SCIENTIFIC ABSTRACT KEMESHIS, P.P. - KEMMERIKH, A.O.

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• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

9 (2)9 28 (1, 2) SOTI/115-519-10-14/29
AUTHORS: Kulikovskiy, L.P., Kemeshis, P.P.
T__ - 7~__ -
TITLE: A Vectormeter With Two Degrees of Freedom
PERIODICAL: Izmeritellnaya tekhnikaj 1959, Nr 10, pp 28-32 (USSR)
ABSTRACT: The above-mentioned vectormeter was developed by tbe
Kafedra avtomaticheskikh i telemekhanicheskikh ustroy-
stv Kuybyshevskogo industriallnogo instituta (Chair of
Automatic and Telemechanical Installations of the Kuy-
byshev Industrial Institute) (Figs 1, 2 and 3). The ba-
sic parts of the vectormeter are the meter of the vec-
tormeter, the phase transducer and the electric corr-
ector. The technical data of the vectormeter are: vol-
tage 220 v; maximum value of measured current, 5 milli-
amperes; maximum value of measured voltage 1.1 v;frame
resistance, 200 ohm; the current constant 3 - lo-5
amp/min; induction in the backlash 620 gauss. The vec-
tormeter was developed for the godograph of the curr-
ent vector. A detailed description and the analytical
method of calculations are given in the article.There
Card 1/1 are 4 diagrams and 2 Soviet references.

S/19 61/000/012/003/097
D209%303
AUTHOR; Kemeahie, P____k_
TITLE: Equations of motion of a vector meter with two de-
grees of freedom
PERIODICAL: Referativnyy zhurnal, Avtomatika I radic-elektronika,
no. 12, 19619 11, abstract 12A60. Liet TSR Mokslu,
Akad. darbai,"Tr. AN Lit SSR", 1961, B 1(2.4), 215-225
TEXT: The principle of operation of a ferrodynamic vector meter
is given, whose moving frame possesses two degrees of freedom. Mo-
ments acting on the moving part of the instrument located in a ro.-
tating field are determined. Dynamic Buler equations for the giver,
instrument are formed. The obtained differential. equations of mo-
tion of the frame enable a full analysis of stat 'ic and dynamic
characteristics of the instrument to be carried out, necessary for
its design. Z-Abstractor's note: Complete translation, 7
Card 1/1

S/263/62/GW/007/010/014
1007/1207
AUTHOR: Kerneshis P. P.
TITLE: Some problems of the theory of electrodynamic vcctorimcters
PERIODICAL: Refcrativnyy zhurnal, otdcl'nyy vypusk. Ismeritel'naya teklinika, no. 7, 1962,38-39, abstract
32.7.256 "Tr. Konferentsii po avtomat. kontrolyiu i rnetodarn elektr. izmereniy, 1959".
Novosobirsk, Sih. Branch of AS USSR, 1961. 79-85
TEXT: It is shown that the measurement of the vector of alternating currents reduces to the determination of
the correlation cocificient for two periodical functions, whereby for one of these functions, amplitude and
phase must be known. The a.c. vector is the geometric sum of functions of sinusoidal signals. The correlation
coefficient makes it possible to find both the amplitude and phase of any harmonic component of a signal.
The simplest among devices for determining complex correlation coefficients is ar. electrodynamic device with
separate (independent) excitation, the so-called clectrodynamic vectorimeter whose short description is given.
By using two such devices with perpendicular deviation axes and excitation currents, one obtains orthogonal
projections for the values of the correlation coefficients (functions). This in turn permits the design of a
vcctorimeter that reproduces the amplitude and phase of the measured signals on a complex plane. Geometric
summation of the correlation coefficients may be done with a single device; the latter gives two perpendicular,
pulsating magnetic fields, phase-shifted by n/2 and forming a single, rotating magnetic field. In the rotation
Card 1/2
Some problenis...
S/263/62/000/007/010/014
1007/1207
plane of this field is located the moving part of the device
lie diagram of the device with two rotating elements and - the frame with two degrees of liberty. The icherna.
3 sketch of the device with the rotating magnetic f an optical summator of deviations is described and
dynamic properties are dealt with, and it is show ields is shown. The working principle of the device and its
analysis of amplitude and phase relations of harm n that the above device may be successfully used for the
onic components of any signal. The 1errod
Vectors. ynamic vectori-
meter with two degrees of liberty is of particular interest as it permits the recording of hodographs of a.c.
[Abstracter's note: Complete translation.)
Card 2/2

KEMESHIS, P.P. [KOmOBis, P.) (KaunaE)
Problems of the dynamics of a.c. compensators. Avtometriia
no.3:83-87 165. (MIRA 19:1)
1. Submitted Sept. 15, 1964.

P.P._[t~eipppAq, P.J; YASINYAVICHENE G.M. [Jasinevicienci G.]
Y
Tranafer functions of a ferrodynamic servosyatem. Trudy All Lit. SSR
Ser. D no.4:189-196 162. 04IRA 18:3)
1. Institut energettki i elektroniki AN Litovskoy SSR.

VAITILAVICIUSy A*.q med. M. kand. ;JIMTAITE,Dop stud. ; KE2SSyTEpRo
Role-of pablic toilets in the spread of intestinal infec
tionse Sveik. apsaug. 8 no*407-39 Apt63.
I& Vilniaus Valst, V.Yapsuko -v
kultetas. universiteto Medicinos fa-

MRMANOV~ L. E.) SHKURKO, E. Do; SMIRNOVA., L. A,) KEWDOVA EA X and JCOLIJOVA,
Go Go (Irkutsk State Scientific Research Antiplagueln-alitute of S*1beria and
Far East)
"Sulfanilamide preparations in experimental melioidosis"
Veterinariya, vol. 39, no. 4, April 1962 p. 51

PISAUVI S.; 'M EW., V.; IIJ?~.OV, D.; DII! 1TROV, 1A.; 0-0--KOV, I .; KEIILZV;~P Z,
Certain data on the effect of cortisone on dog organ"w"a. Suvrem.med.
'!ofla no.12:11-21 159.
1. Iz Natedrata PO Datofiziologila pri Softia. Zav.katedrata:
prof. St. Pisarev.
(COXI'lSONZ pharmacol.)
:0..

PISAREV, S-; KIMILEYA, Z.; KIPROY, D.; DIMITROY, L., N=VA, V.; DOSKOV, I.
Effect of neuroses on the course and therapy of experimental arth-
ritis and myocarditle. Suvrem.med.,Sofia 2 no.1:8-15 160.
1. 1z Katedrata po patologichna fiziolociia pri VMI SoMa. Zav.
latedrata prof. St.Pisarev.
(ARTHRMS exper.)
MYOCARDITIS exper.)
008 exper.)
=
Physiology
BULGARIA
xvA Z. I 1i
KUM I L RCHEVA, K., and SHCHMVA, M., Chair of Pathological
Physiologuy Nead Docent Z. Kemileva), Advanced Medical Institutot Varna
"Cholesterol Content in the Serum and Some Tissues of Thymectomized Rate"
Sofia, Eksperimentalna Iteditsina j Nforfoloriya, Vol 5, No 2, pp 78-82
Abstract: The effect of thymectomy on the cholesterol metabolism of
rats was studied. Overloading of the system vith cholesterol by means
of a special diet did not increase the cholesterol content in the serum
of either normal or thymectomized animals. The cholesterol content in
the serum was lower in thymectomized than in normal animals. Accumula-
tion of cholesterol in the aorta wall was greater for control animals
than in those with an excised thymus. On suppression of thyroid activity
by administration of thymidazole, the situation was reverseds the con-
tent of cholesterol in the aorta wall was higher in the thymecto-
mized than in the control animals. Table, 19 references (2 USSR, 17
Western). manuscript received Feb 06. Russian and English summaries.
Oncology
BULGARIA
maLEvA, z., GURDEVSKI, M., and DEMM-NA, K., Chairs of PathDlogical
-Pfi-y,`s-j-oT6kY-(ITead Docent Z. Kemiley".) and Pathological Anatomy (Ifead Docent
K. P. Popov), Advanced Medical Institute, Varna

PISAR.-,V,St.;_ MNIIaVA.Z,.
Role of certain therapeutic remedies in the recurrence of experi-
mental arthritis and myocarditis. Suvrem. med.,Sofialluo.2-3:133-
137 6o.
1. 1z Katedrata po patologiobna fisiologiia pri VMI - Sofiia, Rukov.
n& Katedrats: prof. St. Pisarev.
(RHZUMTIC HURT DISUSE exper.)

