SCIENTIFIC ABSTRACT BLINOVA, M.V. - BLINOVA, Z. A.

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P Vo(Im- I. Ion W D).(,ar-boxyllo Acidu by Oxidatiull (,(66o wji-Il wil-vic' Al-.1d. Comilitirt SOV/130-33-2-31 2 5/5 I 10110N: All-UnIon Scluritific Roucurch imaittite vor Putrochernical Proccuueu (Vuesuyuznyy tiuLAcIiii,.i-.IL;-.jlcduvatellulcly ItioUtut rieftelthimichc8lcildi pvuLUCLIUUV) SUBMITTED: March 3, 11.111i(.j MLDAVSKIY, B.L.; BLINOVA, M.V. Thermal converoion of ouccinic. acid into r,-ketopimelic acid. Neftekhimiia 5 no.l-.108--llO Ja-F 165. (MRA 18:5) . 1. Voesoyuznyy nauchno-iooledovatellskiy inotitut neftekhimiche- skikh protsessov. - CHISTOV, A.D.; BA7ARNOVA, G.V.; H&K, N.D.: BIMIKOVA, V.I.; BLINOVA M. Ta.; KMNOVA, P.G.; XAKAROVA, N.D.; PRIPISTSOVA, K.D.;- R-HOHOVA,-"- 7W. - ~-- TOLKACHEVA, Te.M.; TYUNUTEVA, V.V.; ZINGHENKO, V.S., red.izd~-va; PAVLOVSEIT, A.A., tekhn.red. [Foreign trade of the U.S.S.R. for 1918-1940; statistical survey] Vneshniaia torgovlia SSSR za 1918-1940 gg.; statisticheskii obsor, Moskva, Vneshtorgisdat, 1960. 1134 p. %*MIRA 13:10) 1. Russia (1923- U.S.S.R.) Glavnoys tamozbonnoye upravlaniye. 2.~Otdel statistW Glavnogo taM02hennogo upravleniya Hinisterstva vneshney torgovli SSSR (f6r'all, except Zinchanko, Pavlovskiy). (Commercial statistics) -BLINOVA~ N*I*;. GARAYMKAYAp LoS. Atian of.the world, published in 1959; book format, Sbor.ist.po kart. no.13369-78 161. (MM 15:5) (Atlaoss) PETRZHAKp K.A.; TOLMACHE;Vp G.M.; USHATSKIYp V#N.; BAK.. M*A.; BLINOVA, N.I.; BUGORKOVp S.S.; MOSKALIKOVAp E.A.; OSIPGVA, ~'OV, Yu.G.; SOROKINA, A.V.; CHERNYSHEVA, L.P.; SHIUAYEVA, L.V.. [Yieids of certain fragments in 'U215pU2111fand pU239 fis_ 235 sion by neutrons] Vykhody nekotorykh oskolkov pri delenii U U238 i FV9 neitronami. d"eleniia. Moskva, Glav. upr. po is- polizovaniiu atomnoi energiip 1960. 14 p. (MIRA, 17:2) 32986 ff S/64 61/000/000/013/033 6 00 B1 04XB1 02 AUTHORS: Petrzhak, K. A. , Tolmachev, G. M. , Ushatskiy, V. N. ;~?~ . S., Moskalikova, E~ A_ o.., ~In Bugorkov, S V . B.~,Petr~cv, Yu.'G., Sorokina, A. V.9 Chernyaheva, L, P., Shiryayeva, L. B. TITLE: Yields of some fragments in the fission of U 235 ~ U2389 and Pu 239 by fission neutrons SOURCE: Krupchitskiy, P. Ao, ed. Neytronnaya fizikap Bbornik statey Moscow, 1961, 217-223 89 95 99 ill 115 TEXT: The authors determined the yield of Sr , Zr , Mo . Ag Cd and Bs.140 in the fission of U 235, U238 , and Pu 239 by fission neutrons. A U235-enriched uranium plate arranged .in the thermal column of a heavy-water reactor of the AS USSR served as neutron source. 300-mg tablets and 1-gg targets were produced from each substance to be fissicned. The fission events were recorded in a fission chamber during the entire irradiation period (Fig. 1). The fission fragment yields were determined from their Card 1/j! 32986 S/641/61/000/000/013/033 Yields of some fragments in ... B104/B102 P-aotivity~ The absolute P-aotivity was measured by two standard instruments with end-window countersi. These standard instruments were calibrated with preparations of the fission fragments "o be studied which had been applied to a collodium film. The absolute P-aotivity of the standard preparations was determined either with a 4n-counter or with an end-window counter havinga idndow thickness of 0-005 + M01 mg/CM2.. Six to eight measurements were made in three to four tablets (Fig. 3)~ The determination error of the fragment yield was between 6 and 11V6. The fragment yield is found to depend on the isotope mass number. There are 3 figures, 3 tables, and 7 references: 3 Soviet and 4 non-Soviet~ The four references to English-language publications read as follows; Engelkemeir, D., Novey T., Schover D_ Radiochemical Studies; The Fission Products, Book 3? div. IV, vol. 99 1334 (1951)1 Radiochemical Studies: The Fission Produots. Book 3, div. IV, vol. 9, Appendix B, 2003 (1951); Keller R., Steinberg E., Glendenin L.. Phys. Rev., 94, 4, 969 (1954); Turkevich A., Niday J., Phys. Rev., 84, 1, 52, 71. Card 2/j 29820 S/020/61/140/006/017/030 B103/B101 cp/ WOO AUTHORSt Blinova, N. I., Solntsev, V. M., and Tolmachev, YU. M. TITLEt Some particularities of the interaction between uranium mixed,' oxide and acids PERIODICA4:., Akademiya nauk SSSR. Doklady, v. 140, no. 6, 1961, 1314-1316 TFM t The authors studied the discrepancy between the initial and final 2+ 4+ UO2 1 U ion ratios on dissolution of uranium mixed oxide in acids without oxidizers. This ratio is 20 on final solution, i~bereas in the initial stage, mainly U(VI) is dissolved, so that the ratio U(VI) t U(IV) is much higher than 20. High-purity U 30. powder was dissolved in CO 2 atmosphere at constant temperatures (25 or 900C) in a) sulfuric, .j W-b)Aperchlorio, and- c) aoetio acids. The solutions were anal zed after 11) 100--min (H 2S04), 10 min (HO10 4), and 40 min (CH3coo U IV~ was d.etermined in the solution by titrating with XMnO 41 the total quantity of U by Card 1/4 820 S702Y61/140/006/017/030 Some particularities of the interaction ... B103 B101 precipitation as ammonium diuranate and igniting to U30.. Ratios of 76 : I in a), 60 0 in b), and) 300 1 1 in a) were found for the beginning solution of U3OV After 2 hr, the ratio U(VI) 3 U(IV) in the solution became I t-1 and remained constantp until dissolving was completed. A precipitation is deposited in the final stage of dissolving, in which the ratio varies between 20 and 10. Once the ratio of lil is reached in the solution as well as in the precipitation, the composition of the precipitation does not change anymore. This is a dark, slightly violet colored powder which becomes grey-green on drying in air, the ratio U(VI) s U(IV) approximating 2tl..