Free Soil Bearing Capacity Calculator Using Terzaghi’s Formula
The most complete Terzaghi bearing capacity tool for US engineers and contractors. Supports strip, square, circular, and rectangular footings with groundwater correction, local vs. general shear toggle, and column load adequacy check in standard US units (pcf, psf, kips, ft).
Ultimate and Allowable Bearing Pressure Analysis for Shallow US Footings
Foundation Geometry
Soil Parameters
0 for clean sand/gravel
0 for saturated clay
999 = no GWT correction
Design Settings
Auto uses local if ϕ < 28 deg
Leave blank to skip adequacy check
Results appear here
Fill in your soil parameters on the left, then click Calculate Bearing Capacity to see ultimate capacity, allowable bearing pressure, and component breakdown chart.
Bearing Capacity Factors
Capacity Components (psf)
Foundation Load Limits Every American Contractor and Engineer Needs to Understand
When a structural engineer hands off a set of foundation drawings, there is one number that makes or breaks the whole design before a single rebar is tied: the allowable soil bearing capacity. It is the maximum load per square foot that the ground beneath your footing can carry without shearing or settling excessively. Get it right and your building stands for a hundred years. Get it wrong and you are dealing with cracked slabs, tilted walls, and a contractor standing in front of a judge explaining why the parking structure failed six months after opening day.
In the United States, geotechnical engineers compute bearing capacity using methods established by Karl von Terzaghi in 1943 and refined through ASTM and ASCE standards. Terzaghi’s general shear failure theory remains the most widely used approach for shallow foundation design, accepted by virtually every building department, state DOT, and private structural engineer across the country. Our calculator implements the full Terzaghi equations in US-standard units, with the groundwater correction tables from Federal Highway Administration NHI-06-089 and shape factors from Terzaghi’s original 1943 publication.
The Three Components of Terzaghi’s Bearing Capacity Formula
Terzaghi’s genius was recognizing that the total resistance of soil beneath a loaded footing comes from three completely separate mechanisms, each dominating in different soil types and conditions. Understanding these three terms is the difference between a geotechnical engineer who blindly plugs numbers into a formula and one who can look at results and immediately tell if something is wrong.
- The cohesion term (c times Nc times Sc): This is the strength that comes from the way soil particles stick together. Clay soils get most of their strength from cohesion. A stiff clay in Houston with a cohesion of 1,500 psf can carry tremendous loads through this term alone, even when its friction angle is near zero. Pure sands have zero cohesion and rely entirely on the other two terms.
- The surcharge term (q times Nq): This is the benefit of burying your footing deeper in the ground. Every additional foot of depth adds a column of soil weight above the footing base that resists the failure wedge from pushing upward. This is why deepening a footing is often a more efficient solution than widening it. The surcharge q equals the unit weight of soil multiplied by the depth Df.
- The self-weight term (0.5 times gamma times B times Ngamma times Sg): This is the resistance that comes from the soil’s own weight within the failure wedge beneath the footing. It scales with the footing width, which is why a wider footing gets progressively more capacity from this term. For cohesionless sands, this and the surcharge term are the only sources of bearing capacity.
Understanding Soil Types and Their Bearing Capacity Behavior
One of the most common mistakes on US job sites is treating soil as a uniform material. A geotechnical investigation through ASTM D1586 Standard Penetration Test (SPT) boring is the standard US method for characterizing what you are actually building on. The SPT N-value correlates to friction angles for granular soils and to relative consistency for cohesive soils, giving engineers the c and phi values needed to run this calculator.
In the Gulf Coast states of Texas, Louisiana, and Mississippi, fat clays (CH in the Unified Soil Classification System) are the dominant surface formation. These soils have high cohesion but near-zero friction angle, meaning the cohesion term carries almost all the load. They are also highly expansive, meaning a foundation that is adequate under static load can be damaged by seasonal shrink-swell cycles that are independent of bearing capacity. In contrast, the glacial till soils of the upper Midwest and Northeast contain dense, well-graded gravels and sands with both high friction angles and some cohesion from silt content, producing excellent bearing capacity from all three terms simultaneously.
The interior Southwest, particularly Arizona and Nevada, presents a different challenge. Caliche formations just below the desert surface can appear to have excellent bearing capacity, and they do, until they are saturated during a monsoon season flood event. The caliche dissolves partially when wet, and footings that performed perfectly for years can suddenly see excessive settlement. Always account for worst-case saturation conditions when selecting your soil parameters, and confirm with ASTM laboratory testing rather than visual inspection alone.
