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Sediment is the result of erosion. Sedimentation is the build-up of eroded soil particles that are transported in runoff from their site of origin and deposited in drainage systems, on other ground surfaces, or in bodies of water or wetlands.
Examples of temporary measures include topsoiling, seeding, slope texturing, synthetic permeable barrier, mulching, RECP coverings, silt fence, rolls, wattles, straw bale barriers, etc.
Part 91, Soil Erosion and Sedimentation Control, of the Natural Resources and Environmental Protection Act (NREPA) (Part 91) provides for the control of soil erosion and protects adjacent properties and the waters of the state from sedimentation.
Sediment yield (SY) is defined as the amount of sediment leaving the watershed or catchment, and gross erosion is defined as the absolute amount of erosion occurring within the catchment.
Sediment consists of mineral and organic particles that are displaced by a variety of surface and mass erosion processes (see entry on Soil Erosion). Sedimentation is a more general term relating to the entrainment, transport and deposition of sediments.
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Erosion control practices are typically designed to prevent detachment and transportation of soil particles while sediment control is designed to trap eroding soil on-site.
Best Management Practices for Erosion and Sediment Control Stabilize soils with vegetation, synthetic products or, if necessary, appropriate chemicals. Divert stormwater so it does not come in contact with exposed soil. Avoid having very steep slopes or other areas of potential high erosion.
Erosion and deposition are related opposites; erosion removes sediment from a land form while deposition adds sediment to a land form. Erosion is the process by which rock and mineral particles are separated from a larger body.

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