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  • Other Sources  (5)
  • 551  (5)
  • John Wiley & Sons, Inc.  (4)
  • Reimer, Berlin  (1)
  • American Chemical Society
  • Blackwell Publishing Ltd
  • Wiley-Blackwell
  • 2020-2022  (5)
  • 1
    Publication Date: 2021-06-22
    Description: The contribution of sediments to nutrient cycling of the coastal North Sea is strongly controlled by the intensity of fluxes across the sediment water interface. Pore‐water advection is one major exchange mechanism that is well described by models, as it is determined by physical parameters. In contrast, biotransport (i.e., bioirrigation, bioturbation) as the other major transport mechanism is much more complex. Observational data reflecting biotransport, from the German Bight for example, is scarce. We sampled the major sediment provinces of the German Bight repeatedly over the years from 2013 to 2019. By employing ex situ whole core incubations, we established the seasonal and spatial variability of macrofauna‐sustained benthic fluxes of oxygen and nutrients. A multivariate, partial least squares analysis identified faunal activity, in specifically bioturbation and bioirrigation, alongside temperature, as the most important drivers of oxygen and nutrient fluxes. Their combined effect explained 63% of the observed variability in oxygen fluxes, and 36–48% of variability in nutrient fluxes. Additional 10% of the observed variability of fluxes were explained by sediment type and the availability of plankton biomass. Based on our extrapolation by sediment provinces, we conclude that pore‐water advection and macrofaunal activity contributed equally to the total benthic oxygen uptake in the German Bight.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Keywords: 551 ; southern North Sea ; coastal sediments ; macrofauna ; bioturbation ; bioirrigation ; organic matter turnover
    Type: article
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  • 2
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    Reimer, Berlin
    In:  SUB Göttingen | 64 A 3198
    Publication Date: 2021-03-29
    Description: Das vorliegende Werk ist das Ergebnis einer mehr als sechsmonatigen bodenkundlichen Erkundungsreise durch fast alle zugänglichen Teile von Südwestafrika (SWA) und analytischer Auswertung der mitgebrachten Bodenproben. Das vorliegende kleine Werk soll über die örtlichen Belange SWA's hinaus Erkenntnisse über Bodenbildung, Bodeneigenschaften und die Möglichkeiten der Bodennutzung auch in anderen ariden Gebieten mit ähnlichen Böden wie in SWA vermitteln. Nur durch ein gründliches Verständnis der Bodenbildung und Bodennutzung aus der besonderen geographischen Situation SWA's und anderer Trockengebiete heraus können schwere Schäden in der Bodennutzung und Bodenkultur vermieden werden. Ein eingehendes Studium des Wesens der betreffenden Böden verhindert, auch Illusionen über Intensivierung der Bodennutzung für SWA und andere Trockengebiete, etwa durch uferlose Bewässerungsprojekte, wie sie in populären Darstellungen und Presseartikeln ohne jede Kenntnis der notwendigen naturwissenschaftlichen Grundlagen propagiert und vielfach ohne Rücksicht auf die verheerenden Folgen in vielen Ländern auch in der Tat umgesetzt worden sind. Mit der Darstellung der Genetik, Beschreibung und Analytik der Hauptböden in SWA soll zum Vergleich mit Böden in Mitteleuropa angeregt werden und damit auch zum Verständnis der besonderen Eigenart der Böden eines Trockengebietes.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: 551 ; Südliches Afrika {Bodenkunde} ; Klimatische Geomorphologie ; Bodenkunde ; Namibia ; FID-GEO-DE-7
    Language: German
    Type: monograph_digi
    Format: 168
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  • 3
    Publication Date: 2021-07-05
    Description: Large urban areas are typically characterized by a mosaic of different land uses, with contrasting mixes of impermeable and permeable surfaces that alter “green” and “blue” water flux partitioning. Understanding water partitioning in such heterogeneous environments is challenging but crucial for maintaining a sustainable water management during future challenges of increasing urbanization and climate warming. Stable isotopes in water have outstanding potential to trace the partitioning of rainfall along different flow paths and identify surface water sources. While isotope studies are an established method in many experimental catchments, surprisingly few studies have been conducted in urban environments. Here, we performed synoptic sampling of isotopes in precipitation, surface water and groundwater across the complex city landscape of Berlin, Germany, for a large ‐scale overview of the spatio‐temporal dynamics of urban water cycling. By integrating stable isotopes of water with other hydrogeochemical tracers we were able to identify contributions of groundwater, surface runoff during storm events and effluent discharge on streams with variable degrees of urbanization. We could also assess the influence of summer evaporation on the larger Spree and Havel rivers and local wetlands during the exceptionally warm and dry summers of 2018 and 2019. Our results demonstrate that using stable isotopes and hydrogeochemical data in urban areas has great potential to improve our understanding of water partitioning in complex, anthropogenically‐affected landscapes. This can help to address research priorities needed to tackle future challenges in cities, including the deterioration of water quality and increasing water scarcity driven by climate warming, by improving the understanding of time‐variant rainfall‐runoff behaviour of urban streams, incorporating field data into ecohydrological models, and better quantifying urban evapotranspiration and groundwater recharge.
