In its most basic sense, density is defined as the equivalent weight of a substance for every specific amount of volume. For example, the normal density of water is 1 gram per 1 milliliter at room temperature.
However, this measurement can change depending on many factors, such as changes in temperature and dissolved substances. Ice has a lesser density than water which is why it floats. Knowing the density of water is important because it can be applied to many other aspects.
The sentence “Density is the mass per unit volume of a substance” is always mentioned in class. That is the technical definition of the term. Mass and weight are often misused because of the confusion about their respective definitions, but since we are only referring to one gravity of Earth, mass and weight are pretty much the same.
Density is a constant factor in all matter that is composed of molecules. In other words, if an object occupies space and has mass, its density can also be measured. It is simply just its weight for every specific volume.
For example, water’s density under normal conditions is 0.9998395 g/ml at 4.0° Celsius (39.2° Fahrenheit), to be specific but is rounded off to 1 gram per mL or cubic centimeter (1g/mL or cc) for uniformity.
Factors affecting water density
The following are the common factors that affect the density of water.
- The density of water is approximately 1 gram per cubic centimeter (1 g/cm3) or 1 gram per milliliter (1g/mL).
- Temperature can also change water density, but the correlation is still unclear and inconsistent.
- When water is cooled at room temperature, it becomes denser over time. Of course, this is true for other substances as well. But the limit ends at 4°C, where pure water is at its most dense.
- There are cases where it is usually the other way around, where further cooling of a substance decreases its density. This phenomenon is usually referred to as ‘negative thermal expansion’ and applies to those bonded with intermolecular forces and other chemical composition factors. One example that can be made for this is molten silica.
Temperature-dependent water density
There was a time in my life when I could use this concept of water density to get back at my older brother and his friends for always picking on me. It was a hot summer day, and they went up this nearby hill to bury their collection of bottle caps.
Then they asked me to return home, get a gallon of water and bring it to them to quench their thirst. I was a kid back then and weighed only 70 pounds. A gallon of tap water at that temperature was a lot for me to carry. So the second time they asked me, I looked for ways to make my job easier.
Thanks to the encyclopedia, I discovered that a gallon of water at boiling point weighed a lot less. So I brought them a lighter gallon of boiling water, and I scampered home immediately without regard for their reactions.
|Temperature (°F/°C)||Density (grams/cm3||Weight (pounds/ft3|
Source: U.S. Department of the Interior, Bureau of Reclamation, 1977, Ground Water Manual, from The Water Encyclopedia, Third Edition, Hydrologic Data, and Internet Resources, Edited by Pedro Fierro, Jr. and Evan K. Tyler, 2007
Ice has a lower density than water.
Looking at the picture below, a big part of the iceberg is submerged in the water. However, you can see that the majority of it is below the water surface. This is because the density of ice is less than that of liquid water. An ice’s density is reduced by 9 percent at freezing point.
One way to understand the difference in water densities in various phases of matter is to look at the structure of ice.
Since ice is solid water, the arrangement of molecules that make it up is stable. Whereas for its liquid phase, the molecular arrangement tends to be more random, and there is a larger distance between molecules, making it denser than ice.
However, the air within a block of ice still makes up for about 10% of its weight, which is why a portion of the iceberg remains above the water surface.
Water is life. Most of the planet is water, and so is most of the human body.
At higher temperatures, water becomes denser. The denser matter will always sink the less dense. In winter, when the surface of the water is exposed to the cold temperature, the ice that forms sinks to the bottom of the body of water which will cause it to freeze.
At the same time, water can also regulate heat, so frozen lakes might take a while to thaw in the summer completely.
The scientific explanation of this concept might be harder to follow because of the other factors that could affect it. For example, the content in the water, like dissolved solids, organic substances, and microorganisms, can increase its weight.
A good comparison would be ocean water and pure water. There is more ocean water content than freshwater, making the former denser.
The heavy ice cubes sink to the bottom of the glass, and the lighter ice cubes float to the water surface.
Credit: Mike Walker
Does heavy ice float?
We have already established that ice floats because it is less dense than liquid water. However, there are special cases where the ice is of a slightly different composition, usually called “heavy ice” made from heavy water.
This type of water is 10.6% denser than regular water and has a chemical of D2O instead of the usual H2O since deuterium (an isotope of hydrogen) atoms have replaced the original hydrogen. As a result, the ice formed from that kind of water is denser than ice from regular water.
How to measure the density
A device for measuring the density of liquids is called the hydrometer, usually made of glass and resembles a thermometer. It is quite easy to use. You can make a makeshift version of it using just plastic straws. It is a thin glass rod with a round bulb at the tip to support and float upright.
To take the measurement, it needs to be submerged in the liquid until it floats. You can see on the printed lines and numbers where the water level matches. The meter will float lower in liquids with low density and higher in those with high density. The basis for all other densities of liquids is water, so when you use it in water, it should hit the 1.000 mark, proving true the specific gravity of water at 4°C.
This device is used to measure the densities of various liquids and has other applications in different fields. For example, it can be used to measure water salinity in-class experiments and get rough estimates of milk fat content since density correlates to how much fat is present in a specific volume of milk.
It is also used to determine sugar content in some alcoholic drinks like beer and wine in the brewer industry to know how long it has been going through fermentation.
The reason why water density is 1
The mathematical formula of density (ρ=m/v) is mass divided by volume, which translates to mass for every given volume. Water is also the standard used for the foundation of the metric unit of mass, establishing that 1 cubic centimeter of water weighs 1 gram. This is no coincidence.
It is also convenient because you won’t have difficulty remembering that number. 1 gram per 1 cc. As mentioned before, it’s not exactly 1. The exact number is rounded to the nearest whole number to avoid errors and maintain uniformity.
There is never a constant density for water as well because air pressure and temperature can alter it even at the slightest bit. Therefore, you must consider these factors in your calculations if you need very accurate numbers. A chart in the next part will guide you with these instances.
However, remember that those values only apply to pure water. Other water types, like seawater,r have different densities due to the salt content. It is around 1.02g/cm3 to 1.03g/cm3, a bit higher than pure water.