Abstract

Boron minerals are a sought-after raw material. The European Union’s total dependence on imported borates means that this has been a critical material since 2014. Due to the increased use of borates in modern economies, data on the predicted boron demand in the coming years indicate that it may become a critical element on a global scale. Formerly, the high boron content in groundwater was the basis for qualifying it as medicinal water (boric water). Nevertheless, the current information on the potential toxicity of boron and the narrow margin between deficiency and toxicity of boron in the human body has caused a tightening of the limits of this element in water intended for human consumption. For this reason, metaboric acid has lost its position as a specific component of curative waters. However, despite the fact that boron is not currently a specific component of curative waters, it is found in measureable concentrations in Polish medicinal water considered therapeutic based on other valuable specific components. High boron content in curative water may be the cause of the problems in some spas when obtaining certificates confirming the therapeutic properties of waters. Literature data indicate that waters with high boron content (above 25 mg/L) should not be freely available for drinking in pump rooms and other places in health resorts. To identify the situation with Polish health resorts, the content of boron in 248 curative water samples was analyzed. In 154 of these samples, the boron concentration was relatively low and did not exceed 5 mg/L. However, in the remaining 94 samples, the boron content exceeded 5 mg/L, and 38 samples had boron content exceeding 30 mg/L. Ten of the 248 samples of curative water had a boron concentration above 100 mg/L, which may be a potential source of boron for industrial recovery. The highest concentration of boron was noticed in a water sample from the Wysowa health resort and was 187.6 mg/L. Unfortunately, most of water intakes with a high concentration of boron (above 100 mg/L) are low-yielding wells. Based on the data collected, Rabka appears to be the best candidate for small-scale boron production in terms of boron content and water resources values.

Highlights

  • The boron content in the lithosphere is relatively high

  • The analyses found in scientific publications typically contain information on the concentration of main ions and specific components

  • The analyses conducted in this paper show a strong correlation between boron conThe analyses conducted in this paper show a strong correlation between boron concentration and Na++, HCO3−− ions and the sum of dissolved solids centration and Na, HCO3 ions and the sum of dissolved solids in the HCO -Cl-Na water type

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Summary

Introduction

The boron content in the lithosphere is relatively high. The value of the boron concentration in the continental crust is on average 10 mg/kg. Boron does not exist in nature as a pure element. It is found in bonded form [1,2]. There are over 200 different boron minerals in nature. The most important boron minerals are compounds containing boron oxide in varying proportions, i.e., tincal (borax) (Na2 B4 O7 .10H2 O), kernite (Na2 B4 O7 .4H2 O), colemanite (Ca2 B6 O11 .5H2 O), ulexite (NaCaB5 O9 .8H2 O), hydroboracite (CaMgB6 O11 .6H2 O), boracite (Mg3 B7 O13 Cl), pandermite (Ca4 B10 O19 .7H2 O) and szaibelyite (ascharite) (Mg2 B2 O5 .H2 O) [3,4]. Today, borax is the most important mineral for the borate industry. Most commercial borate deposits in the world are exploited by opencast mining. Boron is obtained from the brine from Searles Lake (USA) and Chinese sources via controlled evaporation or carbonation [6,7]

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