SCIENTIFIC ABSTRACT VORONKOV, N.I. - VORONKOV, V.V.

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• Collection: Scientific Abstracts
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• Document Release Date: March 20, 2001
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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

GITMAJI, F.M.; SHILO, A.Ye.; GVAYI P.161 4otsent, otv. za v.-fpu.-k
[Experlmntal and theoretical study of two-ol-ajoi pandls for roofs
with proBtressed reinforcement] Experimen~alltio'~teordtichoskoe 9,13,
issledovanie dvAikhslrimYIO'h , panelei dlia perek-~ytiitj o predvaritellno-
napriazhennoi armat,v --. dnepropatrovsk. lnzh6hornc~-stroitellnyk
inatitut. Nauchnoe soobahcbenie, no.45). (WRA 16:8)
(Rainforced concrete conatrucO.on)

AFANASENKOV B.I.; BARTISHEVSKIYj Ye.L.; KOLOMOYTSEV, F.I,*t VOROTIKOV, II.I.,
Aoteent, otv. za vypunk
(Using a water wave nucleus to measure the dieI6~ctria~,dharacterlatica
of liquids] Izmerenie dielektricheakikii kharakt($~rist:Lk malopoternykh
zhidkostei s pomoshchliu volnovodnoi iacheiki.,-~Dnepropetrovsk,
1960. 8 p. (Dnepropetrovsk. Inzhenerno-stroitelinyi,iristitut.
; (MIRA 16:8)
Nauchnoe soobahchenie, no.60). t
1. Zamestitel' direktora. Dnepropetrovskogo, inabbnerno-stroiteltnogo
instituta po nauchnoy rabote (for Voronkov).
(Liquids~-Electric prdp~eirtle,'s)

4 a 41 0 9
ft 1b to is w it 14 Tf a ~m it H -1 IF
v 1.11 u a it
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I i ! ! , I . i Itill 11 1 . . I

VOROT Mr,
BARU, G.O.;BZIZTSE2Y, V.Ya-,'
-IMY, P,G,1MYAJYZ1O#AH.;
~N.Wt-.2
DOMBROVSKIY, G.D,;ZOIOTARET, S. 4-MVIOLMIKO, I.K,;PTATO11OV, P.N.;
Mr-ITT-2Mt A.V,;UGOL1Kj M.F.
t
V. IA- Girahson. Mak.-elev. prom. 23 no.4:23 Ap 115z~. (ML" 10:5)
(Girsheon, Vasilli MovIevich, 1880-1957)

CA
at title 4rontent lot ORY1000 III W414of skiiaplati, M11401
din W Wfus" s of, A, Alv%f:1 -d 11 11
1044*.'N~.. :12, fin I a ~ A aaar -it lite rff#N t ,I ibifetens
Imaidita"s of 41ormigs, 14 water '1111144 all thelf 9 1 couleat-
'11tv chkf ptoblvini invi-Ar"I were thorw. lit whill lite-hervil- ~i
tim, to ovw total whether to %(me fAsalvf" timler at, to I ft xiii.
C-aulilimas. Fur the vxp1l, work water sampfe~ tiett takcn i
from the surface of lbe Neva Rivrr. : Expti. were imide to
'fel. 1) fillal quanu~tv 44 0 offer listmagr 4 tile 'fatuld".
in sirdissary 11"lis atal In lur"amirally
chmisitr In I I r4milvio fit samples #If dlo.K " &ter krlwt lit a he I
Ali fill 1~~aoalh itialvol t M) 4-0, 44 0 In millitivs 14 Ilimid
water fifurnt At Itornro.,inj lentifs. , lit rifailhoriwaa walt Or
temp* ' im mils; (4) Olungr (to 41 co"llent ill Nev.1 Rk~-
ter unipIrs dtirialt idump !a tonpiewr"I aad prr-
condifid" at #it lifie teatim, and lit Im ~211*; O)f in-
mcl, 44". 44 A I'tewiviltive: 41141174 Oullige ill (I flitting
Ourviage .4 "aspre Ill acid mial mfk. at" a. I'lie ( 1
"Cir field. lily the Willilry lacillml.
triell Weft gkor. i-tistraGails. anti ligIL't'. - if W~* I-a-
hUIr,l fhAt I Ir IM-1 .11 1 tIeW *111 liff0c It "'M Of- -Wed
Chat the hp.% of 1) 11.0111 mfors -ilai'lov, I- OV4 1W
k 4111C ill rwilla. till) 141 till- al in
bV lit Ictl -00 NalwIta". L.-r' of 0 lo sh~ Iolt,
mily when 1he Ualujilvif welt *Ifwrl af traipit ~ 114111-1 Oull. ii
lite Irmliq. at vilik-h they writ Nkra. 1twattleirnfoltImi:
sAmplei -Mumlif be stored titulet isli. condilicnis it the 0
cattlent if; to lie tietd. by the WinkIrr fnetfaml. Tables a
data ObtAiried front theve cgills. l4re included
I i3A J, 1p, i I
IL
J

VOROTITKOV, P. P. ---------------------------------------- - ---- ------ --
Bralov, U. S. and Chernovskaya, Ye. N. fl7he baule, of th,
Varuwkoy,
h.vdrochemnical regime of the coastal area of the Barenta Sea In thE)~ J.'Cgi0a CC--Itl'al
n Trudy Murnan. biol. stantsii, Vol. 1, 1941, p. '19-131-31liz
SO: U-3600, 10 JulY 53, (letopis 'Zlhurnal lnykh Statey, ~Io.6, 1949).
i,

USSR /Geopjqs ice Ionic Flaw, 1 Dee 51
Afforestation
.----T-hg Influence of the Afforestxtion of Water-
dhdds on the Magnitude Ionic Flavj- -P.
Taronkov, 0. K. Sokolova, State Aydrol Inst-
lmninc-21. ad
NaIAJ~11 Vo
Ak L~=I, No 4 pp 561-564
ural water flOWiMg.On Earth S 6153~1~a~_Ce'_COn-
-Nkt
Ltain mineral- and organic matter vhose deg of
gru-
._.,.A.U_Tnte ti: if-r _ge , al~-
Y
titles are f6u~d-in'Auspended state,-
in true solns - ate in ionic mol state.-.
Intermediate' :positions are 55SUMed by-inorganic
202T65
WSRI/Geopbysics Ionic Flow I Dec..$3-
..'&fforestation (Contd)
and organic substances dissolved in. vater , in...
tolloidal state. Authors investigated montlily
mda ~Marly'Iquartity of flow 103 /im?), - jorLtc
flow (t/lau2j for toga (forest) and cultivated
1=d, and relation between particle type,
erosion, etc. Submitted by'Acad D.~ S. Belysz-
kin 28 Gep 51.
202T65_
C
t__

maw---
YOROUKOV,P.P., kandidat geograficheakikh nauk
Taske of the hydrometeorolog,tcal service In the f1";1d ofi
hydrochemical work in connection with the Stalin plan for
the transformation of nature. MeteorA gidrol. no 3-?~
F '53. (KM 8:9)
(Water resovces development)
i :1 1:' 11 !JW11,

V_V~ re fo
"'T"drometeorolosic.11 and Condit-iOnn G.,. verninu
the ccc*_Iri~cnce C)f
Of 'Lyi-IZ~' (z, c;f F-4-3' --he R--.i~~n of th-~, Cl;mtrij a _0
7b1
rologiya, No '2,
vilthout der*ring the great inflijerce of tho (1-1.3 ~:e of Wld
charr
waste waters into the Vol.-a an;] its 11-dntartL~ie ai~yr~en ro,rivie, tho iaut.N)v arrives at Vic
conclus-ion that. the sharp deflcienzcy of' ocy~.en in rive- watars,,AAch t7ar cau0c of the
so-callerl dying phenamenon in _21~32_11;4'2 uncLracteriS tic of the Central 76.1-ra, iss -a ra sul t
of 'the extre4me tendencies tor..avil drflq, up under the ccnditions pre-
vailing for the Oka and Kama r-"ver basins durinC the winter and mxtumi7mrnt~-, The par-
iods of dyin.- winters wa,~ concludeJ t,,ot o..:~ a. result of chances 16 the mlicated C~.:rxlltlnns.
The so-called dying 7,-iriter (zamorn~Fj.e zijay~ call be forecasted Jm"aCCONLA,cu, v:it,, tlv~, de-
.-ree and duration of the deviations of the hydroneAeorolo:,ical enladitLon-1: from x1he
for the Cl.-,a and Kainua Ba:3ins. -I- ?j-~, q
jr,f Sr I.
St.1 110v 55,
H :1~ iilfiil~ iii.[111plij 11111!111111

