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Sorting of Clastic Material in Eolian Deposits of Central Kara Kum

  • M. A. Romanova

Abstract

Eolian sorting of clastic material in recent sands of the Kara Kum Desert is analyzed. The mobility of the components is determined by the value of highest gradient of trend surfaces. The causes relating to formation of mineral associations in the eolian sands are examined on the basis of a linear model.

Keywords

Specific Gravity Eolian Sand Clastic Material Sand Transport Quartz Content 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Bagnold, R. A., The Physics of Blown Sand and Desert Dunes, London (1941).Google Scholar
  2. Bondarev, L. G., “Eolian sands along the upper reaches of the Bol’shoi Naryn,” in: Physical Geography of Tien Shan, Izd. Akad. Nauk KirgSSR (1966), pp. 12-19.Google Scholar
  3. Bol’shev, L. N., and Smirnov, N. V., Tables of Mathematical Statistics, Izd. Nauka, Moscow (1965).Google Scholar
  4. Chepil, W. S., “Dynamics of wind erosion: The nature of movement of soil by wind,” Soil Sci. Soc. Am. Proc, Vol. 60, pp. 305–320 (1945).Google Scholar
  5. Chepil, W. S., “The use of spheres to measure lift and drag on wind-eroded soil grains,” Soil. Sci. Soc. Am. Proc., Vol. 25, pp. 343–345 (1961).CrossRefGoogle Scholar
  6. Ermilov, I. Ya., “Eolian accumulation forms in the saline deserts of western Turkmenistan,” Izv. Vsesoyuzn. Geogr. Obshch., Vol. 81, No. 3, pp. 327–333 (1949).Google Scholar
  7. Exner, F. M., “Zur Physik der Dunen,” Sitzber. Akad. Wiss., Pt. II, Vol. 129, Wien, 929–959 (1920).Google Scholar
  8. Fedorovich, B. A., The Role of Wind in the Formation of the Sandy Landscape of the Desert, Tr. Inst. Geogr., Vol. 36, Izd. Akad. Nauk SSSR, Moscow (1940).Google Scholar
  9. Fedorovich, B. A., “Origin and development of sandy strata in the desert,” Azii. Mat. po Chetvert. per. SSSR, No. 2, pp. 221-233 (1950).Google Scholar
  10. Horner, G. N., “Some notes and data concerning dunes and sand drift in the Gobi Desert,” Sci. Exped. Northwest Provinces China, Sino-Swedish Exped., Publ. 40, Vol. III, Geol., No. 5, p. 40 (1957).Google Scholar
  11. Luppov, N. P., “The Middle Pliocene stage in the geologic history of the trans-Caspian region,” in: Problems of Oil and Gas Occurrence in Central Asia, No. 14, pp. 11-37, Gostoptekhizdat, Leningrad (1963).Google Scholar
  12. Orlov, B. P., “Mechanism of advance of individual sand grains and sandy accumulations,” Zemlevedenie, Nov. Ser., Vol. 5, pp. 25–41 (1960).Google Scholar
  13. Petrov, M. P., Moving Sands of the Soviet Union and the Fight Against Them, Izd. Geogr. Lit., Moscow (1950).Google Scholar
  14. Priestly, C. H. B., Turbulent Transfer in the Lower Atmosphere, University of Chicago Press, Chicago (1959).Google Scholar
  15. Romanova, M. A., “Separating the sands of the central Kara Kum into districts according to spectral brightness,” Dokl. Akad. Nauk SSSR, Vol. 156, No. 5, pp, 1095–1098 (1964a).Google Scholar
  16. Romanova, M. A., “Recent deposits of sand in central Kara Kum and the problem of studying subsurface structures,” Sov. Geol., No. 12, pp. 70-89 (1964b).Google Scholar
  17. Senkevich, B. I., “Experimental investigations of eolian erosion of sands,” Izv. Akad. Nauk TurkmSSR, Ser. Biol. Nauk, pp. 21-30 (1962).Google Scholar
  18. Sidorenko, A. V., “Eolian differentiation of material in the desert,” Izv. Akad. Nauk SSSR, Ser. Geogr., No. 3, pp. 3-22 (1956).Google Scholar
  19. Vistelius, A. B., and Sarsadskii, N. N., “Nature of changes in mineral content of concentrates during successive washing of sands,” Zap. Vses. Mineralog. Obshchestva, Pt. 80, No. 2, pp. 143-152 (1952).Google Scholar
  20. Vistelius, A. B., and Yanovskaya, T. B., “Programming problems of geology and geochemistry for use with all-purpose electronic computers,” Geol. Rudn. Mestorozhd., No. 3, pp. 34-48 (1963).Google Scholar
  21. Williams, G., “The effect of eolian transport of sand at various heights on the grain-size distribution,” Dokl. Akad. Nauk SSSR, Vol. 149, No. 2, pp. 410–412 (1963).Google Scholar
  22. Williams, G., “Some aspects of eolian saltation load,” (U.S. Geol. Surv., Wash.) Sedimentology, No. 3, pp. 275-287 (1964).Google Scholar
  23. Znamenskii, A. I., “Movement of barchan sands,” Tr. Turkmensk. Fil. Akad. Nauk SSSR, Vol. 2 (1942).Google Scholar
  24. Znamenskii, A. I., “New principals of protection of industrial and domestic buildings against drifting sand,” in: Objectives and Potentials of Prospecting-Exploratory Work on Oil and Gas in the Western Parts of Central Asia, Ashkhabad (1959).Google Scholar

Copyright information

© Springer Science+Business Media New York 1970

Authors and Affiliations

  • M. A. Romanova
    • 1
  1. 1.Laboratory of Mathematical Geology, V. A. Steklov Mathematical InstituteAcademy of Sciences of the USSRLeningradUSSR

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