Knowl. Manag. Aquat. Ecosyst.
Number 420, 2019
Topical Issue on Fish Ecology
Article Number 49
Number of page(s) 12
Published online 21 November 2019

© M. Rutegwa et al., Published by EDP Sciences 2019

Licence Creative CommonsThis is an Open Access article distributed under the terms of the Creative Commons Attribution License CC-BY-ND (, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. If you remix, transform, or build upon the material, you may not distribute the modified material.

1 Introduction

Fish production in semi-intensive aquaculture depends, in addition to the natural productivity of ponds, on manuring and supplementary feeding (Broyer and Curtet, 2012; Wezel et al., 2013). Manure is added in fishponds in order to increase fish yields by supporting primary production and feed is added to sustain high density of fish stock that can no longer rely on the food produced naturally in the fishpond (Adámek, 2014; Knud-Hansen et al., 1991). The efficiency of using inputs in semi-intensive fishpond management depends on the flow of energy in the food chain towards fish, either through the grazing or the detritus food chains (Pokorný et al., 2005). The availability of abundant zooplankton and macroinvertebrates throughout the growing season plays a key role in maintaining this efficiency in carp ponds. However, the intensification of fish production, together with inputs of nutrients and organic residues from wastewater and agricultural areas, has often resulted in fishpond eutrophication (Nhan et al., 2006; Pokorný and Hauser, 2002). In summer months, hypereutrophic water bodies (Vollenweider and Kerekes, 1982) are characterised by a primary producer community dominated by planktonic cyanobacteria and a low biomass of zooplankton (Pálffy et al., 2013; Scheffer et al., 2001; Sommer et al., 2012). Increased turbidity and availability of nutrients favour the growth of cyanobacteria while fish grazing pressure and lack of edible phytoplankton limit the growth of zooplankton. Fish in hypereutrophic ponds and lakes are threatened by phytoplankton die off followed by drops in dissolved oxygen levels that can even reach lethal values for fish (Jeppesen et al., 1990; Schindler et al., 2008). Such states indicate that the planktonic primary production of the pond exceeds the capacity of the food chain to exploit the produced phytoplankton biomass (Pechar, 2000; Potužák et al., 2007). In addition, the hypereutrophic condition of water bodies is a sign that the system receives nutrients in excess, especially phosphorus, which is considered a limiting factor for the primary production in freshwater ecosystems (Reynolds and Davies, 2001; Schindler et al., 2008).

Improvement of pond water quality and pond effluent is crucial to achieve an ecological sustainable aquaculture (Alongi et al., 2009). A balance between the amount of supplemented nutrients and organic matter added and that used to produce fish biomass is required to avoid excessive fishpond eutrophication (Bosma and Verdegem, 2011). Prior to taking actions to try to improve the water quality in fishponds, it is important to understand the sources, sinks and transformation of nutrients and organic matter in fishponds. The magnitude of total primary production and respiratory processes in the aquatic ecosystem and the use of nutrients can be determined by measuring diurnal changes in dissolved oxygen (DO) concentrations and nutrient balance (Adhikari et al., 2012; Staehr et al., 2010). Using these methods, it is also possible to show how effective the fertilization and application of fish feed is for the growth and the production of fish in ponds.

The aim of this study was to assess the effective utilisation of organic carbon (OC) and nutrient inputs for the production of fish in the Dehtář pond, a typical representative of semi-intensive, hypereutrophic fishponds in the Czech Republic (Pechar, 2000). Specific objectives were to determine ecosystem metabolic rates, carbon and nutrient balance and to compare the inputs to the amount of nutrients that were really needed to attain the produced fish biomass. In addition, phosphorus regeneration in the fishpond and the amount of phosphorus needed to counterbalance its limitation in the system were also measured. We hypothesise that the inefficient use of nutrients, mainly P, its overdosing and then its re-cycling within the aquatic ecosystem lead to hypereutrophic conditions observed in semi-intensive fishponds.

2 Methodology

2.1 Study area

The Dehtář pond (49.0083N, 14.3058E; 406.4 m above sea level) is situated in the upper Vltava River basin and is the last and lowest water body in the system of fishponds in the upper basin of the Dehtářský stream (Fig. 1). It ranks among the ten largest Czech fishponds, having a surface area of 2.28 km2, maximum and mean depths of 5.5 and 2.2 m, respectively, and a catchment area of 91.4 km2 (Potužák et al., 2016). It is used as a polyculture semi-intensive fishpond. Manure and supplementary feed, mainly wheat, rye or barley grains, are added to increase fish production over natural productivity, which is between ca 100 and 200 kg ha−1 yr−1 in this region (Kestemont, 1995; Pechar, 2000). Common carp (Cyprinus carpio L.) usually represents 95% of stocked fish biomass and the remaining 5% are composed of grass carp (Ctenopharyngodon idella Valenciennes 1844), bighead carp (Hypophthalmichthys nobilis Richardson 1845), pike-perch (Sander lucioperca L.), and northern pike (Esox lucius L.). It is one of the fishponds called main ponds as it is stocked with two-year-old carp that are harvested at the end of a two-year growing cycle. Ponds in which younger fish are kept are known as nursery ponds (Pokorný and Pechar, 2000). This study was carried out during the first year of the fish production cycle.