General Shear vs. Local Shear Failure in US Practice
Terzaghi originally distinguished between two failure modes. In general shear failure, which applies to dense, stiff soils with phi greater than 28 degrees, the soil develops a complete failure surface that extends from the footing edge all the way to the ground surface. The failure is sudden and dramatic. In local shear failure, which occurs in loose sands and soft to medium clays with phi below 28 degrees, the soil compresses gradually under load and the failure surface does not fully develop. The soil yields rather than ruptures.
For local shear conditions, Terzaghi recommended reducing the soil strength parameters before applying the standard equations: cohesion is multiplied by two-thirds and friction angle is replaced by the arctangent of two-thirds times the tangent of the original friction angle. Our calculator applies this reduction automatically when you select Auto-Detect mode and the friction angle falls below 28 degrees, or you can force local shear analysis manually for conservative design in soft soils.
For a 2×2 ft square column pad at Df = 1.5 ft on sandy clay with phi = 22 deg, c = 600 psf, gamma = 110 pcf: Nc = 17.7, Nq = 7.8, Ngamma = 5.1. qu = 1.3 x 600 x 17.7 + 165 x 7.8 + 0.4 x 110 x 2 x 5.1 = 13,806 + 1,287 + 449 = 15,542 psf. qa at FOS 3.0 = 5,181 psf. A 20-kip column load on that 2×2 pad = 5,000 psf applied pressure. The footing passes by a comfortable margin.
Step-by-Step General Shear Failure Analysis for US Shallow Foundation Design
This calculator follows the exact calculation sequence a licensed geotechnical engineer would use for a preliminary shallow foundation analysis. Every step is transparent, and the results panel shows the three individual terms that make up the ultimate capacity, so you can see exactly where the soil’s resistance is coming from.
Step 1: Select Footing Shape and Apply Terzaghi’s Shape Correction Factors
Terzaghi’s original 1943 formulas use different shape correction factors for strip, square, and circular footings. These are not approximations; they are empirically derived multipliers from Terzaghi’s own experimental work. For rectangular footings, the calculator interpolates between strip and square behavior using the B/L ratio.
Step 2: Compute the Three Bearing Capacity Factors (Nc, Nq, Ngamma)
The three dimensionless factors depend entirely on the friction angle phi. Our calculator uses the standard Meyerhof Nq formulation combined with Terzaghi’s equation structure, which is the approach used in ASCE-approved geotechnical engineering software and the FHWA NHI design manuals:
At phi = 30 degrees, these factors come out to Nq = 18.40, Nc = 30.14, and Ngamma = 22.40. Compare that to phi = 15 degrees, where Nq = 3.94, Nc = 10.98, and Ngamma = 2.59. The exponential relationship between phi and capacity is why even a 5-degree improvement in friction angle from better compaction or material selection can dramatically change your design.
Step 3: Apply the Groundwater Correction
This step is where most online calculators fall short. The presence of a groundwater table within one footing width B below the footing base significantly reduces bearing capacity because the effective unit weight of submerged soil is only about half of its total unit weight. Our calculator handles all three standard cases:
- Groundwater at or above footing base (Dw < Df): Both the surcharge q and the self-weight term use the effective unit weight (gamma minus 62.4 pcf), which can reduce capacity by 30 to 50 percent on sandy soils compared to dry conditions.
- Groundwater between footing base and one B depth below (Df < Dw < Df + B): The surcharge term uses the full total unit weight, but the self-weight term uses a linearly interpolated effective weight based on how close the water table is to the footing.
- Groundwater deeper than one B below the footing base (Dw >= Df + B): No correction is required. This is the default when you enter 999 ft for the groundwater depth.
Step 4: Compute Ultimate Capacity, Apply FOS, and Check Against Your Column Load
Once the three terms are summed to give the ultimate bearing capacity qu, the tool divides by your selected factor of safety to get the allowable bearing pressure qa. If you entered a column load P in kips, the calculator divides that load by the footing area (B x L for rectangular, B squared for square, pi x r squared for circular) to get the actual applied foundation pressure in psf. If that applied pressure is less than or equal to qa, the footing passes. If it exceeds qa, the tool shows the minimum footing width required to bring the applied pressure within the allowable range.
