SCIENTIFIC ABSTRACT PIVOVAR, N. G. - PIVOVAROV, G. Y.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001341120008-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 99
• Document Creation Date: January 3, 2017
• Document Release Date: August 1, 2000
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

30V/21- 58-? -1 1,12e
Determination of the Limits of a Submerged Surface Jump Alth a --urface-
Ground Structure of the Flow
ASSOC I ATION -
PRESENTED:
SUBMITTED:
NOTE:
the submerged surface jump with
of flow ' regimelV'';, depending
overflow toe, the height of the
features of the flow. There are
references.
a Burface-ground structure
on the dimensions of the
dam, and the hydraulic
3 grapvs and !-' --',oviet
Institut t7idrologii i ridrotekinniki AN UkrSSR Institute
of flydrology and qydraulic Engineering of the AS Vkr-SR,
By Member of the AS UkrSSR, G I Sukhomel
March 15, 1057
appearing
transliteration
Russian title and Russian names of individuals and inst,-
in this article have been used in the
tutions
Card 212

1 -14 - I Q ; 7 - 10 - 11 o00
Translation from: Referativnyy zhurnal, Mekhanika, 19-,7. Nr i0, P ~'Fi USSR)
AUTHOR: Pivovar, N, 0.
T IT LE: Calculation Methcd for the Reinforcement of the B,,,,t )ms Beh~rid
Spillway Dams (Sposob rascheta krepleniva dna za
plotinami)
PERIODICAL: Izv. In-ta gidrol. i gidrotekhn. AN UkSSR, lq~6. Vol 14 (21),
pp 23-36
ABSTRACT: In the opinion of the Author, the prini. ipal ford e ALt~ng on large
reinforcing plates laid on a reverse filter (e.g., for spillwa%
apron plates) is the lifting pressure under the plate caused b,,-
the pressure difference. The effect of pressure pulsations ~s
not accounted for by the A., although, according to data frorr
many investigators, the pressure pulsations have a considerable
magnitude. Data on the velocities prevailing near the bottom
.and the pressure drop within the junction zone of the upper and
lower water levels are studied in order to determine 'he tvpe
and dimensions of the bottom reinforcement required behind the
Card 1 2 spillways. The velocity prevailing near the bottom is. h%

124 - 191,7- 1 () -I I t~oo
Calculation Method for !he Re,nf or( ement of the Bottoms (i ont. )
definition, measured at a le%el of _' perr ent of the height of 11.t
dam. The pressure drop is the difference between the pres, re
in the surface section to be reinforced and the pressure pre-.i:r;jZ
in the tailwater basin. In order to obtain these data, the A, pc !--
formed laboratory experiments on the hydrauli( s (if the taikkalut
basin underneath a spillway dam, assurning the probIrtit fi, hr tA.''
dimensional and using the values: F - 16 - 6,' related it) thc i tmi-
pressed section, and R - 10,000 - 70,000. The experimental data
obtained by measuring the boundaries of the junction-zone regirnen,
the velocities near the bottom, and the pressures, are redu( ed lu
a dam height of I m according to the rules of gravitationa, s,n-,~-
larity and their relationships are presented in a graph. Us~r.w
these relationships, it is possible, in a given case. to pro%;cle ca!'k
lations, based on the given parameter, as follows: The junction of
the headwater and the tailwater and diagrams for the bottom-le%el
velocities, as well as for the pressure drops in the submerged
jump zone. The paper provides a method and calculation procedure
for the reinforcement of the tailwater bottom by solid concrete
plates as well as by perforated concrete plates for drainage, or
by a method of gravel coverage.
Card 2,12 N. A. Preobrazhensl~-.-,

SHVETS, G.I. [Shvets'. H.I.J; ZILIBM. H.S.; KOBERNIX, S.G. [Lobernft. S.H.J;
OLNININ, A.Ta. 1011inyk. O.IA.J;-PIVOVAR, N.G. [Pyvovar, N.H.];
aOZOVSKIT, I.L. [Rozovalicyi, H.T.: DIIXOVhTIT,
M.N. (DidkovelkyiO M.K.J. kand.takhn.nauk, otv.red.; ULNUTSM', Sh.G.
11rentsell. Sh.H.J. red.-leksikograf; SHIKAN, Y.L.. red.lzd-va;
WNIT, R.O.. tekhn.red.
[Russion-Ukrainian hydraulic-engineering dictionary; I)UUU termaj
Ruseko-ukrainakii gidrotakhnichaskil slaver'. 1)000 terminov. Kiev,
lad-vo Akad.nAuk U-SM, 1960. XIV, 192 p. (KIAA 1):?)
(Hydraulic engineering--Dictionaries)
(Russian Ihnguags--Dictionaries--Ukrolnian)

PIVOVARP N.G. LFYvovart H.H.Jv kand.tekhn.nauk
--- IT-
Calculation of relationships for determining the pressure on the
bottom in the section of head and WI water conjugation below
low-head gate daws in the presence of a dentated a ill on the
apron and a deepened pavement at its end. Vistl lwt.gidrol.i
gidrAN URSR 18&19-23 161. (MIRA 15:3)
(spillwaye)

SWICS caM
AMORE MWM Atj~ 97
ON* Mne 0
n=1 yadww for Mechanical t"Und of sawles at high t"Weratures. Cuss 420,
No* 1755bB
SOMIs Isobretudyap pagahlowvyu obrastay, tovanWyo wis1tis no. 3v 1966# 80-ft
TOPIC TAGSs test ebamber.'446operature *a* MAUL4JI QAWP-1141 ;16&1~
ABS'n=Tt This Autbor Certificate, presents a machine for nischmical testing of
samples at high tuqmmtv"so The wachine contains a heating drdoe In the fom
of a closod ob~U with a cylindrical scroan as the heating *low* noubLed in the
sheU, The angle In noutted Inside the heating elements wd the speco Wtvom the
@hen mid screen Is M244 with a coolant (see Fig* I)* To contimmely raintaln,
the heating procese ower long tine periods (on the order of 50 000 bours)p the
heating elawat In In sectimw assembled an folding panels which cool the screens
Inh notion Is vqpUW fm an Independent trmdainwe
UM 1 6M.172

Met IL d1walo
'm cme
MW DAM
Lc.-w 2,&
F190 owtions;
PIP!,
2 iml&t~d trwafonwo.
oil

-i-ne - on,
-i I it , is -4c t or,
I oriti.l v I Ist -) f u9 3' it n Acc.,j. 1,F) J -I
,TnCl

PIVOVAR, S.G. LPyvovar, S.11.). lnzti.-mnkhanik
- Now flax tbreshing machiner7. Mekh.911.boop. 8 no.9:29-31
s 159. (MIRA 13:1)
(11&x prnamoming maebinary) (Threshing machinan)

BCINDARBNXO. M.G. [Bondarenko, N.H.]; VOROKHMSKIT, V.I. [Torone2halkyl.
V.I.J; KITATTGRYA. Z.P.; KOVAL'. N.H.; KOLODA. V.D.; KORSUOV,
0.0.; EMINSEATA. Te.D. [Krewinska. B.Dj- KUKTA. G.M. [Kulrta. H.N.J.
lush.-mekhes.; FIVQYAR. S.G. (Pivover. S.R.): SOLOVIT, V.I.; OLRFI-
RMMO. 0.A. [Olefireako. H.A.). red.; GUMMO, 0.1. (Hulanko, 0.1.1,
takhn.red.
(Now agricniltural mchines) Novi sillslkohoopodarolki anshyni.
Kyiv, Dersh.vyd-vo mil'o'kohospoderalkot lit-ry URS, 1959. 231 P.
(MIRA 13: 4)
(Agricliltural unchinery)

PIVOVAJ%. S. G.
USSI( (600)
Harvesting Machinery
Mechanization of hemp harvest and threshing. Dost sellkh)z- no 9. 195".
Nontlill List of Russian Accessions, Library of CorigreFF, December 1952. Unclassified.

