Last edited 03 May 2018

Ground investigation

1 Introduction
2 Investigation techniques
3 Find out more
- 3.1 Related articles on Designing Buildings Wiki
- 3.2 External references

[edit] Introduction

The level of detail and quality of information available about ground conditions will influence the project team’s ability to develop an appropriate, efficient and easy to implement design and to deal with issues that may arise during construction work, such as the presence of faults, underground obstructions, groundwater, and so on, without incurring unnecessary costs or delays.

Ground investigations are a means of determining the condition of the ground, ideally before beginning construction works. They focus specifically on intrusive geotechnical work such as trial pits and boreholes, and so differ from wider ‘site investigations’ which tend to involve the collation of more general information from the client, from desk studies, walkover surveys, and so on.

Ground investigations can help determine:

Water table level and water flow.
The nature of faults, fissures and voids in the underground.
Ground layer thicknesses and the mechanical properties of soil.
Detailed information about soil and ground samples.

[edit] Investigation techniques

There are a number of techniques that can be used for ground investigations, either individually or in combination. When deciding on the nature, scope and level of detail of ground investigations, consideration should be given to the positive influence information can have on reducing project risks, rather than just the costs of the investigations themselves.

[edit] Trial pits and trenches

Trial pits and trenches are a means of investigating shallow ground conditions and developing an understanding of the profile of soils within the ground. They can be particularly useful where buried structures or contamination is suspected or needs further investigation.

They can be excavated by hand or backhoe excavator, generally to a depth of up to 3.5-4.5 m. Trial pits and trenches can be more cost effective than boreholes but they do not allow for the same depth.

[edit] Window sampling, windowless sample boreholes and dynamic probing

Window sample and windowless sample boreholes can be a quick and economical method for obtaining soil samples, which are recovered by inserting tubes of varying lengths into the ground. They are generally restricted to shallow depths but are suited to sites with limited access, sloping sites, and where minimal disturbance is required.

This is a particular advantage with window sampling which uses tubes with longitudinal openings cut into them and are inserted using either hand-held pneumatic samplers or tracked percussive samplers.

Dynamic probes use similar plant to provide strength profiles of the ground and enable a range of instrumentation to be installed such as piezometers, gas and groundwater monitoring wells, and so on.

[edit] Light cable percussive boreholes

Light cable percussive boreholes can be suitable for sites that have poor access or low headroom. Tripod rigs are used to drill boreholes of up to 450 mm diameter and depths of up to 70 m. This can be a relatively economical technique and is suitable for weaker soils and where high-quality samples are required.

[edit] Rotary boreholes

Rotary boreholes are used where drilled exploration through rock and other solid geological formations such as dense gravel is required. Depths of up to 100 m can be achieved. Bedrock samples can then be taken to the laboratory for examination.

Rotary open-hole boreholes are drilled where an understanding of the presence of voids is more important than the structural details of the ground, and are typically used in areas where mine workings are likely.

Rotary cored boreholes are drilled when the structural details of the underlying rock are required. A core barrel is lowered into the drilled hole and a flush circulated with air/mist or water.

[edit] Sonic drilling

Sonic drilling involves sending high frequency mechanical oscillations down a drill string to the bit. These vibrations fluidize soil particles at the face of the bit which allows for easy penetration through most geological formations where other techniques may be less successful, particularly where the strata is varied. The specific geological conditions will determine the precise frequency to be used.