SCIENTIFIC ABSTRACT VASYUKOV, I.YE. - VASYUNINA, N.A.

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December 31, 1967
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SCIENTIFIC ABSTRACT
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w.~ VASYUKOV, I.Ye., inzh. Cantilever crane mounted in a window aperture. Mont. i -q;jts rab. v stroi. 24 no-900 S 162. 1;: 9) (cranes, derricks, etc.) IMIR VASYUKOV, I.Ye., inzb. ---------- Rotator for automatic welding of spherical tanksm Mont. i spats. rab. v stroi. 21, no.10:20-21 162. (MIRA 15:10) (Welding-equipment and supplies) 124-57-2-2062 TransIat,on trom: Reie: a 1 7%-rv,. zhur,:al lkvlekhar.;~a 1957 Nr 2 r) 8-j (USSR) AUTHOR: Vasyuk~-.-v K -A TITLE- Aralysi~- oi Lc-cal Pressure Chargc- and Cyclogenetic Conditions in, the Tioposphere. Ar,aliz toktl'iiykh izmeneniy davleniyt i iislov.y is v tr-op(.,;-,er(-) PERIOD'CAL: Tr, Ttenlr in-t., prcg-~ozo-,, 1956, N:r 45 (72). pp 3-58 ABSTRACT: The itullict employs the eqiat'ons tor it v(.rtex and for the heat advechon in the tollowing form )0 + )SQ -2 4 u ~)- 4 d, Z) x T x T -aT +- JT w 3T --3- HereQ is !he verticit component of the vcrtic;#.y x and y are the horizortal coordinates. u and v are the veloc'ty components along these ccordinates, w Is the vertic-A) velocAy component, I is the C---.ol-~ parameter, and e& a r. dare the dry adiabatic Card 1/2 rate (A ccoling and the vert.cal I"pse ralt! respec!ivety. Equations 124-57-2-2062 Analy-~is of Loc.Al Pressure Char~ges (con,,) W and (?) are irtegra--.-d along the vertical coordinate i-f.m the grol.nd surface to tile upper I:niff (.1 the atmosphere; the mo:.,% val!.-es (-elati-vc to he',-ght) of the metecrolog.cal ci. mvnts are taken out from under the integral sign. The term w s replacvd I v thv plane VCICL I't.y di-c.-geric e with the a ,d of the c(ilia- tion of (ontinuily Thc. ik-locity ccriapenten's CtI the left sLde of E(Is. (I) and (2) are sul)st.fuled -n acc,_,rdance with 'he geostrophic -wInd erlt_stl~.,ns, 1,,.ipl,,( c! olic. it or 1\1 1 (11 go(q)( !ent i,il) !S I (.pI,ActI-d - oxi 111,11el% )',Y I 1 /4 BY rilvans oi flie equal i ctis, uhfai,:cd arid the I-aromel r , t to rmul j expr ess;oris a r e tound fcr the tinit der val,.ves ct the surface preSSLre and the geopo!ential oi the 500-mb s(.rf.~ce n terms of the der:vjt;%-e!j cf 'he metecro1c,gical elements relative tr~ thc,r coordinates. in the computat.'ors the plane .-elccify diver- gence wits delern-itiea from the given wind- veloc ity observat;ons. A number of sample c(..mput,,.ons are aciduced. The aothcr concl,,,des that considera- tion Gf the cr)mp(:nent ol t.Aned from the pl.~ne ve)cclty d'vergenct- I-y means of direc'. WOW cv;sevaGons a:icrds in improvemert over the resul-s Obtained from i considerat"on ci the vortex translat.on alcrie. S.A. Mashkovich 1 . Atmosphe-- -re 2. Oyclones--Propagatjor, 3. Mazherntios Card ?12 VItSYMOV, K.A.; ZVEREV, N.J.; PED', D.A. Forecisting synoptic processen for the current natural ' period LY the use of analorues. Meteor. i gidrol. no.1 .:27-)3 .Ja 162. (mIiiji 15~1) (Statistical weather forecasting) VASMOV, K.A.; ZV7MV, N.I.; PEDIN DoA. Forecasting atmospheric processes by analogues for a natural synoptic period. Trudy TSIP no,120:3-13 163, (MMA 16:6) (Weather forecasting) VASYUKOV, K.A.; ZVEREV, N.I.; PEDI, D.A. Correlation betimen the state of atmospheric pressure centers amd the veather in the European part of the U.S.S.R. Trudy ?SIP-no.120-114-24 163. (MIRA 16W (Weather forecasting) V A,-:YuK,,,'7, 7 N.