The effect of tidally induced changes in the creekbank water table on pore water chemistry |
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Authors: | Kathleen Agosta |
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Institution: | 1. Marine Science Program, University of South Carolina, Columbia, South Carolina 29208, U.S.A.;2. Belle W. Baruch Institute for Marine Biology and Coastal Research, University of South Carolina, Columbia, South Carolina 29208, U.S.A. |
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Abstract: | Water moved into the creekbank sediments in direct response to the changing levels of the water table caused by the tides. The net water loss of the sediments was 3–30% on each low tide and this loss was confined to within 4 m (horizontal) of the creek. The replacement of this water by incoming tidal water could not supply sufficient nutrients for the growth of creekbank Spartina. However, during ebb tide there was a replacement of water in the creekbanks with nutrient-rich water from the marsh interior as demonstrated by the large changes in pore water chemistry over a tidal cycle. The concentration and the range of a chemical parameter depended upon the stage of the tide, the tidal range, the time of year and (for salinity) the rainfall patterns of the month preceding sampling. Over a single tidal cycle the maximum ranges were: salinity ‰, 26–33; alkalinity, 2·5–13·6 med 1?1, ammonia, 2–400 μm, sulfate, 23·5–29 mmol 1?1. Measurable concentrations of sulfide were only found in a few samples. This high nutrient water can supply nitrogen and probably other nutrients to Spartina. |
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Keywords: | water movement interstitial water water properties salt marshes Spartina South Carolina Coast |
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