SCIENTIFIC ABSTRACT KHALFINA, R. - KHALIFMAN, I.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000721710020-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 17, 2001
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

.- KHALFINA""-.
t
Principles of the civil law of the U.S.S.R. and the Union ReNwed,
Vop. ekon. no.2:108-3-15 F 163. (KIRA 16:3)
(Civil law)

KHALFIN, S.L. (deceased) i,,KIMLFINA~ S.L.; DOVGAL, V.N.; KHALFTI.TA,
N.A.; GREBENNIKUVA, 14.1477T0-7
[Petrology of the Kogtakh gabbro-monzonite-syenite complex
(Kuznetsk Alatau)) Petrologiia kogtakhskogo gabro-montsonit-
sienitovogo kompleksa (ftnetakil Alatau). Novosibirsk,
Nauka, 1965. 90 P. (MIRA 18:12)
21
W
M

KRALFIIIA.V.K.
Some middle Devonian Stromatoporoldea of the southwestern edge of
the Kuznetsk Basin. Trudy Gor.-geol.inst. Zap.-Sib.fil.AN SSSR
no.13:75-101 t53. (MLRA 8:12)
(Kuznetsk Basin--Hydrozoa, Fossil)

AKSARIN,A.Y.,- ANANITIV,A.P.; BMWEITOVA.R.N.; GORNWOV.M.G.; PrRATSUNOVA,
R.T.; YNCROVA.L.I.; IVAIIITA,V.A.; KRAYUSKATA,L.Iff.; KRA OPZYXVA,
P.S.; IJKBZDBV,I.V.; LOMOVITSKAYA.M.P.; POUITAY39VA.O.K.; ROGOZIU,L.A.;
RLWHENKO.G.P.; RZHCtISNITSKAYA,H.A.; SIVOV,A.G.; YOMICHNV,Y.D.;
KRALPIR,L.L.; CHEMSHUA.S.V.; HIKITINA,V.N., redakft_~_
GUROVA,O.A., tekhn.1cheskiy redaktor
[Atlas of leading forms of fossils in the fauna and flora of Western
Siberia) Atlas rukovodiashchikh form iskopaemykh fauny i flory zapad-
noi sibiri. Pod red. L.L.Khalfina. Moskva, Gos. nauchao-t-.,khn.izd-vo
lit-ry po geologii i okhrane nedr. V01-1- 1955. 498 p. Vol-2. 1955.
318 P. (Microfilm] (HLRA 9:3)
1. Tomsk. Politekhniehookiy institut imeni Kirov&.
(Siberia, Western--Paleontology)

KHALFINA, VA.
New representative of the subgenns Labechiella Tabe at Sugirame, from
the Ordovician in Kazakhstan. Trudy GIN no.9:229-231 ' 58.
(MIRA 11:12)
-..0 ~ -
1. Tomakir-rAftakhnichaskiy institut-t
(Kaz;~bat'an--Lamellibranchiata. Fossil)

KHALF AI.K.
Stromatoporoids from Cambrian eediments of fiberia. Trudy
SNIGGIMS no.8t79-83 160. (MIRA 15s9)
(Siberia-Stromatoporoidea)

KULIFINA, Ye- N-
,&ttempt to develop a new method for treating sta=ering in childrau
of sahool age. Trmdy Inst. fiziol. 7:285-295 158. (KIRA 12:3)
1. Iaborstoriya vysehey nervnoy deyatelinouti rebenka (2aV. -
V. 1. Krasnogorskiy), Institutix fisiologii Im. I.P. Paylova, AN SSSR.
(STAiMING) (CHILDM, ABNORML #HD BAGKWARD)
(RM43DILL TICAGHING) -

nnovicht; BREMys K,,H-,retaenZentjj,KgA?j#R! A.K-t
TSUKUM", Illya Ica jjTZDT. B.3,9..red.; SOBWVA, Is. M., tekhn, -r-a'a-.
re tsenzent . ;BONS
vision] FIektronnaia oPtika v televiderdi.
[Electron oPtIcs in televo, 1958. 247 p. (MIRA 11:12)
Koskva, Gos. energe izd-
(Ble ctron oPticG)
(Televisfon-Picture tubes)

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L~' _9 -~. I /I , -1, 4 ~ ", 'OT I., IC /Y
KHALFOH, V.I., inzh.
-- - ------------ F-
Using the attribute system In programming the calculation of
complex sections with double-address digital computers.
Vest. mashinostr. 45 no.lt29-31 Ja 165. (MIRA 18j3)

.CH
2. ussp (600)
4. Tractors
7. Wrability of driving gears of tractor KT-129 Vest.rash.32 n0-11, 1952.
Monthl List of Russian Accessions, Library of Cong-ress, Apr;l -1953, Uncl.

PETROVA, K.G., kand. med. nauk; ABDIYEV,N.,- KHALIDZHANOV, B.
Thromboembolism of the major Vessels in children with toxic
diphtheria of the pharynx with hemorrhagic syndrome. Pedia-
triia, 42 no.8391,-95 Ag'63 (MIRA 1794)
1. 1z kafedry detskikh infektsionn7kh bolezney ( zav. - dotsent
T.N. Nikanova) Kazakhskogo, meditsinskogo institute i Detsko7
klinicheskoy infektaionnoy Bollnitay No.2 (glavnyy vrach F.S.
Sakova) p Alma-Atao

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)424. SURFACE ACTIVITY OF LUBRICATING OIL Ai)I)ITIVkZ Khalif
A. L. (Nortyanoo Khox., 1946, U, No. 11, 50-41 Chem. Ab
Ali )94
0 4 Monpuremonts are rerorted of the surface tonalon of a number of
:
* 'r lubrienting-oll riddition agents at 10-8CO, the offuct of these agents
00 on the nurf9tes tension of a motor oil at 50 and 700, and the atTectivo- are
0
noes of foam Inhibitors. Curves show the surface tozinion of oil with
0 addition of 'horplube, Mntobube, Nranox, And Delo, in concentrations coo
ur to 5%. 1~he highest values ol' surface tension %ri. observed Ar-, rnxi-
0
0 v^tGly at those concentrations whift have boon recomitwnded no optimal
0 by tAis Amorionn mnnufacturers. Upon addition of 1.5% Paranox to a
7 Are*
ki Rutivinn Ayt-ittion oil the foaming factor is 14% highor, and with 1%
I'mranox plim 0.1% Dow foam Inhibitor It Iv 2% lower, than that ol the
M I oll" .'ho Dow inhibitor alro roducou uip vurrmi-4i tn-,Lst,):% nt tite
o
11W U I
A So- It AOCTAtiucFAAL 1,11111414011 CtMOK0100
11.1 .61 all 0.1
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nf 'ho r-o-rtl.c7, o4.' diconj oll-,
SO: U-2,'~",', Sta'cc-- No. 1,

un It flid iia" in V. V. 140kay. Ap.
KhqWmWI 1. A. AWWO&WO (N 4 IVW No. 8. 47-42
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b~Wd in the 0u was mqmmw
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im a *4kr4W% at 40 &M 10', &84=pKW WQ dAMW bl(WO
boo* ;jW im uWAL Trw AUW. 5m. Tat. MAW.
V= Waws&Wmw4 agaft show WtOktv- &W
sib'w~Iwativm of MONWAiS biw^ &ad steak olek.
.W." AM UOAk-.W M* xt=h* MO* 44 mot 61
kb are Uasul ablo
zxwkat
mrAM mm obtAlod Wha WAN 0, % G( Y-lystbalw
ndmd I,' KT ") sMifiva basol an 9 th me of MOM
double boadk OW VMMWS WOWMWY (40 krth- dOW6
mp (OvQ)- The- UUV" is scow cam I v# tho demulaill-
Ook'a pn .. us thew ukd do IMMA Im Its stability to
oxidatiomL R. U. CLARRM.

