SCIENTIFIC ABSTRACT STRUVE, V.V. - STRUZHKO, K.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001653620005-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 3, 2016
• Document Release Date: August 26, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VAITIAPI, Ayzik Abrarovich; STf~ ,.-V.V., Otv. red.; BAYEVA, A.P., red.
izd-va; SIPMSGVA, T.I.I.. red. izdi-va; TSUTKOVA, S.V., tekhn.
red.
[Sumero-Babylonian mathematics; 3d-.lst millernium B.C.] Shumero-
vavilonskaia matematika; III-I tysiacheletiia do n.e.. Moskvaq Izd--
vo vostochnoi lit-ry, 1961. 277 p. WU 14112)
(Mathematics, Babylonian)

STRUVIC,_V.Ya.; SUDAKOV, S.G., red.; VASIL'YEVA, V.I,, red.izd-va;
ROMANOVA, V.V., tekhn.red.
[A meridional are; selected chaoteral Duga meridiana: izbrannye
glavy. Pod obshchei red. S.G.Sudakove. Moskva, Izd-vo geodez.lit-ry,
1957. 255 p. (MIRA 10:12)
(Are measures)

STRUYANSKIY, I.,, zasluzhenny./ vrach RSFSR
After birtb. Rabotnitsa no.1-26-27 Ja 163. (MIRA 16:3) - .-
(INFANTS-CARE AND HYGIENE) (BREAST FEEDING)
V-

DIMEZER, A.A.1 IYITUBA, M.L.: BLINOV, L.F. kandidat sellskokhozyayetrannvkh
nauk; BOLDYRRY, N.L. kandidat peJagoglelieskikh nauk: GAT-GULIKA, Z*36
GRUDEV, D.I., kandidat sellskokho2yaystvenVkh nauk: XBROV, Ta.G..
professor: KOVALINKO, V.D., ;KRYSINA, 0.1.; KURKO, V.I.; LKVI K.Y.,
kandidat sellskokhozya3rstvennykh nauk; MORDEOVICH, M.S.; POPOV, I.P.
kandidat biologicheskikh nauk;SAGALOVICH, Ye.N., agronom; SILIN, V.N,
zootekhnik; Sam x1l A-4a, vrach; SUSHKOVA-LTAKHOVICH, M.L.,
kandidat meditsinskikh naulc-, SRAPOVALOV, Ta.Ta., kandidat sellsko-
khozyayetTenn.vkh nau; SHEIMMTSKIY, E.I., kandidat sellskokhozyay-
stvennykh nauk; YAVNELI, A.Yu., Imndidat meditsingkikh nauk; RODINA,
P.Il, redaktor; YUROVITSKIT, Ye.l., reduktor;PEVZNF.R, V.I., tekhni-
chesldy redaktor.
[Home economical Domovodstvo. Moskva, Gos.izd-vo sel'khoz.lit-ry.
1956. 479 po' (KLRA 10:5)
(Home economics)

STRUTEV, A.I.
let's completely fulfill the objectives proposed by the party
the government; speech by the Vice Chairman of the Council of
Ministers of the R.S.F.S.R. Prom.koop. 14 no-3:8 Yx 160.
(MIRA
and
13:7)
1. Zamestitell Predeedatelya Soveta Ministrov RSFSR.
(Cooperative societies)

STRUM, A.I.
Work of the Coonittee for Pronoting Rcports of the H.S.F.S.R.
Vnesh. torg. 30 no.10:19-22 ,6o. (MIRA 13:10)
1. Zameatitell predsedatelya Soveta Ministrov RSFSR, predeedatel't
Komissii sodeystviya eksportu po RSFSR.
(Russia--commerce)

STRUYEV, Ivan Androyevich; BOGUTSKIY, Boris Vanillyevich; TATEVOSOV,
S.R., red.;' LOKHKATYT, Ye.G., tekhred.
(Health resorts and sanatoriums of the Crimea] Kuroty i sana-
torii Kryma. Kiev, Goo.med.izd-vo USSR, 1958. 67 P.
(MIRIL 12:3)
(CRIMEA-EMALTH RESORTS, WATERING PLACES, ETC.)

STRUM, I.A.
Development of sanatoriums and health resorts in the bkr&irie.
Vrach. delo no.8:110-113 Ag 161. (MIRA 15:3)
1. Kafedra organizat8ii zdravookhraneniya (zav. - kand.med.nauk
K.F. Duplenko) Kiyuvskogo inatituta usovershenstvovaniya vrachey.
(UKRAINE-HEALTH RESORTS, WATEMNG PLACES, ETC.)

STRUM, I.A.; VLASENKO;, N.I. (Kiyev)
Toward better training for public health, orCanizers. Vrach, delo
4:122-125 Ap 162. (PUBLIC 1EALTH ADMINISTRATION) (1,11 -AA 15: 5)
P
a

H24.D'YUKOVA, 1-~.D.; IN ) c)"'V I" I I
A.K., I,IFS;.iI'S, FAMUTINA, D.K.;
SHARAYEVA, L,!I.; VALITS, red.;
bII,RUYFV, M.I., red.; NTKOLAY~'Mi, 1.11:.; red.
(Atlas or the 7,c-,ipr Carb~;nifurous coals of the Donets Basin]
Atlas ugle! nizhnego karbana Donetskogo basseina. [LPI] X.D.
,3erJiuR.,)va A dr. Moskva, Nauka, 1964. 101 p.
(MILRA 18:4)

STRIM',Vp .14.1.
(-;, -, I ;, .1 9tra(Auro i-~nd coal. notolitial (if th(" j,, '. -1
1,7--t. 29.,118-132 157. (1j ~ i ::" )
(Lvov-Vol.vn Ba5in-Coal gfjology)~

