Agricultural engineers often draw upon the classical theories of soil
mechanics in their study of agricultural soil behaviour. These theorie
s are largely based on the assumption that the soil is saturated. In a
n emerging theoretical framework, an unsaturated soil is considered to
have four phases: solid, air, water, and contractile skin (the air-wa
ter interphase). The contractile skin acts like a rubber membrane as i
t induces a matric suction in the soil pores. Suction has been shown t
o affect both strength and volume change characteristics of unsaturate
d soils. The relationship between water content and matric suction (th
e soil-water characteristic) becomes an important component of the uns
aturated soil mechanics framework. In this paper, concepts and implica
tions of these developments for some agricultural shear strength-based
models are discussed. Experimental data highlighting these relationsh
ips are also presented.