OMC from Proctor test data:
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The Optimum Moisture Content (OMC) is the water content at which a soil can be compacted to its maximum dry density using a specific amount of compaction energy. It's determined through standard Proctor or modified Proctor tests.
The calculator identifies the OMC from compaction test data:
Where:
Explanation: The OMC represents the water content that allows soil particles to be packed most densely under specific compaction effort.
Details: Knowing the OMC is crucial for earthwork construction, as it ensures maximum density and strength with minimum compaction effort. It affects bearing capacity, settlement, and permeability.
Tips: Enter the maximum dry density from your compaction curve and the corresponding moisture content. Both values must be positive numbers.
Q1: What's the difference between standard and modified Proctor OMC?
A: Modified Proctor uses higher compaction energy, typically resulting in higher maximum dry density and lower OMC than standard Proctor.
Q2: How does soil type affect OMC?
A: Cohesive soils generally have higher OMC than granular soils. Clay soils may have OMC around 15-25%, while sands may be 8-12%.
Q3: Why is field moisture content often different from lab OMC?
A: Field conditions (compaction method, lift thickness, soil variability) differ from controlled lab conditions.
Q4: What's the acceptable range around OMC for field compaction?
A: Typically ±2% of OMC is acceptable, but specifications may vary by project.
Q5: How often should OMC be determined?
A: Whenever soil characteristics change significantly or at the beginning of major earthwork projects.