Origin of Salts: Difference between revisions

From Saltwiki
Jump to navigation Jump to search
No edit summary
 
(27 intermediate revisions by 5 users not shown)
Line 1: Line 1:
<bibimport/>
Author:[[user:Hschwarz|Hans-Jürgen Schwarz]]  
authors:[[user:Hschwarz|Hans-Jürgen Schwarz]]  
<br>
<br> <br>  
English Translation by [[user:SLeithaeuser|Sandra Leithäuser]]<br><br>  
Back to [[Fundamentals]] <br>  
Back to [[Fundamentals]] <br>
 
*[[Salts in building substrate and subsoils]] 
*[[Road salts - deicing salt]]
*[[Salts of microbiological origin]] 
*[[Salts Resulting from Restoration Materials]]
 


== Abstract  ==
== Abstract  ==
Salts that cause damage to wall paintings and cultural heritage made of stone, brick and other building materials, originate from natural sources or human activities. They are present in seawater, groundwater and even rainwater, as well as in soil or some stones, such as those in flood plains or near the sea. They may be part of the natural cycle of the chemical and physical deterioration of stone. Salts originating from human activities can be linked to emissions from burning fossil fuels, agricultural activities, salt or gun powder storage, some cements and the use of deicing salts. Salts are formed by the accumulation of ions in the wall or on the surface of specific parts of a building, e.g., plinths. The accumulation of ions can be due to soluble salts leaching out of building materials, soil, stone, wet or dry deposits from the atmosphere, but it can also be caused by the metabolism of micro-organisms or anthropogenic intervention.
The salts that cause damage to buildings, including wall paintings, and monuments made of stone, brick and other inorganic building materials, can originate from both natural sources or human activities. Natural sources are, for example, salts present in the ground on which the building stands. But they can also be present in the material itself, for example brick or some cements, depending on their manufacture; in stones near flood plains or from the natural stone weathering cycle. They can be brought in by sea spray and wind, for buildings in coastal areas and some microorganisms growing on building materials may generate some. Salts originating from human activities can be linked to emissions from burning fossil fuels, agricultural activities, automotive combustion engines and the use of deicing salts. Historic buildings may also have been used to store salt or gun powder, or even as stables  Over the years, salts will accumulate within or near the surface of the building as water evaporates. Since what migrates within the stone are the ions of the various salts present when water enters the porous system, the accumulation of ions upon water evaporation may result in the formation of different combinations of them,i.e., different salts to the ones entered the material originally.  


== Introduction  ==
== Introduction  ==
Every naturally occurring liquid water can be seen as a salt solution at different degrees of dilution. This can be established by simple measurement of its electrical conductivity. Porous building materials like stone, brick, mortar and plaster contain salts in their pore space. Wherever water flows through porous materials and evaporates from the surface, eventually some amount of salt efflorescence will be found.<br>
Every natural liquid water can be considered a more or less diluted salt solutions as confirmed by simple electrical conductivity measurements. When water enters porous building materials, such as stone, brick, mortar or plaster, salts will also enter their pore space. As water evaporates at the suface of these materials, salts will accumulate near that area and eventually, some salt efflorescence will result.<br>


Some salts or salt-forming ions are introduced into the monument by human activity. Apart from the historical storage of salt or gun powder, alkaline building materials like water glass or Portland cement, were used extensively in some countries over the last century. Some damages previously referred to as a result of acid rain are now known to be due to these building materials. <bib id="Klemm.etal:1999" /> [[Deicing salts]] should be added to the list of these materials, because they are still being used and they will affect mostly bridges, tunnels and foundations of buildings near roads. Other sources for damaging salts can be fertilisers and detergents that are introduced through ground and surface water.
Some salts are introduced into the buildings or monuments by human activity. These may result from the use of [[Salts in restoration materials|consolidants and/or cleaning agents]] such as alkaline materials, such as water glass [[Salts in building materials|building materials]]; some Portland cement in mortars, as well as historical use of the buildings for storage of salt or gun powder, or as stables. Some damages previously attributed to air pollution are now known to be due to the use of these materials <bib id="Klemm.etal:1999" />. [[Road salts - deicing salt| Deicing salts]] should be added to the list of these materials, especially since they are still in use mostly for roads, bridges and tunnels, affecting these structures and the foundations of buildings near them. Other sources for damaging salts can be fertilizers and some detergents that are introduced through ground and surface water. Finally, cleaning interventions based on the use of alkaline materials followed by an acid rinse, can leave soluble salts behind. This cleaning approach is mostly used for brick masonry in some countries, although there are records of their application on stone facades.  
    
