Talgosse (Alme)
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Talgosse Dahlgosse, Talgasse |
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| Data | ||
| Water code | DE : 27826 | |
| location |
Weser and Weser Leine Bergland
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| River system | Rhine | |
| Drain over | Alme → Lippe → Rhine → North Sea | |
| source | in the Ahden Valley (Büren) 51 ° 33 ′ 46 ″ N , 8 ° 38 ′ 15 ″ E |
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| muzzle | in the Alme near Büren , between Ahden and Wewelsburg Coordinates: 51 ° 36 '6 " N , 8 ° 38' 3" E 51 ° 36 '6 " N , 8 ° 38' 3" E
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| length | 8.1 km | |
| Catchment area | 30.749 km² | |
| Discharge A Eo : 30.749 km² at the mouth |
MNQ MQ Mq |
48.75 l / s 345.58 l / s 11.2 l / (s km²) |
| Left tributaries | N1, N4 | |
| Right tributaries | N2, N3, N5, N6, N7, N8, N9, N10 | |
The Talgosse (also called Dahlgosse , Talgasse and right tributary near Ahden) is an approximately 0.83 km or 8 km long river on the Paderborn plateau . This river is a left tributary of the Alme (Lippe) . The karst valley on which the river is located leads to seepage of up to 78% of the river.
course
The Talgosse consists of several side valleys in the valley system of the Ahdener Grund. The ten tributaries that flow into the Talgosse were named by Feige as tributaries N1 to N10.
Water flow
The side valleys can flow for more than 9 months after the temporary springs, but the mouths of the tributaries only 3–9 months a year. In the main valley, the river sometimes seeps away completely, although the middle course has a relatively strong water flow that separates this river from other chalk rivers in the area. The length of the permanent part of the river is 150–250 m in summer.
geology
The geological substrate consists of limestone and merge limestone.
Water quality
As part of the Water Framework Directive (WFD), the macrozoobenthos (MZB) of the tallow has been examined by the Upper Lippe Water Association .
Individual evidence
- ↑ NZO GMBH: Living waters in North Rhine-Westphalia - implementation timetable for the Lippe - Alme cooperation (DT_26). Ed .: Wasserverband Obere Lippe. Bielefeld 2012, p. 67 (wrrl-wol.de [PDF]).
- ↑ W. Feige: Der Ahdener Grund — On the hydrology of a temporary dry valley on the western Paderborn plateau. Ed .: Geographical Commission for Westphalia GeKo Aktuell. Volume I, 2003, pp. 2–12 (lwl.org [PDF])
- ↑ Self-measurement on ELWAS
- ↑ a b ELWAS specialist information system, Ministry for Climate Protection, Environment, Agriculture, Nature and Consumer Protection North Rhine-Westphalia ( notes )
- ↑ NZO GMBH: Living waters in North Rhine-Westphalia - implementation timetable for the Lippe - Alme cooperation (DT_26) . Ed .: Wasserverband Obere Lippe. Bielefeld 2012, p. 67 ( wrrl-wol.de [PDF]).
- ↑ a b c d e f W. Feige: Der Ahdener Grund — On the hydrology of a temporary dry valley on the western Paderborn plateau . Ed .: Geographical Commission for Westphalia GeKo Aktuell. tape I , 2003, p. 2–12 ( lwl.org [PDF]).
- ↑ ELWAS Web vs 3.3.2. State Office for Information and Technology North Rhine-Westphalia IT - NRW, January 28, 2020, accessed on May 18, 2020 .
- ↑ Protected Areas - Waters - Paderborn District. In: ESRI. Office for Geoinformation, Cadastre and Surveying District Paderborn - State of North Rhine-Westphalia, 2018, accessed on May 18, 2020 .
- ↑ D. Lengersdorf & M. Sältrop: Results report Lippe Water Framework Directive in North Rhine-Westphalia - inventory (environment). Ed .: State Environment Agency Lippstadt (Lippe Office), Ministry for the Environment and Nature Conservation, Agriculture and Consumer Protection of the State of North Rhine-Westphalia. 2005 ( nrw.de [PDF]).
- ↑ a b c Alexander Meyer, Elisabeth I. Meyer & Christina Meyer: Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency . Ed .: Limnologica. tape 33 . Urban & Fischer Verlag, 2003, p. 271-279 .
- ↑ Wasserverband Obere Lippe (Hrsg.): Appendix on the cooperation area Alme and important tributaries (DT 26) - information on the procedure and the waters - monitoring results . 2016, p. 9 ( wrrl-wol.de [PDF]).
