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A pipe with an inside diameter of 2 inches has 37.7 cubic inches (rounded) of interior volume per foot. That means about 6feet 1.5inches per gallon.
Density of liquid A, relative to liquid B = density of liquid A/density of liquid B. The temperatures and pressures for both liquids must be specified.Often the reference liquid (liquid B) is pure water at one atmosphere and room temperature (20 deg C). In that case, the ratio is also known as specific gravity.Density of liquid A, relative to liquid B = density of liquid A/density of liquid B. The temperatures and pressures for both liquids must be specified.Often the reference liquid (liquid B) is pure water at one atmosphere and room temperature (20 deg C). In that case, the ratio is also known as specific gravity.Density of liquid A, relative to liquid B = density of liquid A/density of liquid B. The temperatures and pressures for both liquids must be specified.Often the reference liquid (liquid B) is pure water at one atmosphere and room temperature (20 deg C). In that case, the ratio is also known as specific gravity.Density of liquid A, relative to liquid B = density of liquid A/density of liquid B. The temperatures and pressures for both liquids must be specified.Often the reference liquid (liquid B) is pure water at one atmosphere and room temperature (20 deg C). In that case, the ratio is also known as specific gravity.
The amount of a substance that a liquid holds will be the solubility of that substance in that volume of the liquid - at that temperature.
They are liquid measurements of different magnitude.They are liquid measurements of different magnitude.They are liquid measurements of different magnitude.They are liquid measurements of different magnitude.
Initially Liquid=12lts, 20% liquid=> 2.4lts liquid and 9.6lts water Next 10lts mixture contains 30% liquid => 3lts liquid and 7lts water Finally both mixture mixed % of water= (16.6/22)*100 = 75.45%
The movements in the liquid inner core.
The water that doesn't evaporate into vapor stays in the ocean as liquid water. The oceans have a lot of liquid water. Over time, ocean water is always evaporating and turning into rain and comes back to the ocean; but the salts and minerals carried into the sea from rivers never evaporate. They stay dissolved in the ocean waters and make it saltier and saltier.
The movements in the liquid inner core.
The movements in the liquid inner core.
The Earth's outer core is thought to be a liquid.
The outer core is thought to be the Earth's liquid layer. It lies beneath the mantle and is composed mostly of iron and nickel in a liquid state due to high temperatures and pressure. The movement of this liquid outer core is responsible for generating the Earth's magnetic field.
nothing happens after a solid chages into a liquid.
When a liquid changes into a solid, it undergoes a process called solidification or freezing. The molecules in the liquid slow down and come closer together, forming a stable crystalline structure. This process releases heat energy as the molecules lose kinetic energy, resulting in the formation of a solid with a fixed shape and volume.
Shadows can provide information about the depth and direction of geological features, such as mountain ranges or volcanic peaks, on the surface of the Earth. By studying the lengths and angles of shadows, geologists can infer the approximate shape and elevation of land formations, helping to better understand the Earth's interior composition and structure.
nothing happens after a solid chages into a liquid.
it is true
Molecules at the surface of a liquid are not completely surrounded by other molecules like those in the interior, leading to unbalanced intermolecular forces that cause surface tension. This results in surface molecules experiencing a net inward force, pulling them back into the bulk liquid and causing distinctive properties at the surface.