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Composition , wt % liquid phase solid residue Equilibrium solid phase MgSO4 FeSO4 H20 FeSO4 0 23.44 77.16 FeSO4.7H2O 2.01 20.30 77.69 0.81 48.41 n1 4.46 18.16 77.38 3.30 27.62 6.13 16.00 77.87 4.80 29.57 9.13 15.55 75.32 6.58 29.07 ...
Composition , wt % liquid phase solid residue Equilibrium solid phase MgSO4 FeSO4 H20 FeSO4 0 23.44 77.16 FeSO4.7H2O 2.01 20.30 77.69 0.81 48.41 n1 4.46 18.16 77.38 3.30 27.62 6.13 16.00 77.87 4.80 29.57 9.13 15.55 75.32 6.58 29.07 ...
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Fig . 2. MgSO4 - Fe2 ( SO4 ) 3 - H20 system at 25 ° C . A = MgSO4.7H20 , B = Fe2 ( SO4 ) 3-9H20 , E = eutonic point . Schreinemakers rays imply variable composition of the solids , i.e. , the occurrence of solid solutions .
Fig . 2. MgSO4 - Fe2 ( SO4 ) 3 - H20 system at 25 ° C . A = MgSO4.7H20 , B = Fe2 ( SO4 ) 3-9H20 , E = eutonic point . Schreinemakers rays imply variable composition of the solids , i.e. , the occurrence of solid solutions .
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A. Velikodnyi Institute of Solid - State Chemistry , Ural Division , Russian Academy of Sciences , Yekaterinburg , Russia Received July 12 , 1995 Abstract - Interactions in ternary systems , containing oxides of vanadium , manganese ...
A. Velikodnyi Institute of Solid - State Chemistry , Ural Division , Russian Academy of Sciences , Yekaterinburg , Russia Received July 12 , 1995 Abstract - Interactions in ternary systems , containing oxides of vanadium , manganese ...
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