SCIENTIFIC ABSTRACT MERTSALOV, A. N. - MERTZLIN, R. V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001033620003-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: June 21, 2000
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


83403
S/05 60/000/009/006/008
J's-doo BOI 2 YB06 3
AUTHOR: Mertsalov A. N.
TITLE- The Number of Pilot-balloon Data Necessary for Calculating
the Divergence of Wind Velocity
17,-- 1
PERIODICAL: Meteorologlya i gidrologiya, 1960, No. 9, PP. 49 - 51 V<
TEXT: The present article deals with the errors arising in the calcula-
tion of the divergence of wind velocity. These errors are due to the
fact that the data on wind velocity and direction entered in weather
charts are expressed in round numbers. In the present article, the au-
thor determines the number of data necessary for avoiding these errors.
It is noted that for practical purposes the components of wind velocity
should be determined with an accuracy of + 1 km/hour, In this case, the
divergence is accurate to within + 4 km/hour over a distance of 1000 km.
This value is acceptable. This degree of accuracy can be attained by in-
creasing the number of pilot-balloon data entered in the chart. It is
not possible to eliminate relatively great errors (up to + 20 km/hour)
in determining the divergence, but the probability of these errors is
Card 1/3

'3340
The Number of Pilot-ballo(.i Data Necessary S/05 60/000/009/006/008
for Calculating the Diverge.ce of Wind B012YB063
Velocity
considerably reduced. This is exp ained in greater detail. Next, the
author studies two characteristic %.,Pses of wind distribution. First, he
examines the general case of qua 84 -parallel flow. The second line of
Table 1 gives the number n' pi--balloon data necessary for calculat-
ing divergencies (with an accuracy of 4 km/hour over a distance of
1000 km) at relatively low wind velocities (30-40 km/hour). The second
case described here is a quasi-circular flow in which the wind direction
almost coincides with the direction of the tangent applied to the con-
tour (with a radius of 500 km round the point for which the divergence
is determined). This is frequently the case with calculations of the
divergence for the eye of a cyclone or an anti-cyclone. The number of
pilot-balloon data necessary for calculating the divergence with an ac-
curacy of + 4 km/hour over 1000 km at low wind velocities (20-25 km/hour)
for a dist7ance of 500 km from the center are given in the third line of
Table 1. This table shows that only 3-5 data are necessary to eliminate
the influence of the inaccuracy of the characteristic values of the wind
direction on the calculation of the divergence. The results obtained in
this case are accurate up to 90/116' and even more. However, if the wind
Card 2/3

83403
,/60/000/009/006/008
The Number of Pilot-balloon Data Necessary S/050
for Calculating the Divergence of Wind B012/BO63
Velocity
velocity at a distance of 500 km from the center of the cyclone or
anti-cyclone amounts to 50-60 km/hour, the necessary number of pilot-
balloon data may be found in the second line of Table 1. Finally, it is
noted that the necessary number of pilot-balloon data must be a little
higher than those given in Table 1 since the calculation of divergencies
can also be complicated by the fact that the pilot-balloon data ob-
tained from one of the regions of the investigated contour are frequent-
ly not sufficiently comparable with the spatial variability of the wind.
There are I table and 3 Soviet references.
Card 3/3

- IERTSALOV, A.H.
Wind velocity divergence, vorticity, and the H Laplacian at high
levels in quasi vertical iyelonea and anticyclones. TTudy TSIP
no.112-.1&31 161. (MIRA 14:5)
(Meteorology)

IERTSALOV, A.N.
Preliminp-ry results of testing sam-- forecasting methods of the
evolution and transference of surface cyclones and anticyclone3
suggested by the U.S.A. Trudy TSIP no.125:19-35 163. (MIRA 16:12)

USPENSK17, _".:~-,6oktor fi-z -mat, nau prof.; BELCUSOV, S,L.., knind.
fiz.-mat. nauk; FYAT'YG-";A, K.V.; Mr',, *X. I .; :-.`__-T. A
A.Ii., kand. fiz.-mat. rauk; DAVYDOVA, O.A.; KIGF:M:SKAY4~~
A.F.; FKRIUMIKO, I.A.; ',-'ORSK(X, G.I.; TMI-ASHEVICH, L.V.;
SAMOYLOV, A.I.; ORLOVA, Ye.I.; DZHORDZEIG, V.A.; FETR9KO,
N FEETROSYANTS, ',-..A.; GIAZOVAT*l
N
.V.; DU~30VYT, A.S.; ROI.'.GV, A.I.;
ltjt5$..,BATYAYEVA, T.F.; i3ELISKA'-"A, NI.N.; C"HISTYAKOV, A.D.;
GANDIII, L.S.; BURTSEV, A.I.; 14ERTSAL-01*', A.I..; _:'AahOvYY, I".A.;
BELOV, P.N.; ZYNW,,,A4&#.retsenzent; SIDEHO, G,V.0#V-4,~t-
red.; DUBENT30V, V.H., kana. ilz.-mat. naux, nauchn. reu.;
SAGATOVSKIY, L,,V., red.; BUGAYEV, V.A., doktor geogr- nauk,
prof., red.; ROGOVSKAYA, Ye.G., red.
[I- anual on short-range weather forecasts] Rukovocistvo po
kratkosrochnyir. proEnczam pogody. LeninCrad, Gidrometeoizdat.
Pt.l. Izd.2., perer. i uop. 1964. 519 P. 18: 1)
1. Moscow. TSentrallnyy institut pro,-,,-r,,,zcjv.

-- "' - - " q,
-)VSYA I -,A a
-NNIYGV, V~~ 'r'
c;yc~ogene5iq,
Analyslls ald
in the P-~-jnoBphere. T-.rudv TSIP

MERTSALOVO A.K.
Torticity equation for the surface layer. Trudy TSIF no.W4..
110-111 165. (MIRA 18:11)

ACC NR: AP6025876
AUTHOR: Mertsalov. A. N. (Candidate of physicomathematical sciences)
ORG: HY11rnmnt0nrn1ngjeal Scientific RoseargjLLgnt&r (Gidromteorologicheskiv
nauchno-isslledovatelf~~Y tsentr)
TITM: Influence of the Scandinavian mountains on the formation and movement of
cyclones at the earth's surface
I V
SOURCF.t 1-bteorologiya i gidrologiya, no. 4, 1966, 12-18
TOPIC TAGS: cyclone, meteorologic observation, weather forecasting, atmospheric
pressure
ABSTRACT: This is an extension of an earlier study by the same author (Sbo%4-
nik rabot po regionallnoy sinoptika, no. 9, 1964), giving the empirical
relationships between the initial development of cyclones at the earth's
surface and their subsequent development in the follow-ing 12-18 hours.
This paper gives the results for cyclones whose centers at the initial
time of meteorological observations were situated in one of 13 regions
delimited on the accompanying map, that is, in the territory of the Scan-
danavian mountains or their immediate neighborhL,~d. Study of the in-
fluence of these mourtains is of obvious importance for the western parts
of European USSR. The study was confined to cyclones moving to the east
or southeast at the initial time (deviating not more than +220 from this
Card 1/2 551,515-1
6 -/ /ire

L 3374o-66
ACC NR: AF6025876
direction, provided the cyclone center at this time was situated in
'regions I-VIII, or moving east or northeast is the center was situated in
regions IX-XITI). Only cyclones for the autumn and winter months were-
considered. Only those cyclones for the years 1951-1963 were used,
except for those which caused an exceptional rise of water at the mouth
of the Neva River at Leningrad. The analyzed data are summarized in
tables and reveal that the relationships are similar to those obtained
earlier for lowland regions. These relationships are useful in short-
range forecasting of weather, particularly the pressure field, in.the
-dgstern and northwestern USSR* Orig, art.. has: 1 figure, 1 formula and I tableG
LJPRS: 36,'55ff
SUB CCDE: 04 / SUBH DAM 14Deo65 / ORIG RE F: 001
I
>
Card 2

MUERT-S)ALOV)
Theory Of ore f Dr--a t~on. I Z7. J,-!; S,~s n-. .7E, :,. :-T- -, I . ~' "I
no.8:16-23 ;,I,l If--4. 1 '. 7. )
.1 . ogj t,-eq~ 1. 'ej a -if ~,~ - I.-., y -T~ -;- r,., , -
- t I .
- tie lk. ly hoiLl te t SSSS~, '*'I.

