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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Journal of solution chemistry 22 (1993), S. 651-661 
    ISSN: 1572-8927
    Keywords: Optical indicator ; pH ; acid dissociation constant ; acridine ; benzoic acid
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract A new method of measuring the pH of high-temperature aqueous solutions using optical indicators was developed. The absorbance spectrum of acridine changes as a function of pH, allowing its use as an optical indicator for pH. The pKa of acridine were experimentally determined in KOH-AcOH pH-buffer solutions at temperatures from 5 to 250°C at vaporsaturated pressures: $$pKa = 5.62 + 1158{\text{ }}/{\text{ }}T{\text{ - }}0.7168{\text{ }}lnT$$ where T is in Kelvin. The technique is demonstrated by experimentally determining the pKa of benzoic acid at temperatures up to 250°C where the result was $$pKa{\text{ }}(benzoic{\text{ }}acid) = {\text{ - }}60.67 + 3069{\text{ }}/{\text{ }}T{\text{ }} + {\text{ }}9.5542{\text{ }}lnT$$
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
    Publication Date: 2022-05-25
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geochemistry, Geophysics, Geosystems 18 (2017): 1053–1064, doi:10.1002/2016GC006715.
    Description: During International Ocean Discovery Program (IODP) expeditions, shipboard-generated data provide the first insights into the cored sequences. The natural gamma radiation (NGR) of the recovered material, for example, is routinely measured on the ocean drilling research vessel DV JOIDES Resolution. At present, only total NGR counts are readily available as shipboard data, although full NGR spectra (counts as a function of gamma-ray energy level) are produced and archived. These spectra contain unexploited information, as one can estimate the sedimentary contents of potassium (K), thorium (Th), and uranium (U) from the characteristic gamma-ray energies of isotopes in the 40K, 232Th, and 238U radioactive decay series. Dunlea et al. (2013) quantified K, Th, and U contents in sediment from the South Pacific Gyre by integrating counts over specific energy levels of the NGR spectrum. However, the algorithm used in their study is unavailable to the wider scientific community due to commercial proprietary reasons. Here, we present a new MATLAB algorithm for the quantification of NGR spectra that is transparent and accessible to future NGR users. We demonstrate the algorithm's performance by comparing its results to shore-based inductively coupled plasma-mass spectrometry (ICP-MS), inductively coupled plasma-emission spectrometry (ICP-ES), and quantitative wavelength-dispersive X-ray fluorescence (XRF) analyses. Samples for these comparisons come from eleven sites (U1341, U1343, U1366-U1369, U1414, U1428-U1430, and U1463) cored in two oceans during five expeditions. In short, our algorithm rapidly produces detailed high-quality information on sediment properties during IODP expeditions at no extra cost.
    Keywords: IODP ; Physical properties ; Natural gamma radiation ; Downhole logging
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Soyol-Erdene, Tseren-Ochir; Huh, Youngsook (2013): Rare earth element cycling in the pore waters of the Bering Sea Slope (IODP Exp. 323). Chemical Geology, 358, 75-89, https://doi.org/10.1016/j.chemgeo.2013.08.047
    Publication Date: 2023-02-24
    Description: We studied the diagenetic behavior of rare earth elements (REEs) in a highly productive passive margin setting of the Bering Sea Slope. Site U1345 was drilled during the Integrated Ocean Drilling Program Expedition 323 at a water depth of 1008 m currently in the center of an oxygen minimum zone. Pore water concentrations of fourteen REEs were determined down to ~ 140 meters below the seafloor (mbsf). The REE concentrations were higher in the pore water than the deep seawater, indicating that there was significant liberation from the sediments during diagenesis. There was a major peak at ~ 10 mbsf that was more pronounced for the heavy REE (HREE); this peak occurred below the sulfate-methane transition zone (6.3 mbsf) and coincided with high concentrations of dissolved iron and manganese. At ~ 2 mbsf, there was a minor peak in REE and Mn contents. Below ~ 40 mbsf, the REE concentration profiles remained constant. The Ce anomaly was insignificant and relatively constant (PAAS-normalized Ce/Ce = 1.1 ± 0.2) throughout the depth profile, showing that the Ce depleted in seawater was restored in the pore water. HREE-enrichment was observed over the entire 140 m except for the upper ~ 1 m, where a middle REE (MREE)-bulge was apparent. REE release in shallow depths (2-4 mbsf) is attributed to the release of light REEs (LREEs) and MREEs during the organoclastic reduction of Mn oxides in anoxic sediments. The high HREE concentrations observed at ~ 10 mbsf can be attributed to the reduction of Fe and Mn minerals tied to anaerobic oxidation of methane or, less significantly, to ferromagnesian silicate mineral weathering. The upward diffusion flux across the sediment-water interface was between 3 (for Tm) and 290 (for Ce) pmol/m**2/y.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    Publication Date: 2023-06-27
