2004
DOI: 10.1144/1470-9236/04-039
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Pitfalls in the geological characterization of alluvial deposits: site investigation for reactive barrier installation at Aznalcóllar, Spain

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Cited by 11 publications
(16 citation statements)
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“…The estimated groundwater flow is high (0.5-1 m/d), representing a notable distinct characteristic compared to other AMD-contaminated groundwaters treated by PRB. The average hydraulic gradient was found fairly flat (0.1%), which is expected of highly permeable media [16,19,20]. The values of such hydrodynamical parameters are fairly variable due to seasonal fluctuations and the complexity and heterogeneity of the geologic setting.…”
Section: Site Characterisationmentioning
confidence: 84%
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“…The estimated groundwater flow is high (0.5-1 m/d), representing a notable distinct characteristic compared to other AMD-contaminated groundwaters treated by PRB. The average hydraulic gradient was found fairly flat (0.1%), which is expected of highly permeable media [16,19,20]. The values of such hydrodynamical parameters are fairly variable due to seasonal fluctuations and the complexity and heterogeneity of the geologic setting.…”
Section: Site Characterisationmentioning
confidence: 84%
“…The site investigation carried out for the location and orientation of the PRB, as well as its installation, has been reported in detail previously [20]. Surface mapping and geophysical exploration, boreholes drilling, trenching, vertical electrical sounding, hydraulic testing and water sampling provided data converging on a simple geological model based on three terraces that gave rise to the final design and installation of the PRB.…”
Section: Construction Of the Prbmentioning
confidence: 98%
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“…The system was divided into several parts with different proportions of filling material (calcite, organic compost, and iron cuttings). Further detail relating its operation can be obtained from Bolzicco et al (2004) and Salvany et al (2004).…”
Section: Remediation Measuresmentioning
confidence: 99%
“…Finally, overlaying all of them, the Guadiamar River alluvial deposits, formed by four terrace levels constituted mainly of pebbles, gravels, and sands (Salvany et al 2004).…”
Section: Hydrogeological Frameworkmentioning
confidence: 99%