Sulfur Mineralization: A Key Process for Diagnosing Its Deficiency in Wheat

Core Ideas A simplified balance was used to calculate apparent S mineralization in wheat. Apparent S mineralization predicted relative wheat grain yield. Sulfate‐S before sowing combined with particulate organic C diagnosed S status. Sulfur mineralization in soil should be considered in diagnostic methods based on soil analysis. Consideration of S mineralization could aid the development of S diagnostic methods in wheat ( Triticum aestivum L.) but this process has not been investigated under field conditions. The objectives of this study were to evaluate: (i) the use of a simplified S balance to quantify apparent S mineralization (S min‐app ) during the wheat growing cycle, (ii) the relationship between S min‐app and S mineralization indicators [N mineralized in anaerobic incubation (Nan) and total and particulate organic C (TOC and POC)], and (iii) the reliability of the proposed S mineralization indicators (Nan, TOC, and POC) for diagnosing S availability alone or combined with SO 4 2− –S content at sowing (S ini ). Fourteen field experiments were conducted to evaluate grain yield in response to S fertilization. Soil samples were taken before sowing and S ini , Nan, TOC, and POC were determined. Additionally, S min‐app was calculated in 7 out of 14 experiments through a simplified S balance. The main outcomes were: (i) S min‐app allowed us to compare S mineralization capacity among soils and was closely related to relative wheat grain yield ( R 2 = 0.92), (ii) S min‐app was related to S ini , Nan, TOC, and POC, (iii) POC was the S mineralization indicator that had the best performance for diagnosing S deficiency and its use in combination with S ini allowed for satisfactory diagnosis of S status in wheat via the equation: relative grain yield = 81.5 + (0.19 × S ini ) + (1.56 × POC) (R a 2 = 0.66). Sulfur mineralization proved to be an important process for wheat S nutrition.