The main components of precalibration are evaluation of flow system integrity, homogenization efficiency, water repeatability, zero shift, linearity, primary slope, milk repeatability, purging efficiency, and establishment of intercorrection factors.
From 6 months to 24 months, combined with the primary slope.
Seven primary terrain parameters (elevation, slope gradient, slope aspect, plan curvature, profile curvature, flow direction, flow accumulation) and one compound topographic index (CTI) were generated from a Digital Elevation Model (DEM) acquired using airborne LIDAR (Light Detection and Ranging) systems.
As the primary method of slope enforcement, four rows of stabilizing piles were created, and a series of field monitoring systems was installed to measure the movements of the stabilizing piles and the slope.
After accounting for the "primary" covariates, the slope of weight z score did not significantly contribute to the model.
After accounting for the "primary" covariates, the slope of change in weight z score during the first 3 months of treatment did not significantly contribute to the model.
For our primary outcome, the slope of quality score change was also similar: -0.229 (95% CI −0.644 to −0.185) for controls and −0.549 (−0.831 to −0.267) for mentees.
Primary topographic attributes namely slope, aspect and relative relief were derived from digital elevation model.
This implicates the role of climate as a primary preconditioning factor for slope failures in this highly active tectonic region.
Modifications to porosity and permeability can influence edifice-scale behaviour; for example, a reduction in permeability can result in pore pressure augmentation, which exerts a primary control on volcanic slope stability, seismicity, and eruptive behaviour.
Using this technique, important advances have been made in determining the primary factors influencing fan slope, understanding of avulsion dynamics, identifying autogenic processes driving change on fan systems independent of any change in external conditions, and the mechanics of flow and flood risk on alluvial fans, to name a few.
