SCIENTIFIC ABSTRACT KORTSENSHTEYN, V.N. - KORTUS, J.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
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• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KORTSMISHUYN, V.H.-. BELYAMN D.So akademik.
Stratigraphy and litholog7 of Lower Phleozoic deposits of the Odessa re-
gion. Dokl.AN SSSR 90 no.5:857-869 Js 153. (MM 6:5)
1, Yeevoyasnyy nauchno-tooledovatellskiy institut-prirodnvkh gazov (for
lorteenshtsyn). 2. Akademiya nauk SSSR (for Bolyankin).
(Odessa, District-Usology, Stratigraphic)
Describes five layers of the complex terrigeneous sediments laid
down from bottom to top: 1) sandstone layer, 2) lower argillite layer, 3) lower
layer of interstratification, 4) upper argillite layer, and 5) upper layer of
interstratification, Presented by Acad D. S. Belyankin 1 "pr 53.
260T55
-LE.

KOWSRUSHTRIN, V.H.
Lower Falsosclo deposits In the Od~ssa District. Trudy VNIZ
no.4:29-~56 154. (NLRA 9:1)
(Odessa Mistriot-Goology, Stratigraphic)

0 f? T S E7 rq 9 T- (:-: y N , V IV.
Subject USSR/Mining AID P lo96
Card 1/1 Pub. 78 - 7/21
Authors : Kozlov,, A. L., Kortsenshteyn, V. N. and Savchehko, V. P.
.z
Title : Significance and methods of study of underground water
pressures
Periodical : Neft. khoz., v. 32,, #10, 30-34, 0 1954
Abstract : Genetic and hydrodynamic relations between gas deposits
and the level of the underground water contacted are
discussed. Precise knowledge of the static level is
considered important and various methods are offered for
Ito determination.
Institution : None
Submitted : No date

USSIV Geology - Hydrogeology
Card 1/1
Authors i Kortsenshtcyn, Vi. N.
Title 3 New data on the hydrogeology of Paleocone depositions of central
Caucasia
Periodical Dokl. AN SSSR, 96,, Ed.%5, 1047 1050, June 1954.
Abstract Dataon the.hydrody Inamic characteristics of underground waters-ofPaleo-
cene depositions'in the Stavropol upheaval md in the Mileralovodsk
ladr,e are given. - -These two geo-structures are closely connected idth.
each other in tectonic relations The underground waters of Paleocene
depositions discovered in above mentioned regions are distinguished not
only by piezometric characteristics, but by their unusual saturation with
carbonic acid. Three references. Graph.
Institution All-Union Petro-Gas Scient.-Research Institute
Presented by Academician., S. I. Mironov, March 31, 1954

. . . . . . . .- - - - -
mswkeology
Card
K V -
Authors prtsenshteynt N.
Title 1 dri 6'n of the Stavropol upheaval
rA rma con
Periodical Dolcl. AN Sssap-9161 60 1217'- 1220, June 1954
Abstract The goo-thermal-calculations given in the report characterize strata
found at depths of below 100 m. Hydrogeological factors are ass-inwd to
be'the major ones.affecting the geothermal conditions of the investigair-
ed 5tavropol:region. Four references. Tables, graphs.
Institution All-.Union Petro-Gas Scient. Research Institute
Presented by Academician S. I. Hironov, March 31, 1954

KORTSENSHTEYN, T.N.
Hydrochamiml. characteristics of the Xhadum water-bearing horizon
of the Stavropol Plateau. Dokl.AN SSSR 104 ne.5t771-774 0 155.
()GU 9:2)
l.Tessayusnyy nofteg"*vyy nauchno-issledomtel'okiy institut.
Predstamlens, akedemiken S.I.Mironevym.
(Stavropol Platema-Vater, Umdergroxmd)

KORTSENSHTEYN, V.N.
.11
rharacteristles of the dyn"Ics of undeground wAters of the
Khadum horizon of the Stavropol 'Upland. Gax.prom,no,5:5-8 My '56s
(KLItA 10 - 1)
. (Stayropol.Upland-Water, Underground)

YINS
Some aspects of the formation of under ground waters in the Raikop
horizons of Central and Northwestern Cie-Caucasia. Dokl. All SSSR III
no*611322-1325 D 156* (Kin 1013)
1. Tsesoyasnyy neftegasovyy nauchnoissledovatelfftly institut.
Predstavleno akedealkon S.I. Mironovyu.
(Caucasus, Northern-Voter. Underground)

Ne ).~ ~s c" W) i) * e-f iv
SUBJECTt USSR/Gsology 5-2-28/35
AUTHOR: Kortsonshtoya.1,1.
TITLEt Now Data-ei Hydrogoology of the Region North of the Central
Caucasus (NOT ye.dannyyo po gidregoologii toostrallnege
Pr*dkavkaslyal
PERIODICALi Byull*t*at Mookovskege Obahchostya Ispytateloy Prirody. Otdol
GG*16916heeklY 9' 1957, 29 p~161 (USSR)
ABSTRACTs Hydrogeological conditions In the region north of the Central
Caucasus aro.deterained .by the presence of numerous wator-boaring
horizons in the Mosonsic and Tertiary layers.
There are two hydrogeological provincest the south-eastern
(Mineralovedskly salience) and the northern sno (Stavropol'
elevation).
In the south-oastern province all water-boaring horizons or*
hydraulically interconnected due to the presence of considerable
sanselef fracturing. The feeding zone is located in the moun-
ainous part of the North Caucasus. The p9st-volcanio activity
Caxd /2 f the 211brus greatly affect* underground waterd, which results
!

I
'Al - ();~' /1' 15 IF A", 17/~' /- Y/V k".Icl:
KORTSBNSHTRYN, V.N.
-- .1 -1 -
iaoeous deposits In the western Black 3~a region. 21nidy
VNII no.11:84-114 '57. (MIRk 10:11)
(Black Sea region-Geology, Stratlgraphic)

ZORTSANSHUU. T.N.
Naw data on the hydrogeology of pro-looeeme deposits in central
Ciscaucasia. Indy VNII me.lltlW260 157. - (NM 10:11)
(Caucasus, Northern-Vater, "Underground)

07QUIN - -1 ?5m
New data on the hydrogeology of central Giecaucasia. Biul. MOIP.
otd. geol. 32 no.2-161 Mr-Ap 157. (MIRA 11:3)
(Caucasue, Northern-Water, Underground)

AUTHOR KORTSENSBTEYN V.N. 20-4-49/61
T,ITLE Data on the Underground Water Gas Saturation of the
Sediments of Mineral Water District.
(Novvyye dannyye po gazonasyshchemmosti mozozoyskikh vodonosnykh go-
rizontov Kavkazhkikh Ifinevaltnykh Vod.)
PERIODICAL Doklady Akademy Nauk SSSR, 1957, Vol 113, Nr 4, pp 896 - agg (u.S.S.R.)
ABSTRACT The high saturation with gases of the ground water in relatively lar-
ge areas of the Caucasic mineral spring is known.The springs origina-
te from the jurassio,oretaceous and lower plaeogen strata. CO is the
main component,near Essentuki and Pyatigorsk a content of metRane and
nitrogen,fluctuating within wide limits,can be found.By means of a
depth-sample-taking apparatus (system PD-3,produced by the factory
for control and measuring apparatuses of the Ministry for Mineral Oil
Industry), interesting data were obtained.A drill--:hole,northeast of
Essentuki (village Vinsady) was investigated to a depth of more than
1400 M- It is quite natural that in the case of such turbulent sprin-
ging forth from the drill-hole with so high a gas-factor(15-6%-18-8)
the same values of the quantity of dissolved gas from different depths
could hardly be expected.Degassing the water is already possible iz
depths of about looo m.After the first experiments in June 1955 they
were repeated in September 1956. This time the samples were not taken
from a sputtering drill-hole,but from the mouth and at 15 atmospher-
Card 1/3 es absolute pressure.'The results were similar,however,in the depths

