Wiki User
∙ 12y agolinear
Wiki User
∙ 12y agoIn a Newtonian fluid, shear stress is directly proportional to the velocity gradient. This relationship is described by Newton's law of viscosity, which states that the shear stress (τ) is equal to the viscosity (μ) of the fluid multiplied by the velocity gradient (du/dy). Mathematically, this relationship can be represented as τ = μ*(du/dy).
The difference in velocity between adjacent layers of the fluid is known as a velocity gradient and is given by v/x, where v is the velocity difference and x is the distance between the layers. To keep one layer of fluid moving at a greater velocity than the adjacent layer, a force F is necessary, resulting in a shearing stress F/A, where A is the area of the surface in contact with the layer being moved.
No, the relationship between velocity and height on an incline is not linear. Velocity is influenced by factors like acceleration due to gravity and friction, making it a non-linear relationship.
The relationship between starting length and initial velocity of shortening is typically an inverse relationship. This means that as the starting length increases, the initial velocity of shortening decreases. This relationship is governed by the length-tension relationship of muscle fibers.
The units of velocity gradient are typically expressed as reciprocal seconds (s^-1) or per meter (m^-1), depending on the context. It quantifies the rate of change of velocity with respect to distance or time in a fluid flow field.
The relationship between velocity and pressure in a fluid is described by Bernoulli's principle, which states that when the velocity of a fluid increases, the pressure decreases and vice versa. This relationship is based on the conservation of energy in a flow system.
The difference in velocity between adjacent layers of the fluid is known as a velocity gradient and is given by v/x, where v is the velocity difference and x is the distance between the layers. To keep one layer of fluid moving at a greater velocity than the adjacent layer, a force F is necessary, resulting in a shearing stress F/A, where A is the area of the surface in contact with the layer being moved.
Velocity gradient is the rate of change of velocity with respect to distance in a fluid flow. It represents how velocity changes across different points in a fluid, indicating the level of shear and deformation within the fluid. Typically, it is used to describe the flow behavior or viscosity of a fluid.
No, the relationship between velocity and height on an incline is not linear. Velocity is influenced by factors like acceleration due to gravity and friction, making it a non-linear relationship.
sorry '=
The relationship between starting length and initial velocity of shortening is typically an inverse relationship. This means that as the starting length increases, the initial velocity of shortening decreases. This relationship is governed by the length-tension relationship of muscle fibers.
The difference in velocity between adjacent layers of the fluid is known as a velocity gradient and is given by v/x, where v is the velocity difference and x is the distance between the layers. To keep one layer of fluid moving at a greater velocity than the adjacent layer, a force F is necessary, resulting in a shearing stress F/A, where A is the area of the surface in contact with the layer being moved.
The units of velocity gradient are typically expressed as reciprocal seconds (s^-1) or per meter (m^-1), depending on the context. It quantifies the rate of change of velocity with respect to distance or time in a fluid flow field.
Acceleration is the rate at which velocity changes and the direction of the change.
The relationship between velocity and pressure in a fluid is described by Bernoulli's principle, which states that when the velocity of a fluid increases, the pressure decreases and vice versa. This relationship is based on the conservation of energy in a flow system.
Centripetal force is = mass * velocity square divided by radius
accleration is the speed. Velocity is when you know the speed of an object and its direction.
As depth increases, current speed typically decreases due to friction with the riverbed. This is known as the velocity gradient, where the flow is faster at the surface and slower towards the bottom. It's important to consider this relationship when studying river dynamics or designing structures in rivers.