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  • 2015-2019  (1,530,446)
  • 1980-1984  (12)
  • 2016  (787,937)
  • 2015  (742,532)
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  • 1
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    Unknown
    PANGAEA
    In:  Department of Physical Geography, University of Stockholm | Supplement to: Siewert, Matthias Benjamin; Hugelius, Gustaf; Heim, Birgit; Faucherre, Samuel (2016): Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta. CATENA, 147, 725-741, https://doi.org/10.1016/j.catena.2016.07.048
    Publication Date: 2024-06-19
    Description: To project the future development of the soil organic carbon (SOC) storage in permafrost environments, the spatial and vertical distribution of key soil properties and their landscape controls needs to be understood. This article reports findings from the Arctic Lena River Delta where we sampled 50 soil pedons. These were classified according to the U.S.D.A. Soil Taxonomy and fall mostly into the Gelisol soil order used for permafrost-affected soils. Soil profiles have been sampled for the active layer (mean depth 58 ± 10 cm) and the upper permafrost to one meter depth. We analyze SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, visible ice and water content. These are compared for different landscape groupings of pedons according to geomorphology, soil and land cover and for different vertical depth increments. High vertical resolution plots are used to understand soil development. These show that SOC storage can be highly variable with depth. We recommend the treatment of permafrost-affected soils according to subdivisions into: the surface organic layer, mineral subsoil in the active layer, organic enriched cryoturbated or buried horizons and the mineral subsoil in the permafrost. The major geomorphological units of a subregion of the Lena River Delta were mapped with a land form classification using a data-fusion approach of optical satellite imagery and digital elevation data to upscale SOC storage. Landscape mean SOC storage is estimated to 19.2 ± 2.0 kg C/m**2. Our results show that the geomorphological setting explains more soil variability than soil taxonomy classes or vegetation cover. The soils from the oldest, Pleistocene aged, unit of the delta store the highest amount of SOC per m2 followed by the Holocene river terrace. The Pleistocene terrace affected by thermal-degradation, the recent floodplain and bare alluvial sediments store considerably less SOC in descending order.
    Keywords: Changing Permafrost in the Arctic and its Global Effects in the 21st Century; PAGE21
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-19
    Keywords: ARK-XXVIII/2; AWI_GeoPhy; CT; DATE/TIME; DS3; LATITUDE; LONGITUDE; Marine Geophysics @ AWI; Polarstern; PS85; PS85-track; Swath-mapping system Atlas Hydrosweep DS-3; Underway cruise track measurements; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 67 data points
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  • 3
    Publication Date: 2024-06-19
    Keywords: ANT-XXXI/2 FROSN; AWI_GeoPhy; CT; DATE/TIME; DS3; LATITUDE; LONGITUDE; Marine Geophysics @ AWI; Polarstern; PS96; PS96-track; Swath-mapping system Atlas Hydrosweep DS-3; Underway cruise track measurements; Uniform resource locator/link to file; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 177 data points
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  • 4
    Publication Date: 2024-06-19
    Keywords: Aluminium oxide; Aluminium oxide, standard deviation; Calcium oxide; Calcium oxide, standard deviation; Chlorine; Chlorine, standard deviation; DEPTH, sediment/rock; Iron oxide, Fe2O3; Iron oxide, Fe2O3, standard deviation; Lithologic unit/sequence; Magnesium oxide; Magnesium oxide, standard deviation; OUTCROP; Outcrop sample; Potassium oxide; Potassium oxide, standard deviation; Rulo_Site; Sample ID; Silicon dioxide; Silicon dioxide, standard deviation; Sodium oxide; Sodium oxide, standard deviation; Titanium dioxide; Titanium dioxide, standard deviation; Volcanic glass shards; Washington, USA
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 5
    Publication Date: 2024-06-19
    Keywords: Area/locality; Carbon, organic, total; Carbon, total; Fraction, non-carbonate; HAND; Sample code/label; Sample mass; Sampling by hand; SR4; Washington, USA; δ13C, carbonate; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
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  • 6
    Publication Date: 2024-06-19
    Keywords: Aluminium; Arsenic; Barium; Cerium; Dysprosium; Erbium; Europium; Gadolinium; HAND; Holmium; Iron; Lanthanum; Lutetium; Magnesium; Manganese; Molybdenum; Molybdenum/Uranium ratio; Neodymium; Nickel; Praseodymium; Rare-earth elements; Samarium; Sample code/label; Sample code/label 2; Sampling by hand; Silicon; SR4; Strontium; Terbium; Thulium; Uranium; Washington, USA; Ytterbium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 372 data points
