Abstract
In this study, interdisciplinary approaches are considered to characterize the coastal zone aquifer of the Elbe-Weser region in the North of Lower Saxony, Germany. Geological, hydrogeological, geochemical and geophysical information have been considered to analyze the current status of the aquifers. All the information collectively states that the salinity distribution in the subsurface is heterogeneous both horizontally and vertically. Early age flooding also contributed to this heterogeneity. No general classification of groundwater quality (according to some piper diagrams) could be identified. Helicopter-borne electro-magnetic data clearly show the presence of freshwater reserves below the sea near the west coast. Groundwater recharge largely happens in the moraine ridges (west side of the area) where both the surface elevation and the groundwater level are high. Consequently, submarine groundwater discharge occurs from the same place. All these information will facilitate to develop the planned density driven groundwater flow and transport model for the study area.
Original language | English |
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Article number | 00026 |
Journal | E3S Web of Conferences |
Volume | 54 |
DOIs | |
Publication status | Published - 17 Sep 2018 |
Event | 25th Salt Water Intrusion Meeting, SWIM 2018 - Gdansk, Poland Duration: 17 Jun 2018 → 22 Jun 2018 |
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ASJC Scopus subject areas
- Environmental Science(all)
- Energy(all)
- Earth and Planetary Sciences(all)
Cite this
Characterization of a regional coastal zone aquifer using an interdisciplinary approach - An example from Weser-Elbe region, Lower Saxony, Germany. / Rahaman, Azizur; González, Eva; Wiederhold, Helga; Deus, Nico; Elbracht, Jörg; Siemon, Bernhard.
In: E3S Web of Conferences, Vol. 54, 00026, 17.09.2018.Research output: Contribution to journal › Conference article
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TY - JOUR
T1 - Characterization of a regional coastal zone aquifer using an interdisciplinary approach - An example from Weser-Elbe region, Lower Saxony, Germany
AU - Rahaman, Azizur
AU - González, Eva
AU - Wiederhold, Helga
AU - Deus, Nico
AU - Elbracht, Jörg
AU - Siemon, Bernhard
PY - 2018/9/17
Y1 - 2018/9/17
N2 - In this study, interdisciplinary approaches are considered to characterize the coastal zone aquifer of the Elbe-Weser region in the North of Lower Saxony, Germany. Geological, hydrogeological, geochemical and geophysical information have been considered to analyze the current status of the aquifers. All the information collectively states that the salinity distribution in the subsurface is heterogeneous both horizontally and vertically. Early age flooding also contributed to this heterogeneity. No general classification of groundwater quality (according to some piper diagrams) could be identified. Helicopter-borne electro-magnetic data clearly show the presence of freshwater reserves below the sea near the west coast. Groundwater recharge largely happens in the moraine ridges (west side of the area) where both the surface elevation and the groundwater level are high. Consequently, submarine groundwater discharge occurs from the same place. All these information will facilitate to develop the planned density driven groundwater flow and transport model for the study area.
AB - In this study, interdisciplinary approaches are considered to characterize the coastal zone aquifer of the Elbe-Weser region in the North of Lower Saxony, Germany. Geological, hydrogeological, geochemical and geophysical information have been considered to analyze the current status of the aquifers. All the information collectively states that the salinity distribution in the subsurface is heterogeneous both horizontally and vertically. Early age flooding also contributed to this heterogeneity. No general classification of groundwater quality (according to some piper diagrams) could be identified. Helicopter-borne electro-magnetic data clearly show the presence of freshwater reserves below the sea near the west coast. Groundwater recharge largely happens in the moraine ridges (west side of the area) where both the surface elevation and the groundwater level are high. Consequently, submarine groundwater discharge occurs from the same place. All these information will facilitate to develop the planned density driven groundwater flow and transport model for the study area.
UR - http://www.scopus.com/inward/record.url?scp=85055412755&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85055412755&partnerID=8YFLogxK
U2 - 10.1051/e3sconf/20185400026
DO - 10.1051/e3sconf/20185400026
M3 - Conference article
AN - SCOPUS:85055412755
VL - 54
JO - E3S Web of Conferences
JF - E3S Web of Conferences
SN - 2267-1242
M1 - 00026
ER -