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Sebkhat El Melah brine deposit

As a test of our ability to calculate activity coefficients in natural brines, we consider groundwater from the Sebkhat El Melah brine deposit near Zarzis, Tunisia (Perthuisot, 1980). The deposit occurs in a buried evaporite basin composed of halite (NaCl), anhydrite (CaSC>4), and dolomite [CaMg(CC>3)2]. The Tunisian government would like to exploit the brines for their chemical content, especially for the potassium, which is needed to make fertilizer. [Pg.133]

Table 8.8. Chemical compositions (g l x) of brines from the Sebkhat El Melah brine deposit, Zarzis, Tunisia (Jarraya and El Mansar, 1987)... Table 8.8. Chemical compositions (g l x) of brines from the Sebkhat El Melah brine deposit, Zarzis, Tunisia (Jarraya and El Mansar, 1987)...
See other pages where Sebkhat El Melah brine deposit is mentioned: [Pg.133]    [Pg.133]    [Pg.135]    [Pg.125]   
See also in sourсe #XX -- [ Pg.133 ]

See also in sourсe #XX -- [ Pg.125 , Pg.126 ]



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