Since igneous rocks type at high temperatures, andunderpressure problems ranging native one to number of atmospheres.However,the conditions at the Earth"s surface room somewhat different than theconditionsat which most rocks and also minerals form. Therefore, the materialsareno much longer at equilibrium as soon as they are exposed come surfaceconditions.Under this conditions, over there is a tendency for all ordered solution toseek reduced levels of energy or order. This is all done throughweathering.

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Weathering - the disintegration anddecompositionof rock at or close to the surface of the earth. It affects the rocksin place and no deliver is involved. This distinguishesweatheringfrom erosion.

Mechanical/physical weathering - physicaldisintegrationof a rock right into smaller fragments, each with the very same properties as theoriginal. Occurs greatly by temperature and also pressure changes.

Chemical weathering - process by i m sorry theinternalstructure that a mineral is altered by the enhancement or remove ofelements.Change in step (mineral type) and composition are due to the activity ofchemical agents. Chemistry weathering is dependence on availablesurfacefor reaction temperature and presence that chemically activefluids.Smaller fragment sizes weather by chemical means more swiftly thanlargeparticles early out to an increase of surface ar area. Look at the diagrambelow and you will watch that together the particles obtain smaller, the totalsurfacearea obtainable for chemistry weathering increases.

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Erosion - the organization andtransportationof weathering commodities by a mobile certified dealer such as wind, water, ice.

All three processes may act independently, however willmoreoften 보다 not, happen simultaneously. Various circumstance willhave one weathering process an ext important 보다 another. Theprocessesmay also act in concert through one another.

Types of mechanically Weathering:
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Frost Wedging - water broadens when itfreezes.This photograph shows the individual layers in ~ the sedimentary rockbreaking personal through repeated cycles of freeze-thaw. A similarprocess happens as soon as the absent is continuously wetted and also dried together saltcrystalsdissolve indigenous the absent then flourish when that is dried. Both processescan an outcome in the rocks being heaved - for this reason what was as soon as a nice regularpattern that bricks set in a pavement will eventually come to be a chaoticjumbleof bricks oriented every i m sorry way. Thermal growth andContraction- heating causes rock to expand, cooling outcomes in contraction;differentminerals expand and contract at different rates. This phenomenawilllook very comparable to frost wedging and also salt decision growth, however willtypicallyhappen in climates that undergo too much diurnal temperature changes.
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Mechanical Exfoliation - rock breaksapart inlayers that are parallel come the earth"s surface; together rock is uncovered,it increases (due to the reduced confining pressure) result inexfoliation.The photo is indigenous G. K. Gilbert (1903) in Sequoia NationalPark.The granite boulder is shaped by exfoliation; the boulder is around 40feetin diameter, and the be separate fragment relaxing on the is around 10 feetthick. Exfoliation is an extremely common anytime plutonic igneous rocksare exposed. Since the plutonic rocks cool at depth under greatpressure,they basically de-pressurizes once the overburden is removed.Thiscauses sheets of rock to peel turn off subparallel to the earth"s surface,orwhatever is the least pressurized surface.
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In this photo from Yosemite nationwide Park,the exfoliationsheets are subparallel come the valley walls.
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Abrasion - physical grind of rockfragments.Here, the picture shows part pits that have actually been eroded right into the rock bysandblasting. In addition to the physics weathering (thesandblasting),chemical weathering has actually taken place as the rock reflects some indicators ofsolutionweathering as well.
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Another photo which mirrors the powerfuleffect ofwind generated abrasion is the dual Arch from arches NationalPark.The edges of the arcs have weathered along joints, preexistingtectonicallycontrolled upright surfaces in the rock. Climate mechanicalabrasiontook over and also carved the end the arches.

Types of chemical Weathering:

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Dissolution

H2O + CO2+ CaCO3 --> Ca+2+ 2HCO3- water + carbon dioxide + calcite dissolve intocalciumion and also bicarbonate ionDissolution is very common in locations that have actually a greatdealof limestone. Acidic waters (from contamination or natural) dissolvelimestone enabling for added water to gain entrance. Cancausesinkholes and also karst features as well as dissolution of statutes andgravestones.

