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' <br /> ' The definition of appropriate h drolo accordin to the 1987 Manual includes two im ortan <br /> Y gY g p t <br /> terms that must be clarified. First, the definition of a growing season is needed. The growing <br /> ' season is defined in the 1987 Manual as: "...the portion of the year when soil temperature <br /> (measured 19.7 inches below the surface) is above biological zero (5° C or 41° �." According to <br /> the 1987 Manual this period of time can be approximated by using the "starting and ending dates <br /> ' for the growing season based on a 28° F air temperature threshold at a frequency of 5 years in <br /> 10." Based on this definition the growing season ranges approximately 160 days to 180 days in <br /> � the Minneapolis/St. Paul metropolitan area (160 in the northern suburbs and greater to the south). <br /> Therefore, the required inundation or saturation to the surface for 5% of the growing season <br /> would be 8 or 9 consecutive days that ground water would need to be at the surface or saturated <br /> ' to the surface. <br /> The second term in the appropriate hydrology definition from the above paragraph to be clarified <br /> is "in most years". This means in 5 of 10 years hydrology must exist within a "jurisdictional <br /> ' wetland" for the 8 or 9 consecutive days of the growing season. This means that one observation <br /> date or even one whole year worth of detailed hydrology data may be deemed insufficient to <br /> ' determine if appropriate hydrology exists at a given location. In the event that precipitation <br /> events accumulate to above or below normal during just prior to a site visit or during a more <br /> intensive hydrology study, the data may be confounded by non-normal circumstances and may <br /> ' be considered outside the bounds of "most years". Ideally, both antecedent soil moisture <br /> conditions and precipitation would be normal during all delineations. However, this is not a <br /> realistic impression of climate. Therefore, primary indicators of hydrology must be reviewed <br /> ' with scrutiny prior to determining if hydrology indeed exists. <br /> Wetland hydrology may be observed as standing water (inundation), or may be observed as <br /> ' freestanding water within a soil pit or auger hole (saturation) usually within the upper 12 inches. <br /> These are considered primary hydrology indicators. Examination of the latter indicator requires <br /> digging a soil pit to a depth of 16 inches and observing the level at which water stands after <br /> ' sufficient time has been allowed for water to drain into the hole. The required time will vary <br /> depending on soil texture. This level represents the depth to the water table; the depth to <br /> saturated soils will always be nearer the surface due to the capillary fringe. According to the <br /> ' Hydrology criteria in the 1987 Delineation Manual, for soil saturation to impact vegetation, it <br /> must occur within a major portion of the root zone, typically within 12 inches of the surface. <br /> Only one primary indicator is necessary to make the determination that wetland hydrology is <br /> ' present. However, since a single observation is not enough evidence, based on the percentage of <br /> the growing season this inundation or saturation is required,•these data are only valid when <br /> reviewed while also considering the abundance of recent precipitation events or the seasonal <br /> ' trend of climate when the site visit was made (this may be done through review of precipitation <br /> records where available). In addition to the primary indicators of wetland hydrology, there are <br /> secondary indicators (e.g. oxidized root channels, water-stained leaves, loc.al soil survey data, <br /> ' FAC-Neutral test), of which two must be present to consider the sample point as having wetland <br /> hydrology. <br /> ' Hydrnphytic Vegetation (Wetland Vegetation) <br /> Wetland vegetation is defined in the 1987 Manual as "The sum total of macrophytic plant life <br /> growing in water or on a substrate that is at least periodically deficient in oxygen as a result of <br /> , excessive water content. When hydrophytic vegetation comprises a community where indicators <br /> Svoboda Ecological Resources 7 2180 Abingdon Way <br /> Project No.2007-056-03 Orono,Minnesota <br /> � <br />