Mahakam River

Template:Short description Template:Use American English Template:Use dmy dates Template:Infobox river Template:Location map+ The Mahakam River (Indonesian: Sungai Mahakam) is third longest river (with the third greatest volume discharge) in Borneo after the Kapuas River and the Barito River, it is located in East Kalimantan province of Indonesia. It flows Template:Convert from the district of Long Apari in the highlands of Borneo, to its mouth at the Makassar Strait.

The city of Samarinda, the provincial capital of East Kalimantan, lies about Template:Convert from the river mouth. The delta of the Mahakam River has a specific micro climate which is influenced by high and low tide at sea level.

Summary

The Mahakam River [1] is the largest river in East Kalimantan, Indonesia, with a catchment area of approximately 77,100 km². The catchment lies between 2˚N to 1˚S latitude and 113˚E to 118˚E longitude. The river originates in Cemaru<ref>van Bemmelen, R.W., 1949. The Geology of Indonesia.</ref> from where it flows south-eastwards, meeting the River Kedang Pahu at the city of Muara Pahu. From there, the river flows eastward through the Mahakam lakes region, which is a flat tropical lowland area surrounded by peat land. Thirty shallow lakes are situated in this area, which are connected to the Mahakam through small channels [2]. Downstream of the connection with the Semayang and Melintang lakes, the Mahakam meets three other main tributaries – the rivers Belayan, Kedang Kepala, and Kedang Rantau – and flows south-eastwards through the Mahakam delta distributaries, to the Makassar Strait.

Geology

Kalimantan, where the Mahakam lies, is part of the Sunda Continental Plate. The large island has mountain ranges between Indonesia and Malaysia. As described by van Bemmelen (1949), River Mahakam rises in Cemaru (Template:Convert) in the center of Kalimantan, and from there it cuts through the pre-tertiary axis of the island east of the Batuayan (Template:Convert) and then reaches the tertiary basin of Kutai.<ref>van Bemmelen, R.W., 1949. The Geology of Indonesia.</ref> Its middle course traverses a lowland plain with many marshy lakes. This intermontane depression is separated from the neighboring basin, the Barito depression, by a broad hilly tract of less than Template:Convert altitude. After this region, the Mahakam cuts through the Samarinda anticlinorium and reaches its alluvial delta, which spreads like a broad fan over the shelf-sea, with a base of Template:Convert and a radius of about Template:Convert.<ref>van Bemmelen, R.W., 1949. The Geology of Indonesia.</ref>

Upstream of Long Iram (upstream part of Mahakam river basin), the river is flowing in tertiary rocks (Voss, 1983).<ref>Voss, F.: Kalimantan Timur, Atlas. HWWA Institute, Hamburg, 1983.</ref> Between Long Iram and Muara Kaman (middle Mahakam area) the river is flowing in quaternary alluvium, while in the downstream area between Muara Kaman and the coast including the Mahakam delta, tertiary rocks are again present. The presence of the large delta is explained by the formation and rejuvenation of the hilly region near Samarinda.<ref>IWT Kalimantan, Contribution Delft Hydraulics, Appendix I Mahakam River</ref>

Climate

The Mahakam catchment is around the equator. The average annual rainfall in the catchment area is 3,163 mm. The average runoff is around 1,911 mm.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> According to the Köppen climate classification, this area belongs to type Af (tropical rainforest) and has a minimum temperature of ≥18 °C, while precipitation during the driest month in a normal year is ≥60 mm<ref>Peel, M.C., B. L. Finlayson, and T. A. McMahon, 2007. Updated world map of the Koppen-Geiger climate classification. Hydrol. Earth Syst. Sci., 11, 1633–1644.</ref> The transfer of mass and energy in the tropical zone occurs through general air circulation known as the Hadley cell. According to Seidel et al. (2008), the precipitation pattern in this area is largely determined by this large-scale atmospheric wind pattern, which is observable in several ways throughout the atmosphere. This circulation carries moisture into the air, generating rainfall in equatorial regions, whereas the edges of the tropical belt are drier.<ref>Seidel, D.J., Qiang Fu, William J. Randel & Thomas J. Reichler, 2008. Widening of the tropical belt in a changing climateNature Geoscience 1, 21 – 24, Published online: 2 December 2007, {{#invoke:doi|main}}</ref> Within this circulation, evaporation occurs intensively around the equator on the center of low pressure called the Intertropical Convergence Zone (ITCZ), characterized by the accumulation of clouds in the area. The ITCZ moves following the pseudo-motion of the sun within the 23.5°N and 23.5°S zone, therefore its position always changes according to this motion.