MIROSIINICHENKO, A.M.. SHTROMBKRG, B.I., GARBAR, A.K., NOISEMA, Kh. M.,
STRUTEV, N.J., SAVKOVA, V.P., CHUGUROVA, A. Te.
Technological properties of lower carboniferous coals in the
Western Donets Basin. Koks t khim. no-3:3-8 160. (KIRA 13:6)
1. Treat "Ukruglegeologiya" (for Struyev. Savkova. Chugunova).
2. Ukrainakiy uglekhimicheskiy inatitut (for Miroahnichenko.
Shtromberg, Garbar, Noiseyeva).
(Donets Basin--Coal)

SAVCHUK, S.V.; SEPAKHLXR, A.G.; STRUM, M.I.; SAVKOVA, V.P.
Analysis and properties of Lvov-Volyn' Basin coals. Ugol.
Ukr. 4 no.4:17-18 Ap 160. (ME" 13--8)
1. Duepropetrovskly gorzWy institut (for Savchuk, Shpukhler)o
2. Treat Ukruglegeologii (for Struyev, Savkova).
(Imov-1folyn' Basin-Coal-Analysis)

BOBROVNIK, Danill Prokhorovich(Bobrovnyk, D.P.); BOLDYREVA, Tatlyana
Aleksandrovna[Boldyrieva, T.O., deceased]; ISHCIUINKO, Anton
Markovich; STRMV Mikhail Ivanoy"h- USIKOV, Ivan
Dmitriyevich[U-sykov, I.D.J; KHIZIMAKOV, Andrey Vasillyevi
(Khyzhniakov, A.V.]; SHPAKOVA, Vera Borisovna; SHULIGA, ON,
Pelageya L6kinichna [Shullha, P.L ') doktor geol.-miner. nauk;
GHEKHOVICHY N.Ya_[ChekhoVych, N.IA.), red.; MATVIYCHUK, 0.0.
[Vatviichuk, 0.0.], tekhn. red.
[Lvov-Volyn' Basin] Llvivslko-volynslkyi kamlianovuhollnyi
basin. [Byj D.P.Bobrovnyk ta inshi. Kyiv, Vyd-vo Akad. nauk
UFLSR? 1962. 143 P. (miRA 16:3)
1. Institut geologicheskikh nauk Akademii nauk Ukr. SSR (for
Shullga, IshchenLko). 2. Institut geologii goryuchikh iskopa-
yemykh Akademii nauk Ukr. SSR (for Boldyreva). 3. L'vovskiy
gosudarstvennyy universitet (for Bobrovnik). 4. Ukrainskiy
nauchno-issledovatellskiy gornorudnyy institut (for Khizhnyakov).
5. Trest "IJkrvuglegeologiya" (for Struyev, Shpakova, Usikov).
(1.1vov--Volyn' Basin--Coal geology)

SIJIROKOV, A.Z.; SAVCIIUK, S.V.; STRUM, M.I.
I- ~.-: ~, I " -- - ". --- I I
Coals of the western Donets Basin.
geol. i razv. 7 no.2:73-82 F'64.
Izv. vys. ucheb. zav.;
(MIRA 17t2)
1. Dnepropetrovskiy gornyy institut.

-5 - - I - - --- --
KRIVOBOKOV, Stepan Andreyevich; STRUM, N.A.,redaktor; LOKHRATYY, Te.G.
tekhredaktor
[The Fushcha-Voditea health resort] Kurort Pashcha-Voditea. Kiev,
Goo. mod. izd-vo MR, 1956. 66 P. (MMA 10:5)
(KIZV--MUM RISORTS, VATZRING PIACIS, RTC.)

STRLTyEV, V.; SINELINIKOV, G.
Cast stone. Znan.-sila no*2:29-30 F 155. (MLRA 8:3)
(Stone, Cast)

STRUYEV,V.
Hent of the enrth. Znnn.sila no.9:19-23 S'55. (KLRA 8:12)
(Volcanoes)

STRUM, V.
.Lincrusta. Znan.sila 30 no.12:12-13 D 155. (MLEUL 9: 4)
(wallpaper)

SUBJECT: 11nints 4-5-6/17
AUTHOR: Struyev,
TITLE. Chameleon Pencils (Karandashi Khameleony)
PERIODICAL: Znaniye - Sila, May 1957, #15, p 24 (USSR)
ABSTRACT: In the Soviet Unionstudies of thermo-sensitive paints and pen-
cils were conducted in the post-war years by Professor
V.S. Kiselevt University Lecturer N.S. Rassudova and Engineer
A.M. Laguzina of the Moskva Chemo-Technical Institute imeni
D.I. Mendeleyeva. As a result two scales of thermo-sensitive
pencils were developed. One of them covers the temperature
range from 140 to 6000C with 11 pencils and the other scale
provides (with intervals of 10 degrees) for temperatures from
2300 to 3000 and from 4700 to 5000C and includes 12 pencils.
Besides this, a scale of 18 thermo-sensitive paints has been
established for measuring temperatures from 450 to 8800-
The article explains what causes the change of color and
enumerates cases where the pencils are used.
There are two sketches.
Card 1/2

4-5-6/17
- TITLE: Chameleon Pencils (Kerandashi - Khameleony)
ASSOCIATION: Moskovski khimiko-tekhnologicheskiy institut imeni D.I. Mandel-
eyeva (Moskva Chemo-Technical Institute imeni D.I. Mendeleyeva).
PRESENTED BY:
SUBMITTED:
AVAILABLE: At the LibrRry of Congress.
Card 2/2

STRUYEVA, G.M. [Struieva, H.14.]
Stratigraphic division of rocks in the upper series of the cen-
tral Saksagan' region in the Krivoy Rog Basin (October Revolution,
Friinan, and "'Oth Congross of the CPSU mines). Xauk.zap.Kyiv.un.
16 nn.14:151-156 '5?. (WRA 13:4)
(Saksagan' Valley--Goology, Stratigraphic)

