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Grain size distribution of beach sediments, Kiel Fjord

Microplastic abundance in beach sediments of the Kiel Fjord

We assessed the abundance of microplastic (0.2 - 5 mm) in drift line sediments from three sites in Kiel Fjord, Western Baltic. The first site is intensively used by beach visitors, the second is in close proximity to a sewage plant and the third is polluted with large-sized plastic litter. Samples were split into three grain size classes (0.2 – 0.5, 0.5 – 1.0, 1.0 – 5.0 mm), washed with a calciumchloride solution and filtered at 0.2 mm. Filters were then visually inspected and a total of 180 fragments were classified as microplastic, of which 39 % were analysed using Raman spectroscopy. At the site with intense beach use as well as at the site that is close to a sewage plant 1.8 and 4.5 particles (fibers plus fragments) per kg of dry sediment were found, respectively, while particle abundances reached 30.2 per kg of dry sediment at the site with high litter loads. Our data suggest that intensity of human use and proximity to a sewage plant are not necessarily reliable predictors for high loads of microplastics in beach sediments, while the fragmentation of large plastic debris at site seems to be a relevant contamination source.

Vibration spectroscopy, X-ray diffraction, scanning electron microscopy and computational simulation data related to the growth of Li-carbonate crystals in different solutions

Data collected as part of a research study examining the growth of lithium carbonate (mineral name: zabuyelite, chemical formula: Li2CO3) from aqueous solution in the presence of inorganic additives. Ion-pair interactions within the solutions were examined using Raman spectroscopy, whereas the interactions between precipitated crystals and aqueous solution was tested using attenuated total reflectance infrared spectroscopy. In addition, computational simulations were used to study ion pairing in solution (PHREEQC) and adsorption to crystal surfaces (VASP). Precipitates from the experiments were characterised using Raman spectroscopy, diffuse reflectance Fourier transform infrared spectroscopy (DRIFTS) and X-ray diffraction (XRD). Images of the precipitates were obtained using scanning electron microscopy (SEM). For details of the set up for each instrument and specific parameters for the computational simulations, please see the linked publication.

Raman spectroscopic data from dissociation behavior of sI CH4 hydrates, sII CH4-C3H8 hydrates and multicomponent mixed gas hydrates in terms of thermal stimulation

Natural gas hydrates are non-stoichiometric crystalline compounds containing water and guest molecules such as CH4, C2H6, C3H8, CO2, etc. They are considered as a promising energy resource, a potential geohazard and a contributor to global climate warming. An accurate knowledge of the dissociation behavior of gas hydrates is a necessity for the recovery of natural gas hydrates and the assessment of potential risks of CH4 release from destabilized deposits. To explore the dissociation behavior of gas hydrates, Raman spectroscopy is regarded as a non-destructive and powerful tool. This technique enables to distinguish between guest molecules in the free gas or liquid phase, encased into a clathrate cavity or dissolved in an aqueous phase, therefore providing time-resolved information about the conditions of the guest molecules during the hydrate dissociation process. Experiments were carried out at the Micro-Raman Spectroscopy Laboratory, GFZ. Since the dissociation kinetics of sI hydrates may vary from that of sII hydrates, sI CH4 hydrates, sII binary hydrates and sII multicomponent mixed hydrates were investigated during the experiments. For the in situ Raman measurements, hydrates were synthesized in a high-pressure cell from pure water and the specific continuous gas flow which was the CH4-C3H8 gas mixture for binary hydrates and CH4-C2H6-C3H8-CO2 gas mixture for mixed hydrate system. The p-T condition of the experiment was initially set at 274 K and 7.0 MPa for the sI hydrates whereas 278 K and 3.0 MPa for sII hydrate systems. After the stabilization of the hydrates in the reactor, the temperature of the system was increased one step at a time to mimic global warming and initiate hydrate dissociation. In situ Raman spectroscopic measurements and microscopic observations were applied to record changes in hydrate compositions over the whole dissociation period until the hydrate phase was completely decomposed. Apart from this, hydrates were formed from ice powders and the specific gas/gas mixtures in batch pressure vessels for several weeks. Gas hydrates were recovered and placed into a Linkam cooling stage for further ex situ Raman spectroscopic measurements. Again, the temperature of the stage gradually increased from 168 K onwards to study the dissociation process. In all three hydrate systems, one in situ Raman measurements and at least two repetitions of ex situ Raman measurements (3 repetitions for the CH4 hydrate system) were carried out, therefore resulting in 10 separate experimental tests. This dataset encompasses raw Raman spectra of the 10 experimental tests (4 tests for CH4 hydrates, 3 tests for CH4-C3H8 hydrates and 3 for mixed gas hydrates) which contained Raman shifts and the respective measured intensities. Each Raman spectrum was fitted to Gauss/Lorentz function after an appropriate background correction to estimate the band areas and positions (Raman shift). The Raman band areas were then corrected with wavelength-independent cross-sections factors for each specific component. The concentration of each guest molecule in the hydrate phase was given as mol% in separate spreadsheets for three different hydrate systems as. Further details on the analytical setup, experimental procedures and composition calculation are provided in the following sections.