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and t
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-716 IDR)dmwn
'~e~fiitancos at. higb terapomtures
t
e me"Uremen bigh eloctrical
99 67: and ID8. -MgO..- The PrOBOnCe
dUplayed by SaMPJSS~ COjAAlW
resistance Was ng
Cd ferric O)dda de"eued the tm6,&-.of.thefiiateriian..-.TbdJngiienc6,iDfLpOrO,�i Cm
ty
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tiplo of
fst,AbU,lzed
T6!1;~j _60:ed
J'
~Z

PIVOVAROV A.
Good machines for agriculture. P-567
SOTSIALISTLIK POLLUMAJANDUS. Tallinn, Estonia. Vol. 14, no. 12, June 1959
honthly List of East &mvpean Accessions (KEAI), LC. Vol. 8, No. 9, September 1959
Uncl.

KOIWIKOT. A.G.; FIVOVARDT. A.A.
Calculation of the autumnal cooling of water reservoirs. Dokl.AN SM
93 no.6:1015-1018 D 153. (NUA 6:12)
1. Fisicheskiy fakulltst Moskovskogo gooudarelvounogo univermiteta.
Predstayleno aim"alkou T.T.8huleykin.
(Vater-storage)

PITOYAROT.A.A.
-t
Detiorminatinn of the coefficient of this turl*ilent vertical
temperattiro distribution In the ocean. Trudy 14OZ 11:94-101
154. (KLRA 8:6)
(ocean temperature)

P I YOV ftHuy
Comvntatior. -f w1riter t-~-e raturp meA f I rat irni; I r. w, I - r
rpserv-~- I r a . Dck , . ^,~ ~- no ,- : Y 1, :.~ -, - )
I . K o a k ov ski y go 9 1) da r6 t von nyy un I v F4 r f; I t e t I m. M, V . to mo n 0 s n v a .
Predetavlone akademikom V.Yu.ShmldtDm.
k He oervo Ire) (Lakas- Temperatures)

IDLISNIMT. A,0.; -PIVWABDV, A,A,
Calculation of boat balance and Its Individual components according to
the atmospheric temperature. Trudy NDI 6:10?-119 155. (KEaA 9: 6)
(Atmospheric temperature)

I=, of tho
a 111111111b
**6ratun,
i1aft 088. our
r:60, *be rmd'tbnwa cbmmterimitics
to" ewe mlWo
'-I& AIL'_ ~_.L-
~ 'q
sf-tbe diUy-,
of a so by the total
ct~"
'Wivilftti4m. of
-W fratwo
OrU 4"
IV-4iriatims of the -air,
tskI4

KOLMIKOW. A.G.;PIVOVAROV, A.A.
Method of calculating soil temperature on the basis of a given
state of atimospheric twporature. Temt.Noek.un. 10 no.8:59-65
Ag '55- (KLBA 9:1)
IJ&(90m f I elki morya.
(Soil tomperstur*) (Atmospheric temperature)

ROLISNIZOV, A.G.; PIVOTAROT, A.A.,
I
ftasibility of using air te"rature am a baste for Cosiputiag the
resulting heat balance an a reservoir surface. ltv.Al SM.Ser.
geofts. so-5:534-540 W '56. (NWA 9:8)
1. Moskovskly gooud&r$tvonD7 univereltet twat N.V. Lownemova.
(Meteorology, Mart ti~ (Atmospheric Saimperatwv)

S1 124 ^C, /OCK,
AOO 5/AOC I
Translation from, Referativnyy zhurrial, MekhanlKa, 1q60, No. b, p. I i
AUTHORSi Kolesnikov, A,G.j Pivovarov, A.A.
T ITLE: On the Correlation Between the Coeff iclpnts of njrbu!prics~ vid _Heo
Exchange in the Atmospheric Layor Near the Sea Surfa-e
11.7-
PERIODICALt Tr. Mgrsh- zidrofiz- in-t . AN SSSR, 1958, Vol. 13, pp. 0~--L
TEXT: The author considers two methods for determining the turbulent heit
current through the sea surface. In the first variant, the heat current Is ad plp~
In the formt
- ) - t2 (h, _: )j
e - Emo'pe(rit(Oure at the sea surface is the temperature r~-f '~he a.~
where tj Is thQ te : t2
at the altitude h, Is the heat exchange coefficient. In the second
it Is assumed C,92 (k at 2 1
2 d:z j Z=O
where c2, Y2 are the heat capacity a-nd density of the air, Is the
coefficient. The two methods mentioned are -ompare,l with ".ach other wit.h r--j-
C&rd J/ 2

S/ 1 ~?4 /60 /()0(, Ir)(, 4
A005/AOO I
On the Correlation Between the Coefficients of* Turbulence and Beat. F-xchang,-
the Atmospheric Layer Near the Sea Surface
to their consequences for the seh temperaturu profile. In the first.
the temperature is calculated from t.hp heat conductanne equation with +.h,
stant coefficient under the condition ~f h-at. eq,ill1hrium at the boundary
time-dependent course of the radilali.,e toalaz)ce and ,.hp evaporal,P)n heal --Ir-
assumed to be prescribed). In the se-ond var litnl., 1_r.P equatl')r, of` *.? e
heat conductance In the air (with ar. able reef f i -., ont I s used ft-i i, T :
which Is solved for a prescribed c,,uriie ~lf th- ,~,np-r,iturp ~o Ine all - 3,j-
The comparison of the solut',--ris shows that. these may be Iderill al, w~,.~. -i
approximation, If the heal exchange ?oeff iclent /, is expressed proper-'y UL,'
the parameters of the turbulence coefficient Y.2(z). In the _~, imT .1 o-,; f r,'is,,, ~t F.,
that a laminar boundary layer does not exist, such an expression haF Th.-
., 2~
C4 P ( K) - __T
ln(h/z,,) 1n [(k,, + ,iK.__
Under consideration of a laminar sublayer, the value .-.I somewhat ~i-
A.S. Mnniri
Translator's note: This Is the I`ull translation of' the oriFinal
Card 212

P- -1 %~ f f 3, A.,
,rU=; XLI, A

-4

S~t- ri I
CW-', D-t-,

C=Mkstwol, v -3

:arma

r

;-p-t

A. F.

Lrlz-$n.. A. 1 1.

LL3r! VL3C~, V.e

.*
tb. 6~r ~f A
z7:
.

3. tiroo
20334
S/18 60/000/006/007/011
B 101 YB204
AUTHORS: Pivovarov, A. A., Lavorko, V. S.
TITLE: Vertical attenuation of solar radiation In the seas
PERIOM CAL: Vostnik Moskovskogo universiteta. Seriya 3. fizlka,
astronomiya, no. 6, 1960, 59-63
TEXT: A report I@ given on measurements of the solar radiation penetrat-
ing to various depths of the sea, which were made on the research vessel
"Hookovskiy univeraltet" in Summer and Fall of 1959 in the Black Sea.
As a measuring device a thermoelectric pyranometer system Yu. D.
Yenishevskiy in a water-tight cover, which was connected with a
(GSA-1) galvanometer by means of a flexible line. The hor,rontal position
of the pyranometer was warranted by loading It with appropriate weights.
At the "me time, the incident and the reflected radiation were measured
by means of an albedometer A table gives the measured values, which
were obtained on October 18-;q, 1959 on the Caucasan coast, 8 m,..'es from
the shore under a cloudleen sky, and a calm atmospherel the sea was
C
78 a deep, and the sun's altitude 30-37 From theaquation for the
Card 1/4

