Project

Towards a more fundamental understanding of the freeze-thaw risk in rocks: integration of material parameters and the ambient environment

Code
01P00519
Duration
01 October 2019 → 31 January 2020
Funding
Regional and community funding: Special Research Fund
Research disciplines
  • Natural sciences
    • Geoarchaeology
    • Petrology
    • Geology not elsewhere classified
    • Climate change
    • Geomorphology and landscape evolution
    • Environmental impact and risk assessment
    • Natural resource management
  • Engineering and technology
    • Built heritage and renovation
    • Destructive and non-destructive testing of materials
Keywords
porous media crystallization ice climate monitoring
 
Project description

This project aims to upscale the results of former laboratory freezethaw
experiments to real-time field conditions. These results will help
in understanding the damaging mechanisms related to internal
freezing. Most studies of freeze-thaw risks focus either on durability
testing or on climate analysis. The big challenge is now to integrate
both approaches. Currently, several approaches to estimate the
freeze-thaw risk under real-time field conditions use arbitrary
thresholds which are not material specific. In this project, the
applicant wants to weigh more material specific thresholds, obtained
from laboratory experiments (such as degree of saturation), to the
occurrence of internal freezing and damage propagation in field
conditions. For this, he will install monitored natural stone test walls
near the existing weather stations in the area of Ghent. The test walls
will be equipped with sensors to monitor proxies for ice crystallization
(such as temperature and dilatation). Moreover, the climate files from
the weather stations are being integrated in heat-air-moisture (HAM)
simulations. As the test walls are designed so that they can be
defined in HAM simulations, this provides the possibility for a
feedback between HAM modelling and real-time field observations.
This will result in a better understanding of the freeze-thaw risk in
rocks in our different environments, including local effects such as
the urban heat island.