SCIENTIFIC ABSTRACT S. DOLODONOV - V.G. DOLOTOV

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000410830003-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

- DO;ORKQV,--%"- podpo:.kovnik
Radiation anil chemical reco:anaiosance. Voen.
vest. 41
no.5:5C-53 My 161. (MIRA 14:8)
(Stres.m crossing, Maitary) (Chemical warfare)
(Radioaztive fallout)

- DOLOWMOV# S., podpolkoynik
Under reliable protection. Voon. Yeat. 42 no,8148~-51 Ag
(HIRL 111:7)
t62.
(Gheidoal worfire-Wety measures)
I

3/018/63/000/002-1001/001
A004/A126
ALMIORS: Kolyada, I.., Dolodonov, S., Lieutenant-Colonels
TITLL: -Efficient protection from radioeictive substances and
toxic agents
PUIIODICAL: Voyennyy vestnik, no. 2, 1961 54 - 55
TLXT: The authors describe witys and meaAs for an efficient
protection
from rndioactive substances, toxic agents and war gas in
winter. They point out
that after snow-fall and by snow-storms radio-active fallout
may be carTied -by
snow and storm to areas where a contanination was not to be
expected, and that
radiation monitors do not operate accurately at low
temperatures. They enumerate
the voricus measures and monitoring method5 that are to be
applied by the radia-
tion detection teams., and describe the behaliar and protective
clothing and
menns of an attackirq, battalion in a contamirmtted zorte, as
well as the various
disinfection measuress,to be taken to make suret that all
radioactive substance
and toxic agents are removed.
Card 1/1

-DOLOGOPOLOV, V.L . inzh; DOLOGOIIOIAV L.N. in-ish;
PIUROVA, M.G.,, inzb,-
J,.w -- R--v
MILYAYEIrA$ T.I.
sac
Blectrolumines coat panele. S"tttl" 8 no.11:24-26
11,162.
(XEU 15:10)
1. Voeooyuznyr evetottiklmicheskiy institut.
(Luidnieseencb) (Electric apparatus and appliances)

DOLOGOPOLOV V.I.,, inzh; DOLOCOMLAV,'L.N., inzh;
PETROVA, N.G., inzb;
HILYAWTA, T.I.,, in7,h.
KlectrolumCmescent pamals, 8,#,Otvftkhpika 8
no.ll.-24-26 4-162.
(MIRA 15:10)
1, Vossoyuwm ovetotokhaichookiy inatitut.
(L,jmintescen*) (Electric apparatus and appliances)

V. %' .,- DAYON, M. I.; DETISHEVO K. I.; _RQLTVOSHEYII
A:..~ nmxon, :. - .
I ,ie j_E. p
I ~ I.; SINELEVAS, A, P,
,e -Iisclarge Track-Detect*r Ouxter Inna'Llption of
Owacteristics of isono
.t:'!- Chambers.
'I.:. submitted for the Intl, Oxf, on Cosmic Rays (IVPAP).,
Jaipur IrAia.,
Dec 1963,

1. DOLOGOSHOV V.
2. USSR (601)
4. Shrub a
7. Ripening and fall of fruft and sceds from trees and
bushes. les.khoz. 5
no. 12, 195?.
9. &;L-- j4p+- of Russian Akin 191!Lnp, Library of
Congress, April 1953, unclass

DCIOXO. A.L.. oi;vetetvemVy red,
Kazan railroad on the fortieth anniversary of the Great
Oataber
i
oci,list Revo3ution,,: &a account of its history and
econoaq]
Uzanakaia shelasnaist doroga k 406-1 godovshchino
Velikot Ckriabrl-
SkOi 8OtSi&IietiChDBkOi revoliuteit; tat
oriko-ekonomichaBkU
ocherk. Xessul, 1957- '39 P. WRA 11:6)
1. Ruasia (1923- U.S.S.R.), Xmzanokaya sholesnaya
doroga.
Dorozhuoye muchno-tokhnichesikoye obehchestvo. 20 GjavM7
inshener Kasantkoy sholezncy dorogi.
(Railroads)

.DOIDKlkll, P-., mayster po klailtai kiliteirrikh
perhey
------ ~--: t ~': .; -- -
laving ar*21&r kilns. Sill.bud. 9 no-5:21-22 MY
159.
(HIM 131-3)
(nins)

AUTHOR.i Mezentseva,.E,, oy
_.L. 14~Kkq,]. ya. If. P. Starost4..!!aL_L. Dolmman _~_L. A_,t
ORG: InItitulL spoR. Institut Kristallografii -AN SSSR)
t_qf (Ltyptaliqlprap j --
TITLE: Growing and refining of yttjr up fiiLi~glc! c
SOURCE: Fizika metallov i metallovedeni3re, V. 20, no. 3, 1965,
474-475
TOPIC TAGS: yttrium, yttrium zone rel'Ining, zone refining,
yttrium single crystal,
single orystal growth
ABSTRAM Experimentu have buen maile to combine vacuum crucibleleas
zone refining
of yttrium with simultaneous jn!tin qtals~:- -Yttkum ingots
g _~.q
80 mm long were subjected to crucib.1eless zone refining
K~fng-vhich yttrium single
crystals up to 1 Dun long and 5 = in -lianeter vere successfully
grown. A polymorphic
transformation in yttrium at. 1hT5C nuute it impossible to cbtain
large single crystals.
Zone refining decreasel the,content 4):! irDn, ccpper, and calcium
in the ingots by 2T,
20, and 10 times, respt!ctively. The (vqrgen content decreased by
only 2.4 times, pre-
Bumably because of the forvati,)n of eltable yttrium oxideii,
whose distribution coer-
ficient !:s'elose to 1. For mo.re efftictiie refining of the
growing single crystals,
electric current was p~stssed t1x-ough 11o iingot similltaneously
with the zone fusion.
After 8-hr.processing at a current d-raity of 5 amp/mm2, the
oxygen content in the
ingot anode portion, simultaneously :iorte :rused, was three
-times lower than that near
the cathcde portion. Orig. art.. has-., 1 irigure.
Card 669.794-172

39767
s/147/62/000/002/015/020
E191/E535
AUTHORi Dolomanov, YO.G.
..........
TITLE: Inversion phonomena in real gases in supersonic flow
PERIODICAL: Izvestiya vysshikh uchebnykh zavedoniy,
Aviatsionnaya
tekhnika,-S~no.2, 1516,1, 124-129
TEXT: In the solution of' many technical problems, the
magnitude of the stagnation temperature after ei compression
shock
must be -kno-%,m. For an ideal Seti;j the stagnation
temperature after
the shock is assumed equal to tttat before the shock. In
modern
aircraft, the stagnation quantil:ies (pressure and
temperature)
before the compressior shock a.:-e! so high that relationships
applicable to real gases ithould be used. The change of
enthalpy
in the stagnation process is formulated; the total enthalpy
remains constant when a real gas traverses a compression shock
front. From these statements, the change in the stagnation .
temperature is derived in terms of the initial flow
variables. A
discussion of the expression so obtained making use of
temperature-
volume diagrams of typical reeLl ~;ases shows that a
compression
shock cAn either increase, or decroase, or have no effect
on,.the
stagnation temperature. ~ lihen the stagnation temperature
remains
Card 1/2

