SCIENTIFIC ABSTRACT KRIVSKY, L. - KRIVTSOV, P. T.
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S
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100
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December 31, 1967
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SCIENTIFIC ABSTRACT
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TLAMICHA, A.; KRIVSKYS Le.j.,jDUM, J.
Classification of solar radio storms in the motor rangd and
their frequency 1959-1961. Biul astr Cz 15 no.2:49-52 164.
1. Astronomical Inatitutel Czechoslovak Academy of Sciences,
Ondrejov.
F.PlIvix1f, 1.
- ..- -1- - ,
on tho flare of 1956 Augu3t 3.1 connected with the ejection of
cos.mic ray arter Y-ahaped pLaso. Blul asLr Cz 15 no.2:75-",16
'64.
1. n*,)trunc)mi,::uI Institute, Czectoslovak ;-aetr~my of Science3,
Ondrejov.
K,?-. V~I-K 1." 11,..- .
t,.,rpuscjlar !tn,.j pv turt Cloud fron 1"Ifirf; an p3r'Atll~
Of radio emissior in da,, my dek!t-m tinll' x*n r-,!rl;tl. P'-%..~"
Oz 15 164.
c.cljc-:!'c-.mk Ac,.-je,.ty of Sci-nt:es,
1. Aotrrnomical Institivs!, C7 I
Undrej'ov.
KRIVSKY, L.
Solar-flare origin and nature of the radiation increase
recorded b~ Explorer IV on August 25, 1958. Biul astr Cz
15 no. 4:131-133 164. -1
1. Astronomical Inatitute, Czechoslovak Academy of
Sciences, Ondrajov.
Nl,;~,TOROV? G.;
L. Krivnky,, L.j; L,1-1-~'tloil
1(7,n!;vj,h,t3ric anomaltea as an In.11--ator of rpdiation from a
norr.uscular c3oud following a colar, elhi-nmoopher-1c firkre. G-zcmag. i
aer. 4 no.6:1059-1063 11-D 164. (MIRA 18:1)
1
.&. Geofizicheakly institut Bolgarskc~j A111, Scfiya i Astronortcheakiy
institut Chakhoslovat.-ka:( Akadernii nauk-,
L.,
On the changes in the D-region during flares according to T-'A.
Biul n3tr Cz 16 no.,2:i26 f65.
1. Astronomizal P-stitute of thn Czechoilovak A-ademy of 5::lenceq,
Ondrejov. Sulmitted Atigust 1~, 196.11,
3874~-66
ACC NRa AT6020521 SOURCE CODE: CZ/25i4/65/000/051/O176/oi83
AUTHOR: Krivsky, L.
ORG: Astronomical Institute of the Czechoslovak Acade _of Sciences, Obs.-Crliratory
Cndrejoy
TITLE: Space model of a cloud of solarcosmic and subcosmic particles
SOURCE: Ceskoslovenska akademie ved. Astronomicky ustav. Publikace, no. 51, 1965.
3rd Consul'tation on Solar Physics and Hydromagnetics, Tatranska Lomnica, 13-16
October 1964, 176-183
TOPIC TAGS: Earth planet, solar particle scatter, cosmic ray, subcosmic particle,
solar flare, solar limb, interplanetary space, cosmic particle, solar models '501'fip-
P*9RrICA-C- J 051)71C, *vt)YjWJr,eLe
ABSTRACT: On the basis of previous studies and other viewpoints on flares with out-
flowing cosmic rays recorded on the earth and accumulating near the western limb
of the sun, the article discusses the model of a cloud of solar cosmic and sub-
cosmic particles. Assuming that the central part of a twisted cloud of rapid solar
particles situated between 500 and 900 W flows toward the earth as a sort of a
channel carrying cosmic rays, and on the basis of studies covering 70 cases, it was
found that the main lontigudinal range of flare occurrence lies between 50*E and
55c"d with an accumulation between O*-200W. The 300E position appears to be the
5-6
AT6020521
extreme limit of flares from which a compact cloud of subcoamic particles (PCA
effect) can normally reach the earth. In such cases the central parts cf the clouds
containing higher velocity cosmic particles pass east of the earth. The angular
dimension of the cloud of emitted high-velocity particles to the distance of the
Earth will then be relatively large. Some cases calculated show that the half width
of the effective space angle for cosmic rays is 350-800. Together with the periph-
ery of subcosmic rays, it reaches h50-110' in most cases. The effective angle of
the particle outflow, its half width, and its width at the dijtance of the terrestrial
orbit can be computed and are found to cover a considerable range. The computations
are valid for the first particles in the initial phase of the emission of cosmic
and subcosmic rwjs when no further dispersion of particles due to magnetic inhomogene.
ities in interplanetary space and in the vicinity of planets has occurred. The
author is in favor of a relatively large angular width of the cloud of high-velocity
particles and considers hypotheses of narrow angular beams of such particles to be
unfounded. He adds that extended compact particle clouds will actually obstruct
space navigation and eventually even the escape of interplanetary spacecraft and
crews outside the cloud of high-velocity particles. In the discussion following
the article, the author supported the "magnetic bottle" model of corpuscular clouds.
He also agreed that the effective angle at the distance of 1 au is influenced by the
scatter of solar cosmic and subcosmic. particles in interplanetary space and depends
on the phase of the total solar activity. Orig. art. has: 5 figures. [GC)
SUB CODE: 03 SUBM DATE: none/ OTH REF: 013/ SOV REF: 001/
2 /2 jVX^,_
L 353j3-66 EWT(I)/FCC OW
CODE: CZ/00 7/65/000/003 6V~/bdl~
AUTHOR: Krivsky, L. (Doctor; Candidate of sciences)
'iy us
ORG: Institute of Astronoy i st,
V, Czechoslovak AcadepZ of Sciences (Astronom c av
CSAW
TITLE: Radiation on Mara
SOURCE: Radar, no. 3, 1965, 43-44
TOPIC TAGS: solar radiation effect, solar radiation intensity, Mara planet, Earth
planet, primary cosmic ray, secondary cosmic ray, radiation biologic effect, radia-
tion shielding
ABSTRACT: The article deals vith cosmic radiation on Earth and on Mars, and dis-
cusses the effect of primary and secondary radiation particles on living matter.
