ADVANCES IN POLAR SCIENCE ›› 1991, Vol. 2 ›› Issue (2-English): 24-37.
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Zhu Cheng1, Cui Zhijiu2 and Xiong Hei-gang3
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Abstract:
From the data of the pitting, geoelectrical prospecting, temperature measurement, salt content analysis and detection by layering frost-heaving instruments, the authors discuss firstly the structural features of sediments in the active layers in this region, and proves the presence of the bowl-shaped frost table in the stone-circles area, and then analyse the regulatities of temperature distribution in the active layer, effect of salt content on electric resistivity, thaw-settlement and frost-heaving, and their control on periglacial land-form development. It suggests that the five layers should exist in the subsurface structure , namely, active layer, frost sand and gravel layer, frost volcanic rock permeated by sea water, frost volcanic rock unperme-ated by sea water, and unfrost ancient continental basement. Finally, the permafrost table and its vertical gradient are deduced.
Key words: Active layer, Permafrost table, Bowl-shaped frost table, Salt content, Geoelectrical Prospecting
Zhu Cheng, Cui Zhijiu, Xiong Hei-gang. CHARACTERISTICS OF THE ACTIVE LAYERS ON FILDES PENINSULA OF KING GEORGE ISLAND, ANTARCTICA[J]. ADVANCES IN POLAR SCIENCE, 1991, 2(2-English): 24-37.
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URL: https://journal.chinare.org.cn/EN/
https://journal.chinare.org.cn/EN/Y1991/V2/I2-English/24