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Published By Lankelma
Lankelma is the foremost contractor for onshore in-situ soil testing in the UK. An acknowledged
specialist in CPT, Lankelma also offers a worldwide consultancy and training service.
A.P. van den Berg develops, designs and manufactures geotechnical and environmental soil
investigation equipment for onshore and offshore applications. Specialists in CPT systems and equipment.
Gardline
Gardline Geosciences offers worldwide marine geotechnics, in-house consutancy and services with marine
investigations ranging from nearshore to full ocean depth (down to 3000m).
About the Author
Hans Brouwer studied civil engineering at Delft University in The Netherlands. He has
worked as a part-time lecturer at Amsterdam Polytechnic and was senior partner in a structural
engineering consultancy. He has written a standard textbook in Dutch about the design of
building foundations. He now lives in England where he writes technical textbooks in
English, hopefully to reach a bigger readership.
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Chapter 4
Part 1: Special cones: geotechnical cones
Nuclear density probe
| NUCLEAR DENSITY PROBE 4.5 For many engineering purposes it is essential to obtain accurate information on the in-situ density and porosity of the soil. This requirement has resulted in the development of a variety probes that contain a radioactive source and a detector that can be used in conjunction with the CPT.
Types of probes Essentially two types of probe are available:
- A probe that has the radioactive source mounted near the tip of the
probe and which is inserted into the ground by conventional penetration techniques
- A probe that is inserted into the ground through a pre-formed hole.
In determining the soil density, the gamma radiation emitted by a suitable source (normally caesium 137) is attenuated by either absorption or back-scattering. Compton scatter phenomenon Most available probes have been designed on the Compton scatter phenomenon. Compton scattering is proportional to the charge-tomass ratio of the atoms of the substance, this being approximately 0.50 for carbon, oxygen and silicon, and approximately 1.0 for hydrogen. The amount of back-scattered radiation is related to density with the rate of radioactive back-scatter increasing linearly with a decrease in soil density. Readings of radioactive back-scatter are readily converted to soil density using appropriate calibration curves. Calibration Calibration of the instrument can be carried out by lowering the probe into fluids with known densities of between 1.0 and 2.2 Mg/m3. Typical calibration fluids used would include water, bentonite and aluminium oxide. Alternatively, suitable materials could be compacted to a known density in layers into rigid calibration chambers. The calibration chambers are accurately weighed and the materials’ water content determined. This exercise is repeated at least three times and the probe inserted into the centre of the calibration chamber and readings taken to enable a calibration curve to be determined. A calibration chamber diameter of 1.0 m is recommended since this size should ensure that the sides of the rigid chamber are beyond the normal range of the probe. With the ever increasing environmental and legislative concerns relating to nuclear devices, the potential for the penetration probe to suffer damage – together with a loss of integrity of the source encapsulation with associated ground contamination – expensive remediation is high. Consequently these probes have lost favour as a prime method of investigation. |
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