| Literature DB >> 28771996 |
Pilar Junier1, Edith Joseph2,3.
Abstract
Microorganisms are the main engines of elemental cycling in this planet and therefore have a profound impact on both organic and mineral substrates. As such, past and present human-made structures and cultural heritage can be negatively affected by microbial activity. Processes such as bioweathering (rocks and minerals), biodeterioration (organic substrates) or biocorrosion (metals) participate to the degradation or structural damage of construction and heritage materials. This structural damage can cause major economic losses (e.g. replacement of cast-iron pipes in water distribution networks), and in the case of heritage materials, the entire loss of invaluable objects or monuments. Even though one can regard the influence of microbial activity on construction and heritage materials as negative, remarkably, the same metabolic pathways involved in degradation can be exploited to increase the stability of these materials.Entities:
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Year: 2017 PMID: 28771996 PMCID: PMC5609266 DOI: 10.1111/1751-7915.12795
Source DB: PubMed Journal: Microb Biotechnol ISSN: 1751-7915 Impact factor: 5.813
Microbial metabolisms and effect (negative or positive) on construction and cultural heritage materials
| Microbial metabolism | Negative effect | Positive effect |
|---|---|---|
| Sulfate reduction | Biocorrosion of iron and iron alloys (Dinh | Removal of black crust on stone artwork (Cappitelli |
| Iron reduction | Biocorrosion of iron and iron alloys (Schutz | Production of stable corrosion products via biogenic mineral precipitation (Cote |
| Oxalogenesis | Mineral dissolution and rock weathering (Gadd | Biological patination of metals (Joseph |
| Chemoorganotrophic respiration | Degradation of natural or synthetic carbon compounds | Carbonatogenesis in self‐healing concrete (Jonkers, |
| Removal of organic matter from frescoes (Ranalli | ||
| Redox reactions with metals | Discoloration and deterioration of stained glass. Alteration of pigments (Bastian | Biologically induced mineral formation (Cote |