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Water storage dynamics in a till hillslope : the foundation for modeling flows and turnover times

Amvrosiadi, Nino (författare)
Uppsala universitet,Luft-, vatten- och landskapslära
Seibert, Jan (författare)
Uppsala universitet,Luft-, vatten- och landskapslära,Hydrology and Climate Unit, Department of Geography, University of Zurich, Zurich, Switzerland
Grabs, Thomas J., 1980- (författare)
Uppsala universitet,Luft-, vatten- och landskapslära
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Bishop, Kevin (författare)
Swedish University of Agricultural Sciences,Sveriges lantbruksuniversitet,Institutionen för vatten och miljö,Department of Aquatic Sciences and Assessment,Swedish University of Agricultural Sciences, Uppsala, Sweden
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 (creator_code:org_t)
 
2016-11-28
2017
Engelska.
Ingår i: Hydrological Processes. - : John Wiley and Sons Ltd. - 0885-6087 .- 1099-1085. ; 31:1, s. 4-14
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • 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. 

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

flow pathways
storage
storage dynamics
turnover time
Catchments
Digital storage
Dynamics
Energy storage
Exponential functions
Groundwater
Soils
Travel time
Water
Extended versions
Hillslope discharge
Hydrological properties
Mineral weathering
Vertical equilibriums
Rivers
discharge
flow modeling
hillslope
phreatic zone
porewater
runoff
water storage
water table

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