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3He/4He Signature of Magmatic Fluids from Telica (Nicaragua) and Baru (Panama) Volcanoes, Central American Volcanic Arc. APPLIED SCIENCES-BASEL 2022. [DOI: 10.3390/app12094241] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
Abstract
Constraining the magmatic 3He/4He signature of fluids degassed from a magmatic system is crucial for making inferences on its mantle source. This is especially important in arc volcanism, where variations in the composition of the wedge potentially induced by slab sediment fluids must be distinguished from the effects of magma differentiation, degassing, and crustal contamination. The study of fluid inclusions (FIs) trapped in minerals of volcanic rocks is becoming an increasingly used methodology in geochemical studies that integrates the classical study of volcanic and geothermal fluids. Here, we report on the first noble gas (He, Ne, Ar) concentrations and isotopic ratios of FI in olivine (Ol) and pyroxene (Px) crystals separated from eruptive products of the Telica and Baru volcanoes, belonging to the Nicaraguan and Panamanian arc-segments of Central America Volcanic arc (CAVA). FIs from Telica yield air corrected 3He/4He (Rc/Ra) of 7.2–7.4 Ra in Ol and 6.1–7.3 in Px, while those from Baru give 7.1–8.0 Ra in Ol and 4.2–5.8 Ra in Px. After a data quality check and a comparison with previous 3He/4He measurements carried out on the same volcanoes and along CAVA, we constrained a magmatic Rc/Ra signature of 7.5 Ra for Telica and of 8.0 Ra for Baru, both within the MORB range (8 ± 1 Ra). These 3He/4He differences also reflect variations in the respective arc-segments, which cannot be explained by radiogenic 4He addition due to variable crust thickness, as the mantle beneath Nicaragua and Panama is at about 35 and 30 km, respectively. We instead highlight that the lowest 3He/4He signature observed in the Nicaraguan arc segment reflects a contamination of the underlying wedge by slab sediment fluids. Rc/Ra values up to 9.0 Ra are found at Pacaya volcano in Guatemala, where the crust is 45 km thick, while a 3He/4He signature of about 8.0 Ra was measured at Turrialba volcano in Costa Rica, which is similar to that of Baru, and reflects possible influence of slab melting, triggered by a change in subduction conditions and the contemporary subduction of the Galapagos hot-spot track below southern Costa Rica and western Panama.
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Aiuppa A, Bitetto M, Delle Donne D, La Monica FP, Tamburello G, Coppola D, Della Schiava M, Innocenti L, Lacanna G, Laiolo M, Massimetti F, Pistolesi M, Silengo MC, Ripepe M. Volcanic CO 2 tracks the incubation period of basaltic paroxysms. SCIENCE ADVANCES 2021; 7:eabh0191. [PMID: 34533982 PMCID: PMC8448455 DOI: 10.1126/sciadv.abh0191] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 02/10/2021] [Accepted: 07/29/2021] [Indexed: 06/13/2023]
Abstract
The ordinarily benign activity of basaltic volcanoes is periodically interrupted by violent paroxysmal explosions ranging in size from Hawaiian to Plinian in the most extreme examples. These paroxysms often occur suddenly and with limited or no precursors, leaving their causal mechanisms still incompletely understood. Two such events took place in summer 2019 at Stromboli, a volcano otherwise known for its persistent mild open-vent activity, resulting in one fatality and damage to infrastructure. Here, we use a post hoc analysis and reinterpretation of volcanic gas compositions and fluxes acquired at Stromboli to show that the two paroxysms were preceded by detectable escalations in volcanic plume CO2 degassing weeks to months beforehand. Our results demonstrate that volcanic gas CO2 is a key driver of explosions and that the preparatory periods ahead of explosions in basaltic systems can be captured by precursory CO2 leakage from deeply stored mafic magma.
