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  • 1
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (32 Seiten, 1,50 MB) , Illustrationen
    ISBN: 9783948657000
    Series Statement: IFA-Report 2020, 1
    Parallel Title: Bömer, Thomas Parallele Sprachausgabe Practicable implementation of the requirements concerning safty-related embedded software to DIN EN ISO 13849-1
    Language: German
    Note: Literaturverzeichnis: Seite 25 , Sprache der Zusammenfassungen: Deutsch, Englisch, Französich, Spanisch
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  • 2
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (26 Seiten, 1,48 MB) , Illustrationen
    ISBN: 9783948657000
    Series Statement: IFA-Report 2020, 1e
    Parallel Title: Bömer, Thomas Parallele Sprachausgabe Praxisgerechte Umsetzung der Anforderungen für sicherheitsbezogene Embedded-Software nach DIN EN ISO 13849-1
    Language: English , French , Spanish , German
    Note: Literaturverzeichnis: Seite 21 , Sprache der Zusammenfassungen: Englisch, Französich, Spanisch, Deutsch
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  • 3
    Keywords: Forschungsbericht ; Patientenlagerung ; Höhe ; Technische Sicherheit ; Arbeitsschutz ; Medizintechnische Industrie
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (36 Seiten, 1,24 MB) , Illustrationen, Diagramme
    ISBN: 9783948657529
    Series Statement: IFA-Report 2022, 4
    Language: German , English , French , Spanish
    Note: Literaturangaben , Sprache der Kurzfassungen: Deutsch, Englisch, Französich, Spanisch
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  • 4
    ISSN: 1365-2826
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Corticotropin-releasing factor (CRF-41) is the primary mediator of adrenocorticotropin secretion from the adenohypophysis. This 41-amino-acid peptide is synthesized in perikarya of the paraventricular nuclei, transported to nerve terminals in the external zone of the median eminence and released into the hypophysial-portal circulation. It is also synthesized in multiple extrahypothalamic and peripheral sites. In addition, immunoreactive (ir) CRF-41 is present in the systemic circulation, raising the possibility that systemic measurements might provide a useful index of hypothalamic irCRF-41 secretion. This hypothesis was tested in several rat models. Neither bilateral destruction of hypothalamic irCRF-41 producing perikarya, nor infundibular stalk transection altered peripheral plasma irCRF-41 concentration. Furthermore, central administration of norepinephrine, an agent previously shown to evoke irCRF-41 secretion into the portal circulation, was without effect on peripheral irCRF-41 concentration. Finally, while increased irCRF-41 levels in both the hypophysial-portal and the peripheral circulation were associated with nitroprusside-induced hypotension, bilateral paraventricular nuclei lesions blocked irCRF-41 secretion into the hypophysial-portal circulation without blunting the rise observed in the peripheral circulation. The source of peripheral irCRF-41 remains undetermined; however, the adrenals may be excluded as bilateral adrenalectomy failed to alter circulating irCRF-41 levels. Therefore, our observations do not support the concept that peripheral irCRF-41 levels provide a useful index of hypothalamic secretion of this peptide into the hypophysial-portal circulation under the conditions tested.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-03-14
    Description: This dataset is part of a dataset collection. Please read the documentation in Kiel fjord carbonate chemistry data between 2015 (February) and 2016 (January) doi:10.1594/PANGAEA.876551 for details on sampling, measurement and data processing.
    Keywords: Alkalinity, total; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CO2S; CO2 Sensor; DATE/TIME; DEPTH, water; interpolated; Kiel Fjord; Kiel-Fjord_GEOMAR; pH; Phosphate; Salinity; Silicate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 6
    Publication Date: 2023-01-13
    Description: A HydroC® CO2 sensor was deployed from a pontoon at the waterfront of the GEOMAR west shore building into Kiel Fjord, Western Baltic Sea (Kiel, Germany; 54°19'48.78"N, 010° 8'59.44"E). Since the pontoon is floating the deployment depth of the sensor was constant at 1m. Data of two deployment intervals are published here: February 2015 – May 2015 and August 2015 – January 2016.
