Rocks & Weathering Flashcards
Carbonation- solution
Rocks with calcium carbonate ie. Chalk, limestone
Rainfall combines with dissolved carbon dioxide or organic acid to form a weak carbonic acid
Hydrolysis
Occurs on rocks with orthoclase feldspar ie granite
Feldspar reacts with acid water and forms kaolin, silicic acid and potassium hydroxyl
Acid and hydroxyl removed leaving behind kaolin containing quartz and mica
Hydration
Certain minerals absorb water, expand and change
Oxidation
Occurs when iron compounds react with oxygen to produce a reddish- brown coating
Van’t Hoff’s Law
Rate of chemical weathering increases 2-3 times for every increase of temperature of 10*C
Chemical weathering increases with
Moisture and heat
Efficiency of freeze - thaw, salt crystallisation and insolation weathering is influenced by …
Critical temperature changes
Frequency of cycles
Seasonal variations in temperature
(4) Rock type influences weathering due to …
Chemical composition
Nature of cements in sedimentary rock
Joints and bedding planes
Grain size
Chemical weathering - 4
Carbonation - solution
Hydrolysis
Hydration
Oxidation
Process that affects limestone the most
Carbonation solution
Limestone features are best developed on carboniferous limestone because of
Greater strength
Low porosity
Lower permeability
(6) Amount and rate of limestone solution is affected by
Amount of CO2 in atmosphere, soil and groundwater
Amount of water in contact with limestone
Water temperature
Turbulence of water
Presence of organic acids
Presence of lead, iron sulphides, sodium or potassium
(6) Accelerated solution happens when …
Impermeable rocks join limestone Solution by rivers Solution by mixture (waters of different hardness mix) Margins of snow and ice fields Rainfall and runoff increase When limestone is under soil cover
Limestone pavements
Large areas of bare exposed limestone
Dolines
Large depressions formed by the solution or collapse of limestone