The Effect of Climate Warming on the Hydrochemistry of Alpine Lakes

The hydrochemistry of mountain lakes is highly conditioned by the chemicalcomposition of atmospheric deposition and by climate characteristics. Consequently these ecosystems have proved to be sensitive to long-term changes in both factors. Climate warming seems to be particularly pronounced in the Alpine region. A reduction of snow cover in space and time, due to less precipitation and higher temperatures, means a greater exposure of rocks and soils in the watersheds, which enhances weathering processes. In this paper we aim to evaluate the possible effect of these processes on long-term changes in the chemistry of alpine lakes. Recent climate changes affecting the study area were investigated through a data series referring to temperature, precipitation, snow depth and duration at some stations in the Ossola Valley. Chemical data of 35 lakes located in the Ossola and Sesia Valleys (Central Alps) were used. Lakes were sampled both in the late summer of 2000 and 2001 in the framework of two European Projects and the results compared with previous data (1984–1987). Two lakes (Boden Superiore and Inferiore, 2343 and 2334 m a.s.l., respectively), located in the northern part of the study area, have been sampled more or less continuously since the late 70s, enabling us to evaluate the trends of the main chemical variables. For lakes lying in catchments with highly soluble rocks, a comparison between the two data sets shows an increase of solute contents in the last few years. This result could be attributed to increased weathering rates due to climate warming.     

An Evaluation of Trace Metals in High-Altitude Lakes of the Central Alps

Alpine areas in north-western Italy are subject to high deposition of atmospheric pollutants. Chemical investigations on high-altitude lakes indicate that most of them are recovering from acidification; however, they are still affected by the deposition of pollutants from the atmosphere, especially of heavy metals. This study compares the concentrations of heavy metals in alpine lake waters with those found in atmospheric depositions, to identify the possible contribution of deposition inputs to surface water ecosystems. The results were analysed by multivariate statistical techniques to identify the main emission sources of the various metals. Levels of trace metals in alpine lakes are generally low, and bedrock and surficial geology proved to be a major factor controlling metal concentrations in lake water. In fact, terrigenous elements show a wide range of concentrations while metals of anthropogenic origin, such as lead and cadmium, are often below the detection limits of the method; chrome and nickel are also present in very low concentrations. The median values of heavy metals in Italian alpine lakes are similar to those found in other lake surveys performed in remote areas, especially as regards metals of anthropogenic origin. The Visual MINTEQ model was applied to long-term chemical data of selected alpine lakes, to calculate aluminium speciation and to simulate its change in response to gradual modifications in a unit of pH. The ultimate aim of the modelling was to evaluate the possible threat to aquatic organisms of these highly toxic compounds.

     

Thirty Years of Chemical Changes in Alpine Acid-Sensitive Lakes in the Alps

The Pennask Creek watershed in British Columbia (BC), Canada has been contaminated with acid rock drainage (ARD) and associated metal leaching (ML) as a result of highway construction. By combining existing and newly gathered information, this study determined the extent of metal contamination of the water and sediments, the potential biological impacts of this contamination, the influence of local geology, and estimated the potential risk to aquatic organisms. Surface water and sediment samples from the watershed were analyzed for general chemical parameters and trace metals. Rock samples were analyzed for mineralogy and chemical composition. Metal concentrations in water and sediments downstream of the ARD/ML source were higher than elsewhere in the watershed. Metals of concern include aluminum (Al), copper (Cu), and zinc (Zn). Analysis of historical water quality data indicated that the concentrations of these metals have decreased markedly since 2004, due to remediation efforts. Rock samples collected from the streambeds and banks were not found to be potentially acid generating, but did contain significant levels of metals. Al, Cu, and Zn levels consistently exceeded BC water and sediment quality guidelines for the protection of aquatic life, indicating that adverse biological effects are probable at stations downstream of the ARD/ML source. Benthic invertebrate monitoring over a 10-year period showed low abundance and diversity and a complete absence of sensitive taxa at downstream stations. Risk quotients indicated a likelihood of adverse biological effects for aquatic organisms, including rainbow trout, due to metal contamination in the watershed.