Field monitoring of solute and colloid mobility in a gneissic sub-catchment, South Australia

[1]  M. Litaor,et al.  Review of soil solution samplers , 1988 .

[2]  Hydrology of a forested hillslope during storm events , 1990 .

[3]  Glenn V. Wilson,et al.  Physical and chemical controls of preferred path flow through a forested hillslope , 1990 .

[4]  K. Brown,et al.  Capillary‐Wick Unsaturated Zone Soil Pore Water Sampler , 1991 .

[5]  D. A. Lietzke,et al.  Hydrogeochemical processes controlling subsurface transport from an upper subcatchment of Walker Branch watershed during storm events. 1. Hydrologic transport processes , 1991 .

[6]  D. Chittleborough,et al.  THE INFLUENCE OF MACROPORES ON RUNOFF GENERATION FROM A HILLSLOPE SOIL WITH A CONTRASTING TEXTURAL CLASS , 1991 .

[7]  Tammo S. Steenhuis,et al.  Fiberglass wicks for sampling of water and solutes in the vadose zone , 1992 .

[8]  E. Cotsaris,et al.  Seasonal changes in pathways of dissolved organic carbon through a hillslope soil (Xeralf) with contrasting texture , 1992 .

[9]  W. Jury,et al.  Interpretation of Solute Transport Data Obtained with Fiberglass Wick Soil Solution Samplers , 1992 .

[10]  J. Selker,et al.  Fiberglass Wick Preparation for Use in Passive Capillary Wick Soil Pore-Water Samplers , 1993 .

[11]  W. Stumm.  Aquatic colloids as chemical reactants: surface structure and reactivity , 1993 .

[12]  R. Fitzpatrick,et al.  Field-based comparison of platinum and wax impregnated graphite redox electrodes , 1995 .

[13]  D. Parker,et al.  GEOCHEM‐PC—A Chemical Speciation Program for IBM and Compatible Personal Computers , 1995 .