Vol. XIX, No. 4 (October–December 2015)

CONTENTS


REGIONAL PROBLEMS OF GEOCRYOLOGY

  • Dubrovin V.A., Kritsuk L.N., Polyakova E.I. Temperature, composition and age of the Kara Sea shelf sediments in the area of the Marre-Sale geocryological station

  • Slagoda E.A., Krylov A.V., Popov K.A., Opokina O.L., Drozdov D.S., Rogov V.V., Kurchatova A.N., Orekhov P.T., Ermak A.A., Khodzher T.V., Tomberg I.V., Suslova M.Yu., Zhuchenko N.A., Abramov A.A. Permafrost in Hayes island, Franz Josef Land Archipelago

  • Bobrik A.A., Goncharova O.Yu., Matyshak G.V., Ryzhova I.M., Moskalenko N.G., Ponomareva O.E., Ogneva O.A. Correlation of active layer thickness and landscape parameters of peatland in northern West Siberia (Nadym station)

PERIGLACIAL PROCESSES AND LANDFORMS

  • Vasil’chuk Yu.K., Budantseva N.A., Vasil’chuk A.C., Podborny Ye.Ye., Sullina A.N., Chizhova Ju.N. Multistage Holocene massive ice near the Sabettayakha river mouth, Yamal Peninsula

  • Khimenkov A.N., Sergeev D.O., Vlasov A.N., Kozireva E.A., Rybchenko A.A., Svetlakov A.A. Modern and paleo-cryogenic formations on Olkhon island

HYDRATE FORMATION

  • Bondarev E.A., Rozhin I.I., Popov V.V., Argunova K.K. Assessment of possibility of natural gas hydrates underground storage in permafrost regions

SAFETY OF STRUCTURES AND FOUNDATIONS IN PERMAFROST

  • Khrustalev L.N., Gunar A.Yu. Thermal influence of gas and oil boreholes on the stability of a gravity platform located on the Arctic continental shelf

  • Gorelik J.B. Operation of two-phase thermosyphons with horizontal evaporator tubes: causes of instability

METHODS FOR CRYOSPHERE RESEARCH

  • Olenchenko V.V., Sinitsky A.I., Antonov E.Y., Eltsov I.N., Kushnarenko O.N., Plotnikov A.E., Potapov V.V., Epov M.I. Results of geophysical surveys of the area of “Yamal crater”, a new geological structure

  • http://earthcryosphere.ru//archive/2015_4/eng2015-4/09.Olenchenko_4_2015_eng.pdShirshova L.T., Gilichinsky D.A. , Ostroumova N.V., Yermolayev A.M. Application of spectrophotometry to quantification of humic substances in permafrost sediments