Inversion phenomena in real getsea ... S/1117/62/0(JO/002/015/020
E191/E535
constant the conditions are resforred to as inversion point. There
is an inversion line in the temporature/volume diagram joining all
inversion points. The change in the stagnation temperature of a
real gas through a compression shock is proportional to its charige
of total pressure. The proportionality factor, the "differential
shock effect", is dependent on the initial flow variab 'les and the
specific heat. This effect hafi the same physical significance as
the Joule-Thompson effect. The-relation-of the shock effect to
other properties of the gas is 0111cussed. When a gas is more
compressible than an ideal ga,s the stagnation temperature drops
through the shock; if less compressible, it increases with the
shock. There are 3 figures.
SUBMITTED: October 13, 196.1
Card 2/2

m muinal J29AMAWIM
hCURS1110H Wt
MUM" Lyr2q~ 01yMme A
ZPRAEPAWVWVI)AWi:~~ AFFTIVASD
AP300h723
PEA/M44 W
0/0147/6~/W)/002/0065/0069
AM116 It Db1cmiftnov Ye* 00
TITIM, 09 tile calaullstion of air mrametewo behilul a nonmal Ak[o th
fitagraition-temperatura. inversion taken into-acommt ek v1
801WRt XWZ. Avistat, tekhaike no, 2, l$43l 65-0),
14oa-timiparature Invorsim,, nomal
Topic i-.Vm t fitfignati-on takparaturej ataS4~
shock, stagnation reg:.Lcn,, f.ICRF,, shook froo t',j shook effect
conclusions Me-As by the author in his previous v
~XWTPJ%4Ta-- An anslysill of the ark
(IVWp:,;AV1atsicnnaya t*khn:ft,, not 20 1960). concewilag the
existence,, at the
ohodk, ~ of atagnation-temperixture inversion. I a ym-amitted , 'the
flow parivueters in
the mgt= or the stagnaticei 1~olnt are calcuilated, taking the effect
ol! temperature!
inveralw into account. A jimph-analytical laetha is wied for
calculation of the
i gandynivila and thermoilynewto parameters or Mr (sim. Fill. 1 of
Encloaux,e); the
affee-m of ionization, dISSOCiatiOnt NO mole:1-mle f Ormatlon, and
variable. oFecif io I
beat artr considered. The UiPortance of temptiraturet inversion,
called shock effects'
Is dwoustrated, and a ccaparinon of the d0twed ant theoretical
results ia
greswited in a tuble (see B naloaura) It -ID c0llcludl)d that shock
effect ia
Card 44 1"

L 13590~~)
AOCESBUff Iffis AP3004723
present In all gases, iuA that d1A8(WI&t.LDn,, Ionitatlon, NO
sioUcule fomation,
variable specific heat, and shook effeat act; in tbo name
direotion, that is, they
ilearoaam otapatlon temperature. It Is Rlso coxcluitod that the
graph-analytical
uothod Is much simpler for calculating Sudynamia tuA
thern&Wiamio parameters
than thii mathematical insthodo Orig. art o has; 3 ftgures .15 f
omulas and
I table.
ASSWIMUNt none
BIJBIA11412flol 231joY62 Wt AoQ i ERCLi 02
SUB OWS I AI 110 W 80111~ W~ CAUER 1 001
Cqr41

U V
-1sulimi"n 0t th'i-umplie" d"etw, fur 16tiitAsHl;~ 40
r; 1. CcAubiwa atid k. 1.
e kikk XW1 ifosior, Ttkkool h-so' i 14b
Afsl:~nhtl(4 Pre))--t. 1034, No. 2,2"; W)0;1. or, Ai.
WS4. No. 43400-The orStnti*uttric evA tntntgaft(
tutib'Wo am conlthlr~d. : In the At tomet;k" itw thil
411 Cl in etshipir are ;523 Thn, triAll, oMt41*!
u
thod Is "'Cottl1l)"'led lk% tile u I
lt
a 6"ge with 10 Mt. of I AV Kollm-ti,
hes Ilt "ify
Mth H NO, to a conar. cA I A' wid tilrate ork 6 AJ AIN010.
adt int. toward tht 34 41[F;1MY1C%*Ak&d1.
boll
the ch"se with KHnOa M a w"My alk"J410'. tnoil a
stable violet tolor Is obtained. AddWy willt (titecki INVON,
"mt with Hs% tn c1liarilestunce of tftk cok*i a4A tittle
with H 3190,
The ml ABAIIY* iskel 40 ,0416. 4
t Vwh uld.,4r"I"
n 1.6 hn. Ttm mvft
2L

L*IA..,U',r4UVA, __ie. L., and L. e.
Ltew data ort cry3tallocheraistry and ty-po=rphic
features of cassiterite of
various origins. irudy xin. mus. no 3, 1951.

Ij
0. 'Iff"trent genculs. -4. It. Grigtr'ini and R.I. Riila~-
(INO.-The m0t nilmrtwit amesm" IIIL-
p, incrits occor6ig ir. t-waittHIP. ate Nb,,re. 'A" Fe, Mn Zr
anclTi. rhe=cltlnc.;itadt~3i(rt'teplacvSiib;iwm,~rpi~ini
bit t fmn Indepetid-tit mincni.1 a Own%, n arricf,y of columb te,
WOUMFnice, tirron, and rudle, nost Irequeti0y in mptar .
iotergrowths. 'rhey torn "itgnites of cor I is alit find -
smalitr, Le. in suth & deg= ict ilispersity that Giey arVu
Idgments of cosikerite. WmItite, wtill-
rwnite, suicl hematite w-c onl:r Ibund In thi- dairk-coloted
ones, ani "hour.-gla-m" stru;,tircs of imialtrAte cr)-3t%U
but not lit the Lol.)rlcts zom, is

thtnfore petic, while 14we 14102 11 illamaglictic',
Tilt v"IM nn.11ta ext limetkukly Plitt. and include kmly.
dhti*~-t Cry-Aallitt's of qtlartl ur $41I.Atei. Aniraq tut at-
C"*.,Iy elituentt, Nb Ind W triil~catv t-'# a "Thtin dirgrer the
ParagnittlQ and jl%,m~vm, under vyMch the So
deo;643 Live I-mi fcontivd, Kw thc g%whern. Chartictirt Of
tht p-41. puyln~v In li,hich they mvw. AC tond Sb sre tAlso
Of this typt, thcy ant txduid~ioy reitrix-ted o c"sittriln
I Pl.
Imily b1pyraniWad aystakofaWtc 40C
lor Vie metaxontstic gn-.6m lotiosatkv, which Is Lmk)cd. with.
pept-uLtitts and g,,anitat or cryvt. avhists. which hu,,,v under-
Ir-nt it ropid ternp. detirme on nmrto,,,- rpace vmd1tinni of
crybtal growth. This hipyransklal habit of cassittfite b:
111ways optcifically cumtfkttd with Nis, (LmWdts I'a and Mrs)
as "indiestor" elevarnt. On the other hand, the prismatic'
tryxtid haWt of camittilte otettirring in quorw4src veW h -
&Iwo" cwrrIstcd with W as hid"tor clemen! Cbmidlem Fe
and Xfu inwol(rawlteazdIrilliticritel,
biaxial cassiterite vhkb~ Is always rich In ~mtsursinatlixis,
while colorlem SnO, Iss stalaxiall. CohnnUke, ivolfrunske.
:
tc., do not form oWW Ami. with e"tefire. but "tal-'
ILA IndtpenJently. This astrecis with the iptsoWts, of Neu-
~aps and Noll (C.A. 44, 1377d). ~__W.

OLoMANDVR
A
Altumis mboa.: IV. an Tr 1E
Fao
'W*111951 I.-A 1416, ;~Wlhna of lmoflt~tm- lxt~ hibilt viv
h tilt owttwf ppe at der 'rmt*NJWA
TcOon wit It the %,Qmita. Vol
pubita. SO
tv
bmKi-lilct t4mrArphM
Its) WWA Won it clatil
'.hy4foamnal wi*tl. 4". oat)% tvaunk
fiuG1*p"f' ~ eml sismde* are ptimiry'~mhrmli
-woeoomutr trilwam are bAlui-'ate,
odwtt. Ile etwitt. ajuaysif. (it the rew 14ttial (-.YmA~
and IU x-Iruy mWer diotcrom showa its Indco.1mi mt~ctur-'
etel" ~ 111 the g1lout. of &VIrlostaltv cA'k1(1"Dv)
klutlo CRAI toyactl~IU.~b tit.
ouktAo. U'liolto foritko doue- vWxt*411(to W511 a
L
eiriojetmg co lots tUit QAQQ' 91 ~~,At I'lits, J'ht Ij
ttal outely-44 MeEtted wily 11nm of PC, It"r. M;
pr!~rlttct of t(4*u Owd 440tiol.

