Rocks and Weathering Flashcards
weathering
the decomposition and disintegration of rocks in situ
decomposition
chemical weathering that creates altered rock substances
disintegration
mechanical weathering that produces smaller, angular fragments of the same rock
biological weathering
plants and animals chemically alter and physically break rocks through their growth and movement - not a separate type of weathering but a form of disintegration and decomposition
erosion
wearing away of soil and rock particles that are moved elsewhere by a transport agent
3 types of weathering
mechanical
chemical
biological
oxidation
rocks exposed to air, ferrous soil oxidises and changes to ferric state
rocks exposed by digging, attrition, plate movement, bio. weathering
oxidation equ.
4Fe + O2 –> 2Fe2O3
carbonation-solution
calcium carbonate reacts with acid water, forming calcium bicarbonate which is soluble and is removed by percolating water
carbonation-solution equ.
CO2 + H2O → H2CO3
carbonation-solution conditions
rocks containing calcium carbonate - eg. limestone, generally warmer wetter climates, rainfall combines with CO2 to form a weak carbonic acid-higher pH = more effective
hydrolysis
chemical breakdown of a substance when combined with water
hydration
certain minerals in the rock absorb water, expand and change, causing mechanical stresses also
hydration conditions
water absorbed into rocks - porous/cracked rocks make it more effective
freeze-thaw
water seeps into crack in the rock, freezes, expands, pushing crack open wider, thaws and water fills the crack further, repeating the process, over time breaking the rock