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Kapuas River

Coordinates:0°15′58″S109°52′31″E / 0.2660°S 109.8754°E /-0.2660; 109.8754
From Wikipedia, the free encyclopedia
River in West Kalimantan, Indonesia
This article is about the river in western Borneo. For the river in southern Borneo, seeKapuas River (Barito River).

Kapuas
Aerial view of Kapuas river
Map


Map
Location
CountryIndonesia
Physical characteristics
Source 
 • locationMount Raya atMüller Mountain Range
 • elevation2,278 m (7,474 ft)
Mouth 
 • location
South China Sea
 • coordinates
0°4′0″S109°10′59″E / 0.06667°S 109.18306°E /-0.06667; 109.18306
 • elevation
0 m (0 ft)
Length1,143 km (710 mi)[1]
Basin size98,749.1 km2 (38,127.2 mi2)[2]
Depth 
 • maximum40 m (130 ft)[1] to 50 m (160 ft)[2]
Discharge 
 • locationKapuas Delta
 • average(Period: 2003–2016)6,012 m3/s (212,300 cu ft/s)[3]
Basin features
ProgressionSouth China Sea
River systemKapuas River[4]
Tributaries 
 • leftBungan, Keriau, Manday, Bunut, Embau, Silat,Melawi, Tempunak, Sepauk, Sekadau
 • rightMandalam, Sibau, Awin, Palin, Embaloh, Tawang, Ketungau, Belitang,Sekayam, Tayan, Landak
Kalimantan is located in Kalimantan
Kapuas
Kapuas
main mouth
main mouth
Kapuas River in Kalimantan
A 1945 map showing the two Kapuas rivers of Borneo (Kapoeas on the map)

TheKapuas River (Old Indonesian spelling:Kapoeas River) is a river in theIndonesian part ofBorneo island, at the geographic center ofMaritime Southeast Asia. At 1,143 km (710 mi) in length, it is the longest river on the island of Borneo, the longest river in Indonesia[5][6] and one of the world's longest island rivers.[7] It originates in theMüller mountain range at the center of the island and flows west into theSouth China Sea creating an extended marshy delta. The delta is located west-southwest ofPontianak, the capital of theWest Kalimantan province.[8] This Kapuas River should be distinguished from anotherKapuas, which starts on the other side of the same mountain range in central Borneo but flows to the south, merging with theBarito and discharging into theJava Sea.

Geography and hydrology

[edit]

The river is 1,143 km (710 mi) long and 99,000 km2 (38,000 mi2)[2] theriver basin covers more than 67% of West Kalimantan.[6][9] The river originates near the center of Borneo, south of the Indonesian-Malaysian border, in the joint between the western slope of theMüller Mountain Range, which runs through the island center, and the southern slope of theUpper Kapuas Range (Indonesian:Kapuas Hulu), which is located more to the west. For about 165 km (103 mi) it flows through a mountainous terrain and then descends to a marshy plain.[10] There, the elevation decreases by only 50 m (0.031 mi) over 902 km (560 mi) fromPutussibau to the river delta.[11]

Kapuas Lakes

[edit]

About 350 km (220 mi) from the source, near the northern shore of the river, lies a system ofKapuas Lakes which are connected to the river by numerous channels. These lakes areBekuan (area 1,268 hectares),Belida (600 ha),Genali (2,000 ha),Keleka Tangai (756 ha),Luar (5,208 ha),Pengembung (1,548 ha),Sambor (673 ha),Sekawi (672 ha),Sentarum (2,324 ha),Sependan (604 ha),Seriang (1,412)Sumbai (800 ha),Sumpa (664) andTekenang (1,564 ha).[12] When the monthly precipitation exceeds about 300 mm (12 in), the river overflows its banks, diverting much of its waters to the lakes at a rate of up to 1,000 m3/s (35,000 cu ft/s), and forming a single volume of water with them. This outflow prevents massive flooding of the lower reaches of the river; it also promotes fish migration from the river to the lakes for spawning but drives birds away from the lakes.[13]

Delta

[edit]

The river discharges into theSouth China Sea creating a marshydelta, which spreads both inland and into the sea, with thesilt deposits extending up to 50–60 km (31–37 mi) from the Borneo coast.[11] The delta is located west-southwest ofPontianak, the capital ofWest Kalimantan province, which lies at theequator.[14] The delta has five arms, of which the northernmost is the widest, and is therefore called the Big Kapuas (Indonesian:Kapuas Besar).

