the fracture in sulfur is 1.52 or 1 32nd of its size
The dominant form of breakage for sulfur is brittle fracture, where the material breaks without significant deformation. This is due to the atomic structure of sulfur, which consists of weak van der Waals forces between the molecules, leading to easy cleavage and fracture.
Cobalt's fracture refers to a type of fracture that occurs in metallic cobalt. It is characterized by a clean break in the metal with no deformation or twisting. This type of fracture is common in metals that are hard and brittle.
The bond type in sulfur can vary depending on the compound. In elemental sulfur (S8), the bond type is predominantly covalent, with the sulfur atoms forming a ring structure held together by covalent bonds. In other sulfur compounds, such as hydrogen sulfide (H2S) or sulfur dioxide (SO2), the bond types can include covalent and polar covalent bonds.
Phosphorus and sulfur can form a covalent bond when they share electrons. This type of bond is known as a phosphorus-sulfur covalent bond.
Sulfur in the S8 molecule forms a type of covalent bond called a disulfide bond. This type of bond involves the sharing of electrons between sulfur atoms to create a stable eight-atom ring structure.
Sulfur can exist in different allotropes, including amorphous sulfur, α-sulfur, β-sulfur, and γ-sulfur. The fracture of sulfur can vary depending on its form, but generally, sulfur exhibits a brittle fracture with irregular or conchoidal patterns.
Sulfur typically exhibits a conchoidal fracture when it breaks, resulting in smooth, curved surfaces resembling glass. This fracture is caused by the arrangement of sulfur atoms in its crystalline structure and the brittleness of the element.
Sulfur has a conchoidal fracture, resembling the curved shape of a seashell when broken. It does not have a distinct cleavage because its atomic structure does not easily allow the mineral to break along specific planes.
The dominant form of breakage for sulfur is brittle fracture, where the material breaks without significant deformation. This is due to the atomic structure of sulfur, which consists of weak van der Waals forces between the molecules, leading to easy cleavage and fracture.
Pathological fracture
Sulfur does not exhibit cleavage because it lacks a distinct crystal structure. Instead, sulfur has a conchoidal fracture, meaning it breaks along curved, irregular surfaces similar to glass.
compacted..
Simple Fracture.
The fracture type of the Pumice rock is either jagged or splintery. The Pumice has both fracture and cleavage type.
Zygomaticomaxillary complex fracture
Open....It's called an OPEN FRACTURE.
A compound fracture is when a bone protrudes through the skin.