"soil stabilisation" is a correct and usable phrase in written English.
It refers to the process of making soil more stable and resistant to erosion or damage. You can use it in various contexts, such as construction, agriculture, and environmental conservation. Example: The construction company implemented soil stabilisation techniques to strengthen the ground before building the foundation of the new skyscraper.
Lime and/or Ordinary Portland cement (OPC) are the traditional binders used in soft soil stabilisation.
Soil stabilisation with by-product materials has proved to be a useful cost effective option.
It may nonetheless, be used in soil stabilisation when activated by lime and other pozzolans.
Determining when plants become effective at soil stabilisation is important for developing guidelines and policy for land management.
This research seeks to develop a new ternary blended cementitious binder (TBCB) to replace cement for soft soil stabilisation.
Planted forests are increasingly playing an important role in China for wood and non-wood forest products, carbon sequestration, soil stabilisation, and a range of other ecosystem services.
An alternative modelling for flexible membranes anchored to the ground for soil slope stabilisation is presented using Smoothed-Particle Hydrodynamics to model the unstable ground mass in a soil slope, employing a dynamic solve engine.
Bioengineering features of native vegetation are currently being evolved to enhance soil stiffness, slope stabilisation and erosion control.
Supply might be induced by highly decomposed OM from root litter and by leaching of highly oxidized water-soluble organic products from the forest floor into the mineral soil horizons and stabilisation therein by association with mineral phases [35].
Microbially induced carbonate precipitation (MICP) is a process that has emerged as an attractive alternative ground improvement technique in Geotechnical and Civil Engineering using ureolytic bacteria for soil strengthening and stabilisation.
Supply might be induced by highly decomposed OM from root litter and by leaching of highly oxidized water-soluble organic products from the forest floor into the mineral soil horizons and stabilisation therein by association with mineral phases [ 35].
