Salt Lake City
Salt Lake City, USA

Vibrocompaction Design for Salt Lake City Sediments

Salt Lake City sits on the bed of ancient Lake Bonneville, leaving behind a complex stratigraphy of deep, soft lacustrine silts and fine sands that reach depths of 40 to 60 feet across much of the valley floor. The 2020 Magna earthquake—a magnitude 5.7 event centered just 16 miles northwest of downtown—served as a sharp reminder that these saturated granular deposits are prone to cyclic mobility and liquefaction under seismic loading. In our experience, a proper vibrocompaction design for Salt Lake City must move beyond empirical charts and instead integrate site-specific CPT soundings with the energy delivery capacity of the vibrator, accounting for the high groundwater table that typically sits only 3 to 7 feet below grade. We correlate the target relative density with post-treatment CPT testing to verify that the improved ground meets the performance criteria required by the IBC and local Salt Lake City amendments for the design earthquake.

Designing vibrocompaction on a dry lakebed means anticipating how fine silts and a high water table will interact with 130-ton vibrators to reach a dense, non-liquefiable state.

Service characteristics in Salt Lake City

The contrast in ground response between the east bench neighborhoods and the west-side industrial corridor is something we account for routinely. On the east bench, near the University of Utah, the soils transition into coarser, older Lake Bonneville gravels and the groundwater is often deeper, meaning the vibrocompaction process can rely on dry top-feed methods with fewer stone columns for drainage. Drop down into the Glendale or Poplar Grove areas west of I-15, and the profile shifts to thick, uniform fine sands with silt interbeds; here, the design almost always requires a wet bottom-feed approach, closely spaced probe patterns, and a detailed liquefaction triggering analysis that pairs the site’s standard penetration resistances with the fines content from laboratory grain-size distributions. The saturated conditions in these lower-lying areas demand that the compaction points be sequenced to build up pore pressure gradually, and we typically extend the treatment depth to at least 35 feet to reach beyond the critical liquefiable stratum. This spatial variability means that a single, off-the-shelf vibrocompaction design never fits the entire Salt Lake basin—each grid must be tuned to the microzone it sits on.
Vibrocompaction Design for Salt Lake City Sediments
Vibrocompaction Design for Salt Lake City Sediments
ParameterTypical value
Design earthquake magnitude (Mw)6.0 – 7.0 per USGS deaggregation
Target minimum relative density70 – 85% per ASCE 7-22
Typical treatment depth in valley floor25 – 45 ft
Vibrator power range130 – 180 kW electric/hydraulic
Probe spacing (sands with <15% fines)6 – 10 ft triangular grid
Maximum allowable settlement post-treatment1 inch in 50 years
QA/QC verification methodCPT before/after + SPT check borings

Risks and considerations in Salt Lake City

At an elevation of 4,226 feet above sea level and situated within the Intermountain Seismic Belt, Salt Lake City faces a 50 percent probability of a magnitude 6.75 or greater earthquake within the next 50 years, according to UGS paleoseismic studies on the Wasatch fault. A vibrocompaction design that underestimates the fines content or neglects the post-earthquake settlement potential can leave a warehouse slab or bridge approach with differential movements exceeding 4 inches, effectively severing utility connections. The biggest technical trap we see is assuming that a few SPT blows above the liquefaction threshold are sufficient; without a post-improvement shear wave velocity profile and a re-run of the simplified procedure, residual excess pore pressures can still cause ground deformation during shaking. A solid design ties the compaction grid geometry directly to the tolerable strain the superstructure can accept, not just to a minimum blow count.

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Applicable standards: ASCE 7-22 Minimum Design Loads and Associated Criteria for Buildings and Other Structures, IBC 2021 with Salt Lake City local amendments, ASTM D1586 Standard Test Method for Standard Penetration Test (SPT) and Split-Barrel Sampling of Soils, ASTM D2487 Standard Practice for Classification of Soils for Engineering Purposes (Unified Soil Classification System), FHWA-NHI-16-072 Ground Improvement Methods

Our services

Our ground improvement designs for the Salt Lake basin are always supported by a targeted field investigation program and a verification plan that confirms performance before structural loads are applied.

Liquefaction Mitigation Design

We develop vibrocompaction layouts that pair the site’s SPT N-values with fines content to compute factor of safety against liquefaction per ASCE 7, then size the probe grid and energy input to achieve a minimum FoS of 1.3 for the design earthquake. The package includes a settlement analysis using the Tokimatsu and Seed procedure to estimate residual volumetric strain.

Post-Treatment Verification Testing

We design and supervise CPTu and SPT verification programs to confirm that the densified ground meets the specified relative density and that excess pore pressure dissipation is adequate. Reports include pre- and post-treatment cone resistance profiles overlain with the design target lines.

Common questions

What is the typical cost range for a vibrocompaction design package for a commercial site in Salt Lake City?

For a mid-size commercial lot—roughly 1 to 3 acres—a complete vibrocompaction design package that includes the liquefaction analysis, compaction grid layout, technical specifications, and a post-treatment verification plan generally runs between US$1,360 and US$5,600. The final fee depends on the depth of treatment, the number of CPT soundings we need to evaluate, and whether the project requires an independent peer review for the local building department.

How does vibrocompaction design address the high groundwater table common in the Salt Lake Valley?

We design for a wet, bottom-feed process whenever the water table is within 5 feet of the ground surface, which covers most of the valley floor. The design specifies the vibrator power—typically 130 to 180 kW—and the water flush pressure needed to overcome the hydrostatic head at depth, while the probe spacing is tightened to account for the reduced effective stress in saturated fine sands. We also include a drainage plan for the surface water expelled during compaction.

What QA/QC methods do you require to sign off on a vibrocompaction job?

We do not sign off on ground improvement without a before-and-after comparison of at least three CPT soundings per treatment zone, supplemented by one SPT boring for every 5,000 square feet. The acceptance criteria are written into the design: a minimum cone tip resistance profile that corresponds to the target relative density, and a demonstrated increase in horizontal stress index (Kd) from the CPTu pore pressure data.

Can vibrocompaction be designed for sites with more than 15 percent silt content in Salt Lake City?

It can, but the design must shift from a pure densification model to a hybrid approach. When fines exceed 15 percent, the vibrocompaction points are spaced closer together—sometimes down to 5 feet center-to-center—and we incorporate a dwell time at depth to allow pore pressure to dissipate between passes. In cases where the silt content exceeds 25 percent, we often recommend replacing a portion of the vibrocompaction grid with stone columns to provide drainage paths, and the design report includes a revised liquefaction analysis using the Boulanger and Idriss procedure for transitional soils.

Coverage in Salt Lake City