CITMUMMIDV, A. ir"KI IT31MI Y1. V."), IIIJI.-AIV-1- A. L.
Carbon, Activated, Propane, Butane
Adsorption equilibrium of a propane-butane mixture on activated carbon.
Dokl. AN SSSR 82, No. 1, 1952.
2
501 Monthly List of Russian Accessions, Library of Congress, May __jW, Uncl.
Moskovsk r__Xh_EMo___Te_Z =oogfc_h_e_s_k =y-stitut im. D.I. Mendeleyeva rcd. 31 Oct. 1951
USSR/Chemistry Fuels
"Separation of Propane Butane "exture With A flovine, Layer of Adsorbent, "A. B.
Chernyshev, Corr Men, Acad of Sci USSR,, N. V. Kelitsev, A. K. Khalif
I'Dok Ak Nuk ISSSR" Vol 84Y PP 757-760 , 1qf I---
A chromatographic methof for the sepn of a propane - butane mixt followed by
desorption by means of electric heating was worked out and formulated mathematically.
'he procedure involves use of a movinE layer of adsorbent(activated carbon) in an
adsorption column. The deg of sepn is 98-99%.
232T13

L
F
USSR/Chemical Technology - Chemical Products and Their Application. Treatment of
Natural Gases and Petroleum. Motor Fuels. Lubricants,
1-13
Abst Journal: Referat Zhur - ]Qiimiya, No 19; 1956., 62574
Authort Khalif, A. L Yeremenko, V. S.
Instituti~)n; None
Title: Development Trends of Gas-Gasoline Industry
Original
Pericdical: Gazovaya prom-at', 1956, No 1, 36-40
Abstract: Considered are the basic trends in utilization of associated gases
of petroleum deposits and the new features introduced in the indus-
trial methods of recovery or gas-gasoline and liquified gas by oil
ab-sorptlon, adijorpt.:~nn on colid adeorbents, low temperature con-
densation and rectification.
Card V1

=IMY - A.L.; KOY, I.M.
"MMOMW
Air-cooled refrigerators. Gas.prom. no-11:36-39 N 156. (MLRL 9:11)
(Refrigeration and refrigerating machinery)

--77 -- -
~i- -
11 m-- -=

r\ r, A,
USSR/Chemical TecLology Chemical Products and Their 1-8
Application. Treatment of Natural Gases and Petroleum.
Motor and Jet Fuels. Lubricants.
Abs Jour Ref Zhur - Khimiya, No 1, 1958, 2574
Author Khodanovich, I.Ye., Kbalif, A.L.
Inst All-Union Scientific Research Institute of Natural Gases.
Title Some Problems of Recovery of the Gas Associated with
Petroleum at the Fields of Tatneft Federation.
Orig Pub : Tr. Vses. n.-i. in-t prirodn. gazov, 1957, No 1(9), 3-9
Abstract : The problems considered are those of recovery and trans-
port of the gas at the fields, uninterrupted operation of
the pumping system, and of maximum retention, in the gas,
of the gasoline which is separated at the gasoline reco-
very plant.
Card 1/1

t, V",Pk 1 t T', " "I !
YEPIMOV, L.I#; KRALIF, A.L.
harcoal
Hydrocarbon adsorption by the descending bad of activated c
particles. Trudy VNIIGAZ no.1:17-26 '57. (MMA 11:1)
(Adsorption) (Hydrocarbons)

4jSSR/Chemical TedLlogy - Chemical Products and Their 1-8
Application. Treatment of Natural Gases and Petroleum.
Motor and Jet Fuels, Lubricants.
Abs Jour : Ref Zhur - Khimiya, No 1, 1958, 2547
Author : Kelltsev, N.V., Khalif) A*L.
Inst : All-Union Scientific Research Institute of Natural Gases.
Title : Investigation of the Process of Carbonizing of the Silicate
Catalyst During the Process of Catalytic Cracking of Hydro-
carbons.
Orig Pub : Tr. Wee. n.-i. in-t prirodn. gazov, 1957, No 1(9), 27-54
Abstract ; A study vas made of the process of carbonizing of industri-
al silica gel, containing an addition of alumina, during
catalytic cracking of light gasoline of direct distillatim
The study procedure vas based on investigation of carbon
deposition on the surface of the catalyst, and of the
Card 1/2

KELITSEY, N.Y.; KHALIF. A.,L, "--
Intermittently operating carbon adsorption apparatusas with
horizontal adsorbers. Gazo proms no. 7:44-47 Jl '58. (MIRA 11:7)
(Gasoline)
(Gai industry-Equipment and supolies)

YEUME111KO, v.S.; POPOV, V.I.; KFALIF, A.L.
11atural-gas gasolinee and their use. Gaz. prom. no.F:43-47 Ag '58-
(MIRA 11: 8)
(Gasoline)

KHALIF,
Small natural gasoline installations. Gas. prom. 4 no.4:53-55
AP '59. (Idquofied petroleum ga 9) WRA 12:6)

ZHDANDVA, N.; KUM .-A.--
Drying of gasen by the liquid proceen at elevated temporaturF)fi.
Gaz.prom. 4 no.9:48-51 S 159. (14IRA 12:11)
(Gaseo-Drying)

- -- - - -- - -- - -- -- - ---- -- - - --
YEFIsOVP L.I.; KOROUNK0. T.P.; KITALIF, A.L.-, ESTRIN, 7.11.
.
A-inerption of heavier bydrecarbone from natural gesen by means
of frne-falling particles of activated carbon. Truey VNIIGAZ
no.6-137-1411 159. (MIRA 12:10)
(Hydrocarbons) (Carbon, Activated)

KHALIF. A. L. - TEPIAM, L. I.
- - . 1
kann transfer coefficients diming adsorption by a fixed-bed and
'hy free-falling particlen of the adsorbgnt. Trudy VNIIGAZ no.6.0
149-153 159. (HIRh 1-4:10)
(GlIses) (Adsorption) (magn transfer)
v