New Data on the Underground Water Gas Saturation of
the Mesozoic Sediments of Mineral Water District. 2o-4-49/6i
of 700 , looo.and 1440 m values of the gas factors that had appro-
ximated each other were.obtain ed.For taking the samples a lubrifica-
tor of the usual structure was used such as is used for the sputt-
ering springs of minor.al oil.Illustrations I and 2 show the results
obtained.The ourve.of fluotuatione of the quoted volume of the diseol-
ved gas is striking.Prom the depths 1400 to 7o0 m its quantity.in-
creases from 16.0 to 16.8 1 per 1 1 water, which is directly conneo-
ted with the lowering of the temperature in this interval of depth.
In lower depths (400-25 m),however,the quantity of gas considerably
deoreases.This takes place by the loss of the free gas phase owing
to technical reasons on the occasion of sample taking.The authors as-
sume that gas bubbles develop as free gas phase in depths of 500-6oom.
The rising gas bubbles do not get into the sample taking apparatus
owing to its particular construction.The relatively low tamperature
of water(uP to 130) explains the lack of a gas cushon near to the
mouth. The waters contained in the lower cretaceous sediments are
highly saturated with C02(UP.to 37.g/1),which is 8-1o times higher
than the values known for the region.The here described situations
give evidence of the fact 'that the recent statments made by Smirnov
on the atmospheric origin of the GO 2 of the North-Caucasic mineral
Card 2/3 springs are unfounded.In the light of the above described investiga-

KORTSENSHTEYDI, V. N.
"The mechanism of gas deposit formation in the region of Stavropol"
report pre.,,:-,-ntcd nt- a Confereace In the Dept. of Geological and Geog-,ra-phicel
Sci., on ard Raliowatrical M-Whoes of Search fund Procpecat-ing
for Deposits, 21-26 April 1958.
(Vest. AL- uauk wm, 1958, wo. 7, PP. 125-26)

'-CT"'S
,,'Y?l 7 1y,
Gra~phic mrAhod for procoui~inr cbemical. eall.,a on under6-round wateTs.
Tr-udy TIM no.14':189-198. 15~. (M11&, 32:7)
(Water, UndarfTound)

20-.3-.45/59
AUTHORs Kortsonshtsyn, V. ff.
TIT13# Now Data Concorhing Gas Saturation of Underground Waters of
the Paleogene Strata of Central Ciscaucasia# as Related to
the Problem of the Formation of Now Gas Fields (NOVY70 dannyye
po gazonasyshchennosti podzemnykh vod paleogenovykh gorizontov
Teentrallnogo Predk&vkaz'ya v avyazi 9 voprosami formirovaniya
gazovykh zalezhey)
PERIODICALs 1. 1189 Nr 39 PP* 5T3 - 5T6 (USSR)
Doklady AN SSSRq 19564, Vo
.
ABSTRACTs The regional hydrogeological investigations In the afor*-sald
area were carried out for the purpose of determining the com-
position and the pressure of gases dissolved in underground
watereq which are in direct contaot with gas accumulations.
The author recalls a number of relations between the torm&.
tion of gas accumulations and the saturation with gas of un.
dorground waters (reference i). From the parameters used R -
denoting the saturation pressure of water (davleniye navy.n
shcheniya Yody) or the pressure of the dissolved gases (upru.
Card gow raatvorennykh gazov) is least investigated, Zvon the

20-3-45/59
Now Data Concerning Gas Saturation of Underground Waters of the Paleogene
Strata of Central Ciscaucasiaq as Related to the Problem of the Formation
of New Gas Fields
composition of the dissolved gases is not always known, not
to speak of the saturation pressure. This is an essential do-
fioiency of hydrogeologioal investigations. With regard to
these facts, the investigations on the saturation of the wa-
ters of the productive horizons of the gas producing district
of Stavropol' were conducted by the Institute for Natural Ca-
ses. Depth probes of water were taken by means of special
equipment maintaining its original pressure, the water being
the only phase in which gases are,entirely dissolved. Because
of the preswe lose in the probing instrument a two-phase sys.
tam is formeds Water-gas. The gas is then completely separated
from the water and investigated. The methods were discussed
In earlier papers of the institute. Here, the author enumerat-
es the parameters, which-have an essential influence on the
study of the saturation with gas of the water content of stra-
ta and on the results of the investigation. 1) The 0 volume of
the gas on normal conditions (760 mm, of mercuryl 0 0), Whicfi
is comprising the gas separated from the water as well as the
Card 2/5 amount of gaeg which remains dissolved at atmospheric pressure*
20-3-45/59
New Data Concerning Gas Saturation of Underground Waters of the Paleogene
Strata of Central Ciscaucasia# as Related to tho Problem of the Formation
of Now Gas Fields
2~ The gas composition- 3) The temperature of the layer.
4 The mineralization of the water in the strata. 5j Satura-
tion pressure. The results are compiled in table I missing)
together with the conditions of probe taking and other data.
According to these results schemes of the modification of
the total pressure of dissolved gaa6s in theater of the low-
er palsog*ne and Khadumakiy horizon were constructed. fi-
gures 1, 2). The following conclusions can be drawns 1~ The
water of either of the afor*-said horizons is sharply distin-
guished with respect to their saturation with gas. They are
a3parated from each other and have quite different regimes.
2 The palsogene horizons are saturated by hydrocarbons up
to 60 - 98.%,.which are mainly represented by methane. In
the Khadumskiy horizon the heavy hydrocarbons are almost en-
tirely missing (0#4 - 008 %). They are bound to the lower
paleogene waters (5 - 8 ~0. The nitrogen content of the lat-
tlr_i; higher (8 - 20 %) than in the Khadumakiy horizon
Card 3/5 The waters of the Khadumakiy horizon are in all
20-3-45/59

20-3-45/59
New Data Concerning Gas Saturation of Underground Waters of the Paleogene
Strata of Central Ciscaucasia, as Related to the Problem of the Formation
of New Gas Fields
Composition- 7) The gas accumulations of the Khadumskiy ho.
rizon are in a stage of growth. There are 2 figures, I table#
which is mentioned in the paper, is missing, and 3 referencesp
2 of which are Slavic.
ASSOCIATIONs All-Union Scientific Research Institute-for Natural Gases
(Vsesoyuznyy nauchno-iseledovateltskly institut prirodnykh
gazov)
PRESENTEDs July 5, 1957, by N. M. Strakhov, Academician
SUBMITTEDs July 2, 1957
AVAILABLEs Library of Congress
C&M 5/5

