Atterberg limits, the Glossary
The Atterberg limits are a basic measure of the critical water contents of a fine-grained soil: its shrinkage limit, plastic limit, and liquid limit.[1]
Table of Contents
27 relations: Agronomy, Albert Atterberg, Arthur Casagrande, ASTM International, Austria, Chemist, Clay, Compressibility, Fall cone test, Geotechnical engineering, Granulometry (morphology), Gravimetric analysis, Karl von Terzaghi, Liquid, Permeability of soils, Plasticity (physics), Sand, Shear strength, Shear strength (soil), Silt, Smectite, Soil, Soil mechanics, Strength of materials, Sweden, United States Army Corps of Engineers, Water content.
- Tests in geotechnical laboratories
Agronomy
Agronomy is the science and technology of producing and using plants by agriculture for food, fuel, fiber, chemicals, recreation, or land conservation.
See Atterberg limits and Agronomy
Albert Atterberg
Albert Mauritz Atterberg (19 March 1846 – 4 April 1916) was a Swedish chemist and agricultural scientist who created the Atterberg limits, which are commonly referred to by geotechnical engineers and engineering geologists today.
See Atterberg limits and Albert Atterberg
Arthur Casagrande
Arthur Casagrande (August 28, 1902 – September 6, 1981) was an American civil engineer born in Austria-Hungary who made important contributions to the fields of engineering geology and geotechnical engineering during its infancy.
See Atterberg limits and Arthur Casagrande
ASTM International
ASTM International, formerly known as American Society for Testing and Materials, is a standards organization that develops and publishes voluntary consensus technical international standards for a wide range of materials, products, systems and services.
See Atterberg limits and ASTM International
Austria
Austria, formally the Republic of Austria, is a landlocked country in Central Europe, lying in the Eastern Alps.
See Atterberg limits and Austria
Chemist
A chemist (from Greek chēm(ía) alchemy; replacing chymist from Medieval Latin alchemist) is a graduated scientist trained in the study of chemistry, or an officially enrolled student in the field.
See Atterberg limits and Chemist
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, Al2Si2O5(OH)4).
Compressibility
In thermodynamics and fluid mechanics, the compressibility (also known as the coefficient of compressibility or, if the temperature is held constant, the isothermal compressibility) is a measure of the instantaneous relative volume change of a fluid or solid as a response to a pressure (or mean stress) change.
See Atterberg limits and Compressibility
Fall cone test
The Fall cone test, also called the cone penetrometer test or the Vasiljev cone test, is an alternative method to the Casagrande method for measuring the Liquid Limit of a soil sample proposed in 1942 by the Russian researcher Piotr Vasiljev (Пё́тр Васи́льев) and first mentioned in the Russian standard GOST 5184 from 1949.
See Atterberg limits and Fall cone test
Geotechnical engineering
Geotechnical engineering, also known as geotechnics, is the branch of civil engineering concerned with the engineering behavior of earth materials.
See Atterberg limits and Geotechnical engineering
Granulometry (morphology)
In mathematical morphology, granulometry is an approach to compute a size distribution of grains in binary images, using a series of morphological opening operations.
See Atterberg limits and Granulometry (morphology)
Gravimetric analysis
Gravimetric analysis describes a set of methods used in analytical chemistry for the quantitative determination of an analyte (the ion being analyzed) based on its mass.
See Atterberg limits and Gravimetric analysis
Karl von Terzaghi
Karl von Terzaghi (October 2, 1883 – October 25, 1963) was an Austrian mechanical engineer, geotechnical engineer, and geologist known as the "father of soil mechanics and geotechnical engineering".
See Atterberg limits and Karl von Terzaghi
Liquid
A liquid is a nearly incompressible fluid that conforms to the shape of its container but retains a nearly constant volume independent of pressure.
See Atterberg limits and Liquid
Permeability of soils
A number of factors affect the permeability of soils, from particle size, impurities in the water, void ratio, the degree of saturation, and adsorbed water, to entrapped air and organic material.
See Atterberg limits and Permeability of soils
Plasticity (physics)
In physics and materials science, plasticity (also known as plastic deformation) is the ability of a solid material to undergo permanent deformation, a non-reversible change of shape in response to applied forces.
See Atterberg limits and Plasticity (physics)
Sand
Sand is a granular material composed of finely divided mineral particles.
Shear strength
In engineering, shear strength is the strength of a material or component against the type of yield or structural failure when the material or component fails in shear.
See Atterberg limits and Shear strength
Shear strength (soil)
Shear strength is a term used in soil mechanics to describe the magnitude of the shear stress that a soil can sustain.
See Atterberg limits and Shear strength (soil)
Silt
Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz.
Smectite
A smectite is a mineral mixture of various swelling sheet silicates (phyllosilicates), which have a three-layer 2:1 (TOT) structure and belong to the clay minerals.
See Atterberg limits and Smectite
Soil
Soil, also commonly referred to as earth or dirt, is a mixture of organic matter, minerals, gases, liquids, and organisms that together support the life of plants and soil organisms.
Soil mechanics
Soil mechanics is a branch of soil physics and applied mechanics that describes the behavior of soils.
See Atterberg limits and Soil mechanics
Strength of materials
The field of strength of materials (also called mechanics of materials) typically refers to various methods of calculating the stresses and strains in structural members, such as beams, columns, and shafts.
See Atterberg limits and Strength of materials
Sweden
Sweden, formally the Kingdom of Sweden, is a Nordic country located on the Scandinavian Peninsula in Northern Europe.
See Atterberg limits and Sweden
United States Army Corps of Engineers
The United States Army Corps of Engineers (USACE) is the military engineering branch of the United States Army.
See Atterberg limits and United States Army Corps of Engineers
Water content
Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture), rock, ceramics, crops, or wood.
See Atterberg limits and Water content
See also
Tests in geotechnical laboratories
- Atterberg limits
- California bearing ratio
- Geotechnical centrifuge modeling
- Hole erosion test
- Jet erosion test
- Loss on ignition
- Oedometer test
- Proctor compaction test
- R-value (soils)
- Sand equivalent test
- Tilt test (geotechnical engineering)
References
[1] https://en.wikipedia.org/wiki/Atterberg_limits
Also known as Activity (soil mechanics), Casagrande Device, Liquid Limit, Plastic Limit, Plastic limit (soils), Plasticity index, Shrinkage limit.