The answer is carrying capacity.
The formula for mean particle size is calculated by summing the individual particle sizes and dividing by the total number of particles. Mathematically, it is expressed as mean particle size = (Σ particle sizes) / total number of particles.
No, sediment particles can vary in size from fine clay and silt to coarser sand and gravel. Sediment can contain a mixture of different particle sizes depending on the source and transport processes.
Particles can vary in size depending on the type of particle. For example, an atom is about one angstrom in size, while a typical virus particle can range from 20 to 400 nanometers. In contrast, a dust particle might be around 10 micrometers in size.
If you were to graph particle size and porosity, it would be a constant slope (horizontal line).Porosity is not affected by particle size.
dont no
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.
When stream flow decreases to below the critical settling velocity of a certain size particle, the particle will settle out of suspension and deposit on the streambed. This process is known as sediment deposition and is influenced by factors such as stream velocity, particle size, and sediment concentration.
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 approximate minimum stream velocity needed to move a particle with a diameter of 6.4 can be determined using the equation for the critical velocity of sediment transport. For a particle of this size, the critical velocity is typically around 0.3-0.4 m/s in most natural streams and rivers.
The measure of the largest particles a stream can carry is capacity.
When stream flow decreases below the critical settling velocity of a certain size particle, the particle will settle out of the flow and deposit on the streambed. This process is known as sedimentation and can lead to the formation of sediment layers along the stream channel. Over time, these deposits can alter the shape and depth of the stream channel.
The maximum size of a clay particle is around 0.002 millimeters or 2 micrometers. Clay particles are some of the smallest soil particles, much smaller than silt or sand particles.
The competence of a stream is determined by the stream's velocity and the size of the sediment it can transport. Streams with higher velocities and larger sediment sizes are typically more competent and can transport larger particles.
the deepest will be at the very bottom
FALSE
FALSE