carrying power
A stream with gravel and rocks typically has a higher sediment load. The presence of gravel and rocks indicates that the stream has the ability to transport larger particles, which increases its sediment load compared to streams with smaller particles like sand or silt.
bed load. This type of stream load consists of heavier materials that are transported along the stream bed through rolling, sliding, or bouncing. It tends to move more slowly than suspended load or dissolved load.
Streams transport sediment through three primary processes: bed load, suspended load, and dissolved load. Bed load consists of larger particles that roll or slide along the bottom of the stream. Suspended load includes finer particles, such as silt and clay, that are carried within the water column. Dissolved load refers to minerals and nutrients that are dissolved in the water itself, making them invisible to the naked eye.
A stream is most likely to deposit the rock and soil it is carrying when its velocity decreases, such as in a meander or where the gradient lessens. This allows the stream to no longer have enough energy to transport the sediment, leading to deposition.
My understanding is that every glacier has a certain amount of sediment scraped from the interface of the surrounding bed rock and the moving ice. The total amount of this sediment is the Glacial load. Some significant land features, such as Cape Cod in Massachusetts, are remnants of the load after the ice receded.
Deposition, whereby the sediment load being transported is dropped.
Sediment that is carried by a stream along the bottom of its channel.
Bed load typically makes up a small percentage (10-20%) of the total sediment load moved by a stream annually. Most sediment is transported in suspension as suspended load or dissolved load in the water column. Bed load refers to larger particles like sand and gravel that are rolled or pushed along the stream bed by the flow of water.
Stream load refers to the amount of sediment and materials that are being transported by a stream. It can consist of sand, silt, gravel, and organic matter, and is influenced by factors such as stream velocity, discharge, and erosion within the watershed. Monitoring stream load is important for understanding sediment transport and its impact on water quality and ecosystems.
Generally, the highest percentage of the annual sediment load moved by a stream consists of suspended sediment. These are particles like silt and clay that are carried within the stream's water column. Bedload sediment, which is sediment that is moved along the stream bed through rolling or sliding, typically makes up a smaller percentage of the total annual sediment load.
Sediment that is moved along the bottom of a stream is known as bed load. This consists of larger particles like gravel and pebbles that are transported by rolling, sliding, or saltation along the streambed.
Stream transport sediment in three ways, dissolved load, (ions in solution being carried downstream), suspended load, (suspended sediment that floats freely downstream) and bed load, (sediment that rolls or scoots along the bottom of the river).
The sediment that moves along the bed of a stream is called bedload. Bedload consists of larger particles such as sand, gravel, and boulders that are transported by rolling, sliding, or bouncing along the streambed.
The material that a stream carries in solution is called "dissolved load." This includes various substances such as minerals, salts, and organic matter that are dissolved in the water. The dissolved load is distinct from the sediment load, which consists of larger particles that are transported by the stream. Together, they contribute to the overall transport of materials within the stream system.
sediment
the stream load rock,soil,etc.the stream load rock,soil,etc.
Bed load is a term used in the field of geomorphology to describe the particles such as sand, gravel, and pebbles that are transported along the bed of a river or stream by rolling, sliding, or bouncing. These particles are too heavy to be suspended in the water column, unlike suspended load. Bed load movement can contribute to erosion and sediment transport in river systems.