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The role of macropores in infiltration through a sandy loam was studied using laboratory columns pretreated with water possessing a δ 18 O signature of -8.7‰ and 15 mg l -1 Cl - . A simulated snowmelt pulse of δ 18 O-depleted water containing 1100 mg l -1 Cl - was added to a control column and two columns containing a single vertical...