The maximum size particle a stream can carry is primarily controlled by the stream's velocity and discharge, which is the volume of water flowing per unit of time. Faster-moving water can transport larger and heavier particles due to increased kinetic energy. Additionally, the stream's gradient and channel shape can influence sediment transport, with steeper gradients typically facilitating the movement of larger particles. Lastly, the sediment's shape and density also play a role in determining its transport capacity.
The carrying capacity of a stream refers to the maximum amount of sediment and material it can transport, which is influenced by its discharge and velocity. Higher discharge increases the volume of water flow, allowing the stream to carry more sediment. Similarly, greater velocity enhances the stream's ability to lift and carry particles, increasing its overall carrying capacity. Therefore, both discharge and velocity are critical factors that determine how much material a stream can transport.
virus
A virus is a particle that can carry out some life processes, such as reproduction and evolution, but requires a host cell to carry out metabolic processes. Viruses are considered obligate intracellular parasites and cannot replicate on their own.
The proton carries a positive charge, so it does not carry a negative charge. The β particle (an electron or positron) carries a negative charge.γ rays are electromagnetic radiation and do not carry a charge. The α particle carries a positive charge.
A positively charged subatomic particle is a proton. Protons are found within the nucleus of an atom and carry a positive electrical charge.
The largest size particle that a stream can carry is typically referred to as the stream's competency limit. This limit is reached when the stream's velocity is no longer able to transport a particle of a certain size due to its weight and shape, causing the particle to be deposited on the streambed instead.
The minimum stream velocity needed to carry a particle of sand depends on the size and weight of the sand particle, as well as the characteristics of the stream such as flow rate and turbulence. In general, for typical sand particles, a stream velocity of around 0.3 m/s to 1 m/s is needed to entrain and transport them.
The measure of the largest particles a stream can carry is capacity.
The particle model describes light as a stream of tiny particles called photons. Photons have no mass, but they carry energy and momentum. This model helps explain some behaviors of light, such as the photoelectric effect.
The capacity of a stream is the maximum load it can carry. Capacity is directly related to a stream's discharge. The greater the volume of water in a stream is, the greater its capacity is for carrying sediment. So if a stream's discharge decreases, the stream's capacity also decreases.
Light can act as a stream of photons, which are elementary particles that carry energy and momentum. These photons can exhibit both wave-like and particle-like properties, depending on the specific experimental conditions.
Light exhibits both wave-like and particle-like properties. It can be described as a stream of particles called photons, which carry energy and momentum. This duality is known as the wave-particle duality of light.
The particle thought to carry the electromagnetic force is called the photon.
The measure of the largest particles a stream can carry is capacity.
IF and ONLY IF when the mass of particles are same. Large particle sizes will need high stream's velocity to carry it from one place to another,In another word If the stream velocity is slow than large particle sizes will be stationary.
The carrying capacity of a stream refers to the maximum amount of sediment and material it can transport, which is influenced by its discharge and velocity. Higher discharge increases the volume of water flow, allowing the stream to carry more sediment. Similarly, greater velocity enhances the stream's ability to lift and carry particles, increasing its overall carrying capacity. Therefore, both discharge and velocity are critical factors that determine how much material a stream can transport.
The capacity of a stream is related to its ability to transport sediment and water, which is influenced by factors such as flow velocity, channel shape, and gradient. It refers to the maximum amount of sediment that a stream can carry without deposition. As the flow increases, the stream's capacity also rises, allowing it to transport larger and more sediment. Understanding stream capacity is crucial for managing erosion, sedimentation, and aquatic habitats.