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SEDIMENT TRANSPORT

  • Sediment transport
  • Movement of solid particles, typically by gravity and fluid entrainment

    Sediment transport is the movement of solid particles (sediment), typically due to a combination of gravity acting on the sediment, and the movement of

    Sediment transport

    Sediment transport

    Sediment_transport

  • Sediment
  • Particulate solid matter deposited on a planetary surface

    In Earth and planetary sciences, sediment is a solid material made of loose particles that is transported to a new location where it is deposited. It occurs

    Sediment

    Sediment

    Sediment

  • Swash
  • Turbulent layer of water that washes ashore after a wave breaks

    to result in net onshore sediment transport. If the beachface is steeper than the equilibrium gradient, the sediment transport is dominated by the backwash

    Swash

    Swash

    Swash

  • Sedimentary rock
  • Rock formed by the deposition and cementation of particles

    and can transport heavier clastic material. Besides transport by water, sediment can be transported by wind or glaciers. Sediment transported by wind

    Sedimentary rock

    Sedimentary rock

    Sedimentary_rock

  • HEC-RAS
  • Software for simulating water flow within rivers

    include quasi-unsteady and unsteady flow, two dimensional modeling, sediment transport and water quality modeling, and distributed hydrologic modeling (Rain-on-Grid

    HEC-RAS

    HEC-RAS

    HEC-RAS

  • Fluvial sediment processes
  • Sediment processes associated with rivers and streams

    fluvial sediment processes or fluvial sediment transport are associated with rivers and streams and the deposits and landforms created by sediments. It can

    Fluvial sediment processes

    Fluvial sediment processes

    Fluvial_sediment_processes

  • Coastal sediment transport
  • Movement of sediment along coastal environments

    Coastal sediment transport (a subset of sediment transport) is the interaction of coastal land forms to various complex interactions of physical processes

    Coastal sediment transport

    Coastal sediment transport

    Coastal_sediment_transport

  • Terrigenous sediment
  • Sediments derived from the erosion of rocks on land

    rocks may result in terrigenous sediment. Creation, transport, deposition and lithification of terrigenous sediment into sedimentary rocks make up an

    Terrigenous sediment

    Terrigenous_sediment

  • Pelagic sediment
  • Fine-grained sediment that accumulates on the floor of the open ocean

    Pelagic sediment or pelagite is a fine-grained sediment that accumulates as the result of the settling of particles to the floor of the open ocean, far

    Pelagic sediment

    Pelagic sediment

    Pelagic_sediment

  • Marine sediment
  • Accumulated material on seafloor

    taking thousands of years for any significant deposits to form. Sediment transported from the land accumulates the fastest, on the order of one metre

    Marine sediment

    Marine sediment

    Marine_sediment

  • Longshore drift
  • Sediment moved by the longshore current

    importance to sediment transport. This then led to the development in the concept of "longshore currents," which in turn transport sediment along the coast

    Longshore drift

    Longshore drift

    Longshore_drift

  • Foredune
  • Dune ridge that runs parallel to the shore of a body of water

    river systems. As a result, sediment from tributaries and headwaters are deposited at the mouth of the river. Long shore transport is a linear current off

    Foredune

    Foredune

  • Sedimentation
  • Tendency for particles in suspension to settle down

    sedimentary rock, from initial erosion through sediment transport and settling to the lithification of the sediments. However, the strict geological definition

    Sedimentation

    Sedimentation

    Sedimentation

  • Internal wave breaking
  • Fluid dynamics process driving mixing in the oceans

    circulation. On smaller scales, breaking-induced mixing is important for sediment transport and for nutrient supply to the photic zone. Most breaking of oceanic

    Internal wave breaking

    Internal wave breaking

    Internal_wave_breaking

  • Hans Albert Einstein
  • Swiss-American engineer and educator

    1947 until 1971. Einstein was widely recognized for his research on sediment transport. To honor his outstanding achievement in hydraulic engineering, the

    Hans Albert Einstein

    Hans Albert Einstein

    Hans_Albert_Einstein

  • Okavango River
  • Major river in southern Africa

    28,000 tonnes of suspended sediment and a similar amount of bedload to the terminal swamps. Most of the particulate sediment carried by the river is fine

    Okavango River

    Okavango River

    Okavango_River

  • Deposition (geology)
  • Natural addition of materials to a landmass

    geological process in which sediments, soil and rocks are added to a landform or landmass. Wind, ice, water, and gravity transport previously weathered surface

    Deposition (geology)

    Deposition (geology)

    Deposition_(geology)

  • Clastic rock
  • Sedimentary rocks made of mineral or rock fragments

    to sedimentary rocks and particles in sediment transport, whether in suspension or as bed load, and in sediment deposits. Clastic sedimentary rocks are

    Clastic rock

    Clastic rock

    Clastic_rock

  • Gilgel Abay
  • River in Ethiopia

    million tonnes of suspended sediment to Lake Tana. List of Ethiopian rivers Hanibal Lemma, and colleagues (2019). "Bedload transport measurements in the Gilgel

    Gilgel Abay

    Gilgel Abay

    Gilgel_Abay

  • Bed material load
  • Component in the load of a river system

    load and wash load. The bed material load is the portion of the sediment that is transported by a stream that contains material derived from the bed. Bed

    Bed material load

    Bed_material_load

  • Canterbury Bight
  • Oceanic bight in Canterbury, New Zealand

    six potential sediment sources for beach environments. These are longshore transport, onshore transport, wind transport, river transport (and alluvial

    Canterbury Bight

    Canterbury Bight

    Canterbury_Bight

  • Bedform
  • Geological feature resulting from the movement of bed material by fluid flow

    rates of sediment transport. "Upper plane bed" features are flat and characterized by a unidirectional flow with high rates of sediment transport as both

    Bedform

    Bedform

    Bedform

  • Wave nonlinearity
  • Feature of surface gravity waves

    skewness and asymmetry of surface gravity waves are the main drivers for sediment transport. Sinusoidal waves (or linear waves) are waves having equal height

    Wave nonlinearity

    Wave_nonlinearity

  • Interior Plains
  • Physiographic and geologic region of North America

    reduced the annual transport rate to between 100 and 150 million tons of sediment per year. The artificial structures trap suspended sediment from traveling

    Interior Plains

    Interior Plains

    Interior_Plains

  • Kaikōura Canyon
  • Submarine canyon near New Zealand

    southwest Pacific Basin. It is thought to be the sink for the coastal sediment transport system that carries large amounts of erosional debris northwards up

    Kaikōura Canyon

    Kaikōura_Canyon

  • Kuroshio Current
  • North-flowing current in the northwest Pacific Ocean

    biological processes of the North Pacific Ocean, including nutrient and sediment transport, major Pacific storm tracks and regional climate, and Pacific mode

    Kuroshio Current

    Kuroshio Current

    Kuroshio_Current

  • Inlet
  • Indentation of a shoreline

    Alongshore sediment transport can cause inlets to close if the action of tidal currents flowing through an inlet do not flush accumulated sediment out of

    Inlet

    Inlet

    Inlet

  • Geomorphology
  • Scientific study of landforms

    the landscape. Fluvial geomorphologists focus on rivers, how they transport sediment, migrate across the landscape, cut into bedrock, respond to environmental

    Geomorphology

    Geomorphology

    Geomorphology

  • Suspended load
  • Portion of sediment uplifted by a fluid's flow

    three layers of the fluvial sediment transportation system. The bed load consists of the larger sediment which is transported by saltation, rolling, and

    Suspended load

    Suspended_load

  • Nazaré Canyon
  • Submarine canyon in the North Atlantic Ocean

    The project is investigating the specialized canyon ecosystems, sediment transport and deposition, and the way in which the canyon influences and is

    Nazaré Canyon

    Nazaré Canyon

    Nazaré_Canyon

  • Siltation
  • Water pollution caused by particulate terrestrial clastic material

    preferred for its lack of ambiguity. The origin of the increased sediment transport into an area may be erosion on land or activities in the water. In

    Siltation

    Siltation

    Siltation

  • Aeolian landform
  • Landforms produced by action of the wind

    air. These means of sediment transport can be classified as creep, saltation, and suspension, respectively. Once sediment transport begins, it continues

    Aeolian landform

    Aeolian_landform

  • Traction (geology)
  • clasts interact with the substratum during transport. By contrast, saltation, a related sediment transport process, moves grains across the bottom by

    Traction (geology)

    Traction (geology)

    Traction_(geology)

  • Cross-bedding
  • Sedimentary rock strata at differing angles

    indicates paleocurrent, the rough direction of sediment transport. The type and condition of sediments can tell geologists the type of environment (rounding

    Cross-bedding

    Cross-bedding

    Cross-bedding

  • Hjulström curve
  • Method for determining sediment motion in rivers

    hydrologists and geologists to determine whether a river will erode, transport, or deposit sediment. It was originally published in his doctoral thesis "Studies

    Hjulström curve

    Hjulström curve

    Hjulström_curve

  • Kulfo River
  • River in Ethiopia

    material is 14 mm (gravel). The river transports 53,480 tonnes of bedload and 327,230 tonnes of suspended sediment annually to Lake Chamo. Cytotaxonomic

    Kulfo River

    Kulfo_River

  • Li Guoying
  • Chinese politician

    stated that the Xiaolangdi reservoir's sediment would be managed using natural methods. A proposed sediment transport device would require low investment

    Li Guoying

    Li Guoying

    Li_Guoying

  • Nile
  • Major river in northeast Africa

    built. Annual sediment transport measured at several locations are listed below. The bedload percentages are the ratio of bedload sediment to total (bedload

    Nile

    Nile

    Nile

  • Sedimentary structures
  • Geologic structures formed during sediment deposition

    structures include all kinds of features in sediments and sedimentary rocks, formed at the time of deposition. Sediments and sedimentary rocks are characterized

    Sedimentary structures

    Sedimentary structures

    Sedimentary_structures

  • River delta
  • Silt deposition landform at the mouth of a river

    velocity, which diminishes the ability of the flow to transport sediment. As a result, sediment drops out of the flow and is deposited as alluvium, which

    River delta

    River delta

    River_delta

  • Transportation (disambiguation)
  • Topics referred to by the same term

    (psychology), which concerns psychological immersion in narrative content. Sediment transport, the movement of weathered rocks from one place to another. Transportation

    Transportation (disambiguation)

    Transportation_(disambiguation)

  • Sediment gravity flow
  • Sediment transport mechanism

    A sediment gravity flow is one of several types of sediment transport mechanisms, of which most geologists recognize four principal processes. These flows

    Sediment gravity flow

    Sediment gravity flow

    Sediment_gravity_flow

  • Hemipelagic sediment
  • Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic

    Hemipelagic sediment

    Hemipelagic_sediment

  • Risks to the Glen Canyon Dam
  • the river channel that changed how sediment is stored and redistributed downstream. Since natural sediment transport processes were disrupted, controlled

    Risks to the Glen Canyon Dam

    Risks to the Glen Canyon Dam

    Risks_to_the_Glen_Canyon_Dam

  • Stream power
  • valuable measurement for hydrologists and geomorphologists tackling sediment transport issues as well as for civil engineers, who use it in the planning

    Stream power

    Stream power

    Stream_power

  • Stream competency
  • Concept in hydrology

    mobilize the sediment on the bed of the channel helps us predict whether or not sediment transport is likely to occur, and to some degree, the sediment size likely

    Stream competency

    Stream competency

    Stream_competency

  • Downhill creep
  • Slow, downward progression of rock and soil down a low grade slope

    ridges in the landscape. Creep (deformation) Colluvium Mass wasting Sediment transport Solifluction Clark, Christine Anne. "The important role of soil texture

    Downhill creep

    Downhill creep

    Downhill_creep

  • River morphology
  • Change in shape and direction of river channels over time

    the availability of sediment; the size and composition of the sediment moving through the channel; the rate of sediment transport through the channel

    River morphology

    River_morphology

  • Wash load
  • Sedimentary process of rivers

    the wash loads source of sediment is defined as "sediment in transport that is derived from sources other than the bed." Sediment motion is one way of classifying

    Wash load

    Wash_load

  • Erosion
  • Natural processes removing soil and rock

    material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres.

    Erosion

    Erosion

    Erosion

  • Seabed
  • Bottom of the ocean

    physics of sediment transport and by the biology of the creatures living in the seabed and in the ocean waters above. Physically, seabed sediments often come

    Seabed

    Seabed

    Seabed

  • Hydrological transport model
  • Type of mathematical model

    Saint-Venant equations of continuity and momentum Overland Flow Sediment Transport: 2D total sediment load conservation equation Unsaturated Flow: Richards equation

    Hydrological transport model

    Hydrological transport model

    Hydrological_transport_model

  • Sediment basin
  • conjunction with erosion controls and other sediment control practices. Erosion control Sediment transport Silt fence Florida Department of Environmental

    Sediment basin

    Sediment basin

    Sediment_basin

  • Coastal morphodynamics
  • Interaction of shoreline seafloor topography and fluid hydrodynamic processes

    landforms and physical processes, such as waves, tides, currents, wind, sediment transport, and severe weather events. Shoreline evolution occurs over short-

    Coastal morphodynamics

    Coastal morphodynamics

    Coastal_morphodynamics

  • Sorting (sediment)
  • Distribution of grain size of sediments

    wind patterns at the sediment source can affect grain size, rate of transport and distribution of sediment. Windblown sediment travels one of three ways--rolling

    Sorting (sediment)

    Sorting (sediment)

    Sorting_(sediment)

  • Arthur T. Ippen
  • American hydrologist and engineer (1907–1974)

    supervised by Theodore von Kármán and Robert T. Knapp, explored sediment transport and open-channel high-velocity flows and represented the first American

    Arthur T. Ippen

    Arthur_T._Ippen

  • Laminar sublayer
  • to the bed sediment or other factors are smaller or larger than this sublayer has an important bearing in hydraulics and sediment transport. Flow is defined

    Laminar sublayer

    Laminar_sublayer

  • Glossary of landforms
  • Outwash fan – Type of sediment deposition by a melting glacier Outwash plain – Plain formed from glacier sediment transported by meltwater Rift valley –

    Glossary of landforms

    Glossary_of_landforms

  • Shear velocity
  • Form of shear stress

    velocity profile near the boundary of a flow (see Law of the wall) Transport of sediment in a channel Shear velocity also helps in thinking about the rate

    Shear velocity

    Shear_velocity

  • Geology of the Grand Canyon area
  • Aspect of geology

    to excavate the canyon. Dams in particular have upset patterns of sediment transport and deposition. Controlled floods from Glen Canyon Dam upstream have

    Geology of the Grand Canyon area

    Geology of the Grand Canyon area

    Geology_of_the_Grand_Canyon_area

  • Mouth bar
  • River bar in middle of river mouth

    the sediment transported by the river channel at the river mouth. River mouth bars form because the cross-sectional area of the expanding sediment-laden

    Mouth bar

    Mouth_bar

  • Einstein family
  • Family of physicist Albert Einstein

    University of California, Berkeley, widely recognized for his research on sediment transport. Hans Albert had four children, three biological sons and one adopted

    Einstein family

    Einstein family

    Einstein_family

  • Debouch
  • Water runoff from a smaller place to a larger one

    sediment transport. When a narrow stream travels down a mountain pass into a basin, an alluvial fan will form from the mass deposit of the sediment.

    Debouch

    Debouch

    Debouch

  • Sediment–water interface
  • Boundary between bed sediment and the overlying water column

    In oceanography and limnology, the sediment–water interface is the boundary between bed sediment and the overlying water column. The term usually refers

    Sediment–water interface

    Sediment–water interface

    Sediment–water_interface

  • Stream capacity
  • Total amount of sediment a stream can transport

    The capacity of a stream or river is the total amount of sediment a stream is able to transport. This measurement usually corresponds to the stream power

    Stream capacity

    Stream_capacity

  • Nonlinear tides
  • Hydrodynamic distortions of tides

    oceanography. The nonlinearity of tides has important implications for the transport of sediment. From a mathematical perspective, the nonlinearity of tides originates

    Nonlinear tides

    Nonlinear_tides

  • List of rivers by discharge
  • (PDF). The Pacific and Caribbean Rivers of Colombia: Water Discharge, Sediment Transport and Dissolved Loads. Archived from the original (PDF) on 2012-03-25

    List of rivers by discharge

    List of rivers by discharge

    List_of_rivers_by_discharge

  • Wadi
  • Hydrological feature

    2009. Achite, Mohamed; Ouillon, Sylvain (September 2007). "Suspended sediment transport in a semiarid watershed, Wadi Abd, Algeria (1973–1995)". Journal of