Discharge

[edit]

The average annualrainfall in the catchment area is 3,666 mm. The averagerunoff is around 2,339 mm.[15] Thedischarge rate varies through the year, averaging around 5,600–7,800 m3/s (200,000–280,000 cu ft/s)[16][17] at the delta and 2,000 m3/s (71,000 cu ft/s) upstream, at the confluence of theTawang. The discharge peaks during the rainy seasons in April and November, during which the water level may rise by 10–12 m (33–39 ft) overnight, overflowing river banks and flooding the nearby areas.[6][10][13]

Year, periodMin (m3/s)Mean (m3/s)Max (m3/s)Ref.
Kapuas Delta

0°3′14.0328″N109°11′28.2948″E / 0.053898000°N 109.191193000°E /0.053898000; 109.191193000

0°36′51.534″S109°22′41.2068″E / 0.61431500°S 109.378113000°E /-0.61431500; 109.378113000

2016–20207,803[17]
2003–20166,012[3]
1971–20006,260.1[18]
3,0006,5009,000[2][19][1]
2,0005,5008,900[2][1]
5,600[16]
6,214[20]
Sanggau

0°7′2.5464″N110°35′54.4704″E / 0.117374000°N 110.598464000°E /0.117374000; 110.598464000

2013–20151,1175,2209,394[1]
2000–20155,900[2][1]
1971–20005,069.3[18]
Putussibau

0°51′22.6764″N112°55′26.292″E / 0.856299000°N 112.92397000°E /0.856299000; 112.92397000

1971–2000886.3[18]

Tributaries

[edit]

The largest tributary is theMelawi, which occurs to the left nearSintang, about 465 km from the mouth. Other major tributaries are theLandak,Sekayam,Ketungau,Tawang,Bunut andEmbaloh rivers.[21]

The main tributaries from the mouth:[18]

Left

tributary

Right

tributary

Length

(km)

Basin size

(km2)

Average discharge*

(m3/s)

Kapuas1,14398,749.16,260.1
Landak1788,461.5471.9
Sê Lamboe380.220.1
Tayan2,089.2107.5
Emboewan455.124.1
Sekayam2215,162.6305.3
Kedukul368.117.1
Sekadau1172,672.2136.8
Aja395.218.2
Sepauk1,137.953.5
Belitang2,584128.8
Tempunak1,092.450.2
Melawi47122,585.81,243.4
Ketungau1865,496.2320.8
Silat1,37478.5
Seberuang48128
Kenapai292.817.3
Tawang3,826264.8
Suhaid34023.6
Embau769.351.1
Boyan330.624.6
Bunut3,403.3267.5
Embaloh953,469.8289.5
Palin1,155.599.8
Awin509.344.4
Manday2,896.2251.6
Sibau901,687.7150.3
Mandalam301,771.9157.1
Keriau1,635.8138.4
Goeng275.124.3
Lapung199.417.4
Bungan501,019.787.7
Tanjan327.728.7
Tahoem302.826.3

*Period: 1971–2000

Climate

[edit]

The climate is warm and very humid, with the average annualprecipitation ranging from year to year between 2,863 and 5,517 mm (Köppen Climate-classificationAf), and the number of rainy days between 120 and 309; the largest precipitation was observed in 1976 (120 rainy days) and the wettest in 1988, with only 184 rainy days.[9] The temperature is rather stable with a typical minimum of 24 °C (75 °F) and a maximum of 32 °C (90 °F) throughout the whole year.[22]

