I originally assumed the calmer water in the lagoon would contain fewer particles because the water has the opportunity to settle, and that the wave action at the beach would stir up sediment. In spring 2007, the average amount of sediment in the lagoon was less than half as much as during spring 2006.

This might provide me with a more accurate picture of trends in the data.

A recent Maryland Department of Natural Resources report showed that the volume of bay water with less than 2 mg/l of oxygen went down from 2.01 cubic miles in late July to 1.77 cubic miles in early August.

Last year the SRA’s monitoring ended the first week in November.

I aimed to collect water every three days, although this was not always possible.

Impervious surfaces such as driveways prevent liquids from being absorbed into the ground and generate stronger water flow during rain or similar events. American Museum of Natural History Order Line 0044 (0)1933 664746.

Whether or not I continue this exploration, I am very pleased with the opportunities it has provided me and with the conclusions I have reached.

My hypothesis was that the amount of sediment would increase after rain, but there were few consistent trends.

Between the October 19 and October 25 collections, the number of medium particles rose at the lagoon, while the number of large and fine dropped.

Another confusing find was that the amount of medium sediment often did the opposite from the large and fine particles.

For the samples I had collected with more than 500 ml in the container, I swirled each sample after I removed the top to prevent the sediment from settling.

This issue presents a major problem to the bay's health.The bay has been around for eons, so why is erosion dangerous to the bay's health now?

It was still the third-largest zone for early August in the past 34 years.

During the late winter of 2006 the lagoon was dredged, and as a result the sand shelf I collected from was occasionally underwater.

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