The level of cosmic radiation depends on atmospheric density, magnetic-filed intensit)
and the chemical composition of the air. Approximate data on the density of the
atmosphere around Mars could give men a rough idea of the intensity of cosmic radia-
tion on that planet. So far, estimates are based only on indirect measurements. The
author compares studies by Soviet astronomer-Y_,_1. Moroza and Am3rican scientist
H. Yagoda. It seems that the Martian atmosphere provides less protection against
radiation than does the Earth's ntmosphere. Periodical erruptions of the Sun may
Card 1/2
L 35333-66
ACC NR, Ap6oo9138
result in strong fluctuations of radiation intensity on Mars. There is a possibility";
that this periodic fluctuation may result in repeated new formation of primitive
forms of life. Cosmonauts on Mare may have to retreat into a protective cabin
during periods of high radiation. A postscript to the article indicates that it was
written before results of the Mariner 4 venture had been published. Orie. art.
has: 1 table. [KS)
suB com o6, 03/ SUBM DATE! none
I Card 212
ACC NR' AP7000702 SOURCE CODE: BU/0011/66/019/010/0893/0896
AUTHOR: Serafimov, K.: Krivsky, L.
ORG: Geophysical Institute, Bulgarian Academy of Sciences; Astronomical
Observatory, Ondrejov
TITLE: Effect of superposition of two excessive solar radiations in the middle
ionosphere
SOURCE: Bulgarska akademiya na naukite. Doklady, v. 19, no. 10, 1966, 893-896
TOPIC TAGS: a=, ionosphere, solar chromosphere, chromospheric eruption,
ah= rol I sv;hw ionizing radiation, solar UV radiation, ionosphere
electron density Wavausu, solar radiation aq
ABSTRACT: A study was made of six chromospheric eruptions accompanied by an
eruption filament, which occurred on 29 December 1965 under relatively calm solar
conditions. Ionograms of the Sofia Ionospheric Station were analyzed on the
eruption day and three control days before and after the event in order to obtain
morphologic information and a first approximate determination of the radiation-
frequency range accompanying the phenomena. Examination of critical frequencies
Card I / 2
AP7000702
fj': of the middle and high i.onosphere confirmed that the electronic density
increases due to the superposed action of the six solar eruptions. Study of fE
values led to the assumption that filament appearance was accompanied by a distinct
ionization increase in the E layer. Examination of critical frequencies in the Fl
and F2 layers showed no par ticular changes. The authors believe that UV radiation
in the A (200-800 A) range either does not increase with a filament, of increases
only slightly. It was concluded that the main ionizing radiation which accompanied
superposition of two qaulitatively different solar phenomena on 29 DecemberI
was concentrated in the X-ray range. The paper was presented by Academic an
L. Xrastanov on 23 June 1966. Orig. art. has: 3 figures. [DR)
SUB CODE: 03, 04/ SUBM DATE: none/ORIG REF: 0021SOV REF: 003/
OTH REF: 002/
2 2,
SOBOLEY, V.P., inzhener, loureat Stalinskoy prealtz KRIVSKIT, M.N., Inshener.
Reducing the coist of sarthwork In building canals of average cross section.
Hekh.trud,rab. 7 no,10:42-45 O-N 053. (MJARA 6:10)
(Canal s )
AID P - 3212
Subject USS/Hydraulic Engineering
Card 1A Pub. 3 5 - i6A9
Authors Krivokiy,, M. N. and k. I. Safronovt Engs.
Title I Som types of scrapers
Periodical t Gidr. stroi.j 5. 43-45j, 1955
Abstract : The article discusses certain types of scrapers used in the USA.
Six photoo and 3 tables with data. Five English references,
1953-1955.
Institution : None
Submitted t No date
IV _~
Subje(A
Ca rd 1/1
Author.,3
Title
Y,
USSH/Hydr. Eng.
19/19
AID P - 3955
Pub. 35 -
Krivskiy, M. N. and A. I. Safronov, Engs.
Earth bulldozer.
Periodical Gidr. stroi., 7, 47-48, 1955
Abstract A report on earth-working equipment manufactured in
Euclid and used in the USA. A detail description of
the machine to Iven. Three photos. One Russian ref-
erence (no datel 2 US. 1951-1953.
Institution : None
Submitted : No date
"-RITSUT' M.S.,, Lpshener.
First results of using the D-264 sarthmoving awhine equipped
with a transporter bridge. Oldr.strot. 23 no.2:23-27 136.
(mm 9:8)
(Bartbooving mwhisery)
,~_ - I- ~ - __ ___ r', -1 -
- -i , - - - I , , '. 11 -_
KRIVSKIT, M.N., inzh.
Conference on mechanization of soil stabilizatiom, Gidr.otroi.
26 no.lC.60-62 157. (Min 10: 10)
(Soil stabilization-Congresses)
---
KRIVSKly, X.; S"RONOVO A.
Dump tractor-lorry with 110 ton capacity. Avt, transp, 36 no,,11861 N 058*
(Dump trucks) (Km litil)
XIUVSKIY,_.M.N_, _i_nzb.
Tafiting the experimqntal model of an nxcav&.ting and -.Utting
machine. StroiA dor.mashinostr. no.7:12-15 J1 159.
(14IRA 12:11)
(Excavating machinery--Testing)
KRIVSnT, M inzh.; SOFRONOV, A., inzh.
Rotary giant. Ttkh.mol. 28 no.lli20-21 160. (MM 1302)
(Accavating machinery)
KRIVSKIY, M.X., inzh.
Earth-vorking and cutting mehines in construction of ~ ,rie
Irtysh-Karaganda Canal. Gidr. stroi. 33 no.2%32-35 F .63.
(MIRA 1634,*1
(Irtyah-Karaganda Canal-Farthwork)
ANISIMOVp I.V.; KRIVSUN(IV, V.N.
CharacWristice of the trAnsient conditinm of pirate
Khim. i tekh. topl. i masel 10 no.3:45-5) Mr 165,
(WRA 1.8:
1, Moskovflkiy inslitut kbimichemkogo nqpbiroqtro~ren'.v-. i
Saverodonotakiy filial Orfytnt*j--krnAtruktormkirgt.,
KRIVSUNOV, V. N.; ARONINAP S. Ye.; YANOVSKIY, S. M.j RATUYEV, A. A.
Experimental study of the static characteristics of the athane-
ethylene tower. Khim proin no. 3t221-224 Mr 164. (MIRA 17:5)
V.
leff~the,rritirnl model of the 3thtJ(;
ethtinf-(:"~.ylenn rectification rolm7in. KIIin. pr?~.n.
