Answer:
To determine the value of atmospheric pressure, we can use the concept of hydrostatic pressure. By comparing the lengths of the air column in the capillary tube when held horizontally and vertically, we can equate the pressure difference to the difference in height of the mercury column. Using the given values and the density of mercury, we can calculate the atmospheric pressure.
B. Cobweb
C. Mustardseed
D. Puck
The gravitational potential energy of an object Is always measured relative to the height of the object. It has the equation equal to mass PE = mgh where PE is the potential energy, m is the mass of the object, H is the height of the object and g is the acceleration due to gravity.
The gravitational potential of an object is always measured relative to reference level/another point
Energy is the ability to do work. Energy can change from one energy to another
Gravitational potential energy is the energy that an object has because of its position
The potential energy can be formulated:
Ep = m. g. h
E = potential energy of an object, joule
m = object mass, kg
g = gravity acceleration, m / s2
h = height of an object, m
The higher the object from the surface of the earth and the greater the mass, the greater the potential energy of the object. Earth's gravity also affects the potential energy of objects
Potential energy itself includes mechanical energy
Em = Ek + Ep
Em = mechanical energy
Ek = kinetic energy
Ep = potential energy
The amount of kinetic energy and potential energy of objects is always constant
Determine how potential and kinetic energy changes at each position of the pendulum
Determine the mechanical energy
the potential of an object when it falls from a height
the gravitational potential energy between moon and earth
Keywords: the potential energy, kinetic energy, mechanical energy
Answer:
Reproducibility
Explanation:
The results of an experiment should be reproducible. By repeating the experiment several times, a confidence interval can be determined that will help establish that the results are real, and not an artefact
A wave breaks due to the interference of the ocean floor with its oscillatory motion. As the wave nears the shore and the water gets shallower, the bottom of the wave slows down while the top continues its original speed, causing the wave to break.
A wave will 'break' or crash due to its interaction with the ocean floor as it approaches the shore. Waves follow an oscillatory motion, moving in an up-down pattern. When a wave gets closer to shore, the water becomes shallower which interferes with the oscillatory motion of the wave. The bottom of the wave slows down upon hitting the ocean floor while the top of the wave continues its original speed. This causes the wave to become steep and eventually break, forming the crashing wave front we often see on beaches.
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