Hauptseite: Unterschied zwischen den Versionen

Aus Diatomeen in paderborner Karst-Flüssen
Zur Navigation springen Zur Suche springen
Keine Bearbeitungszusammenfassung
Keine Bearbeitungszusammenfassung
Zeile 1: Zeile 1:
[[Datei:Loc.png|mini|Zuflüsse der Lippe, temporär und "ewige" Flüsse und Bäche]]
[[Datei:Loc.png|mini|Zuflüsse der Lippe, temporär und "ewige" Flüsse und Bäche]]


Karstic rivers are hydrogeologically conditioned to have spatial and seasonal changes in their discharge <ref>MEYER, A., E.I. MEYER & C. MEYER 2003. Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica 33 (4): 271–279. </ref>. In the high plateau of Paderborn (Paderborner Hochfläche), the left tributary of the Lippe, [https://de.wikipedia.org/wiki/Alme_(Lippe) Alme], itself and some of its tributaries are temporary rivers [[glossary]] due to fluctuations of groundwater levels ([https://de.wikipedia.org/wiki/Hungerbrunnen#/media/Datei:Karstaquifer_Schwankungen.jpg Hungerbrunnen]).
Karstic rivers are hydrogeologically conditioned to have spatial and seasonal changes in their discharge <ref>MEYER, A., E.I. MEYER & C. MEYER 2003. Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica 33 (4): 271–279. </ref>. In the high plateau of Paderborn (Paderborner Hochfläche), the left tributary of the Lippe, [https://de.wikipedia.org/wiki/Alme_(Lippe) Alme], itself and some of its tributaries are [[temporary]] due to fluctuations of groundwater levels ([https://de.wikipedia.org/wiki/Hungerbrunnen#/media/Datei:Karstaquifer_Schwankungen.jpg Hungerbrunnen]).


Projects:
Projects:

Version vom 14. Mai 2020, 11:24 Uhr

Zuflüsse der Lippe, temporär und "ewige" Flüsse und Bäche

Karstic rivers are hydrogeologically conditioned to have spatial and seasonal changes in their discharge <ref>MEYER, A., E.I. MEYER & C. MEYER 2003. Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica 33 (4): 271–279. </ref>. In the high plateau of Paderborn (Paderborner Hochfläche), the left tributary of the Lippe, Alme, itself and some of its tributaries are temporary due to fluctuations of groundwater levels (Hungerbrunnen).

Projects:

  • Preliminary sampling at the Menne

Index

Flüsse

  1. Menne
  2. Afte
  3. Alme
  4. Altenau
  5. Ellerbach
  6. Gosse
  7. Piepenbach
  8. Reingraben
  9. Sauer<ref>Meyer, A., & Meyer, E. I. (2000). Discharge regime and the effect of drying on macroinvertebrate communities in a temporary karst stream in East Westphalia (Germany). Aquatic Sciences, 62(3), 216-231.</ref>
  10. Lippe
  11. Rhein

Anderes

Links How to