Home Inspection FYI

Providing Help, Knowledge and Other Useful Information To Home Owners Everywhere

Home Inspection FYI - Providing Help, Knowledge and Other Useful Information To Home Owners Everywhere

Soil Contamination

Soil at a residential property can become contaminated when man-made chemicals come into contact with clean soil. Other sources of soil contamination may be wastes that leach from operational or closed landfills, runoff from livestock manure, direct dumping of hazardous industrial waste, waste piles from mining operations, septic systems and leach fields that breach their boundaries, and storage cisterns that burst underground.

soil contamination Soil Contamination

Inspectors, as well as homeowners, should use extreme caution if they suspect that such conditions exist at a property.

How does soil become contaminated?

Contaminated particles pollute soil either by becoming attached to the soil itself or by residing in the spaces between the soil particles. Sometimes, the contamination may be from a “point source,” such as when pollutants are dumped directly on soil or buried underneath. In other cases, soil becomes contaminated as liquids or gasses from point sources migrate elsewhere, contaminating residential properties downstream. A less visible example of this is when a factory emits hazardous fumes out of its smokestacks, which then travel on the air and eventually fall to the ground farther away.

The three most widespread pollutants in urban and rural residential soils are lead, arsenic and cadmium. These elements were in widespread use in paints and construction practices in the past and persist in soils today because, as heavy metals, they do not readily break down. The following is a brief description of them.

  • The primary source of lead contamination in soil is from paint that contains lead. Paint residue falls to the ground and contaminates the soil as precipitation wears away a home’s exterior. The area with the highest contamination and of greatest concern is the “drip zone,” which extends 6 feet out from the perimeter of a home. Paint residue that fell into the soil decades ago may still persist today, even though leaded paint was banned in the late 1970s. Paint chips may also have become dislodged more recently if, for example, the home’s exterior was power-washed or sand-blasted. Lead may also be deposited in soil as demolished or abandoned structures eventually fall to the ground. Another common source of lead contamination is from leaded gasoline of years past. Soil that is close to a roadway with heavy traffic has the highest risk for this type of contamination.
  • Arsenic is another contaminant that is commonly found in residential soil. Arsenic was a widely used preservative for wood used in exterior structures, such as children’s playgrounds, walkways and gazebos constructed from the mid- to late 1900s until 2004. Arsenic is likely to have leached into the soil surrounding these wooden structures, especially in areas that have heavy precipitation. Areas with old, abandoned wooden structures on them are of concern. Arsenic was also a common ingredient in pesticides, herbicides and fertilizers. It is likely to persist in the soil of historic orchards and agricultural areas where these chemicals have not been sprayed in decades.
  • Cadmium is a common contaminant that has entered the environment and, consequently, the soil at properties as a byproduct of the burning of fossil fuels and municipal wastes, and from the smelting of zinc, lead, and copper.

Why is contaminated soil hazardous?

Contaminated soil is dangerous for humans and animals. People are at high risk for poisoning when they come into direct contact with soil. This may occur when a person conducts any activity in the soil, such as digging, gardening and landscaping, and when soil is tracked into the home. Soil contaminants may be inhaled when soil is kicked up in the air, such as while mowing grass. Children are at particularly high risk because of their propensity for mouthing objects and putting their hands into their mouths without washing.

Pets and wild animals come into contact with contaminated soil when burrowing, eating and drinking from the ground. Changes in soil chemistry affect creatures at the lower end of the food chain, such as arthropods and tiny micro-organisms. Consequently, this puts entire ecosystems at risk, since it may cause a ripple effect through the food chain.

Another serious hazard is that drinking water supplies may become contaminated from contaminated soil. This is of primary concern when residents rely on underground water wells and aquifers for their fresh water supply.

There is a variety of health risks associated with contaminated soil, depending on the level of exposure, the type of pollutant, and the vulnerability of the affected population. Chronic exposure to heavy metals and other contaminants may put exposed individuals at a higher risk for cancers, neural disorders, reproductive disorders, and birth defects. Other less serious side effects may occur with light exposure, such as headaches, dizziness, fatigue and rashes.

 

Contaminated soil also has a negative effect on plant growth and crop yields. Contaminated fruits and vegetables may be hazardous to consume, especially if they are not properly handled and washed prior to eating.

How can you tell if soil at a property is contaminated?

There may or may not be visible indications of soil contamination. One obvious sign of lead contamination may be paint chips around the exterior of the house, if the paint is known to be leaded. Apparent discolorations in soil and strong odors are other indications that the soil may be hazardous. Another possible clue of contamination may be if vegetation fails to thrive in a certain area of soil, although this depends on the vegetation and whether the soil’s natural content is hospitable to such growth.