    Wadi

    Wadi

    Wadi

  • Subhasish Dey
  • Indian hydraulician and educator

    the sediment dynamics phenomena from the viewpoint of core fluid mechanics. S. Dey (2024). Fluvial Hydrodynamics: Hydrodynamic and Sediment Transport Phenomena

    Subhasish Dey

    Subhasish Dey

    Subhasish_Dey

  • Ice rafting
  • Transport of various materials by drifting ice

    (IRD) or ice rafted deposits. Ice rafting was a primary mechanism of sediment transport during glacial episodes of the Pleistocene when sea levels were very

    Ice rafting

    Ice rafting

    Ice_rafting

  • GSSHA
  • Two-dimensional model

    It simulates surface water and groundwater hydrology, erosion and sediment transport. The GSSHA model is used for hydraulic engineering and research, and

    GSSHA

    GSSHA

  • TELEMAC
  • Open source software for computational fluid dynamics

    break Regulation of managed rivers Flow in torrents, Canals wetting Sediment Transport Water quality (temperature, passive tracers ...) ARTEMIS is a scientific

    TELEMAC

    TELEMAC

    TELEMAC

  • Rouse number
  • Non-dimensional number in fluid dynamics

    of suspended sediment and which also determines how sediment will be transported in a flowing fluid. It is a ratio between the sediment fall velocity

    Rouse number

    Rouse_number

  • Filip Hjulström
  • Swedish geographer

    suspended sediment content. His students followed in the same vein, making quantitative studies of mass transport (Anders Rapp), fluvial transport (Åke Sundborg)

    Filip Hjulström

    Filip Hjulström

    Filip_Hjulström

  • Sandstone
  • Type of sedimentary rock

    transported by rivers or by the wind from its source areas to depositional environments where tectonics has created accommodation space for sediments

    Sandstone

    Sandstone

    Sandstone

  • River channel migration
  • Geomorphological process

    meandering streams. In braided streams, channel change is driven by sediment transport. It has been proposed that lateral migration is a particularly dominant

    River channel migration

    River channel migration

    River_channel_migration

  • Attert (river)
  • River in Belgium and Luxembourg

    regional geology, resulting in seasonal variations in water flow and sediment transport. Since 2001, Belgium and Luxembourg have jointly managed the river

    Attert (river)

    Attert (river)

    Attert_(river)

  • Ken Kamrin
  • American applied mathematician

    Advances 7 (17), eabe0631 (2021) Grain shape effects in bed load sediment transport. E Deal, JG Venditti, SJ Benavides, R Bradley, Q Zhang, K Kamrin,

    Ken Kamrin

    Ken Kamrin

    Ken_Kamrin

  • Po (river)
  • River in Italy

    heighten and strengthen levees, increase flood-meadows, resume natural sediment transport and deposition points, enlarge wetlands, afforest, re-nature, promote

    Po (river)

    Po (river)

    Po_(river)

  • Stream restoration
  • Work to improve the environmental health of a river or stream

    restoration of hydrological and geomorphological processes (such as sediment transport or connectivity between the channel and the floodplain) to ensure

    Stream restoration

    Stream restoration

    Stream_restoration

  • Palm Islands
  • Artificial islands in Dubai, UAE

    alongshore sediment transport, and wave patterns.[unreliable source?] The origin of most of the environmental damage stems from disturbed sediment from the

    Palm Islands

    Palm Islands

    Palm_Islands

  • Meander
  • One of a series of curves in a channel of a matured stream

    produced as a watercourse erodes the sediments of an outer, concave bank (cut bank or river cliff) and deposits sediments on an inner, convex bank which is

    Meander

    Meander

    Meander

  • List of river systems by length
  • Pantoja; Martinez, Jean-Michel; Harmel, Tristan (2022-01-13). "Suspended sediment transport estimation in Negro River (Amazon Basin) using MSI/Sentinel-2 data"

    List of river systems by length

    List of river systems by length

    List_of_river_systems_by_length

  • River mouth
  • End of a river where it flows into a larger body of water

    advective transports, inflowing water will also diffuse. At the mouth of a river, the change in flow conditions can cause the river to drop any sediment it is

