Groundwater chemistry in intrapermafrost taliks in Central Yakutia |
| |
Authors: | Email author" target="_blank">N?A?PavlovaEmail author A?B?Kolesnikov V?S?Efremov V?V?Shepelev |
| |
Institution: | 1.Melnikov Permafrost Institute, Siberian Branch,Russian Academy of Sciences,Yakutsk,Russia |
| |
Abstract: | An intrapermafrost aquifer system, which is widespread in the sand deposits of bestyakhskaya terrace of the Lena R. (Central Yakutia), is characterized by generalized data of many-year studies of its groundwater chemistry. The groundwater discharges onto land surface through high-yield springs. The largest such source forms the Ulakhan-Taryn Creek with a mean many-year yield of 20 740 m3/day. The results of generalization were used to show the chemistry of intrapermafrost water to be stable at both many-year and annual scales, to characterize the hydraulic interaction of intrapermafrost water with suprapermafrost and subpermafrost water, to assess the spatial variations of groundwater resources in the intrapermafrost aquifer from the head-formation to the discharge domain. The results of the study are of importance for solving the problem of centralized drinking water supply to large populated localities in the Central Yakutia, including Yakutsk City. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|