IJT-
617-620 Ag 165. -:1 1- ,
KRIVSUNOV9 V.114.
Iroblema In the wthemm.1cal doacriptica of transient processes
in a plate rectificatinn c.-dimn. Tr-arly MIKYM 211,~52-65 163.
(MIRA 17:6)
AITISIMOV) I.V.; KRIVSI)1"011, VJI..
,- - ------
Mathematical description of the static characteristics of
a tray rectification coluran. Khim.prom. no.9:572-575 Ae 162.
(MIFLA 15.9)
(Plate towers)
KRIVSUNOV, V. X.; AXISIKOVV 1. V.
Static characteriatico of plate rectification colu=s. Xhim.
Prom, n0,31219427 Mr 163# (MIRA 16:4)
(Plate towers)
tfgo'R/Cheirds try Polarization 7'u b 49
ChEmistry Adsorption
"A New Form of Chemical Polarizations II, Experimental Proof of the Existence of Ad-
sorption Layers and Investigation of Their Properties," M. Loshkarev, A. Krivtsov,
A. Krytikova, 11 pp
"Zhur Fiz Khim" XXIII, No 2
Measured double-layer capacitance for various electrode potentials in Nae 1 tions
3 so u
with additions of beta-naphthol, thymol, diphenylamine, and other surfa ctive sub-
stances. Existence of dense adsorption layers is confirmed by sharp drop in double-
layer capacitance fur zero surface potential in nolutions with these additions.
Submitted 3 Jun 48.
FA 47/49T19
--~ T 7-~- - -tL-. i .
A geol,"Eical sketch and nineral resources of the reclon
Chelltbint-k, Chellt~blnskoe obl. ~.-os, 17,1.-vo, 19.16. l1w, p., maps. (49-43235)
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KRIVTSOV, A.I.
~4~
Stratigraphic contents of the Sinaen systam in the northeasterp
sector of the Russian Platform. Inform.ebor. TSMII no.1:24-36
155. (MLBA 9:12)
(Russian Platform.-Geology, Stratigraphic)
15-57-2-1258
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 2,
p 7 (USSR)
AUTHOR: Krivtsov_) A. I.
TITLE: New Data on the Stratigraphy of the Lower Carboniferous
at the Eastern Slope of Baltic Shield (Novyye dannyye po
stratigrafii nizhango karbona vostochnogo sklona
Baltiyskogo shchita) ,
PERIODICAL: Inform. sb. Vses. n.-I. geol. in-ta, 1955, Nr 2, pp 40-
45
ABSTRACT., Results of the littiographic study dealing with the Lower
Carboniferous deposits revealed by 60 drill holes along
the middle course of the Onega River complete the
stratigraphy of the Vytegorskiy-Andomskiy region.
According to these now data, the earliest deposits,
lying uncomformably on the Upper Devonian, are comprised
of a sub-mineralization stratum, kaoline clays (l m to
15 m) with remnants of the Upper Turonlan flora.
Card 1/3 Analogs of the Yasnaya Polyana stage, to which the
15-57-2-1258
New Data on the Stratigraphy of the Lower Carboniferous (Cont.)
Patrovskaya series of V. P. Barkhatova completely belongs--K
geologii basseyna yugo-vostochnogo poberezhlya Onezhskogo ozera
i verkhovlyev p. Onegi (Geology of the Southeastern Lake Onega
Shore Basin and the Onega River Headwaters) Gosgeolizdat, 1941--
are represented (from the base upward) by kaolinite-bauxite
stratum (5 m to 25 m), a layer of iron-bearing clays with iron
bean-o.re streaks and a layer of sand-clay deposits (2 m tolS m);
the first two layers belong to the Stalinogrosk (Carboniferous)
horizon and the last one to the Tula horizon. The age of the
Tagazhemskaya series does not begin with the lower Serpukhov,
but with the Oka, through juxtaposition of three limestones of
this series with the rocks of the Aleksinskiy, Mikhaylovskiy,
and Venev horizons. Gigantoproductus iganteus var. typica
Sar. confirms the Oka-age of the Tagazhemskiy series. Inter-
ruption in the deposition occurred in the Oka time along the
middle course of Onega River. The age of the Devyatiny series
is also altered so as to correspond wlLh the Tarusskiy and
Steshevskiy horizons. The area covered by the sea increased
during 'this time. The author correlates the Biryuchavo series
Card 2/3
15-57-2-1258
New Data on the Stratigraphy of the Lower Carboniferous (Cont. )
(sand-clay-carbonate deposits, which a number of investigators
believe to be of various ages--from the Devonian to the Lower-
Middle Carboniferous) with the lower hamurian--the Protvinskiy
horizon--and with the lowest part of the upper Namurian. The
Lower Carboniferous age of the Biryuchevo series is sub-
stantiated by the fact that this series lies directly on the
Devyatiny limestones~without an unconformity; the Lower Carbon-
iferous cycle of the deposit terminates with the Hiryuchevo
series. The upper limit of this series has not been adequately
studied. The Biryuchevo series is known only on the northern
slope of the Vetrenyy belt; during this time continental con-
ditions prevailed on its southern slope.
Card 3/3 Do M. R. - Cho
KRIVTSOY, A.I.
- 'i" I
tratirrpahle nomenclature of the lower Cambrian In the Baltic Sea
region and regions adjacent to it (discussion), Inform.abor.YSICGEI
no.3:46-49 156. (MLELA 10:1)
(Baltic Sea region-Geology, Stratirxaphic)
KRIVTSOV, A.I.
-- - --j-
Harova beds of the middle Devonian 1n the LithuAnian S.S.R. and
neighboring regions. Izv.AN SSSR.Ser,gool,, 21 no.1101-97 N 156#
1. VessoMnyy
I okhrany nedr
MRA 10.1)
yedIMy geologichasly inatitut Hinisterstva geel6gtl
SSSR, leaninMd,
(YAthuanIA--G6010(Vr,
Strntigraph1c)
AUTHOR: Yrivtoov,
TITLE- The Latest Dnta-on Lower Peleonolc Formations on the Fnstern
Slope of the Baltic Shield (Nizhniy paleozoy vostochnogo
sklona Bnltiy'skogo shchita no noveyshiT dmnnym)
PERIODICAL: Izvestiyn Akademli Nauk SSSR, Seriyn Geologicheakaya, 1950,
*41 pp63-75 (USSR)
AB3TRACT: The Author cites the latest data characterizing the lithologic
composition and stratigraphic correlation between the normal
sedimentary deposits of the Cambrian And Sininn Periods of
the eastern slope of the Baltic shield. During 1954, the
author studied the core samples from numerous deep test wells
And uncovered the presence of typical to the Baltic region
"blue clays". The find of the remains of chitinous sheathe of
tubular worms, resembling the "Sabellidites cambriensis Jan"
classified these clays as deposits of the Lower-Cambrian age.
