Application of seismic refraction methods in groundwater modeling studies in New England (USA)

F.P. Haeni

doi:10.1190/1.1442083

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Application of seismic refraction methods in groundwater modeling studies in New England (USA)

F.P. Haeni

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Abstract

Seismic refraction studies were conducted over unconfined glacial aquifers in New England to determine: 1) depth of the underlying bedrock; 2) depth of the water table; 3) saturated thickness of the aquifer in areas not accessible to heavy drilling equipment; 4) areas where thick, unsaturated sediments overlie thickly saturated parts of the aquifer; and 5) locations of test holes and type of drilling equipment needed. These data were used in groundwater models and provided parameter values that required few adjustments during calibration. -from Author

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Geophysics Article

Source-reported bounding extent: 37.16031654673677° to 47.57652571374621° latitude; -81.9140625° to -66.5771484375° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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F.P. Haeni. 1986. Application of seismic refraction methods in groundwater modeling studies in New England (USA). https://doi.org/10.1190/1.1442083

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