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Sinkhole Glossary & Terminology

 

Activity
Commonly used as an indicator of the expansive potential of a clayey soil. The activity of a soil is estimated by dividing the plasticity index by the clay fraction of the soil.

Aquifer
The aquifer is a geologic formation, group of formations, or part of a formation that is capable of receiving, storing and transmitting water. The formation is capable of yielding enough water to support a spring or well.

Atterberg Limit
Tests performed on cohesive (clayey) soils to determine the range of moisture contents over which the soil changes from on physical condition to another. These limits are used as parameters to classify and estimate behavior of the clayey soils.

Auger
An instrument for boring or perforating soils or rocks, for determining the quality of soils, or the nature of the rocks or strata upon which they lie, and for obtaining water.

Bearing Capacity
A measure of allowable bearing (load) placed on a given soil profile before a predetermined failure (yield) criteria is met.

Bentonite
Bentonite is clay formed by the decomposition of volcanic ash, having the ability to absorb large quantities of water and to expand to several times its normal volume.

Blow Count
The number of times a 140-lb hammer must fall 30 inches to drive a split spoon sampler 6 inches.

Calcareous/Carbonate
Refers to earth materials composed of calcium carbonate (CaCO3)

Chemical Grouting
High density polyurethane expandable grout is installed under low pressure to fill voids immediately beneath foundations and/or concrete slabs. This can gently raise foundations upward in a controlled and precise method.

Chert
Rock type composed of amorphous quartz (SIO2). The material is highly insoluble and usually found in the upper zones of the limestone bedrock. It is very hard and difficult to drill.

Cohesive
Soils which exhibit plastic behavior when moist which is generally comprised of clay minerals.

Compaction Grouting
Grout is pumped through steel casings into the ground under high pressure. This seals cavities in the limestone bedrock, compacts loose soils, and fills voids in the overlying soils.

Concrete Shrinkage
The volumetric change (shrinkage) of concrete due to the evaporation of water from the hardened concrete. Tensile stresses are generated and cracks are common.

Confining Unit
A geologic unit, primarily composed of clay minerals, which retards the flow or ground water.

Consolidation
The loss of volume of a cohesive soil mass due to loading (pressure) where water is “squeezed” out over time. Often misused interchangeably with settlement or deformation in sandy soils.

Cover Collapse Sinkhole
Develop abruptly (over a period of hours), and may cause catastrophic damage to houses, commercial buildings, and roadways.

Cover Subsidence Sinkhole
Tend to develop gradually where the covering sediments are permeable, and are transported into underlying carbonate rock, eventually forming a noticeable depression in the land surface.

Dissolution Sinkholes
Formed by rainfall and surface water percolating through joints in the limestone.

Epikarst
The zone of weathering found at the upper surface of the limestone bedrock. The weathering of the limestone surface results in an irregular surface and limestone pinnacles and boulders are common within the zone.

Erosion
The transportation of earth materials, usually accomplished by water, wind, or gravity.

Expansive Soil
A fine-grained clay that is subject to swelling and shrinkage of the soil, varying in proportion to the amount of moisture present in the soil.

Fill
Soils (generally sands) used to backfill excavations and to elevate site grades during construction.

Fly Ash
Such ash recovered from the waste gases, used chiefly as a reinforcing agent in the manufacture of bricks, concrete, etc.

Footing
Footing is the portion of the foundation that transfers the structural load to underlying soils.

Foundation
That upon which anything is founded; that on which anything stands, and by which it is supported; the lowest and supporting layer of a structure; groundwork; basis.

Geologist
A geologist is a person who specializes in geologic research and study.

Geotechnical
Pertaining to practical applications of geological science in civil engineering, mining, etc.

Geotechnical Report
A report produced by geotechnical engineering firms used to communicate the soils conditions below a structure. This report typically will contain ground penetrating radar analysis, soil boring (STP borings), and other specific soil related test.

Geotechnical Engineer
The branch of engineering dealing with the soil and bedrock, especially aspects of foundations and earthworks.

Grout
Grout is a specially designed blend of cement, fine sand, fly ash, water, and sometimes small gravel that is used in the grouting process. When pumped in the ground at high pressure grout will compact loose soils, fill voids in overlying soils, and seal of cavities in the limestone bedrock.

Grouting
Grouting is a method of sinkhole repair or remediation where concrete is pumped under the ground. This is the most inexpensive method of subsurface sinkhole repair. There is no way to determine where the concrete is going or how much will be needed making this form of repair unreliable. Grouting coupled with underpinning is more widely accepted as a proper method to stabilize the foundation of a structure.

Incipient
Beginning to exist or appear; in an initial stage. This is generally used to describe the initial stages of cover subsidence sinkhole activity that may not have resulted as a surface expression.

Indurated
Cemented or compacted sediments.

Kaolinite
Clay sized mineral with a low expansion potential.

