7-8 Stone Decay & Weathering Flashcards

1
Q

It is a naturally occurring solid aggregate of one or more minerals (silicates and non-silicates).

A

Stone

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2
Q

It is usually used as a building material because of its great durability and superior artistic quality.

A

Stone

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3
Q

It is a branch of geology that studies the origin,
composition, distribution and structure of rocks

A

Petrology

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4
Q

It is a branch of petrology that focuses on detailed description of rocks (shape and cleavage relief).

A

Petrography

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5
Q

Causes of Stone Decay:

A
  1. Earthquake
  2. Fire
  3. Terrorism
  4. Vandalism
  5. Neglect
  6. Tourism
  7. Previous Treatment
  8. Wind
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6
Q

(Other Factors) Causes of Stone Decay:

A
  • Flood
  • Rain
  • Frost
  • Temperature Fluctuations
  • Chemical Attack
  • Salt Growth
  • Pollution
  • Bio-deterioration
  • Intrinsic Factors
  • Maintenance
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7
Q

This significantly contribute to masonry decay by causing structural damage, mortar deteriorations and foundation issues.

A

Earthquake

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8
Q

High temperatures during a this can cause chemical changes in masonry materials.

A

Fire

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9
Q

This contribute masonry decay by causing physical damage, exposing structures to harsh environmental conditions.

A

Terrorism

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10
Q

This action involving deliberate destruction of or damage to public or private property, is willful or malicious destruction or defacement of public or private property.

A

Vandalism

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11
Q

This pertains of failure to care for properly, to pay no attention or too little attention to; disregard.

A

Neglect

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12
Q

Heavy tourist traffic may lead to wear and tear of the concrete floor surface, pollution caused by increase vehicular traffic, vandalism and theft.

A

Tourism

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13
Q

The harmful intervention or prior restoration works.

A

Previous Treatment

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14
Q

These forces can break the building’s load path or punch a hole in the building envelope. Can even pick debris up and projects it against the building envelope.

A

Wind

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15
Q

The process that breaks rocks apart without changing their chemical composition.

A

Physical Weathering

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16
Q

Physical Weathering is caused by factors such as:

A
  1. Thermal expansion & compression
  2. Frost disintegration
  3. Salt crystallization
  4. Biogenic physical impact
17
Q

This factor in physical weathering means change in temperature where the rock expands when temperature is increases, and rock contracts when temperature is decreases.

A

Thermal expansion and compression

18
Q

This factor of physical weathering means 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

19
Q

This factor of physical weathering means groundwater moves into 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

20
Q

This factor of physical weathering means 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

21
Q

It is the weakening and subsequent disintegration of rock by chemical reactions; also known as decomposition or decay.

A

Chemical Weathering

22
Q

Chemical Weathering is caused by factors such as:

A
  1. Oxidation
  2. Carbonation
  3. Hydrosis
  4. Hydration
  5. Dehydration
23
Q

Reaction of rock minerals with Oxygen, changing the mineral composition of the rocks

24
Q

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

A

Carbonation

25
Chemical reaction caused by water changes the chemical composition and size of minerals in rock
Hydrosis
26
Absorption of water into the mineral structure
Hydration
27
Removal of water from rock or mineral structures
Dehydration
28
It is the weakening and subsequent disintegration or rock by plants, animals and microbes.
Biological Weathering
29
Factors of Biological Weathering:
1. Plant Roots 2. Burrowing Animals 3. Microbial Activity
30
Breaks down rock minerals by altering the rock’s chemical composition, thus making it more susceptible to weathering. An example of this is lichen (fungi and algae)
Microbial Activity
31
They move rock fragments to the surface, exposing the rock to more intense chemical, physical, and biological processes. Example of this are Piddock shells.
Burrowing animals
32
Growing plant roots can exert stress or pressure on rock. Although the process is physical, the pressure is exerted by a biological process
Plant Roots