In the model (a), mechanical strain (ε(t)) at the location of the osteocytic cell induced an influx of Ca2+ ions (via a relation between ε(t) and model parameter Tεx, the threshold strain magnitude at which maximal Ca2+ oscillation amplitudes are induced). Additional Ca2+ influx was modeled to occur via gap-junctional (GJ) influx of Ca2+ ions from physically connected neighboring cells (a). The filling state of the ER (that was replenished at a parameterized maximal rate, R0) and the influx-induced release of Ca2+ ions from the ER (with a parameterized maximal store capacity, ER0) modulated the Ca2+ oscillations that arose at any given time within osteocytes and precursor cells (a). In precursor cells, NFAT dephosphorylation was influenced by prior Ca2+ oscillation histories (via a relation controlled by the parameter, α). Dephosphorylated NFAT translocated to the nucleus and upon DNA binding, controlled relative mineral apposition rates in differentiated osteoblasts (via a relationship defined by parameters NFATnx, the maximal NFAT DNA binding capacity, and r.MARx, the maximal relative mineral apposition rate, a). To implement the model in idealized representations of bone cell networks in situ, thin cross-sections from the mid-shaft tibiae of young (4 Mo; top panel, b) and senescent female C57BL/6 mice (22 Mo; bottom panel, b) were imaged. Osteocyte (‘asterisk’) and surface precursor cell (‘diamond’) locations within the cortex were determined from imaging and specified for model representation of cell networks in young (top panel, c) and aged animals (bottom panel, c). Finally, based upon literature, cell-cell functional connections were specified for young (top panel, d) and aged models (bottom panel, d).