PISAREV., St.; KEMILEVA, Z.
The role of disord6re of the nervous system on the course and treat-
ment of experimental arthritis and mWocarditim. $mem med,,, Sofia
no.1:83-90 161.
1. Katedra po patofiziologila pri Visshiia meditainaki inatitutl,
Sofila. (Rukov. na katedrata prof. St. Piaarev.)
MrOCARDITIS exper) (ARTHRITIS exper)
NTRAL NERVOUS SYSTEK pbyaiol)
M

PISAREV, S.; KIPROV, D.; NEDEVA, V.; DIMITROV, L.; XEMILEVA Z DOSKOV, Iv.
Studies on the etiology, pathogenesis and therapy, of experimental
myocarditis and arthritis in the dog. Nauch. tr. viash. mad. inst.
Sofia 39 no.2:23-55 160.
1. Predetavena ot prof. St. Pisarev, zav. Katedrata po patofiziologiia.
(MYOCARDITIS exper) (ARTHRITIS RHEMIATOID exper)

"' "*q'I
PISAREV, S., k.m KEMILEVA, Z. k.m.n.; NEDEVA, V.; DIMITROV, L.,
4.$. Lm7n.-rMW7.-rv-.
KIPROV, D n.;
Role of higher nervous activity in the development and recovery from
experimental arthritis and myocarditis. Nauch. tr. viesh. med. inst.
Sofia 39 no.2257-82 160.
1. Predstavena ot prof. PinarcV, zav. Katedrata po patofisiologiia.
ARTHRITIS RHEMIATOID exper)
OCARDITIS exper)
W
(CENTRAL NERVOUS SYSTEM pbysiol)

KEMILEVA, Z.
Role of neuroses in the course of experimental arthritis. ffauoh. tr,
vissh. mod. inst. Sofia 39 no.2:83-112 160.
1. Predstavena ot prof. St. Pisarev, zav. Katedrata po patofiziologiia.
(ARTHRITIS RHEUMATOID exper) (NEUROSES exper)
P"*;i,
"5. F0
Y-EM-5 J-1,
-ni t~ z
R1 I

UMNGER, Petreg ing.
Operation of ball mills and rod mills at supercritical spoeds. Rev
min 12 no.9--392,402 q 161. .
It-
,I

ANDREJEVP N.D. (Andreyevp N.D.); KEMIROVp p.A.
Cybernetics and jurisprudence. Term tud kozl 4 no. 12:
529-531 D 160.

XMITS) Yu,V,, dotsentp kand. tekhn. nauk
- I,-- I- - - C '- -'', t- --.1-t-,
Appraisal of the accuracy of adjustments od dependent quantities
and the relations between measuring results. Izv. vys. ucheb.
zav.; geod. i aerof. no.3:3-9 163, kMIRA 17;1)
1. 146skovskly instAut inzhenerov zemleustroystva.

KBIOUTS, Yu.V.. assistent
Generalized formula for the mean square error of a nonlinear
function. Izv.vys.ucheb.zRv.; geodj aerof. no-5:75-81 1 58.
(MIRA 11:12)
1. Moskovskiy Insititut inzbencrov zeminustroystva.
(Errors, Theory of) (Geodesy)

-Xie n
CZECHOSLOVAKIA/Chemical Technology - Chemical Products and 1-4
Their Applicatlon. Pesticides.
Abs Jour : Ref Zhur .- Khimiyav No 1, 1958, 2342
Author : II. Janok Jan Kemka Rudolf III. Kemka Rudolf
Oblestny ustav pr ~0,
Inst prace, Bratislava.
Title Organophosphorus Insecticides. II. Enzymatic Method of
Determining Small Amounts of Organophosphorus Insecticides
in the Air.
III. Enzymatic Method of Determining E-605, Potosan and
Systox in the Air.
Orig Pub : Pracovni lekar., 1956, 8, ijo 4, 296-298, 298-300
Abstract : Il. Organophosphorus insecticides are determined by means
of inhibition of the cholinesterase of horse serum.
Ill. Descrip-Ulon of the method, including calibration clu-
ves for pure systox ana isoxystox.
Part I see RZhK[iim, 1957, 61120.
Card 1/1
CZECHOSLOVAKIA/Chemleal Technology - Chemical
Products and Their Applications --
Pesticides.
Abs Jour Ref Zhur - Khimiya, No 3s 1957, 8857
Author Janok, J., and Kemka R
Inst
Title The Enzymatic Determination of Small Amounts
of Insecticidal Organophosphorus Compounds.
Orig Pub Chem. zvesti, 1956, 10, No 32 177-182.
Abstract A method is described for the determination
of small amounts of paration preparations (I),
based on the inhibiting effect of the latter on
the action of chlolineesterase (CE). The in-
hibiting effect of I to a'large extent depends
on the source and Purity of the CE. The method
has been tested in a district where trace
Card 1/2

CZECHOSLOVAKIA/Chemical Technology - Chemical 1-7
Products and Their Applications --
Pesticides.
Abs Jour Ref Zhur - Khimiya, No 3, 1957, 8857
amounts of I were found after spraying with
11ekatoks 2011 preparation and is recommended
for the investigation of the toxicity of,
organophosphor *us compounds in conjunction
with the application of more sensitive
chemical methods.
Card 2/2
k6ra&ttA 1risects mid
GL L&St*;F.C. ZOOLOGY. IN SL -'I'S
;J15. JOUR 71nity. -Bcuiogiya, No. 2 , J959, No. 6992
'Not given
T L 17. PArAtil).Otl R&flidUO from
Plants.
195-, A", No-5, 99,")-
1
"T 'Me Gv;zyriu nici~had was used to determine the
dynarnics cA' tl-,,- di.%~,;)Pearencc, of re!ii(I'lles
of die thyl c from
1c,.t,ttjce leavei -itid ,tuc;ir beet leavcrs. 'r,!on-
boxwe iutttlce Was ~,Irrayed WIth an ealulsion of*
.F-605, and bcet-ki in fi(tl(i with ~kfl (IT1111-
~iimi ut' ecatGx 20. :~4anwlen Cr~;m tht~
plarits were, taken perilodic;~Ily, w-~ir,~~. tre,-,tett
wii.ij eUvr and thi,- towicitv w- dut(~rwinekl
by potentionietor accGrding to tae (ingre-,~ -.)f
1/2

~.IYIGEIIRPT& I ICA See.17 Vol.4/2 Public Health, etc. M58
K-T,---,JvNAY_'r_ .
604. EXPERIENCE WITH SPRAYING OF SUGAR BEETS WITH EKATOX 20.
Skdaenosti a postrokovania cukrovej repy Ekatozom 20. Kemka R. and
V a I a n t i np v & 1. Oat. Hyg. Pritce a Chor. z PovolaiMiTIFRU-sliva.
PRACOVNI Lft.(Praha) 1957. 9/2 (144-146) Tables I
The authors describe the instruction given to sprayers and the hygienic measures
in spraying sugar beets with the parathions preparation, Ekatox: 20. They discuss
some inadequacies, and suggest means for their correction. There were no sub-
jective complaints. With a pH-meter the cholinesterase activity in the blood of
sprayers was examined. working from 4 to 38 days with Ekatox 20. There was
a fail in acUvity in 4 cuss after the work was finished.

