SCIENTIFIC ABSTRACT SHCHERBAKOVA, K.P. - SHCHERBAKOVA, M.N.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001548910004-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 4
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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5587. ADSORPTION FRCK SOLUTIONS AND THE RICROK*OSITY OF ACTI VATED 00
CHARCOALS. Kinelov, AV and XV (DOILlady Akad.
4hchar
4
1
W
-7
-
r
0M
t
r*nd. aced. eel.
.
Nauk S.S.S.R., 19", 45, 257-
w; 0
P
U.R.S.S., 19", 45, 214-3; Chem Abstr., 1945,
39, 5150)0
-90
The -baorption of aliphatic alcs.(butyl through hoptyl),
fatty acids (acetic through haptylic), and No oats of' o1ole 00
o ezl and srucle acids fron sq. solne. bu a specially purified .
690
activated cbercoal was studied. At low conans., the adsorption =00
which increased with an increase in mol. wt., 4.4., in

0 J, the "direct Trouble series,* was apparently controlled by
contending forces acting on the adsorbate. At higher cocoas., real
corresponding to nax. adsorption, the vol. of the microporse
or the adsorbent was the factor controlling the cdont, of
adscrption. This was shown t7 the fact that the vol., of the
ods.-xbod solo. was substantially identical for the above
mentioned a6sorbantes, all of which or* charectorlood by a 1290
small, identical cross section. Further oonfirzation is found 809
in the fact that a maller vol. of Meor bed solo. was obseirved .400
Fog', at mx. adsorption of b4lky dye solo., e.g., mothylone blue '*0
Is f I .S L A WU SWI40AC CL.'silfKATIC. tie*
We*

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gill 054143 39 V4R0
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3 4 -3a I It b, if 12 U -is B M, i1, to to
Rorre IMOL X
PCOCESSIS AND P!16
3931. ACTIVATED CHAFODAtt AOSORPTIVEE FROFERTI2S AVID STRUCTURiC.
Kiselov A. V and bhcherbakova. K. P, (Acta Physicochlm,, U.R.S.S.,
In studying the structure of oolid,adeorbents,,.particularly that-
of finely porous ad6orbents of large ab6orbing poyeri conaidaratio'd,
must-be given to the structure of the solid skeletonj the-pordeand
the interface. The last two features can be inveotigated-b~ ~dsorp_
tion methods. Investigations have been made ever a wide concentration
range of the adsorption isotherms of activated charaoal for various
organic substances from aqueous solutions--Mith substance-thO mix
with water, the isotherms pacs through a mazimum and the total content
of the adsorbate in the adsorption volume is much'greater than the
amount adsorbed. For the homologous series of fatty-acids and alcohols,
the limiting adsorbed volumes, expressing approximately the volume of
the adsorption spacey are-constgnt. This rule is accounted for.by
the complete packing of the chai~oal microp6res with the molecules
of those substances. Changes in ~he structuxe of the a'doorbato m a-,

S9CIFUAKOVA, K. S,
I
IlBasic Problofm of Kidnay
for Degree of Candidate of
Agr,lculture Inst, GorIkiy,
bean CultivatIon Techniques in Gorlkiy Oblast." (Dissertation
Agricultural Sciencon) Min iiiphor Education, GorIkiy
1955
SOt M-1036 2V Mar 56

V - - : ~' - -
PIHQHMBKAYA, 011ga Dmitriyevna; -S jrlaz~jxa -
NBTSLtTSIN. P.G., otvetstvannyy redaktor; KASHAROVA, V.G.. redaktor;
SUSHUVICH, V.I., tekhnicheskiy redaktor
[Radio interference from electric transportation ~,ad wayB of controlling
it] Radiopomakht ot elaktrotransporte i bor'ba s nimi. Moskva, Sviazl-
i2dat, 1957. 42 p. (MIRA 10:9)
(Radio-- Inte rf arence)

A-UTH-OR: Shcherbak.0va, K.S. (Enl-ineeln) SOV/110-59-L~-20/23
TITLE: Radio Interference from Househoici Electrical Equipment
and its Suppression (Radiopo.7elkhi sozdavaysmy,,re
bytovymi eiektroustroystvami, i sposoby ikh podavieniya)
PERIODICAL: Vestnik Elekti-opromyshlexinosti,1959,Nr 47pp 69--71(USSR)
AB STRACT: *In power-operated hausehold electrical appliances
L
interference originates mainly in commutator miotors7
which can sometimes be replaced by induction mictors.
Other important sources of radio interferenoe are starting
relays and thermostats. in this respect higt speed
Uiermostats are much better than slow speed ones. The
radio interference from household appliances is usually
Uransmitted over the power cix'cuit and should, therefore,
be suupressed at source,, It is -lurrently required "hat
h-,asehold equipment should be provide,4- with interference
suppression on manufacture. Standard limiting --.--alues of
radio interference in microvolts produced by various types
of household electrical equipment in the frequency rang-9
0.15 - Wo h I-L
I 'c/s without interference suppressir%n are g4ven
in Table 1. The effectiveness of i-nterference suppression
Card 1/3 systems for electrical apparatus can be letermined from
this table. Interference from household equipment is