thumbnail Fig. 1

Location of the Dehtář pond. The crosses indicate the metabolism measurements and water sampling sites. The isobaths in the Dehtář and Posměch ponds show the depths in meters at the water level at maximum filling.

2.2 Sampling and data used

Three platforms equipped with high frequency stations for recording water temperature (Tw ) and dissolved oxygen (DO) (M4016, Fiedler AMS) were installed in the Dehtář pond at three sites (Fig. 1), i.e. at the dam (D), Dehtářský bay (DB), and Babický bay (BB). Tw and DO were recorded in 10 minute intervals at 0.3-m and 1.5-m depths at the dam (site D) and at 0.3-m depth at sites DB and BB. Site D was also equipped with a meteorological station (M4016-A-G3, Fiedler AMS) to record air temperature, wind speed at 2-m height, and shortwave incident radiation at the same intervals as above. The stations were operated from April to November 2015. Maintenance, checking and re-calibration of the stations were performed at weekly or two-week intervals based on algal growth on the sensors.

For the evaluation of water quality and nutrient balance, water samples were taken from the pond, its tributaries, and the outflow. On days of the maintenance of stations, integrated water samples were taken from the top 2-m layer at all three sites and grab samples from the 3-m depth and 0.5 m above the bottom at site D using a Friedinger sampler. All five tributaries (i.e., sites No. 2454, 2456, 2457, 2458, 2459; Fig. 1) and the outflow (No. 2451; Fig. 1) were sampled and their flow was measured once a month from December 2014 to March 2015, and every two weeks from April to November 2015. The samples were analysed for concentrations of nutrients, namely total carbon (TC), total organic carbon (TOC), dissolved organic carbon (DOC), particulate organic carbon (POC), total nitrogen (TN), nitrate nitrogen (N-NO3 ), ammonium nitrogen (N-NH4 +), total phosphorus (TP), dissolved phosphorus (DP), soluble reactive phosphorus (SRP), and chlorophyll a (Chla). The analyses are specified in Supplementary Material, Table S1. The flow was measured using a hydrometric probe (FlowTracker, Sontek, USA). In the pond at sites D, DB and BB, water transparency was measured with a Secchi disc and a multiparametric probe (YSI 6600 V2-4) was used to record vertical profiles of Tw and DO at 0.5 m depth intervals. Water level in the pond was read out at a gauge fixed at the dam structure weekly or more frequently from January to December 2015.

The hydrological characteristics of the Dehtář pond, namely its inflows, outflows, volume of stored water and water level changes, were reconstructed in a daily time step. First, the two-weekly measured data in the inflows were completed by the hydrological analogy from the recorded daily flow data in a nearby stream (the Zlatý potok) and information on the timing of filling up and/or emptying of the ponds situated upstream in the catchment. Then the water balance of the Dehtář pond was calculated as the difference between water inputs (the reconstructed daily inflows plus daily precipitation on the pond surface) and losses of water (evaporation, outflow and seepage). The loss of water by seepage was calculated by subtracting the inputs from the other losses and was positively correlated with the level of pond filling. The precipitation data originated from the climatic station of the Czech Hydrometeorological Institute at České Budějovice (48.9518N, 14.4698E; distance from the Dehtář pond ca 13 km). Daily evaporation from the pond was calculated using the Penman-Montheith formula based on daily average temperature, air humidity, radiation and wind speed data (Wetzel, 2001). The theoretical water residence time was calculated by dividing the average water volume of the Dehtář pond by the average inflow (George and Hurley, 2003).

