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Titlebook: Analysis of Biogeochemical Cycling Processes in Walker Branch Watershed; Dale W. Johnson,Robert I. Hook Textbook 1989 Springer-Verlag New

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Forest Meteorology,erials and energy between the forest and the atmosphere in which it is immersed. Consequently, many of the physical, chemical, and biological phenomena operating in forested watersheds are functions of these canopy-atmosphere interactions.
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Water,h erosion of solid materials over millenia. Dissolution and transport of solutes are a major component of weathering and mineral cycling processes. Besides these hydrologic processes, water is an essential component of biological systems, and the movement of water through vegetation (transpiration)
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Carbon Dynamics and Productivity, the growth, development, and decay of biological systems. These compounds are not only used internally by the autotrophs that synthesize them but are also released by exudation and decay to the heterotrophs that use these compounds for their own growth and development. In forests, a myriad of organ
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Terrestrial Nutrient Cycling,ram’s effort to characterize productivity and nutrient cycling in forests throughout the world (summarized by Cole and Rapp 1981). These early studies not only characterized the nutrient cycles and compared them with other forested watersheds, as originally intended (e.g., Henderson et al. 1978), bu
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