Emmer (Weser)

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Emmer
Emmer in Lügde

Emmer in Lügde

Data
Water code EN : 456
location North Rhine-Westphalia , Lower Saxony ; Germany
River system Weser
Drain over Weser  → North Sea
source West of Langeland
51 ° 46 ′ 38 ″  N , 8 ° 59 ′ 12 ″  E
Source height approx.  308  m above sea level NN
muzzle At Emmern in the Weser Coordinates: 52 ° 3 '25 "  N , 9 ° 22' 53"  E 52 ° 3 '25 "  N , 9 ° 22' 53"  E
Mouth height approx.  65  m above sea level NN
Height difference approx. 243 m
Bottom slope approx. 3.9 ‰
length 61.8 km
Catchment area 535.113 km²
Discharge at the Schieder – Ness gauge .
A Eo : 267.22 km²
Location: 35.03 km above the mouth
NNQ (03.09.1991)
MNQ 1981/2014
MQ 1981/2014
Mq 1981/2014
MHQ 1981/2014
HHQ (28.10.1998)
385 l / s
803 l / s
4.12 m³ / s
15.4 l / (s km²)
71 m³ / s
174 m³ / s
Discharge at the Welsede A Eo gauge : 509 km² Location: 7 km above the mouth

NNQ (10/31/1964)
MNQ 1961/1985
MQ 1961/1985
Mq 1961/1985
MHQ 1961/1985
HHQ (01/15/1968)
1.29 m³ / s
2.2 m³ / s
7.5 m³ / s
14.7 l / (s km²)
70.3 m³ / s
133 m³ / s
Discharge  at the mouth of the
A Eo : 535.11 km²
MQ
Mq
7.71 m³ / s
14.4 l / (s km²)

The Emmer (formerly called Ambriuna in Latin ) is a 61.8 km long, southwest or left-hand tributary of the Weser in North Rhine-Westphalia and Lower Saxony ( Germany ). The Emmerweg and partly the Hanover – Altenbeken railway line run along the Emmer .

geography

source

The Emmer spring in Langeland

The Emmer rises in the Egge Mountains . Its source is located on the eastern slope of the 427  m high Rehberg, north of an eastern foothill called Habichtsberg. It is located in the Langeland district of the city of Bad Driburg , about one kilometer southwest of Langeland .

course

Partial view of the Emmer reservoir before the flood was built in August 2005
Flooding of the Emmer around the Schiedersee in June 2016

Initially the Emmer flows in a north-easterly direction and crosses Langeland. In the village of Erpentrup , the river absorbs the water of the Breitenbach and flows through the areas of the cities of Nieheim , Steinheim to Schieder-Schwalenberg , where it was dammed directly northeast of Schieder after the Diestel and Niese from 1983 to 2015 to the Schiedersee . Since the Schiedersee threatened to silt up due to the sedimentation of the Emmer and also represented a migration barrier for aquatic animals, a flood was built on the north shore of the lake from 2012 to 2015. Due to this flood, the Emmer has been bypassed the Schiedersee since June 2015. Then the Emmer flows through Lügde and Bad Pyrmont . Not far from its confluence with the Weser, the Emmer flows directly past Hämelschenburg Castle , where it drives the mill wheel of the historic mill and a modern turbine for generating electricity. Between Bodenwerder and Hameln in the district of Emmern in the municipality of Emmerthal , the river finally empties after 61.8 km at an altitude of 76  m above sea level. NN from the left into the Weser. At its mouth, the Emmer has an average water flow of around 7.7 m³ / s.

Tributaries

viewed downstream

  • Vossbach
  • Breitenbach
  • Fischbach
  • Mühlenbach (Emmerkebach)
  • Beberbach
  • Sneeze
  • Uhlensenbach
  • Wörmke
  • Dallensenbach
  • Eschenbach
  • Schellenbach

Localities

viewed downstream

Hydrology

The catchment area of ​​the Emmer is 535 km². The discharge on the lower reaches of the Emmer, at the Welsede gauge in Emmerthal, averages 2.2 m³ / s at low water level (MNQ). The mean discharge (MQ) is 7.6 m³ / s, the mean flood discharge (MHQ) 38.4 m³ / s and the discharge during a hundred year flood (HQ100) 229 m³ / s.

natural reserve

The Emmer and its valley below the Emmerstausee up to the confluence with the Weser are completely protected. The section in North Rhine-Westphalia was placed under nature protection in 1992, the section in Lower Saxony followed in 1994.

use

The Emmer in front of the hydroelectric power station at Rischmade

There are hydropower plants along the Emmer in Steinheim, Wöbbel, Schieder ( Emmer reservoir hydropower plant ) and in Bad Pyrmont. There are also barrages in Welsede, Hämelschenburg and Emmerthal that generate electricity using turbines.

literature

  • Johannes Waldhoff: The Emmer. Heimatverein Steinheim, Steinheim 1986.

Individual evidence

  1. a b Topographic map 1: 25,000
  2. a b Topographical Information Management, Cologne District Government, Department GEObasis NRW
  3. ^ Deutsches Gewässerkundliches Jahrbuch Weser-Ems 2014. Lower Saxony State Agency for Water Management, Coastal and Nature Conservation, p. 159, accessed on October 4, 2017 (PDF, German, 8805 kB).
  4. a b Welsede gauge value increased by the drainage of the remaining catchment area (8.3 / s.km² to 25.51 km²), derived from the values ​​of the enclosing intermediate catchment area of ​​the gauges Bodenwerder (Weser), Oelkassen (Lenne), Welsede (Emmer), Afferde (Fluthamel), Klein Berkel (Humme), Uchtdorf (Exter) and Vlotho (Weser) and from the Hydrological Atlas of Germany - annual discharge height
  5. Emmer-Umflut is ready. nw.de, June 15, 2015, accessed on September 17, 2016 .

Web links

Commons : Emmer  - collection of images, videos and audio files