02/07/2024
Temperature variations and the influence of synesthetic turf on subsoils.
It is commonly known that the upper 600mm of ground is susceptible to seasonal moisture variations. Since UK Building Regulation introduction in 1965, foundations were recommended to be at a minimum depth of 600mm below ground level to avoid seasonal variations, of shrinkage, heave (swelling) and frost expansion. The water content in these upper layers is significantly influenced by climatic and environmental factors and is generally termed the zone of seasonal fluctuations or active zone. This is particularly relevant when foundations were laid on clay sub soils. And today, it would be recommend to be no less than 900mm dep in a clay sub soil and deeper where there is vegetation within a theoretic root-affecting zone of influence.
Clay particles are very small and their shape is determined by the arrangement of the thin crystal lattice layers that they form, with many other elements which can become incorporated into the clay mineral structure (hydrogen, sodium, calcium, magnesium, sulphur). The mechanism by which these molecules become attached to each other is called adsorption. The clay mineral montmorillonite, part of the smectite family, can adsorb very large amounts of water molecules between its clay sheets, and therefore has a large shrink–swell potential.
When water is removed, by water demand from vegetation, evaporation or gravitational forces, the water between the clay sheets is released, causing the overall volume of the soil to decrease, or shrink.
Shrinkage by evaporation is similarly accompanied by a reduction in water pressure and development of negative capillary pressures. The seasonal volumetric behaviour of a desiccated soil is complex and this increases with severity of the shrinkage phenomena.
The term ‘Active Zone’ can have different meanings. Nelson et al. (2001) provide four definitions for clarity:
1. Active Zone: The zone of soil that contributes to soil expansion at any particular time
2. Zone of Seasonal moisture fluctuation: The zone in which water content change due to climatic changes at the ground surface.
3. Depth of wetting: The depth to which water contents have increased due to the introduction of water from external sources
4. Depth of potential heave: the depth at which the overburden vertical stress equals or
exceeds the swelling pressure of the soil. This is the maximum depth of the active zone.
We (AHBSS Ltd) have been involved defending a client from accusation that a mature tree has recently caused clay shrinkage problems to a nearby house.
To discount all other possible factors (before felling the perfectly healthy tree) we believe that all factors must be considered. These other factors including: evaporation and volumetric changes in the ‘Active Zone’.
In our case study, the offshoot of the adjacent Victorian property has a brick footing bearing onto a sandy clay only 250mm below ground level (yes! 250mm or three course of brick below ground). In our opinion well with the ‘Zone of Seasonal moisture fluctuation’ and well within an ‘Active Zone’ for evaporation shrinkage.
The reported cracking in the offshoot had only started within the last two to three years, while the tree would be around the same age of the house.
It is a well-established engineering fact that impermeable method of paving where used, will prevent water from penetrating into the ground and can affect the shrink-swell behaviour of the ground. A well-designed permeable paving system, in good condition may actually reduce the amount of shrink-swell activity in the ground immediately below it.
The Institution of Civil Engineers, write that paving moderates variations in water content of the soil and thus the range of shrink-swell behaviour that might be expected.
In our opinion, the thermal balance of the ground beneath and around the offshoot, over time, can increase the likelihood of soil settlement or reduce soil stability and particularly in clay soils, which would affect shallow foundations and hence the structural stability of the building.
We noted that a plastic grass (Synthetic Turf) has been laid over a compacted sub base, up to and abutting the offshoot flank wall. Those alleging tree root shrinkage, cannot say when this synthetic turf was laid, or how it correlates with this change in the offshoot paving and the reported subsidence.
We have searched research studies regards ‘Temperature Amelioration of Synthetic Turf Surfaces’ and we have found that the surface temperatures of synthetic turf (plastic grass) are significantly higher than natural turfgrass surfaces when exposed to sunlight. Reports indicate the surface temperatures of traditional synthetic turf can as much as 35-60°C higher than natural turfgrass surface temperatures. Penn State University’s Centre for Sports Surface Research conducted studies comparing surface temperatures of synthetic turfs composed of various fibre and infill colours/materials and found that the maximum surface temperatures during hot, sunny conditions averaged from 140° F to 170° F. Another study conducted at Brigham Young University found that “The surface temperature of the synthetic turf was 37° F higher than asphalt and 86.5° F hotter than natural turf.”
In our opinion (and without sampling or testing) significant heat increase, beneath the synthetic turf and it’s impermeability would have a significant effect on moisture content in the Active Zone, we estimate in the top 600mm of sub soils.
We have not accepted culpability for the movement affecting these shallow foundations and we have recommend to those allegedly tree root shrinkage, that before we consider felling the tree, which has an environmental, social and neighbourhood benefit, that the Synthetic Turf be lifted and replaced with a permeable paving.
Alan Holmes DipSurv, MRICS, CBuidE CABE, MCIAT
Institution of Civil Engineers, Manuals series. CHAPTER C5 – EXPANSIVE SOILS
Lee D Jones, British Geological Survey. Ian Jefferson, School of Civil Engineering, University of Birmingham
Experimental Research of the Heat Transfer into the Ground at Relatively High and Low Water Table Levels
Tadas Zdankus * , Juozas Vaiciunas and Sandeep Bandarwadkar
Temperature Amelioration of Synthetic Turf Surfaces through Irrigation
A.S. McNitt, D.M. Petrunak, and T.J. Serensits