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Because excess water does not allow the soil particles to get close together, when the soil has dried (after construction is complete), its density will be too low and we can run into issues such as settlement. Water acts as a lubricant, reducing interparticle friction. Maximum soil compaction occurs when soil moisture is at or near field capacity (figure 1) because soil moisture works as a lubricant between soil particles under heavy pressure from field equipment.
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The document discusses compaction of soil including definitions, objectives, degree of compaction, compaction curves, factors affecting compaction, laboratory compaction tests, field compaction methods, and numerical problems related to compaction. Simply put, adding water to a dry soil during compaction allows soil particles to slide past one another more easily Compaction, in general, is the densification of soil by removal of air, which requires mechanical energy
The degree of compaction of a soil is measured in terms of its dry unit weight
When water is added to the soil during compaction, acts as a softening agent on the soil particles. Moisture acts as a lubricant within soil, sliding the particles together Too little moisture means inadequate compaction— the particles cannot move past each other to achieve density. Based on our results, we hypothesize that the scaling approach is independent of the capillary saturation function and that this method might be applied to other models within the pdi system.
