SCIENTIFIC ABSTRACT BRAZHNIKOV, V. V. - BRAZHNIKOVA, M. G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000206820007-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 9, 2000
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

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Modern Units (cont.)
SOV/3222
tance of introducing modern refinery equipment into plants.
Domestic and foreign refining units used in lubricating.oil
production are described and their flow sheets and yields pre-
sented. The book also ncntains sket.ches and descriptions of
basic equipment secured from working drafts, planning organi-
zations and from other available data in this field. Methods
for estimating production costs and nonstutiption rates are listed.
Included also are flow sheets and descriptions of standard
refinery equipment used In lubricating-oll producing units.
The author thanks engineer N.P. Malinovskaya who wrote the
chapter, "General Refinery Facilities Used by Lubricating Oil
Producing Units", and A.I. Skoblo and B.I. Bondarenko who
reviewed the manuscript. There are 42 references: 26 Soviet,
14 English, I French, and I German.
-TABLE.OF CONTENTS:
Foreword:
3
Ch. 1. Atmospheric-Vacuum Pipe Stills 5
Atmospheric-vacuum pipe still (AVT) for lubricatii,-ig-oil pro-
duction (Type 1) 5
Card 2/10

Modern Units (Gont.)
Crude oil and its products
Flow sheet
Basic apparatus of a unit
Consumption estimates
Equipment layoiit
Atmospheric-vacuum pipe still (AVT)(q-~rpe 11)
fjrodu,~,ts
Crude oil and its
Flow sheet
Basic apparatus
Consumption est'imates
Equipment layout
Principal flows of crude oil and
Control and measuring devices
SOV/3222
of intermediate products
Units
propane
Ch. 2. Lubricating Oil Deasphaltization
Lubricating oil deasphaltization with
Flow sheet
Material balance
Basic apparatus
5
6
12
15
15
17
17
17
22
31
32
32
33
36
39
39
44
45
Card 3/ 10

Modern Units (Cont.) SOV/3222
Basic equipment 67
Consumption estimates 69
Layout of apparatus and distribution of equipment 71
Connecting basic apparatus and equipment by piping 72
Control and automation of the process 6
Two-step deasphaltization ~O
Modernized deasphaltization prooess 83
Flow she--t 83
Ch. 3. Units for Refining Lubricating Olls with Selective
Solvents * 86
Refining furfural lubricating oil 87
Flow sheets 89
Material balance 100
Basic apparatus 100
Refining lubricating oil with dual solvents (duo-sol process) 102
Flow sheet 105
Basic apparatus 108
Refining lubricating oils with liquid sulfuric anhydride 110
Card 4/10

Modern Unltr~ (Cont.)
Flow sheets
Material balance
Basic apparatus
Refining lubricating oils with phenol
SOV/~222
Flow sheet
Material balance
Basic apparatus
Control and automation of the process
Hydrolic sealing systems of stuffing boxes of pumps
Ch. 4. Lubricating Oil Deparaffinization Units
Deparaffinization of lubricating oils in a MEK-benzene-
toluene solution
- Flow sheet
Two-step filtering
Material balance
Basic apparatus
Consumption eatimates
Pumps and their connection lines
Layout of equipment
112
l16
116
117
119
124
124
145
149
151
154
154
160
164
165
188
189
192
Card 5/10

Modern Units (Cont.)
Control and automation of the process
Deparaffinization in "reverse order"
Flow sheet
Material balance
Lubricating-oil deparaffinization with propane
Flow sheet
Material balance
Basic apparatus
Deep deparaffinization of lubricating oil
Flow sheet
Material balance
Basic apparatus
.Layout of equipment
Lubricating oil deparaffinization
Flow sheet
Material balance
Basic apparatus
Lubricating oil deparaffinization
Flow sheet
SOV/3222
with dinhloroethane
with urea
193
197
197
200
200
201
201
2o6
2o6
207
210
213
213
214
215
218
218
218
220
Card 6/1o

Modern Unit- (Cont. ) SOV/3222
Materiai balance 222
I*nert gas systej,,i 225
Cooling unit 231
Ch. 5. Unit for Paraffin Produotion 238
Deoiling deposition of sludge or petrolatum 238
Flow sheet 240
Material balance 245
Apparatus and equipment of the unit 248
Consumption estimates 253
Layout of apparatus aiid distribution of equipment .255
Filtering through bleaching olay 255
Flow sheet 255
Material balance 257
Apparatus and equipment 257
Consumption estimates 260
Adsorbent regeneration 26o
Flow sheet of the unit 26o
Basic apparatus and equipment 264
Consumptlon estimates 267
Card 7/ 10