What Makes This Calculator Different from Other Online Terzaghi Tools
After reviewing the top-ranked Terzaghi bearing capacity calculators currently appearing in US Google search results, we identified four critical gaps that this tool addresses: (1) Most competitors only support two footing shapes, skipping rectangular entirely. (2) None of the top ten results implement the three-case groundwater correction table from FHWA NHI-06-089. (3) Only one competitor offers local shear failure mode adjustment. (4) None generate a branded PDF report or show the three bearing capacity term breakdown visually. This calculator addresses all four gaps in a single free tool.
Nc, Nq, and N-Gamma Reference Values with IBC Presumptive Allowable Pressures
Use these reference tables to verify the Nc, Nq, and Ngamma values your calculator produces, and to quickly cross-reference typical allowable bearing pressures for common US soil types against published guidelines including the ASCE 7-22 standard and IBC Chapter 18 presumptive bearing values.
Table 1: Terzaghi Bearing Capacity Factors by Friction Angle
| Friction Angle ϕ (deg) | Nc | Nq | Nγ (Meyerhof) | Typical Soil Type | Failure Mode |
|---|---|---|---|---|---|
| 0 | 5.14 | 1.00 | 0.00 | Soft to medium clay (Su analysis) | General |
| 5 | 6.49 | 1.57 | 0.27 | Very soft clay, peat-adjacent | Local |
| 10 | 8.35 | 2.47 | 0.94 | Soft clay, loose silt | Local |
| 15 | 10.98 | 3.94 | 2.59 | Medium clay, silty sand | Local |
| 20 | 14.83 | 6.40 | 6.19 | Sandy clay, medium dense sand | Local |
| 25 | 20.72 | 10.66 | 13.87 | Dense sand, sandy gravel | General |
| 28 | 25.80 | 14.72 | 22.02 | Dense sand, well-graded | General |
| 30 | 30.14 | 18.40 | 29.65 | Dense sand and gravel | General |
| 35 | 46.12 | 33.30 | 65.18 | Dense gravel, compact granular | General |
| 40 | 75.31 | 64.20 | 156.14 | Very dense gravel | General |
Table 2: IBC 2021 Presumptive Bearing Values (Chapter 18 Table 1806.2)
| Soil Classification | IBC Presumptive qa (psf) | USCS Designation | Notes |
|---|---|---|---|
| Crystalline bedrock | 12,000 | Rock | Best bearing material |
| Sedimentary rock / foliated rock | 4,000 | Rock | Confirm with core samples |
| Sandy gravel or gravel (GW, GP) | 3,000 | GW, GP | Above groundwater |
| Sand, silty sand, clayey sand (SW, SP, SC, SM) | 2,000 | SW-SC | Dense condition |
| Clay, sandy clay, silty clay (CL, ML) | 1,500 | CL, ML | Stiff to hard consistency |
| Silty clay, clayey silt (CL-ML) | 1,000 | CL-ML | Medium consistency |
Note: IBC presumptive values are conservative defaults for building permit purposes. A site-specific geotechnical investigation per ASTM D1586 SPT boring will typically yield higher allowable bearing values, allowing more economical foundation designs. Use Terzaghi’s formula with actual soil test parameters whenever a geotechnical report is available.
Three American Foundation Calculations: Dallas Clay, Denver Gravel, and New Orleans Silt
These examples are representative of the bearing capacity problems engineers and contractors encounter weekly across different US soil regions. All calculations follow the same step-by-step process as our online tool.
Dallas, TX: Clay Soil Office Building Column Pad
A five-story office building in Collin County, north of Dallas. Geotechnical boring through North Texas black clay shows phi = 10 degrees, c = 900 psf, gamma = 108 pcf. Groundwater at 25 ft depth (no correction needed). Engineer proposes a 3.5 ft square column pad at 3 ft depth.
Factors at phi = 10 deg (general shear): Nc = 8.35, Nq = 2.47, Ng = 0.94
qu = (1.3 x 900 x 8.35) + (108×3 x 2.47) + (0.4 x 108 x 3.5 x 0.94) = 9,769 + 801 + 142 = 10,712 psf
Denver, CO: Sandy Gravel Retail Strip Mall
A single-story retail center in Adams County on the Denver Basin gravel. Boring shows phi = 36 degrees, c = 100 psf, gamma = 128 pcf. The site has a seasonal high groundwater at 6 ft, footing depth = 3 ft, footing width = 3 ft square. GWT is 3 ft below footing base, within the influence zone (B = 3 ft, so Dw = Df + B exactly).