 

One of the first things to consider when trying to determine if soil is contaminated is the history of the land. If the land or adjacent areas have ever been used for agriculture, industry, mining, waste disposal or gas dispensing, then there may be a lingering problem. If there have ever been wooden structures on the property prior to the late 1970s, then the land has a higher risk for lead and arsenic contamination.

 

The only sure way to tell if soil is contaminated is to sample the soil and have a certified laboratory test it.  A certified local soils engineer or professional should be employed to conduct soil sampling. Exhaustive testing may be exorbitantly expensive, however, but tests for the most common contaminants are usually affordable. Sampling for lead, arsenic and cadmium is usually less than $100.

What are the options for remediating contaminated soil?

Complete soil mapping and remediation can be a prohibitively expensive venture. Many contaminated industrial and commercial sites qualify for grants based on their “brownfield” status.  However, this does not necessarily apply to residential sites. Local authorities should be consulted to see if there is financial assistance available. Funding may be provided for remediation procedures, depending on the level of risk to the surrounding community.  excav Soil Contamination

Soil remediation methods include the following:

  • Excavation is the most comprehensive and expensive method of remediating soil. After contaminated soil has been identified, it may be removed from the property and transferred to a landfill for disposal. New topsoil is tested, trucked in, and distributed throughout the property to replace the old soil.
  • “Soil blending,” whereby contaminated soil is mixed with fresh soil, results in a mix that has a lower concentration of contaminants and meets local guidelines for acceptable pollutant levels.
  • The soil can be excavated, treated, and then replaced, after it has been deemed safe. Various methods for treating soil may be employed in situ or after excavation. These include applying aeration, heat and/or water, or treating it with chemicals that change the hazardous substances into ones that will biodegrade over time.
  • Bioremediation is a process whereby specific plants or fungi are utilized that naturally break down hazardous materials.
  • Problem areas may be covered or paved over so as to avoid exposure when excavating or treating soil is not an option. This is not a long-lasting solution, although it does help to inhibit the contaminants from spreading further.
  • “Capping” is a procedure whereby problem areas are covered by more than a foot of new topsoil. This may be an adequate temporary solution but, eventually, plant roots may penetrate into the contaminated soil.

What precautions should be taken with soil that is or is suspected to be contaminated?

It is important to take special precautions with contaminated soil, especially when remediation techniques are not feasible.

  • Hazardous areas should be partitioned off, and direct exposure should be minimized.
  • Children’s play areas should be situated away from areas that may be hazardous, such as around the drip zone of a house, or near roadways where gasoline deposits may have accumulated.
  • Shrubbery may be planted around the drip zone of a house to discourage traffic in that area. Consider covering bare soil with mulch if grass will not grow on patches of contaminated soil.
  • Edible gardens should always be located away from hazardous areas. Building raised garden beds with clean topsoil minimizes the possibility of plants growing in unfit soil. Gardeners should always be sure to wash their hands thoroughly after working in the soil, as well as washing vegetables that will be consumed. Special attention should be paid to scraping root vegetables that have come into direct contact with contaminated soil.
  • When mowing grass or working in areas with hazardous soil, wear personal protective equipment, including clothing that adequately covers exposed skin, a dust mask or respirator to prevent inhaling contaminated dirt and airborne particles, and protective eyewear.

Soil may become contaminated in a myriad of ways, and special caution must be taken to minimize the associated risks.  InterNACHI inspectors who suspect that soil or groundwater at a property is contaminated may want to recommend that their client have such conditions investigated and evaluated by a qualified soils engineer or other professional.

Soil Contamination

Soil Compaction and Soil Settlement

Soil Characteristics and Soil Settlement


Soil is a naturally-occurring mixture of mineral and organic ingredients with a definite form, structure, and composition. settlement 1 Soil Compaction and Soil Settlement

Soil characteristics are composed primarily of minerals and organic matter which are produced from parent material which is broken into small pieces by weathering. Larger pieces in soil are stones, gravel, and other rock debris. Smaller particles in soil are sand, silt, or clay. Since the original materials vary from place to place, the exact composition of the soil characteristics varies according to location. A common example of soil composition and soil characteristics by volume might be:

  • 45% Minerals (clay, silt, sand, gravel, stones).
  • 25% Water (the amount varies depending upon precipitation and the water-holding capacity of the soil).
  • 25% Air (an essential ingredient for living organisms).
  • 5% Organic matter or humus (both living and dead organisms).

Mineral particles give soil texture. Sand particles range in diameter from 2 mm to 0.05 mm, feel gritty and can be easily seen in the soil with the unaided eye. Silt particles are between 0.05 mm and 0.002 mm and feel like flour. Clay particles are smaller than 0.002 mm and cannot be seen with the unaided eye. Because of the small particle size, clay soils can sometimes experience large amounts of expansion and contraction in volume with changes in moisture content.

Water and air occupy the pore spaces—the area between soil particles. The final ingredient of a soil is organic matter. Organic matter consists of dead plant and animal material and the billions of living organisms that inhabit soil.

