Search results for "Clean water"

showing 10 items of 442 documents

The key role played by the Augusta basin (southern Italy) in the mercury contamination of the Mediterranean Sea.

2011

The Augusta basin, located in SE Sicily (southern Italy), is a semi-enclosed marine area, labelled as a highly contaminated site. The release of mercury into the harbour seawater and its dispersion to the blue water, make the Augusta basin a potential source of anthropogenic pollution for the Mediterranean Sea. A mass balance was implemented to calculate the HgT budget in the Augusta basin. Results suggest that an average of ∼0.073 kmol of HgT is released, by diffusion, on a yearly basis, from sediments to the seawater, with a consequent output of 0.162 kmol y(-1) to coastal and offshore waters; this makes the Augusta area an important contributor of mercury to the Mediterranean Sea. Owing …

010504 meteorology & atmospheric scienceschemistry.chemical_element010501 environmental sciencesManagement Monitoring Policy and LawStructural basin01 natural sciencesMediterranean seaOcean gyreMediterranean SeaWater Pollution ChemicalSeawater14. Life underwater0105 earth and related environmental sciencescomputer.programming_languagegeographygeography.geographical_feature_categoryPublic Health Environmental and Occupational HealthSedimentGeneral MedicineMercury6. Clean waterMercury (element)Settore GEO/08 - Geochimica E VulcanologiaOceanographychemistryHg sediment Augusta basinItaly13. Climate actionHarbourSeawaterSubmarine pipelinecomputerGeologyWater Pollutants ChemicalEnvironmental MonitoringJournal of environmental monitoring : JEM
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Chemical speciation of Fe, Mn, Pb, Zn, Cd, Cu, Co, Ni and Cr in the suspended particulate matter off the Mejerda River Delta (Gulf of Tunis, Tunisia)

2016

International audience; Fluxes of suspended particulate matter (SPM) and their associated metals were performed off the Mejerda River Delta during both the wet (March) and the dry (July) seasons in 2012, using sediment traps at study stations at depths of 10, 20 and 40 m. Fluxes nearest to the Mejerda outlet were more significant, especially during winter (36 g m−2 day−1), but dissipated further offshore, 24.5–6 g m−2 day−1 at the 20 m and 21.8–4.8 g m−2 day−1 at the 40 m stations. Many variations observed in seasonal and spatial metal fluxes are similar to those of SPM, in particular Pb and Zn, probably because they are associated with the mining activity characteristic of the Mejerda catc…

010504 meteorology & atmospheric scienceschemistry.chemical_elementZinc010501 environmental sciences01 natural sciences[ SDE ] Environmental SciencesWater pollution0105 earth and related environmental sciencesEarth-Surface ProcessesHydrologyCadmiumgeographyRiver deltageography.geographical_feature_categoryToxicitySedimentGeologySuspended particulate matterParticulates6. Clean waterchemistryHeavy metals13. Climate actionEnvironmental chemistry[SDE]Environmental SciencesSediment trapSediment trapChemical speciationWater qualityGeology
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Responses of aquatic plants to eutrophication in rivers:a revised conceptual model

2018

Compared to research on eutrophication in lakes, there has been significantly less work carried out on rivers despite the importance of the topic. However, over the last decade, there has been a surge of interest in the response of aquatic plants to eutrophication in rivers. This is an area of applied research and the work has been driven by the widespread nature of the impacts and the significant opportunities for system remediation. A conceptual model has been put forward to describe how aquatic plants respond to eutrophication. Since the model was created, there have been substantial increases in our understanding of a number of the underlying processes. For example, we now know the thre…

010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectReviewPlant Sciencelcsh:Plant culture010501 environmental sciences01 natural sciencesEcology and EnvironmentNutrientAquatic plantlcsh:SB1-1110Applied researchphosphorusmorphotype0105 earth and related environmental sciencesmedia_commonmacrophytebusiness.industrynutrientEnvironmental resource managementBotanyPlant community15. Life on land6. Clean waterManagementMacrophyteeutrophicationHabitat13. Climate actionConceptual modelEnvironmental scienceHydrologyEutrophicationbusiness
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High-frequency climate fluctuations over the last deglaciation in the Alboran Sea, Western Mediterranean: Evidence from calcareous plankton assemblag…

