Abstract
Polish brines are highly mineralized and can potentially be used for recovery of selected useful elements such as magnesium and potassium. They also contain a number of other elements, including
iodine, bromine, boron, and strontium. The results of the examination of the chemical composition
of groundwater from the Mesozoic formations (bromine, iodine, lithium, magnesium, and strontium
content) of northern and central Poland were analyzed. The basic statistical parameters of the content
of these elements (Br, I, Mg) in brines of the Triassic, Jurassic, and Cretaceous deposits and the content
of lithium and strontium in waters of the entire Mesozoic formations were determined. In order to
indicate aquifers that are the most suitable for the recovery of bromine, iodine, lithium, magnesium,
and strontium, the relationship between concentrations and the depth of retention and dependencies
between selected chemical components of these waters were analyzed.
It has been found that the mineralization and concentrations of magnesium, bromine, and iodine
increase with the age of aquifers, where these waters occur. Triassic waters are the most prospective
for bromine and magnesium recovery among all analyzed aquifers. Furthermore, a relationship between
the content of bromine, strontium, and magnesium has also been observed. The increase in the content of individual elements observed for lithium, strontium, and bromine with the increasing depth
indicates a potential abundance of waters occurring at significant depths. The presented analysis is
an approximation of the content of bromine, iodine, lithium, magnesium, and strontium; however,
it may be the basis for further studies on the perspectives of using brines from the Mesozoic deposits
of central and northern Poland as a source of chemical raw materials.
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