Geotechnical Engineering

geotechnical banner 3Geotechnical engineering is a subcategory of civil engineering that analyzes the mechanics of soils and rocks in the building and excavation for a site.  Every construction design infrastructure that is supported by foundations, above or below ground such as bridges, dams, plants, slopes, structures, tunnels, etc. uses geotechnical engineering.

 

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Geotechnical Engineering Glossary

 

Soil Types (OSHA)

  • Stable rock  -  Natural soilmaterial that can be excavated with vertical sides and remain intact whole exposed.
  • Type A  -  Cohesive soils with an unconfined compression strength of 15 tons per square inch or greater.  Includes clay, sandy clay, silty clay and clay loam.
  • Type B  -  Cohesive soils with an unconfined compression strength greater than 0.5 tons per square inch but less than 1.5 tons per square inch and granular cohesionless soils.  Includes angular gravel, silt, silt loam, sandy loam, and unstable rock.
  • Type C  -  Cohesive soils with an unconfined compression strength of 0.5 tons per square inch or less.  Includes gravel, sand and loam sand.

 

Geotechnical Engineering standards

ASTM Standards

  • ASTM C1242 - Standard Guide for Selection, Design, and Unstallation of Dimension Stone Attachment Systems
  • ASTM D559 - Standard Test Method for Wetting and Drying Compacted Soil-Cement Mixtures
  • ASTM D560 - Standard Test Method for Freezing and Thawing Compacted Soil-Cement Mixtures
  • ASTM D806 - Standard Test Method for Cement Content of Hardened Soil-Cement Mixtures
  • ASTM D806 - Standard Guide for Selection of Dimension Stone
  • ASTM D2434 - Standard Testing Method for Permeability of Granular Soils (Constant Head)
  • ASTM D2487 - Standard Practice for Classification of Soils for Engineering Purposes (Unified Soil Classification System)
  • ASTM D2488 - Standard Practice for Description and Identification of Soils (Visual-Manual Procedures)
  • ASTM D3282 - Standard Practice for Classification of Soils and Soil-Aggregate Mixtures for Highway Construction Purposes
  • ASTM D3966 - Standard Testing Methods for Deep Foundations Under Lateral Load
  • ASTM D4380 - Standard Test Method for Determining Density of Construction Slurries
  • ASTM D4435 - Standard Test Method for Rock Bolt Anchor Pull Test
  • ASTM D4525 - Standard Test Method for Permeability of Rocks by Flowing Air
  • ASTM D4611 - Standard Test Method for Specific Heat of Rock and Soil
  • ASTM D4829 - Standard Test Method for Expansion Index of Soils
  • ASTM D4945 - Standard Testing Methods for High Strain Dynamic Testing for Deep Foundations
  • ASTM D4992 - Standard Practice for Evaluation of Rock to be Used for Erosion Control
  • ASTM D5718 - Standard Guide for Documenting a Groundwater Flow Model Application
  • ASTM D5882 - Standard Testing Methods for Low Strain Impact Integrity Testing for Deep Foundations
  • ASTM D5889 - Standard Practice for Quality Control of Geosynthetic Clay Layers
  • ASTM D6092 - Standard Practice for Specifying Standard Sizes on Stone for Erosion Control
  • ASTM D6128 - Standard Test Method for Shear Testing of Bulk Solids Using the Jenike Shear Tester
  • ASTM D6285 - Standard Guide for Locating Abandoned Wells
  • ASTM D6393 - Standard Test Method for Bulk Solids Characterization by Carr Indices
  • ASTM D6599 - Standard Practice for Construction of Live Fascines on Slopes
  • ASTM D6683 - Standard Test Method for Measuring Bulk Density Values of Powders and Other Bulk Solids as Function of Compressive Stress
  • ASTM D6773 - Standard Test Method for Bulk Solids Using Schulze Ring Shear Tester
  • ASTM D6825 - Standard Guide for Placement of Riprap Revetments
  • ASTM D6940 - Standard Practice for Measuring Sifting Segregation Tendencies of Bulk Solids
  • ASTM D6941 - Standard Practice for Determining Sediment Pond Skimmer Flow Rate
  • ASTM D7099 - Standard Terminology Related to Frozen Soil and Rock
  • ASTM D7407 - Standard Guide for Determinining the Transmission of Gases through Geomembranes
  • ASTM D7765 - Standard Practice for Use of Foundry Sand in Structural Fill and Embankments
  • ASTM D8326 - Standard Practice for Measuring of the Kinetic Energy of Simulated Rainfall

