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Sorption of nalidixic acid onto sediments under batch and dynamic flow conditions

Abstract : The sorption of nalidixic acid (NA) onto artificial sediments composed of Fe-oxides, Al-oxides, clay and quartz sand was studied under both static batch and dynamic flow conditions. Kinetic and equilibrium sorption experiments showed that the presence of clay increased the sorption capacity of synthetic sediment and that bentonite had the highest sorption coefficient compared to kaolinite. Solute reactive transport experiments showed that the breakthrough point and steepness of the breakthrough curve (BTC) were dependent on both clay type and water velocity. Agreement between batch and column results in terms of sorbed amount and retardation factor was poor regardless of the sediment tested. The presence of even a small amount of clay (3%) can decrease the permeability of the mixed bed and lead to the formation of preferential flow paths in the column system. Different sets of column experiments at various flow rates gave rise to different sorbed amounts at complete breakthrough, leading to chemical nonequilibrium in the flow system. However, this kinetic limitation cannot completely explain the breakthrough behavior of NA in the bentonite column, suggesting that other factors are responsible for this disparity. The presence of immobile water regions was unlikely in the column since more than 90% of the pore water was mobile according to the tracer tests. The inaccessibility of reactive sites and limited physical diffusion in the clay-packed column may play a significant role under flow-through conditions. The reactive transport behavior of NA is therefore strongly dependent on the mineralogy of the clay present in sediments.
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https://hal-univ-rennes1.archives-ouvertes.fr/hal-00912787
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Submitted on : Monday, December 2, 2013 - 4:15:54 PM
Last modification on : Friday, July 10, 2020 - 4:07:00 PM

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E. Clervil, M. Usman, E. Emmanuel, V. Chatain, Khalil Hanna. Sorption of nalidixic acid onto sediments under batch and dynamic flow conditions. Chemical Geology, Elsevier, 2012, 335, pp.63-74. ⟨10.1016/j.chemgeo.2012.10.041⟩. ⟨hal-00912787⟩

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