ISHCHENKO, D.I.; RYABOKON', S.M. LRiabokin', S.M.]; STRUYEVA, G.M. Lstraieva, H.M.3
Apatite from the quartz vein of the upper oerles of the Krivo7 Rog.
Gool. zhur. 19 no.4:99-102 159. (MIRA 13:1)
(Krivoy Rog Basin-Apatite)

Yn.N.; FC1-'ENK0, V.Yu.; NOTAROV, V.D.; MC)I,YAVKG,G. I. ;MEL' NIK,
Yu. 11. ; SIROSHTAN, R. 1. ;, DOVGAN1, M.N.; CHERNOVSKIY, M. 1.
SHCHERBAKOVA, K.F.; ZA&RUYKO, L.G.;.GOROSHNIKOV, B.I.;
AKIMENKO, N.M.; SEMERGEYEVA, Ye.l.; RUCHER, V.N.; TAKHTLEYE7,
G.V.; KALYAYEV, G.I.; ZARUBA, V.M.; NAZAFCV, P.P.; MAKSIMOVICH,
V.L.; :ELT_RUYEVA,_q.M.; KARSHENBAUM, A.P.; SKARZHINSKAYA, T.A.;
CHEREDNICHENKO, A.I.; GERSHOYG, Yu.G.; FITADE, A.A.; RADUTSKAYA,
P.D.; ZHILKINSKIY, S.I.; KAZAK, V.M.; KACHAN, V.G.; STRYGIN,
A.I., red.; LADIYEVA, V.D., red.; ZHUKOV, G.V., red.; YEPATKO,
YU.M., red.; SHCHERBAKOV, B.D., red.; SLENZAK, 0.1., red.izd-va;
RAKHLINA, N.P., takhn. red.
(Geology of Krivoy Rog iron-ore deposits]Geologiia nrivorozhskikh
zhelezorudnykh mestorozhdenii. Kiev, Izd-vo Akad. nauk USSR.
Vol.l.[General problems in the geology of the Krivoy Rog Basin.
Geology and iron ores of the deposics of the "Ingulets,"
Rakhmanovo, and Illich Mines]Obshchie voprosy geologii Krivbassa.
Geologicheskoe stroenie i zheleznye rudy mestorozhdenii rudnikov
"Ingulets," Rakhmanovskogo i im. Illicha. 1962. 479 p.
(Krivoy ftbg Basin-Mining geology) (MIRA 16:3)
(Krivoy Rog Basin-Iron ores)

BELEVTSEV, Ya.N.; FOMENKO, V.Yu.; NOTAROV, V.D.; MOLYAVK0,QI.;
MEL'NIK, Yu.P.; SIROSHTAN, R.I.; DOVGANI, M.N.; CHERnOVSK.LY,
M.I.; SHCHERBAKOVA, K.F.; ZAGORUYKO, L.G.; GOROSHNIKOV, B.I.;
AKIMENKO, N.M.; SaERGEYEVA, Ye.A.; KUCHER, V.N.; TAKHTUYEV, G.V.;
KALYAYEV, G.I.; ZARUBA, V.M.; NAZAROV, P.P.; MAKSIMOVICH, V.L.;
STRUYEVA,.G.M.; KARSHENBAUM, A.P.; SKARZHINSKAYA, T.A.;
CHEREDNICHENKO, A.I.; GERSHOYG, Yu.G.; PITADE, A.A.; RADUTSKAYA,
P.D.; ZHILKINSKIY, S.I.; KAZAK, V.M.; KACHAN, V.G.; POLOVKO,N.I.,
red.; LADMVA, V.D., red.; ZHUKOV, G.V., red.; YEPATKO, Yu.M.,
red.; SLENZAK,O.I., red. izd-va; KULICHENKO, V.G.., red.;
RAK111,INAf N.P., tekhn. red.; MATVEYCHUK, A.A., tekhn. red.
(Geology of the Krivoy Rog iron ore deposits] Geologiia Krivo-
rozhskikh zhelezorudnykh mestorozhdenii. Kiev, Izd-vo Akad. nauk
USSR. Vol.l.[Goneral problems of the geology of the KrIvoy Rog
Basin. Geology and iron ores of the "Ingulets," Rakhmanovskiy,
and Illich ore deposits) Obshchie voprosy geologii Krivbassa.
Geologicheskoe stroenle i zheleznye rudy mestorozhdeuii rudnikov
"Ingulets," Rakhmanovskogo i im. Illicha. 1962. 479 p. Vol.2.(Ge-
ology and iron ores of the Dzerzhinskiy, Kirov, Liebknecht, October
Revolution, "Bol'shevik, " Frunze, 22d Partslezd, Red Guard, and
Lenin deposits]Geologicheskoe stroenie i zheleznye rudy mestorozhdenii
im. Derzhinskogo, im.Kirova, im.K.Linkenkhta, im.XX parts"ezda, im.
Krasnoi Gvardii i im.Lenina. 1962. 564 p. (14IRA 16:5),
(Krivoy Rog Basin-Iron o-res)

NASURDINOV, G., STRUYT',VA, 14.
One and a half times the dAily stnndard. Stroitell 2 no.4-5:5 Ap-
M.- '56. (MLRA 10:1)
1. Brigadir montazhntkov zavodn krupnopanellnogo domostroyeniya, Ka-
gnitogorsk (for Nasurdinov). 2. Proizvoditell rabot zavodq krupnopanell-
noiro domontroynniya,Mrq,,nitogorok (for Struyevn).
(Hngnitogorsk-Preenst concrete construction)

T!
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I ~;-59 14 No 4 Prebra-ii ind
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I A
113

