Potassium and Calcium Isotopic Fractionation by Plants (Soybean [Glycine max], Rice [Oryza sativa], and Wheat [Triticum aestivum])

• Published in: ACS earth and space chemistry 2018-07, Vol.2 (7), p.745-752
• Main Authors: Christensen, John N, Qin, Liping, Brown, Shaun T, DePaolo, Donald J
• Format: Article
• Language: English
• Subjects: calcium isotopes; hydroponics; INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; K isotopes; nutrient uptake and transport
• ISSN: 2472-3452; 2472-3452
• DOI: 10.1021/acsearthspacechem.8b00035

We conducted hydroponic experiments growing soybean (Glycine max), rice (Oryza sativa), and wheat (Triticum aestivum) under K and Ca replete conditions to establish the degree of K isotopic fractionation by plants, and compare the isotopic fractionation of Ca and K. Each of the test plants displays fractionation relative to the growth solution favoring the light isotopes of K and Ca. The average δ41K values of the roots from the three plant species were similar, and have an overall average of −0.55 ± 0.24‰ 2s, while the overall average δ44Ca for roots is −0.67 ± 0.44. For leaves, the overall average of δ41K is −0.97 ± 0.4‰, compared to an overall average leaf δ44Ca of −0.83 ± 0.09‰. In the case of the soybean plants, the lightest K and Ca occurs in the stems with average δ41K of −1.31 ± 0.40‰ 2s and average δ44Ca of −1.20 ± 0.19 ‰ 2s. We present a simple box model involving the relative fluxes of K and its isotopic fractionation that reproduces our K isotopic observations and suggests a fractionation of ∼0.8‰ with K uptake from solution by roots. Directly comparing the per amu fractionation of K and Ca reveals an average factor of 2.05 ± 0.50 2s greater fractionation of K isotopes which may reflect their different roles and behaviors in plants.