Jiří Kopáček

Czech University of Life Sciences Prague, Praha, Praha, Czech Republic

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Publications (109)189.78 Total impact

  • Jiří Kopáček · Josef Hejzlar · Jiří Kaňa · Petr Porcal · Jan Turek
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    ABSTRACT: Fluxes of major ions and nutrients were measured in the N-saturated mountain forest catchment-lake system of Čertovo Lake (Czech Republic) from 1998 to 2014. The lake has been rapidly recovering from atmospheric acidification due to a 90% decrease in sulphate (SO42-) deposition since the late 1980s and nitrate (NO3-) contribution to the pool of strong acid anion and leaching of dissolved organic carbon (DOC) have increased. Present concentrations of base cations, phosphorus (P), total organic N (TON), and ionic (Ali) and organically bound (Alo) aluminium in tributaries are thus predominantly governed by NO3- and DOC leaching. Despite a continuing recovery lasting 25 years, the Čertovo catchment is still a net source of protons (H+), producing 44 mmol m-2 yr-1 H+ on a catchment-area basis (corresponding to 35 μmol L-1 on a concentration basis). Retention of the deposited inorganic N in the catchment averages 20%, and ammonium consumption (51 mmol m-2 yr-1) and net NO3- production (28 mol m-2 yr-1) are together the dominant terrestrial H+ generating processes. In contrast, the importance of SO42- release from the soils on terrestrial H+ production is continuously decreasing, with an average of 47 mmol m-2 yr-1 during the study. The in-lake biogeochemical processes reduce the incoming acidity by ∼40%, neutralizing 23 μmol L-1 H+ (i.e., 225 mmol m-2 yr-1 on a lake-area basis). Denitrification and photochemical and microbial decomposition of DOC are the most important in-lake H+ consuming processes (50 and 39%, respectively), while hydrolysis of Ali (from tributaries and photochemically liberated from Alo) is the dominant in-lake H+ generating process. Because the trends in water chemistry and H+ balance in the catchment-lake system are increasingly related to variability in NO3- and DOC leaching, they have become sensitive to climate-related factors (drought, elevated runoff) and forest damage that significantly modify the leaching of these anions. During the study period, increased exports of NO3- (accompanied by Ali and base cations) from the Čertovo catchment occurred after a dry and hot summer, after forest damage, and during elevated winter runoff. Increasing DOC export due to decreasing acid deposition was further elevated during years with higher runoff (and especially during events with lateral flow), and was accompanied by P, TON, and Alo leaching. The climate-related processes, which originally "only" confounded chemical trends in waters recovering from acidification, may soon become the dominant variables controlling water composition in N-saturated catchments.
    No preview · Article · Apr 2016 · Ecological Indicators
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    ABSTRACT: A hybrid anion resin, based on hydrous iron oxide nanoparticles, was tested for in situ phosphorus (P) availability measurement in soils of two mountain stands recovering from acidification and having different P sorption characteristics. Phosphate (P-PO4) sorption capacity of the resin (before saturation) was 48 µmol g-1 on a dry weight basis. Sorption and elution characteristics of the resin were tested under P-PO4 concentrations common in acidic soils (0–0.42 mmol l-1) either with or without the presence of sulphate (0.2 mmol l-1). The advantage of this resin was its low affinity to sulphate. The efficiency of P-PO4 sorption was independent on the sulphate presence and was on average 100±0.2 % (n = 56, ± sd). The P-PO4 recovery of the resin stabilized after six dynamic elution steps (each: 50 ml of 0.5M NaOH, resin:solution ratio of 5:1 by volume). The average efficiency of P-PO4 recovery was 80±7 %, and was used to evaluate field measurements. We determined the amount of bioavailable P-PO4 in the field using resin bags exposed in situ in litter and humus horizons (November-May, June-October) in three consecutive years (2007–2010). Our data suggest this method as a perspective tool to track differences in P-PO4 bioavailability in soils. The results indicate that bioavailable P is negatively related to the soil ability to retain P. http://www.tandfonline.com/eprint/tMzqpx9t5XY3He7jGY89/full
    No preview · Article · Feb 2016 · Communications in Soil Science and Plant Analysis
