The mean soil temperature (10 cm depth) during the soil treatments was 28.2°C with diurnal variations ranged from around 24.0°C (as the lowest in the nights) to 34.0°C (as the highest in the daytime).
One plant trait to achieve conservative water use to increase water availability during reproductive develop is partial stomatal closure at a higher soil water content during the soil drying cycle than normally occurs in most plants [28, 57].
Zn isotopes help to trace which free Zn pool is mobilized by the tree via following the rooting depth and soil solution chemistry in contrasted local environments and how it changes during the soil thawing over growing season.
Sites of corn (Zea mays), soybean (Glycine max), and deciduous hardwood woodlands were sampled to estimate EWT and VWC during the Soil Moisture Experiment 2005 (SMEX05) near Ames, Iowa, USA.
The models were run using Landsat imagery collected during the Soil Moisture Atmosphere Coupling Experiment (SMACEX) in 2002 and model results were compared with observations from a network of flux towers deployed within the study area.
SOC was observed along with soil texture and bulk density during the Soil Moisture Active Passive Validation Experiment in 2012 (SMAPVEX12), the Soil Moisture Active Passive (SMAP) satellite algorithm development field sampling campaign held June 6 to July 19 in Southern Manitoba, Canada.
