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Wells and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE [email protected]
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Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE [email protected]

May 09, 2018

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Page 1: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Wells and Septic Systems in Karst Topography

Barry Glotfelty, Chief

Onsite Systems Division, MDE

[email protected]

Page 2: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Significant Properties of Limestone Derived Soils

• High clay content.

• Strong structure.

• Potential for high shrink – swell in lower profile.

• Vulnerable to soil treatment zone bypass.

Page 3: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us
Page 4: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Outbreaks in Ground Water Systems

Page 5: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Outbreaks in Ground Water Systems

The largest documented ground water outbreak occurred in Georgetown, Texas in 1980 (Hejkal et al., 1982). About 7900 people became ill. Both Coxsackievirus and Hepatitis A virus were found in the raw well water and the outbreak was the result of source water contamination. The contamination source was never identified but the site is within an area of karst (solution-enhanced) limestone with cavernous zones which allows contamination to travel long distances in short periods with relatively little natural attenuation.

Outbreaks in Ground Water Systems

»In Racine, Missouri, 46 cases of hepatitis A were identified in 1992 at a non-community water supply in a karstlimestone setting. A nearby septic system was identified as the contaminant source.

Page 6: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Outbreaks in Ground Water Systems

• In Lancaster County, Pennsylvania, 49 cases of hepatitis A occurred in 1980 as the result of septic tank contamination of a well in a karst limestone area. An outbreak resulting in 1200 cases of shigellosis occurred in 1974 (Wiessman, 1976) as the result of septic tank contamination of source water in a likely karst area in Florida.

Outbreaks in Ground Water Systems

• Craun (1984) reports a total of five outbreaks associated with untreated groundwater in karst or fractured rock areas for the years 1971-1979, including outbreaks in Missouri and Arkansas.

• http://www.epa.gov/safewater/standard/phs.html

Page 7: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Development of a Rapid, Sensitive, and Quantitative Method to Detect Infective Hepatitis A Virus in Water

( 2000-2001) Principal Investigators:

Marylynn V.Yates, Wilfred Chen, UC Riverside

Executive Summary: Microorganisms are responsible for more than 90% of the reported waterborne disease outbreaks in the United States; enteric viruses, such as hepatitis A virus, are

identified as causing almost 10% of these. However, in 50% of the outbreaks, no causative agent is identified due to limitations in our ability to isolate and detect viruses in water samples. Historically, consumption of contaminated ground water has been the source of one-half of the reported outbreaks; in recent years, that fraction has risen to more than two-thirds. The most frequently reported source of contamination in these outbreaks is domestic sewage

from septic tanks, leaking sewer lines, cesspools, etc.

Source: US EPA website

Vicki Poole holds a glass of water on Tuesday afternoon that she got out of a home faucet. The Poole family lives on Glade Road near Walkersville.

Photo by Sam Yu for the Frederick News Post

Page 8: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us
Page 9: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us
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Page 11: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us
Page 12: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us
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Water for Maryland’s Future:What We Must Do Today

Final Report of the Advisory Committee on theManagement and Protection of theState’s Water Resources

M. Gordon WolmanChairman

VOLUME 1: FINAL REPORTJuly 1, 2008

Page 27: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Wolman Report RecommendationsF. State and local governments should discourage the use ofindividual wells in areas at high risk for well contamination.

Of particular concern are wells that are installed in limestone aquifers. As water flows through these aquifers, it can dissolve the limestone, leaving large cracks and fissures, and even producing sinkholes.

These pathways allow surface water to travel so rapidly to the aquifer that the water is not filtered through soil, and microbiological organisms can survive.

Various types of fecal bacteria, viruses, and oocysts of Cryptosporidium and Giardia can be found in the water obtained from wells in this vulnerablesetting.

Groundwater in these areas is considered to be under the direct influence of surface water.

Wolman Report Recommendations

Laws, regulations, policies and procedures are in place to ensure that publicwater systems using ground water under the direct influence of surface wateremploy appropriate treatment to address the potential health threats, butthese requirements do not apply to individual wells.

It is unlikely an individual homeowner could manage this problem: typical homeowners do not have the technical expertise or financial capability to maintain and operate such treatment systems, which are extremely complex and difficult to manage and maintain.

Page 28: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

Wolman Report Recommendations

The Committee recommends the following:

1. MDE should strengthen current regulations for issuing waterappropriation permits to require comprehensive water quality testingfor new subdivisions.

2. Maryland's laws and regulations should be modified as necessary torequire construction of public drinking water systems instead ofindividual wells for new developments where ground water testing orthe presence of specific geologic conditions indicate serious threats towater quality. These systems should be transferred upon completionto a responsible entity, such as a local government utility or theMaryland Environmental Service.

Wolman Report Recommendations

Public water offers greater protection, but the Committee recognizes that a better policy may be to direct development dependent on ground water away from theseareas entirely.

Page 29: Wells and Septic Systems in Karst Topography and Septic Systems in Karst Topography Barry Glotfelty, Chief Onsite Systems Division, MDE bglotfelty@mde.state.md.us

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