We tested radioactive methylammonium (14CH3NI--I+) as a tracer for ammonium (NH +) in root uptake measurements from soil. Tomato (Lycopersicon esculentum Moll. cv T5) in 3 L pots filled with loamy sand soil received 40, 200, or 600 #mol 14CH3NH + or 15NH+. During a 4 h period, the plants absorbed laCH3NH + at slower rates than ~SNH +. Estimates ofNH4 + absorption based on 15NH+ absorption were 0.9-7.9/~mol NH4 + g-l plant dry weight h -l, whereas those based on IaCH3NH+ absorption were 0.2-1.0/~mol NH4 + g-i plant dry weight h -~. After 4 h, approximately one-half of the applied 15N was not recovered in the plants or soil KC1 extracts; apparently, this lSN was either immobilized or nitrified and denitrified by soil biota. By contrast, almost all the t4CH3NH+ remained in the soil solution after 4 h, but after a 10 d incubation, approximately 20% had been released as 14CO~_. These differences in plant absorption rates and movement through soil pools indicate that CH3NH + cannot be used reliably as an NH + analog in soil.