MERTSAWV, IV.,, prepodavatell
Vachine for testing weight indicators. Neftianik 6 no.7:19 161.
(MMA 14t7)
1e Oktyabrlokiy roftyanoy tekhnilam.
(Weighing machines.-Testing)
Jk"
I. t

..MTSALOV, T."'.
Role of the pressure of or-m-ineral vapors ir. s,me s,,,ec-,--s of
their tranformations and the h '.-drothermal process. Biu- MOTP.
Otd. geol. 40 no. 6;142 Y-D 165. (1,111RA 19-1)
1. Sulmitted MaY 6, 1965.

WRTSALOV, IT.
Forge of builders. Sell. stroi. 13 no.10:22 0 '58. OWLRA 11:10)
1. Direktor Tullnkoy odnopodichnoy shkoly itroltellnykb masterov
(desyatnikov).
(Tula--Building trades--Study and teaching)

VERF SHC 11 A,,-, PIA, N , N , z r, t ", , , , ~
. -r. ~ * . -. ., I , -,, - .
,It:.i -," ", I',. -t 1 .: -, --l-, _4 7-~ -:
rinc-. ~ !. r. . : . !, -'? -. .-7 -
I
I !!r,-Il l3kiy e.Kh-;; I- - ". I *~ . . . .. -T t - r. ~ " ~ ,- . " .
I . . . . I

VEFtFSMPACtTNA9 N.N.j POS""OVIKIT, I.Yaa.; MERTSALOV, S.L.
Sensodiatire ser103. Part 7r 1-(2-M-quinazolyl)-4 Rf-thiosemiearbazides and
their properties. Zhur. erg. khim. I no.6t1154-1158 Je 165. (KRA ISO)
1. Urallskiy politekhnicheskiy institut institut imni Kirov&.

ISMSALOV,, V. -
OVoeikov" sails south. Zman-sila 37 no.3-28--31 Mr 162.
OUIA? 25 ~4)
(Voyages and travel) (Oceaucgraphic research)

MIMTSALDV, V.
[%elaved economy] 7akreposhchennoe khoziaietvo. Miunkhen, Izd.
TSentr. obOodinenlia polit.emigrantor U SSSR (TeOPE), 1958.
61 p. (MIRA 11-5)
(Agricultural policy)

MUMS&LOT, T.G.
- -
Konitzberg filtration and ozouization plant Bupplying water to Bern.
Tod. I ean.takh. no-5:36-38 W 158. (Km 11:6)
(Xonitzborg. Switzerland--Water--Ozonization)

--.KRRTSALOV, V.G.
Mobile units for chemical cleansing of low-pressure boilers.
Vod. i aan.takh. no.2:37-39 F '59. (MIR4 12-2)
(Boilers--Incrustations)
Al
4

LEEEDEV, Lev Georg~.yevich; IERTSALOV, Valentin Grigorlyevich;
MELENTIYEVA, V., red.; NA"IAROVA, A., tekhri. red.
[At various li~titudesl Na
vo "Znanie," 1963. 125 P.
(Voyages and
raznykh shirotakh. Moskva, Izd-
(MIRA 16:11)
travels)

S/050/60/000/06/11/021
B007/BO07
AUTHORS. Lyubanskiy, V. A., Mertsalov, V. G.
TITLE: From the Experience Gained by Working With a Wave-meter
rm-16 (GM-16)
PERIODICAL: Meteorologiya i gidrologiya, 1Sj60, No. 6, PP. 32-34
TEXT: A report is given of the working experience gained on a 1,600 ton
vessel sailing on the Atlantic. Besidesihydrological measuremen s, also
the mo'6ion of the waves was investigated by means of the wave-mAter of
the type It rm-16 (GM-16) of the Vilenskiy-Glukhovskiy-sysrem. (GOIN . This
now devAe was tested in 1956 by the Mezhvedometvennaya komissiya (Inter-
departmental Commission) and was released for series production. The
first specimens were used on various expeditions on the Caspian Sea and
during the 3-1ya Kompleksnaya antarkticheskaya ekspeditsiya (Third
5, Comprehensive Antarctic Expedition) on the e/s "0b"' (Expedition Vessel
.14 "ObIL). The device was in operation for nearly three weeks on the
Atlantic Ocean. It is based upon the hydrostatic mode of action. The
Card 1/2

From the Experience Gained by Working With S/050/6o/ooo/o6/11/021
a Wave-meter rm-16 (GM-16) B007/BO07
individual assemblies of this device and its mode of operation are
described. The work carried out with it is described, and some *
recommendations are made on the basis of the experience gained for using
the device as well as for its improvemento There is 1 Soviet reference.
Card 2/2
I- Ma,

RZHEPLI14SKrY. G.V.; MERTSALOV, V.G.
Nomograms for calculating wave periods and heights in the deep
sea from atmospheric pressure gradients. Trudy GOIII no.54:61L
66 '60. (MIRA 14:41
(Waves) (Nomography(14athematics))

IERTSALOV2 V.G,; RZIfEPLITISKIY., G.V.
Practice of prognoses of ocean waves under s~-ipboard,
conditions. Ime-teor. i gidrol. no.10:44-46 C 162. 01'rl-rl.~ 15 :9)
1. Gosudar?tvennyy okeanograficheskiy institut.
-4w.. (waves)

MERTSALOVO V. G.
Further improvement of nomogram for calculating ocean wind
waves from atmospheric pressure gradients. Trudy GOIN no.74.-
75-86 163. (KMA 16:7)
(waves)

MMTSALOV, V.I., lnzhener.
I...
C-.-' 4:
Test rod for -measuring gaps in VKG-133 witches. Rate. i izobr. pre4l.
v atroi. no.15()-.29-32 156. (KIRA 10:5)
(Xlectric switchgear)

L 06987-67 E'.'iT(d)/E,'1P (vJ'11rE_'h'P (k )/EiqP (h)/El,'JP (I)
ACC NR: AT601SZ83 SOURCE CODE: UR/319Z/65/000/01010145/0150
AUTHOR: Mertsalov, Mirtov,
ORG: none
TITLE: Reference generator of random parametric disturbances with an
adjustable correlation coefficient
SOURCE: AN LatSSR. Institut elektroniki i vychislitel'noy tekhrliki. Avtomatika
i vychislitel'naya tekhnika, no. 10, 1965, 145-150
TOPIC TAGS: ;~.Aomatic control R and D, random impulse generator
I L'
ABSTRACT: One of the possible methods ~f statistically testing a system
subjected to random disturbances is considered. The method can be used for
evaluating the effect of component -parameter spread on the performance of an
automatic control system. A reference generator of random parametric
disturbances would be necessary for such tests; it may consist of a random-signal
generator, a correlation -forming unit, and a storage unit. In an experimental
Card JJZ UDC:. 62 - 50 : 519. 25

L 06987-67
ACC NR: AT6018283
hookup, a random signal generator was based on the fluctuation of conductance of
liquid splashes which produced a large number of practically noncorrelated random
signals. Standard equipment was used for the forming and storage units. The
initial-circuit time constant was I nsec. Storage-unit output voltages were
,measured every sec. The discrepancy between the theoretical and experimental
lcorrelation coefficients was found to be within 1074. Orig. art. has: 3 figures,
,14 formulas, and I table.
SUB CODE: 09 4131 SUBM DATE: none ORIG REF: 002
Card 2/Z

N/5
~SIRTSALOV. VDADI-MIR 9ERG:-sYEVTCH 893
-M5
KRYLOV, K.
LTJD IN, L.
Kissladovanlyu Problem Psikhologichaskoy Voyny (Concerning the Problem of
Psychological Warfare, by) Sbornik Statay. V. S. Mertsalov, K. ~Kxlov 1
L. Ludin. Myunkhen, Istkult, 1955
132 D.
Summaries in English, French and German.
At Head of Title: Institut Po Izucheniyu Istoril 1 Kul'Tnry SSSR.

cin _Psease
FD - 16,3
Card 1/1 Pui-,. 14'_-3/2C_-
Author MertsalRK, Ye. N.; Tungachina, Z. M.; Bendyukova, L. Ye; and Voly-
nets,
Title The problem of secondary exanthematous typhus in the Kazakh SSR
Periodical Zhur. mikro. epid. i immun- 7, 11-13, Jul 1954
Abstract Data on secondary exanthematous typhus [Brill's disease] obtained in
epidemiological investigations carried out by epidemiologists in
Kazakh SSR rayon and city sanitary-epidemiological stations in con-
Junction with scientific workers of' the Kazakh Institute of Epidemi-
ology and Microbiology are discussed. A brief statistical analysis
of the data is given. One Soviet reference is cited.
Institution Kazakh Institute of Epidemiology, Microbiology and Hygiene (Dir. Z. A.
Roshchina)
Submitted November 4, 195-3

