RETENTION AND LEACHING LOSSES OF ATMOSPHERICALLY-DERIVED NITROGEN IN THE AGGRADING COASTAL WATERSHED OF WAQUOIT BAY, MA

Citation
K. Lajtha et al., RETENTION AND LEACHING LOSSES OF ATMOSPHERICALLY-DERIVED NITROGEN IN THE AGGRADING COASTAL WATERSHED OF WAQUOIT BAY, MA, Biogeochemistry, 28(1), 1995, pp. 33-54
Citations number
75
Categorie Soggetti
Environmental Sciences","Geosciences, Interdisciplinary
Journal title
ISSN journal
01682563
Volume
28
Issue
1
Year of publication
1995
Pages
33 - 54
Database
ISI
SICI code
0168-2563(1995)28:1<33:RALLOA>2.0.ZU;2-K
Abstract
Extensive areas of the eastern United States are being exposed to elev ated levels of nitrogen in precipitation, with levels of inorganic N i n wet deposition ranging from 5 to over 20 times preindustrial, backgr ound levels. This increase in N loading to the terrestrial system, cou pled with changes in land use in coastal regions in particular, has dr amatically increased the level of nutrient loading from watersheds to the point that coastal waters are today among the most intensely ferti lized ecosystems on earth. Studies in upland, aggrading forests have g enerally found that precipitation N inputs are efficiently sequestered in forest biomass and soil organic matter. However, acidic soils, san dy, porous parent substrates, and chronic inputs of salt spray common to coastal watersheds may all reduce the potential for N sequestration by the terrestrial community. We assessed the role of coastal forests in the long-term storage and retention of atmospherically-derived N i n the watersheds of Waquoit Bay, MA, an increasingly eutrophic estuary on Cape God, by measuring precipitation inputs, storage, and lysimete r outputs below the rooting zone in a chronosequence of sites released from agriculture at different times. Calculated annual retention effi ciencies were relatively low for an N-limited, aggrading forest (40-62 %), and leaching losses did not vary with site age from young pine sta nds to mature beech forests. Nearly all nitrogen input was retained du ring summer months except in months with very high rainfall events. Ni trogen was released during the dormant-season in proportion to water f lux through the forest floor. The composition of lysimeter output was 76% DON, 11% NO3-, and 13% NH4+. Total water flux and infiltration app ear to be more important determinants of N retention in this sandy, co astal site than in more upland forest ecosystems; sandy systems may in herently have a low N retention efficiency.