20334
Vertical attenuation of S/%8/60/000/006/007/'O"
BIOI/B204
radiation I reaching the depth z, which was suggested by A. G. Kolesn,.kov:
exp(-O.z) (1) (lm - intensity of the m-section of the spectrum,
M.1
Om . absorption coefficient) the empirical equation:
12 - Io[O.23exP(-27s) + 0.20exp(-2.35z) #- 0.57exp(-0.50z), (2) was de-
rived. The values calculated by means of this eque i are &.9o given in
the table. The following attenuation coefficients vu_ found: for
-1 -1
1 - 7 m depth 0.32 m 1 for 0.2 - 1 m depth 0.46 m , and for the
upper 20 cm 2.2 m-1 Fig. 2 gives measured results obtained on August
13-159 1959 In the shallow north-western part of the Black Sea; 33 m,
and on August 26-27, in the deeper part (depth 100 m), sun'a altitude
greater than 400. The attenuation coefficients were 0.20 m-1 in -0 m
depth in shallow water, and 0.16 m-1 in deep water. These data show
ood agreement with the measurements carried out by S. G. Boguslavskiy
also In the Black Sea). Mention is made of analogous measurements
l
Card 2/4

20334
Vertical attenuation of ... S/188/60/000/006/007/01-,
B101/B204
carried out by P. P. Kuzlmin in the Kandalakshakiy Bay of the White Sea,
and by T. V. Kirillova and R. F. Byurig in the Sevan Sea. There are
2 figures, I table, and 4 Soviet-bloc references;
ASSOCIATION:
SUBMITTED:
Moskovskiy gosudarstvennyy universitet, Kafedra fiziki
morya i vod sushi (Moscow State University, Department
of Physics of Sea and Inland Waters)
April 23, 11060
141
Legend to rig. 2:
o - Mean values
August 14-15, 19591
& - Mean values August
27, 1959
Card 3/4

Vertical attenuation of
3ma4emse 103
20334
S/18 60/000/006/0C7/01'
B 10 1 Y204
L rjiomia uwepemiA a m
4 ABTS 0,0 ~ 0,2 0.4 0.6 O'B 1.0 1, 5 1 2.0 2,5 3,014.015,01 6 0 7 0
18 X 59 r.
1000 639 582 618 479 441 383 1311 272:2341 16q 130 93 70

19 X 59 r. 000
' 639 590 532 481 44o 3r,6 3 15
, 265 2261 160 129; 92 -
3cptAwe:
no
""'
X
009
662
584
525
411
371)
1
7
3
7C
nw 1 . 44, 31 0
2 2
2 72
, 27 94
'
no Nsmepnm-
1000
639
584
525 480 44 374 3
3 268 0 1 1
16 0
2 X
~
1 1 23
1 4 , 3
9
Legend to the table:
1~ Date; 2) Depth of measurement, m;
3 Mean value: a) calculated,
b measured.
Card 4/4
14

3/050/61/000/001/009/',j67
.3. 00 VY, ey B01 2/B058
.,~ a 1- 2)
AUTHORSs Pivovarov, A. A., -avorko, V. S.
,ITLEz The Diurnal Course of the Solar Raliation Components t.nd
T
the Albedo of the Sea
PERI'DICAUt Meteorologiya i gilr loglya, 1961, No. 1, p~-- 45-46
TEM D~ur i ng the 1'459 expedition on the vessel "Moskovskiy Universitet",
the authors continuously recorded the incident total radiation and the
radiation reflected by the qea surface. Thermoelectric pyranometers ~system
by Yu. D. Yan;chevqFiy), w!.i--h vere connected to a three-point recording
galvanometer _' were usel us radiation receivers. The galvanometer
was mounted on a 7ardanic saspension, specially built for the purpose at
the masterskiye fizicheskogo ftikullteta MGU (Workshops of the Phys,cs
Branch of MGU). The absolute gradaation of the pyranometers was made at
the Karadagskaya aktinometrizhe3Kaya observatoriya, (Karadag Actinometric
Observatory). The observations nade in August and October of lqc~q with
cloudless sky in the open part )f the Black Sea under various wave condi-
Card 1,'4
88349

7he Diurnal fours,, of t?.e --olar '050/61/ODO/JO1/O.-,:,/O~7
7omponents anI tte A7 B0121BG~38
tions were made use of in t:.is 3tudy. The )L)servRtions of the diurnal
course of the incident total raliation over the sea showed that it is
symmetric as referred to the noon time. The data obtained zere used to
check the formulas for calc,;Iating the diurnal course of total radiation
according to the sun's altitile with cloulleSs sky. The formula by
M. Ye. Berlyand (Ref. 1) selertcl for the purpoje is similar to the formula
by Kastrov and may be written iown as formula (1):
IC 0 .9 1 nr. ID / (3in f)
hS ig the gur.'.q alti i.(,, s0th( solar cnnstant. Th(: results of the check
showel w),,i j!' f -, r-r. ~ . ~t 111) with the observation data. Accorling
to the o~,serviiti,~r,3 made hy ti,.c u~thors, the diurnal course of total
radiation. at a sun's a-Iti ,~Je r t jepends linearly on t~-e
sun's -he e juation I3--att /I dir
1 FA.,j 4 1 . 01 - 1X T~ h coall tie fo;nd for the dependence
of the relattun I scattered/ 'direct ~n the ounlo altitude at altitudes of
Card 2/4

The Diurnal Course of the Solar :iadintion J,105o/61//joo/U'. i, Ju~), 007
Components and the Alteio, of the Sea BL'12/"BO58
0
from 10 to 40 , h beine expresned in raJians and the relntioL dir
in .'~. "his formula is similar to formila (4)
1
A 6. 9t. 1 exp ~O
k 2
ottained for the dependence of the to*al-raliation sea albedo on tree sjnls
al ti t Ae. The 2urve 7alc,~.a ted f rom, tni s f-.rm~ia is compared .qi t!_ na t
obtainel from the formula by K. Ya. Kondrat'yev and L. A. Kudr~av-sf,va
("Ref. 4) for the lepenience of tne total-radi-,tion sea albedo or, '..-.e sun's
altit-_ide with clo.A.ess sky and smooth water surface. The cz)mpars3n snows
that the total-radia~ion sea allbelo mair.1-y Je,ends on the m3ve.-.e:- *. Df the
waves. The Bea albed.- for scattered ra,, ,hti3n and smooth water s-i:-face was
calc lated by using tne formula by Kondrat'yev and Kuiryavtseva as wel: as
the ratao of dire7t, to scattereJ solar radiation over the sea. he calcla
tion results s.,.owel that the sea albedo for scattered radiL~tion depends
very little or. ')ie sin's altitude. In the lrasis of the vinaljsis z~f ex-
perimental material it car, be assimei that :.e total raJiatio:~ 3ver the
'arl 3, 4

883L9
The Diurnal ~'ourse of trie Solar '-,ad i -iti )n S; j 9 J/ 6 1 /C ~,0/30 1 ; 0 ~` 5/0C
Components and tne Albelo of tte z;ea B_ 1 17/Bc_~a
sea wi t~ clo,;i1e:is sky is a ' it.ear f-r-tct-n of *hc- sun's ftltitude in tLe
rang(- of the 9,,;n ' s a! ti tAes from t,) ~00. Tnis rel -ition is expressed t v
formi;a (2 Start ~ ng from f formula also ~ro--Iaces good agree-
ment wi tr. tte ~serva ti on data. a'. bed,~ f--r tne totai radi~tlon car, be
calcuiatei from fcrm,,a (4) at wavt,.g _f frm 2 t~: 4 points. There are
3 fig-ires and 4 Soviet referen-es.
'ard 4A

PIVOVARff, A.A.
I
Iffect of solar radimUce pmetrating the sea an the matar
twWw*ture. Okamologlia 3 no.2013-218 163. (KMA 16:(,)
1. Moakovakiy gomWarstvenr*7 udivernitet imeni liox*mova.
(Ocean to"rature)

ANUIMOVA, Ye.P.; PIVOVABOV, A.A.; OBANISA, N.A.
D"endence of the parameter of tfe r-Lgtness cf
-wind speed. Izv. AN SSSR. IlIz. atm. i ckewia I
165.
trie sea -,- r-
no.10:1 11' ~' -. I -,'
im:,,l .~-
i. Moskovskiy gosud&rstvvTuiyy Universitet.

