Answer:
2/1
Step-by-step explanation:
get the first part of each fraction to something divisible by the second part
4· 3=12/6
1· 3=3/3
12÷2= 23÷3= 1
2/1
Answer:
Correct answer is A 2:1
Step-by-step explanation:
When writing a unit rate the denominator is always 1
If you want to obtain a unit rate you divide both quantities by the second one.
what is a unit rate?
A unit rate means a rate for one of something. We write this as a ratio with a denominator of one. For example, if you ran 70 yards in 10 seconds, you ran on average 7 yards in 1 second. Both of the ratios, 70 yards in 10 seconds and 7 yards in 1 second, are rates, but the 7 yards in 1 second is a unit rate.
A. To be accurate, it must be able to give consistent measurements
of a quantity
B. To be accurate, it must be able to make measurements using very
small units.
C. To be accurate, it must be able to make measurements that are
close to the actual value.
D. To be accurate, it must be able to make measurements using very
large units.
M
Characteristics of a scientific measuring tool consist of:
Measure Ability
Usability
Validity
Reliability
Practicability
Essentially the measuring tool needs to be accurate.
Looking at the options, the answer that fulfills these requirements is Option A.
Best of Luck!
Answer:
I want to say your answer is option B.
A. -23
B. 9
C. -11
D. 3
Answer:
B
Step-by-step explanation:
To find f(- 2) substitute x = - 2 into f(x)
f(- 2) = - 2(- 2)³ + (- 2)² + 4(- 2) - 3
= - 2(- 8) + 4 - 8 - 3
= 16 + 4 - 8 - 3
= 9 → B
The current when the resistance is 10 ohms is 24 amps
Variations are simply data that change in values (i.e. not constant)
The types of variations are:
From the complete question (see attachment), we have the following highlights
An inverse variation is represented as:
Where k represents the constant of variation.
The above equation can be rewritten as:
So, we have:
When the resistance is 10 ohms, we have:
Divide both sides by 10
Rewrite the above equation as:
Hence, the current when the resistance is 10 ohms is 24 amps
Read more about inverse variation at: