In West Texas, water is extremely important. The following data represent pH levels in ground water for a random sample of 102 West Texas wells. A pH less than 7 is acidic and a pH above 7 is alkaline. Scanning the data, you can see that water in this region tends to be hard (alkaline). Too high a pH means the water is unusable or needs expensive treatment to make it usable.† These data are also available for download at the Companion Sites for this text. For convenience, the data are presented in increasing order. (a) Make the frequency table. (Round your relative frequencies to three decimal places.) (b) Make the histogram.   (c) Make the relative-frequency histogram.

Linear Algebra: A Modern Introduction
4th Edition
ISBN:9781285463247
Author:David Poole
Publisher:David Poole
Chapter7: Distance And Approximation
Section7.3: Least Squares Approximation
Problem 31EQ
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In West Texas, water is extremely important. The following data represent pH levels in ground water for a random sample of 102 West Texas wells. A pH less than 7 is acidic and a pH above 7 is alkaline. Scanning the data, you can see that water in this region tends to be hard (alkaline). Too high a pH means the water is unusable or needs expensive treatment to make it usable.† These data are also available for download at the Companion Sites for this text. For convenience, the data are presented in increasing order.

(a) Make the frequency table. (Round your relative frequencies to three decimal places.)
(b) Make the histogram.
 
(c) Make the relative-frequency histogram.
In West Texas, water is extremely important. The following data represent pH levels in ground water for a random sample
of 102 West Texas wells. A pH less than 7 is acidic and a pH above 7 is alkaline. Scanning the data, you can see that water
in this region tends to be hard (alkaline). Too high a pH means the water is unusable or needs expensive treatment to make
it usable.t These data are also available for download at the Companion Sites for this text. For convenience, the data are
presented in increasing order.
x: pH of Ground Water in 102 West Texas Wells
7.0 7.0 7.0 7.0 7.0 7.0 7.0 7.0 7.1 7.1 7.1 7.1
7.1 7.1 7.1i 7.1 7.1 7.1 7.2 7.2 7.2 7.2 7.2 7.2
7.2 7.2 7.2 7.2 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.3
7.3 7.3 7.3 7.4 7.4 7.4 7.4 7.4 7.4 7.4 | 7.4 7.4
7.5 7.5 7.5 7.5 7.5 7.5 7.5 7.5 7.6 7.6 7.6 7.6
7.6 7.6 7.6 7.6 7.6 7.7 7.7 7.7 7.7 7.7 7.7 7.8
7.8 7.8 7.8 7.8 7.9 7.9 7.9 7.9 7.9 8.0 8.1 8.1
8.1 8.1 8.1
8.1 8.1 8.2 8.2 8.2 8.2 8.2 8.2 8.2
8.4 8.5 8.6 8.7 8.8 8.8
Make a frequency table, histogram, and relative-frequency histogram using five classes. Recall that for decimal data, we
"clear the decimal" to determine classes for whole-number data and then reinsert the decimal to obtain the classes for the
frequency table of the original data.
Make the frequency table. (Round your relative frequencies to three decimal places.)
Relative
Cumulative
Class Limits
Class Boundaries
Midpoint Frequency
Frequency
Frequency
Transcribed Image Text:In West Texas, water is extremely important. The following data represent pH levels in ground water for a random sample of 102 West Texas wells. A pH less than 7 is acidic and a pH above 7 is alkaline. Scanning the data, you can see that water in this region tends to be hard (alkaline). Too high a pH means the water is unusable or needs expensive treatment to make it usable.t These data are also available for download at the Companion Sites for this text. For convenience, the data are presented in increasing order. x: pH of Ground Water in 102 West Texas Wells 7.0 7.0 7.0 7.0 7.0 7.0 7.0 7.0 7.1 7.1 7.1 7.1 7.1 7.1 7.1i 7.1 7.1 7.1 7.2 7.2 7.2 7.2 7.2 7.2 7.2 7.2 7.2 7.2 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.3 7.4 7.4 7.4 7.4 7.4 7.4 7.4 | 7.4 7.4 7.5 7.5 7.5 7.5 7.5 7.5 7.5 7.5 7.6 7.6 7.6 7.6 7.6 7.6 7.6 7.6 7.6 7.7 7.7 7.7 7.7 7.7 7.7 7.8 7.8 7.8 7.8 7.8 7.9 7.9 7.9 7.9 7.9 8.0 8.1 8.1 8.1 8.1 8.1 8.1 8.1 8.2 8.2 8.2 8.2 8.2 8.2 8.2 8.4 8.5 8.6 8.7 8.8 8.8 Make a frequency table, histogram, and relative-frequency histogram using five classes. Recall that for decimal data, we "clear the decimal" to determine classes for whole-number data and then reinsert the decimal to obtain the classes for the frequency table of the original data. Make the frequency table. (Round your relative frequencies to three decimal places.) Relative Cumulative Class Limits Class Boundaries Midpoint Frequency Frequency Frequency
Make the histogram.
40
0.4
В
0.35
35
30
0.3
0.25
20
0.2
15
0.15
10
0.1
0.05
6.95
7.35
7.75
8.15
8.55
8.95
6.95
7.35
7.75
8.15
8.55
8.95
pH Level
pH Level
40
0.4
35
0.35
30
0.3
0.25
0.2
0.15
0.1
5
0.05
6.95
7.35
7.75
8.15
8.55
8.95
6.95
7.35
7.75
8.15
8.55
8.95
pH Level
pH Level
Make the relative-frequency histogram.
0.4
0.4
0.35
0.35
0.3
0.3
0.25
0.25
0.2
0.2
0.15
0.15
0.1
0.1
0.05
0.05
6.95
7.35
7.75
8.15
8.55
8.95
6.95
7.35
7.75
8.15
8.55
8.95
pH Level
рH Level
40
40
35
35
30
30
10
10
5
5
6.95
7.35
7.75
8.15
8.55
8.95
6.95
7.35
7.75
8.15
8.55
8.95
pH Level
pH Level
Frequency
Frequency
Frequency
Frequency
Frequency
Frequency
Frequency
Frequency
Transcribed Image Text:Make the histogram. 40 0.4 В 0.35 35 30 0.3 0.25 20 0.2 15 0.15 10 0.1 0.05 6.95 7.35 7.75 8.15 8.55 8.95 6.95 7.35 7.75 8.15 8.55 8.95 pH Level pH Level 40 0.4 35 0.35 30 0.3 0.25 0.2 0.15 0.1 5 0.05 6.95 7.35 7.75 8.15 8.55 8.95 6.95 7.35 7.75 8.15 8.55 8.95 pH Level pH Level Make the relative-frequency histogram. 0.4 0.4 0.35 0.35 0.3 0.3 0.25 0.25 0.2 0.2 0.15 0.15 0.1 0.1 0.05 0.05 6.95 7.35 7.75 8.15 8.55 8.95 6.95 7.35 7.75 8.15 8.55 8.95 pH Level рH Level 40 40 35 35 30 30 10 10 5 5 6.95 7.35 7.75 8.15 8.55 8.95 6.95 7.35 7.75 8.15 8.55 8.95 pH Level pH Level Frequency Frequency Frequency Frequency Frequency Frequency Frequency Frequency
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