Heat as a tracer to quantify water flow in near-surface sediments
The dynamic distribution of thermal conditions present in saturated near-surface sediments
have been widely utilised to quantify the flow of water. A rapidly increasing number of …
have been widely utilised to quantify the flow of water. A rapidly increasing number of …
Using diurnal temperature signals to infer vertical groundwater‐surface water exchange
Heat is a powerful tracer to quantify fluid exchange between surface water and groundwater.
Temperature time series can be used to estimate pore water fluid flux, and techniques can …
Temperature time series can be used to estimate pore water fluid flux, and techniques can …
Automated calculation of vertical pore-water flux from field temperature time series using the VFLUX method and computer program
Heat is a useful tracer for quantifying groundwater–surface water interaction, but analyzing
large amounts of raw thermal data has many challenges. We present a computer program …
large amounts of raw thermal data has many challenges. We present a computer program …
Using high‐resolution distributed temperature sensing to quantify spatial and temporal variability in vertical hyporheic flux
Hyporheic flow can be extremely variable in space and time, and our understanding of
complicated flow systems, such as exchange around small dams, has generally been limited …
complicated flow systems, such as exchange around small dams, has generally been limited …
Hydrochemical and isotopic interpretation of interactions between surface water and groundwater in Delingha, Northwest China
Understanding the interactions between surface water and groundwater is of considerable
significance for managing water resources and protecting ecosystems in arid and semi-arid …
significance for managing water resources and protecting ecosystems in arid and semi-arid …
[图书][B] Hydrogeology: groundwater science and engineering
A Dassargues - 2018 - taylorfrancis.com
This text combines the science and engineering of hydrogeology in an accessible,
innovative style. As well as providing physical descriptions and characterisations of …
innovative style. As well as providing physical descriptions and characterisations of …
Experimental investigation of the thermal dispersivity term and its significance in the heat transport equation for flow in sediments
GC Rau, MS Andersen… - Water Resources Research, 2012 - Wiley Online Library
A review of heat and solute transport in sediments demonstrates that the use of heat as a
tracer has not been experimentally evaluated under the same experimental conditions as …
tracer has not been experimentally evaluated under the same experimental conditions as …
Experimental evaluation of the applicability of phase, amplitude, and combined methods to determine water flux and thermal diffusivity from temperature time series …
Vertical fluid exchange between surface water and groundwater can be estimated using
diurnal signals from temperature time series methods based on amplitude ratios (A r), phase …
diurnal signals from temperature time series methods based on amplitude ratios (A r), phase …
Climate change yields groundwater warming in Bavaria, Germany
H Hemmerle, P Bayer - Frontiers in Earth Science, 2020 - frontiersin.org
Thermodynamic coupling between atmosphere and ground yields increasing aquifer
temperatures as a consequence of global warming. While this is expected to manifest as a …
temperatures as a consequence of global warming. While this is expected to manifest as a …
Characterizing the heterogeneity of karst critical zone and its hydrological function: An integrated approach
Spatial heterogeneity in the subsurface of karst environments is high, as evidenced by the
multiphase porosity of carbonate rocks and complex landform features that result in marked …
multiphase porosity of carbonate rocks and complex landform features that result in marked …