'OV/110-59-If-20/23
.Radio Interference from Household Electrical Equipment and its
Suppression
suppressed by screening the source of interference and by
the use of power system filters and also by suitable
choice of materials and designs. In many types of equip-
ment such as irons and electric razors it is difficult to
make the suppression devices both small and safe enough.
Capacitors connected between live conductors and the
-frame of the apparatus may cause the frame to assume
dangerous potentials under certain circumstances.
Accordingly when the frame is not earthed the total
capacitance of all such capacitors should not exceed
0.013 microfarads for 220 V supply or 0.023 microfarads
for 127 V supply. Capacitor block type 3B is used for
interference suppression in household equipment; a
circuit diagram is given in v'j-g _L, and data about the
available range of capacitors is given in Table 2. The
schematic circuit diagram of an electric floor polishing
machine type EPM-1 with interference suppression units
is given in Fig 2. The circuit diagram of a huusehold
'Card 2/3 electric drive with interference suDi-)ression is g.Lven in
Fig 3. The circuit diagram of a ha.-,sehold refrigerator

SOV/110-59-4-20/23
Radio Interference from Household Electrical Equipment and its
Suppression
with interference suppression is given in Fig L '
Details of the capacitors used in all these suppressors
Card 3/3 are given.
There are 4 figures and 2 tables.
SUBMITTED: December 77 1958

adio
(I/IRA 1&-I)

GAYDAMAK, S., student; SMIRNYAKOVA, G., studentka; KUZ'MINA, E., studentka;
LIPOVA, R., studentka; FOMINA, T., studentka; PAVLOVA, N.,
studentka; KALINOVAp M., studentka; 5HCHEU0, ~.., student;
SHCHERBAKOVA, L., studentka; GUDOCHRrNA, L.M.
Effect of salinity on the results of determining the specific
weigInt of soils. Sbor. nauch. trud. haz GPU no.19:197-198 160.
WIRA 15:3)
(Soils--Analysis)

Ya.; .'~;ECMIBAKOVA, L.,, otv. za vypusk; SKIBA, T.y
uekhn. red.
[With hand over heart; collected sketches of foreign writers
on Uzbakistan]Polozha rulm na sordtoo; sbornik ocherkov ino-
stramVich pisatelei ob Uzbekistane. Tashkent, Goo.izd-vo
L-hudozh. lit--,T, 1962. 85 p. Transl,,,ted from French and
other Lm-guages. (MIRA 15:9)
(Uzbekistan-Doscription and travel)

SAFR,03MAN. O.A., inzhmner; VASILIYXVICH, M.G., inzhener;
SHCHERBAKOVA, L.A., agronom.
Evaluating the performance of new checkrow potato planters.
Snl'khozmashina no.8:18-22 Ag 156. (MLRA 9:10~.
(Planters (Agricultural machinery))

USSR/meteorology instruments Jan/Feb 48
Thermometers, Resistance
"Electrical Resistance Thermometers for Obser-
vationb on the Vertical Distribution of Air
Temperature," L. F~ Shcherbakova
"MeteorolA Gidro.l" No 1, pp log-114
Describes relatively simple.method for remote
dete-imindtion- of' air temperature with -resist-
~nce thermometers and ..a,Wheatstone. bridge. Two
types of'thermo'meters: one with open filament,
and one with filament in, metal envelope. Tables
give date from tests with three thermometers
constructed at Main Geophys Obs. Submitted
11 May 47
167T97

USS R
/6.4-237 1.551:551.584 1
V *ShA196" rsdadavanie nekotorykh sposobov kharaktarlsW turbulintnogo I
. "I ~.- --~; I
o__ k nizlinem sloo atmosphery. Lhjkhods of invistigat-,
t exchange by means of observational data in the lower atmosphere.] Len
ing turbulen
614maia Geoilsicheskrio Mjcrvafoytf~j Trudy, 16(78):25-51, 1949. 8 figs;,, 6 tables, 8 refs.,
22eqs. DLC-AnaIvzii% a 6eries of micraclimaicilogical profiles, given in the tiame volum Ie on
i p. 136-143, the author concludes thatifor stable conditions SvEnRup's formula gives the [*st
results, Rossay's formula is adequate for adiabatic and BuDvrLo's equatioa for convective
conditions. LAlizarmA.Ws theury dm-s act agree with observations. The, wind profile for
nonadiabatic conditiona has a definite curvature. depending -an stability. - SitiVect Headings.
1. Atmospheric turbulence 2. Turbulence theaq MIcsometearoloocal prafflasi-A.A.