Modern Units (Cont.)
Continuous filtration througsh bleaching r~iay
Flow sheet
Basic, ,-,.I)paratus
Paraffin distribution
Paraffin distribution seotion
Consumption estimates
Continuous molding of I-nraffln
Ch. 6. Units for Final Lubricating-011. Refining Process
Contact refining of lubricating o1i by nieaiiq of bleaching
Flow sheet
Material balance
Apparatus and equipment
Consumption estimatea
Layout of apparatus and distrIbntIon of equipment
Clay preparation
Flow sheet
Refining by means of a filter
SOV/3222
268
270
273
274
274
277
277
282
clay 282
283
286
286
297
298
300
300,
301
Card 8/10

Modern Units ~%Jont.)
Hydrogen treating of lubricating oiI
Flow sheet
Ch. 7. Vacuum Concentration Unit
Flow sheet
Material balance
Basic apparatus and equipment
Layout of apparatus
Consumption estimates
Control and automation of the process
Ch. 8. Lubricating Oil Compounding Unit
Flow sheet
Material balance
Basic apparatus
Consumption estimates
Distribution of equipment
SOV/3222
305
308
308
3o8
311
311
314
314
316
3.18
320
321
322
325
325
Ch. 9. General Refinery Facilities Used in Lubricating-Oil Pro-
d:ucing Units 327
Tank farms 327
Card 9/10

Modern Units (Cont.)
SOV/3222
Standard refinery pump houses and fin1shed product pump
houses 329
Standard refinery piping 330
Standard refinery equipment used for the deasphaltization ixnit 332
Tank farms for products from selective treatment units 341
Tank farms for products from deparaffinization units 346
Tank f arms for prodticts from vacuum concentration units 347
Tank farms receivIng products froin conLact treatment units 348
Tank farms receiving products from labrAcating-oil compound-
ing units 349
Tank farms receiving products from tYie paraffin producing/
unit 350
Storage tanks for special reagents 351
Bibliography 352
AVAILABLE: Library of Congress
TM/jb
Card 10/10 3-22-6o

ROGINSKIY, S.Z.; TANOVSKIY, M.I.; LU PRY-CHZHAN; GAZIYEV, G.A.; ZHATJROVA,
G.M.; KADJOATS1, B.M.; MAZHNIXOVL V.V YMARK, I.Ye.;
PIORTKOVSKAYA, M.A. t; JIF
Chromatographic determination of the adsorption isotherms of
gnaes and of theEpecific surface of solids. Kin.1 kat. I
no.2:287-293 JI-Ag 160. (MIRA 13:8)
1. Institut fizichaskoy khimii AN SSSR.
(Adsorption)

B./B067
AUTZORS. R.gi-kiy. S. Z., S-t,r of I.E. is -::,3.
lano-kiy. U. I.. I. Ny-chlh~.. C-tyw.. G. A.. Ztuabro a,
B. X.. .1.1 Br,.hntk~, -T. 1.
T=T.X, Rapid -,11; 1 hod of Measuring the Adsorption
of ..- p.r.
FELIODICLI., DcklaJY Akd.Ait took SSSR, t960, V.I. 133. So. 4.
pp. 675.881

" ' of t' ric,
O'
To 3L.C. In heterogeneous catalysis the dim*'
'
T
E
l
p
w
:.
b
:
ou f... axs of great Import" t out . at 1. pt:d to d
1
. rapid
t-'
T
w
Their studies were 0
h"
t ci;Ic
:.rf.
-
,
..
-
4 Of 4-t-11-1-6 th
';'
relation between the C
cato
I) her. lh.
:f
P. by J. 1. Wil.. (it . h a -
pw
r
grap1ml m urw. and the form of the Louth" = 1. theoretically studied. ?h.
result a ,are compared with those .f tbe or alry, .... u. PLC. I
b0
,
th. ..he.. of the ..p-rl-tal T& rstu, Th. gas :. I
Y;.r -- an
I:
~
:
.
r tLon of
iont tion detector an the-buts of P.
(R.f. 5). Th. d
.
haptans was mossured. Nitrogen and $castle*$ argon were used as carrier..
Card I'A

