SCIENTIFIC ABSTRACT MATVEYEV, L.T. - MATVEYEV, M.A.

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SCIENTIFIC ABSTRACT
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856!4 f '5-0 0 3's*000 AUTHORS: Voskresenskiy, A. TITLE: Water Content and Arctic Regions PERIODICAL: Meteorologiya i gidrologiya, B/05 6-0/000/011/002/005 B012Y3063 I. and Matveyev, L. T. Turbulence of Stratocumulus Clouds in the 1960, No. 11, pp. 14-19 TEXT: The firsz papers on the subject mentioned in the title were published by P. A. Molchanov (Ref. 8)! Ye. M. Kropotov (Ref. 3), M. Ye. Shvets (Ref. 11), and L. T. Matveyev (Refs. 5 and 6). Daring the last 5-8 years extensive observations of stratocumulus clouds in the Arctic Regions have been made with the participation of the author. These observations were made during the flights of -,he Letayushchaya laboratoriya Arkticheskogo i a:,tarkticheskogo nauchno-issledovatellskogo inrtituta (Flying Laborato:ry of the Arctic and Antarctic Scientific Research Institute) and two special-purpose expeditions. The equipment of the planes peTmitted an accurate measurement of temperature, air humidity, atmospheric pressure, altitude, velocity, as well as the Card 1A I 85614 Water Content and Turbulence of S/050/60/1000/011/002/005 Stratocumulus Clouds in the Arctic Regions B012/BO63 optical density and water content of the clouds, overloading of the planes, and micropulsatiun of temperature. The data obtained for the humidity and turbulence of Arctic stratocumulus clouds are presented and analyzed. The major part c-r these observations were made between July and September over the regions, free from ice, of the Karskoye Sea, Laptevykh Sea, ar..' the East Siberian Sea. The water content was measured with an C14B-3 (~'!V-3) instrument designed by V. A. Zaytsev and A. A. Ledokhovich. Most of the measurements were made for St and So clouds which have a frequency of 75-80% in the Arctic Regions. It is shown that on an average So clouds have a higher water content than St clouds. The average 7 water content of St clouds is 0.10 g1m3, and that of Sc clouds, 0.14 9/m.". The turbulence of clouds was studied in summer 1957 and 1958. The overloading of the planes was recorded with a transmitter and an optical self-recorder. The transmitter was pla~-ed at the center of gravity cf the planes. The values obtained weieused to calculate the coefficient of turbulence, the vertical velocity, and tne dimensions of the turbulent form-tions. The calculation of k (coefficient of turbulent vertical exchange was based on formula (1): Card 2/k ~ 85614 Water Content and Turbulence of S/050/16 0/000/011/002/005 Stratocumulus Cloiids in the Arctic Regions B012/BO6~ k I-En-I , where I En-I is the-mean absolute vertical overload of the plane; Ir is the average time for which the sign of the o-erload does not change; _L is the relative air density at the plane's altitude 30 (r, 0 is the.66ir 6ensity on sea-level); ano b is a coefficient depending on tU parameters of the plane. This formula was deriviad by Ye*. S. Lyapin Ref.- 4) and A. S. Monin (Ref It This I-ormula was usod by A. S. Dubov ef. 2), P. A. Vorontsov (Rei. 1 , and L. T. Matveyev (Ref. 7). The R relationship betwe'en the vertical'velocity w'of the aircurrent and the' overloading*of the plane is given as w = b (2), where v is the v6 (A n) actual speed of the plane, and 6 n is the overloadi-n,- of the plane. The meaeurements of the overloading were evaluated by the method described in Refs. 1, 2, and 7. Results are given in Tables 2, 3, and 4 and in Fig. 4. There are 4 figures, 4 tables, and 11 Soviet referenceo. Card 319, 1 ,UTUMV L.T. I- Conditions of the formtion and evolution of clouds in caso of YwUma currents and turbulent ozebangs. Isw. As ME. Ser. geafts. no.1&130-240 Ja.161,m (KIRA 14: 1) (Cloud pbysics) NAROVI.YANSKIr, Grigoriy Yakovlevich; SOLONIN, Sergey Vasillyevich; HATUM. .; RUSAKOVA, G.Ya.,. red.; PRAMMU, -V. 7.s, teklm. r'ed. [Equivalent wind and metbods of calculating it3Mcvivalentnyi voter i motody ego rascheta. Leningz-Rd. GidrometeoirAet, 1962. 98 P. (EM 15:9) (Winds) XLTVWV L T ; BARANOV, A. M. 'Cloud p1waics" by A. M. Borovikor and others. .1sylewed by L. Y&tmMq A. M. B&mnov. Meteor. i gidpol. no.22V-63 F 162. (MM 1-5:2) (C290 pbriplas) Bprov v A. M.) ~Qatvorcnmkll, I. I.) (Zako 1. 0. ) (zontarev, V. V.) P.) V. Z. (Ibrguny A. Khv) (Sbmeter, S. m.) X&MUV,- L.T. (Leningrad) I- - r ,,aacUUtj% the beight of the upper edge and vertical thickness of flaky figurative ei-mb-, . lleteor.i gidrol. no.8:3-10 J1 Mik 15.7) [i eig.1162. (Clouds) 00 '0 ACCLIKON NR.- AT4002177 8/292X/43/005AM/0010/0029 (ladograd) A,UTHOt2tt!Zt, 1. T. TITLE: Claud inversiops of dymamio origin and rising inversions in fogs DDURCZ: Vasa. nanchac,-mWorologich. ww*Acb. TnW. v. 0. MAWya fialki wobodnoy ahmosture. ImAngrad. 1963, 10-20 '70PICTAGO: -mateeriDlolty, temperature lavvrelpa~ cloud. fo.go dynoxic ABSTRACT: I'he report considers problems related to the developmcmt of a temperatar,~ field during ft evolution of cloud formationswith partioular develop- mant of temperahm Inversions near cloud boundaries. Various ratios derived by the - I are consider-W In generalizing an equ3bon for local tempershwe variadon Inside a cloud to form' - ----------- r )or ri ify + OM L #r.+ ff Al (Ir w -W -jr)l 1 0 4w ft, I or. +"r + + k-W 7 -7 ACCZBMOK N&- AT4002177 or 4M LF 0 Ar +'It r a Forsule (Continued) Pere T Is tmperat", 0 in potw4W -tompeiifiire, k - coefficient of turlMdence, -w- velocity of nonturbuj& vertiod moUan of air.