My WebLink
|
Help
|
About
|
Sign Out
Home
2019.02.04 CC Packet
Hugo
>
City Council
>
City Council Agenda/Packets
>
2019 CC Packets
>
2019.02.04 CC Packet
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/25/2020 2:34:15 PM
Creation date
2/4/2019 6:30:16 PM
Metadata
Fields
Template:
City Council
Document Type
Agenda/Packets
Meeting Date
2/4/2019
Meeting Type
Regular
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.
/
609
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
Effective April 28, 2015 Chapter Four Subsurface Sewage Treatment System Regulations <br />ii. Organic soil textures or mineral soil textures with an organic modifier; <br />iii. Dominance of hydrophytic vegetation; <br />iv. The soil treatment area at or near the elevation of the ordinary high water level of a <br />surface water or in a concave hill slope position; <br />V. Redoximorphic accumulations or depletions; or <br />vi. The soil expressing indicators of seasonal saturation as determined in Field Indicators <br />of Hydric Soils in the United States: A Guide for Identifying and Delineating Hydric <br />Soils, USDA Natural Resource Conservation Service (2006 and subsequently <br />amended). This field book is incorporated by reference, is available through the <br />Minitex interlibrary loan system, and subject to frequent change. <br />(6) Depth to periodically saturated soil for all existing systems, determined by redoximorphic features <br />in item (5), except subitems (B), unit (i), and (C), units (i), (iii), and (iv), as measured outside the <br />area of the system influence in an area of similar soil. <br />(7) Depth of standing water in the soil observation excavation, measured from the soil surface, if <br />observed. <br />(8) Any other soil characteristics that needs to be described to design a system, such as hardpans or <br />restrictive layers. These other characteristics must be classified according to the Field Book for <br />Describing and Sampling Soils, which is incorporated by reference under Section 2.2 (46). <br />9.7 Determination of loading rate and absorption area size. <br />The effluent loading and absorption area size must be determined by either item (1) or (2). <br />(1) The loading rate based on an examination of soil texture, undisturbed soil structure, and soil <br />consistence at the depth of either the proposed absorption area or the most restrictive layer within <br />three feet of the proposed soil absorption area using the United States Department of Agriculture <br />(USDA) soil classification system as specified in the Field Book for Describing and Sampling <br />Soils, which is incorporated by reference under Section 2.2 (46); or <br />(2) The loading rate based on the percolation procedure described in subitems (A) to (H). <br />(A) Each test hole must be six to eight inches in diameter, and have vertical sides. For mounds <br />and at -grade systems, the bottom of each test hole must be in the upper 12 inches of the <br />original soil. For trenches and seepage beds, the bottom of each test hole must be at the <br />depth of either the proposed absorption area or the most restrictive layer within three feet of <br />the proposed soil absorption area; <br />(B) Soil texture descriptions for percolation test holes must note the depths from the ground <br />surface where texture changes occur; <br />(C) The bottom and sides of the hole must be carefully scratched to remove any smearing and to <br />provide a natural soil surface into which water penetrates. The scarification must not result <br />in the hole having a diameter of greater than eight inches; <br />(D) All loose material must be removed from the bottom of the test hole and two inches of one- <br />fourth to three -fourths inch gravel or clean sand must be added to protect the bottom from <br />scouring; <br />(E) The hole must be carefully filled with clear water to a minimum depth of 12 inches from the <br />bottom of the test hole and maintained for no less than four hours for saturation to occur. <br />The soil must then be allowed to swell for at least 16, but no more than 30, hours. In sandy <br />soils, the saturation and swelling procedure is not required and the test is allowed to proceed <br />if the initial filling of the hole with 12 inches of water seeps away in less than ten minutes; <br />(F) In sandy soils, water depth must be adjusted to eight inches over the soil at the bottom of the <br />test hole. From a fixed reference point, the drop in water level must be measured in inches to <br />the nearest 1/16 inch at approximately ten-minute intervals. A measurement is also allowed <br />to be made by determining the time it takes for the water level to drop one inch from an <br />eight inch reference point. If eight inches of water seeps away in less than ten minutes, a <br />shorter interval between measurements must be used, but water depth must not exceed eight <br />inches. The test must continue until three consecutive percolation rate measurements do not <br />36 Washington County Development Code <br />
The URL can be used to link to this page
Your browser does not support the video tag.