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Affiliation(s)
- Alessandro Aiuppa
- Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Palermo, Italy
| | - Marcello Bitetto
- Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Palermo, Italy
| | - Dario Delle Donne
- Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Palermo, Italy
- Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Napoli, Italy
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
| | - Francesco Paolo La Monica
- Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Palermo, Italy
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
| | - Giancarlo Tamburello
- Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy
| | - Diego Coppola
- Dipartimento di Scienze della Terra, Università di Torino, Torino, Italy
| | - Massimo Della Schiava
- Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Palermo, Italy
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
| | - Lorenzo Innocenti
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
| | - Giorgio Lacanna
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
| | - Marco Laiolo
- Dipartimento di Scienze della Terra, Università di Torino, Torino, Italy
| | | | - Marco Pistolesi
- Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy
| | | | - Maurizio Ripepe
- Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy
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3
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Bundschuh J, Schneider J, Alam MA, Niazi NK, Herath I, Parvez F, Tomaszewska B, Guilherme LRG, Maity JP, López DL, Cirelli AF, Pérez-Carrera A, Morales-Simfors N, Alarcón-Herrera MT, Baisch P, Mohan D, Mukherjee A. Seven potential sources of arsenic pollution in Latin America and their environmental and health impacts. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 780:146274. [PMID: 34030289 DOI: 10.1016/j.scitotenv.2021.146274] [Citation(s) in RCA: 47] [Impact Index Per Article: 15.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/19/2020] [Revised: 02/25/2021] [Accepted: 02/28/2021] [Indexed: 06/12/2023]
Abstract
This review presents a holistic overview of the occurrence, mobilization, and pathways of arsenic (As) from predominantly geogenic sources into different near-surface environmental compartments, together with the respective reported or potential impacts on human health in Latin America. The main sources and pathways of As pollution in this region include: (i) volcanism and geothermalism: (a) volcanic rocks, fluids (e.g., gases) and ash, including large-scale transport of the latter through different mechanisms, (b) geothermal fluids and their exploitation; (ii) natural lixiviation and accelerated mobilization from (mostly sulfidic) metal ore deposits by mining and related activities; (iii) coal deposits and their exploitation; (iv) hydrocarbon reservoirs and co-produced water during exploitation; (v) solute and sediment transport through rivers to the sea; (vi) atmospheric As (dust and aerosol); and (vii) As exposure through geophagy and involuntary ingestion. The two most important and well-recognized sources and mechanisms for As release into the Latin American population's environments are: (i) volcanism and geothermalism, and (ii) strongly accelerated As release from geogenic sources by mining and related activities. Several new analyses from As-endemic areas of Latin America emphasize that As-related mortality and morbidity continue to rise even after decadal efforts towards lowering As exposure. Several public health regulatory institutions have classified As and its compounds as carcinogenic chemicals, as As uptake can affect several organ systems, viz. dermal, gastrointestinal, peptic, neurological, respiratory, reproductive, following exposure. Accordingly, ingesting large amounts of As can damage the stomach, kidneys, liver, heart, and nervous system; and, in severe cases, may cause death. Moreover, breathing air with high As levels can cause lung damage, shortness of breath, chest pain, and cough. Further, As compounds, being corrosive, can also cause skin lesions or damage eyes, and long-term exposure to As can lead to cancer development in several organs.
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Affiliation(s)
- Jochen Bundschuh
- UNESCO Chair on Groundwater Arsenic within the 2030 Agenda for Sustainable Development, University of Southern Queensland, West Street, Toowoomba 4350, Queensland, Australia.
| | - Jerusa Schneider
- Department of Geology and Natural Resources, Institute of Geosciences, University of Campinas, 13083-855 Campinas, SP, Brazil; Faculty of Agricultural Sciences, Federal University of Grande Dourados, João Rosa Góes St., 1761, Dourados, Mato Grosso do Sul, 79804-970, Brazil
