Last reviewed 1 Oct 2026 · 6 min read
Moisture content
Agricultural materials hold water as: free (surface) water, capillary water in pores, adsorbed/bound water on surfaces, and chemically bound water (hydrates). Free water dries first; bound water needs more energy to remove.
Wet basis and dry basis
Let = mass of the wet sample, = mass of dry matter (bone dry), = mass of water.
Wet basis (w.b.): — used in trade, standards and marketing (cannot exceed 100 %).
Dry basis (d.b.): — used in engineering calculations of drying (can exceed 100 %).
Conversions: and .
A grain at 20 % w.b. has . A grain at 14 % w.b. has . Note that the numerical difference is larger on d.b. as the moisture rises.
Mass change on drying
The dry matter stays constant, so for a lot of initial mass at (w.b., %) dried to (w.b., %):
1000 kg of paddy at 22 % w.b. is dried to 13 % w.b.
; water removed . (If a seller is paid for 1000 kg of wet grain, 10 % of the weight is just water that has to be dried off.)
Mixing lots of different moisture
For lots at and at (both w.b.), the mixture moisture is the mass-weighted average of water: . (Dry-matter-weighted averaging is needed on a d.b.)