Database of in situ Raman spectra from Ca- and Mg-ATP solutions at 80 °C, 100 °C and 120 °C for determination of the rate constant of the ATP hydrolysis

In biochemical systems, enzymes facilitate the endergonic reaction of adenosine diphosphate (ADP) to adenosine triphosphate (ATP) via pathways such as oxidative phosphorylation by mem-brane-bound ATP synthase or substrate-level phosphorylation. The energy stored in ATP is re-leased through enzymatic control of exergonic hydrolysis, which powers other essential ender-gonic reactions, thus earning ATP the name as the universal energy currency. The non-enzymatic hydrolysis of ATP to ADP in the absence of biological processes increases and counteracts this biological process. It is believed that this is a key factor in defining the operational limits of liv-ing organisms (Bains et al., 2015). The in-situ procedure developed by Moeller et al. (2022, 2024), which employs Raman spec-troscopy, has facilitated the exploration of the effects of pressure, temperature, and ionic com-position on the kinetics of ATP-ADP hydrolysis in an effective manner. Raman spectroscopy can be combined with a hydrothermal diamond anvil cell, thereby enabling measurements in an isochoric system at pressures up to 2000 MPa (Moeller et al., 2024). Another configuration for in-situ Raman spectroscopy at elevated pressures and temperatures employs an autoclave with optical high-pressure windows, as demonstrated by Louvel et al. (2015). This system is capable of operating at pressures up to 200 MPa, with independent control of pressure and temperature, allowing for isobaric temperature series to be conducted. In living organisms, ATP is activated by complexation with Mg2+. The objective of this study was to provide new kinetic data on ATP hy-drolysis and offer further insights into this key metabolite under extreme conditions, thus ex-tending the datasets of Moeller et al. ([dataset] 2024A, B). This data publication presents the complete set of Raman spectra obtained in situ for Na2H2ATP solutions with MgCl2, CaCl2, and NaCl at temperatures of 80 °C, 100 °C, and 120 °C under vapor saturation or at 20 MPa. The data were employed to ascertain the rate constants for ATP hydro-lysis to ADP across eight distinct chemical compositions. An elaborative thermodynamic model was used to mimic the chemical system at experimental conditions. The results are a compre-hensive database of ATP species concentrations at 80 °C, 100 °C, and 120 °C, which is provided herewith.

Apatite fission-track, apatite and zircon (U-Th)/He, apatite Raman spectroscopic and Vitrinite-reflectance maturity data from the southwestern Tian Shan

This data publication includes the Supplementary Material to Trilsch et al. (2025): “Southwestern Tian Shan: 2. Timing of Cenozoic Mountain Building, Intra-montane Basin Inversion, and Relation to Lithospheric Mantel Indentation” (Tectonics; doi:…..). It comprises thermochronologic (apatite fission track and apatite and zircon (U-Th)/He), stratigraphic, and apatite Raman-spectroscopic data that allow the timing of Cenozoic mountain building in the southwestern Tian Shan of Central Asia; the southwestern Tian Shan is herein defined as that part of the Tian Shan west of the Talas-Fergana Fault Zone that is located at the junction with the Pamir and the Afghan-Tajik Basin and stretches to the Fergana Basin in the north. The refined timing provided supports the synchroneity between major Cenozoic Tian Shan mountain building and India mantle-lithosphere indentation beneath the Pamir and western Tibet, and the instantaneous transfer of shortening across a >500-km-wide foreland, facilitated by structural reactivation.

