Titlebook: North American Temperate Deciduous Forest Responses to Changing Precipitation Regimes; Paul J. Hanson,Stan D. Wullschleger Book 2003 Sprin

Pelvic-Floor

Soil Carbon Turnovertion). If carbon uptake by forest vegetation exceeds C loss by vegetation and soils, the forest is a net sink of atmospheric carbon. Currently, regrowing temperate forest ecosystems of the eastern United States are storing C (Goulden et al. 1996; Greco and Baldocchi 1996; Hollinger et al. 1999; Curt

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Response of Understory Tree Seedling Populations to Spatiotemporal Variation in Soil Moisture shade conditions. Because they are small plants with relatively shallow root systems, they are subjected to water stress to a much greater degree than the more deeply rooted trees, which also have a greater drying effect on the soil through the transpiration of their larger canopies.

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978-1-4612-6506-1Springer Science+Business Media New York 2003

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https://doi.org/10.1007/978-1-4613-0021-2Oxide; Precipitation; Scale; biodiversity; carbon; carbon dioxide; cyclin; deciduous forest; ecosystem; envir

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Soil Carbon Turnovertion). If carbon uptake by forest vegetation exceeds C loss by vegetation and soils, the forest is a net sink of atmospheric carbon. Currently, regrowing temperate forest ecosystems of the eastern United States are storing C (Goulden et al. 1996; Greco and Baldocchi 1996; Hollinger et al. 1999; Curtis et al. 2002).

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