    River mouth

    River mouth

    River_mouth

  • Bioturbation
  • Reworking of soils and sediments by organisms

    on sediment transport and are as follows: Gallery-diffusers create complex tube networks within the upper sediment layers and transport sediment through

    Bioturbation

    Bioturbation

    Bioturbation

  • Coastal engineering
  • Branch of civil engineering

    interest. In case of studies of sediment transport and morphological changes, relevant properties of the sea bed sediments, water and ecosystem properties

    Coastal engineering

    Coastal engineering

    Coastal_engineering

  • Colin Thorne
  • English academic

    bed rivers" United Kingdom - 1985 Gravel Bed Rivers Workshop 2: "Sediment Transport in gravel bed rivers" Colorado State, US - 1990 Gravel Bed Rivers

    Colin Thorne

    Colin Thorne

    Colin_Thorne

  • Eco Bijker
  • Dutch civil engineer

    morphology, sediment transport, and the modelling of coastal dynamics. Bijker is particularly known for formulating a sediment transport model which quantifies

    Eco Bijker

    Eco Bijker

    Eco_Bijker

  • Sadler effect
  • The Sadler effect describes variation in apparent sediment accumulation rates and bed thicknesses back through time inherent to the geological sedimentary

    Sadler effect

    Sadler_effect

  • Sedimentary budget
  • within a coastal system. Sediment sources can include river transport, sea cliff erosion and longshore drift into an area. Sediment sinks can include longshore

    Sedimentary budget

    Sedimentary budget

    Sedimentary_budget

  • Exner equation
  • Law of sediment aggradation

    describes conservation of mass between sediment in the bed of a channel and sediment that is being transported. It states that bed elevation increases

    Exner equation

    Exner_equation

  • East Island (Hawaii)
  • Mostly eroded island of Hawaii

    observations in subsequent years revealed partial recovery. By 2024, natural sediment transport had restored roughly 60 percent of East Island's former land area

    East Island (Hawaii)

    East Island (Hawaii)

    East_Island_(Hawaii)

  • Blowout (geomorphology)
  • Depressions in a sand dune ecosystem caused by the removal of sediments by wind

    direction, wind erosion may be capable of removing and transporting large amounts of sediment particles, which could create blowouts. Thus, although the

    Blowout (geomorphology)

    Blowout (geomorphology)

    Blowout_(geomorphology)

  • Ralph Bagnold
  • British Army officer (1896–1990)

    1979. Sediment transport by wind and water. Nordic Hydrology 10(5):309–322. Bagnold, R.A. 1980. An empirical correlation of bedload transport rates in

    Ralph Bagnold

    Ralph Bagnold

    Ralph_Bagnold

  • Cobble (geology)
  • Clast of rock

    Distributions in Wadable Gravel- and Cobble-Bed Streams for Analyses in Sediment Transport, Hydraulics, and Streambed Monitoring (PDF). Rocky Mountain Research

    Cobble (geology)

    Cobble (geology)

    Cobble_(geology)

  • Spit (landform)
  • Coastal bar or beach landform deposited by longshore drift

    angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water

    Spit (landform)

    Spit (landform)

    Spit_(landform)

  • Peresyp
  • Russian name for the sandbar which forms an estuary lagoon

    of a deltaic system. A peresyp or mouth bar is a deposit of the sediment transported by the river—i.e., a shoal or sandbar—at the river mouth, typically

    Peresyp

    Peresyp

    Peresyp

  • Bombetoka Bay
  • Bay in Madagascar

    common, while coffee plantations abound in the surrounding terrain. Sediment transport and suspension in Bombetoka Bay has significantly changed during the

    Bombetoka Bay

    Bombetoka Bay

    Bombetoka_Bay

  • Sea buckthorn
  • Species of flowering plant

    effectively stabilises slopes, reduces surface runoff, and controls sediment transport, particularly in areas prone to erosion from rainstorms. The fruit

    Sea buckthorn

    Sea buckthorn

    Sea_buckthorn

  • Outwash fan
  • Type of sediment deposition by a melting glacier

    fan-shaped body of sediments deposited by braided streams from a melting glacier. Sediment locked within the ice of the glacier gets transported by the streams

    Outwash fan

    Outwash fan

    Outwash_fan

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