Hydrochemical fluxes in rainfall, throughfall, and stemflow in Pinus sylvestris var. mongolica plantation, northeast China

Rainfall is one of the primary sources of chemical inputs in forest ecosystems, and the basis of forest nutrient cycling. To explore the variations of nutrient cycling and nutrient balance in rainfall redistribution process in urban forest ecosystem, we investigated the chemistry of rainfall, throughfall and stemflow in a plantation of Pinus sylvestris var. mongolica distributed in Harbin city of Northeastern China. Mean nutrient concentrations in stemflow were higher than in throughfall and rainfall. Over the growing season observation, the ions (NO3- , PO43- , SO42- , Cl- , K, Ca and Mg) fluxes in rainfall, throughfall and stemflow were 64.021 kg center dot ha(-1) , 44.928 kg center dot ha(-1) and 15.414 kg center dot ha(-1) respectively. The net throughfall and stemflow deposit was-3.679 kg center dot ha(-1) , in the growing season. The ion input in precipitation, throughfall and stemflow were mainly NO3- , SO(4)(2-)and Ca, and the canopy of P. sylvestris var. mongolica plantation can wash off NO3- and Mg in rainfall, but retain PO43- , SO42- , Cl- , K and Ca slightly. Our findings will facilitate a greater understanding of nutrient balance in canopy water fluxes in an urban area.