The ITCZ drives the Indo-Australian monsoon phenomena which influence the regional climate including the Mahakam catchment. In December, January, and February (winter in the Northern Hemisphere) the concentration of high pressure in Asia and low pressure in Australia make the west wind blow in Indonesia (west monsoon). In June, July, and August concentration of low pressure in Asia (summer in the Northern Hemisphere) and a concentration of high pressure in Australia make the east wind blow in Indonesia (east monsoon). Due to the global air circulation and the regional climate mentioned above, the Mahakam catchment which is located around the equator has a bimodal rainfall pattern with two peaks of rainfall, which are generally occurred in December and May. This is because the ITCZ passes through the equator twice a year, from the Northern Hemisphere in September and from the Southern Hemisphere in March.<ref>Hidayat, 2013. Runoff, discharge and flood occurrence in a poorly gauged basin – The Mahakam River, PhD thesis, Wageningen University</ref>

Discharge

Average discharge of the Mahakam River at Melak (Upper Mahakam), Kota Bangun (Middle Mahakam) and Loa Kulu (Lower Mahakam).<ref name="Statistik Indonesia">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Year	Discharge (m3/s)
	Melak	Kota Bangun	Loa Kulu
1994	1,564
1995	1,647
1996	2,020	2,855
1997	1,884.8
2004	1,396
2005	2,350.95	2,808.95
2007	2,109	2,791.8
2009	1,485
2010	2,022	2,823.52	5,478.5

Average monthly flow (Q–m³/s). Mahakam River at Samarinda:<ref name="PENGELOLAAN SUMBER DAYA AIR WILAYAH SUNGAI MAHAKAM">Template:Cite book</ref><ref name="Rencana Pola Pengelolaan Sda">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Month	2014	2014– 2018	2021
JAN	4,083.38	5,401	3,751.53
FEB	5,863.29	6,965.6	5,290.07
MAR	5,754.92	6,506.5	5,405.59
APR	6,628.15	6,620	5,079.46
MAY	4,151.29	6,121.3	3,898.19
JUN	1,701.62	4,522.7	3,966.51
JUL	1,972.29	3,492	2,674.38
AUG	544.1	2,067.5	1,615.62
SEP	335.68	2,898.4	1,186.52
OCT	638.61	2,914.2	1,226.31
NOV	2,409.33	4,541.5	3,638.79
DEC	5,610.11	5,558.1	2,902.16
Avg.	3,307.7	4,800.7	3,386.26

Average discharge:

Year, period	Discharge	Ref.
Mahakam Delta
2016–2020	Template:Cvt	<ref name="Floating marine debris along Indonesian coasts - An atlas of strandings based on Lagrangian modelling">Template:Cite book</ref>
2003–2016	Template:Cvt	<ref name="Riverine carbon fluxes to the South China Sea: Riverine carbon fluxes to the SCS">Template:Cite journal</ref>
1985–2012	Template:Cvt	<ref name="Remote sensing for Mapping TSM concentration in Mahakam Delta: an analytical approach">Template:Cite conference</ref>
1970–2000	Template:Cvt	citation	CitationClass=web }}</ref><ref name="Past and future trends in nutrient export by 19 rivers to the coastal waters of Indonesia">Template:Cite journal</ref>
	Template:Cvt	citation	CitationClass=web }}</ref>
Samarinda
2021	Template:Cvt	citation	CitationClass=web }}</ref>
2014–2018	Template:Cvt	citation	CitationClass=web }}</ref>
2014	Template:Cvt	<ref name="PENGELOLAAN SUMBER DAYA AIR WILAYAH SUNGAI MAHAKAM">Template:Cite book</ref>
2012	Template:Cvt	citation	CitationClass=web }}</ref>
1996–2005	Template:Cvt	citation	CitationClass=web }}</ref>
Loa Kulu
2010	Template:Cvt	citation	CitationClass=web }}</ref><ref name="KAJIAN PEMANFAATAN SUNGAI MAHAKAM SUMBER LISTRIK ALTERNATIF LINGKUNGAN">Template:Cite book</ref>
Tenggarong
1985–2012	Template:Cvt*	<ref name="Hydrological Regime of Mahakam River Basin Upstream">Template:Cite conference</ref>
Kota Bangun
1996, 2005, 2007, 2010	Template:Cvt	citation	CitationClass=web }}</ref>
Muara Muntai
2010	Template:Cvt	citation	CitationClass=web }}</ref><ref name="KAJIAN PEMANFAATAN SUNGAI MAHAKAM SUMBER LISTRIK ALTERNATIF LINGKUNGAN">Template:Cite book</ref>
Melak
2012	Template:Cvt	citation	CitationClass=web }}</ref>
1998–2010	Template:Cvt	<ref name="Runoff, discharge and flood occunence in a poorly gauged tropical basin–The Mahakam River, Kalimantan">Template:Cite book</ref><ref>Hidayat et al., 2011. Discharge estimation in a backwater affected meandering river, HESS, 15, 2717–2728, 2011.</ref>
1994–2010	Template:Cvt	citation	CitationClass=web }}</ref>

^* Minimum 375 m³/s, maximum 12,200 m³/s (record 24,156 m³/s in 2012<ref name="Runoff, discharge and flood occunence in a poorly gauged tropical basin–The Mahakam River, Kalimantan">Template:Cite book</ref>)

Lakes

File:Melintan.jpg

Lake Melintang at Teluk Tuk with a re-growing burnt swamp forest in the background

There are about 76 lakes spread in the Mahakam river basin and about 30 lakes are located in the middle Mahakam area including the three main lakes (Lake Jempang 15,000 Ha; Lake Semayang 13,000 Ha; Lake Melintang 11,000 Ha).<ref>East Kalimantan provincial government, 2002. Master Plan Sungai Mahakam. Dinas Pekerjaan Umum dan Pemukiman Prasarana Wilayah (in Indonesian)</ref> The lake levels are seasonally fluctuated from 0.5 m – 1 m during the dry period to seven meters during the rainy season. The Mahakam lakes and surrounding wetlands act as water storage [3] as well as a trap of sediment contained in the water flowing into the lakes which are now known to become shallower, presumably as a result of an imbalance between sediment input and slow subsidence.[4]

Fishing is the primary source of livelihood in the Mahakam lakes area, most of the people around the lakes are fishermen. The middle Mahakam Lake area is an area of intensive fishing activity with a productivity of 25,000 to 35,000 metric tons per year since 1970.[5]

Mahakam Lakes:<ref name="Kalimantan-Borneo">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Lake	Coordinates	Eleva-tion (m)	Area (km2)	Mean depth (m)	Volume (106m3)	Basin size (km2)
Jempang	Template:Coord	1	124.36	2.8	352.83	1,012.3
Semajang	Template:Coord	2	104.56	1.1	117.07	2,192.9
Melintang	Template:Coord	2	87.96	1	91.52	1,042.8
Tempatong	Template:Coord	2	18.19	1	17.33	3,970.8
Siran	Template:Coord	1	15.48	1.2	17.9	139.1
Uwis	Template:Coord	2	7.47	1.6	11.84	282.9
Melinau	Template:Coord	1	5.77	1.3	7.61	933.5
Murung	Template:Coord	1	3.23	2.8	9.12	433.8
Kahoypongkol	Template:Coord	2	2.24	0.7	1.54	952.4
Berambai	Template:Coord	0	2.02	1.6	3.26	612.8
Rabok	Template:Coord	2	1.45	0.5	0.725	933.5
Loa Kang	Template:Coord	2	0.7	1.3	0.91	2.1
	Template:Coord	2	0.6	2	1.22	6
Biru	Template:Coord	1