-r, =0 0. 01 degree/m - dry "abaUc grael-ent. -L - opwific had of vapor formation. Op- speafflo heat at oonstant air pressure t), z - aftlade, t - Ume, ZM - onanatift pressure. 1R - belot of b '' atmosybere, g - wxWerstion of gravity, R - specifte ps oangant of cAr (257 My./sec- degree). 7bis eqwdka Is Sea analyzed to prowlae a tboorelloil clarification for the I mill it rising inversions in top of varied orlwja by sKlying previously obWaW daft 1i fop wd considubg ocoditions pressit at zero alkitode lows1im. Curves for be up a, alm disbrOxNam in a fw_ am p1cUsd in reldlon to abilude (see Pop. I and a in as =). ftmewerLw. Clow juverawas ad donamw MAOR. so -- calculate Uppershm hw~ WIft and idwe a cloud for vwvdow vabus @.I -swod k. Orig. I WL bw. 4 figures# I table and 22 formulas, ANODCATIONs J%sw JOVAREWE'rJur. 00 ATD PIMSSo. 3046 ZNC14 02 ; OWNS NO MW MVI ON OTRWOOD L ACCUSION NR: AT4002177 INCLOSM 0 1 Fige- 1. jesperature distribution In a fog, Inrelation to height OF. above ground level I - Initial; 11 - derived assuming the-'rate of temparature variation as constant over I hourl III - cal- culated vith cou3lderation of tins- related tempara-cure variation rate (for I hour fro4 Initial) 0,2 a-1; T, - T 0 w.2CI T - 28OKi ke 5 at/eac;"no - a - 0.002'. hare Is air tomparaturs Imadiatily ova groun4 Cs * O)j Tj to air tem- poraturs, St some fIxed heigbt at at- k. aside. -paranaters. 3/4 ACCBSSION WRi AT4002177 SUCLOSURZ 02 "Fig* 29 In a fogg In rolatIOU to belot Smi" 2evel a a 0;0,511nmlg T, T-0 0o501 To HOKi /sees. its." 0*005s. balases. as above,4 41 ACCESSION NR: - AT&030530-- Ammoit: Marveyev, L. T. S/OOW/63AM/000/0092/0091 '~Tjz4j Investigation of appropriate flight conditions In stratus-like clouds SOURCR: Hauchnsy.3 konforentsiya po aviatsionnoy meteorologil. Moscow, 1960. Matei~aly*. Moscow, Cidr-matoolsdat, 1963, 82-91 TOPIC TAGS: flight condition, stratus cloud, turbulence, advection ABSTRU.7: This paper Is one of 13 previously unpublished reports of the 40 papers given at the Nauchusys, konferent#Iya po voprosm aviateLonnoy met4orolog~Li 'scien- tLfLe conference ce problems of &vL&tLcn meteorology) that was In June and July of 1960 In Moscow at the Glavnoye upravleniye gLdromteorologLchaskoy &'.%--Zhby* SSSR. In recent years the author has developed questions In the theory of the formation and evolution of stratum-ILke clouds. In this article, his attention Is dedicated to the development of a method for calculating the height of the upper and lower boundarLea of these clouds. These characteristics have the greatest practical Interest from the vlewpoLng of wf~-~~tther safety for aviation. In the develojewit of his theory, the author considers those factors which contribute to the process of cloud forwtLon,'svcb as wistore and heat advection, the transfer of the latter by Card 1/2 ACCESSION M: AT4030530 orderly vertical flows, turbulent heat and moisture exchange, and heat given off as a result of phase conversions. The method developed. permits him to trace thC origin of the cloud and the subsequent evolution of are" of moisture content, humidity, and temperature. An analysis of the'general solution of the equation system of the unestablished transfer of moisture and heat in & turbulent atmosphere represents great technological difficulties and may be resolvett by the use of computers. The author, thr;x& a series of marbamatical arguments, derives equations to calculate the upper and lower boundary or clouds, and the foruation of aircraft contrails. Orig. art. ham: 3 figures and 28 formulas. ASSOCIATWK: none gUMaTMs lW#b63 so CODE: AS D&Z ACQ: 17Apr" 30 R17 SOWS 005 IMM: 00 OTHER: 000 CWd 2/2 ACCESSIMPI MRs AR4020753 S/0169/64/000/001/B*U/Mg SOURCE& RZb. Goofisikag Abe. ID327 AMORSs Kazakovaq N. N.s Maty 4i'4ze TITLZs Hotbeds and main results of coleclation of vertical motions of air (based on the date of the drifting station "Sev*rnyy polyus-7") CITED SOURCEs Tr. Arkt. I Antarkt. no-I. I&ta, v. 253. 1963, 161-171 TOPIC TA63i Vertical air notion, pulsation air velocity, turbulent air -Velocity,. convective air velocity, ordered air velocity, vertical atr&to- sph9ric cir velocityp vertical tropopheric air velocity TRANSIATIMs A brief classification of vertical motions as a function of the seals, of the process (phenomenon) Is given* Three categories of vertical velocities are distisguishods Palo tion (turbulent) volocitiest convective volocitical ind ordered (large-seal:) volocitiog. Calculation of vertical velocities of the first and second *ategory was mide by using a mothod propo&ed Cwd 1/2 ACCM1O)9 IMs A24020753 b7 P. Fe Zeyebikov and or* proposed one or the authors or the article. At %h9 limits or the troposphere 9 the values of the vertical velocIty calculated Wy the two Independent methods are In satIniactory agreement. In the strato- spherep the first nethod gives high values for vertical v*19cittas. Le Mstveyev DATS Mgt *3U&r84 SUB COM AN p Al INMS 00 Crd F,/2 SJUMKIN, Nikolay Sergeyevich; MATVEYZV, L.T.v otv. red.: BMMIKAIA. L&L,p red, [Clouds,. pr6cipitation and thundrstorm electricity) Oblaka,, osadki i grozovoe alektrichestvo. 2. perer. i dop. izd. le- ningrad, Gidrometaoizdat, 1964. 400 P. (MIRA 171r) . .1 - . I ,I .:-: - ~, .,., : :, . - , . . . . . .. . I . . . . I - '. , : . '. 7 . ,-- I ~~ , I I - . -- '. , -. - I I 1 1 .