| 词条 | Chungará Lake | |||||
| 释义 |
| name = Chungará Lake | other_name = Chungara | image = File:20120623 Chile 2759 Volcano Parinacota (7704192574).jpg | alt = Blue lake with white conical mountain in the background | caption = The volcano Parinacota rises over Chungará | coordinates = {{coord|18|14|S|69|09|W|display=inline,intitle|notes={{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}}}} | length = {{convert|8.75|km}} | area = {{convert|21.5|-|22.5|km2}} | max-depth = {{convert|26|-|40|m}} | elevation = {{convert|4517|m}} | inflow = Chiefly Río Chungara | outflow = Evaporation and seepage | catchment = {{convert|260|km2}} }} Chungará is a lake situated in the extreme north of Chile at an elevation of {{convert|4517|m}}, in the Altiplano of Arica y Parinacota Region in the Lauca National Park. It has a surface area of about {{convert|21.5|-|22.5|km2}} and has a maximum depth of about {{convert|26|-|40|m}}. It receives inflow through the Río Chungara with some minor additional inflows, and loses most of its water to evaporation; seepage into the Laguna Quta Qutani plays a minor role. The lake formed between 17,000 and 8,000 years ago when the volcano Parinacota collapsed and the debris from the collapse dammed the Lauca River. Since then the lake has progressively grown owing to decreasing seepage. The lake is part of the Lauca National Park; a planned diversion of the lake's waters into the Azapa Valley being abandoned after a decision by the Chilean Supreme Court. NameThe name Chungará or Chungara is derived from the Aymara language and has several different meanings: {{lang|ay|Chunka}}, a type of bush or moss plus the suffix {{lang|ay|ra}} that signifies "covered by"; but this meaning appears to have fallen into disuse. A second meaning is {{lang|ay|Chunkha}} "beard" which together with the suffix means "bearded" and refers to a myth of a bearded man that came to the area and destroyed a community{{sfn|Mamani|1994|p=119}} with fire.{{sfn|Mamani|1994|p=121}} GeographyChungará Lake is located the northernmost part of Chile and close to the border with Bolivia.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} It lies at an elevation of {{convert|4517|m}} in the Chilean Altiplano; it is one of the highest lakes in the world[1] and the second highest-largest after Lake Titicaca in the Altiplano.[2] The lake is part of the Lauca National Park,{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} a nationally and internationally designated protected area,{{sfn|Mamani|1994|p=118}} and a CONAF refuge lies close to the western shores of the lake. There is also a marina{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=341}} and a pumping plant in the northwestern area of Chungará Lake.[3] Chile Route 11 passes by the southern and western shores of Chungará Lake.{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=300}} The lake is about {{convert|8.75|km}} wide{{sfn|Hernández|Bao|Giralt|Leng|2008|p=352}} and covers an irregular surface of about {{convert|21.5|km2}}{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=306}}{convert|22.5|km2}},{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} with two large embayments in the northeastern and the southern sectors of the lake and a narrower one in its northwestern corner. Its deepest point is {{convert|26|m}}{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}{{convert|40|m}} deep{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} and lies in the northwestern sector of the lake.{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=341}} The northern and western side of the lake have steep shores, while the southern and eastern ones are much more gentle;{{sfn|Hernández|Bao|Giralt|Leng|2008|p=352}} the eastern shore is covered by a large alluvial fan{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1215}} and the southern one by sediments deposited by the Río Chungara tributary.{{sfn|Hernández|Bao|Giralt|Leng|2008|p=352}} The lakefloor features platforms, flat areas and sloping areas.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1195}} {{convert|4|km}} northwest from Chungará Lake lies the Lagunas Cotacotani.{{sfn|División de estudios y planificación|2010|p=38}} The volcanoes Parinacota ({{convert|6342|m}}{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1193}}) of Pliocene to Holocene age and Ajoya ({{convert|5293|m}}{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1193}}) of Miocene age lie north and west of the lake, respectively;{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=341}} the northern shore of the lake is formed by lava flows from Parinacota volcano. While Parinacota is well preserved, Ajoya and Quisiquisini ({{convert|5516|m}}{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1193}}) on the eastern shore of the lake are moderately eroded.{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=306}} Farther south from Chungará Lake lies the {{convert|6063|m}} high Guallatiri.