M.,"R IFINIFF-P
U, U
.... .......... ........
!p
VMRONMMV
Basic features in the formation of the behavior:,of the ionic
composition of sm-face water in the steppe and'forest rteppe In
spring. Trudy a4I no.37.44-33 153- 11W,
(Water)
1111 fill
qLE2 1111 MU,
I. Ls S, LIU 1 102
11 11 TIT 1111 M::1 1!, "1111 111111"! 1111
H'AF 1:

'i A
VOROMIOV, P.P.
General features of the behavior of dissolved ox~gsn acA the
photos~ntbesis Process in raservoiri of ~he Tblg;~ O"an. Trmdy
GOI U09*3704-61 153, 11-16)
(Vo3ib-a Vallev-Reservoirs) . (OWgen)~
(Photoe7enthesis)
Rill 111

;001 naak reAttillis cf blopica" c4immimils fn~ f 'p- i-cot il ~;r Ai i d '14
WeW 14:11, t tl~le
-- - -- of tlx6vofj~L ildem, ffs- ciddaed;m Olt t!14L~ vral 9 IN 'i v
-10 f ~ ~ -- i~
dimctif Pt P. Vc .0 deitt
Inif. 1953, R,fezw. 4'~t~ 109~,,ltljm at'llf )FICIlilk V)OIJI
triltiNe-I&OV, VH'l ra , 'in I - i 1, GII:
Me. 83W.-rn order to esciblish the vacrifid nivi " 71"OT'll"
nas cr tt~c Xvibysilev and- Slafin Iftad 1`01117VUEV 1, 11 fifl-cit' MAIrAtC 01' lfl~l TI,IY4Ir'.JiL;t t in wali
imodt ;~f ttllie bljgtnou5 ecainvd.. f ilir 1,waei (61fa w'A flit concit. lit ai!~UnAt IXI!t
Ryt;:xmk micv-ir. Tile vmc~- it cite Y,ilrtt in Ow fe;Ckm pioncto fr-cm 114 trit E113! Ill 111%~ts'crj 41
I,Dj I -d luvwatio~
of Asmakhan cnnmirzc~t Mr--tvich, CA. 45, IP7, '10,910- oft tjj I Lci cill ducly ;I
().Mrng. in the summerartif 0-1f)(Ki Offlr-51li tilt (rir littiftblill U;v 41'
flood pericid; in the "U'rilit'l it 'Untnit-! 114, jildigillij!Jil, t1w, p
, 1. 0
Ilitrat"m/l., in 4tatcr 0.010 mg. ill Vial ftyblus-3: rMirvol: in,, it,, anill,
'Afr
them wuc 0.100 MC, in Itutuntu, ittl 'A-' Itti;td 1:j!;
ltrotopultiot of I- '1141tv 4(f
0.030, in the et" period 0. MO, arad lit v-.191114ir 11.0p.5 rdlhoiljj'l~ the chlorot !t 1! matill
tile c=tC--t "wf nitrates in Vit 1u(LU=-?IFlrCl- ~Crk)o tilt$ >~ '. . '' .,I i, ii
0.100 mg. N/I.; duxLng the spria4- IlLx& al--ulli de~ 'clutir iWalil afilae, lilt 1~ it%pp
4.iver. Ap. trvoi~i-iot 41,
crtavA, =d iti june tcacht.d mrie. Stwiwul vlaitigra iii lite 411,11(l ifill .,wa I
U
nlvxiv~,ti and IS :amjKfs. fivi tio ~, Lit& t ith the ~ in- Air. 'I'lHi uml.-c, c zi 1, lirt-t-hu
&%,dopumif (I The Ml~ttltt j "W1110, 4m the Wi;L ( rP tvld~
0,600-0.020 mg, N/I. to (fit! end cd lit.-: W;-ltlr--Vrxi lit jl-Lqw'&i0)q alkyll. 41"1 tl~ll
rain. during thil. summer. and durbtr ta- lrorfi it Lncxcllr~cd air ~t N,
- L, taul L I V . ,
Si was at a MEX. dLrin t~w! wittior (1,400 r1rJ1.). dar- '"fl,
9 wlicr lit Ole, remxvlm~. .1ifftr9j,
ing tile glowing gellsom tlmve wDs 0.4(0-1.09) Ing. 11;1-5
and during auturrin =d wwti~r i: was ff.CV& ter. Dutiall
but.duriaEgicir-jiumm"it
dca-msed shamlle. Similarly to qitmtti3'~rd 01*30mit0l,
my UU is Vkosli
ne"It d
ill:j 03r it phattjll~~"I(!illl
q.A. I'fie
I'dild by the
iq-i,
1 ImR13 IT to 440 il i isf--
ill ':a;jn wel-alml tiv.
41ptallhaktoli Irrill,
mil7ulvor- fd phlF 11i Iv$-
lm~cllilljlt In ~11~' il'x lit-.
T Mu ultnttel ato plit,
hur'lly t'llittignl. ling
I .. -- II.- - - I-
jI mt nip'llt, mciii
4" tift'M ( -- M'~ , if w'-!o
tilt? t 1"T. v t I
ill - Itc rt.
13111 f4 1111jill- lit It I I
lialfall-twilt !11011111,111111",
Withi INA-2m. Ity-i ,I
lyti'If tilt" l"TIlylit"I 4-.1

VORGICOVO P F .) A14D SCKOaVA., O.K.
"Influence of Afforestation of 71,hters~-eds on tYe Mlne~alizatlon of the
un ~olog,' In-ti,
Water and on the Yagnitude of the Ion R off," Tr. Goo Gid.
No 37 (91)t 91-93, 1953
In the Valday Scientific Research llydrolc--gical Statioh of tho State
11-ydrological Institute, hydrologists have investigated tbe~ rtineraliiation
of the witer flowing off forested and nonforested oblects
onf~rested),
of the observations were tNi T,iyezhnyy (rorested), Usadly67~1 n 0
and Priusadebnyv (nonforested) sitea, and the Arkbiyereyshij, brook. The
total ion runoff from the forested watershed on the averiq6 over, 4 years
amounts to 6.4 mlkn, but from nnforested w-.iters~.eds it is 16.91n/lm. The
mineralization of the witer of foreated vaters~eds for A- yretrs arounts to
45 mg/liter; from ncnforested watera~eds for the sam lenFrtl- cj'Al-me it is
5~1 ng/liter. (RZhGeol, No 1, 1955)

al 1 .1 1 W
1, ,I ILI; I it V
Mill 1101-4 .. ....
lit
TORONMT, P*F*; SCICOLDVAt O.Ke
Itrdrochemicai ch"acteristio of the coloring of Jmrfabe water.
TrUAY GOI uoO*3?t95-,3? 15J.
Nater) (Oolor)

A IN, Oleg Aleksandrovioh; SHATI1,111k, M.G., rodaktor; vu a P.P.,
otv r tchesk
a-O11LB-1-VAn1-Wx _q~*k~,qr ; PIAUM 9 M. Y&. , t a Ichn
(Chemical analysis of Inland vaters-, stu4 under, itatlo6ary
conditions] Xhimichaskii. analls vot sushi; pri stitsioak~rn'ox
1kh Isuchenii, Leningrad, Gidrometeoroloi;icbeakooe'i!liz&~o. 1954.
199 P. (MLRA 8;2)
(Water-Analys is

VORONKOVI, P.P.
Peculiarities in the formtion of the chemical com ~ition of
pop
surface vaters in various geographic zones. Doki.AS.SSSR 94 no.
2:293-296 A 154.
OKUA 7:1)
1. Gosudarstvenny7 gidrologichookiy inatitut. Leninig~aa.
(Water-Analysis) (Elydrolo'gy)
! ;11.A1 IM 'lilt -MI

17
if
Hydrology,
TSM/Miseellansous:
3
22
Card 1/1 Pub. 18/47
,Authors Voronkov, P. P. j
--- ip" th J~rlm~4.'Onl' f"11 .he 1
About--'certain--r~les. it O-CAPO of
Title governfi e A i til
-atriospheric precipita tions-7-7 '7i - - - - - -
-7 Ct Iij, 1'9 5 4'
Periodical Dok. All SSSR .98/5.1 705 68':~ 0
cipit;
0 Oas Wi I
Abstract The chemical composition of at=s 11 er~a
'146,11
southern: ~ re gions- -of the'USiji ~~fa ~.at
river and swamp waters was i!stablishdd. Thel;bA4 H50 I
atmospheric pre cipitatidns-ot' llot~th~~n i ij~ prioilla ~u '10 i i
NaCl part-icles %,hich ~altio s4rve a~s an4iirli'sa4anlhi LeW "11
ions was~detemLned by~the:;iq!~:".reo o~
i'
The laws governing the',formstion~ of 14hdi
outlinedt 'Nelve -U'03a -refelr4nces
+i
il; d
Jnstitution State Hydrological lnstitut~_-~~-IAnink'radll
Pre3ented by: Academician A. G. Betekhtln~'
ia: norl timn land
of CI it)
in
V q;3~ Aor
be t Idma 1e st
3 conta t
P14 30 4
20
i.~n are