    
All natural materials are contaminated with salt-forming ions, varying from low to very high levels. These include building materials, e.g., natural stone or brick, and binding agents, such as lime, cement and renders. The substratum, subsoil consistency, ground- and surface water also play a role <bib id="Roesch.etal:1993" />. Besides natural emissions by volcanoes ((H<sub>2</sub>S, HCl, HF, SO<sub>2</sub> etc.) and sea- water aerosols (NaCl etc.), <bib id=Steiger.etal:1994b/><bib id=Steiger.etal:1997/><bib id=Steiger.etal:2002/><bib id=Becker.etal:2005/>, anthropogenic emissions are becoming more important.
Many building materials are contaminated with salt-forming ions, varying from low to high concentrations. These can include natural stone or man-made ones, such as brick, lime, cement and mortars. The [[Building substrate and subsoils| soil substrate and subsoil consistency]], as well as the ground- and surface water contribute to this contamination  <bib id="Roesch.etal:1993" />. So do natural emissions by volcanoes ((H<sub>2</sub>S, HCl, HF, SO<sub>2</sub> etc.) and sea- water aerosols (mostly NaCl but other salts as well), <bib id="Steiger.etal:1994b"/><bib id="Steiger.etal:1997"/><bib id="Steiger.etal:2002"/><bib id="Becker.etal:2005"/>, but anthropogenic activities are becoming the most important contributors to salt contamination.  


The generation of natural resources and energy, emissions from traffic and so forth, produce a great number of damaging substances, of which sulphur dioxide (with the secondary product sulphate)<bib id=Wittenburg.etal:1993/> and nitrogen oxides (with the secondary product nitrate), are the most familiar. It is still not fully understood, how ozone (O3) and the large number of organic compounds participate in the destruction of cultural goods. Immissions mostly reach the objects through dry or wet deposition <bib id=Steiger.etal:1989/>  by rainwater or fog, but also through accumulation in the subsoil.
Among these are the industrial and traffic emissions, which produce a great number of aggressive substances, such as sulfur dioxide (at the origin of sulfates) <bib id="Wittenburg.etal:1993"/> and nitrogen oxides (originating nitrates), are the most common ones. It is still not fully understood, how ozone (O3) and the large number of organic compounds released participate in the deteroration mechanism of building materials. [[Immissions]] mostly reach the objects through dry or wet deposition <bib id="Steiger.etal:1989"/>  by rainwater or fog, but also through accumulation in the subsoil.


Nitrates and organic salts such as oxalates mostly have a microbiological origin. While nitrates are transported into the object by humidity, oxalates are usually formed in situ, where they remain due to their low solubility.
Nitrates and organic salts such as oxalates mostly are of [[microbiological origin]]. While nitrates are transported into the object by humidity, calcium oxalates are usually formed in situ by microorganisms, where they remain due to their low solubility.


== Literature ==
== Literature ==
<bibprint />
<biblist/>


[[Category:Origin of Salt]] [[Category:InProgress]]
[[Category:Origin of Salt]] [[Category:approved]][[category: Schwarz,Hans-Jürgen]]

Latest revision as of 14:57, 17 November 2022

Author:Hans-Jürgen Schwarz
English Translation by Sandra Leithäuser

Back to Fundamentals


Abstract[edit]

The salts that cause damage to buildings, including wall paintings, and monuments made of stone, brick and other inorganic building materials, can originate from both natural sources or human activities. Natural sources are, for example, salts present in the ground on which the building stands. But they can also be present in the material itself, for example brick or some cements, depending on their manufacture; in stones near flood plains or from the natural stone weathering cycle. They can be brought in by sea spray and wind, for buildings in coastal areas and some microorganisms growing on building materials may generate some. Salts originating from human activities can be linked to emissions from burning fossil fuels, agricultural activities, automotive combustion engines and the use of deicing salts. Historic buildings may also have been used to store salt or gun powder, or even as stables Over the years, salts will accumulate within or near the surface of the building as water evaporates. Since what migrates within the stone are the ions of the various salts present when water enters the porous system, the accumulation of ions upon water evaporation may result in the formation of different combinations of them,i.e., different salts to the ones entered the material originally.

