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Salt marshes atmospheric inputs

Inputs, outputs and exchanges of N with systems adjacent to salt marshes are generally much smaller in magnitude than internal fluxes (Table 22.7). The source and relative importance of various external inputs of N to salt marshes varies from system to system. While the input of N from rivers is potentially large, most of this N is probably not taken up by salt marshes but is processed in aquatic portions of estuaries or routed to the open ocean. On average, the largest input is from N fixation (2-15 g N m year ), followed by atmospheric deposition (0.5-2.2 g N year ). Groundwater inputs are a major source of N in some smaller salt marshes with developed uplands such as found in the northeastern United States. [Pg.1020]


See other pages where Salt marshes atmospheric inputs is mentioned: [Pg.606]    [Pg.1000]    [Pg.1002]    [Pg.1023]    [Pg.211]    [Pg.141]    [Pg.435]    [Pg.407]   
See also in sourсe #XX -- [ Pg.1002 ]




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