25 (5)
AUTHORS: Gushchin, V. P., Kelftsev, N. V., SOV/32 25-9-46/53
Khalif, A. L.
TITLE: S~und -Indicator for the Stream of an Adsorbent, Catalyst, cr
Another Solid Packing in a Column
YERIODICAL: Zavods'.-,aya laboratoriya, 1959, Vol 25, Nr 9 p 1140 (Unil)
ABSTRACTs Larger plants usually use a screw cunveyer connected with a
signal lamp as flowmeter for dispersive materials. Such a
device, however, is impractical for the work of smaller plants
or plants operating with high pressure. It was reported in
1956 (Ref 1) that Hungarian engineers, in studying the separa-
tion of acetylene by the adsorption method, had used sound
indicators (I) for checking the even distribution of the
solid packing in the column, a tuning fork serving as the
main element. At the same time, the device described here
developed and is recommended as an indicatcr of the strexa of
the solid packing. The device was tested in the YNIIGAZ testing
plant which was designed fer the purificatica of hydro.7en in a
mobile layer of active carben (at 50 atm). A scheme (Fig) shows
Card 1/2 that the device is attached to the middle of the cclumn, the

Sound Indicator for the Stream of an Adsorbent, SOV/32-25-9-46/53
Catalyst, or Another Solid Packing in a Column
needle-shaped "feeler" reaching into the stream. The needle
is fastened tG a bronze foil on which there is a piezo-
electric crystal, and connected with two automobile spark
plugs. The sound signals from the plug is transferred tc
the dynamics by means of a low-frequency amplifier. Fo.:- tj~~,L.
purpose, an assembly of the sound-ref lecting device KUUI-~,"
can be used which is produced by the Leningradskiy z;,vod
"Kinap" (Leningrad Plant "Kinap"). The sound intensity cF~n
be adjusted as needed. The device may also be used for the
operational control of the gas lift. There are I figure anJ
1 reference.
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy institut prirednc-2-0
gaza (All-Union Scientific Research Institute for Natural Gaa)
Card 2/2

ZIMUOVAP H.V.; KVLIF, A.L.
Technological indices of the operation of units for drying
casi4-head and natural gasess Gaz, prcap. 5 no. 12:42-45
D ,6o.
(MIRA 14:1)
(Gast Natural-Pipelirps)
Az
IN,.

G40RECEOMKOV, G.%I., IVANOT, A.K.. RTBAX, B.N., KHALIF. A.L.
Efficient methods of processing the condensates from gas-conden-
eate fieldse Gaz.promo 5 no.2:52-54 7 160. (MIRA 13:6)
(Vasnodar I;orritory--Condeneate oil wells)

825 13
'57 28 0 0 s/o65/6o/000/008/007/007
E030/E412
AUTHORS: Rybak, B.M. and Khalif, A.L.
TITLE: Catalytic Cracking or Catalytic Reforming
PERIODICALs Khimiya i tekhnologiya topliv i masel, 1960, No.89
pp.66-70
TEXTs It is claimed that catalytic reforming will be a more
economic process than catalytic cracking for increasing fuel
production in the USSR to meet the 1965 target. Catalytic
cracking is more economic only in those regions without oil such as
in Siberia, Kazakhstan and the Central Asian Republic, which possess
cheap solid or gaseous fuel, so that light petroleum products are
most required. In all other cases, cracking even to produce lower
paraffins, olefins and gases for petrochemicals is uneconomic. The
claim of BOyder is rejected, that in regions without coal or gas,
such as the Urals and parts of European Russia, light products'
requirements are 10 to 20% lower than elsewhere. Contrary to the
situation in the USA9 which has different crude types and where
motor gasoline is the most important product, catalytic reforming is
superior in the USSR because motor gasoline is not the main product
and will not be for at least the next fifteen years. By using
Card 1/3
21n i -Xv
T

825 13
s/05/6o/ooo/oo8/007/007
E030/E4iz
Catalytic Cracking or Catalytic Reforming
reforming, the existing refineries would require only 7076 of the
available USSR crude to satisfy the motor gasoline (FBP 18o to
2000C) requirements for 1965, leaving the surplus free for export.
Further, with some crudeso especially naphthenics, up to 7 - 10% of
the aromatics may be extracted without appreciably lowering the
octane number (motor method) below 80. Diesel and jet fuel
requirements could be met from non-paraffinic and slightly
paraffinic crudes by broadening the fraction from 140 - 3WC to
18o ... 43dc. Catalytic cracking at 350 to 5400C, as advocated by
Agafonov, gives large yields of diesel and high octane number
aviation fuels but-the outlet for these is less than for the
products of reforming. Cracking of distillate residues gives
9 to 12% wt/wt of gases up to C4g and 5 to 10% coke and waste,
while cracking with Tuymazy and Romashk sulphurous crudes gives
5 to 7% gases up to C4, and 8.5 to 10% coke and waste. Cracking
of narrow distillate fractions gives similar results. The high
wastage factor and the fact that sufficient feedstocks can be
obtained for petrochemicals from natural gases and from the gases
from reforming units, therefore makes the cracking process
Card 2/3

KIIALIF, A.L.; KOF, I.M.
Study of the operation of desorbers of oil absorption apparatus. Trudy
VNIIGAZ no.12:150-158 '61. (MIRA 15:1)
(Sorption) (Gasoline)

REGELIMANt M.A.- ;_KHALIF, A.L.; XHUSAINOV, B.Kh.
I
Preparation of .isopentane In anjiaobutane C01UMn, Ga2,p'm, 6 no.3:45-
47- -,61.
- .0 4 (Butane) (Propane) (MI.m 14-.3 1)

VORONCHIXHINA, M.G.; KELITSEVp N.V.; STAROVOYTOVA, A.F.; RRALIF, -A.L.
Obtaining so.lvents from.casing-head gasolines.
159-163 161.
. (Gasoline) (Solvents)
Trudy VNIIGAZ no.12:
(MIRA 15:1)

AEROV, M.E.; GORECHENKOV, V.G.; MOLOKANOV, Yu.K.; SUM-ShIh, L.Ye.; WSYOBWt
A.I.; KHA,4jE,--Aj,,; BROM, I.A.; SATTAROV, U.G.
Effectiveness and maximum loads of industrial absorbers with various
bubble trays. Gaz. prom. 6 no-11:35-38 161. WIRA 15:1)
(Mass transfer) (Plate towers)

ZRDANOVA, Nina Vladimirovna; KMLIFp Alfbert LIvovich; NOVIKOVA, M.M..,
ved. red.
(Debmidification of natural and casinghead gases]Osusbka prirod-
riykh i poputnykh gazov. Moskva, Gostoptekhizdat~ 1962. 110 p.
(MIRA 16:1)
(Gas., Natural)
gn,
i~~ 119 -11,14 Yl MR)

SARKISIYANTS, Gayk Arkad'yevich; BENIYAMINOVICH, Osip klekaandr-ovich;
KELITSEV, Vladimir Vladimirovich; KKL#TSEV, Hikolay
Vladimirovich; POLOZKOV, Vladimir Tikhonovich; KHALIF,,(-,
Al-l-bart-L-1yo-Tiqh iW~ y
j KHODANOVICH, Ivan Yefimovich,; -B-Ek,- N.,
kand. tekhn. nauk, retsenzent; PLETNEV, K.N.,inzh.,red.;LEVINA,
Yo.S., ved. red.j POLOSINA, A.S., takhm red.
[Processing and utilization of jas)Pfir~rabotka t
gaza. (By]G.A.Sarkisliants i dr~ Moskva, Gostbpt#kh1*i&t, 11962.
216 p. W4 16:3)
1. Kafedra gasa Azerbaydzhanskogo ordena Trudovogo Krasnogo Zna-
meni instituta nefti i khimii im. M.Aziabekova (for Raaben., Pletnev).
2. Zamestitell direktor VseBoyuzno n&-uchno-isoledovatellskogo
institute. gazovoy promyshlennosti rfor P,~aben).
(Gas, Natural)
(Gas industry-Equipmant and supplies)

