Fluid pressure gradients, arising from oscillations in intramedullary pressure, is correlated with the formation of bone and inhibition of intracortical porosity

Journal of Biomechanics

Volumn 36, Issue 10, 2003, Pages 1427-1437

  Qin, Yi Xian ^a   Kaplan, Tamara ^a   Saldanha, Anita ^a   Rubin, Clinton ^a  

^a STONY BROOK UNIVERSITY   (United States)

Author keywords

Adaptation; Bone fluid flow; Fluid shear stress; Intramedullary pressure; Osteoporosis; Permeability; Remodeling; Strain; Strain frequency; Stress

Indexed keywords

BONE; FLOW OF FLUIDS; OSCILLATIONS; POROSITY; SHEAR STRESS;

ADAPTIVE PROCESS;

BIOMECHANICS;

ANIMAL TISSUE; ARTICLE; BONE DEFORMATION; BONE DENSITY; BONE MARROW; BONE MASS; CONTROLLED STUDY; CORRELATION ANALYSIS; CORTICAL BONE; DIAPHYSIS; FLUID FLOW; INTERSTITIAL FLUID; MALE; NONHUMAN; OSCILLATION; OSSIFICATION; OSTEOLYSIS; OSTEOTOMY; PERIOSTEUM; POROSITY; PRIORITY JOURNAL; SHEAR STRESS; TISSUE PRESSURE; TURKEY (BIRD); ULNA; VELOCITY;

EID: 0141788762     PISSN: 00219290     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0021-9290(03)00127-1     Document Type: Article

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