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Orlistat exhibited the highest pore water based bioconcentration factors (BCFs) and displayed the largest differences between soil types with BCFs ranging between 30.5 and 115.9.
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Cycling around the sediment redox transition can lead to extremely high pore water phosphate concentrations.
The white patches are warmer (average of 61°C) and feature correspondingly higher pore water H2S concentrations (up to 990 μM).
The results indicate that reverse faults and mixed materials are responsible for comparatively higher pore water pressures.
Very high pore water phosphate concentrations (of up to 300 μM) were reported in a narrow region of sediments densely populated by T. namibiensis.
These sandy sediment environments are generally characterized by low organic matter and high pore water dissolved oxygen concentrations, properties typically considered unfavorable for heterotrophic denitrification.
However, a combination of high pore water pressure (ru = 0.3), and seismic loading are required to produce a factor of safety < 1.0.
This assumption is backed e.g. by simulation results from building physics that consistently show higher pore water levels inside a wall and strongly decreasing saturation towards the surface [30, 31].
When fluoride ions are readily available, such as under typical marine conditions, these high pore water phosphate concentrations can result in the precipitation of authigenic phosphate minerals such as apatite[5, 55, 56].
Because claystone is likely under a high pore water pressure during its compression, and also because it fails slowly, faulting in claystone layers is a possible source for such slow slip events or very low frequency earthquakes.
One is pile response to strong shaking accompanied by the development of high pore water pressures or liquefaction and the other is the response to the pressures and displacements caused by lateral spreading of liquefied ground.
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