| | - Mohammad Ayaz Alam
- Departamento de Geología, Facultad de Ingeniería, Universidad de Atacama, Avenida Copayapu 485, Copiapó, Región de Atacama, Chile
| | - Nabeel Khan Niazi
- Institute of Soil and Environmental Sciences, University of Agriculture Faisalabad, Faisalabad 38040, Pakistan
| | - Indika Herath
- UNESCO Chair on Groundwater Arsenic within the 2030 Agenda for Sustainable Development, University of Southern Queensland, West Street, Toowoomba 4350, Queensland, Australia
| | - Faruque Parvez
- Department of Environmental Health Sciences, Columbia University, 60 Haven Ave, B-1, New York, NY 10032, USA
| | - Barbara Tomaszewska
- AGH University of Science and Technology, Mickiewicza 30 Av., 30-059 Kraków, Poland
| | | | - Jyoti Prakash Maity
- Department of Earth and Environmental Sciences, National Chung Cheng University, 168 University Road, Min-Hsiung, Chiayi County 62102, Taiwan
| | - Dina L López
- Department of Geological Sciences, Ohio University, 316 Clippinger Laboratories, Athens, OH, USA
| | - Alicia Fernández Cirelli
- University of Buenos Aires, Faculty of Veterinary Sciences, Instituto de Investigaciones en Producción Animal (UBA-CONICET), Centro de Estudios, Transdiciplinarios del Agua (UBA), Av. Chorroarín 280, CABA C1427CWO, Argentina
| | - Alejo Pérez-Carrera
- University of Buenos Aires, Faculty of Veterinary Sciences, Centro de Estudios Transdiciplinarios del Agua (UBA), Instituto de Investigaciones en Producción Animal (UBA-CONICET), Cátedra de Química Orgánica de Biomoléculas, Av. Chorroarín 280, CABA C1427CWO, Argentina
| | - Nury Morales-Simfors
- UNESCO Chair on Groundwater Arsenic within the 2030 Agenda for Sustainable Development, University of Southern Queensland, West Street, Toowoomba 4350, Queensland, Australia; RISE Research Institutes of Sweden, Division ICT-RISE SICS East, Linköping SE-581.83, Sweden
| | - Maria Teresa Alarcón-Herrera
- Departamento de Ingeniería Sustentable, Centro de Investigación en Materiales Avanzados SC Unidad Durango, C. CIMAV # 110, Ejido Arroyo Seco, Durango, Dgo., Mexico
| | - Paulo Baisch
- Laboratório de Oceanografia Geológica, Instituto de Oceanografia, Universidade Federal do Rio Grande (FURG), Campus Carreiros, CP 474, CEP 96203-900 Rio Grande, RS, Brazil
| | - Dinesh Mohan
- UNESCO Chair on Groundwater Arsenic within the 2030 Agenda for Sustainable Development, University of Southern Queensland, West Street, Toowoomba 4350, Queensland, Australia; School of Environmental Sciences, Jawaharlal Nehru University, New Delhi 110067, India
| | - Abhijit Mukherjee
- Department of Geology and Geophysics, Indian Institute of Technology (IIT), Kharagpur, West Bengal 721302, India
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Wood K, Liu EJ, Richardson T, Clarke R, Freer J, Aiuppa A, Giudice G, Bitetto M, Mulina K, Itikarai I. BVLOS UAS Operations in Highly-Turbulent Volcanic Plumes. Front Robot AI 2020; 7:549716. [PMID: 33501316 PMCID: PMC7805736 DOI: 10.3389/frobt.2020.549716] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/07/2020] [Accepted: 08/24/2020] [Indexed: 11/29/2022] Open
Abstract
Long-range, high-altitude Unoccupied Aerial System (UAS) operations now enable in-situ measurements of volcanic gas chemistry at globally-significant active volcanoes. However, the extreme environments encountered within volcanic plumes present significant challenges for both air frame development and in-flight control. As part of a multi-disciplinary field deployment in May 2019, we flew fixed wing UAS Beyond Visual Line of Sight (BVLOS) over Manam volcano, Papua New Guinea, to measure real-time gas concentrations within the volcanic plume. By integrating aerial gas measurements with ground- and satellite-based sensors, our aim was to collect data that would constrain the emission rate of environmentally-important volcanic gases, such as carbon dioxide, whilst providing critical insight into the state of the subsurface volcanic system. Here, we present a detailed analysis of three BVLOS flights into the plume of Manam volcano and discuss the challenges involved in operating in highly turbulent volcanic plumes. Specifically, we report a detailed description of the system, including ground and air components, and flight plans. We present logged flight data for two successful flights to evaluate the aircraft performance under the atmospheric conditions experienced during plume traverses. Further, by reconstructing the sequence of events that led to the failure of the third flight, we identify a number of lessons learned and propose appropriate recommendations to reduce risk in future flight operations.
