I believe the answer to this question is "chunking"
I hope this helps.
The boundary layer thickness is usually defined as the distance from the wall to the point where the flow velocity reaches 99 % of the free stream value.
In the very thin boundary layer associated with free stream flows with high Reynolds numbers, a steep rise in velocity occurs perpendicular to the wall.
Boundary layer thickness = 0.37*Distance on x-axis/(Reynolds Number^(1/5))
δ = 0.37*x/(Re^(1/5))
This formula uses 3 Variables:
Variables Used
Boundary layer thickness - (Measured in Meter) - Boundary layer thickness is the distance normal to the wall to a point where the flow velocity has essentially reached the 'asymptotic' velocity.
Distance on x-axis - (Measured in Meter) - Distance on x-axis is the distance of point measured along x-axis form origin.
Reynolds Number - The Reynolds number is the ratio of inertial forces to viscous forces within a fluid which is subjected to relative internal movement due to different fluid velocities. A region where these forces change behavior is known as a boundary layer, such as the bounding surface in the interior of a pipe.
Learn more about Boundary Layer Thickness on:
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Because people or too scared and traumatized to fess up to what had happened to them... It's honestly really sad.
The theory that most strongly suggested that unconscious processes influence personalitys is called Sigmund Freud.
<h3>Who is Sigmund Freud?</h3>
Sigmund Freud, an Austrian, primarily worked on the unconscious areas of the human mind hence the proponent of the psychoanalytic theory.
His theory of personality refers to the theory that view 2 driving factors that drive our personality, the concious and the unconcious factors.
Hence, the theory that most strongly suggested that unconscious processes influence personalitys is called Sigmund Freud.
Learn more about Sigmund Freud here : brainly.com/question/2706543
Answer:
B
Explanation:
A sinkhole, also known as a cenote, sink, sink-hole, swallet, swallow hole, or doline, is a depression or hole in the ground caused by some form of collapse of the surface layer. Most are caused by karst processes – the chemical dissolution of carbonate rocks or suffosion processes.
