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  • Tác giả: Friedman, S.P.;  Người hướng dẫn: -;  Người tham gia: Gamliel, A. (2019)

  • A previously derived analytical solution to the quasi‐linear form of the water flow equation is used to analyze (i) steady, coupled plant water uptake from a surface water emitter in a confined cylindrical soil domain with a non‐evaporating surface in the presence of a shallow water table, and (ii) water uptake from only the water table in the absence of a surface emitter. Illustrative examples serve to analyze and discuss water‐uptake rates of a subsurface, spherical, conceived root zone and the complex water‐flow patterns occurring in either natural fields with shallow groundwater or artificial lysimeters. The coupled source–sink–water table model is also used to illustrate the dependence of the contributions of surface emitter and water table to the overall water‐uptake rate on c...

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  • Tác giả: Lazik, D.;  Người hướng dẫn: -;  Người tham gia: Vetterlein, D; Salas, S.M.; Sood, P.; Apelt, B.; Vogel, H.J. (2019)

  • This variability is attributed to the spatiotemporal heterogeneity of both plant–soil–microbiome interactions and the local conditions governing gas transport. For the characterization of a given soil, the local heterogeneities should be replaced by some meaningful average. To this end, we introduce a line sensor based on tubular gas‐selective membranes that is applicable at the field scale for a wide range in water content. It provides the average CO2 concentration of the ambient soil along its length. The new technique corrects for fluctuating external conditions (i.e., temperature and air pressure) and the impact of water vapor without any further calibration. The new line sensor was tested in a laboratory mesocosm experiment where CO2 concentrations were monitored at two depths ...

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