An aortic sinus is one of the bulging spaces of the aortic root behind an aortic valve leaflet. In the usual three-leaflet arrangement, two sinuses give origin to the coronary arteries; the third is noncoronary. The distal sinus boundary is associated with the sinotubular junction.[ref] A sinus is thus a local part of the root geometry, rather than the whole ascending aorta or the central passage alone.
The geometry has an experimentally testable role in valve motion. B. J. Bellhouse and L. Talbot placed a rigid-walled valve model in a pulsatile water tunnel. Their primary report describes a trapped circulating flow and a downstream stagnation point within each sinus, with much of leaflet closure occurring before net forward flow had ended.[ref] This is evidence from a controlled physical model, not direct observation of every patient or proof that root walls are rigid.
A local circulation can coexist with net forward transport. For an original accounting example, suppose an ideal central stream carries 80 mL/s downstream, while an adjacent recirculating region carries 10 mL/s across a selected internal surface in each direction. The circulating contributions cancel in the net flux through that surface even though the fluid there is moving. Thus net volumetric flow rate alone does not specify the spatial velocity field near a leaflet.
The same distinction matters for washout. A sinus can contain rapidly moving fluid whose paths mostly recirculate; speed alone does not establish how quickly that fluid is replaced. Replacement depends on exchange with the through-flow and can be investigated using a tracer or modeled pathlines. The aortic sinus therefore connects a visible anatomical shape with questions about leaflet loading, local flow and transport history.

Articles by others on the same topic (0)

There are currently no matching articles.