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Dispersion of silica-encapsulated DNA magnetic particles in a homogeneous sand tank.
Chakraborty, Swagatam; Elhaj, Rayan; Foppen, Jan Willem; Schijven, Jack F.
Afiliación
  • Chakraborty S; Environmental Hydrogeology Group, Department of Earth Sciences, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands. Electronic address: s.chakraborty@uu.nl.
  • Elhaj R; Department of Water Sciences and Engineering, IHE-Delft, Institution for Water Education, Westvest 7, 2611 AX Delft, the Netherlands.
  • Foppen JW; Department of Water Sciences and Engineering, IHE-Delft, Institution for Water Education, Westvest 7, 2611 AX Delft, the Netherlands; Water Resource Section, Department of Civil Engineering and Geoscience, Delft University of Technology, Delft, the Netherlands.
  • Schijven JF; Environmental Hydrogeology Group, Department of Earth Sciences, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands; Department of Statistics, Informatics and Modelling, National Institute of Public Health and the Environment, P.O. Box 1, 3720 BA Bilthoven, the Netherlands.
J Contam Hydrol ; 266: 104410, 2024 Sep.
Article en En | MEDLINE | ID: mdl-39067353
ABSTRACT
In this study, we focused on the 3D dispersion of colloids. To our knowledge, we were the first to do so. Thereto, we injected silica encapsulated DNA tagged superparamagnetic particles (SiDNAmag) in a homogeneous coarse grain sand tank. At four downstream locations, SiDNAmag concentrations were determined as a function of time. Longitudinal and transverse dispersivity values and associated uncertainties of SiDNAmag were determined using Monte Carlo modelling approach. The parameter associated uncertainties of hydraulic conductivity as well as of the effective porosity estimated from SiDNAmag breakthrough curves were statistically similar to those estimated from salt tracer breakthrough curves. Further, the SiDNAmag dispersivity uncertainty ranges were then statistically compared with the salt tracer (NaCl, and fluorescein) dispersivities. Our results indicated that time to rise, time of peak concentration and shape of the breakthrough curves of SiDNAmag were similar to those of the salt tracer breakthrough curves. Despite the size difference between the salt tracer molecules and SiDNAmag, size exclusion did not occur, probably due to the large pore throat diameter to SiDNAmag diameter ratio. The median longitudinal dispersivity (αL) of salt tracer and SiDNAmag were 4.9 and 5.8 × 10-4 m, respectively. The median ratio of horizontal and vertical transverse dispersivities to αL, (αTH /αL and αTV /αL, respectively), for salt tracer and SiDNAmag ranged between 0.52 and 0.56. Through the statistical tests, we concluded that the longitudinal and traverse dispersivities of SiDNAmag were not statistically significantly different from salt tracer in 3 dimensions and could be used to characterize the dispersive properties of the medium we used. Our work contributes to a better understanding of 3D dispersion of SiDNAmag in saturated porous media.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: ADN / Dióxido de Silicio / Arena Idioma: En Revista: J Contam Hydrol Asunto de la revista: TOXICOLOGIA Año: 2024 Tipo del documento: Article Pais de publicación: Países Bajos

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: ADN / Dióxido de Silicio / Arena Idioma: En Revista: J Contam Hydrol Asunto de la revista: TOXICOLOGIA Año: 2024 Tipo del documento: Article Pais de publicación: Países Bajos