EXPANSIVE SOIL AND EXPANSIVE CLAY - The hidden force behind basement and foundation problems – When expansive soils absorb water, they increase in volume. The more water they absorb, the more their volume increases. This change in volume can exert enough force on a building or other structure to cause damage. Cracked foundations, floors, and basement walls are typical types of damage done by swelling soils. Damage to the upper floors of the building can occur when motion in the structure is significant. Expansive soils will also shrink when they dry out. This shrinkage can remove support from buildings or other structures and result in damaging subsidence. Fissures in the soil can also develop. These fissures can facilitate the deep penetration of water when moist conditions or runoff occurs.

Building damage: Note displaced bricks and inward deflection of foundation.

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Expansive Soil and Expansive Clay

Cracks in expansive soil: Desiccation cracks in soil caused by drying. 

The hidden force behind basement and foundation problems

Article by: Hobart M. King, Ph.D., RPG

What is an "Expansive Soil"?

Expansive soils contain minerals such as smectite clays that are capable of absorbing water. When they absorb water, they increase in volume.

The more water they absorb, the more their volume increases. Expansions of ten percent or more are not uncommon. This change in volume can exert enough force on a building or other structure to cause damage.

Cracked foundations, floors, and basement walls are typical types of damage done by swelling soils. Damage to the upper floors of the building can occur when motion in the structure is significant.

In a typical year in the United States, expansive soils cause a greater financial loss to property owners than earthquakes, floods, hurricanes, and tornadoes combined.

Expansive soils will also shrink when they dry out. This shrinkage can remove support from buildings or other structures and result in damaging subsidence.

Fissures in the soil can also develop. These fissures can facilitate the deep penetration of water when moist conditions or runoff occurs.

This cycle of shrinkage and swelling places repetitive stress on structures, and damage worsens over time.

How Many Buildings are at Risk?

Expansive soils are present throughout the world and are known in every US state. Every year they cause billions of dollars in damage.

The American Society of Civil Engineers estimates that 1/4 of all homes in the United States have some damage caused by expansive soils.

In a typical year in the United States, they cause a greater financial loss to property owners than earthquakes, floods, hurricanes, and tornadoes combined.

Even though expansive soils cause enormous amounts of damage, most people have never heard of them.

This is because their damage is done slowly and cannot be attributed to a specific event.

The damage done by expansive soils is then attributed to poor construction practices or a misconception that all buildings experience this type of damage as they age.

Homeowners Insurance and Expansive Soils

Damage to a home caused by expansive soils can be catastrophic for a homeowner. Why?

Most homeowners insurance policies do not cover damage caused by expansive soils. The cost of repairs and mitigation can be extremely high - it sometimes exceeds the value of the home.

In many cases the homeowner noticed the problem, didn’t realize its severity, didn’t realize that it was progressing, and the problem progressed to a point where repair didn’t make economic sense.

Expandable, Shrink-Swell, Heavable Soils?

Expandable soils are referred to by many names. "Expandable soils," "expansive clays," "shrink-swell soils," and "heavable soils" are some of the many names used for these materials.

The problem is so unfamiliar to the average homeowner that they don't know what to call it.

Expansive Soils Map

The map on this page shows the generalized geographic distribution of soils that are known to have expandable clay minerals which can cause damage to foundations and structures. It also includes soils that have a clay mineral composition which can potentially cause damage.

How to Interpret the Map

The map is meant to show general trends in the geographic distribution of expansive soils. It is not meant to be used as a property evaluation tool. It is useful for learning areas where expansive soils underlie a significant portion of the land and where expansive soils might be a localized problem.

All construction projects should include a soil analysis to identify the types of soil present and determine their expansive properties. Local occurrences of expansive soils can be found in all of the soil categories shown on this map.

Why Do These Soils Expand?

Soils are composed of a variety of materials, most of which do not expand in the presence of moisture.

However, a number of clay minerals are expansive. These include: smectite, bentonite, montmorillonite, beidellite, vermiculite, attapulgite, nontronite, and chlorite. There are also some sulfate salts that will expand with changes in temperature.

When a soil contains a large amount of expansive minerals, it has the potential of significant expansion. When the soil contains very little expansive minerals, it has little expansive potential.

Changes in Moisture Content Trigger Damage

When expansive soils are present, they will generally not cause a problem if their water content remains constant. The situation where greatest damage occurs is when there are significant and repeated moisture content changes.

The Bottom Line

It is possible to build successfully and safely on expansive soils if stable moisture content can be maintained or if the building can be insulated from any soil volume change that might occur.

The procedure for success is as follows:

·         Testing to identify any problems

·         Design to minimize moisture content changes and insulate from soil volume changes

·         Build in a way that will not change the moisture conditions of the soil

·         Maintain a constant moisture environment after construction

Expert assistance is usually needed to do these things successfully.

Hobart M. King, Ph.D., GIA GG

Hobart M. King is the owner and publisher of Geology.com. He is a geologist with over 40 years of experience, has a Ph.D. in geology, and is a GIA graduate gemologist. Much of his work has focused on coal geology, industrial minerals, gemology, geologic hazards, and geoscience education.

He has authored many of the internet’s most popular articles about rocks, minerals and gems. He writes most of the content published on Geology.com and compiles its daily news. His writing is read by over a million people each month, making him one of the world’s most widely read geologists.

Dr. King earned a Ph.D. and an M.S. in geology from West Virginia University; a B.S. in geology from California University of Pennsylvania; and, a Graduate Gemologist Diploma from the Gemological Institute of America. He is a registered professional geologist in the Commonwealth of Pennsylvania.

He has worked as a geologist in a variety of settings since 1975.

https://geology.com/articles/expansive-soil.shtml

Deflected basement wall: Inward deflection of a basement wall and pilasters. The plumb-bob reveals 9 inches of inward displacement.

Expansive soils map: The map above is based upon "Swelling Clays Map of the Conterminous United States"