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  • 7
    Publication Date: 2024-06-19
    Keywords: Aluminium oxide; Calcium oxide; DEPTH, sediment/rock; Identification; Iron oxide, FeO; Lithologic unit/sequence; Loss on ignition; Magnesium oxide; Manganese oxide; OUTCROP; Outcrop sample; Phosphorus pentoxide; Potassium oxide; Ratio; Rulo_Site; Sample ID; Silicon dioxide; Sodium oxide; Sum; Titanium/Aluminium ratio; Titanium dioxide; Washington, USA; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 765 data points
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  • 8
    Publication Date: 2024-06-19
    Description: In this study we look beyond the previously studied effects of oceanic CO2 injections on atmospheric and oceanic reservoirs and also account for carbon cycle and climate feedbacks between the atmosphere and the terrestrial biosphere. Considering these additional feedbacks is important since backfluxes from the terrestrial biosphere to the atmosphere in response to reducing atmospheric CO2 can further offset the targeted reduction. To quantify these dynamics we use an Earth system model of intermediate complexity to simulate direct injection of CO2 into the deep ocean as a means of emissions mitigation during a high CO2 emission scenario. In three sets of experiments with different injection depths, we simulate a 100-year injection period of a total of 70 GtC and follow global carbon cycle dynamics over another 900 years. In additional parameter perturbation runs, we varied the default terrestrial photosynthesis CO2 fertilization parameterization by ±50 % in order to test the sensitivity of this uncertain carbon cycle feedback to the targeted atmospheric carbon reduction through direct CO2 injections. Simulated seawater chemistry changes and marine carbon storage effectiveness are similar to previous studies. As expected, by the end of the injection period avoided emissions fall short of the targeted 70 GtC by 16–30 % as a result of carbon cycle feedbacks and backfluxes in both land and ocean reservoirs. The target emissions reduction in the parameter perturbation simulations is about 0.2 and 2 % more at the end of the injection period and about 9 % less to 1 % more at the end of the simulations when compared to the unperturbed injection runs. An unexpected feature is the effect of the model's internal variability of deep-water formation in the Southern Ocean, which, in some model runs, causes additional oceanic carbon uptake after injection termination relative to a control run without injection and therefore with slightly different atmospheric CO2 and climate. These results of a model that has very low internal climate variability illustrate that the attribution of carbon fluxes and accounting for injected CO2 may be very challenging in the real climate system with its much larger internal variability.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 9
    Publication Date: 2024-06-18
    Description: In verschiedenen Hanglagen der Ortsgemeinde Essenheim in Rheinhessen (Rheinland-Pfalz) ist der Untergrund rutschgefährdet oder es sind fossile Rutschungen vorhanden. In einer dieser Hanglagen wurde die Erweiterung des Baugebietes „Domherrngärten" geplant. In der Folge dessen war zu klären, unter welchen Randbedingungen die Bebauung realisiert werden kann. Hierzu wurden in mehreren Kampagnen der geologische Untergrund mit Kernbohrungen untersucht und Inklinometermessstellen zur Beobachtung von Hangbewegungen eingerichtet. Die Untersuchungsergebnisse wurden im Rahmen einer Bachelorarbeit zur Durchführung von Standsicherheitsberechnungen genutzt. Auf der Basis aller Untersuchungsergebnisse werden Vorsorgemaßnahmen für die Bebauung in einem rutschgefährdetem Hang aufgezeigt.
    Description: Abstract: Various slopes in the village Essenheim in Rhinehessen/ Rhineland-Pala- tinate are prone to landslides. The planed extension of the building area „Domherrngärten II" is part of such an area. In succession it had to be discussed under which circumstances construction is possible. To analyze the geological features core drillings with rock sampling were executed as well as inclinometers (measurements to detect motion of the slope). The taken data was used in a Bachelor thesis to evaluate the slope stability. On the base of all results references for building on instable slopes are given.
    Description: research
    Keywords: ddc:624.151 ; Mainzer Becken ; Rutschungen ; Ingenieurgeologie ; TK 6014
    Language: German
    Type: doc-type:article , publishedVersion
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  • 10
    Publication Date: 2024-06-18
    Keywords: DATE/TIME; DEPTH, water; File format; File name; File size; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; LATITUDE; LONGITUDE; MULT; Multiple investigations; SO239; SO239-track; Sonne_2; Swath-mapping system Simrad EM122 (Kongsberg Maritime AS); Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 1120 data points
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