在粉碎的或原来松散的土中,掺入足量的石灰和水,经拌合均匀后,石灰与土之间发生强烈的离子交换、碳酸化及结晶作用。石灰的掺入使土的性质发生根本变化,明显地提高了土的无侧限抗压强度及整体强度,由于离子交换作用,减薄了土的吸附水膜作用,促使土颗粒凝集,形成团粒结构,从而降低了土的塑性指数。 石灰稳定土具有较高的强度、较强的板体性、较好的抗 In the crushed or the original loose soil, the incorporation of adequate lime and water, after mixing evenly, lime and soil strong ion exchange, carbonation and crystallization. Due to the incorporation of lime, the nature of the earth changes fundamentally, and the unconfined compressive strength and overall strength of the soil are obviously increased. Due to the ion exchange action, the action of the adsorbed water film on the soil is reduced to promote the agglomeration of the soil particles to form the agglomerates Structure, thus reducing the plastic index of soil. Lime stabilized soil has high strength, strong plate body, good resistance