Abstract

Solidago canadensis L. is a drought-tolerant, invasive plant, characterized by a large biomass of underground and aboveground parts. The aim of this study was to assess the accumulation of manganese (Mn) and copper (Cu) in the roots and rhizomes and the stems, leaves, and inflorescence parts in S. canadensis from two locations that differed in soil pH, organic carbon, and Mn and Cu concentrations. The concentration of the metals in the samples was determined by the AAS method; the pH was determined by the potentiometric method; and the content of organic carbon was determined using Tiurin’s method. The concentration of Mn and Cu in the roots of S. candensis correlated with the concentrations of the metals in the soil without regard to the soil condition or its organic carbon content. With a low soil pH and organic carbon content, Mn accumulation per 1 ramet in the aboveground parts of S. canadensis consisted over 50% of the total Mn content in the plant. In neutral or alkaline soils, the amount of Mn per 1 ramet accumulated in underground parts was over 60%. Regardless of the soil conditions, about 35% of Mn accumulated in rhizomes. Approximately 60% of copper accumulated in the underground parts of S. candensis (45% in rhizomes) without regard to the soil reaction or organic carbon content. The ability of the plant to accumulate large amounts of metals disposes Solidago canadensis as a candidate for the phytoremediation of soils contaminated with heavy metals.

Highlights

  • Manganese (Mn) and copper (Cu) are essential elements for the growth and development of plants (Marschner, 1995)

  • Soils in the Siedlce region are characterized by naturally-occurring heavy metals (Siebielec, 2017) and there are high concentrations of heavy metals connected with the mining industry in Olkusz (Kapusta, Szarek-Łukaszewska & Vogt, 2015)

  • The plants in low pH soil had the highest concentrations of Mn in the leaves, whereas in neutral or alkaline soil, the highest concentrations of Mn were found in the roots

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Summary

Introduction

Manganese (Mn) and copper (Cu) are essential elements for the growth and development of plants (Marschner, 1995). These elements participate in metabolic processes, including oxidation–reduction (redox) reactions in cells, photosynthesis, and the activation of enzymatic reactions (Ducic & Polle, 2005; Millaleo et al, 2010). Plants absorb metals from the soil and the availability of the metals is dependent upon the soil reaction and its organic matter content (Adamczyk-Szabela, Markiewicz & Wolf, 2015; Rosselli, Keller & Boschi, 2003). If the pH of the soil decreases, the absorption of Mn by the plant increases (Watmough, Eimer & Dillon, 2007). The influence of soil pH on the bioavailability of Cu for plants is small.

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