V Stamaite, and the Its di"Unp"Ume. IV, p
-9p
1voulaxly GMKT"t. regatta of ffuntato slauait;~4'
''spood.-with e)WMWI .1 ~ hyd 'to
le, armlowltecal mWn-,
the C*wuu, Tramsbalkalla, cmd4~1 WHO (about 2JI11A)). The lattm'
gorthoutyrn 11beria, Sln& tr]vtab with the rld"tral 10 Y4
-ty about to A halloytke, but Kratwhat dif-'
AllUme t$ Ue "Olloidal.
4j- dmWS In qnm *Mim with chAyrita md Womwynto.. Mt Odt., veakly
aWWv3pk4 with a =1 .674 in hYdiv.
A ZncDMX. stannite bas a sm"rhat differtnt XIMY stnW-; stallnite,
LTSR to 1.774 Is hydrofers1stWti, and 1.7US in
~1, turs thin tmmon stamIte. The mincria Is often thavaW
hYdrUFMIS119. 7a fiMt ateP Of ilia 4xidatibn Is an twkh
ion he Onface to an Ofte-Ovell *'b ampt u1nite, (0-bout
'~4tneftid 110 mid Pit". WhIlt Cu alld 0 arexenipmd. The
M 1142k- yelhw "d pnWact tonfilim Al eurk it no inure Sri.,
~Cu -Allo 11 -
Aydtd istamits, 4L Fa$* WULIUlUckaloysitc~
wwrol itlaormently4mlys
Th. t=I'l~-ral"Isi- of steatite
ol~lgbt cont-2-1-1 W scorodite. The autbom
Is that with chalcorgite, camittrite, topsi, i ionwaWtto sell WMI
a chmp of stannite In OnOt. 7be me of
ndarmunp Ofun mpim" chakeprritt and --sherite. the6addalical
hisbout thapamforrhalm rcandstannite.!
with rescilm rhas, sum . with,olikir sad "396-ir ExtIOWYO Chim.
OW simtral-anal WTI tudic, libowed - -
==lst quarts, Chalcopyrite &lid: sphakrite Won U-I= In It.1.1t,
1.48=1 lmmd dntrw tht--
jiet4w regular lottrifrowtho with Amite S1kd biolrUthinks Oxid
thmWell Wo An~ DOI. Vulfates., Alto,
4ndicatlagummWnsreactious. lAte-hydMbermalcristes. to Ik entirely
jvm*ved; CU is still present In bydrvatanuhe
linsunnitearecalcite covtWtt WheahAlte. Thealida- but removed la
the later stages of ox1dation. Sii is finaliv
t tion of Stannite Wis 3mcibed L; W. P. Ilmden (IW3) &W rtmovel,
61 tajW Al (dertred fnxn ft~d.-pwi of the mothc'r
KAU ~rocklc!xnbiu with Fell~lz "ll)drofer4sitc," W.
With the alliumptim of's secondary t I
-F4 sts"a I bydmtcp.. a

A A-47.
Mvirmoce It in .
L430er junmk clayish schttte, alcuri-Ims. sand! tonts, etc.
wblcb an hamwted by Oniotmnlia 4jod amnatcho-topas-
"It" VVIDS, with jd"nwA Ite, llvori~c' Pica. atanalte.
yr(te. onen( te,
Mitt. hyd. Im "" I" tj'c "Id"tio. ."'I the _jsu&I
Imal cemsite, tmiInthita, wmdte, knd calche
!amlypical. The odWte accors in the ympSer itcto"Ie fin
k ms, summit. with h3dloyofte,, Inwhitatlustsl hisunlavial
';:, Optical ebarmittr ek4l!pi parattl (IOD) am (1101
rot; twins pam"d Obj) ve - 67*1 1.331. A - 13?0
1,44. The chtm. mnal;;i aM the
cunk% show stllaftv + halloysitt In Infitnatt faftnmwths;
tht(ndothemiceffectsomatI80'.MV, BM*, *olP6D';cne
ex.)t!te=$ecffarthxtM*. Tbc pamroesla col Walte with
hath7Att, genrksite I'd. C.Al. 49, IMN), Mite, tic.,
Indkoites he onmrMoo formittka.. Ita ~mg con"C"t Is de-
froM the. ichistj which were dec ipd. by If-conig.
'hydroftrmal volm. vrbkh s4m brmSht *Dmt Ot Smism
forrattlon with ton" and ximpadke ('cl~ V.S. Salmlev.
A(h"vo&V. SWr*aL'mv. Cog. WArkaftP32,
let

F7
Orr -
M*SujAlltx xOd its IntlAlma."r. Inad:P43tion. I
Crirm:v , And R I -Z
Sn ~.vil i hIA" xl,,
to ltelwo. 71'-h4 F;t',Il tm I, I.L;I, 't
AV
imnscAlil ni
'trawl -1:n"ll ivc,21WE i3l rpAl fowc,!
Il-a
zf i~lt;i~lku ti.q 74 K. e. NI J:.
ima th~ ~Pje jjj,,ju~ lyll i-1 cre ",+d,
t~~p;,s -ire puinc"Pa ly 1L IJUL
td~f,

GkUGORIYBV. Iv.Y.: DOLOKkNOVA,, Ye.I.
"
Bertrandite from a tin orig deposit In central
Transbaikalia.
Trudy Min.mux. no.7:1.51--i.14 155. (MLEIL 9:5)
(TranDbaAkalta-Bertrandits)

GRIGORIYICV, Iv.1f.; DUOUNOVA. *re.i.
Joselte from a tin ore deposit In central
Transbalkalia. Trudy Min.
ams. no..7:154-157 '55. (Miak 9:5)
(Translalkall-a-Joneite)

47-
115~
Rig
241 1 5).. ~%mrlng i Ocmr I
Al; bqhv tht cm
*hAks, 4W100 Cal nk
c, ew %4ej VAUMFlto, abd ar OP ti!
at
e
tbt tbaJer ore inh birtlo"bC.Opu4mill.
!,IDPW, -adine, 4 Ard i trmir.4419 ma
a iw%ngs ia lirrh4 &4t do k"mcb, lilt fiu At,
d t to
owd lln'fi~s lat'.1arnstene -ate
so
alteri Abilwl", Asof thlomyrills, the
irto Vfi*i 1 OtIll
an
uh
I t 1111d
-Vito
O)wrBc-TpwcO
ll.,ve
t
vl~

-% u -i 'I- -T
~) e, I ;j ~ 1 0, 1~ - '..
GRIGORITIV, Iv. I.:DOIOWQYLol P"MP
"
Genetto types of tlm~ ore deposits In Transbalkalla. Trudy
KMU 29:
3&51 1156. IP (KLRA 10:4)
(b-jLnSlia*&ha--Tin ores)

A-A -A A
l1+ /1/'
V
15-1957-7-9275
Translation
frora: Referativn y zhurnal, Geologlya, 1957, Wr 7,

p 71
(USISR5
AUTHOR:
Dolomanova, Ye. 1.

TITLE:
_~ranftization o* Sandstone-Shale Rocks
Assimilation a~d

by Hypabyssal Granitio, Intrusiona (K voproau ob
assimil-

yateli i granitizatsil peachanikc)-slantsevykh porod

granitnymi intraziyaml gipabissallnogo tipa).
PERIODICAL:
Sov.
geologiya, vol 51, 1956, pp 113-141
ABSTRACT:
An intrusive granite
porphyry situated between the righb.

hand tributarios of the Ingoda
River--the Sluchaynyy and

Listvenichnyy .111pring3--is younger than
the Paleozoic

sedimentary sandstone-.4bale rocks and the great
granite

Intxualon of old KiqqWysXiy age; It was intruded along

regional zones of def rmation of folds and faults. The
t

intrusive was formed
n acomplex tectonic environment

from magma rich in volatile
constituents, particulanly
Card 1/3
in B and F; these volatiles
produced widespread assilmi-

15-1957-7-9275
Assimilation and Granitization of Sands tone-Shale Rocks by
Hypabyssal
Granitic Intrusions (Cont.)
lation, contamination, and granitization in the andogene and
exogene contact zones. of the Intrusion, The rocks of the min
Intrasive phase are chiefly porphyries with characteristic
n.et-
works of veins of quartz and microoline-I)erthite
segregations
which were ,
produced by earlier autopneutmvtolysis of the granite
porphyries. Biotite granites, leucooratic granites, and fine-
grained bio-tite granites also belong to the min intrusive
phase.
Conttuninated granitoid rocks have developed chiefly in the
endo-
gene zone of the intrunion, characterizedL by variable
structurep
texture, and mineral composition, especially along gently In-
clined contacts, Sandatone-shale xenoliths are distributed
ir-
regularly in the mass and display various degrees or
sssimila-
tion and recrystallization. Granitization of hornfelses is
man-
ifested chiefly in the fornation of quartz and
microoline-per-
thito porphyroblastst in the appearance of topaz and
fluorite,
and in the recrystallization of biotite. Reaction rims of al-
bite, quartz, biotite, and fluorite (sometimes of spatite),
or
of ilmenite or coarsely platy biotite, form about the
hornfels
Card 2/3

