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Found 12 results.

XRF data sheet: Weiße Elster overbank silt-clay deposition (SC40 core, Salsitz transect)

We used stationary XRF spectrometry for analysing elemental composition of Holocene floodplain sediments from a recovered core form the Weiße Elster floodplain. For XRF sample preparation freeze-dried catchment sediments (8 g) were seaved (2mm) to discard the gravel fraction and large organic matter. Further homogenization was undertaken by grinding the samples with a vibratory Retsch mill MM 200. We created uniform pellets by pressing the powdered samples with a carbon-based binding agent in a Vaneox press at 20 t for 2 min. We conducted elemental analyses in a He atmosphere using a Spectro Xepos energy dispersive XRF spectrometer. The total drilling depth of SC40 core is 275 cm. We conducted stationary XRF measurements of 52 samples.

Specimen data from core B1-06 of the Heidelberg Basin, Germany

Specimen data from core P36 of the Heidelberg Basin, Germany

Specimen data from core UN1 and UN2 of the Heidelberg Basin, Germany

X-ray analysis from core P36 and B1-06 of the Heidelberg Basin sedimentary, Germany

XRF element data of fluvial deposits from the Weiße Elster catchment

We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (111 grids of 8*8 km). For XRF sample preparation freeze-dried catchment sediments (8 g) were seaved (2mm) to discard the gravel fraction and large organic matter. Further homogenization was undertaken by grinding the samples with a vibratory Retsch mill MM 200. We created uniform pellets by pressing the powdered samples with a carbon-based binding agent in a Vaneox press at 20 t for 2 min. We conducted elemental analyses in a He atmosphere using a Spectro Xepos energy dispersive XRF spectrometer.

XRF data sheet: overbank silt-clay deposition sampling (4*4 km grid, Weiße Elster catchment, Salsitz-Trebnitz section)

We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (refined grids of 4*4 km). For XRF sample preparation freeze-dried catchment sediments (8 g) were seaved (2mm) to discard the gravel fraction and large organic matter. Further homogenization was undertaken by grinding the samples with a vibratory Retsch mill MM 200. We created uniform pellets by pressing the powdered samples with a carbon-based binding agent in a Vaneox press at 20 t for 2 min. We conducted elemental analyses in a He atmosphere using a Spectro Xepos energy dispersive XRF spectrometer. The XRF element data of the refined 4*4 km sampling grid of recent fluvial sediments in the direct proximity to the Salsitz transect are provided here. The data set has to be understood as a supplement or densification of the 8*8 km sampling grid of the Weiße Elster river catchment: doi:10.1594/PANGAEA.937926.

Magnetic susceptibility, Natural Remanent Magnetisation (NRM) and Characteristic remanent magnetisation (ChRM) of core B1-06, Viernheim, Germany

Magnetic susceptibility, Natural Remanent Magnetisation (NRM) and Characteristic remanent magnetisation (ChRM) of core P36, Ludwigshafen, Germany

Magnetic susceptibility, Natural Remanent Magnetisation (NRM) and Characteristic remanent magnetisation (ChRM) of core UN1 (UniNord1) and UN2 (UniNord2), Heidelberg, Germany

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