My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD04263
CWCB
>
Floodplain Documents
>
Backfile
>
4001-5000
>
FLOOD04263
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:45:45 PM
Creation date
10/5/2006 12:30:12 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Design of Open Channels
Date
10/1/1977
Prepared By
USDA Soil Conservation Service
Floodplain - Doc Type
Educational/Technical/Reference Information
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
256
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).
Show annotations
View images
View plain text
<br />e <br /> <br />e <br /> <br />e <br /> <br />CHAPTER 3. SITE INVESTIGATIONS <br /> <br />Introduction <br /> <br />Methods of investigation and testing of soil conditions along a channel <br />system ate discussed in this chapter. The purposes of these investiga- <br />tions and testing are to evaluate the resistance of the soils in the <br />bed and banks of the channel to erosion forces, to evaluate the sediment <br />transport relationships, to determine slope stability against sloughing <br />and sliding, to estimate earth loads that may act on structural members, <br />and to determine the rate of water movement through the soils. <br /> <br />The procedures include identification, sampling, and testing or evalua- <br />tion of stratigraphic units encountered in the channel system to be <br />modified and an evaluation of the sediment transport characteristics <br />of the system. <br /> <br />Investi~ation Requirements <br /> <br />There are conditions specific to investigations for channel improve- <br />ments that cause them to differ from investigations at other types of <br />construction sites. One usually significant difference is that channels <br />may extend for many miles through a variety of materials. This fact <br />demands that data obtained from anyone test hole must be correlated <br />on as knowledgeable a basis as possible with data obtained at the next <br />test hole, both upstream and downstream. A distinguishing feature of <br />investigations for channel improvements is that almost always they are <br />located in alluvial material. The stability of channels is affected <br />by watershed conditions upstream that control the availability of bed <br />material, and by ground""Water conditions at the site. A similarity <br />with foundation investigations for other structure sites exists in <br />that the in-place characteristics of the soil materials are very <br />important if these characteristics that pertain to erodibility differ <br />from those that exist when the material is disturbed. <br /> <br />The following sequence of work is needed to appropriately recognize the <br />conditions specific to investigations for channel improvements while <br />ensuring that an adequate amount and type of data are obtained. <br /> <br />1. Determine the geomorphology of the deposits in which the channel <br />is to be located to the limit necessary for this purpose. <br /> <br />2. Identify stratigraphic units along the proposed channel route <br />and to a depth of at least three feet below the invert or channel <br />bottom elevation as proposed. A stratigraphic unit is defined in <br />this instance as an identifiable stratum of alluvium or other soil <br />material whose susceptibility to erosion is a reflection of the <br />original materials, mode of accumulation and the changes that have <br />occurred since deposition or soil formation. <br />
The URL can be used to link to this page
Your browser does not support the video tag.