 

Geotechnical Engineering Glossary

A

  • Active fault  -  Is likely to have another earthquake sometime in the future.
  • Aftershock  -  Earthquakes that follow the largest shock of an earthquake sequence.
  • Aggregate  -  A mixture of sand and stone with the major component concrete.
  • Air content  -  The ratio of volume of air to total volume of soil.
  • Aquifer  -  A layer of rock or sediment that holds groundwater within.
  • Alluvium  -  Soil that has been transported to its present location by water.
  • Annual soil loss  -  Predicts the average annual soil loss by multiplying the factors listed below togeather.
  • Asphalt concrete  -  A hot mixture of asphalt cement, rubber, fine and coarse aggregate, and a mineral mixture.
  • Atterberg limits  -  The basic measure of the critical water contents of a fine-grained soil.  The water contents where the soil behavior changes are liquid limit, plastic limit, and shrinkage limit.

B

  • Basic types of rock  -  Igneous rock, Metamorphic rock, and Sedimentary rock.
  • Basin  -  The entire area drained by a main stream and its tributaries.
  • Bearing capacity  -  The maximum average load per unit area of a footing that will not produce failure by rupture of the supporting soil.
  • Bedrock  -  Relatively hard solid rock that commonly underlines softer rocks, or soils.
  • Borrow  -  Material taken from one location to be used in another.
  • Borrow pit  -  A bank or pit where earth is taken from for use as fill elsewhere.
  • Boulder  -  Fragments greater than 256 mm.
  • Branch  -  Small stream.
  • Brook  -  Small stream.
  • Bulk density  -  The ratio total weight of soil to the total volume of soil.
  • Buoyant unit weight  -  The unit weight of a submerged object minus saturated weight of the object.

C

  • Capillart water  -  Water that is under tension in a soil due to stresses produced by menisci forming in the soil pores as water recedes into the voids from evaporation or is lost other means.
  • Clay  -  Particles ranging in size from 0.002 mm and smaller.
  • Climate  -  Precipitation, temperature and other aspects of climate effect how specific soils are formed.
  • Coarse aggregate  -  Particles ranging in size greater than 4.75 mm.
  • Coarse sand  -  Particles ranging in size from 0.50 mm to 1.00 mm.
  • Cobble  -  Rock ranging in size from 65 mm to 256 mm.  Larger than a pebble and smaller than a boulder.
  • Cobblestone  -  Rounded or partially rounded stones used in paving roads and streets.
  • Colluvium  -  Soil that has been transported by gravety.
  • Collapsible soil  -  Low density soils that have considerable strength when dry of moist.
  • Compaction  -  Is rearranging the particles and reduce the voids and increase the density of the soil.
  • Compressibility  -  Measures the change in volume under external forces for any liquid.
  • Compression  -  Squeezing rocks togeather, causing rocks to fold or fracture.
  • Confined aquifer  -  Layers of impermeable rock or sediment that prevent water from seeping into the groundwater from above.
  • Confined stress  -  A deeply buried rock is pushed down by the weight of all the material above.  Since the rock cannot move, it cannot deform.
  • Consistancy limit  -  The water content at which the soil changes from one state to another state.
  • Creek  -  Small stream.
  • Creep  -  A slow and more or less continuous movement occuring on faults due to ongoing tectonic deformation.
  • Crest  -  Land that stands above or almost above surrounding terrain.
  • Crust  -  The outermost layer of the earth ranging from about 6 to 40 miles in thickness worldwide.

D

  • Darcy"s law  -  The rate at which a fluid flows through a permeable medium.
  • Density  -  The ratio of the amount of matter in an object compared to its volume.
  • Discharge velocity  -  The rate of water through a porous medium per unit of total area perpendicular to the direction of flow.
  • Displacement  -  The difference between the initial reference point position
  • and any later position.
  • Dry soil  -  Contains only air and voids.
  • Dry unit weight  -  The weight of soil to the volume of soil or when the soil voids are filled with air and no water. 
  • Ductile strain  -  A rock that does not go back to its origional state.  Remaines deformed when strain stops.

