This website is currently under reconstruction and thus some pages and links may not be present.
We apologise for any inconvenience caused during these alterations.
14 August 2012
Arboricultural Consultant
Dr P.G. Biddle, O.B.E., M.A., D.Phil., F.Arbor.A.
Registered Consultant of the Arboricultural Association
Honorary Fellow, Insitute of Chartered Foresters
Page 57 of Tree Root Damage to Buildings describes the relationship between gravimetric and volumetric moisture content, and provides the correct formulae for converting between the two.
However, at page 266 and figure 16.11 it provides a worked example. In this example, the gravimetric moisture content of the desiccated and control boreholes are first converted to volumetric moisture content, and the difference between the volumetric values is then used to calculate the layer deficit. This fails to take account of the change in volume that is occurring, and thus gives an erroneous result. The correct formula to use, and the correct method, are described in BRE Digest 412 "Desiccation in clay soils" at paragraph 5 on page 6 and Table 2 of BRE Digest 412.
.
You are viewing the text version of this site.
To view the full version please install the Adobe Flash Player and ensure your web browser has JavaScript enabled.
Need help? check the requirements page.