WLIF) A.L.
Modernizing the gaaoline Pl&nts of the Tatar A.S.S.R. and
BashkirJa. Gaz. prom. 7 no.11:39-43 N 162.
Q-IIU 17:9)

T F
in the , rtE,f i r r r

1"I D=Ov V.S.; XHALIFp A~L,j '" KACHUR, 0,Yu,
Foreign technology, Gaz. prom. 8 no.6:40-42 163.
(MIRA 170)

..Y.`
A
L, :! , A. ; .IU"t;KOV' V'(3;.' KI"fd'Fl t-'-; K!"2,HlZ!fZV.--KAYA, N,G,
of g,,_d_r,~t -
- 'L r-!* 3 -j&
.1.0 a - ~~ i~, 1 '11. 1 . r Z, prOn- 10. no- 3:40-46
WRA 1835)
1~

I; e a 9 9 a
Aa r-
A
AY7
SIR
SO
SIR
fell To ftand OWafim of 0"a.Hudh Fwmac M. KhAllf
--
-
SO anid T. Koval. (Stal, 19U, No. 21 Pp. 14-41). (In Bu;m
nr
'
he documentary &W of drawing up a plan for the operation of an
7
lan covers the whole
a
Is d
The main
h
th f
lt
ith
w
open-
ear
urn
oe
ea
.
p
eta period of operation (150 heats) from one complete overhaul to
Soo another. 8ubsidissy and more detailed plans are drawn up during
d
d
d
l
l

Soo s an
l as
operation to cover 5-
24-hour pedoI
s, as we
ay perio
ing of
wrvictip and scoemory o
erations before and after the tap
00- p
p
rns of forms, chits and
heats. in addition. the authors gi
6614 =
similar documents which have to in by the reoponsible
personnel. lbese provide a record of the actual operating character.
istics of the furnsm.
A S S. L A AITALLURCICAL LITERATURE CLAIWKATM*
Ak INT40i oil O.V7a-C
U 5 AV IQ 11
It it a aof a a I, it IN U
0 0 0 0 * 0 0 0 9 0
00 00 0 4 * 0 a 41
doA 1 14
* 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
0 0 49 Is 46 0 00,
0 IS IS 0 4
-00
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roe
coo
x
set
get
200

GONCHARENKOt N.I., kand. tekhn. nauk; BABIY, A.S.; BAYDUK, V.F.;
BAZILEVSKIY, A.R.; MISHCHENKO, N.M.; MALINOVSKIY, V.G.;
NELEPAP V.I.; TOLISKIY, A.A.; TRETIYAKOV, Ye.V., kand.
takhn. nauk; KHALIF Mkj PODOPRIGORA, I.D.
._~j_
Smelting of steel In oxygen- and steam-blown converters with
an acid lining. Met. i gornorud. prom. no.4:20-25 JI-Ag 165.
(MIRA 18:10)

IMLIWUN, L., inzhener-konstruktor; KHALIP, S., brigadir razmetchikov.
Measuring the distance from the plumb line to the selected base
in centering machines and mechanim on ships. Mor.i rech.flot
14 no.2:29-30 7 154. (MLRA 7:1)
(Marine engineering)

KHALIF, Semen LIvovich; YAROVA, L.Y., red.; TIKHOIJOVA, Te.A., takhn.red.
-------- 1- .
[Practices of a layout man in a ship repair yard] Opyt raz-
matchika sudoremontnogo savoda. Izd.2., dop. Moskva. Izd-vo
"Morskoi transport," 1959. 80 P. (MIRA 13:1)
(Ships-Kaintenance and repair)

XHA-LIF, V.B., inzh.
Calculating temperature drop in the insulation of mush
winding of electric machines. Yest.olektroprom- 31
no.2:30-32 I? 16o. (MIR& 13:6)
(Electric machinery-Winding)

~~A 7t
i~ fiWE
MIN

KHALU 74
"----A,.
Petrography of the JurassLc Clays of Northeast Azerbaydzhan. Dokl. AN
Azerb. SSR, 9, No 81 1953, 445-450.
The sandy and siltstone fractions of the somples investigated contained
quartz, feldspar, and detrAus of minerals. The clayey fraction is represonted
by thinly dispersed minerals hpvein an aggrerate structure. Under opticnl tests
these minerals anproximate hydromLca and chlorLte nprearLng In a metamorphicIzed
zone. (RZhGeol, No 1. 1954)
SO: W-311281 11 Jan 55

Ch. "'L.
Monothermite and Illite ~-*ti the Juraosic Clays -)'L r~.ortlle.-stcrn (restne fr
Azerba- dzhani) Dokl. All Azerb. SnT , 9, Vo 9, 1.953, 5.1-t-524
Inform,,!tJon on the -,,dnernlogical ccPPp,-)vitIon :if the Jurm_,inIc clnys of north-
eastern A-zerbayfthan, is presented. 'Me fraction Aess t- an 0.001 --m of four smmplcs
of clay t.91cen from various stratigraphic hori~~,)ns were subjected to thorou,,-h ir,
vestigation (optical, 7-ray structural, thermal, che-nicni, spectrophoto-etric,
physicoche,iical), establishing that the clays in tl-,e Jura.-,sic ~,.ep)sits ~f north-
eastern A.:~erbaydzhan nre monotheriaites and qu-ntititively inferior illites. (RzInGeol,
110 1, 1954)
SO: "i1'-3-1128, 11 Jan 55

r scientific
rvey O~ ational Institutalks.-
SO: sum* No. 631, 26 Aug 55 - S' Ijigher FAuc
Dissertations Defended at USSR
(14)
Soi,
Cv,nd Geol-lds u 1954- Ml
~,O, Bak, p
idal
and Tech"
Soj Azerbaydzho
of the kalen
jLyey lJocks (krg'llites) serbaYd2l'an'"
.alogy of cl, theastern A]
"14inex (Lower Jurassic) of Nor Gubkiny kcad
Inst of Geology M*Feb 55)
Formations
to 99

