Dispersion of silica-encapsulated DNA magnetic particles in a homogeneous sand tank

IF 3.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Swagatam Chakraborty , Rayan Elhaj , Jan Willem Foppen , Jack F. Schijven
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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, (αTHL and αTVL, 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.

硅胶包裹的 DNA 磁性颗粒在均质砂罐中的分散。
在这项研究中,我们的重点是胶体的三维分散。据我们所知,我们是第一个这样做的人。为此,我们在一个均质粗粒砂罐中注入了硅胶封装的 DNA 标记超顺磁性颗粒(SiDNAmag)。在四个下游位置,测定了 SiDNAmag 浓度与时间的函数关系。使用蒙特卡洛建模方法确定了 SiDNAmag 的纵向和横向分散值及相关不确定性。根据 SiDNAmag 突破曲线估算出的水力传导率和有效孔隙度的相关参数不确定性,与根据盐示踪剂突破曲线估算出的参数不确定性在统计上相似。此外,我们还将 SiDNAmag 分散性的不确定性范围与盐示踪剂(氯化钠和荧光素)的分散性进行了统计比较。结果表明,SiDNAmag 的上升时间、峰值浓度时间和突破曲线形状与盐示踪剂突破曲线相似。尽管盐示踪剂分子与 SiDNAmag 之间存在尺寸差异,但可能由于孔喉直径与 SiDNAmag 直径之比较大,因此没有发生尺寸排斥。盐示踪剂和 SiDNAmag 的纵向分散度中值(αL)分别为 4.9 和 5.8 × 10-4 m。盐示踪剂和 SiDNAmag 的水平和垂直横向扩散率与αL 的比值中位数(分别为 αTH /αL 和 αTV /αL)介于 0.52 和 0.56 之间。通过统计检验,我们得出结论:在三维空间中,SiDNAmag 的纵向分散度和横向分散度与盐示踪剂没有显著的统计差异,可用于描述我们所使用介质的分散特性。我们的工作有助于更好地理解 SiDNAmag 在饱和多孔介质中的三维分散。
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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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