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To improve the understanding of soil-landscape development, the initial sediments need to be quantified in space and time.
The initial porosity of reservoir is mainly controlled by the characteristics of initial sediments and deposition conditions, and the pore evolution in late stage mainly depends on the intensity of late diagenesis.
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The consolidation rates were inversely and exponentially related to initial sediment concentrations.
From the 3D-model, an initial sediment volume of 122,608 m3 was quantified.
The transported matter was enriched 6 8 times in fine particles and organic matter when compared to the initial sediment.
After about 50 days of reaction, cadmium, zinc, manganese, and copper dissolution slows to about 30, 10, 5, and 4% of their respective initial sediment concentrations.
This study aims at developing and testing methods for the quantification of initial sediment mass balances in the three dimensions of space and in time.
The two models are run sequentially, with the second model receiving the initial sediment input to check dams from WaTEM/SEDEM.
Additionally, instead of underthrust sediment-filled graben blocks being only vertically loaded, initial sediment accretion may affect overall sediment porosity due to the addition of both vertical and horizontal strains on the subducting sediment (e.g., Moore et al. 2011).
The initial sediment pore water was taken as the measured water composition at the column outlet after the initial equilibration period (Phase I), but prior to urea injection (Table 1).
Finally, 0.2 g initial sediment sample (dry weight) was digested according to the same procedure for the residual phase and the final solution was diluted to 25 ml with Q-water.
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