TY - JOUR

T1 - Microelements in Radon Waters of the Zaelsovsky field (The Southern Part of West Siberia)

AU - Novikov, D. A.

AU - Korneeva, T. V.

PY - 2019/4/1

Y1 - 2019/4/1

N2 - The results of the studies of the mechanisms of microelements accumulation in the radon waters of the Zaeltsovsky field (the southern part of West Siberia) are presented for the first time. The key role of the water-rock system in these processes is shown. The radon waters of calcium hydrocarbonate and calcium-sodium hydrocarbonate composition with total mineralization ranging from 322 up to 895 mg/dm 3 ( 222 Rn = 11-801 Bq/dm 3 ) are prevailing in the field. Metal species such as Ag + , Ba 2+ , Zn 2+ , Ni 2+ , Mn 2+ , Sr 2+ , Fe 2+ are represented by free ions, and Be 2+ , Fe 3+ , Zr 4+ , Ti 4+ by hydroxide complexes. Calculations reveal that the waters are saturated with carbonate (modifications CaCO 3 and CaMg(CO 3 ) 2 , MnCO 3 , FeCO 3 , PbCO 3 ), silicate ((Fe 2+ , Fe 3+ ) 2 - 3Si 2 O 5 (OH) 4 ), hydroxide (FeOOH and MnOOH) and oxide minerals (modification SiO 2 , TiO 2 , Mn 2+ Mn 2 3+ O 4 ). Radon waters are unsaturated with some compounds of zircon, zinc, barium, molybdenum, iron, copper, strontium: ZrO 2 , Zn(OH) 2 , BaCO 3 , CaMoO 4 , FeMoO 4 , CuO, CuMoO 4 , Cu 3 ( 3 ) 2 ( ) 2 , Fe(OH) 2 , Cu(OH) 2 , SrSO 4 , SrCO 3 , 3MgO 2 SiO 2 •2H 2 O etc. In some samples, the observed saturation of water is relatively rare phosphate minerals (Ca 10 (PO 4 ) 6 (OH) 2 , Fe 3 (PO 4 ) 2 •8H 2 O, MnHPO 4 ), chlorargyrite (AgCl) and lead molybdate (PbMoO 4 ). The concentrations of some elements (namely Sr, Pb, Zn Mo, Be) in the radon waters of the Zaeltsovsky field are at the level of their concentrations in rocks.

AB - The results of the studies of the mechanisms of microelements accumulation in the radon waters of the Zaeltsovsky field (the southern part of West Siberia) are presented for the first time. The key role of the water-rock system in these processes is shown. The radon waters of calcium hydrocarbonate and calcium-sodium hydrocarbonate composition with total mineralization ranging from 322 up to 895 mg/dm 3 ( 222 Rn = 11-801 Bq/dm 3 ) are prevailing in the field. Metal species such as Ag + , Ba 2+ , Zn 2+ , Ni 2+ , Mn 2+ , Sr 2+ , Fe 2+ are represented by free ions, and Be 2+ , Fe 3+ , Zr 4+ , Ti 4+ by hydroxide complexes. Calculations reveal that the waters are saturated with carbonate (modifications CaCO 3 and CaMg(CO 3 ) 2 , MnCO 3 , FeCO 3 , PbCO 3 ), silicate ((Fe 2+ , Fe 3+ ) 2 - 3Si 2 O 5 (OH) 4 ), hydroxide (FeOOH and MnOOH) and oxide minerals (modification SiO 2 , TiO 2 , Mn 2+ Mn 2 3+ O 4 ). Radon waters are unsaturated with some compounds of zircon, zinc, barium, molybdenum, iron, copper, strontium: ZrO 2 , Zn(OH) 2 , BaCO 3 , CaMoO 4 , FeMoO 4 , CuO, CuMoO 4 , Cu 3 ( 3 ) 2 ( ) 2 , Fe(OH) 2 , Cu(OH) 2 , SrSO 4 , SrCO 3 , 3MgO 2 SiO 2 •2H 2 O etc. In some samples, the observed saturation of water is relatively rare phosphate minerals (Ca 10 (PO 4 ) 6 (OH) 2 , Fe 3 (PO 4 ) 2 •8H 2 O, MnHPO 4 ), chlorargyrite (AgCl) and lead molybdate (PbMoO 4 ). The concentrations of some elements (namely Sr, Pb, Zn Mo, Be) in the radon waters of the Zaeltsovsky field are at the level of their concentrations in rocks.

KW - GROUNDWATER

KW - HYDROCHEMISTRY

KW - AREAS

UR - http://www.scopus.com/inward/record.url?scp=85064879874&partnerID=8YFLogxK

U2 - 10.1088/1742-6596/1172/1/012096

DO - 10.1088/1742-6596/1172/1/012096

M3 - Conference article

AN - SCOPUS:85064879874

VL - 1172

JO - Journal of Physics: Conference Series

JF - Journal of Physics: Conference Series

SN - 1742-6588

IS - 1

M1 - 012096

T2 - International Conference on Applied Physics, Power and Material Science 2018, ICAPPM 2018

Y2 - 5 December 2018 through 6 December 2018

ER -