CZEMIOSLOV-KIL/Chenical Tcellaol%7. Chonical Products vzid Their 11-18
Application. poaticidc3.
Abs icur: Ref Zliur-10i~Lm., rio 2) 459, 5854-
11, at
Title DetexTdriation of Residue of Soria Systc:Mtic LISOCtiCiLl-cs
in Plants.
OriL; Pub: Pracov--i 1L,-Imr., 1958, 10, ro, 2, 144-152.
.I.bstract: The mioulit of residual systox (I) in m
.Lrayed scl,-d and
suGar bcQt (SB) decreased by !C~ in 14 ema 17 days re-
spectively after sprayinC;, I was not detacted in hops
aftcr 5 weeks. In the spray:Ui(; of SD with natasystox, its
.10u;lt wc, 0 ft
m creaced 3.% ill 1'( ( 0 after the spmying,
~tio-
-An till rt n frc-.i
- . LI after Vila sprayin- vi th cha mnsliter
Russia~j (111), -Viu cm.,.cm-nt of the latter dcc::uas~!d by
Card 1/2
100

KIMEA, Rudolf; KLUCX,, rmrich
Similtaneoue determination of antimony and arsenic in the air of
antimony metal mines. Pracovni. lek*12 no.2:74-79 Kr 160.
1. Ustav hygieny prace a chorob z povolania v Bratislave, pred-
nosta MUDr. Imrich Kluoik.
(AIR POLIMICK)
ANTrmoNY)
ARSEIHC)
~
(MINING)
%"j.t i~-rtr 41

KWGIK,I-;
Excretion of antimony in antimony mill workers. Pracovni. lek. 12
no-3:133-138 AP 060.
I.Istav hygieny prace a ohorob z povolania, Bratislava.
(ANTIMONT metab,)

KLUCIK, I.; - KMA, R.; GRUBBROVA, -T.
Some findingB on the effect and metabolism of fural. Prac. 19k. 13
no.0t455-46I.-N 161.
1. Ustav bygiemy prace-a aborob, z povolania v Bratislave.
(FURANS toxicol)
MKAp R.; KLUCIKp 1.
A proposed exposure test for furfural based upon the estimation of
furoylglycine as a furfaral metabolite in urine. Frac. lek. 14 no.7:
331-3Y7 S '62.
1e Ustav bygieny prace a chorob z povolania v Bratislave, prodnosta
MUDr. I. Klucik.
(FURALDEHYDE)

HEGYII E.: . K!-2,-.TA j,R'-_ rk
caused by chromium ccmpomnds bn WO
Apropos of sk:Ln damage lek. IiOt-Y 44 no.9013-526 164
with CemOnt- Bratial. a katedra lek- fak. UniverzitY Komen-
1. Dermatovenerologick j. -
skeho v Bratislave (vedue . prof, jVjDr*L.Chmel) a Ustav hY
6jeny prace a chorob z POVOlania v Bratislave (veduci MUDr-
I.Kjuclk).

KLUGIK,I.; KMM-,,R. - -' */)
I : -- I
Alpropos of the behqvio~ of trivelent antimony in human blood.
Bratial. lek. list;t 2 ho.109596-602 163.
1. Ustav hygiery prace a ehorob, z povolania v Bratislave;
riaditel: MUDr. Io Klucik.

rj,I-IKAf Rudolf I TAILIBA, Favol
Determination of nickel and cohalt in the air,, in care and biolo-
gical material by analysis of so!;Lttons. Prac, lek. 'AA ntj.?:32(,-
323 3 164.
1. Ustwr hygiony prace a churob -,, v Bratisl,.,ve (riuditerl
prof, dr. M. Nosal).

KEMKA, Rudolf; DOK9KY, Abdrej
Simultaneous determination of furfuryl alcohol and furfural
in the air. Pmo. lek. 7 noo8s353-356 0 1 65.
1. Ustav Hygieny prace a chorob z povolanta v Bratislave
(riaditel - prof. dr. M. Nosal),

n i-i'm rI " U/- -,-- I ~1, V,
mmmm, M.v.
,--m- - m FA" - - --
Yoramtion of the Colchis Lowland during the period of recorded
history. Soob.AN Grus.50 19 no.1:41-48 il 157. (MIRA 10:12)
I- AN GrusSSR, Inatitut geografii im. Vakhushti, Tbiliai.
Predstavieno akademikom A.N.Dzhavakhishvili.
(Colchis--Physical geography)

mmmkmp mo V.p Candidate of Geogr qcj (diss) -- 'Vhe Physical-g ographic charac-
- e
teristics
of Kolkhidaffe Moscow, 1959. 16 pp, (YDR00w State Pod Inst im V. 1.
Lenin), 150 copies (KL, No 22, 1959P 110)

KEMMADZE, Sh. S. C-nd. Physicomath Sci.
Dissertation: " Concerning Regular.R-Groups.n
11/12/30
Moscow State Pedagogical Inst. imeni
V. I. Lenin
SO Vecheryaya Moskva
,S-um 71

XEMADZE, SH. S. PA 192T62
UMANth"Mucs - *as= Algebm
"Regularity of p4roups for the Case pw2," Bb. S.
Kemkhadze, Batum, State Pedagogic Inst imeni Sh.
Rustavell
"Soob Ak Nauk Gruz- SM" Vol XI., No 10, pp 608-6LI+
Given simpler definition of regular p-groups and
demonstrates that the concept of regularity of p-
groups, introduced by Han, coincides vith commu.-
tatlvitv for the case of finite 2-groups. Suba-A4
ted by-Acad N. 1. Muskhelishvili 24 Oct 50.

1 -
2. U~'-M (600)
4. Groups, ~eheory of
7. Uniqueness bases in infinite regidar p-jroups.- Ukr-i,"at-mhur. 4 no. 1, 1951.
9. Monthly List Rf Russian Accessions. Library of Congress, APRIL 1953. Unclassified.

X.F.MHOZEf, S.S
'Kemhadze 9 Uniqueness bases In infinItO fd U 4T
Mathomatical Reviews n. Mat. lurnal 4, 57-64 (1952). t,
lus.
Vol. 14 Ito. 11 siln)
Deaember, 190 The atithor con'siders infinite grourA G in wl
lich any two
clemcnt3 generate a finite regular p-group. Let G havc'in
AlObra; L-scries (presumably transfinitc)
I -LoC ... L,CL, I IC ... CL,-G
in which cach L, Is a normal miligroup and in which 6c
factor group Li+,IL, is cyclic. If alio (lie orders Of demCate
of G are bounded, theit G has a tin iqueness baiic- Ji
'A
Marshall Ila//,; Jr. (Columhus,'OM

0 A
Mathematinal Revicnve
Vol. 14 No# 8
Sept. 1953
Algebra
Kellilladle, S. S. it the deternfirintion of regular
groups. I Is1whi Nattk (N-'*,.) 7, no. 6(.52), 193-
196 ( ,11)52). Oisi i,m)
It il., shown that Ow. defillitioll of l"gillarity ill fillite
p-grotilis its given by Philip I lall redurcs to file sillifile con-
ditioll that forsome( ill thederived groupof
the subgroup generated by a and b, for ;my choice of is alid b
ill the group. Mar3hall Hall (Coltilliblis, Ollio).