AUTHOR., 16 Ti. X. SOV/20-121-6-34/45
TITLEt On the Problem of Geothermic Depth Conditions in Ciscaucasia
(K voprosu o glubinnom geotermicheskom rezhime Predkavkazlya)
PERIODICAM Doklady Akedemii nauk SSSR, 1958, Vol 121, Nr 6, pp 1068 - 1070
(USSR)
ABSTRAM With respect to-depths from 1,5 to 2 km the problem mentioned in
the title remnined completely uninvestigated until recently.Since
ixtrap6lsti6fi of the curve describing the variations of tempers-
turFe'does'not show any reliable results the direct geothermic
mes6dringi iii de4p b6riholes-sre-extremely precious. The author
deals in'this ~'iper *ith depths fgom*'2-3 km wheri 6xtremely high
temperature$, for higher'than,-100 ',- were registered.-Hitherto in
pfiblicationis no-aLich-ififoizations halr6_ been dealt'with. 'According
to--iftdividusl-diaasurings in Wast--oCentfol, and East Ciscaucasia
th6.-euthor dkiwo s6mi goneril-coh6lusions from the results: The
interior of-thf North in Ciscaucasia houreletively high tempers-
turis in-depth-6 *h4re'boring is dtill p6ss-ible. In West- end East
vh4r@-96di6ints'ire 4-5 ii thick the"temperature is
0
Card 1/3 less then 200 . There is a striking contrast between this region

On the--Pr6blem of Geothermic Depth Conditions SOV/20-121-6-34/45
in Ciscaucasia
ind the ~Iaite'districls (Tate-riya, Baishkirpe). .. Tempiiature is in
i depth-from 1-2 km hardly Eore thin 40-50 .-According to the
aIuthoils op-inioi this difference is-due to hydiogeologioal and
geotec`tbEi8il_c6nditiohs;_By thi subterranean water moving from
d-i-6'p"-aep'iei-s16iii.ih-dik6o'tibn of uplifts in many cases the letter
ifiintioned.c6iiditions'fe-voi heat transfer. This is the cause of
the.hi~h tempiraWres which do usually not occur in these depths.
In.0thir"wSid5:1.' without iiater-is"heat transmitter from-the de-
pressloni~,wfiich,ere not jet a6dessible to boriiig the abov6-men-
t16neC.effoot'46~1d not be 066iible. This refers to the import-
ince, 0~:f*- the "iva'-fer pres'suri- 8--yatem (vodon6porfiiye sistems) in
6diinedtiofi"with.the-fe.rmation of geothermic conditions in the
ifitirior.of the'esith '('Ref.1)."Thu's the movement of water in Cia-
ceu6esia..&mounts_4t.iome plid4a4ven to 6ome dozens of meters per
i4ei, (Aifv 2), - iihii In Titeri a -and Baahkiilys_ it a6es' not ex-
cei'd 88me"C'eatiie'M -a.annusll~fRef 3), The *star mosses bubbling
from the--bbreholds ireach'-hundreds-of m3-per day and have a tempera-
ture from,.-90-950. ;They- are an-Ineyhowstible source of 'geothOrmic
4nerg7.Thiie pre 1 figure, I table, and 3 references, 3 of which
Cord 2/3 Pre Soviet.

On the*Problein of Geothermic Depth Conditions SOY/20-121-6-34/45
in Ciscaucasia
'ASSOCIATION: Vs*ioyuzxiyy nsuchno-is~l6db*stel1skiy institut prirodnogo gaze
(All-Union Scientific Research Institute of Natural Gas)
PRESENTED: April 12, 1958, by S.I. Vironov, Member, Academy of Sciences,
USSR
SUBMITTEDt April 119 1958
Card 3/3

KORTSENSII-IEYN,, V.t~., Doe Geol Lin Sci -- (diss) tudy of the
water-,"Poem*" syntem of Cbntral 400-caucusus n
1\ ilnE
problems of the formationj prospecting)and mining of gas deposits."
Mos, 19591 34 PP (,AII*Union Petroleum Uaz; Sci Res Inst VNII. All-
Union Sci Res Inst of Natural Gases W7IIGaz) 150 CODieS. List of
j~Luthorls works at end of text (17 titles) (KL, 36-59, 113)
- 20 -

3(0)
AUTHOR: Kortsenshteyn, V. N.
TITLE: A Zone of Helium-bearing Ground Water in
of the Monocline of Central Cis-Caucasia
zastoynykh podzemnykh vod yurskikh otlozlieniy
Tsentrallnogo Predkavkazlya)
SOV/20-12a-1-471/67
the Jurassic Sediments
(0 zone geliyenosnykh
monoklinali
PERIODICAL: Doklady Akademii nauk 333R, 1959, Vol 125, Nr 1, Pp 173-176
(USSR)
ABSTRACT: New hydrologic data, concerning several bore holes, collected in
the region between Cherkeask and Ispravnaya (Fig 1) have ehown
that numerous helium-bearing and mineralized thick water re-
servoirs of pronounced stagnant character are connected with the
sediments mentioned in the title, The latter condition does not
fit into the familiar hydrogeologic scheme of the region, ac-
cording to which this monocline should be a zone of active water
exchange of the source area of the Mesozoic horizons. Testing by
means of special equipment (Refs 2,3) has made collection of the
most important hydrochemical data certain for the first time.
The author deals with the d i s s o 1 v e d g a s e s
Card 1/3 (Table 1), gives h y d r o o h e i:i i c a I f, h a r a c t e r -

SOV/20-425-1-47/67
A Zone of Helium-bearing Ground Water in the Jurassi~~ Sedi-r-er-to of the Mono-
.cline-of Central Cis-Caucasia
i s t i c 9 of the water, and stresses h y d r o d y n a m i c
p e c u 1 i a r i t i e s . On the basis of these data he draws
a o m e g e n e r a 1 c o n c 1 u s i o n s . As is known the
radioactive decay of various miners,13 disseipinated within sedi-
mentary and eruptive rocks forms the only source of helium in
ground water. The amount of the dissolved helium is proportional
to the amount of radioactive minerals in the rock, to the time
span of helium accumulation (Refs 1,5), and finally to the de-
gree of hydrogeologic isolation in the earth's crust. Therefore,
the approximate hundredfold greater helium content in the zone
of an active water exchange, compared with the analyses cited
here, is understandable. Here, the unique conditions of the
water-bear-4ng rocks, whi-ch are enclosed bet-neen Paleozoic base-
ment and the clayey Lower Cretaceous sediments, plays the de-
cisive role. The age determination (Refs 1,,r) ga7e values be-
tween 627 and 1234 milli-on years. In this case the forraulas of
these references may not be applicable. It may be also that
special conditions of accumulation are to blame for it. In spite
Card 2/3 of interpretive difficulties the origitial source of the 'helium,

BOV/20-125-1-47/67
A Zone of Helium-bearing Ground Water in the Jurassic Sediments of the Mono-
dline of Central Cis Caucasia
must be viewed not as Jurassic but as older rocks (crystalline
basement and metamorphosed Paleozoic) (also compare reference 6).
The oil and gas possibility is clearly negative here. The
strongly ascending saturation pressure of the Jurassic rocks
west of the Cherkesskoye uplift is interenting with regard to
the occurrence of gases containing carbon dioxide, nitrogen, and
methane. There are 1 figure, 1 table, and 6 Soviet references.
ASSOCIATION: Vaesoyuznyy nauchno-issledovatellskiy institut prirodnykh gazov
(All-Union Scientific Research Institute for Natural Gas)
PRESENTED: October 11, 1958, by N. M. Strakhov, Academician
SUBMITTED: October 9, 1958
Card 3/3

