turbidity is pollution, thus runoffs and fertilizer and anything that makes up pollution is turbidity.
Turbidity currents are caused by sand and mud on the continental shelf and slope that is dislodged and thrown into suspension. Turbidity currents themselves are downslope movements of dense, sediment-laden water. Source: I'm in a college level geology course.
Fertilizer can increase turbidity in water bodies when it washes off from fields into rivers or lakes. The nutrients in the fertilizer stimulate excessive algae growth, leading to algal blooms. When these algae die and decompose, they can increase turbidity by releasing organic matter and sediment into the water.
Turbidity in sand can be tested by taking a sample of the sand and mixing it with water in a clear container. After stirring the mixture, observe how quickly the water clears up — the longer it takes for the water to clarify, the higher the turbidity of the sand. Additionally, turbidity can also be measured using a turbidity meter, which provides a numerical value of turbidity in nephelometric turbidity units (NTU).
The unit of turbidity is typically expressed in NTU (Nephelometric Turbidity Units) or FTU (Formazin Turbidity Units). Turbidity is a measure of the relative clarity of a liquid and indicates the amount of suspended particles in the water.
Daniel H. Stern has written: 'Effects of bank stabilization on the physical and chemical characteristics of streams and small rivers' -- subject(s): Erosion, Rivers, Stream channelization, Streambank planting, Turbidity
A dried salt has not turbidity.
The turbidity NTU standards should be less than 5
i have tested the to doing charts and graphs and when stream flow is fast the turbidity raises and and when the stream flow decreases so does the turbidity
The pH and turbidity increases.
Gravity :)
The transport of sediment depends on its grain size and the original location where it was produced. Terrigenous sediment can be transported to the deep sea via rivers or by wind. Material transported by rivers most commonly ends up deposited on thecontinental margin, the shallow portions of the ocean that are within several hundred kilometers of land. When continental margin deposits accumulate fast and get overly steep, or when an earthquake or storm causes the sediment to be resuspended, turbidity currents provide additional transport out to the deep sea. The resuspension of the sediment into the bottom water causes it to be more dense than the overlying water, and thus these turbidity currents flow downslope to the more distant ocean basin -humberto <3