Sol de Mañana
Sol de Mañana | |
---|---|
Highest point | |
Elevation | 4,900 m (16,100 ft) |
Coordinates | 22°25′35″S 67°45′35″W / 22.42639°S 67.75972°W[1] |
Geography | |
Sol de Mañana is an area with
Description
Sol de Mañana lies in the
Steam/water emissions can under exceptional circumstances reach heights of 200 metres (660 ft). Gas vents release
The nearest major communities are
Geology
Off the western coast of South America, the
The Andean
Local
Sol de Mañana is part of the
The heat may originate either in the Altiplano-Puna Magma Body or in the volcanic arc.[29] It is transported upward through convection, forming two heat reservoirs underground that are capped by a clay layer.[30] Precipitation water reaches the reservoirs through deep faults, which also allow heat circulation.[31] Drilling has shown that the reservoirs have temperatures of about 250–260 °C (482–500 °F).[19] The Sol de Mañana geothermal system may be physically connected to El Tatio,[32] with Sol de Mañana being closer to the heat source and Tatio an outflow at lower elevation.[33]
Climate and ecosystem
There is a weather station on Sol de Mañana.[34] Mean annual precipitation is about 75 millimetres (3.0 in) and mean temperatures are about 8.9 °C (48.0 °F).[13] The geothermal field is part of the Eduardo Avaroa Andean Fauna National Reserve[18] and one of the main tourism attractions on the Uyuni-Antofagasta road.[14]
Geothermal power generation
The 1973 oil crisis created the impetus for increased investigation of Bolivia's geothermal power resources, focusing on the Altiplano and the surrounding Andean ranges. Prospecting by the National Electricity Company and the state agency for geology identified Sajama, Salar de Empexa and Laguna Colorada as the most suitable areas for geothermal power generation.[9] A geothermal project began in 1978 and numerous drilling operations were undertaken in the following years; however development ceased in 1993 as the legal and political circumstances were unfavourable. A renewed effort began in 2010, spearheaded by the Japan International Cooperation Agency, during which additional cores were drilled, but as of 2023[update] is still at its early stages[35] and as of 2016[update] is only used as process heat for the San Cristobal mine.[14] An electrical power potential of about 50–100 megawatts (67,000–134,000 hp) has been estimated.[19]
Laguna Colorada/Sol de Mañana are the main focus of geothermal power prospecting in Bolivia; other sites have drawn scarce interest.[3] As of 2016[update] Bolivia did not have any legislation specific for geothermal power generation.[36] Geothermal power development is also hindered by the remote location, which would require building large power transmission networks, and the low price of electricity in the country.[14]
Notes
References
- ^ a b USGS 1992, p. 267.
- ^ Communication Ministry 2020.
- ^ a b Bona & Coviello 2016, p. 35.
- ^ a b c d De Silva & Francis 1991, p. 170.
- ^ Damir 2014, p. 156.
- ^ a b c d e f g h Pereyra Quiroga et al. 2023, p. 4.
- ^ a b c d De Silva & Francis 1991, p. 171.
- ^ Sullcani 2015, p. 668.
- ^ a b c Pereyra Quiroga et al. 2023, p. 1.
- ^ Pritchard et al. 2014, p. 98.
- ^ a b Pereyra Quiroga et al. 2023, p. 2.
- ^ Müller et al. 2022, p. 3.
- ^ a b Suaznabar, Quiroga & Villarreal 2019, p. 2.
- ^ a b c d Bona & Coviello 2016, p. 38.
- ^ Delgadillo & Puente 1998, p. 257.
- ^ Fernandez-Turiel et al. 2005, p. 127.
- ^ Pereyra Quiroga et al. 2023, p. 8.
- ^ a b Ministry of Hydrocarbons and Energies 2022, p. 183.
- ^ a b c d e Sullcani 2015, p. 666.
- ^ a b c Sullcani 2015, p. 667.
- ^ a b c Pereyra Quiroga et al. 2023, p. 3.
- ^ Pritchard et al. 2014, p. 90.
- ^ Fernandez-Turiel et al. 2005, p. 128.
- ^ Ort 2009, p. 1.
- ^ a b Pereyra Quiroga et al. 2023, p. 5.
- ^ Delgadillo & Puente 1998, p. 258.
- ^ Pereyra Quiroga et al. 2023, pp. 5–6.
- ^ Pereyra Quiroga et al. 2023, p. 19.
- ^ Pereyra Quiroga et al. 2023, p. 15.
- ^ Pereyra Quiroga et al. 2023, p. 17.