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    ABSTRACT: Sediment cores from Sargent Mountain Pond, Maine, USA and Plešné Lake, southwestern Czech Republic, record the entire post-glacial terrestrial vegetation, lake algal communities, and chemical dynamics of the watershed and lake from 16,600 and 14,600 Cal Yr BP, respectively, to the present. Both watersheds are underlain by granite, and overlain by till. Total rare earth element (REE) concentrations and fluxes to the sediment declined from deglaciation until forest developed slightly prior to the Younger Dryas (YD) (12,600–11,600 Cal Yr BP) at Sargent Mountain Pond, and immediately after the YD at Plešné Lake, peaked in value just after the YD, and then declined to the present. Before the YD, REE concentrations were dominated by detrital, soluble apatite [Ca5(PO4)3(OH)]. Weathering of apatite contributed the phosphorus (P) sequestered as NaOH-extractable P in the lake sediment. After the YD, REE concentrations and fluxes behave coherently with NaOH-extractable aluminum (Al) and P after forestation in each catchment. Concentrations of extractable REEs, P, and Al peak after the YD and decline coherently to the present. We hypothesize that as climate ameliorated after glaciation, afforestation occurred and organic-rich forest soils developed. These soils produced higher concentrations of dissolved organic carbon (DOC) in soil water and runoff. Concurrently, the weathering of apatite released PO4 and Ca to runoff, raising pH to ~8. The soil DOC complexed with and mobilized Al and REEs, which were transported to the lakes in runoff. There, photo-oxidation of the Al–DOC and REE–DOC complexes caused release of ionic, inorganic Al and REEs, precipitation of Al(OH)3 in the higher-pH environment, adsorption of REEs and PO4 by the Al(OH)3, and irreversible sedimentation. REE concentrations and fluxes declined from the YD to the present because the apatite was progressively depleted in the soil by weathering, while REEs were increasingly retained by secondary Al(OH)3 [and Fe(OH)3 to a lesser degree] in the soil. The adsorption ability of soil and water-column Al(OH)3 for P increased, but for REEs likely declined, as the watershed soils developed and acidified. This natural process was further magnified by atmospheric acidification, as indicated by changes in diatom assemblages.
    No preview · Article · Feb 2016 · Journal of Paleolimnology
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    ABSTRACT: 1. The response of planktonic (phytoplankton, ciliates, rotifers and crustaceans) and littoral (Ephemeroptera, Plecoptera, Trichoptera and Heteroptera: Nepomorpha) assemblages to chemical recovery was studied over a twelve-year period (1999–2011) in eight glacial lakes in the Bohemian Forest (central Europe). The region suffered from high atmospheric pollution from the 1950s to the late 1980s, but has since been recovering from acidification due to 86% and 44% decrease in sulphur and nitrogen deposition, respectively, during the 1990s–2000s. Despite the rapid improvement in water chemistry of all the eight studied lakes, only four have partly recovered so far (low-aluminium lakes), while the other four lakes still remain strongly acidic (high-aluminium lakes). 2. All present lake assemblages are dissimilar by 40–90% from those during the early phase of chemical recovery as a result of species (re)colonisation (ciliates, crustaceans and insects) in the high-Al lakes, and considerable species replacement (zooplankton) and (re)colonisation (insects) in the low-Al lakes. Phytoplankton remained very similar in the high-Al lakes, but changed (loss and/or replacement of some acid-tolerant species) in the low-Al lakes. 3. Aluminium (Al) concentrations were dominant in structuring the assemblages of phytoplankton, rotifers and Nepomorpha, but also affected crustaceans through the seston carbon to phosphorus (P) ratio. Both direct (toxicity) and indirect (P availability) effects of Al control biological recovery in the Bohemian Forest lakes. A concentration of 200 lg L-1 of total Al is the main barrier preventing the high-Al lakes from recovery. In contrast, pH and total P rather than Al significantly influenced Ephemeroptera, Plecoptera and Trichoptera. 4. Although biotic responses (especially in the low-Al lakes) showed important signs of recovery, such as reappearance of some indigenous or acid-sensitive species, decline in eurytopic acid-tolerant species and colonisation by vagile species, the assemblages of all the lakes still suffer from acid stress. Our results also indicate an increasing role of biotic interactions between colonisers and residents leading to the reconstruction of aquatic food webs in the low-Al lakes.