- , 'i I .. ( , -. -, . I- I , . . ACCMSMOIN M: ANUM AII#HCR: Matwerw, Ift T. ~TLM UqWire~ for now-spay In do deteminstion of the flux of inhwW Tj dd earth astallites mad rA imethod for computation of the appsy clood 6" 800RCZ: Koemidbeeklys iseledevaniM v. 2, no. 1, 1964, 109-120 TOPIC TAGS: artMeW earth satellite, meteorological satellite, cloud# cloud boundary, loh-ared radiation. atmospheric turbulent exchapp. civitotion, turbulence coefficimt, opmaum. almospherte tomperature gradient ABSTRACT: IMe author has formulated the requirements which Ehould be imposed on the aacurW of measurement of the flux of infrared radiation emanating from the atmos- phwe and reowded by an artificial earth satellite and premft a method for making use of daft on *s, total 11m of inbared radiation emanating from 69 earlb's awface and 4- -dationary distribution of cloud coves with hvigb.: mosphere. Rmpbade to an the q" allowances we zoade for the effect, of tallft of dsvp under *0 i0fteace of gravity and 09 laftence of 69 =WMdon flux of beat on 69 famodonof the cloud cover ("peoi&Uy Us wner bovedaM, Vwxavlas a" discived for computation of do mpg my clood boundary, So Lnbmudft of im ~MpAbAbe, wd the m a of Uqdd wolve Is a olau& ACCX WON NR: AN026238 R are established between cloud cever characteristics and auch values as the flux of Infrared radiation at the upper cloud boundary, vertical velocity, turbulence coef- ftcIen16 vertical temperature gradient and height of trowpause. All these relationshipe aret derived in fox , appreciably facilitating their analysis. 7he admis- $me agog to FlAblymination of the total flux of Infrared radiation from the upper cloud boundary gbould not =Dad 0. 005 Cal/om-2. min- I (when dke prewribed accuracy of njmAUon of the beigbt of the upper boundary is 250 m); a relative error In determina-: tion of ft flux F of 1-2% leads to an error of computation of do upper cloud boundary not 250 m under all the conditions prevailing in the atmosphere. 7bere to an ad- exceeding ditiond arror lnhvAwW by odw factors which amounts to an additional 250 m; UmWore,: the w1al error In dairg Me uppea cloud boundary by the propomed mediod Is W~Omt +SW ra. Odg. arL but I Ogmv. 39 formul" and 3 tmblm. JJJBOMTJON: pj~ BM CODZ-. DATZ ACQ-. Mw" NO REF KW: 009 ENC14 00 101 3/2 CHIM.AKOV,, A.D.; BURKOVA,, M.V.j ORLOVA,, GIAZOVA,, O.F.; Im P.D.A.; BEMAND, M.Ye.; AMMOVICH, X.G.; POPOVA, BACHURIKA, A.A.;, IS N.V,; -PZ2W',:B,. e ROMOV, NN.; VOLEVAIM vW.M.; FCMUO., PR"TRENKO . W - u14),WTIMKO. 1.V. % PINUS. N. Z. SHMETM, S.M.. BMMXEVAj,.T.F.-, MININA-,---l-4 9: N.N.v naucbn. red.; ZVERECA, N.1.9 nauchn, red,- KURGANSKAYA, naucbn. red.; MMTSAWVA, A.N'.,, nauchn. red.; 1014ASHE-VICH, L.V., naur-bii. red.; SAGATOVMU-Y, N.V., otvo red,; KOTIKOVSKAYA., A.B.,, red. xual of short-range weather forecasting] Rukovodstvo [Mar PO kratkosrocbmym prognomo pogody. Leningrad,, Gidro- meteoizdat6 Pt.2. lzd.2. 1965. 491 p. (MIRA l8t8) 1, Moscow, TSentrallvWy institut. prognozova HATVEYEV,, Leonid Tikhonovlch: TANKOVSKIY, I.A., otv. red.; - -Yj&b~~A-y 9.M:, rad. (Principles of general meteorology: Pbysiza of the auob- phere] Osnovy obshchbi meteorologiii Fizika atmosfery. Leningradt Gidrometeo'Lzdat, 1965. 875 p. (MIRA :LLq,-12) MAT FEYEV, _IL.T.,_prof. Vasilii Alekseevich Belinskii; or. his ,)Oth birthday. j gidrole no.1:64 , 1:0 : ~~, 7 . Ja 166. (fl KIRILLOV, Valgrian Valerianovich; DMITRIYEV, I.N., retsenzent; - ~T otv. red.; YASNOGORC)DSKAYI, M.M., red. [International System of Units of Measurement (S1 1 in meteorology] Mezhdunarodnaia sistems. edinits izmerenii (S1) v meteorologii. Leningrad, Gidrometeoizdat, 1965. 150 P. (MIRA 19:1) fACC Nib AP6032070 SOURCE CODE: UR10392/661002/009/090NODID AUMR-.- Dykova, L Mhadxw=L-~T ORG: none TITLZ: Evolution at the clwad aw temperature nelds in a moving cyclPne (a numerical experi ent) SOURCE: AN SOR. Isvestlya. Fislka &tnwsfsrY i Ok*an&o v- 2- no- 9, 1966, 905-919 TORC TA=: cyclone. elmd Amnation. atmospheric temperature. atmospheric turbulence. cloud water cortent. cyclone cloudiness ABSTRACT: A numerical experiment is performed on the simulation of conditionS for cloud and temperature field formatIODI in & moving cyclone without taking irItO account its thermal asymmetry. The vertical currefflas. turbulent exchange. and Went beat were ecasidered in the initial apations of beat and moisture transfer. The basis of the nweerical solution of the equations is a method which WAS developed earlier by ono of the authors. The colvalstinse are made fdr a large range of variations of the parmsters involved, assamimg different proftles of the vertical vebeity and forms of the boundary conditicov. Much data are obtained allowing an estimation of the influence of the verticid velocity, released latent best. the surface tenwerature. the air moisture. the variation in air temperature, and the cleud water content. Some results of the similarity theory for determining ** ielaiive-coalribution of several parameters are also used. The results of the ~erieal eftniation agree quite well with the experimental data. At the same time. they show that the thermal regime and cloudiness of a cyclone are formed seder the ImMewe of maoW factors which are quite varted, OrIS. art, bus: it. iiiiweNt Ib Ambles, &W 21 Ibrntulas. [AnOwel ebabnot) SM COM 041 BUM DATZ: OeApreol ONG RM 0291 OTH RZF: 0031 212 ACC NRs AI,6012919 A11THORt Lushev, Yu. G. ORG: None TITLE: Numerical plan for a short-1 SOURCE, AN SSSR. Doklady, v. 167, r TOPIC TAGS: weat.her forecasting, cl atmospheric model, atmospheric clouc SOURCE CODE: ?fPN/C',020/66/167/005/1042/1045 TA.