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TEST METHOD FOR THE DETERMINATION OF THE
APPARENT SPECIFIC GRAVITY OF SOILS
GEOTECHNICAL TEST METHOD
GTM-14 Revision #2
AUGUST 2015
EB 15-025 Page 1 of 8
GEOTECHNICAL TEST METHOD:
TEST METHOD FOR THE DETERMINATION OF THE
APPARENT SPECIFIC GRAVITY OF SOILS
GTM-14
Revision #2
STATE OF NEW YORK
DEPARTMENT OF TRANSPORTATION
GEOTECHNICAL ENGINEERING BUREAU
AUGUST 2015
EB 15-025 Page 2 of 8
TABLE OF CONTENTS
1. SCOPE .................................................................................................................................3
2. DEFINITION .......................................................................................................................3
3. APPARATUS AND SUPPLIES ..........................................................................................3
4. SAMPLE PREPARATION .................................................................................................4
5. TEST PROCEDURE ...........................................................................................................4
6. PERIODIC MAINTENANCE .............................................................................................6
APPENDIX ......................................................................................................................................8
A. Specific Gravity Conversion Factor - K Factor (Table 1) ................................... A-1
B. Apparent Specific Gravity Determination (Worksheet) ...................................... B-1
C. Procedure for Calibration of the Volumetric Flask for use
in the Determination of the Apparent Specific Gravity of Soils ..........................C-1
EB 15-025 Page 3 of 8
1. SCOPE
1.1 This manual describes the procedure of the New York State Department of
Transportation Geotechnical Engineering Bureau to determine the apparent specific
gravity of a soil. Values presented in this manual without a decimal point or a
tolerance is approximate.
2. DEFINITION
2.1 Specific Gravity: The ratio of the mass in air of a given volume of a material at a
stated temperature to the mass in air of the same volume of gas-free water at a stated
temperature.
3. APPARATUS AND SUPPLIES
3.1 Oven: A thermostatically controlled oven capable of maintaining temperatures of
230±9° F (110±5° C) for drying the hydrometer analysis samples.
3.2 Balance: An AASHTO M-231, Class C balance for weighing the material to be
used in the analysis.
3.3 Thermometer: A thermometer conforming to ASTM 14.01.
3.4 Sieve: A ¾ in. (19.0 mm), ¼ in. (6.3 mm), No. 10 (2.00 mm) or No. 40 (0.425 mm)
sieve conforming to the requirements of AASHTO Designation M-92 (excluding
Column 7 of Table 1, p. 128) and a pan.
3.5 Flask and Rubber Stoppers: Calibrated flasks (refer to Appendix C) of 0.5 qt. (500
mL) and 1.1 qt. (1000 mL) capacities in which to de-air the soil samples and water.
A rubber stopper is required for each flask containing de-aired water or water and
soil to seal the flask in order to minimize the absorption of air by the water or soil
sample.
3.6 Pulverizing Apparatus: A mortar and rubber covered pestle, or similar device as
specified in AASHTO T-87-86, suitable for separating the aggregated soil particles
without reducing the size of the individual grains.
3.7 Desiccator: A desiccator in which to allow the soil samples to cool without
absorbing moisture after the samples have been dried in an oven.
3.8 Funnel: A funnel to aid in transferring the soil sample from the tare to the flask
3.9 Potable Water: A supply of potable water to de-air for filling the calibrated flasks.
3.10 Water Dispenser: A dispenser for de-aired water to wash down the sides of the flask
during the de-airing process.
3.11 De-airing System: One or both of the following de-airing systems:
3.11.1 Method A: Vacuum: For de-airing water and most soils. It is recommended
that two vacuum systems be available to de-air two flasks simultaneously so
as to both save time and to minimize the error introduced by the de-aired
water or soil absorbing the air in the flask.
3.11.1.a Vacuum Pump: A vacuum pump capable of sustaining a vacuum of
at least 27.0 in. (685 mm) Hg at standard temperature and pressure.