111-58-6-8/25
Interurban Coaxial Cables and Their Electrical Characteristics
also containing five spiral quads.
7here is 1 figure, 1 graph and 1 table.
ASSOCIATION: TsNIIS
Card 212 1. Communication systems - USSR 2. Coaxial cables -
Characteristics

BLOKHIN, A.S.; BORODZYUK, G.G.; LESHCHINSKIY, A.A.; OKSMAXI, A.K.;
KOSMINSKIY, O.F.; MANUSHKIN, A.Ye.; MILEVSKIY, Yu.S.;
DRIATSKIY, N.M.; VASILYEV, V.V.; LIVOVICH, A.A.;
ORLEYEVSKIY, M.S.; YIOROZ, I.A.; OKSIAN, A.K.; KNEL G.S.;
SOROKIN, M.F.; BUTLITSKIY, I.M.; VASILIYEV, L.N.[deceased);
GINTS, Yu.R.; VASILOYEV, G.K.; LUGOVSKO.Y, N.Ye.; KIRILWV,
Ye.V.; STRUYKINA, N.S.; LEVINOV, K.G.;BLOKHIN, A.S., otv.
red.; SLUTSKIN, A.A., tekhn. red.
(K-1920-frequaincy telephone system] Sistema vysokochas-~ptnogo
telefonirovaniia K-1920; informatsionnyi sbornik. (By]A.S.Blokhin
i dr. Moskva., Sviazlizdat, 1962. 319 P. (MIRA 16:4)
(Telephone)

SIPIkHTS14ANY V.O.; STRUYKINA, N.S.
Protection of halanced cable networks from side flow.
Flektrosviazl 17 no.6s49-56 Je f63. (MIRA 16.'1)
(Telepbone lines)

STRUYSKIY, Mo
Mixed sailing of ships and tasks of the navigator personnel*
Rech. transp. 21 no.1:44 Ja 162. (MIRA 16:8)
1. Kapitan gruzovogo-te#lbkhoda laningradekoy remontno-
ekspluatatsionnoy bazy flota Severo-Zapadnogo rechnogo
parokhodstva.
(Navigation)

P/506/61/008/001/001/001
D271/D304
AUTHM --Struiako R.G. and MoroA, W.
TITLE,~ A simple method for measuring the efficiency of shields
and filters
SOURCEz, Warsaw. InstYtut.ktcznogci. Pracet v. 8, no. 1 (22),
1961, 53-70
TEXT- A method is presented for measuring the efficiency of shields
and filters; under some conditions it is also possible to evaluate in-
terference fields by measuring voltage drop on the earth conductor or
on the inains resistance. The method is simple, does not require an in-
terference-free location Lind is suitable for analyzing weak points of
the investigated equipment. Only asymmetrical interference components
are considered in the discussion of physical phenomena outside a lumped
interference source and the following conclusions are reached: 1) In-
terference can be only generated due to insufficient shielding or low
efficiency filters; 2) The level of interference depends on the shield
Card 1/4

P/506/61/008/001/OUI/001
A simple method for ... D271/D304
and filter efficiency, position of the equipment in relation to ground
or large metal masses, resistance of the mains and ground conductor,,
3) Imperfection of the shield causes current flow from shield to ground,
excitation of field due to the shield acting an a source and appearance
of interference 'voltage on the mains resistance; 4) Imperfection of the vl~
filter causes introduction of interference into the mains, current flow
between the shield and ground, excitation of the shield field; 5) Current.
flowing between the shield and ground is proportional to the strengt.h of
the interference field and depends on frequency. The measuring method
~s based on the fact that interference voltage drop on the mains resis-
tan(e or ground-wire resistance is caused by imperfections of both shield
and filter; by eliminating one of the causes, the other can be determined
by a simple voltage measurement. The most suitable method for eliminar-
ing shield imperfections is to use shielded connections between the -n-,
terference source and artificial shielded mains. The influence of an
inefficient filter is eliminated by adding a very efficient filter, for
O~ r 11 4r C-
measturemeni purposes~ If the eliminating means are jvrfe t, interfe e
Card 2/4

P/506/61/008/001/001/001
A simple method ror ... D271/1)304
voltage drop will be negligible when both interference causes are ol_-
minated simultaneously. Comparison measurements of the efficiency of
l'ilters and Shieldn lire done by meamuring voltage drop on the resistance
of* artificijil waina; measuring circuits for, both ctimes are Shown. When
shield efficiency is measured, it is usual to disconnect the ground con-
ductor and reduce the capacity to-ground to a minimum; a Faraday cage is
used to eliminate external fields. Weak spots in shields can be observed
by watching the effect of metal pieces moved round the shield or by
patching the shield with metal plates connected to the mass of the inter-
fering equipment. Relative values of interference carried by conductors
and breaking through the shield are measured in a similar manners In
order to determzne the resultant field strength of the interference, the
relation must be found between measurements performed according to the
described simple method and those performed in accordance with the stan-
dard specifications which usually demand conditions difficult to meet in
towns. Once a sixygle-valued correlation has been established, only the
simplified method needs to be used although it does not produce direct
,riformation about the space distribution of the interference field. The
Card 3/4

P/306/61/008/001/001/001
A simple method for ... 0271/D304
authors express their gratitude to Professor Wilhelm Rotk-ewicz fo-~
his advice and cr-Iticism. There are 14 figures and 17 references,
2 Soviet-.bloc and 15 non-Soviet--.bloc. The references to the English---
language publIcations read as follows. L. Blok and H.F. Heating, Doc.
CA.G.R~E., Paris, v. 3, ref. 328, 1952, B5; Report of Meeting of C.I.
S.P.R. Sub-cownitee A and B Working Groups on ISM interference in Milan
frem 29th Apr--! to Ist May 1957. Doc. C.I.S.P.R. (Secretarlat) 367,
(Octobe-r 1957)i C.G, Seright. RCA Review, March 1951.
Card -1/4

STRUZAK, Ily8ztwd Grzegorz
Characteristics of capacitors operating on high frequencies and
methods of measuring them. Inst laczn prace 0 no.3:41-67 162.

