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The characteristic properties of an aquifer can be used to calculate groundwater velocities, vgroundwater (L/T), according to:
where KH (L/T) is the hydraulic conductivity of the porous media in the aquifer, η is the porosity of the porous media, (dh/dl) is the hydraulic gradient. Note that the velocity of groundwater only has meaning in the direction of the hydraulic gradient which is always perpendicular to contour lines of constant head.
a. Calculate the velocity of groundwater at this site.
b. Assuming that the hydraulic gradient is constant in the region around the industrial site, use the groundwater velocity to calculate the travel time between a spill located at 75 m east and 75 m north of the southwest corner of the site and a private groundwater well located 36 m south and 4 m east of the southwest corner of the site. Note that these locations are located on a line parallel to the hydraulic gradient and perpendicular to your contour lines.
Calculating and Visualizing Sequence Statistics Follow the instructions in this demo file to download a sequence and calculate and visualize its statistics. Save all the command
Consider the 3rd order Bessel function J3(x). Write a script findBessRoots.m that computes all the roots of J3(x) in the interval [0; 40]. Your script must store the roots of the f
Illustration of script Documentation: For illustration, the script to compute the area of a circle could be modified to have comments: The first comment at the startin
Illustration of Output statements: For illustration, >> disp('Hello') Hello >> disp(4^3) 64 The formatted output can be printed to the screen by using the fpr
Objectives In the following exercises, students are required ?rstly to implement code to determine the frequency components present in a signal, and then to extract a desired si
what equation equals 36
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plase help me to convert a theory part of ammonia-vapour simple absorption system into matlab programmong
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