LAPINA, F.Kh.; MERTSALOV,"je.11,
Outbreak of eDidemic hepatitis in student dormitories; vreliminary
report. Voo.virus. 1 no.6:41-43 11-D 156 (MIRA 11:3)
1. Ka%akhakiy institut woldemlologii, mikrobiologii I gigyeny,
Alma-Ata.
tHY.PATITIS, INF-7,CTIOUS, eDidemiol.
In Russia, outburst In student home)

HKRTSALOY, Ye.M.; SAVICHSVA, L.A.; TRATINA. L.P.
-Mmna%W~~
Carrying of dysenter7 bacteria by healthy rMldren in a L-indergarten
(author's abstract). Pediatrita 39 no-3:48-49 Ky-Ja '56. (KLRA 9:9)
1. Iz Kazakhakogo inatituta spidemiologii, mikrobiologii i gigiyany
(dir. Z.A.Roshchina, cauchnyy rukovoditell - chlen-korrespondent
AN Kazakhakoy SSSR Kh.Zh.Zhumatov)
(DYSNNTERY)

KARAKULD11, I.K.; MERTSAWV, Ye.N! CHOKIN, A.P.
Certain aspects of prevention of infectious diseases in the Kazakh
Ropublic. Zhur.mikrobiol.epid. I immun. 28 no.10:11-14 0 '57.
(MIRA 10:12)
1. Iz k&fedry eDidemiologii Kazakhskogo gosudaretvennogo meditain-
skogo inatituta.
(CO194UNICABLF. DISEASES, py-evention and control,
in Russia (Rua))

KARAKULOV, I.K., prof . Yo-,Nv-j--dotq. BEKETAYEVA, A.M.
Aid of the department of epidemiolTy to public health neencieso'
Sov.zdrav. 17 n0-11:50-51 N'58 (min 1,1:101)
1. Iz kafedry epidemiologii (zav. - prof. I.K. Karakulo-v) Kazakhekogo
meditsinskogo instituta (dir. - prof. I.S. Koryakin).
(MLIC HPIAMR,
cooperation of med. schools with pub. health institutions
(Rue))

KARAKULOV, I.K.; 14ERTSALOV, Ye.N.; ~EKETAYEVA, A.M.
j I
Results of activities of ~& Department of Epidemiology of the
Kazakh Medical Institute. Zhur.mikrobiol.epid.i immun. 31 no.9:
141-142 S 160. (MIRA 13:11)
(KAZAKHSTAN--EPIDEMIOLOGY)

SMIMOV, S.M.~ tERT-SALOV, Ya.N.; BUSHIIA, V.T.
a _r. m -~b~ ~ , e-,Ic. ; 1 =,-n.
criticism and bibilog-apty' 7h-_~ '', 7 - -
. 1
40 no.E .143-155 N 163. 041 2,7 ~ ~; )

CHISTYAKOV, A,T).,~ DIFFIKOVA- N.V, ORLOVA, Ye.M.; GIAZOVA, O.P.;
PED', D.A.- M.Ye.; ABRAMOVICH, K.G.; POPOVA,
T.P.,-,, MAI'VE-YEV, L.T.; RAGEURDIA, A.A.; LEBEDEVA, 111.7.;
PESK6V, B.Ye~,'ROFWOV, N.N.; VOLEVAKHA,N.14.; PCHEL.-Op
I.G.; PETRENK6, m iT - ~nQ'IPLENK0. I.V.4 PINUS. N.Z.;
SIIIETER,S.M.. ,jlT. !EEIIA, T.F.; IMININA, L.B.; BEL7SKAYA,
N.N., nauchn, red.-, ZVEREVA, N.I., nauchn. red.3
KURGAIESKAYA, V,Y,,,. naurhn. red.; I~TRTSALOVA. A.N., nauchn.
red.; 10PASHVITCH, L.11., na-achn, ed., SAGAI 7, N.V.,,
otv. red. j i,,~ "' IKOVSKAYA, A.B. ,
[~Ianua-l !-,." short-range weather f'o-, -ting) Rukovodstvc
po kr%-.n,-.l-,-o,3h=jm prognozam pogod,,,, LHningrad.. Gidro-
meteoi7:;;-~t., Pt.2. Izd.2. 1965. 40,1 1-
(m1 it~ 18: 8)
1. Moscow. TSentral'nyy institut
- - -, zov.

MERT3ALOyA,,,M.jW.- LYUBINSKAYA, A.G.. redaktor; UNILINA, L., tekhnichaskiy
-r,e"k"'t or
[Sewing lightweight dresses] Poahivka zhenskogo legkogo plat'ia.
Moskva. Tsesoinznoe kooperativnoe izd-vo, 1953. 49 p. (MLRA 7:9)
(Dressmaking)

L 2ao*r4 C6
ACC NR, AT'006532 (N) RCE ~i~ UR 934/6 000~66
4AUTHOR: -Yertealova, ff. B.
G: State Oceanoararby
OR Institute qagow (GosudarstvemW okeanograficheakiy
_1n
institut)
TITLE: Temperature and salinity variation in the Norwegian Sea
SOURCE:~ Moscow.. Gosudarstvennyy okeanograficheskiy institut. Trudy, no. 84# 1965-
Voprosy.morskoy meteorologii i okeanografii (Problems in marine meteorology- and
oceanography), 20-251
TOPIC TAGS: ocean property, hydrodynamics, hydrography , sea water
ABSTlUxCT: This paper describes an attempt -to use dimensionless curves of predict-
ability for -treating deep-water hydrologic observations in the Norwegian Sea during
the warm season* The author seeks to find an answer to -the question: Is there a
systematic pattern in space and time to the distribution of temperature and salinity
in the ocean, and what is the probability of,a particular value occurring? Data from
the Norwegian Sea for the warm part of the year were chosen for analysis because of
their abundance over the past 60 years. Variability of values was examined in three
ways: 1 1) by determunng the spatial distribution of variation in temperature and
salini ty, - 2) ~ by computing frequency from gradations in different values of the hydre-
logic. elements, and 3) by generalizing the dotertained frequency- in a dimensionless
Card 1/2

ACC NRI AT6006532
form. On the maps of plotted data three well-defined zones appear: 1) rather unifo=
invariant) water, 2) a frontal zone, and 3) a near-shore zone. Variation
is rather large in the last two zones. There is a general tendency for the variation
to decrease with depth, except for a layer -where the reverse is true. For the central
part of the sea,,temperature predictions are equally reliable for any depth. For the
near-shore zone, however, the temperature of the deeper water may be predicted more
the frontal zone, the -temperature of the surface water is more
-reliably, whereasin
surely. def ined. Salinity is much more variable in the surface layer everywhere ind in
the near-shore zone. By use of the dimensionless curves, the probability of observing
s, certain-salinity above the mean value is the same in the frontal zone as in the
--.central part of the sea, and it is the same at 100 m everywhere in the sea. For
salinities below the mean value- the predictability- is the same at the surface in the
~:ceater of the sea and in the frontal zonef but, at depths of 100 m and morep this does
not app4o Decline in salinity,takes place.chiefly in the surface iayer. While not
perfectly reliable# the method proposed by the author may prove rather useful in
.computerized treatment.. Orig.-- art-. has: 2 figures and 4 tablea*
t
50 COM.Ae/ 309 ME: . mnone
Card

~AVIF ERTS,4 L 0 Vq/ 0. 13.
AID P - 1448
Subject USSR/Meteorology and Hydrology
Card 1/2 Pub. 71-a - 22/23
Authors Various
Title Chronicles
Periodical Met. i gidro., 1, 66-67, Ja - F 1955
Abstract 1) 3rd scientific conference of geophysicists of the
Lithuanian SSR in May 1954 in VilInyus, reviewed by
M. V. Sitich and A. I. Buz
2) Conference on questions of aeroclimatology in October
1954 in Tashkent, reviewed by 0,.--..B-.----Mertsalova
3) The Wth All-Union Scientific and Technical Conference
of Hydro Electric Engineers on 26-29 October 1954 in Lenin-
grad, reviewed by N. V. Somov.
4) A letter by Dr. of Agric. Sci. F. F. Davitaya to the
editor mentioning a correction to be made in a previous
issue of this periodical.

