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Input parameters are the initial flow parameters and a 3D topography at depositional time.
The proportion of coarse size aggregate fractions (> 0.25 mm) at eroded slope positions was greater than that at depositional positions.
In this review, we provide a comprehensive cross-disciplinary review on SOC mineralization and sequestration at sites of erosion, along the transport pathway and at depositional sites.
The current state of knowledge on the impacts of erosion-induced soil aggregate breakdown and formation, removal of SOC from eroding sites and deep burial of SOC at depositional sites on the mineralization and sequestration of SOC are presented.
The CO2 emission rate from coarse size aggregate fractions at depositional slope positions (toe-slope and foot-slope) was significantly greater than that at eroded slope positions (summit, shoulder-slope and back-slope).
Spectroscopic analysis of water extractable organic carbon (WEOC) and bulk SOC shows greater presence of aromatics at eroding sites than at depositional sites, likely due to the contribution of eroded upslope materials.
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Particle size is an important textural parameter of clastic rocks because it supplies information on the conditions of transportation, sorting, and deposition of the sediment and provides some clues to the history of events that occurred at the depositional site prior to final induration.
These two areas have few faults and were structurally located in peripheral areas of the paleo uplift at the depositional stage, so they are considered favorable plays for lithologic reservoirs.
Data showed that CS and SG significantly increased the pH of acidic soil at the eroded landscape position but produced no significant change in soil pH at the depositional landscape position.
Outcrop and analogue modelling studies indicate that upward widening zones of distributed deformation, often monoclinal folds, form above blind normal faults and are particularly common features at the depositional surface during the early stages of rifting.
During the initial 22 days of incubation, the CO2 emission rate from coarse size aggregate fractions (0.024 ± 0.009 g C kg− 1 soil d− 1) was six times higher than that from small size aggregate fractions (0.0038 ± 0.0011 g C kg− 1 soil d− 1) at the depositional toe-slope position.
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