RE i
I
4 42 t .11 mi -l"IN
SUM

cH,
USSR/Cosmochemistry - Geochemistry. Hydrochemistry, D
Abst Journal: Referat Zhur - Kh1mill, No 19, 1956, 61318
Authort Xhalifafadej Ch. M.
Institution: None
Titlei Study of the Complex of Absorbed Cathions and Water-Skluble Salts
of Argillites of Aalen-Bayos of Northeasterm AzerbaydEhan as an
Index of Facies Situation
Original
Periodical: Dokl. AN Azerb SSR, 1955, 11, No .12, 839-&3; Azerbaijani resume'r
Abstract:
Card 1/1
Determinations were made of the absorbed complex of clays by treat-
ment with 0.5 N NH4Cl after removal of water soluble salts with dis-
tilled water. The eontent thus determined (in mg/equival. per loo g
of rock): total amount of absorbed complex does not exceed 15-161
M92+ 0.78-4.48; NO' + K+ 0.2; Ca+' 5.46-17.44, rarely 1.8-2.8; in-
creased content of absorbed Ca2+ is attributed to decomposition of
embedded organic substances; ratio (Na'~'+ K+)/(Ca2++ Mg2+) on the
average 40.02, indicates coastal conditions of accumulation of sedi-
ments.
/77,
Zee,

h.14. Itbarn Farg"10 W
MLIFA-M!!fL~C ~ edimnts Of Sol .0utIlealstern
Itaceous a oedimnt$ Ofitute of
a lpstrogrgLPhy of upper Cro of upper Cretacsouo Ilzbak In"t AN Uz.
A.G.BaboLev; spetrogroLpby d bSGv (PTr*dyiv of the tZade - lz'q- (MPA 1415)
Fargw"L" by A.14.Wwakbo z jewed bY Ch.I&Dalira-
jeolbgy, noslOs 1954)- PA*4 (Babaevi k.G.)
c ,o.4%77-79 '56' AgriLphiol k M.)
SSR (Fargans-'Geologyp strat (WamlchodVAGv 2 *

P4

IMIFAZADI. ON.M.
Some problems of the spectrogmphic study of rocks of Aserbaijanian
oil fields. Azerb.neft.khos. 35 no.3:6-7 Mr '56. (RLRA 9110)
(Azerbaijan-Rocka-Spac t ra)

KHALIFA-ZADE, Ch.M.
A new hydromica variety from Bajocian argillites of the southeastern
Caucasus. DokI.AH Azerb. SSR 13 no.6:647-653 '57. (ML-RA 10:8)
i.Predstavleno akademil-om Akadenii naulc Azerbaydzhanskoy SS?
'O*h.A. Azizbekovym.
(Gyulekh-Wromica)
KHALIYA-ZADA, Gh.M.
Mineralogy of middle Jurassic argillitse from northeastern Azerbaijan.
SokI. AN Aserb. SMI 13 no.9:987-990 157. (MM lotg)
1. ruatitut geologii Dagestanskogo filiala, AN SSSR. Predstavleno
akademikom AN Axerbaydzh"9koy.SSR Sh.A. Asisbakovym.
(Azerbaijan-Argillitas)

2o-IU-4-52/63
AVTHOR: Khalifa-Zade# Ch. M.
TITLE- On the Oil-Producing Nature of Argillaoeous Rocks From
the Middle Jurassic of tha South-West Caucasus (K voprosu o
nefteproizvodyashchem kharaktere glinistykh porod aredney
Yuxy yugo-vostochnogo Kavkaza)
PERIODICAL: Doklady Akademii Nauk SSSR, 1957, Vol. 114, Nr 4#
pp. 669 - 872 (USSR)
ABSTRACT: The argillaoeous mass of the Middle Jurassic in the said
territory is considered by many scientists as an "oilmother
suitall(neftematerinakays svita) which feeds the younger
Yurassic and Lower Cretaceous sediments. On this cocasion
the authors produced from the existence of gas eruption places
and from bituminous phonomena. However$ the mineralogical-chemical
nature ~f the argillaceous rocks and the organic substance
contained 'in them is by far not sufficiently well investigated.
The author devoted many years to the mineralogical investigation
of these rocks and their content. Analysis of their mineralo-
Card 1/5 gical composition has shown that they consist of hydromica
2o. 3.14-4-5e/63
On the Oil-Producing Nature Of Argillaceous Rocks From the Middle Jurassic
of the South-West Caucasus
of various degrees of modifioationg those modification having
been brought about by alterations of stadium. This is also
true for the chlorites and the previously formed argillaceous
minerals which underwent a transfer, resedimentation and
diagenesis. Thus it is not possible to reconstruct in a plausible
manner the geochemical picture of sedimentation of the Middle
-Jurassic on the basis of argillaceous minerals only. rn 'Order
to clarify this Picture the author studied the contents of
the autogenous-mineralogioal form of iron# of the orcanic car-
bon and the bitumen. Finallyt the quantity of the primary C org
was computed according to the determined balance of the auto-
genous form of iron. Table 1 shows that all samples have a
comparatively *high content of the residual a org' It seemed
likely that a high content of pyrite iron might be found as
well# but it does not seem so from the table. There are however
high contents of carbonate iron. In spite of these deviations
Card 2/5 a certain regularity in the distribution C org, FeS2 and FeCO 3

20-324-4-52/63
On the Oil-Producing Nature of Argillaceous Rocks From the Middle Jurassic
of the South-West Caucasus
ciple in.Soviet lithology. Strakhov extends this idea also
to diagenesio.The author for hie part therefore endevgred to
reconstruct the possible individual features of the sedi-
ment genesis of the Middle Jurassic rocks on the basis of some
elements of diagenetical formation of minerals. In the course
of this work a number of reversible eystemsformed, their equi-
librium being regulated by the course of decomposition and
oxidation of the Corg' The author believes that the cause
of the weak development of sulphide sulfur lies in the phy-
sico-geographic particularities of the Middle jarassic basin
and in the initial composition of the organic substance..
Apparently it was more brackish than seas usually are. However,
these circumstances had a reducing effect only upon the
carbonate iron minerals, while they acted slightly oxidizingly or nea-
tivily on oiganic matter. Thoref ore such geochemicai uu,,Uizione pre-
vuiiing tne lipoid fraction of the organic matter could not
Card 4/5 produce each a large quantity of bitumen and oil, as would

On the Oil-Producing Nature of Argilladeouo Rocks From 2o-j))I_i~.52/63
the Middle Jurassic of the South-West Caucasus
be required of industrially useful oil-wells. Thorn are 1
figure, 1 table)and 10 references, 9 of which are Sovis'b.
ASSOCIATIONs Geologicheskiy institut Dagestanskogo filiala Akademii nauk SSSR
(Geological institute of the Daghestan Branch of the AS USSR)
PRESENTED: December 25, 1956, by N.M.Strakhov, Member, Aoademy of Sciences,
USSR
SUBMITTEDs November 27, 1956
Card 5/5
AUTHOR: Khalifa-Zade, Ch. m. SOV/ 20-120--1-51/67
TITLE: On the Problz?m cfthe Conditions of the Formaii--2-i of Clayey
7.!ineral~4 In the Jurassic Time of the South_Et,:_'~ '.,.ucaslis
(K vvprf)su ob unloviyakh obrazovaniya glinisty:~h iinl~ralev
,YurY '-'u6-.D-Vo.-vo-hn-Q90 Ka-ikaza)
FERIODIA~AL- Doklady Akademii nauk SSSR, 1956, Vol. 120, Nr pr-,621-~24
( U 3S, R )
ABSTRACT: In a previous paper (Ref - FcOtnote 1, p~ 621) genetio
diagram of the sedizenta~ry cluyoy depozito ras proposed bV
the author, It nhow-3 a trianglu at tile tips of whic-h inter-
layer (mezhaloynyp) cations are placed a:3 well as the con-
tent of -'13* and Si44 in the silicon-oxygen tetrahedrons
of the J~ratified hydrosilicates. As a baai2 of thz pro-
posed genetic diapram the +author employed a quqntitqtive
modification of R , (OH ) in the space betwt)(in thp racketi
c, ~ _r f o r -11 na
papt?r the :4uth(~," -9--~tORIDtorl tv explain t~e ot, fovmn-
Card I/ tinn of the rJncrals ine n t i o ndJ nthp title with thta help