%; PET'll D , ".0 Fore,-~as~'ng the an-cmaly cl' 'he a-,erag. monthly air em-.le:,-P.-,.;rt. p Trudy TEIP nc,.'.32:5--?.-63 1 r,,' - (mIFtA ---7!--c) 04-Qrl;~, - hL i X~ ~6028444 SOURCE CODE: UR/2546/66/000/153/0022/0040 AUTHOR: Vasyukov, K. A - Fed' D. A, ORG: none+ TITLE. Method of forec, st_ing an anomaly of the mean monthly air temperature with -4 consideration of its intensity in the Northern Hemisphere SOURCE4.!Moscow Tsentrallnyy insti_~ ~tK_qgnozov. Trody, no. 153, 1966. Statisticheskii ye hetody dolgosrochnogo prognoza pogody (Statistical methods of long-range weather forecasting), 22-40 TOPIC TAGS: long range weather forecasting, air temperature, atmospheric temperature, 1PLtmospheric current 1 A 4BSTRACTt In this article the authors proceed from the hypothesis that an Allomaly of 'jhe mean monthly air temperature in the Soviet Union is determined by its anomalous :Oevelopment during preceding months over the entire Northern Hemisphere. The fore- ~pasting method must include Information from the entire Northern Hemisphere. The 'kradients of the mean monthly air temperature over the hemisphere which were used as redictors met this condition. The proposed calculation method of forecasting had the form 6 6 6 ~t:=Iaigrad.-Ari+yjPjgradvtiri+:~llgradsAT,4-~aoArs, 1-1 . J-1 A-1 M !there At is the expected anomaly of the mean montirly air temperature at a certain boint in the Soviet Union with a one-month predictability; ai, Bjl Yk are coeffl- qard 1/2 04911-6 CC NRt AT6028444 cients of empirical influence functions for corresponding components of the temper-' ature gradients; gradzone ATi is the zonal gradient of the temperature anomaly betwee-n-the i-th pair of selected points taken in a south-north direction; gradN ATj are meridional gradients of the temperature anomaly for-northern regions of the- hemisphere taken between the same pokits In an east-west direction; gradS ATk are Tneridional gradients of the temperaLure anotwily for southern regions of the hemia- ,,i.rre taken in an east-west direction; rio, A,ro are analogous values pertaining to the same station for which At in found. To compile a forecast by method (1) it is necessary to obtain corresponding data of the mean monthly air temperature at the station level at 12 points of the Northern Hemisphere. For each of these points a table is used to find the monthly temperature anomaly which is then used in the cal- culations in the form of zonal and meridional differences. Then by means of a table corresponding to a given season for each point of interest in the Soviet Union, the future anomaly of the mean monthly air temperature is found as the sum of 19 paired products of the corresponding weights for each of the indicated differences. The 19th term will be the paired product of the temperature anomaly at a given station ATO and its weight ao. The calculations should be carried out twice to avoid additional- ,errors, The temperature field obtained is the probability forecast of an anomaly of the mean monthly air temperature in the Soviet Union, the deviation of which from the actual for each point will be minimal in the sense of least-squaree. The proposed ~method permits, to a,~certain extent, taking into account the characteristics of 'general circulation which appear in the atmsphere of the entire Northern Hemisphere. Orig. art. has: 1 formula, 5 tables, and 1 figure. iSUB CODE:, OV SUB#HDATE: none/ ORIG REF: 005/ OTH REF:.,005- Card 2/2 J VASYUKOV, K.A., kand. fiz.