Salt Data: Difference between revisions

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=== Chlorides  ===
=== Chlorides  ===


Die Chloride der Alkalien und Erdalkalien bilden alle ausgeprägt ionare Verbindungen. Da die Kationen eine niedrige Ladung und einen relativ großen Ionenradius haben, ist ihre polarisierende Wirkung auf die Chloridionen gering. Die Folge ist, dass diese Minerale meist farblos und durchsichtig sind. Weitere gemeinsame Eigenschaften sind die niedrige Lichtbrechung, Glasglanz sowie geringe Dichte. Die Chloride, insbesondere die der Alkalien, sind sehr leicht in Wasser löslich. Im Unterschied hierzu sind die Fluoride schwer löslich. Dies ist auf die relativ geringe Größe des Fluoridions (1.33 Å), und damit die andersartige Koordination der Fluoride im Kristallgitter zurückzuführen.<br>  
The chlorides of the alkali and alkaline earth metals are all pronounced ionare compounds. Since the cations have a low charge and a relatively large ionic radius, their polarizing effect is small on the chloride ions. The result is that these minerals are usually colorless and transparent. Other common features are the low refractive index and low density. The chlorides, especially those of the alkalis are very soluble in water. In contrast, the fluorides are sparingly soluble. This is due to the relatively small size of the fluoride ion (1.33 Å), and thus due to other types of coordination of the fluoride in the crystal lattice.<br>  


to the [[Chloride|Chlorides]]  
to the [[Chloride|Chlorides]]  
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=== More Salts  ===
=== More Salts  ===


to the [[Weitere anorganische Salze|anderen anorganischen Salzen]]  
to the [[more inorganic salts|other inorganic salts]]  


=== Salze mit "organischen" Anionen ===
=== Salts with "organic" anions ===


Salze mit organischen Säurerestanionen spielen in ganz speziellen Bereichen eine größere Rolle. Zu nennen sind hier vor allem die Acetate, die in Museumsvitrinen ein Hauptschadensfaktor sein können.
Salts with organic acid residue anions play in very specific areas a greater role. These are, especially the acetates, which may be in museum showcases a major damaging factor.


[[Organische Salze|Salze mit "organischen" Anionen]]
[[Organische Salze|Salze mit "organischen" Anionen]]


== Metallsalze ==
== Metal Salts ==


Metallsalze der Übergangsmetalle verursachen aufgrund ihrer Farbigkeit oft eine Verfärbung an Baumaterialien. Ihr wichtigtsen Vorkommen sind jedoch metallische Bauteile, Skulpturen, etc., die aufgrund der Umweltbelastung und durch Reaktion mit in der Atmosphäre enthaltenene Reagenzien zu Salzen führen können. Oft handelt es sich dabei um Carbonate oder Sulfate.
Metallsalze der Übergangsmetalle verursachen aufgrund ihrer Farbigkeit oft eine Verfärbung an Baumaterialien. Ihr wichtigtsen Vorkommen sind jedoch metallische Bauteile, Skulpturen, etc., die aufgrund der Umweltbelastung und durch Reaktion mit in der Atmosphäre enthaltenene Reagenzien zu Salzen führen können. Oft handelt es sich dabei um Carbonate oder Sulfate.

Revision as of 14:30, 1 June 2011

<bibimport/> Author:Hans-Jürgen Schwarz
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Abstract[edit]

All necessary data, graphics and images for the identification and characterization of a salt are presented. The structure of the salt systems is subject to the major anions.

The Salts[edit]

Here you will find a general overview of the salts. If you need detail information, please go to the pages of the individual salts. Recent reviews on salt and salt damage can be found at [Leitner.etal:2003]Title: Mauersalze und Architekturoberflächen
Link to Google Scholar and [Steiger.etal:2007]Title: Special issue on salt decay
Link to Google Scholar

Carbonates[edit]

The carbonates are salts of the "carbonic acid"(H 2 CO 3 ). The main structural element is the planar complex anion [CO 3 ] 2 - . The carbonates have a number of characteristics that distinguish them well from other minerals / salts. The most important characteristic is that they all decompose more or less easily under CO 2 when treated with acids. The alkali and alkali earth carbonate salts are colourless. Most of the other carbonates are usually coloured pale, only the heavy metal carbonates can show strong colours (such as azurite). Noteworthy is the extremely high birefringence of the carbonates, which leads to higher order interference colours. Under thermal treatment the carbonates dissociate mostly at temperatures between 500-900 °C. The solubility in water is relatively good, especially in carbonated water.

to the Carbonates

Nitrates[edit]

Biogenic reactions are a major source of nitrates with the [NO 3] - ion . This usually takes place with the help of bacteria, also nitrogen-containing raw materials such as animal waste, manure and other organic substances may play a role. Nearly all nitrates are soluble in water. The nitrates have remarkable structural similarities with the carbonates; characteristic is the isotypy (same crystal structure) between nitronatrite /calcite and aragonite /niter.

to the Nitrates


Literature[edit]

[Filter missing]

an atom or molecule with a negative electrical charge.

the mathematical difference between the largest and smallest refractive index for an anisotropic mineral

In physics, interference is the addition of two or more waves that results in a new wave pattern. The colours are produced by the difference in speed in the fast and slow rays. Minerals have specific and predictable colours in cross-polarized light, and this can help identify them.

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