puricarexfiles: WATER SOURCES SEASONAL CHARACTERISTICS - Over a longer time period, surface water and groundwater chemistry varies with the seasons.

Surface and Groundwater

Characteristics, pH Control and Alkalinity

Surface Water

The ultimate course of rain or melting snow depends on the nature of the terrain over which it flows.

In areas consisting of hard packed clay, very little water penetrates the ground. In these cases, the water generates "runoff."

The runoff collects in streams and rivers. The rivers empty into bays and estuaries, and the water ultimately returns to the sea, completing one major phase of the hydrologic cycle.

As water runs off along the surface, it stirs up and suspends particles of sand and soil, creating silt in the surface water.

In addition, the streaming action erodes rocky surfaces, producing more sand. As the surface water cascades over rocks, it is aerated.

The combination of oxygen, inorganic nutrients leached from the terrain, and sunlight supports a wide variety of life forms in the water, including algae, fungi, bacteria, small crustaceans, and fish.

Often, river beds are lined with trees, and drainage areas feeding the rivers are forested. Leaves and pine needles constitute a large percentage of the biological content of the water.

After it dissolves in the water, this material becomes a major cause of fouling of ion exchange resin used in water treatment.

The physical and chemical characteristics of surface water contamination vary considerably over time. A sudden storm can cause a dramatic short term change in the composition of a water supply.

Over a longer time period, surface water chemistry varies with the seasons. During periods of high rainfall, high runoff occurs.

This can have a favorable or unfavorable impact on the characteristics of the water, depending on the geochemistry and biology of the terrain.

Surface water chemistry also varies over multi- year or multi-decade cycles of drought and rainfall.

Extended periods of drought severely affect the availability of water for industrial use.

Where rivers discharge into the ocean, the incursion of salt water up the river during periods of drought presents additional problems.

Industrial users must take surface water variability into account when designing water treatment plants and programs.

Groundwater

Water that falls on porous terrains, such as sand or sandy loam, drains or percolates into the ground.

In these cases, the water encounters a wide variety of mineral species arranged in complex layers, or strata. The minerals may include granite, gneiss, basalt, and shale.

In some cases, there may be a layer of very permeable sand beneath impermeable clay.

Water often follows a complex three dimensional path in the ground. The science of groundwater hydrology involves the tracking of these water movements.

Table 1-2. A comparison of surface water and groundwater characteristics.

Characteristic	Surface Water	Ground Water
Turbidity	high	low
Dissolved minerals	low-moderate	high
Biological content	high	low
Temporal variability	very high	low

In contrast to surface supplies, groundwaters are relatively free from suspended contaminants, because they are filtered as they move through the strata. The filtration also removes most of the biological contamination.

Some groundwaters with a high iron content contain sulfate reducing bacteria. These are a source of fouling and corrosion in industrial water systems.

Groundwater chemistry tends to be very stable over time. A groundwater may contain an undesirable level of scale forming solids, but due to its fairly consistent chemistry it may be treated effectively.

Mineral Reactions: As groundwater encounters different minerals, it dissolves them according to their solubility characteristics. In some cases chemical reactions occur, enhancing mineral solubility.

A good example is the reaction of groundwater with limestone. Water percolating from the surface contains atmospheric gases.

One of these gases is carbon dioxide, which forms carbonic acid when dissolved in water.

The decomposition of organic matter beneath the surface is another source of carbon dioxide.

Limestone is a mixture of calcium and magnesium carbonate. The mineral, which is basic, is only slightly soluble in neutral water.

The slightly acidic groundwater reacts with basic limestone in a neutralization reaction that forms a salt and a water of neutralization.

The salt formed by the reaction is a mixture of calcium and magnesium bicarbonate. Both bicarbonates are quite soluble.

This reaction is the source of the most common deposition and corrosion problems faced by industrial users.

The calcium and magnesium (hardness) form scale on heat transfer surfaces if the groundwater is not treated before use in industrial cooling and boiler systems.

In boiler feedwater applications, the thermal breakdown of the bicarbonate in the boiler leads to high levels of carbon dioxide in condensate return systems. This can cause severe system corrosion.

Structurally, limestone is porous. That is, it contains small holes and channels called "interstices."

A large formation of limestone can hold vast quantities of groundwater in its structure.

Limestone formations that contain these large quantities of water are called aquifers, a term derived from Latin roots meaning water bearing.

If a well is drilled into a limestone aquifer, the water can he withdrawn continuously for decades and used for domestic and industrial applications.

Unfortunately, the water is very hard, due to the neutralization/dissolution reactions described above. This necessitates extensive water treatment for most uses.