ACC NRt Ai't,O 3 36 14 SOURCE CODE: UR/0188/661000/004/0009/0014
AUTI(OR: Pivovarov, A. A.
ORG: Chair of Physics of the Sea and Inland Waterways , Moscow StAte University
(Kafedre fiziki morya i vod Gushi Moskovskogo gosudar5tvennogo universiteta)
TITLE: Prediction of the mean vertical subglacial water temperature in circulating
bodies of water
SOURCE: Moscow. Universitot. Vearnik. seriya iii. ritiks. astronomiya, no. 4, 1966,
9-14
TOPIC TAGS: Laplace transform, waterway engineering, inland waterway, izr1z=d_-water-
&7=tr=spo. ration, ice , temperature control , f low temperattne measurenmnt , boundary
layer temperature, long range weather forecasting
ABSTRACT: The thermal balance for the ice formation period in a circulating body of
water is discussed since not much research has been done in this direction. The prob-I
lem is complicated by the phase transformations that take place in ice and in water.
A consideration of the heat exchange between the water and the atmosphere through a
snow-ice layer must be combined with an analysis of the heat transfer in the water-
-waterbed system. In the suggested model for the vertical determination of the sub-
glacial temperature, a water basin of limited depth (h) is considered; the coordinate
UDC: 551.48 j 53.5
Cord 1/3

ACC NR% AP6033814
origin is at the surface of the water-ice boundary. The x-axis is positive in t-le
dirvction of the flow, the s-axis is positive in a vertical direction, dcwn fr_'Dr ~`.e
bottom side of the ice layer. All values relatinr to water are denoted ~n, ir.~~ex 1;
values relating to the waterbed are denoted by index 2. Assuming that the heat pro-
pagation in the vertical and in the horizontal planes is by turbulent exchange and
flow, respectively, the water temperature field can be defined by the equation
at, ()f, all q1
4, ril - -
ft oj ot ";' ,
where q, is the thermal discharge per tiniT volume on account of the dissipa~ :on of
the flow energy and of other sources-, cl P, are tr)e calorific capacity and density of
water, respectively; k1 is the coe.ficient of turbulent heat exchange; ul is t1he speed
of flow. With certain boundary coi,ditions and assumptions regarding the ver-~ical -,em-
perature distribution and the water temperature in the headwaters, a generalized solu-
tion of the problem is obtained using a Laplace transfoan. The equation of thermal
conductivity of the bed in the form
k,
is used to determine the therml flow from the bed, considering that it has two com-
ponents: one reflects the effects of the initial therinal reserve in the bed at the
2/3

ACC NR# AP6034011 SOURCE CODE: UR/0213/66/006/005/0881/0885
AUTHORi Voskanyan, A. G.; Pivovarov, A.-A.; Khundzhua, G. G.
ORG: Physics Department, Moscow State University in. M.,B-. Losonosov (Moskovskly
y'- f aku
gosudaretvennyy universitet. Fizicheski I'tet)
TITLE: Direct recording of water-temperature gradients in the sea
R tA
SOURCE: Okeanologiya. v. 6, no. 5, 1966, 881-885
TOPIC TAGS: oceanographic equipment, oceanographic instrument, sea water, resistance
thermometer, pressure gage,
temperature measurement
ABSTRACT: The authors describe a newly developed unit for the direct and continuous
recording of water-temper t dients in t e sea to a depth of 250 m. The unit
_q ure gra
utilizes standard IS-264AYplatinum resistance~thermometers and provides continuous
recording of temperature differences accurate to OAR G the 5-25C range with a
simultaneous depth record accurate to 1%. The shipboard recording equipment consistai
of two EPP-09K3 recordingl~otentiometers connected to the submerged instrument package
by an RShM multicore cable. The instrument is powered by 220-volt, 50-cycle, a-c
current. An overall circuit diagram is shown in Fig. 1. The temperature sensors
(RI, R2, R3, R.4) make up opposite arms of the measurement bridge and form a single
system consisting of two paired sensor sets (see Fig. 2). The depth sensor consists
of a diaphragm manovieter with potentiometric output% Various other aspects of the
cord 1/3 UDCt 551.46.087

FAkCNR,- AP-66-346-fl-
I
C
50
IPPO
A4~w
I
j J:-2 1 -r 7 X I I I
~ig- I. Circuit diagram of ten- Fig. 2. Paired temperature sensor
perature-wasur nt system.
circuitry,' design, and determination of the instrument's basic parameters are re-
Card 213

ACC NRI AP6034011
viewed. For measurement, the paired sensors are mounted in a special holder on a
I-m-long rod attached to the instrument-package casing. The temperature sensors may
be moved along the rod, thus changing the measurement base between them, and the
pressure sensor is located on the top of the casing. The reconmended descent rate
for the package is 0.5 a/sec or less. Thorough testing and analysis of obtained
results have demonstrated the unit's reliability and effectiveness in studying the
structure of temperature fields in the sea. Orig. art. hast 3 formulas and 3
figures.
SUB CODE: 08. 09, 14/ SUBM DATE: none/ ORIG REFI 001/ OTH REF: 001/ j.-IZ -.Z:);
ATD PRESSi 5100

I II
PIVOVAROV, A.A.; ANI~',MOVA, Ye.P.; YERIKOVA, A.N.
Murnal varia~'on of albedo and f;( lar rndint ion perietrat ~nw ', -,
sm. lzv. AN SSSP.. Flz. atm. I okeana I no.'Illzl2lt-le,, N It 1.
' NI; 11
-A
1. Moskovskly gosudfirstvenn-y univers!tAt. Sul~ri'ted Jan,,,-!-Y
15, 1965.

4" N13 A"028362
own com. uR/o362/65/001/on/1216/121-)
14 . ") ~
AMON: N erlkgs~
. 1-1 --. 0 1
nag dyygWy (Noskovskly gosudarstyeaVy universitat)
Mar'- Diunial veto or the Aumo =d the penetration of Solar radiation into 994,
water,
MR. Isv"t1ya. Mika staurtry I ok*ana, Y. 1, no. n, 1965, 1216-
2M0 TM-. albedo, solar radiation, therwelectric pyranowter, total radiation
ANNAMt Us albeft and the solar radiation which penetrated Into the Black Bea
Am We Javestipted in July and August 1964, using the research veattL Nin
unoureants were mad* vith therwelectric pyrananettre susp-en- ded on 1
be" oil awters fr= the vessel and three mters above the water's surface. The
1W
6
teW, radlaUm Uwwasaw rapidly 0.2 caljc~a'mdn when the height or the iis to
10* to 1.4 with the height at 600. Tfie reflected radiation emnsts,'to,
O.Ot e&1100M~ and-dwages slightly when the height of the sun I* more than 261P.
TM albodrot the surface of the sea cowed ty the total radistlowunder a cloudless'
~41W, Is detendiset by = aWrIcal formula,, which Is represented graphically In the
orloisial,article. A special formas, to given for the total incl6wt solar radiation

ACC H16
APS028362
..

-
aMrated Into the voter In com
re
VUeb Ww
Mot wMah the M&r
uted
this is
p
gW
r"est" grigmeaUY In the orlOnal article. ;.
p
p
Orls. srt,. Me: 2 ngures and 11

WSW/ Olda W: '004/ M
~#.
.

