Composition and deposition of throughfall in a flooded forest archipelago (Negro River, Brazil)

The sources of spatial and temporal variation and rates of nutrient deposit ion via throughfall were studied for 9 months in the Anavilhanas archipelag o of the Negro River, Brazil. A total of 30 events was sampled individually for rain and throughfall chemistry in a I-ha plot of flooded forest. Throu ghfall samples were collected in 40 collectors distributed in five parallel transects in the study plot, while rain was collected in 4 collectors in a n adjacent channel. Volume-weighted mean (VWM) concentrations of solutes in rain were consistently lower than in throughfall, except for H+, NO3- and NH4+. Ratios of VWM concentrations of rain to throughfall indicated that K, followed by Mg2+ and PO43- were the most enhanced solutes as rain passed through the forest canopy. The deposition of solutes varied significantly a mong transects, except for Na+ and Ca2+, and was significantly correlated w ith maximum flooding depth, foliar nutrient content, soil fertility and can opy closure for most solutes. The concentrations of PO43- and most major io ns were higher in throughfall compared to those in rain due to canopy excha nge and dry deposition. In contrast, NO3-, NH4+ and H+ were retained due to immobilization by leafy canopy and ion exchange processes. Solute inputs v ia throughfall (not including stemflow) to a floodplain lake (Lake Prate) o f the archipelago accounted for 30 to 64% of the total for most solutes in the lake at high water, which indicates that throughfall is an important so urce of nutrients to the aquatic ecosystem of the Anavilhanas archipelago.