Results 71 to 80 of about 965 (177)
Study of the hydraulic properties of slate processing fines and fitting to Van Genuchten’s model
Slate processing fines could be used as surface material for the revegetation of slate dumps and tailings, because their properties are compatible with plant growth. Yet, the study of their hydraulic properties (water holding capacity and permeability) is essential for knowledge of processes such as water movement and solute transport, water supply to ...
R. Paradelo +3 more
openaire +1 more source
Implementation of the Brunswick model system into the Hydrus software suite
The Brunswick modular framework for modeling unsaturated soil hydraulic properties (SHP) over the full moisture range was implemented in the Hydrus suite.
Efstathios Diamantopoulos +2 more
doaj +1 more source
Introduction: Several mathematical models are being used for assessing the plant response to the salinity of the root zone. The salinity of the soil and water resources is a major challenge for agricultural sector in Iran.
M. Sarai Tabrizi +4 more
doaj +1 more source
Fracture–Matrix Flow Partitioning Governs Retention Regime Transitions in Unsaturated Fractured Rock
Abstract Upscaling unsaturated flow in fractured rock remains challenging because fractures and matrix often exhibit sharply contrasting hydraulic behaviors across saturation states. Here, we demonstrate that unsaturated flow undergoes a transition between matrix‐ and fracture‐dominated regimes.
M. A. Pratama +3 more
wiley +1 more source
Introduction: The forest residuals play an important role in runoff rate, soil erosion, and soil infiltration capacity of protecting mineral (surface) soils from the direct impact of raindrops.
Majid Homapoor Goorabjiri +1 more
doaj +1 more source
Modelling Climate Change Effects on Groundwater Recharge and Temperature for a Pre‐Alpine Lysimeter
Climate change is projected to increase winter groundwater recharge and extreme precipitation events in pre‐alpine regions. Groundwater temperatures will rise by up to 26%, primarily driven by air temperature. These trends pose challenges for future water availability and quality, requiring adaptive water resource management.
Christian Moeck +7 more
wiley +1 more source
Three 1‐D unsaturated zone models (HYDRUS‐1D with isotope fractionation) were calibrated with volumetric water content (θ) alone versus θ and δ18O δ2H from soil water. Adding isotopes constrains the parameter spaces and reproduces isotope profiles despite θ extremes, and reveals heterogeneous recharge in semi‐arid Tamil Nadu, South India.
Isabelle Schmidt +5 more
wiley +1 more source
Extension of the Gardner exponential equation to represent the hydraulic conductivity curve
The relative hydraulic conductivity curve Kr(h) = K/Ks is a key variable in soil modeling. This study proposes a model to represent Kr(h), the so-called Gardner dual (GD) model, which extends the classical Gardner exponential model to h values greater ...
Ottoni Filho Theophilo B. +3 more
doaj +1 more source
Abstract The distribution of soil moisture, resulting from the movement of infiltrated water, plays a fundamental role in the hydrological dynamics of hillslopes and in the triggering of landslides. Although water flow in soils occurs in multiple directions due to combined vertical and lateral fluxes, one‐dimensional (1D) flow models are widely adopted
Danúbia Teixeira +5 more
wiley +1 more source
Soil water retention curve (SWRC) becomes important because it guides when and how much to irrigate, optimizing the use of water; can be obtained in the field or laboratory, being commonly determined in the laboratory with porous plate apparatus, and the determination is compromised by issues such as time and labor.
Ícaro Vasconcelos do Nascimento +8 more
openaire +2 more sources