15-1957-7-9275
AssimilaiAon and Granitization of Sandstone-Shale Rocks by
Hypabysaal
Granitic Intrusions (Gont.)
f rag-me nts .The hybrid granites have been enriched in
biotite;
the plagioclase is more abandant and more basic; and the
content
of V, Nis Cr, and Co has increased. The most strongly
contami-
nated rooks show both grantilitic and poilkilitio textures,
Mia -
rolitic cavities are commonly eneountered in the hybrid
granite
porphyries; these contain, In association with quartz,
albite,
topazj, fluorite, and tourmaline, the ore minerals
wolframite,
molybdenite, and arsenopyrite, which formed by Interaction
be-
tween the granitic magina and the hornfels xenoliths. It is
shown that there is a high oontent of Sn in the
autopneamatoli-
tically altered *normal'* granitess a low content in the
hybrid
rooks, and a decrease In content in the host rocks
proportional
to their distance away from the contact with the intrusion.
Card 3/3 0. V. Bryzgalin

15-57-5-6499
Translation from: Referativny zhurnal, Geologiya, 1957, Nr
5,
p 112 (USSR1
AUTHORS: Grigorlyev, Iv. F., Dolomanova, Ye. I.
TITLE: The Age and Structural Position of the Granite
Intrusions and the Tin-Tungsten Deposits Associated
With Them in the Central Trans-Baikal Region (0
vozraste i strukturnom polozhenii granitnykh intruziy
i svyazL,nnylch s nimi oloiryanno-vollframovykh mestoro-
:,.hdeniy v Tsentraltnom Zabaykallye)
PERIODICAL: Tr. In-ta geol. rud. mestorozhd.. petrogr.
mineralogii
J. geokhimii, 1956, Nr 3, pp 236-269
ABSTRACT: The following intrusive formations are found in
the
central trans-Baikal region ft-he Zachiko ska a tayga
(taiga) and the Daurskiy khrebet. (RangeD: 1~ Variscan
granodiorites-and ultrabasic rocks not widespread;
Card 1/4 2) early Cimmerian (early Mesozoic; biotite
granites

15-57-5-6499
The Age and Stractural Position of the Granite (Cont.)
and other varieties forming the- "Great I'ntrusion" (60
percent of the
area of the central trans-Baikal region), dated by monazite
and
samarskite as 180 to 190 million years old (Early Triassic);
and
3) late Cimmerian granites and granite porphyr~.es,
represented by
small intrusions. These last intrusions contain fragments of
partly
assimilated vein quartz and kersantite as well as fragments
of bio-
tite granite of early Cimmerian age. The geological and
structural
position of the granitoidal intrusions of early and late
Cimmerian
age, which has a direct relationship with the tin-tungsten
mineral-
ization, associated with greisenization, occurE in those
zones where
these intrusions form cupola-like extensions into the
country rock.
A study of the jointing in the Shumilovo region in the
"Great In-
trusion't hits shown that the aggregate of gently dipping
fractures
represents a series of gently inclined waves proceeding in
two
mutually perpendicular directions and forming at thEir
intersections
a system of dome-like bends. The greisen and ore deposits
are con-
fined t~ these zones. The late Cimmerian granitoidal
intrusions
Card 2/

15-57-5-6499
The Age and Structural Position of the Granite (Cont.)
show control by large north-south and northeasterly
fractures super-
imposed on Paleozoic rocks and early Cimmerian intrusions.
This is
demonstrated by a study of the jointing in the region of the
Iqgoda
fracture (a fault) where it is seen that the system of
joints,
associated with the fracture are similar in the Paleazoic
sandy
shales and in the granitoida.1 rocks of the "Great
Intrusion" but not
present in the granite porphyries. The tin-tungsten
mineralization
of the region is of two ages: il; is genetically associated
both with
the early I%mmerian intrusive complex and with the late
Cimmerian
granitoidal masses. The older raineralization is localized
in the
cupola-like extensions of the intrusions, but the younger
minerali-
zation is associated with feather-type joints associated with
regional fractures. The deposits generally occur in the
country
rock over protuberances of the intrusives. Ore-bearing
granitoidal
rocks of both ages are over-saturated in silica, and
alumina, under-
saturated in lime, and are distinguished by a high content of
fluorine. These distinguishing features are eEpecially
strong in
Gard 3/4

13-57-5-6499
The Age and Structural Position of the Granite (Cont.)
the late Cimmerian granite porp),-iyries. The authors
state their
opinion that the early and late Cimmerian granitoidal
rocks are
genetically related and are derived from the same
magmatic source.
Card 4/4 Ye. F. M.

15-57-~-4899
Translation from: Referativny zhurnal, Geolog~ya, 1957, Nr
4,
)) 123 (USSFtT
AUTHORS: Grigorlyev, Iv. F., Dolomanova, Ye. I.
TITLE: Tin Ores Transitional Between CaS31terite-Quartz and
Cassiterite-Sulfide (Ob olovorudn- 'ykh mestorozhdeniyaki
perekhodnykh tipov mezhdu mestorozhdeniyami kassiter-
ito-kvartsevoy i 'kassiterito-sull.-Cidnoy formatsii)
PERIODICAL: Tr. "Ln-ta geol. ziad. mestorozhd. petro-r.,
mineralogii
i geokhimii, 1956, Nr 3, pp 279-301
ABSTRACT: The authors have arrived at the conclusion that
tin
ores which are transitional betweem ca;3siterite-
quartz and cassiterite-sulfide formations should be
clasned as a separate cassiterite-quartz-sulfide for-
mation. These formations are different in a number
of goological and; mineralogical characteristics. The
ore-bearing intrusives of granitoj.ds, with which such
deposits are genetically associated, are intruded
Card 1/3

15--57-4-4899
Tin Ores Transitional (Cont.)
along large regiona.- tectonic dislocations; the fissures
produced
by these dislocations contain -~he ore. The formations are
associ-
ated with the zone of exoconta,.-t -and lie in
sandstone-shale rocks,
granites, effusives, etc. The ore-bearing intrusives are of
small
dimensions and are of the "fissure" type. In composition
they repm-
sent granite-porphyries, or granodiorite-porphyr-;.es (the
Little
KhIngan Mountains), and granodiorites (Yana-Adychi region).
At the
same time, a direct genetic connection of the
caasiterite-quartz-
sulfide formations with the intrusives has been established
only for
certain locations in the trans-Balkal area; here the
association is
with granite-porphyries. Tin ore deposits of the
cassiterite-quartz-
sulfide formation are represented by network zones,
stockwork zones,
brecciated zones, fissured zones, and lenses. The mineral
composition
of the ores in the cassiterite-quartz-sulfide fo:rmations is
unique,
since it includes minerals characteristic of botch the
cassiterite-
quartz,and the cassiterite-sulfide formations. C..-iief
minerals are:
Card 2J3

15-57-4-4899
Tin Ores Transitional (Cont.)
1) ore minerals -- arsenopyrite, pyrrhotine, sphalerite
galena,
chalcopyrite, cassiterite, twagstenite, and scheelite; ~)
non-ore
minerals -- tourrialine, chlorite, muscovite, quartz,
topaz, and
fluorite. Ores of the given formation are multi-stalye.
Changes in
the vicinity of the veins are expr*ssed in greiSenization,
tourmali-
nazation, chloritization, sericitization, and
quartzification. Thus
the ores in these formations are characterized by lack of
the genetic
features of the cassiterite-quartz and cassiterite-sulfide
fannati"
This is caused not only by the composition of the
postmagmatic
solutions themselves, but also by the geologic tLnd
structural en-
vironment in which these formations originated.
Industrially, tin
ores of the transitional type represent large reserves of
low-grade
ore; they sometimes contain tungstenite and othor values.
Gard 3/3 Ye. P. M.