In the basin of the Onega River, these clays lay on t)ie send-
gravel layers of coastal-maritime sediments, corresponding in
age to the Gdov layers. The author assumes that these coastal-
continental and coastRl-,nnritiwe sediments cAn be classified
As deposits of the SlniAn Period of the Lower Faloozoic Era.
Card 1/3 At the All-Union Conference in 1955, on queations of strRti-
11-5R-4-6/16
The Latest Data on Lower Paleozoic Formations on the Fastern Slope of the
Baltic Ohield
graphic and geochronological subdivisions, it was decided to
single out a new, older-than-Combrinn group within the Pnleo-
zoic Era. This group was called either Focambrian or Sinian or
Rifean Period. It was proposed to include into this system
lnminaritic clays and Gdov (Gdovskiy) layers of the Baltic
columnar section (Table 1). The products of the ancient erosive
crust of crystalline foundation rocks and the normal send-
argillaceous deposits underlyin;- the Gdov layers of the Lower
Cambrian period form a part of the Sinian system. Vie Lower
Cambrian deposits are observed Along the coast of the Dvina
and Onega Rays of the Nhite Sea and are Widely spread nlong
the eastern slope of the Baltic shield. The author describes
in detail various formationn and deposits of this period.
In conclusion he distinguishes by age two different sections
in the deposits of the Sinian Period, corresponding to two
epochs In this period. Ono (t-,e Lower-,-)inian epoch) WAS
characterized mainly by the constal-continental regime of so-
dimentnry accumulstions (ancient erosive crust of crystnllino
Card 2/3 foundation rocks and the strPtum of sandy deposits). TheV-
11-56-4-6/16
The Litost Dntn on Lower ralcozoic Formationn on the Fastern Slope of the
Baltic Shield
second (Upper-3inian epoch) was formed mainly by coastal-ma-
ritime argillaceous deposits. This letter regime continued
during the whole Lower-Cambrian epoch. At the end of this
epoch, the sea retreated and this territory and a lerpe part
of north-western part of the European part of the 73SR remained
dr,,- land until the beginnine of the Lower Ordovicinn trans-
gression.
There are 1 table, 3 figures, and 6 Soviet references.
ASSOCIATION: Vspsoyuznyy geologicheskiy institut (v:3PGF1) Yinisterstva,
raolo,vii i okhrnny nedr, Leninprnd (All-Union f",eologic Institute
3f the 11,iniatry of Ceolory nnd Conservntion of Mineral
Resources, Leningrad)
SUBMITTED: February 5,1957
Card 3/3 1. Gaclogleal tlura - Det0rx-i1rnt[cn USSR
- XRIVTSOV, A.I.
-- I - ~- ----------
Some data on the ancient weathered surface of the eastern slope
of the Baltic Shield. Inform.abor. VSEGEI no.16:51-65 159.
(MIRA 15: ))
(Baltic Shield--Petrology)
SOT I ---,
Genesis of Mesoognozolli: bawdtas in Western Siberia. Inform.
abor. VSBGEI no* 20:87-98 159. (MM 114:1'
(Siberiap Western-Ba=ite)
JIRITTSOT, A. I.
Carboniferous sediments in the eastern slope of the Baltic
Shield in conneotion with their bauxite potential. Isv.AN
SSSR.Ser.gool. 24 no.12:10-27 D 159. (MM 1318)
1. Tsemoyusnyy nauobno-Issledovatellskly geologiobeekly Institut
(TSJGJI) Ministerstya goologii i okhrany nedr SSSR, Leningrad.
(Baltic Shield-4,sology, Stratigraphlo)
(Bauxite)
. KRIVTSQV-,, A - I - -
Evaluation of the bauxite potential c' ancient (Sn-Cm ) carbonate
rocks in Gornaya Shoriya. Mat. VSEGEI. 0b. ser. no.21 160.
(MMA 14:7)
Gornaya Shoriya-Bauxite)
rbonatea)
t
KRIVTSOV, A.I.
Evaluation of the bauxite potential of ancient carbonate deposits
I I
;f the Kuznetsk Ala-Tau. Trudy VSEGEI 571l83-*29 161.
(MIRA 1514)
(Kuznetsk Ala-Tau-Bauxite) (Rocks, Carbonate)
-HV=O, -.A,.I- -..-
I --C~
silloilit*a in the Kuznetsk Alatau and
abor. VSMEl n0-5505-103. 162. (MMA
KRIVTSOVI A.I.
Prospects for finding Mecozoic bauxit,?s In the trans-Ural region
and in the northern part of the Turgay trough. Trudy VSEGEI 118:
69-97 164. (WINk 18:2)
IMIVTOSGV~ A,I,
Vow data on the Mesozoic buuyites of tht Urals. L-It. ~ pol. lskof-
no,4:138-152 Jl-Ag 165, (mlm 18:9)
1. Vsesoyuznyy nauchno-isal edovatel I ski y goologicheakiy imtltutp
Leningrad.
SOV,A 37-59- 2, 4535
Translation from: Referativnyy zhurnal. Nletallurgiya, 1959, Nr 2, p 315 (USSR)
AUTHOR: Krivtsov, A. K.
TITLE: Preparation of Electrolytic Coatings With a Pulsati~g C ~rrent (Polu-
cheniye jjal'%,anopokrytiy pri pulsirujushchem toke)
PERIODICAL: Tr. Ivanovsk. khim.-tckhnol. in-ta, 1958, Nr 7. pp 87-95
ABSTRACT, The author investigated the electrolytic depositior (ED) of Cu. Zn,
Ni, and Fe from the solutions of thetr sultittc~., with ~, pul-sat.ing current..
