Scholarly record
CONCENTRATION OF TRACE ELEMENTS IN SOILS HISTORICALLY AFFECTED BY COAL MINING IN SVALBARD
Abstract
A comprehensive, three-year (2013 ? 2015) geochemical analysis of soils has been conducted within impact areas of the main Russian and Norwegian coal mining centers in Svalbard. This study was focused on identifying both natural and technogenic trace elements and rare earth elements within a variety of landscapes with location of emission sources and natural factors of contaminants' distribution having been taken into account. The concentrations of macro, micro elements, Trace Elements (TM) and Rare Earth Elements (REE) were measured to determine the actual concentrations and their spatial distribution. Obtained data was compared with world soils averages and average values obtained in different places in Svalbard. Results of the study show that averages of elements for historically affected by coal mining soils in Longyearbyen and Barentsburg areas can be determined as the following values: Al ? 0.74В±0.17%;Ba ? 135В±65 mg/kg; Fe ? 1.1В±0.1%; Cd - 0.18В±0.3 mg/kg; K ? 0.1В±0.03% mg/kg; Ca ? 0.2В±0.1%; Co - 9.4В±2.8 mg/kg; Mg ? 0.2В± 0.1%; Mn - 219В±82 mg/kg; Cu - 19.4В±9 mg/kg; As - 8.6В±4 mg/kg; Na - 236В±258 mg/kg; Ni - 17В±5 mg/kg; Pb - 10.8В±2 mg/kg; Sr - 238В±151 mg/kg; Ti - 984В±643 mg/kg; Cr - 11.2В±3 mg/kg; Zn - 57В±14 mg/kg; B - 24В±12 mg/kg; V - 32В±6 mg/kg. The average values of Gallium (Ga), Lithium (Li), Niobium (Nb), Zirconium (Zr) and Rare Earth elements (REE) including (Dysprosium (Dy), Europium (Eu), Ytterbium (Yb), Yttrium (Y), Lanthanum (La), Praseodymium (Pr), Samarium (Sm), Scandium (Sc), Cerium (Ce) in studied soils were newly analyzed and equal (in mg/kg); Ga - 14.7В±3.2; Dy - 3.0В±0.9; Eu - 1.5В±0.4; Yb - 3.8В±0.7; Y - 26.0В±6.9; La - 24В±6; Li - 83В±22; Nb - 18В±5; Pr - 2.3В±0.5; Sm - 6.2В±1.5; Sc - 14.0В±3.5; Ce - 53В±13; Zr - 54В±32.
Publication Impact Profile
Publication details
References0
Structured references will appear here after the reference import pass. The count is preserved now so the scholarly record is not incomplete.
View or Download full articleAccess options
SWS access login
Login as SWS Scientific CommitteeLogin as SWS Scientific PartnerLogin as SWS AuthorAuthors and approved SWS contributors will read and export their own linked papers after identity matching by SWS profile, email and SGEM GlobalID.
For librarian assistance: [email protected]
Purchase Instant Access
- Article can be downloaded after successful payment.
- Article may be used according to SWS library access terms.
- Article cannot be redistributed.

