Zobrazeno 1 - 3
of 3
pro vyhledávání: '"David W. Finneran"'
Publikováno v:
Aquatic Geochemistry. 17:567-582
The accurate and precise measurement of total sulfide has been of major interest for well over a century. The most commonly used method involves the formation of a methylene blue–sulfide complex and spectrophotometric measurement of its concentrati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::998624070d05a9a6b6488a9203d9d518
https://doi.org/10.1007/s10498-011-9128-1
https://doi.org/10.1007/s10498-011-9128-1
Autor:
John W. Morse, David W. Finneran
Publikováno v:
Chemical Geology. 268:137-146
The effect of ionic strength (I), pCO2, and temperature on the dissolution rate of calcite was investigated in magnesium-free, phosphate-free, low calcium (mCa2+ ≈ 0.01 m) simple KCl and NaCl solutions over the undersaturation range of 0.4 ≤ Ωca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e427d7ab45292356f7c88e89fe5a47f
https://doi.org/10.1016/j.chemgeo.2009.08.006
https://doi.org/10.1016/j.chemgeo.2009.08.006
Publikováno v:
Aquatic Geochemistry. 13:143-156
The primary factors that control the concentration of total reduced (inorganic) sulfide in coastal sediments are believed to be the availability of reactive iron, dissolved sulfate and metabolizable organic carbon. We selected nine sites in shallow (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::204cfc243215c8ad6a893937cbfaef42
https://doi.org/10.1007/s10498-007-9012-1
https://doi.org/10.1007/s10498-007-9012-1