Short. regular current pulses of a duration commenskiri-te with the
length of the nonstationary processes taking place on -c electrode
passed through the clectrolyzer. The puls,.-s vvere in'erspiced with
appreciahle pauses. The maximum cd of the p(jises vas manv tityles
greater than the mean cd used in electrolysis. The catt 'ode polariza-
tion was studied with an oscilloscope; the quality of the dvposits~ i. C.,
luster, plasticity, and porosity, vkas also studied. It, the ED of Ni the
application of the pulse current caused an increase in the cathode polar-
ization and a decrease in the bath voltage. Under smout1h, surge and dip
conditions (high maximum D of 25 ampldm2) bright Ni deposits were
Card 1/2 fort-ned, porosity decreased, and pitting was absent- Similar
Preparation of Electrolytic Coatings With a Pulsating Current
SOV./I 37-59-2-45 35
phenomena were observed in ED of Fe. In the ED of Cu a pulsating current lu-ts
little effect oil tile appearance and structure of the deposit. In the ED of Zn with is
high cd during the pulses (50 - 250 amp/dm2) tile deposit had j coarse-grained
and dendritic structure, Bibliog;raphy: IZ references.
N. K.
Card 2/2
,em of a aynchronoun
240:94-102 t64.
AXCLIZIN. L.Ye.; BOROZDOV, I.A.; MMILO, V.Ye.; TR=LKIN, V-11- Prinimali
uchastiye: MMTAYEV, F.R.; BIRIMOT, N.Y.; BUBTRI, V.A.; VARMATSKIT,
I.M.; DMO, V.P.; MMMOV, V.S.; DUGUI, Te.T.; WEALOV, K.F.;
IVANOV, P.S.; KMIARRVA, V.P.; MOIJIN, H.I.; HOGILKO. A.P.; PANCHSHKO,
A.I.; PCMYUKOV, S.N.; PRIIHODIKO, N.D.; RUBIN, I.A.; SIDOIMO,
P.A.; TYUTYUNIK, Ys.I.; KHKSLINITSKIT, L.Ta.; BOYDAR'. V.I.;,KRII=Y.,
--LCKSHIN, V.D.; WYIMMO, H.P. RABINXOVA, L.K., red.izd-va;
BCMDT M A. Z.A., takhn.red.
(Types of :mine cross section] Tipovye sachenH-tr -gmykh vyrabotok,
Moskva, Gos.nauchno-takhn.izd-vo lit-ry po gornomu delu. Vol.4.
[Cross section of mines rapportad by a sectional ninforced-concrete
lining of URP-11 panels for 1-, 2- and )-ton railroad care] Sechonlis
vyrabotok, zakroplannykh abornoi zhelazobatonnoi krepliu Iz plit
URP-II, dlia l-, 2- 1 3-tonnykh vagonatok. ig6o. 278 p.
(MULA 13;12)
1. Kharikov. Gosudarstvennyy proyektnyy institut Yuzhgiproshakht.
(Kine timbering)
RALTIR, G.D., inzh.; KRI-VTSOV, A.T., inxh.
RSameonovokaiam Mine. UgDll Ukr. 4 no.8:15-19 Ag 160.
(MIRA 13:9)
(Ligansk Province-4draulic mining)
KRITTSOY A. T.; Ir"Ur, T. S.
Tranoporting awdliary materials in hydraulio mines. %o11
Ukr. 7 no.4925-27 Ap 163. (MIRA 16:4)
It GQzud&rvtvewV7 inatitut po proyektiroyani3ru shakbtnogo
otroltellot,va v yushafth rayonakh SSSR.
(Hydraulia mining) (Mine haulage)
I-V T-
Chemical Abet.
Vol. 48 No. 9
MAY 101 1954
Glasas Olay Products# Refractoriea,
Now Metbed of tieing with cellmic ins. P. KrMwv,
Sim lei. Prom. 29. No. 9,29-31( 1
are sugirsted- (1) arid camin 1 -0. NH#OH
.15, water 4.0. CuSOa 0 05 and raht ' of
Ch k with air-slaked Ihe (1: 1) 7-10 parts; 12) dry caseln
glue 1.0, water 1.5, CuSO4 0.03, and 0Wk 3A parft.
B. Z. Kwnio4r-
.- I- . . i
"The new coating method -,rith ceramic tiles," Construction Indu3try, 1952.
~7 -. ~' I - - -1~;. T -. ' ' - I
- ~ ~ 1 -4 ,
Decorative and house painting; text-book. ~,Ioskva, Trudrezer-vizdat, 1952. 2LIJ p. (54-3.1,5075i
TT320.K7
r , i )-:. . .-,.
K1UvT5Ov# B. ?.
Euilding Knehinery
"l-Tachines and :)ower tools for fin3shing, work In
congtruction, work." H. .'. Petrov. flekh.
strc-Lo 9 no. 4,31-32 Ap 152.
Monthly List of Russian Accessions, Librar., of Ccn.-Tess, JUlY 1952. UNCLAS'TVIL',
- - 1j.
19
" j v I '1~-- Yj V-r -
-- - -- ---- --- -- - - - -
1RIVTSOV, B.P., kand1dat tekhatchemkikh nauk; SHAPIRO,
-- ~ - -- " ~~*' I.P. , nauebrj7 redaktor; $01OLOVA, N.A.,
X.V., takhnicheskiy redaktor
[Tile and mosaic work] Plitochtwe
Trudrexavisdat, 1954* 179 po
(Tile Lqtng) (Mosaics)
Inshenor;
or., nTIOCHIIIA,
raboty Kosk*a,
bWA 719)
XRIVTSOV, Boris PanteleynonoVich.; MUPIRO, Illys Grigorlyevich, inzh.;
-" - - - ' -, - - '- MMI= 9 0. k 0 9 - n a-uo hnyy re d. ; TILINGATER, L, A. , re d. ; PODOBED,
B.G., red.; TOKH2. A.M., takhn.red.; MSON, MA. takhn,red.
[Tiling and mosaic work] Plitochnye i mozaichnye raboty. Izd*2.,
perer. I dop. Moskva. Vses.uchsbno-pedagog.i%d-vo, 1959. 268 p.
(MIRA 13:1)
(Rosales) (Tile laying)
-MtIVT,O;)V, Boris Fanteleymonovich; ~Alhillt(j, 111ya Grigorlyovich,
-iiiZli-., 9.qKfil, Y"a.D., nauchn. red.; LV,,VJ.N, M.I., red.
