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LIMESTONE: NATURAL OR INHERENT PROBLEMS

 

WEATHERING:
Limestone subjected to exterior exposures deteriorates due to weathering or the natural effects of wind, rain, and thermal change.  Limestone is extremely durable. It does, however, absorb water and, since it is a carbonate rock, it is highly reactive when
exposed to acids or even mildly acidic rain water, and it can suffer substantial deterioration.  The most common effect of weathering and erosion is loss of precise detail.

Little can be done to restore edge detailing short of re-carving the stone which is usually infeasible. 

EROSION:
Erosion can be the result of general weathering described above, or it can be a more localized phenomenon based upon handling or exposure.  Wind driven airborne abrasives may selectively wear away detailing on certain elevations, based upon the direction of
prevailing winds.  One of the few effective ways to address this problem is by landscaping where plantings and/or grade can deflect the wind.  Such landscaping and/or grading may range from the simple and inexpensive up to a major and expensive intervention. 

It would have to be consistent with appropriate policy for the management of cultural landscapes.  It may, however, be cost effective when considering the extended life of the marble.

The symptoms of erosion can be as simple as the loss of edge sharpness as described above, or it can be very localized, specific wear due to contact with landscaping and mowing equipment.

Localized damage due to contact by mowing or other maintenance equipment is preventable.  Where there is evidence of recurrent physical damage, steps should be taken to protect the resource(s). 

STAINING:
Discoloration of the limestone, whether general or localized, is staining.  Staining, may be the result of exposure to a variety of exterior substances or to internal occlusions in the stone or structural elements.

Some of the most common types of staining and the causative agents are:

1. Oil/grease stains:  These stains are usually the result of vandalism or use.  A variety of organic or inorganic oils may be absorbed into the stone upon contact.  The depth of
penetration will depend upon the viscosity of the oil/grease, temperature, stone porosity, finish and dryness.

The appearance of grease/oil stains will usually consist of a darkening of the stone at the area of contact.  The edges of the staining will generally be diffused, especially after an
extended period.  There are standard techniques for removing oil and grease stains.

For specific guidance on removing oil/grease stains from limestone, see 04455-10-R and 04455-11-R.

2. Dyes and inks:  The staining could be any color depending on the type and source of the dye.  This type of stain is likely to be extremely localized around the area of contact.  The liquid containing the coloration may be absorbed into the stone and during the normal process of evaporation, the coloring pigment is deposited in the stone. For specific guidance on removing ink and dye stains from limestone, see 04455-18-R.

3. Organic stains:  Organic stains are caused by direct contact with decomposing organic matter, such as leaves, bird or animal droppings, flowers, tea or coffee. Regardless of the
source these stains tend to be a slight reddish-brown in color.  They also frequently disappear after the source has been removed.  These stains may be left to weather and bleach or oxidize out after the removal of the organic source, however a residue may still remain on the stone. For specific guidance on removing organic stains from limestone, see 04455-14-R.

4. Metallic stains: Two major categories of metallic staining occur, they tend to be based  on either iron or copper. The source of the staining may be internal structural components or elements.  A major source is the water wash, or run-off, from adjacent metallic elements, especially bronze.

 a. Rust stains: These stains are reddish-orange and are caused by the oxidation (rusting) of iron. The source of iron staining is usually the structural or connecting
components.  These components are usually hidden and protected; however, water penetration from bad joints or cracks can activate or accelerate rusting.  The
discoloration may be within the stone or it may be a deposit of rust on the surface of the stone.  Surface deposits of rust may sometimes be removed by hand rubbing with a clean cloth.  The examination of the stain should include such rubbing to determine if it is only a surface deposit. For specific guidance on removing rust stains from limestone, see 04400-06-R.

b. Copper stains:  Stains from water run-off from bronze can range in color from a light green to a dark brown. The staining results from the dissolved copper salts (from          copper or bronze) which wash onto the stone, then oxidize. The pattern of the staining is likely to be localized, streaked and in the path of the run-off from the metallic source.      For specific guidance on removing copper stains from limestone, see 04400-07-R.



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