Hydrozincite seasonal precipitation at Naracauli (Sardinia – Italy): Hydrochemical factors and morphological features of the biomineralization process

• Published in: Applied geochemistry 2012-09, Vol.27 (9), p.1814-1820
• Main Authors: Medas, D., Cidu, R., Lattanzi, P., Podda, F., Wanty, R.B., De Giudici, G.
• Format: Article
• Language: English
• Subjects: chemical precipitation; Chlorella; Cyanobacteria; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; environmental factors; Exact sciences and technology; microalgae; microbial communities; Mineralogy; mining; Non silicates; pollution; Pollution, environment geology; remediation; Scytonema; seasonal variation; spring; streams; summer; water flow; zinc
• ISSN: 0883-2927; 1872-9134
• DOI: 10.1016/j.apgeochem.2012.02.016

Hydrozincite [Zn5(CO3)2(OH)6] precipitation from Naracauli waters (SW Sardinia) is, among other things, promoted by a microbial community made up of a filamentous cyanobacterium (Scytonema sp.) and a microalgae (Chlorella sp.). Hydrozincite bioprecipitation is responsible for the natural removal of harmful metals, especially Zn, from the stream waters. Thus, hydrozincite could be used to attenuate metal pollution in mining waters. Information on environmental conditions which promote the biomineralization process is fundamental for the development of remediation strategies. This paper aims to investigate the variables controlling the biomineralization process, and seasonal variation of the hydrochemical factors that affect hydrozincite precipitation. Hydrozincite morphology varies depending on the environmental conditions. Specifically, changes were observed between samples collected in late spring and samples collected in summer, and among samples precipitated under different water flow conditions. According to field observations, correlated with speciation and equilibrium calculation, the maximum intensity in hydrozincite precipitation occurs in the late spring during rainy years. In these conditions, the hydraulic regime in the stream reaches stationary conditions, and saturation index values with respect to hydrozincite reach their highest values. Concomitantly, the Zn2+/CO32- molar ratio reaches values close to 1, indicating that kinetic processes have a role on the hydrozincite biomineralization process.