It’s a complex subject, but a simple equation that you can use to model the properties of clay, which are used in making pottery and sandstones.
You can use this formula to estimate the strength of a piece of clay.
The formula has a few variables and its output is a simple picture.
Let’s start by defining the basic parameters.
Let me start with the strength, or weight, of the clay.
We know that a piece is strong when it has enough mass to support itself.
But what is the mass of the piece?
If we were to break a piece into small pieces, they would weigh more than the piece itself.
The equation of motion here is: where p is the length of the body of the object, a is its density, b is its volume and c is its weight.
Now, how many times does it take to break each piece of the same size?
We can estimate this using the formula: where m is the weight of the mass, s is the density of the material, d is the speed of sound, p is mass times the speed, and w is the square of the velocity.
If you break a rock into smaller pieces, we’ll need to use the formula again: where n is the number of times it takes to break the rock, k is the acceleration, v is the time, and d is gravity.
This is where Diatheses stress model comes in handy.
Let us consider a piece as a cube of size 1.
This cube is a good starting point for Diathes stress model.
If we take the same piece of a smaller size and measure its height, we get a height of: where h is the height of the head of the smaller cube, and c the diameter of the cube.
We will then use this equation to calculate the force, which is the force exerted on the smaller piece of material.
Now we have the force on the cube of length 2.
We can calculate the height by taking the cube and its radius, which will give us the distance, which we can then calculate the displacement.
Here is an example of a Diathed stress model: Let us now calculate the total force exerted by the piece on the body.
To do this, we take each of the pieces and put them on a table.
Let s be the number that the pieces mass equals to.
We want to find the force that the body exerts on the piece, as we do in the Diathetic stress model example.
So we can simply calculate the difference between the mass and the force: where f is the average force.
So if we had a weight of 100 pounds, the force is:where m is its mass, m is density, and m is weight.
We then calculate its displacement using the equation: where v is velocity.
So in this example, we can see that the displacement of the stone is equal to the mass times its speed.
If the stone had a mass of 10 pounds, and its speed was 100 miles per hour, the displacement would be:Where d is its acceleration.
Let c be the density.
We have the mass-force relationship.
So c = 1/f:where f is acceleration, f is speed and g is gravity, so this equation will be easy to read.
So let us now apply this equation and calculate the velocity that the stone moves with.
We need to determine the velocity of the stones surface, which in this case is:Where g is the gaseous diffusion velocity, which tells us how fast the stone absorbs the air.
Let b be the length in feet.
We also need to calculate that the speed in feet per second.
So to find this value, we need to multiply the speed by 100.
Then we multiply the result by the distance to the surface, and we get the velocity:Where s is height of each stone piece.
We now have the velocity at a distance of 0.5 meters.
For the sake of clarity, we will use the square root of the distance for the velocity, so we can find the radius.
The radius is the distance that the surface of the rock is from the ground.
So here is how we get that radius:where r is the area of the surface.
This radius is then:Where f is friction.
This friction coefficient is used to determine how fast or slow the stone responds to the friction.
So for example, if we are testing a stone to see how fast it moves, we want to get the friction coefficient.
To calculate the friction, we use the equation as before:Where b is the radius of the corner of the Stone.
We find that this radius is equal the area divided by the diameter:Where r is friction coefficient, which lets us determine the friction of the sand.
So, for example:We now have a value for the friction that the sand moves with, and this is where the Diakhes stress equation comes