Soil Compaction and Properties for Construction Planning
Fundamentals of Soil Phase Diagrams and Properties
Definition of Phase Diagram: A phase diagram is a schematic and simplified diagram showing the components of a specific material (e.g., concrete consists of cement, water, sand, gravel, and additives). It is used to analyze the properties and volumetrics of a material.
Soil Components: A typical soil sample collected from a site consists of three key components: * Solids: The actual soil particles. * Water: Moisture contained between the particles. * Air: Gas occupying the voids between particles.
Phase Diagram Notation (Weights): Typically represented on the right-hand side of the diagram. * : Weight of solids. Also known as the "oven dry weight." * : Weight of water. * : Weight of air, which is mathematically treated as . * (or ): Total weight or "in situ weight" ().
Phase Diagram Notation (Volumes): Typically represented on the left-hand side of the diagram. * : Volume of solids. * : Volume of water. * : Volume of air. * (or ): Total volume of the sample (). * : Volume of voids (), though this is used less frequently in primary compaction calculations.
Determining Weights: * To get the Total Weight (): Take the in situ sample and weigh it immediately on a balance. * To get the Weight of Solids (): Place the sample in an oven at a specific temperature for eight hours. Weigh the sample afterward; the result is the oven dry weight.
Key Soil Density and Moisture Equations
Unit Weight/Density (): Generic term for mass over volume (). In soil mechanics, there are two distinct types of density used to evaluate compaction.
Equation 1: Moisture Content ( or ): * Formula: * Definition: The weight of water divided by the weight of solids. * Warning: It is not water weight divided by total weight. * Representation: Always expressed as a decimal between and in calculations.
Equation 2: Wet Density (): * Formula: * Definition: Includes everything—solids, water, and air—using the total weight in its natural state.
Equation 3: Dry Density (): * Formula: * Definition: Includes ONLY the weight of the dry soil particles divided by the total volume of the sample. This is the primary indicator of soil compaction.
Equation 4: Relationship between Wet and Dry Density: * Formula: * Utility: This allows for the calculation of dry density without an oven-drying process, provided the moisture content is known.
Illustrative Density Examples
Example 1: Moisture Content Calculation * Data: In situ weight = , Oven dry weight = . * Step 1: Identify and . * Step 2: Calculate water weight: . * Step 3: Moisture content: .
Example 2: Density and Dry Density Calculation * Data: In situ weight () = , Moisture content () = , Total Volume () = . * Wet Density: . * Dry Density: .
Principles of Soil Compaction
Definition: Compaction is the application of mechanical energy to soil to remove air between soil particles, resulting in a more stable foundation.
Phase Diagram Transformation: During compaction, mechanical energy reduces the volume of air (). Because air has no weight, the total weight remains the same, but the total volume () decreases.
Impact on Dry Density: Since , a decrease in volume due to compaction causes an increase in dry density.
Ultimate Objective: In construction, the goal is to maximize the dry density to ensure adequate compaction and minimize future settlement.
The Optimization Problem: * If soil is too dry (minimize moisture), it is difficult for particles to move and compact. * If soil is too saturated (maximize moisture), it becomes soapy, loose, and uncompactable. * The solution is to determine the Optimum Moisture Content (OMC) which allows for the Maximum Dry Density (MDD).
Laboratory Testing: The Proctor Test
Process Overview: A sample is collected from the field, tested in a lab to find the OMC and MDD, and these values serve as the baseline for field work.
Soil Sample Preparation: * Extraction: Use a hand auger to collect about of soil. * Air Drying: The sample is left to dry naturally to remove excess water. This assumes the weight of the air-dried sample is approximately equal to the weight of solids (). * Sieving: The sample must pass through Sieve #4 (opening size of or ). This separates fine aggregate (sand) from coarse aggregate (gravel). Only fine aggregate is used for the test.
Standard vs. Modified Proctor Test: Both use the same concepts. The difference lies in the weight of the hammer, height of the drop, and Number of blows.
The Standard Proctor Apparatus: * Mold Volume: Fixed at . * Components: Detachable base plate, mold, and a removable collar.
Testing Procedure (Step-by-Step): * 1. Select an initial moisture content (e.g., or ). * 2. Add the corresponding water weight to the dry soil (). * 3. Fill the mold in three layers (lifts). * 4. Compact each lift with a hammer falling from a height of for blows. * 5. For the final lift, the soil should project slightly above the mold into the collar. * 6. Remove the collar and trim the excess soil flush with the top of the mold to ensure a total volume of exactly . * 7. Weigh the mold with soil, subtract the mold weight to get the total soil weight (). * 8. Repeated the process for 5 or 6 samples, increasing moisture content by increments (e.g., , , ).
Data Analysis: Calculate for each sample, then convert to using equation 4.
The Compaction Curve and Optimization
Plotting the Results: Plot Moisture Content (-axis) versus Dry Unit Weight (-axis). The resulting trend is a parabola.
Identifying Key Lab Values: * Maximum Dry Density (MDD): The peak of the parabola. * Optimum Moisture Content (OMC): The moisture content value on the -axis that corresponds to the peak dry density.
Reading Blueprints (Specifications): * Engineered fill typically requires "Relative Compaction," such as of MDD. * The field target dry density is calculated as: . * Example: If and the spec is , the field target is .
Field Moisture Range: Using the graph, draw a horizontal line at the target density (e.g., ). The two intersection points on the curve indicate the acceptable moisture range for the field (e.g., to \n).
Field Implementation and Verification
Field Action: Contractors spray water to bring soil within the specified moisture range and use rollers for compaction.
Verification: After compaction, the dry density must be measured in the field using a Nuclear Gauge. * Nuclear Gauge: A tool placed on the ground that provides instant readings of actual field moisture content and actual field dry density.
Final Verification Rule: * The actual dry density measured by the nuclear gauge () must be greater than or equal to the target relative compaction density ().
Real-World Application: Aviation projects (taxi lanes) may specify different requirements, such as compaction and moisture within of OMC.
Questions & Discussion
The lecturer emphasizes that the lab dry density () is always significantly higher than field density results because the lab environment is standardized and controlled. Achieving more than of the lab value in the field is nearly impossible.
Students with questions are encouraged to contact the instructor via Microsoft Teams or email.