Suspended load
A load is the term for particles carried by a stream or river.
The different types of loads in a stream include bed load (particles moving along the stream bed), suspended load (fine particles carried in the water column), and dissolved load (chemical substances carried in solution). These loads contribute to the overall sediment transport and water quality of the stream.
Solid particles in a stream can include sediment, rocks, sand, gravel, and organic material like leaves or sticks. These particles are carried along by the flow of water and can vary in size and composition depending on the stream's location and characteristics.
Particles of sand and pebbles that are less dense than water are carried by a stream through a process called suspension. The flow of the water exerts enough force to keep these lighter particles suspended in the water and move them downstream. The particles are lifted off the streambed and transported until the flow of the water slows down or they encounter an obstacle that causes them to settle.
Sediment that is carried by a stream along the bottom of its channel.
Sediments are carried as the following loads: dissolved, suspended, and bed. A dissolved load is composed of ions in solution. These ions are usually carried in the water all the way to the ocean. ... Particles that are too large to be carried as suspended loads are bumped and pushed along the stream bed, called bed load.
The measure of the largest particles a stream can carry is capacity.
Little sediments are carried by the eroding stream
load or stream load.
The measure of the largest particles that a stream can carry is typically determined by its stream power, bed material size, and flow velocity. Streams with higher stream power and flow velocity are able to transport larger particles. The largest particles a stream can carry before they settle to the streambed are usually referred to as the stream's "bedload" particles.
load
A logarithmic graph would best represent the relationship between stream velocity and the size of particles it can carry downstream. As velocity increases, the stream can carry larger particles due to increased erosion and transport capacity. However, there will be a limit to the size of particles carried downstream as velocity continues to increase.