- n weather forecast of stratified cloudiness 5, 1966, 1042-1045 -tratified dd=., computer calculation fied cloud layers forecasts. The topic's importance is dvie to the influence of clouds upon the important heat transfer and radiation balance of the atmosphere and the earth's surface. The basis of the theory is the concept of a sufficiently complete augmentation of the cloud elements by particles participating in the turnulent excha- nge. The theory does not, but can be extended to account for the fallout of precipita- tion from the cloud and for its radiative heat exchange. The basic system of cloud equations, which for the forecasting is combined with the atmospheric equations of motion and continuity, accounts for turbulence, humidity and the specific water con - tent of the cloud and considers the transfer of beat and water vapor in the turbulent cloud atmosphere. Ground boundary conditions for himidity are approximat,~d by t%e use of a statistically well ce)rrelated linear relationsh1p between the dew ooint and the Card 1/4 -UjC . 5,- 1. 5.11 ACC NR: AP6012919 air temperature near the ground 3urface. Plans, aids nd short-cuts for the solution of the equations with the aid of a digital computer are discussed. Conpatations were compared with the factual prnsence (or absence) of clotidiness on isobaric surfaces with their associated weather data, for 1540 points. The verification factor of the method was found to be about .79 abd the reliability cKiterion was over .57. This recommends the method for practical utilization. Orig. art. has 11 formulas, 2 tables., SVIB CWFI: 04, 09/ SUBM DATE: 30jun65/ ORIG REFt 014 Card MOVIM, I.V.. trishener. Co-istruction of 1,mildings fron lprt:e-nize aavod liaest"no blrc;~h. 31u, - st-ol,tekdi, 10 nc.120T-12 JI ( Z.RA () : A ) 1. MoldavsT-ole otde'len4--,e Vraeso.--.mmogo na3lc.--.uopo itizhenern.0-tt--I-ti-,Ic'lt.-13kogo obithchestya. (Bu I-,Lllnt, 't I ocka ) MUM, 16.T.. lashener. Usperiame vith uslag larip WIdIng blocks of aattml stome. ftrol.prm. 34 no-4:15-18 Ap 156. (Km 9: 8) L. Moldgip-mefemV strar. (ftildiag Oows) '?ovich; PRIX. H.. red.: MOKS, V.. taktm.red. - ~ -Tpm~]L Evecuring the strength of sawn-liamstome structures) Topromy oboopechmadia mnollUwmtl kladok Is pll*nykh Isvestulakov. KIshbwv, Oon.lad-vo Vartle Holdovenladog" 1959. 102 p. (NJU 13:2) (Iduestons) I z0villyfl, .1,&v I ~ I __Y~sll'yevlch) FIT"A, l.., red. [Largo-block and large-pane'L from lime:3tonel Xrupnoblochnoe i pane I I rtoo stroltell- stvo iz pillny-~h izve.;tniakov. hishinevp Kartia veniRske, 1961). IW p. ( M I R..~. -, ~t ; I ) KATMEV,,L.V., vaterinarnyy Yrach Diseases of th* tenoligamentme apparatus of pelvic extreidties in hard bkLUs. Vetax-inariia 41 no.1-1: 62-63 N 164. (KM 18:11) 1. Torosovskaya stantsiya iskwstvennogo osimefteniya sellskokhoz,vaystvennykh zhivotny-kh, Leningradskoy oblasti. PATUNTO 16 tLeniapad) Incremse of the interference rejection of synchranifttion In television. Red' no.1207-40 D 160. (KMA 14:1) (Television-Interfwwas) 4 -V v TOM A, V., st7arshiy nauchnyy sotrudnik. doktor; HATUM, M., mladehiy nauchnyy sotrudnlk* doktor. A =as from practice. Toterinarlia 35 no.2:43-44 F 158. (MIRA 11:2) l.TSenl.rallnyy veterinarno-baktorialogicheskiy institut, Sofiya. (Swine--Diseases and posts) r* I r, M. (Riga) jgDonade effectiveness of concenty-ition of flax production Gn the )calkhoses. VemUs latr ak no.10:23-30 160. (zw -0:9) (latyle-Flax) X. (R4%) -- ! geonamle erfectiveness or ratioml lamtlen 00 ameen--v8t4lan or zo~rze-W ngar-beet production. Testle Letv &k no.1:25-32 161. (mm 1019) 1. Akadenl7a nank Latwlyakoy SSR, Inatitat skomoitikle (%pr beets) MA,TVMV, M.A., Auzh. Freezing of air ducts in mines. Gor. zlrur. no.7:46-o n 163. (MIRA 16:8) 1, Hookovskiy institut radioalektroniki i gornoy elektro- makhaniki. *lA a 9 a 0 al i 00:000:006:00008 *0 *go go* 0*00's C. 4 C. ft 0 a, a '1,' 1, A INS 0 0 9 0 I W V, A, I., 10~ *,-.0* 1 It A j -to loop sbv~l IL 5L. Fad Simmom, TIL F. , I:mk#kk j % A.M. rrs VIS lr~* V%, I AFFARAMS Film Lt 04W TM MIMMATtuS UP SUMA"M. KreaMika. l*M 191 l *0 ectric. to -c, vorfeury &- 1.2 --The a"aratm is an e t 4011 L 't 00 -wa t Amp vapow. quartz (nonvacuum). 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V* 608 so so obv*Uovo No As A&MMIA10 We PO 81022"0 (201'"181000, 00 1 0. 4io, Labarstarbs., 196W04 601 1 W1 go oveoved, prollialuary overimento to deterni see at tM Sol-notalle 184usisso, Is vVelft-celted ST40 essfirued ust ibe a I It to Uposelble to do this by teklag Debye X-roy phiptogregU. swrwixomu so the apperatift at mism-urtallie Imselveleng by die. 0010 solving 00 Irm In korsobleris said. or by doemposing It with W MWT fulphato sclutice, am not gtve satieftotery remits, ad OW slostrqUo wood (" ressimpo" 1by see%%). Vows a at sopeabo lodide *01"Ining frof 1911", am rimally adep%de The eptimme. onditims tar this nofted of %106 Ve NW',2h9lftAM6W4W9A0mr1We The SORGENOW116 10018=84M "Pan%" MOO, In "As fte"ons sms Withe age saw Withoot a prol= removal f goo it Wo ~It* by fAw heavy-Altuld f2ahakim aol4od, vere tbm ;00 tool "JIMPAMI -ftek I*$ at eaft Irm of "Mrsob -Oft""- 1 "Amp em '46641L& d"AW~14 LSIMPOR "UMMOM too Iwo Mra-01. as .0640 Icapas. wov *00900*0000 oooe*-Oooeooooooooooo0009*00**00 00 eag"Itis", Ilmoo ow3re amil" to gftpbito, farrow waft, oqw*. Utoo aswoolum, wou-silleate, espoolus oramiliestop sawAll- 410111te, Isom 81116148 ad prdtOo OM tOW. Li&--i sarreepudiag 00 to hematite a quarts sad s, - I sere also abserved in angles 00 fres *Ash 09 grepUte Ind ben removed by Igaitlem In jS 4141 Vw sowidemee, saggooto that emse st the Imeftelgag we promest is a 00 Nwr "stay womphems state. The petregraphis winsissitift 00 dw "t give mew positive results* Isms, shosiou smalyses at aw so mem-amwile residues after removal of 00 graphite by widatift 00 an giveme 89 00 0000.40*0400.004OW000.004 COOC lo wIll" 'ea2=-Lb--W-,x8b!r a pmddk askams. se doill" i6 dwepw to mamewl am low 04, Ms. 400 AL. M. symosom ~** 4.400 r0 we* 7100 See 400: 400 see lee moo so" Sowing l l AN CEW &$I "low 010 a.. &M assia a I f o -a 000,041 all, ;4, o,ll 0 lam 9 -1 a a 9 a 0 i a 0 0 0 0 0 010 0 0 0 0 0 0 0 0 0 0 0 0 0 0 4-44 1 to 0 02 a-WO-SWO-0-0 0.010-0 -Ab a a a WO 00 000 w a DoOmMmOs d Of d1mb 6 VAN. so 8=1~8da"Wed d IN" p"s. Apd". "M U. IM41 as imw~ b" In qkft bb Guam bw it" vampirpow awl Awbv~ a fth- *AM ws", m- - - a *A-fA" mum &%K% of at #a pwpmw*,A AD-". TI Maw 7~0 ,r-4 -a --- 1 9 r a n 10 j-q;,;jq- ;00 0:00 *010 4 boassaaws aoses -00 . -14L-T -0 fee 14ATV!f.,V, R.A. 'id-ral c~,,jrs, :r, , ..,. , f . . . - . -.. -. ~;uskvj. ~- !,. I z ~ -,., c, n -. rQ I I . 1 ~ t - r-.- ,1 , z4c~- (j..i- a~- , -C .,icr, fil- YJ Tvr-vv. M. A Coshchiy Furs 'Fekwnclooii Sllikatov Course in the T,~,chnclcijr of silicat s, SY) Y. ".. Ya---~ y-v I -,en-yurin. PCD (B, '::-d, 3. S. Z"hv-t (.va, Moskv- ~'t T; V" d. t19,49 Contents: Chast' 4: Tekhiinologiya Steklomass, Proizvodstvo I Obrabotka Sterloizoelly Text covers physical and cnemical properties of glass. its thermal pruperties electrical conductivity, composition, production, and thermal, chemical and mcahanical working. -1 Al Ole 00 -Woe V 6 a 0 M u a 2 "-az I SNAMbldwo tw a Moe- in Zol= b - __7 WSW' metal Or OMAW V VC04ohnn tbar is first appl~t a gay" 11 lWj 4 2 dst. at Clow, coment. Impkilf, "Msist owl a W allicale *Qli~ After this tag" -trim. a I,q- IAZ" is apj&n~ tit Znthw and clay mixed with a -4n A Cat 11mch DW 91916119. 000 Blow. *901AW Ti )00 400 400 0 it too and )btftey, M, At gLUS-ES or TM OSOMPM, n (6) 23-25 (1946). Cavaes of the premixts" destruction of the refractory lin- In In looomotive fireboxom are (1) faulty insta"lattion of &rams* (2) use of low-grade refectories,, (3) use of a binder bavIft a different omposition from that of the br-ickq (4) very rapid drylas of tb3 arebas after installation,, %5) leak- of eommeatore and tubeaq and (6) strong jolts in service. P temiperatum cum of a fuel oil fired loomotive for a L 2D br. period dows abarp variations. Linings for lo - tive finboxas abould bave a "frectoriness not lower than 1730"C. and also high resLetanoe to therml shook. Cm- pressivo. strength 9bou3A be not lower than 120 kg./m, . Ldtial moftenift under a load of 2 kg./m.~~ a1muld be not lower tbon 135eC.p Additional shriWap at UM should not be ovwr 0.7%. , joir row: bmi COS 0AU ne cb, V0 ftooA e mob go wkb com nee gee goo not w I-vablaw Dow WIMAIRY "W" ;-40 omw 009 60149140 4M ASk gas 1* we "alwoodef 369 woul;;*01m;j i's ;i iwl TI *-so 0 0 OLO ! ! 2 ! ! 0 0 0 0 * 0 0 00 -"! !O1! f,9 0 Ole & 0 0. 0 0 00 0 0 0,0 & 0 A _t-x I_ 00 00 :00 00 so: .0w as -**I 00 .00 941 at* =Illo 00 00 LAINWININIFY CP" is OWN" Teftdiff d Sibs"" UAI_"a 'I* a !_-J!nT9 t-Miltum " almakirbei tekk~ OWIpy i W lit U00 00 %1 A. MATV1119... AVV C. N'. lhiwm~iv. IN'tillsh"t by &S III . 100 230 lip ftk-r 14 rubk~. The book covrn mirtbuds of itivegivating clAy%. tw~% ins birmlims materials and glaw. and Analyzing silkat~, Mociple. I al nwtbqd,. deer ilm of apparatus, and ifts1rurtium "I Ijtm r.ic~y -wkn. Ar~ given. It Z K COO It sma.. 410.01' sanowo to Sol*jpj loss a" a I j I a V AM &t a w 4 4 dal 1 0 ft -3 As 0 3 0 V -4 1.9 0.0.0 41 0 ; 00 WO _02 AD 4b Ab ion a[ lob CA J1 ow u a me men" W. A. 1 4*A&4*i ban 9 - ~ ~ ~m T . Ilir -d I :t .MO' i6z; 4 =N4. Vub. ; -.Ma ii-mmar- 6; -tw...ft '40: Mo. m vii 1R. Isim. mowkuqd JG.42f . )- = MAITZIP M.A. Effect of the hydration of glassy and crystalline sodium silicates on the kinetics of their solution@ Trudy MMI no.27:118-228 159. WIRA 15 -.6) (Sodium silicate) (Hydration) -- MAITE-IM, N.A. .Chemical and alchoacopic investigation of the structure of sodium silicates hydrated in the vitreouO state. Trudy MKUI no:27:129-136 1590 (MIRA -15:6) (4dium silicate-Analy8is) MATVL'YEV,, M.A.; RABUKRIN., A.I. Using soluble glaso for waterpmof molds In precimlon casting. Trudv 14EETI no.27:156-171 159. (MIRA 15:6) (Cilaaa) (Molding (Younding)) MATVEM, MA.; RkBUKHIR, A. 1. RNdd analyals of liqulA gU". 71n, VIMO 6 no.5:592-593 161. (KM 14:10) I, "Ovskly lastitut imai D.I. Hoaddoym. (Gl"s) HATAVEM, H. A. Hatveyev, M. A. - OThe methodology, for detsivaning the solubility and the silica modulus of vitreous alkline firilicates,0 Trudy Moak. khim.-tekhnol. Im. Mendeleyeva, lamw 15, 19". p. 1M-69 SO: U-5240, 17, Dec. 53, Ustopis 'Zhurnal Inykh Statey, No.25, 1949)- M-11EM. N.A. 35329- HATVUEV, M-A. Polucherde vodoustoychivykh bysokoprochnykh BtroYdetaleY iz gipsa. Trudy Mosk. Khim. Takhnol. In-Ta T.m. mendeleeva, Vyp. 16, 1949, S. 43-52 SD- latopis' Zhurnallnykh Statey Vol. 34, Moskva, 194c) MAT7EM, M. A. 35328. Opredelenie Rastvorimosti Sh&,elochnykh "ilikatov, Gidrati--c-%,annykh 'I- Steklovidnom Sontoyanil. 'Trudy ~Iosk Kbim.-Takhiol. In-Ta Im. :4.-ndeleeva, vyp. 16, 1949, S. 110-13 SO: Letopie'Zhurnal'nykh Statey, Vol. 34, Nbskva, 1949 KATVEYEV, M. A. 264,16 Ustaaovleniye mikrostruktur7 metallurgicheakikli shalakov po kldmichesima nalizu. SbDraik nauch. Rabot po vyazhushchim materialam. m., 1949, s. 164-74. SOt LETOTIS' NO. 35p 1949 IIJMMM, . Y. A. Techno'logy (W.--ter -Psistance -l' r-msima b~Alding mmteri;lls :Inrl its ':), Promst.roii,d.