Met. I gidro., 1, 66-67, J-a.- F 1955
Card 2/2 Pub. 71-a - 22/23
AID P - 1448
Institution: main Administration of the Hydrometeorological Service
at the Council of Ministers of the USSR
Submitted : No date

KCRTSALOVAP 0,,B.
,%t, - -
Woo ~-- - ~_r
Methods for the aeroclimatological processing of temperature
data as suggested for the aeroclimatological manual. TrudT Tashk.
geofiz.obeer. no.11/12:14-17 156. MLRA 10:8)
l.TSentral'naya, aeralogichoskaya observatori7a.
-(Atmospheric temperature)

!-T,RTSAT,CIV,l., 0.3., -,,_
-- - , -14#it'inds ftr cniculating r)4-.rnnni%il m-nn mnthly t4--peratnres.
rn rudy ITITI~K no.1:114-130 157. ilari)
(Atmospheric tomperature)

80571
~3. Too 0 sov/169-59-7-7174
Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr 7, pp 102 - 103
(USSR)
AUTHORg Mertsalova 16 O.B.
TITLE. On the Accuracy of Computing the Average Monthly Velocities
(for Many Years) of~_,Wind in the Free Atmosphere
N ,
PERIODICAL: Tr. N.-i. in-ta aeroklimatol., 1958, Nr 5, PP 35 - 41
ABSTRACT: Proceeding from the formula m - (Y - ' wherein m Is the
f _n
statistical mean-error, Cr is the root-mean-square deviation,
and n is the number of observations, the author compiled the
tables of the m-values for n-values from 10 to 500 and Or -values
from 2 to 10, Moreover, on the basis of data of many years for
each month, the ~Y -values are presented in the table from 5
stations located at various geographic latitudes; the values
pertain to the levels: groundll.5 and 5 km, for 4 seasons of
year. On the basis of the two tables mentioned, it can be
Caj,d 1/2 determined that the accuracy of the mean velocity varies from

80571
sov/169-59-7-7174
On the-Accuracy of Computing the Average Monthly Velocities (for Many Years)
of Wind in the Free Atmosphere
0.1 to 0.4 m/sec and from 0.3 to 1.3 m/sec respectively for n - 500 and 50 and
for O~ -values changing from + 2 to + 9 m/sec. This method for determining
the accuracy of computing the mean velocity of wind contains the following
errors: 1) the curve of distribution of the frequency of wind velocity deviates
from the normal Gauss error-distribution curve, In particular, that pertains
to the lower layer of atmosphere up to an altitude of I km. 2) Observations
from pilot balloons present essentially a selective method, because the pilot
balloons are not launched, as a rule, when fogs, precipitations, low cloudiness,
and strong winds occur. In result of the causes mentioned, the m-values com-
puted by the formula are understated Indeed. Basing on the statlsti~:al eva-
luation of the aerologic materials available the author assimes that the
accuracy of the mean velocities of wind computed for n -,- 300 per month near
the earth surface are greater than I m/sec in the lower layers and equal to
1 - 2 m/sec in the troposphere, For n -e-' 50 the ace-aracy of determining the
mean values of the velocity of wind amounts to 4 - 5 rq/sec,
M.T. Golltsman
Ca,rd 2/2

BELYAYEVA . V.N.;,!T~7~AI~VA, O.B.; PASHKOV, Z.D.
Use of the mean quadratic temperature departure and the height of
isobaric surfaces in aeroclimatology. Trudy, HIIAK no.16:20-27
162. (MIRA 15:11)
(Meteorology)

~-CCZSSIO'111 NR: AT4028296 S/2667/63/000/024/001810022
H02: Gavrilava, Z. T.; Mertsalova, 0.
T7TLE: Mfethod of treating radio sounding observations for calculating the standard
atmosphere
SOU41CE: 'lloscow. Nauchno-isaledovatel'skiy institut aeroklimatologii. Trudy*,
no. 24, 1963, 18-22
TOPIC TAGS: standard atmosphere, atmospheric temperature, atmospheric pressure,
atmospheric density, radio sounding observation, aerological station
ABSTRACT: The authors describe the utilization of material obtained from radio
sounding observations and the method of its processing for obtaining temperature
characteristics and pressure by latitude belts and, as a whole, for the northern
hemisphere. Material is obtained from 225 stations on the northern hemisphere for
the period covering January 1950 through June 1956. 145 of these stations weie
seiected for calculating the standard atmosphere. The stations were located non-
uniformly in the northern hemisphere. Best observations came from Europe, Japan,
and North America. Observations were made on Wands and on seve:ral weather ships
in the oceans. The number of stations and observations per latitude are presented
Cardl l/2

I
ACCESSION NIR: AT4028296
in a table. An average interlatitude temperature was assumed in the calculations of
the standard atmosphere. The majority of.radio soundings were accomplished in the
IGY (1957-59). In view of the comparatively small number of observations made at
great altitudes, all the primary processing was produced by season. No less than
10 observations were used for determining average values, and no less than 50 in
each region were used for determining recurrences of observations. Orig. art. has:
3 tables
ASSOCIATION: Nauchno-issledovatel'skiy institut aeroklimatologii (Scientific
Research Institute of Aeroclimatology)
SUMMITTED: 00 DATE ACQ: 16Apr64 EWL: 00
SUB CODE: AS NO REF SOV: 006 OTHER: 000
C.,d 2/2

ACCESSION NR: AT4028297 S/2667/63/000/024/0023/0053
AUTHOR: Mertsalova, 0. B.; Sokolova, M. V.; Syfccheva, Ye. F.
TITLE: Climatic characteristtcs of the temperature in a model of the standard
atmosphere
SOURCE: Moscow. Nauchno-Issledovatel'skiy institut aeroklimatologii. Trudy*,
no. 24, 1963. 23-53
TOPIC TAGS: meteorology, standard atmosphere, air temperature, climate, climatoloi
gy, troposphere, stratosphere
ABSTRACT: Vertical cross-sections have been constructed for a mean meridian, as
well as curves showing the distribution of temperature with height for various
latitudes. The method for constructing the cross-sections and curves is described.-
A method is also described for computation of the temperature of the boundaries of,
the confidence intervals. The distribution of temperature with height on standard* -
days is given. Standard days are classified as polar night, polar day, hot day, t
cold day and tropical day. The figures and tables, which are analyzed in the text "
reveal much of the content and scope of the article. Figure I -- Annual Merldional
temperature cross-section; Figure 2 -- Seasonal meridlonal temperature cross-sec-
gn; Figure,) Curves of the vertical distribution of temperature by latitude
CU, 3

ACCESSION NR: AT4028297
zones during the year; Figure 4 -_ Curves of the vertical distribution of tempera-
ture by latitude zones during the winter; Figure 5 -- Curves of vertical distribu-
tion of temperature by latitude zones during the summer; Figure 6 -- Distribution
of temperature by latitude as a function of height; Figure 7 Histograms of fre-'
quency of temperatures over the northern hemisphere; Figure 8 Determination of
the temperature of boundaries of confidence intervals; Figure 9 -- Distribution of~
temperature of different probabilities in the tropical zone during the year;
Figure 10 -- Distribution of the temperature of different probabilities in the
temperate zone during the year; Figure 11 -- Distribution of the temperature of
different probabilities in the polar zone during the year; Figure 12 -- Distribu-
tion of the temperature of different probabilities In the northern hemisphere dur-
ing the year; Figure 13 -- Distribution of temperature with height in the polar
night and polar day; Figure 14 -- Distribution of temperature with height on cold
and warm days; Figure 15 -- Distribution of temperature with height over the trop-
Ics, in the middle latitudes. and as a mean for the northern hemisphere. The tables
supply statisticaj data used in constructing the figures. The characteristics of
the different classes of standard days are described In detail. orig. art. has:
I formula. 15 figures and 3 tables.
ASSOCIATION: Nauchno-i&sledovatellskly Institut aeroklimatologil, Moscow
Card 2/3

:ACCESSION Na: AT4o28297
(Scientific Research institute of Climatology)
SUBM17TED: 00 DATE ACQ: 16Apr64
SUB CODE: AS NO REF SOV: 019
ENCL: 00
OTHER: 008
Card

ACCESSION NR: AT4028298
AUTiTOIZ: geKtsalova, 0. B.; Sokolova, M. V.
TITLE: Mean and extreme pressure values
S/2667/63/000/024/0054/0058
SOTJRCE: Moscow. Nauchno-issledavatel'skiy institut aeroklimatologii. Trudy*,
no. 24, 1963, 54-58
TOPIC TAGS: atmospheric pressure, northern hemisphere, seasonal pressure, annual
pressure, standard pressure, latitude belt
ABSTRACT: The authors describe a method of calculating mean pressure distribution
at altitudes for three latitude bolts and for the entire northern hemisphere as wall
as a method of obtaining extreme pressure values. The three latitude belts are the
tropic (0-30ONL), temperate (30-60ONL), and polar (60-90ONL). Processing of obser-
vations above the altitude of isobaric surfaces, according to tbe separate stations
for obtaining the mean values by region and latitude belts, was produced by ~he
method previously described by Z. I. Gavrilova and 0. B. Mertsalova (this issue).
The number of observations used for determining mean altitudes is the same as for
temperature. The values of the extreme air pressure in the northern hemisphere and
the mean annual air pressure is plotted in Fig. 1. The differences of seasonal
~/3
C
ard