INA Call Nr; AF 1108825
Transactions of the Third All-Union Mathematical Congress, Moscow, Jun-Jul 156,
Trudy '56, V. 1, Sect. Rpts., Izdatellstvo AN SSSR, Moscow, 1956, 237 Pp.
Kaluzhnin, L. A. (Kiyev). Generalizations of Basic Theorem
of the GalolB Theory. 23-24
There are 4 references, 2 of vhich are Frence, and 2 English
Kemkhadze, Sh. S. (Batumi). Second Pr&er Theorem for Regular
-- w__' _-
p-Groups. 24-25
Kontoravicb, P. G., (Sverdlovsk). On the Theory of Bemi-
groups in the Group. 25-26
There are three references, 2 of which are USSR and I English.
Kostrikin, A. 1. (Moscow). Nil-potent Groups and Lie Rings 26
Kulikov, L. Ya. (Moscow). Universal Complete Abelian Groups. 26-28
Lyu-Shao-syue (Moscow). On Splitting of Infinite Algebras. 28

71-1

AUTHOR: Kemkhadze, Sh-ff,-~Batumi) SOV/42-13-3-36/41
TITL.5s On Invariants of Finite Regular p-Groups (0b invariantakh
konechnykh regulyarnykh p-grupp)
PERIODICALj Uspekhi matematicheskikh nauk, 1958, Vol 13, Nr 3 p 246 (USSR)
ABSTRACT% Accordin g.to the author [Ref 1j a p-group G is called regular
if to every pair of elements a,b F- G there exists an element
a of the oom-utator group lj~,b I of the subgroup fa,b~ such
that (ab)P - aPbPsP; Every finite regular p-group has & base
of uniqueneesp i.et-there exists at lesat one sequenoe of
elements 9,,02, ... 10, with the orders such
that every element of 0 can be represented uniquely in the form
9 a 9k1 0k2..d kt4 9 O:Ek < p (r.1 929 ... I w).
1 2
The author shows:
1. Choosing in a finite'regular p-group two bases of uniqueness
GIP'Q2'0'0,0 . and ata.,G.., ak , where the orders of the
t'l pt2,...fpP"Pand 011 a 2 OLk
elements are p p up ...,p
I rl 2
and ckl :>OY:~ ... 17' O(k' then Q. k and for all i.
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On Invariants of Finite Regular p-Groups SM/42-13-3-36/41
2. For a decreasing order th* invariants of the subgroup A
of a regular p-group G are divisors of corresponding invariants
of G.
There are 3 references, 2 of which are Soviet and I English.
Card 2/2
i Kz 4Z

KDMUDZE, U.S.
First Republican.0opference of Professors and Teachers of Mathematics
of the Pedagogical Inatitutes of the Georgian S.S.R. Usp. mat. nauk
16 no.2t251-253 Mr-A '61. (K= 14;5)
(Mlathematics-Congreases)

KRWADZE p shoso
DeteMination of nilpotent groupo. Soob. AN Gru$. SM 26
no.4.-385-387 Ap 161. (MIRA 14:$)
1. BatumskiY PedagOgicheskiy institut imeni Shota Rustavell,
PrAtistavleno chlenom.46rrespondentom Akademij nauk GruxSSR.
Gas, chopmWili. ".'.'.^ I I
(Groupa,-Theory of)

KE.MXHADZE9 Sh.S.
P-regular groups. 3oob. AN Grua, SSR 27 no.1:3-8 Jl 161.
(MIRA 16&8)
1. Batumskiy gosudqetvannyy pedagogicheskiy institut im.
Sh.Rustaveli. Predstavleno akademikom AN Grua. SSR G.S.Chogoahvil-i.
(Groups, Theory of)

KEWHADZE, Sh,s,
Determination of BaerIx nil-group. Soob. AN Gruz. M 33 no. 21
.79-284 F 164. (MMA M9)
1, Batamiskiy padagogiahoskiy inatitut imord. 3h.ftustavalt.
Predstnvleno akdemikm O.S.Chagoshvih.

HEMMUZE , Sh.S,
Quasi-nilpotent groups. Dokl. AN SSSR 155 no. 5:1003-1005
Ap 164. (MIPA :70-5)
1. Predstavlono akademikom A,I.Malltsevym.
~, ~ % t'. f , ,
fm

MIKHADZE, Sh.S.
Stable groups of automorphisms. Dokl. All SSS11 158 no.3:510-512 5 164.
(MIRA 17;10)
1. Batumskly pedagogicheskiy institut im. Shota Rustaveli. Predutav-
Iono akademikom A.I.Malltsovym.

KEMKHADZE, Sh.S.
Some properties of factorizable groups. Soob. Ali Gruz. SSR 35 no.2:
257-263 Ag 164. (MnU 17t12)
1. Batumskiy pedagogicheskiy inatitut im. Sh.RuBtavell. Submitted
November 26,, 1963.

H, VKH A U S h
-x t, nria 11 ynllpotent aroup~ D" -urrxncrph~~srpo. AN 'friv.
C,
~SR ~4 no.2t265-270
IS My 164. (MIRA 181
1. Patuin:;kiy gosudarst-vennyy podf)gogichoskiy in-stitut. im.
Ruot,vv~,I.i. Suhritted Fr-bmar.,,, 1P2 1963.
VIA PIQ4
WN,
g., ig

PLOTKIN, B.T.; KE24KHADZE, Sh.S.
Scheme for the construction of radicals in groups. Sib. mat. shur.
6 no*5:1197-1201 S-0 165. (MIRA 18:10)

B A LEZ 111 , S. ', . ; YJ,',1,ffJ1ADZ E) T. V. ; Z It blldilil-j.-~ i . ~M.
Using certain electrochemical methods in sturying the mechanism
of the action of inhibitors of the corrosion of carbon steel in
son water. Soob. AN Gruz. SSR 35 no.lz155-162 J1 164.
(HIRA 17: 10)
1. Gruzinskiy metallurgicheskiy institut. Predstavleno akademikom
F.N. Tavadze.

KDUMDZE,, T.Y.
Corrooim-reoletance of cteel-10 in no& water, Soobs AN Gruz.
WR 33 no.3t635-642 Mr 164 (MIRA 170)
1. Gruzinskiy metallurgicheskiy Institut, Tbilisi. Predstavleno
akademikom F.N.TavacIzs,.
Rn
ne

1:1-afmADZE, V. S.
7~1511~rl, ~-.-
'AR
- -I
Kemkhndze. V. S., Balazin, S. A., "Inhibiting actlon of aliehyles." (p. 1848)
Sn: Journal of Goner-1 Ctirli~m (Zhurnal Obshchei Khtmil),

(g. Batumi); LOGINOVo A.Te. (g. Uluga); EIITROT, T.A.
--!n~(~Voronezh)
A good textbook tChemistry." B.A.Balezin, B.A.Pavlov. Reviewed
by V.S.Kemkhadze, A.I.Loginov, V.A.Khttrov). Xhim.v shkole 11
no.5:74-76 S-0 '56. (MLRA 9:11)
(Chemistry) (Balazin. S.A.) (Paylov, B.A.)

DETIN, G. ;
Honored oil manter, Naftlanik 9 no,987--6 S 1!~4 (MIP-A ISO)
1. Nachallnik otdola ekonomioheskogo analiza TSentrallnoy
nauchno-imaludovateltakoy laboratoril tresta A-m-.mmefterazvedko
(for Detin). 2. Instraktor Rayonnogo komiteta Fommunist.1cheskoy
partil Azerbayfthanat rayon ims 26 Bakinckikh komissarov (for
Kemko).