3(5)
AUTHOR: Kortsenshteynp V. NO SOV/20-128-3-43/58
TITLE: Some Rew Data on the Tectonics of Central Ciecaucasia in
Connection With Hydrogeological Investigations
PERIODICAM. Doklady Akademii nauk SSSR, 1959, Vol 128, Nr 3P PP 590-593
(USSR)
ABSTRACT: The investigations of reoent years mentioned in the title
(Refs la - 3) make possible the indication of several fracture
dislocations in various h6rizons of Lower Paleocene deposits.
These fractures explain - in a most simple and convincing way -
several peculiarities of the pressure of subterranean waters as
well as their hydro- and geochemistry. It can be asserted that
distinct regional changes in pressure and other characteristic
values are mostly bound to tectonio fractures* They interrupt
the c'onnection of the water-bearing horizons# and build up,
sui Seneris, subterranean dame with a lower and upper crown
(under water, upper water). The damming caused by the fractures
explains the sharp zonal hydrodynamicalt geo- and hydrochemicall
Card 1/3 sometimes also goothermalg contrasts (Ref 1b). There are much

Some New Data on the Tectonics of Central Ciscaucasia SOV/20-'128-3-43/58
in Connection With Hydrogeological Investigations
more fractures than is generally assumed, but they lie in the
depth, and are difficult to ascertain. Therefore the respective
knowle&ge of geologists is often derived from the investigation
of hydraulic systems (Ref 3)- Only the most important
fractures of regional character are discussed here, It is
possible that they will be finally proved by other geological
methods. The d i a t u r b a n c e of M i n e r a n y y e
v o d y (Fig 1: 1 - I, Refs 16, 1 d, e);
S a h~ g 1 1 e y e v a k o y e d i a t u r b a n c e
(Figl, 11 -119 Rof 1 zh, z); Ube Z'he nskoye
d i s t u r b a n a e Fig I : III -, III, Ref 1 zh); Kuba~koye
di s turbanc. e RiglzIV.- IVt.Ref 1 zh).
It is interesting that the Kubaruskdje diiturba*dd 1-ies very
exactly upon one of the transverse inflections of Ciscaucasia
Yu. P. Masurankov, Ref 2); Manyabskoye d i a t u r b a n c e
ig I A Va V, Fig 2 g, Ref I zh). Figure 2 shows some details
R
Card 2/3

Some Now Data on the Tectonics of Central Ciscaucasia SOY/20-128-3-43/58
in Connection With Hydrogeological Investigations
of tectonios of Central Ciscaucasia. The deliberations made
here do not claim that the disturbances mentioned should be
considered evident. From the author's point of view, they
explain many hydrogeological rules in the best way. There are
2 figures and 3 Soviet references.
ASSOCIATION: Vaesoyuznyy nauchno-isaledovatellskiy institut prirodnogo gaza
(All-Union Scientific Research Institute of Natural Gas)
PRESENTED: March 23, 1959, by N. S. Shatskiyp Academician
SUBMITTEDi February 20t 1959
Card 3/3

KORTSM Mi. Tollf _N_ukhixo_Y_Iph.L OTCHMIKOV. A.K., doktor geol.-miner.
wa-,red.; SHORMOVA, L.I., vedushchiy red.; PMOSMA, A.S.,
tokhn.red.
[Hydrogeology of the go*-bearing area of central Ciscaucasia;
in connection with studies of the forwtion, investigation. and
development of ges pools] Gidrogeologiia gasonoonoi provintoli
25entrallnogo Prodkovkazlia; v oviazi a voprossal foralrovaniia
razvedk:L i rezrabotki gazovykh salesbei. Pod red. A.K.Owchinni-
kove. Koskva, Goo.nauchno-tokhn.isd-vo neft. i gorno-toplivnot
lit-ry, 1960. 260 p. (MIU 13:12)
(Caucasus, Northom-Goz, Natural--Geology)
(Caucasus, Northam--Water, Underground)

Principal results of hydrogeological research in the Stavropol
gas-bearing province; 1953-1959. Trudy VNIGNI no-32:122-151 160.
.(MMA 14:7)
1. Vsesoyuznyy nauchno-issledovatellskiy institut prirodnogo
ga2,a,
(Stavropol Territory-Gas, lbtural--Geology)
. (Stavropol Territory-Water, Underground)

1:oxinum pooLible concort.1',%tion or diusolvod ~-~~xocar,:ons in
undurl'yovrAt uuters of Crcj-,'-,,c:cous horii,=,u of Ciauauc,-.~;ir- in
I
tion w*1 -Lh tho outim4tion of -,,roz;- ective oil and L;as roz5ourc--s
of 1:-,cczoic Dold. AV SLiL41~ i37 no. 1:162-16' '~r-Ap
I
1. VL;Uao";,vzr"V-y
Cazcv. Prk~d~t-vlez:o Trofi:,,,.ukom.
(Alatuoia, Sou~L-1urr-41'k4cor, Vndor,-~rou.,d:;
(Potrolatin --oolo,,-y' (Gao, I:Ltvral--Geo1oL?y)

KORTSENSHTEYNO V.N.
Somis problems of thojory and practice In the estimation of oil and
gaupotentials an the basis of hydrogeologic criteria. Sov.geo:L. 4
no,,4:17-27 Js 161* (MIRA 34:15)
1. VuesoyuzAyy nauchno-iosledovateltakiy institut prirodnogo gaza.
(Petroleizi geology)
(Gas, Natural-Peology)

~IIS ~11_ --,-V-,jKortsenshteyn, V. N.]
_;,!ORTEWSTEIII, V
Son6 problems in the.theory and practice of evaluating the
petroleum and gas prospects accordivig to hydrogeologic criteria,
Analele geol. geogr 16 n0.1:45-56 Ja-Mr 162.

KORTSENSJITEYN, V-N,
Mechanism of the discharge of deep underground waters into the
Caspian Depression. Dokl. AN SSSR 142 no-3:667-669 Ja 62.
(?/,IRA 15:1)
1. Vsesoyuznyy nauchno-issledovatel'skiy institut prirodnogo gaza.
Predstavleno akademikom D.V.Nalivkinym.
(Caspian Depression--Runoff)

KWSFMIITEYN, V.N.
- ---------
Recent geother.=Ll data on the Bukhmrs-lbiva 0i-1 amd gas bearir79
lxrovince. Dokl.AN.SSSR 145 no./+:875-878 Ag 162. (MM 15:7)
1, VaesoyumW mmohno-iseledovatellskiy inatitut prirodnogo
gaza. Predetavleno akademikom D.V.Nalivkinym.
(Uzbekistan-Earth temperature)
w

KORTSENSHrEYN. V.N.
Hydrogeology of the Gamli gas field and adjacent regions. Trudy
VNIIGAZ no-15:3-143 162. OaRA 1518)
(Gasli region-Water, Underground)
(Gazli region-Gas, Natural--Geology)

KCRTSENSHTEYNI V.N.; KAWEVAI A.F.
Conditions for the formation of deposits of carbonated mineral
waters. Geol,i Seofiz. no.5:132-135 162. (MM 15:8)
1. Vseaoyuznyy nauchno-issledovateltakly Institut prirodnykh
gazov i TSentralinyy institut kurortologii i fizioterapii., Dbskva.
(Mineral waters)

KORTSENSHTEYN, Vollf Nukhimoidxh. doktor geol.-miner. nauk; Prini-
mali uchastiyet SPEVAK, Yu.A.;ZHIGALIN, B.I.; MUKHIN,
*fu,,V., kand. geol.-miner. nauk, nauchnyy red.; BOGACHEVA,
N.G., ved. red.; STAROSTINA, L.D.j tekhn. red.
(Methods for hydrogeological studies of oil- and gas.
bearing regions) Metodika gidrogeo6logiobbakikh iseledovanil
neftegazonosnykh raionov. MoAv's., Gootoptekbizdett, 1963.
167 p. (MIRK -16t 5)
(Oil field brines)

