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Forest Nitrogen Dynamics in Response to Increasing Nitrogen Deposition: Comparing Above-Canopy and Soil Fertilizations in a Mature Beech Forest. [PDF]
Teglia A +11 more
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Potential decoupling of CO2 and Hg uptake process by global vegetation in the 21st century. [PDF]
Yuan T +15 more
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Journal of Hydrology, 2004
Point throughfall data were generated in two representative red oak stands of a small Madrean watershed in northeastern Mexico during the 2000 and the 2001 wet seasons. Cumulative gross precipitation for 18 selected events was 392.9 mm, while the mean cumulative point throughfall flux from 38-fixed gauges was 331.0±9.0 mm (84.2±2.3%).
D.E Carlyle-Moses +2 more
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Point throughfall data were generated in two representative red oak stands of a small Madrean watershed in northeastern Mexico during the 2000 and the 2001 wet seasons. Cumulative gross precipitation for 18 selected events was 392.9 mm, while the mean cumulative point throughfall flux from 38-fixed gauges was 331.0±9.0 mm (84.2±2.3%).
D.E Carlyle-Moses +2 more
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Organic halogens in spruce forest throughfall
Chemosphere, 1998Abstract Deposition of dissolved organic halogens by throughfall was determined in a small spruce forest site in Denmark (56°28'N, 8°24'E). The mean annual deposition of dissolved organic halogens was 377 g ha−1yr−1, and larger than the general deposition by precipitation.
G. Öberg, C. Johansen, C. Grøn
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Throughfall variation under tree crowns
Journal of Geophysical Research, 1961It is suggested that the experimental design for sample measurement of throughfall may be improved. Specifically, distance and direction from trunk may constitute a significant source of variation that could be separated in analysis of variance from the unexplained variation.
Benjamin B. Stout, Richard J. McMahon
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1999
Forest canopies affect the amounts of water and nutrients reaching forest soils. Water and nutrient inputs under forest canopies are thus different from those in nearby open areas. Canopies intercept and retain part of the incident precipitation (intercepted water), which is eventually evaporated from the canopy and lost to the atmosphere.
Juan Bellot, Anna Àvila, Anselm Rodrigo
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Forest canopies affect the amounts of water and nutrients reaching forest soils. Water and nutrient inputs under forest canopies are thus different from those in nearby open areas. Canopies intercept and retain part of the incident precipitation (intercepted water), which is eventually evaporated from the canopy and lost to the atmosphere.
Juan Bellot, Anna Àvila, Anselm Rodrigo
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From rainfall to throughfall in a maritime vineyard
Science of The Total Environment, 2012This study deals with the characteristics of throughfall produced by vine (Vitis vinifera L.) in one of the most common pedoclimatic conditions for grape production: a soil derived from marine sediments under a temperate Mediterranean climate, and located rather close to the seacoast.
G, Brecciaroli +4 more
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Throughfall and stem-flow in wheat
Agricultural and Forest Meteorology, 1985Abstract The total amount of water reaching the ground, obtained by sealing the soil surface with latex, was compared with throughfall in the central third of the inter-row of a mature wheat canopy. For both rain and irrigation there were no systematic differences between the two collection methods, which indicates that stem-flow amounts were not ...
D BUTLER, N HUBAND
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Walker Branch Throughfall Displacement Experiment
2003The Walker Branch Watershed (∼100 ha), located at 35°58′ N latitude and 84°17′ W longitude, is a part of the U.S. Department of Energy’s (DOE’s) National Environmental Research Park near Oak Ridge, Tennessee (Johnson and Van Hook 1989). Long-term (50-year) mean annual precipitation is 1352 mm, and mean annual temperature is 14.2°C.
Paul J. Hanson +2 more
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Ammonia and Nitric Acid Dry Deposition and Throughfall
Water, Air, & Soil Pollution, 1995Since 1991 measurements of fluxes of ammonia have been carried out periodically at a forest location in the western part of Denmark. The ammonia deposition velocities and fluxes are estimated from gradient measurements done by denuders and micrometeorology.
Andersen, H. V., Hovmand, M. F.
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