I - '& - i-. L ';' t i& t 4, a 4 a z e S t t a a % t S e a S q C 1! v . 0 - 9 - % . I . , - ~ - . _' ~
0 6 a 0 4 0 0 0 0 0 6 0 a 0 0 010 0 0 0 0 0 0 0 0 0 4b 9 9 0 G a 6 a 6 e

I-A. ~a M, fL'_I 1-

CA
00
0* ;
00 , I
' letting and hardening of cozents used for stopping oil wells,
00 : leovar and Balan. Stroltelmii* Materialut (Building MaOrtals) No.2.3"I
00
(ii6bj.-T~sts were made to ascertain the Influence of water contg. petrol-
0 S sun and petroleum emulsions an the setting and hardening of *sment used
o for plugging oil wiells. Addos of 6,10 and 15% of pvtroltum(tho a=pn. is
00 given) were made. The results of these are tabulated and show t1at: (1)
00 wall addne. of petroleum (6%) do not Influence the 4ualitiss of asaentt
00 (2) only oements of high quality. which harden quickly. can be used for

plugging wells.
00
H.V. Kondoidy

N* 0

00
so t
L-9
_ 041
~jI
'it " IV
4
,g -00*0 O's &0 0*4 41 t *a 04
4

K&MRp A.j, icand.tekhn.nauk
Possibilities of reducing pover consumption by the pneumatic
equipment of operating flour mills. Muk.-elev. prom. 28
no.12:16-18 D 162. (MIRA 161l)
1. Odeaskiy tekbnologicheakiy institut im. Lomonosova,
(Flour mills)

A.
Resources in designing pneumatic conveying systems for fla--i- mills,
Muk.-elev. prom. 29 no.3:20-22 Mr 163* (MIRA 16 :9)
lo Odesskiy teklmo'Logicheskiy institut.

DZYADZIO, A.M.; KEMPER. A.S.
Determining the soaring speed of particles. Izv. vys.ucheb. zav.;
pishch. takh. no. 2:110-114 158. (MIRA 11:10)
1. Odeaskiy tekhnologicheskly institut imeni I.Y.Stalina, Kafodre
promyshlennoy rentilystaii, gidravliki i naeosov.
(Pneumatic-tube transportation--Fluid dynamics)

DZYADZIO, A.R.; jj~j A.S.
Pneumatic tranoportation of cereal prcdvcts in horizontal tubea.
Izv, vyv. ucheb. zav,;pishq.h. tekh. no-3:79-85 160. 011w, 14:8)
1. Odesskiy tekhnologichookiy institut im. I.V. Stalim, Kafedra
proVuhloomoy ventil7atsiip f;idravliki i nasosov.
(Coreal.products) (Pneumatic-tube transportation)
Z~T

KEMMER, A. S.
Cand Tech Sci - (diss) "Pneumatic transport of grain products in
horizontal pipes." Odessa, 1961. 30 PP; (Ministry of Higher
and Secondary Specialist Education Ukrainian SSR, Odessa Tech-
nological Inst of the Food Industry and Refrigeration Industry);
200 copies; price not given; (KL, 7-61 sup, 238)

IEMWIR, A.S.; DZYADZIO, A.M.
At
Nomographs for the design of the tube systems for horizontal
pneumatic-tv* transportations Izvevys.ucheb6zavo; PiBhch.tekh.
no.3:145-149 162. (MMA 15s7)
I* Odeaskly tekhnologiohaskiy institut imeni Lomonosova, kafedra
promyshlannoy ventilywtvii,, gidravliki i naeosov.
(kneumaiia conveying)

- - j
; DZYADZIO, A.M. I
Analyzing the electric power consumption of horizontal pneumatic
conveyinF aystems, Izv.vys.uchob.zav.; pishch.tekh. no.4ilO6-
4
109 162. (MIRA 15-11)
1. Odesakiy tekhnologicheskiy institut im. M.V.Lomonosova.,
kafedra promyshlennoy ventilyatsii, g1dravliki i nasosov.
(Pneumatic conveying) (Grain-Tranaportation)

KEMER, A. S.- DZYADZIO, A. M.
Calculating the velocity rate of soaring under free and
constricted conditiones Izvo vysw uchebe zav,,; pieihcb. telh.
n0.5:113-3-19 '62. (MIRA 15:10)
1. Odesskiy tekhnologichealdy institut imeni Lomonosova,
Ahlspnqy_~vqZ*QUUii,, gidrayliki i nasosov.
kafedra_pron7
(Paeumatic conveying)
(Dynamics of particles)

--1--_-__'V~,q, - .- r I _e - ~~ -011.;~~-_,~', 4%01, ` ".."M i,
4T@ * -st, a III 111 0 111 111 o * e ip a
Vv~ *040640466094 0 0
0 3~ 111 4 S 6 1 1 It 10 It U 11 U It 14 1? If S J3 n At 5 J6 V X JO 10 It 9 U It Is 0 V - P - -r Q .4 asto
It A I' L I I - . , -
a a R .1-t. It.. A-1 _AA N go Ix It 6 1 IF __s
-00
Do ydratift Glaubses "a bs, the
jI1jrWU!N AND]. PONFILOV.
Mintral. SIOWO 6. 190-DtN(1931); chimmie & lVito (ju dchydm.
t
06 t: ::`g
Om of Nsa.S(4 I01fjO shoorvId that beat n*Wto an obtsilried ljy crushivil to 1 -8 mm,
00 Of- dism. The tinte of drying can be reduved cons~"Wy by nw"tely heating tha,,
Thornin, temp. required toprevrot wvttiWr-
SO a!'- of the crystals by the WIM of .1 . to about 32' fat the decaby4rate. It inct"Llast
,9 proorsaivIrly. but slawly, to the productim of crystals with 10% HoO. and then move
00 a ; -.
rapkily, to reach 62* at the end of the drying. iTftts with a gunnel drier, perfumed
R!, drum drier, unperfurawd drum drier, makin; the crystals fall thire4b a rising current
a(aif, and with& ta"t boviagemperpomed4ryingtroysshowtd that bestrestults werv
A 0
obtained in the last-asentioned sipp. witis sk at 68* at the InW and 371 at Uw OMW.
:0 j1- Under theme cooditions. turbes the crystids me a tmnstcrrvd from one My to the nest .00
00 a i at 30-mko. interva* (Woulmer's, saft can be dried satisfactorily in 6-6 bm with a fuel- C*
utilitatibn effirienew of 43%. A. PAIFININAII-COM11111
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12 .00
age
nee,
Call
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0 40 0 0 0 * 0 0 0 IS 0 0 0 0 0 40 9 0 0 * 0 9 0 6 0 0 16 006 46 1
go 00 00 es 000

- - ----E
KIMM, H.
fiThe distilling kiln In the Tarnow Lumber Plands.0 P. 30. (PRZEMM DRZEM
Vol. 6. No. 1, Jan. 1955. Warszawa, Poland)
SO: Monthly List of East Axropean Accessions. (ML). LC. Vol. 4, No. 4.
April 1955. Uncl,

1, -1.
lp;)jyin!~- cqst~jjjfjc,,j -,s a r.-,.3thod OP dry-rij-, wood. P. 4"
P-.,ZZ--;'7,LAr) Lo-!-,, lol. 1C, no. 2, 1915-5.
.0 - `11 1
~t_): I' r,,tjjj~ L-' st of East ~~uropean Accez:,siono, L.;, Val. -,,, no. 10, Oct. 1(;::r
Uncl.

