In a coastal salt marsh ecosystem, the water cycle and nitrogen cycle interact closely. During a spring tide, seawater floods the marsh, depositing dissolved inorganic nitrogen (mainly
NO3− and
NH4+) at a concentration of
0.8mg L−1. The total volume of seawater flooding the marsh is
5000m3. The marsh plants, primarily Spartina alterniflora, take up this nitrogen for growth. After the tide recedes, evaporation and plant transpiration remove water from the marsh soil.