Long-term impact of cement plant emissions on the elemental composition of both soils and pine stands and on the formation of Scots pine seeds

We investigated the long-term impact of the largest Russian cement plant on mesopodzol sandy soils and Scots pine stands. We determined the distributions of the total and available pools of Ca, Mg, K, Na, Mn, Fe, Zn, Ni, Cu, Pb and Cd in the soil profile to a depth of 60 cm (illuvial horizon) as well as the accumulation patterns of these elements in the vegetative and generative organs of Scots pine trees. High Ca accumulation in the impact zone soils was a result of CaO emissions by a cement plant. Also, CaO became the main cause of soil profile alkalization due to neutralization of soil acids and formation of calcium hydroxide or carbonates. Alkalization immobilized substantial amounts of Fe, Mn, Zn and Ni in the soil, reducing their availability. The most prominent effect of long-term cement production was a prominent Mn deficiency in vegetative and generative Scots pine organs due to the exhaustion of the available Mn pool in the illuvial horizon. The miniaturization of cones, a decrease in seed yield and a reduction in seed germinability were observed in the emission impact zones. Pretreatment of Mn-deficient seeds with manganese eliminated Mn deficiency but did not increase seed germination. [Display omitted] •Emissions of Ca compounds by the cement plant cause strong soil alkalization.•Substantial amounts of elements are immobilized in the soil due to its alkalization.•Heavy metal toxicity depends on its available pool rather than total pool in the soil.•The decrease of available Mn in the B-horizon leads to Mn deficiency in pine organs.•Cement dust impact lead to cone miniaturization, reduced seed yield and germinability. Cement plant emissions do not increase heavy metal toxicity for Scots pine trees due to soil alkalization but greatly affect the bioavailability of manganese for plants.