Different types of soil stabilization have been performed for thousands of years below are the basic Soil Stabilization:
Soil Stabilization with Cement: Soil-cement can be mixed in place or a central mixing plant. Central mixing plants can be used where borrow substance is required. The mixed soil-cement is then hauled to the job site and spread on the prepared subgrade.
Mechanical: This is mainly the oldest type of soil stabilization. Mechanical solutions involve bodily changing the property of the soil somehow, to affect its scale, solidity, and other characteristics. This is probably the most popular and most natural method for soil stabilization. This is also the common and oldest way for compaction. The process of mechanical stabilization involves physical force on the soil. This helps to change the physical properties of the soil. The most common process in the mechanical method is dynamic compaction. It removes the deformation of the soil and makes it uniform throughout under a compressed surface. It is similar to effective compaction but the wave is used for the stabilization.
Chemical: Soil stabilization with cement, lime, bitumen come under the chemical soil stabilization. The vapor mass gets lowered, surface tension increases and the rate of evaporation levels. The freezing point of pure water gets reduced and it results in the arrest or reduction of frost heave.
Polymers: This is the new and the latest methods of all and is driven by the latest technologies. Both of the previous types of soil stabilization have been around for hundreds of years, only in the past several decades has technology opened up new types of soil stabilization for organizations to explore. Soil stabilization with polymers is one of the best and modern techniques of soil stabilization. Soil Stabilization Innovations is the pioneers of the practice of using polymers for soil stabilization, and create products that cost less, last longer, and are environment-friendly. These are mixed with the soil and that in turn creates sure that soil is stabilized.
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