-matem. nauk; ZVEREV, N.I., kand. fiz.-matem. iii7~,R;--PED', D.A., kand. geograf. nauk Rhythms In the atmosphere and some methods of evaluating them. Meteor. i gidrol. no.lt47-49 Ja 165. (MIRA 18:2) 1. TSentrallnyy institut prognozov. 11 A SYLIFOV , K- A PED ta t i tic&l A ta r i:, clualitity (A 165. S/169/62/'000/007/109/14Q D228/D307 AUTHORS. Vasyukov, K. N Zverev, N. I. and Ped', D. A. TITLE: Usin:f the principle of analogousness when forecasting synoptic processes and the weather for five days PERIODICAL: Referativnyy zhurnal, Geofizika, no. 7, 19629 48, ab-- stract 7B257 (Tr. Tsentr. in-ta prognozov, no. 116, 1962, 13-23) TEXT: The N-500 values for a standard grid of points, located ev- ery 40 of latitude and 120 of longitude on the territory, b,)unded by 360V1, 840E, 760N, and 360W, were taken 10rom the average maps for natural synoptic processes (NS.P) in January and 2ebru.ary, 1938- 1955. After this the signs of the geopotential differences, respec- tively clutracterizing the zonal and the meridional flow components, were determined for m,2ridionally and latitudinally neighboring points. The values +1, 0, and -1 were respectively ascribed to positive, zero and negative differences. The resulting magnitudes, --of the r-Aeridional and the zonal wind components for all NSP were Card 1/ 4 Using the principle ... 8/1069/62/000/007/109/149 D228/D307 printed on tape. T'he analogs of the N-500 averages for t1he para- meters P '? and PA_ , characterizing tile similarity of fields with re- spect to their cirCLilational features, were selected for the firot 20 maps by means of the electronic computer "Po-oda". The value,,3 ~)'I P,P and P,, were calculated from the formulas-. n,,)+- n. Rf n + n PA n + n where n(O n- , n n is the number of cases when the signs of .+ t~/_ "IL + I/~_ - the meridiona'l (nP) and -the zonal N) flow components in two'cori- parable N-500 fields of NSF do, or do not, coincide. The comparison of all NSP with the original 20 allowed the distribution of the de- gree of analogy for the fields of the 500-mb surface's January geo- potential to be obtained from the parameters of q and o a it also Card 2/4 T Ik S/169/62/000/007/109/149 Usind the principle D228/D307 allowed the natural frequency of analogous processes to be exposed separately according to the development of the meridional and the zonal air-flow components. Utilizing the criterion p. all processes can be divided according to their degree of analogy Tri'to three ca- to-ories: the analog (P ?,0.4), the non-analog (p -0.3, +0.4),.. and the reverse analog (P -0.3). Utilizing the criterion PA , too, we will obtain the analog ;>0.8, the non-analog p = 0.2 + 0.8, PA_ X and the reverse analog o /4 0.2. The criteria are established ...,ith a 10~ guaranty. In practical work, when classifying all processes into three categories, the degree of guaranty should be established jointly according to both criteria for the analog p,,>,.0.4 and 0.6, the non-analog -0.3 iv~HuAc; over Ni-ALO, at3 -V the idd of If - y %v.ti 3O.L", withunt any Nil.. 1f.,VC11(C11J[ej)2, 1). 125- 7'. ,1~ 0.7M2, over I'll .,.t 318' gave 11 without NIL. and hytholvi; of the "ttalyzatc gave i-j-Pr3CO; over Ni- A1:0, aL ;J-2;? the yjehl of If was 27.01' without any Nil,. 11~SCIMC.11%, 1). 102-3', in. -20', (in C.7668. drhydro- geoatud only ferbly over Pit or Ni-A1101; over 110~ at 153' it gave . 