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The freshwater lens of Benjamín Aceval, Chaco, Paraguay: a terrestrial analogue of an oceanic island lens

La lentille d’eau douce de Benjamin Aceval, Chaco, Paraguay: un analogue continental des lentilles d’eau douce d’île océanique

Lentes de agua dulce de Benjamín Aceval, Chaco, Paraguay: una analogía terrestre de lentes de islas oceánicas

巴拉圭查科地区Benjamín Aceval的淡水透镜体:海洋岛透镜体的陆地类似体

A lente de águas doces de Benjamín Aceval, Chaco, Paraguai: uma analogia terrestre da lente de uma ilha oceânica

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Abstract

The occurrence of a freshwater lens in the Paraguayan Chaco, 900 km away from the ocean, is reported. It is located underneath sandstone hills, surrounded by lowlands with predominantly saline groundwater. Its geometry was delineated using geoelectrical and electromagnetic investigations. The unusual height of the fresh groundwater level can be attributed to the presence of a confining layer at depth. The lens receives its recharge exclusively from rainfall during the hot and humid summer months. It predominantly contains water predating the atmospheric atomic bomb tests, some of it probably up to a thousand or more years old. The water balance shows that extraction currently does not exceed recharge in normal years. However, the available volume of groundwater leaves little room for a further increase of extraction in the future. Recharge is augmented by return flow from thousands of latrines and cess pits, and this has lead to widespread contamination of the groundwater by faecal bacteria.

Résumé

La présence d’une lentille d’eau douce dans le Chaco Paraguayen, à 900 km de l’océan est rapportée. Elle est située sous des collines gréseuses, entourées de basses terres à prédominance d’eaux souterraines salines. Sa géométrie a été déterminée grâce à des investigations géophysiques électriques et électromagnétiques. L’altitude inhabituelle du niveau d’eau souterraine peut être attribuée à la présence d’une couche imperméable en profondeur. La lentille est rechargée exclusivement par les précipitions durant les mois chauds et humides de l’été. Elle contient principalement de l’eau antérieure aux essais atomiques dans l’atmosphère, probablement d’un âge de 1,000 ans et plus. Le bilan hydrique montre que les prélèvements n’excèdent pas actuellement la recharge pour des années normales. Cependant, le volume d’eau souterraine disponible ne laisse que peu de possibilité pour une augmentation des prélèvements futurs. La recharge est augmentée par les infiltrations provenant de milliers de latrines et de fosses à excréments, ce qui conduit à une large contamination de l’eau souterraine par des bactéries fécales.

Resumen

Se informa la ocurrencia de lentes de agua dulce en el Chaco Paraguayo, situado a 900 km del océano. Están localizadas debajo de lomas de areniscas, rodeadas por terrenos bajos con agua subterránea predominantemente salina. Su geometría fue delineada usando investigaciones geoeléctricas y electromagnéticas. La altura inusual del nivel de agua subterránea dulce puede ser atribuida a la presencia de una capa confinante en profundidad. Las lentes reciben su recarga exclusivamente de la lluvia durante los cálidos y húmedos meses de verano. Contienen mayormente agua anterior a las pruebas atmosféricas de las bombas atómicas, alguna de ellas probablemente hasta mil años o más de antigüedad. El balance de agua muestra que la extracción actualmente no excede la recarga en años normales. Sin embargo, el volumen disponible de agua subterránea deja poco espacio para un aumento adicional de la extracción en el futuro. La recarga se ve aumentada por el flujo de retorno de miles de letrinas y pozos negros, y esto ha dado lugar a una contaminación generalizada de las aguas subterráneas por bacterias fecales.

摘要

距离海洋900千米的巴拉圭查科地区发现有淡水透镜体。它位于砂岩丘陵之下,周围是主要含咸水的低地。通过地电和地磁调查描述了其几何形状。地下淡水水位与众不同的高度可归因于在深部存在着承压层。透镜体的补给仅仅依靠高温潮湿的夏季降雨。透镜体主要含原子弹爆炸实验之前的水,有些水的年龄可能达1000年或者更长。水平衡显示,目前的抽水量没有超过正常年份的补给量。然而,地下水的可利用量给将来增加抽水量留的余地很小。数千个厕所、粪坑的污水回流增加了对地下水的补给,这导致了地下水受到粪便细菌的广泛污染。

