My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2006-01-09_REVISION - M2001088
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M2001088
>
2006-01-09_REVISION - M2001088
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/15/2021 6:08:03 PM
Creation date
11/21/2007 5:41:42 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2001088
IBM Index Class Name
Revision
Doc Date
1/9/2006
Doc Name
Application
From
Gary Rinderle Construction Inc.
To
DMG
Type & Sequence
CN1
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
86
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
oaiaioo <br />MATER MANAGEMENT <br />Endnote -- MATER MANAGEMENT <br />This report gives information on the soil properties and site features that affect water management. The degree and kind <br />of soil Limitations are given for pond reservoir areas; embankments, dikes and levees; and aquifer-fed excavated <br />ponds. The Limitations ere considered "Slight" if soil properties and site features are generally favorable for the <br />indicated use and limitations are minor and are easily overcome; "Moderate" if soil properties or site features ere <br />not favorable for the indicated use and special planning, design, or maintenance is needed to overcome or minimize the <br />Limitations; end "Severe" of soil properties or site features are so unfavorable or so difficult to overcome that <br />special design, significant increases in construction costs, and possibly increased maintenance are required. <br />This report also gives far each soil the restrictive features that affect drainage, irrigation, terraces and diversions, <br />and grassed waterways <br />POND RESERVOIR AREAS hold water behind a dam or embankment. Soils best suited to this use have low seepage potential in <br />the upper 60 inches. The seepage potential is determined by the permeability of the soil and the depth to fractured <br />bedrock or other permeable materiel. Excessive slope can affect the storage capacity of the reservoir area. <br />EMBANKMENTS, DIKES, AND LEVEES are raised structures of soil materiel, generally less than 20 feet high, constructed to <br />impound water or to protect land against overf tow. In this report, the soils are rated as a source of material for <br />embankment fill. The ratings apply to the soil material below the surface layer to a depth of about 5 feet. It is <br />assumed that soil layers will be uniformly mixed and compacted during construction. The ratings do not indicate the <br />ability of the natural soil to support an embankment. Soil properties to a depth even greater than the height of the <br />em' '~ment can affect performance and safety of the embankment. Generally, deeper onsite investigation is needed to <br />del _. ,nine these properties. Soil material in embankments must be resistant to seepage, piping, end erosion end have <br />favorable compaction characteristics. Unfavorable features include less than 5 feet of suitable material and a high <br />content of stones or boulders, organic matter, or salts or sodium. A high water table affects the amount of usable <br />material. It also affects trafficability. <br />ADUIfER-FED excavated ponds are pits or dugouts that extend to a ground-water aquifer or to a depth below a permanent <br />wafer fable. Excluded are ponds that are fed only by surface runoff and embankment ponds that impound water 3 feet <br />or more above the original surface. Excavated ponds are affected by depth to a permanent water table, <br />permeability of the aquifer, and quality of the water as inferred from the salinity of the soil. Depth to bedrock <br />and the content of large stones affect the ease of excavation. <br />DRAINAGE is the removal of excess surface and subsurface water from the sot L. How easily and effectively the soil is <br />drained depends on the depth to bedrock, to a cemented pan, or to other layers that affect the rate of eater movement; <br />permeability; depth to a high water table or depth of standing water if the soil is subject to ponding; slope; <br />susceptibility to flooding; subsidence of organic layers; and potential frost action. Excavating and grading and the <br />stability of ditchbanks are affected by depth to bedrock or to a cemented pan, large stones, slope, and the hazard of <br />cutbanks caving. The productivity of the soil after drainage is adversely effected by extreme acidity or by <br />toxic substances in the root zone, such as salts, sodium , or sulfur. Availability of drainage outlets is not considered <br />in the ratings. <br />
The URL can be used to link to this page
Your browser does not support the video tag.