Abstract

Selenium is an essential bio-element, but because of its bioaccumulation potential, it can become toxic and is an important pollutant. The ubiquitous mineral calcite (CaCO3) has the ability to immobilize anions as SeO32− by different sorption or coprecipitation processes. Experimental studies have found that SeO32− can incorporate in the crystal structure of calcite by substituting CO32−. The presence of foreign ions in aqueous solution strongly affects CaCO3 precipitation, helping stabilize less stable polymorphs such as vaterite and aragonite or hydrated phases. In this work, we studied the aging process of calcium carbonates precipitated from aqueous solutions highly supersaturated with respect to CaCO3 and slightly supersaturated with respect to CaSeO3·H2O under ambient conditions, for times up to 30 days in which solids were kept in the remaining aqueous solution. Under these conditions, CaCO3 precipitated mainly as low crystallinity vaterite aggregates that hosted up to 16% atomic ratio Se:C. Vaterite purified and increased its crystallinity with aging time, but the vaterite–calcite transformation was strongly inhibited. The incorporation of Se(IV) in vaterite did not significantly affect the cell parameters or the external morphology of the aggregates. The precipitation of selenite as CaSeO3·H2O was conditioned by the availability of free Ca2+ and SeO32− that was not previously incorporated into precipitated carbonates.

Highlights

  • Selenium is a trace element, but it is widely spread on the Earth’s surface

  • This work aims to advance knowledge in this regard, following a protocol similar to that used in previous works [27], which basically consists of monitoring in the laboratory the aging of precipitated calcium carbonate in the presence of foreign ions in the aqueous solution left over from precipitation

  • The presence of dissolved Se(IV) plays an important role in the precipitation of calcium carbonate from aqueous solution at room temperature. It has a great influence on the composition of the precipitated phases and especially on the crystallization sequence of the different CaCO3 polymorphs

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Summary

Introduction

Selenium is a trace element, but it is widely spread on the Earth’s surface. Its distribution is very heterogeneous, it has been estimated that, on average, the lithosphere contains about 0.05 ppm of Se. Some extremely polluted soils in USA, Ireland, and India reach 100 mg of selenium per kg, but concentrations over 0.1 mg per kg are uncommon [1,2,3]. High concentration of selenium is associated with mining, ore treatment, or industrial activities [4]. Selenium is used as a pigment in the glass industry and is of interest in electronics because of its photo-electronic and semiconducting properties. As Se is an essential element for human beings, it is commercialized as a nutritional supplement and is used as a soil fertilizer and in the cosmetics industry [5]

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