2018

Abstract A high resolution study, with a centennial scale resolution, has been performed on the calcareous plankton assemblage (coccolithophores and planktonic foraminifera) at Ocean Drilling Program Site 976, Alboran Sea (Western Mediterranean), focusing on the interval between 20 and 9 ka, in order to reconstruct changes in surface and subsurface water dynamics and productivity. The biotic surface water proxies integrate the extremely detailed (multi-decadal scale) geochemical data set and the pollen record already available at the core, thus providing a complete paleoenvironmental/paleoceanographic reconstruction. The results highlight the sensitivity of the calcareous plankton in record…

010506 paleontology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOceanography01 natural sciencessapropel Holocene sapropel S1Deglaciation14. Life underwaterStadialGlacial periodYounger DryasMeltwaterEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesPaleontologyWesterliesSettore GEO/01 - Paleontologia E Paleoecologia15. Life on land6. Clean waterOceanography13. Climate actionUpwellingGeology
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A multi-isotope analysis of Neolithic human groups in the Yonne valley, Northern France: insights into dietary patterns and social structure

2019

With the arrival of the Neolithic to Europe, new ways of life and new subsistence strategies emerged. In the Paris Basin (northern France), the appearance of some monumental funerary structures during the Middle Neolithic highlights in particular the increasing complexity of the social organisation. At the same time, several sites, such as open-air cemeteries, do not display any evidence of such arrangement. In the southeast of this area, the two primary routes of neolithisation meet. Several funerary parameters attest to the diverse influence received from other surrounding cultures. In order to assess potential differences in diet, and therefore on purported social distinctions at the int…

010506 paleontologyArcheologyBone collagen060102 archaeologyEcology[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologySubsistence agricultureContext (language use)06 humanities and the artsStructural basinConsumption (sociology)Arqueologia01 natural sciences6. Clean waterGeographyAnthropology0601 history and archaeologyDomesticationComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesTrophic levelIsotope analysis
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The influence of religious identity and socio-economic status on diet over time, an example from medieval France

2019

International audience; In Southern France as in other parts of Europe, significant changes occurred in settlement patterns between the end of Antiquity and the beginning of the Middle Ages. Small communities gathered to form, by the tenth century, villages organized around a church. This development was the result of a new social and agrarian organization. Its impact on lifestyles and, more precisely, on diet is still poorly understood. The analysis of carbon and nitrogen isotopes in bone collagen from the inhabitants of the well-preserved medieval rural site Missignac-Saint Gilles le Vieux (fifth to thirteenth centuries, Gard, France) provides insight into their dietary practices and enab…

010506 paleontologyArcheology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistorymedia_common.quotation_subjectPopulation[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologyDiversification (marketing strategy)01 natural sciencesReligious identity0601 history and archaeologyMiddle AgesArqueologia MetodologiaeducationSocioeconomic status0105 earth and related environmental sciencesmedia_common2. Zero hungereducation.field_of_study060102 archaeology06 humanities and the arts15. Life on land6. Clean waterAgrarian societyGeographyAnthropologyEthnologyTerrestrial ecosystemDiversity (politics)
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Rhinocerotid tooth enamel 18O/16O variability between 23 and 12 Ma in southwestern France.

2006

Abstract The relationship between the oxygen isotope ratio of mammal tooth enamel and that of drinking water was used to reconstruct changes in the Miocene oxygen isotope ratio of rainfall (meteoric water δ 18 O MW ). These, in turn, are related to climatic parameters (temperature, precipitation and evaporation rate). δ 18 O values of rhinocerotid teeth from the Aquitaine Basin (southwestern France) suggest a significant climatic change between 17 and 12 Ma, characterized by cooling together with precipitation increase, in agreement with other terrestrial and oceanic records. To cite this article: I. Bentaleb et al., C. R. Geoscience 338 (2006).