13V0 11 and 25.95o Nil,; hydrolysis of Lhe CAWYL.Ate g.1% L pinacolone and sorut EtClNfc, was isolated fromtheoriginaleatilyzate. EtCIIPfi\'IIjov,,rPdat34C' gave 35.6% 11 and 10.2% Nll~; over Ni-AI,O, at 34W the yield of 11 wai 4 with Nfi,; ovEr 71103 3870 11 with 18.2% N113 reaulted; hytfiuly,i~. gave I:tDz, while the catalyzate atso gave stmie phunylprolwne. ThL, is the Ist example of dehydrogenation of aliph3tir. amines to i ketinjities (cf. C.A. 29, 2~~54). G. M. Kf~Aapof~_ WiNPIGO, S.V.;_VASYUNIHA. N.A. _.._ Production of polyatemic alcoh*la from nonedible vegmtable raw materials. Gidroz. i lesokhim. prom. 9 ne.6:3-6 156.(mmA 9:1o) l.Vn~so.vuz*7 nanchno-losledovatel'skly inatitut gidroliznoy sullfitnospirtovoy promyshlennosti (for Chepige). 2.Inatitut organicheakay khinii Akadomii nauk SSSR. (AlcohoW (Raw materipils) yff ~ -[ 1--" rv 1 &" Irf , A; i'v' I CHXPIGO, S.Y., kand.takhn.nauk; BALANDIN, A.A., akndemik; VASTUNINA, N.A., kand.khim.nauk; SERGI M , A.P. Preparing polyatomic alcohols by means of entnlytic conversion of polyeaccbarides of vegetable origin. Xhim.nauka I prom. 2 no.4:416-424 '57. (MIRA 10:11) (Alcohol) (Polynaccharides) BALMIDIN, A.A.; VASYUNIKA, N.A. - RARTSHEVA. G.S.; CHVIGO, S.V. - iiim-~ Catalysts for hydrogenation of polysaccharides. Izv.AN SM.Otd. khim.nauk no.3;392 '57. (MLRA 10:5) 1.Institut organichaskoy khimii im. N.D. Zelinskogo Akademii nauic SSSR I Ysesoyaznyy nauchno-issledovatellskiy institut gidroliznoy promyshlannosti. (Catalysts) (Hydrogenation) (Polyeaccharides) AUTHORS: Balandin, A. A., Academician, and 20-1-22/42 Vasyunina, N. A. TITLE: Note on the Selective Hydration of Monosaccharides and Polyatomic Alcohols (Izbiratellnoye gidrirovaniye monosakharidov i mnogoatomnykh spirtov). PERIODICAL: Doklady AN SSSR, Vol. 117, Nr 1, PP. 84-87 (USSR) ABSTRACT: I. According to scientific and patent publications (reference 1) the following reactions take place above nickel catalysators in an aqueous solution at a hydrogen pressure of 150-300 atm. 1) Monosaccharides are hydrated almost entirely to polyatomic alcohols at a temperature of 120-1300C (xylose to "xylite", glucose to sorbitol) 2) At a temperature rise, the hydroxyl groups of the alcohols are split off, primarily the end groups. In this way 1,2 propylene glykol is produced from glycerine, and isopropyle alcohol from this substance. Alcohols of higher order do not loose their hydroxyl groups as easily as the alcohols of lower order. 3. The production of uric acids from monosaccharides (in quantities not exceeding a few per- Card 1A cents mills) at a lack of hydrogen is even more difficult Note on the Selective Hydration of Monosaccharides and 20-1-22/42 Polyatomic Alcohols which acids cause an acid milieu-reaction. 4) The declompo- sition reactions of the C - C combination, occuring mostly in the center of the molecule, to a certain extent compete with this reactions, in general, however, they take place at even higher temperatures (220-2300C). In this way propylene glykol and glycerine is produced from sorbitol.II. It appears from the references 3 and 4, that at an hydrolysis of hydrocarbons the cracking of the C - C combination occurs in the position 3,4v The explanation of this phenomen given by Shmidt is refuted by the authors, just as the opinion by Natta, Rigamonti and Beata (reference 4). 