Source Water and Water Quality
Delaware's Source Water and Water Quality domain tests where the water comes from and what is in it before and after treatment. About 90% of Delaware's public supply is groundwater drawn from aquifers such as the Magothy, Cheswold, Frederica, Piney Point, and Aquia; the northern county surface supplies come from the Brandywine, White Clay, and Red Clay. The exam expects you to read a water-quality report, convert units correctly, and recognize which standard applies.
Core rules
- Source water assessments and wellhead protection identify contamination threats and promote local protection.
- Contaminant groups: microbial, inorganic chemicals, organic chemicals, radionuclides, and disinfection byproducts.
- Regulatory terms: MCL is enforceable; MCLG is a non-enforceable health goal; an action level triggers treatment; a treatment technique requires a specified process; an MRDL limits disinfectant residual.
- Nitrate is reported two ways. Nitrate as N has an MCL of 10 mg/L; nitrate as NO3 has an MCL of 45 mg/L. Convert: NO3 = NO3-N × 4.43.
- Hardness is expressed as CaCO3. Multiply calcium mg/L by 2.5 and magnesium mg/L by 4.12, then add.
- Know the meaning of pH, alkalinity, turbidity, conductivity, TDS, temperature, iron, manganese, and arsenic in source and finished water.
- Coastal aquifers face saltwater intrusion; agricultural areas face nitrate; many aquifers carry iron and manganese that cause staining and taste complaints.
Worked example
A well report gives calcium 40 mg/L and magnesium 12 mg/L. Calcium as CaCO3 = 40 × 2.5 = 100 mg/L. Magnesium as CaCO3 = 12 × 4.12 = 49.4 mg/L. Total hardness = 149.4 mg/L as CaCO3, a moderately hard water. If the same report listed nitrate as N at 8 mg/L, nitrate as NO3 would be 8 × 4.43 = 35.4 mg/L, still below the 45 mg/L NO3 MCL.
Traps
Reporting nitrate as N when the limit is written as NO3; treating an MCLG as enforceable; confusing hardness with alkalinity; mixing ppm and mg/L, which are equal in dilute water; ignoring temperature effects on chlorine demand; assuming groundwater is automatically free of microbial risk.