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Affiliation(s)
- Kieran Wood
- Department of Aerospace Engineering, University of Bristol, Bristol, United Kingdom
| | - Emma J. Liu
- Department of Earth Sciences, University College London, London, United Kingdom
| | - Tom Richardson
- Department of Aerospace Engineering, University of Bristol, Bristol, United Kingdom
| | - Robert Clarke
- Department of Aerospace Engineering, University of Bristol, Bristol, United Kingdom
| | - Jim Freer
- School of Geographical Sciences, University of Bristol, Bristol, United Kingdom
- University of Saskatchewan Centre for Hydrology, Canmore, AB, Canada
| | - Alessandro Aiuppa
- Dipartimento di Scienze della Terra e del Mare, University of Palermo, Palermo, Italy
| | - Gaetano Giudice
- Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
| | - Marcello Bitetto
- Dipartimento di Scienze della Terra e del Mare, University of Palermo, Palermo, Italy
| | - Kila Mulina
- Rabaul Volcanological Observatory, Rabaul, Papua New Guinea
| | - Ima Itikarai
- Rabaul Volcanological Observatory, Rabaul, Papua New Guinea
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5
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Liu EJ, Aiuppa A, Alan A, Arellano S, Bitetto M, Bobrowski N, Carn S, Clarke R, Corrales E, de Moor JM, Diaz JA, Edmonds M, Fischer TP, Freer J, Fricke GM, Galle B, Gerdes G, Giudice G, Gutmann A, Hayer C, Itikarai I, Jones J, Mason E, McCormick Kilbride BT, Mulina K, Nowicki S, Rahilly K, Richardson T, Rüdiger J, Schipper CI, Watson IM, Wood K. Aerial strategies advance volcanic gas measurements at inaccessible, strongly degassing volcanoes. SCIENCE ADVANCES 2020; 6:6/44/eabb9103. [PMID: 33127674 PMCID: PMC7608812 DOI: 10.1126/sciadv.abb9103] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 04/06/2020] [Accepted: 09/18/2020] [Indexed: 06/11/2023]
Abstract
Volcanic emissions are a critical pathway in Earth's carbon cycle. Here, we show that aerial measurements of volcanic gases using unoccupied aerial systems (UAS) transform our ability to measure and monitor plumes remotely and to constrain global volatile fluxes from volcanoes. Combining multi-scale measurements from ground-based remote sensing, long-range aerial sampling, and satellites, we present comprehensive gas fluxes-3760 ± [600, 310] tons day-1 CO2 and 5150 ± [730, 340] tons day-1 SO2-for a strong yet previously uncharacterized volcanic emitter: Manam, Papua New Guinea. The CO2/ST ratio of 1.07 ± 0.06 suggests a modest slab sediment contribution to the sub-arc mantle. We find that aerial strategies reduce uncertainties associated with ground-based remote sensing of SO2 flux and enable near-real-time measurements of plume chemistry and carbon isotope composition. Our data emphasize the need to account for time averaging of temporal variability in volcanic gas emissions in global flux estimates.
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Affiliation(s)
- E J Liu
- University College London, London WC1E6BS, UK.
- University of Cambridge, Cambridge CB23EQ, UK
| | - A Aiuppa
- Università di Palermo, 90123 Palermo, Italy
| | - A Alan
- GasLAB, Universidad de Costa Rica, San José, Costa Rica
| | - S Arellano
- Chalmers University of Technology, Göteborg, Sweden
| | - M Bitetto
- Università di Palermo, 90123 Palermo, Italy
| | - N Bobrowski
- Heidelberg University, Heidelberg, Germany
- Max Planck Institute for Chemistry, Mainz, Germany
| | - S Carn
- Michigan Technological University, Houghton, MI 49931, USA
| | - R Clarke
- University of Bristol, Bristol, BS8 1TR, UK
| | - E Corrales
- GasLAB, Universidad de Costa Rica, San José, Costa Rica
| | - J M de Moor
- Universidad Nacional, Heredia, 40101-3000 Costa Rica
| | - J A Diaz
- GasLAB, Universidad de Costa Rica, San José, Costa Rica
| | - M Edmonds
- University of Cambridge, Cambridge CB23EQ, UK
| | - T P Fischer
- University of New Mexico, Albuquerque, NM 87131, USA
| | - J Freer
- University of Bristol, Bristol, BS8 1TR, UK
- University of Saskatchewan, Centre for Hydrology, Canmore, Alberta T1W 3G1, Canada
| | - G M Fricke
- University of New Mexico, Albuquerque, NM 87131, USA
| | - B Galle
- Chalmers University of Technology, Göteborg, Sweden
| | - G Gerdes
- Chalmers University of Technology, Göteborg, Sweden
| | - G Giudice
- INGV, Osservatorio Etneo, Sezione di Catania, 95125 Catania, Italy
| | - A Gutmann
- Johannes Gutenberg-Universität, Mainz 55128, Germany
| | - C Hayer
- University of Manchester, Manchester, M13 9PL, UK
| | - I Itikarai
- Rabaul Volcanological Observatory, Rabaul, Papua New Guinea
| | - J Jones
- University of New Mexico, Albuquerque, NM 87131, USA
| | - E Mason
- University of Cambridge, Cambridge CB23EQ, UK
| | | | - K Mulina
- Rabaul Volcanological Observatory, Rabaul, Papua New Guinea
| | - S Nowicki
- University of New Mexico, Albuquerque, NM 87131, USA
| | - K Rahilly
- University of New Mexico, Albuquerque, NM 87131, USA
| | | | - J Rüdiger
- Johannes Gutenberg-Universität, Mainz 55128, Germany
| | - C I Schipper
- Victoria University of Wellington, Wellington 6012, New Zealand
| | - I M Watson
