Biology subjects

Berzlanovich, A.

Publications and source records attributed to Berzlanovich, A..

3 recordsLinked to original sources

bioRxiv2025

Cement lines are stiffer and harder than bone but exhibit different mineral-mechanics relationships due to thicker and shorter mineral particles

The remarkable mechanical performance of bone arises from its complex hierarchical structure and from the presence of numerous internal interfaces joining the different components. Formed during bone remodeling, the cement line (CL) is a thin interface surrounding osteons. Although often neglected due to its small size, the CL has been suggested to play an important role in bone fracture toughness. However, there is an ongoing debate about its specific structure and mechanical behavior. Here, we investigate the composition-mechanics relationship at the CL and surrounding bone in human osteons using multiple methods in a correlative manner. We found that the CL is stiffer and harder than adjacent osteonal tissue. However, the CL requires more mineral than bone to attain the same stiffness and hardness. Analyzing the nanoscale properties of the mineral, we found thicker but shorter particles at the CL. Using a mechanical model, we interpreted the lower aspect ratio of the mineral particles as a less effective way to reinforce the collagen matrix. Casting our findings into a computational model, we questioned the possible protective role of the CL, which is not a soft interface as traditionally believed.

bioengineering↗

bioRxiv2024

The mineralization of osteonal cement line depends on where the osteon is formed

The cement line (CL) is a thin layer separating secondary osteons from interstitial bone and other osteons. It is assumed to play a significant role in bone fracture resistance, owing to its ability to deflect or arrest microcracks. Despite the possible role for bone quality, the CL is still one of the least understood microstructural features of bones, with unknowns on CL composition, mineralization, and mechanical properties. This study, focusing on CL mineralization, aims to elucidate the interplay between the mineral content of the CL and of adjacent bone tissue. Using quantitative backscattered electron imaging, osteons with different degrees of mineralization coming from human femoral samples were analyzed. We implemented a spatially resolved analysis of the mineral content in layers along the CL, considering both regions inside the osteon (i.e., formed soon after CL deposition) and outside (i.e., already present at the time of CL deposition). We found that the mineral content of the CL correlates strongly with the mineral content outside of the osteon, but not inside. Assuming the mineral content of the osteon as a proxy of its age, we demonstrate that not only the osteon, but also the CL increases its mineral content with time. However, the rate of increase is lower in the CL. Importantly, the specific value of the high initial mineral content of the CL depends on the mineral content of the local surrounding, in which the osteon was formed. Our findings highlight the central role of the local degree of mineralization of the bone around the osteon for building the CL.

bioengineering↗

bioRxiv2020

Three-dimensional interrelationship between osteocyte network and forming mineral during human bone remodeling

During bone remodeling, osteoblasts are known to deposit unmineralized collagenous tissue (osteoid), which mineralizes after some time lag. Some of the osteoblasts differentiate into osteocytes, forming a cell network within the lacunocanalicular network (LCN) of bone. To get more insight into the potential role of osteocytes in the mineralization process of osteoid, sites of bone formation were three-dimensionally imaged in nine forming human osteons using focused ion beam-scanning electron microscopy (FIB-SEM). In agreement with previous observations, the mineral concentration was found to gradually increase from the central Haversian canal towards preexisting mineralized bone. Most interestingly, a similar feature was discovered on a length scale more than 100-times smaller, whereby mineral concentration increased from the LCN, leaving around the canaliculi a zone virtually free of mineral, the size of which decreases with progressing mineralization. This suggests that the LCN controls mineral formation but not just by diffusion of mineralization precursors, which would lead to a continuous decrease of mineral concentration from the LCN. Our observation is, however, compatible with the codiffusion and reaction of precursors and inhibitors from the LCN into the bone matrix.

biophysics↗