KORTSFM:HTMO V.N.
Theory of estimating oil and gas potentials from data on the
g,,ae saturation of mderground waters under conditions Of
ohifted phadeequillbrim. Dokl., AN SSSR 150 no.3s635-638
W "63, (MIRA 16:6)
L Vaeaoyuznyy nauchno-isaledovatellskiy institut prirodnogo
gaza. Pz*dvt&vIeno akademikom N.M. Strakh
(Phase rule and equilibriumro
(Oil field brines-Analysis)

KORTSENSHTEYN, V.N.
Origin of carbon dioxide in Lower Cretaceous gas pools of
western Ciscaucasia.- Dokl. AN SSSR 152 no.2:434-437 S 163.
(MIRA 16 ill)
1. Vaesoyuznyy nauchno-issledovatel'skiy institut prirodnogo
gaza. Predstavleno akademikom N.M. Strakhovym.

KORTSENSHTEYN, V.11.
Some features of the water-pressure system of the Ciscaucasian
Mesozoic. Dokl. AN SSSR 152 no.3:706-708 S t63. (MIRA 16312)
1. Predstavleno akademikom A.A.Trofimukom.

KORTSENSfITEYN, V.N.
8ubsurface geothermic conditions in Ciscausia. Dokl. AN SSSR 154 no.6:
1334-1336 F 164. (MIRA 17:2)
1. Vsmsoyiiznyy nriuchno-issledovatellskiy institut prirodnogo gaza. Pred-
stavleno akademikom D.V.Nalivkiriym.

KORTSENSIITEYN
Forecasting oil and-gas potentials according to deep investigations
of underground waters ard the estimation of probable oil "d gas
reserves. Dokl. 0 SSSR 158 n0-4:856-859 0 164.
(RIR,A 17:11)
1. Vsesoyuzvtyy nauchno-issledovatellskiy institut prirodnogo gaza.
Predstavleno akademikom A.A. Trofimukom.

KORTSENSHTEYN, V.N.
Subsurface geothermal regime of the South Mangyshlak trough.
Dokl. All SSSR 159 no.2036-339 N 164. (MIRA 17.-12)
1.*Vaesoyuznyy nauehno-issledovatellakily institut prirodnogo gaza.
Predstavleno akademikom D.V. Nalivkinym.

Tj 11. 11
C020gy of' the La;
in connection 14,thl 1-Le
ga
,Mel
pools, their f-),. . tiov., and Jov,-,.-cpint-,-%--. Tmady
VNITGAZ
17:10)

KGRTSENSHTEYN, V.N.
Analysis of the observations of the variations of the undisturbed
natural regime of the Paleogene water pressure system in central
Ciscaucasia under the effect of the development of gas fields,
Dokl. AN SSSR 162.no.2t4l&421 My 165. (MIRA 18s5)
1. Vaesoyusnyy nauchno-iseledovateliskly institut prirodnogo gaza.
Submitted December 22, 1964,

the
,,art ~'Il' lh~t Mvjwy,-hh,k :fri*--r-,,;d!d. I.A-A''. I'Ll I,
(MIRA 18:2.0)
2. Vgc,.,ioy-u-7n.,ry n og o
gaza. SULTi-Ittij 9, 1965.

FROLOV., N.M.; AVERIYEV, V.V.; DUEHIN, I.Ye.; LYIJBIMOVA, Ye.A.; Prinimali
uchastiye: GOLIDNW, V.M.; MAVRITSKIY, B.F.; SEDOVp N.V.;
YAZVIN, L.S.; KUTASOV, I.M.; STARIKOVA, G.N.; KORTSENSHTEYN, V.H.,
red.
(Methodological instructions for studying thermal waters in
boreholes.] Metodicheakie ukazaniia po izueheniiu termallnylch
vod v skvashinakh. Moskva, Nedra, 1964. 139 p. (Moskow. Vse-
soiuznyi nauchno-iseledovatellskii institut gidrogeologii i
inzhenernoi geologii. Trudy, no.17). (KERA 19;1)
1. VseBoyuznyy nauchno-issledovatellskiy institut gidrogeologii
I inzhenernoy geologii,, Moskva (for Frolov, Golldberg, Mavritskiy,
Sedov, Yazvin). 2. Institut vulkanologii Sibirskogo otdelezliya
AN SSSR (for Averlyev). 3. Institut merzlotovedeniya. AN SSSR
(for Dukhin). 4. Institut fiziki Zemli AN SSSR (for Lyubimova,
Kutasov,, Starikova).

TOPTOSYTIN-3.3KIVY , YA. 1".
'T[5
661.6
.K8
Belastungsprufungen von bauwerken und konstruktionen. Lelpzig, Fachbuchverlag, 1955.
140 p. illus., diagra.. tables. Translation from the Russian: "Naturny7e ispVt.%,3iya
stroitell,7kh konstrulctaii".
"Literaturnachweis": p. 140.

------------------
i7

-Tc .4-r.-2
F~ S III I S -131 a
jr, t'
L,t
PI:
i1.19, Bind F() r -3
uP, -L a I Cor S t an t s

I
r
I I
- 11 ria zwuk;.L,,v - tu -- -~- rvs~ -
. . all ra -- , --- inat-i-- -t- Ariatallograf jj7:-AU-SS&R,jjnatitutti~ -~t'
-- 1, an co-orit -, .,a I-

DISTLERP G.I.; SOTNIKOV, P.Sy KORTUKOVA, Ye. 1.
Effect of the stz-ucti=e of po2yvinyl alcohol films on the mechanim
of their pyrolysis. Dokl. AN SSSR 156 no. 3:652-653 164.
(MIRA 17:5)
1. Institut kristallografti AN SSSR. Predstavleno akademikom
V.A.Karginym.

ACC NR, AP6011584 SOURCE CODE: UP/0051/66/020/003/054I/0541
Kortukova,-Ye- 1.,q- Lebedelm,
AUTHORS: Distler, G I.; kotovt~ A.
V. N.
ORG:. none
TITLE: New infrared polarization textures
1966, r-41
SOURCE: Optika spektroskopiya, v. 20, no. 3
TOPIC TAGS: light polarizationi polarization filter, ir optic system,
ir spectroscopy
ABSTRACT: This Is a continuation of earlier work (Opt. I spektr. v. 5..
219, 1958 and v. 4, 41qj 1956) done at the Institute of Crystallography
AN SSSR on the creation of optical textures tfiat_-~-515-rlze 1hrrared rut
1-f _o HE 71 b epresent note describes new optical textures (PTI-3) which
polarize radiation up to 6.5 p. The textures have sufficiently high
transparency and high degree of polarization. A plot of the polariza-
tion curves and a table listing the transmission and degree of polariza-
tion for different wavelengths are presented. The table shown of the
.spectral transmission of the textures reaches 40% and their degree of.
polarization is close to 100%. The samples have absorption bands at
Card 1/2 UDC: 535.5-15

__ACC NRi AP_6_0l1584________
3, 3.4, and 5.8 ~L,* due respectively to the vibrations of the hydroxyl,
methylene, and carbonyl groups of the polyvinyl alcobo'y bind ing, medium
The textures can endure temperatures to at least 100C I-or a long time
without noticeable change in the optical charactert3tics. They should
find application in the infrared spectroscopy and in optical ifistrument
building. Orig. art. has: I figure,-.and 1 table.
.SUB CODR: 20 SUBM DATE: 07Aug65 ORIG REF: 002

