Sediments Quality Assessment of Jacarepaguá Lagoon: The Venue of the 2011 Rock in Rio

• Published in: Clean : soil, air, water air, water, 2012-09, Vol.40 (9), p.906-910
• Main Authors: Araruna Júnior, José Tavares, Benedetti, Paula Elias, Pires, Patrício José Moreira, de Almeida, Ricardo Froitzheim Rinelli
• Format: Article
• Language: English
• Subjects: 2012 Rock in Rio; Jacarepaguá Lagoon; Quality assessment; Sediments
• ISSN: 1863-0650; 1863-0669
• DOI: 10.1002/clen.201100667

In order to aid in the efforts of the 2016 Olympic Games, the organizers of 2011 Rock in Rio decided to build a permanent venue next to the Olympic Park. The area is problematic from the geotechnical point of view since it presents soils with low shear strength, low permeability, and high plasticity, so major soil improvement works were carried out. Bored soil–cement columns were placed to increase soil shear strength and reduce compressibility. A meter thick fill composed of gneiss residual soil was placed and trenches were digged to drain rainwater. However, earlier studies conducted on Jacarepaguá Lagoon have detected the presence of heavy metals in these sediments. In this study, an environmental survey on the Jacarepaguá Lagoon sediments took place in order to choose a place where its sediments could be dredged to be later used in the drainage facilities. The results indicated areas where the threshold level 1 (low probability of adverse effects) issued by the general procedures for sediments quality assessments for dredging purposes, Resolution no 344 of the Brazilian Federal Government, was surpassed. Levels above the limits established for cadmium (Cd), lead (Pb), copper (Cu), nickel (Ni), and zinc (Zn) were detected. Based on this consideration the State Environmental Agency issued a permit allowing the organizers of 2011 Rock in Rio to dredge an area close to City of Rock in order to obtain coarse sediments for the drainage facilities. In addition, it was found that those sediments were ideal for this application since their hydraulic conductivity is on the order of 10−2 cm/s. The coarse sediments that present low probability of adverse effects are found in the area delineated by the red circle in Figure 5. This area is very close to the City of Rock and there is no need to transport the sediments and, in addition, it was found that those sediments were ideal for drainage facilities because their hydraulic conductivity is on the order of 10−2 cm/s.