The Quarterly journal of the Geological Society of London . Diagrams shewing the variations in density of brine flowing through a block of Bath Weatherstone under various pressures. >^=f=^ Number of experiments. cleared of all the salt in the solution; but later, on using a weakerbrine, I found that the effluent was a much stronger brine than theinflowing solution, deriving its salt from the pores of the experienced considerable difficulty in removing the salt from thepores, hot water and long-continued soaking failing to eliminate 94 MB. W. E. BALDWIN-WISEMAX OX [Feb. 1907. all trac
The Quarterly journal of the Geological Society of London . Diagrams shewing the variations in density of brine flowing through a block of Bath Weatherstone under various pressures. >^=f=^ Number of experiments. cleared of all the salt in the solution; but later, on using a weakerbrine, I found that the effluent was a much stronger brine than theinflowing solution, deriving its salt from the pores of the experienced considerable difficulty in removing the salt from thepores, hot water and long-continued soaking failing to eliminate 94 MB. W. E. BALDWIN-WISEMAX OX [Feb. 1907. all traces of the salt long after the experiments had terminated:and the whole test was an excellent object-lesson of what may beexpected when a water-bearing rock is overpumped in the vicinity ofthe sea—an experience which has been realized in more than oneseaside resort deriving its water-supply from sub-surface , for the reason that the temperature of a solution and thenature of the salt affect so radically the rate of flow, it seems to this point has not previously received the attention thatit deserves, to be most essential that the temperature and densityof any underground stream sho
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
