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  • 1
    Publication Date: 2024-01-09
    Keywords: 170-1039B; 170-1039C; 170-1040C; 205-1253A; 205-1254A; Caesium; Costa Rica subduction complex, North Pacific Ocean; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; ICP-MS, Thermo Finnigan, Element 2; Joides Resolution; Leg170; Leg205; North Pacific Ocean; Ocean Drilling Program; ODP; Rubidium; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 98 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-01-09
    Keywords: 205-1253A; 205-1254A; 205-1255A; Barium; Bromine; Caesium; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fluorine; ICP-MS, Thermo Finnigan, Element 2; Ion chromatography; Joides Resolution; Leg205; North Pacific Ocean; Ocean Drilling Program; ODP; Rubidium; Sample code/label; Strontium-87/Strontium-86 ratio; Thermal Ionization Mass Spectrometry (TIMS); δ6Li; δ7Li
    Type: Dataset
    Format: text/tab-separated-values, 124 data points
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Kastner, Miriam; Solomon, Evan A; Wei, Wei; Chan, Lui-Heung; Saether, Ola M (2006): Data report: Chemical and isotopic compositions of pore fluids and sediments from across the Middle America Trench, offshore Costa Rica. In: Morris, JD; Villinger, HW; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 205, 1-21, https://doi.org/10.2973/odp.proc.sr.205.208.2006
    Publication Date: 2024-01-09
    Description: Pore fluid and sediment chemical and isotopic data were obtained for samples from Ocean Drilling Program (ODP) Leg 205 Sites 1253, 1254, and 1255 in the Costa Rica subduction zone. The chemical and isotopic data reported here were generated in our shore-based laboratories to complement shipboard inorganic geochemical data. Li isotopic analyses were carried out by L.-H. Chan at Louisiana State University (USA). The data reported herein include fluoride, bromide, rubidium, cesium, and barium concentrations; Li and Sr isotopic compositions in pore fluids; and Rb, Cs, and Ba concentrations in representative bulk sediments. The data also include new pore fluid fluoride and bromide concentrations from corresponding ODP Leg 170 Sites 1039, 1040, and 1043. O.M. Saether's Site 1039 and 1040 fluoride concentration data are shown for comparison. Basal sediment fluoride concentrations and Li and Sr isotope ratios at both Sites 1253 and 1039 show reversals that approach modern seawater values. Br/Cl ratios are, however, conservative throughout the sediment section at Sites 1039 and 1253. The observed sharp F and Br concentration maxima, Rb and K concentration minima, the most radiogenic 87Sr/86Sr ratios, and highest 7Li values along the décollement and fracture zone (Sites 1040, 1043, 1254, and 1255) strengthen the evidence obtained during Leg 170 that a deeply sourced fluid, originating from fluid-rock reactions at ~150°C and corresponding to between 10 and 15 km depth, is transporting solutes to the ocean.
    Keywords: 170-1039B; 170-1039C; 170-1040C; 205-1253A; 205-1254A; 205-1255A; Costa Rica subduction complex, North Pacific Ocean; DRILL; Drilling/drill rig; Joides Resolution; Leg170; Leg205; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Aquatic geochemistry 4 (1998), S. 253-272 
    ISSN: 1573-1421
    Keywords: Inorganic tracers ; dilution factor ; leachate attenuation ; redox zones ; groundwater
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Groundwater downgradient from Trandum municipallandfill was investigated in summer 1996, with a viewto assessing the distribution of redox-sensitivespecies. The water table at Trandum is 10–26 metersbelow the surface. Monitoring well filters have beeninstalled at depths of up to 15 m below water table,covering an area of 400 m by 200 m. Groundwaterinfluenced by the landfill seems to be confined tothis area. Pristine groundwater has a chemicalsignature indicative of calcite and pyrite weathering.Groundwater influenced by leachate from the landfillexhibits an excess of alkalinity relative to calcium,which is likely to be derived from degradation oforganic matter in the landfill. Groundwaterimmediately below and downstream of the landfillcontains elevated concentrations of Fe and Mn, largelymobilized under reducing conditions from the aquifermatrix and reflected in depleted HNO3-extractable Feand Mn in sediment samples from the same area.Groundwater samples allow the tentative identificationof redox zones based on oxidized and reduced forms ofFe, Mn, N and S. A methanogenic zone is notobserved.
    Type of Medium: Electronic Resource
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