{ "processes":[ { "id":"solwcad", "version":"1.0.1", "jobControlOptions":[ "sync-execute", "async-execute" ], "outputTransmission":[ "value" ], "links":[ { "href":"https://civ.pi.ingv.it/project/solwcad/", "rel":"about", "type":"text/html", "hreflang":"en-US", "title":"SOLWCAD | Computational Infrastructure for Volcanology" }, { "href":"https://www.pi.ingv.it/progetti/eurovolc/#solwcad", "rel":"alternate", "type":"text/html", "hreflang":"en-US", "title":"EUROVOLC: Volcano Dynamics Computational Centre" }, { "href":"https://www.sciencedirect.com/science/article/pii/S0009254106000532?via%3Dihub", "rel":"describedby", "type":"text/html", "hreflang":"en-US", "title":"The compositional dependence of the saturation surface of H2O + CO2 fluids in silicate melts" }, { "type":"application/json", "rel":"self", "href":"https://voice.pi.ingv.it/geoinquire/processes/solwcad?f=json", "title":"Process description as JSON", "hreflang":"it-IT" }, { "type":"text/html", "rel":"alternate", "href":"https://voice.pi.ingv.it/geoinquire/processes/solwcad?f=html", "title":"Process description as HTML", "hreflang":"it-IT" }, { "type":"text/html", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=html", "title":"Jobs list as HTML", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=json", "title":"Jobs list as JSON", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/execute", "href":"https://voice.pi.ingv.it/geoinquire/processes/solwcad/execution?f=json", "title":"Execution for this process as JSON", "hreflang":"it-IT" } ], "title":"SOLWCAD", "description":"Fortran code to compute the saturation surface of H2O-CO2 fluids in silicate melts of arbitrary composition.", "keywords":[ "Fortran code", "saturation surface", "other keywords..." ], "examples":[ { "payload_example":{ "inputs":{ "swinput.data":{ "value":{ "ndat1":1, "ndat2":2, "kl":0 } }, "sw.data":[ [ "1.00d8", "1273.", ".0400", ".0200", ".7653", ".0032", ".1201", ".0027", ".0246", ".0006", ".0018", ".0132", ".0378", ".0306" ], [ "2.00d8", "1173.", ".0200", ".0010", ".7053", ".0032", ".1301", ".0027", ".0146", ".0006", ".0118", ".0232", ".0378", ".0306" ] ] }, "outputs":{ "solwcad_out":{ "format":{ "mediaType":"text/plain" } } } } }, { "curl_example":"curl -i -k -L -X POST \"https://voice.pi.ingv.it/geoinquire/processes/solwcad/execution\" -H \"Content-Type: application/json\" -d '{ \"inputs\":{\"swinput.data\":{\"value\":{\"ndat1\":1,\"ndat2\":2,\"kl\":0}},\"sw.data\":[[\"1.00d8\",\"1273.\",\".0400\",\".0200\",\".7653\",\".0032\",\".1201\",\".0027\",\".0246\",\".0006\",\".0018\",\".0132\",\".0378\",\".0306\"],[\"2.00d8\",\"1173.\",\".0200\",\".0010\",\".7053\",\".0032\",\".1301\",\".0027\",\".0146\",\".0006\",\".0118\",\".0232\",\".0378\",\".0306\"]]}, \"outputs\":{\"solwcad_out\":{\"format\":{\"mediaType\":\"text/plain\"}}}}'" }, { "curl_jobStatus_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>\"" }, { "curl_jobResults_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>/results?f=json\"" } ] }, { "$defs":{ "chart":{ "type":"object", "required":[ "chartType", "domain", "series" ], "properties":{ "chartType":{ "type":"string" }, "domain":{ "type":"object", "properties":{ "key":{ "type":"string" }, "label":{ "type":"string" }, "unit":{ "type":"string" }, "values":{ "type":"array", "items":{ "type":"number" } } }, "required":[ "key", "label", "values" ] }, "series":{ "type":"array", "items":{ "type":"object", "properties":{ "key":{ "type":"string" }, "label":{ "type":"string" }, "unit":{ "type":"string" }, "values":{ "type":"array", "items":{ "type":"number" } } }, "required":[ "key", "values" ] } } } } }, "id":"conduit", "version":"2.2.1", "jobControlOptions":[ "sync-execute", "async-execute" ], "outputTransmission":[ "value" ], "links":[ { "href":"https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2000JB900428", "rel":"describedby", "type":"application/pdf", "hreflang":"en-US", "title":"Dynamics of magma flow in volcanic conduits with variable fragmentation efficiency and nonequilibrium pumice degassing" }, { "href":"https://www.nature.com/articles/17109", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Strain-induced magma fragmentation in explosive eruptions" }, { "href":"https://doi.org/10.1002/2016JB013383", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Non-Newtonian flow of bubbly magma in volcanic conduits" }, { "href":"https://doi.org/10.3389/feart.2021.681083", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Deep Magma Transport Control on the Size and Evolution of Explosive Volcanic Eruptions" }, { "href":"https://doi.org/10.1016/S0377-0273(02)00381-5", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Coupled conduit and atmospheric dispersal dynamics of the AD 79 Plinian eruption of Vesuvius" }, { "href":"https://link.springer.com/article/10.1007/s004450000123", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Textural heterogeneities in pumices from the climactic eruption of Mount Pinatubo, 15 June 1991, and implications for magma ascent dynamics" }, { "href":"https://doi.org/10.1130/G25402A.1", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Origin of basalt fire-fountain eruptions on Earth versus the Moon" }, { "href":"https://doi.org/10.5194/se-1-61-2010", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Rheological control on the dynamics of explosive activity in the 2000 summit eruption of Mt. Etna" }, { "href":"https://doi.org/10.1016/S0377-0273(03)00319-6", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Dynamics of magma ascent and fragmentation in trachytic versus rhyolitic eruptions" }, { "href":"https://doi.org/10.1016/j.jvolgeores.2008.05.012", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Vent conditions for expected eruptions at Vesuvius" }, { "href":"https://doi.org/10.1016/j.chemgeo.2006.06.007", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"The effect of H2O on the viscosity of K-trachytic melts at magmatic temperatures" }, { "href":"https://doi.org/10.1016/S0377-0273(98)00101-2", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"The role of magma composition and water content in explosive eruptions: 1. Conduit ascent dynamics" }, { "href":"https://doi.org/10.1029/93JB02972", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Magma flow along the volcanic conduit during the Plinian and pyroclastic flow phases of the May 18, 1980, Mount St. Helens eruption" }, { "href":"https://doi.org/10.1016/0377-0273(93)90104-Y", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Modeling of the ascent of magma during the plinian eruption of Vesuvius in A.D. 79" }, { "href":"https://link.springer.com/article/10.1007/s004450050253", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Role of carbon dioxide in the dynamics of magma ascent in explosive eruptions" }, { "href":"https://doi.org/10.1016/S1464-1895(99)00142-8", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Numerical simulations of magma ascent along volcanic conduits" }, { "href":"https://doi.org/10.1016/S1464-1895(99)00144-1", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"The role of water content and magma