MXESSION NR: AP5019759
of the forbidden gap of the films is 0,15 ev, the transi-rions of the electrcna in
~ntri-isic: absorption region are direct, an(4 th- uf the lr;Sb
I s a~'.i-'buted ~c the
e q., rll'u.i eIhan that of the s-ingle ci- I
ca,ri-r densit,
y in. t he produr-l j-
hr
I'i6-urea and I table. IIG2j
ASSOCIA1170N.- none
SUBMI'I'l =,: i itn64 ENCL: CIO Sr-,,0P
I= II(TV, Ci()! OTHER-. X~ 3

. KORTUNUV . A.
Gm industry on the eve of the 22d Congress of the CPSU. Gaz.
p:tom. no.10zl-7 0 261. (M32A 34M)
(Gas industry)

KORTUNOV, A.
Gas industrT at a new stage of its development. Gaz.prom. 7 no-1:
1-3 162. (MIRA 15-1)
(Gas industry)

I KORTMIOVP A. Minister of-(~onstruction for the Oil Industry
"Some Problem in Building Large Pipelines.," Pravda., p. 20 9 Doc 55
Translation - Current Digest of the boviet Prew., Vol-7., No.49., page 29., 18 Jan 56

KORIVNOV, A. K., Minister or Constru~,tlon of Petroleum Induatry EnterpriGes
"For a Further Increase in Construction" Stroitel'stvo predpriyatiy neftyanoy
promyshlennosti, No. 1, March 1956, PP- 1-3.
The author makes a vivid comparison between what the Ministry of Construction of
Petroleum Industry Enterprises has accomplished during the 1951-1955 Five Year Period
and what it has to accomplish according to the 1956-1960 Five Year Plan. A number
of figures, straight and in percentage, are given.
SurmarY - 55o426

- .. - -I tq~
ll'o' , 7- c t i,,' ,,, v, I //~, /,~' -
Pipeline transport In the U.S.S.R. Strol.prod.neft.pron.2
no-10:1-3 0 157. (KIRA 10:10)
m
1. Nachallnik Glavnogo uprayleniya gazovoy provqahlennosti pri
Sovete Kinistroy SSSR.
(Pipelines)

USSR/General Problems. Methodology. History. Scientific A
Institutions and Conferences. Instruction.
Questions Concerning Bibliography and Scien-
tific Documentation
Abs Jour Ref Zhur-Khimiya, No 3, 1958, 6823
Author A. K. Kortunov
Inst
Title Gas Industry to the 40th Anniversary of the
Great October Revolution
Orig Pub Gaz. prom-st'. 1957, No ll~ 1-3
Abstract No abstract
Card 1/1
WRTUNOV, A.K.
nic&l progress jLnd means for lovering the cost Of
courses of tech 3 no.5:1-5 MY
pipeline construction. Stroi. prod. neft. Prom- (MIRA
I.Nachallnik Glftvn099 'UpravlOuiYu gazovoy prowahla'=08ti pri Sovets
ministrov SSSR. (Pipelines)
V

KORTUOV, - A.K. -
-~- -
- - , f
-,.- ,
low stage in the development of the gas industry. (6w. pros. no~4:
1-3 Ap 158. (HLU 13:34)
(Gas industry)
~'N

KOXWOV, A.Z.
Further developuent of the gas industry, Gas. prom* no.10tl-3
0 158, (NIU U:n)
I
(Gas manufacture and worics )

11(2,4)' PHASE I BOOK EXPLOITATION SOV/2536
Moscow. Institut neftekhimicheskoy I gasovoy promyshlennosti.
Problezy nefti I gaze (Oil and Gas Problem) Moscow, Gostoptekhizdat, 1959.
362 p. (Series: Its: Trudy, vyp 24) Errata slip Inserted. 2,000 copies
-printed.
Sponsoring Agency: Ministerstvo vysshsgo obrazovaniya SSSR.
Exec. Ed.: G. F. Morgunoval Tech, Ed.: I. G. Fedotovaj Editorial Board;
K. F. Zhigach, Professor (Reap. Ed.), I. M. Muravlyevp Profeasorp A. A.
Tikhomiroyp Candidate of Economic Sciencesp V. N. Vinogradov, Candidate
of Teohnidal Sciences, M. M. Charygin, Professor, F. F. D=ayev, Professor#
I. A. Charnyy, Professor, V. N. Dakhnov, Professor, G. M. Panchenkov,
Professor,
PURPOSE: This collection of articles is intended for specialists in the
petroleum and gas Industry, It will also be of interest to scientific
renearch inatituteep teachers and students of vuzes.
Card 1/6

Oil and Gas Problems SOV/2536
COVERAGE: This collection of articles revievs problems connected with natural
and synthetic gas production. A number of articles are devoted to the
study of regional oil- and gas-bearing zones, the crystalline beds underlying
the Volga-Urals petrclif.arous region, tectonics of the C68Pidn depression,
seismic prospecting, oil well logging, development of oil and gas fields,
petroleum-bearing formations and their physicochemical characteristics, and
petroleum engineering. Other articles deal with gas turbine enginfeand
their possible use in the oil and gas industry, the production of carboxy-
methyleellulose compounds, the application of ionic exchange tars to the
organic cataly~sis, continuous coking of heavy petroleum residues, (fluidi-
zation), the improvement of lube oil production, and the influence of
acid esters on properties of lubricating oil and grease. The book contains
a number of photograpbe~ tables, flow sheets, and diagram, among which
those relating to coal gasification and conversion of heavy petroleum reai-
dues over a fluidized bed catalyst deserve special attention. References
accompany Individual articles.
TABLE OF CONTENTS:
._~ortpqy_,, A. K. Development of the Gas Industry in the USSR 3
Yerofeyev, N. S. Problems in the Search for New Gas Fielft 38
Card 2/6

Oil and Gas Problems
SOV/2536
Bakirov., A. A. Classification of Large Petroleum-and Gas--Bearing Provinces
(Regional Zones) and Geotectonic Regularity of Their Distribution Under
the Earth's Crust 43
Florenskiy, V. P. (Deceased)p T. A. Lapinskaya, and V. S. Knyazev. Some
Results of the Petrographic Study of Crystalline Beds Underlying the
Volga-Ural Petroliferous Province 65
Kazakov, M. P. Tectonic Pattern of the Caspian Depression and Adjacent
Regions 85
RyabJnkin,, L. A. Application of Reproductive Photoregistrations in
Seimic Prospecting 95
Larionov., V. V. Study of Porosity and Saturation of Oil Reservoir Rocks
by Applying Radiometric Methods in Oil Well Logging 107
Shchelkaohev, V. N., N. N. Baranovskaya., G. L. Govorova,, and M. A. Guseyn-
Zade. Investigations Made by the Department of Theoretical Mechanics
in the Field of Subsurface Hydrodynamics and the Development of
Petroleum-Bearing Strata 122
Card 3A