Physikalisch-chemische Prozesse in der Stratosphaere

Dieser Antrag fasst die folgenden Einzelvorhaben zusammen: 1. Laboruntersuchungen zur Kinetik von Ionen- und Radikal-Konversionsreaktionen und Photolyseprozess innerhalb stratosphaerischer fluessiger Aerosol-Teilchen (Antrag-Nr. 095068), 2. Experimentelle Untersuchungen zum Wachstum und Gefrierverhalten von stratosphaerischen Aerosol- und PSC-Einzelteilchen (Antrag-Nr. 095135), 3. Studie zur Ozon-Restauration durch photochemische Prozesse (Antrag-Nr. 0 95136), 4. Koordination des Deutschen Ozonforschungsprogramms (Antrag- Nr. 0 95 xxx).

Microplastic fibers and microplastic fragments abundance, Kiel Fjord

Daten für Kiel-Buelk_MP

<div> Citation: Schröder, Kevin; Kossel, Elke; Lenz, Mark (2021): Microplastic fibers and microplastic fragments abundance, Kiel Fjord [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926914, In: Schröder, K et al. (2021): Microplastic abundance in beach sediments of the Kiel Fjord [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.926922 <div style="overflow-x: auto;", aria-label="Table of data for this location"><table>\n <tr> <th>Event</th> <th>Location</th> <th>Type</th> <th>Size fraction</th> <th>Color desc</th> <th>Microplastic [#/kg]</th> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Blue</td> <td>0.454</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Red</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Other</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Blue</td> <td>1.125</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Red</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Other</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Blue</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Red</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Other</td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fragments</td> <td>0.2 - 0.5 mm</td> <td></td> <td>0.227</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fragments</td> <td>0.5 - 1 mm</td> <td></td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>Microplastic fragments</td> <td>1 - 5 mm</td> <td></td> <td>0.000</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>synthetic fibers</td> <td></td> <td></td> <td>1.578</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>coloured fibers</td> <td></td> <td></td> <td>3.833</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>all fibers</td> <td></td> <td></td> <td>17.362</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>Bülk</td> <td>plastic fragments</td> <td></td> <td></td> <td>0.225</td> </tr> </table></div></div> <div> Citation: Schröder, Kevin; Kossel, Elke; Lenz, Mark (2021): Grain size distribution of beach sediments, Kiel Fjord [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926921, In: Schröder, K et al. (2021): Microplastic abundance in beach sediments of the Kiel Fjord [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.926922 <div style="overflow-x: auto;", aria-label="Table of data for this location"><table>\n <tr> <th>Event</th> <th>Repl</th> <th><0.01 µm [%]</th> <th>63-0.01 µm [%]</th> <th>75-63 µm [%]</th> <th>90-75 µm [%]</th> <th>106-90 µm [%]</th> <th>125-106 µm [%]</th> <th>150-125 µm [%]</th> <th>180-150 µm [%]</th> <th>212-180 µm [%]</th> <th>250-212 µm [%]</th> <th>300-250 µm [%]</th> <th>355-300 µm [%]</th> <th>425-355 µm [%]</th> <th>500-425 µm [%]</th> <th>600-500 µm [%]</th> <th>710-600 µm [%]</th> <th>850-710 µm [%]</th> <th>1-0.85 mm [%]</th> <th>1.18-1 mm [%]</th> <th>1.4-1.18 mm [%]</th> <th>1.7-1.4 mm [%]</th> <th>2-1.7 mm [%]</th> <th>2.36-2 mm [%]</th> <th>2.8-2.36 mm [%]</th> <th>3.35-2.8 mm [%]</th> <th>4-3.35 mm [%]</th> <th>4.75-4 mm [%]</th> <th>5.6-4.75 mm [%]</th> <th>6.3-5.6 mm [%]</th> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>1</td> <td>0.43</td> <td>0.00</td> <td>0.00</td> <td>0.01</td> <td>0.10</td> <td>0.25</td> <td>1.32</td> <td>3.60</td> <td>8.31</td> <td>16.78</td> <td>32.38</td> <td>24.06</td> <td>9.43</td> <td>2.68</td> <td>0.44</td> <td>0.14</td> <td>0.04</td> <td>0.02</td> <td>0.02</td> <td>0.01</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>2</td> <td>0.41</td> <td>0.00</td> <td>0.02</td> <td>0.03</td> <td>0.10</td> <td>0.25</td> <td>1.43</td> <td>4.39</td> <td>10.12</td> <td>18.03</td> <td>32.19</td> <td>21.65</td> <td>8.35</td> <td>2.50</td> <td>0.40</td> <td>0.11</td> <td>0.02</td> <td>0.01</td> <td>0.01</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>3</td> <td>0.39</td> <td>0.00</td> <td>0.03</td> <td>0.05</td> <td>0.09</td> <td>0.21</td> <td>1.12</td> <td>3.19</td> <td>7.72</td> <td>15.10</td> <td>33.58</td> <td>25.38</td> <td>9.79</td> <td>2.72</td> <td>0.44</td> <td>0.12</td> <td>0.03</td> <td>0.02</td> <td>0.02</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>4</td> <td>0.87</td> <td>0.01</td> <td>0.02</td> <td>0.02</td> <td>0.07</td> <td>0.19</td> <td>0.98</td> <td>2.87</td> <td>7.05</td> <td>14.24</td> <td>32.60</td> <td>26.82</td> <td>10.19</td> <td>2.97</td> <td>0.67</td> <td>0.25</td> <td>0.09</td> <td>0.05</td> <td>0.03</td> <td>0.03</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> </tr> <tr> <td>Kiel-Buelk_MP</td> <td>5</td> <td>0.40</td> <td>0.00</td> <td>0.01</td> <td>0.02</td> <td>0.07</td> <td>0.23</td> <td>1.18</td> <td>3.38</td> <td>8.04</td> <td>15.64</td> <td>34.12</td> <td>24.59</td> <td>8.72</td> <td>2.66</td> <td>0.64</td> <td>0.21</td> <td>0.05</td> <td>0.04</td> <td>0.01</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> <td>0.00</td> </tr> </table></div></div>