11, - ,- ;' __, -_ -1 -1
I j -k-[ -I. II ,I-
GRIGORITMI, Iv.F.; DOIMNOVA. 're.i.;
WAtion *f tin mineralittation to dilces in Trwisbalksliae
Isv.AN
SSIM.Ser.tgeol. 22 no.1:61,7-89 Jet 157. (MW 10:3)
1. Institut goologit radnykh voetoromhdanijr, petrogri4fii,
mineralogii
I geokhinii AN SSSR, Moskyas
(Tranv%ika1ia-TIji ores) (Dikes (Deologr))

"MR, -"I,
in, IU 00 06 devisih W MAW; Am
pm&Ar~meo~ h*ITW WAS olitmiled.
Me co4~131r~ m0sp art Intl ~:l ko'l Nt
cdiiaitiu,~: with xiwwalgiie. leM,)wA ty voOv.
mo)"ije'_ iffpIlle. L Sind Holle,13.
oft loo; k4fjin1t;4 hmoy.,31 kkiteq, .1 low -
gviTUik1N ,
- - V~.w I I
i.'
it) 4 a
6 Ilm rJolaceillcos 4& tl;L-t
mWtciftc, praicandary
sf%,"us a:n!rwmkit1!'
ivilerpovilbit %V101 it, (a In
!liap$ t0trngolw. cr]~Iso folum of pris
ImUt. uhW111n M311 i N~ 1 t3
is)36. ~Ctaorli V26314 with 01111"~ *t smt:3 04 %feall
at
41C 4 L14
!11. im wr t e I$ V, P~Pli! i 01~i polLict Of in
I orAti ty'lustt- cueltu.e
112j$. ~ d TIM i!:tj.
psc. 3.
wr o.k=d loan
vi"11 bhdoin m tIIAM4. 1,00, 1~n the
is ' r,
q1obdi1cre
WO an the )pst. ai s(Ai, AM

ii6l~w RIO 'b.;
00111 and -XV0
M&Y k4istst -tbe -mcly=044M, 110"m
rwf~;it 10 4
WOW lines 010wrWil"t"mi
pr
vutm~ - 11v0d3r$r? ve BIV'64 i0kh, 3hovf I rit lillay 'c"11; 1in
0-napi). !of midlnpnulj~' It 13mbans no tariN. ja
aul)n" rxATN)QA t )-.. C., &.5
.1 tIL -typ! tonnulae ('
or Cop Mme -irish 0,3 MVAS' MiD.
gm"' Ititats 1bu cumiAm pbassibeh,
P" A0 OR-. are *I* t vioxiab.1it, In
CA- Is- i1i)
Is m0y
to hyds*jcqj VMrdoos o ioitieokt~- 119m
1*11bisixitcd b* 16e !44"
04"At *lid sswipal exem-ita.,W #W wtadi,oin Fird-10M.
Pi, !~d,
Wal the TAbBlW4rt%
61- rp4mil sn i~"
n1k ithow an); 11M hjhtx*r.-PA e ~-Mo
Whh. kip Aul. bui I tt"~;6;pv NIS Tbos Lut I wl C rarr, C) r. f"s.
11)z 11~0 mtents are ohniho it. b3th;
W!, "Wooet. VC4)fAilks stluf~h F- which 13 mbstut
iu And tbis notam COS wLIch b 4.stvi svt':r
i1a t'1(JiL1'r Wp":t' Mn0_bCj JV.'f
-xm K.
Imm-P, iaop*44 o-AiNfer!1 I
mrtmim Tu N b Ijk[I nt~~.jj!jjjt
IfOW !';-rAV, 1101 iMfladll A-1~ ~:Zfiff~ h;3 C-3
rarp i1mm,'t'i) U.

DOLMANOTA. Tellsayeta Ivemovaal SHIPUIJX. Y.K., oty.
rod.; IVANOV, B.V.,
T--Tal mmyc
red-.jig
[Ingwla tinwolframim deposlatim &i4 thoir genetic
ch^racteriaticel
OlOVMlnnO-vOl'frAmov:r~ mestoarshAentia tng(Ainukogo
rudnogo uzla I
ikh pnotichaskle onobannosslo lloWma, I:md--vo
Akadensuk S=. 1959.
297 P, (Akedealis nm* SMv Inatitut gpol*gii rudnykh
mestoroshdanil,
petragrafii, mineralogil I geoldtimll. Trud;r, no*23J
(MIU 13:2)
(Ingodis T&lley,--T!Lzt orso)
(Ingots Valley-.1-NuWten ores)

GRIGORlYINS, I.F.; DOLCIOSOVA
Gearksite. tmdy Min.muz. nc-.10:1.8!--186 '59. (MIRA
16t8)
(Gearksite) (Transbaikalla-tiearhoutite)

s/o15/6o/ooo/ooq/oo4/005
A052/A129
AWHOR: Dolomanovas Yeo I.
TIMEt Tin-tungaten deposits of the Ingodlnifk mining field and
their
genetic chitracterlstios
PEMODICALt Referativnyy zhurnal Geologlya, *LV6, no. 9, 299,
abstract 17792
(Tr. In-ta geol. rudn. mentA)rozhil. petrogr., mineralogii i geo-
khim:U. AN SSM. 1959, no. 23, 2.9c,? piiges, Illustrations,
maps).
TECT: Tin-tungsten deposits of the Ingodinskmining field are
located In
thit rare metal zone or Ulie Tranobaikal region. A short
geological and petro-
graphiqa.1 description of the area and its taotonJ'.c
i!,tructure is given; the
petrochemical characteristics of the tin-:bearing grinitoida and
6f the sand-schist
rooks of the meso-upperp&leozoic am containing thejo are
investigatedi 'the Ingo-
dinsk tin deposits, the loevo-Ingodlnak iMu-tungal;en deposits
and the "Novoye"
molibdentim-tin -tungsten deposits are deiscribed. '11w ginesis
of the Ingodinsk de-
posits and their place In the general genetic class!Lfication of
tin deposits are,
analyzed. The deposits of the Ingodinsir minir.,g x"ield are
connected genetically
with the neokimeridgian granite-porphyries. Ibis conneotion is
proved by the
Cs.rd 1/2

YAKZHMI Alekoandr AmIreyevich, doktorgeo),min.naukv
prof. (1907-1961);
.-DOMM.-OVA MD.I., red.; WCHIMIMIVA, S.V.,, red.
izd-.va;
tiFw) ~.f.~-tWms red*
[Characteristics of the distribution and formation
of i"luorite
deposits in r,-ani3b&ikalia]:~akc-nme~vnosti
rawashcheniia i for-
mirovanila flluoritovykh rnsterozhilenii
Zabaikallia. Moskyap
Goagooltekhizdat, 1962. 249 p. (MM 15:9)
(Transbaikelia-.-Fluorite)

DKOUNOTA, Ye. 1.
Zeoliteo from the ShirlOVaylL Gors, iteposit in eastern
Tramsbalkalla.
Trudy Min.mus. no.33:172-I!78 162. (KW l6s2)
(Trawbuiltalia-Zoolites)

DOTAIM IMTMWVA, Yu.S.; ARAPYTA, G.A.
TI and Sn contafting bmi&in-tite flm the BDI'ohaya
Shirloveya
Gora deposit (eastezm Tranobsikalla)o I'mdy Him.mus.
no.23il79--
190 162, (MIRL 1612)
(Tranab&-Lk&lia-3&udan-tite)

DOLOHANOVA, Ye.I.; MOLEVA, V.A.
'k~
11 an'MV I
Ds ali ~ from the depos't of tbe
casserite-quartz-sulfide
formation in Siberia. Trady Miia. muz. no.14:215-218
163.
(KIRA 16:10)
(Siberia-Danalite)

DOLOMANUVA. Ye.I,
.1--l~m..'...
Lead-zinc mineralization il-i somo
caesiftrit"uartz-sulfide
deposits of isastern Transbaikal!~a,. Trudy IGEM
no.831468-504
163, (KUA 16:11)

ZVY&GIN, ~jbla; S(JBOLI,*VA# S.V,l MOIEVA, V.A.
Dloctahodra.1 Almmita IN h-ca the,
L#v*-Itlgcdlruik tin-tungaten
deposit in TranablOaliab Dckl. AN 88SH 165
tic.2t4lO-412
9 165. (min isili)
1. Submitted M&y 2.1# 1965b

iy, 'cn3.c chamct(Lristicn .r uf lor c1' r
r r - r r t sul--: ~il tt (,,,! p t L ~i e 1. 3 th A 11
-i () 11 c o1 I ~ r c r, s c 1 f flvi v -11 F ts o 10! f
tr
~11.111 In'tcrtirnists, 1P,59.

