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. 2015 Nov 23;67(3):873–891. doi: 10.1093/jxb/erv502

Table 2.

Contribution of inorganic anions to equimolarity with cations in the leaf

Ionic concentration (mmol g–1 DW) Equimolarity (%) Contribution to equimolarity (%)
Cations Anions Inorganic anions Organic moleculesa SO4 2–+PO4 3– NO Cl
BS 1.76±0.05 b 0.58±0.09 b 32.6±4.4 b 67.4±4.4 a 14.3±0.9 b 17.1±3.4 a 1.1±0.2 b
SP 1.96±0.08 ab 0.65±0.08 b 32.7±3.6 b 67.3±3.6 a 24.3±1.9 a 7.7±2.2 b 0.7±0.05 b
N 2.10±0.05 a 0.72±0.06 b 34.4±3.0 b 65.6±3.0 a 8.9±0.3 b 25.0±2.9 a 0.5±0.02 b
CL 2.02±0.07 a 1.49±0.04 a 74.3±2.0 a 25.7±2.0 b 10.6±0.4 b 0.8±0.1 b 62.9±2.0 a
P-value * *** *** *** *** *** ***

Treatments consisted of the basal nutrient solution (BS) alone or supplemented with 5mM nitrate (N) or the sulphate+phosphate (SP) salt mixture containing the same cationic balance as in the CL and N treatments.

Anions and cations measured to calculate the data in the respective columns were: Cl, NO3 , SO4 2–, and PO4 3–anions; and K+, Ca2+, and Mg2+ cations.

Mean values ± SE, n=4–6. Levels of significance: *P≤0.05 and ***P<0.001. ‘Homogeneous group’ statistics was calculated through ANOVA test.

a Not measured: deduced from quantification of inorganic ions.