Effective gamma for self-weight: no correction needed (Dw = Df + B). Nq = 37.8, Nc = 50.6, Ng = 78.0
qu = (1.3x100x50.6) + (384×37.8) + (0.4x128x3x78.0) = 6,578 + 14,515 + 11,980 = 33,073 psf
New Orleans, LA: Soft Delta Clay Strip Footing Check
A two-story residential structure near Metairie. Soft marine clay: phi = 0 degrees (phi = 0 analysis, undrained condition), Su (cohesion) = 520 psf, gamma = 98 pcf. Groundwater at 2 ft, footing depth = 3 ft. Using strip footing, B = 2 ft. GWT is above footing base (Dw = 2 ft, Df = 3 ft), so effective gamma = 98 – 62.4 = 35.6 pcf applies.
At phi = 0: Nc = 5.14, Nq = 1.00, Ng = 0.0. q = 98×2 + 35.6×1 = 231.6 psf
qu = (1.0x520x5.14) + (231.6×1.0) + 0 = 2,673 + 232 = 2,905 psf
Six Expert Tips for US Foundation Sizing and Geotechnical Parameter Selection
Always Confirm Your Phi and c from Lab Testing, Not Correlation Tables
SPT N-value correlation charts give you a starting point, but cohesion and friction angle vary enough within a single soil stratum that design on correlations alone is risky. On any project over $500,000 in foundation cost, run at least one ASTM D3080 Direct Shear Test or ASTM D4767 Triaxial Compression Test on representative samples. The fee is under $400 per test and can prevent catastrophic under-design.
Do Not Apply FOS 3.0 Blindly to All Combinations
FOS 3.0 is standard for dead plus live load under static conditions. Under ASCE 7 seismic or wind load combinations, many local jurisdictions accept FOS 2.0 because these loads occur at low probability of exceedance and are already factored. Applying FOS 3.0 to seismic combinations often results in unnecessarily oversized footings that drive up project costs with no real safety benefit.
Widening a Footing Is Less Efficient Than Deepening It
When a footing fails the adequacy check, the instinct is always to make it wider. But look at the three terms: the surcharge term grows linearly with depth at no increase in width. Deepening a footing from 2 ft to 3 ft adds 110 pcf x 1 ft = 110 psf of surcharge, which, multiplied by Nq = 18 at phi = 30 deg, adds 1,980 psf to ultimate capacity. That is often cheaper than the additional concrete in a wider pad.
Use the Wet-Season Groundwater Depth, Not the Field Measurement Date
Groundwater corrections assume the worst-case seasonal high. A boring drilled in August in Phoenix will show a water table 30 feet lower than the January measurement at the same location. For the Pacific Northwest, Midwest, and Gulf Coast, always use the seasonal high groundwater elevation from USGS well data or local hydrogeological reports, not the depth measured on the day of the boring. The USGS National Water Information System provides historic groundwater level records for thousands of US monitoring wells.
Check Differential Settlement, Not Just Bearing Capacity
A footing that passes the bearing capacity check can still cause serious structural damage through excessive differential settlement. For sands, immediate settlement can be estimated using elastic theory or Schmertmann’s method. For clays, consolidation settlement per Terzaghi’s 1D consolidation theory governs. A bearing capacity adequate design with 6 inches of differential settlement across 50 feet of building will still crack walls and jam doors. Always pair a bearing capacity calculation with a settlement estimate on clay sites.
Increase B, Not FOS, to Solve Failures on Sand Sites
For cohesionless sand sites where the bearing capacity is marginal, widening the footing is the more efficient solution because the self-weight term scales with B. Going from a 3 ft to a 4 ft square pad on medium dense sand can increase qu by 25 to 40 percent through the Ngamma term alone. In contrast, on clay sites where all the capacity comes from the cohesion term, widening the pad does almost nothing to ultimate capacity. Know which term is dominant before choosing your design approach.