DOLOKINO, V., red.; YISUKO, A,, tikJin.red.
(Put chemistry to work for the good of the Soviet
people;
a collection of 14pers) Xhiiniiu - na tlago covetskogo
cheloveks; sborn1k natarialov. Simfercpoll, Krymizdat,
1958.
72 p. (MIRA 12:4)
(Chemical industries)

BLUDILIN, Vikhail Aver 'yanovich;_DOIa:IVO,
tekhn. red. red. FISENKO, A.0
(FiLin potential ]Glavnyi re2;exT,, Simfero;oll,
F:2~izdat,, 1960.
15 P. (MIRA 15:n)
1. GlavWy inzheimir KamyshInuun-skogo zhelezortidnogo
kombinnta
(fcv Bludilin).
(Kerch Peninsula-Iron taki oteel plarits-Tochno logical
in-
novations)
t
z

MA110vt VaWdy Vladimiravich; DDLOMINO, N., reol.;
FISENKO, A.)
tekhn. rod. .1 ..... I - ~ -,-. ~ --- - - . I
(Extracting large blocks]0obyeha kruprorka blokov.
Simfero It
Kryidzdat,, 1961. ." p. (MM 15: lIr J
(Crime a-Building atones)

KTIOPMR0, Ivan Androyevicb; DOJX~INO, N., red.;
POLYAKOV, I.,, red.;
ISUFOVA, V.p tekhn. r6dr--:- ---
(Making every minute i.-ount]Dccc)zha kazhdoi
irdmtoi. Sinfero It
Krymizdat, 1961. 29 :p. (KUU 15:12r
1. Direktor Simferopollskogo koxhavomo-obumogo
lcombinata im.
F.Ye.Dzerzhinskogo (for Khomenko).
(Simferopoll-Shoe industry-IjLbor p,oductivity)

.9 Petr Stepanovich, I-and, okon. naWc; DOLOP.30 V
red. 1
FESIICFMKO ==1--f -
POLYAROV) Lp red.; FISENK01, A.p tewl~'.--rec
[Towards a now upourp in slAle
i)mu ekanomiki sovkhozov; v
idku isellskogo khoziaistva.
(Crimea-State 1'&-ma)
farm econovy]K novorm pod"-
ponoshchl isuchaiunhchim.ekono-
S-."Lmferopollj, Kr7nizdat, 1961. 54
(KMA 150-1)
p.

SOBCHUKI B.A.; 401 GLAD YSIIEVSKAYA,
,OSILITSKUS-L.U. [Niloshytellcyi, L.14.1;
T.N. [Madyshavolka, T.M.]
Carboxymyoglobin in rats dmring acute carbon
monoxide-poisoning.
Mr. biokhim. zhur. 33 no.6t848-855 161. (WRA 14:12)
I. Department of Bioch-amistq and Department of
General Hygiene
of Lvov Modical Instivate.
(CARBON I-IONOXIDE-:PHYSIOLOGICAL &,eECT) (MYOGLOBIN)

VALITUKIIJ 14; PT?~TiLMMA,-1-
b'surdamentil advantages of soc.,IA.lism in
utilizing pro~luction
funds. Fin. SSSR 22 no.3%48-1,*57 Mr 161. (PURA
14-7)
(Capital) (cmiunlLmn)

ARALKIN, Iaouid Ivanovich; TALITUKH., tonstantin
Kurtovidh;
DOW.rEUWAL_y.l&a, Favlovap; MANDRYGINA, Faina
'Ilwsandrovua; PIZSHCVSKIY, B.P.,, red.; MATSUK,
A.V.,j
red. izd-va; MINA, T.D., telln. red.
[Stuly of the p-oduction or tie means of
production uniler the
conditions of Us gewral crivis of capitalism;
based an the
U.S.A.30obark vosproizvods-tva v usloviiakh
obshc]2ego krizisa
kapilAlizma; wL primere SShA [By] L.I.AbiLlkin i
dr. Ml)skva,,
VyssWa shkoltt,, 1962. 218 pt (MIIU -15:8)
(United Statep-Economic conditions)

DOLUTII-,HINA~ Z. 0.
Dolotikhina, Z. G. -- "Me Interrelatiorship between HiCh
Rye Grass and
Its Components When It is Introduced into tho Field Grass
Mixtures in Bel-
gorod Oblast." Leningrad Orler of Lenin SULte U J-meni.
A. A. Zhdanov. Len-
inerad, 1956. (D 4sseration 'For the Degree cof Candidate
in Biological c:ciences).
So. Knizhnaya Letopis 1, no. 11, 1956, pp im-M

KHODZUTET, Aj:zam Aulumpovichl DOLMIDI, Y,,, red.;
KKL'NIKOV. A. , tekhred.
(Food indust:q, of Uzbekistan lunder the sayan-year
plan] Pishche-
vaia promysbilennostl Umbekictma ir somiletke.
Tafhkent,. Goa.
isd-vo Uxbekekoi SSR, 1959. 411 P4, (mim 13:8)
Wzbekistan-Food industry)
~.i

DOLOTKAZINO A;-.A.p felldelier (Dagomys
Ilrasn&larskolgo kr4ya)
I -. -
Case of =ti= eaused by aulphur plugs in the eam. Fel
I d. i
akush. 26 no*3t/+7 Or 161, (MBA 14:3)
(CHILDRENt DUF) (EkR-ZARH AND HYGIENE)

USSR/Cultivated Plnnts. Tecl-inical I'Luits. Oil ancl IT
Subar 116aning Plnnts.
Abs Jour : Rof Zhur-Biol., No 157 3.9587 63',!(-,,'A
Author _j_.jj; otkazi
ti
porimant and Ariolioration Station
Ins t . : Kc.ra- imi H130ri,
of' the All-Union Scient-.1fic 11csoarch Distituto
of' Hydraulitic Enginacrfn~,, mCl luaclioration.
Title : Ar. Experiment in Sprin1rcling Finc-Fiber Cottor.
in Turknonistan.
OriC~, Pub: Khlopkovodstvo, 1957, IT(-) 51 514%
Lbstract : In 1956, at the Moslwa kolldicz in Mary
Oblastt
a fi-AC oxi)crimont vas conducted by tho Kar,~.-
Ku-i Exporinunt Ni(-l Anclioration Station ~,f tho
.Pd:L-Union Scientific Research Institutu, of Hy-
dri.iulic Enginooring an,,' Amolioration. Sprin-
eased cotton yields bY 3,7 c.-mtners/
Ulm incr
Card : 1/;)-

USSR/Cultiv.-Aud Plants. Tr;chn:Lcal Plants. Oil and
Sugar EbarIng IInnts.
Abs jour : -Ref Zhur-Biol.) Nc) 15, 1950, 68203
hcc-:,!.ro, as conpa-rc-d with natural irrigatioa~
-in-,9- thu cxpondituro of i!- er vas signi-icantly
lov.,or. Plants d-mclopcd sir.Alarly und..,r both
methods of irri~-ationj but on tho sprinkled
plots: tho plants prcsarvod , lz,,rf;(.,r nivibar
of saodcasos. -- A., M, Smirnov
Ca r (1 2/2
112

DOMTKAZIN,joYaos imahe
Results of eiperiviente In sprinkler Irrigation of
cottons Trudy
VINGIN 32:5"0 159. (MIRA. 13:8)
(Cotton-IrrIgation) (Sprinkler irrigation)

AUTHOR: SOV/94-58-11-9/28
Z'huravlev, P.A.
Kuznetsov, I.IL
Kogan, G.M.
Kondakov, Yee-.A.
Nesterenko, P.S.
TITLE: The Inst till at ion of a Radiation Recuperator on a
Cupola
(Ustanovka radi&tSionnoj:,o rekuperatovt nj vairw3ke)
PERIODICPL: Promysh1pnnaya Bnergetika, 1958, '1 19. (USSR)
Nr 11 , P
ABSTEUCT: This st4-,r;estion was aw&rdel a fifth previi-am
in an
All-Union Power Economy competition. 111tberto little
use ;:ias been made of waste heat from foundry cupolas
largely because the heat exchangers become dirty very
quickly and therefore inefficient. Metal radiation
recuperators of simple construction have recently been
used abroad for this puxpose. The authors proposed the
installation of radiation recuperators for heating
blast air on two oupolao of' 18 tons per hour upiva,:7d.s.
A sketch of thol equipment is given. The reci:Lperutc-r
Card 1/,> consists Df two Metal tubeE with an annular gap of