Daten für Kiel-Tirpitzmole_MP

<div> Citation: Schröder, Kevin; Kossel, Elke; Lenz, Mark (2021): Microplastic fibers and microplastic fragments abundance, Kiel Fjord [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926914, In: Schröder, K et al. (2021): Microplastic abundance in beach sediments of the Kiel Fjord [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.926922 <div style="overflow-x: auto;", aria-label="Table of data for this location"><table>\n <tr> <th>Event</th> <th>Location</th> <th>Type</th> <th>Size fraction</th> <th>Color desc</th> <th>Microplastic [#/kg]</th> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Blue</td> <td>0.947</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Red</td> <td>0.313</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.2 - 0.5 mm</td> <td>Other</td> <td>0.000</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Blue</td> <td>0.470</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Red</td> <td>0.470</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>0.5 - 1 mm</td> <td>Other</td> <td>0.000</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Blue</td> <td>0.313</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Red</td> <td>0.470</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fibers</td> <td>1 - 5 mm</td> <td>Other</td> <td>0.313</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fragments</td> <td>0.2 - 0.5 mm</td> <td></td> <td>4.413</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fragments</td> <td>0.5 - 1 mm</td> <td></td> <td>6.463</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>Microplastic fragments</td> <td>1 - 5 mm</td> <td></td> <td>16.072</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>synthetic fibers</td> <td></td> <td></td> <td>3.296</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>coloured fibers</td> <td></td> <td></td> <td>5.672</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>all fibers</td> <td></td> <td></td> <td>37.973</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>Tirpitzmole</td> <td>plastic fragments</td> <td></td> <td></td> <td>26.944</td> </tr> </table></div></div> <div> Citation: Schröder, Kevin; Kossel, Elke; Lenz, Mark (2021): Grain size distribution of beach sediments, Kiel Fjord [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926921, In: Schröder, K et al. (2021): Microplastic abundance in beach sediments of the Kiel Fjord [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.926922 <div style="overflow-x: auto;", aria-label="Table of data for this location"><table>\n <tr> <th>Event</th> <th>Repl</th> <th><0.01 µm [%]</th> <th>63-0.01 µm [%]</th> <th>75-63 µm [%]</th> <th>90-75 µm [%]</th> <th>106-90 µm [%]</th> <th>125-106 µm [%]</th> <th>150-125 µm [%]</th> <th>180-150 µm [%]</th> <th>212-180 µm [%]</th> <th>250-212 µm [%]</th> <th>300-250 