SOY/20-120-3-51/67
On the Problem of the Conditions of the Formation of Clayey Minerals in
the Jurassic Time of the South-Eaat Caucasus
of the said diagram. They were investigated by him through
several years by means of a whole complex of methods (Refs 1-6).
Clays are there in general composed of hydromica metamor-
phosed, to various degrees, Crystallochemical formulae of the
hydromica, obtained by a relative computation of the chemi-
cal composition of the fraction < 0001 mm from various
districtsp are given (Table 1). They are +mootly considerably
modified because 6f the replacement of K according to the
scheme R + 0 (OH In order to clarify the problem ac-
cording to which tyke of diaintogration(acidous or alkaline)
the modification of the hydromica proceeds and to which
clayey mineral this or that crystallochemical formula. be-
longs, the author entered the data from the chemically
investigated samples into the diagram ij a fourfol I- coordi-
nation, taking into consideration the K - and(OH ) content
in3the s&ace between the pqckets and the modification of
Al +g Si '. The analysis of the Jurascic :pediments on the
basis of the separation of lithogenetical rock types showed
that the latter formed in a shallow -m_-tar i~z_,servoir and
Card 2/4 with respect to facies belong to differont cactions of the

SOV/ 20-120-3-51/67
On tha Problem of the Conditions of the Formation of Clayey Mincrals in
the Jurassic Time of the South-E3st Caucasus
continental slope of the shelf. k humid climato was prevalent
in the catchment. ttreas. From the Upper Jurassic time on-
wards the climate became dryer and the relief peneDiaineda
A characteristic arid climate prevailed in the Tithonian age.
Such an abrupt change of conditions, more exaotly of the
type of sedimentation, showed a clearly marked effect on
the clayey minerals, Figure 2 shows crystallographical data
on the hydromica from the respective area. The position of
the points in the diagram may point to the fact that an
acidous or alkaline medium was locally generated. An acidous
type of disintegration could also be favored by climatic
conditions. in spite of some deviations the points on the
whole are situated in such fields of the diagram which char-
acterize the different modifications of hydromica. There
are 2 figures, I table, and 7 referencos, 6 nf which are
Soviet.
Card 3/4

SOY/ 20-120-3-5 1/67
On the Problem of the Conditions of the Formation of Clayey Minerals in
the Jurassic Time of the South-East Caucasus
ASSOCIATION: Geologicheskiy institut Dagestanskogo filiala Akademii nauk
SSSR
(Geological Institute of the Dagestan Branch,kS USSR)
PRESENTED: October 23, 1957, by N. Mo Strakhov, Member, Academy of
Sciences, USSR
SUBMITTED; October 17, 1957
1. Clays--Geology 2. Minerals--Geology 3. Geochemistry
Card 4/4

3(8)-
-AUTHORS: Khalifa-Zadet Ch. M., Abbasova, S. M. SOV/20-125-5-43/61
TITLE: Chamositc Clays From the Kimmeridgian Stage Sediments of the
Southeastern Caucasus (Shamozitovyye gliny iz otlozheniy
kimeridzha yugo-vostochnogo Kavkaza)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 5, PP 1110-1113
(USSR)
ABSTRACT: The sediments mentioned in the title have a siliceous
appearance and a green-gray and olive-green color. The
rocks of this stage are developed in the axial and near
axial parts of the Dibrarskaya geosyncline. They lie trans-
gressively on various Dogger-horizons. Upwards in the section
the Kimmeridgian Stage is abruptly overlain by a red Tithonian-
mass. The thickness of the Kimmeridgian Stage fluctuates bet-
ween 180 and 200 m and is lithologically represented by sand-
stones, "aleurites" and "aleuritid' argillites. These sedimento
have a flysch structure here. They belong to the facies of
sediments from the coastal part of a shallow sea. Results of
the microscopic study are given. The green color (Ref 2) is
said to be due to a chloritic substance. In order to explain
Card 1/3 the nature of the -reen scaly minerals found (residue after

'Chamosite Clayn From the Kimmeridgian Stage Sediments SOV/20-125-5-43/61
of the Southeastern Caucasus
treatment with 5 % HC1), the content of soluble iron was
determined accordinf; to the method of reference 3 (Ta& 1).
Since the majority of the total iron (approximately 80 %)
is represented by soluble iron (10-12 A in the minerals) it
can be asserted that 35-40 ~- of these clays consist of chamo-
site. Its extraction was not OUCCeGBfUl. The fine fractions
(after HC1 treatment) were invostigated thermally (Pig 1),
chemically (TaW.03) and with X-rays (Table.R). Thus it was
determined that the argillites of the Kimmeridgian Stage in
the southeastern Caucasus consist of hydromica and chamosit~~
of various origins. The bydromicas are apparently related to
the clayey rocks of the oource areas which conoist of shaly,
Dot:ger argillite and Lusitanian limestones. Consequently these
hydromicas are related to the Middle Jurassic clay3tones.
Chamcsite originated from clayey sediments bj a chemical
process in the diagenetic stap. The small amotint of organic
carbon indicates a spont;y,sediment of a neutral or weakly
reducing medium (Tablai). This favored the formation of a
leptochlorite facies. The iron came into Kimmeridgian waters
Card 2/3 from the adjoining mainland in an oxide form as a mechanical

C"), ilays From the Kimme-ridgian Stage Sediments
of the Southeastern Caucasus
suspension, The clay and silica required for the formation
of are of volcanic origin (Ref 1). The
Kimmeridgian sediments were systematically enriched with
volcanic dust, which fell from volcanoes of the adjoining
mainland (region of the Kura depresaior),which wero active
at that time. There are 1 figure, 3 tableaand 9 references,
8 of which are Soviet.
ASSOCIATION: Geologicheakiy institut Dageotanakogo filials, Akademii nauk
SSSR ( Geological Institute of the Dagestan Branch of the
Academy of Sciences,USSR)
PRESENTED:
SUBMITTED:
Card 313
December 26, 1958, by N. M. Stral:hov, Academician
December 15, 1956
3 (5)

