Types of weathering Flashcards
types of mechanical weathering are (3)
- freeze thaw weathering
- salt crystallisation
- wetting and drying
freeze thaw weathering is when
- water enters cracks in the rock face and freeze, expanding in doing so and so putting stress on the rock fissure
- the water then melts, and the rock relaxes
- this repeated over time means pieces of rock fall off, and the rock below expands with the release of pressure, so forms new cracks
- this makes the new layer of rock susceptible to further weathering
salt crystallisation is when
salt from sea water forms crystals inside cracks when the water evaporates, building up pressure and expanding the cracks
wetting and drying is when
some permeable rocks such as clay expand when they absorb water and retract when dry, so form cracks which make it vulnerable to freeze thaw weathering and salt crystallisation
biological weatheirng is when
rock is broken down by plant or animal activity
three examples of biological weathering are:
- (shellfish)
- (algae and fungi)
- (roots)
- the piddock shellfish has a shell which drills into soft chalk rock and so weakens its structure
- algae and fungi can break down minerals and create solution, so ‘dissolving’ the rock surface
- plant roots exploit cracks int he rock and grow, so expanding the crack and weakening the structure
types of chemical weathering are (4)
- oxidation
- hydration
- hydrolysis
- carbonation
- oxidation is when
- and the rocks most affcted are
- when rocks disintegrate as oxygen dissolved in sea water reacts with minerals to produce hydroxides and oxides
- ferrous rocks are especially affected (iron rich)
hydration is when
when water is added to rock and the rock expands, forming cracks and then weakening the structure. permeable rocks such as limestone are most affected
hydrolysis is when
when midly acidic water reacts with rock, it creates dissolved clays and salts, which degrades parent rock and weakens it
carbonation is when
- when dissolved CO2 in rainwater forms weak carbonic acid (H2CO3).
- this reacts with rocks such as chalk or limestone to form bicarbonates which then dissolve easily in water, so are washed away.
what product of fossil fuel combustion adds to carbonation
sulphur dioxide and nitrogen dioxide