2.3 Metabolism measurements, phosphorus regeneration and phosphorus demand

Ecosystem metabolic rates in the pond were calculated using a model developed for lakes (Hanson et al., 2003; Staehr et al., 2010) expressed in the equation: ΔO2t =GPP−ER−F−A. In this formula, ΔO2t is the change in dissolved oxygen over time, GPP the gross primary production, ER the total ecosystem respiration, F the oxygen exchange with the atmosphere, and A includes other processes affecting the concentration of dissolved oxygen such as inflow, outflow, leakage or photochemical decomposition of humic substances. ΔO2t was determined from measured dissolved oxygen concentrations that were area and volume weighted at each of the three sites. The F values were modelled as a function of the concentration gradient between the actual and saturation values of dissolved oxygen concentration at a given temperature and the coefficient of wind and temperature dependent reaction according to Staehr et al. (2010). The values of A were neglected as insignificant for the conditions present at the Dehtář pond (Coloso et al., 2011; Staehr et al., 2010). Since the primary production is zero at night, the ecosystem respiration was calculated from the decrease of dissolved oxygen in the pond during the night and from exchange with the atmosphere (Lauster et al., 2006; Sadro et al., 2011). Furthermore, assuming that ecosystem respiration is the same during the day and night, the hourly average respiration was multiplied by 24 hours to obtain total daily ecosystem respiration (ER). Daily net ecosystem production (NEP) was obtained by summing the change in oxygen concentration from all time steps from dawn to dawn. Gross primary production (GPP) was obtained by summing daily NEP and daily ER.

Regeneration and demand of orthophosphate phosphorus by the planktonic community were calculated from the monthly metabolic rates (Kamarainen et al., 2009; Knoll et al., 2016). First, the values of the GPP, ER and NEP were converted from oxygen units (mg m−2 d−1 O2) to carbon units (mg m−2 d−1C) multiplying them by 0.33 (i.e., mass ratio of O2 and C assuming a photosynthetic quotient of 1.15 (Knoll et al., 2016). Then, the net planktonic production (NPP) was calculated as the difference between GPP and autotrophic respiration (Rauto), where Rauto was assumed to be 70% of ER according to previous studies in eutrophic lakes (Biddanda et al., 2001; del Giorgio and Peters, 1993; Staehr et al., 2010). Heterotrophic respiration (Rhetero) was assumed to be 30% of ER according to the same studies. Phosphorus regeneration was then obtained by dividing Rhetero by seston C/P ratio and phosphorus demand was obtained by dividing the NPP by seston C/P ratio (Kamarainen et al., 2009; Knoll et al., 2016).

2.4 Balance of organic carbon and nutrients

The balance of organic carbon, nitrogen and phosphorus in the Dehtář pond was calculated from May to October 2015 using the equation: ΔMt = GPP + IN + AD + FF + M − ER − OUT − FISH − RET. In this equation, ΔMt is the change in the quantity of organic carbon or nutrients in the pond water between the beginning and the end of the balance period, GPP is the gross primary production (applicable for organic carbon only), IN, AD, FF, and M are the inputs from inflows, atmospheric deposition, fish feed, and manure, respectively, ER is the loss of organic carbon by ecosystem respiration, OUT and FISH are the outputs from the system by outflow plus seepage and by the uptake into the produced fish biomass, respectively, and RET is the calculated residual of the balance and represents retention in the sediment and/or loss to the atmosphere. The inputs by the inflows and atmospheric deposition and the outputs by the outflow and seepage were calculated for each month as the product of the monthly averaged measured concentrations and the corresponding monthly volumes of water entering or leaving the pond. Afterwards the monthly values were summed over the study period. The concentrations in the atmospheric deposition used were from the measurements of bulk precipitation at the Slapy reservoir. It is a long term project monitoring atmospheric deposition carried out by researchers from the Institute of Hydrobiology (Biology Centre of the Czech Academy of Sciences) (Kopáček et al., 1997). The volume-weighted means in the atmospheric deposition collected from May to October 2015 and used in the balance were 3.1 mg l−1, 1.34 mg l−1 and 42 µg l−1 for TOC, TN and TP, respectively, and the depth of precipitation was 307 mm over the same period. The concentrations of TOC, TN and TP in manure, feed and fish were obtained from the literature. The TOC, TN and TP inputs in manure, feed and output in harvested fish were estimated by multiplying their quantity with their respective concentrations. The mean concentrations of TOC, TN and TP in manure (cattle straw manure) were 100, 5.0 and 1.3 g kg−1 (MA-CR, 1998) whereas those for the feed (wheat grain) were 420, 15 and 4.0 g kg−1 (Čermák et al., 2008; Hlaváč et al., 2015; Rachon et al., 2015), respectively. Concentrations of TOC, TN and TP in fish biomass were considered to be 150, 40 and 7 to 9 g kg−1 (specifically for each species), respectively (Rothschein, 1983). The fish growth was estimated by empirical growth models for each species based on their stocked size and weight, and considering mortality losses that were calibrated for the Dehtář pond on six previous 2-year production periods with available data for stocking and harvest.

3 Results

3.1 Fishpond management

The Dehtář pond started refilling just after autumn fish harvest in November 2014 but the surface level did not reach the level planned for the 1st year of the production cycle (i.e., 405.85 m a.s.l.) due to dry weather conditions and little inflow (Fig. 2). The average pond morphological parameters during the balance period May–October 2015 were significantly smaller than its nominal values (i.e., volume 2.56 hm3, flooded area 1.57 km2; maximum and mean depths 4.7 and 1.6 m, respectively). The water renewal in the pond was minimal during the May–October period, with a theoretical water residence time of 1.6 years. The outflow from the pond occurred only through seepage, except at the end of October when a small amount of water was discharged through the main pond outlet at the dam.

