GEOTECHNICAL

Standard Penetration Test (SPT)

Soil density test in borehole per IS 2131

Also calledsptstandard penetration testspt n valuepenetration test
Related on InfraLens
CODES
Definition

Standard Penetration Test (SPT) is the most-widely-used field test in Indian geotechnical practice for in-situ characterisation of soil strength and density. Standardised in IS 2131:1981 (revised 2024), the test consists of driving a split-spoon sampler (50 mm OD, 35 mm ID) into the soil at the bottom of a borehole using a 63.5 kg hammer dropped from 760 mm height. The number of hammer blows required to advance the sampler the second and third 150 mm increments (combined) is recorded as the N-value. Lower N-values indicate looser cohesionless soils or softer cohesive soils; higher N-values indicate denser/stiffer materials.

SPT N-values are correlated to virtually every geotechnical design parameter. For sandy soils, N is correlated to relative density (loose: N < 10; medium: 10-30; dense: 30-50; very dense: >50), angle of internal friction (φ), modulus of elasticity, and allowable bearing pressure (Terzaghi-Peck, Meyerhof, Bowles correlations). For cohesive soils, N is correlated to undrained shear strength (cu ≈ 5N to 12N kPa, with substantial scatter) and unconfined compressive strength. For Indian projects, IS 6403 Cl. 5 provides tabulated bearing capacity values directly from N-values, which most routine designs use without explicit shear-strength computation.

The primary limitations of SPT are well-recognised: significant scatter in N-values due to hammer-energy variability, sampler condition, and operator technique; inadequate for soils with gravel >50 mm size; not usable in saturated dense sands where dilation gives spuriously high values. Modern Indian practice supplements SPT with: Cone Penetration Test (CPT, IS 4968) for continuous profile, Pressuremeter Test for in-situ deformation modulus, and laboratory triaxial testing of UDS samples for high-importance structures. For routine residential and commercial work, 3-5 boreholes with SPT every 1.5 m depth, terminated 5 m below founding depth or in firm strata for ≥ 3 m, remains the Indian standard practice.

Typical values
Loose sandN = 0-10
Medium sandN = 10-30
Dense sandN = 30-50
Very dense sand / soft rockN > 50
Soft clayN = 0-4
Medium clayN = 4-8
Stiff clayN = 8-15
Hard clayN > 15
Where used
  • Routine site investigation for buildings — 3-5 boreholes
  • Bearing capacity computation per IS 6403 Cl. 5
  • Pile capacity estimation — N-values along shaft and at toe
  • Liquefaction susceptibility assessment per IS 1893 Part 1 Annex F
  • Foundation type selection — raft vs piles based on near-surface N profile
Acceptance / threshold
Per IS 2131:1981: standard 63.5 kg hammer, 760 mm drop height, 50 mm OD split-spoon. N-value from second + third 150 mm penetration; first 150 mm discarded as 'seating'. Energy correction (N60) applied for hammer type. Refusal at N > 50 in 150 mm noted; not pursued further.
Site example
Site reality: a Bhopal site investigation reported SPT N-values 5, 8, 6, 9 in the upper 4 m. Designer planned isolated footings at SBC 75 kN/m² (per IS 6403 correlation). At construction, excavation revealed a 30 cm thick weathered shale layer at the founding depth that the SPT had missed (sampler bypassed it). Direct examination of excavation revealed actual SBC ≥ 250 kN/m² at the foundation level. The project saved ₹35 lakh on foundation by switching to smaller footings — but only because the site engineer caught the missed lens. Always inspect excavation against the soil report; SPT can miss thin firm layers.
Frequently asked
What is SPT in soil mechanics?
Standard Penetration Test (SPT) is a field test where a 50 mm OD split-spoon sampler is driven into a borehole bottom by a 63.5 kg hammer dropped 760 mm. The number of blows for the second and third 150 mm penetration is recorded as N-value. SPT is the most-widely-used in-situ test for routine geotechnical investigation in India.
How is N-value correlated to soil properties?
For cohesionless soils: relative density (loose N<10, medium 10-30, dense 30-50, very dense >50), friction angle φ (Peck-Hansen-Thornburn correlation), modulus E (Bowles), and allowable bearing pressure (IS 6403 Cl. 5). For cohesive soils: cu ≈ 5N to 12N kPa (with scatter), unconfined compressive strength qu ≈ 12N to 24N kPa. Many empirical correlations exist; calibration to local geology is recommended.
What are limitations of SPT?
Significant scatter in N-values due to hammer energy variability (energy ratio can vary 50-100% between rigs); not usable in gravels >50 mm or in saturated dense sand (dilation gives spuriously high values); operator-dependent for borehole cleaning and sampler advancement. Modern Indian practice supplements SPT with CPT (Cone Penetration Test) for continuous profile and laboratory triaxial testing for important structures.
Related geotechnical terms