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Principal Investigator: Christopher R. Jacobs, PhD Project Staff: Henry J. Donahue, PhD and R. Lane Smith, PhD Project Category: Bone & Joint and Osteoporosis - 2004 Objective: Bone cells occupy fluid filled voids (lacunae) in the mineralized matrix and interconnected by small tubes (canaliculi). As the bone matrix is cyclically loaded, fluid flows in the lacunar-canalicular network from regions of high matrix strain to low matrix strain and back in an oscillatory fashion. Although, it has been demonstrated that bone cells respond to steady and pulsatile fluid flow with a transient elevation in intracellular calcium concentration, increased release of paracrine factors, and increased gene transcription, our preliminary data indicate that these responses are fundamentally different from those observed for oscillating flow. Our central hypothesis is that oscillatory fluid flow in vivo provides an important mechanism of mechanotransduction, and furthermore shear stress level, frequency, time course, low-level steady flow, and cell morphology modulate the cellular response. Research Plan: This project is divided into four specific aims:
Work Accomplished: All of the work in the project has been completed. Five publications in peer-reviewed journals resulted from the project. A competing renewal application has been completed and is in review at the NIH. Expected Outcome: The long-term goal of these studies is to better understand the how mechanical loading influences the behavior of bone. Increased understanding of this relationship will lead to the identification of novel targets of therapeutic interventions in bone diseases with a mechanical component such as osteoporosis. Funding Source: NIH Funding Status: Active |
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