Shrimp and fish pond soils: processes and management
Introduction
Properties of the pond bottom soil (sediments) and processes occurring at the bottom soil and in the soil–water interface are very important regarding the well being and growth of fish or shrimp in ponds. Nutrients and organic residues tend to accumulate at the bottom and are, thus, to some extent, removed from the water phase. However, an excessive accumulation beyond what could be defined as the carrying capacity of the sediments may result in the deterioration of the pond system, as specified later. Such development seems to be of special importance for shrimp culture, since shrimps live in the soil–water transition zone. Reactions and fluxes within and across the water–soil interface are very significant in natural aquatic systems and even more in intensive aquaculture systems. Organic matter settles and accumulates on the pond bottom in extensive, semi-intensive and intensive ponds. Anaerobic conditions develop in the sediments of intensively stocked and fed shrimp ponds, the process being more pronounced with the increase in pond intensification. The development of anaerobic conditions constrains production and is a barrier to further intensification.
Three terms describing pond bottom soils are used here and in the technical literature. The term “sediments” is used in the limnological and oceanographic literature pertaining to the fact that bottom of lakes and oceans are made mostly of materials sedimenting from the water during long periods of time. Ponds are constructed in native soils, having bottom soils. Later, both the sedimentation of plankton and feed residues as well as the scouring of loosely consolidated soil and deposition of fine particles on the bottom, leads to a change in the properties of the bottom soil. Often, one finds in the stagnant or deeper parts of the pond an accumulation of very soft loose material, relatively rich in organic matter that is often called sludge. Sediments accumulating in lined ponds, having high organic matter concentrations would also be defined as sludge. There is a continuum from bottom soil, through sediment to sludge. In this work, the terms bottom soil and sediment will describe the bottom of the pond, while the term sludge will be used specifically to the soft, fluidized, organic-rich residue.
This manuscript is a literature review of the physical, biological and chemical processes occurring at the pond bottom that influence aquaculture production, giving special attention to shrimp culture including supporting data obtained in fish ponds. In addition, potential technologies to mitigate problems occurring at the soil–water interface in ponds are discussed.
Section snippets
Accumulation of nutrients and organic matter in pond soils
Cultured aquatic animals accumulate between 5% and 40% of nutrients in the feed (carbon, nitrogen, phosphorus). A summary of nutrient accumulation by fish and shrimp is given in Table 1.
The average nutrient retention by fish and shrimp, calculated from published data listed, is 13% for carbon, 29% for nitrogen and 16% for phosphorus (Table 1). The low carbon recovery is probably due to the fact that a large fraction of carbon in the feed is lost by respiration.
Accumulations of carbon, nitrogen
Microbial activity in pond bottom soils
Sediments are enriched with nutrients and organic matter by sedimentation of organic materials to the pond bottom. The concentrations of nutrients (including organic carbon compounds) in the pond bottom soil are typically several orders of magnitude higher than those found in the water (Table 3). The amounts of nutrients in a 1-cm layer of the pond bottom are normally about 10 or more times higher than the equivalent amounts in a 1-m deep water column. The bottom becomes a favorable site for
Sediment oxygen demand in shrimp ponds
Dissolved oxygen concentration is one of the critical factors affecting processes and conditions at the sediment–water interface. Sediment oxygen demand (SOD) is an indicator of the intensity of the mineralization process and benthic community metabolism. A compilation of SOD data for shrimp and fish ponds is given in Table 4.
SOD is commonly determined by different methods: sediment cores, in situ tubes, benthic chamber, whole pond budget calculations and calculations based upon oxygen profiles
Redox reactions in the pond bottom soil
When oxygen is depleted, other terminal electron acceptors can be used to mediate the decomposition of organic matter. Many anaerobic processes taking place in the pond bottom lead to the production of reduced and potentially toxic compounds. Anaerobic conditions may affect aquaculture production both due to the unfavorable conditions at the pond bottom, or affect it through the diffusion of the reduced compounds from the sediment upward to the water column.
The sequence of redox reactions as
Effects of accumulated sediment on shrimp production
Pond bottom conditions are more critical for shrimp than for other aquaculture species because shrimp spend most of their time on the bottom, burrow into the soil and ingest pond-bottom soil Boyd, 1989, Chien, 1989. The distribution of penaeid shrimp in the natural environment can be influenced by sediment characteristics Williams, 1958, Hughes, 1968, Rulifson, 1981, Somers, 1987. Penaeid shrimp commonly burrow into the substrate to hide from predators Fuss and Ogren, 1966, Boddeke, 1983.
Management of shrimp pond bottom soil
Theory, laboratory experiments and field data indicate that the conditions in the pond bottom are very important to the success of aquaculture production systems. This is especially true for semi-intensive to super intensive shrimp production systems. Control of pond bottom reactions is possible through the use of several means.
An important principle is to Minimize coverage of the pond bottom by sludge. The effect of reduced sediments on pond productivity is lowered if the area covered by
Conclusions
The natural carrying capacity of pond bottom seems to be a limiting factor toward further intensification of aquaculture systems. This point was clearly demonstrated in fish culture and seems to be true for shrimp pond intensification. Moreover, there is evidence that the deterioration of the pond bottom, the increase in the amount of waste accumulation and the development of anaerobic conditions hinder shrimp utilization of feed, retard growth, possibly create stress and lead to the increase
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2023, AquacultureCitation Excerpt :However, options for aquaculture regions have not been studied yet, even though the trend toward org-C accumulation is expected to continue due to expanding aquaculture activities. For instance, aquaculture ponds worldwide cover an area of 1.11 × 108 ha and accumulate an annual estimated 200 tons ha‐1 org-C (an equivalent 7.5–10 cm layer of wet newly deposited material) (Avnimelech and Ritvo, 2003; Boyd et al., 2010). Therefore, it is relevant to explore the distribution of org-C and its impacts on sediment P release in the aquaculture ponds.