EB 15-025 Page 4 of 8
3.11.1.b Filtering Flask: A heavy walled filtering flask with the side opening
attached by plastic or rubber tubing to the vacuum pump and the top
opening attached by plastic or rubber tubing to a stopper to be
inserted in the calibrated flask. The filtering flask acts as a trap to
prevent soil particles from passing into the vacuum pump.
3.11.1.c Safety Cabinet: A rigid enclosure with an access door, made of
Lucite, Plexiglass, or other suitable material, in which to place the
filtering flask and calibrated flask during de-airing. The purpose of
the safety enclosure is for protection in the event of an implosion of
the flask when subjected to the vacuum.
3.11.1.d Vacuum Gauge: A standard vacuum gauge, for measuring the pump
vacuum, capable of measuring the range of 0 to 30 in. (0 to 760 mm)
of Hg.
3.11.2 Method B: Boiling: For de-airing soils that effervesce violently when
subjected to a vacuum.
3.11.2.a Hot Plate: A hot plate on which to heat the soil sample and water to
boiling. When heating, the calibrated flask containing the soil sample
and water should be placed in a pan containing a ½ to 1 in. (12.7 to
25 mm) thick layer of sand to evenly distribute the heat from the hot
plate.
3.11.2.b Glass Funnel: A small glass funnel to be used as a vent cap on the
flask to avoid loss of material when boiling the soil sample.
4. SAMPLE PREPARATION
4.1 Dry the soil sample in an oven at 230±9° F (110±5° C) for at least 12 hours or until
the sample achieves a constant weight, whichever occurs first.
4.2 Place the sample in the desiccator and allow cooling to room temperature.
4.3 Carefully break up the soil agglomerations using the pulverizing apparatus without
reducing the size of the individual grains.
4.4 Separate the sample on the desired sieve size (¾ in. (19.0 mm), ¼ in. (6.3 mm), No.
10 (2.00 mm) or No. 40 (0.425 mm). For material finer than ¼ in. (6.3 mm), 100 g
of material are normally used (200 g for minus ¾ in. (19.0 mm) samples). However,
if sample material is limited, as little as 50 g (100 g for minus ¾ in. (19.0 mm)
samples) may be used.
5. TEST PROCEDURE
5.1 Add sufficient potable water to a 0.5 qt. (500 mL) calibrated flask to saturate the soil
sample to be tested.
Note 1: For a minus ¾ in. (19 mm) sieve sample, use a 1.1 qt. (1000 mL) flask.
EB 15-025 Page 5 of 8
5.2 Thoroughly dry the outside of the flask and the inside of the neck and weigh the
flask and water. Record the weight to the nearest 0.01 g on Form SM 294b Apparent
Specific Gravity Determination, Line 7 (Appendix B).
Form SM 294b uses the International System of Units (g, °C) for recording the
weights (Weight of flask & water, Weight of flask, soil & water, etc.) and
temperature.
5.3 Place a funnel in the flask and add approximately 100 g of the soil sample to the
flask.
Note 2: For a minus ¾ in. (19 mm) sieve sample, add 200 g of the soil sample to the
flask.
5.4 Remove the funnel, clean off the outside of the flask and the inside of the neck and
weigh the flask with the water and soil sample. Record the weight to the nearest
0.01 g on Line 6.
5.5 Wash down the inside neck of the flask using the water dispenser to wash the fines
into the body of the flask.
5.6 De-air the sample by either of the following methods:
Note 3: Some samples may effervesce violently when subjected to a vacuum. These
samples should therefore be de-aired by boiling.
5.6.1 Method A: Vacuum: Place the flask inside the safety cabinet and apply a
vacuum to the flask to de-air the soil sample. Occasionally swirl the flask
gently to facilitate the release of air. For safety considerations, release the
vacuum before swirling the flask. The door of the safety cabinet should be
closed while the flask is subject to the vacuum.
