Monitoring pond water quality to improve shrimp and fish production

The proper management of pond water quality plays a significant role for the success of aquaculture operations.

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Each water quality parameter alone can directly affect the animals´ health. Exposure of shrimp and fish to improper levels of dissolved oxygen, ammonia, nitrite or hydrogen sulfide leads to stress and disease. However, in the complex and dynamic environment of aquaculture ponds, water quality parameters also influence each other. Unbalanced levels of temperature and pH can increase the toxicity of ammonia and hydrogen sulfide. Thus, maintaining balanced levels of water quality parameters is fundamental for both the health and growth of culture organisms. It is recommended to monitor and assess water quality parameters on a routine basis.

In this article the most important water quality parameters such as oxygen, pH, temperature, salinity, turbidity and nitrogen compounds are described with insights on how these parameters influence each other. Table 1 gives an overview of the water quality parameters with their standard values.

Table 1: Water quality parameters and their standard values

Parameter	Standard values
(Dissolved) Oxygen	> 4.0 mg/l
Temperature	Species dependent
pH	7.5 – 8.5
Salinity	Freshwater: <0.5 ppt Brackishwater: 0.5 - 30 ppt Saltwater: 30 - 40 ppt Optimum: 15 -25 ppt
Carbon dioxide (CO2)	< 10 ppm
Ammonia (NH4+/NH4-N)	0 – 0.5 ppm
Nitrite (NO2-)	< 1 ppm
Hardness	40 – 400 ppm
Alkalinity	50 – 300 ppm
H2S	0 ppm
BOD	< 50 mg/l

Dissolved oxygen (DO)

Dissolved oxygen (DO) is one of the most important parameters in aquaculture. Maintaining good levels of DO in the water is essential for successful production since oxygen (O₂) has a direct influence on feed intake, disease resistance and metabolism. A sub-optimal level is very stressful for fish and shrimp. It is therefore important to keep DO at optimum levels of above 4.0 ppm.

The dynamic oxygen cycle of ponds fluctuates throughout the day due to phytoplankton photosynthesis and respiration (Figure 1).

Figure 1: The daily cycle of oxygen in a pond

As shown in Figure 1 maximum DO will occur in the late afternoon due to the buildup of O₂ during the day through photosynthesis. As phytoplankton (microscopic algae) usually consumes the most O₂ and since photosynthesis does not occur during the night, DO levels decline. Critically low DO occurs in ponds specifically when algal blooms crash. The subsequent bacterial decomposition of the dead algae cells demands a lot of oxygen. Managing the equilibrium of photosynthesis and respiration – as well as the algae growth - is an important task in the daily work of a farmer.

The DO concentration in water goes up as temperature goes down, and decreases when salinity increases.

When feeding the fish and shrimp, oxygen demand is higher due to increased energy expenditure (also known as specific dynamic action). To face this higher oxygen demand, several measures can be taken:

Other sources of oxygen than photosynthesis are diffusion or transfer from air to water. Wave action or mechanical aeration is forcing this oxygen diffusion. Paddlewheel aerators accomplish this by breaking water into small droplets and increasing contact of water surface with air. Aspirator aerators compel air into the water through a venture and a propeller. Another reason for aeration is the circulation of aerated water through the pond.

Biochemical oxygen demand (BOD)

Biochemical oxygen demand (BOD) of the pond can affect the oxygen cycle and thus, the oxygen equilibrium. Five-day biochemical oxygen demand (BOD₅) is the amount of DO needed by aerobic biological organisms in the water to break down organic material present at a constant temperature during a 5-day period.

BOD₅ is an important water quality variable that may be required to demonstrate compliance with water quality permits issued by the governments and to achieve farm certification.

The BOD₅ of pond aquaculture effluents usually ranges from 5 to 20 mg/l. The greater the BOD, the more rapidly oxygen is depleted.

Temperature

Temperature is another important water quality parameter. It can affect fish and shrimp metabolism, feeding rates and the degree of ammonia toxicity. Temperature also has a direct impact on biota respiration (O₂ consumption) rates and influences the solubility of O₂ (warmer water holds less O₂ than cooler water).

