Select two distinct values of X, designated X1 and X2, from the table, read the corresponding values Y1 and Y2 from the table, and calculate the slope from the formula: slope = (Y2 - Y1)/(X2 - X1)
The table should give you a set of points. Take two coordinated pairs off the table and use the formula y2 - y1 divided by x2 - x1 (rise over run) to get your slope. Then take the slope and one of your points and plug it into y = mx +b with m being the slope, and b as the y-intercept.
Hydraulic gradient
take two ordered pairs. then do difference of y's divided by difference of x's and that is your slope
Choose two distinct points from the table and designate their coordinates as x1, y1 and x2, y2. The slope of the line then will equal (y2 - y1)/(x2 - x1).
Gradient is the steepness of a slope.
Slope is rise over run, so if you have a rise of 2 and a run of 4, then the slope is 0.5. If the table gives rises and runs, then just follow the two until they meet, that should be the slope.
Select two distinct values of X, designated X1 and X2, from the table, read the corresponding values Y1 and Y2 from the table, and calculate the slope from the formula: slope = (Y2 - Y1)/(X2 - X1)
The slope of the water table is called the hydraulic gradient. This gradient represents the rate of change in water table elevation over a specific distance. It is an important factor in determining the direction and velocity of groundwater flow.
The table should give you a set of points. Take two coordinated pairs off the table and use the formula y2 - y1 divided by x2 - x1 (rise over run) to get your slope. Then take the slope and one of your points and plug it into y = mx +b with m being the slope, and b as the y-intercept.
Hydraulic gradient
take two ordered pairs. then do difference of y's divided by difference of x's and that is your slope
Choose two distinct points from the table and designate their coordinates as x1, y1 and x2, y2. The slope of the line then will equal (y2 - y1)/(x2 - x1).
Changing the slope of the stream table affects the speed and direction of water flow. A steeper slope creates faster water flow, which can result in more erosion and deposition. Conversely, a flatter slope slows down water flow, leading to less erosion and deposition. These changes in flow dynamics can cause differences in the shape and size of channels, as well as the amount and distribution of sediment carried by the water.
The answer will depend on what information the table contains!The answer will depend on what information the table contains!The answer will depend on what information the table contains!The answer will depend on what information the table contains!
Pick any two points in the table. The slope of the line is(change in the y-value from one point to the other)/(change in the x-value from the same point to the other)
-- Measure how far the slope rises in 100-ft of horizontal distance.-- That number is the percent of slope, or the "grade".-- If you want the angle of the slope, divide the number by 100, and look upthe "arctangent" of the answer in a table or on a calculator.