Fish were stocked in November 2014 and in March 2015 (20% and 80% of the stocked biomass, respectively). The total biomass of the stocked fish was 390 kg ha−1 and consisted of 97% of common carp, 2.3% of grass carp, 0.6% of pikeperch, 0.1% of pike, and 0.1% of bighead carp. The body weight of the stocked common carp was 360 g on average and increased to ca 1.1 kg at the end of the growing season, according to our fish growth model. As in many Czech fishponds, also weed fish, dominated mainly by topmouth gudgeon (Pseudorasbora parva Temminck & Schlegel, 1846) and including roach (Rutilus rutilus L.), common bream (Abramis brama L.), silver bream (Abramis bjoerkna L.), rudd (Scardinius erythrophthalmus L.), and Prussian carp (Carassius gibelio Bloch, 1782) (Musil et al., 2007), were present in the Dehtář pond. Their biomass and time of pond invasion were not recorded in this study but were noticed later, at the fish harvest in 2016 (J. Potužák, pers. commun.). The biomass of stocked fish nearly doubled by the end of the study period, when it was 750 kg ha−1, according to the fish growth model. Cattle manure was used in the pond at the beginning of the growing season from March to April in the amount of 2200 kg ha−1. Wheat grain was used as supplementary feed with 4, 13, 26, 37 and 20% of total feed applied in May, June, July, August and September, respectively. The amounts of fish feed took into account water temperature, visually assessed zooplankton biomass and increasing biomass of fish stock. Fish were fed twice a week in May and three times a week in the remaining months. The total amount of supplementary feed used over the study period was 1900 kg ha−1. The food conversion ratio (FCR) that was calculated by dividing the feed amount (kg) by the live weight gain (kg) of the fish was 5.7.

thumbnail Fig. 2

Water inflow, outflow and losses by seepage, and trend of surface water level in the Dehtář pond during the period from November 2014 to December 2015.

3.2 Stratification and water quality

Thermal and oxygen stratification in the water column at site D during May–October 2015 showed a general polymictic pattern (Fig. 3). Nevertheless, during periods of warm and still weather, the water column stratified and DO rapidly exhausted above the bottom, leading to hypoxia. Largely depleted DO in such temporarily formed hypolimnion was measured in the first half of June, during almost the whole of July until early August, and in the beginning of September. In late summer and autumn, stratification became unstable with frequent mixing of the entire water column. Nevertheless, a temporary mild stratification was observed in September and early October, when differences in Tw in the water column were low (usually <0.5 °C) but DO concentrations at the surface and above the bottom differed significantly from the middle layers of the water column.

Dissolved and particulate fractions of OC, N and P concentrations increased gradually in the Dehtář pond during the May–October period (Fig. 4b, e, h). The DOC and POC concentrations increased approximately twofold: DOC from about 11 to 20 mg l−1 and POC from about 4 to 9 mg l−1. Inorganic carbon (TIC) increased relatively less from about 21 to 30 mg l−1. A similar seasonal pattern of C concentrations also occurred in the inflow into the pond (Fig. 4a), but its effect on concentrations in the Dehtář pond was minimal due to a very low flow during the summer (Fig. 2). Phytoplankton was present in the pond at a high concentration all year, with a drop in spring and then a gradual increase during the growing season, as evidenced by an increase in Chla concentration from approximately 30 µg l−1 in spring to more than 100 µg l−1 at the end of summer (Fig. 4c) and from the transparency of water decreasing from 0.65 m in May to 0.4 m in summer (Fig. 4f). TN concentration in the pond gradually increased from ca 1 to 2.5 mg l−1 concurrent with an accumulation of organic N (ON), while inorganic forms of nitrogen (N-NO3 and N-NH4+) were low during the whole season (<0.05 mg l−1). TP concentration also increased throughout the growing season to nearly 200 µg l−1 in the later summer and autumn, while SRP was relatively low (10–40 µg l−1). Despite low concentrations of inorganic N and P forms, biomass of seston increased during the whole growing season with a sestonic molar C/P ratio ranging from 100 to 150 (Fig. 4i).

thumbnail Fig. 3

Stratification of (a) water temperature (°C) and (b) dissolved oxygen (mg l−1) in the Dehtář pond at site D during the period from May to October 2015 plotted using weekly or two-weekly measured profiles.

thumbnail Fig. 4

Water quality in the Dehtář pond at site D and its inflow in 2015: (a) total carbon (TC), total organic carbon (TOC) and dissolved organic carbon (DOC) in the total volume-weighted inflow to the pond, (b) TC, TOC and DOC in the pond, (c) chlorophyll-a (Chla) in the pond, (d) total nitrogen (TN), nitrate nitrogen (N-NO3 ) and ammonium nitrogen (N-NH4 +) in the total volume-weighted inflow to the pond, (e) TN, N-NO3 and NH4 + in the pond, (f) water transparency (Z-Secchi), (g) total phosphorus (TP), dissolved phosphorus (DP) and soluble reactive phosphorus (SRP) in total volume-weighted inflow to the pond, (f) TP, DP and SRP in the pond, (i) C/P ratio in the pond.