Resumo

É reportada a ocorrência de uma lente de água doce no Chaco paraguaio, a 900 km do oceano. Situa-se por baixo de elevações areníticas, rodeada por terras baixas com águas subterrâneas predominantemente salgadas. A sua geometria foi delineada utilizando investigações geoelétricas e geomagnéticas. A altura pouco usual do nível piezométrico da água doce pode ser atribuída à presença de uma camada confinante em profundidade. A lente recebe a sua recarga exclusivamente da água de precipitação durante os meses quentes e húmidos do verão. Contém predominantemente água atmosférica anterior aos ensaios com bombas atómicas, alguma dela provavelmente com mais de mil anos de idade. O balanço hídrico mostra que, em anos normais, as extrações atuais não excedem a recarga. Contudo, o volume de águas subterrâneas disponível não permite muita margem para um aumento futuro das extrações. A recarga é aumentada pelo fluxo de retorno proveniente de milhares de latrinas e fossas, o que conduziu a uma contaminação alargada das águas subterrâneas por bactérias fecais.

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References

  • Ayers JF, Vacher HL (1986) Hydrogeology of an atoll island: a conceptual model from detailed study of a Micronesian example. Ground Water 24(2):185–198

    Article  Google Scholar 

  • Bailey RT, Jenson JW, Olsen AE (2009) Numerical modeling of atoll island hydrogeology. Ground Water 47(2):184–196

    Article  Google Scholar 

  • Barrett B, Heinson G, Hatch M, Telfer A (2002) Geophysical methods in saline groundwater studies: locating perched water tables and fresh-water lenses. Explor Geophys 33(2):115–121

    Article  Google Scholar 

  • Batu V (1998) Aquifer hydraulics: a comprehensive guide to hydrogeologic data analysis. Wiley, New York, 752 pp

    Google Scholar 

  • Baydon-Ghyben W (1898) Nota in verband met de voorgenomen putboring nabij Amsterdam [Note concerning the water well drilled near Amsterdam]. Koninglijk Instit Ing Tijdschrift 1888–89:8–22

    Google Scholar 

  • Bear J, Cheng A-HD, Sorek D, Ouazar DS, Herrera I (2010) Seawater intrusion in coastal aquifers concepts, methods and practices. Springer, Berlin, 625 pp

    Google Scholar 

  • Bitschene PR (1987) Mesozoischer und känozoischer anorogener Magmatismus in Ostparaguay: Arbeiten zur Geologie und Petrologie zweier Alkaliprovinzen [Mesozoic and Cenozoic anorogenic magmatism in eastern Paraguay: studies of geology and petrology of two alkaline provinces]. PhD Thesis, Heidelberg University, Germany]

  • Bitschene PR, Báez Presser JL (1989) The Asunción Alkaline Province (eastern Paraguay): geologic setting and petrogenetic aspects. Zentralbl Geol Paläontol 1(5–7):959–971

    Google Scholar 

  • Cartwright I, Weaver TR, Simmons CT, Fifield LK, Lawrence CR, Chisari R, Varley S (2010) Physical hydrogeology and environmental isotopes to constrain the age, origins, and stability of a low-salinity groundwater lens formed by periodic river recharge: Murray Basin, Australia. J Hydrol 380:203–221

    Article  Google Scholar 

  • Chesnaux R, Allen DM (2008) Groundwater travel times for unconfined island aquifers bounded by freshwater or seawater. Hydrogeol J 16(3):437–445

    Article  Google Scholar 

  • Christiansen AV, Auken E (2012) A global measure for depth of investigation. Geophysics 77(4):WB171–WB177

    Article  Google Scholar 

  • Clarke WB, Jenkins WJ, Top Z (1976) Determination of tritium by mass spectrometric measurement of 3He. Int J Appl Radiat Is 27(9):515–522

    Article  Google Scholar 

  • Comin-Chiaramonti P, Civetta L, Petrini R, Piccirillo EM, Bellieni G, Censi P, Bitschene P, Demarchi G, De Min A, de Barro GC, Castillo AM, Velazquez JC (1991) Tertiary nephelinitic magmatism in eastern Paraguay: petrology, Sr–Nd isotopes and genetic relationships with associated spinel-peridotite xenoliths. Eur J Mineral 3(3):507–525