µm [%]</th> <th>355-300 µm [%]</th> <th>425-355 µm [%]</th> <th>500-425 µm [%]</th> <th>600-500 µm [%]</th> <th>710-600 µm [%]</th> <th>850-710 µm [%]</th> <th>1-0.85 mm [%]</th> <th>1.18-1 mm [%]</th> <th>1.4-1.18 mm [%]</th> <th>1.7-1.4 mm [%]</th> <th>2-1.7 mm [%]</th> <th>2.36-2 mm [%]</th> <th>2.8-2.36 mm [%]</th> <th>3.35-2.8 mm [%]</th> <th>4-3.35 mm [%]</th> <th>4.75-4 mm [%]</th> <th>5.6-4.75 mm [%]</th> <th>6.3-5.6 mm [%]</th> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>1</td> <td>0.14</td> <td>0.02</td> <td>0.19</td> <td>0.67</td> <td>3.00</td> <td>6.67</td> <td>12.17</td> <td>10.44</td> <td>9.27</td> <td>7.72</td> <td>10.17</td> <td>10.40</td> <td>8.79</td> <td>7.89</td> <td>4.57</td> <td>3.47</td> <td>1.78</td> <td>1.04</td> <td>0.69</td> <td>0.36</td> <td>0.12</td> <td>0.08</td> <td>0.08</td> <td>0.07</td> <td>0.02</td> <td>0.00</td> <td>0.09</td> <td>0.00</td> <td>0.09</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>2</td> <td>0.12</td> <td>0.03</td> <td>0.20</td> <td>0.66</td> <td>2.99</td> <td>6.77</td> <td>12.44</td> <td>10.46</td> <td>9.19</td> <td>7.71</td> <td>11.25</td> <td>10.88</td> <td>9.08</td> <td>7.94</td> <td>4.16</td> <td>2.79</td> <td>1.27</td> <td>0.77</td> <td>0.43</td> <td>0.19</td> <td>0.18</td> <td>0.08</td> <td>0.12</td> <td>0.04</td> <td>0.06</td> <td>0.06</td> <td>0.00</td> <td>0.14</td> <td>0.00</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>3</td> <td>0.22</td> <td>0.00</td> <td>0.14</td> <td>0.59</td> <td>2.83</td> <td>6.56</td> <td>12.69</td> <td>11.29</td> <td>10.08</td> <td>8.79</td> <td>12.44</td> <td>10.65</td> <td>8.31</td> <td>6.63</td> <td>3.39</td> <td>2.30</td> <td>1.12</td> <td>0.60</td> <td>0.41</td> <td>0.25</td> <td>0.14</td> <td>0.12</td> <td>0.13</td> <td>0.05</td> <td>0.07</td> <td>0.04</td> <td>0.03</td> <td>0.00</td> <td>0.12</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>4</td> <td>0.21</td> <td>0.03</td> <td>0.20</td> <td>0.61</td> <td>2.73</td> <td>5.78</td> <td>10.69</td> <td>9.54</td> <td>8.31</td> <td>7.33</td> <td>9.29</td> <td>8.99</td> <td>8.95</td> <td>8.72</td> <td>5.32</td> <td>4.40</td> <td>2.63</td> <td>1.78</td> <td>1.24</td> <td>0.95</td> <td>0.42</td> <td>0.33</td> <td>0.20</td> <td>0.26</td> <td>0.17</td> <td>0.25</td> <td>0.04</td> <td>0.16</td> <td>0.46</td> </tr> <tr> <td>Kiel-Tirpitzmole_MP</td> <td>5</td> <td>0.18</td> <td>0.03</td> <td>0.17</td> <td>0.61</td> <td>2.51</td> <td>5.43</td> <td>10.17</td> <td>9.23</td> <td>8.46</td> <td>7.59</td> <td>10.32</td> <td>10.75</td> <td>10.29</td> <td>9.28</td> <td>4.93</td> <td>3.88</td> <td>2.16</td> <td>1.37</td> <td>1.05</td> <td>0.42</td> <td>0.33</td> <td>0.16</td> <td>0.18</td> <td>0.10</td> <td>0.07</td> <td>0.08</td> <td>0.09</td> <td>0.05</td> <td>0.11</td> </tr> </table></div></div>

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