3.3 Metabolic rates and phosphorus regeneration

High-frequency measurement of the DO concentration at depths of 0.3 to 1.5 m showed large fluctuations of their daily values from hypersaturation to deeply hypoxic values (Fig. 5a). The DO concentrations in these layers were always higher than the critical survival concentration of about 2 mg l−1 for cyprinid fish (Svobodova et al., 1993). The metabolic rates showed very dynamic changes characterized by frequent alternations between periods of autotrophy and periods of heterotrophy (Fig. 5b, c). The number of autotrophic days (NEP > 0) was almost equal to the number of heterotrophic days (NEP < 0) with a proportion of 53% and 47%, respectively. Daily rates of NEP ranged between −6.8 and 7.8 g O2 m−2 d−1 with an average of 0.2 g O2 m−2 d−1 (Fig. 5c) and the Dehtář pond was therefore slightly autotrophic. GPP rates varied between 0.1 and 21.1 g O2 m−2 d−1 with an average of 8.5 g O2 m−2 d−1 (Fig. 5b). ER rates varied between 0.4 and 24 g O2 m−2 d−1 with an average of 8.2 g O2 m−2 d−1 (Fig. 5b). Monthly averages values of GPP and ER were higher from June to September while NEP increased moderately in May and August (Tab. 1). The rate of P regeneration in the planktonic community was in the range of 8–19 mg m−2 d−1 while P demand ranged between 8 and 22 mg m−2 d−1 (Tab. 1).

thumbnail Fig. 5

Daily average values from May to October 2015 for: (a) dissolved oxygen concentrations at depths of 0.3 and 1.5 m and oxygen saturation concentration at the water surface; (b) gross primary production (GPP) and ecosystem respiration (ER); (d) net ecosystem production (NEP).

Table 1

Monthly metabolic rates of C (g m−2 d−1), C/P ratio of seston (mol mol−1), P regeneration (mg m−2 d−1) and P demand (mg m−2 d−1) in the Dehtář pond water from May to October 2015.

3.4 Organic carbon and nutrient balance

Total inputs of OC into the Dehtář pond during the 2015 growing season were 1025 t (Tab. 2). GPP, fish feeds and manure were the pond's main sources with a contribution of 82, 13 and 3.5% of all OC inputs, respectively. Manure was included in the balance because, although it was used before the beginning of the balance period, its decomposition is slow and its effect persists during the growing season. Ecosystem respiration was the main pathway of OC output from the system and accounted for 79% of all OC inputs. A small amount of OC (1.7%) left the system through the outflow and seepage, and an even smaller fraction (0.9% of OC inputs) was assimilated in the produced fish biomass. The fraction of OC that accumulated in the pond water, the calculated retention in the sediment, and/or loss of OC to the atmosphere represented 2.9 and 15.8% of all OC inputs, respectively.

Inputs of N and P into the Dehtář pond during the growing season of 2015 were 9.0 t and 2.0 t, respectively (Tab. 2). The main source for both nutrients was aquaculture: feed and manure applications contributed 73% of N inputs and 86% of P inputs. Inflows were the second most important source of nutrients into the pond and contributed 27 and 13% to TN and TP inputs, respectively. Unlike OC, relatively higher percentages of nutrients inputs were incorporated in the biomass of produced fish, namely 25 and 23% for TN and TP, respectively. The outflow and seepage accounted for 14% of TN and 6% of TP inputs in the pond. A significant proportion of N accumulated in the pond water during the growing season (i.e., 52% of TN inputs), whereas only 9% of TN was retained in the sediment and/or lost from the system. In contrast, the accumulation of P in pond water and P retention were 10 and 61% of TP inputs, respectively, indicating that P is more susceptible to sedimentation than N.

Table 2

Balance of OC, N and P in the Dehtář pond from May to October 2015 in metric tons and percentages related to total inputs.

