THE RELATIONSHIP BETWEEN RIVER FLOW AND MICROCYSTIS AERUGINOSA BLOOMS IN THE NEUSE RIVER, NORTH CAROLINA

Robert R. Christian, Wade L. Bryant, Donald W. Stanley

NCSU Libraries Repository (North Carolina State University Libraries) · 1986 · 35 citations · 1 references

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Abstract

Extensi ve bl ooms o f bl ue-green a1 gae domi nated by M i crocysti s aeruginosa have occurred during some, b u t n o t a l l , recent summers along the Neuse Ri ver, North Carol i na.Nutrients are present in excess of a1 gal needs year-round in the Neuse, b u t blooms seem to develop only d u r i n g those summers with periods of sustained low flow.W e postulated t h a t t h i s 1 inkage between bloom formation and river flow results from faster growth and 1 onger residence time of a1 gae i n the river a t 1 ow f l ows.To eval uate t h i s hypothesis, we devel oped a mathematical simul ation model f o r predicting t h e concentrations of a1 gae in the 1 ower Neuse under various f 1 ow conditions, taking i n t o account the e f f e c t s t h a t f l ow has on r i ver vel oci t y (and hence time-of-travel ) and other variables affecting a1 gal growth such as l i g h t intensity and water depth.Information on the timeo f -t r a v e l of water and a l g a e within the r i v e r came from a s e r i e s of dye tracer studies.In the laboratory we evaluated the regulation of growth of M. aeruginosa by l i g h t and temperature.-Model predictions were in good agreement with observations of bloom occurrence or non-occurrence from 1979 t o 1985.For the months from May through September we evaluated the maximum flow rates, as gaged a t Kinston, N.C., t h a t would a1 low f o r bloom formation.The r e s u l t s were t h a t the combination of water temperature and daylength in July was most conducive t o bloom occurrence, while May and September were the 1 east conducive.Our results may be useful in the management of: (1) low flow augmentation a t the Fa1 1 s Reservoir, ( 2 ) n u t r i e n t 1 oading reduction, and ( 3 ) water use within the Neuse River basin as we1 1 as interbasin transfers invol v i n g the Neuse.

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