The specific gravity of tar ranges from
1.1 to 1.25
Specific gravity is a fundamental physical property that helps us understand how dense a substance is compared to water. It's defined as the ratio of the density of a substance to the density of a reference substance, which for liquids and solids is typically water at a specific temperature (usually \(4^\circ \text{C}\) or \(20^\circ \text{C}\)). Since specific gravity is a ratio of densities, it is a dimensionless quantity.
Tar is a dark, viscous substance obtained from the destructive distillation of organic material such as wood, coal, or peat. Coal tar, derived from coal, is commonly used in road construction and roofing.
The specific gravity of tar is an important property for various engineering applications, particularly in pavement design and construction. Different types of tar can have slightly different specific gravities, but there is a typical range.
Based on standard material properties and engineering references, the specific gravity of tar generally falls within a certain range. The provided options give us possible ranges.
Comparing these options with known properties of tar, the specific gravity of tar is commonly found to be slightly greater than 1, indicating it is slightly denser than water. The range that aligns with the typical specific gravity of tar is 1.1 to 1.25.
A specific gravity of 1.1 means that tar is 1.1 times denser than water. A specific gravity of 1.25 means it is 1.25 times denser than water.
Knowing the specific gravity of tar is crucial for:
It's often useful to compare the properties of tar with other similar materials like bitumen, which is more commonly used in modern road construction.
| Property | Tar | Bitumen |
|---|---|---|
| Origin | Destructive distillation of organic matter (coal, wood) | Petroleum processing |
| Chemical Composition | Higher aromatic content, includes phenols and cresols | Higher aliphatic content |
| Specific Gravity | Typically 1.1 - 1.25 | Typically 1.0 - 1.05 |
| Durability | Less durable, higher temperature susceptibility | More durable, lower temperature susceptibility |
Specific gravity is closely related to density. Density is mass per unit volume \((\rho = \frac{m}{V})\), usually measured in \(\text{kg/m}^3\) or \(\text{g/cm}^3\). Specific gravity (\(\text{SG}\)) is calculated as:
\(\text{SG} = \frac{\rho_{\text{substance}}}{\rho_{\text{reference}}}\)
For tar (a liquid/solid), the reference substance is usually water. The density of water at \(4^\circ \text{C}\) is approximately \(1000 \, \text{kg/m}^3\) or \(1 \, \text{g/cm}^3\).
If the specific gravity of tar is 1.2, its density is approximately \(1.2 \times 1000 \, \text{kg/m}^3 = 1200 \, \text{kg/m}^3\) or \(1.2 \times 1 \, \text{g/cm}^3 = 1.2 \, \text{g/cm}^3\) (assuming water density at standard conditions). This relationship allows us to easily convert between specific gravity and density.
Therefore, the specific gravity range of 1.1 to 1.25 for tar indicates its density is typically between \(1100 \, \text{kg/m}^3\) and \(1250 \, \text{kg/m}^3\) at the reference temperature.
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