Introduction[edit]

Every natural liquid water can be considered a more or less diluted salt solutions as confirmed by simple electrical conductivity measurements. When water enters porous building materials, such as stone, brick, mortar or plaster, salts will also enter their pore space. As water evaporates at the suface of these materials, salts will accumulate near that area and eventually, some salt efflorescence will result.

Some salts are introduced into the buildings or monuments by human activity. These may result from the use of consolidants and/or cleaning agents such as alkaline materials, such as water glass building materials; some Portland cement in mortars, as well as historical use of the buildings for storage of salt or gun powder, or as stables. Some damages previously attributed to air pollution are now known to be due to the use of these materials [Klemm.etal:1999]Title: Schwefelisotopenanalyse von bauschädlichen Sulfatsalzen an historischen Bauwerken
Author: Klemm, Werner; Siedel, Heiner
Link to Google Scholar. Deicing salts should be added to the list of these materials, especially since they are still in use mostly for roads, bridges and tunnels, affecting these structures and the foundations of buildings near them. Other sources for damaging salts can be fertilizers and some detergents that are introduced through ground and surface water. Finally, cleaning interventions based on the use of alkaline materials followed by an acid rinse, can leave soluble salts behind. This cleaning approach is mostly used for brick masonry in some countries, although there are records of their application on stone facades.

Many building materials are contaminated with salt-forming ions, varying from low to high concentrations. These can include natural stone or man-made ones, such as brick, lime, cement and mortars. The soil substrate and subsoil consistency, as well as the ground- and surface water contribute to this contamination [Roesch.etal:1993]Title: Damage to Frescoes caused by sulphate-bearing salts: Where does the salt come from?
Author: Rösch, Heinrich; Schwarz, Hans-Jürgen
Link to Google Scholar. So do natural emissions by volcanoes ((H2S, HCl, HF, SO2 etc.) and sea- water aerosols (mostly NaCl but other salts as well), [Steiger.etal:1994b]Title: Determination of wet and dry depostion of atmospheric pollutants on building stones by field exposure experiments
Author: Steiger, Michael; Dannecker, Walter
Link to Google Scholar[Steiger.etal:1997]Title: Sea Salt in Historic Buildings: Deposition, Transport and Accumulation
Author: Steiger, Michael; Behlen, Andreas; Neumann, Hans-Herrmann; Willers, U.; Wittenburg, Christian
Link to Google Scholar[Steiger.etal:2002]Title: Immissionsbelastung durch salzbildende Stoffe und Wirkung auf mineralische Baustoffe
Author: Steiger, Michael; Behlen, Andreas; Wiese, Utz
Link to Google Scholar[Becker.etal:2005]Title: Luftschadstoffe und Natursteinschäden
Author: Becker, Karl-Heinz; Brüggerhoff, Stefan; Steiger, Michael; Warscheid, Thomas
Link to Google Scholar, but anthropogenic activities are becoming the most important contributors to salt contamination.

Among these are the industrial and traffic emissions, which produce a great number of aggressive substances, such as sulfur dioxide (at the origin of sulfates) [Wittenburg.etal:1993]Title: Ein Vergleich von Schwefeldioxid-Depositionsgeschwindigkeiten auf Naturwerksteine aus verschiedenen experimentellen Ansätzen (Comparison of sulfur dioxide deposition velocities on building stones from different experiments)
Author: Wittenburg, Christian; Mangels, Henning; Wolf, Falk; Steiger, Michael; Bothmann, Thomas; Dannecker, Walter
Link to Google Scholar and nitrogen oxides (originating nitrates), are the most common ones. It is still not fully understood, how ozone (O3) and the large number of organic compounds released participate in the deteroration mechanism of building materials. Immissions mostly reach the objects through dry or wet deposition [Steiger.etal:1989]Title: Variability of aerosol size distributions above the North Sea and its implication to dry deposition estimates
Author: Steiger, Michael; Schulz, Michael; Schwikowski, Margit; Naumann, K.; Dannecker, Walter
Link to Google Scholar by rainwater or fog, but also through accumulation in the subsoil.

