Fate and effects of nutrients and heavy metals in experimental salt marsh ecosystems

Fate and effects of the macro nutrients nitrogen and phosphorus, and the heavy metals zinc, copper and cadmium, brought into experimental salt marsh ecosystems via sediment supply, were studied over a three-year period. The supply of sediment from the Marsdiep (at a low and high rate) and from the harbour of Delfzijl (at a high rate) led to an increase of the macro nutrients and heavy metals in the top soil. The growth of the salt marsh plants Aster tripolium, Puccinellia maritima and Spartina anglica and the uptake of the macro nutrients and heavy metals by the plants was only slightly affected by the addition of sediment. A high load of sediment led to an increase in growth or in the concentrations of the macro nutrients or heavy metals in the plants at a number of sampling dates, but only minor differences between treatments were found. From a mass balance constructed over a three-year study period it could be concluded that about 50% of the macro nutrients and heavy metals were retained in the salt marsh sediment. This was equal to the retained amount of organic matter, indicating that retention of the elements was closely related to retention of organic matter. The 50% loss of the macro nutrients and heavy metals probably occurred via ebb tides after resuspension of sediment and organic matter.     

Effects of nitrogen addition on the growth of the salt marsh grassElymus athericus

Effects of nitrogen addition on the growth of the salt marsh grassElymus athericus were studied under greenhouse conditions. The addition of inorganic nitrogen (in the form of nitrate or ammonium and ranging from 0–24 g N/m²) stimulated the growth ofElymus athericus at the highest addition. Addition of nitrogen led to an increase of the soil nitrate concentrations both in the nitrate and ammonium treated soil in the first period of the experiment, whereas no differences were present at the end of the experiment. Ammonium in the ammonium treatments was transformed to nitrate within 15 days. In another experiment the values of the stable isotope nitrogen-15—expressed as δ¹⁵N-in nitrogen compounds used as fertilizer, in salt marsh soil and ofElymus athericus were measured. The δ¹⁵N of the N-compounds added (between ?3.2 and +2.6‰) were lower than the soil (ca.+10‰) and plants (ca.+8‰). During growth in water culture the δ¹⁵N of the leaves, stems and roots ofElymus athericus decreased from +9‰ to ?1‰. The latter value was close to the °¹⁵N of the N-compounds used in the water solution. Addition of N-compounds in soil culture, however, did not lead to such a decrease of the °¹⁵N ofElymus athericus. The difference in δ¹⁵N between soil nitrogen and the N-compounds added may be too small to be used successfully in ecological studies of nitrogen fluxes in the salt marsh environment.