Soil available water capacity (AWC) is a key function for human survival and well-being.
However, its direct measurement is laborious and spatial interpretation is complex. Digital …

The rapid warming of the Arctic is changing the conditions for agricultural activity in
southwest Greenland markedly, which necessitates studies of the physical properties of the …

Parameterization of theeffective properties as input in hydrogeological models for simulating
water flow is a time consuming and costly process, and it is characterized by high …

In this study, a tracer field experiment was conducted to study the temporal dynamics of
bromide movement in a loamy tile‐drained agricultural landscape. Moreover, tritium …

Atterberg limits are broadly used for engineering and geology purposes as well as in
agricultural and environmental applications. Laboratory methods used for their …

Core Ideas Two methods each to measure each Atterberg limit (SL, PL, and LL) were
evaluated. A Vis‐NIRS technique successfully estimated Atterberg limits for fine‐grained …

Purpose Soil–water characteristic curve (SWCC) models have generally been developed
based on measurement results in the low suction range. However, different mechanisms …

Estimation of a soil–water retention curve (SWRC) is essential for modeling the water flow
and solute transport. A simple method to fit the measured retention data is the Campbell …

Soil available water capacity (AWC) is a key function for human survival and well-being.
However, its direct measurement is laborious and its spatial interpretation is complex. These …

Disclosed are methods and systems for accurate modeling of the soil-water retention curve
(SWRC) for any soil texture class and with varying amounts of soil organic matter. The …