ACCESSION NR-. AT4028298
mean pressures are presented in tables for the three zones, as well as for the
northern hemisphere as a whole. Orig. art. has: 3 tables and 1 figure.
ASSOCIATION: Nauchno-issladovatel'skiy institut aeroklimatologii (Scientific
Research Institute of Aeroclimtology)
SUBMITTED: 00 DATE ACQ: 16Apr64 ENCL: 01
SUB CODE: AS NO REF SOV: 006 OMER: 000
Card 2/3

Acassimi NR: AT4028298
HKAd
-25
20-
1w,
10 --45 20~ 25.V 40 jaUzo r0 4w 4w, AW
ENCLOSURE: 01
Fig. I Distribution of mean
annual (1) and extreme (2) air
pressure (11,M) in the northern
hemisphere
3/3

S/2667/63/000/024/0059/0060
ACCESSION NR: AT4028299
1410R: Martsalova, 0. B.
ku-
TITLE: Calculation of air density
SOURCE: ~1oscow. Nauchno-issledovatel'skiy institut aeroklimatologii. Trudy*,
no. 24, 1963, 59-60
TOPIC TAGS: air density, northern hemisphere, latitude belt, mean density, isobar
surface
ABSTRACT: In this paper the author presents a method of calculating mean density
values for three latitude belts and the entire northern hemisphere as well as the
principle density intervals. Air density in radio sounding observations was not
directly observed. The mean seasonal and annual density values for the tropic,
:temperate and polar belts, as well as for the entire northern hemisphere, were cal-.
~Iculated by the mean temperature and pressure values for the corresponding belts.
Calculations were derived by the formula
-P-
RT
where p is the air'pressure in millibars, T is the temperature in K, R is the
Card W

H
ACCESSION NR: AT4028299
specific gas constant equal to 2.870386 x 10 -6 erg/g degree. Humidity was not con-
sidered in the density calculations. The results are presented in Fig. 1. Linear
interpolation was used for the differences between the reference altitudes. Orig.
art. has: 1 fomula and 1 figure.
Nauchno-isaledovatel'skiy institut aeroklimatologii (Scientific
Research Institute of Aeroclimatology)
SUBMITTED: 00 DATE ACQ: 16Apr64 EXCL; 01
SUB CODE:,\AS NO REP SOV; 000 OMIER: 000 .
Card 21X 2-"
WEB=
. . . . . . . . . . . . . . . . . . .'' rl~~Af

_1 2653C6-66 E'.1a(1)1kG W
ACC N14... ATS028832 W2667/65/000/030/000/00V
SOURM COM
kta I AL .~13
:,FTITLE'.': AethodS_for the of-the veitica1 correlitions of temperature and
comp4tition
-the ree n of
;pressure.-in f atmosphere and some conseque ces, the-results obtained
Vskir Inatitut aeratrif-stal Trudy, no., 30p:
:1965. 0korrelyatSionnykh zavisickostyakh tempokratury I davleniya v svobodnoy stmosfee-e
(Correlztions~ of temperalure and pressure In the free atmosphere), 3-17
TOPIC TAG&~ stratospherep- atmospheric sounding- tropospherep atmospheric pressurep
atmospheric tempewattire, data.correlation
ABSTRACT.: The paper describes the data and the methods used for the computation of C~
correl'ation-coeffictents of temperature andpressure in the -free atmosphere. Correja-
tions.between temperatures at various altitude levels and cross-correlation between
temper -ature and pressure was studied.0ne aim was to.extend the range of altitudes oE.
the. studies: to -include both the troposahere and the stratosphere.:The
Ascope,.ot:geogrA0h1cil coverage was. also ext40nded;. data. f con 19 stations of. the Northerul~--_,-
h
em sed- L we Ing achines and
p ere. were . 'The. calculat ons Fe ~ made: on analytical comput m
-,on the EV-40 perfdrating electronic computeri The basic meteorological data were ex_'a:
-tracted.from Rerological telegrams of, the International Geophysical Year and the Inter..
6rd 1/2
a&vahld

L 76532-66 EWT(I)/I-CC ON
SOIR UVz667165/000/030/0063/0071.
ACC NRs ATSQ28834 CME:
M.V,
AUTRORil Mertsalova, Ois Sokolovg,
I-0
OpC.,. -none.
xat various levels in the free
~,TITLB: Statistical relationships.between pressur
atmos here~
p
scuRCE.-. Moscow, Nauchna-issledovatell.skft institut aeroklimatolo9L jrudy, no. 309
A davlanlya v svobodnoy atmo-
1965. 0 koLrrqlyatsionnykh zavLrfxostyakh temperatury.
:Sfere~',(Correlations_of temperature and.pressure-in the'free atmosphere), 63-71
JOPIC TAGSZ- free atmosphere atmospheric pressure, atmospheric
sounding
ABSTRACTt This article discusses statisticallrelationships-and correlation between
-free Atmosphere pressures a,tvariousaltitude levels, for 19 stations of the northern
hemispheie and ~ for two seasons (Winter-and.summer). Methods for the calculatio.n-of the
:vressure correlation coefficients have.been described before by one of the authors
O.B.~Afertsalovao. in this publication, 1965, 3-17. The data used were obtained during'.
1957-1960 by radiosounding ascentsi all~exceeding the 25 kn.heightt,for the.ground le-
~Vel: and-,the fol lowing gtItLtudes-of -the Iso baric levels of 850. 700, 500'_ 300, 200i
100, -and 56 t6. some- 30 mb:and 20 mb data were,. also used. Computational processing and -
Card

LL26533-6~t EaT(1)/FCC G1
ACC NRs AT50288351 SOTACE CODEt UR/2667/65/000/030/0092/0101
V a4
AUTHM. ffertnlovai.0.8,1 Fedorova, A*14a
ORGt none
.TITLE: :,Correlation between temperature and pressure In the free atmog2here over the
northern hemisphere
SOURCE:, Moscow. Nauchno-issl:dovatellskLy Inltitut aerokl4matologil. Trudy, no. 30,
105. 0 korrelyatsionnykh zavisimostyakh temperatury I davlentya v svobadnoy atmosfere
(Correlations oftemperature and pressurg In the free atmosphere), 92-101
i TOPIC, TAGS:. free atmosphere# atmospheric pressure, atmospheric
-temperature, troposphere, stratosphere
- ABSTRACT: To gain insight into the crosscorrelation between temperature and pressure
in the troposphere and in the stratosphere, crosscorrelation coefficients between tem-
perature and pressure were computed at the whole range of available altitude level da-
!,ta, from station ground level, to, 25 - 28 km heights. The results are presented in
I form of graphs depicting isocorrelate lines (lines of equal crosseerrelation coeffici-
ents) as functions.of temperature.at a given height H. (abscissa), and pressure at a
Aesired oressure I-correlating height H '(ordinate) Graphs are presented for three re
P.
resentative latitude groups: Keflavi? - northern: Rome - moderate and Aden - tropical
The basic.,'ielationships are clearly depicted in these graphs. All stations show zones
Card 1/3,

I - ~ ~ - -.- - L
J~-
tt-
,
.. .

L 26t-3,S-66
if high positive correlation coefficients in the tropoephere (e.g. between temperature
at 6km_ and pressure. at. 12 km for Rome, summer); there Is a zero rossing zone and nega.
tive correlation for 10 ~m temperatureSL and all other pressures; there is a zone of
high negative' correlation; and a zone of substantial correlation in the stratosphere.
Correlation coefficients between temperature and pressure at the same height are loca-
1ed in the graph on a 45 degree line. The isocorrelate graphs are similar for the nor-
thern and the moderate latitudes, but quite different for the tropical latitudes. This
can be seen byLcomparing the graphs diown in Fig. I (Rome) and Fig. 2 (Aden). The au-
.thors discuss these and other features of the hemispheric crosscorrelation picture in
letail, with the additional consideration of the influence of seasons. They also note
the crosscorreiation coefficients between temperature and pressure at equal
tudes never attain the high values found for the correlation of certain lower altitude
temperatures with higher altitude pressures. In these latter cases crosscorrelation co
!fficients as high as .8 - 'gLoccur. Thus the temperatures appear to be more signifi-
an related to higher and lower Altitude pressures than to pressures at their own
~
tly
levels. Orig. art, has 4 figures.
3U9 CODE: 04 SUBM OATS: 00 ORIG REP: 009 OM REF 1 003 t
Card 3/3-1

