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Separate envelope experiments were performed at different Ca concentrations (via CaCl2 addition), which consisted of approximately 1 (background DOM concentration), 10, or 30 mM Ca in order to capture typical behavior at high soil porewater Ca concentrations [33, 37].
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However, legumes may suppress their energy-consuming symbiotic N2 fixation at high soil N availability.
We present data aimed at answering the question: is symbiotic N fixation reduced at high soil salinities?
In support of our second hypothesis, we found that for three of the four soils variables (soil moisture, organic matter, and microbial biomass) FD appeared to have the most positive effect at higher soil resource levels.
However, the increase of emodin content at higher soil nitrogen was only significant in FBM.
Specifically, GO dispersions exhibit Newtonian behavior in intermediate range at low concentration and typical shear thinning behavior at high concentration.
In some cases at Sites 1 and 3 there are distinct very high soil strength values close to the soil surface.
Leaf damage increased the N content in FBP at both soil N levels and in FBM at the higher soil N level and decreased the N content in FJ at the lower soil N level.
First, at high matric potentials soil organic matter affected soil water retention mainly through altering soil structural parameters and thereby soil bulk density.
, 7) show an alternating behavior at progressively higher frequencies.
We argue that, although the tilt angle of the modules affects the soiling rate, the high soiling rate observed at the northern most locations (Arica and Iquique) is mainly due to the high aerosol loading at those sites.
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