File:Karstaquifer Schwankungen.jpg

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Deutsch: Karstwasserspiegel in Karst-Aquifern schwanken. Bei größerer Niederschlagsmenge (oder Schneeschmelze) kann der Wasserspiegel des wassergesättigten Teils eines Aquifers beträchtliche Meter steigen (die wassergesättigte Zone (phreatische Zone) vergrößert sich in ein u.U. höheres, älteres Stockwerk). Wenn dann der hydraulische Wasserdruck klüftiges oder brüchiges Karstgestein durchdringt, wird eine intermittierende Karstquelle periodisch oder episodisch aktiv. Auf der Schwäbischen Alb gibt es neben der Quelle Hungerbrunnen eine Reihe weiterer Quellen, die wegen gleicher Eigenschaften als „Hungerbrunnen“ bezeichnet werden.

English: The water table (solid red line) of the phreatic zone of a karst aquifer may rise considerably in (immediate or somewhat delayed) response to extensive precipitation or snow melt. Usually dry places in the outcrop area of the vadose zone may become active springs during such periods of elevated ground water table (dashed red line).
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Date/TimeThumbnailDimensionsUserComment
current17:02, 2 October 2019Thumbnail for version as of 17:02, 2 October 20191,800 × 883 (963 KB)Gretarsson (talk | contribs)Cropped 26 % vertically using CropTool with precise mode: unnecessarily large empty area in the upper third of the image removed
16:04, 25 February 2010Thumbnail for version as of 16:04, 25 February 20101,800 × 1,200 (944 KB)Ulrichstill (talk | contribs){{Information |Description={{de|1=Karstwasserspiegel in Karstaquifern schwanken. Bei größerer Niederschlagsmenge (oder Schneeschmelze) kann der Wasserspiegel eines wassergesättigten Aquifers beträchtlic

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