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Statements

Subject Item
dbr:Silica_cycle
rdf:type
owl:Thing
rdfs:label
Silica cycle Cycle du dioxyde de silicium Ciclo del silicio
rdfs:comment
El ciclo del silicio es un ciclo biogeoquímico durante el cual los minerales de silicio se intercambian entre diferentes organismos y la corteza terrestre. El silicio es un bioelemento esencial para algunos seres vivos y uno los elementos más abundantes en la tierra, especialmente en forma de dióxido de silicio o sílice (SiO2). El ciclo del silicio tiene lugar mediante la meteorización de las rocas, la exportación biogénica y el entierro como sedimentos marinos en escalas de tiempo geológicas. Presenta un alto grado de solapamiento con el ciclo del carbono y tiene una función importante en el secuestro de carbono.​​​ Le cycle du dioxyde de silicium est le cycle biogéochimique dans lequel le dioxyde de silicium SiO2 (ou silice) est transféré entre les différents systèmes terrestres. Le silicium est un élément bioessentiel et c'est aussi l'un des éléments les plus abondants sur Terre. Le cycle du dioxyde de silicium a un chevauchement significatif avec le cycle du carbone (cycle carbonate-silicate) et joue un rôle important dans l'enfermement du carbone par le biais de l'altération continentale, de l'exportation biogénique et de l'enfouissement sous forme de limons à l'échelle des temps géologiques. The silica cycle is the biogeochemical cycle in which biogenic silica is transported between the Earth's systems. Silicon is considered a bioessential element and is one of the most abundant elements on Earth. The silica cycle has significant overlap with the carbon cycle (see carbonate–silicate cycle) and plays an important role in the sequestration of carbon through continental weathering, biogenic export and burial as oozes on geologic timescales.
rdfs:seeAlso
dbr:Reverse_weathering
foaf:depiction
n7:Stephanopyxis_grunowii.jpg n7:WOA09_sea-surf_H4SIO4_AYool.png n7:Silica_cycle.jpg n7:Silicon_cycle_and_balance_in_the_modern_world_ocean.png n7:Calocycloma_sp._-_Radiolarian_(32163186535).jpg n7:SiO_H2O.jpg n7:Low-temperature_processes_controlling_silicon_dissolution_in_seawater.png n7:Marine_Silica_Cycle.png
dcterms:subject
dbc:Silicon dbc:Biogeochemical_cycle
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58513265
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1123248662
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dbc:Silicon dbr:Quartz dbr:Phytolith dbr:Surf_zone dbr:Fluvial dbr:Methanogenic dbr:Sponge_spicule dbr:Carbon_sequestration dbr:Residence_time dbr:Phototroph dbr:Photoautotrophic n15:Low-temperature_processes_controlling_silicon_dissolution_in_seawater.png dbr:Hydrologic_cycle dbr:Carbon_cycle dbr:Choanoflagellate dbr:Residence_time_(fluid_dynamics) dbr:Carbonate–silicate_cycle dbr:Wind_wave dbr:Global_carbon_cycle dbr:Siliceous_ooze dbr:Crust_(geology) dbr:River_delta dbr:Phytoplankton dbr:Clay dbr:Carbonate dbr:Biogeochemical_cycle dbr:Silicon_isotopes dbr:Beaches dbr:Rhizarian dbr:Diagenesis dbr:Diatom n15:Silica_cycle.jpg dbr:Meltwater dbr:Pedogenic dbr:Herbivore dbr:Abyssal_zone dbr:Greenhouse_effect dbr:Hydrated dbr:Radiolaria dbr:Atmospheric_carbon_dioxide dbr:Polymorphism_(materials_science) dbr:Interglacial dbr:Oxygen_cycle dbr:Lithogenic_silica dbr:Pelagic_zone dbr:Biogenic_silica dbr:Suspended_solids dbr:Biogeochemistry dbr:Export_production dbr:Continental_margin dbr:Southern_Ocean dbr:Submarine_groundwater_discharge dbr:Sponge dbr:Dissolution_(chemistry) dbr:Climate_change dbr:Sequestration_of_carbon dbr:Enstatite dbr:Biosphere dbr:Δ30Si dbr:Paleoclimatology dbr:Marine_microorganism dbr:Nutrient_cycle dbr:Marine_food_web dbr:Radiolarian dbr:Silicification dbr:Paleoceanography dbr:Weathering dbr:Glacial dbr:Biological_carbon_pump dbr:Opal dbr:Heterotrophic dbr:Orthosilicic_acid n15:Silicon_cycle_and_balance_in_the_modern_world_ocean.png dbr:Proxy_(climate) dbr:Marine_sediments dbr:Undersaturation n15:SiO_H2O.jpg dbr:Isotopic_signature dbr:Chert dbr:Hydrothermal_vent dbr:Abiotic dbr:Silicon_isotope_biogeochemistry dbr:Organic_carbon dbc:Biogeochemical_cycle dbr:Photic_zone dbr:Amorphous_solid dbr:Siliceous_sponge dbr:Silicic_acid dbr:Upper_mantle_(Earth) dbr:Silicoflagellate dbr:Inorganic_carbon dbr:Aeolian_processes dbr:Ocean_sediment dbr:Authigenic dbr:Euphotic_zone dbr:Aeolian_dust dbr:Silicate_minerals
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n12:9K3Sd wikidata:Q60790673 dbpedia-es:Ciclo_del_silicio dbpedia-fr:Cycle_du_dioxyde_de_silicium
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n7:Silicon_cycle_and_balance_in_the_modern_world_ocean.png?width=300
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left
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dbp:footer
Changes in ocean silicic acid can make it difficult for the marine microorganisms that construct silica shells
dbp:footerAlign
center
dbp:image
Stephanopyxis grunowii.jpg Calocycloma sp. - Radiolarian .jpg
dbp:width
170
dbo:abstract
El ciclo del silicio es un ciclo biogeoquímico durante el cual los minerales de silicio se intercambian entre diferentes organismos y la corteza terrestre. El silicio es un bioelemento esencial para algunos seres vivos y uno los elementos más abundantes en la tierra, especialmente en forma de dióxido de silicio o sílice (SiO2). El ciclo del silicio tiene lugar mediante la meteorización de las rocas, la exportación biogénica y el entierro como sedimentos marinos en escalas de tiempo geológicas. Presenta un alto grado de solapamiento con el ciclo del carbono y tiene una función importante en el secuestro de carbono.​​​ The silica cycle is the biogeochemical cycle in which biogenic silica is transported between the Earth's systems. Silicon is considered a bioessential element and is one of the most abundant elements on Earth. The silica cycle has significant overlap with the carbon cycle (see carbonate–silicate cycle) and plays an important role in the sequestration of carbon through continental weathering, biogenic export and burial as oozes on geologic timescales. Le cycle du dioxyde de silicium est le cycle biogéochimique dans lequel le dioxyde de silicium SiO2 (ou silice) est transféré entre les différents systèmes terrestres. Le silicium est un élément bioessentiel et c'est aussi l'un des éléments les plus abondants sur Terre. Le cycle du dioxyde de silicium a un chevauchement significatif avec le cycle du carbone (cycle carbonate-silicate) et joue un rôle important dans l'enfermement du carbone par le biais de l'altération continentale, de l'exportation biogénique et de l'enfouissement sous forme de limons à l'échelle des temps géologiques.
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37748
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