    Keywords: 323-U1345A; Bering Sea Paleoceanography; Cerium; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dysprosium; Erbium; Europium; Exp323; Gadolinium; Holmium; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Lanthanum; Lutetium; Neodymium; Praseodymium; Ratio; Samarium; Terbium; Thulium; Ytterbium; Yttrium
    Type: Dataset
    Format: text/tab-separated-values, 323 data points
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  • 6
    Publication Date: 2023-06-27
    Keywords: 323-U1345B; Bering Sea Paleoceanography; Cerium; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dysprosium; Erbium; Europium; Exp323; Gadolinium; Holmium; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Lanthanum; Lutetium; Neodymium; Praseodymium; Ratio; Samarium; Terbium; Thulium; Ytterbium; Yttrium
    Type: Dataset
    Format: text/tab-separated-values, 1346 data points
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  • 7
    Publication Date: 2023-11-03
    Description: We investigated benthic foraminifera in cores GPC03 and GPC04 in the northeast tropical Indian Ocean (TIO) over the past ~450 ka to evaluate the ballasting effect of particulate organic matter (POM) and the long-term zonal change during the mid-Brunhes dissolution interval (MBDI). Today, interannual climate and oceanographic variability in the TIO is governed by the Indian Ocean Dipole (IOD), which manifests as asymmetric zonal oceanographic change. Here we provide our sediment geochemical, stable oxygen and carbon isotope data and faunal data of benthic foraminifera in core GPC04.
    Keywords: AGE; Aluminium oxide; Bay of Bengal; Benthic foraminifera; Calcium oxide; DEPTH, sediment/rock; HI1808_GPC04; Iron oxide, Fe2O3; Isotope ratio mass spectrometry; Magnesium oxide; Major element; Manganese oxide; Oxygen isotope stratigraphy; Hidden Markov Model (HMM); PC; Phosphorus pentoxide; Piston corer; Potassium oxide; Principal component analyses (PCA); Principal component loading of PC axis 1; Silicon dioxide; Sodium oxide; Stable carbon and oxygen isotopes; Sulfur; Titanium dioxide; Trilobatus sacculifer, δ13C; Trilobatus sacculifer, δ18O; X-ray fluorescence (XRF), discrete measurement
    Type: Dataset
    Format: text/tab-separated-values, 1364 data points
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  • 8
    Publication Date: 2023-11-03
    Description: We investigated benthic foraminifera in cores GPC03 and GPC04 in the northeast tropical Indian Ocean (TIO) over the past ~450 ka to evaluate the ballasting effect of particulate organic matter (POM) and the long-term zonal change during the mid-Brunhes dissolution interval (MBDI). Today, interannual climate and oceanographic variability in the TIO is governed by the Indian Ocean Dipole (IOD), which manifests as asymmetric zonal oceanographic change. Here we provide our sediment geochemical, stable oxygen and carbon isotope data and faunal data of benthic foraminifera in core GPC04.
    Keywords: Ammobaculites sp.; Anomalinoides sp.; Anomalinoides spissiformis; Astrononion echolsi; Bay of Bengal; Benthic foraminifera; Bolivina sp.; Brizalina pacifica; Brizalina seminuda; Brizalina striatula; Bulimina alazanensis; Bulimina striata; Bulimina tenuata; Buliminella exilis; Cassidulina sp.; Cassidulinoides akitaensis; Chilostomella ovoidea; Cibicidina sp.; Cibicidoides bradyi; Cibicidoides mundulus; Cibicidoides renzi; Cibicidoides sp.; Cibicidoides wuellerstorfi; Counting 〉105 µm fraction; Dentalina sp.; DEPTH, sediment/rock; Discorbinella sp.; Eggerella bradyi; Ehrenbergina carinata; Eilohedra levicula; Epistominella exigua; Fissurina spp.; Foraminifera, benthic, total; Foraminifera, benthic agglutinated; Foraminifera, benthic hyaline; Foraminifera, benthic porcelaneous; Fursenkoina bradyi; Fursenkoina sp.; Glandulina sp.; Globobulimina pacifica; Globobulimina sp.; Globocassidulina subglobosa; Glomospira gordialis; Gyroidinoides globosus; Gyroidinoides soldanii; Gyroidinoides sp.; Gyroidinoides subangulatus; Haplophragmoides sp.; Heronallenia sp.; HI1808_GPC04; Hoeglundina elegans; Ionella sp.; Karreriella subglabra; Lagena spp.; Laticarinina pauperata; Lenticulina sp.; Linaresina semicribratus; Major element; Martinottiella communis; Melonis barleeanus; Melonis pompilioides; Miliammina sp.; Nodosaria spp.; Nonion affine; Nonionellina sp.; Nuttallides umbonifer; Oolina hexagona; Oolina melo; Oridorsalis plummerae; Oridorsalis umbonatus; Paracassidulina carinata; Paracassidulina neocarinata; PC; Piston corer; Planulina ariminensis; Pleurostomella sp.; Polymorphina sp.; Pullenia bulloides; Pullenia jarvisi; Pullenia subcarinata; Pyrgo cf. murrhina; Pyrgo murrhina; Pyrolinoides acuminatus; Quinqueloculina akneriana; Quinqueloculina elongata; Quinqueloculina seminulum; Quinqueloculina sp.; Recurvoides sp.; Reophax sp.; Reussella pacifica; Rhabdammina sp.; Siphonaperta sp.; Siphouvigerina ampullacea; Sphaeroidina bulloides; Spirosigmoilina sp.; Spirosigmoilinella sp.; Split; Stable carbon and oxygen isotopes; Stainforthia fusiformis; Stilostomella sp.; Textularia sp.; Tosaia sp.; Triloculina trigonola; Uvigerina dirupta; Uvigerina hispida; Uvigerina peregrina; Uvigerina proboscidea; Valvalabamina depressa; Valvulina sp.; Virgulina sp.
