210 Pb as tracer of contaminant transport in a complex canyon-channel system (Gulf of Cagliari, South Sardinia, Western Mediterranean Sea) Barsanti M.

Slides:



Advertisements
Similar presentations
P. Sapienza, Laboratori Nazionali del Sud (INFN)NOW2004, sept A km 3 detector in the Mediterranean: status of NEMO Motivation for a km 3 detector.
Advertisements

17. Radiometric dating and applications to sediment transport William Wilcock OCEAN/ESS 410.
Lecture 3 Trace Elements in Seawater What are trace elements? Why are they important? Principal of Oceanographic Consistency. Profiles shapes as clues.
FOREST FIRE IMPACT ON AIR QUALITY THE LANCON-DE-PROVENCE 2005 CASE S. Strada, C. Mari Laboratoire d'Aérologie, Université de Toulouse, CNRS, Toulouse,
Dating models using man-made radionuclides Part 1: 137 Cs flux, vertical profiles and inventories Roberta Delfanti ENEA –La Spezia, Italy 1 IAEA Regional.
RADINUCLIDES IN THE OCEANS: a tool for understanding the ecosystems functioning Roberta Delfanti ENEA – Marine Environment Research Centre, La Spezia IAEA.
© NERC All rights reserved London’s Soil Chemistry: A continental scale anomaly Dee Flight, Andreas Scheib and the Geochemical Baselines Team British Geological.
Uranium and Thorium Distributions in the Sediments Collected from the Western South Okinawa Trough and the Northern South China Sea Chun-Yen Wang, Li-Wen.
J. Kirk Cochran Marine Sciences Research Center State University of New York Natural and Anthropogenic Radionuclides in Coastal Systems- Examples from.
Trace Metal Analysis of Sediments in the Park River Watershed, Hartford, CT Jonathan Gourley and Victoria Doñé Environmental Science Program Trinity College,
The Interplay between a Mountainous River and Nearby Submarine Canyon in Southern Taiwans Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry,
From John Milliman Fluvial Discharge of Sediments from Taiwan = 380 Mt/yr (Dadson et al., 2003) A prelude 380 Mt/yr  36,000 km 2 = 10,555 ton km -2 yr.
Nepheloid transport vs gravity flows gravity flows and sea level narrow, steep shelves receive much sed different type of gravity flow mass and chemical.
Lecture 3 Trace Metals in Seawater What are trace elements? Why are they important? Principal of Oceanographic Consistency. Profiles shapes as clues for.
Isotopic and Element Characterisation of Potential Sources of Aerosols entering the South Atlantic Ocean Roulin Khondoker The Team Dominik Weiss, Tina.
29 th International conference SEGH, 8-12 July Toulouse, FRANCE 2013 Health risk estimate for groundwater and soil contamination in the.
Cation Exchange Definition: substitution of ions in solution for those held by a mineral grain. Associated with many different types of materials found.
Mercury Accumulation in Alpine Lakes, Colorado David Manthorne, USGS Mark Williams, CU-Boulder.
Gamma spectrometry in deep sea water
1 Pollutants in air, soil, and living organisms Eiliv Steinnes Department of Chemistry Norwegian University of Science and Technology NO-7491 Trondheim.
H41F – 0838: Constructional canyons built by sheet-like turbidity currents: Observations from offshore Brunei Darussalam K.M. Straub, St. Anthony Falls.
Inductively Coupled Plasma-Optical Emission Spectrometry (ICP-OES) Figure 1. The Varian Vista-PRO CCD Simultaneous ICP-OES in the Physical Geography laboratories.
in tin pest and pest free Monika Leodolter-Dvorak and Ilse Steffan
Nuclear Analytical Techniques applied to Element Analysis of the Danube Delta Lacustrine Sediments and Soil L.C. Dinescu Horia Hulubei National Institute.
Biogeochemical Assessment of Shallow Sea Environments (White Sea, Russian Arctic) S. Koukina, G. Korneeva, L. Ametistova and T. Bek P.P. Shirshov Institute.
IAEA International Atomic Energy Agency WG39: Global Trends in Pollution of Coastal Ecosystems: retrospective ecosystem assessment Jae R. OH Marine Environment.
The Rare Earth Elements
Significance Caffeine and ibuprofen may negatively affect plant growth.  Caffeine and ibuprofen generally exist at concentrations below 1 ppm in surface.
Elemental composition of Tibetan Plateau top soils and its effect on evaluating atmospheric pollution transport Chaoliu Li, Shichang Kang, Qianggong Zhang,