00 A
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9
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004
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Mgl&UWMAL UTMTOM CLAUIPICA
flow VQMLAW
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A T ME
r-jm:- "N - M. - -- ~

nl*!ERIKH,, A. 0.
..........
UM/Geopbysics Water Levels Sep/Oct, 51
~Causes, for the Rising of Ground Water Levels in
the Tobol River Basin,," V. A. Areflyeva, A. 0.
Kewerikh, Inet of Geog, Acad Sci USSR
"Iz A Nauk SSBR, Ser Geog" No 5, PP 45-50
Describes periodical rising of ground vaterefol-
loved by periods of decrease. Max rise of vater
levels in lakes was observed in 1947; from then
until 1950 the level dropped 80 ca. Similar
phenomena vere observed in West Siberia and Kaza-
kbstan.-A projected plan in to lower the waters
,,of Lake Okunev into IAke Tomoye and Miass River to
."ve flooded'territury so. forests of Ka"brodsk.
205T56

ARUIYL?VA,V.A.; KUMIKH,A.0.
Z'
Drying out of trees and the dying of forests from an excess
of moisture. Priroda 44 no.5:96-98 Ky 155. (MLRA 8:7)
1. Inatitut geografii Akademii nauk SSSR
(Siberia, Western-Torests and forestry)

EOMMMI, A.0. (Moskva)
Opening of rivers. Priroda 0 no.4:125-126 AP 156. WaA 9:7)
I.Inatitut geografli Akedemli nauk SSSR.
(Ice on rivers, lakes, ate.)
Ar

p
A,
MNUWKH, A*09 - ~_f ~snow cover distribution in the Polar Urals. Izv. AN
__ 1111)
BSSR, Sore geoge no*4:69-73 JI-Ag 157. (MINA
1. Institut geogrElfii AN SSSR-
(Ural Mountains--Snow)

AUTHOR:
TITLE:
PERIODICAL:
ABSTRACT:
ASSOCIATION:
Card 1/1
SOV/10-59-5-9/25
Dolgushin, L.D. andXammazjXhL _A0.
Mountain Lakes of the Subpolar and Polar Urals
Izvestiya Akademii nauk SSSR, Seriya geografiches-
kaya, Nr 5,pp 76-82 (USSR)
There are over 4,000 lakes and tarns in the mountainous
parts of the Subpolar and Polar Urals. The surface of
these lakes rarely is more than 1-2 sq kmg though the
lakes of tectonic origin are larger, but the largest
of them all, the Bol'shoye Shchuch9ye Lake, has only
11.74 sq km. All these lakes and tarns could be cli-
vided into two groups; tectonic lakes, and lakes and
tarns formed in the depressions left by melted glaciers.
Lakes of the last groups are usually small but often
very deep, (tables 1 and 2), The authors describe some
characteristic for each group* There are 4 photographs
3 tables, 1 set of diagrams and 3 Soviet references,
Institut geografii AN SSSR (The Institute of Geography
AS USSR)

!- : -, --,- - - - --- --
A - -j 12- 4'/, x AI I/
.,/T' e. - /V r , X - ~- I
DOLMSHIN,
ftw'glaciers in the Ur&ls. J2V. AN SsSR. Sere geog. no.6167-73 W-3
'57o (min 11: 1)
1. Inatitut geografit AN SSSR-
(Ural Mountains--GlacierO

Ice la7ers..Priroda 46 no.2:125 -r '57. NLRA 10:3)
1. Institut geografii Akademii nauk SSSR, Moskva.
(Ice an rivers, lakes, etc.)

'~) +
GHT&M, S.Yum; ZIHINA. R,P.;.,X2H=W, A.O.; MIN, V.N.; KUYSHINOVA, K.Ve;
HURZAYEV,,E.K~,'doktor geograf.nauk; RYAZANTSLIV, S.N.; FORMOZOT,
A.R.; FRATKIN. Z.G,; CHBUKOV, L.A..; ZABIROV, R.D.: KCROVIN, To.?.:
ROZANOV, A.R.; RODIN, L.Ye.; WJBTSOV, R.I.; SPYGINA, L.I., red.
izd-va; POLINOVA. T.P., tekhn.rede
[Central Azia; its pbysical geograptW] Sredniaia Aziia; fiziko-
goograficheaknia kharakteristika. Moskva, 1958. 647 P- (MIRA 11:6)
1. Akademiya nauk SSSR. Institut geografii. 2. Institut geografii
Almdemii nauk SSSR (for Geller, Zimina. Kemmerikh, Kunim, Kuvehinova,
Murzayev, kazantsev, Formozov. Freykin Chubukov). 3. Almdemiya
nauk Kirgizakay SSR (for Zabirov)o 4. Akademiya nauk Uzbekskoy SSR
(for Korovin)- 5- Pochvennyy institut AN SSSR (for Rozanow). 6.
Botanchaskiy institut AN SSSR (for Rodin). 7. Akademiya nauk
Kazakhskoy SSR (for Rubtsov)
(Soviet Central Asia--Physical geography)

AUTHORt Kemmerikh, A.0. 3OV/26-58-1-36/36
TITLE: Ice vers (Ledovyy rezhim rek)
41
PERIODICAL: Priroda, 1958,~Nr 1, p 128 (USSR)
ABSTRACT: The USSR's dimensions from north to south and west to east
bring about very different ice conditions on her rivers, due
to the various climatic conditions. In January most Russian
rivers are covered by ice except the'small rivers of the me-
dium altitudes of the Black-Sea slope of the Caucasus, the
Carpathian effluents of the Dnestr river that are mainly fed
by rain and melting water, and the rivers of the Crimea,
Lenkoran' and Kopet-Dag. Usually there is no stable ice cover
on the rivers of the mountain regions of the Caucasus, Tyanl-
Shan' and Pamirs. The heaviest ice cover is observed on the
rivers of North and Northeast Siberia, where the air tem-
perature is extremely low and the snow cover comparatively
insignificant. By the end of winter, these rivers have an
ice cover of 2 m, while the smaller rivers freeze down to the
bottom of the river bed. An ice cover of up to I m thick-
ness is observed on the rivers of the North of the European
USSR. This is explained by a higher air temperature in winter,
Card 1/2 greater flow velocities and a thicker snow cover on the ice,

Ice Conditions on Rivers SOV/26-58-1-36/36
The same applies to the central belt of West Siberia. In the
South of European Russia and in the lower regions of Soviet
Central Asia, the ice cover on the rivers rarely exceeds
25 to 30 cm in thickness. Rapids and waterfalls do not freeze,
even under severest frost conditions. Layers of ice up to
6 m thickness, due to special conditions, such as subterraneous
sources or ice blocks from the vicinity of waterfalls, are
fourd in the Verkhoyansk-Kolyma mountain region and the polar
and near-polar regions of the Urals. On the other hand, under-
ground sources and waters of higher temperature may cause un-
frozen patches of water in the midst of river ice. Unfrozen
patches can also be caused by warmer lake water entering a
river. This can be observed every year with the Angara, Neva,
Svirl, Volkhov and other rivers. Industrial waste water and
sewage may also cause unfrozen patches.
ASSOCIATION: Institut geografii AN SSSR, Moskva (Institute of Geography of
the AS TISSR, Moscow)
Card 2/2