    No preview · Article · Jan 2016 · Freshwater Biology
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    ABSTRACT: Mountain forests in National park Bohemian Forest (Czech Republic) were affected by bark beetle attack and windthrows in 2004–2008, followed by an extensive tree dieback. We evaluated changes in the biochemistry of the uppermost soil horizons with the emphasis on carbon (C) and nitrogen (N) cycling in a near-natural spruce (Picea abies) mountain forest after the forest dieback, and compared it with an undisturbed control plot of similar age, climate , elevation, deposition, N-saturation level, and land use history. We hypothesised that the high litter input after forest dieback at the disturbed plot and its consequent decomposition might influence the availability of C for microorganisms, and consequently, N transformations in the soil. The concentrations of dissolved organic C (DOC) and N (DON) in soil water extracts rapidly increased at the disturbed plot for 3 yeas and then continually decreased. Net ammonification exhibited a similar trend as DOC and DON, indicating elevated mineralization. Despite the high ammonium concentrations found after the forest die-back (an increase from 0.5 mmol kg-1 to 2–3 mmol kg-1), net nitrification was stable and low during these 3 years. After the DOC depletion and decrease in microbial biomass 5 years after the forest dieback, net nitrification started to rise, and nitrate concentrations increased from 0.2–1 mmol kg-1 to 2–3 mmol kg-1. Our results emphasize the key role of the availability of organic C in microbial N transformations, which probably promoted microbial heterotro-phic activity at the expense of slow-growing nitrifiers.
    Full-text · Article · Jul 2015 · PLoS ONE
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    ABSTRACT: Glacial lakes in the Bohemian Forest (Šumava, Böhmerwald) belong to the most atmospherically acidified lake districts in the world. Available historical data and regular monitoring (since 1984) provide a valuable background for long-term ecological research of the catchment–lake ecosystems. This paper is an overview of recent projects covering the last two decades. The review of published papers provides details on the organization and aims of present research on the Bohemian Forest lakes that currently focuses on chemical and biological recovery of the catchment–lake systems from atmospheric acidification, and effects of climate change and forest vigour on biogeochemical processes in terrestrial and aquatic ecosystems.
    Full-text · Article · Jul 2015
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    ABSTRACT: Using relationships between the composition of precipitation and emission rates of sulphur and nitrogen compounds and dust from 1978 to 2012, we modelled concentrations of sulphate, nitrate, ammonium, chloride, and base cations and pH of precipitation in the Tatra Mountains (central Europe) back to 1900. The modelled precipitation chemistry exhibited a high degree of temporal coherence with the lake water chemistry in 1937 and during the period 1984–2014. The ionic composition of lake water reflected progress in their acidification until the late 1980s, and then a rapid recovery. The response of lake water chemistry to changes in precipitation chemistry differed for individual ions, nutrients, and among lakes, predominantly reflecting the proportions of soil in their catchments. Important differences occurred in nutrient concentrations. In-lake concentrations of dissolved organic carbon (DOC) and total organic nitrogen (TON) exhibited inverse patterns to nitrate. DOC and TON were higher in lakes with a higher proportion of soil in the catchments, and increased in many lakes during recovery from acidification, while nitrate concentrations were higher and decreased most steeply in the catchments with sparse soils. Lake water concentrations of total phosphorus (TP) were spatially similar to that of DOC and TON, but increased most steeply during recovery in lakes with a high proportion of till soils. Our results indicate that chemical recovery of mountain ecosystems is seriously modified by catchment biogeochemistry and may result not only in elevated DOC leaching, but also in an increase of terrestrial export of TON and TP to the receiving surface waters.