Karst
Karst is a generic term which refers to the characteristic terrain produced by erosional processes associated with the chemical weathering and dissolution of limestone or dolomite, the two most common carbonate rocks in Florida. Karst is an area of limestone terrain characterized by ravines, sinks and underground streams.

Limestone
A sedimentary rock consisting primarily of calcium carbonate, often in the form of the minerals calcite or aragonite, and sometimes with magnesium carbonate in the form of dolomite.

Lintel
Lintel is a horizontal architectural member supporting the weight above an opening, as a window or a door.

Liquid Limit (LL)
The moisture content at which a cohesive soil (clay) ceases to behave plastically and flows (as a viscous fluid).

Loss of Drilling Fluid Circulation (LOC)
Occurs when drilling fluid is lost to voids or openings in underlying geologic units. In addition, drilling fluid may be lost due to drilling conditions (clogging or drill bit, etc.)

Masonry
Stone, brick, concrete, or similar building materials bonded together with mortar to form a wall.

Moisture Content
Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture), rock, ceramics, or wood on a volumetric or gravimetric basis.

Monolithic Slab
A monolithic slab is one of four different types of foundations. One of the four types of foundations. Foundations were footings and slabs are poured together.

Montmorillonite
Any of a group of clay minerals characterized by the ability to expand when they absorb large quantities of water.

N-Value
The sum of the blows required to drive a split spoon sampler 12 inches of soil.

Overburden Soils
The sediments located directly over the bedrock. These soils are generally composed of sand and clay in Florida.

Peat
An organic-rich soil or sediment with greater that 50% by dry weight organic component.

Plastic Limit (PL)
The moisture content at which a cohesive soil (clay) ceases to be brittle and becomes plastic (able to be molded).

Plasticity Index (PI)
The range of moisture over which a cohesive soil behaves plastically. The PL is calculated as the liquid limit minus the plastic limit and is expressed as a whole number.

Potentiometric Surface
A hypothetical surface representing the level to which groundwater would rise if not trapped in a confined aquifer.

Raveling
An erosional process where groundwater transports soil particles by seepage forces (drag) downward into fractures and openings in underlying geologic units.

Settlement
Deformation of soil in the (downward) vertical direction. Settlements observed in soils may be the results of several conditions, including loading, drag forces from moving water, and erosion.

Shallow Grouting
Grout is pumped at low pressure in low volumes at 6-8 feet below a structure. This will compacted loose soils, stabilizing a structure.

Sinkhole
Formed when soluble limestone and dolomite are dissolved by acidic rainwater. This creates solution channels, fissures, and interconnected void veins within the limestone formation. As water percolates through the overburden soils into the limestone formation, part of the soil is transported into the limestone formation.

A sinkhole, also known as a sink, shake hole, swallow hole, swallet, doline or cenote, is a natural depression or hole in the surface topography caused by the removal of soil or bedrock, often both, by water. Sinkholes may vary in size from less than a meter to several hundred meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. They may be formed gradually or suddenly, and are found worldwide. These terms are often used interchangeably though many will distinguish between those features into which a surface stream flows and those which have no such input. Only the former would be described as sinks, swallow holes or swallets. ¹

Soil Series
Soil series is a classification derived by the USDA originally used for agricultural purposes. In general, the upper 6 or 7 feet of soils are described in the soil series.

Solution Sinkhole
A solution sinkhole is a small diameter opening in the limestone bedrock. The small opening may be in-filled with sediment from above or (if the limestone is sufficiently shallow) may produce a small “hole” in the ground surface. The latter is often referred to as a “chimney sinkhole”.

Surficial Aquifer
The ground water contained in the upper sequences of sands or other overburden sediments in general, the upper surface is free to move with changes in ground water volume change (due to increases/decreases in rainfall, evaporation).

Underpinning
Underpinning is a method of subsurface repair in which metal piers are driven into the ground and imbedded in the underlying limestone. Once the piers are secured into the limestone, they are then attached to your business or home with brackets. Underpins are usually installed around the perimeter of the structure at set intervals. If needed, pins can also be placed under the interior of the structure, such as under interior load bearing walls. When interior pins are needed, the homeowner often has to move out and flooring must be removed for installation. Exterior perimeter underpinning, coupled with interior pinning, is widely considered the best way to stabilize a structure where sinkhole activity is present. Some grout may also be added to provide lateral support to the pins. Underpinning is often a very expensive process, the cost of which may exceed available property insurance limits. For this reason, insurance companies rarely recommend this method of repair because payment of full policy limits is often warranted.

Water Table
The planar, underground surface beneath which earth materials, as soil or rock, is saturated with water. The upper surface of the surficial aquifer.

Weathering
The various mechanical and chemical processes that cause exposed rock to decompose.

Weight of Hammer (WHO)
An event where the drilling hammer, rod, and bit are allowed to rest on the bottom of the borehole and advance under their own weight.

Weight of Rod (WOR)
An event where the drilling rod and bit (before the placement of the hammer on the anvil)

¹ Source: Wikipedia