-t. 1951- Eont _LLIt 2: Russ-an Access--mg, Ubrary of Congress, Noveraber 1952. T*CLAS-31FIED. I-VITnaw, M. A. Fbwdryj~ lydrosilicates as SUAIng lbterla for :Xo]As wA Cores,,* M. A. latvaM., X. P. Tkacheakof Tisch Scip TMIL GlavIltuash. Lltey Prols" go 8, pjp 19~-21 GAves. characteristics -or sodlum bydroalllcates, by both aTaeous aid vepor mitthods, and d1scusmw their blndlft- cope ity in sank-clay autts In INDIA mad eor* moklm. Mft (30 or allieate Is sufficient for cbtalulag good r*mats. P.-'L V77% UN of gas%* my-- is NO" INSOMM a" #or )w I A. mat K. M. TkMrblmhD =='=ANQAw.vG~Mw)- Olawas" 16. tamed 4 , M. day. quartz. saw. ciav grog, I as, knobw am. OW Zr vili- - CAIV~ Optimuns ratios of bond and filless a detil.by"ns N. hydnxilmst obtained by medied of own bydration with Various ss-,Its. n? ,t,,; AH in the cc. of twelve re . geired to hydr.te I S. of vi!nwm elk. officate. Oplimma III, awde- lus (Ah xits 2A-3.0- Rest mines were: (a) W)% gM 4round a to;"" Sir" of 491K) openina per s4. am. ww 10 bvk irlwAll- rate. (b) 110% , VvW (size as in (a)). 25 posed. asibratos. 15 reir.C-~7 C13y, Aftd M hydrosilkinte. sisal W 9U% knotin grog (v- an in (a)) asp] It) hydrunificate. Witter was added to (a j. 1 6). anti (c) -o sive 16. 25. and 13 parts per I(M) parts of mix. resp.. an w". basis. InaHcam.Alww2.S-3.(l&zd Fil 0.0 Z". 11. Z. Kansich USSR/knaineerlng - Refractories, Nov 51 Technology "Iffect of Steen Pressure on Physicomechanic&I Prop- erties of Silica Brick With Addition of GramUated Bodium Silicatet" P. P. Dudnikoyp Corr Mm, Acad Sci UMR, M. A. Matyeyev, S. I. Turchik "Dok Ak Nauk SSSR" Vol LMM,, No 2, pp 255-258 Introduction of sodium silicate into sand-lime alct intensifies formation of calcium. hydrosill- as-600 dub to Increased content of active ai]4c&f find increases effect of higher stem pressure 112 autoclive In reipect to Improving strength of Refriwtbrteii if NOT Tecbnology (Contd pro6uct made by bydrotbarMa method. 7n adda, doimuio~44 Sodium siliewtA dsero~iaas aetvr mtboorp- tj" of brick, baying favorable effect on its froet-resistanco. 29M, t' CI 'IL. VI ti t ak. I L:L- at ;-t4 la tt 1 k~~ A lot R I' :,A,t -[Tilt A#,:oshkov, M.I. "Textbook of Mining" M*tyllurgizdut Alymmakiy, A.M. (two books) Voronin. V-14. 3orodetakiy, P.I. Kaplunov, R.P. Ratvayev_ M&L. Pollyakov, N.N. Tarasov, L.ya. Selodkov. Yu.V. C., f .: S-:4~L ~ .. . .- i I . I - A[ ~- ...... - I - -*:,I Technol.. if ='Yurh 84i =41 4(1952); Cf. 275(19M).-B. previw~ of hydrated ChlorldcF, 01 e the hy, 2" ' tile jujF. of th droglicatc bilcks Is ab batches. In the sante I 1120 stability of the t Mcklit am. also natural FeSO,.7H%O, N43904.10 at 2 to 3%. C41W4 2H tho reaction Products. a M% (in the quartz sum Alicate hydrattes whkb I x1otts., Mg(olfh 6 C. mble Mg silicatc The YoW elfectliv snltL 01A aw .U to 4 atm.. gitaintainetf-, natural activated SA, b Increaws-ibe wech. stm 4m a,W erk~skb addiffin bf. A., 1" 4y Akad- Nczk NS-SAL 'IF. AMR. Zkltr. 11, NO. It 10(nlstx-aw that Snudi tunts. Ca - UK CT Na witter g1m rml bint'ling reactiom of f rze addL41 to thC tilixing walcr. for the productimi of CAi Ity- Rei. bl' such n0das. to the tht injvh. properties usid the -itre,improwd. Particularly ilte, r0chardhe, asitakhanite, ill allits. If Afg( Oilh art., folind 0111ong rec NnOtl rupidly M-acts with I fret Ca-0 to forul Stable Ca up the onech. stivaigth of the CjWtS Mill MMAtO $10, to tea 61 equal rnech. characit-r. ~~ are gM11111.1led Mt 511kal'.. resmire H the putot1ave is 2 hirs. The ttw of tripoli as the quattz satid, cousiderably latai V eps-Imite, astmhanite, maddedtothebatch. W.E. _MW IMP I. s . a 4 0 -. .01111MU&I Abitracts we 5 VOLO GerAraL arA l'byideva Chemimtry a of dm dehydration of gndhun U A ILMM=-U No. 8(1951).-1-n order to del. the twip. Inter-I it, which dehydration of vitreous Na silicates occurred, samples iiiade Irom N&AUSO: by steatning (100*. 1 atru.) 1 (1). 2 (19). 3 (M), 4 (IV). and 5 (V) hrs. and contg. I I.S8, 12. 10, 12.90, 14,64. and 16.9070 jjjO, mit., and an 1111st6med sample (VI) wa heated In a thermographic app. that re- corded temp. P3 a function of time. V1. 1. 111, and IV had pairs of endothermle poiPts, at 130 and 570*, IW and 640*, 1130 amid 650*, and 1415-55 and 640,-W*, resp. llandVwere similar to I and IV. resp. The higher teinp.3. were points of ,complete dehydration. The magnitude of the 'hennal ef- Aect Increased with the degree of hydration ' f bailti temp. in- itervals. The steaming app. and thermal data ~r:_, shown in diagrams. J. W. Loweberg. Jr. rIONLRY. V.I.; 3AVIN. G.N., professor, doktor, retxonsent: KAKAROT, V.S., professor, doktor, retsenzent; KATOW N A radaktor; TROWMA. M.L., rodaktor; TATOSHIM, TO.J., I-91ch"I'lle-do'k,ly redaktor [Roloto for deep ulnas] Pod*smwo ustanawkl dlia glubokikh obakht. Moskva,, Goo. nanchno-tekbno Ind-vo lit-ry po chornot I tsystnol ustallarg1l, 1954, 227 p. [Microfilul (Km 7:10) 1. Tits"resident AN USSR (for Say4n) (Nine hoisting) be,kmMPA~ a"Ill Alskseyevich; 12OXTSKrY. A.T.. rod&Kor; PARTOVSlrrT, A.V., --aro ed r; NVMMON. I.K., tokhnicheskiy redaktor r rVater supply and ventilation systems In ore-d-resbing mills] Vodo- snabsbeide I vosdukhodnvuye ustanovid obegatetelInfth fabrik. Moskva. Goa. ranihno-tskhn. Isd-yo lit-ry p-D chernoi I tevetnol metallurgil, 1954. 39o p. (MLRA 8-3) (Ore dressing) (Metallurgical plants) M j4T * - * - ' h Uil: ) tL v - - - it /) IH7- i f- ~// i , /.)