STRUZAK,I 1(.G.
1,
General case of cLzvrentp and volt.-Iges ir, it uniform electric line.
Krehiw alaktrotech 12 n .b.2:229-236 163.
1. Ins:.~rtut Laczno:;ci, Oddzial Wroclaw.

STRUZAKY FL.G.
Contribution to tho thuory of a two-teminal network built from
section of a uni-form elcctric line. Archiw elektrotech 12 no.2:
237-263 163.
1. Inotytut Lacznosci, Oddzial Wroclaw.

STRUZAK, Ryszard Grzegorz, mgr inz.
Ceramic tube condenser with reduced inductance. Przegl
telekom 35 [i.e. 361 no.3:88-90 Yx 163.

S,muur, n.
15 years of' ai~rj.cuLfmral econory in People's !'oland. P. 525
J~()IejE (Panstwo-,:e V.y--iav;rictwo ~olnicze i Lesne) lbarsuwa, Volard,
Z1. L',' 110 111, July 1959
:.-nl.hly List o~l East Luropean Accessions (EEAI) LC, Yol. ~) N,,. 9, ziepteiber 1959.
1 ncl.

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ussR/meteorology - Psychrometers Dec 48
"Measuring the Water Content of Fogs With the
Help of a Heated Psychrometer," L. R. Struzer
"Meteorol I Gidrol" No 6, pp 81-84
Concludes'great deal of effort has been vasted
uselessly in trying to develop nev heated psy-
cbrometers in the USSR. This effort is use-
less because calculations show minlymm error
even for Ideal Instrument is still too great
to accurately determine vater content of fogs.
Submitted 21 may 47.
17oT81

7 -:-.:1 -.P
't *f trie size i~nd sh,--i3 of fields
b r L 6 1
ricultur:d crops, ~--es. i step' 5, a- 195)
9. Monthl List of Russian Accessions, Library of Congress, 1953, Uncl.

KONSTMfPIIIOV,A.R.; STRUZER.L.R.
Meantirement of t.he total evaporntion nnd tranapirAtion of alliL
culturnI rror)a by means of evaporimeters. Trudy GGI no.45:66-94
151~. (M.UIA 9:11)
(PInnta-TranspirAtion) (Sveporntion) I

14-1-515
rn
.Lranslation
from: Referativnyy Zhurnal Geografiya, 1957, Nr 1,
P. 57 (USSR)
AUTHOR: Struzer, L. R.
TITLE: Random Errors Made in Calculating the Evaporation Value
by the Turbulent Diffusion Method (Sluchaynyye oshibki
velichin ispareniyap rasschitannykh po metodu turbu-
lentnoy diffuzii)
PERIODICAL: Tr. Gos. gidrolog. in-ta, 1955, Nr 46, pp. 66-86
ABSTRACT: The precision of the turbulent diffusion method was
evaluated in the summer of 1954 by especially conducted
field experiments in Dubovka (Rostovskaya oblast'), in
Koltyshy (Leningradskaya oblast') and at Valday. Eight
sets of devices were installed for measuring humidity
and temperature at heights of 0.5 and 1.5 m above the
line of displacement to evaluate the variability of
the gradient values of metereological elements. One-
hour series of observations were made giving 216
psychrometer readings, or 72 mean averages for 7
minute temperature, absolute humidity and evaporation
Card 1/3 intensity values. Hourly measurements were taken

Ili-1-515
R
,andom Errors Made in Calculating the Evaporation Value by the
Turbulent Diffusion Method
several times during the day. Statistical processing
of the data obtained by the use of the turbulent dif-
fusion method indicated that random errors, dependent
on the variability of metereological element gradients,
reach very considerable proportions. Much more ex-
tensive averaging in necessary to obtain any kind of
reliable data on evaporation. To determine a 5 day
evaporation total, 15 to 20 daily measurements of 10
minutes each should be made to avoid an error'that
would exceed 3.0% of the amounts measured for 9~% of the
cases. it is necessary to make 10 minute measurements
15 times a day to insure the same precision in calculat-
ing a total for a 24 hour period. For 'an hourly total,
one must make 90 measurements with 3 readings in each.
The present method recommended for hydrometeorological
stations does not insure the required precision even for
a perlod of 5 days or more. The existing network of
Card 2/3 stations is completely Imeffective for obtaining daily

STRUM, L.R.
~
Use of soil evaporimeters in agricultural fields in zones of inad4quate
moisture. Trudy GGI no,48:87-112 '55. (MI2A 9-7)
(Nvaporation)

14-1-516
Translation from: Referativnyy ZIjurnal, Geografiya, 1957, Nr 1,
P- 57 (USSR)
AUTHOR: Struzer, L. R.
TITLE: Precision in Determining Evaporation by the Thermal
Balance Method (K voprosu o tochnosti opredeleniya
isparen1ya *metodom teplovogo balansa)
PERIODICAL: Tr. Gos. gidrolog. in-ta, 1956, Nr 54 (108), pp. 80-91
ABSTRACT: An evluation is given of the random errors occuring in
the method used for determing the amount of evaporation
from natural underlying surfaces. These errors dopend
on errors made in gradient observations. The article
analyzes data collected from studies made in 3 differ-
ent parts of the USSR. A total of 11 hourly series of
studies was made to observe temperature and absolute
humidity gradients. The detailed set up of these studies
has been described previously by the author (ref. 515).
Card 1/3 The calculation formula:

14-1-516
Precision in Determining Evaporation by the Thermal Balance Method
E B - P
+ g I~t/6 e
where E is evaporation; B is the radiation balance of Its
underlying surfaces; P is the flow of heat in the soil;
6t and Lie are the difference of temperatures and ab-
solute humidity between the z and z2 levels; g, a con-
stant depending on the units of meApurement, was pre-
sented as E = xy, where x = B-P; y = 1/(l + 0.64At/Zle).
Here y depends only on 6e andZ~t. For each hourly
series y was calculated - the average hourly value of y,
&- the mean quadratic deviation and the variation co-
efficient V . The interdependence of the mein quad-
ratio devia,
Jion O-E) and the variation coefficient (VE),
product of xy of corresponding characteristics of these
cofactors, is determined. This dependance was estab-
lished to determine how far errors of the value of y ar-
foot the errors made in calculating evaporatl~n by the
thermal balance method. The relationship of E and V
depends on the coefficient of correlation between x aKd
y. The latter fluctuates within the limits of 0.2 +
Card 2/3 0.1. The value of the relative error (~E) in detei_-_

14-1-516
Precision in Determining Evaporation by the Thermal Balance Method
mining E, dependent on the sureness of (a) and the number
of repetitions (number of 10 minute cycles of observa-
tions per hour --q ) is determined by the equation
_q E - ta Vf/Y~71 , where.t is the maximum standard-
ized devia ion. The same m t9od was used to determine
the exactitude of evaporation totals for 24-hour and 5-
day periods. It was established that random errors in
calculating evaporation values by the thermal'balance
method are about 1-5 to 2.5 times smaller than those
made in using the turbulent diffusion method. When de-
termining a 5-day evaporation total, it is sufficient to
take gradient measurements for five 10-minute periods in
24 hours to avoid errors exceeding 20% of the amount
measured in 80% of the cases. Thirty 10-minute periods
will ensure the same precision in calculating'the daily
total. A mean hourly value of evaporation may be ob-
ta-ined with the same precision by making 15 10-minute
cycles of gradient observations, i.e., observations mhculd
be made within 1 hour with 3 pairs of psychrometers.
Card 3/3 A* Be

STRUM, L.R.; RUSIN, N.P.
Comparison of various methods for the determination of evaporation
from agricultural fields. Trudy GGI no.57:93-124 '56. (KIRA ior6)
(Sal Stappe-Rvanoration)

KNIMIR, Prokofiy Pavlovich; SPENGISH, O.A., kand.geogr.nauk, otvetstvennyy
red.; jTR
XZJL,I.R., kand.fis.-mat.nauk, otvetetvennyv red.;
GROSMAN, R.V., red.; VLADIMIEROV, O.G., tekhn.red.
[Physical properties of the snow cover] Fizicheskie avoistva
snezhnogo pokrova. Leningrad, Gidrometeor.izd-vo, 1957. 178 p.
(MIRA 10:12)
(Snow)

of 33ils.
dcal pr,-,-,C-rti(-,S
,
-
,~
.(,
~1-.Ysjcal al"(l ci
loo015
195s
2
,
,
2:".11r Di)1-*1 2
J
Struzerj L.B,-
ti3j, if the Deej~
111st t Water-11u,"il-.1c

Title . 5 tile
ults
11
LayL!rs
1957, TID 4, 86-91
ori --- luD
-L by the DuJov scientific
tc(
tz
- -,lore
ere cDjjCjl1c
serv--tions w cilest'lut, S_
)ry :,!'
t
Ob
ract
;:At -
..I Labora
3si-
The necharical COLIP
earch 11Y0,r3102;ic
Res
ley.
CTowill:; bar for a considera-
jils under
horocel'o"Is
s_
is
tile soil-
-)il-s-absoil ,,,isture of
of the S.
Tile T
tioll
tile mds-
-like loan) -
11 lepth (forest not exceed
,le c It
a depth of 15 TI) did E; It a 4%
alill
o
Sial'soil, !-~p ~U,)ture Of V,,e capillaries, equ
-.1 f or
I
isture ru
, 1. D
if tile
ture -all water ca,,3city. The n
till 24
n 19 May
of the Over ariod of observatiOlls, fro
and up,,ra,
i
ya dePth
6
-
le
tile entire "' ards to t
was Clirected d:;vIlw
aulle,
Card 1/2
27
""I= piarl Dd of )bservations cons-
02 Lill. Data oa the therml balance indicate that
.)Illy 33 rzi if ri-Asture ar,_ !)r'mided erer~
etically f~_,r the
,
(_13,~rnward m:,vement i:i tle for-m of v--I)--,r, while only 23 mm
were capable of '-ein~; transferred Li t,-.e state _)f film
water. -- E.A. Daitriyev
Can! 2/2

TTURK, L. (Turc, L.1; PTRUZJCR,,L -.R.,,Fed.; GROSMAN, R.V., red.;
VLADIMIROV, 0,G., tekhn.red.
[Moisture relationships in soils] Balans pochvennoi vlagi.
Leningrad, Gidrometeor.izd-vo, 1958. 227 p.[Translated
from the French] (MIRA 12:6)
(Soil moisture)

STRUZER, L.R.
Sources of systematic errors occurring in tho determination of evapora-
tlon by the gradient method. Trudy GGI no.63:63-85 158
(MIRA 12:3)
(Evaporation) (Errors, Theory of)

