Septic Drain Field Remediation

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    Septic Drain Field

    RemediationSoils 401 Section 001Joseph P. Smith

    3/29/2013

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    Introduction

    Septic systems are commonly used as a sewage holding and treatment option when city

    wastewater treatment plants are not available. Septic systems consist of three major parts: a

    toilet, a septic tank, and a drainage field. The septic tank is designed as a box with one inlet and

    one outlet. The box is sized to be long enough to allow the large particles to settle and form

    sludge by the time they reach the end of the box. These solids are digested by bacteria through

    anaerobic (no air) or aerobic (with air) digestion. A layer of scummy film will form and float on

    top of the fluids in the tank. The outlet is designed so that only water will be discharged from

    the tank. The outlet is built above

    the sludge and a baffle wall is added

    to prevent the scum from escaping.

    The outlet water is released through a

    drainage field for a natural treatment.

    I will focus my project on how to

    amend a failing drainage field in a

    septic system.

    A proper drainage field is designed for percolation in soil before the effluent reaches the

    bedrock and water table. Soil acts as a filter for the septic water, removing the surplus of organic

    material that sewage is composed of. The soil functions to remove biochemical oxygen demand

    (BOD), phosphorous, and salts. When a soils hydraulic capacity is very low (i.e. clay), the

    water will not percolate through the soil quickly enough and the drainage field will not be

    Image 1: soil absorption and purification layersabove the water table (Septic Systems andTheirMaintenance).

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    effective. Moreover, the water in the septic system will back up. To create an effective drainage

    field, the soil surrounding the drainage field will have to be altered. Conversely, having soil that

    is too coarse and porous will not effectively treat sewage because the water will pass through the

    soil too quickly. When this happens, organics do not have time to attach to soil. Drain fields can

    fail for numerous other reasons including soil compaction from vehicles driving over the drain

    field, system overload from increased use in a short period of time, and root systems clogging or

    disrupting the system (Owens and Rutledge, n.d.). It is my goal to create a soil remediation plan

    at a site with a failing septic system. Keep in mind that septic system installation and

    remediation costs money. For the duration of the report, it will be assumed that the builder is

    willing to spend money for a quality and long lasting product.

    Site and Soil Description

    Merigold, Bolivar County, Mississippi

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    Image 1: Site (Google Maps)

    Soils at site

    o Brittain silt loam, nearly level phase (forestdale)o Dowling clay (sharkey)o Forestdale silty clay loam, nearly level phase

    The problem at the site occurs in all three soil types because they all have very low hydraulic

    conductivities (Rycroft and Amer, 1995). This is problematic because with low conductivity,

    water cannot drain from the septic tank and the potential for a sewage backup arises. Sewage

    water will pond on top of the drain field, causing damage to the land above it. The location is in

    Bolivar County, MS, just outside of the town of Merigold. To get to the site, drive north from

    Merigold on Park Street. The site is on the left of the road (west). The site is on farmland and a

    small stream runs through the site. There are roads within 500 feet of the soil site boundary. As

    the site is for a septic tank, there are homes in proximity of the site. I am going to take a

    hypothetical look at a builder buying a plot of land and building a house on the site. For this

    project, the landowner wants to include a septic system in the field. As the depth of soil

    increases, the soil characteristics vary slightly. With an increase in depth, the pH increases,

    cation-exchange capacity decreases, hydraulic conductivity slightly increases, water content

    decreases, and percent clay does not follow any set pattern. The soils clay contents are all very

    high which causes low hydraulic conductivity in the soils. In a septic system, septic water is

    released through a drainage field to trickle through the soil. This removes the high organic

    content from the water before it enters the bedrock and water table. In the case of soils with a

    low hydraulic conductivity (i.e. clay), septic water cannot pass through the soil to reach the water

    table (Owens and Rutledge, n.d.). This causes backups in the septic system and leads to septic

    failure. See the appendix section for site soil characteristics.