AN IS! WVP 0 Ye P. ; I'llWN A RO 70 4# A*, kand. f 1, z. -nut tem. nAtl~
f-alrlilntion of the coofflelents o' thp vertIcal
exchange of hPat in seas und re norwr_irs. Meteor. ', r! dr- ~ -
no.2 133-38 F 166. fm" I ~r)- '.
1. Moskovskly gow,daretvannyy universitet. Subm',11od Mnrvl-. 6,
1964.

KOLSSNINOT, A,G.,. PIVOTAROT, A.A.
Calculating the rate Of 00-07fng of reservoirs In fall. Test. Kosk. un.
Ser. mt. mekh., astron., fit., khim. 11 no.2:47-52 "A.(KIRA 10-12)
1. Wedra fi2tki morya I Yod sushi NoskovskW goeudaretyennogo unt-
vartiteta.
(Reservoirs)

V/
in"Irv.04.
gig vo-HIJ.-If
.-Ion S C u
-.0 oil 8.41 1 8~& i
-0
EV,
I SP
0
909 00 p.131819
it's
,a win
Vill
V-5
Bill'
v -3 J,
Ing
till' '18 ja
410 v Vill
43

DRYUM, A.M., laureat Stalinskoy premil, lashener, GAMBURG, Yq.Tu., in-
sh*ner, retsensent; GOIDYKIN. M.K., Inshener. retsensent; X&U=V, A.A.,
kandidat tekhnicheakikh amuk, retsensent, EMU. 1.N., JDto*nt, kandi-
dat tokhnichookikh nauk. retsensent.- UWNOV, A.A., inshen*r, retsensent;
SAMOV, X.N., laurisat Stalinskoy prenii. Inshenier. rets*ns*nt; CM-
NTSOV, T.B., inshener, reteensent.- VALMV. G.A., inshener, retsensent;
NXTUS, N.A. laureat Stalinskoy premii. inzhener, rete9usent; XOVI-
KOV. V.A., dotsent, retsensent. PIVOVAROV, A.L.. imshener. risteensent;
POGODIN. A.M.. Inshener, reteensent. UOIJUROV. L.R., Inshemer, retsen-
sent; PIVOYAROV, A.L., inihener, reteenzent, POGODIN, A.M., inshener,
rates ; "RWIPT L.R.. inshener, reteensent; SHUPWV, V.I., kan-
didat tokhnicheakikh amuk, retsensont. XLTKOV, A.F., inshener, retmen-
sent; TUN(S. D.M., tekhnicheekly redaktor, VULHA, G.P.. takhnicheskiy
redaIrtor.
[Technical handbook for railroad son] Tekhalcheakii spravochnik sh*-
lesnodoroshnike. Vol. 8. (Signaling. central control, block syst,su, and
communication] Signallsataiis, teentralisatelia, blokirofta. avian'.
Red. kolleglia A.F.Bar&nov Ci dr.] Glav.red. 1.7.kidoi. Hooky&, Go&.
tr*Asp. shel-dor. isd-vo. 1952. 975 P. (CArd 2) (MIRA 8:2)
(Rallroada-Sigualing) (Failroade-Comminication systene)

RARANOV. A.7., rodaktor; BIZYMIN, D.D., r*daktor ' VAKOIN, W.I.. otvetstven-
nyy rodaktor tow professor, doktor takhnichaskikh nauk; VXMISOV, B.S.,
redaktor; IVLfflY, I.V., rodaktor.- "HCWK, I.D.. r*dmktor.- RUDDY, To.?.,
glarnyy red1aktor; SOROLInKIT, Ta.l.. rodaktor; SOWOUBOV. V.V., reduktor;
GHIUVSKIT, V.A.. rodsktor. ALMOV, A.A., inshonor; AUGHKIN, B.T.. in-
&honer, "AIM ITIV, To.T.. loureat Stallaskoy promil, Inshoner, BILUKO,
I.M.. doveent-t BORISOV, D.P., dotsent, kandidat tokhnichoaklich nauk;
ZHILITSOV, P.N.. Inshener, ZBAIL, N.H., inshoner; ILIT=ZDV, V.I.. dotmont,
kandidat tiekhnichoskikh nauk-, KAZ&KOV. A.A., kandidat tokhniohookikh n&uk;
KRATZM. L.P.. kandidat tokhnichemkikh naak, KOTLYARMO, N.Y., dotsent,
kandidat tiekhnichookikh nank; MAYSHEV, F.V.. professor, kandidat tokh-
nichoskikh nauk; WARKOV, N.V., inshonor; 5118PRS, V.S., dotsiont, kandl-
dat tokhnichookikh nauk; NOVIKOV, V.A., dotsent; OMMV. 5.A., Inshenisr;
PIMV, I.I., kandidat tokimicbeekikh nauk, PIVIE0. G.N., Inshener; PO-
GODIN. A.K.. inshoner; NAMAIJ, P.N., dotsent, kandidat t*khniehookikh
nauk; ROGINSM, T.N., kandidat tokhnicheakikh nauk; RTAIANTBIV, B.S.,
lauroat Stalinskoy pr*uil, doteent. kandidat takhnichookikh nauk;
SNAMMIT. A.A., Inxhoner; TU'DMN, A.B., inthener; SHASTIN, V.A.,
laureat Stalinakoy promil, Inshoner SHUR, B.I., iashener- GOICKUKOV,
V.I., Inshoner, roteensent; NOVIKOV: V.A., dots*nt, reteensent; Alk-
NAX'T1V, To.T.. laureat SW Inskoy promil, reteensent;
(Technical handbook for railroad men] Takhalchookil opravochalk sheles-
rLodorothnika. Vol. 8. (Signaling, central control. block systes, and
covmnication] Signalisatatia, toontralizatolia, blokirovta, evias'.
Red. kolleglia A.P.Baranov Cl dr.] Glav.rtd. Z.F.Budoi. Noskya, Gas.
transp. thol-dor. Izd-vo, 1952. 975 p. (Continued on next card)

PITOTARDT A.M., detsent, kandidat flaiko-catemUcheskikh mauk.
Calculation of the shearing force in beading fr**ly supported
plates with siagle- and double-connected are" . Trudy XXI
se.17:102-111 155. (MLRA 9t7)
1.Wodra tooreticheskey viekhaalki.
(31&stlc plate* &&d shells)

Conentradona of shearing stresses
t orsion of ldsMMkmdL. Akad. Nauk SSSR. Prilt'
Mat. Meh. 17, 253-259 (IM). (Russian)
IMbeiiiiatima Reviews The investigated priernatic rods are subject to pure tor-

10
14 NO
Val sion and their crowsections are indented by redntrant angk-s
.
. with sharp vertices. The choice of the torsion (unction de-
WW- 1953 pends on the point where the stress is to be determined It
the contour of the crow-section has no angles with sharp
vertices, or if the point is distant (rom those vertices, the
nuthor refers to a previous (unavailable) paper [Akad.
lqauk &SSR. Infenernyl Sbornik 15 (1953)] and to M C.
(Akad. Nauk SSSR. Prikl. Mat. Nleh. 15,
245-250 (19SI); these Rev. 13, 288] Where tile CODVenical
f unctions are listed.
In this work the author uses the method of finite chilet-
ences to construct a stress function, which would deternuut
the stresses in the neighbourhood of Ehatp vertices, wheie
the concentration of stresses is unusually great, Assuming
that the cross-section is Bymmmetrical and the axis of bN m -
metry is through the vertex of an angle, the author dvrivv,
general expressions for the stresses near the verte), lie
illustrates his theory on three examples with the foflo-,N;uwg
cross-sections: (a) a square with a cut, where the angle Ah 0',
M an angular bar (the crose-section compos"I of two
rectangles at a right angle); (c) a sector of a circle. The
stiesses near the vertex are tabulated and graphet].
T. Le3er (Lexington, Ky.)

