Difference between revisions of "HOAL Petzenkirchen"
Jump to navigation
Jump to search
m (catchment size update, small edit at context of investigations, update of reference links, additional reference links) |
|||
| Line 8: | Line 8: | ||
== Catchment size == | == Catchment size == | ||
| − | The catchment area is | + | The catchment area is 66 ha. |
== Climate == | == Climate == | ||
| Line 23: | Line 23: | ||
== Context of investigation == | == Context of investigation == | ||
| − | The purpose of the HOAL project is to advance the understanding of water related flow and transport processes involving sediments, nutrients and microbes in small catchments. The HOAL catchment is ideally suited for this purpose, because it features a range of different runoff generation processes (surface runoff, springs, tile drains, wetlands), the nutrients inputs are known and it is convenient from a logistic point of view as all instruments can be connected to the power grid and a high speed Local Area Network (glassfibre). A number of innovative measurement techniques are being tested or will be tested including video cameras, distributed temperature sensing, soil moisture clusters, genetic markers as well as a range of isotopic techniques. The HOAL is operated jointly by the Vienna University of Technology and the Federal Agency for Water Management and takes advantage of | + | The purpose of the HOAL project is to advance the understanding of water related flow and transport processes involving sediments, nutrients and microbes in small catchments. The HOAL catchment is ideally suited for this purpose, because it features a range of different runoff generation processes (surface runoff, springs, tile drains, wetlands), the nutrients inputs are known and it is convenient from a logistic point of view as all instruments can be connected to the power grid and a high speed Local Area Network (glassfibre). A number of innovative measurement techniques are being tested or will be tested including video cameras, distributed temperature sensing, soil moisture clusters, genetic markers as well as a range of isotopic techniques. The HOAL is operated jointly by the Vienna University of Technology and the Federal Agency for Water Management and takes advantage of the "Vienna Doctoral Programme on Water Resource Systems" funded by the Austrian Science Foundation. |
== Measurements/Equipment == | == Measurements/Equipment == | ||
| Line 29: | Line 29: | ||
== Links to project webpages == | == Links to project webpages == | ||
| − | *[http://www. | + | *[http://www.waterresources.at/index.php?id=123 Project home page Vienna Doctoral Programme on Water Resource Systems] |
| − | *[http:// | + | *[http://www.baw.at/index.php/ikt-projekte/1608-hydrological-open-air-laboratory.html Project home page Federal Agency for Water Management] |
== References == | == References == | ||
| − | * | + | *Blöschl, G., Carr, G., Bucher, C., Farnleitner, A. H., Rechberger, H., Wagner, W. and Zessner, M. (2012): [http://www.hydrol-earth-syst-sci.net/16/457/2012/hess-16-457-2012.pdf Promoting interdisciplinary education – the Vienna Doctoral Programme on Water Resource Systems. Hydrology and Earth Systems Science, Special Issue on: Hydrology Education in a Changing World, 16, 457-472.] |
| − | *Eder, A., Exner-Kittridge, M., Strauss, P., Blöschl, G. (2014): [http://www.hydrol-earth-syst-sci.net/18/1043/2014/hess-18-1043-2014.html Re-suspension of bed sediment in a small stream – results from two flushing experiments, Hydrol. Earth Syst. Sci., 18, 1043-1052, DOI: 10.5194/hess-18-1043-2014.] | + | *Eder, A., Exner-Kittridge, M., Strauss, P., Blöschl, G. (2014): [http://www.hydrol-earth-syst-sci.net/18/1043/2014/hess-18-1043-2014.html Re-suspension of bed sediment in a small stream – results from two flushing experiments, Hydrol. Earth Syst. Sci., 18, 1043-1052, DOI: 10.5194/hess-18-1043-2014.] |
*Eder, A., Strauss, P., Krueger, T., Quinton, J.N. (2010): Comparative calculation of suspended sediment loads with respect to hysteresis effects (in the Petzenkirchen catchment, Austria). JOURNAL OF HYDROLOGY, 389(1-2), 168-176, DOI: 10.1016/j.jhydrol.2010.05.043. | *Eder, A., Strauss, P., Krueger, T., Quinton, J.N. (2010): Comparative calculation of suspended sediment loads with respect to hysteresis effects (in the Petzenkirchen catchment, Austria). JOURNAL OF HYDROLOGY, 389(1-2), 168-176, DOI: 10.1016/j.jhydrol.2010.05.043. | ||
| + | *Exner-Kittridge, M., Niederreiter, R., Eder, A. and Zessner,M. (2013): [http://www.iwaponline.com/wst/06705/1026/067051026.pdf A simple and flexible field tested device for housing water monitoring sensors at point discharges. Water Science and Technology, 67 (5), 1026-1033.] | ||
*Klaghofer, E. (2004): FLOODRISK Teilprojekt „Bodenerosion (Schwebstoffquelle)“ | *Klaghofer, E. (2004): FLOODRISK Teilprojekt „Bodenerosion (Schwebstoffquelle)“ | ||
*Strauss, P., Leone, A., Ripa, M.N., Turpin, N., Lescot, J.-M., Laplana R. (2007): Using critical source areas for targeting cost-effective best management practices to mitigate phosphorus and sediment transfer at the watershed scale. SOIL USE AND MANAGEMENT, 23(1), 144-153, DOI: 10.1111/j.1475-2743.2007.00118.x. | *Strauss, P., Leone, A., Ripa, M.N., Turpin, N., Lescot, J.-M., Laplana R. (2007): Using critical source areas for targeting cost-effective best management practices to mitigate phosphorus and sediment transfer at the watershed scale. SOIL USE AND MANAGEMENT, 23(1), 144-153, DOI: 10.1111/j.1475-2743.2007.00118.x. | ||
Revision as of 15:25, 28 April 2015
Hydrology Open Air Laboratory (HOAL) (in preparation)
Location
The catchment is situated in Petzenkirchen, in the western part of Lower Austria (15° 9’ E, 48° 8’ N).