111. Subsequently, the multiplett-theory of catalysis is applied to the reactions (reference 5)- It furnishes the correct sequence of hydration and hydrolysis of various compounds, comprising furane derivates, "tripticene" and of organic peroxydes. This theory separates the reacting atoms within the molecule into index-, doublet groups 1-177-1n (M) Card .2/4 (1) IB C B... C Note on the Selective Hydration of Monosaccharides and 20-1-22/42 Polyatomic Alcohols These atoms are in contact with the catalyst (but not necessarily at the same time). The reaction velocity is the higher, the better the structural and energetic correspondence is complied with. This correspondence is the more perfect, the lower the enerGetic threshold ( -E), or, the greater the value E - - 0 - 0 )(2) --r-AB -CD* (-qAK' QBK'-'~C1C'9DK If the indices of the reactionq concerned are taken and the values of Q are introduced into equation (2), the results of table 1 for a nickel catalyser are obtained. IV. The influence of structure on the velocity of the reaction of one special type is effected by the substituents, which are posed outside the bounds (lizaramochnyye zamestiteli"), In this way the introduction of a substituent, i.g. at the atom A in formula (1) influence the quantity QAB and QAK in formula (2). From this results a modification of E (rt:ference 11) and subsequently the reaction velocity is modified. From the further equations (3) it follows, th t by means of the introduction of a substituent at A 6E - - 6 F Card 3/4 -(T6&S - 69,AD+6QAK) (4). From this the equation aE -'Y -6 AF. Note on the Selective Hydration of Monosaccharides and 20-1-22/42 Polyatomic Alcohols is deduced. From this it follows, that the reaction proceeds the faster, the more the free energy of the reaction 64&F is reduced by the process of substituting. The values of 6A F are given in table 2 and 3 for the compounds under investigation here. The sequence of reactions computed from Lhe tables are in accordance with the experimental results. It follows, therefore, that the application of the multiplet theory in the field of the hydration of monosacchariies and of polyatomic alcohols 6ogpegse ood grogects. There are 3 tables and 12 references, highgare lav c. ASSOCIATION: Institute for Organic Chemistry imeni N. D. Zelinskiy AN USSR (Institut organicheakoy khimii im. N. D, Zelinskogo Akademii nauk SSSR). PRESENTED: September 6, 1957 AVAILABLE: Library of Congress Card 4/4 WYUNINk, N.A.; HUAMIN, A.A.; GHEPIGG, S.V.; BARYSHEVA, G.S. Catalytic hydrogenation of wood and other T)Iaat maLerials. Izv. AN =R Otd.khim.nauk no.8:1522-1523 Ag 160. WU 15:5) 1. Lwtitut organicheskoy khinii im. N.D.Zelinokogo LN SSSR i Gosudarstvennyy nauchno-Assledovatelf.9kiy institut gidroliznoy prorqehlemosti. (I(Ood-Chemistry) (Hydrogenation) .VA,5-jUNjNk,j"A ; BALUMIN, A.A.; KARZHEV, V.I.; RA-BINOVICH, B.Ya.; - CMPIGOj S.V.; GRIGCRYAN, Ye.3,; SLUTSM, R.L. Production of glycerol and glycols by hydrogenolysis of xylitol. Khim.prom. no.2:82-86 F 162. (MIRA 15:2) 1. Institut organichaskoy khimii AN SSSR8 Vsesoyu=yy nauchno- iseledavateliskiy institut po pererabotke nefti i gaza i polu- cheniyu iskusstvannogo zhidkogo topliva., i MONIIGS. (Glycerol) (Glycols) (Xylitol) klo g'- droll, zr,:~y ~t. ss if z,-u c- VASYUNINA, N.A.. BALANDIN, -A.A.,; MAMATOV, Yu. I Hydrogenolysis of xylite. Part 1: FXfe-.t of temperature and pressure. Kin.i kat. 4 no.1:156-162 Ja-F 163. OMU 16:3.) 1. InBtituf organicheskoy kbimii imeni N.D.Zelinakogo AN Szi6R. , (lylitol) (Hydrogez*aysl6)