4 Discussion

4.1 Structure of fishpond ecosystem, trophic conditions and metabolism

The ecosystem structure of Dehtář pond reflected the effect of reared fish that were stocked at high density. The phytoplankton community were dominated by colonial, filamentous algae and cyanobacteria during the summer months (Fránková et al., 2017), submersed aquatic plants were absent whereas emergent macrophytes were sparse in the littoral zone (K. Šumberová et al., unpubl. data). The zooplankton community was composed mainly of small-sized zooplankton species (e.g. Bosmina longirostris, nauplii, cyclopoid copepods, rotifers) and macroinvertebrates were rare (Potužák et al., 2007). These results are comparable to those of Iglesias et al. (2011) who found that small-sized zooplankton were inversely related to fish density in lakes. This ecosystem structure may be explained by the spectrum of the natural food of common carp and the present weed fish. Adult common carp are primarily bottom feeders and prefer macroinvertebrates but they are also water column feeders and consume larger zooplankton (Adámek et al., 2003). High predation pressure by intentionally overstocked fish eliminates large zooplankton individuals and macroinvertebrates at a high rate (Rahman et al., 2006). Weed fish compete with common carp for macroinvertebrates and large zooplankton, especially Daphnia, further reducing zooplankton and macroinvertebrate biomass (Musil et al., 2014). The zooplankton community is thus dominated by small individuals that cannot control the growth of larger and colonial species of phytoplankton (Matsuzaki et al., 2009). The abundance and diversity of macroinvertebrates were further reduced in Dehtář pond by frequent hypoxic conditions above the pond bottom and low biomass of macrophytes (Lemmens et al., 2015). This alteration of the grazing food web structure leads to autochthonous organic matter being accumulated and not being used in the food chain and subsequent fish biomass production, but instead sinking to the pond bottom and being degraded by microbial loop communities (Deines et al., 2015; Přikryl, 1996).

TOC, TN and TP concentrations in the Dehtář pond increased during the study period, mainly due to the accumulation of sestonic (or particulate) organic matter, nitrogen and phosphorus in water. The reason was apparently the increasing phytoplankton biomass as evidenced by the increase of Chla. The increase in the total amount of nutrients during the growing season was obviously due to feed addition rather than to inputs from the surrounding catchment, since the inflow and outflow were negligible. The low water exchange rate and small precipitation observed during this study further supported nutrient accumulation and growth of phytoplankton biomass in the Dehtář pond. These results are consistent with the results of Hopkins et al. (1993), who found that Chla, nutrients and organic matter concentrations were negatively correlated with water exchange and positively correlated with pond production.

N-NO3, N-NH4+ and SRP were low during the whole season. These low concentrations may be explained by denitrification and nutrient uptakes by the growing phytoplankton. Despite the relatively low concentrations of SRP throughout the growing season, phosphorus availability was clearly not a factor limiting the growth of phytoplankton. This is apparent from the molar C/P ratio of seston that varied between 100 and 150 (Fig. 4i), hence not differing much from the Redfield ratio (i.e., 106) in phytoplankton not limited by phosphorus (Hecky and Kilham, 1988; Vrba et al., 1995). There are two plausible explanations of this continuous growth and increase of phytoplankton biomass at such low inorganic nutrient levels: (i) Biotic recycling of organic P in the water column may explain this sustained growth of phytoplankton (Kamarainen et al., 2009; Knoll et al., 2016). Indeed, the calculated P needs for the planktonic community were the same as the P regeneration rate (Tab. 1). In addition, common carp excrete substantial amounts of nutrients that favour phytoplankton growth (Chumchal and Drenner, 2004). (ii) Sediment-bound P could have been released during the study period in the deepest parts of the pond where anoxic conditions were prevailing at the sediment water interface (Sondergaard et al., 2003).

In this study, the Dehtář pond can be classified as slightly autotrophic, based on the calculated metabolic rates. This indicates that the production of organic matter by phytoplankton was higher than its aerobic degradation by various living components of the Dehtář ecosystem. GPP and ER in Dehtář were comparable to lakes with similar trophic status (Tab. 3) where production of organic matter by phytoplankton and/or macrophytes was the source of OC that fuelled ER (Laas et al., 2012). On the other hand, GPP and NEP in the Dehtář pond were higher compared to those from heterotrophic lakes with lower trophic status (Tab. 3). In such lakes, various living components of the ecosystem breakdown organic matter by respiration at rates that exceed its production by photosynthesis. This occurs mainly in clear-water, humic and mesotrophic lakes receiving substantial terrestrial organic matter to fuel respiration (Duarte and Prairie, 2005). However, heterotrophy is not always supported by allochthonous OC in lakes. It can also be supported by autochthonous OC accumulated in lake sediment over time. Lake Apopka is an example of a heterotrophic lake in which excess respiration is supported by organic matter originating from a massive burial of macrophytes in the lake sediment. An irreversible ecological disturbance caused by hurricanes switched the community of primary producers from a macrophyte dominated one to a phytoplankton dominated (Bachmann et al., 2000). Despite substantial external OC inputs (feed and manure), the ecosystem metabolism was not heterotrophic in the Dehtář pond. A part of these inputs and GPP were respired while another part was retained in the sediment or metabolised anaerobically by methanogenesis and released into the atmosphere as carbon dioxide (CO2) or methane (CH4) (Oliveira Junior et al., 2019). Based on the findings of Rutegwa et al. (2019), Dehtář pond may have released 2 tons of diffusive CH4-C corresponding to 0.2% of total OC inputs to the pond over six months of this study in 2015. Total CH4 emission can be even higher if bubble flux of CH4-C is accounted for.

