4.7 Article

Tracing the fate of phosphorus fertilizer derived cadmium in soil-fertilizer-wheat systems using enriched stable isotope labeling

Journal

ENVIRONMENTAL POLLUTION
Volume 287, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2021.117314

Keywords

Cadmium; Phosphorus fertilizer; Wheat; Stable isotope labeling; Source tracing

Funding

  1. Swiss Parliament via the National Research Program (NRP) Healthy Nutrition and Sustainable Food Production (SNSF) [69, 406940_145,195/1]

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The use of phosphorus fertilizers containing cadmium can lead to toxic heavy metal pollution in arable soils. Soil pH is a key factor affecting the partitioning and uptake of cadmium in soil-wheat systems. The majority of applied cadmium remains in the soil and is potentially available for plant uptake in subsequent crop cycles.
Applying mineral phosphorus (P) fertilizers introduces a considerable input of the toxic heavy metal cadmium (Cd) into arable soils. This study investigates the fate of P fertilizer derived Cd (Cd-dff) in soil-wheat systems using a novel combination of enriched stable Cd isotope mass balances, sequential extractions, and Bayesian isotope mixing models. We applied an enriched Cd-111 labeled mineral P fertilizer to arable soils from two long-term field trials with distinct soil properties (a strongly acidic pH and a neutral pH) and distinct past mineral P fertilizer application rates. We then cultivated wheat in a pot trial on these two soils. In the neutral soil, Cd concentrations in the soil and the wheat increased with increasing past mineral P fertilizer application rates. This was not the case in the strongly acidic soil. Less than 2.3% of freshly applied Cd-dff was taken up by the whole wheat plant. Most of the Cd(dff )remained in the soil and was predominantly (>95% of freshly applied Cd-dff) partitioned into the easily mobilizable acetic acid soluble fraction (F1) and the potentially mobile reducible fraction (F2). Soil pH was the determining factor for the partitioning of Cd-dff into F1, as revealed through a recovery of about 40% of freshly applied Cd-dff in F1 in the neutral pH soil compared with about 60% in the strongly acidic soil. Isotope mixing models showed that F1 was the predominant source of Cd for wheat on both soils and that it contributed to over 80% of the Cd that was taken up by wheat. By tracing the fate of Cd-dff in entire soil-plant systems using different isotope source tracing approaches, we show that the majority of Cd-dff remains mobilizable and is potentially plant available in the subsequent crop cycle.

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