Delta

File:Nypha.jpg

Nypa in Mahakam Delta

The Mahakam delta is a mixed fluvial-tidal dominated delta. The delta covers about Template:Cvt, consisting of mangrove areas near the shore, Nypa swamps in the central areas, and lowland forest near the apex, corresponding to the first bifurcation.[6] Fishery development in this area has converted a vast area of mangrove into shrimp ponds (tambak). However, recent mangrove restoration efforts have taken place in the delta by replanting mangroves in abandoned shrimp ponds and encouraging silvofishery.<ref name=":15">Template:Cite journal</ref> Many areas in the Mahakam delta are already naturally recolonized by mangrove vegetation contributing to ecosystem restoration.<ref>Template:Cite journal</ref> Mangroves also function as sedimentation-enhancing strategies by capturing sediment-causing accretion.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

The delta has three main distributary systems directed Northeast, Southeast, and South. The area between distributaries consists of a series of tidal channels generally unconnected to the main distributaries.<ref>Wiweko A., 2002. The modern Mahakam delta in Modern, ancient deltaic deposits and petroleum system of Mahakam area, Totalfinaelf E&P Indonesie.</ref> The distributary channels are narrow and rectilinear with the depth ranging from Template:Convert and distributary channel bifurcations appear every Template:Convert.<ref>Allen, G.P., Chambers J.L.C., 1998. Sedimentation in the modern and Miocene Mahakam Delta. Indonesian Petroleum Association</ref>

This lower Mahakam area is the second most productive hydrocarbon basin of Indonesia which contains around 3 billion barrels of oil and 30 Tcf of gas reserves.<ref>Mora S., Ten Haven L., 2002. Petroleum system of lower Kutai basin in Modern, ancient deltaic deposits and petroleum system of Mahakam area, Totalfinaelf E&P Indonesie.</ref> Field geological investigations in this area were started in 1888 and in 1897 exploration drilling discovered oil at a shallow depth of Template:Convert on the Louise structure. Production started in 1898 followed by expansion of exploration to the entire Mahakam.<ref>Homewood P, Roy D., 2002. A historical perspective on the exploration of the Mahakam in Modern, ancient deltaic deposits and petroleum system of Mahakam area, Totalfinaelf E&P Indonesie.</ref>

Tributaries

The main tributaries from the mouth:<ref name="Kalimantan-Borneo">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Left tributary	Right tributary	Length (km)	Basin size (km2)	Average discharge (m3/s)*
Mahakam		980	77,243.65	3,897.7
	Loa Haor	120	463.4	11.6
	Jembayan	180	1,365.6	34.7
Karang Mumus		40	318.3	7
	Tenggarong		297.1	6.8
Separi			329.8	9
Kedang Rantau		132	3,631.8	77.8
Kedang Kepala		323.9	15,703.5	582.1
Belayan		319	9,977.3	556.6
Pela (Semayang)		10	2,206.2	65.9
	Kedang Murung		435.1	10.3
	Bongan	20	2,161.4	117
	Kedang Pahu	144	6,800.3	300
Muyub		48	738.2	32.4
	Kelian		270.7	14.4
Pariq		64	1,006.9	50.6
	Ratah		3,302.9	191.7
Merah		51	275	13.8
Medang			839.3	43.5
Alan		32	410.6	22.6
Boh		71	6,624.4	365.1
Nyaan		72	495.8	29
Tepai			797.3	50.8
Melaseh			848.2	59.6
	Cihar		375.4	27.3
Serata			247.9	19
	Kosso		410.4	32.7
Sikê			289.3	23
	Danum Parae		503.3	42.4
	Sihi		265.7	22.4
	Usok		448.5	35.5

^*Period: 1971–2000

Ecology

File:Kantongsemar.jpg

Nepenthes, called kantong semar by the locals, is an insect-eater plant found in the Mahakam peat area

