Effect of concentration of silica encapsulated ds-DNA colloidal microparticles on their transport through saturated porous media

Journal Article (2022)
Author(s)

Swagatam Chakraborty (Universiteit Utrecht)

J.W.A. Foppen (IHE Delft Institute for Water Education, TU Delft - Water Resources)

Jack Schijven (Rijksinstituut voor Volksgezondheid en Milieu (RIVM), Universiteit Utrecht)

Research Group
Water Resources
Copyright
© 2022 S. Chakraborty, J.W.A. Foppen, Jack F. Schijven
DOI related publication
https://doi.org/10.1016/j.colsurfa.2022.129625
More Info
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Publication Year
2022
Language
English
Copyright
© 2022 S. Chakraborty, J.W.A. Foppen, Jack F. Schijven
Research Group
Water Resources
Volume number
651
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Abstract

We investigated the transport and retention kinetics of silica encapsulated – silica core double stranded DNA particles (SiDNASi) through 15cm saturated quartz sand columns as a function of a wide range of colloid injection concentrations (C0 = 8.7×102 - 6.6×108 particles ml-1). The breakthrough curves (BTCs) exhibited an overall 2-log increase of maximum relative effluent concentration with increasing C0. Inverse curve fitting, using HYDRUS1D, demonstrated that a 1-site first order kinetic attachment (katt) and detachment (kdet) model sufficed to explain the C0-dependent SiDNASi retention behaviour. With increasing C0, katt log-linearly decreased, which could be expressed as an overall decrease in the single-collector removal efficiency (ƞ). The decrease in ƞ was likely due to increased electrostatic repulsion between aqueous phase- solid phase colloids, formation of shadow zones downstream of deposited colloids and removal of weakly attached colloids from the solid phase (quartz sand) attributing to increased aqueous phase-solid phase intercolloidal collisions as a function of increasing SiDNASi concentration. Our results implied, firstly, that the aqueous phase colloid concentration should be carefully considered in determining colloidal retention behaviour in saturated porous media. Secondly, colloidal transport and retention dynamics in column studies should not be compared without considering colloid influent concentration. Thirdly, our results implied that the applicability of SiDNASi as a conservative subsurface tracer was restricted, since transport distance and retention was colloid concentration dependent. However, the uniqueness of the DNA sequences in SiDNASi imparts the advantage of concurrent use of multiple SiDNASi for flow tracking or porous media characterization.