tension
The force that pulls atoms apart is called fission. Nuclear reactors use controlled fission to produce massive amounts of energy.
a difference in osmotic water potential between the source and the sink
gaestrum contain bioactive compounds : β-glucan-protein complex; its useful as antiimflamatory, antioxidant and cytotoxic actifities. Calcium oxalate is a common compound found in geastrum. The formation of calcium oxalate crystals stretches the layers of the outer walls, pushing the inner and outer layers of the peridium apart.
Apart from distance to the epicenter, local geological conditions play a significant role in the intensity of seismic shaking. Areas built on soft sediments or unconsolidated materials may experience stronger shaking compared to those on solid bedrock, as softer materials can amplify seismic waves. Additionally, the direction of the seismic waves and the type of construction in a region can also affect how much shaking is felt.
The layers of Earth are sorted by density due to the process of gravitational differentiation that occurred during the planet's formation. Heavier materials, such as iron and nickel, sank toward the center, forming the core, while lighter materials like silicates rose to form the mantle and crust. This sorting is driven by the force of gravity, which causes denser materials to move inward and less dense materials to stay outward. As a result, the Earth has a layered structure with distinct compositions and densities.
Tension stretches or pulls apart the crust.
Tensile force stretches objects by pulling them apart along their length. This force is exerted when an external force is applied to stretch or elongate a material, causing its molecules to separate and create tension within the object.
Generally materials that fly apart are being pushed rather than pulled. We could devise a mechanism that pulls materials apart - for example, if we attach two hooks and pull them on winches in opposite directions. In that case we would describe the force as mechanical in nature. But it is more likely that things get pushed apart by their own internal pressure.
When there is a divergent boundary, regardless if the plates are ocean-ocean or continental-continental, tensional stress pulls on the crust. Rocks have weaker tensional strength than compressive strength, so they are easier to pull apart.
When a wire is pulled, it is said to be in tension. Tension is the force that stretches the wire and tries to pull it apart. This is in contrast to compression, which is the force that pushes a material together.
The force that stretches a spring is called tension force. This force appears when the spring is being pulled or stretched in one direction.
Internal forces act within a body and include tension, compression, and shear forces. Tension is a pulling force that stretches materials, compression is a pushing force that compresses materials, and shear is a force that causes adjacent parts of a material to slide past each other.
Tensile force / stress.
Tensile force tends to pull a body apart by stretching or elongating it. This force acts in the opposite direction to compressive force, which tends to push a body together. Tensile force is commonly experienced in materials like ropes, cables, and springs.
Tension
When you pull on something, it stretches a bit. Even materials you think are rigid, stretch if enough force is applied. The numbers are very important since they say a lot about the characteristics of materials. Of course all this depends on the thickness of the thing that stretches, so engineers use units that include the cross-sectional area. Strain (Think INch) is the deflection or distance the material stretches. Stress (Think pRESSure) is the force/cross-section, perhaps PSI.
An elastic force that stretches or pulls on the molecules in matter is known as tension. This force occurs when an object is being stretched or pulled in opposite directions.