Title | Evaporation loss of Hydrocarbon in Handling Petroleum |
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132 Evaporation Loss of Hydrocarbon in Handling Petroleum* by Ikutoshi Matsumura** Summary: Evaporation lossesof hydrocarbonsfrom various sources, such as refinery plants, oil terminals and gas stations, were studied. A correlation involvingthe volumeof discharged gas, temperatureand hydrocarbonconc...
132
Evaporation
Loss of Hydrocarbon by Ikutoshi
in Handling
Petroleum*
Matsumura**
Summary: Evaporation lossesof hydrocarbonsfrom various sources, such as refinery plants, oil terminals and gas stations, were studied. A correlation involvingthe volumeof discharged gas, temperatureand hydrocarbonconcentrationwas derivedfor crude oil and petroleumproducts. These gas emission sourceswere classified according to their mode of evaporation. As a result, hydrocarbonemissionfactors in terms of annual mean value were obtainedfor various emissionsources,such as cone and floating roof tanks, loading tankers, tank trucks and gas stations; and also the hydrocarbonemissionfactorsfar crudeoil and suchpetroleumproductsas naphtha, gasoline, kerosene,diesel oil and fuel oil. The hydrocarbonemissionfactors obtained in this study were smaller than thosepresented by the U. S. EPA. The calculated hydrocarbonemissionfactor for loading a tanker which was calculatedfor the first time, was less than 1/5 of that for loading a tank truck. The hydrocarbonemission factor for loading various kinds of vesselswith keroseneand diesel oil was about 1/500 of that for loading the same types of vesselswith gasoline. 1
2
Introduction
In Japan, photochemical smog began to appear several years ago, but its causes are still not clearly known. As a preventive measure for such photochemical smog, it seems necessary to prevent discharge of hydrocarbons which were regarded as one of the major causes. But quantitative measurements of hydrocarbons from stationary sources had not been made in Japan. In the U. S. A., API (American Petroleum Institute) investigated evaporation losses of hydrocarbons from cone roof tanks1),2), floating roof tanks3), gas stations4) and transportation facilities5),6) from 1957 to 1963, and the U. S. EPA7) (Environmental Protection Agency) calculated a HC (Hydrocarbon) emission factor based on the results of API investigation. But the HC emission factor proposed by the U. S. EPA would not necessarily be applicable to the cases in Japan, because the climate and the surrounding conditions in Japan are different from those in the U. S. A., and the object facilities for the EPA investigation are also different. Therefore, in this paper a study of evaporation losses of hydrocarbons from refinery plants, oil terminals and gas stations is presented. HC emission factors were obtained for storage and transport of crude oil and petroleum products such as naphtha, gasoline, kerosene, diesel oil and fuel oil. * **
Received July 16, 1974 Nippon Oil Co ., Ltd. (3-12, 1-chome, bashi, Minato-ku, Tokyo 105)
Method
2.1
and
Investigated
Facilities
Method
In order to calculate the HC emission factor, the volume of discharged gas and HC concentration of the gas were measured for each source. In measuring the gas volume, the gas outlet such as a breathing valve and hatch were closed so that discharging gas could be conducted to an anemometer, which had an inlet of 4 in. diameter and was capable of measuring a gas velocity as low as 0.2 M/S. The
gas
volume
the cross sectional the velocity of the
was
obtained
by
multiplying
area of the anemometer by gas stream. The gas sampled
in a 100ml syringe at the gas outlet was brought to the laboratory and analyzed by gas chromatography
with
gaseous HC ard normal with
6
FID.
The
component paraffin,
carbons
were
equivalents and those and so on. 2.2
Investigated
concentration
of
each
was calculated as standthat is, all hydrocarbons calculated
with
5 carbons
as
n-hexane
as n-pentane
Facilities
Investigation was carried out throughout 1973 at refineries, oil terminals and gas stations located mainly in Yokohama but also those located in various other places in Japan. HC emissions from following facilities were investigated. (1)
Floating-roof
tank:
nominal
capacity
3,000
∼100,000kl
Nishi-shin-
(2)
Cone-roof
tank:
nominal
capacity
1,300∼
18,000kl
Bulletin of The Japan Petroleum Institute
Matsumura:
Evaporation
Loss of Hydrocarbon
in Handling
Petroleum
133
(3) Underground tank at a gas station: nominal capacity 10kl (4)
Tanker:
loading
(5) Tank truck: (6)
Tank
(7)
Automobile:
3
car:
Results
capacity
1,800∼5,000kl
loading capacity 2kl/l hatch loading
capacity
gasoline
and
40∼58kl
tank
capacity
40∼60l
Discussion
3.1 Evaporation Loss from Storage Tanks To calculate the quantity of HC emission from a storage
tank,
the
gas
sources
were
according to their mode of evaporation concentrations, and the HC emission breathing and were obtained. 3.1.1
working
Cone
Roof
latile
Petroleum
losses
Tank
classified and HC factors for
of various
for
Storage
tanks of
Fig.
