Confluence

Meeting of two or more bodies of flowing water From Wikipedia, the free encyclopedia

Confluence

In geography, a confluence (also conflux) occurs where two or more watercourses join to form a single channel.[1] A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers, forming the Ohio River); or where two separated channels of a river (forming a river island) rejoin downstream from their point of separation.

Thumb
Confluence of the Bhagirathi and Alaknanda Rivers at the Ganges in Devprayag, India
Thumb
The same confluence viewed from upstream at a different time; note the swirl of sediment from the Alaknanda River

Scientific study

Summarize
Perspective
Thumb
Confluence of the Mississippi, Missouri, and Illinois rivers with normal water levels in 1991, and during a flood in 1993

Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools.[2] The water flows and their consequences are often studied with mathematical models.[3] Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern [downstream of confluences] of increasing stream flow and decreasing slopes drives a corresponding shift in habitat characteristics."[4]

Another science relevant to the study of confluences is chemistry, because sometimes the mixing of the waters of two streams triggers a chemical reaction, particularly in a polluted stream. The United States Geological Survey gives an example: "chemical changes occur when a stream contaminated with acid mine drainage combines with a stream with near-neutral pH water; these reactions happen very rapidly and influence the subsequent transport of metals downstream of the mixing zone."[5]

A natural phenomenon at confluences that is obvious even to casual observers is a difference in color between the two streams; see images in this article for several examples. According to Lynch, "the color of each river is determined by many things: type and amount of vegetation in the watershed, geological properties, dissolved chemicals, sediments and biologic content – usually algae." Lynch also notes that color differences can persist for miles downstream before they finally blend completely.[6]

Flow zones

Thumb
Hydrodynamic features of a river/flume confluence can be separated into six identifiable distinct zones, also called confluence flow zones.

Hydrodynamic behaviour of flow in a confluence can be divided into six distinct features[7] which are commonly called confluence flow zones (CFZ). These include

  1. Stagnation zone
  2. Flow deflection zone
  3. Flow separation zone / recirculation zone
  4. Maximum velocity zone
  5. Flow recovery zone
  6. Shear layers

Engineering

Thumb
Arroyo J. Benítez transition structure within the eastern abutment of the river Monterroso culvert network.

The broader field of engineering encompasses a vast assortment of subjects which concern confluences.

In hydraulic civil engineering, where two or more underground culverted / artificially buried watercourses intersect, great attention should be paid to the hydrodynamic aspects of the system to ensure the longevity and efficiency of the structure.[8]

Engineers must design these systems with consideration of factors that ensure the discharge point is structurally stable as the entrance of the lateral culvert into the main structure may compromise the stability of the structure due to the lack of support at the discharge; this often constitutes additional supports in the form of structural bracing.[9][10] The velocities and hydraulic efficiencies should be meticulously calculated and can be altered by integrating different combinations of geometries, components such a gradients, cascades and an adequate junction angle which is sympathetic to the direction of the watercourse’s flow to minimise turbulent flow, maximise evacuation velocity and to ultimately maximise hydraulic efficiency.[11]

Cultural and societal significance

Summarize
Perspective
Thumb
The fountain at Point State Park in Pittsburgh, at the apex of the confluence of the Allegheny (top) and the Monongahela

Since rivers often serve as political boundaries, confluences sometimes demarcate three abutting polities, such as nations, states, or provinces, forming a tripoint. Various examples are listed below.

Many major cities, such as Chongqing, St. Louis, and Khartoum, arose at confluences; further examples appear in the list. Within a city, a confluence often forms a visually prominent point, so that confluences are sometimes chosen as the site of prominent public buildings or monuments, as in Koblenz, Lyon, and Winnipeg. Cities also often build parks at confluences, sometimes as projects of municipal improvement, as at Portland and Pittsburgh. In other cases, a confluence is an industrial site, as in Philadelphia or Mannheim. Often a confluence lies in the shared floodplain of the two rivers and nothing is built on it, for example at Manaus, described below.