Catchment size
The catchment area is 66 ha.
Climate
The climate can be characterised as humid with a mean annual temperature of 9.3 °C and a mean annual precipitation of around 750 mm. Mean annual flow from the catchment is about 4 l.s-1 and increased up to 2000 l.s-1 during a flood event in the 1980s. Catchment evapotranspiration varied from about 400 to 700 mm/yr in the period 2000-2009.
Geology
Topography
The elevation of the catchment ranges from 268 to 323 m a.s.l. with a mean slope of 8%.
Vegetation/Land use
At present, 87% of the catchment area is arable land, 5% is used as pasture, 6% is forested and 2% is paved. The crops are mainly winter wheat and maize.
Context of investigation
The purpose of the HOAL project is to advance the understanding of water related flow and transport processes involving sediments, nutrients and microbes in small catchments. The HOAL catchment is ideally suited for this purpose, because it features a range of different runoff generation processes (surface runoff, springs, tile drains, wetlands), the nutrients inputs are known and it is convenient from a logistic point of view as all instruments can be connected to the power grid and a high speed Local Area Network (glassfibre). A number of innovative measurement techniques are being tested or will be tested including video cameras, distributed temperature sensing, soil moisture clusters, genetic markers as well as a range of isotopic techniques. The HOAL is operated jointly by the Vienna University of Technology and the Federal Agency for Water Management and takes advantage of the "Vienna Doctoral Programme on Water Resource Systems" funded by the Austrian Science Foundation.
Measurements/Equipment
Links to project webpages
- Project home page Vienna Doctoral Programme on Water Resource Systems
- Project home page Federal Agency for Water Management
References
- Blöschl, G., Carr, G., Bucher, C., Farnleitner, A. H., Rechberger, H., Wagner, W. and Zessner, M. (2012): Promoting interdisciplinary education – the Vienna Doctoral Programme on Water Resource Systems. Hydrology and Earth Systems Science, Special Issue on: Hydrology Education in a Changing World, 16, 457-472.
- Eder, A., Exner-Kittridge, M., Strauss, P., Blöschl, G. (2014): Re-suspension of bed sediment in a small stream – results from two flushing experiments, Hydrol. Earth Syst. Sci., 18, 1043-1052, DOI: 10.5194/hess-18-1043-2014.
- Eder, A., Strauss, P., Krueger, T., Quinton, J.N. (2010): Comparative calculation of suspended sediment loads with respect to hysteresis effects (in the Petzenkirchen catchment, Austria). JOURNAL OF HYDROLOGY, 389(1-2), 168-176, DOI: 10.1016/j.jhydrol.2010.05.043.
- Exner-Kittridge, M., Niederreiter, R., Eder, A. and Zessner,M. (2013): A simple and flexible field tested device for housing water monitoring sensors at point discharges. Water Science and Technology, 67 (5), 1026-1033.
- Klaghofer, E. (2004): FLOODRISK Teilprojekt „Bodenerosion (Schwebstoffquelle)“
- Strauss, P., Leone, A., Ripa, M.N., Turpin, N., Lescot, J.-M., Laplana R. (2007): Using critical source areas for targeting cost-effective best management practices to mitigate phosphorus and sediment transfer at the watershed scale. SOIL USE AND MANAGEMENT, 23(1), 144-153, DOI: 10.1111/j.1475-2743.2007.00118.x.