Particle tracer transport in a sloping soil lysimeter under periodic, steady state conditions

JOURNAL OF HYDROLOGY

卷:569

Article

Wang, Chaozi^1,2  McNew, Coy P.²  Lyon, Steve W.³  Walter, M. Todd⁴  Volkman, Till H. M.⁵  Abramson, Nathan⁵  Sengupta, Aditi⁵  Wang, Yadi⁵  Meira Neto, Antonio Alves⁵  Pangle, Luke⁶  Troch, Peter A.^5,7  Kim, Minseok⁸  Harman, Ciaran⁸  Dahlke, Helen E.² 

[1] China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100083, Peoples R China

[2] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA

[3] Stockholm Univ, Dept Phys Geog, SE-10691 Stockholm, Sweden

[4] Cornell Univ, Dept Biol & Environm Engn, Ithaca, NY 14853 USA

[5] Univ Arizona, Biosphere2, Landscape Evolut Observ, Oracle, AZ 85739 USA

[6] Georgia State Univ, Dept Geosci, Atlanta, GA 30303 USA

[7] Univ Arizona, Dept Hydrol & Water Resources, Tucson, AZ 85721 USA

[8] Johns Hopkins Univ, Dept Geog & Environm Engn, Baltimore, MD 21218 USA

关键词: Colloid;    Transport;    Vadose zone;    Tracer;    Transient;    Unsaturated;   

DOI  :  10.1016/j.jhydrol.2018.11.050

来源: Elsevier

【 摘 要 】

Colloid transport through complex and dynamic (i.e. non-steady-state) hydrologic systems is rarely studied, owing to the difficulty of constraining initial and boundary conditions and quantifying colloid-porous media and colloid-colloid interactions in transient flow systems. Here we present a particle tracer experiment conducted on a sloped lysimeter receiving periodic rainfall events for 10 days. Four unique, DNA-labelled particle tracers were injected both in sequence and in parallel, together with a conservative tracer (deuterium), over the course of the first day and allowed to move through the system. Discharge-particle tracer concentration curves and the spatial distribution of particle tracer mass retained in the soil at the end of the experiment were found to be highly dependent on the timing of the tracer injection and the precipitation input and subsequent dynamic response of the water table. Overall, neglecting the total DLT recovery rate, the DLT particle tracer breakthrough trend (DNA-labelled particle tracer 4) was similar to deuterium and decreased over time with the exception of a few peaks later in the experiment. The individual particle tracer breakthrough curves suggest a complex system with different fast transport mechanisms (e.g. capillary barrier and size exclusion effect) and slow retention-release mechanisms (e.g. straining, physical-chemical adsorption), which resulted in particle tracers transferring faster than deuterium in the first 10 h of the experiment but being exceeded by deuterium soon after deuterium started to break through. The experiment not only highlights the interaction of repeated colloidal pollution events in hydrologic systems with different pre-event saturation conditions, but also the benefits of using multiple synchronous or sequential tracer applications to dissect explicit formulations of water flow and colloid transport processes in complex and dynamic hydrological systems. Such explicit process formulations could help improve understanding hydrologically-controlled transport through catchments and the quantitative prediction of these processes with water quality models.

【 授权许可】

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