[Laying tile.--I, rosaics,
zaichrqe I kBIlolitovye
skva, Vynshain shkolu,
and "xyloliths.".l
raboty. Izdjej
1964- 301 P.
Plitochnye, mo-
erer. i dop, Mo-
(MIRj% 17:7)
.................................. ..... --
Inexhaustible possibilities for the skillful
machinery. Biul..tekh. inform. 3 no.10:-43 0
(BUlding machiner7)
XR:VTBOV, B.S,O Insh.
.-,~ 7, Using oompressed lavdnated wood for the repnir of conatruction
machinery b earings. Blul takh. inform. 4 no.2:18-19 7 158.
(Plywood) (Bearings (Yachinery)) (MIRA 11:3)
KRIVTSOV, B.S., Insh.
Fully mechanized mortar plants. Bluletekh.inform. 4 an-11:7-9
N 158. (KIRA M12)
(*rtar) (Mixing machinery)
KRIVTS,GV..,B-. S. , Insh.
Operation of tower cranes In assembling houses with materials
taken directly fron trucks. Blul.tekh.lnforn.po stroi. 5
no.9:11-12 S 139. ' (MIRA 12:12)
(Cranes, derricks, etaJ
(Precast concrete construction)
drying and heating
Blul.takh.inform.
(Leningrad-Drying
undnr construction
5 no.11:20-23
(MIRA 13W
(Heating)
IZZUITELI I S.A.p oty. red.; SKURAT, V.K., otv. red.; ZUBAREV,
S.N.p otv. red.; MOIMYEV, S.L.p otv. red.; ASTAFIYETA,
A.V.p kand. tekhn. nauko rod.; VASIKOVSKIY, YeA., red.;
VISIINEVSKIY, Ye.L., red.; ICRIYK red.; KOHOTKIN,
I.N., red.j MITROFANOV, S.Lp doktor tekL. naukp red.;
NORKIN, V.V.9 kand. tekhn. naukp red.; NIKITIN, A.A.p red.;
RUDNEV, A.P.p red.; SLASTUBOV, V.G.p red.; TKACIEV, F.A.p
red.1 RAUKHVARGER, Ye.L., kand. tekhn. nauk, red.;
FEOKTISTOV, A.T.fdeceaaed), red.; ZAYTSEV, A.P., red.
(Safety regulations for the dressing and sintering of fer-
rous and nonferrous metal ores) Pravila bezopasnouti pri
oboganhchenii i aglomeratnii rud tavetnykh i chernykh me-
tallov. Moskva, Nedra, 1964. 106 p. (MIRA 18:4)
1. Russia (1917- R.S.F.S.R.) Gouudarstvemyy komitet po
nadzoru za bezopasrym vedeniyem. v promyshlennosti i gor-
nor;u nadzoru.
I-- KRIVTSOV, G., yurist; KOR.OTXOV, V., yurist; GRIGORIYEV, A., yurist
Our consultations. Sov. profeciuzy 18 no.7:45-47 Ap 162.
MRA 15:3)
(Labor passports) (Vacations, Employee)
(Insurance, Disability)
TIMFEYEVt M., yurist; XRIVTSOV, G., yurist; YULIYEV, 1. (g.Saratov)
Our consultations. Sov. prcfsoiusy 18 no.8:46 16~. OUR& 1534)
(Employees, Dismissal of) (Overtime) (Eminent domain)
'PARSHIN, k,Ys.: KRIVTSOV G F.- SLICDHNV. I.P.. podpolkoynitc. red.;
MYASHIK- -- , - a h;. red.
(Privileges, pensions, and side for servioemen and their familtaij
a handbook] LIgoty. pensti i posobiia voennoolushaahchin i ikh
saullam; sprovochnik. Moskva, Voon. izd-vo Ht-va obor. SSSR, 1958.
259 p. (Pensions, Military) (HIRA 11:5)
SHVACHKIN, Yu.P.;KRIVTSOV, G.G.
. Preparation of 6( -014 -~.(4-liydroxy-6-mothyl-2-pyrimidyl)-41aninae
VesteMeak. un. Sor.2: KHim. 18 no.4*.91-92 Jl-Ag t63. (MIRA 16:9)
1. Kafedra(erganichaskoy khimii. eloskovskago universitata.
Al;iiine)' (Pytamidft6) (tub*n isotopes)
S,-PIACHKIN, Yu.P.; IMTVTSOV. G.G.
Potential antimetabolites. Part 13: Synthesis and proper-ties of
cc -'-.,./4-~-(4-hYdrOV--6--mathYl-2--pyramid~yl)-alanine. Miur.
ob. kbim. 34 no.7t216,1-216,1 il 104 (MIn I'll 18)
1. Moskovsk~-y gomdars",;venn7y unliverg-Ifet imeni M,V.Iomonosova.
KRIVTSOV, G.S.
Geometrical methods for interpreting isolated hodographS of refletted,
waves@ Uchosap~TGU no*36tl44-157 160* (KIPA 34:5)
(Seismic. waves)
1. KRIVTSOV. 1.
2. USSR (6oo)
4. Windmills
7. Improved collective-farm windmill. Sell.stroi. 2 no. 1, 1947
9. Yonthly List of Russian Accessions, Library of Congress, March 1953, Unclassified.
r Lf~ll n
Mla ......
RAY,
KRIVTSOV, I.P.. aspirant
Grab buckets with a high pivot center for automatic
loaders. Trudy XMIT no-34:13-18 159- (MIRA 13:1)
(Loading and uuloading-Equipment and supplies)
KRIVTSOV, I. P., Cand Tech Sci -- "Study of the process of
scooping friable material by a grab bucket with-4ft
4,wtvt~ 64% 1
overhead twn4-ng center (for A4e automatic loader)." ~I rkov,
Mrl- P~ I t Vol-IJ6
1961. (Ar'kov A*40"J'Inst) (KL, 3-61, 245)
h
- 255 -
STOGOV,-V,N,-,- doktor tokhn.naukj UtM'jOV, I.P.9 inzh-
Loader shovel with upper pivot center. Stroi. i dor. mash. 6
no.2:11-14 F 161* (MIRA 1415)
(Power shovels)
KRIVTSOVj K.
"Effectiveness of Technolo in Agriculture in the Soviet Union. Tr.
