Soil Exploration
Subsurface exploration is the first and most critical step in any geotechnical project. Its purpose is to identify the stratigraphy, obtain samples for laboratory testing, and determine engineering properties in-situ.
Important
A thorough exploration program typically costs 0.5% to 1% of the total project budget but prevents costly failures, delays, and over-design. Skipping this step often results in expensive change orders during construction.
Planning the Program
The extent of an exploration program depends on the variability of soil conditions and the importance or sensitivity of the structure.
Depth of Boring
Borings must extend below the significant stressed zone (also known as the pressure bulb) where the structural loads have a measurable effect on the soil.
- Isolated Footings: Explore to a depth of to (where is the footing width) below the foundation level.
- Mat Foundations: Explore to a depth of (where is the lesser dimension of the mat).
- Piles: Borings should extend into the anticipated bearing stratum to ensure its thickness and competency.
- Retaining Walls: Explore to a depth of to (where is the wall height) below the bottom of the wall.
Spacing of Borings
Spacing guidelines depend heavily on the project type:
- Multi-story Buildings: Borings are typically spaced 10-30m apart, often in a grid pattern.
- Highways: Borings are usually spaced 300-500m along the centerline, with closer spacing in areas of erratic soil.
- Dams: Borings are spaced 40-80m along the centerline of the dam.
Boring Methods and Rock Coring
Various methods are used to advance a borehole depending on the soil type and required sample quality.
Common Boring Techniques
Auger Boring: Suitable for shallow depths in soft/stiff clay and sand. It is not recommended for rock or below the water table in loose sand due to hole collapse.
Wash Boring: Uses a high-velocity water jet to displace soil. It is a very common method for driving a casing and rapidly advancing the hole, but it completely destroys soil structure.
Rotary Drilling: Uses a rotating drill bit with drilling mud (like bentonite) to support the hole walls. This is essential for deep borings and rock coring.
Rock Quality Designation (RQD)
When drilling into bedrock, a diamond-tipped core barrel retrieves solid rock cylinders. The quality of the rock mass (how fractured it is) is quantified by the RQD.
Rock Quality Designation
$$
RQD = \frac{\sum \text{Length of intact core pieces } \ge 100 \text{ mm}}{\text{Total length of core run}} \times 100\%
$$Standard Penetration Test (SPT)
The SPT (ASTM D1586) is the most widely used in-situ field test worldwide, primarily used for granular soils.
SPT Procedure
- Drive a standard split-spoon sampler (50.8 mm outside diameter) into the soil at the bottom of a borehole.
- Use a 63.5 kg (140 lb) hammer dropped from a free-fall height of 760 mm (30 in).
- Drive the sampler a total of 450 mm (18 in) in three 150 mm (6 in) increments.
- N-value: Sum the number of blows required for the last two 150 mm increments (totaling 300 mm or 12 in). The first 150 mm is considered the seating drive and its blow count is discarded.
SPT Corrections
The raw field N-value () must be corrected for energy efficiency () and overburden pressure () to ensure standardization.
Standardized SPT N-value
$$
(N_1)_{60} = C_N N_{60}
$$Energy Correction (): Corrects to a standard 60% energy efficiency.
Energy Correction for SPT
$$
N_{60} = \frac{N_{field} \eta_H \eta_B \eta_S \eta_R}{60}
$$Overburden Correction (): Normalizes the N-value to an effective overburden pressure of 1 atm ().
Overburden Correction Factor
$$
C_N = \sqrt{\frac{p_a}{\sigma'_v}} \le 2.0
$$Advanced In-Situ Testing
Beyond the SPT, modern geotechnical engineering relies on continuous, highly instrumented probes to gather precise data without retrieving physical samples.
Cone Penetration Test (CPT)
An instrumented conical probe is pushed into the soil at a constant rate (20 mm/s). It measures:
- Tip Resistance (): Relates to soil strength and density. High in sands.
- Sleeve Friction (): Friction measured along the cylindrical sleeve behind the cone tip.
- Friction Ratio (): Defined as (expressed as a percentage). Crucial for soil classification (High for clay, Low for sand).
Advantages: Provides a continuous profile, highly repeatable. Disadvantages: No physical sample retrieved.
Pressuremeter Test (PMT)
A cylindrical balloon-like probe is lowered into a borehole and inflated radially against the soil walls.
- Measures the pressure required to expand the cavity and the corresponding volume change.
- Extremely useful for determining the in-situ horizontal stress, the shear modulus (), and providing highly accurate data for lateral pile design and settlement of shallow foundations.
Flat Dilatometer Test (DMT)
A flat stainless-steel blade with a circular expandable steel membrane is pushed into the soil.
- The membrane is inflated pneumatically, and two pressures are recorded: the pressure to just lift the membrane off the blade, and the pressure to expand it 1.1 mm into the soil.
- Excellent for determining the Overconsolidation Ratio (OCR), lateral earth pressure (), and constrained modulus of the soil.
Sampling
Retrieving soil from the ground for laboratory evaluation is a primary goal of exploration.
Sample Disturbance
Disturbed Samples: The soil structure is destroyed, but the composition and index properties (grain size, Atterberg limits, specific gravity) are preserved. Examples include samples from a Split-spoon sampler or Auger cuttings.
Undisturbed Samples: The natural soil structure and in-situ moisture content are preserved as closely as possible. These are strictly required for reliable shear strength and consolidation tests. Examples include thin-walled Shelby Tube samples or Piston samplers.
Interactive Soil Exploration
Explore different soil exploration techniques and visualize boring logs.
SPT N-Value Correction Calculator
Energy-Corrected Blow Count
= 0.0
Accounts for hammer efficiency and rod length.
Overburden Correction Factor
= 0.00
Normalizes to 100 kPa effective stress.
Fully Corrected Blow Count
= 0
Used for design correlations (e.g., relative density, bearing capacity).
The Standard Penetration Test (SPT) involves dropping a 140 lb hammer 30 inches. Different hammers transfer energy differently. The normalizes this to 60% theoretical free-fall energy. adjusts for depth, because soil at greater depths appears artificially stronger due to confinement.
Geophysical Methods
Geophysical exploration techniques provide rapid, non-destructive, indirect measurements of subsurface conditions without drilling physical boreholes.
Common Geophysical Techniques
- Seismic Refraction: Uses the travel times of generated elastic waves (P-waves and S-waves) refracting off denser, deeper layers. It is highly effective for determining the depth to bedrock and the density of soil strata, but cannot detect soft layers beneath hard layers (velocity inversion).
- Electrical Resistivity: Measures the apparent electrical resistance of the ground by inducing a current and measuring the potential difference. Differences in resistivity correspond to changes in soil type (clays vs. sands), moisture content, and groundwater salinity.
- Ground Penetrating Radar (GPR): Transmits high-frequency electromagnetic pulses into the ground and records the reflections. Excellent for shallow investigations, locating buried utilities, voids, or archaeological artifacts.
Key Takeaways
- Subsurface Exploration is mandatory for determining stratigraphy and engineering properties () required for safe foundation design.
- SPT N-values must be corrected to to standardize results across different drilling rigs and depths.
- Rock Quality Designation (RQD) quantifies the competency of a fractured bedrock mass.
- CPT, PMT, and DMT provide high-resolution, continuous data on in-situ stiffness, shear strength, and lateral earth pressures, significantly outperforming traditional SPT in many advanced applications.
- Undisturbed Samples, typically obtained via thin-walled Shelby Tubes, are absolutely critical for evaluating the strength and compressibility of cohesive soils (clays).