Th. height or Vio stop. recorded ... r-po -tratlo.
Z's 11 the

'
the ad rbat.. fte desorption C-irvt. recorded .0 bl p-
m
4
1
:
er gas through the column P-it too c.l."ItAt.4 or it. toot h.-I
lag of adsorption. I . . . wXlo,ti.. of this ..th.4 it%* column, is cot
but the .ampl. is p.riodIc&I ly injo-te; into t hs colm,an Ug
.1d.h the -,rrI or .a fl ..*. The -Pri- t than '"'1 *4 ZY 10-15
11h. assumption of - t-di 11"Y bll,h*4. .I ib.-
,
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~
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adsorbed by I a of adsorbent (amcle/C) Is which C I. the oyillbri-=
:c-.stratt A; k is the cometsat of the detector -c-)t - is the
:
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recorder tapol C is the eight of the adsorbent (g); and Si
1:
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o ..... Th. to " , -,d,
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e
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hyd razido Sol nick .tly )'go rod-.d fro. NS(SO,),. ZnO-14-5 Z.50,.
p
WW arbs. black. ?h. "I... for Ke. silica Cal T , nickel hydroxide, and
dJ.'OKIt .. " In good &6r 4MOnt with those obt.1n:d by the ".-
two hotiqu: Par odiortoMts :ith a large number of very narrow parts (active
Card 214

ho~rw-lrw were -s-tI3 t-- ~. f, If the
I rj
"-Is xth.d -.' to f Z'-b-r '-'!led- Th- -ut!.-' -~ k
. an, r-kly f,r fro; or I" th. C.,,,
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.1lica, get To and, mick.1-hydr-11. :her- ar.
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3/MO/60/%33/OC4/CLO/%=
BOX/W67
R~M

B017/BO55
AUTHORS: Gaziyev, G. A., Yanovskiy, M. I., Brazhnikov, V. V.
TITLE: Simplified Chromatographic Method for the Determination of
Adsorbent and Catalyst Surfaces
PERIODICAL: Kinetika i kataliz, 1960, Vol. 1, No. 4, PP. 548-552
1
TEXT: A simple and rapid chromatographic method for the determination of
adsorbent and catalyst surfaces was developed. The surface area was found
by determining the vapor volume of reaction products adsorbed on
adsorbents and catalysts at fairly low concentrations. Fig. I gives a
scheme of the experimental arrangement. The surfaces of adsorbents and
catalysts were calculated by the equation Sg . A . V 9 (5), where S9 is
the specific surface and V 9 is the specific volume of adsorbed vapor. The
method was tested using various adsorbents and catalysts and the results
are listed in a table. The relation between the surface area of various
adsorbents and catalysts and the volume adsorbed, as determined for
S/195/60/001/004/007/015
Card 1/2

Simplified Chromatographic Method for the S/195/60/001/004/007/015
Determination of Adsorbent and Catalyst Surfaces B017/BO55
n-heptane, is shown graphically in Fig. 3. Experimental and calculated
values are in good agreement. The dependence of V9 on the amount of the
liquid sample introduced is shown graphically in Fig. 4. According to
Table 5, the experimental and calculated values at various carrier gas
velocities are in good agreement. N2 or Ar were used as carrier gas. A
linear relationship was found to exist between the adsorbed volume and the
specific surfaces of the adsorbents and catalysts. There are 5 figures,
1 table, and 10 references: 3 Soviet, 2 US, 1 British, and 3 German.
ASSOCIATION: Institut fizicheskoy khimii AN SSSR (Institute of Physical
Chemistry of the AS USSR)
SUBMITTED: April 28, 1960
Card 2/2

SAKODYNSKIY, X.I.; VOIZOV,, S.A.; MALAFEW, N.A.; zwwixovlj~ Me.
2MVeROWKUV,, N.M., alcademik
Separation in preparative colimns. Dokle AN SWR U8 no 2&391+-
396 Ja 163* NM 16%2)
1. "iziko-khimicheskiy institut im. L.Ya. LnTova.
(Gas chrcmatog-taphy)

KAZAKEVICH, V.Ye., WZFINIKOV,.,V
_,,V.; VOLKOV, S.A.; SAKODYNSKIY, K.I.
'Automatic samp-ling in preparative chrombtography. Khim.i tekh.
topl.i masel 8 no.llt49-52',,, N. 163o (MIRA 16:12)
1. Fiziko-khimicheskiy institut im. L.Ya.,.arpova.