composition on explosive eruption dynamics" }, { "href":"https://doi.org/10.1016/0012-821X(94)90037-X", "rel":"related", "type":"application/pdf", "hreflang":"en-US", "title":"Erosion processes in volcanic conduits and application to the AD 79 eruption of Vesuvius" }, { "type":"application/json", "rel":"self", "href":"https://voice.pi.ingv.it/geoinquire/processes/conduit?f=json", "title":"Process description as JSON", "hreflang":"it-IT" }, { "type":"text/html", "rel":"alternate", "href":"https://voice.pi.ingv.it/geoinquire/processes/conduit?f=html", "title":"Process description as HTML", "hreflang":"it-IT" }, { "type":"text/html", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=html", "title":"Jobs list as HTML", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=json", "title":"Jobs list as JSON", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/execute", "href":"https://voice.pi.ingv.it/geoinquire/processes/conduit/execution?f=json", "title":"Execution for this process as JSON", "hreflang":"it-IT" } ], "title":"CONDUIT", "description":"CONDUIT4 is a Fortran code for computing the one-dimensional, steady, isothermal, multiphase and multicomponent flow of magma in volcanic conduits. The code solves the compressible mass balance and momentum balance equations separately for a gas phase and a dense phase constituted by liquid+crystals (below fragmentation), or by pyroclasts (above fragmentation). A user-defined fragmentation efficiency parameter describes the relative amounts of non-vesicular ash, vesicular pumice, and free crystals generated at fragmentation; while another user-defined parameter describes pumice degassing disequilibrium. The model takes either choked flow or atmospheric pressure conditions at the conduit exit, with the alternative being part of the solution thus depending on the selected conditions. The numerical algorithm searches for such an exit condition by adapting the mass flow-rate to the selected conduit diameter. Thermodynamic equilibrium phase between the gas (H2O+CO2) and the silicate melt is calculated through the SOLWCAD model (Papale et al., 2006, [Chemical Geology, 229(1-3), 78-95]), implemented within CONDUIT4. Magma fragmentation is determined based on Maxwell's theory for visco-elastic materials, as described in Papale (1999) [Nature, 397(6718), 425-428]. The viscosity of the liquid is calculated according to Giordano et al. (2008) [Earth and Planetary Science Letters, 271.1-4: 123-134], and the effect of crystals on viscosity is based on the model of Costa et al. (2009) [Geochemistry, Geophysics, Geosystems, 10(3)]. The transport and constitutive equations, as well as the numerical approach, are detailed in Papale (2001) [Journal of Geophysical Research: Solid Earth, 106(B6), 11043-11065].", "keywords":[ "Fortran code", "conduit flow" ], "examples":[ { "payload_example":{ "inputs":{ "melt_composition":{ "value":{ "sio2":0.7669, "tio2":0.0012, "al2o3":0.1322, "fe2o3":0.0039, "feo":0.0038, "mno":0.0007, "mgo":0.0006, "cao":0.008, "na2o":0.03, "k2o":0.0512 } }, "volatiles":{ "value":{ "h2o":0.05, "co2":0.02 } }, "crystals":{ "value":{ "c":0.1, "den":2800.0 } }, "fragmentation":{ "value":{ "fe":0.2, "pd":0.9, "dp":0.0002, "ds":0.0002, "dc":0.0002 } }, "pressure_temperature":{ "value":{ "p":100000000.0, "t":1050.0 } }, "geometry":{ "value":{ "g":"conduit", "l":4000.0 } }, "searching_mode":{ "value":{ "f":88393000.0 } } }, "outputs":{ "gas":{ "transmissionMode":"value" }, "velocity":{ "transmissionMode":"value" } } } }, { "curl_example":"curl -i -k -L -X POST \"https://voice.pi.ingv.it/geoinquire/processes/conduit/execution\" -H \"Content-Type: application/json\" -d '{\"inputs\": {\"melt_composition\": {\"value\": {\"sio2\": 0.7669, \"tio2\": 0.0012, \"al2o3\": 0.1322, \"fe2o3\": 0.0039, \"feo\": 0.0038, \"mno\": 0.0007, \"mgo\": 0.0006, \"cao\": 0.0080, \"na2o\": 0.0300, \"k2o\": 0.0512} }, \"volatiles\": {\"value\": {\"h2o\": 0.0500e0, \"co2\": 0.0200e0} }, \"crystals\": {\"value\": {\"c\": 0.1, \"den\": 2800.0e0} }, \"fragmentation\": {\"value\": {\"fe\": 0.2, \"pd\": 0.9, \"dp\": 200e-6, \"ds\": 200e-6,\"dc\": 200e-6} }, \"pressure_temperature\": {\"value\": {\"p\": 1.0e8, \"t\": 1050.0e0} }, \"geometry\": {\"value\": {\"g\": \"conduit\", \"l\": 4000.0e0} }, \"searching_mode\": {\"value\": {\"f\": 0.88393e8} } },\"outputs\": {\"gas\": {}, \"velocity\": {} } }'" }, { "curl_example_alsoByReference":"curl -i -k -L -X POST \"https://voice.pi.ingv.it/geoinquire/processes/conduit/execution\" -H \"Content-Type: application/json\" -d '{\"inputs\": {\"melt_composition\": {\"value\": {\"sio2\": 0.7669, \"tio2\": 0.0012, \"al2o3\": 0.1322, \"fe2o3\": 0.0039, \"feo\": 0.0038, \"mno\": 0.0007, \"mgo\": 0.0006, \"cao\": 0.0080, \"na2o\": 0.0300, \"k2o\": 0.0512} }, \"volatiles\": {\"value\": {\"h2o\": 0.0500e0, \"co2\": 0.0200e0} }, \"crystals\": {\"value\": {\"c\": 0.1, \"den\": 2800.0e0} }, \"fragmentation\": {\"value\": {\"fe\": 0.2, \"pd\": 0.9, \"dp\": 200e-6, \"ds\": 200e-6,\"dc\": 200e-6} }, \"pressure_temperature\": {\"value\": {\"p\": 1.0e8, \"t\": 1050.0e0} }, \"geometry\": {\"value\": {\"g\": \"conduit\", \"l\": 4000.0e0} }, \"searching_mode\": {\"value\": {\"f\": 0.88393e8} } },\"outputs\":{\"gas\":{\"transmissionMode\": \"reference\"}, \"velocity\":{\"transmissionMode\": \"value\"}}}'" }, { "curl_jobStatus_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>\"" }, { "curl_jobResults_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>/results\\?f=json\"" } ] }, { "$defs":{ "chart":{ "type":"object", "required":[ "chartType", "domain", "series" ], "properties":{ "chartType":{ "type":"string" }, "domain":{ "type":"object", "properties":{ "key":{ "type":"string" }, "label":{ "type":"string" }, "unit":{ "type":"string" }, "values":{ "type":"array", "items":{ "type":"number" } } }, "required":[ "key", "label", "values" ] }, "series":{ "type":"array", "items":{ "type":"object", "properties":{ "key":{ "type":"string" }, "label":{ "type":"string" }, "unit":{ "type":"string" }, "values":{ "type":"array", "items":{ "type":"number" } } }, "required":[ "key", "values" ] } } } } }, "id":"pybox", "version":"1.1.0", "jobControlOptions":[ "sync-execute", "async-execute" ], "outputTransmission":[ "value" ], "links":[ { "href":"https://civ.pi.ingv.it/project/pybox-2/", "rel":"related", "type":"text/html", "title":"CIV repository" }, { "href":"https://doi.org/10.5281/zenodo.2616551", "rel":"describedby", "type":"application/pdf", "hreflang":"en-US", "title":"PyBox: a Python tool for simulating the kinematics of Pyroclastic density currents with the box-model approach, Reference and User's Guide" }, { "href":"http://dx.doi.org/10.1016/j.jvolgeores.2016.08.002", "rel":"describedby", "type":"text/html", "hreflang":"en-US", "title":"A fast, calibrated model for pyroclastic density currents kinematics and hazard" }, { "href":"https://doi.org/10.5281/zenodo.18920969", "rel":"cite-as", "type":"text/html", "title":"PyBOX-Web release on Zenodo (DOI: 10.5281/zenodo.18920969)" }, { "href":"https://github.com/silviagians/PyBOX-Web", "rel":"source", "type":"text/html", "title":"PyBOX-Web