Note 4: If any portion of the sample is splashed above the calibration line, it must
be washed down immediately with de-aired water. If any of the sample is pulled by
the vacuum from the flask, the test is invalidated and must be rerun.
5.6.2 Method B: Boiling: Insert a small glass funnel in the neck of the flask to
prevent the loss of any of the soil sample. Heat the sample to boiling using
the hotplate and the pan containing the ½ to 1 in. (12.7 to 25 mm) thick layer
of sand. Boil the sample for one half hour, then cool to room temperature.
Note 5: If any portion of the sample is splashed above the calibration line, it must
be washed down immediately with de-aired water.
EB 15-025 Page 6 of 8
5.7 Fill a 1.1 qt. (1000 mL) flask to approximately the middle of the flask bulb with
portable water at about 86° F (30 ° C). Apply the vacuum to the flask to de-air the
water. Occasionally swirl the flask to facilitate the release of the air. The door of the
safety cabinet should be closed while the flask is subject to the vacuum.
5.8 When the water or soil and water sample has been de-aired, remove the flask from
the vacuum. De-airing is adequate when no bubbles can be seen after gently swirling
the flask.
Note 6: Flasks containing a de-aired soil sample or de-aired water must be kept
stoppered to minimize the absorption of air.
5.9 Using de-aired water, fill the flask containing the de-aired soil sample to the point
that the bottom of the meniscus is at the calibration line. Carefully add the de-aired
water by pouring down the side of the flask to avoid mixing air into the sample.
5.10 Dry the outside of the flask and the inside of the neck without disturbing the
meniscus. Weigh the flask with the soil and water to the nearest 0.01 g and record
the weight on Line 12.
5.11 Place the thermometer in the flask, read the temperature to the nearest 0.1° C and
record the value on Line 9.
5.12 Determine the Calibrated Flask Reading from the appropriate Table of Weights for
Calibrated Flask and Water vs. Temperature for the flask used (refer to Appendix C)
and record the value on Line 10.
5.13 Round the temperature to the nearest 0.5° C and determine the K Factor from Table
1 (Appendix A). Record the value of the K factor on Line 15.
5.14 Add the weight of dry soil (Line 8) and the weight of the flask and water from the
appropriate table (Line 10) and enter the result on Line 11.
5.15 Find the weight of displaced water by subtracting the weight of the flask, water and
soil (Line 12) from the calibrated weight of the flask and water plus soil (Line 11).
Enter the result on Line 13.
5.16 Calculate the specific gravity by dividing the weight of dry soil (Line 8) by the
weight of displaced water (Line 13) and enter the value on Line 14.
5.17 Correct the specific gravity to 68° F (20° C) by multiplying the specific gravity
(Line 14) by the K factor (Line 15) and enter the result on Line 16.
6. PERIODIC MAINTENANCE
6.1 Following each test:
6.1.1 Wash and air-fry the flask used in the test. Use care to avoid scratching the
inside of the flask with the wire cleaning brush.
6.1.2 Inspect the flasks for cracks or defects. Discard damaged or defective flasks.
6.1.3 Return the flasks to the storage cabinet to reduce the possibility of damage.
6.2 Daily:
6.2.1 Drain the accumulated water from the vacuum pump. Open the stopcock and
drain the fluid until only oil flows out.
EB 15-025 Page 7 of 8
6.2.2 Check the oil level and fill as needed. The oil level should be slightly below
the fill line shown on the window to allow for expansion of the soil when
the pump is warm.
6.3 Weekly:
6.3.1 Wipe the oil and grime from the surface of the vacuum pump.
6.3.2 Check the vacuum of the pump. Attach a vacuum gauge to the suction line
and verify the vacuum to be at least 27.0 in. (685 mm) of Hg.
6.4 Periodically:
6.4.1 Check the condition of the plastic or rubber vacuum tubes and replace when
necessary.