AUTHOR: SOV/20-126-2-40/64
Khalifa-Zade, Ch. M.
TITLE: On the Genesis of the Priaamu-rskoye Deposit of Siderite5
of South Dagestan (0 genezise Prisamurskogo mestorozhdaniya
sideritov Yuzhnogo Dagestana ) I
PERIODICALs Doklady Akademij nauk SSSR, 1959, Vol 126, Nr 2,
Pp 371-374 (USSR)
ABSTRACT: In the total ore-balance of the Caucasus, the siderite-ore
of Dagestan takes the leading position. The problem
mentioned in the title is, however, still insufficiently
an)
investigated. In this region the Prisamurekoye (Near Samuri
deposit is the most important and best known. There are 2
hypotbesee on its genesis: a. the siderite-ore was formed out
of Bea-water as colloidal carbonate (FeCO, 3* nH20). The iron
precipitation is explained by a high C02 -partial pressure
in the atmosphere &Ekg tO JW8 io peribd (Ref 2), b. the af ore-
said ores developed due to the activity of iron-bacteria in
an Aalenian water in a milieu of H 2S fermentation. Careful
Card 1/4 facial-lithologioal investigations have shown that the
_7
k

On the Genesis of the Prisamurskoye Deposit of SOV/20-126-2-40/64
Siderites of South Dagestan
distribution zone of the ore-concentration of siderites is
confined to isolated parts of a shallow sea (Fig 1), rich in
islands. Between these islands the accumulation of fine-grain
material and of iron was favored. The facial map of the
deposit (Fig 1) illustrates the form, size, and position of
the siderite-formation area as well as its correlatioh to
other facial types of sediments in the shallow open sea. The
ore-formation area ran almost parallel to the coastline of
the old continent of Paleocaucasus (2iblel). The sources which
favored the enriching with iron are to be sought in the
paleographic conditions pertaining to the upper Aalenian of
the East Caucasus. An exceptionally warm and damp climate
(Ref 6), encouraged an extensive weathering in the catchment
area as well as a substantial transporting of iron into the
waters. Terrigenous material was only gradually carried in.
The parts of the old continent adjoining the coast, formed
an extensive marshy plain which was drained by brooks and
small rivers. The iron ran into the water predominantly in
oxide form and as colloidal salts. Conveyance was taken care
Card 2/4 of by ground solutions which were distributed over the marshy

On the Genesis of the Prisamurskoye Deposit of SOV/20-126-2-40,/64
Siderites of South Dagestan
plain. The iron therein was of a bicarbonate form. This is
the lot form in which the iron was carried out. The 2nd form
was the oxide migration. In the strong outflow of the rivers
the gels of ferric hydroxides played an important role. The
brine which fell into the water in large quantities, partly
coagulated while the 'remainder was carried on into the
pelagian part of the shallow sea, and there accumulated as a
sediment rich in iron and clay. The ferric hydroxide which
did not become sedimentary in the coastal waters was
considerably diluted by terrigenous material. This was but
not the case with the isolated waters and therefore the
Fe203 content in the dispersed initial-sediments of these
waters were 4-5 times greater than in the neighbouring
synchronous loamy sediments of the open sea. The wooded islands
favored this process. They gradually sank during the ore
formation. The isolated parts were levelled out in stages.
There siderites and sideroplesites developed, which on the
periphery, followed the pistomesite and braunite. In the
Card 3/4 adjacent sediments of the open sea only calcite-braunite-

On the Genesis of the Prioamurskoye Deposit of SOV120-126-2-0164
Siderites of South Dag6stan
ankerite concretions are distributed. The structural
properties of the ores are not connected with the
sedimentogenesis, but are completely conditioned by the
diagenetic process. There are 1 figure, 1 table, and
6 Soviet references.
ASSOCIATION: Geologicheskiy institut Dagestanskogo filiala Akademii nauk
SSSR(Geological Institute of the Dagestan'Branch of the
Academy of Sciences, USSR)
PRESENTED: January 17, 1959, by K~ M. Strakhov, Academician
SUBMITTED: January 15, 1959
Cara 4/4

Profiles of iront caloilm, rzgnosiun, and manganese distribution
in different facics of AaIcnian deposits of Dagheetan. DoU. All
SSSR 135 no-3:720-723 N 160. (VIRA 13:3-2)
1. Fredstavleno iL%adi. IIX. Streihovym.
(Darheatan-Geor.-hemistry)

KH&LIFA,,ZADF., Ch.M.
Mineralogical and geochemical zonation of sideritic deposits in
Daghestan, Izv.vys.ucheb.zav.1 geol.i razv. 5 no.3:70-84 ~h- 162.
0 (MIRA 15-4)
1. Dagestanskiy filial AN SSSRP Geologicheskiy institut.
(Daghestan--Siderite)

KHALIFA-ZADE, Ch.M.
Stages of ore formation in sideritic deposits of Daghestan. Zap.
Vses. min. ob-va 91 no-1:117-121 '62. (MIRA 15:3)
1. Geologicbeskiy institut Dagestanskogo, filiala AN SSSR.
(Daghestan--Ure deposits)

KULIFP-,ZADE., Ch~,14;
Geological and mineralogical characteristics and genesis of the
siderite deposits in Daghestano Savo geol. 6 noq6:119-125 Je 163,
(MM 16:7)
1. Geologicheskiy institut Dagestanskogo filiala AN SSSR.
(Daghostan-.Siderite)

Y,-HALIFA-ZADE,,~hjnjr17 ViijilrArl; ABBASOVA, SoInAz VIkhaylovna;
- ALIILV, Abdul Gadzhi, oty. red,; KLINI':;(;VA, I.A., red.
izd-va; GUSEVA, A.P., tekhn. red,
(Siderite deposits in Daghestan] Siderltovye zaIezhI
Dagestana, Moskva, Izd-vo AN SSSR, 1963. 133 p.
. (MIRA 16,9)
1. Chlen-korreapondent All Azerb,SSR (for Aliyev),
(Daghestan--Siderite)

KHALIFA-zADL?, ch.m.
Siderite deposits in the southern part of Daghestan. Biul. MOIp.
Otd.geol. 38 no,1:137-148 Ja~g 163. (MIRA 16:5)
(Daghestan-%~derite)

KHALIFAZADE, Ch.M.
Adsorption of chrysoidine in minerals and its significance in
studying oil-bearing terrigenous sediments. Izv. vys. ucheb. sav.;
neft' i gaz 4 no.3tl'7-21 161. (MIRA 16:10)
1. Azerbaydzhanskiy gosudarstvennyy universitet im, S.M.Kirova.
g ag-

KHALIFAZADE, Ch.M.; ALIYEV, G-M.A.
Facies profile of bitumen distribution in the Middle-j~irassic
sediments of the southeastern Caucasus. Izv.vys.ucheb.3av.;
neft' i gaz 5 no.12:9-13 162. (MITRA 17:4)
1. Azarbaydzhannkiy gosudarstvennyy universitet imoni Kirova.

SULTANOV, K.M.; KHALIFA-ZADE, Ch.M.; SAMEDOV, S.S.
Jurassic otratigraphy of the sediments of the Kuna oil-
bearing region. Izve vyu, ucheb, zav.; neft' i gas 6
no.8t9-13 163. (MIRA 17t6)
1. Azerbaydzhanskiy gosudarstvennyy universitet imeni Kirova i
Inatitut geologii Dagestanskogo fil.jela AN SSSR.