Quick Reference: USCS Soil Types, Friction Angles, and Allowable Bearing Values
Use this table as a sanity check for your input parameters. If your site’s cohesion or friction angle falls well outside the typical range for the identified soil type, verify the lab test data or boring log before proceeding with design. Values below reflect normally consolidated, undisturbed in-situ conditions at shallow depth. Parameters can vary significantly with depth, density, and stress history.
| USCS Soil Type | Phi (deg) | c (psf) | γ (pcf) | Typical qa (psf) at FOS 3 | Region Examples |
|---|---|---|---|---|---|
| Clean Gravel (GW, GP) | 32 to 40 | 0 | 120 to 140 | 4,000 to 8,000 | CO, WY, UT alluvial fans |
| Sandy Gravel (GM) | 28 to 35 | 0 to 200 | 118 to 135 | 3,000 to 6,000 | Rocky Mountain valleys |
| Clean Sand (SW, SP) | 28 to 36 | 0 | 100 to 125 | 2,000 to 4,500 | FL, GA coastal, AZ desert |
| Silty Sand (SM) | 26 to 30 | 0 to 400 | 110 to 128 | 1,500 to 3,000 | Midwest loess deposits |
| Sandy Clay (CL-ML) | 18 to 26 | 300 to 800 | 106 to 122 | 1,500 to 3,000 | SE Piedmont residual soils |
| Lean Clay (CL) | 10 to 20 | 500 to 1,200 | 100 to 120 | 1,000 to 2,500 | Midwest, Mid-Atlantic |
| Fat Clay (CH) | 0 to 10 | 800 to 2,000 | 95 to 115 | 800 to 1,800 | TX Gulf Coast, LA Delta |
| Silt (ML) | 22 to 30 | 100 to 600 | 100 to 118 | 500 to 1,500 | River flood plains nationwide |
Frequently Asked Questions About Foundation Pressure Limits and Terzaghi’s Method
Soil bearing capacity is the maximum load per unit area that soil can support without experiencing shear failure or excessive settlement. It governs the size of every footing, column pad, and wall foundation in a building or structure. If the actual load from the building exceeds the allowable bearing capacity, the footing either punches through the soil or causes the soil to heave sideways, both of which result in catastrophic structural failure. In US construction, bearing capacity is calculated using methods established by ASTM D1143, ASCE 7, and IBC Chapter 18, and the results must be confirmed by a licensed geotechnical engineer for any permitted structure.
The FOS of 3.0 accounts for three main sources of uncertainty that are unavoidable in routine geotechnical practice: (1) spatial variability in soil properties that even thorough boring programs cannot fully capture, (2) the difference between small laboratory samples and the actual failure volume of soil beneath a loaded footing, and (3) long-term changes in soil strength due to wetting, drying, seasonal fluctuations, and adjacent construction. The ASCE standard recommends FOS 3.0 for permanent structures under static load, FOS 2.0 for wind or seismic load combinations, and FOS 1.5 for temporary construction loads. Using a higher FOS than required adds cost without meaningfully improving safety; using a lower FOS than required increases risk without reducing cost.
Terzaghi observed through experiments that the geometry of a footing affects how the soil failure wedge develops beneath it. A strip footing (also called a continuous wall footing) mobilizes a plane-strain failure mechanism, which gives it the lowest shape correction factors but is the most conservative base case. Square and circular footings develop a three-dimensional failure mechanism that provides more soil resistance, which is why the cohesion term gets multiplied by 1.3 for these shapes. Circular footings also get a smaller self-weight multiplier (0.3) compared to square (0.4) because the curved boundary reduces the effective failure volume on the sides. For rectangular footings, Terzaghi’s equations interpolate between strip and square behavior using the B/L ratio.
Groundwater reduces bearing capacity by decreasing the effective unit weight of soil. Submerged soil weighs approximately 62.4 pcf less per cubic foot than dry soil because the water buoys the soil particles upward. This effect reduces both the surcharge term (q = effective gamma times depth) and the self-weight term (gamma in the Ngamma term). For a sandy site with gamma = 120 pcf and seasonal high groundwater at the footing base, the effective gamma for the self-weight term drops to about 57.6 pcf (120 minus 62.4), cutting the Ngamma contribution by more than half. This is the single most common calculation error on US job sites where groundwater tables fluctuate seasonally, and it is exactly why our tool implements the full three-case groundwater correction table from FHWA NHI-06-089.