One other way that confluences may be exploited by humans is as sacred places in religions. Rogers suggests that for the ancient peoples of the Iron Age in northwest Europe, watery locations were often sacred, especially sources and confluences.[12] Pre-Christian Slavic peoples chose confluences as the sites for fortified triangular temples, where they practiced human sacrifice and other sacred rites.[13] In Hinduism, the confluence of two sacred rivers often is a pilgrimage site for ritual bathing.[14] In Pittsburgh, a number of adherents to Mayanism consider their city's confluence to be sacred.[15]

Notable confluences

Summarize
Perspective
Thumb
The White Nile and Blue Nile merge at Khartoum; April 2013 satellite view

Africa

Asia

Thumb
The Nam Khan flows into the Mekong at Luang Prabang in Laos
Thumb
The confluence of the Jialing and the Yangtze in Chongqing. The Yangtze flows left to right across the bottom of the image.
Thumb
The Kolam Biru in Kuala Lumpur

Australia

Europe

Thumb
The Seine becomes a single channel at the west end of the Île de la Cité in Paris. The Pont Neuf can be seen.

Seine

  • The Seine divides in the historical center of Paris, flowing around two river islands, the Île Saint-Louis and the Île de la Cité. At the downstream confluence, where the river becomes a single channel again, the Île de la Cité is crossed by the famous Pont Neuf, adjacent to an equestrian statue of King Henri IV and the historically more recent Vert Galant park. The site has repeatedly been portrayed by artists including Monet, Renoir, and Pissarro.
  • Further upstream, the Marne empties into the Seine at Charenton-le-Pont and Alfortville, just southeast of the Paris city limits. The site is dominated by the Huatian Chinagora [fr], a four-star hotel under Chinese management.
Thumb
The Mosel flows into the Rhine at Koblenz.

Rhine

  • The Rhine carries much river traffic, and major inland ports are found at its confluence with the Ruhr at Duisburg, and with the Neckar at Mannheim; see Mannheim Harbour.
  • The Main flows into the Rhine just south of Mainz.
  • The Mosel flows into the Rhine further north at Koblenz. The name "Koblenz" itself has its origin in the Latin name "Confluentes". In German, this confluence is known as the "Deutsches Eck" ("German corner") and is the site of an imposing monument to German unification featuring an equestrian statue of Kaiser Wilhelm I.
  • Upstream in Switzerland, a small town also named Koblenz (for the same reason) is where the Aare joins the Rhine.

Danube basin

Thumb
The triple confluence in Passau; from left to right, the Inn, the Danube, and the Ilz.
  • Passau, Germany, sometimes called the Dreiflüssestadt (City of Three Rivers), is the site of a triple confluence, described thus in a guidebook: "from the north the little Ilz sluices brackish water down from the peat-rich Bavarian Forest, meeting the cloudy brown of the Danube as it flows from the west and the pale snow-melt jade of the Inn from the south [i.e., the Alps] to create a murky tricolour."[22]
  • The Thaya flows into the Morava in a rural location near Hohenau an der March in Austria, forming the tripoint of Austria, Czechia, and Slovakia.
  • The Morava flows into the Danube at Devín, on the border between Slovakia and Austria.
  • The Sava flows into the Danube at Belgrade, the capital of Serbia.
  • In karst topography, which arises in soluble rock, rivers sometimes flow underground and form subterranean confluences, as at Planina Cave in Slovenia, where the Pivka and Rak merge to form the Unica.[23]

Other

Thumb
Confluence of Oka and Volga rivers

North America

Thumb
The confluence of the Allegheny and Monongahela at Pittsburgh, forming the Ohio
Thumb
The Ohio flows into the Mississippi at Cairo.
Thumb
The Rideau Falls in Ottawa, where the Rideau River tumbles into Ottawa River at its mouth.

Mississippi basin

Atlantic watersheds

Pacific watersheds

Thumb
The confluence of the Rio Negro (black) and the Rio Solimões (turbid) near Manaus, Brazil.

South America

Confluences of non-rivers

Thumb
A section of the Industrial Canal in New Orleans also serves as the channel for the Gulf Intracoastal Waterway and the Mississippi River-Gulf Outlet Canal. The waterways are said to be 'confluent'

Occasionally, "confluence" is used to describe the meeting of tidal or other non-riverine bodies of water, such as two canals[26] or a canal and a lake.[27] A one-mile (1.6 km) portion of the Industrial Canal in New Orleans accommodates the Gulf Intracoastal Waterway and the Mississippi River-Gulf Outlet Canal; therefore those three waterways are confluent there.

The term confluence can also apply to the process of merging or flowing together of other substance.[28] For example, it may refer to the merger of the flow of two glaciers.[29]

See also

References

Loading related searches...

Wikiwand - on

Seamless Wikipedia browsing. On steroids.