Oil afid Gas Problems
SOV/2536
Gharnyyj I. A., and I. D. Umrikhin. Determination of Parameters of the
Formation Made on the Basis of Observations of the 0111 Well Un-
stabilized Inflow 140
Kershenbaum, Ya. M. Manufacturing Gone-type Rock Bits 146
Kuzmak, Ye. M.9 A. I. Kurdin, and K. P. Yefremova . Tnereasing the
Wear Resistance of Rock Bits by Reinforcing Them With a Hard
Metal Alloy 156
Tomlenov, A. D. Stability of Biaxial Plastic Tension 170
Markhasin, E. L. (Deceased), and A. A. Petr,)synri~s. Cutting Tempera-
ture in Round Milling Performed by Plane Cutters 174
Belokon', N. 1. Thermodynamic Processes of Ga6 Turbine Units 183
Porshakov., B. P. Comparable Characteristics of Gas Turbine Unit
Systems 233
Card 4/6

Oil And Gas Problem
SOV/2536
Bichentay, R', N. Gas Turbine Engines and Prospects of Utilizing Then
in Petroleum and Gas Industry 246
Zhigach,, K. F.,, M. Z. Finkel'shteyn, I. M. Timokhin, and Ye. M.
Mogileirskly. Study of PbyBicochemical Properties of Fractions and
Lov Folymerization Compounds of Carboxymethyleellulose, and Their
Production 257
Topchiyev.,.A. V., Ya. M. Paushkin, I. F. Bayev, M. V, Kurashev, and
0. 1. Shuleshov. Present State of the Synthesis of Benzene
Homologs and Their Chenical Processing 269
Isagulyants, V. I. Ionic Exchange Tare and Their Application to
Organic Catalysis 286
Gurvich,, V. L. (Deceased), A. I. Skoblop Ye. V. Smidovich, N. P.
Zsyts9va.# N. S. Kazanskayap V. N. Petrov, A. S. Suvorov, and
A. A. Shcherbakov. The Process of Continuous Coking of Heavy
Petroleum Residues Carried Out Over a Povdered Coke .298
Card 5/6

AUTHORs Kortunovp A.K.p Engineer SOV95-59-2-5/13
TITLE. On the Construction of the Trans-Canadian Gas Pipeline (Ha
atroitelistva Tran4kanadskogo gazoprovoda)
PERIODICALt Stroitel'stvo truboprovodov, 1959t-Nr 2p PP 11-15 (USSR)
ABSTRACT: The author visited with a group of specialists of the Glav-
gaz the ooneiruotion sites-of the Traz)s-Canadian Pipeline.
In zhis article he given a briof description of all the main
phases of construction pertaining to the pipeline as well as
of the various installations, such as compreesor stations,
aoruboop"res for cleaning of gap, water coolers, etc. In
referring to machinei and equipment used by constructors the
author drawn soiie comparisons with Soviet machinery an 'd
methods. The article concludes with a series of recomimend-
ations pertaining to urgent improvements to be introduced in
the USSR - in technology its well as in equipment - to attain
a higher degree of efficiency in the construction of pipe-
lines.
There are 10 photographs and 1 map.
Card 1/1

KORTUNOV, A.K.
Development of the gas industry in the U.S.S.R. Trudy 14INOW no.24:
3-37 '59. (MIRA 13:3)
(US, Natural)

-', g1p4MOT., Alsksey Kirlllavlchl ZEMAYOVICS. Osorgly Tyachoslavovich;
GOOMMIT, Vladijil' i~iw-vlchj IM, I%odomly Afanamlyevich;
KLIMUSHIM, Alsksandr Mikheylovichl SOLQWIK, G.Te., vedushchly
red.; POWSINA9 A*Gas tokbnend* Il..--.
[Us pipeline In Cando: construction and exploltatichl Gazovala
megistrall lansay..stroltellatTO I skepluatatells. Pod redo A.Z.
Kortunovs. Koakvs, Gosnauohno-tekhA.lzd-vo neft. i gorno-toplivnol
lit-ry. 1960. 258 p. (Him 13:5)
(Canada--%a, latural.-PIpallnes)

Kortunov, A- N.
0
The potential of the USSIR gas industry. New York,,
U.S. Joint Publications Research Service, 1960.
171 P. tables. OPRS: 3177-D)
Excerpt translated from the original Russiant
Gasovyye rusursy SSR9 Moscow, 19599 ppe 5-103.

jKORTUNDV, A.K. - -
Gas industry Iti 1960. 5 no.I:I-4 Ja 160.
(MIRk 13:4)
(Gas industry)

KORTUEOV2.A IZVIN~ F.D., red.; YERSHOV, P,R.j ved.
red,; TROMOV, A.V., tekhn. red.
[Years of a great upsurge; gas indu.,--'Vry to the 22d Congress of
the CPSU] Gody krutogo podwema; gazovaia promyshlennost' k XXII
suezdu KPSS. Moskval Gos.naucbno-tekhn. izd-vo neft. i gorno-
toplivnoi lit-ry, 1961. 49 p. NM 34: 12)
I*Nachallnik Glavnogo upravleniya, gazovoy promyehlennosti SSSR
(for Kortunov).
(Gas industry)

RASHIDOV, Sh.; ALIMOV, A.; KORTUNOV, A.
To the Central Committee of the Communist Party of the Soviet Union,
the Council o'f Ministers of the Soviet Union) and to Comrade N.S.
Khrushchov,, First Secretary of the Commmist Party of the Soviet
Unior and Chairman of the Council of Ministers of the Soviet Union.
Stroib truboprov. 6 no. 2-2 F 161. (MIRA 14:5)
1. Sekretarl TSentrallnogo komiteta Kommunisticheskoy partii
Uzbekistana (for Rasbidov). 2. Predeedatell Soveta Ministrov
Uzbeksk SSR (for Alimov). 3. Nachallnik Glavgaza SSSR (for
17
Kortunov
(Uzbekistan-Gas, Natural)

KORTUNOV. Aleksey Kirillovich
Now stage in the development of the gas industry, Zhil.-kome
khoz. 12 no.6t8-9 Je 162. (MIRA 15A2)
1. Ministr SSSRt nachallnik Glavnogo upravleniya gazovoy
proqrshlennosti pri Sovete Ministrov SSSR.
(Gas, Natuiel)

KORTUNOV0A.K.
Gas industry on tha threshold of 196~. (6z. f-rcm. 8 no.!.i-3~63
~MIRA 1,7-.-)

OvPral", mec'narlization of' the consimc:".1or cl,
-18z
38 (,'.11 RA
Fred6eulatell Go3udarstvenncgo rro,- ;,--r cis~. unogo komi-'eta p0
gazo-xoy prurnysbienrost] SSISR, MLn"atr SSSR.

