The absolute amount of nitrogen in the atmosphere has kept constant over time because it is not a gas that reacts readily with other elements - it is relatively inert.
However, the relative level of nitrogen in Earth's atmosphere has changed over time as the atmosphere was "terraformed" by the life evolving on the planet. For instance in the Cretaceous times the atmosphere was much richer in Oxygen (30%) than today (20%) which means that then the %Nitrogen was 70% rather than 80%.
Carbon dioxide is kept at a constant level by an exchange between the atmosphere and various sinks, such as oceans, plants, and soil. These sinks absorb and store carbon dioxide, helping to regulate levels in the atmosphere. The balance between carbon dioxide sources, such as human activities and natural processes, and sinks maintains equilibrium in the carbon cycle.
Liquid nitrogen can be kept at room temperature at sufficient pressure. Otherwise, it is a gas.
Earth's lower atmosphere is kept warm by the greenhouse effect, where certain gases trap heat from the sun and prevent it from escaping back into space. These greenhouse gases, such as carbon dioxide and water vapor, help regulate Earth's temperature and make it suitable for supporting life.
The atmosphere is of vital importance for life on earth. Without atmosphere life would be impossible. It gives us air to breathe and protects us from meteorites and ultraviolet rays from the sun. The atmosphere absorbs so much heat that temperatures on earth are such that life is possible.
While greenhouse gases play a crucial role in maintaining Earth's temperature and supporting life, an excess of these gases in the atmosphere can lead to global warming and climate change, which can have harmful effects on the environment and biodiversity. Therefore, it is the accumulation and imbalance of greenhouse gases that are considered harmful, rather than their presence in the atmosphere.
Carbon dioxide is kept at a constant level by an exchange between the atmosphere and various sinks, such as oceans, plants, and soil. These sinks absorb and store carbon dioxide, helping to regulate levels in the atmosphere. The balance between carbon dioxide sources, such as human activities and natural processes, and sinks maintains equilibrium in the carbon cycle.
What variables must be kept constant
Carbon dioxide is absorbed; also other oxides of sulfur and nitrogen if the atmosphere is polluted.
Liquid nitrogen can be kept at room temperature at sufficient pressure. Otherwise, it is a gas.
All variables except one, the experimental variable, are kept constant in an experiment.
In Table 2.1, the variable that is typically kept constant is referred to as the control variable. This variable is maintained at a consistent level across different experimental conditions to ensure that any changes in the dependent variable can be attributed to the manipulation of the independent variable.
The factor that is kept constant in an experiment is called the controlled variable. It is important to keep this variable constant to accurately measure the effect of the independent variable on the dependent variable.
Gases in a closed system can be kept constant through regulating pressure and temperature. Water levels can be maintained by controlling inflow and outflow rates or using a float valve mechanism to adjust levels automatically. Additionally, sensors can be used to monitor levels and trigger adjustments as needed.
If pressure is kept constant, the volume will decrease.If volume is kept constant, the pressure will decrease.
Temperature and amount (number of moles) is kept constant.
Yes, Earth's gravitational force holds our atmosphere in place. The gravitational force between Earth and the atmosphere prevents it from drifting off into space. The atmosphere is made up of gases like nitrogen, oxygen, and carbon dioxide, which are all kept close to Earth's surface due to gravity.
His constant pace was one thing that kept him ahead of everyone. This is a sample sentence using constant.