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L 07893-67
ACC NR& A1602l635 SOURCE CODE:
00 6/o2O/C,03/0279/0281
AUTHOR: Drazhnikov Ye. M.; Dzantiyev, B. G.; Popov, V. N.; FrusGiyan, Ye. X.; Shalc,
,.I
A
meyev,
ORG: none
TITLE: Installation for the investigation of processes
der laboratory conditions
SOURCE: Atomnaya energiya, v. 20, no. 3, 1966, 279-281
of chemonuclear synthesis un- I
.Xnthesis, chemical energy conversion, fission product, radia-
TOPIC TAGS: chemical. s-
tion chemistry/ KhYaU-4 chemical synthesis unit, IRT nuclear reactor
ABSTRACT: The article deals with a -oossible direct 'use of atomic energy by trans-
lorming the energy of the fission fragments directly into chemical energy, bypassing
intermediate energy forms such a smeclianical, thermal, or electrical. In such a pro-
cess, a mixture of simple gases passes through a chemonvelear unit, Vfnich is essen-
tially a flow-It-,hrough fuel element. The radiation produces radiation- chemical reac-
tions that produce the end products. An example is the production of N02 from air
under the influence of radiation. The authors describe special devices for the pro-
duction of chemonuclear synthesis constructed at the institute of Chemical raysics
;! intended
All SSSR, in particular a circulating chemonuclear
to investigate synthesis in the gaseous phase under laboratorl conditions. The ap-
paratus constitutes a closed loop in which the gas mixture is circulated by a com-
uDc: 621.o39: 541.15

L 07893-67
ACC Wq- AP6021635
pressor. The products of the chemonuclear synthesis are produced continuously as the
gas mixture flows through a thermostatically maintained irradiator located in the
vertical experimental channel of a research reactor. The irradiator tubes are filled
with finely dispersed nuclear fuel, such as glass wool containing U23-5, Blo, or Li".
Another version of the irradiator, in 'which the fuel is deposited on discs, is also
used. The reactor products are extracted from the gas mixture in a block of traps.
A filter block decontaminates the gas mixture. The apparatus can also be used with
other sources of ionizing radiation (electron accelerator., cyclotron, or cobal instal,
lation). The apparatus described was tested with the electronic accelerator of the
Institute of Chemical Physics AN SSSR, in the IRT-1000 reactor of the Institute of
Atomic Energy im. 1. V. Xurchatav, and in the IRTL-2000 reactor of the Institute of
nu
.Ruclear Power AN BSSR. gie ex]~eiiments have shown that the KhYaU-4 apparatus permits
investigation o? chemonuclear synthesis processes in various gas systems. Orig. art.
has; 3 figures.
SUB CODE: a8/ sum DATE: 14Aug65/ oRiG REF: ooi/ om w: ooi
~Z1 o6,-

BRAZHNIKOVA, A.V., akusherka (Bizhbulynkskayn rayonnaya bolinitsa Bashkirskoy
Case of malformed fetus* Felld.i akush. 23 no.6:53-54 -Ye 158
(MIRA 11:6)
(LABOR, COMPLICATJW)

POLESHCHUKI L.M., kand.tekhn.nauk; fW=IINIKOVA LV Inzh.
I
4
Clarifying slurry from electrode manufacture by means of
centrifugation. Vod. i san. tekh. no.12:15-16 D 162.
- (MIRA 15:12)
(Centrifugation)
(Sewage-Purification)

BRAZIINIKOVA, E.F.; "JABINOMM, S.V.
Characteristics of the position of periqslw-ong of spectral binary
orbits. Astron. zhur. 42 no.3-.678-679 My-is 169~. (MATU 18 5)
1. Moskavskiy gosudarstvennyy pedagogichoskiy ln3tit~.ut irreni V.I.
lAnina.

RUDZIT, E.A.; BRAZW..',IKOVA, J.D.
Effnct of synthelio antinooplastdc proparat"cii,,t rn the d4jhyd.:-ase
activity of the extracts of normal aid twnorcus tissue3. Vor. onk.
11 no.6.-58-62 165. zv-m
1. Iz laboratorii khimioterapil (zav. - kand.med.naa- E.A.Rudzit)
Novokuznetskogo nauchno-lssledoratellskog~o -K:,i."lii4l,r,,-farmatsevi,iche:~kogo
instituta Ministerstva. ?dravookbruneniya W.r. 1,and.AnIm.naul;
A.G.Nehenkin).

BRAMNIKOVA, L. A.
Brazhnikova, L, A. "Respiratory change of duck eggs during incuuaticn,
Tfudy Wauch.-issled. in-ta ptitsevodstva, Vol. XIIL, 1948, p. 240-65
SO: U-2888, Letopis 4hurnalinykh Statey, No. 1, 1949

13RAZiiNIKGVA, L. A.
Brazhnikova, L. A. ItIncrease of effectiveness of goose egg incuuation," Trudy
Nauch.-issled. in-ta ptitsevodstvaj Vol. XIX, 1948, p. 266-91
SO: U-2688, Letopis Ztmmallnykh Statey, No. 1, 1949