E

  • Earthquake  -  A sudden movement on a fault, and the resulting ground shaking, and radiated seismic energy caused by the slip.
  • Elastic modulus  -  The ratio of the stress applied to a body or substance to the resulting strain within the elastic limits.
  • Elastic strain  -  A rock that goes back to its origional state.
  • Emissivity  -  The surface depends on the material effectiveness in emitting energy as thermal radiation and varies between 0.0 and 1.0.
  • Erosion  -  The natural wearing away of the earth's surface by rainfall and surface runoff.

F

  • Falsic  -  Magmas that are rich in silica and aluminum.
  • Fault  -  A rock fracture showing evidence of relative movement.
  • Fault plane  -  A flat surface along which there is slipage during an earthquake.
  • Fine aggregate  -  Particles sand or crushed stone ranging in size less than 9.55 mm.
  • Fine sand  -  Particles ranging in size from 0.10 mm to 0.25 mm.
  • Footing  -  A structural member used to distribute the loads to the soil in such a way that the load bearing capacity of the soil is not exceded.
  • Foreshock  -  Relatively smaller earthquakes that precede the larger earthquake in a series.
  • Fractured  -  A rock that has broken abruptly into pieces.

G

  • Glacial till  -  Soil that has been gouged out of the earth's crust by ice at one location and deposited at another.
  • Gravitational water  -  Water that is free to move through a saturated soil mass under the influence of gravity.
  • Gravity  -  A force pulling togeather all matter.
  • Gravity wall  -  A retaining wall that depends upon its own weight for stability.
  • Ground failure  -  A general term referencing landslides, liquefaction, and lateral spreads.
  • Ground motion  -  Movement of the earth's surface from earthquakes or explosions.
  • Groundwater  -  Water that has traveled down from the top soil to fills the cracks and openings in the rocks and sand.
  • Gully  -  A channel from errosion during intersmittent and concentrated flow of water during heavy rain. 

H

  • Harmonic tremor  -  Continuous rhythmic earthquakes that can be detected by seismographs.
  • Head  -  The source of a stream.
  • Headwaters  -  The smallest streams that combine to make a larger stream.
  • Heat capacity  -  The ratio of heat transferred to raise the temperature of an object.
  • Horizontal stress  -  Stress acting in a horizontal direction.
  • Hydraulic gradient  -  A dimensionless number expressing the change in height (pressure) to length between any two points.

I

  • Igneous rock  -  Formed from the cooling and solidification of hot liquid magma.
  • Infiltration  -  Water movement in the soil.  Pore spaces in the soil allows water to infiltrate and percolate.
  • Intermediate rock  -  Between mafic and felsic rocks.
  • Interplate  -  Processes dbetween the earth's crustal plates.
  • Intraplate  -  The processes within the plates.
  • Irrigation  -  Applying water to crops by means of canals, ditches, pipes, sprinklers, etc. to meet their water requirements.
  • Isolated footing  -  A single stand alone footing used to support a structural load from a single column.

J

K

  • Kinetic energy  -  The energy in moving objects or mass.  If it moves, it has kinetic energy.

L

  • Landslide  -  A sudden and quick downhill mass movement of loose soil and rocks.
  • Latent heat  -  The energy absorbed or released by a substance during a constant temperature or phase change from a solid to liquid, liquid to gas or vise versa.
  • Lateral spread or flow  -  Landslides that commonly form on gentle slopes and that have rapid flow movement.
  • Leaching  -  The removal of material from soil and materials by the constant movement of water.
  • Liquefaction  -  When water-saturated sediment temporarily looses strength and acts like a fluid.
  • Liquid  -  A liquids molecules are close together with no particular pattern and continually move past each other, this allows it to flow and move about.  Having little space between the molecules leaves little room to compress.
  • Liquid index  -  Scaling the natural moisture content of a soil sample to the liquid limit and plastic limit.
  • Liquid limit  -  The minimum water content at which soil just begins to flow.
  • Locked fault  -  A fault that is not slipping because frictional resistance on the fault, it's stuck.

