Battle of Honey Springs

The São Gonçalo Channel (Portuguese pronunciation: [sɐ̃w ɡõˈsalu]) is a navigable channel connecting two large coastal lagoons, Lagoa Mirim and Lagoa dos Patos, in the state of Rio Grande do Sul in southern Brazil.[1] At its eastern end, it separates the municipalities of Rio Grande to the south from Pelotas to the north.

32°08′48″S 52°37′31″W / 32.14667°S 52.62528°W / -32.14667; -52.62528

Course

The Mirim-São Gonçalo basin covers an area of about 62,250 km2 (24,030 sq mi), of which 47% are in Brazil and 53% in Uruguay. Its main source of water, the Lagoa Mirim, is located in the coastal plain, with an average width of 20 km and an area of 3,750 km2 (1,450 sq mi), of which 2,750 km² are in Brazilian territory and 1,000 km² in Uruguayan territory.

The two systems are connected by a 76.6 km (47.6 mi) natural channel called São Gonçalo, which drains from Lagoa Mirim to Lagoa dos Patos. However, in times of drought, this flow is reversed and the salt water flows from Lagoa dos Patos through the São Gonçalo canal to Lagoa Mirim. The São Gonçalo Channel is located in the west-southern part of the Lagoa dos Patos system. The natural flow regime of the canal is complex, with periodic reversals in the direction of flow, which is why the canal is called the Gonçalo Canal. The average discharge is 700 m3/s (25,000 cu ft/s) to 1,200 m3/s (42,000 cu ft/s) and the flow velocity is 0.6 m/s. The maximum freshwater discharge reaches 3,000 m3/s (110,000 cu ft/s) during floods, while the discharge is zero during long dry seasons, when the flow is generally directed towards the Lagoa Mirim. This natural channel has a sinuous course, varying in width from 200 m (660 ft) to 300 m (980 ft) and in depth up to 10 m (33 ft).[2]

The region is part of the geomorphological provinces of the Coastal Plain and the Uruguayo-South-Rio-Grande Shield, and in the Brazilian part of the region are Aceguá, Arroio do Padre, Arroio Grande, Bagé, Candiota, Canguçu, Capão do Leãu, Pedro Osório, Pelotas, Pinheiro Machado, Piratini, Rio Grande, Santa Vitória do Palmar and Turuçu.[5]

Ecology

The lake and the wetlands around it form one of the main hydrographic basins of Rio Grande do Sul, which contains a wide variety of flora and fauna and, together with Lagoa dos Patos, forms the largest lagoon complex in South America. The Lagoa Mirim and its surrounding wetland complex form one of the main transboundary river basins in South America, which is of great ecological and economic importance. The main uses of the water are irrigation and human consumption. Two important environmental reserves, the Taim Ecological Station in Brazil and the Humedales del Este in Uruguay, are located on the shores of the basin. The Taim Ecological Station is a federal nature conservation unit of integrated protection and aims to protect the environment. Known worldwide as one of the most important nature reserves, it preserves marshes, lakes, fields, dunes and forests, and is home to a wide variety of plant and animal species.[5]

The Humedales Del Este eastern wetlands in Uruguay, have been included in the list of the Convention on Wetlands of International Importance - Ramsar Convention, which is made up of an ecosystem of about 560,000 hectares, including 10 protected biosphere reserves, national parks (Bañados de San Miguasn, Laguna de Josrón - Isla de Lobos, Cerro Largo); Protected landscapes (Cerro Catedral - Sierra de Sosa, Asperezas de Polanco, Sierra Del Tigre, Quebrada de los Cuervos); Protected areas with managed resources (Laguna Merín and India Muerta).[5]

Sluice system

The lock separates the São Gonçalo Canal from the Lagoa dos Patos at 15 km and the Lagoa Mirim at 61 km. The sluice dam was built in 1977 to prevent the inflow of salt water into the Lagoa Mirim, as a result of the development of the two countries between Uruguay and Brazil. This navigation channel has two leveling sluice gates 17 m high and 8 m wide. The system of operation of the sluice depends on the fluviometric level of the Lagoa Mirim: when the average level of the Lagoa Mirim is close to 1 m below sea level, the sluice starts to regulate the flow between the São Gonçalo channel and the Lagoa dos Patos. The water level in the Lagoa Mirim is controlled during this period by partial or complete closure of the lock gates and by reducing the opening time of the navigation lock. During the remaining time the locks will remain partially open. In summer, the lock channel is opened four times a day at fixed times to allow the passage of vessels.[2]

