1) Domain: The domain is all the values for x that will produce a real number for y Factor the denominator to find where y is not defined: f(x) = 2÷(x² - 2x - 3) f(x) = 2 ÷ (x-3)(x+1) The domain is all real numbers except x=3 and x=-1
Range: The range for y is all the values that y can take, given the domain. The range is all real numbers, because y approaches both positive and negative infinite at different points on the graph.
The y-intercept is where x=0 y= 2 ÷ (0² - 2(0) -3) y= 2 ÷ -3 = -2/3
The x-intercept are the points at which y=0. Let's use the factored form again: f(x) = 2 ÷ (x-3)(x+1) This function has no x-intercepts. All values of X either produce a real number, or are undefined in the case of x=3 and x=-1
Horizontal Asymptotes As X approaches inifinite, how does y behave? f(x) = 2÷(x² - 2x - 3) As x approaches both positive and negative infinite, the dominate term in the denominator, x², is vastly greater than 2, and thus y approaches zero. The horizontal asymptote is zero, in both the positive and negative direction.
Again, let's consult the factored form: 2 ÷ (x-3)(x+1) There are vertical asymptotes at both x=3 and x=-1. As x approaches these numbers, depending on whether x is a little bigger or smaller than either one, y approaches positive and negative infinite, since the denominator of the function approaches zero. Therefore, there are both positive and negative vertical asymptotes at both x=3 and x=-1
As for the graph, we'll leave that to you and the many applications that can aid in such a task!
Earth can be divided into three main layers: the core, the mantle and the crust. Each of these layers can be further divided into two parts: the inner and outer core, the upper and lower mantle and the continental and oceanic crust.