/, ~/I ,'I BUDMIROV,P.; KATVJM,M., dotsent. Quicklime in the oroduction of silicate building materials. Stroi. mat., Isdal. t konstr. I no.4:17-20 Ap'55. (MM A 6: 10) 1. DeystyttelInyy chlen Akademil nauk SSSR. (Bricks) (Building blocks) AID P - 4017 Subject USSR/Power Card 1/1 Pub. 26 - 6/31 Authors Gunzburg, D. B., Dr. Tech. Sci., M. A. Matveyev, Kand. Tech. Sci. Title On packed lining for boiler surfaces. Periodical Elek. sta. 11, 20-23, N 1955 Abstract Authors report on research made on properties of lining used to improve Imperviousness of waterwalls. A detailed description of tests made with different types of lining is given. Liquid glass, cement and magnesium solutions were used and proved to be satisfactory. The method of preparing these linings is described. Six diagrams. Institution : None Submitzed : No date MOVE T mikholl DwyA, nsydiya Alskmandrevus; :;=kfz $Ww- I. r. . La"As U&*C Phn '7W( 9 1. .' asuchM "daktor; IRDOLOT. S.A., redaktor; LTUDCMXAU, N.I., tokbatcheskly redaktor [ftrous silicate products] Forlsty* elliketays, Isdelita. Moskva. Goss Isd-vo lit-27 po strolt. asterlaUm. 1956. 106 p. OULAA !".10) (Building materials) (Silicates) G]UGORIYBY. Petr filkoleyevich [deceassOll, 1khmil Alskeendrovich; m m P&D"Am- VJYBYSHBYA.G.T., redaktor.- GJADLIW, A.m., TOM - [Soluble glass; production, properties, and use] Rastwortmas staklo; poluebenlet svolstvo I prImenente. Moskwa. Goa. Izd-vo lit-ry po strolte meterialam, 1956. 442 p. (X= 10:2) (Abluble class) .I ---.I ~' -ti I . -I . .i - -:..:.i- . .iz .. . t '0~ /.,) J) _~ 1, f/(/ e- //I ell, I/./ - USSWMemicsl TecbnO109Y. O'emical FrodhictB and Their ApPlIcation. J-1-2 GUBB. Ceramics. bAlding Jkt*xials. Abe jour: Referat Zh.-Kh.., No 8, 195T, ;75917 Author N.A. Pktveyev,. Inst y a.,-,d Silica Modulu of Vit Title Determination of Solubli-it- 8 Mous All-line Silicates. Orig Pa: Sb. ranch. robot po khi-ii i tekhnol, silikstov. M., Prmstroy- izdat, .1956, 333-338- Abstauct: The Methods of the determInation of the solubility of vitreows alkaline silicates of Na In an open vessel and a thermstat are described. It is noted that the 1st method based m the preli- minary hydration of the saWle. can be applled to alkillne Bili- cates of any silica modulus; 1A is preferable to determine the solubility of milkallne silir-a-tes of silica wAuli 4 3 using the 2nd method. card 1/1 UWR/ftmical Technology. Chemical Proetucts and their Application. J-12 Glass. Ceramics. Building Materials. Abe Jour: Referat Zh.-I(h., No 8, 1957, 27596 Author : X -A - Yktveyev InBt f__ Title Influence of Dissolution Dimtion and Water Temperature on Solu- bility of Hydrated Vitreous Godium Silicates. Orig Pub: Sb. nouch. rabot po, khiati i tekbnol. silikatov. M., Promtroyiz- dat, 1956, 365-370. Abstract: The methods of invesUiption axe denexibed and their remlts axe d1scussed,; it is noted that the solubility of higb-nDdalar hydra- W vitreoQs sodium sillcates risen insignificantly vith the rise of water temperature. Me dissolution duration increaseB the solubility of hydrosilicaLtes of a slov degree of dispersion and does not influence the xolub:Llity of hydro-silicates of & raised dispersion degree. CArd 1/1 .58- SOV/137-58-7-14202 Translation from: Referativnyy rhurnal. Metallurgiya, 1958, Nr 7, p 34 (USSR) AUTHORS: Matveyev, M.A., Matveyev, G. M. -- 000400mmlill- TITLE: On the Determination of the Thermodynamic Propertiez; of Some Silicates (K orr-edeleriyu termodinamicheskikh svoystv neko - torykh silikato-,r) PERIODICAL: V sb. - Fiz. - khirn. osnovy keramiki. Moscow, Promstroyiz - dat, 1956, pp 504-506 ABSTRACT: The formation of a silicate of the type NaZO-nSiO2 is broken down into two processes, namely, the formations of the bonds Si-O and Na-0. Modification of thermodynamic properties of &Z, &H, and AS (&3) in the process of formation of NaZO- nStO2 is registered approximately as AG n = AGNa+ rAGSi where AGn is the variation of the property in the formation of the given silicate, AGSi is tl,.e variation of the entropy in the formation of Si-O bonds in the metasilicate, and AGNa is the variation in the entropy during rhe formation of Na-0 bonds in the metasilicate; it is assumed that AGSi and AGN does not depend on n. AGN a and AGSi are found with the aid of tabulated data for meta- and Card 112 orthosilicates; these values are used for other compositions. SOV/137-58-7-1420? On the Determination of the Thermodynamic Properties of Some Silicates The calculations produced: AS 0 - - 2 A I as0 Na - S, ~ - 2.1 entropy units for Na.0 - 3SiO2' ASIIa0 ,3SiO? = 51.6 entropy units, AH= - 7q0.4 kcal, AZ : - 74 1.3 kcal. z - P S t). 1. Silicates-Thermoiynamic properti,-.- Card 2/2 00 7-v---,Yc V~ /;,;, ~ U33R /themical Technology. Chemical Products 1-12 and Their Application Silicates. Glass. Ceramics. Binders. Abs Jour: Referat Zhur - Khiodya, No 9, 1957, 31562 Author : Hatveyev M., Smirnova K. Title : Porous Panels for Pneumatic Transfer of Pulverulent Materials Orig Pub: Stroit. materialy, izdeliya i konstruktsii, 1956, No 8, 28-29 Abstract: Description of the technological process of production, and testing procedures for air- permeability, of porous chamotte panels, made with water glass, for pneumatic transfer of dust-like and pulverulent materials. Card 1/1 T- USSR /themical Technology. Chemical Products 1-12 and Their Application Silicates. Glass. Ceramics. Binders. Abs Jour.