VOIIONKOV. Pavel Pavlovich, kandidat gisografichentikh nauk; Z;hYXOV, B.D.
red&rIo?7-T6kTo-r gaograficheskilch nauk, professor; SWILINA,
M.K., radaktor; SOLOYMCHIK, A.A., takhnichasklyL redaktor
(Formation of the chemical cortitution of warface watd~i of steppe
and wooded steppe zones of the Xuropean territories oithe IV.S.S.R.
Formiroyanis khimicheskogo, sostav& poverkhaostm7kh va~ atewl
i lesostepnoi zon Drropeiskol teritorli'SSSR. Pod Hed4if B.Ntalkova.
Leningrad, Gidrometeorologichookoe lzd-v, 1955. 35o pd'~VQU)8:10)
(Watar-Analysis) (Stappes)

AID P - 31S3
Subject s MR/Meteorology
Gard1A Pub. 71-a - 10/23
Author : Voronkov,, F. P.
Title : On using a chemical process to determine the ponte~t of ground-vater
runoff of a river
Periodical t Met. i gidr.,, 5p 40-44, SIO 1955
Ab~tract The author criticizes A. T. Ivanov's method of deteradning the
chemical properties of a river runoff by analizing'only ground:wutors
and surface water without considering the permanent water tablo and
seepage water. Five Russian roferendes.. 19484953~
Institution None
Submitted No date

Im Pill

14-57. -kr2207
-Translation from: Referativnyy zhurnal, Geografiya,~1957, 6o
p 74 (USSR)
AUTHORS: Bogoroditskiy, A., Voronkov, P.P.
TITLE: Surface Waters in Northern ,Kazakhstan (PoXerkhnostnyye
vody Severnogo Kazakhstana, in Kazakhstanj
PERIODICAL: S. kh. Kazakhstana, 1956, Nr 8) Pp 35-37
ABSTRACT: The.GGI,(State Hydrological InstituteY~~expedition to
the Akmolinsk, Kokchetav, and Kustanayidistricts in
the spring of 1955 determined that the~lmineral content
of the waters running throught the network of fine
streamlets on the slopes of water collectors during
spring floods was generally 50 to 150 mg/l. This
means that these slope waters are suit6,ble for drinking,
industry, irrigation, etc. However, the chemical
quality of these waters deteriorates r'eatly as they
run further through the lower parts of.the relief and
Card 1/2
Tj
H F II ~1 i 11 11V
I

-Surface Waters in Northern Kazakhstan (Cont.)
in the valleys of the river system. This is caused by the fact
that chlorides and sulfates, leached out of the ground, have been
accumulating here for centuries. The author makes recommendations
as to where slope water collection areas should be located, and how
to prevent the increase of their salinity,
Card 2/2 G. D.
IM M
I M
.11 i=Mr

I I f. i.
I il , ~ f ,
. ! H ~~l Till! I'l 11111 , 111111 ~!Hl - I ;
: : i I ~: 1, 1 11 ': u "1l W!, TII R11111 1111,11 11111*11:H III
I I : I i i; : j, . -1 1 i

VORONKOV, P.P.
Hydrochemical principles of constructing artificial Uks$ In zones
of insufficient humidity. DALAN SM 111 ao-1~178-181 Insufficient
humidity. DokI.AN SM Ill no-1:178-181 K-M '560 (KLU 10:2)
1, Gosudaretven"y g1drologicheekly instl%ut, .1kepedit"Iya Po Isn-
cheniyu vodnykh resursov tselinnykh 1, salashnftli zemelo. Predstav'-
Isno akademikom N.M.Strkhovym.
(Reservoirs)

-vcRaffov, P.P.
Hydrochemical, description of the main cmt~gorlom:'oF murfpmo watem
-BokLAN GSSR 111 no,2--438-01 N 1560 10:1)
1. Gosudarstvannyy g1drologIcheskly inst!tut.X)3-psd'Us1q,&,po lxucbe-
niyu, vodrVch resursov toolinrqkh i zalashiqL'i vothille Pi.edotavleno
ELIcitdomikom N.M.. Strakhavym.
(Witter supply) Olydrology)
il MJ-1 N,

16A,641;~~ ii In, ,i !,!.I 4U, iii, www""W",
........ ... idly.- ........... .......
15-1957-10-1417'(D
Translation Referativnyy zhurnal, Geologiyap 195T,, Vr~ 3.0.. 1i 130 (USSR)
AUMOR: Voronkov, P, P.
TIM: Development of the Chemical Composition of the ftrfa~e Walers of the
Steppe and Forest-Steppe Zones in the MMpeen Part df the USSR ~
(Formirovaniye Almicheiskogo sootam pov*rkhnos*Lnykh Wjd staphox,i
.2eaoi9t9pno,y-Zon Yevrdpeyskoy territorii SSSR)
ABSTRACT: Bibliographic entry on the author's dissertation for '+Ate degree of'
Doctor of Geographical Sciences,, presented to k1V (Mosoow State
University)., Leningrad 1957,
ASSOCIMON: MGU (Moscav State Ublversilty)., Moscov.

voRoNKaV ) P
AUTHORS: Voronkovo P. P.; Eogoroditskiyj A. P.
T17M General HydrIoebemical Outline of Water Supply Ela'nenU of ArtificUl
Basins of Northern Kazakhstan (Obsbehaya gidrokWaich~ekaya
kharakteristika elementov vodnogo pitaniya iskwstvei2hykh vodo7emmr
lkwernogo Kazakhatana)
MIODICALs Yeteorologiya i Gidrologiya,, 1957., No. 2j pp, .16-43 (-VOS.S.R,)
ABSTRACT: The article presents hydrocherdeal data to be c~nsidetred in selecting
sites for reservoirs to be used as water supply;for industrial and
public consumption, In plam3ing ponds., excavations sites
sbov1d be chosen at such e1evations to excludethe admission of
highly mineralized ground waters and lessen effect of alluvial
soil levels,
The basic factors affecting the chemical quality of water accumaLiting
in reservoirs are: 1) mineralization and chemical composition of
waters of various origin which supply artificial basins: a. soil-
surface., b, soil-underground and a, undergroutid watems; 2) pro-
portionate amounts of these waters entering within IL-Ked periods;
Card 1/4

of Artificial Basins of Northern Kazakhstan
3) evaporation from area of the surface and the'precir.Atation falling
on it; and 4) quantitative outline of water us6~And losses to in-
filtration.
Of these factors,, 1)a. is most importantj tbesell~are witers occurring
durin spring flood stage and for average reser.yoirs.~(2000 - 8000
671;3 comprise 70 - 80% of azmual runoff,, and ICO% Xor smaller
onw, Water basins of the European part of the;' U*S*PR, are
characterized by having a soil-underground lsye-~ salIWLfied by
soluble compounds, mostly chlorides. The author coadudes that
the higher the artificial basin is situated with reference to the
salinified part of the talueg, the greater the possibUlty of
accumulating good quality water in the basin.
Personalities cited by the author are: P, Fliv oronkov (2)., for h:Ls*
paper on chemical composition of s=face vatel-11 of the steppe and
forest-steppe zones of the European sector of,th'.
I U&SISORI; K* PO
Voskresenskiy (3), for his hydrological calcul4tiondfor planning
works on small rivers., streams., and temporary irater c9urses. There
are 2 figures: 7ig, 1 indicates, general outline of vineralization in
milligrams per liter and composition of chief anions' (% equiv.) of'
Card ~/4

General Hydrochemical Outline of Water Supply Ejpnentgq
of Artificial Basins-of Northern Kazakh~tan
riverbed waters during the spring high water period f*L- small and
medium water basins (observations pointV are pijajoinU4 with solid
black dots; various bachurings are used for varid~us %,~.ontents of
HCOi and Cel). Fig. 2 portrays the sama., but for micro-stream waters
swipled on slopes of water basins during the spring high water period.
Only the % of HMJ is depicted in the 3 tYPes ofhach~'xing, The
regions included in the figures are Nuatanay, Wkchetav,, and Akmolinsk,
drained by such streams at, the-Tobol., Avat,, Ullkayak,.Sary-Turgayj
Ubagan., Ia)3imj Chaglinka., Ifura., and Selety,
There are four equations developed by thr autbor, An explanation of Eq, (1)
my serve to clarify Eqs. 2., 3,, and 4. 9q. M:
MK A w B
C - D
in which A jH + M + M V
-MH V 31 Jtt;
B -M V~jo+ 0, V
C
C a +YjP+ Voc
r, -VIICI)+Vjio + 8-5VCT*
Card 3/4

