SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:DiVA.org:uu-155591"
 

Search: onr:"swepub:oai:DiVA.org:uu-155591" > Groundwater dynamic...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Groundwater dynamics in a till hillslope : flow directions, gradients and delay

Rodhe, Allan (author)
Uppsala universitet,Luft-, vatten- och landskapslära
Seibert, Jan (author)
Stockholms universitet,Uppsala universitet,Luft-, vatten- och landskapslära,Institutionen för naturgeografi och kvartärgeologi (INK)
 (creator_code:org_t)
2011-01-13
2011
English.
In: Hydrological Processes. - : Wiley. - 0885-6087 .- 1099-1085. ; 25:12, s. 1899-1909
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • Knowledge of groundwater dynamics is important for the understanding of hydrological controls on chemical processes along the water flow pathways. To increase our knowledge of groundwater dynamics in areas with shallow groundwater, the groundwater dynamics along a hillslope were studied in a boreal catchment in Southern Sweden. The forested hillslope had a 1- to 2-m deep layer of sandy till above bedrock. The groundwater flow direction and slope were calculated under the assumption that the flow followed the slope of the groundwater table, which was computed for different triangles, each defined by three groundwater wells. The flow direction showed considerable variations over time, with a maximum variation of 75 degrees. During periods of high groundwater levels the flow was almost perpendicular to the stream, but as the groundwater level fell, the flow direction became gradually more parallel to the stream, directed in the downstream direction. These findings are of importance for the interpretation of results from hillslope transects, where the flow direction usually is assumed to be invariable and always in the direction of the hillslope. The variations in the groundwater flow direction may also cause an apparent dispersion for groundwater-based transport. In contrast to findings in several other studies, the groundwater level was most responsive to rainfall and snowmelt in the upper part of the hillslope, while the lower parts of the slope reached their highest groundwater level up to 40 h after the upper parts. This can be explained by the topography with a wetter hollow area in the upper part.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Keyword

hillslope hydrology
groundwater dynamics
flow direction
riparian zone
NATURAL SCIENCES
NATURVETENSKAP

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Find more in SwePub

By the author/editor
Rodhe, Allan
Seibert, Jan
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
Articles in the publication
Hydrological Pro ...
By the university
Uppsala University
Stockholm University

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view