| GRADUATE STUDENTS GATHERING 
                                DATA FOR WETLANDS PROJECT
 Wetlands on Guam occur predominantly 
                                in the southern one half of the island. This is 
                                an underpopulated region of small coastal villages 
                                separated by steep and rolling topography etched 
                                into volcanic rocks. Terrains are variously covered 
                                with grasslands or ravine forests, or they have 
                                degenerated into badlands. End-member wetland 
                                types include tidal estuarine, tidal riverine, 
                                non tidal riverine, permanent palustrine, and 
                                ephem
  eral 
                                palustrine, but combinations of these are common. 
                                Their origin, distribution, evolution, and vulnerability 
                                are related to bedrock geology, soil and slope 
                                processes, tectonics, sea level changes, and to 
                                land use modifications. Their function and value 
                                as to flood control and affecting water quality 
                                are the subject of considerable research at WERI. 
 This project is aimed at developing a geochemical-sedimentation 
                                model that describes the flux of metals and nutrients 
                                being stored and moving through a perennial palustrine 
                                wetland downslope from a large tract of badlands. 
                                The study involves establishing hydrologic parameters, 
                                measuring slope retreat and sediment throughput 
                                out of the badlands, and chemically analyzing 
                                surface runoff and wetland pore waters, the latter 
                                through a gridded lysimeter array in the wetlands. 
                                Preliminary analysis of pore waters indicates 
                                that the wetlands are mobilizing and storing iron 
                                and manganese that enter from the badlands via 
                                groundwater seepage and in suspension. Concentrations 
                                of those metals may exceed three orders of magnitude 
                                beyond normal Guam river waters.
 The project has been funded by the 
                                Government of Guam, Bureau of Planning. Future 
                                related research will involve a) analyzing geochemical 
                                cycling in tidal riverine and estuarine wetlands, 
                                b) quantifying badlands denudation rates, c) studying 
                                geochemical reactions involving manganese and 
                                iron in the wetlands and downstream at the coast 
                                where they are co-precipitate on reef debris. 
                               For More Information on Wetlands 
                                Projects send e-mail to Dr. H. Galt Siegrist: 
                                [email protected] |