L 26531-6.6 E-4-1(1~/FCC C-',
ACC, NRc AT5028836 SURCE COM, UR/2667/65/000/030/011MI32
'AUTHOR: Krylovay L.M.;.qertsalova. 0.9.
ORG: -none
V-

TITLE:-Variationsof air density in the free atmosphere over certain regions of the
northern-hemisphere
SOURCE: Moscow. Nauchno-issledovatellskiy institut aeroklimatologii. Trudy, no. 30,
1965. 0 korrelyatsionnykh zavisimostyakh temperatury I davleniya v svobodnoy atnosfere
(Cn-rrelations of tem'perature and pressure in the free atmosphere), 119-132
TOPIC TAGS: free atmosphere, atmospheric density, atmospheric pressure,,
atmospheric temperature
ABSTRACT: Methods were developed for the determination of the root mean square devi-
.ation of the air density, using observation statistics of air pressure and temperature
The problem has recently gained importance due to progress in aviation and rocketry
~
necessitating air density evaluations at higher altitudes. Geographical, attitude and
seasonal distributions of density and of density deviations were computed and presen-
ted in form of graphs and tables, and,their.salient features discussed. The air densi-
ty.was.zcalculated from the equation of state
WRTV - 10 5'r/M
where, --alrdensity In grams/meter, p - pressure In mbl R gas constant, ecrdal to
Card 1/3

L 26531-66
c.rd 2/3

L 26531-66
ACC NRt AT5028836
puter. The air.density deviation 0: is related to the deviations of pressure, and
temperatu re, c~ , by the Dines 'f 0~;Hflt (71).
P "P
r 2r., 'P
F-IPP + -OT P r -- --,
where r is the Correlation coeftitietit b~t w6en pressure and temperature. The re-
sults reusaled presence of disturbed layers, having increasing density deviations with
altitude-Fig. I shows.this phenomenon for three stations-, it can be explained by the
behaviour of the correlation coefficients, on the basis of (2). Aphysical explanation
was found inthe restructuring of the temperature fields,in the passage from the tropo
:Spheric.to the stratospheric regimes. Due to paucity of stations with high level data
no geographical --ap of density deviations was nade. Instead, a density distribution
was developed for avertical section over a geographical line based on 12 stations, rui
ning from the Antile islands overNorth America;, and Canada (Edmonton) to Greenland,
Icel,a-,,A and over Central Europe to Aden in the south of the Arabian peninsula. The
.large deviations of density over Canada during winter show the result of frequent etrc-
tic air 1 0 latitude. Orig. art. has:-4 figures* 5 formulas and
nvasions down to the 50
2 tables,
QrH REP: 001
. ; I

BH,WiKtWA, A.S.; MERTSALOVA, O.B.
The latitudinal mean quadratic deviaton of *he C,'
the free atmosphere ovjr the northern hEwlsphare. Tlri-,y
no.30:133-145 165. -11~tA 10: 1,2 i
I

Differences in alteration of th, I ....... t!~
.,P,znooth rausc)e in rapid and ta coritra, t ior
Alwiflialova ;in(] S. -i !- '*I - I ;~ I ' ;
SSSR. Q4, 2l3-lYIW,,0: r 73, - :-~ . ',:;
oscillographic studv of the rv-lo~~ i. o., ~ - ' -~,c
Intact and excised Aftad,oifn .t
and at 2(N) kc, appiled ax tindt-r w
contrat tion mirler rOlv:i am im; w. -.J I.. old, I t '~- .,I.
tinn of Fpcoituncom cotitrilctiwi, (,j til , i :rl oop, w-
(rilictinn re-sistance -riscs at hoth i,td h,gh f",j- w ,
of applied a.c.; in sporitalicnis contructiOns. "hich hall t 1, c
characteristics of phase x;ltr-kctiOI-. the. resistance ",rv5
at low-frequency ax and iN unahcred at TOO, fi-equ-C7
Thus the tone of the niu5cle may he defiried a., ,. toriscq'i-cr
of a decrease of the conctI. of ir" ions in tht: iubgLrute. an
alteration of the collotdil matter leadi~!g to biliffirig "f thl-
ions. I h ntra tjon nota'nic 3~;ifts take pNce ill 11'o
surfaces"oft'h'e'Zicelles with ,iaxaholl `lf thc
forces connected with the.iunctvina' prut6l' cDrn-~Il` f
actomyosin. The results of re--,ist-lQe detlis' arc ~,i Ie~::
gr~Ipbically'. G. NI. Konolap-tl
PC q
)ItIJ

1 11~11'.4~,-- e -Yz " -), , -) /,~ ,
J I
AIADZfIAWVA, N.A.; _ItM~~
Yrequenc7 range of anomalous dielectric lession in smooth muscles
duricg the state of a Ocatch" tonne (with summary in English].
Diofizilca 3 no.1:23-30 158. (MMA 11:2)
1. Institut biologgicheakoy fiziki AN SSSRO 140sk-vs. Arkhangel'skiy
gasuderstvannyy meditainakiy institut.
(KUSGISS) (NIaGTROPHTSIOLOGY)

x.- 4,
a I I- 1~
MERTSALOVA, S. N. Cand Bibl Sci -- (disc) Altere+4on--af the electric parameters
of the smooth muscles of mollusks during various types of contractions."
Arkhangellsk, 1959. 17 pp (Inst of Biol Phys, Aced Sai USSR. Arkhangel*sk
State Med Inst), 220 copies (KL, 50-59, 125)
-19-

SIM I TS, Yu.F.;-IIMT5ALGVIL,1-V.; SAVELYEVA, L.L. Prinimali uchas"iye:
Ye.S.; KILACHITSMA, I.R.; l'ILla`,, T.A.) red.;
UfUDKONSKAYA, telchn. red.
[Textbook of the Latin ltinguagelUchebnik latins~.ogo iazyl-a.
Pod obshchei rod. R.F.Shulltsa. I o-qlva, I!iedCJz, 1~i62. 203 p.
15-10)
1. ~' 'ollektiv kursa latirnlogo yan.-ka, I,torogo 'vo koiskogo
i~editsir,!3kcgo in-s-tituta imeni ll,.I.Pi.-ogova (for 3liullts,
crtsalov,, l7n-,-cllyrva, Sinal-im, Eilach-ltshaya)-
(LATIII: C IIIE-LIJ: GU AGE)

-- ~ ~Py
R-aiTSAL.O.VA, YE. N., KOSAVEL, V. M., SU'-KuWVA, N. F., TDIONICH, 0. F.
"Study of the bactericidal properties of the "khB" preparation."
report submitted at the 13th A3.1-Union Congress of Hygienists, Epidemiologists
and Infectionists, 1959.

NERTSJ'Wl,~, Ye. T.
"Clinical Observal",,ns .--.ec-ar,1inr Zffect of N'onsp-clfic --uusta-~ces in c0!71
Treatment of`Tu~)erculous '-14nin~-itis in ChIldren." -~an~ '-.ed Sci, Khar'~ov
'Medical inst, Khar'kov, 1955. (!~J,, No 14, Ac)r 5~)
Sum. No. 704, 2 'Jov 55 - -"urvey of Scieritific and Tec,~ijical 5is~ertatiwls
Defended at U-3SR Hic7her .-.ciucp-tional Institutions (16).

MIKHATLENKO, Ye.A., prof.; PERTSEDIN, R.N.
Improving the design and increasing the durability of cL1.'.,1'vaLor
cutter-type blades. Trakt. i sellkhozmash. no.11:20-21 N 165.
(MIRA 18-,12')
1. Zhitomirskiy sellskokhozyaystvennyy institut.

EXE~~ MMICA See.12 Vol.12/4 Ophthalmoloa April 58
646. THREE CASES OF TUBERCULOSIS OF THE PALPEBRAL CONJUNCTIVA
(Russian text) - Mertslin M.S. - TRUD.TURKMEN TRAKHANST.
1956, 4 (1-17-152)
Literature data concerning the pathogenesis. clinical aspects and therapy of conjunct
ival tb are cited. and case notes on 3 children with conjunctival tb adduced. (S)

EXCERPTA MICA Sec.12 Vol.12/4 Ophthalmology April 58
710. PLASTIC CORRECTION OF CICATRICIAL LID EVERSIONS BY A FREE
FLAP OF SKIN, TAKEN FROM THE AURAL PINNA (Russian text) -
,.Merts lin M. S. - TRUD.TURKMEN.TRAKH.INST. 1956, 4 (153-162)
Data cuTre-d rr-o-m-7ffe-T11-te-r-ature are presented concerning types of plastic opera-
tions, conditions necessary for normal healing of the free tissue flap. themethods of
free skin plastic operations and the author's own experience, the plastic operations

WgiH
I 11~~,W_-~~
were performed for the purpose of restoration of the LujifarL'i7.1%VIMTM of partial resto-
ration of the conjunctival fornices in cases with coarse L:h:,rt, M changes with
eversion of the lids of various actiology, and of complete or gjAMI restoration of
the lids. Two case records are cited. (S)
N

KMTSLIN.9 H.S.; BERDYYEV, A.B.
Our experience in organizing surgical treatment for patients with
complicated forms of trachoma under the conditions of collective
cotton farms in Turkmenia. Trudy Turk.nauch.-isal.trakh.inst.
6:17-20 160. (MIRA 15M)
(CONJUNCTIVITIS, GRANULAR)
(TURDENISTAN-CONJU?ICTIVA--SU.RGERY)

MERTSLI BERDYYEV, A.B.
!~~~
J
Immediate results of operations for tracoma carried out :Ui rural
areas of Turkmenistan. Trudy Turk.nauch.-isal.trakh.inst. 6:21-24
,6o. (Krm 15211)
(TURKMISTAN--CONJTRICTIVA--SURGERY)
(CONJUNCTIVITIS,GFANULAR)

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."m Hurt It, t'1111, V, I-N the
loo I + orwo I Arid d. J4
6,6,v! iw- ~ I % I - or.0 I In wiloreh ir I, m.4-
fract bii a -ctic. And tile lultwrlpts mict w (fie tw-i
t
i
li
l
1sua
i
%.
v agree we
l Wish Ow lilej4ur"I vuluclo
I
l
r exp(l. Valli" of -W And 0 fiq
'
l. .1.111144 Weir fuund (a tie 'Ii
12. 31.107, an(I dictlaylauffine, 0, 14 'fl,
00 3 1 A'S 1 4(1'1 (11) butYfic avid, (UMM, 21,40, and w1u.

00 vote 0 13. .11.71 At t4j*: (Vt dictitylanditle, (l.t". ac ~#u, C*
And cri;II H111310#11 III, I) Im. C1.3fl. at w. 4V1)

00 a
dl~ I to Olitte, (1.101o, 33011. allot pvtkiftw, 11AM, AA :44 or 0

00 30 - (VIII) 111MR41ttt 0 M, M4,25. Awl mdalf,l .1,
'
-1 fl
i
I
4 114 35
A
4
.
at MI
:
,t
) l
c, WW
I, Is Mo. air.) On
'
1
11 0M
w

0 111
?
. at t
; tire Ov.1"ITIS (fill clicl.- I-It'll
!7~v' " .Ill Vo pit. *fill kVID . Cltcl. ftef. In-11
T
,.Soo
K.1" v a v1rItktmtti*m A qlala it;
he litclatilre Sim"-
1. 11 111 A"* evellent Agreement. IV. V acul VI '-1 ;00
gF colt And VII. VIII, IX 1-n4kfcorable slevial:om 1,e 4100
lnIVthecalv&"Iue-"-
I'm ;V. VI. VU, VUI they are I'm high. in CK. orv.k'j.
is ki litit 7 cak-d. 6 Moth. OvvLati-mot (wni tile vak-A.
VAN 41
awrilwd t
t
l l
k
i
h
0

26 C
" luti
ua
tiver-
uterw(
in at t
e or
silm (tat "f the Y.1c"I (41. C. A. 29, :Mlse),
0

too 0
eal
--T 117 It oft Qw a it 0 1 w of 9 is 4
It A41'
or
40 40
48 a 0 0 411

: W 4 It If If w

A
:
: A

004
Field
"See
.
00 fin. I
-
'
' 1611C
kitp
ttw crit
040 1he 1.4,

J! Imif&v
frKn
field tKi
ael Off
unXI I

Oil
A I* It fT.LLi19C.O(.L kIfIlt.ttiffe
IS 0 Aw to &I
I, it it
:10
of v a OF 60 41 u a Od
I V t A I M do A
:t 1414f loortuaftoo to the dauble Glittetti of co-
w
Al
l
R
00
,
-
eflaw
ff-t (Sudeco tiluslete-odubu
ty), .
rrot. Ckeon. (11:8. S. R.) 5, 1 Ark ON 1 WIA) An
-
goo
IS MA41C 10 V11plain the lh&PC fit * i-W)Ifk'rM'l VIVSV
(
w
K"em. 1"I
or a 2-uqu
emll. of layrr forman love
4 temp. chlovit of Ift&VIlact Pro"In 'm fh~ v
sotndtkrIrCcontctr"ctatuvv~
lit"aturr thow that the vs-rielfccl acutmahno
N- dixtrumi ~ C is deed. by the rapid ice,:-wz.~e in
-4 a mrfa~-wtivc liquid. with (all in teml...
utfi(ton, (If a %mail trulp. ~wfr. of ~-ay~
c
1
zoo
fitswKiLticti ties
L-00
.4111, Q..
a a a I w I" I da a 0 v
9 it n ft It Of Ko a

AS

A

00

00 C
00 r hg
of z
of
IT

60 of

%A
so to
00

a
A 1 01 L A ACIALLUPUK&L
ra u lot Ar 10
1, t to to tv t9 it a a it
0 Gie 0 0 a a o
0
0 6 G 0 6 6 4 al 6-0 0 614 0 a a a 0 0 0 660,146sac,
111 is " u Is 14 a 14 ff N 19 la It L) Ll 14 IS it U 11 IS Q 41 0 1 J Q r,
Or A
"Dt.1
k%W #TWM wilk a
kodws" ub" 49 b"
stattlia. J. 64a.
(U. R.) S. 16141(103); cf. C. A. 19. 46"'.
probiom CA law a 2
a kwer CdOt. aw (todu ft =a
I 1111:11111S. at tempo. Md
WoO. Ud AMOM. Of thA 21106L. for U11111
I ubm we cadveamt is Rio Itud (be other il am
(Quowhig: 0-coMim, NErw. bc=W. cWxW.
plewfix MW 70erwuw. Thcw xyttems belose
sausm that while they have sp.
rmpLkt t It
erw
=00
400
a**
coo
a00
zoo
.0
t:o a
too
CiAllifKA1100
AM-4 1 8 OW 0 -0 1 1 9 5 0 0 3 S f
991t matt 1118111twn Olt*
0 * 0 0 6

1~ I 1.11A 1-1-1-1 101-
00 tj
00
A a . I L aBIT&I.1.14110KA4. 4.111RAl"I
a tL
u is AT 10 's
0 0 09000 00 0 11 11 Of *0 00 11
IT440 0 O'o 0 6 0 0 :
M C-A -Vk M P.1
All
Y" I'llMl -Uq11d qg.. it. V 00
711
401144Y INV 11W1411fifflo fit Ifir
'yNtritif KL'I oil lo-. 111- .60
(Cl at (I so*, IT and all Atid C 11N -00
k)'- W' "Id W' ft tis Omchdd It ?,. STAtetn -00
3tIN-HI()- C,11,N-IftO AM C,HIIN-HtO
= have at
nw tempt. a Wis. clit. temp. (4 layer gcpn. S. .00
00*
goo
aoo
400
goo
of*
AltIVOCA111011
too
WO 40 0 41 0 41 0 0 0 0 00 0 a Soo Goo 000 111 0o
4:0

0 cr a 00
96690660ragais 0 0
U I I I - 1 6 1 a , , , . tj 1) 14
L it it r
c
to its SlItLivi"KAt 1,11041
. . I
Ir D U is kis .0 at:
ev
00 0 0
It
000 0 0
0Cra 0 Cr 0 a G a a a S
6a t a Oi as 0 a 0a 1070' lie a a of 40 0 4 a 4r a
161p11 11 4) a Al r) A 1? ist 0
A I AA 00 ~C W it

00
arist f
physicachemicall p"Pemell of Same amine
J
dents CApdb(O Of 94WILdOG. R. V. Illfirg4sult 14.
OF. S. S. U.) S. x8"10935); f I i-K-li
4ew
ntiev, C. A. 19, T76W-'.-The
vild, 4"41 tbiric thirstuiti de"cripts. to the systcutil A 0-
-MV
Inti-iratei and KI&N-vatef was dcwtoml by ths,
JIM
tuld of trutfsoce temiAtil. Me twOllteirms ad ituffitce
CIL
of wMe aminc-oratew systell" vintsible ud wvu
astion
k-S Stuslocuux to chow of istuloweric comp&%
ow
r1plailtrit hy tile rapitt ill,-tlllAl div,wiltill .4
=
CVIMI,d. isad tile knuvi-um 4 tit. P-scdotirrizati,
evil lot'. the Mostly rot., am firl,wilus,
&XW. IWAMAND tile 1-illittillit -101141F -6 -IIAIPIV IkWkWtll
AVASCRIL
oct birsinch Owl :1 fatuity d,vvhtj~d mittimia slidtird
ivt
with incivese of tauts. towersi he auninc. C. H. 1.400