- University of Bristol, Bristol, BS8 1TR, UK
| | - K Wood
- University of Bristol, Bristol, BS8 1TR, UK
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Madrigal-Solís H, Jiménez-Gavilán P, Vadillo-Pérez I, Fonseca-Sánchez A, Quesada-Hernández L, Sánchez-Gutiérrez R, Calderón-Sánchez H, Pardo-Vargas C. Application of hydrogeochemistry and isotopic characterization for the assessment of recharge in a volcanic aquifer in the eastern region of central Costa Rica. ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES 2020; 56:446-464. [PMID: 32903064 DOI: 10.1080/10256016.2020.1814277] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/09/2020] [Accepted: 07/30/2020] [Indexed: 06/11/2023]
Abstract
In the eastern region of central Costa Rica, land use in the sub-basins of the Maravilla-Chiz and Quebrada Honda rivers (47 km2) is dominated by agricultural and livestock production, while groundwater resources constitute the main drinking water supply. This study aimed to (a) evaluate the location of groundwater recharge areas and groundwater flow paths, and (b) provide a characterization of the hydrochemistry and possible anthropic impacts. Groundwater was collected from 20 sites during the dry and rainy seasons and analysed for major ions, water stable isotopes and 222Rn. Approximated recharge areas were estimated through a local altitudinal line based on isotopic compositions in springs. The hydrochemical and isotopic characterization of groundwater showed that the main recharge areas occur in the upper part of the basin, except for springs in the middle part of the basin probably due to a certain hydraulic disconnection from the upper part that facilitates local recharge processes. In the lower basin, groundwater exhibited greater transit times and longer flow paths. Low nitrate, chloride and sulphate concentrations found in groundwater indicate low leaching of fertilizers or urban wastewaters. Our results are focused to improve water resources and agricultural management plans in a dynamic tropical landscape.
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Affiliation(s)
- Helga Madrigal-Solís
- Laboratory of Environmental Hydrology, School of Biological Sciences, Universidad Nacional, Heredia, Costa Rica
| | - Pablo Jiménez-Gavilán
- Department of Geology and Ecology, Faculty of Sciences, University of Málaga, Málaga, Spain
| | - Iñaki Vadillo-Pérez
- Department of Geology and Ecology, Faculty of Sciences, University of Málaga, Málaga, Spain
| | - Alicia Fonseca-Sánchez
- Laboratory of Environmental Hydrology, School of Biological Sciences, Universidad Nacional, Heredia, Costa Rica
| | - Luis Quesada-Hernández
- Laboratory of Environmental Hydrology, School of Biological Sciences, Universidad Nacional, Heredia, Costa Rica
| | - Rolando Sánchez-Gutiérrez
- Stable Isotopes Research Group and Water Resource Management Laboratory, School of Chemistry, Universidad Nacional, Costa Rica
| | - Hazel Calderón-Sánchez
- Laboratory of Environmental Hydrology, School of Biological Sciences, Universidad Nacional, Heredia, Costa Rica
| | - Carlos Pardo-Vargas
- Department of Geology and Ecology, Faculty of Sciences, University of Málaga, Málaga, Spain
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7
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Pering TD, Liu EJ, Wood K, Wilkes TC, Aiuppa A, Tamburello G, Bitetto M, Richardson T, McGonigle AJS. Combined ground and aerial measurements resolve vent-specific gas fluxes from a multi-vent volcano. Nat Commun 2020; 11:3039. [PMID: 32546707 PMCID: PMC7298010 DOI: 10.1038/s41467-020-16862-w] [Citation(s) in RCA: 15] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/18/2019] [Accepted: 05/26/2020] [Indexed: 11/23/2022] Open
Abstract
Volcanoes with multiple summit vents present a methodological challenge for determining vent-specific gas emissions. Here, using a novel approach combining multiple ultraviolet cameras with synchronous aerial measurements, we calculate vent-specific gas compositions and fluxes for Stromboli volcano. Emissions from vent areas are spatially heterogeneous in composition and emission rate, with the central vent area dominating passive emissions, despite exhibiting the least explosive behaviour. Vents exhibiting Strombolian explosions emit low to negligible passive fluxes and are CO2-dominated, even during passive degassing. We propose a model for the conduit system based on contrasting rheological properties between vent areas. Our methodology has advantages for resolving contrasting outgassing dynamics given that measured bulk plume compositions are often intermediate between those of the distinct vent areas. We therefore emphasise the need for a vent-specific approach at multi-vent volcanoes and suggest that our approach could provide a transformative advance in volcano monitoring applications. Combining multiple ultraviolet cameras with synchronous aerial measurements, the authors here present vent-specific gas compositions and fluxes for Stromboli volcano. The results show that gas compositions vary between different vents, mirroring differences in eruptive behavior.
