Blood and interstitial fluid have many functions in a bone. They transport nutrients to, and carry waste from, the bone cells (osteocytes) buried in the bony matrix. They are involved in the transport of minerals to the bone tissue for storage and the retrieval of those minerals when the body needs them. Interstitial flow is considered to have a role in bone's mechanosensory system. Bone deformation causes the interstitial flow over the cell processes of the osteocyte creating a drag on the fibers that connect the cell; the drag force created by the flowing interstitial fluid is sensed by the cell [1][2][3][4]. A full physiological understanding of this mechanosensory system will provide insight into the following three important clinical problems: (i) how to maintain the long-term stability of bone implants, (ii) the physiological mechanism underlying osteoporosis, and (iii) how to maintain bones in long-duration space flights and long-term bed rest.Since one purpose of this work is to describe how these fluid systems work, consideration is limited to cortical bone in the mid-diaphysis of a long bone.Although most of what is described is also applicable to the bone tissue at other anatomical sites, the discussion is more concise and direct if this limitation is stipulated.The majority of the motive force for the blood flow is from the heart, but the contraction of muscles attached to the bone and the mechanical loading of bone also contribute to this motive force. The majority of the motive force for the interstitial fluid flow is due to the mechanical loading of bone, but the contraction of muscles attached to bone and the heart also supply some of its motive force. The influence of the mechanical loading of a whole bone on the fluid system's maintenance of the bone tissue is critical. The fluid flow resulting from the mechanical loading is modeled by the theory of poroelasticity. This theory models the interaction of deformation and fluid flow in a fluid-saturated porous medium. The theory was proposed by Biot [5, 6] as a theoretical extension of soil consolidation models developed to calculate the settlement of structures placed on fluid-saturated porous soils. The theory has been widely applied to geotechnical problems beyond soil