William H. McDowell – författare

The Ecosystems Research Center (ERC) was established at Cornell U ni­ versity in October 1980 by the Environmental Protection Agency (EPA) with the goals of: 1. Identifying fundamental principles and concepts of ecosystems sci­ ence and the determination of their importance in understanding and pre­ dicting the responses of ecosystems to stress, the description of the basic mechanisms that operate within ecosystems, and an examination of the stability of ecosystem structure and function in the face of stress. 2. Testing the applicability of those theoretical concepts to problems of concern to the EPA through a consideration of retrospective and other case studies. In line with these goals, the Hudson River ecosystem provided the basis for the first major retrospective study undertaken by the ERC. The goal of the project was to develop recommendations concerning how ecosystem monitoring can and should be carried out in support of EPA''s regulatory responsibilities. Our hope was and is that the experience gained from this study will be broadly applicable to a range of manage­ ment problems involving estuarine ecosystems, and will lead to more effective regulation.

The Ecosystems Research Center (ERC) was established at Cornell U ni­ versity in October 1980 by the Environmental Protection Agency (EPA) with the goals of: 1. Identifying fundamental principles and concepts of ecosystems sci­ ence and the determination of their importance in understanding and pre­ dicting the responses of ecosystems to stress, the description of the basic mechanisms that operate within ecosystems, and an examination of the stability of ecosystem structure and function in the face of stress. 2. Testing the applicability of those theoretical concepts to problems of concern to the EPA through a consideration of retrospective and other case studies. In line with these goals, the Hudson River ecosystem provided the basis for the first major retrospective study undertaken by the ERC. The goal of the project was to develop recommendations concerning how ecosystem monitoring can and should be carried out in support of EPA's regulatory responsibilities. Our hope was and is that the experience gained from this study will be broadly applicable to a range of manage­ ment problems involving estuarine ecosystems, and will lead to more effective regulation.

This book highlights recent advances in the discipline of biogeochemistry that have directly resulted from the development of critical zone (CZ) science. The earth's critical zone (CZ) is defined from the weathering front and lowest extent of freely circulating groundwater up through the regolith and to the top of the vegetative canopy. The structure and function of the CZ is shaped through tectonic, lithologic, hydrologic, climatic, and biological processes and is the result of processes occurring at multiple time scales from eons to seconds. The CZ is an open system in which energy and matter are both transported and transformed. Critical zone science provides a novel and unifying framework to consider those coupled interactions that control biogeochemical cycles and fluxes of energy and matter that are critical to sustaining a habitable planet.  Biogeochemical processes are at the heart of energy and matter fluxes through ecosystems and watersheds. They control thequantity and quality of carbon and nutrients available for living organisms, control the retention and export of nutrients affecting water quality and soil fertility, and influence the ability for ecosystems to sequester carbon. As the term implies, biogeochemical cycles, and the rates at which they occur, result from the interaction of biological, chemical, and physical processes. However, finding a unifying framework by which to study these interactions is challenging, and the different components of bio-geo-chemistry are often studied in isolation.  The authors provide both reviews and original research contributions with the requirement that the chapters incorporate a CZ framework to test biogeochemical theory and/or develop new and robust predictive models regarding elemental cycles. The book demonstrates how the CZ framework provides novel insights into biogeochemistry.

This book highlights recent advances in the discipline of biogeochemistry that have directly resulted from the development of critical zone (CZ) science. The earth''s critical zone (CZ) is defined from the weathering front and lowest extent of freely circulating groundwater up through the regolith and to the top of the vegetative canopy. The structure and function of the CZ is shaped through tectonic, lithologic, hydrologic, climatic, and biological processes and is the result of processes occurring at multiple time scales from eons to seconds. The CZ is an open system in which energy and matter are both transported and transformed. Critical zone science provides a novel and unifying framework to consider those coupled interactions that control biogeochemical cycles and fluxes of energy and matter that are critical to sustaining a habitable planet.  

Biogeochemical processes are at the heart of energy and matter fluxes through ecosystems and watersheds. They control thequantity and quality of carbon and nutrients available for living organisms, control the retention and export of nutrients affecting water quality and soil fertility, and influence the ability for ecosystems to sequester carbon. As the term implies, biogeochemical cycles, and the rates at which they occur, result from the interaction of biological, chemical, and physical processes. However, finding a unifying framework by which to study these interactions is challenging, and the different components of bio-geo-chemistry are often studied in isolation.  

The authors provide both reviews and original research contributions with the requirement that the chapters incorporate a CZ framework to test biogeochemical theory and/or develop new and robust predictive models regarding elemental cycles. The book demonstrates how the CZ framework provides novel insights into biogeochemistry.