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Forest ecosystems represent a major type ofland use in Germanyand in Europe. They provide a number of functions, or ecosystem services, beneficial to humans, namely biomass production, regulation of the water- and energy cyde, C and N sequestration, erosion control, recreation, and they act as habitat for numerous species. The stability of forest ecosystems in Europe as influenced by the deposition of air pollutants has been a matter of debate for more than 20 years. Besides atmospheric deposition, other environmental conditions affecting forest ecosystems, such as temperature, CO content of the atmosphere 2 and precipitation, have significantly changed in the past and continue to change in the future. Quantifying and predicting the effects of these changes on ecosys tem functioning are achallenge to ecosystem research and also a requirement to establish sustainable use of forest ecosystems in the future. This book summarizes results of long-term, interdisciplinary ecosystem research conducted in two forested catchments and coordinated at the Bayreuth Institute of Terrestrial Ecosystem Research (BITÖK), University of Bayreuth, Germany. It does not aim to summarize all the research of BITÖ K in the past decade, which would go far beyond the studies in these two catch ments. Instead, we concentrate here on the long-term developments in the biogeochemistry of carbon and mineral elements and on the water cyde, at both the plot and the catchment scale.
Distinguished multinational contributors present research of small catchments to examine a variety of environmental problems, especially those of acidification, forest management and land-use changes. Divided into two parts, it introduces theoretical concepts followed by a review of atmospheric deposition and evaluation of weathering and erosion processes. The second half deals with the methodology of the given discipline, stressing novel approaches and discussing problems.
​This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change. The evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future. The BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme.
This international rigorously peer-reviewed volume critically synthesizes current knowledge in forest hydrology and biogeochemistry. It is a one-stop comprehensive reference tool for researchers and practitioners in the fields of hydrology, biogeoscience, ecology, forestry, boundary-layer meteorology, and geography. Following an introductory chapter tracing the historical roots of the subject, the book is divided into the following main sections: · Sampling and Novel Approaches · Forest Hydrology and Biogeochemistry by Ecoregion and Forest Type · Hydrologic and Biogeochemical Fluxes from the Canopy to the Phreatic Surface · Hydrologic and Biogeochemical Fluxes in Forest Ecosystems: Effects of Time, Stressors, and Humans The volume concludes with a final chapter that reflects on the current state of knowledge and identifies some areas in need of further research.
Stream Ecosystems in a Changing Environment synthesizes the current understanding of stream ecosystem ecology, emphasizing nutrient cycling and carbon dynamics, and providing a forward-looking perspective regarding the response of stream ecosystems to environmental change. Each chapter includes a section focusing on anticipated and ongoing dynamics in stream ecosystems in a changing environment, along with hypotheses regarding controls on stream ecosystem functioning. The book, with its innovative sections, provides a bridge between papers published in peer-reviewed scientific journals and the findings of researchers in new areas of study. Presents a forward-looking perspective regarding the response of stream ecosystems to environmental change Provides a synthesis of the latest findings on stream ecosystems ecology in one concise volume Includes thought exercises and discussion activities throughout, providing valuable tools for learning Offers conceptual models and hypotheses to stimulate conversation and advance research
Hydrobiogeochemical patterns were studied in two forested catchments in the Czech Republic, one underlain by leucogranite (Lysina), the other by serpentinite. The objective was to compare and contrast element pools and fluxes in the catchments with similar topography, vegetation, climate, and atmospheric deposition, but different lithology. High weathering rates at the serpentinite site resulted in magnesium as the dominant cation on the soil exchange complex and in drainage water. Other basic cations (calcium, potassium, sodium) showed relatively low concentrations and outflow in streamwater. The catchment exhibited high base saturation (BS) in mineral soil, and near neutral soil and stream pH, despite elevated inputs of acidic deposition. Slow growth of Norway spruce may be caused by potassium deficiency, magnesium oversupply and/or nickel toxicity. In contrast, the leucogranite site showed low concentrations of exchangeable basic cations on the soil exchange complex and in streamwater. Soil and drainage water were highly impacted by acidic deposition. Soil pH was acidic throughout the soil profile, and the BS of the mineral soil was low. Supplies of basic cations from atmospheric deposition and soil processes were smaller than inputs of sulfate on an equivalence basis, resulting in low pH and high concentrations of aluminum in drainage water. Needle yellowing in Norway spruce was possibly the result of magnesium deficiency. These catchments served as valuable end-members of ecosystem sensitivity to severe levels of acidic deposition. The second objective was to apply a plant-soil-water model PnET-BGC/CHESS at Lysina. Forest growth and hydrobiogeochemistry were simulated for the period 1550-2050. Simulated concentrations of sulfate, fluoride, calcium, magnesium, sodium, potassium, silica, iron, and aluminum were similar to streamwater concentrations measured in 1990-1994. The model moderately overpredicted hydrogen ion, chloride and dissolved organic carbon, and highly overpredicted nitrate and especially ammonium. A scenario of sulfur inputs reductions by 67% of 1991-1994 values in 1995-2050 predicted a further decrease in soil BS between 1995 and 2050. A simulation in which inputs of sulfur were reduced by 90% showed an increase in BS after 2030. Simulations showed that desorption of previously stored sulfur to drainage water would delay recovery from acidic deposition.
Elements move through Earth's critical zone along interconnected pathways that are strongly influenced by fluctuations in water and energy. The biogeochemical cycling of elements is inextricably linked to changes in climate and ecological disturbances, both natural and man-made. Biogeochemical Cycles: Ecological Drivers and Environmental Impact examines the influences and effects of biogeochemical elemental cycles in different ecosystems in the critical zone. Volume highlights include: Impact of global change on the biogeochemical functioning of diverse ecosystems Biological drivers of soil, rock, and mineral weathering Natural elemental sources for improving sustainability of ecosystems Links between natural ecosystems and managed agricultural systems Non-carbon elemental cycles affected by climate change Subsystems particularly vulnerable to global change The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals. Book Review: http://www.elementsmagazine.org/archives/e16_6/e16_6_dep_bookreview.pdf
"Since the early 1960s, the Hubbard Brook Experimental Forest in the White Mountains of New Hampshire has been one of the most comprehensively studied landscapes on earth. This book highlights many of the important ecological findings amassed during the long-term research conducted there, and considers their regional, national, and global implications." -- P.2 of cover.