SOV/94-58-11-9/*')3
The Installation of a Radiation Recuperator on a Cupola
P ITIM, the rectvperator is 6,000 mm high and
congtructional details are given. The method. of
installing the device is briefly described. The
equipment laas proved satisfactory in service and
economises about 1,180 tons of coke a year.
There is I figure.
Card )/,>

all
A JAI

DOTAMT. 0.P.. inzh.
N -
-I
Safety measures in using natural gas in furnaces and drying
alprparatua.
Bezop.truda v prom, 11 no.80.5-18 Ag 159. (MMA 12 i'11)
1. Avtonobillun savoil la. likhachava.
"k0alls latill-al-Wety IMAllures)

DOWiv%lp 11 G.P.
Using natural gas to hea-4 b1a3t air in cupolas* Gaze
promo 7 no.5s
39-41 '62, (MIRA 17:11)

MARIYENBAKH, L.M., doktor tekhn.awks prof.j DOLOTOV,
O.P., insh.
Using natursI 11as for 11110ijUng cast Iron,
Vsatmashlnostr, 43
no.8t65-70 Ag 163. (FaRA. 16:9)
(Cast iron-YAttallurgy-) (Gas, Natural)

MARIMMAKH) L. M. ; DOLOIXV) G. P.
"Die praxis und die perspektiive der answendung des
naturE;ases bei dem schmelzen
des gusseisens."
paper submitted for 32nd Intl ConS, Foundry Congress, Warsaw,
13-17 Sep 63.

POLOTOV, G.F., kaild. takhn. nauk; I-VAIDAK017,
Ye.A., inzh.;
zwlvov, B.P., inzt,., retsonzant, F'-TLll-'CI!OV,
7u,'?.,
kard. tekbn. naukp red.
[Design ard calculation of IndustrIal furnaces and
driers;
foimdry furnaces] Konstruktsi~a i raschet zavodi(ikh
pechei
i nushil; pechi liteinykh tsckhav. Moslwap
Mashinoatroeniep
19!55. 23EI P. (ml 11A 18: 8)

13AM; s.Ye.j-TLX~..Gop*
Sr,slting Gawt Iron tviLng natuml PO& GusPrOO6 3.0
noa2t27-31
165. OURA 10112)

DODDTOV I .
Deviation of mapetio compassms. Mor. flot. 24 no.5t
17-18 W 164. (MIRA 18:12)
1. Starshiy deviator Leningradskoy bazy Okeanrybflota.

!pi
~ Hl.
; P

MRI'AilOW. Yevileniy Ivanovinh Dt,WT-'fV. Mikhail
filkitovich, SIA'S"Tty,
P"trovieh, '.11~101910VA: T01,111M, r.71., tekhnaod,
NIT-2 and UET-2w cutter-laadotrsl )Yeol'Ve kombainy
UFT-2 I LW-22.
VoR "ca, Ugletekhlzdtit, 1951o 191 P.- (PM 13:8)
(Ccal mWirg mftehl-abry)

I III & K 0
FaTplosive Mithod of caving in Clines or maelvougo.I
OohbLne,
awl Mcl M-5,51775-r. 1952, 18-21).
The motbod Involvos 111thoraving antl do-4ollabing
others.,
It la Cavoribad In detdil. Tius cud timbar are saved In
comparison with
the hand mothod xwed proviously. (1)
iweOsate SDurco clipping

DOLOTOV N P.- MDaEK(YPA, V.A.- SINITO, A.I..; BABOXIN,
otivtetTemiy7 rail.;
IIIWAMW"N Z i ~OR OVA' Z.A., i"O'L;. red.
(Handbook for workers and minor grede inspectors in mine
transpor-
tation in the Moscow Pasizill Phmisftn dlia rabochikh i
mle.dshego
nadzora uchatitka vmitiisha)dmtUOgD transporta
Pbdmoskovnojv basipelua.
Koi3lcva. Ugletekbiz&A, 1953. 22 p. (MXBA 11:7)
(MOSCOW Basim.-Mine haulage,)

IUIZNIIOV, G.A.,ot,vetstvennyy redaktor;
OKHRIMMO, T.A.,radektor Isdatelletva.; NADZINSKATA,
A.A.,
takhnicheskiy redaktor
(Manu4l on longwall work in the Moscow Basin]
Plantatft rabochago
lavy podmoskovnogo banceina. koskva, Ugletakhisdat,
1956.
174 p. (MIMA 10:5)
(Koscow Basin--Coal mineB and mining)

DOID". N.p ~
Industrial training of N*scow Basin miners. Dexop.truds
v prom.
I no.7:6-7 JI 157., (KMA 10:19
1. Glavnyy Inshenor uprairlonlys,fullskogo okrugo
Goegortekhmadsora
SSO.
(Nosoov Daeln-NIning ongineeriW-Safety measures)

DOIDTOV. N.P.. insh.; ZABIAVSKIT. P.M., lnzh.;
ILITSUNDY, V.I.. Inzh.
7. ...... wWASWWV"-l.--..
Observe safotr r-lquirsivents In designing machines and
macbantorlot
Bezop, truda v pron. 2 no.7M-16 JI 158. (MIRA Ilig)
(Coull miuing mcbinory)

NECHIP)RENKOV M.M., im%4.1 DOLOTOVI N.P.0 insh.
Safety z"sureo in mines of the Moscow Basin*
Dezop.truda. ir prCu.
4 no.6:25-27 J9 160* (mift 34:3)
1. Upravleniye Tullskogo okz-uga Gosgortekhnadzora
RSFSR.
(Moscow Basin-Coal idnes Wid mininh-4Mfety measures)

NECHIPOPMXDp H.M.;jpjpWV,_N'p,4, Insh.j SUBBOTIN., A.A.,
Geroy Sotsia-liatichav-
kop truda; TERMXOV., P.R.,, Iaux-sat lenl*Bko7 premil
Effective methods for imprimrhig work sanitation in
mining* Bez6petruIt
v prom. 6 no.7:" J:L 162. (MIRA 15:7)
1. Rachallnik Upravlemiya, TVL'skogo okruga
GoBudarstvennogo komiteta,
pri Sovete Ministrov 43FSR j* nadzoru, za boxopaortym
vedeniyem rabot
v jxromyshlennosti i gornomu wdsont (for Nechipor-enko).
2. Nachaltnik
Tallakogo koDibinata ugollnoy prompdaennosti
Podmoskovskogo basseym
Misisterstva ugollnoy promphlennosti SSSR (for Subbotin).
3. Glavrqy
inzh. Tullskogo kombinata u4jollnoy prmyWennost-I
Podmoskovskogo
basseyna Minlisterstra vgollroy protg7ablennosti SSUR (for
Permyakov).
(Tula Province-Coal mimas and minirig--Safety measures)

SUBBOTIN, A.A., rzeroy Sotsiallotichoskogo Truda;
FEWAROV, P.11.2
laureat 14ninskoy premii; NWHIPORERO, M.M.; TLOTOV2
II.P.
Mach4nization and automation in mines of the
Priokskiy Economic
Council. Benop-truda v pram. I no.41-2-3 Ap 163,
01IRA 1614)
1. Xachallnik Tul'skogo kowbtna-bt qvllnoy
prawahle=osti
Padmos'wmogo baeseyna Min:Lstsrstva ugollnoy
promrshlormosti
SSSR (for Subbotin). 2. GlavW insh. Tullskogo
kombinata
uxolsncly proWshlsrLnosti 1))d;vozik-vvncgo baa
OOYTIa Ministerstva
ugolittoy prcayahlonnosti MISR (ftrr Ferayakov). 3.
Naebal'nik
Upravlaniya TuVakogo Arujita %ndarBt-vsnnogo
komiteta pri
Sovete Hiniatrov RSPSR po naftoru sa basopaonym
vedeniyem rabot
v promychlennosti, i gornomi indzorn (for
Nechiporenko). 4. Glav-
nyy insh. Upravleriiya Tulleikogo okruga
Disudarstvannogo komiteta
pri Sovete Ministrov RSFSR p) nadsoru ma basopasnym
vedeniyem
raIxit v promyshlennosti i gornoma nadzoru (for
Dolotov).
(Tula Province--4',oal isines and mining)
. (Autowtion)

STARUMMA, A.D,
Causes of accidents and traumatIsn at ebemical industry
enterprises. Bezop. trudiL '? prom. S. no.9.-22-24 S
164
(MIN. 18t1)
I. UpravlenlyA Tallskogo oltruga Goa-adarstirennog,
kcm-.lteta pr4
Sr Ae Ministrov RSFSR po nadzoru -,& bezopasny-n
vedenlysm rabot,
v prmyshlennostl 1. gomami naftcri.

