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δ is the angle between slope direction and the horizontal shaking direction of the earthquake; θ is the slope angle; γ sat is unit weight of the saturated soil layer, and γ t is unit weight of the soil over the groundwater table; H is the depth of sliding mass.
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The threshold for repeats and nonrepeats are based on the size of confidence intervals and significance testing, which are closely related to coverage depth, size of sliding window, and filtered times.
where c′ is effective cohesion, φ′ is the effective friction angle, γ is the unit weight of the sliding mass, l is the depth of the sliding mass and kh is the coefficient of horizontal earthquake acceleration.
The number of particles along depth is dependent on the depth of the sliding surface, and varies in different position.
The depth of the sliding surface and the position of the flysch bedrock are assumed based on the landslide geometry.
Depth of dynamic sliding surface will be deeper along with the increase of peak ground acceleration, as shown in Fig. 2.
Note that the source area, the depth of the sliding surface, and the volume of the landslide mass could be estimated according to the topographical maps before and after the earthquake.
In addition, the landslides at the metamorphic terrain have deeper depth to sliding surface than those of the sedimentary landscape.
The processing depth dependence on the number of sliding cycles of MoS2 and mica is shown in Figure 17c.
These four parameters: H p, L p, T1, and T2 are closely related to sequencing depth S d and length of sliding window L w.
This could largely conquer the inaccuracy of read depth calculation for each type of sliding windows arising from hard masking of the reference genome.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com