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The value of experimental data and modelling for exploration of hydrological functioning: The case of a till hillslope
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Luft-, vatten och landskapslära.
2017 (engelsk)Doktoravhandling, med artikler (Annet vitenskapelig)
Abstract [en]

Successfully modeling one system response (e.g. hydrograph or solute transport) sometimes gives the false sense of well-characterizing the modeled system. This is partly because of the well-known equifinality issue; during the calibration process multiple parameter combinations can produce similarly good results. One step forward towards a better-defined system is using measured (at relevant scale) values for the model parameters, as well as using multiple conditions to constrain the model.

But when not enough, or relevant, field measurements are available, virtual experiments (VE’s) can be used as a supplementary method to model calibration. The advantage of VE’s over model calibration is that they can also be used to explore assumptions both on the system hydrological processes, and on the model structure.

One goal of this study was to utilize both field measurements and models for better characterization of the S-transect hillslope, located in Västrabäcken catchment, Northern Sweden. This included (a) characteristics in space: system vertical boundaries, hydraulic parameters, pore water velocity distribution, spatial correlation of flowpaths, soil water retention properties; (b) characteristic of system’s dynamic behavior: storage – discharge relationship, transit time distribution, turnover time; and (c) outputs’ sensitivity to external forcing, and to small scale structure assumptions. The second goal was to comment on the value of field measurements and virtual experiments for extracting information about the studied system.

An intensely monitored study hillslope was chosen for this work. Although the hillslope has already been the subject of multiple field and modelling studies, there are still open questions regarding the characteristics listed above. The models used were the Vertical Equilibrium Model (VEM), and the Multiple Interacting Pathways (MIPs) model.

It was found that the hillslope was well connected; from the near-stream areas up to the water divide the storage – discharge relationship could be described as an exponential function. Also, the dynamic storage (which controls the hydrograph dynamics) was much smaller comparing to the total hillslope storage. The unsaturated soil storage was found to be more sensitive to water table positions than vertical flux magnitude. The dynamic condition of external forcing (precipitation and evapotranspiration) affected the transit time distribution (TTD) shape. And, opposite to expectations, TTD was not sensitive to micro-scale structural assumptions tested here.

sted, utgiver, år, opplag, sider
Uppsala: Acta Universitatis Upsaliensis, 2017. , s. 80
Serie
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, ISSN 1651-6214 ; 1579
HSV kategori
Identifikatorer
URN: urn:nbn:se:uu:diva-331856ISBN: 978-91-513-0115-0 (tryckt)OAI: oai:DiVA.org:uu-331856DiVA, id: diva2:1150395
Disputas
2017-12-15, 13:00 (engelsk)
Opponent
Veileder
Tilgjengelig fra: 2017-11-17 Laget: 2017-10-18 Sist oppdatert: 2018-03-07
Delarbeid
1. Water storage dynamics in a till hillslope: the foundation for modeling flows and turnover times
Åpne denne publikasjonen i ny fane eller vindu >>Water storage dynamics in a till hillslope: the foundation for modeling flows and turnover times
2017 (engelsk)Inngår i: Hydrological Processes, ISSN 0885-6087, E-ISSN 1099-1085, Vol. 31, nr 1, s. 4-14Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Studies on hydrology, biogeochemistry, or mineral weathering often rely on assumptions about flow paths, water storage dynamics, and transit times. Testing these assumptions requires detailed hydrometric data that are usually unavailable at the catchment scale. Hillslope studies provide an alternative for obtaining a better understanding, but even on such well‐defined and delimited scales, it is rare to have a comprehensive set of hydrometric observations from the water divide down to the stream that can constrain efforts to quantify water storage, movement, and turnover time. Here, we quantified water storage with daily resolution in a hillslope during the course of almost an entire year using hydrological measurements at the study site and an extended version of the vertical equilibrium model. We used an exponential function to simulate the relationship between hillslope discharge and water table; this was used to derive transmissivity profiles along the hillslope and map mean pore water velocities in the saturated zone. Based on the transmissivity profiles, the soil layer transmitting 99% of lateral flow to the stream had a depth that ranged from 8.9 m at the water divide to under 1 m closer to the stream. During the study period, the total storage of this layer varied from 1189 to 1485 mm, resulting in a turnover time of 2172 days. From the pore water velocities, we mapped the time it would take a water particle situated at any point of the saturated zone anywhere along the hillslope to exit as runoff. Our calculations point to the strengths as well as limitations of simple hydrometric data for inferring hydrological properties and water travel times in the subsurface.

