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Soil-Structure Interaction Seminar - Foundation Performance ...

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Geology<br />

GENERAL SOILS AND GROUNDWATER<br />

The Houston area is located on the Gulf of Mexico Coastal Plain, which is underlain largely by<br />

unconsolidated clays, clay shales and poorly cemented sands to a depth of several miles. Nearly<br />

all soil of the area consists of clay, associated with moderate amounts of sand. Some of the<br />

formations in the Houston area consist of Beaumont, Lissie, and Bentley .<br />

• The Beaumont formation has significant amounts of expansive clays, resulting in shrink/swell<br />

potential. Desiccation of this formation also produces a network of fissures and slickensides in<br />

the clay that is potential plains of weakness. The Beaumont formation generally occurs in South,<br />

Southwest, East, and Central Houston. The Lissie and Bentley formations generally occur in<br />

North and part of West Houston. These formations consist of generally sands and s-andy clays.<br />

These soils 'are generally low to moderate in plasticity with low to moderate shrink/swell<br />

potential.<br />

General <strong>Soil</strong>s Conditions<br />

Variable soil conditions occur in the Houston area. These soils are different in texture,<br />

plasticity, compressibility, and strength. It is very important that foundations for residential<br />

structures be designed for subsoil conditions that exists at the specific lot in order to minimize<br />

potential foundation and structural distress. Details of general subsoil conditions at various parts<br />

of the Houston area are described below. These descriptions are very general. Significant<br />

variations from these descriptions can occur. The General soil conditions are as follows:<br />

Location<br />

Northwest and Northeast Houston,<br />

including Kingwood, The Woodlands,<br />

Cypresswood, Copperfield, Atascocita<br />

area, Fairfield, Worthom, and Oaks of<br />

Devonshire<br />

<strong>Soil</strong> Conditions<br />

Generally sandy soils occur in these areas. The<br />

sands are Houston, including generally loose<br />

and underlain by relatively impermeable clays<br />

and sandy clays. This condition promotes<br />

perched water table formation which results in<br />

the loss of bearing capacity the shallow<br />

foundations such as a conventionally-reinforced<br />

slab or post- tensioned slabs. This condition<br />

also may cause subsequent foundation settlement<br />

and distress.<br />

GEOTECH ENGINEERING AND TESTING, INC. -------------·<br />

6

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