I r L T
General Wrochemical Outline of ii ~rSv~pply E~lawntr-,-
of Artificial Baaim of Northern Kazakhstan
In the last mentioned equalities,, MR and VH repr4sent,zineralization
and volume of water of the reservoir at the begic'ming iof tbe
calculation period; M)7p., Vnp stand for the mean!colloidal minerali-
zation of the inflax and its volume,, HA and Vj? Up the .,man Minerali-
zation of the ice and volume of water forming as~result of thawing.,
'I ti0fii VICT U the
Vvo is volume of water being expended ill ice form
runoff amount. VOC. is the volume of precipitation falling on the
reservoir surface., and Vgr,7 is the amount of evaporation.
There are references, all of which are Slavicil~
ASSMIATIONt
FEMUM BY:
StIBMr=s
AWLABLE:
Card 4/4

aatures in the fornxtion of chemical co"'mition of water in
artificial bodies of water and calculation of t6ir mi~~srmllzatlozi.
Trudy Iab. ozeroved. 7.;121-128 158. (MIRA 11:10)
l,Gosud,arutvemWF gidroluglebookly- Institut Glalvzogo "Vleniya
Gidrometeorol ogicheskoy slushby BSSR,
Mrdrolov)

-4CC NR' AT6035249 SOURCE CODE: UR/318616610001137/058/0124
AUTHOR: _V~p~qp~oV, Pj_j~,_(Professor; Doctor of geographlepal aatOnces);
Sokolova, 0. K.
ORG: none
TITLE Formation of the chemical composition of local run-,,od wilters
SOURCE: Leningrad. Gosudarstvcnnyy gidrologicheakiy Inst[tut. Trudy, no. 1371#~
1966. Formirovaniye khimicheskogo sostava vod mestnogo sf.oka (Formation. of the
chemical composition of local runoff), 58-124
TOPIC TAGS: water, chemical composition, surface'~vater,`;underground water,
organic chemical, soil chemical
ABSTRACT: On the basis of hydrochemical observations made duping expeditions
repeated over a number of years, the conditions of organic slibstances dissolved in
local run-off waters in Northern Kazakhstan and the Altay tableland -As examined.
The principal characteristics ofthe quantity and quality of tiie:se substances in
waters of different origin are given: atmospheric waters, waf~er discharged by
rivulets along mountain slopes, and river water collected in smalLcatchment
1/2
Card

&L. NK, AT6035249
basins. The latter are examined as waters forming the com~ositi6r, of organic
substances disst.-Ived in the various thicknesses of soil mate0al d~'iring discharge
into river bed systems during the principal hydrological periods. The wealth of
data accumulated makes it possible to include in the article ;~8~ome:discussion
pertaining to the origin and transformation of organic substanc es dissolved in
natural'Waters. The text includes 7 maps of the area. Ori'~. art has: 15 figures
.9
[GC]:
and 19 tables.
SUB CODE: 07, 08, 20/ SUBM DATE: none/ ORIG REF: ~,,0,08/
2/2

J~
! , ~ '! ~: ;, ! 1 1 11
I 111 i ii 1' 1: i 11111! " llii~! 111111. [ ~,:il 111,11,11 Ill - 1111,111"IF, I ~'
.. : 1, 1 :1 ; i I . : 4
i ~ I I i I i , T ; .1 i I

1111 lid:
., ij
I
I

VORONKOVI P.P.
Regularties In the process of the forzation and:ywnUg of the
chemical composition of siaters from local runof?. T~udy GGI.
no.102:Z3-U9 163. (MA 16:8)
(Water-Compoeition):
it

VORONKOV, P.P.
Formation of the chemical composition of atmospheric waters and
the effect of it on uoil solutions and waters 6om slopes. Trudy
GGI no.102:7-42 163. (KMA 16,.8)
(Precipitation (Meteorology)-Co~position)

VORONKOV P.P.
Basic factors and regularities in the for-mation of the chemical
composition of water in small reservoirs. Tru4 GGI'. no.102s
120-135 163, (HIRA 16t;3)
(Water--Composition)
1h ii IiH; I

VCRONKCVF,POP B A, V.I.
Content of nutrimnts for plants combining nitrogen, phosphorus,
and iron in waters of various origin a Tr~* G61, no. 102 t 13&168
163. (KRA 1618)
(Water--Composit-lon) (Plants--Nutrition)

42396 1/
8/089/62/0113/00VO03/011
B102/BIOP~":
AUTHORZ: V ronkov It ~1.1. Panner, 13.~ I., Flerovo, 1". 'Areflyev, It,
V. , Basalayev, Y. lot Korolov$ V# Mof Mookalevo So 3;' Osipovs
V, P,
TITLE: 30-?Iev linear electron accelerator. designOd f~r neutron apeco,
troscopy
PERIODIC&L: Atomnaya.enereiyay vg 13, not 41 19624 13 2 7 336
TEXT: The accelerator, de3igned,by 6e 4diotekhni~hcskiy~institu t Mi SOM
(Radio Engineering Institute AS US5111)-and Uised f6r,'neutron spectroscopy at.
the Ordena Lenina Institut atomnoy energii im, I. V. kuichatova 0 SSSR
(Lenin Order Institute of itomic Energy itdeni LV~4' Kurchatov A6 USSR), is
4 'traveling-wave accolera,tor zhich produces a pul'Ped e~,Icctron beam with
an.,energy of 30 Mev and a current of up to 500 ma.' It 1,:operates on
244 LW= st a pulse repe ti tion f requency of 100 cps'!'and itith pulse durations
of 0.6 0.2, or 0.05,4cec. tt.the input of the-`d1iuphra'&med waveguide there
is a field of 150 kv"cm, The efficiency of h-f i~derey
conversion is. 30-3YA
The mWimum h-f po-ver for 10.0 cm is 20'Uw.i ,/The diaphragmed waveguide
116

510891621,13100410031011
30-hiev linear electron B102/B108~
was d~si4ned a3 a homo-eneous system nith constant phas 6 volo'city 2).
Each of ito six cells has four 4-m-m openings to improve~thc,ovacuation of
the system. The h-f powor frum the generator is fed to~ the accelerator
throiteh a a taneard square f ceder waveguide (34 bY 72 -mm i 6 m ~ long) wherein~
1i - type Yraves are excited. This wavef:uide is, enclooed,jon each side by
10
glass windows of circul;ir comical s1hape. The h-f p
,enerator is an unsolt-
dered klyztron equipped with a titnnium getter and,fed by a 11hyratron modu-
lator. The modulator is fe& with direct current fr6m !,.~rectifter with ~1
voltage regulator at its primaxy ninlin- I-odulato
r 7 tn!;~ klyntron ure
conrect.-t' by a 65-Mw P111,30 transformer t~oost jj.63 The klystron operates
at a maximwm voltage of 320 kv. Its h-f excit-". tion is mid~lziaviag' no tron %,ith
a po'.',er of 10-15 To prevont h-f breakdown in the 10,'y5trcint its voltage:
CUPI)ly i3 C'Ut Off FlUtOMAtiCally when excess curren tis amoulit ~0130,*', or if
.an h-f breakdown occurs in the accelerator part. The jUloed"injection
current Is supplied by a. three-clec trod e electron Gun:d~aiEned similarly
to Pierce's double-electrode Cun (Pie. 6). The vacuum. ~ ateml of the
accelcratur is conricoted-to thre'a titanium ion getteir pu ps all d aienea 'by
the iizU-.o--tokhnicheekiy institut All US:j.R (PhysicoteahnNml ln~ateituto A3
UkrS~jlO. 7he necossary o)orating vilcuum 0f(2-0-10-6 lig qan be cre.atoi
Card 2/6

i/089/62/613/00'4/003/011
30-14ev linear electron ... B102/BlOB
f" byone;auch pump and the threa enBure continuoue operatton for 10-12 bra al
day during' threc--to four months. A act of mechanical ~ump's;ia us(id au a
for,_-pu:.:f. (10-2 to 1073 mm The controls and avii tch Ceni are installedo;
in a separate building. The accelerated electron bepm is fq'cused onto a
U238 tapect in a water pool. The bremustr, ar
ahluttg4hich occur.3 in the t
get product?3 noutrons by (p n) or (y-, f) reactions. The ne)atr ne of
~/Vl - 5 Liev have Max-~;eliian energy' dia tribution. The yield isijo 4 neutrons,,
"per mr-Tho entire. unit. is enclosed by a concrete shield 10 .5 in thick) pro-
vided with 3everal experimental channels (.100, 200, addi300 wo widt)(Fig-7),
~he current, sp'cctrum, pulse shape, aiid'radial distribuiion of the current
density of the electron beam -were measuredo -Numbrical data are given for.-
time of flight and background,, There are 9 figures a~nd'i2.tables.
:MMITTED t Dezember 181*1961
Card 3/6

