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Correspondingly, our hypothesis was that maintaining high inputs of plant-derived carbon is important to the formation and stabilisation of soil structure, and this in-turn may support a greater diversity of habitats for microbial communities thereby ensuring more robust soil ecosystem function.
Improvement of load bearing capacity of the soil may be undertaken by a variety of ground improvement techniques like stabilisation of soil, adoption of reinforced earth technique etc. Reinforced earth technique is considered as an effective ground improvement method because of its cost effectiveness, easy adaptability and reproducibility.
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The stabilisation of soils with additives is a chemical process that can be used to improve soils that contain weak engineering properties.
Hydrated lime on the other hand is used extensively for the stabilisation of soils with high clay content where its main advantage is in raising the plastic limit of the clayey soil [2, 8].
The traditional chemical stabilisation of the soil is a frequently used improvement process.
These results suggest that there is potential in using Lime or Portland cement activated GGBS blend for the stabilisation of natural clay soil for sustainable and low carbon building materials production.
The stabilisation of road subgrade soil may improve its mechanical properties considerably, however under the combined effect of cumulative traffic load and weathering these materials deteriorate over time and lose performance.
In order to investigate whether key metals played any role in the stabilisation of PrP in soil, mte was mixed with copper or manganese.
Plants and earthworms, as soil ecosystem engineers, play a crucial role during stabilisation of organic matter in soil through its incorporation into soil aggregates.
Acceptable trade-offs were found between the amount of soil stabilisation possible and the prioritisation goals, while uncertainty in the prioritisation scores did not significantly affect the results.
The stabilisation of organic materials in soils by the soil matrix is a function of the chemical nature of the soil mineral fraction and the presence of multivalent cations, the presence of mineral surfaces capable of adsorbing organic materials, and the architecture of the soil matrix.
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