LESSON 8: STONE WEATHERING Flashcards
stone buildings and monuments from the cultural centers of many of the world’s urban areas. frequently these areas are prone to high levels of atmospheric pollution that promote a variety of aggressive stone decay process. severe threat to much to our cultural heritage
stone decay
a conservator or restorer needs to be able to identify the different types of stone deterioration or various physical manifestation of stone alteration and decay, measuring its extent, severity and rate
morphology (of stone deterioration)
importance of morphology of stone deterioration
a.) diagnose possible causes and effects
b.) plan conservation strategies
weathering
- physical weathering
- chemical weathering
- biological 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
physical weathering
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
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 reaction
chemical weathering
the reaction of rock minerals with oxygen, changing the mineral composition of 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