LESSON 8: STONE WEATHERING Flashcards

1
Q

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

A

stone decay

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2
Q

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

A

morphology (of stone deterioration)

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3
Q

importance of morphology of stone deterioration

A

a.) diagnose possible causes and effects
b.) plan conservation strategies

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4
Q

weathering

A
  1. physical weathering
  2. chemical weathering
  3. biological weathering
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5
Q

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

A

physical weathering

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6
Q

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.

A

biogenic physical impact

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7
Q

changing temperature; temperature increases-rock (minerals) expands; decreases rocks (contracts)

A

thermal expansion and thermal compression

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8
Q

repeated cycle of ice formation and ice melt in the pore spaces and fractures of rocks; water freezes, volume increases by about 10%

A

frost disintegration.

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9
Q

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

A

salt crystallization

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10
Q

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

A

biogenic physical impact

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11
Q

weakening and subsequent disintegration of rock by chemical reactions; also known as decomposition or decay, is the breakdown of rock by chemical reaction

A

chemical weathering

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12
Q

the reaction of rock minerals with oxygen, changing the mineral composition of rocks

A

oxidation

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13
Q

process of rock minerals reacting with carbonic acid; carbonic acid dissolves or breaks down minerals in the rock

A

carbonation

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14
Q

chemical reaction caused by water changes the chemical composition and size of minerals in rock

A

hydrosis

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15
Q

absorption of water into the mineral structure

A

hydration

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16
Q

removal of water from rock or mineral structures

A

dehydration

17
Q

weakening and subsequent disintegration of rock by plants, animals, animals and microbes

A

biological weathering

18
Q

growing plant roots can exert stress or pressure on rock. although the process is physical, the pressure is exerted by a biological process

A

plant roots

19
Q

move rock and fragments to the surface, exposing the rock to more intense chemical, physical, and biological process. many animals such as piddock shells, bore into rocks for protection

A

burrowing animals

20
Q

breaks down rock minerals by altering the rock’s chemical composition, thus making it more susceptible to weathering

A

microbial activity

21
Q

chemical weathering

A
  1. oxidation
  2. carbonation
  3. hydrosis
  4. hydration
  5. dehydration
22
Q

biological weathering

A
  1. plant roots
  2. burrowing animals
  3. microbial activity