    Article  Google Scholar 

  • Comin-Chiaramonti P, Cundari A, Piccirillo EM, Gomes CB, Castorina F, Censi P, De Min A, Marzoli A, Speziale S (1997) Potassic and sodic igneous rocks from eastern Paraguay: their origin from the lithospheric mantle and genetic relationships with the associated Parana flood tholeiites. J Petrol 38(4):495–528

    Article  Google Scholar 

  • Comin-Chiaramonti P, Cundari A, DeGraff JM, Gomes CB, Piccirillo EM (1999) Early cretaceous–Tertiary magmatism in eastern Paraguay (western Paraná Basin): geological, geophysical and geochemical relationships. J Geodyn 28:375–391

    Article  Google Scholar 

  • Comin-Chiaramonti P, Marzoli A, de Barros GC, Milan A, Riccomini C, Velazquez VF, Mantovani MMS, Renne P, Tassinari CCG, Vasconcelos PM (2007) The origin of post-Paleozoic magmatism in eastern Paraguay. Geol Soc Am Spec Pap 430:603–633

    Google Scholar 

  • Cooper HH, Kohout FA, Henry HR, Glover RE (1964) Seawater in coastal aquifers. US Geol Surv Water Suppl Pap 1613-C:84

    Google Scholar 

  • Cortelezzi CR, Colado UR, Muñoz L (1988) Disyunción columnar en areniscas mesozoicas (Formación Misiones), Republica del Paraguay [Columnar jointing in mesozoic sandstones (Misiones formation), Republic of Paraguay]. Notas Museo Del Plata Geol 76:169–175

  • Dose EJ, Stoeckl L, Houben GJ, Vacher L, Vassolo S, Dietrich J, Himmelsbach T (2014) Experiments and modeling of freshwater lenses in layered aquifers: steady state interface geometry. J Hydrol 509:621–630

    Article  Google Scholar 

  • EN ISO 748 (2007) Hydrometry: measurement of liquid flow in open channels using current-meters or floats. ISO, Geneva

  • Facetti-Fernandez JF, Stichler W (1995) Analysis of concentration of environmental isotopes in groundwater and rainwater from Paraguay. In: Proceedings of the Symposium on Isotopes in Water Resources Management, Vienna, March 1995, pp 439–444

  • Fetter CW (1972) Position of the saline water interface beneath oceanic islands. Water Resour Res 8(5):1307–1315

    Article  Google Scholar 

  • Geyh M, Grosjean M, Nunez LA, Schotterer U (1999) Radiocarbon reservoir effect and the timing of the late-glacial/early Holocene humid phase in the Atacama Desert, northern Chile. Quat Res 52:143–153

    Article  Google Scholar 

  • Greskowiak J, Röper T, Post VEA (2013) Closed-form approximations for two-dimensional groundwater age patterns in a fresh water lens. Ground Water 51(4):629–634

    Google Scholar 

  • Grosjean M, Veit H (2005) Water resources in the arid mountains of the Atacama Desert (northern Chile): past climate changes and modern conflicts. In: Huber UM, Bugmann HKM, Reasoner M (eds) Global change and mountain regions: an overview of current knowledge. Springer, Dordrecht, The Netherlands, pp 93–104

    Chapter  Google Scholar 

  • Günther T (2004) Inversion methods and resolution analysis for the 2D/3D reconstruction of resistivity structures from DC measurements. PhD Thesis, Freiberg University, Germany

  • Herzberg A (1901) Die Wasserversorgung einiger Nordseebäder [The water supply of some North Sea baths]. J Gasbeleuchtung Wasserversorgung 44:815–819 (in German)

  • Houben G, Hauschild S (2011) Numerical modeling of the near-field hydraulics of water wells. Ground Water 49(4):570–575

    Article  Google Scholar 

  • Houben G, Tünnermeier T, Eqrar N, Himmelsbach T (2009) Hydrogeology of the Kabul basin (Afghanistan), part II: groundwater geochemistry. Hydrogeol J 17(4):935–948

    Article  Google Scholar 

  • Ivanov NN (1954) The determination of potential evapotranspiration (in Russian). Izvestiia Vsesojuszogo Geograficheskogo Obschetva, Ser. T, 86 (2), Izd-vo Akademii Nauk SSSR, Moscow

