Menne

Aus Diatomeen in paderborner Karst-Flüssen
Zur Navigation springen Zur Suche springen

Aquatic states and hypotheses


Hypotheses regarding ecology and biogeography of diatoms in temporary streams in each aquatic state.


The Lippe - Alme System

The Menne is a tributary of the Altenau, which is a tributary to the Alme, the Lippe tributary which flows into the Rhine.

The Menne was studied by Meyer et al. in 2003, looking into the effect of karstic drought on macroinvertebrates. The aim of our study is to characterize the diatom communities in ephemeral and inundated locations along this stream.

Characterization of the Menne from Meyer 2003 <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>

Modified from Meyer et al 2003

ELWAS Gewässer-Id: 2782852 (keine Info)

Catchment area = 7.5 km2
Length = 7 km (3 401.849 m)
Widths = 0.5 - 2 m
Permanent spring and springbrook = 150 m
Elevation = 195 - 245 m
Stream slope = 1.7 - 2.0 %
Substrate: limestone rocks, coarse gravel and cobbles
Debris: high before next flood event

Average data

Variables Meyer et al 2003 Our study
Q (m/s) / 0.01 - 0.1
Conductivity (µS/cm) 500 - 630 350 - 601
pH 7 - 7.4 7.85 - 8.13
Temp / 12 - 13.6
Water hardness (ºdH) 15.7 - 16.2 /


Tributary to Altenau

Sampling sites

Modifiziert von Meyer et al 2003, Probenahmeorte an der Menne
Sampling site Lat Long Elevation [m]
M1 51.589308 N 8.755923 E 245
M2 51.589975 N 8.754721 E 244
M3 51.590694 N 8.754786 E 231
M4 51.597248 N 8.760392 E 208
M5 51.602579 N 8.762742 E 195

Perennial springbrook: M1, M3 Perennial spring: M2

Temporary stream section: M4, M5

Weitere Info

Links

Erstes Sampling 22.05.2020 Zweites Sampling 09.09.2020