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_PERMIT FILE - M1997053 (36)
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_PERMIT FILE - M1997053 (36)
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Entry Properties
Last modified
2/26/2024 1:09:03 PM
Creation date
11/20/2007 6:02:08 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1997053
IBM Index Class Name
Permit File
Section_Exhibit Name
EXHIBIT I SOILS INFORMATION
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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I <br /> U.S. DEPARTMENT OF AGRICULTURE PAGE 3 OF 3 <br /> RURAL RESOURCES CONSERVATION SERVICE 01/28/97 <br /> tWATER FEATURES <br /> note -- WATER FEATURES--Continued <br /> Information on the extent of flooding based on soil data is less specific than that provided by detailed engineering <br /> Igh <br /> veys that delineate flood-prone areas at specific flood frequency levels. <br /> Hi water table (seasonal) is the highest level of a saturated zone in the soil in most years. The depth to a <br /> sonaL high water table applies to undrained soils. The estimates are based mainly on the evidence of a saturated <br /> e, namely grayish colors or mottles in the soil. Indicated in this report are the depth to the seasonal high <br /> er table; the kind of water table, that is, "Apparent", "Artesian", or "Perched"; and the months of the year that <br /> the water table commonly is high. A water table that is seasonally high for less than 1 month is not indicated in <br /> s report. <br /> An "Apparent" water table is a thick zone of free water in the soil. It is indicated by the level at which water <br /> Inds in an uncased borehole after adequate time is allowed for adjustment in the surrounding soil. <br /> n "Artesian" water table exists under a hydrostatic beneath an impermeable layer. When the impermeable layer has been <br /> penetrated by a cased borehole, the water rises. The final level of the water in the cased borehole is characterized as <br /> Iartesian water table. <br /> A "Perched" water table is water standing above an unsaturated zone. In places an upper, or "Perched", water <br /> le is separated from a lower one by a dry zone. Only saturated zones within a depth of about 6 feet are <br /> icated. <br /> P ding is standing water in a closed depression. The water is removed only by deep percolation, transpiration, <br /> 1poration, or a combination of these processes. <br /> This report gives the depth and duration of pending and the time of year when ponding is most likely. Depth, duration, <br /> Iprobable dates of occurrence are estimated. <br /> Depth is expressed as the depth of ponded water in feet above the soil surface. Duration is expressed as "Very <br /> ef" if less than 2 days, "Brief" if 2 to 7 days, "Long" if 7 to 30 days, and "Very long" if more than 30 days. The <br /> ormation is based on the relation of each soil on the Landscape to historic pending and on Local information about <br /> the extent and levels of ponding. <br /> t <br /> 1 <br />
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