Table 3

Example values of metabolic rates in some selected lakes. Z mean (m): mean depth of the lake, GPP (mmol O2 m−2 d−1): gross primary production, ER (mmol O2 m−2 d−1): ecosystem respiration, NEP (mmol O2 m−2 d−1). International country codes based on the ISO 3166 standard published by the International Organization for Standardization ( are in parentheses.

4.2 Use efficiency of nutrient inputs

The efficiency of using OC, N and P inputs in the production of fish biomass in the Dehtář pond was 0.9, 25 and 23% of all OC, TP and TN inputs. The assimilation of OC by fish in this study is comparable to the results of Boyd et al. (2010) who reported the efficiency of OC use in the range of 0.86 to 3.44% in tilapia ponds. Our value is lower than the OC use efficiency reported by Zhang et al. (2016) who observed higher values, ranging from 4.5 to 8.3%, in polyculture ponds of swimming crab, white shrimp and short necked clam in China. This higher efficiency of OC use apparently resulted from a better use of OC inputs by the reared species exploiting different feeding niches. The efficiency of N and P use reported in our study is also in the range of the values reported in other studies of polyculture fishponds. On average, produced fish utilise ca 25 and 20% of N and P, respectively, of all N and P inputs (Hargreaves, 1998; Rahman et al., 2008).

This comparison shows that in general the efficiency of using OC, N and P inputs is relatively small in the current practice of managing semi-intensive fishponds. A large proportion of inputs (more than 95% of OC and three quarters of N and P) in this type of ponds is not used by the reared animals. In the Dehtář pond, there are two obvious reasons for this low efficiency: (i) high predation pressure on zooplankton due to high fish biomass, which causes poor transfer of C from phytoplankton via zooplankton and/or benthic macroinvertebrates to fish; and (ii) low digestibility of the wheat grain used as fish feed. Under such conditions, the fish must be fed by supplementary feed. The low share of zooplankton as a source of food for fish in Czech semi-intensive ponds can be further demonstrated by the fatty acid (FA) composition of the produced common carp. The FA composition in fish muscles reflects the diet (Steffens, 1997). Zooplankton and macroinvertebrates that feed on algae are rich in omega-3 (n-3) and omega-6 (n-6) polyunsaturated fatty acids (PUFA) while cereals are carbohydrate rich and poor in n-3 PUFA (Böhm et al., 2014). The contents of n-3 and n-6 PUFA and the ratio n-3/n-6 PUFA are several times lower in carp which feed mostly on cereals in densely stocked ponds than in extensive ponds, where conditions are favourable for large zooplankton (Steffens and Wirth, 2007). Similarly, Mráz et al. (2012) showed that fish produced in semi-intensive Czech fishponds supplemented with cereals have low levels of n-3 and n-6 PUFA and low n-3/n-6 PUFA ratios suggesting the low contribution of zooplankton and macroinvertebrates in their diet and demonstrating low efficiency of using algal primary production in fish biomass production.

The low ability of reared fish to digest cereals is another reason that may explain the low efficiency of using OC, N and P inputs in the Dehtář pond (Degani, 2006; Fagbenro, 1999). The absence of phytase in the carp digestive tract and the presence of digestive enzyme-resistant compounds in cereals (e.g. phytates) is a reason that has been suggested to explain this low cereal digestibility (Fagbenro, 1999). The low digestibility of cereals increases FCR leading to an accumulation of wastes from feed in the fishpond. The FCR in our study was 5.7, which is higher than the average FCR of 4.7 in carp ponds using cereals as supplementary feed (Woynarovich et al., 2011). Thus, partially digested grain promotes primary production by releasing nutrients (P and N) instead of serving as direct feed for fish. They end up becoming part of the pond bottom and may be ingested again along with plant detritus by carp after being partially degraded by bacteria. Detritus may contribute approximately 70% of the natural food of common carp in extensively managed ponds (Adámek et al., 2003). However, more research is needed to understand this pathway of nutrient use from feed. The poor quality of supplementary feed used in the Dehtář pond may also be used to explain the contribution of supplied feed to fish production. Fish biomass production in this study (370 kg ha−1) was lower than the expected production of 565 kg ha−1, which should be achieved with an average FCR value for carp ponds that use wheat as a supplementary feed (Woynarovich et al., 2011). The FCR of grain is lower than the optimal one that ranges between 1.5 and 2 (Craig et al., 2017).

