soil bacteria that precipitate calcium carbonate: mechanism and applications of the process

Clicks: 206
ID: 158830
2018
Article Quality & Performance Metrics
Overall Quality Improving Quality
0.0 /100
Combines engagement data with AI-assessed academic quality
AI Quality Assessment
Not analyzed
Abstract
Bacteria with ureasic activity are microorganisms found in soil that in presence of urea and calcium, they can produce calcium carbonate, a process known as microbiologically induced calcium carbonate precipitation (MICP). This article discusses this process and its mechanism, as well as bacterial urease, calcium carbonate crystals formed, and factors that affect the efficiency of MICP, as type of bacteria, bacterial cell concentrations, pH, temperature and calcium and urea concentrations. In addition, applications as removal of heavy metals in water, bioconsolidation, biocement and CO2 sequestration are also discussed.
Reference Key
chaparro-acua2018actasoil Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Sandra Patricia Chaparro-Acuña;Mónica Liliana Becerra-Jiménez;José Jobanny Martínez-Zambrano;Hugo Alfonso Rojas-Sarmiento
Journal Rapid communications in mass spectrometry : RCM
Year 2018
DOI 10.15446/acag.v67n2.66109
URL
Keywords

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.