Flora and fauna

[edit]
A bridge on the outskirts of Pontianak

In the upper and middle reaches, the river flows through densetropical forests; the rich flora and fauna are the subject of international research.[9] Discoveries of new species are frequent, such as theKapuas mud snake (Enhydris gyii), which was discovered in 2003–2005 by German and Americanherpetologists. This species is remarkable because it can spontaneously change its skin color, similar to thechameleon.[23][24]

Otters and crocodiles are common in the Kapuas River, but frogs are nearly absent.[25]Agile gibbons (Hylobates agilis),Müller's Bornean gibbons (Hylobates muelleri),Prevost's squirrels (Callosciurus prevostii), andtreeshrews inhabit the trees above the river.[26]

There are twonational parks on the river banks,Betung Kerihun with an area of 8,000 km2, andDanau Sentarum (an area of 1,320 km2), the latter includes the Kapuas Lakes.[9][27]

Fish

[edit]
Thesuper red arowana, either considered a variant of the Asian arowana or its own species, is only found in Kapuas

About 300 fish species have been identified in the riverbasin, of which 234 are of high economic value.[5] There are more fish species than any other river basin in Indonesia.[28] They belong to 120 genera and 40 families with the two major groups beingcyprinids andcatfish. More than 30% of the species originate from the sea and inhabit the delta areas.[29] Among the economically important species arefood fish such asPangasius catfish,giant gourami,kissing gourami,snakeheads, and large cyprinids such asTormahseers andbarbs such asLeptobarbus andPuntioplites, and species for theaquarium trade such as thesuper red arowana and variousrasboras.[28] Because ofoverfishing and habitat degradation, several species are threatened. Among theseendangered species are the arowana andwhite-edge freshwater whipray, and thewallago catfish, which formerlymigrated in large schools up and down the Kapuas River.[28]

Part of the high species diversity in the Kapuas is related to the many different habitats in the river basin. In the headwaters arefast-flowing highland streams, typically dominated by smallloaches, and small —often acidic (blackwater)— forest streams andpeat swamps with species such as the tinySundadanio rasboras,Sphaerichthys gouramis, andmacropodusine gouramis.[28] The main river also includes several habitats, ranging from the nearshore to open waters. In the deepest sections, no light exists and in one species,Lepidocephalus spectrum, this has resulted in a complete reduction of both eyes and pigmentation (similar tocavefish).[30]

FemaleHemirhamphodon pogonognathus, about 4 cm (1.6 in) long

Owing to the warm climate and abundance of food, most fishes breed all through the year with only a few species likefire eel (Mastacembelus erythrotaenia) having certainreproductive periods. The number of individuals per species is relatively low.[clarification needed] The large variety of species may be explained by the fact that some 6,000 years ago, the Kapuas River, as a tributary of theSunda River, was connected to other tributary rivers ofSouth Sumatra,Java, and theMalay Peninsula. Apart from fish, there are numerouscrabs,prawns (such as the giant freshwater prawnMacrobrachium rosenbergii),[31]water striders, and otheraquatic insects.[32] The rich flora and fauna result in very complexfood chains, with fishes consuming foods ranging from fruits toother fish. For example,Hemirhamphodon pogonognathus feeds exclusively on terrestrial insects. Abundant fruits and seeds enter the river after falling from large trees that bend over its waters.[33] The feeding habits of the fish in the Kapuas River are distributed as follows: 54% areomnivores; 36% are carnivorous and eat other fish (14%), insects (5%), and mixed small forest animals (17%). The remaining 10% are herbivorous, with 4%specialising in algae.[25]