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    Literature Review

    Jones and Taylor focused on laboratory research to determine changes in soil hydraulic

    conductivity with respect to time after effluent application. Clogged pores were thought to lead

    to reduced hydraulic conductivity and consequent septic system failure. The experimental results

    show that clogging in septic system sands happens based on the cumulative effluent load. There

    were found to be three phases of clogging. The rate of clogging in the initial phase is seen by

    reduction of hydraulic conductivity that is directly proportional to the volume of effluent

    percolated. This occurs because of organic solids deposited at the sand and gravel interface.

    Clogging rates are significantly slower in the second phase. In the second phase, organic

    material deposited is nearly equal to organic materials leaving the system so essentially no

    clogging occurs. The third stage sees a high rate of clogging and a rapid decrease in K. It is

    concluded that an absorption system should function without clogging for a long time if the

    second phase of clogging could be extended for a longer period of time. Soil clogging occurs 3-

    10 times faster under anaerobic conditions because air converts some deposited organic material.

    Sands with high initial K clog slower than sands with relatively low initial K value (Jones and

    Taylor, 1964).

    Clogging Stage % of initial hydraulic

    conductivity after completion ofstage

    Phase Rate

    Initial 100 -

    Phase I 25 Moderate-Rapid

    Phase II 10 SlowPhase III 1 Very Rapid

    Table 1: Three phases on drain field soil clogging (Jones and Taylor, 1964).

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    Jones and Taylor showed that hydraulic conductivity experiences an enormous decrease

    from its initial value. The data is important because we want to idealize conditions that lead to

    maximized phase II duration. The important thing to take away from this chart is that once phase

    II is complete, phase III occurs at a very rapid rate. Phase III clogging leads to a very low

    hydraulic conductivity (for example, 0.3 in/h compared to initial of 30 in/h) and possible system

    failure.

    From your home, sewage goes to a

    septic tank before the effluent water

    containing high amounts of organics and

    salts is filtered through the drain field. In a

    drain field, effluent goes to a trench where is it

    distributed to a layer of gravel that sits above soil. It has been found that effluent is well treated

    at the soil/gravel interface (Gill et al, 2007) which causes a great deal of organic build up at the

    interface (Jones and Taylor, 1964). This buildup reduced permeability and can lead to system

    failure. To deal with this buildup, every year or so, effluent should be sent to a second drain

    field so that the first drain field can be rejuvenated (McKinley and Siegrist, 2010). The

    rejuvenation takes place when naturally occurring microbes digest the built up organic material

    in the soil and at the soil/gravel interface. If this isnt done, septic drain fields will not last as

    long as their potential life span.

    At the site in Merigold, MS, the clay soil is not good for septic system installation. As

    previously discussed, clay soil does not have a high enough hydraulic conductivity to keep

    effluent under the soil surface. This will lead to water damaged lawns and system backups.

    Image 2: Typical septic system (Owens andRutledge, n.d.)

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    Sewage can back up as far as the inside of your house, creating serious health hazards (Lindbo,

    et al, n.d.).

    Soils that are too wet will have gray spots. These soils should be avoided because wet

    soils will not allow effluent to drain well. Additionally, wet soils do not treat effluent as well as

    dry soils because wet soils lack oxygen. Oxygen treats effluent by removing pathogens and

    other contaminants that can get into drinking water when soil is too wet (Lee and Jones, n.d.).

    There are a number of soil characteristics to look for when designing a septic drain field.

    First, the soils should not be too clayey or too sandy. Soil with too much clay will not drain well

    and soil with too much sand will drain too fast so that effluent does not have proper exposure

    time to be treated. The soil should be gently sloping so that is does not reach the water table too

    fast to treat effluent. It should be permeable enough to allow effluent transport. Areas with

    rocks near the surface should be avoided because rocks block effluent transport. Areas with

    vegetation should be avoided as large root systems will interfere with the drain fields ability to

    function ("Septic Systems and Their Maintenance").