Temperature cannot obviously be controlled in a pond. Aquatic animals modify their body temperature to the environment and are sensitive to rapid temperature variations. For each species, there is a range of temperature conditions (Table 2). It is therefore important to adapt fish and shrimp progressively when transferring them from tank to pond.

Also, the O₂ cycle and thus, the DO levels can be affected by changes in the environment; a cloudy day will diminish the photosynthetic O₂ input to DO. Correspondingly, uncommonly high temperatures will decrease the solubility of O₂ in water and hence lower DO. When a pond is in “equilibrium” DO will not change drastically.

Every 10 °C increment in temperature doubles the rate of metabolism, chemical reaction and O2 consumption.

Table 2: Temperature (°C) conditions for aquatic species

Species	Lower lethal temperature	Preferred temperature	Upper lethal temperature
Rainbow trout	0	13 - 17	24 - 27
Nile tilapia	8 - 12	31 - 36	42
Tra catfish	9	23 - 27	33
Crucian carp	0	25 - 32	38
Channel catfish	9	22 - 29	37
Cobia	1	21 - 27	33
Tiger prawn	14	25 - 30	36
White shrimp	14	> 20	40

Carbon dioxide (CO₂)

Carbon dioxide (CO₂) in ponds is primarily produced through respiration by fish/shrimp and the microscopic plants and animals that constitute the pond biota.

Carbon dioxide levels (and toxicity) are highest when DO levels are lowest (Figure 2). Thus, dawn is a critical time for monitoring DO and CO₂. High CO₂ concentrations inhibit the ability of fish and shrimp to extract O₂ from the water, reducing the tolerance to low O₂ conditions and inducing stress comparable to suffocation.

Figure 2: The daily cycle of oxygen and carbon dioxide in a pond

An increase in CO₂ may also decrease the pH, which can lead to toxicity of nitrite. If plants in the water absorb too much CO₂ for photosynthesis during the day, the pH will increase, and the fish and shrimp are subjected to higher un-ionized toxic ammonia (NH₃) concentrations.

Carbon dioxide concentrations above 60 ppm may be lethal. In an emergency, CO₂ can be removed by adding liming agents such as quicklime, hydrated lime or sodium carbonate to the pond water.

At higher temperatures, fish and shrimp are even more susceptible to pH variations.

pH

pH is a measure of acidity (hydrogen ions) or alkalinity of the water. It is important to maintain a stable pH at a safe range because it affects the metabolism and other physiological processes of culture organisms. It can create stress, enhance the susceptibility to disease, lower the production levels and cause poor growth and even death. Signs of sub-optimal pH are besides others increased mucus on the gill surfaces of fish, unusual swimming behavior, fin fray, harm to the eye lens as well as poor phytoplankton and zooplankton growth. Optimal pH levels in the pond should be in the range of 7.5 – 8.5.

The CO₂ concentration in the water also influences the pH, e. g. an increase in CO₂ decreases the pH, as already mentioned above (Diagram 1). As phytoplankton in the water utilizes CO₂ for photosynthesis, the pH will vary naturally throughout daylight hours. pH is generally lowest at sunrise (due to respiration and release of CO₂ during the night) and highest in the afternoon when algae utilization of CO₂ is at its greatest. Waters of moderate alkalinity are more buffered and there is a lesser degree of pH variation.

Diagram 1: CO₂ and pH correlation, influencing the toxicity of NH₃

Ammonia

Ammonia is a very important parameter for good fish and shrimp production. Under particular conditions, ammonia can easily rise (through accumulation of overfeeding, protein rich, excess feed wastes and excreted ammonia) to dangerously high levels.

The higher water temperature and pH, the greater the concentration of the toxic ammonia form (NH3)

Ammonia in water exists in two forms, as ammonium ions (NH₄⁺), which are nontoxic, and as the un-ionized toxic ammonia (NH₃). The relative proportion of the one or the other depends on water temperature and pH. If the phytoplankton absorbs too much CO₂ during the day, and therefore increase the pH to a value above 8.5, the fish and shrimp are subjected, depending on the total ammonia nitrogen concentration, to high ammonia concentrations (NH₃). As little as 0.6 ppm (mg/l) free ammonia (NH₃) can be toxic to many kinds of fish and shrimp, causing gill irritation and respiratory problems.