--A ratio of 10 is maintained for 48 hr in, the powder, when the water is saturated with CO 2' 'When U30ais dissolved in HNO 3' a stable ratio of 21l is conserved in the powder during the entire time of-dissolving. It was foun a that the uranium atoms in U30a do not play the same role. It is difficult to find a',different explanation for ~e- the varying..U(VI) s U(IV) ratios in the solution and in the precipitate during the,reaotion of U 0 with acids. It is presumed that U 0 which is 2 5 Card 2/4 29a2O. 5/020J61/140/006/017/030 Some particularities of the interaction ... B103/B101 pos:ibly a compound of U(V) forms in the final stage of U 308 solution in acids. Probablyq U(V) disproportions to U(VI) and U(IV) in a ratio of 10, when it-is dissolved in acids. It might be possible, however, ~that U205 is not a comDound of U(V), but for instance UO 3' UO2. When it is dissolved in acids, a ratio of U(VI) s U(IV) w 10 will result. In this case, U308 should have a composition of say UO 3' UO 3' UO 2. UO 3*U205 is suggested, until the structure of U 308 is finally cleared up. Tbe U 308 formed reactsq however9 much slower with acids than the initial U 0 3 a molecule. It is presumed that the peculiar course of the reaction described is characteristic of many chemical compounds; oxides, sulfides, and further compounds (basic and double salts) of metals, the atoms of which show different valences, will react, presumably, sometimes in an analogous way. Papers by Vikt. I. Spitsyn, G. M. Resmeyanovaq Ye. A. or Kanevskiy (ZhNn,5., 1938 (1960)) and by G. M. Nesmeyanova, G. M. Alkhaza-hvili (Atomnaya energiya, A, 330 (1960)) are mentioned. There ar~ 3 tables and 6 references$ 4 Soviet and 2 non-Soviet. Card 3/4 29820 S/02q/61/14o/oo6/ol7/030 *4artioularities of the interaction... B103/BlOl ASSOCIATIONt Radiyevyy institut im. V. G. Khlopina Akademii nauk SSSR (Radium Institute imeni V. G. Khlopin AS USSR) PRESENTEDt May 24, 1961,by A. A. Grinberg, Academician SUBMITTED: may 18, 1961 Card 4/4 BUINOVA, N.L.; TOLMACHKV,, YU.Ne Problem of the equivalence of uranium atoms in uranous-uremile oxide. Radiokhimia, 4 no,4:447-451 (MIRA 15:11) (Uranium oxide) XJNOVA., N.L.; ROMANOV., G.A.; SOLINTSEV, V.M.; TODUCIM7, Yu.M. Nwetic properties of U205o Dokle AN OM 347 no*5#1112-M3 V t62, (KM 1602) 1. Radiyern, inetitutime TOO. Iblopina, AN SSSR~ Predstavleno a.kademikom A*Ae Qqnbergome (Uranium oxides-Mapetic properties) /Va-P(b 4', L L972- U L ACCFSSION N_R: AP4043855 'T 'Esp"G 8/0186/64/0D6/004)'0463/0466 -Blinova, N. 1-:;,, Kurbatov, V. V.; Solntsev, V. I.A. TME: A roentgenometric study lot the system U sub 3 0 sub 8 U sub 2 0 sub 5 ~A ~A 11641 463-466 ------ e--~dv ruct U r.a d at urei-xray TOPIC TAOS nitm oxide, oxi Ys a dif ra va lattimeonstant, rbombic lattice, uranium pentoxide h' b di- ng U0 in sulfuric acid or! ABSTRACT- nle authors prepared U20 eit er y Soo V1 3 by reducing with hydrogen at 390C, and then determined Re lattice constants U308 by x-rav diffraction analysis during the reoxidation of U 0 to U10 They found ?t5l 8* that3 as ",'20~ Is sat~.,ratcd with oxygen, only the U,O:: crv~ A 1r, -b- served in all the inter-mediate stages, and stable ~iffrac *, I ?T) ice of the U 0 latt. appear only after reachingg an empir ica ! 3 8 The entire range of compositions from U 0 to U 0 is thu 8 Vinua cemparison of the x-ray diffraction patie5rns 1A the authors to conclodi-, in up- position to the hypothesis of Milne (Am. Miner., 36, 5-0, 417, a;-.,' that the U 0 lattice is a deformed U 0 lattice. On the bas~ir, or hc~mulogy, thc 3 8 2 5 ~wd' 1/2 most likely structure for the U 0 lattice Is a rhombic structure, Produced by the gradua I penetra t ion 4im oxysen. 24,a --into- the, U,U. unit Ce I I a "ThL authors thank :14 TolmA ev .ku. Auibi-- orig, art. has: 2 tables and Frak , eh for h s Va A A e advice." igure. ASSOCIATIM None SUMMED: 18Jan64 E14CL: 00 SUB CODE: IC, OP M REF SOV- 004 OTHER: 012 :,Caro BLINOVA,,-~,kp- ,,- -- - Productivity of bits and econorde efficiency of rotar7 drilling. Trudy VNIIBT no.6sI50-161 162 ' (MM 16:6) (Boring) I. SHMV, S.I., obahchiy red. JJVQVAVofivJw, otv.red.; IVAIIOV, Yu.M., red. kart; IGNATINKO, A.B., red.kart; 11OLISNAOVA, I.G., red.kart; LIUMA, S.K.. red.kart; PZNTSON. Ye.E., red.kart; P3BFILYEVA. N.A., red.kart; SERGAYEVA, S.I., red.6rt-, SHIRNOVA, A.L., red;-7---- kart; KHOLODOK, V.D., red.kart; ~amAN, Ye.M., red.kart; KUZNNSOVA. O.L., tekhn.red.; LIFSHITS, N.I., tekhn.red.; SMICHU, A.T.. takhn.red. ['World atlas] Atlas mira. Moskva, Glav.upr.goodes. i kartografii Ma SM, 1959. 324 pe (MIRA 12:12) (Atlases) :3~ 4 U; I - ;R - . IHOLIN, A.I.; PLINOTAO Moo "ably nauabnyy votrudaik. Using the neutron-panw-ray method for determining the position of oil-water c.ontact in forvAtions penetrated by the well. Trudy M no.15t213-221 153* Mu 9: 8) (Oil well logglM, Radiation) I PHASE I BOOK EXPLOITATION 749 Barsukev, Oleg Aleksandrovich; Zlinova, Nina Mikhaylevna; Vybornykh, Sergey Fedorovich; Gulinp Yur-i-y-ITe-R-s-a-na-r-o-vi-c-h--,---D-a-RMT6v, Vladimir Nikolayevich; Larionov, Vyacheslav Vasillyevich; Rholin, Arkadly Ivanovich Radloaktivnyye metody issledovaniya neftyanykh i gazovykh skvazhin (Radioactive Methods for Exploring Oil and Gas Wells) Moscow, Gostoptekhizdat, 1958* 314 P- 5,000 copies printed. Reviewers: Tarkhov, A.G., Doctor of Physical and Mathematical Sciences, Professor, Department of Ore Geophysics of the Sverdlovsk Mining Institute im.eni V.V. Vakhrusheva; Executive Ed.: Shorokhova, L.I.; Tech. Ed.: Polosina, A.S. PURPOSE: The book was authorized as a textbook by the Ministry of Higher Education for students of geological and geophysical sections at petroleum vuzes. It is also intended as a handbook for geologists and geophysicists dealing with the theory and techniques of modern radioactive methods of oil well exploration., Card 1/10 Radioactive Methods for Exploring (Cont.) 749 covERAGE: The authors stress the physical prineiples of radiometry of oil and gas wells, describe the operation of radiometric instru- ments and measuring procedures, and interpret the obtained data. In 1953, the authors working at the Laborutoriya Radioaktivnykh Metodov Issledovaniya Skvazhin (Laboratory of Radioactive Oil Well Logging) of the Moscow Petroleum Institute were the first to solve one of the most important problems, i.e., the use of radioactive methods to determine the location of oilfield water in eased wells. The authops developed the radioactive isotope method and the special modifications of neutron methods for well surveying which have been used extensively by industry since 1954 in the explora- tion of petroleum resources. A method using sodium activation to establish the location of oilfield water was developed in 1954 at the Petroleum Institute of the USSR Academy of Sciences. N.M. Blinov wrote chapter I; V.N. Dakhnov, the introduction and chapters II, V, and VII; A.I. Kholin, chapter III; O.M. Arutinov, O.A. Barsukov, Ya. Ya. Gorskiy, and V.V. Larionov, chapter IV; V.V. Larionov and A.I. Kholin, chapter VI; Yu.A. Gulin and I.I. Felldman, chapter VII; O.A. Barsukov and K.A. Barsukov, chapter VIII; O.A. Barsukov, chapter