Mobility and bioaccessibility of inorganic contaminants in soils in the vicinity of copper smelters (Copperbelt, Zambia) Vojtěch ETTLER 1, Martin MIHALJEVIČ.
BIONAD 18 Month Meeting July 7th, 2015, Inescop Premises, Elda (E) LIFE12 ENV/IT/352 Determination of trace elements in traditional dyes, naturalized dyes.
Lead isotopes in South Atlantic seawater from the UK GEOTRACES transect along 40°S Maxence Paul Mark Rehkämper, Tina van de Flierdt, Dominik Weiss.
Case study: 137 Cs as tracer for sedimentation processes in an Italian coastal area Roberta Delfanti, ENEA - La Spezia, Italy IAEA Regional Training Course.
Surface Area/Grain Size Relations Figure , page 31; Horowitz, A.J., A Primer on Sediment Trace Element Chemistry, 2 nd edition, Lewis Publishers,
Sediments Toxicity of the rivers draining Ibadan Metropolis Southwestern, Nigeria. 1 Ajibade, O.M and 2 Abimbola, A.F. 1 Department of Earth Sciences,
Cation Exchange Definition: substitution of ions in solution for those held by a mineral grain. Associated with many different types of materials found.
Is There a Link Between Epizootic Lobster Shell Disease and Contaminants? Lawrence A. LeBlanc 1, L. Brian Perkins, and Deanna Prince 1 1 School of Marine.
Simon H. 1,. , Kelemen Sz. 1, Gabor A. -I. 1,2, Preoteasa L. 3, Begy R
Catherine Jeandel, Marseille 2004: Geochemistry in KEOPS Chlorophyll (mg m -3 ) Among the objectives of KEOPS - Identification of the mechanisms of natural.
“To predict the future of coastal areas is necesary to know how was it in past”
CHARACTERIZATION OF NATURAL AND ENGINEERED NANOPARTICLES: SHAPE, SIZE AND CHEMICAL COMPOSITION Lucia Manangon
M.Shirchenko, JINR KIAE detectors test & restoration 1. Restoration of the detectors 2. Characterization of KIAE detectors 3. Next steps and.
Physical and Chemical characterization of the aerosol during the cruise Guieu/Losno/Bonnet/Blain/Gaudichet 1) Scientific objectives:  Determine the particles.
2007 INTEX Data Meeting The Vertical Distribution of HCl over the Pacific during INTEX-B Saewung Kim, Bob Stickel, Greg Huey, Melody Avery, Jack Dibb,
LIFE12 ENV/IT/352 Determination of trace elements in commercial dyes, crude chromophore, purified dyes and naturalized dyes Alessandro D’Ulivo BIONAD 24.
Controls on sediment availability on the continental shelf and implications for rates of morphologic evolution Patricia Wiberg University of Virginia with.
1 A&WMA 25 June,  The Aral Sea is the third largest source of mineral dust in Asia.  Human health effects are associated with atmospheric particulate.
Associate Prof. Meral TOPCU SULAK
TRACE METAL AND DIOXIN DEPOSITION HISTORY IN HURRICANE KATRINA IMPACTED MARSH SEDIMENT Gopal Bera* and Alan Shiller (The University of Southern Mississippi,
Dr. Claudia Benitez-Nelson University of South Carolina Radionuclides in Ocean: A General Introduction to Marine Radioactivity.
Possible transportation routes of heavy metals in floodplains
Progress in 2017 Work-plan elements
Predicting Hotspots for Heavy Metal Contamination in Bumpus Cove, TN Melissa A. Magno, Arpita Nandi, and Ingrid Luffman, Department of Geosciences, East.
TRACE METALS IN SOFT TISSUE OF MARINE BIVALVE NOAH’S ARK (Arca noae) FROM BIZERTE LAGOON (NORTHERN TUNISIA) F. Ghribi *, J. Richir , D. Boussoufa ,
PIXE measurements of heavy metals of Tsunami sediment samples
REGIONAL GEOCHEMICAL MAPPING OF TOPSOIL HEAVY METALS: A SCORPAN KRIGING APPROACH CONDITIONAL ON SOIL MAP DELINEATIONS AND LAND USE F. Ungaro 1 N. Marchi.
By Reid Brown and Rio Diniakos
Elemental analysis of glass by laser ablation inductively coupled plasma optical emission spectrometry (LA-ICP-OES)  Emily R. Schenk, José R. Almirall 
RADINUCLIDES IN THE OCEANS:
Table 1: Laser Ablation parameter
UK GEOTRACES 40° S Atlantic Ocean Water column Biogeochemistry
Atomic emission spectrometry
(Hautes-Fagnes, Belgium) during the Industrial Revolution
Managing New Zealand lakes: Theodore Alfred Kpodonu
Shallow -water sediments: Early diagenesis in sandy sediments
Speed Dating Speed Dating H Na Speed Dating Speed Dating K Be.
Airborne Contaminants from Mining Operations In Arizona
POPs and HMs Summary , EMEP TFMM.
10th TFMM meeting, June, 2009, France, Paris
Victoria Schoenwald Undergraduate Program
Presentation transcript:

210 Pb as tracer of contaminant transport in a complex canyon-channel system (Gulf of Cagliari, South Sardinia, Western Mediterranean Sea) Barsanti M. 1, Delbono I. 1, Schirone A. 1, Conte F. 1, Delfanti R. 1, Del Core M. 2, Tamburrino S. 2, Sprovieri M. 2 1 ENEA, Marine Environment Research Centre, La Spezia, Italy 2 CNR, IAMC UOS Capo Granitola, Campobello di Mazara (TP), Italy

Study area Sarroch Gulf of Cagliari (Sardinia, IT) Many submarine canyons Continental shelf ~ 15 km wide StationWater depth (m) Location A2TM625S. Elia–Foxy Canyon A3TM636Sarroch Canyon A4TM907Carbonara Canyon A6TM787Pula Canyon

Methods 0.5 cm 1 cm Box-corer Sub-cores with PVC tubes (10cm Ø) Sub-cores sliced on board (0.5cm in the top 3 cm and 1cm thereafter) 210 Pb and 137 Cs -> Gamma spectrometry with four high resolution ORTEC HPGe Trace elements -> Inductively coupled plasma optical emission spectrometry (ICP-OES; iCAP 6000)

625 m depth 210 Pb and 137 Cs profiles Sarroch CF-CS 0.24±0.01 g cm -2 y ± 0.01 cm y ± ± 2

636 m depth Sarroch CF-CS 0.18 ± 0.01 g cm -2 y ± 0.02 cm y ± Pb and 137 Cs profiles 1956 ± 5 C ostant R ate S upply

907 m depth Sarroch 210 Pb and 137 Cs profiles 210 Pb xs

787 m depth Sarroch 210 Pb and 137 Cs profiles

Grain size composition A2TM A3TM

Grain size composition A6TM A4TM

210 Pb and 137 Cs profiles normalised to clay fraction A6TM

Al-normalised trace elements vs depth A2TM A3TM A4TM Ni, Pb, Cr, V, Zn and Hg Co, Ni, Pb, Cr, V, Zn and Hg Pb, Cr, V, Zn and Hg As and Pb Pb, Cr and Zn As and Hg Pb, Cr, V and Hg Hg V and Hg Pb and Hg Ni, Pb, Cr, V, Zn and Hg A6TM

Al-normalised trace elements vs time A2TMA3TM

Enrichment Factor – (EF Al ) vs time A2TM A3TM Identified and selected the TE values before the '20s along A2TM and A3TM cores as geochemical natural background to calculate the Enrichment Factor.

Conclusions Four sediment cores were collected in 2014 from the Gulf of Cagliari in the thalwegs of submarine canyons (depth range m). 210 Pb and 137 Cs dating for A2TM and A3TM cores provides the pollution history of the most populated and industrialised area of Sardinia. Regional natural background levels for trace elements are defined for the first time: Pb = 25 mg/kg, As = 13 mg/kg, Hg = 0,03 mg/kg. Highest Enrichment Factors values were observed for Pb, As and Hg with an increasing trend starting from the 1970s for the A3TM core and from the 1940s for the A2TM core, pointing out a significant anthropogenic input.