Preliminary results from both the pilot plot and the six undisturbed control plots indicate decreasing pore water salinity with increasing distance from the creek in marsh areas vegetated by J. roemerianus. In contrast, the S. alterniflora vegetation in the pilot plot shows increasing salinity along the same path of increasing distance from the tidal creek. However, the S. alterniflora salinities collected from the six undisturbed control plots did not continue the trend.
The six undisturbed control sections indicate a higher
concentration in average pore water salinity within the J.
roemerianus vegetation compared to that of S. alterniflora
(Figure
2). This also seems to be the case regarding salinities in the
pilot plot, however, the other manipulations underway obscure
this result. Support for the difference between vegetation types
results from how the two different plants deal with their saline
environment. J. roemerianus is a salt "excluder"; the salt
stays in the pore water. On the other hand, S.
alterniflora is a salt "excreter"; the salt is taken up from the
pore water and then excreted from the leaves.
This study examined pore water concentrations of phosphate
(PO4=) in the six undisturbed control plots and found higher
levels in the S. alterniflora than the J. roemerianus
(Figure 3)
. Whether the difference results from uptake, mineralization, or
exchange is unknown.
From the data collected in the six undisturbed control
plots, it appears that distance from the tidal creek plays a
major role in determining pore water ammonium (NH4+)
concentrations. The two near locations of both the S.
alterniflora and J. roemerianus had higher levels of ammonium
than the two far locations
(Figure 4).
The samples from this analysis were collected by suction lysimeters on six dates ranging from July 20, 1993 to August 11, 1993. Tidal creek water was not pumped into the pilot plot at regular intervals until late August 1993.