File:Jempangbird.jpg

Birds at the intermittent inlet of Lake Jempang from the Mahakam River

Mahakam and its floodplain is an ecologically important region. A total of 147 indigenous freshwater fish species had been identified from the Mahakam.<ref>Christensen, M.S., 1992. Investigations on the Ecology and Fish Fauna of the Mahakam River in East Kalimantan (Borneo), Indonesia. Int. Revue ges. Hydrobiol., 77(4).</ref> The Mahakam hosts the freshwater dolphin Irrawaddy dolphin (Orcaella brevirostris; called Pesut by local people) a critically endangered species, which is included in CITES (Convention on International Trade in Endangered Species of Wild Fauna and Flora) Appendix I.[7]

The Mahakam river basin is also important breeding and resting place for 298 bird species, among them 70 protected and five endemic species: the dusky munia, Bornean whistler, Bornean peacock-pheasant, Bornean blue-flycatcher and Bornean bristlehead.[8] Some 160,000 ha of the delta has been recognised as an Important Bird Area (IBA) by BirdLife International.<ref name=bli>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

A research cluster ([9]): "Upsetting the balance in the Mahakam Delta: past, present and future impacts of sea level rise, climate change, upstream controls and human intervention on sediment and mangrove dynamics" extensively researches the Mahakam. The cluster's objective is to study the impact of external forcing factors such as sea-level rise, climate change, upstream sediment, as well as human interference on past, present, and future development of the Mahakam delta in different time scales.

Pollution

Logging and mining activities have contributed to the "alarming rate" of pollution of East Kalimantan's Mahakam River. Tests of water pollutants showed levels increased sharply between 2009 and 2011. Despite the growing pollution, it is claimed that "the water is still safe for consumption."<ref>Template:Cite news</ref>

Unsafe concentrations of heavy metals have been observed in Mahakam fish. A 2015 study found lead concentrations over 1000 times safe levels along with unsafe levels of copper, zinc, and cadmium.<ref>Template:Cite news</ref>

Bridges

Bridges include the Template:Convert Mahakam Bridge and the Template:Convert Kutai Kartanegara Bridge. The latter collapsed on 26 November 2011, it took 3 years of planning and one and half years more to rebuild a new bridge on the same spot. The new Kutai Kertanegara Bridge has been open for public use since 8 December 2015, after an opening ceremony held by a local regent.

Social aspect

File:Ponton coal.jpg

Ponton transporting coal through the Mahakam

The River Mahakam is an economic resource for fishermen and farmers and a freshwater source, as a waterway since ancient times until today. It is in this river basin where the Kutai kingdom evolved. The Kutai history is divided into two periods, Kutai Martadipura (around 350–400 AD) and Kutai Kartanegara period (around 1300). Kutai Martadipura, a Hindu kingdom founded by Mulawarman at Muara Kaman, is regarded as the oldest kingdom in Indonesia.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Kutai Kartanegara was founded by settlers from Java at Kutai Lama near the mouth of Mahakam. In around 1565, Islam was extensively spread in Kartanegara by two Moslem preachers from Java, Tunggang Parangan and Ri Bandang.<ref>Allan J. & Muller K., 1988. The Times Travel Library: East Kalimantan, Ed. By P. Zach, Times Editions.</ref>

The Dayaks are the indigenous people inhabiting Kalimantan beside the Kutais and the Banjars. Since the 1970s transmigration of people to East Kalimantan was organized by the Indonesian government, especially in areas near River Mahakam. Transmigration aims to migrate people from overpopulated Java, Bali, and Madura islands to stimulate greater agricultural productivity in the outer islands. By 1973, almost 26% of the land under cultivation in East Kalimantan was being worked by migrants.<ref>Babcock, 1986 as cited by Stadtmueller T., 1990. Soil erosion in East Kalimantan, Indonesia. Proceedings of the Fiji Symposium Research Needs and Applications to Reduce Erosion and Sedimentation in Tropical Steeplands, June 1990: IAHS-AISH Publ. No.192,1990.</ref>

See also

• List of drainage basins of Indonesia
• List of rivers of Indonesia
• Kutai Kartanegara Bridge

File:Mahakam bridge.jpg

The Mahakam bridge in Samarinda