CM
3/of-9/62/013/6c)4/003/011
30-Mov linear electron B102/B106
Table I.
(1) pulze duration, Awac; o,6 0,2 0,05
~2~ pulse current, ma; 160 250 160 320- 160;~ 5')0
Bel,max' f"Ov 27,5 25,0, ~1,5 25,0 32, Q 29,0
Wrelative neutron yield., 9 10 .545 6 1 2,5
Fig. 7. 6hielding system.
Legend: (1) acceleratori (2) targetj
(3) experimental channels.
Cnrd 4/ 6

30-Lev linear electron
ow~
Fig. 1. 13lock dia-
gram of accelerator.
Legends (1) accpler-,
12,
ator tube; M wave-
guide viindovi3 ; (3)
electron aun;(4) tarr',
tot with mode
rator;
(5) titaniun, pump;(6)
1r
forepumps; (7) pulse
transformer guns; (a)
9 7
gun modulator; (9)
kl, stron modulator i
(IO)klystron; (11)
pulse transformer of
klystron; (12) magnet-
ron; (13)macnetron modu- CM CM
lator;-414)starting block; I
(15)focusing coils.
tard 5/6

UIM39/62/013/004/003/011
30-yev linear electron ... .01021BIOa
Fig. 6. --Acctron Cun.
Le ze A-- (1) anode, (2) electrode ne~ar the cathodej (3)~ gridj (4) cat~ode.l
Fig. 2. Diaphra We-d iNaveguide sec-`
tion. 1) - 2 7 mr.1 P a ~O mm, , a/)-
0' 14, 2b - 86 :vi~i, d. 6.4 ITIM, over.-
all leeigth 400 c!i, -.-a 1,1 thickness
7'
Card 6/6

VORONKOV -R4 M*--
-7- VON: 27
10 1
2
AUTHORSs 0. T. and M. R.
TITLEs Muchnays, konferentelya Mookovskogo Lumhonerno-fis Whesko m
institute (Scientific Conference of the Moso*w Emsinsering
Physics Inatitiate) 1962
PERIOD'ICAL, Atox=ya energiyat v, 13, no* 61 19629 603 - 606
TEM The annual conference took place In Usk 1962 irLth nore, than 40(~
delegates participating. A review in given of these lectuselthat are
assumed to be of interest for the r*aderi of LtoanayiL energlys.1 They!sra
followingo A. I. Leypunskiy, future of fast reactorml A. A. Versillysi,
design of accelerators for superhigh snergiss'l 1. Ta. Pomeranoh4k,
analytiiity, uniterity, and saymptotio behavior of strong intetiotio" at
high onergiesl A. B. Migdal,phanostanological theory-for the many- a
probleml Tu.'D~ Fivayskiyq deceleration of modium-energy antiptatons in
nattorl Y-U-.Y.-Tagan, Ya. A. Icsilevskiy, theory of the Xaesba~er effeatj
Ryasanov# theory of Ionization losses in nonhaaogeneaue'vediuall~
-fconductivity
YU. Ivenovj A.,A'.'Rukha4sop.h of-saboriticsvplassao
Pard Ih',

8/089/62/013/006/019/027
Ifauohnaya konferentelys,... B10213186
Ye. To. Lovetskiy, A. A. Rukh4dze, electromagnetic waves IA' nonhomo~sneous
plesmal Yu. D. Kotov, 1. L. Rozentalf, the origin of fast cosmic Munn";
Yu. M. Nanny, muon depolarization in solidsl V. G. VaTlsmov~' Yu. It. GraehU4,
B., A. Dolgoshein, V. 0. Kirilloy-Ugx7umov, V. 3-. RoSsnov, A.j. Ssmoylov#
p- capture by various nuclei; V. S. Doeidovi V. G. KirLllov-lUgryumoy
A. K. Ponosovp V. P. Protasov, F. V. Sergoyov, saittering ofix- mosono at
5' v 15 Vey In & propane bubble chumberl S. Ya.
Nikitin, M-1~. Aynui4inov,
Ya. X. Solektorl S. M. Zombkovskiyg A. F. Crashing suou prodiwtLonln x-p
Interaotionsl B. A. Dolgoshein, agark ohemberal N. O..Yolkov'
V. X. Lyapid*vmkiy, 1. M. Obodovskly, study of operation of" conviotion
volt Pu
chamberl K. 0. Finogenovo production of square 164 of high
age s
amplitudes; 0. V. klakeakov, problems of color vision, V. Z; LyapLdmkiy#'
relation between number of receivers and number of indopendOM, ooloral
To$ me Sudry'amtsev, M. 1. Sobolev, Is 1. Tisongsus L. W."funitskiy'v
on,
Y. of Paysulov, deteriinatiork of the moment of electron trohsition~ 0t os-
'cillator forces and the width@ of the 80huhmn-Rungs 'bands of soleoul4ar
oxygenj B. To. Gavrilovp A. V. Zharikov# T. X. ltiqko,' doodmoalitioi of the
volume charge of intense ion beinal To. A. Xrsmar-Ageyev~t T-o S. Ti~**blu,
measurement of neutron spectral 0. 0. Doroob nko now
noutroq rooordingi V. 1. Ivanovq desimetry MmALlogy 70 Tor,onkovt
'Car& 2/4".

S/O89j62/013/006/019/027
Hauchnaya konferentalya... B1021B166
design of 30-Mev eloctron linear acoolerstorl Ye. Pyat~oov A. A. Glaakoir,
V. G. Lopato, A. I. Finogenov, G. N. Skepskiyp V. D. Selemnevt.experimental
characteristics of low-energy electron linear accelerators; G.~A. Zeytlenk,
V. M. Levin, S. I. Piskunov, V. L. Smirnov, V. K. Khokhlov, radiocirouit
parametero of M (LUE) -type acoelerntoral 0. A. Tyagunovo 0. A, VaIldnort
B. M. Gokhberg, S. I* Xorshunov, Vo I.'KotoVj Ye. M. Morozo acnelarator
classification and terminology; 0. S. Milovanovp V. Bo Vaftksiti, P.R.
Zenkevicht theoretical analysis of magnetron 'operationj A~r. G. Tragov,
P. R. Zenkevich, calculation of attenuation in a diaphyagmated vaveguide;
Yu. P. Lazarenko, A. V. Ryabtsev, optimum attenuation length for linear
accelerator; A. A. Zhigarev, R. Ye. Yelioeyev,, review on trajeotographs;
I. G;. Morozoval G. A. Tyagunov, review on more than 500 ion sources;
M. A. Abroyanp V. L. Komarov, duoplasmatrqn-t~pe eourcel s.':Kuznetoov,
A. I. Solnyshkov, calculation and production of intense ion beaw;
V. M. Rybin (Ye. V. Armenskiy), inductive current transmittera:!of high
sensitivity; V. I. Koroza, G. A. Tyaganov, kinetic deacr .iption of linear
acceleration of relativistic electrons; A. D. Vlasov, phatie 004illations
in linear acoeleratorej E.'L. Burshtoyn, G. V. Vookreaenskiyj beam field
effects in the waveguide of an electron linear accelerator; R i S. Boboviko,rg
Card 3/4

VORONKOV,, S.T., inzh,
Heat insulation of large zteam turbines* Emerg.'~stroi;. no.32:30-
37 t62* (faRk 16:5)
1. TSentrenergot6ploizolyatsiya.

7 -- ---
5
i , i
I II Ii L !: ~,:: I
....

