My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
12-12-1987 Planning Packet
Orono
>
Planning Commission
>
1987
>
12-12-1987 Planning Packet
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/4/2024 11:33:42 AM
Creation date
1/4/2024 11:30:41 AM
Metadata
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
183
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
* Soils Information <br />To provide for proper sewage treat <br />ment, the soil treatment system must <br />be located in suitable soil. <br />Presently 31 counties have a detail <br />ed soil survey map. An accelerated soil <br />survey program is underway to com <br />plete detailed soil surveys for the en <br />tire state by 1990. These show the <br />occurrence and distribution of each <br />kind of soil and are a good starting <br />point for the lot owner. The delineated <br />areas on the soils map are called "map <br />ping units" which consist primarily of <br />the soil for which the unit is named and <br />soils with similar characteristics. In ad <br />dition there are areas within the unit <br />consisting of soils that are different. <br />Soil types occupying an acre or more <br />within the mapping unit are indicated <br />by a series of map symbols. The mini <br />mum size of the mapping unit, how <br />ever, depends on the scale of the prim <br />ed map. The smallest mapping unit <br />area designated is about 3 acres. This <br />means that the soils map itself cannot <br />be used to determine the suitability of <br />a specific site. Yet, the soil survey in <br />formation is still useful as background <br />and an indication of potential problems <br />which may be encountered on the lot. <br />The local Soil and Water Conservation <br />District can often provide unpublished <br />soils information if a county lacks a <br />published soil survey. <br />The crests of knolls and hills as well <br />as slightly sloping portions of hills are <br />likely areas for placement of waste <br />treatment systems. Depressions, drain <br />age swales that collect runoff from the <br />surrounding area, and excessively steep <br />slopes (figure 1) should be avoided. <br />Future landscaping plans must be <br />considered to provide access to the site <br />not only during the construction phase <br />but afterward so the septic tank can be <br />pumped periodically. <br />Indicating two or three potential <br />waste treatment sites on the lot pro <br />vides additional flexibility if the pri <br />mary site is unsuitable. Some sanitary <br />ordinances require locating two areas <br />suitable for a waste treatment system <br />on a lot. <br />After this preliminary information <br />has been obtained and evaluated, the <br />site evaluation in the field can begin. <br />Site Evaluation <br />To locate the sewage treatment sys <br />tem properly, soil texture, the presence <br />of soil mottling, direct water table <br />measurement, and land slope should <br />be thoroughly evaluated. The first step <br />in conducting the site evaluation is to <br />make a soil boring at least 3 feet deep <br />er than the bottom of the proposed <br />seepage trenches at the approximate <br />center of the proposed system. <br />The first boring determines the <br />presence of soil mottling or a water <br />table. Soil mottling indicates the pres <br />ence and depth of seasonally occurring <br />water tables during dry periods. Water <br />tables can be measured directly during <br />wet periods by leaving the boring hole <br />open for at least 24 hours. <br />Well-drajned soil is often brown or <br />red, while poorly drained soil is gray. <br />The color difference is due to the peri <br />odic water saturation. Mottled soils <br />consist of spots of gray and brown or <br />gray and red. Where mottled soil oc <br />curs, it is assumed the soil is saturated <br />during wet periods (unless the area has <br />been artificially drained). <br />Depth to soil mottling determines <br />the depth at which soil treatment <br />trenches can be placed, since there <br />needs to be a 3 foot vertical separation <br />between the trench bottom and sea <br />sonal water tables (figure 3). <br />Areas of periodically saturated soils <br />can disrupt operation of the sewage <br />treatment system. When the trenches <br />are installed in a saturated soil zone, <br />effluent entering the system during wet <br />periods cannot m.ove away and will <br />either come to the surface or back up <br />into the house. These saturated zones <br />often are unrelated to the existing re <br />gional water tables or surface waters <br />because zones of unsaturated materials <br />generally separate the two. <br />Land slope should be estimated for <br />the proposed system. Knowledge of <br />the land slope assists in the system's <br />design and in selecting the effluent dis <br />tribution metfiod. Steeply sloping land <br />areas should be avoided to reduce con <br />struction problems. However, some <br />contractors will install trenches along <br />the contour on slopes as great as 30 <br />percent. While such construction is dif <br />ficult and costly, the sewage treatment <br />system will function properly when <br />correctly installed. <br />Soil texture can be used to estimate <br />the percolation rate which is then used <br />to estimate the size of the treatment <br />area which will need to be investigated. <br />Figure 3. Interpretation of soil mottling. <br />WELL DRAINED <br />CAN MEASURE WATER table <br />directly <br />(Soil IS Never <br />Soturoted) <br />(In Boring Hole <br />Left open <br />for 24 Mrs .* <br />ASSUME <br />SATURATION <br />AND <br />PRESENCE OP <br />v;atertaqle <br />tOufinq W.i Peftodi) <br />- Cro» <br />Woter foDle m <br />Soil Becomes <br />Safuroted <br />O <br />Soil Ones <br />os Water raOie <br />IS Lowered <br />Soil Docomes <br />Re-soturoted <br />es se <br />Bnghi Colors <br />Iron finely Dissolved <br />Tnroughour <br />Ihe Profilfe <br />Dull Colors <br />Fine Iron Porficles <br />ore Oissoi**: .1 <br />in the water <br />Alternating ol <br />Oey and Red Colors <br />witri Iron Precipitated <br />Neor Soil Pores <br />.1 <br />3
The URL can be used to link to this page
Your browser does not support the video tag.