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    Source Fact

    "Drainfield Rehabilitation."Pipeline Winter 2005: 1-

    7. wvu.edu. Web. 28 Mar. 2013.

    Soil fracturing can be used to open soil

    for better hydraulic conductivity andpermeability.

    Gill, L.W., OSulleabhain, C., Misstear, B.D.R., and

    Johnston, P.J. 2007. The Treatment Performance ofDifferent Subsoils in Ireland Receiving On-Site

    Wastewater Effluent. Journal of EnvironmentalQuality 36:1834-1855.

    Most septic tank effluent treatment takes

    place in the distribution gravel and thefirst 300 mm of subsoil.

    Jones, J.H., and Taylor, G.S. 1964. Septic Tankeffluent through sands under laboratory conditions.

    Soil Science Vo. 90, No. 5:301-309.

    Under aerobic conditions, soil cloggingby deposited organics occurs in three

    phases. The first and third phases show

    rapid declines in hydraulic conductivity.However, the second stage shows low tono decline in hydraulic conductivity. If

    the second phase of clogging can beextended, the performance of soil

    absorption septic systems can bedramatically improved.

    McKinley, J.W., and Siegrist, R.L. 2010.Accumulation of Organic Matter Components in Soil

    under Conditions Imposed by Wastewater Infiltration.Soil Sci. Soc. Am. J. 74:1690-1700.

    Effluent should be redirected to a seconddrain field to give the first drain field

    time to recover. Naturally occurringmicrobes digest built up organic matter at

    the soil/gravel interface.

    Lee, Brad, and Jones, Don. "Septic Systems in

    Flooded and Wet Soil Conditions."Home &Environment. Purdue Extension, n.d. Web. 29 Mar.

    2013..

    Wet soils do no treat effluent because

    there is no oxygen present to removepathogens and other contaminants.

    Lindbo, David, Rashash, Diana and Michael Hoover.

    "Soil Facts."North Carolina State University. NorthCarolina Cooperative Extension, Web. 28 Mar. 2013.

    .

    Backups can reach the inside of your

    house, creating serious health hazards.

    Owens, Phillip, and Rutledge, Moye. "Septic DrainField Design and Maintenance."Phosphorous Best

    Management Practices. USDA, n.d. Web. 28 Mar.2013.

    .

    Clay soils will not allow wastewater toinfiltrate fast enough to remain below the

    soil surface.

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    Ransom, M. D., W. W. Phillips, and E. M. Rutledge.

    1981. Suitability for septic tank filter fields andtaxonomic composition of three soil mapping units in

    Arkansas. Soil Sci. Soc. Am. J. 45:357-361.

    For septic drain fields, soils with a slope

    greater than 15% are rated severe by theSoil Conservation Service.

    Radcliffe, D.E., West, L.T., and Singer, J. 2005.

    Gravel Effect on Wastewater Infiltration from SepticSystem Trenches. Soil Sci. Soc. Am. J. 69:1217-

    1244.

    With a greater difference in gravel to

    biomat hydraulic conductivity, gravelmasking increases and effluent flow

    slows.

    Rycroft, David, and Mohamed Amer. "Prospects forthe Drainage of clay soils."FAO Irrigation and

    Drainage PaperRome (1995): 19-22. Print.

    Soils with low hydraulic conductivity(clay), will drain more slowly than soils

    with high conductivity.

    "Septic Systems and Their Maintenance."

    Department of Soil Science at NC State University,

    Main Page. N.p., n.d. Web. 28 Mar. 2013..

    Gently sloping, thick, permeable soils are

    best for drain fields. Soil should not have

    gray spots as these indicate that it isexcessively wet. It should not be toosandy or clayey.

