course mth 163 could you send me a random fully worked example on how to find the average rate change with midpoint formulas? the last two problems i worked the regular way. I could not come up with a conclusion
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21:29:03 Query 4 basic function families What are the four basic functions? What are the generalized forms of the four basic functions?
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RESPONSE --> linear;y=x;y=mx+b;straight line quadratic;y=x^2;y=ax^2+bx+c;parabola expoinential;y=2^x=y=A*2^(kx)+c;increasing/decreasing horizontal asymptote power;y=x^p;y=A(x-h)^p+c;negative;horizontal and vertical asymptotesy=c and s=h; peven/odd graph symmetric or antisymmetric
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21:29:13 ** STUDENT RESPONSE: Linear is y=mx+b Quadratic is y=ax^2 + bx +c Exponential is y= A*2^ (kx)+c Power = A (x-h)^p+c INSTRUCTOR COMMENTS: These are the generalized forms. The basic functions are y = x, y = x^2, y = 2^x and y = x^p. **
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21:31:20 For a function f(x), what is the significance of the function A f(x-h) + k and how does its graph compare to that of f(x)?
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RESPONSE --> it is a power function the graph would be symmetric.
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21:36:03 ** STUDENT RESPONSE: A designates the x strectch factor while h affects a y shift & k affects an x shift INSTRUCTOR COMMENTS: k is the y shift for a simple enough reason -- if you add k to the y value it raises the graph by k units. h is the x shift. The reason isn't quite as simple, but not that hard to understand. It's because when x is replaced by x - h the y values on the table shift 'forward' by h units. A is a multiplier. When all y values are multiplied by A that moves them all A times as far from the x axis, which is what causes the stretch. Thus A f(x-h) + k is obtained from f(x) by vertical stretch A, horizontal shift h and vertical shift k. The two aren't the same, but of course they're closely related. **
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21:45:45 query introduction to rates and slopes, problem 1 ave vel for function depth(t) = .02t^2 - 5t + 150 give the average rate of depth change from t = 20 to t = 40
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RESPONSE --> 20 cm per secod
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21:47:37 ** depth(20) = .02(20^2) - 5(20) + 150 = 58 depth(40) = .02(40^2) - 5(40) + 150 = -18 change in depth = depth(40) - depth(20) = -18 - 58 = -76 change in clock time = 40 - 20 = 20. Ave rate of depth change = change in depth / change in clock time = -76 / 20 = -3.8 **
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RESPONSE --> ok
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21:52:47 What is the average rate of depth change from t = 60 to t = 80?
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RESPONSE --> change in depth is -200 change in clock time is 20 average rate of depth change is -180
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21:54:41 ** depth(60) = .02(60^2) - 5(60) + 150 = -78 depth(80) = .02(80^2) - 5(80) + 150 = -122 change in depth = depth(80) - depth(60) = -122 - (-78) = -44 change in clock time = 40 - 20 = 20. Ave rate of depth change = change in depth / change in clock time = -44 / 20 = -2.2 **
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RESPONSE --> i had everything right until the clerical error in the change in depth. why would the 78 have double negatives?
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21:57:41 describe your graph of y = .02t^2 - 5t + 150
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RESPONSE --> i am getting help with this i have the steps confused but my graph is a parabola with a vertex at -125,0 and crosses the x axis at 124,1 and again at -126,-1
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21:58:04 describe your graph of y = .02t^2 - 5t + 150
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22:00:47 ** The graph is a parabola. y = .02t^2 - 5t + 150 has vertex at x = -b / (2a) = -(-5) / (2 * .02) = 125, at which point y = .02 (125^2) - 5(125) + 150 = -162.5. The graph opens upward, intercepting the x axis at about t = 35 and t = 215. Up to t = 125 the graph is decreasing at a decreasing rate. That is, it's decreasing but the slopes, which are negative, are increasing toward 0.**
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22:02:24 describe the pattern to the depth change rates
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RESPONSE --> they are in equal 20 cm intervals
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22:03:42 ** Rates are -3.8, -3 and -2.2 for the three intervals (20,40), (40,60) and (60,80). For each interval of `dt = 20 the rate changes by +.8. **
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22:08:58 query problem 2. ave rates at midpoint times what is the average rate of depth change for the 1-second time interval centered at the 50 sec midpoint?
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RESPONSE --> i have no idea i cant find this examples in my notes
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22:11:12 ** The 1-sec interval centered at t = 50 is 49.5 < t < 50.5. For depth(t) = .02t^2 - 5t + 150 we have ave rate = [depth(50.5) - depth(49.5)]/(50.5 - 49.5) = -3 / 1 = -3. **
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RESPONSE --> i dont understand where this came from, can you explain this to me?
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22:14:00 what is the average rate of change for the six-second time interval centered at the midpoint.
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RESPONSE --> ?????????
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22:17:12 ** The 6-sec interval centered at t = 50 is 47 < t < 53. For depth(t) = .02t^2 - 5t + 150 we have ave rate = [depth(53) - depth(47)]/(53 - 47) = -18 / 6 = -3. **
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RESPONSE --> ok, this is why i am lost not enough info and examples to know if i am doing the problem right.
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22:17:33 What did you observe about your two results?
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RESPONSE --> I have no clue how to get the variables and this lost me
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22:17:52 ** The two rates match each other, and they also match the average rate for the interval 40 < t < 60, which is also centered at t = 50. For a quadratic function, and only for a quadratic function, the rate is the same for all intervals having the same midpoint. This is a property unique to quadratic functions. **
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23:18:09 query problem 3. ave rates at midpt times for temperature function Temperature(t) = 75(2^(-.05t)) + 25. What is the average rate of depth change for the 1-second time interval centered at the 50 sec midpoint?
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RESPONSE --> ???????????????? i have plugged the values into the equation, I have no idea.
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23:18:45 STUDENT RESPONSE: .46 degrees/minute INSTRUCTOR COMMENT: More precisely .4595 deg/min, and this does not agree exactly with the result for the 6-second interval. Remember that you need to look at enough significant figures to see if there is a difference between apparently identical results.**
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23:19:40 what is the average rate of change for the six-second time interval centered at the midpoint.
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RESPONSE --> dont know
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23:20:23 STUDENT RESPONSE: .46 degrees/minute INSTRUCTOR COMMENT: The 1- and 6-second results might possibly be the same to two significant figures, but they aren't the same. Be sure to recalculate these according to my notes above and verify this for yourself. The average rate for the 6-second interval is .4603 deg/min. It differs from the average rate .4595 deg/min, calculated over the 1-second interval, by almost .001 deg/min. This differs from the behavior of the quadratic. For a quadratic that the results for all intervals centered at the same point will all agree. This is not the case for the present function, which is exponential. Exact agreement is a characteristic of quadratic functions, and of no other type. **
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