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That is exactly what it means - however there is still the question of rate of reaction and equilibrium.

As an example - thermodynamics favor the conversion of diamond back to something more like graphite at normal room conditions, but the process is so slow that no one will observe the change within their mortal lifetime (nor will their great-great-great-great grandchildren). The point is that the rate of reduction of N2 to NH3 is not especially fast.

There are also competing reactions and the tendency of the reverse reaction to occur - which becomes pronounced as equilibrium is approached.

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Surface tension reduction in a liquid system can be achieved by adding surfactants or surface-active agents. These substances disrupt the intermolecular forces at the liquid's surface, reducing the cohesive forces between molecules and lowering the surface tension.


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Adding salt to water decreases the vapor pressure of the water. This is because the salt particles disrupt the formation of water vapor molecules at the surface of the water, making it harder for them to escape into the air.


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Reduction of surface tension in liquids can lead to changes in their behavior, such as increased spreading and wetting on surfaces. This is because lower surface tension allows the liquid molecules to spread out more easily, resulting in improved interactions with other substances.


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Related Questions

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Unequal heating of Earth's surface causes differences in temperature, creating areas of high and low pressure. Warm air rises at the equator, creating low pressure, while cold air sinks at the poles, creating high pressure. Wind then flows from areas of high pressure to areas of low pressure to equalize the pressure difference, resulting in the formation of wind patterns.


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Yes, the asthenosphere rises close to the surface beneath mid-ocean ridges. This upward movement occurs due to the reduction in pressure as tectonic plates diverge, allowing the hot, partially molten rock of the asthenosphere to ascend. As it rises, it contributes to the formation of new oceanic crust through volcanic activity at these ridges. This process is a key part of plate tectonics and ocean basin formation.


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rock