- Referat Zhur Khimiya, No 9, 1957, 31497 Author : Matveyev M.A., Koyfman I.S., Grechanik L.A. Title : Vibratory Comminution of Sand and Its Use In the MakiM of Borosilicate Glass Orig Pub: Steklo I keramika, 1956, No 11, 3-9. Abstract: Grinding of sand (3) was effected in M-10 and M-200 vibratory mills. Degree of dispersion of S was evaluated on the basis of screen analysis data and specific surface values. It was found that most effective in grinding of 3 during the first 1 5 hours, wheen a specific surface of 3300 cWlg Is attained with a residue on the C ard 1A USSR /themical Technology. Chemical Products 1-12 and Their Applicaticii Silicates. Glass. Ceramics. Binders. Abs Jour: Referat Zhur - 10-iimiya, No 9, 1957, 3!497 screen of 10000 apertures/cm2 (5%). Comparative study of vibratory grinding using different grind- ing bodies has shown that greatest output capac- ity of the mill is attained with steel balls, - which are most wear-resistant but cause contlam- Ination of the 3 with metall1c Fe. Milling with porcel&in and glass balls decreases the output by 2-3 times. Use was also made of glass balls manufactured at Vie same plant; cost of the balls expendez. in -vibratory comminution of-1 ton of sand Is 2 times less than that of porce- lain balls. For glass in which a Fe,03 content of more than 0.1% is permissible, milling of S clard 2/4 USSR /themical Technology. Chemical Products 1-12 and Their Application Silicates. Glass. Ceramics. 3inders. Abs Jour: Referat Zhur - Knimiya, No 9. 1957, 31497 can be carried out in a housing without an irj~- ternal rubber lining, which is of great prac- tical importance since the life of the lining does not exceed 150 hours of operation. To reduce dust formation and Improve mixing of the batch It is advantageous to humidify the sand 5 minutes prior to termination of the mixing. Early molateninp of the S Impairs the degree of comminution. Output of a cont,:Lnuous operation unit, with a feed of the aero-mixture under the milling bodies, Is 1.7 times higher than that of an intermittent operation mill, yielding a pro- duct of the same degree of dispersion. Most C ard 3,* ME Ahemical Technology. .1"hemical Products 1-12 and Their Application Silicates. Glass. Ceramics. Binders. Abs Jour: Referat Zhur - Khimiya, No 9, 1957, 31497 advantageous is a grinding of S to a specific surface of 2000 exie/g, which is attained in a M-200 mill within I hour. C ard 4/4 (YI /~T V F-'Y USSR/Che-3ical Technology - Chemical Products and Their Application. Silicates. Glass. Ceramics Bindersy 1-9 Abet Jouymal: Referat Zhur - Khl Iya, No 19, 1956, 62238 Author: Matveyev, M. A., Gludina, N. I. Imstitution: Bone Title% Rapid Method of Chemical Analysis of Soluble Glass Original Perindical: Tr. Mosk. KlUm.-tekhnol. in-ta, 1956, Nu 21, 49-56 Abetractt A photocolorimetric method of analysis has been deveLoped for a rapid determination of S102 in glassy, soluble, alkaline silicates and their solutions. It is shown that this method, in combination with the vol,=etric method for determinction of the content of alkalies, permits to determl e within 1.5-3 hours the z-ilica modulus of glassy alkaline silicates. card 1/1 IN P TV E_ ~ 1~ V~ PN /~ USSF/Chenipal Technology - Chemical Products and Their* Application. Silicates. Glass. Ceramics. Binders, 1-9 Abet Journal: Referat Zhur - Khimiya, No 19, 1956, 62239 Author: Matveyev, M. A. 1-titution: None Title: On Dehydration Temperature of Glassy Hydrated Sodium Si-:icpLtes and the Determination of the Degree of Their Hydration Original Periodical: Tr. Moak. kbim.-tekhnol. im-tal 1956, No 21, 57-6o Abstract: The investigation has shown that the maximum temperature af de- hytration of Na silicates is of 30-35 0. The same interval deter- mines the beginning of dehydration of soluble hydrosilicate glass. Determination of hygroscopic moisture content of glassy, hydrated, alkali silicates should be carried out at 350. Content of hygro- scopic and hydrate water in hydrated soluble glass of the same cam- position increases with increasing number of fractions in its particle size range. On increase of drying temperature of hydrated Card 1/2 USSR/Chemical Technology - Chemical Products and Their Application. Silicates. Glass. Ceramics. Binders, 1-9 Abet Jourial: Referat Zhur - Khimiya, Ro 19, 1956, 62239 Abstract: soluble glass above 30-350 solubility and binding properties de- crease. A simplified procedure is reccamended for determination of the degree of hydration of glassy alkali silicates. -4krd 2/2 -UMTBV, N.A.; SHIMOVA, K.A. Porous ceramic tiles for the aeration of c1rainage water. Gor. khos. Mosk. 30 no.8:30-31 Ag 156. (%(LU q: 10) (Tiles) ry I USSWMA01cal Technology. Chemical Products and Their Application -- Silicates. Glass. Ceramics. Binders, 1-9 Abet Journal: Referat Zhur - Kb1miya, No 2) 195T, 5133 Authors Budr1kov, P. P., '-ftwz4"V)-1 Institution: AcMaW of Sciences WM Title: Synthesis of Sodium Trisilleste in the Crystalline State and Study of Its Prqperties Original Publication: Dokl. AT SSSR, 1956,, 1o7, No 4, 547-550 Abstract: The posability has been ascertained of the formation in the FA20- S102 system., of a new compound Ns,20.3M2, In crystalline state, vItbIn the range 700-7500. There are given: rate of crystallization curve of vitrouD Nv0-3S10!2j results of x-ray Investigations (inter.- planar distances of crystal lattice of WaLpO-3SI02); optical constanl;s of N&20.3SiO2 crystalej de-isity, solubility and coeffidient of thental expansion of crystalline N&20-3SI%. A study has also been made of the Wration capacity of crystalline 3&20.35i~o. It In noted that Card 1/2 :,a~,,I~j~*=--i~.~-_,,j;~~~--------, i - . . - . 'I - . - . .~ .1 i I . -11 1 , . -* ~- --.