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The observed sediment partitioning is likely caused by a combination of frost-related sediment transport and Azorella cushions acting as sediment obstructions.
However, lateral variations in subsidence regime and shifts in sediment supply led to significant variations in shelf-margin architecture along-strike, directly impacting sediment partitioning between the shelf and the deep-water areas.
Seismic units U2, U3+U4+U5, U6, and U7 are interpreted to correspond respectively to oxygen-isotope stages 1, 3, 5, and 6, implying that sediment partitioning and sequence architecture in the ECS have been controlled by glacio-eustasy and global climate changes.
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These growth faults influenced sediment pathways, controlled sediment partition and provided increased accommodation for deltaic depocenters.
The genesis of these facies and their location in the depositional sequences are controlled by the fluctuation of terrigenous inputs during sea-level changes ("sediment volume partitioning").
When applying equilibrium sampling of HOCs in sediments, equilibrium partitioning concentrations in lipids (c lipid ⇌ sediment) can even directly be calculated by c polymer and a compound-specific lipid to polymer partition coefficient (K lipid,polymer): {c}_{mathrm{lipid}kern0.24em rightleftharpoons kern0.24em mathrm{sediment}}={c}_{polymer}times {K}_{lipid, polymer} (8).
Sediments from a lagoon were collected to assess sediment-solution partitioning during percolation.
The study shows that release and sediment-eluent partitioning of metal(loid)s are impacted by interactions between the studied factors.
The channel bifurcation of the main channel and the mouth of the incipient chute channel controls sediment and flow partitioning and development of the chute.
Soil quality differences were consistently documented among the three watersheds by: (1) quantification of soil indicator variables, (2) calculation of soil quality index values, and (3) comparison of indicator variable and index results with independent assessments of soil function endpoints (i.e. sediment loss, water partitioning at the soil surface, and crop yield).
Though not well understood, Hg complexes with organic and inorganic ligands in surface waters and sediments, and its partitioning is determined by the types and characteristics of the ligands and other chemical factors such as conductivity (27).
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