Linked from
The 57 pages that link to Sedimentation, each with the reason it gives.
Sediment transportCompared with: It is the depositional counterpart to the movement emphasized by transport.
Soil erosionRelated: Eroded soil deposited in channels and reservoirs creates sedimentation.
ErosionCompared with: Deposition is the endpoint of transport, rather than the removal of material.
Brownian motionCompared with: Directed settling can compete with random Brownian displacement.
MicroplasticsRelated: Some microplastics settle into riverbeds and seabed sediments, depending on their properties.
SedimentRelated: Sedimentation occurs when transport can no longer keep particles moving.
Indoor air qualityRelated: Some particles leave the air by settling onto indoor surfaces, where they can later be disturbed.
Terminal velocityRelated: Particle settling rates often depend on each particle's terminal velocity.
Phosphorus cycleRelated: Phosphorus bound to particles can settle in aquatic sediments and leave circulation.
ReservoirRelated: Sediment gradually occupies reservoir space and reduces storage capacity.
Sedimentary basinRelated: Accumulation turns available basin space into layered sedimentary fill.
CentrifugationNarrower topic: Centrifugation accelerates sedimentation to make separation faster or possible for small particles.
Soil conservationRelated: Eroded soil can settle in reservoirs and channels, reducing storage and altering waterways.
GradualismRelated: Successive deposits preserve a record of change built up over time.
Stokes' lawRelated: Stokes' law predicts the drag opposing a particle's downward motion.
AdvectionCompared with: Particles can move relative to the fluid, so their transport is not solely advective.
Lake TanganyikaRelated: Lake sediments preserve records of climate, fires, and human activity.
Drinking water treatmentRelated: Settling removes flocs formed during coagulation before water reaches filters.
Membrane filtrationCompared with: It removes settleable solids by motion through a fluid rather than membrane retention.
CentrifugeRelated: Centrifuges accelerate sedimentation, separating suspended particles far faster than gravity alone.
SuspensionRelated: Gravity gradually separates many suspensions into clearer fluid and settled solids.
UnconformityRelated: Deposition before and after a hiatus creates the rock packages separated by the surface.
Gravity separationRelated: Gravity separation often depends on particles settling at different rates.
Coastal geomorphologyRelated: It builds coastal landforms where sediment supply exceeds removal.
Danube DeltaRelated: It builds islands and shallow banks as the Danube slows near the sea.
SiltNarrower topic: Silt accumulation can bury habitats and alter river or lake beds.
ClearcuttingRelated: Eroded soil from harvested slopes can enter streams and settle in aquatic habitats.
Dongting LakeNarrower topic: Sediment deposition has altered Dongting’s depth, shoreline, and capacity over time.
Graded beddingNarrower topic: Graded bedding is a pattern produced during sediment accumulation.
ShaleNarrower topic: Shale begins as deposited mud, commonly settling in low-energy water.
Deforestation in MadagascarRelated: Eroded soil from cleared slopes accumulates in rivers, wetlands, and coastal waters.
Sediment pollutionRelated: Particles settle from the water column and accumulate on stream and lake beds.
VarveNarrower topic: Annual layers arise when sedimentation changes predictably through the year.
Accommodation spaceRelated: Only deposited material fills accommodation space.
LandformRelated: Deposited sediment builds features such as deltas, floodplains, and dunes.
Magmatic sulfide depositRelated: Dense sulfide droplets may settle and accumulate at the base of magma bodies.
SandRelated: Deposition builds the beaches, dunes, and beds where sand collects.
Sedimentary structuresRelated: Depositional conditions determine which structures form and survive.
Abraham Gottlob WernerRelated: The settling of material from water offered Werner a mechanism for forming layered rocks.
Stream ecologyRelated: Fine sediment can bury streambed habitat and affect organisms that live or feed there.
Tarbela DamRelated: Sediment carried by the Indus gradually reduces reservoir storage and affects infrastructure.
Chocolate milkRelated: It explains why cocoa can collect at the bottom of an unstirred drink.
SiltstoneRelated: Silt settles when transporting flows lose enough energy to carry it.
Geochemical cycleRelated: Sedimentation transfers dissolved and particulate elements into long-lived sedimentary reservoirs.
Kagera RiverRelated: Eroded soil can accumulate in the Kagera channel and Lake Victoria.
Badlands National ParkRelated: Ancient sediments created the strata now exposed in the park’s formations.
Land (terrain)Related: Sedimentation builds land in deltas, floodplains, and other depositional environments.
Mechanical screeningCompared with: It can classify particles by settling behavior instead of screen aperture.
Faxén's lawRelated: The law relates background flow variations to forces on settling spheres.
MudrockRelated: Mudrock begins when fine particles settle and accumulate in a depositional environment.