    Full-text · Article · Jul 2015 · Biogeochemistry
  • Jiří Jan · Jakub Borovec · Jiří Kopáček · Josef Hejzlar
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    ABSTRACT: Purpose Numerous extraction procedures have been used to characterize phosphorus (P) forms bound to iron (Fe) and aluminum (Al) (hydr)oxides in soils and sediments. We propose a simple modification of a widely used P fractionation method that more precisely quantifies P associated with active Fe and Al (hydr)oxides, which are mostly responsible for P binding and its potential release to water. Materials and methods We modified the original sequential extraction [H2O, bicarbonate-dithionite (BD), NaOH, HCl] by adding short (10-min) extractions with BD and NaOH prior to the respective original steps. The method was verified using (1) dissolution kinetics of Fe and Al minerals of different crystallinity and (2) liberation of P, Fe, and Al from natural samples of soils, sediments, and settling seston, containing different proportions of amorphous and crystalline Fe and Al (hydr)oxides. Extracted P was analyzed for reactive and non-reactive (mostly organic) P forms. Results and discussion Both mineral and organic P forms associated with Fe and Al were almost completely liberated from the samples during the 10-min BD and NaOH extractions, respectively. Prolonged extraction period caused a partial P re-adsorption onto the solid phase in some samples. The 10-min extractions were able to dissolve amorphous Fe and Al (hydr)oxides (ferrihydrite, amorphous AlOOH) and a portion of more crystalline Fe and Al minerals, approximately related to their surface area. Conclusions The additional short extraction steps allow a rapid and more precise quantification of P associated with active Al and Fe (hydr)oxides, and better estimate the amounts of these Fe and Al forms in soils and sediments than the original method. Our simple modification of the traditional method thus provides new and useful information for environmental studies focused on potential P mobility across a solid phase-water interface.
    No preview · Article · Jul 2015 · Journal of Soils and Sediments
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    ABSTRACT: Nitrogen (N) deposition is globally considered as a major threat to ecosystem functioning with important consequences for biodiversity, carbon sequestration and N retention. Lowered N retention as manifested by elevated concentrations of inorganic N in surface waters indicates ecosystem N saturation. Nitrate (NO3) concentrations in runoff from semi-natural catchments typically show an annual cycle, with low concentrations during the summer and high concentrations during the winter. Process-oriented catchment-scale biogeochemical models provide tools for simulation and testing changes in surface water and soil chemistry in response to changes in sulphur (S) and N deposition and climate. Here we examine the ability of MAGIC to simulate the observed monthly as well as the long-term trends over 10–35 years of inorganic N concentrations in streamwaters from four monitored headwater catchments in Europe: Čertovo Lake in the Czech Republic, Afon Gwy at Plynlimon, UK, Storgama, Norway and G2 NITREX at Gårdsjön, Sweden. The balance between N inputs (mineralization + deposition) and microbial immobilization and plant uptake defined the seasonal pattern of NO3 leaching. N mineralization and N uptake were assumed to be governed by temperature, described by Q10 functions. Seasonality in NO3 concentration and fluxes were satisfactorily reproduced at three sites (R2 of predicted vs. modelled concentrations varied between 0.32 and 0.47 and for fluxes between 0.36 and 0.88). The model was less successful in reproducing the observed NO3 concentrations and fluxes at the experimental N addition site G2 NITREX (R2 = 0.01 and R2 = 0.19, respectively). In contrast to the three monitored sites, Gårdsjön is in a state of change from a N-limited to N-rich ecosystem due to 20 years of experimental N addition. At Gårdsjön the measured NO3 seasonal pattern did not follow typical annual cycle for reasons which are not well understood, and thus not simulated by the model.
    Full-text · Article · Jun 2015 · Science of The Total Environment
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    Meelis Seedre · Jiří Kopáček · Pavel Janda · Radek Bače · Miroslav Svoboda
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    ABSTRACT: Good understanding of forest productivity and carbon (C) storage capacity is essential for better understanding of C dynamics and climate modeling. Studies of old-growth forest C dynamics from central and eastern Europe are rare and the few remaining pristine forests represent a unique opportunity to study natural forest dynamics in an otherwise managed landscape. We studied protected old-growth Norway spruce (Picea abies L.) stands in the Bohemian Forest, Czech Republic, to explore total ecosystem C pool (live and dead biomass and soil) variability in forest ecosystem as a function of stand age and elevation. These old-growth forest ecosystems store very high amounts of C, up to 570 t C ha -1 , and 393 t C ha -1 on average. Live biomass is the dominant C pool followed by mineral soil, forest floor and dead biomass. We found that total C significantly decreased with increasing elevation (1025–1338 m a.s.l) from 456 to 294 t C ha -1 , predominantly driven by decreases in live biomass and forest floor C pools. Significant changes take place in individual pools based on age and elevation gradients, but total C was not significantly different between stands age 116–145 years. Contrary to some recent findings that old-growth forest ecosystems continue to sequester C long after maturity, our data supports the hypothesis that old-growth forests reach a steady state and become C neutral. They accumulate same amount of C through photosynthesis than is lost by decay and leaching. This study provides a detailed overview of C pools of old-growth Bohemian Forests and highlights the importance of including all major C pools in forest ecosystem C studies.
