TY - JOUR N2 - In the southern Spitsbergen area, thermal and mineral waters are primarily associated with subpermafrost deep circulation, being mixed with shallow circulation and glacial waters. Four thermal springs, located in the region of Stormbukta (Sørkappland), were studied and analyzed. In the thermal waters, the main cation is sodium, while the main anions are chloride and bicarbonate. The temperatures of the mineral and thermal waters range from 3.4 to 15.1°C. The pH values are between 7.43 and 8.41. The total dissolved solids (TDS) content of the geothermal waters is in the range of 346–4031 mg/l and the Olsok thermal spring has the highest TDS values. Based on the variation in physicochemical characteristics, two thermal water types were distinguished in the study area. The first type is associated with thermal waters originating from deep circulation waters. The second type is associated with the thermal and mineral waters originating from the mixture of subpermfrost hot brines with glacial waters. L1 - http://journals.pan.pl/Content/103316/PDF/Polish%20Polar%203-18%201-T.Olichwer%20i%20in.pdf L2 - http://journals.pan.pl/Content/103316 PY - 2018 IS - No 3 EP - 331–348 KW - Arctic KW - Svalbard KW - thermal water KW - water chemistry A1 - Olichwer, Tomasz A1 - Tarka, Robert PB - Polish Academy of Sciences PB - Committee on Polar Research VL - vol. 39 DA - 2018.10.02 T1 - Thermal and mineral springs of southern Spitsbergen SP - 331–348 UR - http://journals.pan.pl/dlibra/publication/edition/103316 T2 - Polish Polar Research ER -