Bergerosion i utskovskanaler

Today’s climate changes will probably give rise to precipitation in Sweden, which will cause more floods in Swedish rivers. Many of the Swedish rivers are regulated and have lots of hydro-electro power plants. Higher floods in the rivers will give greater water loads on the dams, which mean that a h...

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Bibliographic Details
Main Author: Mörén, Lena
Format: Bachelor Thesis
Language:Swedish
Published: Uppsala universitet, Institutionen för geovetenskaper 2005
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-88882
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record_format openpolar
spelling ftuppsalauniv:oai:DiVA.org:uu-88882 2023-05-15T16:33:46+02:00 Bergerosion i utskovskanaler Rock Scour in Spillway Channels Mörén, Lena 2005 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-88882 swe swe Uppsala universitet, Institutionen för geovetenskaper Uppsala : Institutionen för geovetenskaper UPTEC W, 1401-5765 05 020 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-88882 info:eu-repo/semantics/openAccess Erodibility Index Erosion of rock mass Scour Spillway channel Water load Geoengineering Geoteknik Student thesis info:eu-repo/semantics/bachelorThesis text 2005 ftuppsalauniv 2023-02-23T21:44:30Z Today’s climate changes will probably give rise to precipitation in Sweden, which will cause more floods in Swedish rivers. Many of the Swedish rivers are regulated and have lots of hydro-electro power plants. Higher floods in the rivers will give greater water loads on the dams, which mean that a higher discharge through the sluice gates and in the spillway channels is needed. High discharge of water in a spillway channel can create scour of the material in the channel. Usually, for spillways in Swedish hydropower plants, this material is rock and the scour is in form of rock blocks. Scour downstream of dams can in the worst case endanger the dam construction. The purpose of this study was to identify the extent and the type of rock scour that may appear in spillway channels of Swedish hydro power plants. The scour in rock material in a spillway channel is usually caused by pressure fluctuations in the water, which can cause large differences in pressure on the top and bottom surfaces of blocks. This pressure difference can be high enough to lift whole blocks. The main factors that affect this kind of scour are the crack pattern of the rock mass, the geometry of the spillway, the discharge of water and the surface fluctuation in the water. In this study a numeric model analyse, a field study and a literature study has been made in order to examine the influence on scour of the orientation of cracks in a rock mass. A rock mass containing a group of cracks with small or no dip is more likely to scour when it is exposed to discharging water. The orientation of the cracks in a rock mass relative to the direction of the water flow has also an impact on the capacity of the rock mass to resist scour. In the field study the scour pattern in the spillway channels of the hydro power plants in Ligga, Harsprånget, Porjus, Satisjaure and Seitevare was examined. The scour of rock mass in the spillway channels in Ligga, Harsprånget and Porjus has been extensive. The rock mass in these channels has bedding cracks of small ... Bachelor Thesis Harsprånget Uppsala University: Publications (DiVA) Harsprånget ENVELOPE(19.819,19.819,66.886,66.886) Ligga ENVELOPE(19.947,19.947,66.780,66.780)
institution Open Polar
collection Uppsala University: Publications (DiVA)
op_collection_id ftuppsalauniv
language Swedish
topic Erodibility Index
Erosion of rock mass
Scour
Spillway channel
Water load
Geoengineering
Geoteknik
spellingShingle Erodibility Index
Erosion of rock mass
Scour
Spillway channel
Water load
Geoengineering
Geoteknik
Mörén, Lena
Bergerosion i utskovskanaler
topic_facet Erodibility Index
Erosion of rock mass
Scour
Spillway channel
Water load
Geoengineering
Geoteknik
description Today’s climate changes will probably give rise to precipitation in Sweden, which will cause more floods in Swedish rivers. Many of the Swedish rivers are regulated and have lots of hydro-electro power plants. Higher floods in the rivers will give greater water loads on the dams, which mean that a higher discharge through the sluice gates and in the spillway channels is needed. High discharge of water in a spillway channel can create scour of the material in the channel. Usually, for spillways in Swedish hydropower plants, this material is rock and the scour is in form of rock blocks. Scour downstream of dams can in the worst case endanger the dam construction. The purpose of this study was to identify the extent and the type of rock scour that may appear in spillway channels of Swedish hydro power plants. The scour in rock material in a spillway channel is usually caused by pressure fluctuations in the water, which can cause large differences in pressure on the top and bottom surfaces of blocks. This pressure difference can be high enough to lift whole blocks. The main factors that affect this kind of scour are the crack pattern of the rock mass, the geometry of the spillway, the discharge of water and the surface fluctuation in the water. In this study a numeric model analyse, a field study and a literature study has been made in order to examine the influence on scour of the orientation of cracks in a rock mass. A rock mass containing a group of cracks with small or no dip is more likely to scour when it is exposed to discharging water. The orientation of the cracks in a rock mass relative to the direction of the water flow has also an impact on the capacity of the rock mass to resist scour. In the field study the scour pattern in the spillway channels of the hydro power plants in Ligga, Harsprånget, Porjus, Satisjaure and Seitevare was examined. The scour of rock mass in the spillway channels in Ligga, Harsprånget and Porjus has been extensive. The rock mass in these channels has bedding cracks of small ...
format Bachelor Thesis
author Mörén, Lena
author_facet Mörén, Lena
author_sort Mörén, Lena
title Bergerosion i utskovskanaler
title_short Bergerosion i utskovskanaler
title_full Bergerosion i utskovskanaler
title_fullStr Bergerosion i utskovskanaler
title_full_unstemmed Bergerosion i utskovskanaler
title_sort bergerosion i utskovskanaler
publisher Uppsala universitet, Institutionen för geovetenskaper
publishDate 2005
url http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-88882
long_lat ENVELOPE(19.819,19.819,66.886,66.886)
ENVELOPE(19.947,19.947,66.780,66.780)
geographic Harsprånget
Ligga
geographic_facet Harsprånget
Ligga
genre Harsprånget
genre_facet Harsprånget
op_relation UPTEC W, 1401-5765
05 020
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-88882
op_rights info:eu-repo/semantics/openAccess
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