    Full-text · Article · Jun 2015 · Forest Ecology and Management
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    ABSTRACT: We investigated litterfall chemistry and fluxes, and cellulose decomposition in litter floor in mature, unmanaged Norway spruce stands in the catchments of Plešné and Čertovo lakes (Czech Republic) during 2003–2013. The Plešné forest was infested by the bark beetle (Ips typographus) in 2004, and 88%–99% of trees had died by 2011. Total litterfall and its composition were similar in both catchments in 2003. The litterfall increased from 5.4 to 42 t ha−1 yr−1 after the infestation and remained relatively high (5.0 t ha−1 yr−1) until the end of the study even though > 52% of trees were already broken. The chemical composition of most spruce litter categories changed after infestation, with the most pronounced trends in C (decrease) and Ca (increase) concentrations. Moreover, Mg, K, and P concentrations increased in the total Plešné litter due to an increasing proportion of rowan litter. Cellulose decomposition increased in the litter floor after infestation.
    No preview · Article · Jun 2015 · Boreal Environment Research
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    Petr Porcal · Jiří Kopáček · Iva Tomková
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    ABSTRACT: The photochemical release of inorganic nitrogen from dissolved organic matter is an important source of bio-available nitrogen (N) in N-limited aquatic ecosystems. We conducted photochemical experiments and used mathematical models based on pseudo-first-order reaction kinetics to quantify the photochemical transformations of individual N species and their seasonal effects on N cycling in a mountain forest stream and lake (Plešné Lake, Czech Republic). Results from laboratory experiments on photochemical changes in N speciation were compared to measured lake N budgets. Concentrations of organic nitrogen (Norg; 40-58 µmol L-1) decreased from 3 to 26% during 48-hour laboratory irradiation (an equivalent of 4-5 days of natural solar insolation) due to photochemical mineralization to ammonium (NH4+) and other N forms (Nx; possibly N oxides and N2). In addition to Norg mineralization, Nx also originated from photochemical nitrate (NO3-) reduction. Laboratory exposure of a first-order forest stream water samples showed a high amount of seasonality, with the maximum rates of Norg mineralization and NH4+ production in winter and spring, and the maximum NO3- reduction occurring in summer. These photochemical changes could have an ecologically significant effect on NH4+ concentrations in streams (doubling their terrestrial fluxes from soils) and on concentrations of dissolved Norg in the lake. In contrast, photochemical reactions reduced NO3- fluxes by a negligible (<1%) amount and had a negligible effect on the aquatic cycle of this N form.
    Full-text · Article · Dec 2014 · PLoS ONE
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    ABSTRACT: Mountain lakes in the Bohemian Forest, on both the Czech and German sides, were atmospherically acidified mainly in the 1960s–1980s and have since been recovering from acidification. In 2007, we performed the first complete study on littoral macroinvertebrates in all eight lakes. The goals of the study were to 1) compare macroinvertebrates in the lakes during the process of recovery and 2) investigate relations between the occurrence of taxa and water chemistry. Lake water pH varied from 4.6 to 5.7, concentrations of dissolved reactive Al and labile Al ranged from 118–601 and 11–470 μg l-1, respectively, and DOC concentrations were <6 mg l-1. Altogether 73 taxa were identified from all lakes; a positive relationship was found between pH and the number of macroinvertebrate taxa. The highest number of taxa was found in the least acidic lakes Laka and Grosser Arbersee, including the mollusk Pisidium casertanum. In contrast, the lowest diversity was found in the most acidified Čertovo jezero. Cluster analyses of macroinvertebrates and water chemistry suggested pH as the key factor influencing the occurrence of macroinvertebrate taxa. An interesting finding was the occurrence of the boreo-montane water beetle Nebrioporus assimilis in Prášilské jezero, which is the first documented record of this species in the Czech Republic since 1960.
