Talk:Salts of microbiological origin: Difference between revisions

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Author: [[Benutzer:Hschwarz|Hans-Jürgen Schwarz]]
<br> back to [[Origin of salts]]


== Abstract ==
Microbial organisms produce a significant number of organic and inorganic acids. On Objects, they can transform into damaging salts.
== Introduction ==
The metabolism of microorganisms as well as higher organisms, produces acids and salts, which are excreted and can accumulate in buildings or in their proximity. The biogenic sourceof nitrate as a result of livestock has long be established. However, nitrate is also produced by microorganisms. Furthermore, a large number of other organic acids can be detected, particularly oxalates like calcium oxalate ([[whedellite]]) which has been found on wall paintings. The presence of oxalates, i.e. the salts of oxalic acids, is an indication for microbial activity.
Microorganisms, particularly bacteria, are morphologically similar to one another, but display a very distinct metabolically-physical variance in comparison to higher organisms. A group of widely occuring bacteria, which grow chemo-lithoautotrophically, i. e with reduced inorganic compounds or ions as hydrogen or electron donors. These include:
*[[ammonium]] oxidants, oxidize ammonium into nitrite
*nitrite oxidants, oxidize nitrite into nitrate
Ammonia and nitrite oxidants are combined into the group of nitrifiers. At the present time, the majority of ammonia comes from intensive livestock farming.
Apart from the above mentioned bacteria, sulfur oxidizing bacteria from the genus thiobacillus are widely distributed. These organisms grow lithoautotophically, as well, and they can oxidize reduced sulfur compounds such as sulfides, molecular sulfur or thiosulfate into [[sulfate]].
== Literature ==
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[[Category:SalzHerkunft]][[Category:Mikrobiologie]] [[Category:Schwarz,Hans-Jürgen]] [[Category:R-HSiedel]] [[Category:R-SLaue]] [[Category:Bearbeitung]]

Latest revision as of 15:32, 6 September 2012

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