We address transport by transit times (i.e., the age of water parcels leaving a storage as discharge, deep loss, or evapotranspiration) in subvertical soil systems, key to our understanding of water quality in catchments and streams. While the use of field and lysimeter observations to constrain and validate modeling approaches is generally accepted, different views exist on the relative ranges of applicability of spatially integrated or spatially explicit approaches. This study specifically illustrates how one class of spatially integrated models of transport, based on StorAge Selection (SAS) functions, fares with respect to spatially explicit hydrologic models in a case where detailed tracer data from experimental lysimeters exist and for...
The contribution of groundwater to streams is controlled by temporally and spatially variable ground...
Time-variable transit time distributions (TTDs) and StorAge Selection (SAS) functions have been wide...
Many details about the flow of water in soils in a hillslope are unknowable given current technologi...
We address transport by transit times (i.e., the age of water parcels leaving a storage as discharge...
Distributions of water transit times (TTDs), and related storage-selection (SAS) distributions, are ...
Understanding transit times (TT) and residence times (RT) distributions of water in catchments has r...
Spatially integrated water transport dynamics at the hillslope scale have rarely been observed direc...
International audienceGroundwater age tracers provide essential characteristics of residence time di...
Travel and residence times are well-known descriptors of hydrologic and solute transport in the vado...
AbstractSolute transport in hillslope is often ruled by the water dynamics at the vadose zone and th...
StorAge Selection (SAS) functions describe how a catchment selectively removes water and solute of d...
Transit times through hydrologic systems vary in time, but the nature of that variability is not wel...
We propose a mathematical framework for the general definition and computation of travel time distri...
In hilly and humid forest areas with highly conductive soils, subsurface flow consider as the main m...
StorAge Selection (SAS) functions describe how catchments selectively remove water of different ages...
The contribution of groundwater to streams is controlled by temporally and spatially variable ground...
Time-variable transit time distributions (TTDs) and StorAge Selection (SAS) functions have been wide...
Many details about the flow of water in soils in a hillslope are unknowable given current technologi...
We address transport by transit times (i.e., the age of water parcels leaving a storage as discharge...
Distributions of water transit times (TTDs), and related storage-selection (SAS) distributions, are ...
Understanding transit times (TT) and residence times (RT) distributions of water in catchments has r...
Spatially integrated water transport dynamics at the hillslope scale have rarely been observed direc...
International audienceGroundwater age tracers provide essential characteristics of residence time di...
Travel and residence times are well-known descriptors of hydrologic and solute transport in the vado...
AbstractSolute transport in hillslope is often ruled by the water dynamics at the vadose zone and th...
StorAge Selection (SAS) functions describe how a catchment selectively removes water and solute of d...
Transit times through hydrologic systems vary in time, but the nature of that variability is not wel...
We propose a mathematical framework for the general definition and computation of travel time distri...
In hilly and humid forest areas with highly conductive soils, subsurface flow consider as the main m...
StorAge Selection (SAS) functions describe how catchments selectively remove water of different ages...
The contribution of groundwater to streams is controlled by temporally and spatially variable ground...
Time-variable transit time distributions (TTDs) and StorAge Selection (SAS) functions have been wide...
Many details about the flow of water in soils in a hillslope are unknowable given current technologi...