M. m I rah. M I OIDM ~ NJ
Water supply for m!ne fl.~:-es in the Mc;sz,)w
?;tsln. Fv-.~Z,P. r"lca
prc--. 9 no.12.16--18 P '64. Ov " RA 18 3
',Nil I skc8cy o irugFA It cm,. teta
-,adz,-,ru i,,

ACC NRt U-1 /000y'006/004 OPWOL
/0314/65
AUTHOR: K zub, V. S. (Candidate of chemical scitincee); 121.1
atova,_j,- ~- (Engineer)
ORG: none
TITLE; Corrosion of metallic m&terials in th-i produ..Ntion
ofAjph,!!i
SOURCE: Khimicheakoye i neftyanoye mlishinost:roye~iy3j no. 8,
196.5, 40
TOPIC TAGS: corrosion, stainless steel,, alumLnum, titanium,
nickel, copper$
organic syntht~tie process, alloy, distillatiolip corrosion
resistant alloy/NIKW10-20
alloy, lKhl8N9T stainless steel, KhIMM-2142T sl;aix~Lese steel,
Kh2lN14D stainless
steel, M311428MN3'r stainless steel \%
ABSTRACT: The norrosion resistance o:r kl_JA
.&0) (AD-1)1~ Tl._(V.rl)o Ni'p C~
20%nd stabiloss steels A
were t,
tudied in the wmthei3is, dAstillatior. '-Md purification
processes of diphonylolpropane. Tito zlipecimemi were tested in
the following
media corresponding to these processest phenol / DF3 (2-5%), t
90-1200C
(in the liquid and gaseous phases); d1phenolpi.-opane C16CODH
impurities,,
t - 80 C; dipheny1c1propano / water ~ intpurit:,es, t 1000G.
For the
synthesis and distillation processes the most stable material
both In the
liquid and gascouA phase is aluminm gmde A4:* (grade AD-1 was
lose stable)s
Also) the results of toots indicated that an increaeo in the
medium tem~pera-
.turo from 90 to IVIC does not affect -the con;tsion rate of
the materials
UDCr 620.19!1:546.62lt74:669-15:547.62

AP6014665-
AC C ~1
studied. _�j4jnjm- steels and litmlva. are corrosion-resictant
miterialii in a
solution of 30% acetic acid with imptvIties of' phenol, borcn
fluoride, wid resins.
In the purification of-diphenylolpropano froin residues of
phenol, 'IF and resins
containing water vapDr, an aqueous Bolgtion 1)f phenol and
hydrofluOric at',Ad is
formed. In. this meditun copper and steAttless steels
Kh23N28H3D3T and Khl#Nl2W.T,
alloyed with copper awl molybdenum and, possessing high
resistance f.n hydrofluoric
acid, are corrosion-resisting materials., Th,as the tests arxi
resul4ing d&ta pervat
the recommendation of the metals ae structuriLl materials for a
spe,:-,ific process
in the production of fiphenylolpropane;s Orijg4 art, has: I
table. [JPRS3
SUB CODE: 139 07 SUBM.DWE: none WIG MY 1 003
Card 2/2_

DUMOT, V.A.
Genesis of mount &In-stoppe friWmntary soils of ropat
Dagh Evith
summry in ftlishl, Pballyovedenie U0.706-41 JI 158.
(KIRL 110),
1. TSentzi6lljqy Wrey poohvvveideniya is. V.V.
Dokachayeva AVmAsmij
nauk SSSR, LenlAgmd. (Kopet Dagh-Soll fbrmation)

~C- DOLOTOT, V.A.
Agricultural
TSentre wise
utillsation *f solls Lm VologU Province. Sbor. rab.
pwhvo no.,'4192-2(e l6o. (KIRL 13: 9)
(Vologda h-oviuce-Soilm)

ZAVALISHIN, A.A.; QQL2TOV, V.A.
In mmory of Konstantin Dmilxlevich Glinka.
Pochvovedenie
no.9tll7-* ' S 162. (MIRA 16:1)
(GUnka, Konstantin Dmitrievich, 1867-19r)

DOLOTOV, V.A..
FragmenULl soils as a growth medium for
tragacanth-bearing
milk vetches in Kopet-Dag, Trudy Bot, inst. Ser. 5
no.11:
212-228 163, (MIRA 16:10)

DOIDMVI, V*Ae
Studying soil formation cf arable lands in the east of
the Ruasian
Plain. Poehvovedenie no.901-38 Ag [i. e. S1 163. (MM
16:10)
1. TSentrallnyy muzey pochvovedeniya imehi V.r.
Dokuchayeva.
(Kirov Province.-Soil formation)
(Udmurt A. S. S.. It.-Soil formation)

DOLOTOV~ V.k.
Effeot of cultivated plants on soil, Bote Shur,, 48
no.lOtl495-1499
0 '63. 1 (MIM 17:2)
1. TSantrallnyy muzey pochmmedaniya imeni
V.V.Dokucbayeva, Leningrad.

DOLOTOV, V.A.
Recent data on the liming Of acid Boils. PrJroda 5),
no.7:22-23
J1 165. (MIRA 18:7)
1. TSentrallnyy muzey pochvi3vedenlya Im.
VOT.Dokuchayeva, Leningrad.

Le.i Livin - -,y ng
~ciiull. ni .1 4:

110 1 QT0. '~"A V -I C*,, - I i, 1 N I KO V, F. N'
P, .
Adaptabillty and r-liabillty of (in rtutommitic
crnt.~-..
Trudy MFI 5201-84 163. (V]-IA Iq,"l)

000 ODOIA019/AOlj~
AMMON
-M AW0565
b.)
-SWRCE: Rot,, Sh. AyUmat talmkh i - v3iLA i0lo" - takhn 6Svodnrr tom,
Abs. SA133~
AWHOR a Mlotov, V i,,04 TOM0.10 16, 1
OWN A-.,
TIME: kdaptabillty~ and -rellabilAty.of a_~dlllrlter-
1963 95-106
CITED SWRGS: Tr. Fwsk. energ4 In- 0 t 1: . , : ,
vy I i52
TOPIC UGSj nass !j-0onutioli w9r"tionl ~f irodessi.ng, industrivil
aulomatic control i,
Supervisory control
funimmital uwlts intended for a:
TRMSIATIONs -The rwults ..t?f a develLopment tif
Usterm of contralJmDd are reported
A piant--41,-ia lnfcrmat-lor. ietw:)r.k enc0-_Fz&-jsns all
department,33. devices that Callect
, r: -~;._rv I n " - =,-a t ~_~~n . 7h 1 q natiark pipes tio? fintA re
-1,-Lf, r7na t 1, nT.
r. appara*_aa Viich deLermine Ui- :irrivral inc ~r
about the entiro procoan zycle are located. The 3j.rU0tL1!'e is i~~
tion is de.9cribed of a cmitral cade-scamJ-.ig gemarator (CM) 'Wid n
switching anit. The CS0 produtes, in -the immon InforMILUOn netwoik,
cont- lnuousi~r
n1rcula-Ung code su=3. The oode scans rei.*Divad at the depar,=ep,tk,'L
pointz; Wle
nsed Xor vrotting up componsating aigrials of any pbysicianatiara,
J.'he central-
1/2

-65
L 51857
'AWESSION M: 4R4046%5
-anlt -pirTf=2 of tsen-sors At all departmental;
points. The problems of adaptabIlity of the '4T;serrrotekhaika-3"
cenLralIzed
info=aIt-11-on nyst,~m to t1w condAtlow of production are discussett.
In such sysLoms,
an wmntita redistr',.birAor. and degeneration of apparatao, ao
coTFarod to
1decentraitod and local zMtumt, 191m,plate, Oray the elomon,-W
dl.-PoL~y
with the procesBJ~ng, Buch as sansors and actuatorap re=ln near tho
pmduction
machineal sLI1 oiber apparatae itre-mved to Cho canter. Reliabil-ity
of Emch centers
Is discussed. Eight I title.
-'DP 7
SO 4GODEs V- M
I Card 2Lt2