Oxidation (rust)

4Fe+2 +3O2--> 2Fe2O3 ferrous iron + oxygen incorporate to form ferric ironoxide(hematite)

Will occur to every iron-bearing silicates tovarying degrees.Common reaction minerals space hematite, limonite, and goethite.

Hydrolysis2KAlSi3O8+ 3H20 --> Al2Si2O5(OH)4+ 4SiO2 + 2K(OH) potassium feldspar in acidic water hydrolyses tokaolinite+ quartz + potassium hydroxide

Silicate mineral (unstable at the earth"ssurface) weatherto form clay mineral such together kaolinite (stable in ~ the earth"ssurface).Feldspars commonly weather to produce clay minerals.

Factors that influence chemical weatheringClimateLiving organisms bioturbation acid production and also mineraldecompositionTimeMineral ingredient Goldich Dissolution series (Bowen"s Reaction Series)

Chemical Weathering assets Clays steels ores rounding of boulders (chemicalexfoliation)

Soils and Soil Formation

Dependence the weathering kind on the meantemperatureand yearly rainfall.

Weathering rates depend top top the ingredient of therock,temperature variety and rainfall amount. Weathering producessoils.Soils may or may not remain in place, and also any soil may be a combinationof residual and transported material.

Residual soil: continues to be in place; has not beentransported(gruss).

Transported soil: Transported by wind orwaterand deposited.

A finish soil file will have actually the followingcomponents:

O horizon: necessary debris and leaflitteron the surface.

A horizon: Topsoil - leaching, water movementdown, Organicand Mineral product transported downward.

B horizon: Subsoil - build-up of dissolvedmaterialand good clays, hardpan.

C horizon: Partially transformed parent absent material.

Bedrock: Unweathered parental rock material.

These horizons are not present in all floor profiles.In locations of rapid erosion, B & C may be current or C only. In someareas no floor profile will develop at all.

Factors in soil Formation

Climate: The better the rainfall amount,the morerapid the price of erosion and leaching. Laterites type in humidclimateswhere only Al2O3(Bauxite) and also Fe(OH)3 remain. Topography: The steeper the surface ar slope,the morelikely any kind of eroded product is to it is in transported out of the system. parental Material: Granites are an ext resistantto weatheringthan gabbros. Sandstones are much more resistant come weathering thanlimestonesin humid climates, yet limestones are an ext resistant than sandstones inarid climates. Plant and also Animal activity: Plant and also animalactivityproduces humic acids that are an effective erosion agents. Tree canphysically erode as well as chemically erode. Plants stabilizesoilprofiles, animals (including man) often tend to destabilize the soil profile,increasing erosion. Time: Reaction rates are slow, the longer arock unithas been exposed, the much more likely the is to be weathered.These components can it is in remembered by the acronym ClORPT -Climate,Organicactivity (plants and animals), Relief (topography),Parentmaterial, and also Time.

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Mineral stability

Sediments are the by-product of weathering.Sedimentsare particles of minerals, several of them changed from the initial rock,some simply lessened in sized, and some brand-new minerals by reaction.The security of minerals deserve to be predicted utilizing the Bowen"s reactionseries,however, in the situation of the weathering collection this is known as theGoldichDissolution Series:

Olivine

MgPyroxeneCalcic Plagioclase

Mg-CaPyroxeneCalcic-Alkalic Plagioclase

AmphiboleAlkalic-Calcic Plagioclase

Biotite Alkalic Plagioclase

Potassium Feldspar

Muscovite

Quartz

Minerals crystallize native a melt in ~ differenttemperaturesduring the migration and also emplacement the the magma. Those mineralsthat crystallize at higher temperatures will certainly be the the very least stable in ~ thesurface. Indigenous this the is evident that quartz will be the moststablemineral in the weathering environment, and also will be a dominantconstituentof sediments and sedimentary rocks.