Rasp Z t V.A. U.-Yvaytv; Xd.1 V.3. Prot0pCp0v; Tech. Ed.- R.I.
B;14'a! Ina.
PIURKSE; This work I* Intended for meteorologists, hydrologists, 4~hl
h711:~;1h1,1,c'1,t., pgrticul~rly those engaged in the study of an,ow
And Ica and evaporation processes.
CCV`rRAG % This book contains papers on hydrophyalca Which Ware pr* -
sent! d And ds cu as ed at the Third AIJ.Unlon Hydro;oglcal Confarwnco~j
In 14ningrad, October 1957. The Conference published 10 volumes
on various Aspects or hydrology of which this Is number 3. The
.d.-torlal board In charge or the series Includ : . A:,Vr)rvayev
Ch Irm a ) O;A. Alokin BlIzny" (decea:ed)y 0 . Morsuk,
M. "a llk~ft ,L itakiy, O.P. Kalinin, S.W.
MA.PjmDo an
X.-I:av,*,y B.3. he L ' ' M.P. Henkel', B.P. Orlov,
T ~. io~o., A.K. FroaLryakov"o.L. 30kDI0vNkIY, O.A. Spangler,
A.I. Cnebotar.v, And 3.9. Cherkavskly. This volume is divided In-
to 2 sections-. the first contains reports from the subsection
or the study of evaporation processes, and the second contain&
reports from the snow and Ica subsection. References accomwasw
each article.
,Lr.
...... ~1.9~y ~_ T_Y_ (Candidate of Physical and Mathematical Sciences,
3,30 Leningrad] fladlation Balance of Water Bodies
Vor.ntf.v, P.A. rCandidate of O*oxraPh!cal Sciences. 000 Lenin-
of Meteorologc&I Conditions Over
Er, rjWN.J. [Jun4or Scientific Worker, 000 Laningradl
The
ect 0 Ater Surfaces on the Air Transformation 59
Daltr..'Teva'. X.0. [Candidate of Geographic A' Sciences, Tell
M~ecowj Infiltration Into Deep Beds In Relation to the D~terulna-
Lion of Evaporation 64
ffa-_A1A=a21_A_r V.P. Pughkarey [Candidates or Physical
O'na Matnematic 3ci;nc`*nd, 002-LoanIngrad) Beale Trends In the
Study or Evaporation From 8 Oround Surface 72
(corresponding Member of' the Ax.rbaYdzhan Ace.
of Sciences, Doctor of Agricultural Sciences] Relation be.
tween 3oll's and the Hydrological Conditions 84
lCandidato or Technical Sciences, 04 Leningrad)
DeteraInIng Evaporation by the Heat balance Method Using the Data
of' Standard NeteorologIcs.1 Observations 92
0, _[Candidate of OeographIcsa Sciences.
Nu:~n X.P. 000 lAnlngr&dl
Fja5_nt Method for Determining Evaporation 1. tha, AroumA--
and Its ApplIcatlon Within the Station Network 95
Konl'jantinov Ajt- fCandidato of Physlema and Mathematical
Sul "nc_is_,_VHtQL 001 VaIday) Coup tin& Tvaporatl0h P. the Ground
According to Data Supplied by Meteorological Stations 103
--atrusar-L.A. (Candidate of PhIsical and Mathematical Sciences,
Estimating the Error In the XzIstIng Methods for
Determining Evaporation Prom the Ground 110
Blrrukov NJ. (Candidate or Osologlo&4 and Nineralogical
FTFK5-1:,~n.tItut. or Forestry, Uspenskoys) Computing Tots.1
9~,poratlon or the Talga Zone as Ixomplirled by the Forest Rangs
o the Xad nokovs koye Forest District in the Vologodakays Oblast 1 11 9(

Vol4MO06KIlf, L.Sh.; L'iMUZER, ~.R.
Rotary ail.aratus for measuriq; the velocity vector of continuous
media. Trudy GOO no.108:64-72 160. (MIRA 13:11)
(Flow meters)

RUSIN) K.P.; STRUZER, L.R.; S14MOVP S.A.; TRIFONOVAp T.S.
lotters to the editors. Izv.AN SSSR.Ser.geog. no.3:152 Yq-Je
162. OURA 15 S5)
(Geography)

S/531/62/000/129/002/004
D218/D308
AUTHORS: Rozenshtok; Yu. L., and Struzer, L. R.
TTTL7': Results of tests on a recording heat-balance
meter (Iteplobalansografl)--a new instrument
for the recording of heat-balance components
SOURCE: Leningrad. Glavnaya geofizicheskaya observa-
44.*oriya. Trudy. no. 129. 1962. Metody
meteorologicheskikh nablyudeniy i obrabotki.
51-65
T-,,'XT: The instrument was developed at the Agrofizicheskiy
institut (Agrophysical Institute) and was designed for'the deter-
mination and automatic recording of tho following heat balance
components: radiative balance R, heat loss by evaporation LE,
tuAulent heat transfer P, and the flow of heat into the soil
B. it is also capable of recording the difference in the tem-
perature and humidity of air between two different levels in
Card 1/3

S/531/62/000/129/002/004
2--esults of tests on... D218/D308
the ground layer, and the turbulent transfer coefficient K. All
the cuantlities are automatically recorded ten times per hour on
a moving chart. 1,:oreover, R, P, LE and B can be auto-
matically integrated over any predetermined interval of time
(between 6 minutes and several months). The recording of instan-
taneous and integrated values of these quantities takes into
"'Iccount their signs. A detailed description of the device was
given earlier: (Il,leteorologiya i gidrologiya, no. 8, 1961). The
present paper reports some typical results obtained at various
observatories, e.g., mean hourly temperature and humidity gradi-
ents, diurnal variations of B, and so on. Comparison with
other methods showed that all the above parameters could be
r.n.easured with at ieast the same accuracy as in the case of stand-
methods. The device is recormmended for incorporation in the
Service whenever necessary power supplies
and adequately qualified personnal are available. With minor
modifications it may be used for the automation of a network of
stations co-cerned with the determination o.4L' th-e above quantities.
Card 2/3