VORORKOV, Serrqy.,Timofeyavich; ISMOV, David 2-InovIyevich; KAKEN=KIY,
Favlovicho )mnd.tekhn.nauk; ZELIKS0110 LARICNOV,
G.Te., tel:hn.rad,
[Heat insulation for electric stations) Teploy:'~Ia i1joliataiia na
elektricheakikh stantaiiakh. Pod boshchei red.. S.P.Kamenstskogo.
Moskva, Gos.energ,izd-vo, 1958. 423 P. . (HIRA 11:7)
(Blectric power plants) (InsiLlation (ffea~t))

~V!CIRQNKO V ,. 5a-rgvy-TJZ04' y~ylcb, ISIEROV, David ZinovIyevicl-I
V14ENETSKIY Sollomon Pavlovich, kand. tekhn. nauk),
SMEL Ili TKOVA,L.K. red.
(Heat Insulaltio*n In electric power plants] Tepl6v;aia 120-
liataiia na elek-trichesk1kh stantailakh. lzd.2."~ perdr.
i dop. Moskva, Emergila, .1965. 471 p. WJRk18:5)

8(6), 14(6) SOV/01-59-7-1/21
AUTHOR: Iserov, D.Z., Voronkov, S.T., Engini'pers!
TITLE: The Repair of the qeat Insti ation at PoWer 'Plants
PERIODICAL: Energetik, 1959, Nr 7, pp 1-4 1 Js s q�

ABSTRACT: V
The authors present some recommendations for the ther-
mal insulation of steam. pipelines.~ btzri#g~ the pa St
years, at a number of district the wal power planto,
the thermal insulation was reconst:r
oted on a large
'
scale. However, the insulation of W.ilvea,'flange ,
joints and other shaped pipeline s,eotioi~s, an well
as boiler caBings , remained in an un,eatisfactory con-
dition at inany thermal power plants'. The most serious
deficiencies were caused by the fact th6A.the actual:
operating o-onditions were not consl~ere~ when instal-
ling the insulation for'the first:time: the properties,
U
of the different types of steel useo for the equip-
ment, the necessity of inspectingyrelded joints du-
Card 1/4 ring basic overhauls, the,expansion; of Austenitic

~W91 59-7-13/21
The Repair of the Heat Msulation at Power Plan~6
Seledtion of ma- 11
steel pipelines, vibration and the.
terials being more stable and reliable in mechanicalt
respect. Presentlyq the necessary *theordtical premises~
have been established for organizing the' repair of theI,
thermal insulation with a determination.of its eff,~.c-
tiveness. Aluminum linings improve:ponsiderable the
length of service of thermal insula:tion~and reduce
heat losses. New designs of heat in6ulation were 'de-
veloped under consideration of actual operation co-n-
ditions of power plant.9, facilitating the transition
to industrial methods of fitting an 'd repair-Tig thermal
insulations. By order of Tsentroenergotoploizolyatsii
(TsETI), the vibration laboratory:XTB of Glavonergo-
remont conducted studies of the influence of vibration
on the durability of thermal insula,tion~'materials at
the Cherepets GRFS. Investigations:'of vibratilon sour-
ces in turbine and boiler houses sh"ovied', t-hat vibra-
tions cause changes in the insulation material struc-
Card 2/4 ture, leading to formation of air iockets, higher

SOV/91-59-7 I/-
The Repair of the Heat Insulation at Power Plan.M;e
temperatures at the outer surfaces':;of the insulation
layert decreasing the length of servied of insula,;ing
material. Yeasurements showed that. fo~example, ee-
der lines produce steady-state and periodic Oscil1R-
tions at frequencieB Of 12.5 and 5~)'cy6l~s. 0scilla..
tions higher than 10 cycles destroy th6 internal,iin8u-
lation layers. TsETI developed and!inslalled effi.-
cient types of detachable insulations for valvesand
flanges, mats with a glass wool shell end a protective
sheet metal lining. The unjversal~;detachable ins-ala-
tion for flanges and valves of ste4m and ivater pipe-
lines consists of an aluminum housing lined with mi-
neral wool held in place by mesh W~ire 01ind covered with
aebestos-cement plaster. The material and -technologi.-
cal basis for the production of thermal insulation
material has been established. TsPTI produced deta-
chable insulation shells'for diame'tersjof up to159
mm. In 1957, TsTT1 started the pr6duction of mineral
Card 3/4 wool with a planned output of 8,000 tons annually.

"OV/9 1 9-7-1/21
The Repair of the Heat Insulation at Power Plants
Semi-industrial tests of perlite, ne.,'highly effec-
tive insulating material for tempe't-atures of 600-1)00
degreesp Nvere completed. TsETI plans t_he~ constructiton
of an installation at Dimitrov ( ~~,bskovskaya Oblast'),
producing adequate amounts of perl~Lte for thermal po-
vier plants.
Card 4/4

9. Monthl List of Russian Accessions, Library of Congress,, O[i~[ 12,52. -/9W, uncl.
; 1, 1 1 1
I li I .
i . 1, .
; 7 p

,Z~~~uzhener. 1,~YA07, D.Z., imhener.
ProDaratory- work for reconjitruotlug the heat thmillitiom in
electric oower p1nitte. 'Blek.sts.28 no.7:6-11 J1 j~157.
(316ctrla power olant)

tr L F2c
+Ffe-lIMITI fit Iv:fIA4
i u rli i ivo t r 'Lh-o'.11t '111.3 Vell w.
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We WIM
I t !1 11111 -1 -1 11 11 1 - I 1p:11 it'll[ 1, 111 ,4,11
T.-'pT l

Steam Boilers
Drying brick walls of s-I'aam boUers. Rab. imerg. 2 'To- 31 1952,
Monthl. List of Russian Accessions, Libr'ary:of Congress , ~,Iay 1j,52
Uncl.
:1 :1111 iffli ,I 11111M.M111j, MINN. HIM:
ki

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6003935 56ifl"M. C~Dr. 3741
AUTHOR: Sukhareve, L. A. 01osco1-0-Vo!r~on1!V;o*V,'
M., 's
L. Ye.: Of nc6w);'r%JTarlamove, A. ll. om 676
I CR o a C o'7W
Vorontsovap Oe
ORG: none
TITLE: Investigation of alestoners": an! ~th4s~ ba~tsi -i
systems
SOURCE: Mekhani
ka polimerov, n04
TOPIC TAGSt elastomer, syn,thetidi rubbler,~: polyami~
ABSTRACT: Physicomechanical. nnd ther~pp si~
I -- --" -1
on the basis of binary and ~ternary syotents with' id.
polyamide, polyvinyl chloride (PVC), hri4"ubber~!h~
The binary and ternary systems with o~tiuj4j V hy s!il
Were,chosen on the basis of,corioositLbu piropartyj;
ert~ies i of;
onous change of physicomechanical: prop'. , I ~'
A
ratio of the PVC and nitrtlo-aciylic ~ctti: vas ofbi
to chemical interaction. I t W.M
4 shown that itit
properti Can, b
e9 of polyamide In; therrial aglng a J
Card 1 2 UDC 67d:01~519~
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VORONKOVI V. d
Qtvationa dictated by lifev Sov.profsoluzy 16 zj*;9:19L-21 X7 160.
1. Predsedatell zavkoma X3.inskogo kombinatL'Lak~08tve4nogo
volokn
(sociallsi competition)

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qj,JwAr,lred.; DMITRYUK, A.N., red.; INKIN, S.G.it red'; MSIMOV,
I.A., red.; ROKMOV, N.Ye., redo: P=REMP red..; CHURKIN,
AV.v red,- TEMITIM, G.A., red.; KOLOSOVA. 2.~4,,, t6khn.red.
Sochi. Uningrad, Oos.izd-vo *Iakunstvo." 1959.! 19 ]P*# illuo,
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(Sochi--Description)

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DAYCHIK, M.L. kand.tekhr.nauk; VILIFERTg K.I.;
V"ROETY41 4L . I'd,
Devices for statistical Investiptio-na of ar-.02161-atibna, streg!le3,
and deformations,. Avt.pom, 29 no.10-.22-25, :b 16J. (MIRA 16-,10)
1. Gosudarstvannyy sqyuzjVy ordrna Trudavogo Krnanolp Znawni
nauchno-issledovatellskiy a-Ttomobillmyy i avto~otornyy institut.
p
p

29823 i
S1020V611140100610221030
B107/B'101
AUTHORS: Ayzatullin, T. A., Voronkov V. G., and~Zubov, V. P.
TITLE: Dependence of the limiting pressure of.the explosiveness
of gaseous hydrazoic acid on tho spark~'P'ulse,intensity
PERIODICAL: Akademiya nauk SSSR. Dokladyj v. 140, no. 6, 1961,
1356 - 1357
TEM It is assumed that the limiting pressure of:the,,sxplodiieness
drops with increasing spark energy and then reaches a c6natant;value. TbAB
is explained by assuming the ocomrence of two differetit~!Igniiion mechanisms
(L. N. Khitrin, Fizika goreniya i vzryva (Physics of combustion and explosion
explosion), M., 1957). It is shown in the present paper that.these
assumptions do not hold for gaseous hydrazoic acid. In,this:case the
limiting pressure was found to decrease continuously withincreasing spark
pulse intensity. The experiments were carried out.in " 11-am diameter
spherical glass vessel. Fused-in electrodes gave a 3 mal spark gap in the t4l""
center of the vessel. The electrodes were connected to'an auto-transformer
secondary, while capacitors of defined capacitance were:ldischarged over the
primary. Hydrazoic acid was prepared by the reaction of pure stearic acid
Card