IX; O.A. Barsukov and A.I. Kholin, chapter X; and S.F. Wbornykh, chapter XI. There are 66 references scattered through the book, 37 of which are Soviet, and the rest English. The book contains 21 tables and 146 drawings. Card 2/10 Radioactive Methods for Exploring (Cont.) 749 TABLE OF CONTENTS: Introduction 3 Ch. I. Physical Principles of Well Radiometry 10 1. Radioactivity and the law of radioactive decay 10 2. Radioactive radiation and their characteristics 18 3. Brief data on the structure of the atomic nucleus 22 4. Artificial transformation of elements and nuclear reactions 23 5. Neutron sources 27 6. Interaction of particles with matter 30 Ch. II. Radioactive Characteristics of Rocks 47 7. Natural radioactivity 47 8. Neutron characteristics of rocks 59 9. Induced radioactivity of rocks 66 Card 3/10 Radioactive Methods for Exploring (Cont.) 749 Ch. III. Methods of.Well Radiometry 69 10. General data and classification of methods of well radiometry 69 11. Method of natural radioactivity of rocks 71 12. Method of tagged atoms (isotope method) 73 13- Method of scattered gamma radiation 78 14. Neutron-neutron method (method of neutron density) 15. Neutron-gamma method 16. Method of induced activity 83 17. Spectrometry of gamma radiation in wells 85 Ch. IV. Radiometric Instruments 88 18. General data and specifications to be met by radio- metric instruments 88 19. Gamma-ray indicators 89 20. First radiometric well instrument 95 21. MNI one-channel instruments for operation on a triple-core cable 96 22. Two-channel instruments (1955 NGGK-55 model) for operation on a single-core cable 100 23. Auxiliary instruments and equipment for radiometric surveys ill Card 4/10 Radioactive Methods for Exploring (Cont.) 749 24. Testing instruments for the absence of the interrelation of channels and for linearity ill 25. Procedure of measurements In wells 113 26. Selection of conditions of measurement 115 27. Quality control of measurement 119 28. New models of radiometric instruments 120 Ch. V. Theoretical Principles of the Gamma method of Well Surveying 137 Ch. VI. Interpretation of Results of Measurements by the Natural Radioactivity Method 151 29. Calculation of fluctuation distortions 151 30. Distortions of gamma-method diagrams connected with measurement procedures and operation of the instruments 156 31. Adapting gamma-method readings to uniform well conditions 158 32. Establishing the boundaries and determining the thick- ness of layers according to intensity curves of natural gamma radiation 16q Card 5A0 Radioactive Methods for Exploring (Cont.) 749 33. Evaluation of relative intensity of gamma radiation 172 34. Qualitative evaluation of radioactivity of minerals 176 35. Correlation of well profiles according to intensity curves of natural gamma radiation 177 36. Lithological disintegration of well profiles 180 37- Use of gamma-method data in studying collector characteristics of rocks 183 Ch. VIII. Intepretation of Diagrams of the Scattered Gamma- radiation Method 183 38. Principles of the theory of the scattered gamma- radiation method 183 39. Elimination of the influence of changes in the density of the drilling solution 191 40. Evaluation of the density of rocks 193 41. Evaluation of the porosity of rocks 195 42. Making more precise the lithological, characteristics of the well profile 196 43. Depth of prospecting method of scattered gamma radiation . and the collar influence 199 44. Height determination of cement elevation 200 Card 611 o 'Radioactive Methods for Exploring (Conte) 749 Ch. VIII. Principles of the Theory of Neutron-Neutron and Neutron- Gamma Methods in Well Surveying 203 45. Distribution of neutrons emitted by the point source of thermal neutrons In an infinite homogeneous medium 203 46. Distribution of thermal neutrons in rocks of varying water content in the case of a fast neutron source 207 47. Distribution of neutron-gamma radiation in a homogeneous medium 222 48. Distribution of neutrons in media of varying neutron properties 225 Ch. IX. Interpretation of Diagrams of Neutoron-Neutron and Neutron-Gamma Methods 239 49. Evaluation of diameter influence, types of well filling and bracing 239 50. Determination of correction, taking into account the indicator length 247 Card 7/10 Radioactive Methods for Exploring (Cont.) 749 51. Lithological breaking-up of rocks and the correlation of well profiles according to neutron-surveying methods 250 52. Method of determining porosity 254 Ch. X. Use of Neutron Methods for Breaking-Up Oil and Water Saturation Collectors 26o 53. Physical principles of breaking-up oil-bearing and water-bearing layers by neutron methodo 261 54. Analytical evaluation of the difference in the intensity of neutron-gamma radiation in water- and :oil-bearing layers 262 5~- Measurement procedures 266 5 - Interpretation of measurement data 269 57. Breaking-up of oil-and water saturation collectors by the spectrometric method 271 58. Breaking-up of oil-and water saturation collectors by the neutron-neutron method 273 Card 8/1o Radioactive Methods for Exploring (cont.) 749 Ch. XI* Procedure and Diagram Interpretation by the Tagged Atom Method 276 59- Selection of radioactive Isotopes and technique in preparing activated liquid, 276 6o. Some general directions on conducting well surveys by the tagged atom method 279 61. Determination of absorptive layers and piping between layers in working and pressurized wells 283. 62. Determination of damaged spots in the column and zone losses in clay solution circulation in the drilled well 290 63. Determination of the height of cement elevation in back of the column and of the thickness of the cement ring 291 64. Testing the hydraulic break of the layers 295 65. Making more precise the depths in perforating the eased columns 301 Card 9/1o 'Radioactive Methods for Exploring (cont.) 749 66. Basic trends in the future development of the isotope method 302 Ch. XII. Use of Radioactive Methods in Exploring and Surveying Other Natural Resources 304 AVAILABLE: Library of Congress Card .10/10 IS/jmr 11-26-58 CHALOV, N.V.; LAPPO-DANILEVSICIY, Yu.K.; GORYAGHIKII, Ye.F.; BLINOVA, N*N.; ZHDANOVA,, L.A. Chemicomechanical degradation of linters in the presence of sulfuric acid. Sbor.trud.NIIGS 12:87-98 164. (MIRA 18:3) '6'Ll'vo VR At, - F. USSR / Cultivated Plants. Fodders. m-4 Abs Jour#.