FIVOTAROV, AeM. (Moscow)
.WW"vImWWq"W
Deteralmstlon of tangential stresses in torsion of prismatic bar@ and
of the beading mosient of freely resting plate*. Insh.abor. 15:61-72 153.
(Nuu 7: 1 )
(Strains and stresses)

PITOYAROV, A. W.
Ilasticity and Plasticity, Plans and Spatial Problems of the Theory of Elasticity. (1698)
Inshener"y 3boralk, Vol 15, 1953. pp 61-714?
MoxQue ".
scalmlatlon of Tangential Stresses In the Twisting of Prismatic Rods and Shearing Porces
In the Banding of freely Supported Plates.'
No 0. Slobodyanskly's proposed method (Prikladnaya Hatematike I Kekhanika, Vol 15, No 2,
1951, pp 245-250) of calculating derivatives of unknown functions In the solution of
problems by mans of finite dIfferenees is used for the calculation of tangential stresses
14 the twisting of prismatic rods and shearing forces in the banding of freely supported
Plates.
SO: ReferatIvW Zhurnal-Kekhanika, No 1, Jan 1954; SO: 30785, 28 July 1954~
(v- I

1
0o
7

dm* ftwodsd !Aga RUPAMI

A looi*W MWXk%_lt"~ jj
Ot 4 1XIMA
--W 4414

Aj (2) ar;
li tiftl vnot 6i
'
Tiw
UAU vii)- drooltv MA A%Ilk rtsi4wftllkA~, "tj,
*4 4w-, ow iwA. Affm "'Wilk

I . . . . . . . . .

7.
9. Monthly List of Russian Accessions. Library of Congress. 1953. Unclassified.

V t~-V f~ Alu,4, A. M.
USSR/katboviaties - Strains
Mar/Apr 53
DConceetration of Tangential Stresses During Twisting of Prismatic FAds,9
A. M. ftwovarev, Moscow
mat i CK~
~ ~V_
17m Me 2o pp 253-259
1~ F1
D46_~,_O~ Odes"
not omcnMw66~s in the ewe where the cross-sectional profile
of the zmAq contains inemiag angles (i.e. cross sections in the sbape of cross,
elbow, Indented rectangle, etc.). Constructs grapbs describing the tangential
strosses near these angles equal to 0 and 900. Cition his related work, *Deter-
ailastiam of Tmogential Stresses During Twisting of Prismatic Rods and of the
Cross-cutting force Dwring Banding of a Freely Posting Platepa Inabenomw
Sboxvift, Val 15v 1953-

, . - . A I I
, I . .,. .
.. . I ~ .
I . . I
I . i
-. --- - % ~ u a ;j - ~f ~ - ~ k
I Tc -

Wei
&a haial
JV 9
it its #90"
doomy llm~ #01;111 (in RUNSiOA). T?WT
102-111, 19w Ref. i'A Mt"- no. ti. 1914S, Rev. 7713.
The tnTCSttg&(1)r. it b&kCd W the CCRUItf Of M. G. SlObOdygnakY
Wr(4 Att;;. A1*&A 15, no. 2. 1 M 11. antif La Its first pUt, drallal
with singly Itaked pla-es, to Identical with (he authat'o preceding
pape-C JR&J. Zk Mvkb~ 19S4, Rev, 16% 1. The tienimse Miet an
the periphery Is detertolned by the equation
LO ff C'T~ P
W

Simitafteougly, V 0, and 00 the Perip"CY

fl
and a + I -nambm*f p3lAts eqtddlamm fmm tht CturelpoWnS
miles Of the PD461y' k Or, - - - - anjo, ftmard by the rAdil
drawn Imm any point in the rtSion C to, the sfafts%ld pMrAs# with
The internal nomals to thr, Pv,-1Ph*ry IA these Pal'"S.
Y.211

j'~
4

A' P A
n f t'- I~o~. nj- for be n
cf t.- In-ncary
2,, v 7-.z r n a a o . 4 , I n 6 26
a '-'s tract "'.'r. ir- ta", 1 ')5" 32
B- intr.-):!uct- on sp~!c'~i: i-rx4Ta' parts of t~~e lr,:~n
f r, c e 0`1 1 '~ M i :3rC e 0 t'-.;? CC;"~ I aj r,
s c! or., a - n8 3 i,,If." P r
t,! -:-a' n oundary va
for t'-Ie are determ'.ned by a
dirfert~nce mf~t-.od, a net wit, i -o-,.gh step width is use,:.
Tho autncr considers nuzerical 4~xampies frr a semicircular and a
triani,-ular e~,uilFltpra, plate which 13 SLbLect to a uniformly
distrib,ated streas.
Abstracter's note : C~,mTlete translation.
Card 1/1

PIVOVAROV, A.N. (Moskva)
Representation of real numbers by a system of ring counLers witt.
pairwise mutually prime numbers of digits. Izv. AN SSSR. 'ekh.
k1b. no.0101-106 Jl-Ag '65. (MIRA 19ill)

.:-, ~, , M. YR . ; IT I',. K, I.-
f A . S- . ; S ~- . : I '% , IN . 7 . ; I ', -I'( I ~ ; 1,; ' , . . .1, .
~Ilomm . r t) ems 0 '1" f! re p.-P-,er. !. ' -r. '.:~ *-r~s, e,-. I,#- !-; ! , t.'-? , . '. V 7 - J~
Ir"ll'FIL" loil. i,C,7.11. he 7 Op. 11 r ... : , -,-( 31 J- I . .. . .. . 11 .

L 19313-6j RDS ASD/AFFTC Pi-4
ACCE33ION NR: AR3005872 S/0271/63/000/007/3044/30"
SOURCE-3: RZh. AvtomatikR, tolomakhanika J Nry*ch1i3lito11nnyi tokhnika, Abs. ? 13227
A'JTITOR: Pivovnrov, A. S.
TIME: A.Ralse generator with fixed frequencies
CITED SOUR'CE: Avtoratika I priborostr. ',',auchno-tekhn. sb., no. 3, 1962, 53-55
MP'AC pulse generator, fixed frequency, computer component
TPANST-ATION: This fixed frequency pulse generator can be used for adjustin7 ele-
rents and units of electronic di,7.1tal conputers and also as a generator of ~i.-.:Lng
pulses in different conputin- machines. The generator has the following charac-
teristico: the amplitude Of pulses of volta7e with negative polarity is 9 v; t1he
range of fi:md frequencies for tracking pulses 0.5 to 5.0 mc; the pulse duration at
all frequencies 80 nanoseconds; the temperature range 0 to 400C. The V-enerator
consists of 'Lhc following units which are listed. The master generator has a cir-
cuit wit-h delayed positive feedback. A self-oscillating mode with a period deter-
mined essentially by a delay line is set up in the generator; changes in the delay
ti:-.e make it po3sible to rezulate the frequency of the generator. Am er-itter
Card 1112

IQ313-
ACMSI,O'~' !,R: A-R30053,72
follower which 3erves as a buffer 3taFe for matching the high output impedan,~o of
the master Fenerator with the low input impedance of the shaping stage. 'A. 'I-he
s~-.arln:- st-a-,c i:-, intended to shape p%xlses of the sane given duration at all Cra-
quer.cies. it is a 3eries oscll-latin-. circuit which satisfies the condition
""u, in > T-,, , , t It-.c*rcforo its paramoier3 arc worIked out so that T 4tu,inl 7:ien
t-".e Input gi,-nal sho-j-1d bo reL-arded as a voltage drop and there will be aperiodiz
circuit R ). 2p N"JL7, at the same time wo obtain a
sh:lr-i r-d7o anplitude and "noise" Is 7-inimal in the period between
711-e +.2-~o inplifier input in accorr-':in,-,-?
o-,,tvjt. !he t-a-.-;'Lc~rner is made of a ferrite
If turn.-, and w2 = 8 turns. 'Ibe output
accordir~ to *~-.e -IIa7r-am of Uhf- anitter follower. In
cn fre-quenc-le- )f 50' and 750 kc and on 1, Z, 4,
-77 2, 1.4, 1, 0.5, 0.25, and 0.2 microseconds
:'--lector "or tl,e final s+V17c of 2n v ma-:Lmm, the
S. 7here wore tvo I--i!!trationo, and also two
referen-c:-.
DA M- A " ~ : 1 ".A S:? CrTS: 1E, CP ENCLs 00
Cord 2/2