010506 paleontologyGeochemistry010502 geochemistry & geophysicsPalaeoclimate01 natural sciencesIsotopes of oxygenMammal/dk/atira/pure/sustainabledevelopmentgoals/clean_water_and_sanitationPaleontologystomatognathic system[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPaleoclimatologymedicinePrecipitation0105 earth and related environmental sciencesGlobal and Planetary ChangeEnamel paintStable isotope ratioAquitaineMioceneOxygen isotope ratio cycleTooth enamelstomatognathic diseasesmedicine.anatomical_structure13. Climate actionEnamelvisual_artOxygen isotopesMeteoric watervisual_art.visual_art_mediumGeneral Earth and Planetary Sciencessense organs[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologySDG 6 - Clean Water and SanitationGeology
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Facies variations in response to Holocene sea-level and climate change on Bora Bora, French Polynesia: Unravelling the role of synsedimentary siderit…

2017

International audience; Five mixed carbonate-siliciclastic sedimentary facies were identified in the barrier-reef lagoon of Bora Bora using microfacies and statistical analyses of 70 sediment samples taken at high resolution from two vibrocores. Fades and fades successions were interpreted with respect to Holocene sea-level and climate changes. The windward lagoon core is characterized by sideritic marly wackestones and foraminifera-sideritic wackestones, deposited around 7700 years BP (years before present) during the early-mid Holocene transgression. At that time, extensive weathering and erosion of iron-bearing minerals from the volcanic island, due to a wetter climate, were expressed in…

010506 paleontology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaSideritechemistry.chemical_compoundGeochemistry and Petrology14. Life underwaterLithificationReefComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyGeologybiology.organism_classification6. Clean waterOceanographychemistry13. Climate action[SDE]Environmental SciencesSiliciclasticProgradationGeologyMarine transgression
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Applicability and consequences of the integration of alternative models for CO<sub>2</sub> transfer velocity into a process-based lake mo…

2019

Abstract. Freshwater lakes are important in carbon cycling, especially in the boreal zone where many lakes are supersaturated with the greenhouse gas carbon dioxide (CO2) and emit it to the atmosphere, thus ventilating carbon originally fixed by the terrestrial system. The exchange of CO2 between water and the atmosphere is commonly estimated using simple wind-based parameterizations or models of gas transfer velocity (k). More complex surface renewal models, however, have been shown to yield more correct estimates of k in comparison with direct CO2 flux measurements. We incorporated four gas exchange models with different complexity into a vertical process-based physico-biochemical lake mo…

0106 biological sciences010504 meteorology & atmospheric sciences010604 marine biology & hydrobiologyEddy covariancechemistry.chemical_elementAtmospheric sciences01 natural sciences6. Clean waterCarbon cycleAtmospherechemistry.chemical_compoundWater columnchemistryTotal inorganic carbon13. Climate actionGreenhouse gasCarbon dioxideEnvironmental scienceCarbonEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesBiogeosciences
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The stoichiometry of particulate nutrients in Lake Tanganyika — implications for nutrient limitation of phytoplankton

1999

We studied the potential nutrient limitation of phytoplankton by means of seston nutrient stoichiometry and nutrient enrichment bioassays in the epilimnion of Lake Tanganyika. In most cases, the particulate carbon to phosphorus (C:P) ratio was high and indicated moderate P deficiency, while the respective C:N ratio mainly suggested moderate N deficiency. The N:P ratios of seston indicated rather balanced N and P supply. In three two-day enrichment bioassays in April—May 1995, a combined addition of P, N and organic carbon (glucose) always increased primary production in comparison to untreated controls. Primary production also slightly increased after the addition of phosphate-P, while the …

0106 biological sciences010504 meteorology & atmospheric sciencesbiology010604 marine biology & hydrobiologyPhosphorusSestonchemistry.chemical_elementPlanktonbiology.organism_classification01 natural sciences6. Clean waterchemistry.chemical_compoundNutrientAlgaechemistryEnvironmental chemistryEpilimnionBotanyPhytoplanktonAmmonium0105 earth and related environmental sciences
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