Tributaries

Major tributaries of the Mirim-São Gonçalo basin:[3]

River Mouth

coordinates

Length

(km)

Basin size

(km²)

Average discharge

(m3/s)

São Gonçalo Channel
Arroio Pelotas 31°46′24.1176″S 52°16′51.3516″W / 31.773366000°S 52.280931000°W / -31.773366000; -52.280931000 901.5 23.5
Arroio Fragata 31°48′3.2292″S 52°22′21.0468″W / 31.800897000°S 52.372513000°W / -31.800897000; -52.372513000 219.7 5.4
Arroio Teodósio 31°50′41.0964″S 52°23′20.0832″W / 31.844749000°S 52.388912000°W / -31.844749000; -52.388912000 285.6 6.9
Arroio Pavão 31°58′7.9536″S 52°25′4.1916″W / 31.968876000°S 52.417831000°W / -31.968876000; -52.417831000 178.2 4.3
Piratini 32°0′56.5416″S 52°25′10.1604″W / 32.015706000°S 52.419489000°W / -32.015706000; -52.419489000 120 5,590.1 141.9
Lagoa Mirim
Arroio Moreira 32°8′29.1156″S 52°41′5.3844″W / 32.141421000°S 52.684829000°W / -32.141421000; -52.684829000 314.2 7.5
Arroio Parapó 32°10′16.7196″S 52°43′31.5372″W / 32.171311000°S 52.725427000°W / -32.171311000; -52.725427000 280.1 6.6
Arroio Chasqueiro 32°16′4.6524″S 52°47′14.9928″W / 32.267959000°S 52.787498000°W / -32.267959000; -52.787498000 398 8.9
Arroio Grande 32°20′55.3704″S 52°47′37.1076″W / 32.348714000°S 52.793641000°W / -32.348714000; -52.793641000 1,153.4 23.3
Arroio Bretanha 32°29′18.1248″S 52°58′9.534″W / 32.488368000°S 52.96931500°W / -32.488368000; -52.96931500 488.1 10.6
Sanga do Meio 32°38′30.552″S 53°5′12.0012″W / 32.64182000°S 53.086667000°W / -32.64182000; -53.086667000 407.5 8.7
Jaguarão 32°39′11.736″S 53°10′56.064″W / 32.65326000°S 53.18224000°W / -32.65326000; -53.18224000 270 7,541.2 147.3
Tacuarí 32°46′13.4472″S 53°18′31.7412″W / 32.770402000°S 53.308817000°W / -32.770402000; -53.308817000 230 5,288.5 101.5
Cebollatí 33°9′3.2616″S 53°37′32.3688″W / 33.150906000°S 53.625658000°W / -33.150906000; -53.625658000 235 17,513.5 337
San Luis 33°31′33.3696″S 53°32′37.7916″W / 33.525936000°S 53.543831000°W / -33.525936000; -53.543831000 2,949.8 54.1
Arroio San Miguel 33°36′9.6264″S 53°31′56.856″W / 33.602674000°S 53.53246000°W / -33.602674000; -53.53246000 2,236.6 38.8
Arroio Del Rey 33°4′35.9004″S 53°14′28.446″W / 33.076639000°S 53.24123500°W / -33.076639000; -53.24123500 1,183.4 19.7

References

  1. ^ U. Seeliger (2004). "Catchment–lagoon–estuary–coast interactions of the Patos–Mirim system, south Brazil". In Luiz D. de Lacerda; Ricardo E. Santelli; Egbert K. Duursma; Jorge J. Abrão (eds.). Environmental Geochemistry in Tropical and Subtropical Environments. Springer. pp. 19–27. doi:10.1007/978-3-662-07060-4_3. ISBN 9783662070604.
  2. ^ a b c d e f g Marcelo D.M., Burns; João, Vieira (2012). "Influence of Sluice Dam in the movement of marine catfish (Siluriforms, Ariid) in São Gonçalo channel, Patos-Mirim System".
  3. ^ a b c d e "Atlantic East Coastal".
  4. ^ a b Heline, Olivera; Elisa, Fernandes; Osmar, Möller Jr.; Felipe, García-Rodríguez (2019). "Relationships between Wind Effect, Hydrodynamics and Water Level in the World's Largest Coastal Lagoonal System".
  5. ^ a b c "Bacia Hidrográfica Mirim - São Gonçalo (BHMSG)".