LESSON 8 Flashcards
Importance of Morphology of Stone Deterioration
- diagnose possible causes and effects
- plan conservation strategies
types of weathering (deterioration of structures)
- physical weathering
- chemical weathering
- biological weathering
is the process that breaks rocks apart without changing their chemical composition
physical weathering
Physical weathering is the process that breaks rocks apart without changing their chemical composition and caused by factors such as:
- thermal expansion and thermal compression
- frost disintegration
- salt crystallization
- biogenic physical impact
(changing temperature; temperature increases-rock (minerals) expands; decreases rocks (contracts).
thermal expansion and thermal compression
(repeated cycle of ice formation and ice melt in the pore spaces and fractures of rocks; water freezes, volume increases by about 10%).
frost disintegration
(groundwater moves into empty pores of rock by capillary action; water evaporates, salt crystals grow and accumulate, putting pressure
on the rock; common in drier climates).
salt crystallization
(plants can grow in cracks; the pressure of a
confined growing root can make cracks in the rocks larger, and as roots grow they can break rocks apart)
biogenic physical impact
Weakening and subsequent disintegration of rock by chemical reactions; also known as decomposition or decay, is the breakdown of rock by chemical mechanisms.
chemical weathering
types of chemical weathering
- oxidation
- carbonation
- hydrosis
- hydration
- dehydration
(reaction of rock minerals with Oxygen, changing the mineral composition of the rocks)
oxidation
(process of rock minerals reacting with carbonic acid; carbonic acid dissolves or breaks down minerals in the rock)
carbonation
(chemical reaction caused by water changes the chemical composition and size of minerals in rock).
hydrosis
(absorption of water into the mineral structure)
hydration
(removal of water from rock or mineral structures)
dehydration