB-1 ) phenol formaldehyae resin as binder;
After 6 months' immersion in water, the residual tensile strength was
83-4, for GRP from T-1 glass fabric and,TH-1. (TK-1) resin, the residual
Z; -I
binding strength 68.21~, the modulus of elasticity in tension. 65-85f, the
modulus of elasticity in bending 33-67", while the corresponding values for
VFB-1 resin are 85.2, 77.9, 61.0 and 73-7. (4) Effect of the thickness in.
the case of GRP from T-1 glass fabric and TN-1 resin, after 6 months'
immersion in watert For 2.2, 5.0-5.2 and 10.2-10.8 mm thick GRP, the
residual tensile strength was 68.0, 83.4 and 81.2~,, the residual b6nding
strength 66-5, 68.2 and 69.8%, the residual elasticity modulus in tension
63-7, 65.8 and 65-TPI and the residual elasticity modulus in bending 26-7f
33.8 and 57.4% of the respective original values. There are I figure and
3 tables.
Card 21 12

S/191/61/000/003/009/015
B120203
AUTHOR% Romanenkov, I. G.
TITLEi Effect of storing in water on the anisotropy of strength and
deformation properties of glass-reinforced plastics
PERIODICAL: Plasticheskiye massyj no. 3, 1961, 44-48
TEXTs The present paper gives results of experiments of the influence of
storing in water on the anisotropy of strength and deformation properties,
(under stress by pull and-bending) of glass-reinforced plastics., Specime .no
of seven industrial and experimental materials of Soviet-made structural.,,.
glasa-reinforced plastics on the basis of various binders and glass
fillers were tested, i.e., among high-strength glass-reinforced plastics9
glass Textolites with Butvar phenol (GI-3 (BF-3) and b!FF-1'(VFB-1)) and
polyester (nH-1 (PN-1)) binders. Specimens from three experimental lots of
glass-reinforced plastics on the basis of glass mate and phenol binders;
as well as a glass-reinforced plastic of the Glakrezit type, were also
tested, Binders used were the water-resistant varnish P-21 (R-21) and V/
phenol alcohols subjected to moisture. Two lots of glass-reinforced
Card 1/9

B/191/61/000/003/009/015
Effect of storing in water- B124/B203
plastics were made by the method developed by I. P. Berkovich and
A. R. Vitenberg, co-workers of the NIIPM, and one lot by the improved
technology of the VNIIS. Glass-reinforced plastics of the Glakrezit type
were developed by B. S. Ltvov and Ye. M. Gromakovskiy, co-workers of the
VNIISV; they consisted of alkaline glass mat and the phenolic binder
K-6 (K-6) with 30% alabaster. The effect of moisture on the physico-
chemical propert-Iles of glass-reinforced plastics was established in
longitudinal, transverse, and diagonal direction; the effect of prolonged,
storing in water on the anisotropy of strength and elasticity of glass
Textolites made of non-alkaline spun glass of brand T (T) was studied in
the direction ofthe warp, of the filling, and under an angle of 450;
that of materials with glass mats made of drawn alkaline glass fiber
"21p) with starch size (10-12%) oriented at an angle of 1 50 to the
longitudinal axis was studied in the longitudinal and transverse direction,
0
and under an angle of 415 . The effect of moisture on the physicomechanical
properties of Glakrezit- was studied in the longitudinal and transverse
direction. Specimens for the tensile test were taken according to
POCT4649-55 (GOST 4649-55), those for the bending tests according to,
GOST 4648-56. Table 1 shows the effect of storing in water on the
Card 2/9