-:Ref::ZhuT-B1q-;..,, No ,6.0 .1958, 25096 Author: .. Kaplupqvskly, S,J.,j Inst "Askaniya--N6Vd'1 ihstitute-i"of-Hybridization and Acclimatization of Livestock Title Experimental:,,ISowing.of Corn at the "Askaniya-Nova" Institute.- Orig Pub:. sb ~'~Kukur"u;zi -'. - V`:' 19 5 5, ~~g 'vyp 61 m., Sel k,h-ogiz, 1956, lio-114 Abstract: The "Askaniya-Nova" Institute of Hybridization and Acclimatization of Livestock conducted in 1955 a series of experiments t.o study the agrotechny of corn raising for green feed and grain. The highest green stuff yield with two harvests came from square- pocket planting (50 X 50) with 4 plants per bunch. Good results were also shown by mixed sowings of Card 1/2 89 NIWA, A.Ye.,, AVXRBM. T.D .;-~~ILP~.;'.:MATUSLiVjc% V.S.; SHqHXIKUMVA, N.V.; HASHKIROVA, Te *- R. Woodesing of waste thiosul-fate liquore produced in the removal of hydrogen sulfide from gages. Koko i khim. no.12:40-4 160.. (MMA 13:12) I-* trralfskiy Muchno-issledotatel'skiy khimichaskiy iustitut.(for Bashkirova). (sewage-jawif ication) (Sodium thiosulfate) AVM:LBM,, T.D.; APAK.UOV, I.A.; MAXDUROVAI 0,V,; BAKINA., N.PoLBLDWA, ___Ior,; BURU, A.Ao; AVDEYEVA, love Removal of sulfur from wastegases of copper and sulfur plants by the method of afterburning. Xhim.prom. no-4:281-288 Ap 162. OUR& 15:5) 1. Urallskly nauchno-issledovateltakiy Irbirnicheskiy institut i MDdnMorskiy madno-sernyy kombinat. (Gases-Purification) (Sulfur oxides) MATUSEVICHP L.N.; BUNOVA, N.P. Crystallization of salts from aqueous temperatures. Zhur. priklo khim, 37 solutions at different no. 4%71(~-716 Ap 164. (MIRA 17:5) MATUSEVII'~'By L.N.; BLINOVA, ILP, 1.3ohydric crystallization at the varIcnis cooling rates of solutions. Zhur. prik".. khim. 37 no.10:231CP-2311, 0 164. (14TRA Mn I BOd EMMIUMal SCV/5721 Vsesoy,u;zo,*a astrcmetricbeakaya Loafcrentsiya. Trudy 14-y AstrcmetricheaRoy koaferantsil SSM, Klyev, 27-30 maim 1958 g. tiran-sactions of the 14th Actrc-matrical Conference of the USMO~Neld in Kiyov 27-30 May 1958) Mosemr, Izd-vo AN SZZSH, 1960. 440 2. Erratz clip Inserted. 1000 copies printed. Sp6nsoring Agency: Akmd=iya nauk B832. Glavnaya astronomichesWe. dbeervutoriya (Pu3l-ovo). Resp. Ed,: 14. S. Zverev, Corresponding Me=bcr~ Academy of Sciences USSR; Ed. of Publishing House: 11. K. Zqrchik; Tech. Ed.: R. A. Zr-m=Weva. PMOSE, The book is- Intended for antro:i6mors and astroybvoicists, particulv.]~ly those Interested in astrmotrical research. CUTEME: This publication.precento the Transactionsiof the 14th Astr=etrical Conference of the USSR, hold in Kiyev 27-.7,0 May 1958. It includes 27-reports and 55 scientific papers presented at the planary'mecting or the Coarcrence Ca=d Transactions of the l4t~ Astrometrical (Cont.) BOOM and &t the special sectional meetings. An,appendix contains t1he resolutions adopted by the Conference, the composition of the.committees) the agenda, and th,.~ list of ~axticij%ants at the Con2erence. A brief summary in English Is given at the end of each article. References-foUaw individual article3. The Presidium of the Astrametrical Committee (Chairman M. S. Zverev), vhich supervised th: pre~aratlon of tbla publication, expresses thasiks to the wnmbara of th secretariat. V. M. Vasillyev, 1. G. Kollchlaakiy, A. B. One- gina,, and Xh., 1. Pbtter. TABLE OP CalTMMi Pareword Address by A. A. Mikhqlav,;CbeIrmau of the Astronomical Council ~r the i Academy of Sciences USSR T REPORMS OF THk ASM010MICAL CMarM AM SUBOMM-IMS wowmai CO ASTRMUMCAL WMM PMMM By vmjous nqsTjTmaiS Carl 2YL16 T--svsAticas of the 14th Ast-r=etrical (Cant.) OV/5721 Vasillyev V. Mep k and Do Do Polo:hentsLy Application of Punch- Oira 9&-~:hlues for Calculations Made W the Time Service at the MsIn Astroncutleal ObBervatory . Yealpovs, M. I., azd D. V. Zagrabia. Solution of the Pmblem of ('=,alling a Catalogue of Right Asceasioas of 358 Stars, Uoing Zua:h-4sxd Machinea Yeeiro-m, H. E. The Cs1culation of Memerides of Apparent Right Ascenslzcs of stwo in the Time Service Progm Khrashchev, L. 1. A Comps--ison of Rrrcra in Tine Determination M&IO With Dirfermt Mtroamical InstrMents i 328 332 335 337 leilfrIkP G.. P.J. AO At TO-3hilina, and No Be Blinova. One Caas of the i 30 Deterzinstion of rom*ltuda Aear."Iyevs, P. M. The Effeat of ifind on the Results of the Astro- nomical Determination of TIms 345 cact t*::6 BLINOVA, N.V.; SOVZ, I.Ye. investigation of the Pioht's three-mirror telescope. Sbor.st.LITHO no.4701-97 -159. (MM 16: 10) PETROV, N.Tu.; BLINOVA, N.Y.. red.; SHCHEDRIZIA. II.L., tekhn.red. E ~Ietorical and legal sketch] Sovety narodnogo khosiatetva; istoriko-pravovoi ocherk. Moskva, Gos. icd-vo iurid. lit-ry. 1958. 83 P. (MIRA 12:1) (Russia--Economic policy) F i LAZARET, Boris Mikhaylovich; BLIkOVA ._ vw-~,-_,~z-~' _7d.1 BTKOVA, Vj., tekha,red, [Anforcing the obserfance of prices and regulations in Sovitit , commerce] KontroV sa sobliudenism teen i pravil sovetzkol. torgovli. Moskva, Gos.isd-vo iurid.lit-ryg 1959. 82 P. - (MIRA 12:6) (Retail trade) (Price regulation) XOSLOVA, Tokaterina Iv.anovna; UKANSKITj Ya.l., dotsent, otv,.red,; BLIITOTAq I V. red.; LUMA, Tel** takhnorod, [Soviet construction; textbook for a specialized course] Sovetskoe stroitelletvo; uchebuos posoble po spatskurau. Noskrat I~wwo vyssbego Vereduago spatelalinogo obrasovanlia RSM* 1960, 150 pe* (vm A 14:12) (Constructien Induetry) KALININ~ G.S., dote.; GONCHAROV, A,F*j dotsvp otvq red*j. BLIIOVAj N.V*.q red. [The Soviet state and law in the law in the period of the consolidation of'Soviet rule# October 1917-Ju2y 19181 Sovet- skoe gosudarstvo A pravo v period uprocheniia Sovetskoi vlastis, oktiabrl 1917 - iiull 1916 gg,,-, lektsii dlia studentov VIUZI- Moskvas Vses. iurld. zaochnyi in-t- 'No-l- 1960. 88 p. (MIRA 15:1) (Russia-m-Politiesand government) (Russia-~-Revo'Lutionj, 1917-1921) BMIOVA , N. Ye. "The Carbon Dioxide and Oxygen Content of Venous Blood in Rickets Cases,, 7op. Ped. i Okhtan later. i Det., 16, No.6, 1948 Chair, Pediatric FacuIty and Chair Biochenistry, Leningrad Pediatric I-led. 1nst. C-4 Acid-Un brium In np* and losic ceollitim in dMm. RVI-turavi.. ..d X-K-Bliocim (Unin. "d redist. Inst.). 110prosy pedial. i OkArday Mattf- 140m i Defitto 18. No. 1, 9-14(IWO).