Emneord
flow pathways, storage, storage dynamics, turnover time
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-331679 (URN)10.1002/hyp.11046 (DOI)000441296100001 ()
Tilgjengelig fra: 2017-10-16 Laget: 2017-10-16 Sist oppdatert: 2018-10-12bibliografisk kontrollert
2. Soil moisture storage estimation based on steady vertical fluxes under equilibrium
Åpne denne publikasjonen i ny fane eller vindu >>Soil moisture storage estimation based on steady vertical fluxes under equilibrium
2017 (engelsk)Inngår i: Journal of Hydrology, ISSN 0022-1694, E-ISSN 1879-2707, Vol. 553, s. 798-804Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Soil moisture is an important variable for hillslope and catchment hydrology. There are various computational methods to estimate soil moisture and their complexity varies greatly: from one box with vertically constant volumetric soil water content to fully saturated-unsaturated coupled physically-based models. Different complexity levels are applicable depending on the simulation scale, computational time limitations, input data and knowledge about the parameters. The Vertical Equilibrium Model (VEM) is a simple approach to estimate the catchment-wide soil water storage at a daily time-scale on the basis of water table level observations, soil properties and an assumption of hydrological equilibrium without vertical fluxes above the water table. In this study VEM was extended by considering vertical fluxes, which allows conditions with evaporation and infiltration to be represented. The aim was to test the hypothesis that the simulated volumetric soil water content significantly depends on vertical fluxes. The water content difference between the no-flux, equilibrium approach and the new constant-flux approach greatly depended on the soil textural class, ranging between similar to 1% for silty clay and similar to 44% for sand at an evapotranspiration rate of 5 mm.d(-1). The two approaches gave a mean volumetric soil water content difference of 1 mm for two case studies (sandy loam and organic rich soils). The results showed that for many soil types the differences in estimated storage between the no-flux and the constant flux approaches were relatively small.

Emneord
Volumetric soil water content, Vertical flux, VEM, Catchment water storage
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-331688 (URN)10.1016/j.jhydrol.2017.08.042 (DOI)000412612700061 ()
Forskningsfinansiär
Swedish Research Council, 2011-4889
Tilgjengelig fra: 2017-10-16 Laget: 2017-10-16 Sist oppdatert: 2018-01-13bibliografisk kontrollert
3. Value of virtual experiments for a hillslope scale system understanding
Åpne denne publikasjonen i ny fane eller vindu >>Value of virtual experiments for a hillslope scale system understanding
Vise andre…
(engelsk)Manuskript (preprint) (Annet vitenskapelig)
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-331730 (URN)
Tilgjengelig fra: 2017-10-17 Laget: 2017-10-17 Sist oppdatert: 2018-01-13
4. Water age dependence on vertical flux assumptions
Åpne denne publikasjonen i ny fane eller vindu >>Water age dependence on vertical flux assumptions
(engelsk)Manuskript (preprint) (Annet vitenskapelig)
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-331731 (URN)
Tilgjengelig fra: 2017-10-17 Laget: 2017-10-17 Sist oppdatert: 2018-01-13
5. Following tracer through the unsaturated zone using a Multiple Interacting Pathways model: implications from laboratory experiments
Åpne denne publikasjonen i ny fane eller vindu >>Following tracer through the unsaturated zone using a Multiple Interacting Pathways model: implications from laboratory experiments
(engelsk)Manuskript (preprint) (Annet vitenskapelig)
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-331732 (URN)
Tilgjengelig fra: 2017-10-17 Laget: 2017-10-17 Sist oppdatert: 2018-01-13

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