Nitrite (NO₂^-)

Nitrite (NO₂^-) is another form of nitrogenous compound that results from feeding and can be toxic to shrimp and fish. Nitrite is an intermediate product of the transformation of ammonia into nitrate by bacterial activity. The absorbed nitrites from the gut bind to hemoglobin and reduce its ability to carry oxygen.

An increase in CO₂ may decrease the pH to a value below 6.5, which can lead to toxicity of nitrite through the formation of nitrous acid (HNO₂). At 2 ppm (mg/l) and above, nitrites are toxic (injurious or lethal) to many fish and shrimp.

Hydrogen sulfide (H₂S)

Hydrogen sulfide (H₂S), a colorless, toxic gas, is a by-product of the deterioration of organic matter, usually under anaerobic conditions. Anaerobic soils with moderate to high organic concentrations can be a significant source of H₂S, which is toxic to shrimp and fish even at low concentrations since it hinders their respiration. If the bottom soil becomes black and a rotten egg odor is recognized when sediment is disturbed, it indicates anaerobic conditions and the presence of H₂S. Hydrogen sulfide is highly toxic in the unionized form (comparable to ammonia). However, the unionized form is predominant at low pH (< 8) and high temperature. At pH 7.5 approximately 14 % of the sulfide is in the toxic H₂S form and at pH 6.5 about 61 %. Therefore, sulfide concentrations should be below 0.002 ppm.

Many marine species live in close proximity to sediments that often contain H₂S. Some even live in them. From the data in Table 3 it is clear, that the range of susceptibility to H₂S poisoning is huge.

Table 3: Toxicity of H₂S to various aquatic organisms

Common name	Species name	LC50 (ppb)
Channel catfish	Ictalurus punctatus	846.7
Indian prawn	Penaeus indicus	179.3
Oriental river shrimp	Macrobrachium nipponense	51.0
Crab	Portunus trituberculatus	31.5
Black tiger shrimp	Penaeus monodon	62.6
Pacific white shrimp	Litopenaeus vannamei	60.2

Drying and tilling pond bottoms, in addition to maintaining thorough aeration of ponds and frequent water exchange, are effective means in diminishing hydrogen sulfide.

Alkalinity

Alkalinity is the buffering capacitiy of water and represents its amount of carbonates and bicarbonates. Alkalinity can affect the potential for primary productivity and also the water pH. In case the water pH fluctuates greatly during the day, lime can be used to increase alkalinity in the water to stabilize the water pH. Values of 50 – 100 mg/l are considered moderate and are recommended. Total alkalinity has been traditionally expressed as milligrams per liter (ppm) of equivalent calcium carbonate (CaCO₃). Generally, alkalinity varies from site to site. In the seawater, alkalinity is normally higher than 100 ppm but in freshwater areas, alkalinity is often low, particularly during the rainy season. Low alkalinity in freshwater or in low salinity areas will affect the survival rate and molting of shrimp.

Hardness refers to the concentration of calcium and magnesium in water.

Waters can be classified by the degrees of hardness
0 - 75 mg/l	soft
75 - 150 mg/l	moderately hard
150 - 300 mg/l	hard
Over 300 mg/l	very hard

Hard waters have the ability to buffer the effects of heavy metals such as zinc or copper which are toxic for fish and shrimp. Thus, hardness is a crucial parameter in maintaining good pond “balance”.

Salinity

Salinity represents the total concentration of dissolved inorganic ions, or salts, in water. It plays a significant role for the growth of culture organisms through osmoregulation of body minerals from that of the surrounding water. For better survival and growth an optimum range of salinity should be maintained in the pond water. If salinity is too high, fish and shrimp will start to lose water to the environment. Younger shrimp appear to tolerate a wider fluctuation of salinity than the adults. Drastic changes of salinity may also alter the phytoplankton fauna and their population densities and lead to instability of the ecosystem. Lowering the salinity by more than 5 ppt, at each time of water exchange, is not recommended.

Conclusion

Careful monitoring of water quality parameters is important to understand the interactions between parameters and effects on shrimp and fish feeding, their growth and health. Each water parameter alone may not tell much, but several parameters together can reveal dynamic processes taking place in the pond. Water quality records will allow farmers to note changes and make decisions fast so that corrective actions can be taken quickly.

References

upon request