Part I Response Mechanisms of Hydrological Processes in the Near-Surface Environment
1. Surface Runoff Generation, Vertical Infiltration and Subsurface Lateral Flow
1.1 Key Definitions
1.2 Surface Runoff Mechanisms: Conversion of Rainfall into Runoff
1.3 Infiltrability Models for Non-Structured Soils (Infiltration in an Ideal Soil)
1.4 Influence of Macropores and Surface-Exposed Fractures on Infiltration, Runoff Generation and Lateral Preferential Flow
1.5 Non-Infiltration Types of Rainfall Losses
2. Rainfall-Induced Runoff and Subsurface Stormflow at the Hillslope Scale
2.1 Kinematic Flow Approximation to Runoff on Idealized Hillslopes and Basic Characteristic Solutions
2.2 Overland Flow over Impermeable Surface
2.3. Coupled Overland Flow and Infiltration Models
2.4 On an Analytical Approach to Coupled Surface and Subsurface Hydrological Processes
3. Models of Dissolved Component Transport at the Hillslope Scale
3.1 Mathematical Problem Formulation
3.2 Solute Transport in the Rain Water Flowing over Impermeable Soil Surface
3.3 Solute Transport in Surface Runoff Coupled with Infiltration into Underlying Soil
3.4 Solute Transport along Lateral Subsurface Flowpaths
4. Contaminant Sorption and Transport by Suspended Particles with Runoff