AUTHOR: Kemmerikh, A.0. SOV-26-50-8-13/51
TITLEs T~a Urals Near the Arctic Region (Na pripolyarnom Urals)
PERIODICALt Priroda, 19589Ar 8, pp 74-79 (USSR)
1\
ABSTRACT% The Polar Ural mountains are bounded by the river Khulgi in
the North and the mountains Tellpos-Iz in the South. In this
area rich deposits of coal, rock crystal, gold, and other
rare metals have been discovered. There is a large supply
of lumber, furred animals, ate. At the present time only
rock crystals (piezoquartz) is mined. The high water capa-
city of the rivers, the great level differencei and the geo-
logical conditions are a good base for the construction of
hydroelectric power atationso especially on the Pechora, Usa,
etc. The forests in the Polar Urals reach an altitude of
450 - 650 m. The highest mountain is the Narodnaya with an
elevation of 1,894 m above sea level. The mountain zone is
120 - 150 km broad. The Polar Urals are composed of meta-
morphio rocks with intrusions of granites and granodiorites.
The Narodnaya mountains is made up of quartzites and quartz-
ite conglomerates. In summer the temperature during daytime
is 18 - 2000. During niglit frosts often occur. In winter
Card 1/3 the temperature in the foot hill regions drops to -530C, in

The Urals Near the Arctic Region SOV-26-58-8-13/51
summer it rises to 340C- Ih the mountains the frost is often
considerably less severe. Winter with frost and snow cover
lasts in the plains adjadent to the Polar Urals 7 months and
in the mountains above ltOOO m 9 months. On the western
slopes the snow cover reaohesj during winterj2 - 3 m, on the 2
eastern slopes 60 am* Glaciers cover a total area of 4-7 km
The watersh *ed divides the weathert too. In the west cloudy
and stormy weather may be observedq whereas 8 - 10 km east of
the watershed the sun shines. The western slopes are drained
to the Pechora, the eastern to the Obl. The water in the ri-
vers is supplied 50 - 60% by smelting snow, 25 - 34% by rain,
and 15 _ 30~G by underground water. The water drained in the
west is 30 1/seo per km2, in the east 15 l/sec per km2.. There
are manv mountain lakes, none of them having an area of more
than 1 km2. They often attain a depth of 20 , 30, and even
50 m- In the future the Polar Urals will be transformed in-
to an industrial area with plants, mines, towns, ate.
Card 2/3 There are 8 photos and 1 map.

The Urals Near the Arctic Region SOV-26-58-8-13/51
ASSOCIATIONt Institut geografii Akademii nauk SSSR (Institute of Geo-
graphy of the USSR Academy of Sciences)
1. Art'&.c regions--U53R 2. Artic reg.lons-.-Economic aspects
3. C-11mate.-Arct1c regions 4. Physical geography--Ar-tic regions
Card 3/3
tz
5
R

AUTHOR: Kemmerikh, A.0. SOV-26-58-8-48/51
TITLE: The Summer Low-Water Mark (of Rivers) (Letnyaya mezhen')
~7
'PERIODICAL: Priroda, 1958,NNr 8, pp 125-126 (USSR)
ABSTRAM In summer the rivers feed from underground waters andrain.
The summer low sets in at different times in the diverse re-
gions of the USSR. It starts at the end of April in the semi-
arid and steppe regions of Kazakhstan, the Lower Volga region
and in the south of the Ukraine. Some rivers, as the Boll-
shoy and Yalyy Uzeni, dry out completely and fill up only
during the autumn rains. The rivers of the Aral-Caspian de-
pression carry less than 5% of their annual amount. In the
steppe regions of the North Caucasus, Lenkoran', the West-
Siberian depression and the south of the Ukrain the rivers
do not carry more than 10% of their annual flow-off. The
rivers of the Urals have their summer low at the end of June.
Some, however, carry even more water than in other seasons
due to heavy rainfalls. The quiet-flowing rivers of West
Siberia carry up to 30 to 406 of their annual flow-off.
Many rivers of the Lena basin and the right affluents of the
Yenisey start their summer low in July for about one month,
but sometimes do not have a summer low. The summer low of
Card 112 the mountain rivers of the Altay, Central Asia, the Caucasus

The Summer Low-Water Mark (of Rivers) SOV-26-58-8-48/51
and Sakhalin sets in at the end of July. Here the level
does not vary considerably, because the eternal snow on the
mountain peaka playa an important rolo in this respect. The
summer low varies with respect to time and flow-off in the
rivers of the Black-Sea shore side of the Caucasus, the af-
fluents of the Dnestr, that come from the Carpathian Moun-
tains. There is a great regularity and extended summer low
in the mountain rivers of the mountainous parts of the Cri-
mea, Lenkoran', north slope of the West Caucasus and the
Baltic elevation. There is no summer low in the river basins
of Soviet Par East, East Sayan, Transbaykalia, the Vitimo-
Olyokminek mountain region, Yana and Indigirka. The know-
ledge of the individual river summer lows may assist in plan-
ning and balancing hydroelectric resources and irrigation
systems.
ASSOCIATION: Institut geografii AN SSSR /Moskva (The Geographical In-
8titute AS USSR /Moscow)
1. Inland waterways--USSR
Card 2/2

KM4PIKHp A. 0,,, Candidato Geogr got (diss) -- "The conditions of runoff
foxmation and the hydrography of the Tjortbern, Subpolar, and polar Urala".
Moscow, 1959. 15 pp (Acad Sci TJSIM~ Inat of Geogr), 110 copies (KLY No 23p 1959p
162)

BOGOTATIMISKIT, G.P.; DURAYST, T.M.; NEDOSEM, D.Y.; DAHILOTA, N.A.,
avtor kart; XZKMgff,_A.0j, avtor kart, Prinimal uchastiye
GALITSCIT. Kjf'., kand.okonom.nauk, nauchnyy red.;
ZABILIN, I.K., )mnd.geograf.nank, nauchnyy red.; SAMSONENKO,
L*Y*, nsuohnn red.; FRATKIN, N.G., kand.geograf.nauk, nauchnyy
red,*, KALICMMIT,* G.K., red.kart; BILIC 0. R.K., mladshiy
red,; GUM, D,A,l takhnered.
(The earth and the people; geographical calendar for 19601 Zenlia
I liudil geografichaskii kalandarl 1960, Moiskya, Geografgis,
1959. 381 p.[_ Seasonal phenomena In U.S.S.R.naturej-8axon-
W ia4laniia v prirode SSSR. Sost.N.I.Danilova, A.O.Kemmerikh.
12 maps. (KMA 130)
(Geography-Dictionaries) (Calendars)

AUTHOR: Kemmerikh, A.0. SOV/26-59-1-31/34
TITLE: Rivers in Winter (Reki zimoy)
PERIODICAL: Priroda, 1959, Nr 1, pp 125 - 126 (USSR)
ABSTRACV." The article gives a brief survey on the water dis-
charge of the USSR's principal rivers during the
coldest winter months. There is 1 table.
ASSOCIATION: Institut geografii AN SSSR /Moskva (The Geographical
Institute of the AS USSR /Moscow)
Card 1/1

AUTIiOR: Kemmerikh, A.0. SOV/10-59-1-11/32
TITLE: River-nan-_-=--in -th"'e Northern, Subpolar and Polar
Urals (Stok rek severnogo, pripolyarnogo i polyar-
nogo Urala)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya geografiche-
skaya, 1959, Nr 1l PP 85-90 (USSR)
ABSTRACT: The author emphasizes the significance of the study
of water resources of areas in connection with the
proposed constructions of hydro-technical projects,
and a railroad along the eastern slope of the Ural
mountains. In this article, the author gives a
general description of the physico-geographical
and climatic features of these areas, and presents
a map of the average annual run-off of local rivers,
based on 40 years of observations. According to
the author's estimate, the average a nual run-off
of rivers of these areas is 118.7 km3, with an aver-
age module of run-off at 12.3 lit/sec per square km.
Card 1/2 The average annual run-off of rivers on the eastern

