Resistivity (DC) method applied to aouifer protection studies

• Autor(a) principal: Braga, Antonio Celso de Oliveira [UNESP]
• Data de Publicação: 2006
• Outros Autores: Malagutti Filho, Walter [UNESP], Dourado, João C. [UNESP]
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: Repositório Institucional da UNESP
• Texto Completo: http://dx.doi.org/10.1590/S0102-261X2006000400010; http://hdl.handle.net/11449/69130
• topic: Aquifer protection; Dar zarrouk parameters; Resistivity; aquifer; clay soil; electrical conductivity; electrical resistivity; groundwater pollution; hydrogeology; sandy soil; transmissivity; vertical electrical sounding; Brazil; Canoas; Rio Grande do Sul; South America

Resistivity (DC) method using vertical electrical soundings (Schlumberger array) are conducted In the vicinity of Canoas/RS, applied to environmental studies with the objective of Investigating groundwater conditions, The present paper shows a geoelectrlcal Identification of the lithology and an estimate of the relationship between the resistivity and Dar Zarrouk parameters (transverse unit resistance and longitudinal unit conductance) with the properties such as aquifer transmlssivlty and protection of ground water resources, In the saturated sediments, resistivity values defined the following sequence: clay layers (resistivity < 40 ohm-m) and sand layers (resistivity > 40 ohm-m), Two sand layers were identified; one corresponding to the unconfined aquifer and another to the confined aquifer between two clay layers, In the map of the transverse unit resistance of the unconfined aquifer, the tendencies of high values can be associated with the zones of high transmissivity; hence, these zones are suggested for the installation of monitoring wells, The map of longitudinal conductance Illustrates the Impermeability of the confining clay layer, Values of S > 1.0 siemens would indicate zones in which the confined aquifer would be protected; In comparison, values of S < 1.0 siemens would indicate zones of probable risks of contamination. © 2006 Sociedade Brasileira de Geofísica.