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    Solutions

    The proposed problem is to fix a failing septic system. In the situation at hand, a

    prospective builder wants to install a septic system in a low permeability clay soil. It is

    important to note that septic systems can fail for many reasons other than low permeability clay

    soil. This section will look at solutions for installing a septic system in clay soil as well as fixing

    a failed system after installation.

    To create an effective septic drain field, the clay soil will have to be addressed. One way

    to do this is to fracture the soil (Drainfield Rehabilitation), a process similar to hydraulic

    fracturing in shale formations to extract natural gas. In this process, a pneumatic hammer

    punctures the soil and creates many small holes. Air is pumped into the holes to crack the soil.

    Polystyrene pellets, used to prop the fractures open, are injected into the soils. This process

    creates a higher permeability in the clay soil.

    Another way to install a septic drain field in clay soil is to do a complete overhaul and

    excavate the clay. The area would be backfilled with a soil that is better suited for drainage and

    effluent filtration. If the soil is too wet, perimeter drainage systems will have to be installed to

    ensure a dry drain field.

    Once the drain field has been installed, failures can arise from floods, increased water

    usage over a short period of time, organic buildups in soil or at the gravel/soil boundary, and

    vegetation root systems clogging the drain field. To fix the problem, soil fracturing and a

    complete system rebuild are options. Another option to fix the problem of organic buildup is

    blasting high pressured water through the system to break up chunks of organics. Vacuums are

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    used to gather the excess material pumped through the system. Installing a second drain field is

    another way to fix the problem of organic buildup (McKinley and Siegrist, 2010).

    Discussion

    When installing anything, septic system included, it is a good idea to start things the right

    way. Soil fracturing is a plausible short term fix for compaction, but it does not give a drain field

    the proper starting point. The use of soil fracturing has been met with varied results and it is

    only legal in certain states (Drainfield Rehabilitation). This is evidence enough that soil

    fracturing should not be used at installation to create a drain field. While expensive, the decision

    to excavate the clay soil and replace it with a more suitable soil will be the best long term option

    at installation. It is beneficial to initially install two drain fields to avoid organic buildup over

    years of use.

    The options for system failures that occur in the later stages of a septic systems life vary.

    It is important to diagnose the cause of system failure. If the system fails due to organic buildup,

    reinstalling soil for the drain field is not necessary and is very expensive. Assuming the builder

    did not initially install two drain fields, a second drain field should be built so microbes can

    digest organic buildup while the opposite drain field is used. If the builder had installed two

    drain fields initially, the problem would be unlikely to occur.

    If the failure occurs from overuse, it is a good idea to conserve water for a while to let

    ponded effluent infiltrate the soil. Other measures should not be necessary in this case. If root

    systems interfere with the drain field, it is a good idea to remove them. Again, other measures

    should not be necessary in this case.

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    Conclusion

    To install an effective septic system in clay soil, a complete overhaul must be done. The

    clay soil should be excavated and replaced with a gently sloping soil that does not contain too

    much clay or too much sand. The soil at the site has high water content, so perimeter drains

    should be installed around the drain field to keep the soil dry. To reduce future organic buildup,

    the builder should install two drain fields that can be used at different times (one in use while the

    other rejuvenates).

    Once installation has been completed, the easiest fix for many problems is prevention.

    The owner should avoid system overload by conserving water. To do this, the owner should

    avoid doing multiple loads of laundry, dished, etc. in the same day. The owner should avoid

    driving on the land above the drain field to avoid soil compaction. The owner should not plant

    trees or shrubs near the drain field to avoid root systems clogging or disturbing drainage.

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    Literature Cited

    "Drainfield Rehabilitation."Pipeline Winter 2005: 1-7. wvu.edu. Web. 28 Mar. 2013.

    Gill, L.W., OSulleabhain, C., Misstear, B.D.R., and Johnston, P.J. 2007. The Treatment

    Performance of Different Subsoils in Ireland Receiving On-Site Wastewater Effluent. Journal of

    Environmental Quality 36:1834-1855.