29,
S%Y~o /14'0/006/022/030
Dependence of the limiting pressure... B107 101
with sodium azide. The tests were carried'out at room,temperature.
Result: The logarithm of the limiting pressure P of th6.explosiveness is
a linear function of l/C 0.2 (C - capacitance). Fig. 1,gives~P'as a
function of C. Another test series was carried out with a mixture of 25~~
hydrazoic acid and 75% calcium-chloride dried air.~ The~;'resuitb may be
/Cn Vr
bxpressed by log P - A + B, where A, BO and n are constants dependent on
(P/i,1+2/n .,:~
the respective mixture. The expression log ~A/To:+'B derived by
i
N. N. Semenov (N. N. Semenov, Tsepnyye reaktsii (Chain reactions), M. 1934)
for thermal self-ignition evidently represents a more general rule
applying not only to oxidation reactions and thermal self-igidtion, but
also to decomposition reactions and spark ignition of ividelylvarying
explosive systems. There are 3 figures and 8 referenceilc 6'Soviet and
2 non-Soviet. The reference to the English-language pul)lication reads as
follows: M. V. Blance, P. G. Guest, G. Elbe, B. Lewis, ~J. Chem. Phys.,
11, 798 (1947).
Card 2/3

29823t/020/6111 40/006/022/030
Dependence of the limiting presaure,o.. BlOVBIOV~'
ASSOCIATION: Moskovskiy gosudarstviannyy universitet im.1! it. V,
Lomonosova
(Moscow state University imeni 11. V. Lomon6sov),,
PRES.ENTEDt May 24, 1961, by N. 11. Semenovp Academicia,n'
SUBMITTEDt April 18, 1961
Pig. 1
10
a-5-1
0 W J0,k
1CWrd 3/3

AYMULLI1,19 T.A.; VORMOV, V.G.; ZUBOVo V.P.
Limit pressure for the expl.o.slven.oas of gasmjiv hydzimic acid
as a function of the spark impulse pawOrf Voklt~ 104 1.40 no. 6:
1356-1)57 0 161. (PURA 111111).
1. Moskovskly oosudarstvennyy universitet im. V.Lorionosova.
(Hydrazol acid) (Zxpi6~Aons)
rii:
.1 7,117,1171711i 11, ~,I

----- -----
660
1. 11-OROMOV, V. G.; '"W.70OV, M, 11.
2. USSR Wo)
"The Convection of a Cold Flame in Combuntible Mixtures
Containing 0.03 Percent Carbon Bisulfide", Zhur. Fiz. Khim
13, No.12, 1939. Leningrad, Inst. of Chemical Physics,
Pbysico-Chemical Lab., Academy of Sai. USSR. Received
11 Aug. 1939.
9. Report U-1615, 3 Jan. 1952.

5W $OV/62-59-1-4/38
AUTHORS: Blyumberl-, H. A., Varonkov, V. G., N. 11"..
TITLE: Gaseous Initiation by Ozone During tho,Proaeat3 of Paraffin
Oxidation (Gazovoye initsiirovaniye w4onom:v protsesse okis-
leniya parafina)
PERIODICAL: Izvestiya Akademii nauk SSSR. Otdeleniye khimicheskikh nauk,
1959, Ur 1, pp 25 - 29 (USSR)
ABSTRACT: In the,present paper the authors inventigated the problem
of the applicability of ozone as a gaseousliniti4%tor in
the oxidation of liquid phases. The'rie-thod:of oxidation
described in (Ref 3) has been. already applied. The paraffin
"Kepsen" was oxidized from brown coa1 ,3upp~lied by the Gerlian
Democratic Republic. Experimental dat.a sho it a number of
particular features which occur in tl e addition of o2one
during the oxidation of liquid hydroo(Lrbo~s. The kinetic
curves of the increase in the acid wimberri Iin paraffin
oxidation are preaented in (Fig I). The effrnt of the stimula-
tion with which the reaction was excited tit the beginning
may be seen from it. If ozone aoto iii it tor a longer period
Card 1/4 a very peculiar phenomenon is observi'd. The reaction is
11 F ~i

Gaseous Initiation by Ozone During the Proccon of Paraffin .1107/62-59-1-4/36
Oxidation
accelerated (the period of induction,Js sho'rtened) while
the limiting yield of acids is simultonejus 'ly reduced.
Similar phenomena were also observed in thel. application
of other stimulants. In this connection the experiments
with uninterrupted transition of ozoni zed air were some-
what startlingfor the respective kinetic curve indicates a
reaction course with maximum velocity~land 0 very high.degree
of oxidation. It was ansumed that thelprocean of oxidation
changes in this cane and.oxidation isr.:produioed no longer
by molecular oxygen but by ozone. If.t~olecxilar oxygen
par,ticipates in the reaction it is included only in very
small quantities. (Fig 2) confirms the conclusion that a
strong stimulation of the process causes, apart from its
acceleration, a reduction of the tran6forma tion degree. Inter-
esting results were obtained (Fig 3).'
,by the application of
different temperature conditions during the initial ntage and
the development of the oxidation process effected by a *shock"
at the beginning. It may be neen frorj:lit that the kinetic
curve of acid numbers does not vary In any'case. At present,
Card 2/4 the paraffin is oxidized by meann of~the m~nCanese oxide

Gaseous Initiation by Ozone During the Process of Pataffi-~ SOV/62-59-1-4/38
Oxidati6n
catalyst under commercial conditions,~Ilvrhereby the process
is very complicated, however. Production is simplified
and continuous oonditiona of oxidation are~entablished
by the application of ozone as a gasepus inibiator. It
must be emphasized that oxidation by 6%oniied air ensures
good quality of the oxidation productl;~%thich meets the
requirements called for synthetic fatty acida. SimultaneousIy
a complete utilization of raw material will be achieved..
For comparison some properties of the~':,oxidation products
synthesized in the presence of the ma1;iffaneqe.c;atalyat;cin
the one hand and by uninterrupted oxidation itith ozonized
air on the other hand are shown in tha~~ tableo These data
were obtained at the laboratory of tho Veesoyuznyy nauchno-
issledovatel'skiy institut zhirov (All-Uni6n Scientific:
Research Institute of Pate) in the Sh6bekitskiy 1[ombin;s.t
under the supervision of N. K. Manlkovfikaya. There aro
3 figurce, I tableo and 15 refarennwllj~ 0 0t vhiah are Soviet.
Card 3/4

, ! :A A I I I 1111" i ;H t If11111-:0i 11
I TO
Gaseous Initiation by Ozone During the Process of Paraffin SOV162-59--i-4138
Oxidation
ASSOCIATION: Institut khimicheskoy fiziki AkademA nau~ SSSR (Inst!*tute
of Chemical Physics of the Academy ofi Sciences, USC-R)
Moskovskiy gosudarstvenhyy universiti~t im~ 11. V. Lomariosova
(Moscow State University imeni M. V.'~Lomonosov)
SUBMITTED: May 29, 1957
Card 4/4

'H ]l tldi 1:111 Ell 111,111i filillill"I 1111,1111*11' H11 -I! 111iii
Hill

C-to f) C4 ) V, i-1
AUTHORS: Voronkov, V.P. and Frolov, A.!!.
TITLE: Coincidence Circuit for Work with Small~'Amplitude Puises.
(3khema sovDadeniy dlya raboty s impull~-jami Inaloy am,,JitWy)
PERIODDOAL: Pribory i To-khnika Ekspex-iai�rilta, 19'01 14,t,3, 40-42
(USSR)
ABSTMICT11: The circuit (Fig.1) operates on tlle:-C-rinc~i>le of differ-
ent amplification of coincident and nontcoin6ldent pUlSes.
Negative pulses from two input elements I "transducers" E-re
shaped by short-circuited cables and passed to
the tubes A 1~ and J1 These ztage,s producea two
1 2 3 1 i
len-thened and inverted pulses; the positive,swings are
suppressed by the resistance r and 10'r.-arallel-connected
crystal diodes DAr-44. Normally, the TaLlseo at the
anodes of the tubes Al and Jl;) and,,also', at t:ae anodes
of tubes J1 Jq. jaust- be of. equal amplitude,. The pulses
3
from the tubes pass� along tile a ab 1 es ~L, and Z2
2
-o points,i B 'and C In
(PK-50) to point A and also t
the case of coincidence, the -ulses at joint: A add to-
P
gether and pass throulLh the detector todone !of the inputs
E of tile differential araplifier (J1 and ~1 The
Card 1/4 5 1 6

