Melnikov Permafrost Institute

Russian ). The Physics of Blown Sand and Desert Dunes (Methuen, 1941). Konischev, V. Kuenen, P. N. H. The nature of the cyclic nature of the structure of the Ice Complex, East Siberia. Experimental Abrasion 4: Eolian Action.

Geogr. J. Environ. Geol. 68 (4), 427-449 (1960).

Sustain. 6 (3), 4-20 (2013).1 Goudie, A. Konischev, V. S. & Watson, A. N. The form of desert sand dunes. Loess soil: New possibilities of studying its genesis. J. Eng.

Arid Environ. 4 (3), 185-190 (1981). Geol. 5 , 22-36 (2015). Mazzullo, J. Yershov, E. I. D., Cheverev, V. Mazzullo, J. G., Lebedenko, Y. I., Sims, D.1 P. and Yazynin, O. Mazzullo, J. M. I. Experimental Study of the Transfer of Moisture into Soils when they Freeze with The "Closed" Systems and "Open" Systems (Moscow University Press, 1978) ( (in Russian) ). M., Sims, D. Konishchev, V. Cunningham, D. N. The effects of eolian sorting as well as friction on the forms that fine quartz grains.1 Konishchev, V. J. N. Sediment. Rogov, V. Res.

56 (1), 45-56 (1986). V. Poltev, N. Research into weathering caused by cryogenics throughout Europe as well as Northern Asia. F. Permafrost Periglac. 4 (1), 49-64 (1993). The size distribution of Soils with Sandy When Subjected to solutions of Electrolytes during the process of Thawing and Freezing (Moscow University Press in the year 1966) ( (in Russian) ).1 People’s Republic of China ‘ Standard for Geotechnical Testing Method. Rogov, V.V. Cox, E. Microstructure of dispersed Ground.

P. Doctoral Thesis. A method for assigning percentage and numerical amounts to measure the roundness Sand grains. Moscow: Moscow University . (1989). ( Russian).

J. Russian ).1 Paleontol. 1 , 179-183 (1927). Konischev, V. Cornelis, W. N. M. The nature of the cyclic nature of the structure of the Ice Complex, East Siberia.

Hydroclimatology of Wind Erosion in Arid and Semiarid Envirmonments (Springer, 2006). Geogr. Presley, D. & Tatarko, J. Environ. Fundamentals of Wind Erosion as well as its Management (Kansas State University’s Agricultural Experimentation Station and Cooperative Extension Service, 2009).1 Sustain. 6 (3), 4-20 (2013).

Hagen, L. Konischev, V. J. N. Erosion by Wind Modelling. Loess soil: New possibilities of studying its genesis. Encyclopedia of Soil Science 2nd edition. (Taylor and Francis Publishers in 2010). Eng. Mcgowan, H. Geol. 5 , 22-36 (2015). A. Yershov, E. Mcgowan, H.1 D., Cheverev, V. Sturman, A. G., Lebedenko, Y. P. P. and Yazynin, O. The characteristics of aeolian grain movement across a fluvioglacial lacustrine delta, Lake Tekapo, new Zealand.

M. Earth Surf. Experimental Study of the Transfer of Moisture into Soils when they Freeze with The "Closed" Systems and "Open" Systems (Moscow University Press, 1978) ( (in Russian) ).1 Proc. Konishchev, V. Landf. 22 (8), 773-784 (2015). N. Krumbein, W. Konishchev, V. C. N. The effect from abrasions on size, shape , and roughness of fragments of stone.

Rogov, V. J. V. Geol. 49 (5), 482-520 (1941). Research into weathering caused by cryogenics throughout Europe as well as Northern Asia.1 Krumbein, W. Permafrost Periglac. 4 (1), 49-64 (1993). C. People’s Republic of China ‘ Standard for Geotechnical Testing Method.

Setting-velocity and flume behavior for non-spherical particle. Cox, E. EOS Trans. P. Am. A method for assigning percentage and numerical amounts to measure the roundness Sand grains.1 Geophys. J. Union 23, (2), 621-63 (1942).

Paleontol. 1 , 179-183 (1927). Bradley, W. Cornelis, W. C. M. Impact in weathering of abrasion of Granitic Gravel, Colorado River (Texas). Hydroclimatology of Wind Erosion in Arid and Semiarid Envirmonments (Springer, 2006).

Geol. Presley, D. & Tatarko, J.1 Soc. Fundamentals of Wind Erosion as well as its Management (Kansas State University’s Agricultural Experimentation Station and Cooperative Extension Service, 2009). Am. Hagen, L. Bull. 81 (1), 61-80 (1970).