Transport and economic value

[edit]
Large ships on Kapuas River

The Kapuas River is the major waterway connecting the center of the island with its western coast. The large river width and depth (up to 27 meters[7]) support intensive cargo and passenger shipping over most of the river length. Ships with adraft of up to 3 meters can navigate up toSintang, 465 km from the mouth, and those with a draft of up to 2 meters can reach the town ofPutussibau (902 km from the mouth). Logging and rafting of timber occur all along the river. Fishing is also common, especially at the Kapuas Lakes and near the river delta.[10][34] TheTayan Bridge which opened in 2016, crosses over the river and is the longest bridge in Kalimantan.[35] Another major bridge over the area is the Kapuas I Bridge. In 2022, the local government decided to build a newer bridge to accommodate increased traffic in commuters and goods, located to be in parallel with the existing bridge.[36]

See also

[edit]

References

[edit]
  1. ^abcdefDavid Fernando, Munõz Pauta (2017).Tidal influence on the discharge distribution at two junctions of the Kapuas River (West Kalimantan, Indonesia) (Thesis).
  2. ^abcdefKarl, Kästner (2019).Multi-Scale Monitoring and Modelling of the Kapuas River Delta.doi:10.18174/468716.ISBN 978-94-6343-411-9.
  3. ^abTing-Hsuan, Huang; Chen-Tung, Arthur Chen; Hsiao-Chun, Tseng; Jiann-Yuh, Lou; Shu Lun, Wang; Liyang, Yang; Selvaraj, Kandasamy; Xuelu, Gao; Jough-Tai, Wang; Edvin, Aldrian; G.S., Jacinto; Gusti Z., Anshari; Penjai, Sompongchaiyakul; B.J., Wang (May 2017)."Riverine carbon fluxes to the South China Sea: Riverine carbon fluxes to the SCS".Journal of Geophysical Research: Biogeosciences.122 (5):1239–1259.doi:10.1002/2016JG003701.S2CID 135024272.
  4. ^Hukum Online."Keputusan Menteri Kehutanan No. SK.511/MENHUT-V/2011" (in Indonesian).
  5. ^abGöltenboth, Friedhelm (2006)Ecology of insular Southeast Asia: the Indonesian Archipelago, Elsevier,ISBN 0-444-52739-7 p. 157
  6. ^abcMacKinnon, p. 133
  7. ^abNoni Arnee (21 August 2009)."Pesona di Bawah Garis Katulistiwa" (in Indonesian). Suara Merdeka. Archived fromthe original on 8 March 2012. Retrieved22 March 2010.
  8. ^Kapuas RiverArchived 26 April 2015 at theWayback Machine, Encyclopædia Britannica on-line
  9. ^abcd"Betung Kerihun National Park (Transborder Rainforest Heritage of Borneo)". UNESCO World Heritage Centre. 2 February 2004.Archived from the original on 24 December 2019. Retrieved26 December 2019.
  10. ^abcGreat Soviet Encyclopedia. Vol. 11. Moscow. 1969–1978. p. 367.{{cite book}}: CS1 maint: location missing publisher (link)reduced electronic versionArchived 24 March 2012 at theWayback Machine
  11. ^abMacKinnon, p. 131
  12. ^MacKinnon, pp. 152, 159
  13. ^abMacKinnon, p. 160
  14. ^"South Kalimantan".Archived from the original on 3 March 2016. Retrieved4 November 2010.
  15. ^Supplement ofLehmann, Fanny; Vishwakarma, Bramha Dutt; Bamber, Jonathan (2021)."How well are we able to close the water budget at the global scale?"(PDF).Hydrology and Earth System Sciences.26:35–54.doi:10.5194/hess-26-35-2022.Archived(PDF) from the original on 4 January 2022. Retrieved21 February 2022.
