Abstract

AimsThe release of heavy metals (such as Pb and Cd) from foliar litter play an important role in element cycling in alpine forest ecosystems. Although natural forest gaps could play important roles in the release of heavy metals from foliar litter by affecting the snow cover during the winter and solar irradiation during the growing season, few studies have examined these potential roles. The objectives of this study were to document changes in Pb and Cd dynamics during litter decomposition in the center of gaps and under closed canopies and to investigate the factors that controlled these changes during the winter and growing seasons.MethodsSenesced foliar litter from six dominant species, including Kangding willow (Salix paraplesia), Masters larch (Larix mastersiana), Mingjiang fir (Abies faxoniana), Alpine azalea (Rhododendron lapponicum), Red birch (Betula albosinensis) and Mourning cypress (Sabina saltuaria), was placed in litterbags and incubated between the gap center and closed canopy conditions in an alpine forest in the eastern region of the Tibetan Plateau. The litterbags were sampled at the snow formation stage, snow coverage stage, snow melt stage and during the growing season. The Pb and Cd concentrations in the sampled foliar litter were determined by acid digestion (HNO3/HClO4).Important findingsOver one year of decomposition, Pb accumulation and Cd release from the foliar litter occurred, regardless of the foliar litter species. However, Pb and Cd were both released from the foliar litter during the winter and accumulated during the growing season. Compared with the gap center and the canopy gap edge, the extended gap edge and the closed canopy showed higher Pb and Cd release rates in winter and higher Pb and Cd accumulation rates during the growing season, respectively. Statistical analyses indicate that the dynamics of Pb were significantly influenced by frequent freeze–thaw cycles in winter and appropriate hydrothermal conditions during the growing season, the dynamics of Cd were strongly influenced by species and the presence of a forest gap at different decomposition stages. These results show that forest gaps could inhibit Pb and Cd release from foliar litter in the alpine forest of western Sichuan. In addition, a decrease in the snow depth in the winter warming scenario would promote the release of Pb during foliar litter decomposition. There exist some difference that may be influenced by litter quality, microenvironment and microtopography during litter decomposition.

Highlights

  • The amount of certain elements delivered to the soil by decomposing litter is an important component of sustainable forest management [1]

  • Heavy metal dynamics have frequently been studied in forest ecosystems [9,10,11], data regarding the dynamics of Pb and Cd during litter decomposition in alpine regions, because of variation in the radiation and snow cover, regarding the effects of forest gaps on Pb and Cd dynamics, remain relatively scarce

  • Our results indicate that freeze-thaw cycles in winter and the suitable hydrothermal environment during the growing season at the extended gap edge and under the closed canopy could promote the release of Pb during foliar litter decomposition

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Summary

Introduction

The amount of certain elements delivered to the soil by decomposing litter is an important component of sustainable forest management [1]. Lead (Pb) and cadmium (Cd) have been considered among the top 20 pollutants on the USEPA priority list [2]. These heavy metals are toxic to most soil organisms when present in excessive concentrations[3], and the toxicity to soil organisms has a negative impact on material circulation and energy transformation of alpine forest ecosystem. In our previous studies of foliar litter decomposition, the seasonal snow cover had a significant impact on mass loss, nutrient dynamics and microbial biomass in the alpine forest [6,7,8]. Heavy metal dynamics have frequently been studied in forest ecosystems [9,10,11], data regarding the dynamics of Pb and Cd during litter decomposition in alpine regions, because of variation in the radiation and snow cover, regarding the effects of forest gaps on Pb and Cd dynamics, remain relatively scarce

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