Table of Contents
ToggleIntroduction
The specific gravity of soil particles is an important parameter in geotechnical engineering. It is used to calculate various soil properties such as void ratio and degree of saturation. One of the common laboratory techniques for determining the specific gravity is the pycnometer method. This method is applicable for both fine-grained and coarse-grained soils and provides accurate results when proper care is taken during the test.
Theory
The pycnometer method is based on the principle of comparing the mass of a known volume of soil with the mass of an equivalent volume of water. The specific gravity (G) of the soil is calculated using the relation:
Where:
- M1 is the mass of the empty pycnometer.
- M2 is the mass of the pycnometer filled with oven-dried soil.
- M3 is the mass of the pycnometer containing the soil and water.
- M4 is the mass of the pycnometer completely filled with water only.
This method is similar in concept to the density bottle method but uses a larger volume, typically requiring about 200–300 grams of oven-dried soil. It is especially effective for soils with medium to coarse grains, where a significant percentage of particles pass the specified sieve sizes. (In many cases, the exact sieve size criteria will be specified by the particular standard (such as ASTM or IS) used in the testing protocol.)
Equipment and Apparatus
To perform the pycnometer test, the following equipment is required:
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Pycnometer: A glass jar of about 1 liter capacity fitted with a conical brass cap that has a small 6 mm diameter hole. The cap is provided with a washer to ensure no leakage, and marks on the cap and pycnometer ensure consistency in filling.
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Weighing Balance: Accurate to at least 1 gram.
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Glass Rod: For shaking the contents.
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Vacuum Pump: Used to remove entrapped air from the soil-water mixture.
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Oven: For drying the soil sample.
Procedure Used in Determination of Soil Specific Gravity Using the Pycnometer Method
The following step-by-step procedure outlines how to determine the specific gravity using the pycnometer method:
1. Preparation:
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Clean and dry the pycnometer thoroughly.
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Screw the cap tightly and mark the cap and the pycnometer with a vertical line along their axes. This mark ensures that the cap is replaced in the same position each time, keeping the internal volume constant.
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Weigh the empty pycnometer (record this as M1) to the nearest 0.1 g.
2. Soil Sample Preparation:
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Place approximately 200–300 g of oven-dried soil into the pycnometer.
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Replace and tighten the cap, then weigh the pycnometer with the dry soil (record as M2).
3. Adding Water:
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Unscrew the cap and add a sufficient amount of de-aired water to cover the soil.
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Reattach the cap securely.
4. Removing Entrapped Air:
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Shake the pycnometer thoroughly using the glass rod.
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Connect the pycnometer to the vacuum pump to evacuate the entrapped air. For fine-grained soils, maintain the vacuum for about 20 minutes; for coarse-grained soils, about 10 minutes is sufficient.
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After the initial vacuum, disconnect the pump and fill the pycnometer about three-fourths with water.
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Reapply the vacuum for an additional 5 minutes until no air bubbles emerge from the water.
5. Final Weighing:
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Completely fill the pycnometer with water up to the calibration mark.
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Dry the exterior of the pycnometer carefully and weigh it (record this as M3).
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Record the temperature of the contents for accuracy, as temperature variations can affect the density of water.
6. Water Calibration:
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Empty the pycnometer, wash, and dry it.
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Fill it with water only, screw the cap to the mark, dry the exterior, and weigh it (record this as M4).
Observations and Data Recording for Specific Gravity by Pycnometer Metho
| S.No. | Observations and calculations | Determination No. | ||
|---|---|---|---|---|
| 1 | 2 | 3 | ||
| 1. | Pycnometer No. | 1 | 2 | 3 |
| 2. | Room temperature | 26°C | ||
| 3. | Mass of empty pycnometer (M1) | 580 g | ||
| 4. | Mass of pycnometer and dry soil (M2) | 800 g | ||
| 5. | Mass of pycnometer, soil and water (M3) | 1707 g | ||
| 6. | Mass of pycnometer and water (M4) | 1570 g | ||
| 7. | M2 - M1 | 220 g | ||
| 8. | M3 - M4 | 137 g | ||
| 9. | G = (7) (7) - (8) |
2.65 | ||
Precautions for Determination of Soil Specific Gravity Using the Pycnometer Method
To ensure the accuracy and reliability of the test results, consider the following precautions:
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Sample Preparation: The soil sample must be completely free from lumps. If lumps are present, they should be broken down to maintain consistency.
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Entrapped Air: Ensure that all entrapped air is removed using the vacuum pump, as trapped air bubbles can cause errors in the measurement.
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Weighing Accuracy: Use a well-calibrated weighing balance and check its accuracy before starting the test.
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Consistent Volume: Ensure the pycnometer is always filled to the calibration mark for consistent volume during each weighing.
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Temperature Control: Record the temperature of the water/soil mixture, as water density is temperature-dependent.
Conclusion
The pycnometer method is a reliable laboratory technique for determining the specific gravity of soil particles. By carefully following the procedure and taking the necessary precautions, accurate measurements can be achieved. Understanding this method is crucial for further analyses in soil mechanics, such as calculating the void ratio and degree of saturation. This article aims to provide a clear and comprehensive guide for students and practitioners in the field.

