Skip to Main Content
Skip Nav Destination

Mineral dissolution, the primary mechanism of release of inorganic species/nutrients to the Earth’s surface, can be influenced by heterotrophic microbial activity. Heterotrophic (also known as organotrophic) bacteria may affect mineral dissolution directly or indirectly via a number of mechanisms, which can be grouped in two main categories: (1) dissolution from bacterially-formed organic and/or inorganic products; and (2) chelation or uptake by cells, either in suspension or attached to mineral surfaces. In this chapter, the principles of mineral dissolution and of heterotrophic biology in relation to dissolution are discussed. A review of recent evidence of the role of heterotrophic bacteria in mineral dissolution, with particular emphasis on the mechanisms involved, is presented.

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Close Modal

or Create an Account

Close Modal
Close Modal