    Full-text · Article · Sep 2014 · Biologia
  • Jiří Kopáček · Josef Hejzlar · Petr Porcal · Maximilian Posch
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    ABSTRACT: Using data on long-term monitoring of water quality, mass budgets, and empirical models, we quantified chloride (Cl) leaching from major diffuse and point sources in a large central European catchment (upper Vltava river, Czech Republic) over a 110-year period (1900–2010), with the major aim to evaluate the influence of historical changes in land use and management practices on Cl leaching from agricultural land. The Cl input to farmland in synthetic fertilizers, livestock feed, and atmospheric deposition tripled in the 1950s–1980s (from 23 to 64 kg ha−1 year−1 on average), and then abruptly decreased to ~14 kg ha−1 year−1 during 1990–2010. The proportion of drained agricultural land rapidly increased from 4 % in the 1950s to its maximum of 43 % in the 1990s. Until the 1950s, the Cl leaching from agricultural land followed a simple dose–response function. Then, agricultural soils retained on average 16 ± 4 kg ha−1 year−1 of Cl during 1959–1985, when the most important changes in land use and management practices occurred, and subsequently became a net Cl source of 11 ± 3 kg ha−1 year−1 on average during 1986–2010, when Cl input to soils declined and drainage of new land ceased. Our data suggest that the temporal changes in the Cl storage in agricultural land are associated with changes in Cl concentrations in both permanent soil water and soils. Physico-chemical conditions in freshly drained soils, namely elevated aeration and high concentrations of soil organic matter (SOM), and high Cl inputs probably resulted in a Cl immobilization in soils by formation of organic chlorine (Clorg) and adsorption that was higher than the Cl production from Clorg mineralization and desorption. In contrast, Clorg mineralization and Cl desorption exceeded the Cl retention during the consecutive period of low Cl inputs and decreasing SOM concentrations in agricultural soils. Our study implies that changes in land use and agricultural management can significantly affect dose–response functions even for Cl, which is traditionally considered and modelled as a conservative ion.
    No preview · Article · Aug 2014 · Biogeochemistry
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    ABSTRACT: Anthropogenically derived nitrogen (N) has a central role in global environmental changes, including climate change, biodiversity loss, air pollution, greenhouse gas emission, water pollution, as well as food production and human health. Current understanding of the biogeochemical processes that govern the N cycle in coupled human-ecological systems around the globe is drawn largely from the long-term ecological monitoring and experimental studies. Here, we review spatial and temporal patterns and trends in reactive N emissions, and the interactions between N and other important elements that dictate their delivery from terrestrial to aquatic ecosystems, and the impacts of N on biodiversity and human society. Integrated international and long-term collaborative studies covering research gaps will reduce uncertainties and promote further understanding of the nitrogen cycle in various ecosystems.
    Full-text · Article · Jul 2014 · AMBIO A Journal of the Human Environment
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    Jiří Kopáček · Petr Porcal · Josef Hejzlar

    Full-text · Dataset · Apr 2014
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    Jiří Kopáček · Petr Porcal · Josef Hejzlar

    Full-text · Dataset · Apr 2014
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    Jaroslav Vrba · Jiří Kopáček · Jan Fott · Linda Nedbalová
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    ABSTRACT: We examined long-term data on water chemistry of Lake Rachelsee (Germany) following the changes in acidic depositions in central Europe since 1980s. Despite gradual chemical recovery of Rachelsee, its biological recovery was delayed. In 1999, lake recovery was abruptly reversed by a coincident forest die-back, which resulted in elevated terrestrial export of nitrate and ionic aluminum lasting ~5 years. This re-acidification episode provided unique opportunity to study plankton recovery in the rapidly recovering lake water after the abrupt decline in nitrate leaching from the catchment. There were sudden changes both in lake water chemistry and in plankton biomass structure, such as decreased bacterial filaments, increased phytoplankton biomass, and rotifer abundance. The shift from dominance of heterotrophic to autotrophic organisms suggested their substantial release from severe phosphorus stress. Such a rapid change in plankton structure in a lake recovering from acidity has, to the best of our knowledge, not been previously documented.