1
Discharged Gas Volume vs. Tank for Breathing of Cone Roof Tanks
Capacity
Fig.
2
HC Concentration of Discharged Gas of Cone Roof Tanks vs. Atmospheric Temperature
Vo-
(1) Breathing Loss Factors breathing
affecting
the
from
cone
a
of oil, temperature HC emission factor relation emitted.
between
quantities roof
of emission
tank
and tank was obtained
these
factors
are
the
by kind
capacity. The from the cor-
and
the
quantities
(a) Seasonal variation of discharged gas volume and discharging time from tanks From the investigation of a crude oil tank having a capacity of 18,000kl, it was noticed that discharge and intake of the gas were caused by temperature difference during the day, and it was found that the emission of hydrocarbons was accompanied by the discharge of the gas in the tank. Therefore, the discharged gas volume from the tank was measured for a period of one year. The results obtained were in a range from 80m3/ hr to 150m3/hr and were not depending on the seasons. It is concluded that the amount of discharged gas by breathing depends on the daily temperature difference and not on the average temperature. The average daily temperature difference in
winter.
tank in
be
in
The
with
and
pointed
discharged
its HC
is 7℃ discharge
temperature
summer
perature, depends
Yokohama
out
of increase
7∼8hrs
that
in
in
HC
gas depends
summer the
gas took
winter.
and
on
the atmospheric
and that the amount on both the discharged
should
of
the tem-
of HC emission gas volume and
concentration.
(b) Tank capacity and discharged gas volume The correlation between tank capacity, V (kl), and discharged gas volume, Q (m3/hr), by breathing is shown in Fig. 1. An empirical equation Volume
16, No. 2, November
1974
Q=K1V2/3 where
K1 is the
constant
(2) depending
on
oil pro-
perties as follows; Gasoline: K1G=0.20 Crude oil: K1C=0.16 Light naphtha: K1L=0.21
the
10∼11hrs
concentration
Thus
9℃
from
It
between Q and V is obtained as follows;
(c)
HC concentration of the discharged gas
HC
concentration
a cone
roof tank
during
the
The the
day,
although
correlation
perature
T
From
between
(℃)
discharged
and gas
Fig.
concentration is expressed
of the
discharged
by breathing
the
C (%)
2, the
it changes the HC
constant
in
between
and the atmospheric as follows;
K2 is the
seasonally. tem-
concentration
is shown
correlation
from
constant
atmospheric
LogC=0.017T+LogK2 C=K2 exp (0.039T) where
gas
is almost
depending
Fig.
the
of 2.
HC
temperature
(3) (4) on oil pro-
Matsumura:
134
Table
1
HC
Vapor
Composition
Pressure Weight of
of
and Each
Discharged
Mean Kind
Gas,
Loss of
Reid
Molecular of Oil
Fig.
3
Table
Tank Capacity vs. HC Emission Breathing of Cone Roof Tanks
2
Emission Roof
perties
Evaporation
Factor Tank
of
Breathing
Factor
from
a
for
Cone
(kg/day・tank)
as follows;
Gasoline: Crude oil: Light
K2G=16 K2C=12
naphtha:
K2L=21
(d)
HC emission factor of breathing from cone roof tanks After multiplying the discharged gas volume shown in equation (2) by the HC concentration shown in equation (4), and converting the concentration unit by using the mean molecular weight of HC, the HC emission in weight per unit time is obtained as shown in Table 1. Thus,
where
the
following
equation
F: HC emission in weight per unit time (kg/hr) V: Tank capacity (kl) T:
Atmospheric
M:
Mean
temperature
molecular
discharged t:
K1, K2: The annual time day
of the
depending
between
average
discharged
factor
the
annual and gas
factors
of breathing
shown
in Table
tank
capacity
in Fig.
breathing
average
30℃.
loss from
gas
(℃)
Fig.