source code repository on GitHub" }, { "type":"application/json", "rel":"self", "href":"https://voice.pi.ingv.it/geoinquire/processes/pybox?f=json", "title":"Process description as JSON", "hreflang":"it-IT" }, { "type":"text/html", "rel":"alternate", "href":"https://voice.pi.ingv.it/geoinquire/processes/pybox?f=html", "title":"Process description as HTML", "hreflang":"it-IT" }, { "type":"text/html", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=html", "title":"Jobs list as HTML", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/job-list", "href":"https://voice.pi.ingv.it/geoinquire/jobs?f=json", "title":"Jobs list as JSON", "hreflang":"it-IT" }, { "type":"application/json", "rel":"http://www.opengis.net/def/rel/ogc/1.0/execute", "href":"https://voice.pi.ingv.it/geoinquire/processes/pybox/execution?f=json", "title":"Execution for this process as JSON", "hreflang":"it-IT" } ], "title":"PYBOX", "description":"PyBOX is a Python software for simulating the propagation of gravity-driven pyroclastic density currents (PDCs) using a box-model approach. It predicts two-dimensional inundation areas using the energy-conoid method and topography derived from the Copernicus GLO-30 Digital Elevation Model (DEM), a DSM-product. Simulations support multiple particle-size classes", "keywords":[ "Python code", "Box model", "Pyroclastic density currents", "Invasion maps", "Hazard assessment" ], "metadata":[ { "title":"Source repository", "role":"repository", "href":"https://github.com/silviagians/PyBOX-Web" }, { "title":"Silvia Giansante", "role":"author", "href":"https://orcid.org/0009-0008-2803-0873" } ], "examples":[ { "payload_example":{ "inputs":{ "lon":14.428, "lat":40.82, "l0":150, "h0":150, "theta0":500, "multiple_values":[ { "eps0":0.01, "rhos":1000, "ds":0.0001 } ], "dt":0.5, "margin":5000 }, "outputs":{ "input_data":{}, "dem":{}, "invasion_map":{}, "spatial_evolution":{}, "deposit_thickness":{} } } }, { "curl_request_example":"curl -k -L -X POST \"https://voice.pi.ingv.it/geoinquire/processes/pybox/execution\" -H \"Content-Type: application/json\" -d '{\"inputs\":{\"lon\":14.428,\"lat\":40.820,\"l0\":150,\"h0\":150,\"theta0\":500,\"multiple_values\":[{\"eps0\":0.01,\"rhos\":1000,\"ds\":0.0001}],\"dt\":0.5,\"margin\":5000},\"outputs\":{\"dem\":{\"transmissionMode\": \"reference\"},\"spatial_evolution\":{\"transmissionMode\": \"value\"}}}'" }, { "curl_request_with_qualified_example__href-only_not_supported_yet":"curl -k -L -X POST \"https://voice.pi.ingv.it/geoinquire/processes/pybox/execution\" -H \"Content-Type: application/json\" -d '{\"inputs\":{\"lon\":{\"value\":14.428},\"lat\":{\"value\":40.820},\"l0\":150,\"h0\":150,\"theta0\":500,\"multiple_values\":[{\"eps0\":0.01,\"rhos\":1000,\"ds\":0.0001}],\"dt\":0.5,\"margin\":5000},\"outputs\":{\"dem\":{\"transmissionMode\": \"reference\"},\"spatial_evolution\":{\"transmissionMode\": \"value\"}}}'" }, { "curl_jobStatus_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>\"" }, { "curl_jobResults_request":"curl -k -L \"https://voice.pi.ingv.it/geoinquire/jobs/<jobID>/results\"?f=json" } ] } ], "links":[ { "type":"application/json", "rel":"self", "title":"This document as JSON", "href":"https://voice.pi.ingv.it/geoinquire/processes?f=json" }, { "type":"application/ld+json", "rel":"alternate", "title":"This document as RDF (JSON-LD)", "href":"https://voice.pi.ingv.it/geoinquire/processes?f=jsonld" }, { "type":"text/html", "rel":"alternate", "title":"This document as HTML", "href":"https://voice.pi.ingv.it/geoinquire/processes?f=html" } ] }