Abstract
A regular monthly inventory of water-level height and water quality of about 100 wells along the coast from Visakhapatnam to Bhimilipatnam was made for a 13-month period during 1974–1975. The electrical conductivity of the waters is found to vary with seasonal water-level fluctuations. It is, however, observed that this variation has two different patterns. The first pattern is that when the water level lowers the electrical conductivity decreases, and the second pattern is that when the water level lowers the electrical conductivity increases. The geological environment is the same for both cases, but the two patterns result from water-table fluctuations in two different hydrogeological zones.
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