Interstitial water was extracted from field-moist soils and chalk by immiscible displacement with a dense, inert fluorocarbon liquid. The only special equipment required is a high-speed centrifuge. Yields of interstitial water from soils at field capacity are typically 20-50% of the total water present; yields from chalk range up to 90%. The interstitial water was analyzed for about 20 solutes principally by inductively coupled plasma emission spectrometry. The water extracted from a chalk sample appeared to be representative of all the water present, but with a clay soil, there was evidence of some fractionation of N03-N. Organic carbon ((2-7) X 10~3 M) was frequently the most abundant solute in the solutions extracted from ten topsoils. Other typical solute concentrations were in the range 10~3-1( 4 M for N03-N, Na, Mg, Si, S, Cl, K, and Ca and less than 10™6 M for the trace elements Cu, Zn, and Ba.