M

  • Magnitude  -  A number that represents the relative size of an earthquake.
  • Mafic  -  Magmas that are rich in iron, magnesium, and calcium.
  • Mantle  -  The earth's interior between the outer core and the crust, approximately 1,740 miles wide.
  • Marble  -  Result of heat and pressure imposed on limestone or dolostone.
  • Marsh  -  Wetlands that features permanent large areas of land with shallow bodies of water that include a large amount of grasses.
  • Mass flow rate  -  The average velocity of a mass that passes by a point.  In engineering, mass flow rate is often used, along with the conservation of mass to determine how much product moves through a pipe or duct.
  • Medium sand  -  Particles ranging in size from 0.25 mm to 0.50 mm.
  • Mediun texture soil  -  Very fine sandy loam, loam, silt loam, or silt.
  • Metamorphic rock  -  Started as some other type of rock, but has changed substantilly from its earlier metamorphic form.
  • Mineral  -  A naturally occuring inorganic element or compound having an orderly internal structure.
  • Moisture unit weight -  The total weight of soil per volume of soil or when the soil voids are filled with water and no air.
  • Mouth  -  A place where a stream enters another larger stream.
  • Mulch  -  An organic or inorganic material applied around plants or to the top of the soil.

N

  • Narrows  -  narrow part of a stream.
  • Neutral soil  -  Having a pH between 6.6 and 7.3.
  • Normal force  -  Always perpendicular to the surface it contacts and equal to the weight of the object.
  • Normal stress  -  Stress perpendicular to a given plane.

O

  • Oceanic trench  -  A linear depression of the sea floor.
  • Organic material  -  Decomposing animal and plant material.
  • Organic soil  -  Contains a high percentage of organic material.
  • Quartzite  -  Result from the deformation of sandstone.

P

  • Perched water table  -  The saturation point where the downward flow action in the soil is by the force of gravity.
  • Percolation  -  The downward movement of water through the soil, made possible by pore spaces in the soil.
  • Permeability  -  The quality of the soil to enable water to move downward through the soil.
  • Pier  -  A buried foundation normally cast in place rather than being forced into the ground.
  • Pile  -  A member of a deep foundation driven into the ground.
  • Plastic index  -  The range of water content over which the soil remains in the plastic state.
  • Plastic limit  -  The water content at which the soil changes from semi-solid state to solid state.

  • Plasticity of soil  -  The soils ability to undergo deformation without cracking of fracturing.  At this state the soil can be moulded into different shapes.
  • Plate tectonics  -  The earth's crust and upper mantle composed of several large, relatively thin rigid plates, that move relative to each other.
  • Ploughing  -  Turning the soil by mechanical cultivation of agricultural soils to a depth of 20 to 30 cm deep.
  • Poisson's ratio  -  The elastic ratio between lateral strain and longitudinal strain.
  • Ponding  -  Standing water on soil in a closed depression.
  • Pore air pressure  - The pressure of air within the void space of a saturated soil.
  • Pore pressure  -  The pressure exerted by the fluid within the pores or voids in a porous material.
  • Pore pressure coefficient  -  A ratio of pore pressure and normal stress at a certain point within a slope.
  • Pore pressure ratio  -  The ratio of pore water pressure to vertical over strained pressure at a given depth of soil.
  • Pore space  -  Spaces in the soil, between the mineral and organic matter, they are filled with air and water.
  • Porosity  -  A measure of a rocks and soil capacity to store fluids.
  • Post  -  A timber used in a vertical position.
  • Precipitation  -  Water that falls to earth from the atmosphere.
  • Pressure  -  The force exerted perpendicular to the surface of an object and is expressed as force per unit area.

Q

  • Quarry  -  An open pit where fill, gravel, minerals, sand, and/or stone is taken from.

R

  • Refraction  -  The bending, or deflection of the seismic wave path caused by its passage from one material to another having different elasstic properties.
  • Relative density  -  The density or ratio of any substance relative to another substance.
  • Richter scale  -  A mathematical device that compares the size of earthquakes.
  • Ring of fire  -  A zone of earthquakes surrounding the Pacific Ocean where about 90% of the world's earthquakes occur.
  • River  -  large stream.
  • Rock  -  An aggregate of one or more minerals.
  • Runoff  -  The water flow that occures on the ground surface when the soil is at full capacity from excess water from rainfall.
  • Runoff curve number  -  The water flow that occurs when the soil is infiltrated to full capacity and excess water or rain.

