Exact(4)
The first step is to project the influence boundaries for the upper and lower sides to the flat and inclined seams, respectively.
The line equations for the lower and upper major influence boundaries (γ L and γ H) that intersect the prediction point at x p are shown in Eqs.
Based on the concept of the influence function method, the final subsidence at a surface point is the summation of all influences received at this point caused by the extraction in the coal seam within the influence boundaries.
These days we are witnessing a rearrangement of the influence boundaries.
Similar(56)
Obstacles considerably influence boundary layer processes.
These two lines are the lower and upper influence boundary lines.
They can be determined by finding the intersection points between the inclined coal seam and the lower and upper influence boundary lines, respectively.
It should be noted that the P-Z line equally divides the angle formed between the lower and upper influence boundary lines drawn downwards from the surface point P. The nadir angle is determined by.
Similarly, the coordinates of the intersection point between upper influence boundary and the coal seam are determined as: x_{text{H}} = frac{{x_{text{p}} tan gamma_{text{H}} - h_{1} }}{{tan alpha + tan gamma_{text{H}} }} (8) y_{text{H}} = left( {x_{text{H}} - x_{text{p}} } right)tan gamma_{text{H}} (9).
Comparison of the domain 1 residues in MNV and HNV that are predicted to lie close to the boundary substrate and active site highlighted two strong potential candidate residues that could influence boundary cleavage.
Its techniques of survey and boundary demarcation set a new standard, serving as a model for later British colonial boundary commissions and influencing boundary-making theory through the present day.
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