The answer depends on what h is and who you are!
The slope is 3.
Undefined: You cannot divide by zero
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There are two things you need to remember. First, given a line y=mx+b, where m is the slope and b is the y-intercept, the slope of the line perpendicular is going to be -1/m. Next, if you have the point where the lines cross, you want to use the point-slope form of a line to get the equation of the perpendicular line. Suppose the lines cross at (h,k). Then the point-slope form of the equation for the perpendicular line crossing at (h,k) will be (y-k)=-1/m(x-h). This can be brought into the slope-intercept form y=(-1/m)x + h/m + k.
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The slope is 3.
The formula to calculate pH slope is ΔpH/Δlog[H+], where ΔpH is the change in pH and Δlog[H+] is the change in the log concentration of hydrogen ions. This formula is used to determine the sensitivity of a pH electrode.
Undefined: You cannot divide by zero
8
There are two things you need to remember. First, given a line y=mx+b, where m is the slope and b is the y-intercept, the slope of the line perpendicular is going to be -1/m. Next, if you have the point where the lines cross, you want to use the point-slope form of a line to get the equation of the perpendicular line. Suppose the lines cross at (h,k). Then the point-slope form of the equation for the perpendicular line crossing at (h,k) will be (y-k)=-1/m(x-h). This can be brought into the slope-intercept form y=(-1/m)x + h/m + k.
Approximately 17.1739 mm per h.
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Slope is the rise over the run, the distance up and down, divided by the distance side to side. aka y=mx+b We find math slope using some particular slope formula. by the help of this formula we can find math solutions.
... doesn't change slope :/ solved lol
Permeability can be determined from the B-H curve by calculating the slope of the curve in the linear region, where the relationship between magnetic flux density (B) and magnetic field strength (H) is approximately linear. The permeability (μ) is defined as the ratio of B to H (μ = B/H). In practice, one can take the values of B and H from the linear portion of the curve and use them to calculate the permeability at that specific point. Additionally, the initial permeability can be assessed by evaluating the slope at the origin of the B-H curve.
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