  16. ^abEtko, Kuusisto (26 August 2004)."WORLD WATER RESOURCES AND PROBLEMS"(PDF).Archived(PDF) from the original on 21 February 2022. Retrieved21 February 2022.
  17. ^abDelphine, Dobler; Elodie, Martinez; Rinny, Rahmania; Budhi Gunadharma, Gautama; A. Riza, Farhan (2021)."Floating marine debris along Indonesian coasts – An atlas of strandings based on Lagrangian modelling"(PDF).Archived(PDF) from the original on 7 January 2022. Retrieved7 January 2022.
  18. ^abcdEric, Tilman."Kalimantan-Borneo".
  19. ^Radhika, Radhika; Firmansyah, Rendy; Hatmoko, Waluyo (November 2017)."Computation of surface water availability in Indonesia based on satellite data".Jurnal Sumber Daya Air.13 (2):115–130.doi:10.32679/jsda.v13i2.206.Archived from the original on 14 February 2022. Retrieved10 April 2023.
  20. ^"Indonesia-Integrated Swamps Development Project"(PDF). November 1992.Archived(PDF) from the original on 5 February 2022. Retrieved5 February 2022.
  21. ^"South Kalimantan".Archived from the original on 3 March 2016. Retrieved4 November 2010.
  22. ^Pontianak, Borneo ClimateArchived 10 September 2017 at theWayback Machine. ClimaTemps.com
  23. ^Murphy, John C.; Voris, Harold K.; Auliya, Mark (2005)."A new species ofEnhydris (Serpentes: Colubridae: Homalopsinae) from the Kapuas river system, West Kalimantan, Indonesia"(PDF).The Raffles Bulletin of Zoology.53 (2):271–275.Archived(PDF) from the original on 17 March 2009. Retrieved4 November 2010.
  24. ^"Snake displays changing colours".BBC News. 26 June 2006.Archived from the original on 19 March 2018. Retrieved9 January 2007.
  25. ^abMacKinnon, p. 162
  26. ^MacKinnon, pp. 52–53
  27. ^Yuliani, Elizabeth Linda; Indriatmoko, Yayan; Ernawati, Seselia; Prasetyo, Leon Budi; Zul MS (October 2007)."Promoting Good Governance in Danau Sentarum National Park under Decentralization"(PDF). Archived fromthe original(PDF) on 8 October 2012. Retrieved4 November 2010.
  28. ^abcdRoberts, T.R. (1989). "The freshwater fishes of Western Borneo (Kalimantan Barat, Indonesia)".Memoirs of the California Academy of Sciences.14:1–210.
  29. ^MacKinnon, p. 143
  30. ^Deein, Gridsada; Tangjitjaroen, Weerapongse; Page, Lawrence M. (2014). "A revision of the spirit loaches, genusLepidocephalus (Cypriniformes, Cobitidae)".Zootaxa.3779 (3):341–352.doi:10.11646/zootaxa.3779.3.2.PMID 24871728.
  31. ^Samuel, Samuel; Aida, Siti Nurul."AKTIVITAS PENANGKAPAN DAN DISTRIBUSI UDANG GALAH (Macrobrachium rosenbergii) DI DAERAH ALIRAN SUNGAI KAPUAS, KALIMANTAN BARAT".researchgate.net. Jurnal Penelitian Perikanan Indonesia. Retrieved7 September 2024.
  32. ^MacKinnon, p. 132
  33. ^MacKinnon, p. 161
  34. ^MacKinnon, p. 457
  35. ^"Jembatan Terpanjang di Kalimantan Ini Tahan 100 Tahun".Tempo (in Indonesian). 23 March 2016.Archived from the original on 14 April 2016. Retrieved4 July 2017.
  36. ^Caratri, Endah (14 July 2022)."Duplikasi Jembatan Kapuas I Mulai Dibangun Kementerian PUPR – Berita Daerah".Archived from the original on 10 April 2023. Retrieved14 July 2022.

Bibliography

[edit]
Sumatra
Java
Kalimantan
Sulawesi
Lesser Sunda Islands
Maluku
Western Papua

0°15′58″S109°52′31″E / 0.2660°S 109.8754°E /-0.2660; 109.8754

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