| _bx_events_caption_title | Means and rangesfor all sediment nitrogen parameters are shown in Tables 28-31. | ||
| _bx_events_caption_place | ocean123 | ||
| _bx_events_caption_event_start | 30.03.2011 15:49 (419 Days Ago) | ||
| _bx_events_caption_event_end | 29.03.2012 15:49 (54 Days Ago) |
![]() |
![]() |
![]() |
![]() |
Empty
|
![]() |
![]() |
![]() |
![]() |
The Niagara River mouth and the Genesee River mouth showed no variation with respect to distance from shore or from east to west, for any nitrogen forms measured.In the nearshore zone, mean nitrate concentrations were generally highest along the 8 km contour. The mean nitrate concentrations at the 8 and 4 km contour showed the same basic west to east fluctuations (Figure 3*0; however, the magnitude of the nitrate concentration was greater at the 8 km contour. Nitrate concentrations througout the year were significantly higher at the eastern end of the study area.Station 357, a Coach Outlet Store Online Genesee River mouth station, had concentrations which were greater by a factor of 10^ over the other stations sampled. This area of high nitrate content was consistent throughout the year, with a mean of 4.4 and a range of 3.4 to 5.8 mg N/g. It is believed that this area of high concentration was a function of an unknown change in geomorphology.Ammonia concentrations showed Increasing concentration with increasing distance from shore during the majority of the study period with only one exception, Transect 219-22l, which showed decreasing values with increasing distance from shore for each cruise. The highest areal concentrations were along the 8 km contour from Station 206 to 215 and along the 4 km contour from Station 211 to 220 (Figure 35).Generally, it can be stated that the 8 km contour had Coach Bags Outlet higher organic-N concentrations than did the 4 km contour, but consistently the observed organic-N concentrations between the 8 and 4 km contour, were seen to be inversely proportional throughout the study area (Figure 36).Yearly total-N fluctuations followed those of organic-N (Figures 36-37 ). This phenomenon is obvious, since generally >50% of the total-N concentration was organic in nature.The Niagara River mouth for purposes of description was divided into a western and eastern zone. The western zone included Stations 363-374 and 376, and the eastern zone included Stations 375 and 377-386. The means and ranges Christian Louboutin Outlet for the carbonate carbon (CC) and the organic carbon (OC) at the collections from the western zone were 1.44$ CC, 0.10-6.75 CC and 0.21$ OC, 0. 03-1.34 OC, respectively. The means and ranges for CC-OC Christian Louboutin Shoes in the eastern zone samples were Coach Outlet Stores 0.88$ CC, 0.68-1.073 CC and Coach Bags On Sale 0.07$ OC, 0.05-0.14$ OC, respectively. During the IFYGL project 38 samples were Coach Handbags Outlet analyzed for CC-OC, thirty-threesamples from the western zone and five from the eastern zone. Table 32 shows that the western zone sample means and ranges were consistently higher in CC-OC than those from the eastern zone.
- There are no comments yet






