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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 …
Numerical simulation of magmatic hydrothermal systems
The dynamic behavior of magmatic hydrothermal systems entails coupled and nonlinear
multiphase flow, heat and solute transport, and deformation in highly heterogeneous media …
multiphase flow, heat and solute transport, and deformation in highly heterogeneous media …
The system H2O–NaCl. Part II: Correlations for molar volume, enthalpy, and isobaric heat capacity from 0 to 1000 C, 1 to 5000 bar, and 0 to 1 XNaCl
T Driesner - Geochimica et Cosmochimica Acta, 2007 - Elsevier
A set of correlations for the volumetric properties and enthalpies of phases in the system
H2O–NaCl as a function of temperature, pressure, and composition has been developed …
H2O–NaCl as a function of temperature, pressure, and composition has been developed …
Experimental investigation of the thermal dispersivity term and its significance in the heat transport equation for flow in sediments
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 …
Numerical simulation of multi-phase fluid flow in structurally complex reservoirs
Realistic simulation of structurally complex reservoirs (SCR) is challenging in at least three
ways:(1) geological structures must be represented and discretized accurately on vastly …
ways:(1) geological structures must be represented and discretized accurately on vastly …
Hybrid finite element–finite volume discretization of complex geologic structures and a new simulation workflow demonstrated on fractured rocks
The generation of computational meshes of complex geological objects is a challenge: their
shape needs to be retained, resolution has to adapt to local detail, and variations of material …
shape needs to be retained, resolution has to adapt to local detail, and variations of material …
Semianalytical solutions for cocurrent and countercurrent imbibition and dispersion of solutes in immiscible two‐phase flow
We derive a set of semianalytical solutions for the movement of solutes in immiscible two‐
phase flow. Our solutions are new in two ways: First, we fully account for the effects of …
phase flow. Our solutions are new in two ways: First, we fully account for the effects of …
Hydrothermal, multiphase convection of H2O‐NaCl fluids from ambient to magmatic temperatures: a new numerical scheme and benchmarks for code comparison
Thermohaline convection of subsurface fluids strongly influences heat and mass fluxes
within the Earth's crust. The most effective hydrothermal systems develop in the vicinity of …
within the Earth's crust. The most effective hydrothermal systems develop in the vicinity of …
Phase separation, brine formation, and salinity variation at Black Smoker hydrothermal systems
We present the first fully transient 2‐D numerical simulations of black smoker hydrothermal
systems using realistic fluid properties and allowing for all phase transitions possible in the …
systems using realistic fluid properties and allowing for all phase transitions possible in the …
Non‐Fourier thermal transport in fractured geological media
In a similar way to solute transport, heat transfer in porous media is governed by advection
and dispersion processes, and “non‐Fourier” behavior, characterized by early breakthrough …
and dispersion processes, and “non‐Fourier” behavior, characterized by early breakthrough …