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Last edited 06 Jan 2022
Subsidence of buildings
Subsidence occurs when the soil beneath a building is unstable and sinks downward. This is not the same as ‘settlement’, which is caused by the weight of the building, but it can still have a negative impact in terms of the overall structural stability. The opposite effect of subsidence is ‘heave’, where the site upon which the building is situated moves upwards and/or sideways.
According to Subsidence Support, ‘Over the last 10 years the adverse effects of subsidence caused by shrink-swell behaviour of soil have cost the economy an estimated £3bn, making it the most damaging geohazard in Britain today.’
 Signs of subsidence
- Sudden appearance of cracks, especially after a prolonged period of dry weather.
- Vertical and diagonal cracking in specific areas, tapering in width between the top and bottom.
- External cracking which also occurs in the same area internally.
- Opening and closing of cracks on a seasonal basis.
- Cracking occurring around weak structural points, such as doors and windows.
 Causes of subsidence
Subsidence is usually caused by the ground shrinking through a loss of moisture. This is more common after prolonged periods of dry weather. Areas where clay forms a significant proportion of the soil can be vulnerable, particularly where the clay is highly shrinkable as it then also has a tendency to expand when wet.
Other causes of subsidence may include:
- Absorption of moisture by trees and shrubs which can cause the water content of the ground to fall. For more information, see Tree root subsidence.
- Collapsing drains, culverts, hidden mine shafts, and so on.
- Buried organic material being which decomposes and destabilises all or part of a building’s foundations.
- Swallow holes or solution cavities.
- Improperly compacted ground.
- Sand or silt-based soils losing their water-soluble plant nutrients, in a process known as leaching.
 Methods of prevention and remediation
Tree Root Barriers made of high-density polyethylene can be a quick and cost-effective preventative method. As root growth can cause desiccation of soils, the use of barriers means that trees can be maintained and building occupiers not be unduly disrupted.
In minor cases of subsidence, re-pointing may be the only remedy required. If subsidence is more serious then the most common remedy is underpinning. This involves excavating soil from beneath existing foundations and replacing it with material, usually concrete, to form a new foundation beneath the existing one.
Research has shown that the majority of subsidence problems involve trees and vegetation to some extent. However, in practical terms it is very difficult to predict which trees will cause future problems. Removal of trees may not be desirable (due to the potential for heave), or may not be possible due to Tree Protection Orders (TPOs).
NB Trees in Hard Landscapes, A Guide for Delivery, published by the Trees and Design Action Group in September 2014, defines subsidence as: ‘…the downward movement of the ground supporting a building. Problems arise when the movement varies from one part of the building to the other, when cracks and structural damage can occur.’
- Brownfield land.
- Burland scale
- Carlisle cathedral.
- Contaminated land.
- Cracking and building movement.
- Defects in brickwork.
- Defects in construction.
- Defects in stonework.
- Ground conditions.
- Interferometric synthetic aperture radar InSAR.
- Latent defects.
- Right of support.
- Tree root subsidence.
- Uplift force.
- Using satellite imagery to monitor movements in megaprojects.
- Why do buildings crack? (DG 361).
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