SA S.S.
Strattgraphy ,)f t,~f,
~Ilrru3ic s(idlirjents of the Kuma oil- aTd gas-
hearing region, Jzv-vYs.uchsb.zav.; neftl i gaz 7 no.4:10-11
164. (MIRA 1'7:'5*,
1. Azerbaydzhanskiy gosudarstvennyy unimrsitet imeni Kirova.
KHALIFA-ZADE, Gh.M.; OSTREMSKIY, M.R.
Thermoanalytic determination of 'the content of siderite
(magnesium siderite) in ferruginous carbonates. Izv.All
Azerb.SSR. Ser.geol.-geog.nauk no.2:63-67 164. (WRA 18:11)

KIIALIFE.M- S.M.
of el,~r,~c,nts on
thp formation of agp
ii-radl rjti~,d and ~rrnd~,Iteej
42 90-J,'Y5 b, V, a8t6'1
Uzbplc~,kiy --l-ris"A I'lil,

Ir
AP601-8.U3 SOURCF CODE: upt/00,L(,-/~-,,1/000/C02/C,090/C'09,gjI
I AUTHOR- Nikolayev t,?;
ORG: Uzbek Institute of 1=?.oi- bgrnolo -1 diolotry bind Ncol-o~,,Z (TJJz*t,,jVsk1y ~zntit,ut"
i cmkologiL); Uzbek TwAital,.~-, ~J ~-.nd
(Uzbe1crkj.y instAut valctuin 1 syvovotok)
TITLE: Effect of certain complex compoinids of tracc-, c-`Levinnts (,n the phtigocy~lc
activity of laukocytes and agglutinin fonnAiori in irr~idj,a'.f-~j ;P.A
rabbits
SOURCE: Zhurnal inikrobiologii, epldelniolorLi i innunobiologij., no. 2, L965, 90-95
TOPIC TAGS: r lil, ~t, :tnt xni.n 0
imunity, radii,-:0,1on I-Aologif; offect
AB3TRACT: Tile allthors at"died the &ffeot or ooamide (complex
compound of cobalt chloride with the amide of nlootinic acid))
co3u, vitamin Bt f forramide X (oomplex oom.pound of forrous ohlo-~ f
ride with the amide of nlootinio acid), ferramide 11 (complex
oompound of forroUs slAlfate with the nmido of n1cotinio acid) and
cuprio glutauilde (complex eowpound oC cuptio ohlorldo with gluta-
ininlo acid) on the phngooytio aobivlt-J~ of leukooytes -And antibody
formation Ift-rabbito Immunized'eagainst Sta hylopopous qurquq-~und
irradiated (500 r)v...-A-11-thedo 0opper
UDC: 616.9-022-06: 616-001.Z81-0,15-777-9-
1/2 O1?:[6i6-I5-:997-J4
'M,%r,4RAa -'JIM
ANN
-z
ACC I'P
AF6ole-Ja3
'laied antibody gynthesin in non-i5rdiated rabbito (coamide and
.Vitamin B 12 by 2o).2*9 'timeq, Co by 441 timenj feiramido 1i 2
,,tiMe3; ferr4mide 11, 3#7 times' and MIPMO 9111tamida 4 times).
The phagoeytotio Index was ino'
reaved an average of
,rabbits (ooamide and vitamin B 16 In these
- 20-21%; COJU - 38.7"; and
-.0uprio glutamide - 42%), NeItUr ferramide showed ar-y'oeffeot In.
,this respect, A Statistically ralia~60 increase lno5j)eanumber of
:Ieukooyten wan obtained only with Co Coamide C
nd vltn",-a'
min Bt, stimUlatod antibody aynthoaja in rabbits e~,-poned to a
.radia on dose of 500ri they had no effeet,orl the phasocytotio
.ii2dex and the vumber of Idukooytobd
.''The best r0sUlts were ob-, if
',tained- wi.th. Cojui` Orig. art. has: 2 ~ablas. [JFWi]
SUB CODE: 06 SUBM DkM 12Aug63 / ORIG Iff: 014 / ON REF: 001
2

MALIF1401, I.
Brief comments. Agrobiologiia no.6:926-930 11-D 161. (MA 15:2)
(Bee culture) (Sweet clover)
(Ants)

BRO ADA14 [Kerle, Adam~ Brother Adam) (Angliya);,Ig ransla
jLLMIAN _J, [ t tor
Some problems of selecting pairs in breeding honey bees.
Agrobiologiia no.6.879484 11-D 161. OUILL 15:2)
(Boo culture)
"t �r
MW

KHALIFMAN, I., laureat Gosudaretvennoy premii
Living model of a living system. Nauka i zhizn' 29 n0.5:83 Yq
t62. (Insect societies) (MIRA 15:11)

,PaIFMAN Iosif -Aronovich; ZUBKOV, M.A., otv. red.; TOKAREVA, T.M.,
tekhn. r-ed-.-
(Password of crossed antennaolParol skreshchennykh antenn.
Moskva, Detgiz, 1962. 413 p. (MIRA 16:2)
(Insects)

KHALIFMAN, I.
Ants and forest protection. Agrobiologiia no-3:474-476 YO-Je
163. (KIRA 16:7)
(Ants) (Forest insects-Biological control)

KHLLIFW, 1. A.
"Honeybees (Biology of the Honeybee Tmdly)." Sub 25 Ma," 51,
Moscow Order of Lenin State U Imeni M. V. Lomonosov.
DIBeertations presented for saienca and engineering degrees In
Moscow during 1951.
SOx Sum. No. 480, 9 MaY 55

KHALI RNIAN, I.A.
Pchely (Bees) . Izd. 2-e.
!!ozkva, Goskulttpro5vetizdat, 1952. 256 1).
SO: Monthly Li3t of Russian Accessions, Vol. 6, No. 1, April 1953

1. A. --- -- I
Br.,p Culture
Trained bees, Znanie-siltt, No. 1, 1952
9. monthly List of Russian Accessions, Library of Congress, March 1952 JW. Unclassified.

1. 1. KHALIFEAN
2. USSR (600)
4. Bees
7. "Bees". Reviewed by G. Avetisyan. Pchelovodstvo, 29 no. 12. 1952.
9. Monthl List of Russian Accessions, Library of Congress, April -1953, Uncl.

ol
Ir)lo
Vol 7, 54.

KIIALIFKANT, I.
"Bees and Fertility", p. 11. (PRIRCDA I UANIE, Vol. 6, no. 9, Nov. 1953,
Sofiya, T3u1g,,-,.ria).
SO: Monthly List of East European Accessions, LC, Vol, 3, No. 4, April 1~54

-KHAIIFRAUI- I.A., kiLndidat-biologicheskikh-naiik, laureat Stal Inskoy -prom I L
Bees and crop yields. Hauka i zh1zn' 20 no-7:12-14 J1 '53- (MMA 6:7)
(Yertilization of planta) (Bees)
F
JT

f I -I r- IV It/ IV) - It I I
GUBIN, A.F.; XUALUMAN, I.A.
i
(Pollination of farm crops by beos) Opylente sollskokhosiaistvannarkh
rastenii pchelami. Moskva, Znarlie, 1954. 30 P. (HLRA 10:4)
(Fertilization of plants) (Bees)