Soil Compaction

The concern with soil in respect to building is the ability of soil to bear the load of the structure while remaining stable. Ensuring long-term stability requires proper soil compaction and consolidation of soil before a permanent load is placed upon it. Examples of a permanent load would be foundation footings and walls or a concrete floor or driveway slab. Soil compaction is most important.

The excavation process disturbs soil, loosening it and causing spaces between soil particles to become much larger. For this reason, engineering specifications often require that foundations be placed on undisturbed soil instead of using soil compaction and other methods.

In areas at which a home is built partially or completely on fill soil, such as homes built on hillsides, that fill soil must be made as solid as possible before a permanent load is placed on it. This is done by mechanical soil compaction. Soil is placed in layers (called “lifts”). Each layer of soil is mechanically compacted by impact and sometimes by vibration.

When the soil in larger areas such as a hillside lot are compacted, heavy equipment is used. For soil in smaller areas like backfill around basement foundation walls, a jumping jack tamper is used which is operated by one person.

Compactionof the soil is the process of forcing air from the spaces between the soil particles. Soil compaction with a jumping jack tamper is somewhat inexact. In determining the point at which soil is adequately compacted, the operator listens to the tone of the tamper impacting the soil. When soil is adequately compacted, the tone will have a ringing quality which will not change. A change in tone indicates that the soil compaction is still taking place.settlement 2 Soil Compaction and Soil Settlement

Compaction increases the density of the soil and improves its ability to bear a load. Compaction is affected by a number of factors:

  • Soil type (clay, sand, silt, level of organic matter, etc.)
  • Soil characteristics (uniformity, gradient, plasticity, etc.)
  • Soil thickness
  • Method of soil compaction
  • Moisture content of the soil at the time of compaction.

Consolidation is the process of forcing water from the spaces between soil particles. Soil is more permeable to air than to water. This means that the compaction process may remove from the soil a large percentage of air, but a significant percentage of water may remain.

Soil undergoes both primary and secondary consolidation.
Primary consolidation is short-term and takes place during the mechanical compacting process. Secondary consolidation is long-term and takes place after the compaction process is complete and the permanent loads are in place.

During secondary consolidation, the weight placed on soil slowly forces water out of the spaces between soil particles. As this happens, soil particles will move close together and settling will occur. The source of the weight would be both the structure and the overlying soil.

The amount of secondary consolidation which can be expected increases with the depth of the affected area. An excavation with backfill 15 feet deep would experience more secondary consolidation than an excavation with backfill 8 feet deep.

A common scenario is when a structure is built partially on undisturbed soil and partially on compacted fill. Soil in these two areas will consolidate at different rates as the weight of the newly-built structure forces water from between soil particles. This is called “differential settlement”.

Settling will be reflected in any part of structure bearing upon the settled soil. In adequately-compacted soil, settling will be so minor that evidence won’t be visible. Extreme differential settlement will create stresses which are relieved by cracking.

Which materials crack depends on the properties of the material and the rate of settling. More brittle materials will crack first. The effects of soil movement are most often seen as cracks in interior and exterior wall coverings like drywall and plaster and in masonry foundation walls.

Even concrete, which most people think of as brittle, can bend if pressure is applied slowly over a long time period. If pressure is applied over a shorter time period, concrete will crack.

Fine-Grained Soils

Compaction and consolidation are affected by the composition of the soil. Fine-grained soils have more interior surfacsettlement 3 Soil Compaction and Soil Settlemente area and can hold more air and water than course-grained soils.

Here’s an example of the effects of fine-grained soils. Drywall is made of much courser particles than cement. An ounce of drywall dust contains about 5,000 square feet of interior surface area. An ounce of cement dust contains about 50,000 square feet of interior surface area.

This means that fine-grained soils like clays have more interior surface area which can contain water. In order to force water out of the spaces between particles, surface tension must be overcome. “Surface tension” is the tendency of water to cling to a surface. When you fill a glass with water, it’s surface tension that makes the water level slightly higher around the edges where water comes into contact with the glass surface. Water is clinging to the glass.

The greater interior surface area of fine-grained soils results in greater surface tension. Fine-grained are also typically low-permeability soils, meaning that water moves through them slowly. These conditions increase the amount of time and pressure required for soil to consolidate. Soils will continue to consolidate until the resistance to pressure of the materials of which the soil is composed reach equilibrium with pressure from the weight of soil and structure above.

The rate of consolidation is affected by the soil composition, levels of moisture saturation, the amount and nature of the load on the soil and state of consolidation of the soil.

Another moisture-related problem is the addition of excessive moisture to the soil. This can create a condition in which water is absorbed into spaces between soil particles. Soil becomes less dense, which reduces its ability to support a load.

Thanks to Nick Gromicko and Kenton Shepard, InterNACHI’s Director of Green Building