Adsorption vs Absorption: The Distinction That Decides Everything
Two mechanisms capture water, and confusing them is the root of most desiccant mistakes. Adsorption is a physical process: water molecules adhere to the vast internal surface of a porous solid through Van der Waals forces. Silica gel, activated clay and molecular sieve are adsorbents; they stay solid, do not change chemically, and their capacity is capped by available surface area. Absorption is a chemical process: the desiccant reacts with and dissolves into the water it captures. Calcium chloride is an absorbent; it deliquesces, turning into a brine, and its capacity is governed by how much active material it contains, which is why it reaches 300–600% of its weight where adsorbents plateau at 25–40%.
The second decisive property is the adsorption isotherm, the curve of how much water a desiccant holds at a given relative humidity. Molecular sieve has a steep early isotherm: it grabs water hard at very low RH and drives an enclosure bone-dry. Silica gel rises gradually and performs best in the mid-range. Clay sits below silica gel but is cheap and stable. Calcium chloride does the opposite of all of them, its uptake accelerates as RH climbs toward 100%, which is exactly why it dominates the high-humidity, long-voyage container problem. Choosing a desiccant is choosing the isotherm that matches your enclosure's humidity profile.