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Affiliation(s)
- T D Pering
- Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK.
| | - E J Liu
- Department of Earth Sciences, University College London, London, WC1E 6BS, UK
| | - K Wood
- Department of Aerospace Engineering, University of Bristol, Bristol, BS8 1TR, UK
| | - T C Wilkes
- Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK
| | - A Aiuppa
- DiSTeM, Università di Palermo, via Archirafi, 36, 90123, Palermo, Italy
| | - G Tamburello
- Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Via Donato Creti, 12, 40128, Bologna, Italy
| | - M Bitetto
- DiSTeM, Università di Palermo, via Archirafi, 36, 90123, Palermo, Italy
| | - T Richardson
- Department of Aerospace Engineering, University of Bristol, Bristol, BS8 1TR, UK
| | - A J S McGonigle
- Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK.,School of Geosciences, the University of Sydney, Camperdown, NSW, 2006, Australia.,Faculty of Health, Engineering and Sciences, University of Southern Queensland, Toowoomba, QLD, 4350, Australia
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8
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Wygel CM, Peters SC, McDermott JM, Sahagian DL. Bubbles and Dust: Experimental Results of Dissolution Rates of Metal Salts and Glasses From Volcanic Ash Deposits in Terms of Surface Area, Chemistry, and Human Health Impacts. GEOHEALTH 2019; 3:338-355. [PMID: 32159023 PMCID: PMC7007129 DOI: 10.1029/2018gh000181] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/15/2018] [Revised: 08/02/2019] [Accepted: 08/19/2019] [Indexed: 05/13/2023]
Abstract
Explosive volcanic eruptions lead to ash deposition and subsequent leaching of contaminants into soils or surface water, impacting flora and fauna, including human health. This study determined the control of ash surface area and chemical composition on ash dissolution rates. Fresh, unhydrated ash samples from four contrasting volcanoes were analyzed in the laboratory. Column leachate tests were used to compare leaching rates over a range of basaltic to andesitic ashes as a function of time and surface area, to analyze the effects of ash deposition. It was found that surface area, measured both geometrically and by multipoint Brunauer-Emmett-Teller analysis, generally increases for a short time, gradually decreases, then increases over the rest of the leaching experiment, due to area to mass ratio fluctuations. After the column leachate tests, postleaching water analyses for elemental compositions were conducted by inductively coupled plasma-mass spectrometry and ion chromatography. Steady state dissolution rates initially decayed rapidly due to the smallest size fraction of ash (dust), which provides a large area of fresh leachable surfaces as well as the rapid dissolution of highly soluble metal salts. Some of the dissolved concentrations of elements relevant to human and ecosystem health such as F, Cd, Se, As, and Cr rose above World Health Organization (WHO) drinking water standards within an hour of experimental leaching. In nature, however, safe consumption standards are further dependent upon bioaccumulation and chronic exposure. As such, individual and recurring ash deposition events have applications to emergency response and preparedness in volcanic regions.
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Affiliation(s)
- C. M. Wygel
- Department of Earth and Environmental SciencesLehigh UniversityBethlehemPAUSA
| | - S. C. Peters
- Department of Earth and Environmental SciencesLehigh UniversityBethlehemPAUSA
| | - J. M. McDermott
- Department of Earth and Environmental SciencesLehigh UniversityBethlehemPAUSA
| | - D. L. Sahagian
- Department of Earth and Environmental SciencesLehigh UniversityBethlehemPAUSA
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9
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Abstract
A hidden carbon cycle exists inside Earth. Every year, megatons of carbon disappear into subduction zones, affecting atmospheric carbon dioxide and oxygen over Earth's history. Here we discuss the processes that move carbon towards subduction zones and transform it into fluids, magmas, volcanic gases and diamonds. The carbon dioxide emitted from arc volcanoes is largely recycled from subducted microfossils, organic remains and carbonate precipitates. The type of carbon input and the efficiency with which carbon is remobilized in the subduction zone vary greatly around the globe, with every convergent margin providing a natural laboratory for tracing subducting carbon.