SOV/10-59-1-11/32
River Run-Off in the Northern, Subpolar and Polar Urals
slope is 44.3 km 3,
lit/see per square
western slope 74.4
12.3 lit/see per sjuare
1 map and 4 Soviet
with an average module of 9.0
km and that of rivers on the
W and an average module of
km. There are 4 graphs,
references.
ASSOCIATION: Institut geografii AN SSSR (Institute of Geography
of the AS USSR)
Card 2/2

3 (7)
A-TIJOR: Kemmerikh, A. 0. 00V/50-59-4-11/ I
2
TITLE: Chart of the Avernge Discharge of tho ftivors in the !rorthern,
Pre-polar and Polar Ural (Ktirta sredrieCo 2toka rek Severnogo,
Pripolyarnogo i polyarnogo Urala)
PERIODICAL: Meteorologiya i gidrologiye-, 1059, '1r -~, Pr 17-501 (USSR)
ABSTRACT: The numerous rivern of the Northern, Prr,-Polgr and 11olar Ural
serve as sources of water nower. Their potential is much
greater than the real utilization of their possibilities.
Industry develops very fast in these regions, large
hydroelectric power statiorLq will be built in the next few
years, the water of the Pechora, on the banks of which they
are to be erectedt will be conducted to the Kama.
Hydroelectric power stations bill also be built on the Usa
and on other rivers. At present, a railroai line is under
construction along the cast slope of the Ural. In connection
with all this, the main characteristic of the discharge of
these rivers, the diqtribution of the same over the mentioned
area, as well as the.-determination of the amount of these
discharges, are given hero in default of direct hydrometric
Card 1/3 observations. A chart of the average discharge is given here

Chart of the Average Discharge of the Rivern in the SO-1/50-59-4 11121
Northern, Pro-polar and Polar Ural
(Pig 1) on the basis of the observation-i of '1954-57. The
corrolation between the nvovaC,~ nnniinl disolh,irgo nnrl tho mqnn
height of the basin is tak.en hero aq ri basis for this chr~rt.
24 out of the 33 points were chosen a," up tc standarl, ~)O
of them refer to nn obs~:rvptlon neriod of 15-4.0 yearst 20
to 10-15 years, and 30 ~*".) to 5-10 yoltr,~)' In contrPat to tho
high-mountain parts of the Alpa, the C"aucno.is rmrl 3cviat Centr-PI Aaii.
the variation of the discharge on the UrR1, Rt conparatively
low mean heights of the catclraont drainal-a arens, takes place
proportionall,v to the riae in the mean height of the catchment
drainage area. The g3~ndipntl )f this change varies between
3-8 and 8.5 I/sec km' per 100 n; the gradients decrease from
north to south. The new chart givan here is more accurate than
the former charts (Refs I and 2). This can be seen very
.~.distinctly from the fact that a much higher discharge
(~:,--30 l/sec km2) was found in the high-mountain section of
the mentioned part of the Ural. On the other hand, the chart
given here shows only the discharge of areas over 1000 km2 in
an accurate way,, For smollor areas, th--~ DhYsical-geographical
Card 2/3 conditions of stnFtil catrhmr,nt ~Iraina-e areas have to be
0

Chart of the Average Discharge of the Rivnr3 in the SOV/50-59-4-11/21
11orthern, Pro-polar and Polar Ural
conaidorid. The area of the highest discharge coincides with
the area of the highest precipitations, and is situated on the
western slopes of the Ural - in the basins of the rivers
Shumort Koslyuj Ilych, Podcherem rn(l Visnern.. In the upper
U 2.
course of these rivers, the discharge is more than. 30 1/sec kr,
Much water is also transported by the Great and Small Usa, the
left-hand tributaries, and the tipper courues of the rivArs
Kara, Shuch t ya, Sob I , Voykor, Syn I , Lyapin., Severnaya Soo Iva,Kosba
and Yayva. In connection with the higher PrOCiDitations on thO
west slope of the Ural, also the absolute arount of discharge
is bigger at equal heights of the riest slore f-han of 'the cast dope
of the Ural. At an average annual disehArge of 12.3 l/sec 1-m2
for the whole area of the Ural investigated, it iv
12 on the
16.1 1/nec km2 on the west slope, and 9.0 113cc kr
east slope. There are 1 flaure and 2 Soviet references.
card 3/3

-- UXMIKH._ ".k--
Some hydrographic featurso of the trans-Ural forest-stOPPO tons-
Trudy In" t. biol. UFAN SSSR no.19223-35 ;o6o. . (MIR& 13:10)
(Siberia, Western-lLydrblogy)

10!~WRIKH ? Aleks2Z Oakarovichj LIVOVICH, M.I.,q doktor geogr. naukj
otv. red.; WrINSIMII'V.S., red. izd-va; HYLIKA, Yu.V.v
tekhn. red.
[Hydrograpby of the Northern.. Sub-Arctic,, and Arctic Urals]
Gidrografiia Severnogoj, Pripoliarnogo i Pollarnogo Urala. Mo-
skva# Izd-vo Akad.nauk SSSR, 1961. 136 p. (MIRA 15.-1)
(Ural Mountafts-Hydrograpby)

~ ~ ~ . ~.. ~ 1! , ",
- 1 1- t, - I
,'Ia:il, Arctic Uralss. ~ . 1 j,;`m,7
- floods in t, - Arctic and suL (!:-T- -~ 1, : I
~
11 3:35-36 '!r 161
C', 1 0 (Ua,al 'l:oul,lt-lainz;--:?loods)

-KEMMERIKH.-A.0., kojid.geografonauk
Deepest lake in the Urals. Priroda 50 -no.4:13.2 Ap 161.
(MIRA 14:4)
1. Institut geografii AN SSSR, Moskva.
(Bollehoye Shchuchlye Lake)

KEMMERIKHJ A.091 kand.geografonaukj MALIK, L.K.; KACHURIN, B.S.
Spring floods. Priroda 50 no.5:124-125 My 161. (MIU 24:5)
1. Institut geogra-fii AN SSSR (Moskva).
(Spring) (Floods)
I ~
A

KEMMERIKH, A.0 kand.geograf.nauk
Underground waters in the deserts of Central Asia. Priroda 50
no-12:98-101 D 161. (MIRA 14:1Z)
1. Institut geografii AN SSSR, Moskva*
(Soviet Central Asia--Water, Underground)

DANILOV, Vatallya Anatol'-yevna; KE0OUKH, Aleksandr Oskarovich;
RODOMAN, b.B... red.; KI111YADOVA, z.V., mlad. red.
[Seasons of the year] Vremena goda. Moskva, Mysllp 1964.
172 p. (MIRA 18:1)

KEMMERIKH, A,O., kand. geograf. nauk (140sk-v6)
Spring mud flove in the Ural Mountains. Priroda 54 noo3i 814)
126-127 Mr 165. (MIRA 1

KEW-011KHO A.O., kand.geografonauk (Moskva)
Southernmost glacier of the Urals. Priroda 54 no.7:76 77 11 965*
(MI RA 18:7)

ARMAND9 D.L.; BUDAGOVSKIYI A.I.; VENDROVp S.L.; VITVITSKIYj G.N.;
GELLER, S.Yu.; GERASIMOV, I.P.; DZERDZEYEVSKIY, B.L.; GWKH, I.S.;
I *
GRIGORIYEVP A.A.; DANIWVAp N.A.; ZRIVAGO, A.V.; gMMERIKH A.O.-
KRAVCHENKOI D.V.; KUVSHINOVA., K.V.; MEDVEDEVA, G.P.*; UU-ifflR~,u.L.;
CHUBUKOV., L.A.
Aleksandr Petrovich Galltsov, 1909-1965; an obituary. Izv. AN
SSSR. Ser. geog. no.6:145 N-D 165. (mm 18:11)