- ^ Pereyra Quiroga et al. 2023, p. 18.
- ^ Cortecci et al. 2005, p. 568.
- ^ De Silva & Francis 1991, p. 172.
- ^ Lagos et al. 2023, p. 5.
- ^ Pereyra Quiroga et al. 2023, pp. 1–2.
- ^ Bona & Coviello 2016, p. 36.
Sources
- Bona, Paolo; Coviello, Manlio (April 2016). Valoración y gobernanza de los proyectos geotérmicos en América del Sur: una propuesta metodológica (PDF) (in Spanish). CEPAL.
- Communication Ministry (25 July 2020). "Diputados aprueba financiamiento para construcción de Planta Geotérmica Laguna Colorada" (in Spanish).
- Cortecci, Gianni; Boschetti, Tiziano; Mussi, Mario; Lameli, Christian Herrera; Mucchino, Claudio; Barbieri, Maurizio (2005). "New chemical and original isotopic data on waters from El Tatio geothermal field, northern Chile". Geochemical Journal. 39 (6): 547–571. .
- De Silva, Shanaka L.; Francis, Peter (1991). Volcanoes of the central Andes. Vol. 220. Berlin: Springer-Verlag.
- Delgadillo, T. Z.; Puente, Héctor G. (1998). The Laguna Colorada (Bolivia) Project: A Reservoir Engineering Assessment (Report). Transactions-Geothermal Resources Council. pp. 257–262.
- Fernandez-Turiel, J.L.; Garcia-Valles, M.; Gimeno-Torrente, D.; Saavedra-Alonso, J.; Martinez-Manent, S. (October 2005). "The hot spring and geyser sinters of El Tatio, Northern Chile". Sedimentary Geology. 180 (3–4): 125–147. .
- Damir, Galaz-Mandakovic Fernández (2014). "Uyuni, capital turística de Bolivia. Aproximaciones antropológicas a un fenómeno visual posmoderno desbordante". Teoría y Praxis (in Spanish). 16: 147–173.
- Lagos, Magdalena Sofía; Muñoz, José Francisco; Suárez, Francisco Ignacio; Fuenzalida, María José; Yáñez‐Morroni, Gonzalo; Sanzana, Pedro (29 June 2023). "Investigating the effects of channelization in the Silala River: A review of the implementation of a coupled MIKE ‐11 and MIKE‐SHE modeling system". WIREs Water. .
- Ministry of Hydrocarbons and Energies (April 2022). Informe de rendición pública de cuentas inicial 2022 (PDF) (Report) (in Spanish).
- Müller, Daniel; Walter, Thomas R.; Zimmer, Martin; Gonzalez, Gabriel (1 December 2022). "Distribution, structural and hydrological control of the hot springs and geysers of El Tatio, Chile, revealed by optical and thermal infrared drone surveying". Journal of Volcanology and Geothermal Research. 432: 107696. S2CID 253033476.
- Ort, Michael H. (October 2009). Two new supereruptions in the Altiplano-Puna volcanic complex of the central Andes. 2009 Portland GSA Annual Meeting.
- Pereyra Quiroga, Bruno; Meneses Rioseco, Ernesto; Kapinos, Gerhard; Brasse, Heinrich (1 September 2023). "Three-dimensional magnetotelluric inversion for the characterization of the Sol de Mañana high-enthalpy geothermal field, Bolivia". Geothermics. 113: 102748. S2CID 259617984.
- Pritchard, M. E.; Henderson, S. T.; Jay, J. A.; Soler, V.; Krzesni, D. A.; Button, N. E.; Welch, M. D.; Semple, A. G.; Glass, B.; Sunagua, M.; Minaya, E.; Amigo, A.; Clavero, J. (1 June 2014). "Reconnaissance earthquake studies at nine volcanic areas of the central Andes with coincident satellite thermal and InSAR observations". Journal of Volcanology and Geothermal Research. 280: 90–103. ISSN 0377-0273.
- Suaznabar, Paola Adriana Coca; Quiroga, Bruno Pereyra; Villarreal, José Ramón Pérez (2019). "Well Drilling in Sol de Mañana Geothermal Field – Laguna Colorada Geothermal Project" (PDF). GRC Transactions. 43.
- Sullcani, Pedro Rómulo Ramos (2015). Well Data Analysis and Volumetric Assessment of the Sol de Mañana Geothermal Field, Bolivia (PDF). National Energy Authority (Iceland) (Report). United Nations University.
- USGS (1992). Geology and mineral resources of the Altiplano and Cordillera Occidental, Bolivia (Report). doi:10.3133/b1975.