6.4.2 Clean the filtering flask as needed.
6.4.3 Check the accuracy of the balance and recalibrate if necessary.
6.4.4 Check the dry weight of the calibrated flask. If the dry weight varies by more
than 0.01 g from the weight used in the calibration, check the calibration of
the flask.
EB 15-025 Page 8 of 8
APPENDIX
APPENDIX A
EB 15-025 A-1
Specific Gravity Conversion - K Factor Temp (° C) K Temp (° C) K
16 1.0007 23.5 0.9992
16.5 1.00065 24 0.9991
17 1.0006 24.5 0.9990
17.5 1.0005 25 0.9989
18 1.0004 25.5 0.99875
18.5 1.0003 26 0.9986
19 1.0002 26.5 0.99845
19.5 1.0001 27 0.9983
20 1.0000 27.5 0.99815
20.5 0.9999 28 0.9980
21 0.9998 28.5 0.99785
21.5 0.9997 29 0.9977
22 0.9996 29.5 0.99755
22.5 0.9995 30 0.9974
23 0.9993 30.5 0.99725
Table 1
APPENDIX B
EB 15-025 B-1
APPENDIX C
EB 15-025 C-1
Procedure for the Calibration of the Volumetric Flask for use in the
Determination of the Apparent Specific Gravity of Soils
TABLE OF CONTENTS
1. SCOPE .............................................................................................................................C-2
2. CALIBRATION PROCEDURE ......................................................................................C-2
3. COMPUTATIONS FOR FLASK CALIBRATION CURVE ..........................................C-3
4. FLASK CALIBRATION WORKSHEET (Table 1) ........................................................C-4
5. FLASK VOLUMETRIC TEMPERATURE CORRECTION CURVE (Figure 1) ..........C-5
6. GRAPH FOR COMPUTED CALIBRATION CURVE (Figure 2) .................................C-6
7. TABLE OF WEIGHTS FOR CALIBRATION FLASK
AND WATER vs. TEMPERATURE (°C) (Table 2) ......................................................C-7
APPENDIX C
EB 15-025 C-2
Procedure for the Calibration of the Volumetric Flask for use in the
Determination of the Apparent Specific Gravity of Soils
1. SCOPE
1.1 This appendix describes the procedure of the New York State Department of
Transportation Geotechnical Engineering Bureau to calibrate the volumetric flask
used in the determination of the apparent specific gravity of a soil. Values presented
in the appendix without a decimal point or a tolerance is approximate.
2. CALIBRATION PROCEDURE
2.1 Inspect the flask to be calibrated to ensure that it is free of cracks and imperfections
in the glass. Assign the flask a unique alphabetic or numeric identification and
permanently mark the designated characters on the flask.
2.2 Wash the flask with soap and water. Rinse and drain the flask and place in a 230° F
(110° C) oven to dry overnight.
2.3 Remove the flask from the oven and allow cooling to room temperature. Make
certain there is no moisture on the inside or outside of the flask. Weigh the dry flask
and record the weight to the nearest 0.01 g on the Flask Calibration Worksheet
(Table 1), Line 3 and Line 11, and on the graph for the computed Calibration Curve
(Figure 2).
2.4 Fill a 1.1 qt. (1000 mL) flask to approximately the middle of the bulb with potable
water at a temperature such that the temperature of the water after de-airing is
between 64° and 72° F (18° and 22° C). The de-airing process causes the water
temperature to decrease approximately 9° F (5° C) in approximately 15 minutes of
operation.
2.5 Fill the flask to be calibrated with de-aired water so that the bottom of the meniscus
is at the calibration line. Dry the outside of the flask and the inside of the neck. Use
care when drying the inside of the neck to avoid touching the meniscus. Weigh the
flask and water and record the weight to the nearest 0.01 g on the Flask Calibration
Worksheet, Line 2.
2.6 Place the thermometer in the flask, read the temperature to the nearest 0.1° C and
record the value on Line 1.