.480
too
-00

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6
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raftaw
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(am
r
thc-y (C -A

so geqnwttk f
gone of tay

00 temp. of lay
is wrmg in
i~indcpende
0
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ti
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A,--
i It*- 51-03..
U 0 AT 00 Ll
tv tv I? a As K
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. 04 to agasea too 0
0 4 0 0 * #4 # 0"4- 0 6 a' 0 0 4 a a a 0 9 006
of Is a m a ft a S m , - 1) . 0 PO
it 4 &
1, --A I I $A 0 CC W It A tj )' ~,' 6,- .1 - 7 4. ".1 - , 1, 1-
.00
-00
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CrXit:~Ajifl .00
R. Gfm' Cke", (U. S
VV
'A "it. dikcu-^i4m of TAkak
VrJ) in regard to ibe rcWftai 1~iw-ti fkv
n( vis~ooity iwthermg and the tuttumol sh,
larmatiort Of birmry *y4tesn* twsr thr io
GwmA -40
iion, It is oowluded Mat lhi~ th-tv
ing that the nature of Vi~-ily g-01CM1, -00
01 the Zone Of IAV-.-t f0llngttilln.
L %tud,d,kv
A 0
A 0
&*0
-00
40
A0
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met -A a 0d ~i-- I w
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cl
80 *60~0"4;000000000000000000'A
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03 1 1 Iasi 1 1 41611111swn

00 4 I a L

00 mall

J. GO
homal
00

00 4r PhNH
00
4 0
00 Tye AM
7
A
04 3 6
facrellfil
so C4H&N
d
ecrem
houlav
temp. I
at IKU
of a h
exisitem

1 Went
with t
Placed
amitw-
a
917ALLUR"AL LITEALTI'A
0 a 3:1
t
0
t
u 11 &V 00 Ll
0 .0
'

it ItanAshk 0 M)9 SUP A;L) J40 hol? JOPIC A, U41 "eige

A- I
L tZ. . . 0 a

am&" ad some imkie~-Waw
bkbw GrWkd tumpmftm ad 0 ikft
R,-V,. Uauuaaad V. F. Vst.=ucv.
S. R.) S. AWIV(1936).-Thr
ag clect of the amiacs cspdt~e of giving in. -Ibe
ilts. with 11CO an amine-Water "Items WjLq
I-
th PhNH.-H.0 of the crit. temp. Ur"' and
ad crit. telup. 63. itktcrval of
at a temp.
1
ag ttf-rY liPtems: 11.0-1
WH,
Ift-CAN. fW)-ftNHs-PhClfNlI,.
m
b
H
oo
O-P
li
sHulfs.-Cliffax. Up
. z
I Its and '00
OAtr d the stulacs derre"" In the
Cd4N# PhCHsHilt. PbNHNM. with zoo
(40-W') The homogenizing "ty of
H.NH. lacrem . white thmit of C.jj,jN
- No direct c"Laaction exists between the -09
' Ing Wica of cot. Pits. at an arbitrarily selected
d their phys. coasts. On the hasis of the re%Wts
daa alf tka mixt. PliNthrUto. the existeace
crit. temp. In the system is asmazed. The do*
of considerable retrognide soly. and the art=&-
lit
l
t
h
W
m
0
c
. PQ
a
s (a t
e
do
curvu accord Wal '0
prVviatts don of the existence al WgWy
04
temps. for a writs of aamstraitilying '
mter Sys-erms. Chas. ailanc -.00
All,

CLASSIVICATICH

S 0- V-TA An A t I ed 0 1. -j a (3 3
Kta n ~ %%
000000 0 0 0
0 0 0 0

I

-A 11-6 12

140 Fam I

6
: tuts.
lor,3-of
6 friet

00 C. A..

sin
.
9
a
.
1
and
I, the

he
therms
im.
1. the
,fte
*I antl
,
'me t
A 9
P~w A
MITAILLURCM&L LIT26.1
-SLA
29,3.,
69 ti
0 0 0
of*
a 45
616~0_- 9, If'O.C0,04-10 COG 06t66666646 go
4";
it
-~A-J- I - A. M a (C W Its It 4 h j
I c=-m at attic" tein7cmr-S of b-M wa .00
. V. Meridin. J Grit. C" W S S. R) S,
3S~~-d' C. A. 29, 5wis- It t,, Otown gri--
. ;~ the* basis of Stakhov-kil*s flWMdIA III
2_411C). * - viodledl - X) + w2XI, "ll"'
r, are surtwe uILMOU of the mist. And the 1-1 -00
rumpuncuis d the binary mixt., re-P.. and -
. fracticis Cd the I%t Component. that tic P-ly- zoo
Crit. temps. could tie rithrr rorwa~e I-
ilm. axis. the form depetkitnig on 'tie relation tit
and the terip. citeffs. of the fwlj Vg"Him"14-111%
f4muL td Pavlt-v4il aft(f Sirato doeq wit lpvr
and is true only f(w 'Peciai ca,~. -00
soln.
-40
.00
00
zoo
CLASSWICATIC.
An a ow 3 IxTt
Al . 4 1 1* 614
0 0 0 0 0 0 00 0 0 It *off 00 0 too
g:
0*00 **a 000.0 00 0 0 *0 go 0 go 0 too 0 1;1

X L 0 M
A
00
00 13;:
00
OR
A 1 4 S L 4 -tFA46LURQK.j LIFtO.1
ST a 6 9"
W C, & it a At W
0 00 0 N 0 0 0 0 0 0 &
0 00
10 0 660000
Is
it a a-ii a u t3 14 Is 15 V 16 14 0 41 Q 41 4,1 0
-A-1
)OV C..Poll
..ectilses ..0 tifCoatol'Is of.
teuslon La phydeachomical
Axos. oxil. anal. ph vi-cht," 1-00
S R 41.1(11135) ---On
1; Fm & charatette3f- of thermal Ict llnata~Arl
t;7x~~ctrvc furru of the isotherms (if surface tm-liam tit All -00
,olde birtary systmi is slao%m. This dLurATit can be At)
I to the tairtary Syst-11% formed toy ccimptaucnt~ thAt -00
pli~
live tit lindisivac& etwinlati. A coat i1stious %arriono of sintitilAr
mgrams oaf sudave tritskin was develtiliral. Ascliiiwtilw
tween the thermail distax" Mail thor devutupit tit -sitt-At, zoo
lecuiltm front the additive Value for 2 A-l"kilml. m
'he xyttesn' &A well A' III Millie Cil-I fill All 1.11a,
ctat;sed, Of interest is the rol"tt'11011.11 fit dIAtT4j11S fit 111,- 0*0
Avaitarici of co6rdinistex of aiurface
(W c roe
t
goo
see
woo
CLASS-FiCATtON
moo
-T--i - if - F- goo
or a a is 'Ifurs A I I a OW .3 di 0 ali
00 ~-, -I 1 6 0 of 0
00 00 0: 0 0 a 0 444
0000
0000019000 ow 000000 00 0

**Go --a- :-e-0 *F'e & a & 4 4b 49 a aa a 6 4 41 4; 0
#61841606 age 0000 666604,0
1 3 1 1
2 a .2116171024 oil V111 Is 11 16 0 a 19 6) 41 4j
a 9 1* it If 11 W Isis usi "AlI a) 'A 0 P0
A 111- J It L &--ft- F~ Q I I 1 9 t I-1-,LAA M CC 9019,4~1- 1i t I t I a it A 6 - -
.
V
1
1 J.
-'!4 0
A If , .0 ~~ ( . 1-f" ~ _
. ,.I _
,

j
v
00
00 for all 3 ratios a Cj(~%Ifr 11p. The Mal. devtin -00
00 Item additivity (kpends (MI the ratio of CjfsS;H. to
-0
T gaaftealzial properties of binary liquid "WAW-61 1. HrO " corresponds Io 34, !7 and 34%. resp., for the
00 a LLPW(ed solubility in the quateram Sys": AtAtal- ratios 1:3. 1 1 and :1 1 U1. Limited solubility in
WjHn,.WdIae-9i ridine It' F Ust Kchkinttev am
15-21
1 S
R
1% S
S
r the jusixeraM gyalm.
'
17
Add
Nd
31
.
.
.
'
Ge". (
mcochem
h
f
l
i
F -
.
.
2
. The homogenizing effect of the
rational t
lit
A
I
.
es o
y
p
93C)). li&wj on general princ
p ern
,