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- Q17157498 subject Q7353747.
- Q17157498 abstract "Microbiologically induced calcium carbonate precipitation (MICP) is a bio-geochemical process that induces calcium carbonate precipitation within the soil matrix. Biomineralization in the form of calcium carbonate precipitation can be traced back to the Precambrian period. Calcium carbonate can be precipitated in three polymorphic forms, which in the order of their usual stabilities are calcite, aragonite and vaterite. The main groups of microorganisms that can induce the carbonate precipitation are photosynthetic microorganisms such as cynobacteria and microalgae; sulfate-reducing bacteria; and some species of microorganisms involved in nitrogen cycle. Several mechanisms have been identified by which bacteria can induce the calcium carbonate precipitation, including urea hydrolysis, denitrification, sulphate production, and iron reduction. Two different pathways, or autotrophic and heterotrophic pathways, through which calcium carbonate is produced have been identified. There are three autotrophic pathways exist. However, all three pathways result in depletion of carbon dioxide and favouring calcium carbonate precipitation. In heterotrophic pathway, two metabolic cycles can be involved: the nitrogen cycle and the sulfur cycle. Several applications of this process have been proposed, such as remediation of cracks and corrosion prevention in concrete, biogrout, sequestration of radionuclides and heavy metals.".
- Q17157498 wikiPageExternalLink www.biomason.com.
- Q17157498 wikiPageWikiLink Q103910.
- Q17157498 wikiPageWikiLink Q10872.
- Q17157498 wikiPageWikiLink Q11474.
- Q17157498 wikiPageWikiLink Q11982.
- Q17157498 wikiPageWikiLink Q127418.
- Q17157498 wikiPageWikiLink Q131877.
- Q17157498 wikiPageWikiLink Q1361502.
- Q17157498 wikiPageWikiLink Q136560.
- Q17157498 wikiPageWikiLink Q171917.
- Q17157498 wikiPageWikiLink Q182168.
- Q17157498 wikiPageWikiLink Q189315.
- Q17157498 wikiPageWikiLink Q192900.
- Q17157498 wikiPageWikiLink Q19663458.
- Q17157498 wikiPageWikiLink Q19904193.
- Q17157498 wikiPageWikiLink Q23767.
- Q17157498 wikiPageWikiLink Q23775.
- Q17157498 wikiPageWikiLink Q29548.
- Q17157498 wikiPageWikiLink Q319827.
- Q17157498 wikiPageWikiLink Q4049396.
- Q17157498 wikiPageWikiLink Q412078.
- Q17157498 wikiPageWikiLink Q421362.
- Q17157498 wikiPageWikiLink Q48318.
- Q17157498 wikiPageWikiLink Q48743.
- Q17157498 wikiPageWikiLink Q589518.
- Q17157498 wikiPageWikiLink Q610457.
- Q17157498 wikiPageWikiLink Q648314.
- Q17157498 wikiPageWikiLink Q708.
- Q17157498 wikiPageWikiLink Q7353747.
- Q17157498 wikiPageWikiLink Q742637.
- Q17157498 wikiPageWikiLink Q82551.
- Q17157498 wikiPageWikiLink Q827291.
- Q17157498 wikiPageWikiLink Q93315.
- Q17157498 wikiPageWikiLink Q975983.
- Q17157498 comment "Microbiologically induced calcium carbonate precipitation (MICP) is a bio-geochemical process that induces calcium carbonate precipitation within the soil matrix. Biomineralization in the form of calcium carbonate precipitation can be traced back to the Precambrian period. Calcium carbonate can be precipitated in three polymorphic forms, which in the order of their usual stabilities are calcite, aragonite and vaterite.".
- Q17157498 label "Microbiologically induced calcite precipitation".