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A water molecule has three atoms: 2 hydrogen (H) atoms and 1 oxygen (O) atom. Thats why water is sometimes referred to as H2O. A single drop of water contains billions of water molecules.
The recommended SMCL for TDS is 500 mg/L (with an upper limit of 1,000 mg/L), and for EC, it is 900 S/cm (with an upper limit of 1,600 S/cm). EC and TDS also have short-term SMCL that are generally allowed only under rare circumstances at 2,200 S/cm and 1,500 mg/L, respectively.
Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, permafrost (frozen soil), immobile water in very low permeability bedrock, and deep geothermal or oil formation water.
How deep is my well? Go to the well records search and find the Well Construction Report for your well. The report will indicate the drillhole depth and the casing depth.
Naturally occurring contaminants are present in the rocks and sediments. As groundwater flows through sediments, metals such as iron and manganese are dissolved and may later be found in high concentrations in the water.

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The eight parameters are Dissolved Oxygen (DO), Electrical Conductivity (EC), Total Dissolved Solids (TDS), salinity, pH, turbidity, Total Suspended Solids (TSS), chloride and other parameter is depth to groundwater level.
Some substances found naturally in rocks or soils, such as iron, manganese, arsenic, chlorides, fluo- rides, sulfates, or radionuclides, can become dis- solved in ground water. Other naturally occurring substances, such as decaying organic matter, can move in ground water as particles.
Ground water may contain dissolved minerals and gases that give it the tangy taste enjoyed by many people. Without these minerals and gases, the water would taste flat. The most common dissolved mineral substances are sodium, calcium, magnesium, potassium, chloride, bicarbonate, and sulfate.

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