2.7 Subtract the weight of the dry flask (Line 3) from the weight of the flask and water
(Line 2) and enter the result on Line 4.
2.8 Use the Flask Volumetric Temperature Correction Curve (Figure 1) to determine the
value of (1+3tE)G1 for the temperature recorded on Line 1. Enter the appropriate
value on Line 5.
Note: The flask is calibrated by the manufacturer at 68° F (20° C). Weights at
temperatures other than 68° F (20° C) must be corrected to agree with the weight
corresponding to the volume of water in the flask at 68° F (20° C). The weight of
water in grams equals the volume of water in cubic centimeters at 39° F (4° C).
APPENDIX C
EB 15-025 C-3
Above 39° F (4° C), the volume of the flask and water will expand in accordance
with (1+3tE)G1.
2.9 Divide the weight of water (Line 4) by the value of (1+3tE)G1 (Line 5) to obtain the
volume of the flask. Enter the value on Line 6.
2.10 Repeat Section 2.4 through 2.9 until five values of the volume of the flask (Line 6)
are within 0.1 cc.
3. COMPUTATION FOR FLASK CALIBRATION CURVE
3.1 Average the five values of the volume of the flask obtained from Section 2.10 and
enter the result on Line 9.
3.2 Convert the average volume of the flask to the average weight of water in the flask
at the given temperatures of 54°, 61°, 68°, 75°, 82° and 90° F (12°, 16°, 20°, 24°,
28° and 32° C) (Line 7) by multiplying the value of (1+3tE)G1 at the given
temperature (Line 8) times with average volume of the flask (Line 9). Enter the
result in the appropriate column on Line 10.
3.3 Add the weight of the water at the given temperature (Line 10) to the weight of the
dry flask (Line 11) and enter the sum in the appropriate column on Line 12.
3.4 Plot the values of the weight of the flask and water (Line 12) versus the
corresponding values of temperature (Line 7) on the graph for the computed
Calibration Curve (Figure 2).
3.5 The values for the weight of the flask and water can be obtained directly from the
Calibration Curve, or the Calibration Curve can be used to generate a table of values
for the weight of the flask and water for temperatures from 61° to 82° F (16° to 28°
C) in 1/10° increments (Table 2).
APPENDIX C
EB 15-025 C-4
Table 1
APPENDIX C
EB 15-025 C-5
Figure 1
APPENDIX C
EB 15-025 C-6
Computed Calibration Curve Figure 2
APPENDIX C
EB 15-025 C-7
TABLE OF WEIGHTS FOR CALIBRATED FLASK AND WATER VS. TEMPERATURE (°C)
(CALIBRATED FLASK READING)
Comp. by:________________
FLASK DESIGNATION ____________ Check by:________________
Temp (°C)
Wgt. Of
Flask and
Water
Temp (°C)
Wgt. Of
Flask and
Water
Temp (°C)
Wgt. Of
Flask and
Water
16.0 20.0 24.0
.1 .1 .1
.2 .2 .2
.3 .3 .3
.4 .4 .4
.5 .5 .5
.6 .6 .6
.7 .7 .7
.8 .8 .8
.9 .9 .9
17.0 21.0 25.0
.1 .1 .1
.2 .2 .2
.3 .3 .3
.4 .4 .4
.5 .5 .5
.6 .6 .6
.7 .7 .7
.8 .8 .8
.9 .9 .9
18.0 22.0 26.0
.1 .1 .1
.2 .2 .2
.3 .3 .3
.4 .4 .4
.5 .5 .5
.6 .6 .6
.7 .7 .7
.8 .8 .8
.9 .9 .9
19.0 23.0 27.0
.1 .1 .1
.2 .2 .2
.3 .3 .3
.4 .4 .4
.5 .5 .5
.6 .6 .6
.7 .7 .7
.8 .8 .8
.9 .9 .9
Table 2