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C153445 Feasibility Study
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C153445 Feasibility Study
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Last modified
11/19/2009 11:29:57 AM
Creation date
10/5/2006 11:35:14 PM
Metadata
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Template:
Loan Projects
Contract/PO #
C153445
Contractor Name
Summit Reservoir and Irrigation Company
Contract Type
Loan
Water District
32
County
Montezuma
Bill Number
HB 84-1128
Loan Projects - Doc Type
Feasibility Study
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<br />4. Install filter drain and berm on the middle section of <br />the south dike. <br /> <br />Geologic Investigations <br /> <br />The general geology of the area consists of Dakota sandstone. <br />Hard to friable feldspar, quartz, .and sandstone occu~ in the north <br />abutment. The formation dips f~om 0 - 400 south-southeast. Grey <br />marly limestone (Mancos shale). lies flat to 70 dip southward as <br />seen at the spillway. The Mancos shale, which is about 700 feet <br />thick, overlies Dakota sandstone (about 200 f feet thick) dipping <br />southward at about 120 i feet per m~le. <br /> <br />.The geo.logic investigations conducted to support this study <br />were minimal. Soil samples and in-place densities were taken at <br />one location on the west dike and one on the south dike. Sieve <br />analysis were performed on the samples to determine a gradation <br />curve. The soils at the sample sites are classified as clay. <br /> <br />The sample site on the west dike was just south of the <br />horseshoe bend on a sectio~ of the embankment about 25 feet high <br />(see Drawing V-B). Two soil samples were taken, one from the <br />embankment and one from the foundation. . <br /> <br />The sample site for the south dike was about the middle of <br />the middle section, over one of the seepage locations (see Drawing <br />V-B). Again samples were taken from the foundation and the <br />embankment. <br /> <br />Results from the tests are described on Table V-A. <br /> <br />Designs and Structures <br /> <br />1. Grourid Recontouring - when Summit Reservoir was enlarged <br />in 1938, material was borrowed from just below the toe of the <br />embankment. These areas were never recontoured so water that <br />seeps through the embankment collects in the borrow areas. The <br />water that collects in the borrow areas form marshes, ponds, and <br />promote vegetative growth that seriously inhibits inspection of <br />the embankment. Also the collected water, if on the toe of the <br />dike, may saturate the embankment sufficiently to cause slumping. <br />About 2100 feet of the west dike and 1400 feet of the south dike <br />needs to be recontoured. (See Drawing V-C for locations). . <br /> <br />Recontouring the west dike generally involves reshaping the <br />ground to its natural gradient which slopes away from the dike. <br />Cuts would be made during the recontouring with excess material <br />placed away from wat~r drainage paths. <br /> <br />One area, about two thirds of the way south on the west dike <br />will be a little more difficult because the ground is fairly flat. <br />This section appears to have quite a lot of seepage. The ground <br />will be recontoured to collect water at one surface drain which <br />will include a measuring flume. Use of the measuring flume will <br />-21- <br />
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