CHEMICAL REACTIONS

Numerous chemical tests must be conducted to ensure effective control of a water treatment program.

Because of their significance in many systems, three tests, pH, alkalinity, and silica, are discussed here as well.

pH Control

Good pH control is essential for effective control of deposition and corrosion in many water systems. Therefore, it is important to have a good understanding of the meaning of pH and the factors that affect it.

Pure H₂O exists as an equilibrium between the acid species, H⁺ (more correctly expressed as a protonated water molecule, the hydronium ion, H₃0⁺) and the hydroxyl radical, OH^-.

In neutral water the acid concentration equals the hydroxyl concentration and at room temperature they both are present at 10^-7 gram equivalents (or moles) per liter.

The "p" function is used in chemistry to handle very small numbers. It is the negative logarithm of the number being expressed.

Water that has 10^-7 gram equivalents per liter of hydrogen ions is said to have a pH of 7. Thus, a neutral solution exhibits a pH of 7.

The pH meter can be a source of confusion, because the pH scale on the meter is linear, extending from 0 to 14 in even increments.

Because pH is a logarithmic function, a change of I pH unit corresponds to a 10 fold change in acid concentration. A decrease of 2 pH units represents a 100 fold change in acid concentration.

Alkalinity

Alkalinity tests are used to control lime-soda softening processes and boiler blowdown and to predict the potential for calcium scaling in cooling water systems.

For most water systems, it is important to recognize the sources of alkalinity and maintain proper alkalinity control.

Carbon dioxide dissolves in water as a gas. The dissolved carbon dioxide reacts with solvent water molecules and forms carbonic acid according to the following reaction:

CO₂ + H₂O = H₂CO₃

Only a trace amount of carbonic acid is formed, but it is acidic enough to lower pH from the neutral point of 7.

Carbonic acid is a weak acid, so it does not lower pH below 4.3. However, this level is low enough to cause significant corrosion of system metals.

If the initial loading of CO₂ is held constant and the pH is raised, a gradual transformation into the bicarbonate ion HCO₃^- occurs.

The transformation is complete at pH 8.3. Further elevation of the pH forces a second transformation into carbonate, CO₃^2-.

The three species carbonic acid, bicarbonate, and carbonate can be converted from one to another by means of changing the pH of the water.

Variations in pH can be reduced through "buffering" the addition of acid (or caustic).

When acid (or caustic) is added to a water containing carbonate/bicarbonate species, the pH of the system does not change as quickly as it does in pure water.

Much of the added acid (or caustic) is consumed as the carbonate/bicarbonate (or bicarbonate/carbonic acid) ratio is shifted.

Alkalinity is the ability of a natural water to neutralize acid (i.e., to reduce the pH depression expected from a strong acid by the buffering mechanism mentioned above).

Confusion arises in that alkaline pH conditions exist at a pH above 7, whereas alkalinity in a natural water exists at a pH above 4.4.

Alkalinity is measured by a double titration; acid is added to a sample to the Phenolphthalein end point (pH 8.3) and the Methyl Orange end point (pH 4.4).

Titration to the Phenolphthalein end point (the P-alkalinity) measures OH^- and 1/2 CO₃^2-; titration to the Methyl Orange end point (the M-alkalinity) measures OH^-, CO₃^2- and HCO₃ .

Silica

When not properly controlled, silica forms highly insulating, difficult to remove deposits in cooling systems, boilers, and turbines.

An understanding of some of the possible variations in silica testing is valuable.

Most salts, although present as complicated crystalline structures in the solid phase, assume fairly simple ionic forms in solution. Silica exhibits complicated structures even in solution.

Silica exists in a wide range of structures, from a simple silicate to a complicated polymeric material. The polymeric structure can persist when the material is dissolved in surface waters.

The size of the silica polymer can be substantial, ranging up to the colloidal state.

Colloidal silica is rarely present in groundwaters. It is most commonly present in surface waters during periods of high runoff.

The polymeric form of silica does not produce color in the standard molybdate based colorimetric test for silica. This form of silica is termed "nonreactive".

The polymeric form of silica is not thermally stable and when heated in a boiler reverts to the basic silicate monomer, which is reactive with molybdate.

As a result, molybdate testing of a boiler feedwater may reveal little or no silica, while boiler blowdown measurements show a level of silica that is above control limits.

High boiler water silica and low feedwater values are often a first sign that colloidal silica is present in the makeup.

One method of identifying colloidal silica problems is the use of atomic emission or absorption to measure feedwater silica.

This method, unlike the molybdate chemistry, measures total silica irrespective of the degree of polymerization.

https://www.gewater.com/handbook/Introduction/ch_1_sourcesimpurities.jsp

RELATED POSTS: