Concepts
211 concepts
photoreductive dissolution
rising limb
sensor integration
transmissivity feedback
A modeling approach where downslope flow responds to rainfall or snowmelt recharge through accommodating new recharge within a rising water table within a thicker and more transmissive saturated zone
tritium concentration
Arctic browning
Damköhler number
Dimensionless number comparing transport timescale to reaction timescale, used to determine whether transport or reaction processes dominate
GMWL
Global Meteoric Water Line
MAOC
Nominal oxidation state of carbon (NOSC)
SOC
Saturated zone
Schmidt number
UV254
XANES fitting
X-ray Absorption Near Edge Structure spectroscopy fitting method using reference compound spectra to identify chemical species
ammonium
aromaticity index
calcium uranium carbonate complexes
carbon evasion
The transfer of CO2 from water to atmosphere through gas exchange at the air-water interface
carbon partitioning
Distribution of carbon between different reservoirs including atmosphere, subsurface, and exported dissolved phases during weathering processes
chlorite dissolution
clay concentration
coercivity spectra
complex terrain
Mountainous regions with significant topographic variability that influences weather and climate processes
d-excess
data representativeness
density fractionation
Physical separation method to isolate soil organic matter pools with different physicochemical protection mechanisms
diffusion-limited environment
Subsurface conditions where chemical transport is limited to diffusion rather than advection, creating oxygen-depleted anoxic conditions
electrical mobility
excess-air conditions
flux-weighted age distributions
free advective mass outflux boundary
functional zonation
matric potential
matrix diffusion
Process controlling environmental tracer and groundwater age distributions in fractured rock systems through diffusive exchange between fractures and rock matrix
mean
metabolomes
noble gas recharge parameters
Parameters including recharge temperature, elevation, and excess-air conditions that control dissolved noble gas concentrations in groundwater
oceanic teleconnections
organic carbon depolymerization
piston-flow model
porosity evolution
Changes in rock porosity and permeability due to mineral dissolution and precipitation reactions during weathering
reaction network
river migration
Lateral movement of river channels through erosion and deposition processes over time
sediment transport
The movement of eroded soil and rock particles by water flow
sheet flow
Overland flow that occurs when rainfall intensity exceeds the rate at which water can enter the soil
sorption distribution coefficient (Kd)
streamflow deficit
The difference between observed streamflow and expected or baseline streamflow, representing water shortage