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S/191 61/000/003/009/015
Effect of storing in water... B124 203
Legend to Table 1: Decrease in tensile and bending strength of glass-
reinforced plastics after storing in water. (1) Brand of glas
reinforced-plastic, (2) binder, (3) filler, (4) volume-weight, g/cm3,
5) thickness of specimen, mm,.(6) type of test, (7) structural direction,
glass Textolite KAC-r(KAST) of the "Karbolit" plant, (9) glass
Textolite KArT B (KAST-V) of the "Karbolit" plant, (10) glass Textolite of
the Leningradskiy zavod sl 'oistykh-plastikov (Leningrad Plant of Lamihated
Plastics), (11) glass-reinforced plastic of the NIIPM (first lot
(12) glass-reinforced plastic of the TsNIISK (second lot), (13) glass-
reinforced plastic of the NIIPM (third lot), (14) Glakrez 'it of the
VNIISV, (15) BF-3, (16) VFB-1, (17) PN-1, (18) phenol alcohols, (19) R-21,
(20) K-6, (21) glass fabric of brand T, (22) mats of drawn.alkaline glass
fiber of equal orientation, (23) mats of drawn alkaline glass fiber of
varying orientation, (24) glass mats of alkaline composition with powdery
filler - alabaster, (25) tension, (26) bend*n , ~27~ warp, (28) filling,
I g
0
(29) angle of 45 , (30) longitudinal direction 31 transverse directiong
(32) t, kg/CM2
150 to the longitudinal direction, (33) strength limi I (34)in
initial state, (35) after storing in water, hr.-Note: The ratio of the
strength limit of specimens stored in water to that of control specimens is
given between parentheses (in
Card 6/9
100-

S1191 61/000/003/009/015
Effect of~storing in water.... B124 B203
CHINKCH"e MOAYAM YI)PYrOCTR cT.expopAncyoxos tipm pac-fqme)jmm wirmde noue swAepmmeamms B, sojte
AiOAYJI- Ynpyroml, MrICA2XIO,

BR;r manpameff-
CTPYKTYPMO
G noue
suAep*tfmsux iFsoAe, wm
MAPKa Horo cocrox"Ns Hfinpagile"lle is HCXOAHOK
OCTOR""ll
C
240 384
490 960 21W
CTeKiToTexamiT KACT OIP9CTR,%CIIHe no octiove 20.6 18.0 18.4 17,9 18.0

5 (87,3 .(89.3) (86.9)
(87 3
no YTKY (�r 1
.0 12, U.2 10.25 I

IoA yritom 45-

.7 (83.3)

7.9 (74.3) (68.4
.1
(81,5) (70.2) (53.7) (56.7)
HnO no OcHose QQV 15,5 8.35 - 8.55 8.5 8,0
(53.8) (55,2) (54.8) (51-6)
noyTKY lo.0 4,8 - 4,7 4.4 4.3

mom 45* 0-14
no
6
9 (48.0)
3
2 (47.0)
2
85 (44.0)
2
9 (43 0)
2
8
A y , ,
(33.3) .
(29.7) ,
-(30.2) .
(29
CTepulOTCHCTOART KACT-B GRacramccune f7o oviose 20,5 18.2 18,4 17.85 U.6

IO
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1 (88,4)

10
1
9.8
(8
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(87.0)
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(85.8)
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rIoA ymom 45 8,0 .5.1 4.0 3.1 3 4
'
Card 7/9-
& n0 MHOBC 16.0. (63,7)
13.8 50.o (39.8)
12.4 (42.
5)
13.1

SI1911611000100310091015
Effect of storin g in water ... 124/B 03
no yuk 6.7 4
4 - 4
3 4
4
.

nOA yrnom 45*

16 .
(65.6)

3
6
-
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5 .
(64.3) .
(65.6)
3
1
1
(64,'A) .
(62,5) .
(55.3)
CTCXnO-TeKCTM'IJIT - 11-1 COR3Y.G;l 170 milose 11,5 - 4
7 5
1
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(4' 7) .
(44.3)
yrnom 45
rIOA 4.4 - 2.4 1.85
(53.3) (42,0)
CMAMMICTIM I 1PIMrIM
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16
3
15
1
7.:,
15
(nepBaR nap
nm) nonepewoe 22
0 .
(79,S) .
(74.0) ,
(77.0)
. - 18,7 16.9 18.6 18.9

11POAgnbHM
14.8
8
3 (95.0) (81,3)
11
6 (94.6)
9 (85.9)
. - , .0 1.-

rloil yriom 15'
11 0 (16.1)
(78.3)
(60.7)
(52.7
2
K npOAOJlhftOMY 7.2
(65.4) - 7.7
(70,7) 6,55
(59.5) 6.
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(59
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Card 8/9

S/191/61/000/003/009/015
Effect of storing in water.... 3124/B203
Legend to Table 2: Decrease in the modulus of elasticity of glass-rein-
forced plastics under stress by pull and bending after storing in water.
(1) Brand of glass-reinforced plastic (2) type of test, (3) structural
direction, (4) elastic modulus, kg/cm~,