Fate of selenium in biofortification of wheat on calcareous soil: an isotopic study

Abstract

Selenium (Se) biofortification of staple cereal crops can improve the Se nutritional status of populations. A field trial employing an enriched stable isotope of Se ( 77 Se) was undertaken over three consecutive cropping seasons in a coarse-textured, calcareous soil in Gilgit-Baltistan, Pakistan. The objectives were to (1) assess the feasibility and efficiency of Se biofortification, (2) determine the fate of residual Se, and (3) assess the consequences for dietary Se intake. Isotopically enriched 77 Se ( 77 Se Fert ) was applied, either as selenate or as selenite, at three levels (0, 10, and 20 g ha −1 ) to a wheat crop. Residual 77 Se Fert availability was assessed in subsequent crops of maize and wheat without further 77 Se Fert addition. Loss of 77 Se Fert was c.35% by the first (wheat) harvest, for both selenium species, attributable to the practice of flood irrigation and low adsorption capacity of the soil. No 77 Se Fert was detectable in subsequent maize or wheat crops. The remaining 77 Se Fert in soil was almost entirely organically bound and diminished with time following a reversible (pseudo-)first-order trend. Thus, repeat applications of Se would be required to adequately biofortify grain each year. In contrast to native soil Se, there was no transfer of 77 Se Fert to a recalcitrant form. Grain from control plots would provide only 0.5 µg person −1 day −1 of Se. By contrast, a single application of 20 g ha −1 Se VI could provide c. 47 µg person −1 day −1 Se in wheat, sufficient to avoid deficiency when combined with dietary Se intake from other sources (c. 25 µg day −1 ).

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