Terzaghi recommended using local shear failure mode when the soil is too loose or too soft to develop a complete Prandtl-type failure surface. In practice, this occurs when the friction angle phi is below approximately 28 degrees. For these conditions, Terzaghi reduced the effective cohesion to two-thirds of the measured value and replaced phi with the arctangent of two-thirds times tan(phi). Our Auto-Detect mode applies this reduction automatically when phi falls below 28 degrees. You can also force local shear mode manually, which is appropriate for preliminary conservative estimates on sites where exact soil parameters are not yet confirmed by laboratory testing.
For granular soils (sands and gravels), the Meyerhof correlation is a widely used starting point: phi approximately equals 25 plus 0.15 times the corrected N60 value, capped at 45 degrees. So N = 20 gives phi approximately 28 deg, and N = 40 gives phi approximately 31 deg. For cohesive soils (clays and silts), the undrained cohesion Su approximately equals 29 times N60 to the power 0.72 for normally consolidated clays, or use the consistency classification: N = 4 to 8 (soft, Su 250 to 500 psf), N = 8 to 15 (medium, Su 500 to 1,000 psf), N = 15 to 30 (stiff, Su 1,000 to 2,000 psf), N above 30 (hard, Su over 2,000 psf). These correlations carry significant uncertainty. Confirm with at least one direct shear test or unconfined compression test before finalizing foundation design.
Terzaghi’s 1943 equations remain the standard for routine shallow foundation design throughout the US. More advanced formulas by Meyerhof (1963), Hansen (1970), and Vesic (1973) add shape, depth, inclination, and base tilt correction factors that Terzaghi’s original equations omit, and they are used on more complex projects. However, Terzaghi’s equations are still accepted by most US building departments for standard soil conditions, and they are conservative, which is a safety advantage. ASCE 7, IBC Chapter 18, and FHWA NHI manuals all reference Terzaghi’s framework as the foundational method. For inclined loads, eccentric loading, or sloped ground surfaces, move to Hansen or Vesic formulations with more complete correction factor sets.
IBC 2021 Table 1806.2 provides presumptive allowable bearing pressures that building departments can accept without a geotechnical investigation for simple, low-risk structures. Values range from 1,500 psf for sandy clay or silty clay, to 2,000 psf for sand and silty sand, to 3,000 psf for sandy gravel or gravel, up to 12,000 psf for crystalline bedrock. These presumptive values are conservative by design. Most real soil conditions, once tested, will support higher allowable pressures than the IBC presumptive values, which is why a geotechnical investigation typically pays for itself in foundation cost savings on any building over 5,000 square feet of floor area.
Eccentric loading occurs when the resultant column load does not act through the centroid of the footing, such as when a moment load from wind or seismic forces accompanies the axial column load. Terzaghi’s original formula assumes concentric loading. For eccentric conditions, use Meyerhof’s effective area method: compute the effective footing dimensions as B’ = B minus 2eB and L’ = L minus 2eL, where eB and eL are the eccentricities of the resultant load in each direction. Use B’ and L’ in all bearing capacity calculations and in the area computation for applied pressure. The maximum eccentricity in any direction should not exceed one-sixth of the footing dimension (the kern condition) to avoid tension at the footing-soil interface, which most soils cannot sustain.
When phi = 0 degrees is entered (the total stress or undrained analysis case for saturated clays loaded rapidly), the calculator uses Terzaghi’s special-case bearing capacity factors: Nc = 5.14, Nq = 1.0, and Ngamma = 0.0. This is Skempton’s undrained bearing capacity solution for phi = 0 soils, and the cohesion input should be the undrained shear strength Su from an ASTM D2166 unconfined compression test or an ASTM D4767 consolidated undrained triaxial test. For this case, all the bearing capacity comes from the cohesion term, and the surcharge term contributes a constant offset equal to the overburden pressure. The self-weight term is zero because there is no frictional resistance in the failure wedge when phi = 0.
Terzaghi’s equations have several important limitations. They assume a rigid, rough footing base (meaning the soil does not slide under the footing), homogeneous soil from the footing base to a depth of at least 2B, and a horizontal ground surface. They also assume static loading and do not account for seismic conditions, cyclic loads, or dynamic effects. The equations are derived for shallow foundations where the depth-to-width ratio (Df/B) is 1.0 or less. For deeper footings (Df/B greater than 1.0), use Meyerhof’s depth correction factors. The formula also does not address settlement: a footing can be adequate in bearing capacity but still cause unacceptable settlement in compressible clays, which requires a separate consolidation analysis.