Coincidence Circuit for Work with S--,iall Amplitude P~.Ises.
Card 2/4
larger of the pulses arrivinG at b4e DtDi-ats B mnd C is
passed to point A but the detector to which the small.or
pulse is a-.plied is switched off by the.Ilar-er pulse. The
difference in amplitudes 4U at pointi?, E i and A izc;
amplified by the differential amplifier',' i.e!.~ at the
I
anodes of J1 5 and J16 aPpear Pulses 0 opp~,osite polarit-
ies and with a.MDlitude U, proportional to AO~ UOX
U
i 111A. UbX
where K, is the gain of the differential aplif ier to the
difference. From the anodes of and Jj~ I the pullses
5
pass to the input of a second differential a~nplifier
(cathode and Crid of J1 At the anodo of,~p appears'
a pulse with an amplitude proportional U A U
t
8%
Uc K where K is the gain of the
2 "110 U5A

120-3-10/40
Coincidence Circuit for Work vrith Small -Amplitude Piilses.
second differential amplifier to the di~,fereuoe. When only,
one of the input elements operates, pulses o'% equal ampli-
tude USX arrive at the input to the first differential
amplifier. At -the anodes of J1 and :fl6 appear pulses with
amplitudes K Us% . where K is thezain of the first
3 3
differential amplifier when equal amplitude pulses are applied
to each of its inputs. In this case, the Dulse at the anode
of A is determined by the unbalance betueen the branches
7
of the second amDlifier: U where K4 is the
U140 = K4 - K3 &X
gain of the amplifier stage A to pulses a;plied simultan-
7 P
eously to the cathode and grid of the valve.; K1~2 is made
very much greater than K K 7 so U UH_
i'o.) the
3 4 c
pulse at the anode of JI is many timed greater tit coinci-
dence than vihen caused by a single input -Pulpe. The,pulse
at the anode of J17 is lengthened, amplified, discriminated
and registered. The threshold of the diiscriihinator is set Up
so that non-coincident pulses are not registored. The
Card 3/4

Coincidence Circuit for Work with Small Amplitude, Pulses.
selection coefficient a is,defined asithe j7atio of the
amplitude of a single input pulse to the wnplitudo of equal
c,oincident pulses ivhi(-.h give, the sarae ouitput~ voltage i.e.:
lK2/K3 4.
In practice, for pulso durations T^.'5~~' 10-9 see. a 18.
The cables Z and had to be care'Pully'matched into
1 Z2 i
their load impedances. The pulses at thie anodes of valves
-171 and J12 and J1 and J1 4 were.equalized by variable
3
resistances in the anode cirduits of J1 '': and J1 The
4 '
valves (6%k'ln) had to be carefully sele",ctedi. Time resolut-
ions up to T-5 x 10-9 sec (Fig.2) for !in-puts dovin to
"0.03 ~ uere obluained,. There are 2 i-11U.'st-rations and no
references.
.SUBLILITTED: March 13, 1956.
AVAILABLE Lilbrary of ConGreSO.
Card 4/4 1. Amplitude modulation 2. Coincidence ci.~cuita'-Operation

1:7 T-f 1% "1 v
FROX A
Coi=idemcs cirviitt; fo: q-jc!-r-t iota: with
Prit . i tekh . eksrl . no 3 . 410-41 1'57. I'D: 9)
(Pulse techniques (.zliectronice)) (Photoeleetran~ymiltipliers)
(e,lectronio circuits)

; cn M, - - . I
Card 1/1 Pub. 146 - 36/44
Author : Likhachev, V. M.; Kutsenko, A. V.; Voronkov, V. P.'
Title : Problem of the investigation of relativistic partialies by' the wthod
of nuclear photo-emulsions in an impulse magnetic field
jeriodical : Zhur. eksp. I teor. fiz., 29, No 6(12)) Dee 1955,,694-8915
Abstract : The emulsion method rarely solves the problem of the sign and exact
energy of particles. This problem can be solved mdre completely if
the nuclear emulsion is placed during irradiation into a'powerful
magnetic field, computations showing that sign an&'iimpul.~e (momentum)
.an lysis of particles according to magnetic bending can be carried
out sufficiently ace-irately only in magnetic fieldl'streniohs of the
order 1 to 1.5.lo5 G and higher, which is.at presepit. possible only
in the form of individual :Unpulses. In works withfaccelfirators also
giving beams of particles by itdividual impulses,,-6he pr4aent autbors
found the use of impulse magnetic fields very conlri~ nient,thanks to
the possibility of synchronization of the beam of particles and the
field (they acknowledge that the idea of creating :duch an arrangement
was proposed by G. M. Strakhovskiy In 1951). They employed such an
impulse magnetic field for measuring the spectra o~ photons from the
synchrotron of the Physical Institute, Aead. Sci..,LUSR.'; The appa-
ratus consists of a current oscillator (P. L. Kapifsa, P~oc. Roy.
Soc., A 105, 1924), coil and control. They thank~~rofesu*or V. I.
'Veksler for assistance.
Institution: Physical Institute im. P. N. Lebedev, Acad. Sci. USSR
Submitted : August 12, 1955

IJ . ............ --I .......I........ .
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if 7
LIN, q,
PIT I
JLII ::--I :;A
IA
-77 7 i-ITI till ;M171
i i 4g1
L"IM44
q- L LLL

S/l94/61/000/j)G2/010/039
D216/D302
AUTHOR. Voronkov, V.S.
TITLE: Design for optimum processes in ceirtailt relaypon-
trol svstems

PERIODICAL: 'VlZtronika,
Referativnyy zhurnal. Avtomatika 1 radioeld
no. 2, 1961, 32, abstract 2 V244.(Tr. Ilosk. aviats.

TEXT
The in-ta, 1959, no. 112, 39-49)
f; 8
f View
eed
de
n f
r an
m the
i
ti
fr
int
: mum -
o
s
o
o
o
op
po
p
g
of operation - automatic relay control system is 6onside 'red. The
system is of a special type, being actuated by two perturbations.
The form of the optimum correcting force is derived for two Opera-
ti6ns of the system (stabilization and tracking).' In realizing
the o ptimum automatic control system CAI? (SAR the autli_r sugge.sts
*
for t e1y; .9L".1ple Pdas-
he elements of non-linear feedbacks comparati v
ive.- RIZ and RC f our-po 1e s with rie 1 s.~ ;re erevL66S.
ay 4-; f
Card 1/1
11j!jj:j1!vjq
01

72-
B102/Bi
AUT M-%....
T6k6nkb* V. T.
TITLI~s., Theirmodyp"ic, equilibrium at the Hiles, ~'f 890sn'ttag of larte
Visiket tverdiDgo tel a tvo 5 9 riot '29.. 1
PERIODICALs: 511 574
TEXTv T.he, 'tions, 6U thermodynamic equilibrium:$ 4. diM~uvs*4 for t1W
three-phace. oys,te'w" eo'L'I:d (2) 7~it4uid (I )-gaseous (0) lilkO e,*A*iv stiplifying
assumptions, su.cli-'98-1-,peglecting the ef,'ects of oryttA line 4rivatedom w4
of slow vhase~ trAnsitions at the Interface'With
element cvn~Oe'i.44:(Ag.: 0 Oe line of sepwration, liv A464o~i, to W sbifrU4
by & thue -6aunink. A c40ge ~ in free energy 6F. Tmi~ dryitidlivalla", front
is in th'rm-d_ ature cauisi'pd: fV is aaaMed, W
. e O'y "i6', quilitrima# Ats cu:vv
0 'A
be c mpenpatedf.. the. same R the case for the malt 410(1 ji In MMbW1-
cal.equilibrium.0' The
Bit &$a
are
Card
;1

lh~'. :J1
The.rrftb 4d.~pamio:-04'ixilibriux 810 1
v.(2' -ore, t e ourface,tensic ''Coifficiewto 0 Abo ta ter-
h6i~ And
face,6 solidiftedtion; E> -je. MR1 UGS~_, 1U ~440 kprlt % #A
c lled the*.1crj6ta11iiatiq angleq, for It 9'r 0~-
and one"
Finally, the'Osid*-of.complete wattening lp
40d
-(2), is. dlways-469W.Ve. For a film of thioknena.- 646 4,4witrius DONAL-
tion with'tb4-'solid.,pbass reads b/343 v :Wbir*.j "ifie; bias' al malt-
ingi the", density,-'of the liquid and
'Trom Fh a orY tAllis'ation temperaturs T The fjj~s too2fi; not- im ipiplft
0
librium, its' A'qi;id is in'motion and phasip trallsl=o- !k ii 0
to- the solid,,'pq,cur. The film 166048108, distaw"
from the line of separation; at the oritical value';
Ah~- f il M+--*br'eaks- 0 These relAkioile iml #~ia' 6OX4 for 0~0 );Of 0(
'Caid 2