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Hillslope permeability architecture controls on subsurface transit time distribution and flow paths
Uppsala University, Sweden.ORCID-id: 0000-0003-2662-9264
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2016 (Engelska)Ingår i: Journal of Hydrology, ISSN 0022-1694, E-ISSN 1879-2707, Vol. 543, s. 17-30Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Defining the catchment transit time distribution remains a challenge. Here, we used a new semi-analytical physically-based integrated subsurface flow and advective–dispersive particle movement model to assess the subsurface controls on subsurface water flow paths and transit time distributions. First, we tested the efficacy of the new model for simulation of the observed groundwater dynamics at the well-studied S-transect hillslope (Västrabäcken sub-catchment, Sweden). This system, like many others, is characterized by exponential decline in saturated hydraulic conductivity and porosity with soil depth. The model performed well relative to a tracer-based estimate of transit time distribution as well as observed groundwater depth–discharge relationship within 30 m of the stream. Second, we used the model to assess the effect of changes in the subsurface permeability architecture on flow pathlines and transit time distribution in a set of virtual experiments. Vertical patterns of saturated hydraulic conductivity and porosity with soil depth significantly influenced hillslope transit time distribution. Increasing infiltration rates significantly decreased mean groundwater age, but not the distribution of transit times relative to mean groundwater age. The location of hillslope hydrologic boundaries, including the groundwater divide and no-flow boundary underlying the hillslope, changed the transit time distribution less markedly. These results can guide future decisions on the degree of complexity that is warranted in a physically-based rainfall–runoff model to efficiently and explicitly estimate time invariant subsurface pathlines and transit time distribution. 

Ort, förlag, år, upplaga, sidor
Elsevier B.V. , 2016. Vol. 543, s. 17-30
Nyckelord [en]
Flow pathline distribution, Integrated subsurface flow and transport model, Saturated–unsaturated flow, Semi-analytical solution, Svartberget catchment, Time invariant transit time distribution, Catchments, Flow of water, Groundwater, Groundwater resources, Hydraulic conductivity, Porosity, Runoff, Virtual reality, Saturated-unsaturated flow, Subsurface Flow, Transit-time distributions, Infiltration, analytical method, complexity, discharge, experimental study, flow pattern, hillslope, permeability, rainfall-runoff modeling, saturated medium, soil depth, time series analysis, unsaturated flow, water flow, Sweden
Nationell ämneskategori
Oceanografi, hydrologi och vattenresurser
Identifikatorer
URN: urn:nbn:se:ri:diva-57261DOI: 10.1016/j.jhydrol.2016.04.071Scopus ID: 2-s2.0-84969560068OAI: oai:DiVA.org:ri-57261DiVA, id: diva2:1616187
Anmärkning

Funding details: Natural Sciences and Engineering Research Council of Canada, NSERC; Funding details: Svensk Kärnbränslehantering, SKB; Funding details: Vetenskapsrådet, VR; Funding details: Kempestiftelserna; Funding text 1: We thank James Craig and Jan Seibert for their support throughout the process. This research was funded by NSERC Discovery Grant and NSERC Accelerator to J.J.M, NSERC Discovery Grant to I.F.C. The Krycklan catchment study is supported by the Swedish Science Foundation (VR) SITES, ForWater (Formas), Future Forest, Kempe Foundation, SLU FOMA and SKB.

Tillgänglig från: 2021-12-02 Skapad: 2021-12-02 Senast uppdaterad: 2023-06-02Bibliografiskt granskad

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Amvrosiadi, Nino

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