S

  • Sand  -  Soil particles ranging in size from 0.05 mm to 2 mm that do not shrink or swell when drying or wetting.
  • Sandstone  -  Rock composed of sand sized particles.
  • Saturated soil  -  Has its voids completely filled with water.
  • Saturated unit weight  -  The total weight of soil per volume of soil or when the soil voids are filled with water and no air.
  • Sediment  -  Solid material deposited or transported by ice, water, or wind.
  • Sedimentary rock  -  Formed from pre-existing rocks or pieces of once living organisms.
  • Seepage velocity  -  The actual velocity of a fluid flowing through the void spaces in the soil.
  • Seismic wave  -  An elastic wave generated by an impulse such as an earthquake or an explosion.
  • Shear  -  Pushes one side of the rock in one direction, and the other side of the rock in the opposite direction.
  • Shear strain  -  Opposing forces acting parrallel to the cross-section of a body.
  • Shear stress  - Tends to deform the material by breaking rather than stretching without changing the volume by restraining the object.
  • Shrinkage limit  -  The maximum water content at which further reduction in the water content will not cause decrease in volume of soil.
  • Silt  -  Particles ranging in size from 0.002 mm to 0.05 mm.
  • Silt clay  -  Particles ranging in size from 0.002 mm to 0.05 mm.
  • Slate  -  Fine-grained rock derived mainly from shale.
  • Slip rate  -  How fast two sides of a fault are slipping relative to one another.
  • Slope  -  The land surface is inclined from the horizonal plane.
  • Slump  -  The measure of consistancy of newly mixed concrete.
  • Soil  -  Sediments or other unconsolidated solid particles produced by the physical and chemical decay of rocks.
  • Soil solids  -  Mineral particles resulting from the physical decay of the parent rock.
  • Solid waste  -  Waste other than sewage, mostly solid material.
  • Span  -  The distance between supports.
  • Specific gravity  -  A dimensionless number, is the density or ratio of any substance to another substance.
  • Spring  -  A pool or other sourceof water that feeds a stream.
  • Storm water  -  Surface run off after a rainfall.
  • Strain  -  The deformation, stretched or compressed, of a material compared to its original length.
  • Stress  -  The force per unit area of cross-section.
  • Surface faulting  -  Displacement that reaches the earth's surface during slip along a fault.
  • Surface tension  -  The energy or force at the surface of a liquid that holds it together.
  • Surface wave  -  A seismic wave that is trapped near the surface of the earth.
  • Swamp  -  Wetlands that features permanent large areas of land with shallow bodies of water that include a large amount of trees.

T

  • Temperature gradient  -  Describes in which direction and what rate the temperature changes in a given area.
  • Tension  -  Rocks that are pulled apart, break apart, or lengthen under tension.
  • Terrace  -  A conservation practice for soil and water management to prevent rainfall runoff on sloping land from causing serious errosion.
  • Thrust fault  -  Raised fractures where the earth has mostly shifted vertically.
  • Tillage  -  Turning the soil by mechanical cultivation of agricultural soils to a depth of 20 to 30 cm deep.
  • Topsoil  -  The top layer of soil that contains most of the nutrients that normally occuring in the soil, usally between 2 to 10 inches.
  • Trace element  -  Naturally occuring elements found in small amounts in the soil.

U

  • Unconfined aquifer  -  Water that seeping into the groundwater from above.
  • Unit weight  -  The ratio of the total weight to the total volume.
  • United Soil Classification System (USCS)  -  A method for identifying and grouping soil.  Coarse grained, Fine grained, and Highly organic.  Only particles smaller than 3" are considered USCS.

V

  • Very coarse sand  -  Particles ranging in size from 1.00 mm to 2.00 mm.
  • Very fine sand  -  Particles ranging in size from 0.05 mm to 0.10 mm.
  • Void  -  Spaces between particles.
  • Void ratio  -  The ratio of the volume of voids to the volume of solids.
  • Volume  -  Is the space occupied by a mass.
  • Volume of voids  -  The ratio of total volume of soil minus volume of solid soil.

W

  • Water content  -  The ratio of weight of soil to the weight of water or the quantity of water contained in a material.
  • Waterlogged  -  Saturated with water
  • Water table  -  The underground boundary between the surface of the soil and the area where groundwater fills the cracks and openings in the rocks and sand.
  • Weathering  -  A breakdown in the chemical or physical changes in rocks or sediments at or near the earth's surface by atmospheric changes.

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Tags: Equations for Soil