14.2
In a civil engineering project, a road is planned through mountainous terrain. To estimate the earthwork required, engineers calculate the volume of soil between the existing terrain and the planned road level.
The planned path of the road is modeled as a rectangular region in the xy-plane. A continuous height function represents the varying elevation of the terrain above this base.
To estimate the volume of soil to be excavated or filled, the region is divided into smaller, equal sections. The area of each section is then calculated by the product of its sides.
The midpoint rule approximates a double integral by evaluating the function at each sub-rectangle's midpoint. Within each section, a central point is identified to estimate the approximate height.
The soil height is evaluated at each midpoint. These values approximate the height difference within each section.
From each section, a vertical column of soil is formed by multiplying the rectangular area of each section by its corresponding height.
Similarly, approximate volumes for each column are calculated. Adding all these small volumes gives an approximate total volume of soil above the reference level.
The midpoint rule for a double integral provides a practical method for estimating volume over a rectangular region when the surface height varies continuously. In civil engineering, this method is useful for approximating the amount of soil to be moved when planning a road across uneven terrain. The road footprint is represented as a rectangle in the xy-plane. At the same time, the terrain elevation above a flat reference level is described by a continuous height function f(x,y). The objective is to approximate the volume of soil lying between the surface and the reference plane.
Partition of the Region
To apply the midpoint rule, the rectangular base region is divided into smaller sub-rectangles of equal size. If the rectangle is partitioned into m intervals in the x-direction and n intervals in the y-direction, then each sub-rectangle has an area
\begin{equation*}\Delta A = \Delta x \, \Delta y\end{equation*}
This subdivision replaces the irregular terrain over the full region with a collection of smaller sections that are easier to analyze.
Midpoint Approximation
Within each sub-rectangle, the midpoint (xi*, yj*) is determined. The function value f(xi*, yj*) gives the approximate terrain height for that section. Each sub-rectangle is then treated as the base of a vertical column of soil whose volume is estimated by
\begin{equation*}f(x_i^*, y_j^*) \, \Delta A\end{equation*}
Thus, the height at the midpoint serves as a representative value for the entire section.
Estimated Total Volume
The approximate total volume is obtained by summing the volumes of all such columns:
\begin{equation*}\iint_{R} f(x, y)\, dA \approx \sum_{i=1}^{m} \sum_{j=1}^{n} f(x_i^*, y_j^*) \, \Delta A\end{equation*}
This approximation becomes more accurate as the region is divided into finer sub-rectangles, making the midpoint rule an effective tool for estimating earthwork volumes in engineering applications.
In a civil engineering project, a road is planned through mountainous terrain. To estimate the earthwork required, engineers calculate the volume of soil between the existing terrain and the planned road level.
The planned path of the road is modeled as a rectangular region in the xy-plane. A continuous height function represents the varying elevation of the terrain above this base.
To estimate the volume of soil to be excavated or filled, the region is divided into smaller, equal sections. The area of each section is then calculated by the product of its sides.
The midpoint rule approximates a double integral by evaluating the function at each sub-rectangle's midpoint. Within each section, a central point is identified to estimate the approximate height.
The soil height is evaluated at each midpoint. These values approximate the height difference within each section.
From each section, a vertical column of soil is formed by multiplying the rectangular area of each section by its corresponding height.
Similarly, approximate volumes for each column are calculated. Adding all these small volumes gives an approximate total volume of soil above the reference level.
From Chapter 14:
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