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CONCLUSIONS AND RECOMMENDATIONS <br />F'rom the results of our analysis and investigation,, it is <br />concluded that. <br />le Lady Slipper r <br />_ .r w <br />by siltation accelerated <br />resulting from urbainiz,ati,on, within r, <br />tributary drainage <br />primarily area . <br />2* Lady Sl,ipper Park i,s an <br />wetland <br />containing delailduous scrub shrub vegetation ant <br />a'bout acres depth <br />phosphorus felat 0i <br />301 The annual Phosphorus loading received by Lake Owasso <br />it,hriough, Lady Sliipper Park, is about three to four percent of <br />the total loading the liake _ <br />401 The south bay * _ Wabiasso, <br />maximum f <br />depth fringed , - <br />vegetation +r primarily of cattails. <br />5* About 98 percent of the total, phosphorus loading received by <br />,Liake Wiabasso comes fromi Lake Owasso and passes through _ <br />south bay prior, to reaichin,g the main lake (Barr,, 1991). <br />6* The volume of f illing that has occurred irt the open water <br />area of' the Lady Slipper Park wetland is about 13, 000 cubic <br />yards i <br />701 The f illing that has occiurred, in Lady Slipper Park between <br />,1923 and 1991 represents a 58 percent Volume for +` <br />bay d is, most likely the result of submerged aquatic <br />vegetative growth _ <br />