LESSON 9: STONE DETORIATION PATTERNS GENERAL TERMS Flashcards

1
Q

modification of the material that does not necessarily imply a worsening of its characteristics from the point of view of conservation. for instance, a reversible coating applied on a stone may be considered

A

alteration

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2
Q

human perception of the loss of value due to decay

A

damage

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3
Q

chemical or physical modification of the intrinsic stone properties leading to loss of value or to impairment of use

A

decay

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4
Q

decline in condition, quality, or functional capacity

A

degradation

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5
Q

process of making or becoming worse or lower in quality, value, character, etc depreciation

A

deterioration

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6
Q

any chemical or mechanical process by which stones exposed to the weather undergo changes in character and deteriorate

A

weathering

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7
Q

individual fissure, clearly visible by the naked eye, resulting from separation of one part from another

A

crack (fissure)

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8
Q

crack subtypes:

A
  1. fracture
  2. star crack
  3. hair crack
  4. craquele
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9
Q

may be due to weathering, flaws in the stone, static problems, rusting dowels, too hard repointing mortar. vibrations caused by earth tremors, fire, frost, may also induce cracking

A

cracking

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10
Q

cracking should not be confused by this, which consists of detachment along bedding or schistosity planes, not necessarily oriented vertically.

A

delamination

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11
Q

in this, mechanical overload is not noticeable, transitional to splitting

A

delamination

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12
Q

change in shape without loosing integrity, leading to bending, buckling, or twisting of stone block

A

deformation

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13
Q

this degradation pattern mainly affects crystalline marble slabs (tombstones, marble cladding)

A

deformation

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14
Q

separated, air-filled, raised hemispherical elevations on the gface of stone resulting from the detachment of an outer stone layer. this detachment is not related to stone structure.

A

blistering

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15
Q

in some circumstances, is caused by soluble salts action

A

blistering

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16
Q

local loss of stone surface from internal pressure usually manifesting in the form of an irregularly sided crater

A

bursting (enclatement)

17
Q

sometimes preceded by star-shaped face fracturing. this deterioration pattern is due to the increase of volume of mineral inclusions (clay, iron minerals, etc.) naturally contained in the stone, and situated near its surface. the corrosion of metallic reinforcing elements may also induce.

A

bursting

18
Q

not to be confused by the term bursting, this term refers to loss of material due to a mechanical impact, which may have crater shape if the object hitting the stone surface is hard and small (a bullet for instance)

A

impact damage

19
Q

detachment process affecting laminated stones (most of sedimentary rocks, some metamorphic rocks), it corresponds to a physical separation into one or several layers following stone laminae. the thickness and shape of direction with regards to stone surface

A

delamination

20
Q

sub-type of delamination; detachment of multiple thin stone layers (cm scale) that are sub-parallel to the stone surface. the layers may bend, twist, in similar way as book pages

A

exfoliation

21
Q

not to be confused with delamination, it is the kind of detachment totally independent of the stone structure

A

scaling

22
Q

efflorescence’s and biological colonization can be detected in-between the laminae

A

delamination

23
Q

detachment of single grains or aggregates of grains

A

disintegration

24
Q

relationships of distintegration with the substrace:

A
  1. it affects only the surface of the stone or can occur in depth, damage usually starts from the surface of the material
  2. on crystalline marble, granular disintegration may reach several centimeters in depth, sometimes more
25
Q

sub-types of disintegration

A
  1. crumbling
  2. granular disintegration
  3. powdering, chalking
  4. sugaring
  5. sanding
26
Q

detachment of aggregates of grain from the subtrate. these aggregates are generally limited in size (less than 2cm). this size depends of the nature of stone and its environment

A

crumbling

27
Q

occurs in granular sedimentary (e.g. sandstone) and granular crystalline (e.g. granite) stones. granular disintegration produces debris referred to as rock meal and can often be seen accumulating at the foot of the wall actively deteriorating.

A

granular disintegration

28
Q

refers to size or corresponding grains, terms sometimes employed for describing granular disintegration of finely grained stones

A

powdering, chalking

29
Q

refers to size or corresponding grains, employed mainly for white crytalline marble

A

sugaring

30
Q

refers to size or corresponding grains, used to describe granular disintegration of sandstone and granite

A

sanding