    Keywords: CO2S; CO2 Sensor; Kiel Fjord; Kiel-Fjord_GEOMAR
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
    Publication Date: 2023-07-11
    Description: The high surface productivity triggered by nutrient-rich Benguela upwelled waters results in significant enrichment of organic carbon in the sub-surface waters due to enhanced mineralization in the water column and benthic fluxes. Hence, microbial oxygen-consuming processes are promoted, driving oxygen depletion that favours trace gases i.e. methane (CH4) and nitrous oxide (N2O) production at relatively shallow depths. Also, gas-rich subsurface waters are transported towards the surface waters during upwelling, enhancing trace gas sea-air fluxes. Within the EVAR project, we investigate the variability of these fluxes on seasonal and shorter timescales to understand the intensity of the Benguela upwelling system as the source of these greenhouse gases relative to the atmosphere. The data might serve as a base for projections under a changing climate. The fieldwork took place during the cruise SO283 (March 19th – May 25th, 2021) onboard the R/V SONNE from and to Emden (Germany). The main area of the sampling was the Namibian shelf between 18°S and 25°S which is suggested to represent some regional hotspots of trace gas emissions to the atmosphere, in particular in the vicinity of the upwelling cells. Over 260 discrete water samples were collected from the Niskin bottles at different stations for the determination of the concentrations of CH4, N2O, and dissolved inorganic carbon (DIC). 200ml seawater samples were fixed with 200 µL of saturated HgCl2 solution straight after sampling and trace gas was quantified in return. Dissolved CH4 and N2O were measured by an in-house designed purge and trap system with a dynamic headspace method back on land. In brief, a subsample is purged with an inert ultrapure carrier gas of Helium, and the gases are focused on a cryo-trap operated at about -120°C. The volatile compounds are desorbed by rapid heating and analyzed by a gas chromatograph (GC; Agilent 7890B), equipped with capillary columns and a Deans Switch, which directed the components to the flamenionization detector for CH4 detection and electron capture detector ECD for N2O detection. To explore the carbonate system Dissolved Inorganic Carbon (DIC) was measured in the institute. About 5.00 ml of each fixed discrete sample was acidified by 10 % phosphoric acid, resulting in release of inorganic carbon content of the sample. An automated infra-red inorganic carbon analyzer (AIRICA, Marianda, Tulpenweg 28, D-24145 Kiel) equipped with an infrared detector LICOR 7000 (LI-COR Environmental – GmbH, Homburg, Germany) was used to quantify DIC. A 3-fold measurement of the pH was also carried out in 120 ml of discrete samples directly after sampling using the HydroFIA pH system (4H Jena Engineering, 24148 Kiel, Germany). We calculated the average pH value of the corresponding sample after Müller and Rehder (2018) and corresponding total alkalinity and pCO2 after Dickson et al. (2007).
    Keywords: Benguela Upwelling System; Biogeochemical cycle of Trace Gas; Carbon dioxide; CTD/Rosette; CTD-RO; DEPTH, water; EVAR; Event label; LATITUDE; LONGITUDE; Methane; Namibia; Nitrous oxide; oxygen deficient zones; SO283; SO283_28-1; SO283_29-1; SO283_30-1; SO283_31-1; SO283_32-1; SO283_36-1; SO283_37-1; SO283_38-1; SO283_39-1; SO283_43-1; SO283_47-2; SO283_49-1; SO283_50-1; SO283_51-1; SO283_52-1; SO283_53-1; SO283_57-2; SO283_58-2; SO283_59-1; SO283_60-1; SO283_62-1; SO283_64-1; SO283_66-1; SO283_68-1; SO283_69-1; SO283_73-1; SO283_75-1; SO283_77-1; Sonne_2; South Atlantic Ocean; The Benguela Upwelling System under climate change – Effects of VARiability in physical forcing on carbon and oxygen budgets
    Type: Dataset
    Format: text/tab-separated-values, 778 data points
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  • 8
    Publication Date: 2023-08-12
    Description: Upward transport and/or mixing of trace gas-enriched subsurface waters fosters the exchange of nitrous oxide (N2O) and methane (CH4) with the atmosphere in the Eastern-South Atlantic (ESA). To date, it is, however, unclear whether this source is maintained by local production or advection of trace-gas enriched water masses. So, the meridional and zonal variability of N2O and CH4 in the ESA were investigated to constrain the contributions of the major regional water masses to the overall budget of N2O and CH4. The fieldwork took place during the cruises M99 (July 31st - August 23rd, 2013) and M120 (October 17th - November 18th, 2015) onboard the R/V METEOR, which encompassed close-coastal and open ocean regions off Angola and Namibia. To investigate the regional concentration gradients of N2O and CH4 and corresponding sea-air fluxes, seven hydrographic sections (six zonal transects and one alongshore transect) were conducted between ~10°S and 26°S. Concentrations of dissolved N2O and CH4 in surface waters were continuously measured by using the Mobile Equilibrator Sensor System. To evaluate, the oceanic-atmospheric trace gas exchange, the atmospheric N2O and CH4 in ambient air were measured at several sporadic locations, with an inlet installed at 35 m height. The data were quality controlled by comparing with the data generated by NOAA in the nearest atmospheric sampling station (23.58° S, 15.03°E, Station NMB (Gobabeb, Namibia)). Also, to better understand the underlying patterns of the trace gas in the ESA, the vertical profiles were investigated by measuring discrete samples of N2O using the dynamic headspace method on M99. N2O and CH4 concentrations were also measured using a purge and trap system during M120 expedition.
