Magnetic Resonance Monitoring and Numerical Modeling of Soil Moisture during Evaporation. Issue 1 (29th March 2018)

• Record Type: Journal Article
• Authors: Merz, Steffen; Balcom, Bruce J.; Enjilela, Razieh; Vanderborght, Jan; Rothfuss, Youri; Vereecken, Harry; Pohlmeier, Andreas
• Is Part Of: Vadose zone journal. Volume 17:Issue 1(2018)
• Page Start: 1
• Page End: 15
• Publication Date: 2018-03-29
• Subjects: Soil science -- Periodicals; Zone of aeration -- Periodicals; Groundwater flow -- Periodicals; Groundwater flow; Zone of aeration; Periodicals; Electronic journals; 631.4
• DOI: 10.2136/vzj2016.10.0099
• Languages: English
• ISSNs: 1539-1663

Abstract

Abstract : Core Ideas: Evaporative drying of soil columns was monitored in high resolution using NMR. Soil moisture data were used for validating a water, vapor, and heat flow model. The Richards approach was insufficient under Stage II conditions. NMR is a feasible technique for soil moisture measurements under Stage II conditions. Evaporation from bare soil surfaces can be restrained to a great extent with the development of a dry layer at the soil surface where capillary hydraulic conductance ceases and water flow proceeds only by gas phase transport. Model calculations and preliminary experiments with model porous media have shown that this surface layer can be very thin. An accurate characterization of these processes is required, which is provided by noninvasive magnetic resonance (MR) methods. The evaporative drying of a silt loam and a sandy loam was monitored at high spatial resolution in laboratory experiments. The MR data were used to assess the performance of two numerical models: (i) the Richards equation, which considers isothermal liquid water flow, and (ii) a coupled soil water, heat, and vapor flow numerical model. The experimental results reveal two distinct drying regimes for both soil types where, at the onset of the second evaporation stage, a dry surface zone developed with increasing thickness over time. This layer revealed that water loss inside the soil coincided with a relatively low evaporation rate as the liquid continuity to the soil surface vanished. The modeling results clearly demonstrated the need to consider heat and vapor flow. It was shown, as a proof of principle, that MR relaxation time spectra may serve as a proxy to follow desaturation processes where spatially resolved transverse relaxation can reveal a secondary evaporation front.