Flowmetry and geocálculo graceli. sábado, 2 de maio de 2015 Flowmetry and geocálculo graceli. Imagine the flow of a heart. While the side to up the b descends and vice versa. So we have. Dfapi * x / t in m, y * dfbpi [Flow diameter times pi x b, divided by the time when m]. Where one side rises and falls each other. Thus we have a temporal graceli flowmetry and n-dimensional]. Imagine a three dimensional triangle [like a rubber balloon of the type children play], and that while one hand undergoes a pressure causing the other sides dilate, thus we have the two sides increasing progressively in relation to time and flow pressure increasing angles instantly. Plc / T = x * Laf / t, y * lbf / T = vâab / t Pressure side c / time = x side-flow / long side b y flow / time, the angle variation ab / T. Where internal angles never be 180 degrees. The same process occurs for other geometric shapes. With this it can form a trigonometry varied flows. Where sine, cosine and tangent adds to the ...