P:','OVAI-OV A 7 P. N
Croi no r rip,' ~i
S'~' t1a ',& ~ 0 g
:-nt Re
, !3 p Ov
,~ 6 Mft 2,1 T17" 4
A , my 5

PIVOVAROV, A.S. -
Fixed-frequency pulse generator. Artm.i prib. no.3:53-55
JI-3 162-. (MIRA 16:2)
1. VychislitelInyy tsentr AN UkrSSR.
(Oscilli~tbrs, Elec tron- tube)

'A41 1;6~1*ujvk U
8/0065/65/00P/008/0050/00n
4-Piv6varov 16J-X&
A*
O"t a Control of product Vil"Ovity
BMW
mase -.no~ 3 1065 SO42
tekbw~ogiya jcPUV;.J
-cofitro sma
-automatIM h tical -modal -
_qrqmy affiliat NrPi., "meftakhima"omot,' has used the Groz.
The ny
simplli-g-sirstenz -for- this automatic
P loum~institvts im~iir~ 0 eve a
can 1-6f the production concentrate 'entering the,viscosimeter. A reliable con
:'0UuOus:-IndGx'6f:thG viscosity of the~concentrats obtained has thus been achieved.
Relationships bartween the ~vlscoslty and the-parameters.of the main process were
determinedo' -rrom these data a model of the process was compiled on the EMU-10
--eleictronic analog computer-and several modifications of the control system were
alternately, hwestizated. After confiming the-reliability and quality of these.
the beat variation Vas solected and tbs. optimal adjustments for it.
Were simultaneously determined* From this variation the apparatus of the MAUS
systim- vat - seleated and later - was installed ~ in a plant where it:Amderwent indus-
trw: til" Thi $"too abosen for automatio'.control of the viscosity consists
-7
)A- 0

KOZLOV, M.V.; PIVOVAROV, A.T.; MINIKOVSKIY, Ya.I.; OPRISHRO, A.A.
Au toma t, - c ~,r, tro ' of* tr.i. - . r -u -a '~ I nr, c. f r, tip. a J .h *.h ! v!~ - .
10ilm. i Lekh. top]. '. riia.,P, 4 Ap
(MIRA 1 ':-,
~. Gr,3znensk-'y f~!,al fJau,t,.nc~-1,Fsi(-doN,atc-ilskogo ~ jr,,.vej,.,-nOL7(
~nstltuta pc, komplexrnoy avt,,rw,!izjAtqi, proizvodstvannylkl,
p-otsessov v neftyanoy i kt,IILI( :f-!4koy ;,,-orVvhlennwq' '.

KM 7.OV, M.V.; PIVOVAR(V, A.T.; KALiNTTV, H.P.
Alitcmitic conLrc-' of ":f, ~'
tool. i masel 10 Mr 16~. j %4 .
'. Grr,znenskly fiiia- Naijcr,nr-- qF,-.cvateI'r'wg ,, .:
imtituta po komplexsnay avtrmt,. I " ilr si ,vcdE , . - - ~7y~ -i
prol-sE ssov v w Ityancy , kit i-x- ~,,P- ~,.v ~ - cayAti1e 11r, ~ - I .

I :*; VA U_
is .1-
, -ray s~~ectral ana'yal basea on t
I of externai st,&ndard in I
jAcolidary spectra with the absorption characteristica cf samF'es
t,uken into ac,:ount. Zav. lab. 31 no.9zIO81-1084 165. (KRA ,
. Kazakhokly nauchno-1.93ledovatel Iskiy I nstitut mllner-a, 'r,0,-( 3y-lyb -

SIMHENKO, V.V.; PIVCVAROV, A.V.; HUBANOV, I.A.
Single-crystal focuBing ~tort-ave X-ray quantl~met-_r. Prh.
i tekh. eksp. 8 no.4:189-190 :-'-Ag 163. 11 1 ~ ! -I
1. Nauchno-issledovatel'skly inatItut minerallnogo ByrIya
Ministerstva goologil I okhi-FAny nedr KazSSR.

~ . V , - " - Ti C"J ,A. V . , 'n z r .
I . . . - I I , , 4, v L, ~ .
ftr -3 .4 ' ~ r " -,m -,, .: ..~ I . 11 1.- , . n
. k4 - - , - j
. I ~, ,I I I ~ ~ .

ACCESSION I'M: AP4038783
AU711OR: Pivovarov, A.V.
S/0048/64/028/005/0880/0881
Tlil.E: Aoproximate calculation of the integral defining the intensity of X-ray
f iuoresconce in irradiation by a continuous Spectrum /Report, seventh Conference on
X-'Ray Spectroscopy hold in Yerevan 23 Sep to 1 Oct 19637
SOURCE: AN SSSR. Izvestlya. Seriya fizichoskaya, v.28, no.5, 1964, 880-881
TO~IC TAGS: x-ray excitation, fluorescence integral
ABSTRACT: Simplified methods are discussed for evaluating the integral
A.1 ~ ki
P2. X11 + dk,
for the intensity of x-ray fluorescence (M.A.Blokhin. Fizika rentgenovskikh luchey,
Gostekhizdat.M.1957). The number of independent variables is reduced from 3 to 2 by
the substitutions m w %qAo. q* - Al/3 A Numerical computations were performed,
and curves of q0 between 0.1 and 10.0, anod* showing P21 as a function of q* (0 < qs<
Ic 5) for the values 1.5, 2 and 3 of m. Curves are also given showing as f unctions of
Card 1/2

ACCESSION XR: AP4038783
q0 (0 < q* w- 5) the coefficients In the three term Lagrange interpolation formula,
based on the values 0, 1, 1.5, 2 and 3 for a, for P2i as a function of m. The ap-
plication of the curves and the calculation of the parameter X when several fluores-
cent materials are present Is discussed very briefly. Orig.art.has: 3 formulas and
2 figures.
ASSOCIATION: KazakhAkly Institut alneral'nogo sy*r'ya (Kazakh Institute of Mineral
Raw Materials)
SUBMI 00 DATE AOQ: 12Jun64 ENCL: 00
SUB CODE: OP NR REY SOV: 002 OTHER: 000
Card 2/2

PIVOVAPOV, A.V.
Relative Intensity of the t- series line of the X-ray spect:-im
of rare-earth elements. Zav. lah. 29 no.9tlO82 161.
(MIRA 17:1)
1
1. Kazakhskly institut C nerallnogo syr1ya.

mo- F0119/631000/004
cam N Nal.,4P30049 17
A
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vovarov
nja~.:-
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Ste
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smier., "hum
io, the, IOU S elevienti: -'32 Go 37 Rb~--. 40 Zr, 4 Nb.
'malytii6il' Was relabulati d. A
62 Pb i 7 3 Ti j'.90 a e
gram &'collinator-..~r,
rangement ato*r siii4d. OrlX. art. has:.