From the Russian" P 931 FAGVTUDOKM, Vol. 6s No. 4, Apr. 1954,,
Budapest, Hungaryl 0
501 Monthly List of East European Accessions, (EEAL), LC, Vol. 3, No. 12,
Dec- 1954s Uncl.
MMIZVs R.Mq pklVTMt-",j kand. arkhitektury,, nauchMy redefrinlrAll
uc)2aatiye: BOGDANOVO I.M., inzh.; WHOM, V.F., inzb.,-, VOLFIANO
B.L.; inzb.; DAVIDOVICHp L.N.p kand, tekbno naukp rateenzentj DENI-
. SOVt Yu.M., rod.1 ROZOT, L.K., takhn, red,
[Design of city garages] Proektirovanie gorodBkikh garazhei. Lenin-
gradp Goos izd-vo lit-ry po atroit.p arkhit. i stroit. materialam
1961. 183 P. (Garages) (MM -141101
KRIVTSGV, K.S.
Krlyteov, KI-S. and Rabinovich, D.L. ftLabor shifts In the Leningrad population,u
Sbornik materealov no kommunal, khoz-vu, No. 5, 1948, p. 62-73
SO: U-2888, Letbpis Zhurnallnykh Statey, No. 1. 1949
\,XRIVTSUV, U,
Regulation of wages and production potontilile. Sots. trud 6
no. 1174-79 Ja 161. (MIRA 14:1)
(White Russia--Wage payment systems)
(White Ruesia--Induntrial management)
:CHI V.j KRIVTSOVp N.1 ROZHINI P
. I
Use, labor intensity indices as
in an enterprise. Sots. trud 8
(Labor productivity)
plannin work
F 163. IMMA 16:2)
management)
IMIVTSOV, U.N., inshener; GOLIIIBZM, A.E., inzhener.
Reconstruction of a boiler's rear and. Inergetik 1 no-3:11-13 Ag 153-
(PT-RA 6:8 )
(Steam toilers)
- h'RIVTSOV,_ N.N., in-ib.; .-jJC-AL, A.U., in-.,14., red.
(Fandbook on the ropair of ty)iler equip-,ont)
po ro::.ontu kotollnogo oborudovanlia. 2.) nlach. dol). I
izinonannou lzd. Moakva I
., Enorgila, 1964. 211. p.
(MIRA 18: 3)
XRIVTSOV, N.V., ROSOLOVSKIT, V.Ta., ZINOVSTRV,-A.A~
Integral beats of solution of parchlorto acid* Zhur. neorg. kh1m.
3 no.4:772-77)+ Ap 160. (MIRA 13:7)
1. Institut obahchey i neorganicheakoy khImil im. M.So Kurnakova
Akademli nauk SSSR*
(Parcbloric IL31A) (Eleat of solution)
ROSOLOVEKIr, V. Ta.; KRIVTSOV, N.V.. ZINOVIYZT, A-A.
Integral heats of solution of perchlor1c aub
Wride and of Its
mixtures with perchloric acid in water at 25 , Zhure neorge
khis. 5 no.4:778-781 Ap 160. (MIRA 13:7)
1 Institut obahchey I neorganicheekay WAL Im. B.3. lurnakova
;~ademil nauk SSBR-
(Chlorine oxide) (Perchloric acid)
(Beat of solution)
2 2 0 D
S/041901/005/007/016/043/XX
B004/B060
AUTHORS# ZinoV'yqvf A* A.,
TITLEs Anhydrous Lead Perchlorate
PERIODICALs Zhurnal neorganicheskoy khImii, 1960, Vol- 5, No. 7,
pp. 1416 - 1422
TEXT; The authors proceed from a paper by A. L. Chaney and Ch. Mann
(Ref.3). While these researchers succeeded in synthesizing anhydrous lead
perchlorate, analyses have shown that their preparation was contaminated
by products of thermal decomposition. The authorn of the present article
succeeded in avoiding thermal decomposition by allowing the Perchlorate to
re-crystalliae in 7% perchloric acid 8 be filtered off in dry nitrogen,
and to be dehydrated gradually from ;00t to 200-2200C at 2-4 ma RZ. The
grayimetric analysis yielded 50-98% Pb, 48-89% Cl, the theoretical content
being 51.02% Pbs 48.90 Cl. The specific gravity d25.was 4.84,10.02,
0 4
solution heat at 25 C, and dilution 1 1 2500 was found to have a value of
(1-04510.010)kcal/mole. The thermographic curve was taken by N.S.Kurnakov's
Card 1/4
86459
Anhydrous Lead Perchlorate V078/60/005/007/016/043/XX
B004/BO60
pyrometer (Fig.1). Three end8thermic effects (228, 280, 290 0C) and two
exothermic effects (360, 400 0 were observed. The compound melts at
280 0C. Fig.2 shows that endothermic effects appear both in the heating and
in the cooling curves. PbO and PbC12 were found in 0 2 and Cl. gases as
residues of thermal decomposition. The effect at.2280 C is interpreted as
phase transformation, but requires further studies. At 290 - 300 0 , an
overlapping occurs between the endothermic effect or melting and the
exothermic effect of oxygen separation, Decomposition setting in violently
at 360 0C is sharply decelerated at 580 C. Xt this atage, half of the
separable oxygen is liberated. The authors assume a formation of the com-
al
pound Pb \Clo 4 or PbO(ClO 4)2' Intensive 0 2 liberation was again observed at
0 4'
400 C, the residue consisting of 91 PbO and 91A PbCl 2' The difference
,V
between the isotherms of oxygen separation rate at 380 0 and 420 0C, an
shown in Fig.5 ' goints to a complicated process. All of the oxygen is
liberated at 420 C. There are 5 figures and 8 referencest I 'Soviet, I US,
Card 2/4
Anhyctroufj Lead Perchlorate
86V9
5/078/60/005/007/016/043/YX
B004/BO60
5 German, and 1 French.
ASSOCIATIONs'Institut obshchey'i noorganicheakoy khimii im. H.S.Kurnakova
Akademii'nauk SSSR, La'boralvoriy'a neorganicheskogo sinteza
(Institute of General and Inorganic Chemistry imeni
N. S. Kurnakov of the Academy of Sciences LrBSR, Laboratory
of Inorganic Synthesis)
SUBMITTEDt April 8, 1959
Card 3/4
valhl
0
4 1/$,
I I
.AV
X-
701-
It -
so. ,
$0 .
a -
29 - I
A
d
I
Fig-5: Isotherms of oxygen separation rate.
