University of Cambridge > Talks.cam > G.K. Batchelor Laboratory lunchtime seminar > Settling of Solid Precipitates in Water

Settling of Solid Precipitates in Water

Add to your list(s) Download to your calendar using vCal

If you have a question about this talk, please contact .

Over 2 billion years ago banded iron formations (BIF) developed as a consequence of aqueous iron (FeII) precipitating due, in part, to the new presence of oxygen in the Archaen ocean. The outstanding question is how long did it take for the precipitates to rain out of the ocean column, setting onto the ocean floor to form BIF ? We examine an idealisation of this circumstance by performing laboratory experiments in which a solution of ferrous chloride (FeCl2) is combined with a solution of sodium hydroxide (NaOH). If the limiting concentration of one of these two solutions is small, tiny precipitates of “rust” (Fe(OH)3) form, which slowly settle. At larger concentrations, however, the precipitates accumulate into progressively larger flocs that initially settle rapidly, but then form convective flow patterns. Understanding these dynamics is a work in progress.

This talk is part of the G.K. Batchelor Laboratory lunchtime seminar series.

Tell a friend about this talk:

This talk is included in these lists:

Note that ex-directory lists are not shown.

 

© 2006-2024 Talks.cam, University of Cambridge. Contact Us | Help and Documentation | Privacy and Publicity