KORTUNOV, A.K.
Gas industry of the Soviet Union. Neft. khoz. 42 no.9/10;
13-17 S-0 164. (MIRA 17;12)

KORTUNOV, A.K.
Final year of the seven year plan for the gas iydustry. Gaz. prom.
10 no.1:1-4 165. (MIRA 18:10

KORTUNOVI A.K.; KORSHROV) le.S.; KU',11BUSOV, P.L.; BARABASH, B.B.;
I- ----N~6kNV, A.I.; SaKIROV, M.Z.; ALI-ZADE, M.A.; KHOODUAYEV,
A.K.; ALEKSODROVp A.V.p red.
(Gas indul3tl*y In the U.S.A.) Gazovaia pronWahlennost' SShA.
Moskva, Nudra, 1964. 339 P. (miRA 18:9)

L 27955-66
XCC NR-,--jMOl?739 SOURCE CODE., 57669--e,16 )00 0016
AUTHCR: Yuryshev, A. N.; Vasiltyev, N. P.; Skomorovskiy, Ya. Z.; Kortumno V. A-4
Yeliseyev, M. Ya.; Vaynshell A. Z.
ORG: none-
T1TLE:_ Determination of the-parameters to beconaidered for anchor reinforc=ezav
of pipelines
SOURCE: Stroitellstvo traboprovodov, no. 1p 1966, 16-19
TOPIC TAGS: pipelines concrete. .- I I ,III~I
ABSTRACT: Jhe first operations on the introduction of thiiaid~d anchors lit
b-6
nereto ballast in swampy or flooded regions in the USSR are goil
~on under the auspices of the Ministry or the Gas Industry# Experiments
Yerformed in.1065 showed that troadod anchors have great advantages of
of
lightness and cheapness over concrete ballast Anchors consistint, two
threaded rods plus a -barid- -to -g'o -over- the- top-- of a -pipe -sia-U-1-3brivem
!designed. with tread blade diameters from 250 to WO mm, thread intervals of
mm, These anchors exe to be tested on the Belousovo-Laningrad gas
!pipeline. The authors demonstrate in this article a calculailon method which
ithey have developed to determine the loads.and requirements placed on the
lanchor devices they have designed for the cases where the limiting ftetors in
Icalculation arei the load placed upon a pipeline section by an anchor; the
!maximal permissible bend in pipeline between anchor sections; and the load.
I or
!carrying capacity of the denices themselves# The load carrying' capacity
'the anchors depends direotlyon the conditions of the soil into whiah a 0
:screwed, and oan be determined diraotly by measuring the torque required to-1
penetrate the ground. rig..ar . as: 1 figure and 7 formulas.
SUB CODE: 13-, SUBM DATEs none
Card 3 Ij UDC.- 621.6A3.002,001.24
7 7---

KELER, V.R.., otv. red.; MILLIONSHCHIKOV, M.D.p akademik, red.;
BLOKHIIII J'%N., red.; BLOUINTSEV, D.I.; red.; CAIEDENKOp
B.V., akadomik, red.; ZAYCHIKOV, V.11., red.; KEELDYSH, iA.V.p
akademik, rod.; KIRILLIN, V.A., akademik, red.; KORT11"OV,
.V.V., red.; WNIN, Andrey.Sergeyevich, prof., doktor fiz.
matern. nauk, red. (1921),- NE34EYANOV, A.N.., akademik, red.;
PARIN, V.V., red.; REBINDER, P.A., akademik.. red.; SEMENOV,
N.N., akademik, red.; FOK, V.A., akademik, red.; FRANTSOV,
G.P., akademik, red.; ENGELIGARDT, V.A... akademikj, red.;
KREMEVA, G., red.; BALASHOVA, A.# red.; BERG,A. I. akademik, red.
[Science and mankind, 1964; simple and precise information
about the principal developments in world science3 Nauka i
chelovechestvo, 1964-; dostupno i tochno o glavnom v iniro-
voi nauke. Moskva, Izd-vo "Znanie," 1964. 424 P.
(MIRA 18:1)
1. Deystvitellnyy chlen AMN SSSR (for Blokhin"iPtit-ii)q-2~-Ch:Len-
korrespondent AN SSIIR (for Blokhintsev). 3. Akactemiya nauk
SSSR Ukr.SI.(for Gnedenko).

KORTUS.. B.
Problems in the econonky of water resources in Czechoslovakia pe 50o
Vol* 27, no. 1, 1956 Wroclaw
GZALdOYL~MO GIOCIZ-AFICZ1,1E
SOURCE: East European Acession List' (EEAL) Library of Congress
Vol. 5., no. 8. August 1956

KORTUS, B.
The cement industry in the Opole region. p9619.
PRZEGIAD GEOGRkFICZNY. Warszawa, Poland. Vol-30, no-4, 1958.
Monthly List of East European Accessions Index (EEAI), LC. Vol. 8. No. 9, September 1959
Uncl.

KGRITS, Brcnislav
Personal report of a stay in the U.S.S.R. 1rze(,,! geogr 36
no.l-.209-210 TU-

.--KORTM, Bronislaw- (Krakow)
Donbas and Upper Silesia; comparative analysis of two
industrial regions. Czasop geograf 35 no.1:29-50 164.

KORTUS., . Bronipl"-, (&akow)
"'Atlas of the Ukrainian and Moldavian S.S.R.". Reviewed by
Bronislaw Kortus. Czasop geograf 34 no-4t436-437 163.

KCRTIIS, Bronislau
%oography of the aWng industries of the capitalist worldIm by
M. Rolsino Reviewed 6y Bronislaw Kortue. Przegl geogr 35 no&2~
287-289 63.

KORTUS, Bronislaw
"Geography of the heavy industry of t,~e U.S.S.R." by Ps
Stispanow, Reviewed Iq Bronislaw Kortus. Przegl geogr 34
no.4t796-798 162.

KORTUS, F.
Why the "Comets" falle P. 3040 (SKRZYDIATA FOLSKA, Vol. 10, Ho. 19, May 1954,
Warszawa, Poland)
SO: Monthly List of East European Accessions, (BEALL LC, Vol. 3, 110* 12, Dec.
1954, Uncl.'

KORTUS J- V 0
Closed airfields; a story. (To be contd.) p.5. (SKRZYDIATA FOLSFA, Warszawa, Vol& 11p
Nom. 11, Mar. 1955)
SO: Monthly List of East European Accessions, (EEAL), LC, Vol. 4, No. 6, June 1955,
Uncl.

TO'S 0 J7
DiAr:
Physical methods for the concentration of uranium ores-.
Iosef KnEll s and Mlo likek. Jadein-d -ewrv&~S-
-1 o u I ze res more eltictently, and to use
even poor ores economically, tile following phys. methods of
sepn. can be used: 1. Automatic radiometric dassifica-
tion, in which ore pleco bigger than 4-cm. diam. are ac-
cepted or rejected by GM counteim. 2. Gravitational
cLissification, using water or heavy suspensions (e.g., of
finely dispersed metals or arsenopyrite or blast furnace dust)
of ore ground to 1-40 mm. S.' Metation, for evert finer
are, which seps. the sulfides (to which U mintrals clieg) from
carbonates, making poWtile more enottomirtl extit. with
acids. As flotation agents are sugev!ed fatty acids, higher
IMUICS, iso&tyl Phosphates, hexametaphosphatQ. and
ree,iduts frota the sulfmmtlon of aits. 4. Sclective grind-
Ang in 1)311 mills: with or without water. Examples of ac-
tUal PtOdtilLthm VtcCtSSC5 arP, glYtil. H. Newcomb&-
lei,

qlaw
,XORV-q,- -Brylik
The industrial complex of the Apsheron Peninsula. Prze91 geogr 35
no.4s569-589 163,
e-,-

KC-TI111, I
.~ 4 u,) 0 .
"Sore economic questions concerning 'Lhe trealMent of uranium ores."
JPDET'A ENERGIE. Praha, Czechoolovskia. Vol. 5, no. 3, YIE-7. 10/59-
1
Monthly h!A of East 'European Accessions (EEAI), LCI, Vol. 8, 17o. 6, Jur 59, Uncles

KORTUSP J,
Use of radioisotopes in Australian industry and researoh. Jaderns.
energis 6 no.208-0 7 160.
I

-KORIUSI- ~J~
I I-
Nuclear fuel processing In the enterprise Surochemicp Molp Belgium,
Jadarna onergis 7 no.lit3S8-389 N 161.