11/11/2022 0 Comments Elster online 2013 download“Moderate” indicates that values can be used in terms of proportions within the data set. Overbank silt-clay deposition and intensive Neolithic land-use in a Central European catchment – coupled or decoupled? Science of the Total Environment 806: 150858, ELSTER ONLINE 2013 DOWNLOAD REGISTRATIONPANGAEA, (DOI registration in progress)īallasus, H., Schneider, B., von Suchodoletz, H., Miera, J., Werban, U., Fütterer, P., Werther, L., Ettel, P., Veit, U., Zielhofer, C., 2022. XRF data sheet: Weiße Elster overbank silt-clay deposition (SC40 core, Salsitz transect). Zielhofer, C., Ballasus, H., Schneider, B., von Suchodoletz, H., 2021. XRF data sheet: overbank silt-clay deposition sampling (4*4 km grid, Weiße Elster catchment, Salsitz-Trebnitz section). PANGAEAīallasus, H., Zielhofer, C., Schneider, B., von Suchodoletz, H., 2021. XRF element data of fluvial deposits from the Weiße Elster catchment. PANGAEAīallasus, H., Zielhofer, C., Schneider, B., 2021. Master data sheet: Weiße Elster catchment sampling (fluvial sediments) within an 8*8 km grid as sampling template. PANGAEAīallasus, H., Zielhofer, C., 2021. Grain size data sheet: Weiße Elster overbank silt-clay deposition (SC40 core, transect Salsitz). Within the Weiße Elster floodplain at Salsitz SC40 position two parallel overlapping core runs were recovered using vibra-coring.īallasus, H., Zielhofer, C., von Suchodoletz, H., Schneider, B., 2021. At few sites with complex fluvial stratigraphies, duplicate samples were taken and then mean values were calculated subsequently. Sediment bulk material were sampled from recent streambeds of Weiße Elster sub-catchments with a spade. GRADISTAT v9.1 for the calculation of D50 (median of grain size), D75/D25 and D75-D25 (interquartile range of grain size distribution) was used. In addition, grain size analysis from SC40 core samples were conducted using dry-sieving technique for the sand fraction and a SediGraph III 5120 (Micromeritics) for the silt and clay fraction. Subsequently, stationary XRF spectrometry (Spectro Xepos energy dispersive XRF spectrometer) was applied for analysing elemental composition of bank and streambed samples from the Weiße Elster sub-basins (111 grids) and SC40 core samples. Further, a core was recovered from the Weiße Elster floodplain and a total number of 52 geochemical samples was obtained from this SC40 core. Based on the grid, a map was created in which the primarily represented geological unit were assigned as a raster-cell parameter. The sub-catchments samples were classified according to their geological features. Thus, the extracted sediments contain the geochemical signal of the respective sub-catchment. A grid of 8*8 km cells was arranged over the entire Weiße Elster catchment. Hydro-sedimentary provenance analysis, catchment-scale approach, XRF analysis, Fluvial Geomorphology, Holocene, overbank silt-clay depositionįor XRF sediment provenance analysis in the Weiße Elster catchment of Central Germany sediment bulk material of recent streambeds from sub-catchments were sampled within a systematic mesoscale framework. Earth and Planetary Sciences – Earth-Surface Processes, Stratigraphy
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