    Keywords: Eastern Boundary Upwelling Syetms; Enhancing Prediction of Tropical Atlantic Climate and its Impact; Methane; nitrous oxide; PREFACE; SACUS/SACUS-II; Southwest African Coastal Upwelling System and Benguela Niños; trace gases
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
    Publication Date: 2024-01-15
    Description: Dissolved Inorganic Carbon (DIC) is one of four parameters measured in order to determine the marine carbonate system. The AIRICA system (Serial No. #027, Marianda, Tulpenweg 28, D-24145 Kiel) works by acidifying (2 acid strokes of 10 % phosphoric acid) a discrete sample amount (2100 µL), generating CO2. The carbon is released out of the water with the help of a carrier gas (99,999 % Nitrogen) that streams through the acidified probe (180 ml min-1). The gas flows through a NAFION dryer and Peltier cooler in order to dry the gas stream. The AIRICA system measures the CO2 concentration by using an infrared detector LICOR 7000 (LI-COR Environmental – GmbH, Siemensstrasse 25A, 61352 Bad Homburg, Germany). Once in the LICOR detector, the CO2 generates a peak, whose area is directly proportional the carbon released, allowing DIC concentration to be calculated when the exact amount of the sample is known. With the help of certified reference materials (Reference material for CO2 measurements, University of California, San Diego, Scripps Institution of Oceanography, Marine Physical Laboratory, 9500 Gilman Drive, La Jolla), previously unnoticed blank impurities can be fixed, leading to more precise measurements and more valuable data. A precision of 1.5-2 µmol kg-1 can be reached. In addition, an average of three repeated measurements is determined, with a maximum deviation of 3 µmol kg-1.
    Keywords: Alkalinity, total; ARA04/2019; ARA04/2019_134; ARA04/2019_135; ARA04/2019_136; ARA04/2019_137; ARA04/2019_138; ARA04/2019_139; ARA04/2019_140; ARA04/2019_141; ARA04/2019_142; ARA04/2019_143; ARA04/2019_144; ARA04/2019_145; ARA04/2019_146; ARA04/2019_147; ARA04/2019_148; ARA04/2019_150; ARA04/2019_151; ARA04/2019_153; ARA04/2019_154; ARA04/2019_155; ARA04/2019_158; ARA04/2019_159; ARA04/2019_161; ARA04/2019_163; ARA04/2019_164; Aranda (1989); Aranda Cruise 2019; Automated Infra Red Inorganic Carbon Analyzer (AIRICA); BI_Keri; BO1; BONUS_INTEGRAL; BONUS INTEGRAL; Bottle number; Carbon, inorganic, dissolved; CT; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Event label; F13; F18; F33; F69; FK2; FK5; I3; Integrated carbon and trace gas monitoring for the Baltic Sea; LATITUDE; LL12; LL7; LONGITUDE; MS10; MS2; MS4; MS6; MS8; RR1; RR3; RR5; Salinity; SR3; SR5; SR7; Station label; US4A; US6B; UTÖ-CTD
    Type: Dataset
    Format: text/tab-separated-values, 478 data points
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  • 10
    Publication Date: 2024-01-15
    Description: Purge and trap system (P&T) with gas chromatograph to analysed methane and nitrous oxide. The in-house designed purge and trap system (P&T) determines methane (CH4) and nitrous oxide (N2O) concentrations in seawater samples by dynamic headspace method. After desorption of volatile compounds with an inert ultrahigh purity carrier gas (Helium 99.999 % and additional preparation by purifier – VICI – Valco Instruments Co. Inc.), the gases were analyzed by a gas chromatograph (GC) (Agilent 7890B), equipped with a flame ionization detector (FID) for CH4 measurements and an electron capture detector (ECD) for N2O measurements. The analytical system consists of four main components: Firstly, the purge chamber (200 x 24 mm), with integrated frit (porosity 2, Erich Eydam KG, Kiel, Germany) to purge the seawater with helium to displaced dissolved gases. Secondly, the trap (stainless steel, 700 mm x 1/8”, U-shaped), filled with HayeSep D (60/80 mesh, CS Chromatographie