The determination of the soil pore size distribution, water retention curve, and derived
parameters that control important processes in soils, such as water supply for plants; …

A variety of magnetic resonance relaxometry methods have been developed to determine
pore size in porous rocks. Uncertainties in pore-size estimates may occur due to uncertainty …

This study used eight empirical equations such as Kozeny-Carman (KC), Terzaghi, Hazen,
Slitcher, Kruger, Sauerbrei, NAVFACDM7, and Zamarin to estimate saturated hydraulic …

Two experiments were carried out to determine the quantitative lipid requirements for
ovarian maturation of Litopenaeus vannamei (Boone) broodstock. The first experiment …

In headwater catchment, the calibration of hydrological models is complex due to the
scarcity of data in mountainous areas. Here, an innovative methodology is developed to …

In granite aquifers, fractures can provide both storage volume and conduits for groundwater.
Characterization of fracture hydraulic conductivity (K) in such aquifers is important for …

A multi-method geophysical survey, including helicopter-borne electromagnetics (HEM),
transient electromagnetics (TEM), and magnetic resonance sounding (MRS), was conducted …

As a long-standing problem, the physics of freezing and melting temperature depressions of
water in millimeter-sized pores remains elusive. We devised a series of experiments on the …

Surface nuclear magnetic resonance (surface-NMR) is a promising technique for exploring
shallow subsurface aquifer structures. Surface-NMR can be applied in environments that are …

The relaxation phenomena observed in the electrical low-frequency range (approximately 1
MHz–10 kHz) of natural porous media such as sandstones are often assumed to be directly …