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1193}} {{wide image|Chungara panorama.jpg|upright=5|1000px|Panorama of Chungará Lake}}{{clear}}HydrologyThe water temperature reaches its maximum during March with {{convert|13.5|C}} and a minimum in January with {{convert|3.5|C}} according to one study,{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=343}} while temperatures on the lakefloor range between {{convert|6.4|-|6.2|C}}.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1194}} Water levels vary by {{convert|0.5|m}} between seasons{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} and fluctuations of {{convert|3|-|2|m}} have been recorded.{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} The present-day water levels are the highest in the history of the lake and there is no evidence of former lake highstands, {{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} and the depth of the lake has generally increased during the course of its history. There are some long term fluctuations in water levels, including a deepening episode during the latest Pleistocene and three or four episodes of water level lowstand during the middle and late Holocene{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|pp=1217-1218}} at about 10,500, 9,800, 7,800 and 6,700 calibrated radiocarbon years ago. Since about 5,000 calibrated radiocarbon years ago lake levels have been high.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1220}}The Lake Chungará is part of a {{convert|260|km2}}[2] large high-elevation watershed in the Altiplano,{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} bordered on the west by the Lauca River watershed and on the east by the Bolivian frontier;{{sfn|División de estudios y planificación|2010|p=17}} the watershed is surrounded by snow-covered volcanoes.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1194}} The largest tributary of the lake is the Río Chungara with a discharge of about {{convert|0.3|-|0.46|m3/s}} which originates on Guallatiri volcano{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1195}} and drains the area of the Nevados de Quimsachata (Acotango, Capurata and Umurata);{{sfn|División de estudios y planificación|2010|p=17}} this river contributes about 4/5 of the water to the lake and enters Chungará Lake on its southeastern corner{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} through a river delta.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1215}} Other tributaries are the Chachapay,{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1215}} Mal Paso ({{convert|15|l/s}}),{{sfn|División de estudios y planificación|2010|p=17}} Ajata ({{convert|20|l/s}}) and Sopocalane ({{convert|30|-|160|l/s}} only during wet periods) creeks which originate on Choquelimpie{{sfn|División de estudios y planificación|2010|p=17}}/Ajoya volcano,{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1195}} which have formed river deltas where they enter the lake; some of the deltas are submerged.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1214}} In addition, springs supply water into the lake from its western{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} and northern shores where volcanoes border the lake.{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=306}} There are no inflows on the eastern side of Chungará Lake.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1215}} Chungará Lake has no outlet; its waters evaporate at a rate of about {{convert|1.2|mm/year|in/year}} and also seep into the groundwater table{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} at a rate of {{convert|0.2|m3/s}}.{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} The water chemistry of the Cotacotani Lakes imply that they receive water from Chungará Lake{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=309}} at a rate of about {{convert|0.25|m3/s}}; this constitutes over half of the inflow to the Cotacotani Lakes.{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=316}} The role of this underground outflow has progressively decreased through the history of the lake as silt has accumulated in the breccia through which the groundwater seeps out.{{sfn|Hernández|Bao|Giralt|Leng|2008|p=361}} The Cotacotani Lakes eventually drain into the Lauca River. The total volume of the lake is about {{convert|0.426|km3}}. Chungará Lake is polymictic/well mixed{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} and its waters transparent enough that sunlight can reach most of the lake floor.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=347}} The waters of the lake are slightly alkaline and saline{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} and show influence of dolomite rocks.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=347}} This lake chemistry is homogeneous throughout the lake{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=308}} and the lake waters are subject to strong currents at the surface.