4
Some
in daytime
per
temperature HC
Q=1+0.16P(m3/kl
and
3, where
of
Discharged Gas Volume vs. Reid sure, for Filling one Kiloliter Product in Cone Roof Tanks
Vapor PresPetroleum
ferent Reid vapor pressures P (kg/cm2), are shown in Fig. 4. The relation between P and Q is expressed as follows;
on oil properties
temperature
average
annual is
discharged
is shown
atmospheric
is 18℃,
(℃)
of HC in the
gas
Constants
emission
is 9hrs.,
weight
Temperature
correlation
the HC
is derived
filling)
(6)
Multiplying the HG concentration in equation (4) by the discharged gas volume in equation (6), the HG emission factor of filling a cone roof tank is expressed as follows;
emission
a cone roof tank
are
2.
(2) Filling Loss When a cone roof tank is filled with one kiloliter of petroleum, more than one cubic meter of gas is discharged, because of evaporation of the petroleum. The discharged gas volumes Q (m3/kl) for filling one kiloliter of petroleums having dif-
where
The
F: HC emission factor of filling a cone roof tank (kg/kl filling) P: Reid vapor pressure (kg/cm2) T, M, t, K2: Same as equation (5)
correlation
between
atmospheric
temperature
Bulletin of The Japan Petroleum Institute
Hydrocarbon
in Handling
135
Petroleum
under
the following Storing
conditions;
product:
Light
naphtha
Reid vapor pressure: Atmospheric
temperature:
Surface
the
the
roof:
50℃
pontoon: the
under
38℃,
the
the
beneath
temperature to
of
under
Temperature
rises
32.8℃
temperature
Temperature
As
0.95kg/cm2
the
31℃
roof:
40℃
pontoon
average
occasionally
rate
of
emission
of
HC becomes 50m3/hr. Secondly a gasoline with 0.68kg/cm2 Reid vapor pressure was measured under the following conditions; Surface
Fig.
5
HC Emission Factor vs. Atmospheric rature for Filling Cone Roof Tanks
Table
3
HC Emission Factors Cone Roof Tank
a
temperature
average
of
18℃
temperature
of
3 shows
and the
30℃.
Table
3.1.2
Floating
Roof
the
Volatile
Petroleum
for
the
results
Tanks
of
of
and easily
is emitted,
and
ノ
annual
a
by direct
evaporated.
discharged
conduction
Thus
through
of
HC vapor a breathing
summer,
emitted
on the
emission.
quantities a floating
(1)
The
petroleum
wall
remaining is emitted.
temperature
of HC
of
emitted.
emission
crease
in
Volume
15, No. 2, November
the
was
the
10∼15m3/hr
temperature
roof,
the
tem-
and the atmospheric with regard to the It was
vapor
the
45℃,
tempcrature
the
of
average
HC
there of
rate
emission
are
the
44
roof
under 1974
found for
the
that 1℃
HC in-
pontoon
60℃
of for
15m3/hr
of
the
of
gas
is 20,600
days
is
above
when
the
50℃
in
the
the for
roof
is over
temperature
the
average
60℃ of
rate
of
the gas
テ
The
annual
kg/year・tank, surface a
Breathing Loss the
amount where
temperature
gas,
サ
The
of these two cases from determined.
perature under the pontoon temperature were measured amount
internal
vapor
of HC emissions roof tank were
First,
65℃,
to
Gasoline tank (Reid vapor pressure 0.68 kg/cm2, tank capacity 5,000kl) The HC emission factor, 75kg/day.tank, was obtained by using the following values: 100 % for HC concentration, 68 for the mean molecular weight of HC, 2hrs/day for the period when in
of the HC
for for
temperature
of the
part and
50℃.
to
year.
roof lowers
evaporates
roof
the
50℃
50m3/hr
kg/year・tank,
surface
wall
40
サ
the
tank is exposed.
60
emission.
valve. On the other hand, when withdrawing the petroleum from a floating roof tank, the and
roof
pontoon
(b)
the roof is heated
solar heat
summer, gas,
surface
Storage
When storing petroleums such as naphtha, gasoline etc. in a floating roof tank, the petroleum beneath
in
emitted
The
gas
obtained.
for
beneath
50℃
annual
discharged
Temperature
the
the
(a) Light naphtha tank (Reid vapor pressure 0.95kg/cm2, tank capacity 5,000kl) The HC emission factor, 468kg/day.tank, was obtained by using the following values: 100% for HC concentration, 62 for the mean molecular weight of HC, 4hrs/day for the period when the surface temperature of the roof is above
and HC emission factor in equation (7) is shown in Fig. 5. From Fig. 5, average HC emission factors were obtained for annual average atmospheric
of
under
The average rate of HC emission was 15m3/hr. Calculation of HC emission factor was made using the above data.
Tempe-
of Filling
temperature
Temperature
amount
of
where
there
temperature
of
the
HC
emission
are
30
roof
days
is above
is 2,230 when 6...