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Johannsen, Alfred; Seifert, Alfred (1981): (Table 1) Chloride concentrations in water obtained from observation wells on Helgoland Dune, North Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.784694, Supplement to: Johannsen, A; Seifert, A (1981): Trinkwassergewinnung und -versorgung auf Helgoland - von den Anfängen bis zur Gegenwart. Meyniana, 33, 41-59, https://doi.org/10.2312/meyniana.1981.33.41

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Published: 1981 (exact date unknown)DOI registered: 2012-07-19

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Abstract:
The hydrogeological conditions are unfavourable for a sufficient supply of drinking-water. The small size of the catchment area, the large hydraulic gradient inside the steep 'Buntsandstein'-cliff and the low geodetic level of the 'Dune Island' and the foreshore at the eastern foot of the cliff do not allow the formation and recharge of a sufficiently exploitable geodetic freshwater dome over the underlying saltwater. This means that until recently the provision of sufficient drinking-water for the island's inhabitants, for its garrison as well as for visiting ships was a problem. This problem has now been solved by the desalination of seawater.
Coverage:
Latitude: 54.185000 * Longitude: 7.912600
Date/Time Start: 1952-01-01T00:00:00 * Date/Time End: 1952-01-01T00:00:00
Minimum ELEVATION: -3.57 m a.s.l. * Maximum ELEVATION: 0.75 m a.s.l.
Event(s):
Helgoland_Dune1952 * Latitude: 54.185000 * Longitude: 7.912600 * Date/Time: 1952-01-01T00:00:00 * Location: German Bight, North Sea * Campaign: Helgoland * Basis: Marine Station Helgoland * Method/Device: Bucket, plastic (WB)
Comment:
ELEVATION [m a.s.l.] represents the sampling depth (Entnahmetiefe).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample IDSample IDJohannsen, Alfredobservation well (Beobachtungsbrunnen)
2ELEVATIONElevationm a.s.l.Geocode
3ChlorideCl-mg/lJohannsen, Alfred
4Elevation 2Elev2m a.s.l.Johannsen, AlfredSockel-Oberfläche in m NN
Size:
78 data points

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