If temperature increases, then pressure increases. Temperature measures the average speed of particles, so if the temperature is high, then the particles are moving quickly and are colliding with other particles more forcefully. Pressure is defined as the force and number of collisions the particles have with the wall of its container. So if the high temperature causes the particles to move quickly, they are going to collide more often with the container, increasing the pressure.
This remains true as long as the number of moles (n) remains constant.
temperature,pH and substrate concentration
The average temperature of the Earth remains relatively constant due to a balance between the amount of incoming solar radiation absorbed by the Earth and the amount of heat energy emitted back into space. This balance is maintained by factors such as the greenhouse effect, which traps some of the heat in the atmosphere, and natural feedback mechanisms that help regulate the climate. If this balance is disrupted, it can lead to changes in the Earth's temperature.
In a container the volume remain constant but the pressure increase.
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
Factors such as light availability, temperature, nutrient availability, and water availability have an immediate effect on net primary productivity. Any changes in these factors can directly impact the rate at which plants can photosynthesize and grow, thus affecting NPP.
temperature,pH and substrate concentration
The atmospheric pressure has no effect on the speed of sound when the temperature is constant. The air pressure has no influence on the sound.
In science, as in real life sometimes several 'factors' effect the outcome of an experiment. In order to make the problem easier to study one or more of these is 'held constant' or not allowed to change in order to see the effect of the other variables. EX. Gas volume can be effected by both pressure and temperature. In order to understand the effect of pressure, Boyle kept the temperature constant. He then changed the pressure to see what happened to the volume of a gas. This gave him what is now called Boyle's Law: The volume of a gas varies inversely as the pressure when the temperature is held constant.
In science, as in real life sometimes several 'factors' effect the outcome of an experiment. In order to make the problem easier to study one or more of these is 'held constant' or not allowed to change in order to see the effect of the other variables. EX. Gas volume can be effected by both pressure and temperature. In order to understand the effect of pressure, Boyle kept the temperature constant. He then changed the pressure to see what happened to the volume of a gas. This gave him what is now called Boyle's Law: The volume of a gas varies inversely as the pressure when the temperature is held constant.
Supply voltage , temperature , frequency are factors that effect the electrical parameters of opamp
Charles Law
the relation is given by charles law which says that the volume of a constant mass of gas at constant pressure is directly proportional to the temperature so increase in temperature causes an increASE in the volume
Z. Gat has written: 'The Effect of temperature on the citrus crop' -- subject(s): Citrus, Climatic factors, Effect of temperature on
illness, excerise, surrounding, stress
Factors such as the Earth's rotation, temperature differences, and pressure gradients contribute to global winds. Areas where winds are weak are often near the equator, where the temperature is relatively constant and the Coriolis effect is weaker, or in areas of high pressure where the pressure gradient is low.
light soil temperature soil type soil moisture outside temperature
The average temperature of the Earth remains relatively constant due to a balance between the amount of incoming solar radiation absorbed by the Earth and the amount of heat energy emitted back into space. This balance is maintained by factors such as the greenhouse effect, which traps some of the heat in the atmosphere, and natural feedback mechanisms that help regulate the climate. If this balance is disrupted, it can lead to changes in the Earth's temperature.