Nitrates and organic salts such as oxalates mostly are of microbiological origin. While nitrates are transported into the object by humidity, calcium oxalates are usually formed in situ by microorganisms, where they remain due to their low solubility.

Literature[edit]

[Becker.etal:2005]Becker, Karl-Heinz; Brüggerhoff, Stefan; Steiger, Michael; Warscheid, Thomas (2005): Luftschadstoffe und Natursteinschäden. In: Siegesmund, Siegfried; Auras, Michael; Snethlage, Rolf (eds.): STEIN. Zerfall und Konservierung, Edition Leipzig, 35-45.Link to Google Scholar
[Klemm.etal:1999] Klemm, Werner; Siedel, Heiner (1999): Schwefelisotopenanalyse von bauschädlichen Sulfatsalzen an historischen Bauwerken, Wiss. Mitt. Inst. Geol. TU Bergakademie FreibergLink to Google Scholar
[Roesch.etal:1993]Rösch, Heinrich; Schwarz, Hans-Jürgen (1993): Damage to Frescoes caused by sulphate-bearing salts: Where does the salt come from?. In: Studies in Conservation, 38 (4), 224-230, UrlLink to Google ScholarFulltext link
[Steiger.etal:1989]Steiger, Michael; Schulz, Michael; Schwikowski, Margit; Naumann, K.; Dannecker, Walter (1989): Variability of aerosol size distributions above the North Sea and its implication to dry deposition estimates. In: Journal of Aerosol Science, 20 (8), 1229-1232Link to Google Scholar
[Steiger.etal:1994b]Steiger, Michael; Dannecker, Walter (1994): Determination of wet and dry depostion of atmospheric pollutants on building stones by field exposure experiments. In: Zezza, Fulvio; Ott, Heinrich; Fassina, Vasco (eds.): The conservation of monuments in the Mediterranean Bassin: Stone and Monuments: Methodologies for the Analyses of Weathering and Conservation, , proceedings of the 3rd international symposium, Venice, 22-25 June 1994, , 171-178.Link to Google Scholar
[Steiger.etal:1997]Steiger, Michael; Behlen, Andreas; Neumann, Hans-Herrmann; Willers, U.; Wittenburg, Christian (1997): Sea Salt in Historic Buildings: Deposition, Transport and Accumulation. In: Moropoulou, A.; Zezza, F.; Kollias, E.; Papachristodoulou, I. (eds.): 4th International Symposium on the Conservation of Monuments in the Mediterranean - Proceedings, , 325-335.Link to Google Scholar
[Steiger.etal:2002]Steiger, Michael; Behlen, Andreas; Wiese, Utz (2002): Immissionsbelastung durch salzbildende Stoffe und Wirkung auf mineralische Baustoffe. In: Institut für Steinkonservierung Mainz (eds.): Salze im historischen Mauerwerk, IFS, Mainz, 1-10.Link to Google ScholarFulltext link
[Wittenburg.etal:1993]Wittenburg, Christian; Mangels, Henning; Wolf, Falk; Steiger, Michael; Bothmann, Thomas; Dannecker, Walter (1993): Ein Vergleich von Schwefeldioxid-Depositionsgeschwindigkeiten auf Naturwerksteine aus verschiedenen experimentellen Ansätzen (Comparison of sulfur dioxide deposition velocities on building stones from different experiments). In:: VDI-Berichte 1060 (Materialien in ihrer Umwelt), , 383-392.Link to Google Scholar

crystallization of a dissolved salt

Water glass is the common name for a liquid solution of alkaline silicates, also known as Sodium silicate Na2SiO3 or liquid glass.

Retrieved from "https://saltwiki.net/index.php?title=Origin_of_Salts&oldid=7042"