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Affiliation(s)
- Terry Plank
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA.
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10
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Forearc carbon sink reduces long-term volatile recycling into the mantle. Nature 2019; 568:487-492. [PMID: 31019327 DOI: 10.1038/s41586-019-1131-5] [Citation(s) in RCA: 20] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/28/2018] [Accepted: 02/08/2019] [Indexed: 11/08/2022]
Abstract
Carbon and other volatiles in the form of gases, fluids or mineral phases are transported from Earth's surface into the mantle at convergent margins, where the oceanic crust subducts beneath the continental crust. The efficiency of this transfer has profound implications for the nature and scale of geochemical heterogeneities in Earth's deep mantle and shallow crustal reservoirs, as well as Earth's oxidation state. However, the proportions of volatiles released from the forearc and backarc are not well constrained compared to fluxes from the volcanic arc front. Here we use helium and carbon isotope data from deeply sourced springs along two cross-arc transects to show that about 91 per cent of carbon released from the slab and mantle beneath the Costa Rican forearc is sequestered within the crust by calcite deposition. Around an additional three per cent is incorporated into the biomass through microbial chemolithoautotrophy, whereby microbes assimilate inorganic carbon into biomass. We estimate that between 1.2 × 108 and 1.3 × 1010 moles of carbon dioxide per year are released from the slab beneath the forearc, and thus up to about 19 per cent less carbon is being transferred into Earth's deep mantle than previously estimated.
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11
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Aiuppa A, Fischer TP, Plank T, Bani P. CO 2 flux emissions from the Earth's most actively degassing volcanoes, 2005-2015. Sci Rep 2019; 9:5442. [PMID: 30931997 PMCID: PMC6443792 DOI: 10.1038/s41598-019-41901-y] [Citation(s) in RCA: 59] [Impact Index Per Article: 11.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/11/2018] [Accepted: 03/20/2019] [Indexed: 11/09/2022] Open
Abstract
The global carbon dioxide (CO2) flux from subaerial volcanoes remains poorly quantified, limiting our understanding of the deep carbon cycle during geologic time and in modern Earth. Past attempts to extrapolate the global volcanic CO2 flux have been biased by observations being available for a relatively small number of accessible volcanoes. Here, we propose that the strong, but yet unmeasured, CO2 emissions from several remote degassing volcanoes worldwide can be predicted using regional/global relationships between the CO2/ST ratio of volcanic gases and whole-rock trace element compositions (e.g., Ba/La). From these globally linked gas/rock compositions, we predict the CO2/ST gas ratio of 34 top-degassing remote volcanoes with no available gas measurements. By scaling to volcanic SO2 fluxes from a global catalogue, we estimate a cumulative “unmeasured” CO2 output of 11.4 ± 1.1 Mt/yr (or 0.26 ± 0.02·1012 mol/yr). In combination with the measured CO2 output of 27.4 ± 3.6 Mt/yr (or 0.62 ± 0.08·1012 mol/yr), our results constrain the time-averaged (2005–2015) cumulative CO2 flux from the Earth’s 91 most actively degassing subaerial volcanoes at 38.7 ± 2.9 Mt/yr (or 0.88 ± 0.06·1012 mol/yr).
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Affiliation(s)
| | - Tobias P Fischer
- Department of Earth and Planetary Sciences, New Mexico University, Albuquerque, USA
| | - Terry Plank
- Lamont-Doherty Earth Observatory, Columbia University, New York, USA
| | - Philipson Bani
- Laboratoire Magmas et Volcans, Université Blaise Pascal - CNRS -IRD, OPGC, Aubière, France
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12
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Abstract
One of the biggest challenges in volcanic hazard assessment is to understand how and why eruptive style changes within the same eruptive period or even from one eruption to the next at a given volcano. This review evaluates the competing processes that lead to explosive and effusive eruptions of silicic magmas. Eruptive style depends on a set of feedback involving interrelated magmatic properties and processes. Foremost of these are magma viscosity, gas loss and external properties such as conduit geometry. Ultimately, these parameters control the speed at which magmas ascend, decompress and outgas en route to the surface, and thus determine eruptive style and evolution. Eruptive styles at a single volcano may transition from explosive to effusive behaviour (or vice versa) at any given time. This review examines the underlying controls on eruptive styles such as magma viscosity, degassing and conduit geometry at volcanoes with silicic compositions.
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13
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Stix J, de Moor JM. Understanding and forecasting phreatic eruptions driven by magmatic degassing. EARTH, PLANETS, AND SPACE : EPS 2018; 70:83. [PMID: 31007532 PMCID: PMC6448360 DOI: 10.1186/s40623-018-0855-z] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 12/21/2017] [Accepted: 05/01/2018] [Indexed: 06/09/2023]
Abstract
This paper examines phreatic eruptions which are driven by inputs of magma and magmatic gas. We synthesize data from several significant phreatic systems, including two in Costa Rica (Turrialba and Poás) which are currently highly active and hazardous. We define two endmember types of phreatic eruptions, the first (type 1) in which a deeper hydrothermal system fed by magmatic gases is sealed and produces overpressure sufficient to drive explosive eruptions, and the second (type 2) where magmatic gases are supplied via open-vent degassing to a near-surface hydrothermal system, vaporizing liquid water which drives the phreatic eruptions. The surficial source of type 2 eruptions is characteristic, while the source depth of type 1 eruptions is commonly greater. Hence, type 1 eruptions tend to be more energetic than type 2 eruptions. The first type of eruption we term "phreato-vulcanian", and the second we term "phreato-surtseyan". Some systems (e.g., Ruapehu, Poás) can produce both type 1 and type 2 eruptions, and all systems can undergo sealing at various timescales. We examine a number of precursory signals which appear to be important in understanding and forecasting phreatic eruptions; these include very long period events, banded tremor, and gas ratios, in particular H2S/SO2 and CO2/SO2. We propose that if these datasets are carefully integrated during a monitoring program, it may be possible to accurately forecast phreatic eruptions.
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Affiliation(s)
- John Stix
- Department of Earth and Planetary Sciences, McGill University, 3450 University Street, Montreal, QC H3A 0E8 Canada
| | - J. Maarten de Moor
- Observatorio Vulcanológico y Sismológico de Costa Rica (OVSICORI), Universidad Nacional, AP 2386-3000, Heredia, Costa Rica
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14
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Schwandner FM, Gunson MR, Miller CE, Carn SA, Eldering A, Krings T, Verhulst KR, Schimel DS, Nguyen HM, Crisp D, O'Dell CW, Osterman GB, Iraci LT, Podolske JR. Spaceborne detection of localized carbon dioxide sources. Science 2018; 358:358/6360/eaam5782. [PMID: 29026015 DOI: 10.1126/science.aam5782] [Citation(s) in RCA: 29] [Impact Index Per Article: 4.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/12/2016] [Accepted: 07/06/2017] [Indexed: 11/03/2022]
Abstract
Spaceborne measurements by NASA's Orbiting Carbon Observatory-2 (OCO-2) at the kilometer scale reveal distinct structures of atmospheric carbon dioxide (CO2) caused by known anthropogenic and natural point sources. OCO-2 transects across the Los Angeles megacity (USA) show that anthropogenic CO2 enhancements peak over the urban core and decrease through suburban areas to rural background values more than ~100 kilometers away, varying seasonally from ~4.4 to 6.1 parts per million. A transect passing directly downwind of the persistent isolated natural CO2 plume from Yasur volcano (Vanuatu) shows a narrow filament of enhanced CO2 values (~3.4 parts per million), consistent with a CO2 point source emitting 41.6 kilotons per day. These examples highlight the potential of the OCO-2 sensor, with its unprecedented resolution and sensitivity, to detect localized natural and anthropogenic CO2 sources.
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Affiliation(s)
- Florian M Schwandner
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. .,Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles (UCLA), Los Angeles, CA 90095, USA
| | - Michael R Gunson
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Charles E Miller
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Simon A Carn
- Department of Geological and Mining Engineering and Sciences, Michigan Technological University, Houghton, MI 49931, USA
| | - Annmarie Eldering
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Thomas Krings
- Institute of Environmental Physics, University of Bremen, 28334 Bremen, Germany
| | - Kristal R Verhulst
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.,Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles (UCLA), Los Angeles, CA 90095, USA
| | - David S Schimel
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Hai M Nguyen
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - David Crisp
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Christopher W O'Dell
- Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USA
| | - Gregory B Osterman
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
| | - Laura T Iraci
- NASA Ames Research Center, Moffett Field, CA 94035, USA
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