-In septic cam tbt lotal Illood Cos was 5 Vol. I- below SIMItal in most In. ktancr-.4. Oxygrif ctuilent w&4 thailufly Intel 7.2-7.3 vW. Irt, a I A UOMIAI 8.3%- vubstances are I ghtly normal In Isnost MOVIC71. toik mwnallcl= al."Ibac Plasma. Cs lly in twic ,'but individual vurlmlons are Veal Cl rR*s in eryttat. O.M.K. ~od and their reactions in toxk and "P "m 1. Kattanskayn and N Moved Pediat. lost.). V pf-Y pedgel-l.", i Ddstw 18. No. I y .)m IS The level of Ilm enlymes and the type of IvArtion it- Opolibe it, 11miruirial, of I"ilk air 11111virm III mpitc. mod toxic tutditims. III the (1411irt, low levels of lipase and valmlism we cluumcictibise, with.. We cultance-nicut o( lipulysis an irritation by ntilk ail- tuinistrallo".. In toxic comitious it higher vatalAw with Icu 1(mvtbtg *( liliam is foundi &nil the milk teactkm is sTn"ally SICK. In chlittren With "ItT11411"l. 4.0114filiatir, lipaw MR) ard law an IOW, VAIAIAW ill FUSISCr high, 41111 the "Alk trat.2% is T"We, G. M. KiW4,411oft WIULINA, S.K.; ANANIIKA, N.V.,;.BL Dynamics of some'bio6hemical indiesoja-children-during an interparoxyamal period of theumatle ftver. Vopokh.mat. i dot. 8 no.2t22-27 F163. (IEEPk 16#7) 1. Iz kafedry fakulltetskoy pediatril, (zav.- '4aystvitellnyy chlen OW SSSR.,zasluzhannyy dayatell nauki prof. M.Maslov Edeceasedl Leniviradekogo pediatrichookogo maditainskogo in- stituta. (RHEUMATIC FEM) (BLOOD-ANALYSES AND GHEMTRY) SAPIR) A.D.: BIRYUKOV, N~D.; HATAL-NIKOV) S.G.; MOLOVA, Z.M.;- NkINA, V.R.; SHUVANOVA, N.V.; KRASIMNINNIM)VA, Ye.F.; Exchange of experience* Zav.lab. 28 no.6:670-671 162. OMIRA 15:5) 1. Chelyabinskiy metalltrgicheskiy zavod (for Sapir). 2. Institut neorganicheskoy khimii Sibirskogo otdeleniya AN SSSR (for Biryukor). 3. Moskovskiy khimiko--tokhno.- logiohe,skiy institut imond Merdeleyeva (for Katallni-kovy Frolova). (Chemistxy, Analytical) 'MoA., red.; B.MOV4jS.Yai., red*; KRASNCV, A.I., takhn.red. [Problam~ in the.economice.of the agriculture of the.Chuvash A.S S.R.; a collection of artiolemil-Voprosy a.konomiki sel'skogo khoilaistva.0huvashokol-ASSR,; oborhik statei. Pod red. K.A. Andreevs, Chebokeary, 0huvashakoe gos.isd-vo, 1957. 242 pi (MM 12:6) 1,Chabokeary Chuvashakiy nauchno-issledovatel'ski'y institut 'literatury. istorii i skonomiki. (Cbuvashia--i~riculture-Jeonomic aspects) SON T. The use of comparisons in a 5th class program. Geog. v shkole no.2:36-39 Mr-AP '53. (MLRA 6;5) (Geography-Study and teaching) q4II I j1,~Lu II i I I I 11 LT -LIIJI UI 8LINOVA~ T. A. BLINOVAJ T. A. -- "Effects of Low Concentrations of Benzenej Styrene, and Alpha-Methyl Strene on the Blood Under Chronic Experim- ental Conditions." 4Dissertations For Degrees In Science and Engineering Defended at USSR Higher Educational Institutions)(29) Min Public Health RSFSR, Lenengrad Sanitary-Hygienic Inst, Leningrad, 1955 SO: Knizhnaya Letopis' No 29, 16 July 1955 For the Degree of Candidate in Medical Sciences BLINOVA V.~416PLOTHIKOWA. N.V.; VOLROV, N.M.; SYSOYNTA, A.V.; AVDRYEV, P.P.: W N. Kh.A.; RODIRA. ?.M.; GUSLTA. L.L.; KAMENSUY. V.1., red.; BYKOV. A.M., tekha.red. (Economy of Tambov Province; a statistical manual] Narodnoe khoziai- stvo Tambovskoi oblaBti; stati ticheskii sbornik. [Tambov] 12d-vo "Tambovelmia pravda.0 1957. 1; pe (MIRA 11:3) 1. Tabmovskaya oblast'. Statistichaskoye upravlenlye. 2. Statisti- cheekoye upravlonlye Tambovskoy oblasti (for all except Kamenskiy, Bykov). 3, Nachallnik Statisticheakogo upravleniya (for lamenakiy) (Tambov Province--Statistics) /7) 137-1958-3-4882 1~ranslation from: Referativnyy zhurnal, Metallurgiya, 1q58, Nr 3, p 61 (USSR) AUTHORS: Lidov, V. P., Blinova, V. A. TITLE: Experience in Smelting Lead-copper Matte With Sodium Sulfide (Opyt plavki svintsovo-mednogo shteyna s sernistyrn natriyem) PERIODICAL: Sb. nauchn. tr. Gos. n.-i. in-t tsvetn. met., 1957, Nr 13, pp 232-234 ABSTRACT: Card 1/2 The shaft smelting of Pb-Cu matte was carried out under industrial conditions. The matte was composed of 19.2 percent Pb and 13.4 percent of Cu, with an addition of converter slag (composed of 2.4 percent Pb, 1.3 percent Cu, 14 percent ZnO, 36.8 percent FeO, 28. 8 percent SiOZ , 10. 61 percent CaO, and 6.54 percent A1203), some industrial sodium sulfide (approxi- mately 70 percent NaZS) , and some Fe- scrap; the charge ingredients, namely: the matte, the converter slag, the sodium sulfide, and the Fe scrap, constituted, respectively, 57 percent, 35.3 percent, 6.2 percent, and 1.5 percent of the charge. In com- parison with the smelting of an analogous charge, but without the addition of Na?S, the weight relationship Cu:Pb in the matte ob- tained increased from 1.9 - 2.6 to 3.8 (5.4 percent of Pb instead 8 137-1958-3-4882 .Fxperience in Smelting Lead-copper Matte With Sodium Sulfide of 10.4 - 14.4 percent) ; Pb content in the waste slag was reduced from 0.9 - 1.7 to 0.7 percent. Cu content in the matte diminished from approximately 27 percent to 20.7 percent. Ye. Z. Card Z/2 ZHILIMKIY, Ye.S., zasluzhennyy vrach RSFSR; EYDELISHTEYN, S.I.,, kand. med.nauk; Prininali uchastiye: AGRONIK, S.Ye., vrach- BLINOVA V A. vrach; GOSPODIROVA, N.Y.., vracb; MARAIKINA,, V.N., vrach; -iiWhYEVAP X.I., vrach, .0 Importance of nicrobi ogical analysis in the treatment O:r,;-) otorhinolaryngologica diseases with antibiotic aerosolS4 Sbor.nauch.-prak.rab.Poliklin.in.F.E.Dserzh. no.23152-162 161 (MIRA 3.68Z (OTORHINOIARYNGOLOGY) (ANTIBIOTICS) (AEROSOL THMAPr) m BLINOVA-,-V.A.; ZHILINSKIY, Ye.S. [deceased] Prevention of side reactions in antibiotic therapy. Antibiotiki 9 no.7:667-669 Jl 164. (MIRA 18:3) 1. Poliklinika imeni Dzerzhinskogo (glavnyy vrach I.G. Karakozov), Moskva. BLINOVA, V.L.; XRAVTSOVAs, V.I. .Drainage map in the glacier atlas of Moimt Elbrus. Inform.abor. 0 rab.Geog-ofak.Mosk.goa.un.po Me2hdunar. geofiz.godu noM93-iO2 162o (KMA 16 z 2) (Elbrus, Mount-Glaciero) (Elbrus, Mount-Drainage-Hapo) BUNOVA., V.L. Studying the discharge of-the Gara-Bashi River using the 4drochemica method,, Informsebor.o rab.Geog.Fak.Molk*gopeun~ po MeWunarigeofizigodu no.9tlO3-n6 162. (KMA 16$2) Gara-BELshi. River-Runoff) 3LI!n!t,.Y.U.p,I~IHIDOV, A.A*; IOLIN. Ys.S.-. MAKUSHKIN, Ya.G.: MYZIN. L.M.-, PHIWAKOV, H.P.; POMILIO, A.I.; BOROVIX, Z.G.; YBYREMOV, I.A.; KOPAYGCRODSKIY. A.Be; HARIWOVI A.M.; NWOROSHKOVA, 0.1.; POKROVSKIY, A.F.; ROIIANOVSKIY, A.A.; RASSADNIKOV, Ye.l., red.; SAVELIYXV, V.Io, red.; FRIDKIN, A.Mo, tekhn.redi [Electric power in the Uxale during the pact 40 years] Inergetilm Urela za 40 let- Moskva, Goa, energ, ixd-vo, 1958. 141 p. (KIRk 11:5) (Ural mountain region-Electric power) BLIHDVI V.N. inzh.; WZILISKIT. V.B., insh. Gas relay protection of transformers in pover system. Blek.sta. 29 no.6:87 Je 158. (MIIU 11:9) (Blectrio transformers) (Bleatric relays) BLINOVA, VeNe.inzh.