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  • Two historical premises of the hydro-equilibrium model as applied to the Dundas Tableland are challenged : firstly, that dryland salinity is secondary, or induced by European settlement; and, secondly, that reasons for significant evapotranspirative
  • The groundwater recharge-discharge model, or hydro-equilibrium model, has driven Victoria dryland salinity research for the last 30 years. This paper challenges its application to the Dundas Tableland, south-western Victoria, on historical grounds