Lake County Transportation Network

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Recommended publications
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  • American Shad Habitat Plan Update
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  • Directions to Florida Lake Ramps
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  • Physiochemtcal Effects of the Wekiva River On
    Phvsiocheniical Ejjee(,l,; oftlu: Wekiva River on the SI. Johns River. Central Florida Keellings I Physiochemtcal Effects ofthe Wekiva River on the St. Johns River, Central Florida David Keellings University (~/'Cent}4(JI Florida Introduction th The St. Johns River is a 6 order river which flows north from I its headwaters in Indian River County a distance of 310 miles to its outlet with the Atlantic Ocean in Duval County. It is a slow moving meandering river which widens into several lakes throughout its flow and has an average elevation change of less than 1 inch per mile. The St. Johns River is considered to be a blackwater river (Clewell, 1991). Blackwater rivers are characterized by tea-colored water caused by high concentrations of Dissolved Organic Matter (Meyer, 1990). The Wekiva River is a calcareous river fed by Wekiwa Spring and Rock Spring. It joins the St. Johns River as a single channel where the boundaries of Seminole, Lake, and Volusia Counties meet (Figure I). The surrounding river bank is forested with wetland species including cypress (TlLYOuiuJ11 sp.) and red maple (Ace}' I'lfhI'1IJ11) transitioning to upland oak communities through cabbage palm tSabul palmetto). This confluence of water provides an opportunity to observe the effect on water chemistry when a spring fed river joins a blackwa­ ter river. Physiochemical properties of water were measured at eight stations. Six of these stations were located in the St. Johns River up­ stream from its confluence with the Wekiva River. One station was placed in the Wekiva River upstream from its confluence with the St.
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  • F L O R I D a Atlantic Ocean
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