ER A K'D*V-IA
-V,!.9-12&
Q kh"Aitteristilre turbulesitnago oboat" PO
_m'stl vetm [Determination or turbuWat
n!!!d7u`&dtkhtu it. Cuch-ge by -krooKm-
mean gradient of wind velocity.] LrXingrad. Glavi~ia MUM-
-,I-_-&gCjj&_TruJy. 16(79):102-IDS, 1049. 2 refs., 4 "p. DLC---i he alitilor de"ps tne losmula
Z K-.;,- ~~! for the computation of the coefficient of exchange, knowirIg the standard deviation
AI
r. of the horizontal 'kind velocity and the vertical gradient arslai of the-mean wind. It is
not assumed that the momentum is constant on the path of mixing, as it was done by ErM
in a similar treatment. A difficulty involved Is the value of the coefficient C (preuraiRM
J-1), which seemi to depend on the stratificarlon. Subjeel Headinry., 1. Turbulent exchatv
2. Wind fluctustionL L Ertel IL-A.A.
Ind, --------

SHCHUR A VA, L,Y.
Field investigation of the effect of afforeotation on wind velocity,
radiation balance and turbulent exchange. Trudy GGO no.29:-11-44 152.
(Afforestation) (Meteorology, Agricultural) (MIRA-11:1)

SHCHXRBAKOVA. LY ,." ;w1,",
'~' -
- .
w-kua protiles iu inters trip forest grids. Trudy GGO no.43.-13-16
. -~40 (MnU 11:5)
(Winds) (Afforestation)

YOW", Y.G.4 GMICHINA, K.V.; IGHMOV, V.D.; 11EC1i;Mj'V' I.N.; POROVSKIMI
1,A,: TUP0110VA, T.S.: TSYGANOVA, A.M.; RUSIN, N.F., otv.red.;
RITAYTSAW, A.M.i red.; KUZIMIN, L.A., red.; OLIMPOV, Y.G., red.;
aMMIH, I.S. , red.; B.-HUIN, I.A., red.; ITECHAM, I.N., red.;
SHCHARBAKOVA, L.F., red.; MARTYNOV, S.I., red.; SIMONOV, Ya.P.,
--* IVAR6V''-A.P., red.; BESSOITOV, H.P., red.; YAS140GORODSKAYA,
14.m.: red.; VLADIMIROV, O.G., tekhn.red.
(Directions for hydrometeorological stations and -postal Nastavlenie
,gidrometeorologicheskim stantaiiam i postam. Leningred, Gidro-
Toeteor.izd-vo. No-3, pt.l. [Observations at meteorological stations]
Mete orol ogi clip 911~ia nablindentia na stantsiiakh. 1958. 223 P.
WIRA 12:12)
1. lbissia (1923- U.S.S.R.) Glavnoye ii-pravlaniye gidrometeorologri-
cheskoy sluzhby. 2. Sotnidniki Metodicheako-o otdela Glavnoy _-Po-
fizicheskoy observatorii im. A.I.Voyeyk-ove (for Volokh, Gushchina,
Igrunov, Nechayev, Pokrovsk-qya, Trifonova, TSyganova). 3. Glavnoye
-upravlaniye Gidrometeorologicheskoy slnzhby SSSR (GUGMS)(for Kitaytsev,
Kiiztmin, Olimpov, Skiteykin). 4. Glavywya geofizicheskaya observatoriya
(GGO) (for Berlin, Nechayev, 1hisin, Sherbakova). 5. Mestnyye -upravieniya
Gidrometeorologichaskoy sluzhby (for Martynov, Simonov, Ivanov, Bes-
sonov).
(Me to orology-Observn t ions)

0-/169j62/000/012/081/095
D228/D307
L.F.
---- --- - ---- - --
of the results of snow measuring surveys
and recommendations for improvingf the method of
Mnoii cover observations
".e-!Qrit:ivnyy zhurnal, Geofizilca, no. 12, 1-962, 56,
ZL~)St~rzict 12V354 (In coliection: rjnczhn. pohrov, yego
ras-3rostr. i roll v nar. kh-ve, M., 36 Sit, 19621
.5 - 14
"hc results of analyzing the data of snow measuring
si,trveys in a aad on a typical -open traverse are stated.
These were c,-xricC, out at the hydrom e teoro logical and agromcteorolo-
,,ica'L stations o. 0
-f f Gorlhiy, uiisk, ;IavL;orod Gatayskiy hray), Solyan-
ha (I~rasnoyarskiy hray), a7ad Chismy- (BasW.-iriya) and at the Dubov-
skaya disciiarfc statioll C',ostovshaya oblast')-. These data were com-
,)ared wita results from a continuous sno.! me-a-suring survey, made
simultancously on a number of parallel measuring lines distributed
Card 115

