Unsaturated Zone Dynamics and Their Implications for Groundwater Resource Sustainability

Session ID#: 281133

Session Description:
Groundwater sustainability strongly depends on processes in the unsaturated (vadose) zone, which control infiltration, storage, and the timing and quality of recharge. Despite advances from theoretical and experimental studies, significant gaps remain in understanding and quantifying vadose‑zone processes. This session invites contributions that advance knowledge of unsaturated zone dynamics and their implications for groundwater resources under changing climates, land use, and ecosystems. We welcome observational, experimental, and modeling studies of flow and contaminant transport across scales, including soil–plant–atmosphere interactions, preferential flow, fracture and karst systems, groundwater contamination, and responses to extreme events such as droughts and intense precipitation. Integrative studies combining field observations (e.g., soil moisture, tracers, geophysics), remote sensing, laboratory experiments, and numerical or data‑driven modeling are especially encouraged. The session aims to foster interdisciplinary dialogue to improve vadose‑zone representation in groundwater assessments and support sustainable water‑resources management across diverse hydrogeologic settings.
Index Terms:

1402 - Critical Zone [CRITICAL ZONE]
1829 Groundwater hydrology [HYDROLOGY]
1838 Infiltration [HYDROLOGY]
1875 Vadose zone [HYDROLOGY]
Primary Convener:  Kashif Mahmud, PhD, Midwestern State University, Kimbell School of Geosciences, Wichita Falls, United States
Conveners:  Kyle C Fredrick, Pennsylvania Western University - California, Biology, Earth, and Environmental Sciences, California, United States, Valentina Prigiobbe, University of Padua, Padua, Italy and Maria Clementina Clementina Caputo, National Research Council Water Research Institute, Bari, Italy
See more of: Hydrology