5 Conclusion

The use efficiency of OC, TN and TP inputs in the produced fish biomass was low, indicating an overloading of OC, N and P in the Dehtář pond, similar to other polyculture carp ponds with comparable fishery management practices. Respiration was the main output of OC from the pond, while accumulation in water and sediment were the main routes for N and P, respectively. This overloading by inputs impairs pond water quality, and primary production does not contribute much to fish production. The main reasons are high fish density and the disruption of the natural food chain in the pond. This also increases the pollution potential of effluents from fish farming activities and emissions of greenhouse gases. Unused inputs represent avoidable production costs. Our results from the Dehtář pond, which were obtained under low flow hydrological conditions when many pond processes were well recognizable, call for more research into pond management practices that will help to improve fish production efficiency while minimizing pollution risks in Dehtář pond and other hypereutrophic carp ponds. These practices include the decrease of fish stock density, stopping the use of manure and replacing cereals by draff or mechanically treated cereals.

Supplementary Material

Supplementary material provided by the author.

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The study was financially supported by the Ministry of Education, Youth and Sports of the Czech Republic − projects “CENAKVA” (LM2018099), FISHPOND2014 (No. LD14045, programme LD–COST CZ), Grant Agency of the University of South Bohemia (Nos. 122/2019/Z and 046/2017/Z), and by the Grant Agency of the Czech Republic (No. 17-09310S). The high frequency monitoring of limnological variables were done in the framework of the FP7 project NETLAKE (EU COST Action ES 1201). The authors are grateful to the fishery company Rybářství Hluboká cz. s.r.o, and the Czech Hydrometeorological Institute (České Budějovice branch) for providing fishery production and precipitation data, respectively.


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Cite this article as: Rutegwa M, Potužák J, Hejzlar J, Drozd B. 2019. Carbon metabolism and nutrient balance in a hypereutrophic semi-intensive fishpond. Knowl. Manag. Aquat. Ecosyst., 420, 49.

All Tables

Table 1

Monthly metabolic rates of C (g m−2 d−1), C/P ratio of seston (mol mol−1), P regeneration (mg m−2 d−1) and P demand (mg m−2 d−1) in the Dehtář pond water from May to October 2015.

Table 2

Balance of OC, N and P in the Dehtář pond from May to October 2015 in metric tons and percentages related to total inputs.

Table 3

Example values of metabolic rates in some selected lakes. Z mean (m): mean depth of the lake, GPP (mmol O2 m−2 d−1): gross primary production, ER (mmol O2 m−2 d−1): ecosystem respiration, NEP (mmol O2 m−2 d−1). International country codes based on the ISO 3166 standard published by the International Organization for Standardization ( are in parentheses.

All Figures

thumbnail Fig. 1

Location of the Dehtář pond. The crosses indicate the metabolism measurements and water sampling sites. The isobaths in the Dehtář and Posměch ponds show the depths in meters at the water level at maximum filling.

In the text
thumbnail Fig. 2

Water inflow, outflow and losses by seepage, and trend of surface water level in the Dehtář pond during the period from November 2014 to December 2015.

In the text
thumbnail Fig. 3

Stratification of (a) water temperature (°C) and (b) dissolved oxygen (mg l−1) in the Dehtář pond at site D during the period from May to October 2015 plotted using weekly or two-weekly measured profiles.

In the text
thumbnail Fig. 4

Water quality in the Dehtář pond at site D and its inflow in 2015: (a) total carbon (TC), total organic carbon (TOC) and dissolved organic carbon (DOC) in the total volume-weighted inflow to the pond, (b) TC, TOC and DOC in the pond, (c) chlorophyll-a (Chla) in the pond, (d) total nitrogen (TN), nitrate nitrogen (N-NO3 ) and ammonium nitrogen (N-NH4 +) in the total volume-weighted inflow to the pond, (e) TN, N-NO3 and NH4 + in the pond, (f) water transparency (Z-Secchi), (g) total phosphorus (TP), dissolved phosphorus (DP) and soluble reactive phosphorus (SRP) in total volume-weighted inflow to the pond, (f) TP, DP and SRP in the pond, (i) C/P ratio in the pond.

In the text
thumbnail Fig. 5

Daily average values from May to October 2015 for: (a) dissolved oxygen concentrations at depths of 0.3 and 1.5 m and oxygen saturation concentration at the water surface; (b) gross primary production (GPP) and ecosystem respiration (ER); (d) net ecosystem production (NEP).

In the text

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