Chemical equilibria and zoning of subsurface water from Jáchymov ore deposit, Czechoslovakia

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

2

Scientific paper

Water samples from the surface and from different levels of the Svornost mine (Jáchymov, Czechoslovakia) were analyzed and Eh and pH were measured in the field. The saturation indices ( I = log ( Q / K ) = F /2.303 RT ) of water- P CO 2 in normal earth's atmosphere, water-calcite, water-Fe(OH) 3 and water-pyrite are given. The P H 2 in water characterizes individual redox zones of water body which are consistent with the secondary zones of sulfide ore deposits. Complexing among the major ions of water and temperature changes were considered in the calculations. Space dependence of individual physico-chemical characteristics of water is discussed in detail.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Chemical equilibria and zoning of subsurface water from Jáchymov ore deposit, Czechoslovakia does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Chemical equilibria and zoning of subsurface water from Jáchymov ore deposit, Czechoslovakia, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Chemical equilibria and zoning of subsurface water from Jáchymov ore deposit, Czechoslovakia will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1390057

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.