AUTHORSt Alekin, 0. A., Corresponding Member of the AS USSR, 2o- 1U-4-19/63
Brazhnikoya, L. V.
TITLE: New Data on the irainage of Materials in Solution From the
Territory of the USSR (Novyye dannyye po stoku rastvorennykh
veshchesty a-barritorii SSSR)
PERIODICAL; Doklady Akademii Nauk SSSR, 1957, Vol- 114, Nr 4, PP. 748-750
(USSR)
ABSTRACT: The entire drainage of materials in solution is subdivided in-
to the drainage of organic and mineral substances. The drainap
of mineral subetances is subdivided into the drainage of
colloidal substances and of ions. The major portion of the en-
tire drainage consists of the drainage of ions and its study is
of great importance fdr the knowledge of erosion- and accumula--
iLon-processes on the surface of the earth. Reference is made to
some preliminary works on this subject. The material of facts
gocumulated during recent years on the hydrochemistry of large
rivers made another calculation of the drainage of ions possi -
t1e. These data were collected by the network of hydrological
stations of the Hydrometerologioal Service of the USSR up to
1955. Various data found.in publications were also found. The
most data were obtained for large rivers, data on medium and
Card 1/2 small rivers are scarce. Furthermore the data on the European

New Data on the Drainage of Materials in Solution From the 2c- 114-4-19/63
Territory of the USSR
ASSOCIATIONs
SUBMITTEDs
part of the USSR are much more complete than those on the
Asiatic part. The entire drainage of ions from the entire terri-
tory of the USSR, according to recent calculations, amounts to
358,11 million tons (not counting the small basins without
drainage). Differences against earlier measurements are pointed
out. The bulk of dissolved salts (70,7%) is carried out into
the oc4an. 97,81 + lo million tons of salts flow into the Aral-
Caspian'Basin and salify it. The smallest quantity of salt
(31,23 million tons) is transported to the Pacific, the great-
estsjuantity of salt flows into the Arctic Sea (185,58 million
ton . The value of the coefficient of ion drainage averaged
for the entire territory of the USSR amounts to 17,9 tons/km2
per year. The total value of the drainage of dissolved substanr~
ces from the territory' -- 'of the USSR amounts to 473,29 mil
lion tons per year, of chat 3*54,64 million tons flow into the
sea and 118, 65 million tons into basins without drainage.There
are 2 tables and lo references, lo of which are Slavic.
Hydrochemical Institute of the AS USSRNoYocherkassk(Gidrokhi-
micheskiy institut Akademii nauk SSSR,,g. Novocherkassk)
December 24, 1956
Card 2/2

0 A A
20-5-40/60
AUTHOR ALEKII17O.A.,Corresponding Mlember of the Academy,
BRAMINIKOVA3 L.V.
TITLE --NDW-Ua-T-a-G-offaM1ffrng the Average Composition of River Tater for the
.Territory of the U.S.S.11.
(Novyye dannyye o arednem, soatave rechnoy vody dlya territorii
SSSR, -Russian)
PERIODICAL Dolklady Akaderii Nauk SSSR,T957, Vol 114,Nr 5,P2 1o62-1o65(U!S-S-R-)
ABSTRACT The annual average chemical composition of th4viater of a river ba-
sin represents an important characteristic. It comprises individual
peculiarities of the composition And regime of smaller parts of the
basin. This value, calculated on the basis of several years' data
on the chemistry and drift of the river,,oharacterizes the chemi-
.cal composition of water.The average river-water composition is
therefore for larger basins within a certain period of time a move
or less stable value of great gooohemioal importance-The values
of several years for ocean basins were calculated in the U.S.S.R.
in 1951; during recent years they were defined more precisely by
ion drift.Average values of the mineralization of river water of
the ocean basins as well as of individual rivers reflect general
regularities of the hydrochemioal zone.Mineralization is lowest for
the basin of the Polar Sea (105,2 mg/liter) and especially for the
-
Pacific (52,4 mg/liter), their water-qollectina ar
eas being con8i-
derably moistened and the bottoms washed out by centuries of lixi-
Card 1/4 viation.The difference in favor of the Frozen Ocean is caused by

