Biotrapping Ureolytic Bacteria on Sand to Improve the Efficiency of Biocementation.

Microbially induced calcium carbonate precipitation (MICP) has emerged as a novel technology with the potential to produce building materials through lower-temperature processes. The formation of calcium carbonate bridges in MICP allows the biocementation of aggregate particles to produce biobricks. Current approaches require several pulses of microbes and mineralization media to increase the quantity of calcium carbonate minerals and improve the strength of the material, thus leading to a reduction in sustainability. One potential technique to improve the efficiency of strength development involves trapping the bacteria on the aggregate surfaces using silane coupling agents such as positively charged 3-aminopropyl-methyl-diethoxysilane (APMDES). This treatment traps bacteria on sand through electrostatic interactions that attract negatively charged walls of bacteria to positively charged amine groups. The APMDES treatment promoted an abundant and immediate association of bacteria with sand, increasing the spatial density of ureolytic microbes on sand and promoting efficient initial calcium carbonate precipitation. Though microbial viability was compromised by treatment, urea hydrolysis was minimally affected. Strength was gained much more rapidly for the APMDES-treated sand than for the untreated sand. Three injections of bacteria and biomineralization media using APMDES-treated sand led to the same strength gain as seven injections using untreated sand. The higher strength with APMDES treatment was not explained by increased calcium carbonate accrual in the structure and may be influenced by additional factors such as differences in the microstructure of calcium carbonate bridges between sand particles. Overall, incorporating pretreatment methods, such as amine silane coupling agents, opens a new avenue in biomineralization research by producing materials with an improved efficiency and sustainability.

Aging decreases osteocyte lacunar-canalicular turnover in female C57BL/6 mice.

Osteocytes engage in bone resorption and mineralization surrounding their expansive lacunar-canalicular system (LCS) through LCS turnover. However, fundamental questions persist about where, when, and how often osteocytes engage in LCS turnover and how these processes change with aging. Furthermore, whether LCS turnover depends on tissue strain remains unexplored. To address these questions, we utilized confocal scanning microscopy, immunohistochemistry, and scanning electron microscopy to characterize osteocyte LCS turnover in the cortical (mid-diaphysis) and cancellous (metaphysis) femurs from young (5 mo) and early-old-age (22 mo) female C57BL/6JN mice. LCS bone mineralization was measured by the presence of perilacunar fluorochrome labels. LCS bone resorption was measured by immunohistochemical markers of bone resorption. The dynamics of LCS turnover were estimated from serial fluorochrome labeling, where each mouse was administered two labels between 2 days and 16 days before euthanasia. Osteocyte participation in mineralizing their surroundings is highly abundant in both cortical and cancellous bone of young adult mice but significantly decreases with aging. LCS bone resorption also decreases with aging. Aging has a greater impact on LCS turnover dynamics in cancellous bone than in cortical bone. Lacunae with recent LCS turnover have larger lacunae in both age groups. The impacts of aging on LCS turnover also varies with cortical region of interest and intracortical location, suggesting a dependence on tissue strain. The impact of aging on decreasing LCS turnover may have significant implications for bone quality and mechanosensation.