Abstract
We demonstrate that with certain type of shoreline, geomorphology and soil properties these shock waves proceed in the soil to the extent that they cause vibrations of high-raised buildings near shore. Measurements of vibrations assumed to be initiated this way were made in buildings in the IAHR - Ice Symposium host town Lahti.
It is shown here that the occurrence of the measured vibrations can be correlated with rapid cooling and warming periods when snow-free ice exists on lake Vesijärvi.
A simple statistical model is presented for prediction of the vibration risk by meteorological data, and the frequency of the problem is analyzed by this model.
A finite-element model of the initiation and progress of the ice-induced vibrations is also made and used to demonstrate the phenomenon.
An experimental method to determine the location of the cracking is demonstrated
| Original language | English |
|---|---|
| Title of host publication | Proceedings of 20th IAHR International Symposium on Ice |
| Publisher | University of Helsinki |
| Pages | 501-511 |
| Volume | 1 |
| ISBN (Print) | 978-9-5210-5979-7, 978-1-6299-3395-5 |
| Publication status | Published - 2010 |
| MoE publication type | A4 Article in a conference publication |
| Event | 20th IAHR International Symposium on Ice 2010 - Lahti, Finland Duration: 14 Jun 2010 → 17 Jun 2010 |
Conference
| Conference | 20th IAHR International Symposium on Ice 2010 |
|---|---|
| Country | Finland |
| City | Lahti |
| Period | 14/06/10 → 17/06/10 |
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Vibrations in buildings induced by thermal cracking of lake ice. / Makkonen, Lasse; Törnqvist, Jouko; Kuutti, Juha.
Proceedings of 20th IAHR International Symposium on Ice . Vol. 1 University of Helsinki, 2010. p. 501-511.Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings › Scientific › peer-review
TY - GEN
T1 - Vibrations in buildings induced by thermal cracking of lake ice
AU - Makkonen, Lasse
AU - Törnqvist, Jouko
AU - Kuutti, Juha
PY - 2010
Y1 - 2010
N2 - Cooling and warming of lake ice induces thermal cracking. On lakes with large open areas the cracking induced shock waves in the ice may involve a lot of energy and eventually advance to the shore. We demonstrate that with certain type of shoreline, geomorphology and soil properties these shock waves proceed in the soil to the extent that they cause vibrations of high-raised buildings near shore. Measurements of vibrations assumed to be initiated this way were made in buildings in the IAHR - Ice Symposium host town Lahti.It is shown here that the occurrence of the measured vibrations can be correlated with rapid cooling and warming periods when snow-free ice exists on lake Vesijärvi. A simple statistical model is presented for prediction of the vibration risk by meteorological data, and the frequency of the problem is analyzed by this model. A finite-element model of the initiation and progress of the ice-induced vibrations is also made and used to demonstrate the phenomenon. An experimental method to determine the location of the cracking is demonstrated
AB - Cooling and warming of lake ice induces thermal cracking. On lakes with large open areas the cracking induced shock waves in the ice may involve a lot of energy and eventually advance to the shore. We demonstrate that with certain type of shoreline, geomorphology and soil properties these shock waves proceed in the soil to the extent that they cause vibrations of high-raised buildings near shore. Measurements of vibrations assumed to be initiated this way were made in buildings in the IAHR - Ice Symposium host town Lahti.It is shown here that the occurrence of the measured vibrations can be correlated with rapid cooling and warming periods when snow-free ice exists on lake Vesijärvi. A simple statistical model is presented for prediction of the vibration risk by meteorological data, and the frequency of the problem is analyzed by this model. A finite-element model of the initiation and progress of the ice-induced vibrations is also made and used to demonstrate the phenomenon. An experimental method to determine the location of the cracking is demonstrated
M3 - Conference article in proceedings
SN - 978-9-5210-5979-7
SN - 978-1-6299-3395-5
VL - 1
SP - 501
EP - 511
BT - Proceedings of 20th IAHR International Symposium on Ice
PB - University of Helsinki
ER -