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28 +Deceased Hwlrologicol and Linii7olo~iculAspucrs of’ Lriku MoniloIii7g Edited by Pertti Heinonen, Giuliano Ziglio and Andre Van der Beken (. 1 INTRODUCTION Groundwater input to lakes and seas has received increasing attention during the last ten years, as better techniques have been developed to quantify this flow and assess its hydrological and ecological importance. This source term occurs wherever a continental aquifer is hydraulically connected to the coastal areas of lakes and seas.
1994. Small catchment research in the evaluation and development of forest management practices, in Moldan, B. and Cerny, J. (Eds), Biogeochemistry of Small Catchments: A Toolfor Environmental Research, John Wiley & Sons, Chichester, SCOPE Report 51, 383408. Turner, J. V. and Macpherson. D. , 1990. Mechanisms affecting streamflows and stream water quality: An approach via stable isotope, hydrogeochemical and time series analysis, Water Resour. , 26, 3005-3019. Vogt, K . , Grier, C. C. and Vogt, D.
Physical (thermal and optical conditions) and chemical variables. e. bacterioplankton, phytoplankton, zooplankton, bottom fauna, periphytic communities, macrophytes, fishes, etc. The biocoenosis is the living part of the ecosystem. Of course, a biocoenosis can best be characterized by different biological methods, phytoplankton counting, species diversity, etc. Many of these themes will also be discussed in this present book (see Part Two). g. Hutchinson, 1957; Wetzel, 1983): (a) the oxygen status, including the organic compounds affecting the oxygen budget; (b) the nutrient (phosphorus and nitrogen) status; (c) the acidity status; (d) the harmful substances, including heavy metals and a large number of organic compounds.