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1195}} GeologyThe lake was formed by volcanic-tectonic phenomena;{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} specifically, a major collapse of the Parinacota volcano dammed a former Rio Lauca, forming Chungará Lake, at some time between 8,000 and 15,000 - 17,000 years ago.{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} This collapse involved about {{convert|6|km3}} and covered about {{convert|140|km2}} with debris;{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1194}} before the collapse took place the lakefloor of Chungará Lake consisted of alluvial and river sediments left by the Rio Lauca{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|pp=1199-1200}} which drained the area. Upon damming, water from the river accumulated and formed Chungará Lake.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1218}} The exact time of the collapse is controversial. Faulting also played a minor role in the formation of the lake basin,{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} with a southwest-northeast trending fault disrupting sediments in the northwestern sector of the lake.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1196}} Since the birth of Chungará Lake, about {{convert|10|m}} of sediment have accumulated on its floor.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1219}} Volcanism in the area has been ongoing since the Paleozoic{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=342}} and has continued until recent times, which has influenced Chungará Lake.{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=16}} A number of volcanoes such as Parinacota, Ajoya and Quisiquisini grew on a Miocene ignimbrite basement that crops out east of the lake;{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=306}} of these only Parinacota has been active in the Holocene, depositing tephra within the lake.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1194}} ClimateTemperatures at the lake average {{convert|4.2|C}},{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} fluctuating between {{convert|20|-|12|C}} at day and {{convert|3|-|-10|C}} at night.[2] The climate of Chungará Lake is arid{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} and annual precipitation on Chungará Lake amounts to about {{convert|330|mm/year|in/year}}, considerably smaller than the evaporation rate.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=346}} This precipitation occurs during summer when moisture is transported into the region from the Amazon{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} and the Atlantic Ocean; this is known as the "Bolivian Winter".{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=300}} Annual precipitation varies under the influence of the "ENSO" phenomenon. In addition, the area is characterized by a high solar insolation.[10] Human useThe area of the lake is inhabited by Aymara people who engage in animal husbandry, using alpacas, cattle, llamas and sheep and live on farms and pastoral refuges.{{sfn|Mamani|1994|p=118}} Environmental issuesIn the 1970s water was pumped from Chungará Lake to the Azapa Valley to allow for irrigation, but quickly ceased when water levels dropped and the flora and fauna of the lake were damaged.{{sfn|Herrera|Pueyo|Saez|Valero-Garces|2010|p=300}} For this purpose, the Canal Chungará was built by the Chilean Ministry of Public Works to transfer water into the Laguna Cotacotani which is the headwater of the Lauca-Azapa system.{{sfn|División de estudios y planificación|2010|p=17}} This project was opposed by environmentalists.{{sfn|División de estudios y planificación|2010|p=18}} On the 19th December 1985 the lake was the subject of a major legal case when the Chilean Supreme Court ruled that international obligations such as the CITES need to be considered by the Chilean government[11] and prohibited the use of the waters of Chungará Lake;{{sfn|División de estudios y planificación|2010|p=18}} the ruling by disallowing the use of the waters of Chungará Lake forced the Arica y Parinacota Region to seek other sources of water for the growing economy.{{sfn|División de estudios y planificación|2010|p=5}} Accumulation of rubbish in the area of Chungará Lake has become a major issue, as a lot of waste is discarded by for example drivers on the Chungara–Tambo Quemado road between Chile and Bolivia. The Chilean government has thus organized cleanup operations to remove some of the waste.[12] BiologyThe lake hosts a diverse plant and animal community.{{sfn|Mamani|1994|p=118}} The landscape around the lake includes wetlands known as bofedales; otherwise the vegetation in the region of the lake consists mainly of Polylepis dwarf trees, shrubs and tussock grasses.{{sfn|Moreno|Giralt|Valero-Garcés|Sáez|2007|p=5}} Andean gulls, fish, flamingos and taguas occur at Chungará Lake.[12] The shoreline vegetation draws birds in such as Andean gull, Chilean flamingo, crested duck, giant coot and Puna plover.