1~

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PIVOVAROV, A.V., insh.
Signaling and telemetering of voltage and current Und to at
traction substations. Trudy TSNII MPS no.232:21-35 162.
(KIRA 15:9)
(Electric milroads-Current supply)

FIVOTAMY. A.V.; WSKUTOV, D.P.
Use of the "single linem method in plotting the characteristic
curves of photographic emulsions. Zav.lab. 26 no.12:1379 160.
(MMA 13: 12 )
1. lazakhskiy institut minerallnogo syrlyn.
(Photographic emulsions)

F I VCVAJIvV, All I Uert Y&kov~evich; ig
T A .' ','. , E. A. , nauc hr, re,i.
.Design of auxiliary mte,,-ia, :'or w-,cc-
ao king ritlustrien]
So n* r. nhu,, hn,- Iqnl t -t 41- w:

PIVOVAROV, A.Ys.
rping the EVK-~-' ,q Fk pl,:kW of *.Ip numbbr of
Star. i insLr. ')6 n,).t...l .'o li,'. "M:lu ',Pis)

DRANOVSYIY, M.G.; GDRODETSI,IY, Yu.G.-, FIVJV"IrV, A.Ya,
Auto-~-tic duratle feeder for r---e Z*r. p?-3,m. * '. --,. _: I C-- -
F *,(-,
1. ( K-1 :-tA wl. -
I
(Lumt,,,r--DrN irij,) (Wo-xiwor~in;! machinery)

PTVOVAP-V, B.I., Inzh.
Constructing the breakwater of the outer harbor of the iremetchng
Hydroelectric Power Station. Gidr.stroi. 30 no.8:42-43 Ag
160. (MIRA 13-8)
(Breakwater@)
(Kremench~ug Hydroelectric Power Station)

ACC NR, -AT7000191 - ---------SOUR -C9-CODE--UR/0000/64/000/000/0196/0204
AU-IHOR: Volodarskiy, R. F.; P~vovsrov, B. L.
ORG: none
T10,1LE: Some questions of the deep structure Of the earth's crust in Ciscaucasia
SOURCE: Moscow. Universitet. Kafedra geofizicheakikh metodov issledovaniya zemnoy
kory. Geofizicheskiye issledovaniya (Geophysical research), no. 1. Moscow. Izd-vo
Mosk. univ., 1964, 196-204
-+ C'_ ro vk~r_ -,
TOKC TAGS: rearth crust. Mohorovicic discontinuity, earth structure, Conrad dis-
continuity/Ciscaucasus
A3ST RACT: An attempt is made on the basis of analysis of geophysical, chiefiy gravity,
data to map the deep tectonic structure of the central and eastern Giscaucasus. The
presence of two deep density interfaces, the Mohorovicic and the Conrad discontinuities,
is assumed. To compute the depth of the Moho discontinuity, the author use the formula
HM . 15.449 + 1.131 Hc - 0-056 Agr' where Hc is the mean depth of the Conrad dis-
contiauiLy. and Agr are values of the regional gravity field. Construct[on of the
interface was made in two ways: on basis of the Ag" field chart at a
Moho the
height of 30 km from a network of regional profiles and by using Tsuboi's method.
The results obtained are almost identical. The following conclusions are made:
1) regions of increased crustal thickness are characterized by negative gravity
Card 112

ACC NR. -AT7000191-
anomalies; 2) the basic structural elements of Ciscaucasus have a "Caucasus" strike;
and 3) all basic structural eleaents of Ciscaucasus are reflected in the deep
structure of the earth's crust. Orig. art. hasi 2 foraulas and 1 figure.
SUB CODE: 08/ SUBM DAM 05Nov64/ ORIG REFt 008/ OTH REP: 001/
Card

PArMLFYEV, Yu. and PIVOVAROV A I., .
*Navigation and Maneuvers, of the Merchant Marine In Time ~)f o~ar," liava-i
State Transportation Frubilshing iiouse,
I'

smosomm" Over ploommook, st-
1b.
fs~. low 4 g%
.%. wvswd. the ormemy cd 1 prm*"4
t1w *&.Ir madd"hig, *---,d 6v u-Ins loot
.w" to IsIor tow snob" OVA 110M "I-k6md Ow
i bets mv qW.Gd oh. atom-d-
bmwom %,I of..

rrvovktov, Fedor %aaillyovich, zaal. atro-Ael' USSR, brigtidir
karen.7hchikov; C!2-'IL', L.P., red., SInCM111, P.G., tekhr..
red.
(The intel-,r, ted brign(le in construction)Komplekannia brignda nn
stroitellstve. Kharlkov, Kharlkovakoe knizhnoe izd-vo, 1~,62. 14 j.
(MMA 15:12)
(Khnrk,,v -Construction industry)

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- I

ISAKORI140 B.N. ; YAMOVICH, I.A. ; ZUYEV, G.P. ; KRASOV, V.G. ; %IlPJ4OV, V.F. ;
?TVOVAROV, F.Ya.
Klx-emd-metzle apparatus for the e x-tractlon of uranlum and ra-re
astals from aqueous solutions. Atom. energ. 3.2 no.6;503-513 Je 1621.
(MIRA 15:6)
(Extraction apparatuB)

--o ':'r
1'r rc:.- t: i ali
ua-
De
t-t
Ln:; tr In- t c c t"
L t, r L t
V t I-L
r t D- o .'s o - ::n u-
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-- -,-I- , - *-
I I . I .
4 . ~ t ), 4 , ,
4. Tob --co
7. N. D. I-,-4,r v .'olllect~v- Fam . Taba~( I i iw. , , '195.'.
I-Ionthl IIW ' iorary of ong:-~s ; , :.a-ch I. ~'n A , ; ~ .' ',- '.
,y List of Aiii,3'an- I-

FIVOVAROVA, G.N.
Some data on the change in nitrogen metabolism in chi.-ldren and
adolescents vith epilepsy. Vop. paikh. no. 3:303-309 159.
(MIRA 1,3: 10)
(NITWW Kz:TABOLISM) (El"I UPSY)

PrVOVAROV, G.N. (Leningrad)
University of scientific knowledge for teachers. Hat.v shkole
no.6s82 N-D 162. (KRA 16W
laningrad-Teachers, Training of)
Nhthematics-Study and teaching)
~

prVOTAROV, G.N. (Ianingrmd)
Forms for evaluating the ~mowledge of students in mathematics.
Kat.v shkole no.6:14-11 I-D '57 (MIRA 10:11)
(Mathematics--Study and teaching)

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'PITi-E: A I
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PERIuDICAL: R';~ K~, TE
r r-~- i 'ILI [it i t
5
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it! Y, 1 61,
TI.,- c ivr c t r
a nd t) T' T
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31-
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-3 f 1 8 00 t I 5C C I , r 10 1 1, 1 t e s. T~ P v~
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and -):-,t
is showi- -.c,41 v F; ;rc I T'
c),). &.r z c t e r i S " i c s u f
c3n,ecial v:,, ~i.i( j fi I n 1 1 d
unode. s i, i!
Uurve t r(, c,,' i - n- c t,
C,.ir v e 2 is f:):- a mail , ~Lpj eEn- ' Fd c.,t".,
relates to at., xide ct,'_Lode. T ,-. elife testz c
catho:Ies a-a sl~Dvn _n i(i .rf -, v!,ere C-,ir ve 1 c Dr i e s
Lo an ir,T,r(,LntPr., cnLi.:)~'.e, ri,ile ~;urvp __1 is; f:,r an ON-
c~-thode. Tie rc-activ *JDn .1-enomenon it; an
cathode is illustr,~ted by Curves 1 Eind 2 in F1 ki,e 5;
first cuive sl.ovs t1.(, current ch~ractr-ristic aft,i
initial activtiDrj, vl,i-"f- the second curve
t~-.e curient, chF.r&-t,r--:ic ior tLe ser-.e cat~.ode 7- f ti- r
was exposed to I ~ e ac t i , i, of U e atm- sphf, ~ e fo r -I i 1 - I
of 15 days. TIr, c. ~;.,Le :)' tI.e t 'ydroLen x_-~,urr in - -
diffei-ent tI:,7i_~!trDn_L -:-,- a fui.cti--r, _)f tle tl_ t-, --
is shjwzi ,n roz. tiebe, it Ls se,,i :!-'~
Uq T 1?/3 -pressure clzrize -let_ I.,,uib _Didl~r -.1
c,