  • Kinzelbach W, Aeschbach W, Alberich C, Goni IB, Beyerle U, Brunner P, Chiang W-H, Rueedi J, Zoellmann K (2002) A survey of methods for groundwater recharge in arid and semi-arid regions. Early Warning and Assessment Report Series, UNEP/DEWA/RS.02-2. United Nations Environment Programme, Nairobi, Kenya

  • Langevin CD, Guo W (2006) MODFLOW/MT3DMS-based simulation of variable density ground water flow and transport. Ground Water 44(3):339–351

    Article  Google Scholar 

  • McClain ME (ed.) (2002) The ecohydrology of South American rivers and wetlands. IAHS Spec. Publ. 6, IAHS, Wallingford, UK, 215 pp

  • Riccomini C, Fernandez Velázquez V, de Barros GC (2001) Cenozoic lithospheric faulting in the Asunción rift, eastern Paraguay. J South Amer Earth Sci 14(6):625–630

    Article  Google Scholar 

  • Spitz K, Moreno J (1996) A practical guide to groundwater and solute transport modelling. Wiley, New York, 461 pp

    Google Scholar 

  • Stoeckl L, Houben G (2012) Flow dynamics and age stratification of freshwater lenses: experiments and modeling. J Hydrol 458–459:9–15

    Article  Google Scholar 

  • Stuyfzand PJ (2008) Base exchange indices as indicators of salinization or freshening of (coastal) aquifers. In: Proceedings of the 20th Salt Water Intrusion Meeting, Naples, FL, USA, June 2008, pp 262–265

  • Sültenfuß J, Roether W, Rhein M (2009) The Bremen mass spectrometric facility for the measurement of helium isotopes, neon, and tritium in water. Isot Environ Health Stud 45(2):83–95

    Article  Google Scholar 

  • Vacher HL (1988) Dupuit-Ghyben-Herzberg analysis of strip-island lenses. Geol Soc Amer Bull 100:580–591

    Article  Google Scholar 

  • Veit H (1995) Jungquartäre Landschaft- und Klimaentwicklung der zentralen Anden und ihres westlichen Vorlandes: Kenntnisstand und Probleme [Upper Quaternary landscape and climate evolution of the central Andes and their western foreland: state of research and problems]. Geomethodica 20:163–194

    Google Scholar 

  • Velazquez VF, Comin-Chiaramonti P, Cundari A, de Barros GC, Riccomini C (2006) Cretaceous Na-alkaline magmatism from the Misiones Province (Paraguay): its relationships with the Paleocene Na-alkaline analog from Asunción and geodynamic significance. J Geol 114(5):593–614

    Article  Google Scholar 

  • Velázquez VF, Fonseca Giannini PC, Riccomini C, Martins Sallun AE, Hachiro J, de Barros GC (2008) Columnar joints in the Patiño formation sandstones, eastern Paraguay: a dynamic interaction between dyke intrusion, quartz dissolution and cooling-induced fractures. Episodes J Int Geosci 31(3):302–308

    Google Scholar 

  • Vogel JC (1967) Investigation of groundwater flow with radiocarbon. Proc. series, IAEA, Geneva, pp 355–368

  • Vogel JC (1970) Carbon-14 dating of groundwater. Proc. series, IAEA, Geneva, pp 225–239

  • Werner AD, Bakker M, Post VEA, Vandenbohede A, Lu C, Ataie-Ahstiani B, Simmons CT, Barry DA (2012) Seawater intrusion processes, investigation and management: recent advances and future challenges. Adv Water Resour 51:3–26

    Article  Google Scholar 

Download references

Acknowledgements

This study was funded by the German Federal Ministry of Economic Cooperation and Development (BMZ) within the Paraguayan-German Project 2004.2189, carried out jointly by the Secretaria del Medio Ambiente (SEAM), Paraguay, and the Federal Institute of Geosciences and Natural Resources (BGR), Germany.

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Correspondence to Georg Houben.

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Houben, G., Noell, U., Vassolo, S. et al. The freshwater lens of Benjamín Aceval, Chaco, Paraguay: a terrestrial analogue of an oceanic island lens. Hydrogeol J 22, 1935–1952 (2014). https://doi.org/10.1007/s10040-014-1169-2

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