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=344}} The phytoplankton of the lake is dominated by diatoms in winter and by chlorophyceae in summer.{{sfn|Sáez|Valero-Garcés|Moreno|Bao|2007|p=1195}} Algae include both the large Cladophora and Nostoc genera and the small Botryococcus braunii, Cocconeis placentula, Cyclotella andina and Nephroclamys subsolitaria; the second and the third are diatoms. Copepods such as calanoids and cladocera make up the zooplankton.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=344}} Microbial colonies occur on the shores of Chungará Lake.{{sfn|Pueyo|Sáez|Giralt|Valero-Garcés|2011|p=340}} FishThe most important fish in Chungará Lake are Orestias chungarensis and Trichomycterus species.{{sfn|Mühlhauser|Hrepic|Mladinic|Montecino|1995|p=344}} The killifish Orestias chungarensis has been found in Chungará Lake{{sfn|Vila|Morales|Scott|Poulin|2013|p=931}} and is most closely related to other Orestias species in the Lauca National Park but also to fish found in Salar de Ascotan and Salar de Carcote. This reflects that these waterbodies and the Lauca River were once joined by the former Lake Tauca.{{sfn|Vila|Morales|Scott|Poulin|2013|p=938}} In Chungará Lake these fish occur at elevations of over {{convert|4.5|km}}; Orestias is among the fish with the highest occurrences in the world.[14] They are further considered to be threatened species by the International Union for Conservation of Nature and the Chilean National Museum of Natural History.[15] The rainbow trout also lives in the lake and is considered an invasive species there as it feeds on the threatened Orestias fish; the Chilean government has thus envisaged to take measures to eradicate the fish from the lake.[15] See also
References1. ^1 {{cite journal |last1=Urrutia Silva |first1=Osvaldo |title=Jurisprudencia nacional, nuevos Tribunales Ambientales y derecho internacional del medio ambiente |journal=Revista de Derecho (Valparaíso) |date=2013 |issue=40 |pages=475–507 |doi=10.4067/S0718-68512013000100015 |url=https://scielo.conicyt.cl/scielo.php?pid=S0718-68512013000100015&script=sci_arttext&tlng=en |issn=0718-6851}} [1][2][3][4][5][6][7][8]2. ^1 {{cite journal |last1=Pozo |first1=Karla |last2=Perra |first2=Guido |last3=Gomez |first3=Victoria |last4=Barra |first4=Ricardo |last5=Urrutia |first5=Roberto |title=TEMPORAL TRENDS OF POLYCYCLIC AROMATIC HYDROCARBONS (PAHs) IN A DATED SEDIMENT CORE OF A HIGH ATITUDE MOUNTAIN LAKE: CHUNGARA LAKE- NORTHERN CHILE (18° S) |journal=Journal of the Chilean Chemical Society |date=2014 |volume=59 |issue=3 |pages=2564–2567 |doi=10.4067/S0717-97072014000300008 |url=https://scielo.conicyt.cl/scielo.php?pid=S0717-97072014000300008&script=sci_arttext&tlng=en |issn=0717-9707}} 3. ^1 2 3 {{cite journal |last1=Urrutia |first1=Roberto |last2=Yevenes |first2=Mariela |last3=Barra |first3=Ricardo |title=DETERMINACIÓN DE LOS NIVELES BASALES DE METALES TRAZA EN SEDIMENTOS DE TRES LAGOS ANDINOS DE CHILE: LAGOS CHUNGARÁ, LAJA Y CASTOR |journal=Boletín de la Sociedad Chilena de Química |date=December 2002 |volume=47 |issue=4 |pages=457–467 |doi=10.4067/S0366-16442002000400017 |url=https://scielo.conicyt.cl/scielo.php?pid=S0366-16442002000400017&script=sci_arttext&tlng=pt |issn=0366-1644}} 4. ^1 {{cite journal |last1=Dorador |first1=Cristina |last2=Pardo |first2=Rodrigo |last3=Vila |first3=Irma |title=Variaciones temporales de parámetros físicos, químicos y biológicos de un lago de altura: el caso del lago Chungará |journal=Revista Chilena de Historia Natural |date=2003 |volume=76 |issue=1 |pages=15–22 |doi=10.4067/S0716-078X2003000100002 |url=https://scielo.conicyt.cl/scielo.php?pid=S0716-078X2003000100002&script=sci_arttext&tlng=pt |issn=0716-078X}} 5. ^1 {{cite web |title=Región de Arica y Parinacota |url=http://www.sea.gob.cl/regiones/region-de-arica-y-parinacota |publisher=Servicio de Evaluación Ambiental |accessdate=10 November 2018 |language=es}} 6. ^1 2 {{cite web |title=Más de 30 toneladas de basura son extraídas en operativo de limpieza del Lago Chungará |url=http://www.gobiernointerior.gov.cl/noticias/2016/04/21/mas-de-30-toneladas-de-basura-son-extraidas-en-operativo-de-limpieza-del-lago-chungara/ |publisher=División de Gobierno Interior |accessdate=10 November 2018 |language=es |date=21 April 2016}} 7. ^1 2 {{cite web |title=Acuerdan medidas para erradicar trucha arcoiris del lago Chungará |url=http://www.subpesca.gob.cl/portal/617/w3-article-90784.html |publisher=Subsecretaría de Pesca y Acuicultura |language=es |date=9 November 2015}} 8. ^1 {{cite web |title=Conociendo los peces de Bolivia: Las ninfas de las montañas (Orestias spp.): Peces que habitan el Altiplano de Bolivia |url=http://www.mnhn.gob.bo/econoticias_proc.php?Seleccion=278 |publisher=Museo Nacional de Historia Natural de Bolivia |accessdate=10 November 2018 |language=es |date=6 July 2017}} }} Sources{{refbegin}}
External links{{Arica y Parinacota Region rivers and lakes}}{{DEFAULTSORT:Chungara Lake}} 2 : Lakes of Chile|Lakes of Arica y Parinacota Region |
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