The phrase "absorption of soil" is correct and usable in written English.
It can be used in contexts related to environmental science, agriculture, or soil science, particularly when discussing how soil takes in water or nutrients.
Example: "The absorption of soil is crucial for maintaining healthy plant growth and preventing erosion."
Alternatives: "soil uptake" or "soil absorption capacity".
Urban soils are normally enriched in 'black carbon' soots which strongly bind to most organic and inorganic pollutants inhibiting soil-to-plant pollutant transfers [ 17], and are likely to reduce the extent of gut absorption of soil-bound ingested toxins.
From soil, vegetables can take both nutrients and toxic elements, such as heavy metals, directly by root adsorption and indirectly, through foliar absorption of contaminated soil particles.
The concentration of soil organic matter in the topsoil layer plays an important role in the absorption of herbicides.
Density of vegetation and rainfall absorption capacity of soils, influence the rate of surface runoff and affects the drainage texture of an area (Gregory and Gardiner 1975; Gregory 1976; Montgomery and Dietrich 1989; Trucker and Bras 1998).
Related to how water moves through the soil and the absorption properties of soils is the soil's ability to perform an important function in pollution control (pesticides, nitrates etc.).
Increased root length and numbers of root hairs also increase the surface area of root which enhances the absorption of nutrients from soil.
Artificial cultivation of tea trees leads to the absorption of more superficial soil nutrients, and the application of unified fertilizing guidelines and chemical fertilizers can result in the origin-related special fragrance gradually disappearing with storage time [5, 6].
In rice, overexpression of OsIRT1 leads to increased Fe and Zn accumulations in shoots, roots and mature seeds, suggesting OsIRT1 is a functional metal transporter for iron, and it is responsible for the absorption of iron from soil, especially under Fe-deficiency [ 24- 26].
The most important components of these models are the atmosphere (including air temperature, moisture and precipitation levels, and storms); the oceans (measurements such as ocean temperature, salinity levels, and circulation patterns); terrestrial processes (including carbon absorption, forests, and storage of soil moisture); and the cryosphere (both sea ice and glaciers on land).