Service GmbH, Langerwehe, Germany) to enrich the relevant gas compounds. Thirdly, a connected calibration sampling loop for incorporate gas standards. Finally, the GC, which is connected via 10-port-2-pos valve, is used to separate CH4 and N2O with a special column circuit and a Deans-Switch unit, which regulates the carrier gas flow to the FID or ECD. The GC is run isothermally at 45 °C with a helium flow of 3 mL min-1 respectively 6 ml min-1 in column 1 and column 2 (Length 10 m or 30 m, HP-PLOT/Q+PT, Diam. 530 µm, film 40 µm). Column one allows the pre-separation and separation of undesirable compounds and through column two a further separation between CH4 and N2O is realized. In the FID-mode (Deans-Switch regulates the carrier gas flow to the FID) CH4 is detected during the first 5.0 minutes. After 5.8 minutes the GC system switches in the ECD-mode via Deans-Switch and N2O is detected (6.3 min total runtime). The FID works at 250 °C and the ECD at 345 °C. The FID uses Helium and ECD uses 10 % carbon dioxide in nitrogen as make up gas (in each case 25 ml/min). To ensure the measurement's accuracy, calibration standards are measured daily before and after the actual water samples. The calibration range is chosen, so that the samples are within the limits of the calibration methane (CH4) and nitrous oxide (N2O). The standards follow the same time sequence and pathway as the samples. For CH4 and N2O a standard deviation lowers than 1 % is desirable. After successful calibration, the water samples can be measured. The seawater (poisoned with mercury (II) chloride) is stored at 4 °C in 200 ml glass bottles without a headspace. A 100 ml glass syringe (volume calibrated, Fortuna®, Optina®, Poulten & Graf GmbH, Germany) pulls the seawater sample from the glass bottle without creating air bubbles. Around 10 mL of the sample are pushed out of the syringe over valve three into the purge vessel (filled to 1/5). The exact volume of the sample to be measured is calculated with the help of a caliper. The loaded carrier gas passes through a Nafion drying tube (type: MD-050-24S-2092917-06, Ansyco, Karlsruhe, Germany), removing water residues. Then a helium stream (around 100 mL min) transports the water free gases to the cooling trap, where they are capture and concentrated. After 10 minutes of purge time, the trap is placed in a hot water bath (95 °C) and via 10-port-2-pos valve the gas components travel to the GC. At this point in time, the column system is connected to the FID. Methane has a shorter retention time (5.0 min) than N2O, so it is possible to switch after 5.8 min to the ECD-mode to detect N2O (with a 6.3 min retention time). At the end of the measurement day, standards will be remeasured to determine the drift behaviour of the system. In addition, a blank (purged seawater) can be measured, whereby experience shows that the concentration is zero.
    Keywords: ARA04/2019; ARA04/2019_137; ARA04/2019_138; ARA04/2019_139; ARA04/2019_140; ARA04/2019_141; ARA04/2019_142; ARA04/2019_143; ARA04/2019_144; ARA04/2019_145; ARA04/2019_146; ARA04/2019_147; ARA04/2019_148; ARA04/2019_149; ARA04/2019_150; ARA04/2019_153; ARA04/2019_154; ARA04/2019_155; ARA04/2019_157; ARA04/2019_158; ARA04/2019_159; ARA04/2019_163; ARA04/2019_164; Aranda (1989); Aranda Cruise 2019; BO1; BO3; BONUS_INTEGRAL; BONUS INTEGRAL; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Event label; F13; F33; F69; FK2; FK5; I3; Integrated carbon and trace gas monitoring for the Baltic Sea; LATITUDE; LONGITUDE; Methane; Method comment; MS10; MS2; MS4; MS6; MS8; nitrous oxide; Nitrous oxide, dissolved; Oxygen, dissolved; RR1; RR3; RR5; SR3; SR5; SR7; Station label; US4A; US6B; UTÖ-CTD
    Type: Dataset
    Format: text/tab-separated-values, 1216 data points
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