20-5-40/60
Ifew Data Concerning the Average Composition of
River Water for the Territory of the U.S.S.R.
the inareaned mineralization of the rivers Onega,Northern Dvina
and Lean,which are formed under special eircumetances.The avera-
ge mineralization is nome-what higher in the basin of the Atlan-
tic Ocean,in the Black Sea and the Azov Sea (267 m6/1) is higher
than that of the Baltic Sea (12o,2 mg/l).Most highly mineralized
arc the basins without outlet of the Caspian Sea and Lake Aral
(344,4 rig/1),especially the Amu-Darya river.The Volga lowers their
average value.This average value reflects the lov; mineralization
of the floods which represent the main part of the annual flow and
it cozen closer to them in'this respect.The average chemical wa-
ter composition of all ocean basins of the U.S.S.R. has similar
common featui~S.Lve**ere dominate HGO and G-a1which is obaracr
teristic of Ihe f~oods.This feature is also characteristic of tho
majority of ourface waters,as a natural consequence of centuries
of washing of surface rooks by precipitations,which formerly were.
above the erosion basiB.For basins without outlet a somewhat higher
B041 '-content (up tQ 2o% equ) at the expense of HQ03 f-reduction
was found.For a comparison of average Laineralization with the e-
lements on the income side of the salt balance of a* basin,one has
at present to make use of the mineralization of atmospheric pre-
cipitations,since they are quantitatively the most aocessible.From
a comparison of the obtained figures one could apparently draw the
card 2A conclusion that the major part of the ion composition of river wa-

New Data Concerning the Average Composition of 2iver
'Vater for the Territory of the U.5.S.A.
20-5-40/60
ter is with regard to its origin connected with the precipitations.
Ilore,than that,the content of 501 '_ C11-and Na-ions surpasses even
in concentrated (i.e.exposed to ivaporation)atuiospherio waters their
content in river water.This conclusion oan,however,not be vally ac-
cepted.Such considerable amounts of salt as oome into a wa~er-collec-
ting basin together with the precipitations have induced -many inve-
stigators to consider the precipitations as the determinant factor
for the increasing salt-oontent of the bottom and in the mineraliza-
tion of surface waters.Without denying the essential im.-portance of
precipitations for the formation of surface waters,some oircumstan-
oes must be mentioned which reduce that importance.In the atmosphere
there occar,beaide soluble matter (aerosals),suspensiQns of aeolian
dust of local origin in the lower layers.The usual collection me-
thod of the precipitations and the mentioned suspensions does not
make it possible to ad-parate them.Therefore the latter,whether in a
dry state or with the rain,enter into the measurement containers.
But in falling down to the earth they might have a different fate.
'ITransit" salts of this kind can be displaced by the wind several
times a year without having had an actual influence on the ion drift
of the river.Thus there originates an exaggerated idea on the am-
00
ount of salts falling out with precipitation and on their participa-
Card 3/4 tion in the mineralization of the river water.The true share of these

20-5-40/60
Ilew Data Concerning the Average Composition of River
1.7ater for the Territory of the U.S.S.R.
. aeolian and suspended salts in the formation of the -river wa-
terB has to be clarified by further investigation.
(2 tables, 8 Slavic references)
ASSOCIATION Hydrochemical Institute of the Academy of Sciencesof the IIJT.S.S.R.
P11t;SENTED BY
SU3,11ITTED 21.1-1957
AVAILABLE Library of Congress.
Qqrd 4/4

%U` 1102
Alekin , G. it Da tnko , U G __'W'
~irazhnj'kovo, L. V.
TITLE: Investigation of Chemical Processes in Natural Waters
I
kIzucheniye khimicheskikh protsussov v prirodnykh vodakh)
Conference in Novacherkasak (Soveshchaniye v Novocherkuske)
PFRIODICAL: Vestnik kkalemli nfiuk S33A, 1958, Nr 8, pp. 119-120 (IJSSR)
ABSTRACT: The 1:1411hytirochemical conference was h,,1;1 in Novo~h:lrk~insk
from -lay 6-11. Tt had been calle6 by the Gi,4rokhimi.cheskiy
I
ingtitut C;Y_Irochemical Institute), '4?.t wps attenjej b.~v Pbout
25- persons: representatives of scicntific r33e~:rch institutes,
of universities, of planning and.economic organizations of a
number of republics an! r-rigions of the U-,',:;R. The main subjects
discussel in the conference were investigations of the inter-
action of natural wnters with rock, soil ani silt. Such in-
vestigations were considered to be particularly interesting
which attempted to givo a model of the formation of natural
waters. A consii~.,rable number of reports Joalt with the inves-
tigation of the carbon%to equilibrium in natural waters and of
the factors exerting an influence on this process. Reports
Card 1/2 were also given on research lealing with the dynamics of or-

Investigatiin of ChemicLl Procesnes _'n SOV/-4/0-58-8-25'43
i"atural Waters
ganic substances in natural waters. The methois used in the
separation of organic substances from natural waters and in
the investigation of their composition were found to be imper-
feet. The investigation of the qualitative composition of or-
ganic substances found in natural waters should be intensified
by reverting to the use of spectrophotometry in the infrared
range, and to that of chromatography. The importance of hori-
zontal and vertical shifting of waters for physico-chemical
and biological processes is also shown. The necessity of devo-
ting more attention to the investigat~;on of the relation bet-
woen hydrochemical processes with hydrometeorological and
hydrological conditions was emphasized. Reports were also
given on research dealtng with the regulation of rivers con-
nected with the constructi-I-M of hydroelectrical power plants
and other hydrotechnical constructions.
Card 2/2.

