Accordingly, negative linear relationships between diurnal changes in nitrate and Cl - and SO 4 2- contents were highly significant (Figures 12A,B ).
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Changes in <sup>15</sup>NO<sub>3</sub> <sup>-</sup> Availability and Transpiration Rate Are Associated With a Rapid Diurnal Adjustment of Anion Contents as Well as <sup>15</sup>N and Water Fluxes Between the Roots and Shoots.
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