Construct · 3 fields · 3 citations
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In environmental engineering, leaching is the release of soluble constituents from a solid waste as water percolates through it, producing leachate, the contaminated liquid draining from a landfill, whose composition and long-term risk Kjeldsen and colleagues reviewed. The mechanism is the same seep-and-dissolve process the metallurgist runs on purpose and the soil undergoes naturally: a liquid moves through a porous solid and carries dissolved matter out of it. Here the carried matter is pollution to be contained, measured by leachate concentration and cumulative release.[1]
In hydrometallurgy, leaching is the selective dissolution of a valuable metal from an ore or concentrate by a water-based solvent (a lixiviant such as sulfuric acid or cyanide) that percolates through or is mixed with the crushed solid and carries the metal into solution for later recovery. Free's Hydrometallurgy sets out the thermodynamics and kinetics that govern it. It is the identical percolation-and-dissolution construct seen in soils and landfills, here steered deliberately to win metal, and measured by the fraction of metal extracted and the leaching rate.[2]
In soil science, leaching is the downward removal of soluble substances (nitrate, bases, and salts) from the root zone as water percolates through the soil profile, a natural loss that depletes fertility and can carry nitrate into groundwater. Brady and Weil's The Nature and Properties of Soils treats it as a central pathway of nutrient movement. It is the same construct as the metallurgist's ore leach and the landfill's leachate (liquid percolating through a porous solid and carrying dissolved matter away), here an unwanted loss rather than an engineered extraction, measured by leachate concentration and nutrient loss per area.[3]
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