S/531/62/000/129/002/004
Results of tests on... D218/D308
An important feature of the instrument is that it incorporates
an electron computer so that the recorded quantities may be con-
verted automaticaliy into K, E and P (these are deduced from
the recorded values R, B and the temperature and humidity
differences). There are 3 figures and 9 tables.
Card 3/3

ROZEIIIS11TOK, Yu,L.; STRUZER, L.R.
Results of testing the new "thermobalance-graph' deViOe for
recording the components of thermal balance. Trud7 GGO no.1292
51-65 162. (MIRA 16:2)
(Meteorological instruments)

S/531/62/000/129/003/004
D216/D~-08
AUTHORS: Struzer, L. R_,, and Istomin, A. P.
TITLE: Thermoelectric method of measuring the air
temperature gradient in the ground layer of
the atmosphere
SOURCE: Leningrad. Glavnaya geofizicheskaya observa-
toriya. Trudy. no. 129. 1962. Metody
meteorologicheskikh nablyudeniy i obrabotki.66-87
TEXT: A review is given of the theory of the.thermoelectric
method for the determination of temperature and temperature
gradient in the ground layer of the atmosphere. A theoretical
estimate is made of radiation errors, and some design calcula-
tions for a thermoelectric gradient meter are reproduced. These
calcuiations were used as a foundation for the design of a. ther-
moelectric gradient meter which was developed and built by the
authors. The gradient meter consists of three pairs of junctions
Card 1/3

S/531/62/000/129/003/004
Thermoelectric mothod... D218/D308
connected in series. The output is measured by rn3-47 (GPZ-47)
galvanometers or M -198/2 (DI-198/2) microammeters (sensitivities
of the order of 10-7 amp/division). Analysis has shown that
air-temperature measurements with unshaded thermocouples are
subject to considerable radiation errors. Even in the case of
the very thin wires used in this instrument, the error may be of
the order of 0.30 for low velocity wind and ma-v reach uD to
0.6 - 0.80for wires which are 0.1 - 0.2 mm in diameter. it
follows that a radiation shield must be provided. It was found
that the radiation error could be reduced by attaching the thin
thermocouDle wires to much thicker wires of the same material.
The minimum length of the thin wires which was sufficient to
ensure that the thermal conditions at the junction were indepen-
dent of the thermal conditions of the thicker wires was esti-
mated to be 10 - 15 mm for wires having a diameter of 0.05 mm.
The length decreases with decreasing diameter and with decreasing
Card 2/3

B/531/62/000/129/003/004
Thermoelectric method... D216/D308
thermal conductivity. In the present instrument, in which such
wires are employed, the radiation error in temperature gradient
measurements at a height of 2 m and wind velocity of 2 - 3 m/seo.
is between 0.02 and 0.060, depending on the nature of the under-
lying surface. Field measurements shovied that the instrument
was sufficiently robust. Its readings differed systematically
from the readings of aspiration psychometers. It is recommended
that the thermoelectric method of measuring the temperature
gradient should be used as a general network instrument. There
are 10 figures and 5 tables.
Card 3/3

UZ
-Asey ~'.ojionovich; !;~TR `E:!~, :-R., otv. red.;
VIASCNA, Yu. V. , red. ; Al"UNS, R. A,, -'Khn. red. ; BIRAYNINA,
,.I., tekhn. red.
[Evoporation in nature] Isparenie V Drircde, Leningrad,
Gidrometeorizdat, 1963. 589 p. (VIRA 16:11)
,. Evo r)o ration (meteorologv) )

'ACCESSION NR: AT4033567 S/2922/63/009/000/0242/0247
AUTHOR: Struzer, L..R.; Lozovskiy, V. V.
TITLE: Some experimental data on the behavior of inertia temperature sensors in an
anisotropically turbulent air flow
;SOURCE: Voesoyuznoye nauchnoys meteorologicheskoye soveshchaniye. lot, Leningrad,
1961. Pribory* i metody* nablyudeniy (Instruments and methods of observation);
trudy* soveshchaniya, v. 9. Leningrad, Gidrometeoizdat, 1963, 242-247
TOPIC TAGS: meteorology, air turbolence, atmospheric surface layer, meteoro-
logical instrument, atmospheric gradient measurement, air temperature
ABSTRACT: The method presently used for making gradiefit measurements -- visual
readings of temperature on the mercury thermometers of aspiration psychrometers at
two or more levels -- is extremely difficult and is characterized by considerable
systematic and random errors. The Glavnaya geofizicheskaya observatoriya (Main
Geophysical Observatory) carried out experiments in 1959-1960 for improvement of
the method. Parallel measurements were made using different instruments and
various techniques. This report deals with the results of temperature gradient
measurements. Ordinary aspiration psychrometere vere used, as well as thermoelec-
tric gradient meters in which one junction of the thermocouple was at the 0.5 M
Co~d- 1 3

ACCESSION NR: AT4033567
level and the other at the 2.0 m level. The gradient meter designed by M. A.
Kaganov, with semiconductor sensing elements, also was used. The principal dif-
ference in these instruments is the inertia of the sensing elements. In the
thermoelectric gradient meter it was about I second, for the mercury thermometers
of the psychrometers it was 18-20 seconds, and for the semiconductor thermometers
of the Kaganov gradient meter it was 40-60 seconds. There was a large difference
between the readings of the p6ychrometers and the thermoelectric gradient meters.
The following characteristics were noted: 1) at night both instruments give
identical values of temperature and humidity gradients; 2) during the day the
temperature gradients measured with the gradient meter were up to 0.15C greater
than the values indicated by the psychrometers; 3) in the region of positive
values of the humidity gradientn~e> 0.5 mb both instruments give virtually identi-
cal humidity gradients; 4) at-Ae