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� <br /> 1 . . <br /> Discussion <br /> , Type 1/1L <br /> The description provided for Type 1 wetlands and the reference to the absence of wetland <br /> vegetation in basins that are only flooded very temporar�y raises a regvlatory question. One of <br /> ' the criteria for a jurisdictional wetland is the presence of hydrophytic vegetation (1987 Manual <br /> pp 16 - 26). Type 1 wetlands often are found in agricultural fields and often are determined to be <br /> jurisdictional on the basis of an aeria135mm slide review; the quality of the slides is poor under <br /> ' the very best of circumstances. . The determination of regulatory jurisdiction is based on normal <br /> circumstances or as defined by the COE, being agriculturally cropped 51 out of 100 years (i.e. by <br /> inference l�cking sufficiem hydrology for either 5 or 12.5 percent of the growing season). <br /> , The Wetland Conservation Act (WCA) determines noimalcy as agricultural cropping for 6 out of <br /> 10 years (MnRules 8420.0110, Subp 53; 8420.0122 Subp.l, A and B). Typically, notmalcy on <br /> , agricultural lands is detertnined by the review of the aforementioned low quality 35mm aerial <br /> slides and judgments are made as to whether an area is cropped or if the crops are subject to <br /> hydrological stresses. The process is highly subjective and can be biased by excessive <br /> ' precipitation that may occur early in the crop growth cycle. <br /> Field examination of these areas may indicate the presence of smartweed and some of the other <br /> , indicated species in seasonally abnorn�ally wet years whereas in norn�al years, hydrophytic <br /> vegetation is absent. It is highly probable that the proce.ss of detern�unation of Type 1 wetlands as <br /> jurisdictional in many cases is extending beyond the legitnnate definition of Type 1 wetlands and <br /> ' the intent of the 1987 Manua1. <br /> Does a Type 1 basin need to be flooded for 5 percent of the growing season (the lower <br /> 1 definitional bound for jurisdictional hydrology) or 12.5 percent (the upper definitional bound for <br /> jurisdictional hydrology) in order for hydrophytic vegetation to develop? In practice, the St. Paul <br /> District of the Corps of Engineers (COE) (also applied in practice under the Wetland <br /> I Conservation Act) appfies the 5 percent hydrological definition but if that is too short to allow <br /> the development of hydrophytic vegetation under normal conditions than the absence of <br /> hydrophytic vegetation would make those Type 1 wetlaads non jurisdictional. <br /> ' T 1L — bottomland hardwoods — ses an difficult re lato uestion. Tools for the <br /> YPe Po �1�Y 8`� rY 9 <br /> evaluation of hydrology for non-cropped areas are much mare data intensive and are also subject <br /> , to precipitation event variab�ity. Measurement tools for the determination of precipitation <br /> norn�alcy are a combination of evaluating annual precipitation and comparison to a 30-year <br /> rolling average along with extensive near ground surface early season hydrological monitoring. <br /> ' If the water levels are within 12" of the surface for less than 8.5 da.ys in the general latitude of <br /> the Twin Cities (5 percent of the growing season), than the area is not wetland if waxer levels are <br /> ' within 12" of the surface between 5 percent and 12.5 percent of the growing season (21 days in <br /> the general latitude of the Twin Cities) according to the 1987 Manual (Table 5 pg. 36), the area <br /> may be wetland but usually �s not. However, the standard practice of the St. Paul COE �s to <br /> , declare any areas that exceed the 5 percent criteria to be judged jurisdictional wetlands. Areas <br /> with water levels within 12" of the surface in excess of 12.5 percem of the growing season are <br /> wetlands. <br /> , Svoboda Ecolo 'cal Resources 218o Abin on Wa <br /> Si Sd Y <br /> Project No.2007-056-03 Orono,Minnesota <br /> ' <br />