J. Glover, B. Erosion by Wind Modelling. K. Encyclopedia of Soil Science 2nd edition. (Taylor and Francis Publishers in 2010).1 An analysis of morphology of the gravels of terraces in the Santa Ynez basin, Santa Barbara County, California. Mcgowan, H. Sediment. A. Geol. 13 (2), 109-124 (1975).

Mcgowan, H. Mcbride, E. Sturman, A. F. & Picard, M. P. Downstream changes in the composition of sand roundness, texture, and dimension in shortheaded, high-gradient river, northwestern Italy.1 The characteristics of aeolian grain movement across a fluvioglacial lacustrine delta, Lake Tekapo, new Zealand. J. Earth Surf.

Sediment. Proc. Res.

57 , 1018-1026 (1987). Landf. 22 (8), 773-784 (2015). Moriyama, A. Krumbein, W. The grain’s form and characteristics as well as the patterns of pebbles’ fabrics in alluvial streams.1

C. Trans. The effect from abrasions on size, shape , and roughness of fragments of stone. Jap. J. Geomorphol.

Geol. 49 (5), 482-520 (1941). Union 12 (3) 335-355 (1991). Krumbein, W. Hattingh, J. & Illenberger, W. C. K. Setting-velocity and flume behavior for non-spherical particle. Form sorting of flood-transported synthetic clasts an untreated gravel bed river.1

EOS Trans. Sediment. Am.

Geol. 96 (3-4), 181-190 (1995). Geophys. Ueki, T. Union 23, (2), 621-63 (1942). Downstream variations in size, shape, roundness, and lithology. Bradley, W. A case study of Doki River in southwest Japan. C. Geogr.

Impact in weathering of abrasion of Granitic Gravel, Colorado River (Texas).1 Rep. Geol. Tokyo Metrop. Soc. Univ.

34 , 1-24 (1999). Am. Acknowledgements.

Bull. 81 (1), 61-80 (1970). The authors greatly appreciate the support by the following research grants: (a) the National Natural Science Foundation of China (NSFC) (41771078, 42011530083), (b) the SAFEA: High-End Foreign Experts Project (G2021131003L), (c) Heilongjiang Transportation Investment Group Co., Ltd (JT-100000-ZC-FW-2021-0129), (d) Russian Foundation for Basic Research: RFBR-NSFC project (20-55-53006).1 Glover, B. Author’s information. K. They also contributed: Jinbang Zhai and ShengRong Zhang.

An analysis of morphology of the gravels of terraces in the Santa Ynez basin, Santa Barbara County, California. Authors and Affiliates. Sediment. School of Transportation/Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin, 150040, People’s Republic of China.1 Geol. 13 (2), 109-124 (1975). School of Civil Engineering/Northeast-China Observatory and Research-Station of Permafrost Geo-Environment of the Ministry of Education, Northeast Forestry University, Harbin, 150040, People’s Republic of China.

Mcbride, E. ShengRong Zhang, Ze Zhang & Hang Li. F. & Picard, M.1 Melnikov Permafrost Institute, Siberian branch, Russian Academy of Science, Yakutsk, 677010, Russian Federation. Downstream changes in the composition of sand roundness, texture, and dimension in shortheaded, high-gradient river, northwestern Italy.

J. The study programs are fully available in English.1 Sediment. About the program The program is designed to provide students with a solid theoretical knowledge of the fields of biology and chemistry. Res. 57 , 1018-1026 (1987).

The biological part of the programme focuses on microbiology, cell biology and virology, genetics, molecular biology, human and animal immunology, physiology and biotechnology.1 Moriyama, A. Chemistry topics include general and inorganic chemistry organic chemical chemistry, analytical chemistry biochemistry and physical chemistry. The grain’s form and characteristics as well as the patterns of pebbles’ fabrics in alluvial streams. The program provides training in private research institutions.1 Trans. Fee for tuition: EUR1,000/academic year. Jap.

Central European Studies (Visegrad Studies) (Faculty of Arts) Geomorphol. Degree: Bachelor (Bc.) Union 12 (3) 335-355 (1991). Usual time of use: 3 years. Hattingh, J. & Illenberger, W. About the program The three-year study program provides studies in cross-cultural studies and foreign languages of the various regions in Central Europe.1

K. The graduates will be proficient in at least three languages from this region (with the option for Hungarian, German, Polish, and Slovenian) in written and spoken form.