3URKOVSKAYA, Ye.Kh., naucYwyy sotrudnik; IGRUNOV, V.D., nauchnyy sotrudnik;
K-~OCHAYIT, I.N., nauchnyy sotrudnik; BGBRIKOVA, V.H.; T-HaSITT'YDVA,
T.N.; SHCIMP-BAKOVA, L.F.; B~MTLIN, 1.2., otv.red.; KITAYTSEV, A.M.,
red.; KUZIMIN, L.A., red.; OLIMPOV, V.G., red.; aITMIN, 1.5.,
red.; RUSIN, N.P., red.; KIRTYNOV, S.I., red.; SIMONOV, Ya.P.,
red.; MANOV, A.P., red.; BESSONOV, N.P., red.; T.AS]IOGORODSKAYA.
M.M., red.; VLADIMIROV, O.G., tekhn.red.
(Directions for hydrometeorololgical stations and postal Ifastavlenie
g1dromateorologicheskim stant5iian i postam. Leningrad, Gidromeleor.
(Continued on next card)

BURKUVSKAYA, Ye.Kh. --(cant inned) Card 2.
izd-vo. No.). pt.2. [Workini, up mterials of meteorolo-ical
ovservations] Obrabotkn jqjte~ivlov meteorologicheskikh
nabliudenii. 1958. 85 P. (MIRA 13:1)
1. Russia (1923- U.S.S.R.) Glavnoye upravleniye gidrometeoro-
logicheskoy sluzhby. 2. Glavrava geofizicheskaya observatoriya im.
A.I.Voyeykova (for Burkovskaya, Igrunov, Nechayev). 3. Starshiye
inzhenery Nsuchno-issledovatel'scogo instituta aeroklimatologii
(for Bobrikova, Terentlyeva). 4. Glavnoye upravleniye Gidrometeo-
rologicheskoy sliizhby SSSR (for GGUGMS) (for Kitaytsev, KnzImin,
Olimpov. Skiteykin). 5. Glavnsys geofizicheakays observatoriya (GGO)
(for Berlin, Nechayev,.Rusin, Shcherbakova). 6. Upravleniye gidro-
,meteorologichealcoy sluzhby (URS) (for Martynov, Simonov, Ivanov,
Bessonov).
(Meteorr1cgT--Observers' manuals)

V169/62/000/012/081/095
-11aly--is of the rc.,;Ults ... D228/D307
u
I
ni.-Cormly ovcr rcl~-.tivcly e-,-.I:cnsivc territory. Comparison of the
results of: ---,1017 surveys on a typical open traverse and in
L>
a triantric showed 'clac ~'ort,.icr to i,ossess more advantages than the
CI
1 at t c r ..',, typical traversc can be chosen mor--- easily for the pur-
-)ose of uetting accurate average values for the snow cover depth*
a- --xacteri.-,tic of the
ad t ac water reserve, and it crives a truer ch
3now cover c1isuribution. .,~'or all snow survey traverses in an open
area the values f7or tho coefficient of variation of the snow cover's
depth -reatly excced those for the coefficient of variation of its
dcnsi~:y. The v- 1-Lic of the mean square deviation of the depth from
the average dcpth rises as the depth.o-r- the snow cover increases.
;.*or the -,ieaii square deviation of the'density this regularity is not
observed aziywherc. The 1.)reclsion, with which the average depths
and densities of the snou cover and the average water reserves in
it were deter-minoO., was sufficient in all continuous snow measuring
su-rveys. `mal)- c,21--ors in the determination of the snow cover depth
~ -e-
- zc also obt ined in surveys on an open linc and in a triangle at
the stations of' Gor"Idy, ~~ubovskaya, Slavgorod and Solyarka, ifnen
th,c weather conditions were favorable -and the quality of the obser-
Card 2/ rz

S/169/62/000/012/031/095
-aanlysis of t1ie results ... -0223/0307
vations was rood. The dcnsity error was sufficiently low only when
nun~)Cr dc----i-y nca~;urcments war not less than 20. in the
.a
uL-Laor's opinicii, for Zlat arid hilly terrain with gentle slopes the
IC-LLrth of an open traverse typical of such coun-
try azlou-ats to 2-3 la-,I. This suff'ices for the -mean value, of the snow
covcr depth on the traverse to coincide, to ~-,-ithin 10-11j'a, xeith the
aver--re dr--,)th for the i-faole snow survey. area. . Investigation of
errors in -casurcz~icn'-P~