BR.kZMIIMVA, L.V.
%!t
,r_ I
Ion discharge of rivers in the eastern part of the Greater Caucasus.
Gidrokbim.inat. 28:59-68 '59. (MIRA 12:9)
1. Gidrokhimicheshy institut Akademij nauk SSSR, g.Novocherkasak.
(Caucasus-Rivers) (water-composition) (Ions)

PHASE I BOOK EXPLOITATION SOV/5374
Akademiya nauk SSSR. Gidrokhimicheakiy institut
Gidrokhimicheskiye materialy, t. XXX (Hydrochemical substances,v.30)
Moscow, Izd-vo AN SSSRI 1960. 213 P. Errata slip inserted.
2,000 copies printed.
Sponsoring Agency: Akademiya nauk SSSR. Gidrokhimicheskiy institut
(Novocherkassk).
Editorial Board (Title page): Resp. Ed. 0. A. Alekin, N. V.
Veselovskiy, Deputy-Resp. Ed. V. G. Jatsko, G. S. Konovalov,
M. 1. Kriventsov, P. A. Kryukov; Resp. Secretary and K. G.
Lazarev. Ed. of Publishing House: D. N. Trifonov. Tech. Ed.:
I. T. Dorokhina.
P M OSE: This publication is intended for hydrologists, hydrochemists,
and hydrometeorologists.
COVERAGE: This is a collection of 22 articles on the hydrochemistry
of rivers and water bodies in the USSR. The authors discuss

Hydrochemical Substances
SOV/5374
pollution, spectrographic methods of determining the content of
microelements in water, and the content and discharge of ions,
gases, as well as chemical, biogenic, and organic substances.
A map showing the distribution of the ionic discharge of rivers
in the USSR is the most complete to appear in print to date. No
personalities are mentioned. Each article is accompanied by
references.
TABLE OF CONTENTS:
Brazhnikova. T,. V. (Gidrokhimicheakiv inatitut AN SSSR,
Novocharkassk- Hydrochemical Institute AS USSR, Novocherkassk].
Map of the Ionic i)ischai-ge of Rivers in the USSR 3
Fesenko N * G , and V. I. Rogozhkin [Hydrochemical Institute
AS USSR1. Ac;umulation of Phosphorus and Nitrogen Compounds
in the Tsimlyanskoye Reservoir Between 1954-1957, and the
Change in Their Discharge at the Site of the Hydroelectric
Power Facility 10

BRAZHNIKOVA, L.V.
Map representing the ion discharge of rivers of the U.S.S.R.
Gidrokhim. amt. 30:3-9 060* (MIRA 13:9)
1. Gidrokhimicheskiy institut Akademii nauk SSR, Novocherkasek.
(watir-Conposition) ~(Rivers)

ALMN, O.A.-I DATSID, V.G., doictor khimicheskikh
nauk; BRAZRNIKOVA, L.Y.
V'SR-
Methods for hydroohomical analyses of natural waters. Test#AN
30 no-81121-123 Ag 160. (MIRA 13:8)
1. Chlen-korrespondent AN SSSR (for Alekin).
(Water--Analysis)

BRAZHNIKOVA L V Cand. Chem. Sci. (diss) "Ion Flow of Aivers
of USSR." Irkutsk, 1961, 19 pp. (Irkutsk State Univ.) 180 copies
(KL Supp 12-61, 255).

ALEKIN, BRAZHNIKOVP., L.V.
A contribution to the study of the ruooff of dissolved substances
161.
from the land of the globe. GidrokhIm. mat. 32:12-24~Ml. 24:6)
11 Gidrokhimicbeskiy institut AN SSSR Novocherkassk.
(Water-Composition5
(rtunoff)

AIEKIN, O.A.; BRAZHNIKOVA, L.V. -
r- _.
Annual distribution of ion discharge in rivers of the U.S.S.R,
Gidrokhim.mat. 34:12-18 161. (MIRA 15:2)
1. Gidrokhimicheskiy institut AN SSSR, Nov9cherkassk.
(Rivers) (Water--Composition)

ALEKINq O.A.; DATSK09 VeGsj ERAZHNIKOVAl L.V,
Fourteenth All-Union Conferenoe on Hydrochemiatry. Zhur.VKHO 6
noolt94 161, (faRA 3-4:3)
(Watel'%-Axalysis)

DATSKO, V.G., p-nf.; FESENKO, N.G., kand.khimicheskikh nauk; BRAZHN.ILKOVA,
L.V.; PONOMAREV, I.F., prof.
Fifteenth All-Union Hydrochemical Conference. Zhur. VKhO 6 n0.6:
70Z 61. (MIRA 14:12)
(Water conservation--Congresses)

DATSKO, V.G.,, doktor khimenauk; FESENKO, N.G.,, kand.khiTn.nauk; -P~
L.V. kand.kbim.nauk
Hydrochemical sources for the comprehensive utilization and protection
of water resourses. Vest.AN SSSR 31 no.9:135-136 S 161.
(KMA 1l+: 10)
(Water-Analysis) .