    Type: Dataset
    Format: text/tab-separated-values, 11766 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Wehrmann, Laura Mariana; Risgaard-Petersen, Nils; Schrum, Heather N; Walsh, Emily A; Huh, Youngsook; Ikehara, Minoru; Pierre, Catherine; d'Hondt, Steven L; Ferdelman, Timothy G; Ravelo, Ana Christina; Takahashi, Kozo; Zarikian, Carlos Alvarez (2011): Coupled organic and inorganic carbon cycling in the deep subseafloor sediment of the northeastern Bering Sea Slope (IODP Exp. 323). Chemical Geology, 284(3-4), 251-261, https://doi.org/10.1016/j.chemgeo.2011.03.002
    Publication Date: 2024-01-06
    Description: We studied microbially mediated diagenetic processes driven by carbon mineralization in subseafloor sediment of the northeastern Bering Sea Slope to a depth of 745 meters below seafloor (mbsf). Sites U1343, U1344 and U1345 were drilled during Integrated Ocean Drilling Program (IODP) Expedition 323 at water depths of 1008 to 3172 m. They are situated in the high productivity “Green Belt” region, with organic carbon burial rates typical of the high-productivity upwelling domains on western continental margins. The three sites show strong geochemical similarities. The downward sequence of microbially mediated processes in the sediment encompasses (1) organoclastic sulfate reduction, (2) anaerobic oxidation of methane (AOM) coupled to sulfate reduction, and (3) methanogenesis. The sediment contains two distinct zones of diagenetic carbonate formation, located at the sulfate–methane transition zone (SMTZ) and between 300 and 400 mbsf. The SMTZ at the three sites is located between 6 and 9 mbsf. The upward methane fluxes into the SMTZ are similar to fluxes in SMTZs underlying high-productivity surface waters off Chile and Namibia. Our Bering Sea results show that intense organic carbon mineralization drives high ammonium and dissolved inorganic carbon (DIC) production rates (〉 4.2 mmol/m**3/y1) in the uppermost 10 mbsf and strongly imprints on the stable carbon isotope composition of DIC, driving it to a minimum value of -27 per mil (VPDB) at the SMTZ. Pore-water calcium and magnesium profiles demonstrate formation of diagenetic Mg-rich calcite in the SMTZ. Below the SMTZ, methanogenesis results in 13C-enrichment of pore-water DIC, with a maximum value of +11.9 per mil. The imprint of methanogenesis on the DIC carbon isotope composition is evident down to a depth of 150 mbsf. Below this depth, slow or absent microbially mediated carbon mineralization leaves DIC isotope composition unaffected. Ongoing carbonate formation between 300 and 400 mbsf strongly influences pore-water DIC and magnesium concentration profiles. The linked succession of organic carbon mineralization and carbonate dissolution and precipitation patterns that we observe in the Bering Sea Slope sediment may be representative of passive continental margin settings in high-productivity areas of the world's ocean.
    Keywords: 323-U1343; 323-U1344; 323-U1345; Bering Sea; Bering Sea Paleoceanography; Calculated (Moore et al. 2004); COMPCORE; Composite Core; DEPTH, sediment/rock; Event label; Exp323; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Ion activity product, Log; Joides Resolution; Mass spectrometer Thermo Electron Delta plus IRMS; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 508 data points
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  • 10
    Publication Date: 2024-04-26
    Keywords: Center for Marine Environmental Sciences; File format; File name; File size; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; MARUM; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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