    Full-text · Article · Feb 2014 · AMBIO A Journal of the Human Environment
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    ABSTRACT: Ionic and nutrient compositions of tributaries to Plešné Lake (PL, 4 inlets, granite bedrock) and Čertovo Lake (CT, 7 inlets, mica schist and quartzite bedrock) were analyzed in 3-week intervals from October 1997 to November 2012. Norway spruce stands, dominating both catchments, were damaged during this study: 93% of the PL mature trees died due to bark beetle infestation between 2004–2011; 14% of the CT forest was seriously damaged by windthrows and bark beetle in 2007–2011. Almost all dead biomass remained in the catchments. Prior to the forest damage, water chemistry of tributaries exhibited trends typical for areas recovering from strong atmospheric acidification, such as decreasing concentrations of strong acid anions, base cations, ionic aluminium (Al i), and protons (increasing pH). Chemistry of tributaries draining the af-fected sub-catchments rapidly changed after the forest damage. Concentrations of nitrate immediately in-creased, reaching the maximum values (up to 350 μmol.l –1) within 3–6 years after the forest dieback, then started to decline. Nitrate became the dominant anion and its leaching was accompanied by similar trends in Al i and potassium (K +) concentrations, and decreasing pH. Increases in magnesium (Mg 2+) and calcium (Ca 2+) leaching were less steep than those of Al i and K + , but continued at elevated rates until the end of the study. The elevated leaching of phosphorus (P) and dissolved organic carbon (DOC) and nitrogen (DON) occurred immediately after forest dieback. The DON concentrations increased more steeply than DOC, resulting in decreasing DOC:DON ratios. Because almost no biomass was removed from the damaged fo-rest, leaching of K +
    Full-text · Article · Nov 2013
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    Jiří Kopáček · Josef Hejzlar · Petr Porcal · Maximilian Posch
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    ABSTRACT: Using dynamic, mass budget, and empirical models, we quantified sulphate-sulphur (SO4-S) leaching from soils in a large central European catchment (upper Vltava river, Czech Republic) over a 110-year period (1900-2010). SO4-S inputs to soils with synthetic fertilisers and atmospheric deposition increased in the 1950s-1980s, then rapidly decreased (~80%), and remained low since the middle 1990s. The proportion of drained agricultural land rapidly increased from 4 to 43% between the 1950s and 1990s; then the draining ability of the system slowly decreased due to its ageing. Sulphate concentrations in the Vltava exhibited similar trends as the external SO4-S inputs, suggesting that they could be explained by changes in atmospheric and fertiliser S inputs. The available data and modelling, however, showed that (i) internal SO4-S sources (mineralization of soil organic S in the drained agricultural land), (ii) a hysteresis in SO4-S leaching from forest soils (a net S retention at the high S inputs and then a net release at the lowered inputs), and (iii) hydrology must be taken into account. An empirical model was then employed, based on parameters representing hydrology (discharge), external SO4-S sources (inputs by synthetic fertilisers and atmospheric deposition), and internal SO4-S sources (mineralization related to soil drainage). The model explained 84% of the observed variability in annual SO4-S concentrations in the Vltava river during 1900-2010 and showed that forest soils were a net sink (105kgha(-1)) while agricultural land was a net source (55kgha(-1)) of SO4-S during 1960-2010. In the late 1980s, forest soils changed from a sink to a source of S, and the present release of SO4-S accumulated in forest soils thus delays recovery of surface waters from acidification, while S losses from agricultural soils increase the risk of future S deficiency in S-demanding crops.
    Full-text · Article · Oct 2013 · Science of The Total Environment

Publication Stats

2k Citations
189.78 Total Impact Points

Institutions

  • 2015
    • Czech University of Life Sciences Prague
      • Faculty of Forestry and Wood Sciences
      Praha, Praha, Czech Republic
    • Institute of Hydrobiology CAS
      Budejovice, Jihočeský, Czech Republic
  • 1993-2015
    • Academy of Sciences of the Czech Republic
      • Institute of Hydrobiology
      Praha, Praha, Czech Republic
  • 2013-2014
    • Biology Centre of the ASCR
      • Institute of Hydrobiology
      Praha, Praha, Czech Republic
  • 1996-2012
    • University of South Bohemia in České Budějovice
      • • Faculty of Science
      • • Department of Ecosystem Biology (KBE)
      Budejovice, Jihočeský, Czech Republic
    • Nemocnice České Budějovice
      Budejovice, Jihočeský, Czech Republic
  • 2006
    • Institute of Technology and Business in České Budějovice
      Budejovice, Jihočeský, Czech Republic
  • 2002
    • University of Sistan and Baluchestan
      Dowzdāb, Sīstān va Balūchestān, Iran
  • 2001
    • Charles University in Prague
      Praha, Praha, Czech Republic