Cation Effect on the Water Activity of Ternary (S)-Aminobutanedioic Acid Magnesium Salt Solutions at 298.15 and 310.15 K

2016 ◽  
Vol 61 (9) ◽  
pp. 3190-3199 ◽  
Author(s):  
Christoph Held ◽  
Elena N. Tsurko ◽  
Roland Neueder ◽  
Gabriele Sadowski ◽  
Werner Kunz
1992 ◽  
Vol 30 (1-3) ◽  
pp. 499-513 ◽  
Author(s):  
N. Nagamori ◽  
A.J. Plumpton ◽  
J.-J. Panneton

Clay Minerals ◽  
1982 ◽  
Vol 17 (4) ◽  
pp. 463-469 ◽  
Author(s):  
J. Torrent ◽  
R. Guzman

AbstractFerrihydrite transformed to crystalline Fe(III)-oxides in salt solutions but the degree of transformation generally decreased with increasing concentration (decreasing water activity) and haematite was favoured over goethite. More transformation occurred for chloride than for nitrate or sulphate and more for calcium than for magnesium or sodium. Calcium and magnesium favoured haematite over goethite. The results support the hypothesis that haematite not only can be formed but will be favoured over goethite in natural environments with low water activity, for instance dry or saline soils or sediments. The ionic environment modifies the general water activity effect.


1987 ◽  
Vol 52 (4) ◽  
pp. 1118-1119 ◽  
Author(s):  
MARÍA L. POLLIO ◽  
DORA KITIC ◽  
GUILLERMO J. FAVETTO ◽  
JORGE CHIRIFE

1986 ◽  
Vol 51 (4) ◽  
pp. 1037-1041 ◽  
Author(s):  
DORA KITIC ◽  
DENISE C. PEREIRA JARDIM ◽  
GUILLERMO J. FAVETTO ◽  
SILVIA L. RESNIK ◽  
JORGE CHIRIFE

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