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Several parameters, namely the role of surface structure, moisture, pressure and temperature, are major factors that can influence the CO2-adsorbent interactions.
In the real-world phenomena, the periodic variation of the environment (e.g., temperature, moisture, pressure, seasonal effects of weather, reproduction, food supplies, mating habits, etc).
Three-dimensional (3D) measurements of the Earth's surface and atmospheric thermodynamic state (temperature, moisture, pressure, precipitation, and so forth) have been made indirectly from satellite measurements for many years [1, 2].
Weather is all about the actual state of the atmosphere with respect to wind, temperature, moisture, pressure, cloud cover and other instantaneous measurements.
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The observed moisture-pressure dynamics are qualitatively reproduced using a hysteretic Richards' equation model.
This paper presents a sand column dataset on the soil moisture-pressure dynamics above a simple harmonic oscillating water table.
For all oscillation periods except for the shortest (T= 268s), the formation of a hysteretic moisture-pressure scanning loop was observed.
At shorter periods the contrary exists with the extent of moisture-pressure variations greatly reduced and, for periods less than 15 min, the dynamics become non-hysteretic.
This paper presents a new laboratory dataset on the moisture-pressure relationship above a dispersive groundwater wave in a two-dimensional vertical unconfined sand flume aquifer driven by simple harmonic forcing.
At the shortest period (T= 268s), the observed moisture-pressure relationship was observed to be non-hysteretic but with a capillary capacity that differs from that of the static equilibrium wetting and drying curves.
Consistent with the decay of the saturated zone groundwater wave, the size of the observed moisture-pressure scanning loops decayed with increasing distance landward and the decay rate is larger for the shorter oscillation periods.
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