    Jones, J.H., and Taylor, G.S. 1964. Septic Tank effluent through sands under laboratory

    conditions. Soil Science Vo. 90, No. 5:301-309.

    McKinley, J.W., and Siegrist, R.L. 2010. Accumulation of Organic Matter Components in Soil

    under Conditions Imposed by Wastewater Infiltration. Soil Sci. Soc. Am. J. 74:1690-1700.

    Lee, Brad, and Don Jones. "Septic Systems in Flooded and Wet Soil Conditions."Home &Environment. Purdue Extension, n.d. Web. 29 Mar. 2013.

    .

    Lindbo, David, Diana Rashash, and Michael Hoover. "Soil Facts."North Carolina StateUniversity. North Carolina Cooperative Extension, Web. 28 Mar. 2013.

    .

    Owens, Phillip, and Moye Rutledge. "Septic Drain Field Design and Maintenance."Phosphorous

    Best Management Practices. USDA, n.d. Web. 28 Mar. 2013..

    Ransom, M. D., W. W. Phillips, and E. M. Rutledge. 1981. Suitability for septic tank filter fields

    and taxonomic composition of three soil mapping units in Arkansas. Soil Sci. Soc. Am. J.45:357-361.

    Radcliffe, D.E., West, L.T., and Singer, J. 2005. Gravel Effect on Wastewater Infiltration fromSeptic System Trenches. Soil Sci. Soc. Am. J. 69:1217-1244.

    Rycroft, David, and Mohamed Amer. "Prospects for the Drainage of clay soils."FAO Irrigation

    and Drainage PaperRome (1995): 19-22. Print.

    "Septic Systems and Their Maintenance."Department of Soil Science at NC State University,Main Page. N.p., n.d. Web. 28 Mar. 2013. .

    "Web Soil Survey." USDA Natural Resources Conservation Service. N.p., 22 Feb. 2013. Web.22 Feb. 2013. .

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    Appendix

    Location: Bolivar County, MS

    AOI 47.1 acres

    Soil Acres in AIO

    Bd 1.Brittain silt loam, nearly

    level phase (forestdale)16.9

    Dc 2. Dowling clay (sharkey) 25.3

    Fe 3.

    Forestdale si lty clay

    loam, nearly level

    phase

    4.9

    0-25 cm 25-50 cm 50-100 cm 100-150 cm 150-200 cm

    Bd 5.3 5.3 5.9 6.2 6.2

    Dc 6.8 6.8 6.8 7.4 7.5

    Fe 5.3 5.3 5.9 6.2 6.2

    0-25 cm 25-50 cm 50-100 cm 100-150 cm 150-200 cm

    Bd - - 10.5 10.5 10.5Dc 39.6 27.9 27.9 23 22.2

    Fe - - 9.2 9.2 9.2

    Soil pH

    Chemical Properties

    Cation-Exchange Capacity, milliequivalens per 100 grams)

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    0-25 cm 25-50 cm 50-100 cm 100-150 cm 150-200 cm

    Bd 1.7 0.21 1.9 2.7 2.7

    Dc 0.2 0.21 0.21 0.89 1

    Fe 1.7 0.21 1.9 2.7 2.7

    0-25 cm 25-50 cm 50-100 cm 100-150 cm 150-200 cm

    Bd 32.2 33.3 30.4 29 29

    Dc 40.3 44 44 40.2 39.6

    Fe 33.2 33.3 30.3 28.9 28.9

    0-25 cm 25-50 cm 50-100 cm 100-150 cm 150-200 cm

    Bd 34.6 47.5 30.5 22.5 22.5Dc 61.2 75 75 60 57.5

    Fe 37.9 47.5 30.5 22.5 22.5

    Saturated Hydraulic Conductivity, mm/s

    Water Content, One-Third Bar (%)

    % Clay

    Physical Properties