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Plumbing Arithmetic
Summary from RJES
Formulas, Conversions
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CHARLE'S LAW - Constant Pressure
states that at constant pressure, the volume of a gas is directly proportional to its absolute temperature.
V
1
T
1
=
V₁ T₁ =
V
1
T
1
=
V
2
T
2
V₂ T₂
V
2
T
2
BOYLE
'S
LAW
- Constant Temperature
states that at constant temperature, the pressure of a gas is
inversely
proportional to its
volume.
P
1
V
1
=
P_1V_1=
P
1
V
1
=
P
2
V
2
P_2V_2
P
2
V
2
GAY-LUSSAC'S
LAW
-
Constant
Volume
States that the pressure of a gas is directly
proportional
to its temperature when the volume is held
constant.
P
1
T
1
=
P₁ T₁ =
P
1
T
1
=
P
2
T
2
P₂ T₂
P
2
T
2
PERFECT GAS
also known as the ideal gas, describes the behavior of an ideal gas under various conditions.
P
1
V
1
/
T
1
=
P₁V₁/T₁ =
P
1
V
1
/
T
1
=
P
2
V
2
/
T
2
P₂V₂ /T₂
P
2
V
2
/
T
2
1 horsepower
476
Watts
334
Kj kg
Latent heat fusion
required to turn
ice
to liquid
273° K
melting point
of ice
0° K
absolute zero
temperature
4° C
densed
condition of
water
760mm
of Hg= 14.7 psi
standard atmospheric pressure
<'latex>1000 kgm^3</latex>
density of water
1000
k
g
/
m
3
1000 kg/m^3
1000
k
g
/
m
3
density
of water
4.19
k
J
/
k
g
°
C
4.19 kJ/kg°C
4.19
k
J
/
k
g
°
C
specific heat capacity of
water
2
.72
Naperian
Logarithm
1 Celsius
-273.15° Kelvin
Law of
Sines
Arithmetic
Sequence -
nth
term
a
n
=
aₙ =
a
n
=
a
1
+
a₁ +
a
1
+
(
n
−
1
)
∗
(n - 1) *
(
n
−
1
)
∗
d
d
d
Arithmetic Sequence - sum of n terms
S
n
=
Sₙ =
S
n
=
n
/
2
∗
n/2 *
n
/2
∗
(
a
1
+
a
n
)
(a₁ + aₙ)
(
a
1
+
a
n
)
Percentage
% = (part/whole) * 100
part
= (percentage/100) *
whole
whole
= (part/percentage) * 100
Simple Interest
F
=
F=
F
=
P
(
1
+
r
t
)
P(1+rt)
P
(
1
+
r
t
)
Compound Interest
A
=
A =
A
=
P
∗
P *
P
∗
(
1
+
r
/
n
)
n
∗
(1 + r/n)^n*
(
1
+
r
/
n
)
n
∗
t
^t
t
Distance
d
=
d =
d
=
√
(
(
x
2
−
x
1
)
2
+
√((x₂ - x₁)² +
√
((
x
2
−
x
1
)
2
+
(
y
2
−
y
1
)
2
)
(y₂ - y₁)²)
(
y
2
−
y
1
)
2
)
Distance
: point and a
line
d
=
d =
d
=
∣
A
x
0
+
|Ax₀ +
∣
A
x
0
+
B
y
0
+
By₀ +
B
y
0
+
C
∣
/
√
(
A
2
+
B
2
)
C| / √(A² + B²)
C
∣/√
(
A
2
+
B
2
)
Effective Rate
E
R
=
ER=
ER
=
(
1
+
r
/
m
)
m
−
1
(1+r/m)^m-1
(
1
+
r
/
m
)
m
−
1
Force, Pressure, Area
F
=
F=
F
=
P
∗
P*
P
∗
A
A
A
Rise
, Slope, Horizontal distance
R
=
R=
R
=
S
×
H
S×H
S
×
H