-. KOZNLISZIY, V.Be.inshe Automatic unloading of electric power lines In Ural power eystems, Blekatae' 29 noo'11:51-34 N 158*' (MM n: 12) - (Ural Nomtain region-31ectric power distribution) BLINOVA, Ye.I. Materials on the distribution of bottom vegetation in the.region of the White Sea Biological-Station of the Moscow State Univer- sity.. Trudy Belomorobiol.sta.MU lt22-34 162. (MML 16tl) 1. Kafedra nlzshikh rasteniy Moskovskogo gosudarstvennogo universiteta. (white Se"lgae) (White Sea-Benthos) XMOVAp le,I,, (Murmansk) Wgraso i~ the Barent a Sea* Pri-roft 51 no*12:105 V 162, (MIM 3.5112) (BiLrento Sea.Eel*pzt) BLI140VAl Ye. I. Distribution-and quantitative indices of commercial algae of the Murmansk sublittoral (Barents Sea). Rast. res. I no. 4083-w590 1,65 (MIRA- 19 %1) 1. Vsesoyuznyy nauabno-issladovatellskiy institut morskolp rybnogo khozyaystva, i okeanografii, Moskva. Submittect July 20, 1965. Vertical distribution and quantitative evaluation of macrophytes of Aynovy Islands (the Barents Sea). Trudy K4BI no-8:41-55 165. Epiphytes of Laminaria of the Murmansk Coast of the Barents Sea. lbid.:56-62, (H= 19: 1) 1. Vsesoyuznyy nauchno-issledovateliskiy institut morskogo rybnogo khozyaystva i okeanografiio laboratoriya kormovoy bazy. KOZHINI L.I.,, prof.~ glav. red.; ABAKLJMOV, V.A., zam. glav. red.; BLIYOVA, Ye.N. red.; BYROV,, V.P., red.; S.G., red.; POWLYAK~ S.I., red.,- VELICHKO, Ye.bt., red. (Papers of young scholars] Trudy molodykh uchenykh. I-loskva2 Pishchevaia promyshlennost', 1964. 261 p. 1. Moscow. Vsesoyuznyy nauchno-issledovatellskiy institut morskogo rybnogo khozyaystva i okeanografii. Vsesoyuznyy nauchno-issladovatellskiy institut morskogo rybnogo kho- zyaystva i okeanografii,, Moskva (for Abakurpov, Blinova, Bykov). BIZENOVA., Ye. N. *A'Hydrod~na~cal Thebx7,of Pressure an'd-Temperature Waves and of Centers of Atmosphere Action," Dokl,,-AN S=p 39,, Noe7s 1943 Chief$ Geophysics ObservatAry 'zp 77' AL c7i, 4t lution 0i the n=-hut;~f f otlans on -fir ZI A10 Vl~r '3(7) N, PHASE I BOOK EXPLOITATION SOV/1837 Akademlya nauk SSSR. Institut fiziki atmosfery Raboty po dinamicheskoy m~teorologii (Works on Dynamic Meteorology) Moscow, Izd-vo AN SSSRs-1958. 186 p. (Series: Its% Trudy, vyp. 2) 1,500 copies printed. Resp. Ed.: I.A. Kibell, Corresponding Member, USSR Academy of Sciences; Ed. of Publishing House: K.P. durov. PURPOSE: The istue of the Instituten'Trudy[Transactions) is intended for scientists and research workers engaged in weather forecasting and climatology. COVERAGE: This collection of articles represents the results of 12 studies in dynamic meteorology, carried out from 1951 through 1954. They treat weather forecasting techniques using the methods of dynamic meteorology as well as general theoretical questions in the study of climate. All authors, Card l/ 4 Works on Dynamic Meteorology SOV/1837 except N.I. Buleyev and A.D. Christyakov, are associated with the Geofizlcheakly Institut (Geophysical Institute of the Academy of Sciences). A.D. Christyakov and N.I. Buleyev are' associated with the TsentralInyy Institut prognozov (Central Institute of Forecasts), OUGMS. References accompany each article. TABLE OF CONTENTS: Foreword 3 _Djinov;a,_Y&j. The Theory of the Annual Rate of Non-zonal Circulation of the Earth's Atmosphere 5 Obukhov, A.M., and A.S. Chaplygina. Change In the Barle Yield in the Middle Troposphere 23 Monin, A.S. Transformations of Energy in the Zonal Circu- - lation ofthe Atmosphere, 50 Card 2/4 Works on Dynamic Meteorology SOV/1837 _jj1jngx&,_Y&,N. The Effect.of Non-linear-Terms in the Equations of Thermohydrodynamics When Solving a Problem Dealing With the Long-range Forecast of Meteorologic Elements 54 Buleyev, N.I... and G.I. Marchuk. The Dynamics of the Large- scale Atmospheric Processes 66 Blinova, Ye.N.J. and G.I. Marchuk. The,Theory of the Annual It-at-e--of-R-111urely zonal circulation 105 Marchuk, G.I. The Annual Rate of the Circulation Index 114 Marchuk, G.I. The Large-scale Thermohydrodynamic Processes in the Baroclifiic Atmosphere . 119 Marchuk, G.I., and N.M. Kireyeva. The Problem of Expansion By Small Parameter of the Solutions of Equation Systems in Hydrothermodynamics.as Related to Atmospheric Processes 142 Card 3/4 Works.on Dynamic Meteorology SOV/1837 Christyakov, A.D. Forecasting Temperature and Wind in the Upp6r Troposphere and the Lower Stratosphere 16o Kogan, S.Ya. The Short-range Forecast of Pressure Field in the Central Troposphere.With the Aid of the Linear Fridman's Equation 167 Kogan, S.Ya. The Solution of a Non-linear Problem Related to the Short-range Forecast of Pressure Field - 177 AVAILABLE: Library of Congress MM/Jmr 6-15-59 Card 4/4 UTI~ 0 R S Bli nova, Ye. N. , Corresponding Member AS USSR SOV/2o-1 2o-2-15/63 Be ouso;~,.. Z. T I T Non-Lineur Nor.-Steady Problem of the Determination of the Planetary Flow Pattern at t'-u Midlevel of the AtiTion-nhare (NelineyrLaya nestat- sionv_rnaya zadacha opr(-deleniya poley davltiriya planetarnogo aiasshtaba ne- srednem urovne atmosfary) P _--~ R I C, D 1 C17.1: Dokiady Ak~idemii naulk 0121>R, 1958, Vol. 120, Nr 2, pp. 281 - 284 ABST' CT- In 194*3 one of the authors ol~' this -oauer recommended a hve.:~o- dynamic method for the lone-term forecLt~;t of pressure fields and t'. e f ow lines ijt atmospheric midleve' . An equation 'or the vortex (a simplified e6t.111tion by A.A.Fri&man) and one of the 'Ailer .(.!,'yler) equations' were used for solvinE this problem. This. P-im was achieved by a linearization of the equations with resgect. to west-east tr--nst'er. The solution of the non-linear nrobl ~m of loni;-terrn weati.erforecast by the methods of hydrodynazie -s was facilltated by electronic computers. The most oirriple solution is obtained for the midlevel ~f'tha atTosnhere. Some variants of Card 1/3 such a solution sui.-.-ested in-1954. 1~ this PaDer the methods Non-Linear Non-S,:ee_dy Problem of IthG Deterirdnation of the SIGjV/2o-12o-2-15/63 Flanethry Flow Pattern at the Midleval of the Attriosp .nore and some-resuits of the application of one of these vari-n.t.s are d4scussed. The equation for the floxy function can be used as th; initial equftion, as was done p*reviously: + (f,A41)+2 LJ 0, where a and&ddenote ,at a 2sin ak 0 the rad.iv,.s and the anCular velocity respectively of the earth. .Further, the equation 2 /2 1 - COSY 2 a -- -1 at 2 0 0 ln 1 _ cos. DY, AV)+2c4a 0sin a' Ans.0 'holds. :dg'dA Let the function lp be known. The forecast of the values of %v can be achieved by means of time steps in the computation. CowDutation is discussed in short. The authors also make a few suggestions for the performance of this computation by means of Card 2/3 electronic computers. The problem under discussion was carried Von~-Linear Non-Steady Problem of the Determination of BOV/20-12o-2-15/63 ~l anetary Flow Pattern at the Midlevel of the Atmosphere out with the BECM (Bollshaya elektronnaya schetnaya mashins: All, SSSR)(great.electronic computer of the AS USSR). Examples con-' cerning the forecast of the absolute topography of the 700 millibar siirface covering periods of up to 10 days are computed. One of these examples is illustrated by three-figures. There are 3 figures and Soviet refirences. ASSCCIATION:Tsentral1nyy institut prognozov (Central Institute of Weather Forecast) -SUBMITTED: February 14, 1958 1. Planetary-atmospheres-Theory 2. Weather forecasting 3. Mathematics--Applieations C;Lrd 3/3 AUTHOR: Blinoj!~~. Corresponding S011/20-123-3-46/54 Academy of Sciences, USSR TITLE: On the Problem of the Forecasting of the Smoothed Values of the Meteorological Elements at the Mean Level.of.the Atmosphere (K voprosu o prognoze sglazhennykh znacheniymeteorologicheskikh elementov na srednem urovne atmosfery) PERIODICAL: Doklady Akademii nauk SSSR, 195Bt Vol 123, Nr 3, pp 440-442 (USSR) ABSTRACT: The field of the current function Y on the mean level of the atmosphere may be calculated by means of the transport equjation of thp absolute curl + 2 CJ 0 ( w aA -a e t a21 sine 0 a denotes the radius of the Earth; c4 -the angular velocity of , 0 the Earth's revolutionj th*e complement of'the latitude; ;k- the longitude (which increases from West to East) of the place; t the time. Moreover it holds that Card 0 (sin 2 ~ ) sin 6) 14 2 sin On tfie Problem of the Forecasting of the Smoothed SOV/20-123-3-i6/54 Values of the Meteorological Elements at the Mean Level of the Atmosphere The motion on the mean level of the atmosphere is assumed to be turbulent and the author endeavors to find a summarizing statistical description of this motion by means of the first equation. This investigation is carried out according to a method developed by L. V. Keller (Ref 1). The first equation contains only one function y (e,Alt) and the author seeks the smoothed values rr (6p;jjt) of this function. The deviations from the smoothed values are denoted by y' (0,A,t) so that TIMIAlt) 7 T(()I;k,t) Smoothing is then applied to the firs equation. The equation deduced in this way (besides the sought function contains the 2 smoothed quantities 'a w which may be expressed by the C) moments of correlation (moment avyazi). Calculations are discussed step by step and the final expression is given explicitly. Smoothing may be carried out by various methods. Card 2/3 .On the Problem of the Forecasting.of the Smoothed SOV/20-123-3-16/54 Valuetwof the Moteorologieal,Elements at the Mean Level of the Atmosphere If it is carried out by averaging over a circle of latitude, a system of equations is obtained the solution of which can immediately give the forecast of the circulation index. There is I Soviet reference. ASSOCIATION: Institut prikladnoy geofiziki Akademii nauk SSSR (Institute of Applied Geophysics of the Academy of Sciences, USSR) SUBMITTED: August 6, 1958 Card 3/3 -3 AUTHOR: TITLE: PERIODICAL- 28413 S/169/61/ooo/Oo7/o73/1o4 Aoo6/Aic)i Blinova, Ye.N. On the theory of a long-range waather forecast by taking into accomt vertical velocities and fluctuations of the tropopause level Referativnyy zhurnal. Geofizika, no. 7, 1961, 69-70, abstract 7B431 (V sb. "Vopr. dinamich. meteorol.", Moscow, AN SSSR, 1960, 12_2D) TEXT: The present study solves the problem of a long-range pressure and temperature forecast with the attempt of taking into account the effect of verti- cal velocities and fluctuations of the.tropopause level. Initial values are: the equation of the tropopause and conditions on it in spherical coordinates, written down for the tropopause altitude g OR ~Lq t). the equation of continuity in spheric coordinates integrated over.Z from 0:)to taking into account the condition on the tropopause the equations of motion along axes Q,?, and the barometric formula. In the equations of motions those terms are neglected which contain the component of velocity along the radius. It is considered that the motion of the atmosphere consists of a purely zonal circulation and its distur- bances. The velocity of the basic motion is represented through the angular ve- Card 1/ 3 26413 S/169/61/00o/007/073/104 On the theory ... A006/A101 locity of air motion in respect to the earth. If the pressure on the tropopause is equal to zero, the barometric formula serves to obtain the value of pressure at a purely zonal circulation and deviation from pressure. The equation of mo- tion along axis 9 and the equation of pressure at a purely zonal circulation pre- determines the altitude of the tropopause. Linearization of the conditibn on the-tropopause and of the equation of motion yields a formula for determining the elements of disturbance of velocity and pressure components. Instead of the disturbances of components it-Is convenient to take their products by the alti- tude of the tropopause, which are then replaced by the derivatives, with respect to the axes, of some functions T and Three equations are obtained to deter- mine T, q/ and g '. To integrate the obtained system of equations, the Haff method is employed. The solution is sought for in the form of a product of two functions one of which depends only on the latitude, and the other one on the longitude and time. To determine the unknown functions a uniform system of con- ventional differential equations is obtained. If the solutions are searched in the form of series in associated Legendre polynomials, an infinite system of al- gebraile equations for 'm is obtained after eliminating the functions ~ m(e) and Y m(B). Using the presence of a small parameter,in the system to be solved, the solution of equations may be represented by expansion in a series in powers of Card 2/ 3 On the theory ... 