Abstract
Red mud, which is a solid waste produced in the alumina production process, is classified as dangerous due to its high pH. In this work, the concentration of chlorides was monitored by measuring the conductivity of the anolyte, which initially was distilled water. The steady and nonsteady-state chloride diffusion coefficients were estimated from the "time lag"� and "equivalent time" between diffusion and migration experiments. The capillary water absorption, apparent porosity and pore size distribution of concretes were also analyzed. The addition of red mud apparently ensured lower chloride diffusion in the tested mixtures due to its superfine particle-size distribution and its "filler"� effect. Red mud lengthened the service life of the concrete to 35 years (double that of the reference concrete). This finding is very positive since it indicates a delay in the onset of the rebar corrosion process caused by the migration of chloride ions.
Highlights
The huge volumes of industrial waste produced today represent one of the world’s greatest environmental problems
Red mud is the main waste generated in the production of aluminium and alumina by the Bayer process from bauxite ore
The red mud was received in the form of a paste containing about 40% free water
Summary
The huge volumes of industrial waste produced today represent one of the world’s greatest environmental problems. The Brazilian NBR 10004/2004 technical standard classifies red mud as dangerous, and the worldwide production of red mud exceeds 117 million tons/year. These vast quantities of wastes call for the search for widely consumed target products into which they can be incorporated, and motivated this study of the influence of added red mud on the characteristics of cement mortars and concrete. Red mud is the main waste generated in the production of aluminium and alumina by the Bayer process from bauxite ore. Ranking third in worldwide production in 2009, Brazil produced 26.6 million tons of bauxite It has the world’s third largest bauxite ore reserves (around 3.5 billion tons), concentrated mainly in the northern part of the country (State of Pará)[2]
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