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Tidal influences on the saline interface of a shallow unconfined aquifer have been investigated by using both dc resistivity traversing and cross-borehole resistivity tomography (CRT). Variations in bulk resistivity structure obtained through resistivity traversing provide a clear general picture of the structure of the saline interface and its mixing zone. On all three resistivity traverses there...
Direct current resistivity traversing has been used to characterise the nature of the saline interface at Te Horo on the Kapiti Coast in New Zealand. The results show that the interface in the vicinity of the settlement, which relies on bores for potable water, has intruded inland 10m further than in undeveloped areas. Resistivity traversing has been particularly successful in defining subsurface...
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