V169
S/078/60/005/007/016/043/XX
B004/BO60
Card 4/4
#0
LUZHORSo
TITLEs
FERIODICALt
L- 14463
8/078J63/008/001/019/026
B124/Bie6
Krivtdov, N. V., Zinov'yev, A. A.
Melting-point diagrams In the systems LIC110 - CS(Clo and
RaCIO - Ca(Clo 4 4)2
4 4
Zhurnal neorganicheakoy khimii, Y. B# no. 1, 19639 W - 191
TEXTj The visual polythermal method using the Xurnakov pyrometer and the
thermographic method using a device whose principle has been described by
1. A. Zakharova et al. (Zh. neorgan. khimii, 5, 914 (1960)) were used for
determining the melting-point curves. A chromel-alumel thermocouple with
a millivolt ammeter was used for temperature measurement. Lithium per-
ohlorate shows no polymorphous phase transitiong melta, without decomposi-
tion, at 249~t2ft and decomposes quickly at about 470OC- In the ca-Se of
sodium perchlorate, the polymorphous transition takes place at 3080C1 its
melting point,with partial decomposition occurring, lies at 482140C and
the temperature of its quick decomposition at about 5700C. calcium per-
chlorate shows two endothermal effects (at 342 and 4060C) and one exothermal
one (at 4650C), the first two being traced back to transitions in the solid
state and the third to thermal decomposition. The melting-point curve of
Card 1/3
S/078/63/008/00i/019/026
Melting-point diagrams ... B124/B186
the system lithium perchlorate calcium perchlorate shows two transition
points and transition levels at 342 and 4060C, corresponding to the poly---
morphous transition of the latterl the polymorphism of the mixtures is-
proved by the fact that the intensity of the heat effects at 342 and 060c
rises with the content of calcium perchlorate in the mixture. The melting
point of the eutectic mixture containing 76.9 equ.-~ L12(C'04)2 and 23-1
equ.-% Ca(dio 4)2 is 2280C. Decomposition sets in above.37000. In the
system sodium perohlorate - calcium perchlorate decomposition occurs at
3800c; the eutectic mixture composed of 44.9 equ.-~ Na2(C'04)2 and 55-1 eqp'_~
Ca(Clo 4)2 melts at 2930C. In the range with high sodium perchlorate con-
tent, two solid solutions with an eutectic point at 2700C were found for a
composition of about 29 equ.-% Na2(C'04)2 and 71 equ--% Ca(Cl04)2' The
following solid phases can be present in the system sodium perchlorate
calcium perchlorates (1) )r..Ca(CIO 4)2 above 4o6ocl(2) P-Ca(CIO 4)2 between
342 and 4060C, (3) a-Ca(ClO 4)2 below 3420C, (4) solid solution at on the
basis of sodium perohlorate and (5) solid solution ct4 on the basis of
Card 2/3
5/07 63/006/001/019/026
Molting-point diagrams**# B124YB186
sodium perohlorate. There are 4 figures and 4 tables* The English-
language referenoo iet M, M. Markowitz et &I, J. Phya. Cheat 65t 261
(1961).
ISSOCIATIONt Inatitut obahchey i neorguniohookoy khinii in. N. S. Xurnakove
Akadexii nauk SSSR (institute of general and Inoirganio
Chemistry imeni N. S. Kurnakov of the ko&domy of Soiences
USSR)
SUBMITTEDo March 20, 1962
Card 3/3
KRIVTSOVp NoVo; ZINUVIYEVp A.A,
Fusibi2lty in the oystem LiCIO4 - NaCIO,47 Ca(CI04)2 -
Zbur. neorg. khim. 8 no,lls2589-2592 N 163,
(MIRA 17:1)
1. Institut obahchey i neorganichaakoy khimii imeni N.S.
Kurnakova AN SSSR.
I
KRIUS-OVIi N.V.; TITOVA, K.V.j R LOVSKIY, VJa.
Enthalpy of the formatiort of guanidinium perchlorate, nitrate,
a-ad sulfate, Zhur. neorg. khIz. 10 no.2s4%-457 F 163.
(MIRA 18-.11)
1. In3titut obshchey I neorganicheskoy khiaii Imeni Kurnakova
AN SSSR, laboratoriya okisliteley. Submitted Febr. 29, 1964.
AUTHORS: Krivtsov, P. I. . and Korobov, V. V. 72-2-5/10
TITLE i Mvanced "rience for All 01asa Futortas (Pbro&vpy t)pyt~!Ij~jk
vao ntokultio7e nvody)-
PERIODICAL* Steklo i Keramika, 1957, Vol. 14), No. 2, pp 21-22
ABSTIRACT: An account is given of a norm of 500 hours for continuous operation
of the machines at the Bytoahevsk r1ass factor-I being increased without
deterioration of product. It is computed that the interruptions at the
end of each 500-hour peri9d cut down the production for the total of
the machims by 1703000 m4 in the course of a )ear. Longer continuous
operation of the machines tends to cause devitrification, Innovators
successfully experimented with increasing the continuous operation to
1,500 or 2,000 hours, at ti-e same tim increasing the content of
ammonium oxide for the oxidation of the calcium, establishing the
following percentages: SiO2, 72,1; A1203, 1.8; Fe203i 0.15; CaO, 6,8
Card 112
Advanced Experience for All Glass Factories 72-2-5/10
Mzo) 3.81 Na20 Plus K20, 15.0; SO, 0.35. Explanation is given of
other reasuras taken, such as a careful rej;ulation of the anount
of mterial put into the bath at a tire, control of the heat factors,
etc, ne weight of the plato- r~lass uas brought down by 2.5%. The
various rwasures taken increased the econouV and produW~veness
of operations enormously.
ASSOCIATIONi
PRESEUMD BY:
SUBMTTEDs
AVAIIABLEt Library of Congress
Card 2/2
AID P - 2076
Subject USSR/Electricity
Card 1/1 Pub. 26 - 18/29
Author : Krivtoov, P. T., Eng.
Title : Machine tool for cold bending pipes without sand filling
Periodical: Elek. sta., 4, 47-48, Ap 1955
Abstract The article describes in detail a new machine tool used
to bend pipes at a construction project. A diagram is
presented.
Iniititution: None
Submitted : No date