    Description: Seasonal isotope and hydrogeochemical dynamics of surface‐ and groundwater in a large urban area following the dry summer of 2018, which was characterized by a temperature anomaly and precipitation deficit.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: 551 ; ecohydrology ; hydrogeochemistry ; isotopes ; tracers ; urban green spaces ; urban hydrology
    Type: article
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  • 4
    Publication Date: 2021-06-16
    Description: Information on water balance components such as evapotranspiration and groundwater recharge are crucial for water management. Due to differences in physical conditions, but also due to limited budgets, there is not one universal best practice, but a wide range of different methods with specific advantages and disadvantages. In this study, we propose an approach to quantify actual evapotranspiration, groundwater recharge and water inflow, i.e. precipitation and irrigation, that considers the specific conditions of irrigated agriculture in warm, arid environments. This approach does not require direct measurements of precipitation or irrigation quantities and is therefore suitable for sites with an uncertain data basis. For this purpose, we combine soil moisture and energy balance monitoring, remote sensing data analysis and numerical modelling using Hydrus. Energy balance data and routine weather data serve to estimate ET0. Surface reflectance data from satellite images (Sentinel‐2) are used to derive leaf area indices, which help to partition ET0 into energy limited evaporation and transpiration. Subsequently, first approximations of water inflow are derived based on observed soil moisture changes. These inflow estimates are used in a series of forward simulations that produce initial estimates of drainage and ETact, which in turn help improve the estimate of water inflow. Finally, the improved inflow estimates are incorporated into the model and then a parameter optimization is performed using the observed soil moisture as the reference figure. Forward simulations with calibrated soil parameters result in final estimates for ETact and groundwater recharge. The presented method is applied to an agricultural test site with a crop rotation of cotton and wheat in Punjab, Pakistan. The final model results, with an RMSE of 2.2% in volumetric water content, suggest a cumulative ETact and groundwater recharge of 769 and 297 mm over a period of 281 days, respectively. The total estimated water inflow accounts for 946 mm, of which 77% originates from irrigation.
    Description: Approach to quantify ETact, GWR and water inflow that considers the specific conditions of irrigated agriculture in warm, acid environments. It combines soil moisture and energy balance monitoring, remote sensing data analysing data analysis and numerical modelling using Hydrus. The final model results suggest that GWR accounts for one third of the total water inflow, of which 77% originates from irrigations. image
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Keywords: 551 ; actual evapotranspiration ; ground heat flux ; groundwater recharge ; Hydrus ; irrigation ; net radiation ; Sentinel‐2 ; soil moisture
    Type: article
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  • 5
    Publication Date: 2021-09-29
    Description: Dinitrogen (N2) fixation is a major source of bioavailable nitrogen to oligotrophic ocean communities. Yet, we have limited understanding how ongoing climate change could alter N2 fixation. Most of our understanding is based on short‐term laboratory experiments conducted on individual N2‐fixing species whereas community‐level approaches are rare. In this longer‐term in situ mesocosm study, we aimed to improve our understanding on the role of rising atmospheric carbon dioxide (CO2) and simulated deep water upwelling on N2 and carbon (C) fixation rates in a natural oligotrophic plankton community. We deployed nine mesocosms in the subtropical North Atlantic Ocean and enriched seven of these with CO2 to yield a range of treatments (partial pressure of CO2, pCO2 = 352–1025 μatm). We measured rates of N2 and C fixation in both light and dark incubations over the 55‐day study period. High pCO2 negatively impacted light and dark N2 fixation rates in the oligotrophic phase before simulated upwelling, while the effect reversed in the light N2 fixation rates in the bloom decay phase after added nutrients were consumed. Dust deposition and simulated upwelling of nutrient‐rich deep water increased N2 fixation rates and nifH gene abundances of selected clades including the unicellular diazotrophic cyanobacterium clade UCYN‐B. Elevated pCO2 increased C fixation rates in the decay phase. We conclude that elevated pCO2 and pulses of upwelling have pronounced effects on diazotrophy and primary producers, and upwelling and dust deposition modify the pCO2 effect in natural assemblages.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Exzellenzcluster Ozean der Zukunft http://dx.doi.org/10.13039/501100010783
    Description: H2020 Environment http://dx.doi.org/10.13039/100010681
    Description: Villum Foundation http://dx.doi.org/10.13039/100008398
    Description: Horizon 2020 http://dx.doi.org/10.13039/100010661
    Description: Research Foundation http://dx.doi.org/10.13039/100005930
    Description: Federal Ministry of Education and Research http://dx.doi.org/10.13039/501100002347
    Keywords: 551 ; subtropical North Atlantic Ocean ; N2 fixation ; C fixation
    Type: map
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