Clouds.
Moisture can be both a liquid and a gas. A gas, such as steam, is wet if you touch it. Moisture is more commonly though of as a liquid, however. Water is a liquid, and a moisture, Steam is a gas, and a moisture.
If the question is what do you use to measure MOISTURE, then the answer is a Moisture Meter. A type of moisture meter, the hygrometer, measures humidity and temperature. The moisture content of wood, hay, concrete, paper, leather, veneer, and cardboardand a great many things is critical to how these materials cure over time. For example, hardwood will split or crack (called "checking") if the wood acquires and releases moisture too quickly. The U.S. Department of Agriculture says " If the wood is too wet when it is put into place, it will eventually dry to a moisture content approximating that of the conditions under which it is used. This drying in place will be accompanied by shrinkage. In a house, this shrinkage may cause loosening of fastenings and settling of the building with resulting plaster cracks, drywall nail popping, and unsightly openings around trim and moldings. Excessive shrinking of studs, sheathing, and siding decreases the weather-tightness of walls, loosens fastenings, and may reduce the mechanical stiffness of walls. If wood is dried too far below the average moisture content it will reach in use, swelling may cause drawers, windows, and doors to stick. Concrete will fail if it does not maintain proper moisture content while curing. Greenhouse plants do poorly under improper moisture (humidity) levels. If you have ever had firewood that would not burn properly, it is most likely due to having too much moisture content. Moisture content is typically monitored by hand-held moisture meters although there are permanently installed sensors (such as inside large HVAC systems) to provide constant monitoring.
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A oft-repeated water vapor myth is that warm air can "hold" more water vapor than cool airbecause as the air warms its molecules move farther apart, making room for more molecules. This leads to the idea that as air cools its molecules move closer together, "squeezing" out water vapor.
No. The keyword in this term is "relative." Relative humidity stands for the amount of moisture currently in the air with respect to (or relative to) the amount of moisture that can be held in the air. Colder air can hold less moisture than warm air, so there's a much greater chance of having 100% relative humidity when it's cool out than when it's warm out. For example, if you wake up on a cool morning and experience dew on the ground, it is because the cool air is holding as much moisture (i.e. humidity) as it possibly can. So you are experiencing 100% relative humidity. However, if that same amount of moisture stays in the air throughout the day, once the air warms up, the higher temperature allows for more moisture to be present in the air, and the air may not be fully saturated with moisture, thus you have a relative humidity that is less than 100%. So no, you do not have to be underwater to experience 100% relative humidity; in fact, underwater there is no air to surround you... so you're not experiencing any relative humidity at all.
Clouds are an example of suspended water droplets or ice crystals in the Earth's atmosphere. They form when air rises and cools, causing moisture to condense into visible droplets or crystals.
It actually means compressed or concentrated. Example: the power must not be condensed.
Condense comes from the word "condensation". It is the process of moisture forming on a solid object from evaporated water. For example, when you take a shower, the steam is formed from water, which later is found condensed on your bathroom mirror. ~Ashton
Typically on any cooling surface in a humid environment. For example, leaves warmed by the sunlight during the day, will collect condensed moisture (dew) as they cool during the evening. When the sun rises and re-heats the leaves, the dew will eventually evaporate.
Bound moisture is water that is nothing but for crystallization. Unbound moisture is the moisture that is present in the water once evaporation occurs, for example dew.
Sedimentary rock is formed by suspended solids dropping to the bottom and building layers that will compress down under the weight of water and go hard after the water source has disappeared, and the moisture has evaporated out of the silt left behind.
The steam condensed into droplets.
amount of moisture in the soil
If you are referring to any metal particles suspended in water I believe the term you are looking for is Colloidal. For example.... Colloidal Silver is silver particles suspended in water.
The definition of Distillation is A process in which a solution is boiled so the vaporized solvent can be collected and condensed into an uncontaminated liquid.
By "more condensed", do you mean "denser"? If so, the answer is "usually but not always". The most famous example of a substance where the solid form is less dense than the liquid form at the same temperature is water.
A protoplasm is composed of fats, proteins and other molecules which are suspended in water. It is an example of a colloidal suspension.