DATSKOP V.G., doktor khim*nauk)- FFSENKO) Me, kand,khim.nauk~~
L,V. kand.khimenauk -
I
Studies of the chemical composition of surface waters. Vest.AN
SSSR 32 no.8:124-125 Ag 162. MU 15:8)
(Water-Composition)

ALEKIN, O.A.; I]RAZENIKOVA, L.V.
Relation bel;een the ionic runoff and the runoff of matter in
suspension. Dckl..AN SSSR 146 no.1:203-206 S 162. (MIRA 15:9)
1. Chlen-korrespondent AN SSSR (for Alekin).
(Geochemistry)

DATSKO, V.G., doktor khimicheakikh nauk; PONOMAREV, A.F., doktor
khimicheskikh nauk; FMENKO, N.G., kand.khimicheakikh nauk;
I RWHNIKOVA, L,V. kand.kbimicheskikb nauk
Sixteenth Hydroche*ca.1 Conference. Zhur. VKHO 7
no.6:690 162. (MIRA 15:12)
(Water-Composition)

O.A. ALEKIN, L.V. BPAZMMVA (USSR)
Pcsrrying'-aut.by'thi rivers of dissolved -substances from continents and its
connection vith 6ecbwdcal- erosion of theiEarth surface."
Report 'sented .atithe Conference-on Chemistry of the Earth's C~us tj
Pre
Mowcaw 14-19 Mar 63

ALEXIN, O.A.; B!A~l IIIO~A, L.V.
Methods of calculating ion flow. Gidrokhim. mat. 35-.135-148 163.
(MIRA 16.-7)
1. Gidrokhimichdakiy institut, Novocherkasak.
(Water-Composition) (Ions)

ALEKIN, 0. A.; BRAZIINIKOVA, L. V,
Several regularities connecting the ionic runoff with the runoff
rP suspended silt. Izv.Vses.geog-ob-va 96 no. 2:115-123 Mr-Ap
164. . (MM 17:5)

YAKUSHEVA I A. S . ; DP% A L V
Chemical compositi-n of atmospherle preedpitatlan In t.ho lapper
reaches of tb.E Sa.. River. Gid~okhim. mat. 37~23-2c, t64. (MIRA 18s4)
1. Gidrokiiii-nicheskiy institut Glavnogo upravlen.1ya gidrometeoro-
logicheskoy sluzhby pri Sovete ~Lintstrov !USSR, Novochorkassk.

ALCKIN, D.A.; RI~fAZIPUK ;
Studying ionic ranoff of m-10 basins based on the example of the
Sal River. Gidrokhim..mat 3700-41 164. (MIRA 18-4)
1. Gidrokhimichoskiy inatitut Glavnogo upraiilenlya gidrometeoro-
logicheskoy sluzhby pri Sovete Ministrov' SSSR, Novocherhassk.

A I ~11,'K I N ,0.4.; BTUZHNM(*,VA, i,.V.
Significance of the proc~:ss of weatherIng cf' rock '~ " or ti-,e
minoralization oC worface waters. Gidrokhim. Inat'. 37i9P-108
16./. fl,'IHA 18~4)
1. Gidrokhimicheskiy ins"itut G3.avno.-c upravleniye. eidranetecrcl-
logicheakoy slazhby pri Sovete Ministrov SSIIRL, %ovocherkassk.

AUKINY Oleg Aleksandrovich;_~R~A
EPAGUNOV~ E.S., red.
(Runoff of dissolved solids in the U.S.S.R.] Stok
rastvorennykh veshchestv s territorli SSSR. Moskva,
I'llauka, 1964. 143 p. (I-11RA 17:9)

DATSKO, V.G.,,doktor khim. na,uk; PONOMAREV, N.F., doktor kbim. nauk; FESEHKOp
I N.G., kand.khim. nauk; BRAZHNIKOVA, L.V., kand.khim.nauk .
The 17th hydrochemical conference. Zhur. VKHO 8 no.6t695 163.
(MIRA 17-2)

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to
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