26413 8/169/61/000/007/0"/104 A006/AlO1 this parameter. Assuming the altitude of the tropopause over the pole to the equal to infinity, terms with small parameters vanish. Representing the solu- tion of the problem by series In spherical functions, the value P is eliminated and already solved equations of long-range weather forecast are obtained. Taking this solution as an initial one (as the first approximation) the solution of the actual problem is represented with an accuracy up to the magnitude of first order in respect to the small parameter. The final solution for 71, and is ob- tained in the form of the sum of associated Legendre polynomials with different coefficients, determined from boundary and initial data. As initial data the author used the diEtribution of pressure for the northern hemisphere at the ini- tial moment-. When finding the distribution of vertical vilooities,, the following formula is taken as a basis: z (vp sin Q + v s -in 0 . 6 0 ?1 VQ and Vkare excluded by means of It and 99by the af re entioned method. Using the values found for F and tP an expression for vertical velocities is obtained. The formula obtained for the forecast of the field of vertical velocities is si- milar to formulae for pressure forecast. N. Chuzavkova [Abstracter's note: Complete translation] Card BLINOVA, Ye.N. Hydrodynamicall investigation of nonstationary atm:)spheric processes on a planetary scale. Dokl. A14 S-SSR 140 no.2:354-357 S '61. MRA 14:9) 1. Ob"yed3nennyy meteorologicheskiy vychislitel'nyy tsentr AN SSSR i Gidrometeorologich6skoy sluzhby SSSR. Chlen-korrespondent AN SSSR- (Geopbysics) (Atmospbere) LMMOVAp Yee N. Three-dimensional problem eond#rnixg the forecasting Of flaUsned values of meteorological elements,, Dokl-i AN SSSR ul *no.6-.13554359 D 162, (KM 16:1) I* VychislitellmV meteorologioheskiy teentr. Chlen-korrespondent AN SM. (Weather forecasting) ACCLSSION;NR: AP4014029 S/0049/64/000/001/03.10/0323 AUTHOR3 Blinova,, Ye.,N T.ITLE.- The'status and immediate objective of the hydrodynamic theory of climate :and of long range weather prediction Cpresentod at the Symposium on Numerical Methods of.1deather Prediotion,, Hoscow., 24 Juno. 19627 -110-123 SOURCE: AN SSSR. Izv. Seriya geofizicheskaya,, no, 1., 1964,, -TOPIC TAGS: hydrodynamic theory,, hydrodynamic climate theoryj, weather predictionp ,.Weather forecasting, long-range weather prediction., long-range foreeastings boundary value problem, thermodynamics .ABVLRA.CT: The author gives a brief survey of modern hydrodynamical methods of short- and long-range forecasting. Basic -trends in developing a theory of climate arA of long-range forecasting are discussed. ~Previous works on the hydrodynamical theory of cl~maie have developed a theory that permits one,, for a given config- uration of,continents and oceans and for a given influx of solar heat,, to deter- minethe basic features of climatio distribution of tomparatme, pressure, and wind,- (in which th4fe is a yearly period) by'solving the boundary value problem of "Cbrd 1/2 ACCESSION NR: AA014029 thermodynamics, This theory may now be refined and, at the same time,, generalized for the problem of long-range weather forecasting in which processes with a yearly period are not'distinguished but,are examined 'together with nonperiodic processes (depending on initial data). Beg:~=ing with velocity functions that neglect previous quasigeostrophic or quasisolenoidal movements) the author derives expres- I sions for the various parameters required in my adequate climatic theory to permit lor4,'-range forecasting, Work of this kind should mpke it possible not only .to extend the forecasting interval and to improve the quality of the predictions,, but it z4ould aid in solving the basic questions on hydrodynamics and thermody---l namics of atmospheric movements on a planetary scale. Ands in particular, it should aid in solving problem associated with the goal of controlling climate, Orig. art, has:! 23 for=aas. USSOCIATION: Vy*chislitellnM motoorologichoskiy tsentr (Meorological Computing~, ,Center) iSUBIMTEDi 19Jul63 DATE AGQ: 14Feb64 ENCLs 00 1 NO Ra Spv: o:L6 -OTHER: 00 SUB CODE: AS Card 2/2 BLISM O.N. DetermiTting the initial wind and prossure fields from the distribation of temperatures and the vertical motions of air, Dokl. AN WSR 149 "11064024-826 -ApI (MMA 160) 1, Vyohislitellnyy meteorologicheakiy teentr, Chlen-korrespondent AN SSSR. (Atmospheric pressure) (Vends) BLINOVAj_ Yq.N., otv.red.; NIKOIAYEVA, L.X., red.izd-vaj VOLKOVAj tekbn. red.; HAKUNI, Ye,V., takhn. red. [Hydrodynamic long-range weather forecasting) Gidrodinami- cheskii dolgosrochrqi prognoz pogody. Moskva, Izd-vo "Nauka," 1964. 105 p. (MIRA 17-.2) 1. Akademiya nauk SSSR., Ob"yedinenzWy moteorologichaskiy vychislitel'My tsentr. 2. Chlen-korrespondent AN SSSR (for Blinova). Ail 4CIMSSION -MR: AT4034671 S/000of"1000/0000005/0018 ..AUTHOR: 81 inova. Ye. N. '~:!-TJTLE: The hydrodynamic theory of climate and long-range weather forecasting ~SOURCE:. -AN SSSR. Ob"yedinenny*y meteorologicheskly vy*chIsIIteI'ny*y tsentre amic ldhg-range weather' .7'Gidrod.inamicheskly dolgosrochny*y prognoz pogod)* (Hydrodyn forecasting). Moscow, Izd-vo' "Hauke," 1964, 5-18 TOPIC TAGS: meteorology, weather forecasting. long-range weather forecasting$ climate, climatology, climate theory- ABSTPACT: In earlier studies (Ookl.,AN SSSRO 140, No. 2, 1961; Ookl. AN SSSR, 140, No* 3. 1961) the author reduced-the problem of long-range forecasting of meteoro- .1''logical elements to the solution of a system of differential equations describing not only aperiodic.processes, but also processes possessing an annual period (cII_ matic processes). On the basis of this Initial work the author now has proposed a specific scheme for solution of the derived system of differential equations. The paper begins with a general consideration of the problem., followed by a detailed solution of the equations and selection of numerical values of the parameters In the problem. The forecasting problem Is solvedlin time steps. All equations In Ithe problem are written so that an implicit system Is obtained relative to th .2 BLINOVA, Ye,N, State and prospects of the development of the hydrodynamic theory. of climate and long-range weather forecasting. Trudy MMTs no.2: 3- 20 164 (Mila 1881.) A G a 'L A L.Ak It- Y. G. Is -3-j 1 -2 AA N.AXAP -t'4-A A, sit, A V101 o - , pboclost A" Gas Goa o l IN kow firm. I Na. TIM 1 471- 0 g ideid.t.1 tly. that U;A film, i~; torn."I for the wt of l1w k4tbiv Substfu waftv Sislymilk UK41 In the pnimu (l I d I b A l1 lle. Sts"ShA. The itit). avtone. GJC,) van m In " r0 u, AvOlit y IA-