For routine shallow foundations under concentric loading on level ground, Terzaghi is the standard US approach and is conservative enough to be safe on most soil conditions. Meyerhof’s method adds shape, depth, and inclination correction factors and is preferred when the load is inclined, the footing is significantly deeper than it is wide (Df/B greater than 1.0), or the ground surface is sloped. Vesic’s method uses similar correction factors to Meyerhof but with slightly different Ngamma and is preferred by many structural engineering firms for their internal calculation standards. All three methods will give results within 15 to 25 percent of each other for standard conditions. Your project’s geotechnical engineer will specify which method to use in the geotechnical report, and that method should govern the final design.
No. Terzaghi’s bearing capacity equations apply exclusively to shallow foundations where the depth-to-width ratio (Df/B) is approximately 1.0 or less. Deep foundations such as driven piles, drilled shafts, and micropiles develop their capacity through a completely different mechanism: side friction along the shaft length plus end bearing at the tip, both of which depend on the soil properties at depth rather than at the surface. For driven pile capacity, use our Pile Driving ENR Formula Calculator for a dynamic estimate, or use static pile capacity methods per FHWA NHI-16-009 for final design. Drilled shaft capacity follows FHWA GEC-010, which uses separate alpha and beta methods for side friction.
The unit weight input in this calculator is the unit weight of the soil surrounding and beneath the footing, not the concrete. Use the soil’s total (moist) unit weight from the geotechnical report, typically 95 to 130 pcf for most US soils. The weight of the concrete footing itself is typically not included in the Terzaghi bearing capacity calculation because it is usually assumed to be approximately equal to the weight of soil it displaces (concrete weighs 150 pcf versus soil at 110 to 130 pcf), making the net additional load from the footing relatively small. However, the net footing weight above subgrade should be included in the applied load P when computing actual foundation pressure for the adequacy check.
Yes, in virtually all US jurisdictions. Building permits for structures subject to IBC require that foundation designs be prepared or reviewed and signed by a licensed professional engineer (PE) registered in the state where the project is located. This calculator provides preliminary analysis for estimating purposes, field checking, and educational use. The results cannot substitute for a site-specific geotechnical investigation report prepared by a licensed geotechnical engineer, or for foundation design plans sealed by a licensed structural PE. For residential projects exempt from engineering requirements in your jurisdiction, always confirm compliance with local building codes and the applicable version of IBC or IRC before using any calculated bearing capacity value in a permit application.
Terzaghi’s formulas assume a single, homogeneous soil layer from the footing base to at least twice the footing width below the base. In real US sites, multiple distinct soil strata are common, especially in coastal plains, river valleys, and post-glacial regions of the upper Midwest and Northeast. For layered soils, the geotechnical engineer selects the governing parameters based on the weakest layer within the failure zone (typically one to two footing widths below the base). If a weak layer exists just below the footing but a stronger layer is immediately beneath it, Meyerhof and Hanna’s punching shear method for layered soils is more appropriate than Terzaghi’s standard formula. For significant layering, request that the project geotechnical engineer perform the layered soil analysis rather than using a single-layer online tool.
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Browse HubLegal Disclaimer and Editorial Transparency
This soil bearing capacity calculator and accompanying content are provided for informational, educational, and preliminary engineering estimation purposes only. All formulas are based on Terzaghi’s 1943 general shear failure theory, Meyerhof’s bearing capacity factor equations, and FHWA NHI-06-089 groundwater correction procedures. These are publicly available engineering standards.
The outputs of this calculator do not constitute professional engineering advice or design recommendations. All foundation designs for permitted construction projects in the United States must be reviewed and sealed by a licensed professional engineer (PE) registered in the project’s state. Foundation failures can result in property damage, serious injury, or death. Do not use this tool as the sole basis for construction decisions on any permitted project.
USCalculators.com makes no warranty as to the accuracy or fitness of these results for any specific site conditions. Users assume all risks associated with the application of these results to real engineering problems. When in doubt, retain a licensed geotechnical engineer to perform a site investigation and provide site-specific recommendations.
Editorial note: This page is written by the USCalculators.com editorial team. We accept no payment for content rankings or tool recommendations. External links to ASTM, ASCE, FHWA, and IBC are provided for authoritative reference only and do not constitute endorsement of this website by those organizations.