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Brazilian Journal of Biology

Print version ISSN 1519-6984On-line version ISSN 1678-4375

Braz. J. Biol. vol.63 no.2 São Carlos May 2003

http://dx.doi.org/10.1590/S1519-69842003000200004 

The effect of particle size on the leaching of Scirpus cubensis Poepp & Kunth

 

O efeito do tamanho de partícula na lixiviação de Scirpus cubensis Poepp & Kunth

 

 

Bianchini Jr., I.I,II; Antonio, R. M.II

IDepartamento de Hidrobiologia, Universidade Federal de São Carlos, Via Washington Luís, km 235, CEP 13565-905, C.P. 676, São Carlos, SP, Brazil
IIPrograma de Pós-graduação em Ecologia e Recursos Naturais, Universidade Federal de São Carlos, Via Washington Luís, km 235, CEP 13565-905, C.P. 676, São Carlos, SP, Brazil

Correspondence

 

 


ABSTRACT

An investigation was made on the effects of detritus particle size on leaching rates in organic matter, and the associated environmental changes caused by detritus re-cycling in an oxbow lake (Lagoa do Infernão). Experiments were conducted during the decay of an aquatic macrophyte specie, S. cubensis, which in turn led to the formation of colored compounds. The S. cubensis were collected from the Lagoa do Infernão and taken to the laboratory where they were washed, dried, and fractionated using a sieve pedological set. The detritus was classified into six groups according to size, viz. 100, 10, 1.13, 0.78, 0.61, and 0.25 mm. Overall, the fragmentation process tended to increase the detritus fraction to be dissolved and to decrease the leaching rates owing to the possible dissolution of refracting matter. Fragmentation also caused the amount of colored compounds to increase and appeared to favor dissolved electrolyte release. Finally, in Lagoa do Infernão fragmentation is probably mediated by the metabolic action of benthic communities.

Key words: leaching, detritus, coloured compounds, kinetic, aquatic macrophyte.


RESUMO

Foram realizados estudos a fim de verificar os efeitos do tamanho de partícula dos fragmentos nos coeficientes de lixiviação da matéria orgânica e as mudanças, associadas ao ambiente, causadas pela ciclagem de detritos em uma lagoa marginal (lagoa do Infernão). Os experimentos foram desenvolvidos durante a decomposição de uma espécie de macrófita aquática, Scirpus cubensis, que também gerou compostos coloridos. Os exemplares de S. cubensis foram coletados na lagoa do Infernão e levados ao laboratório, onde foram lavados, secos e fracionados em um conjunto de peneiras pedológicas. Os detritos foram classificados em seis grupos, de acordo com o tamanho: 100, 10, 1,13, 0,78, 0,61 e 0,25 mm. No geral, o processo de fragmentação tendeu a incrementar a fração do detrito a ser dissolvida e diminuir os coeficientes de lixiviação, em razão de possível dissolução da matéria orgânica refratária. A fragmentação também favoreceu a formação de compostos coloridos e a liberação de eletrólitos dissolvidos. Na lagoa do Infernão, a fragmentação, provavelmente, é mediada pela ação metabólica da comunidade bentônica.

Palavras-chave: lixiviado, detrito, compostos coloridos, cinética, macrófita aquática.


 

 

INTRODUCTION

It is now well established that an efficient method for describing aquatic ecosystems consists in conducting field and/or laboratory experiments together with mathematical simulation studies. This is particularly true when experimental results provide essential information for the parameters employed in fitting the data to a given theoretical model. This philosophy is being adopted in an ongoing project aimed at modeling the detritus recycling processes in an oxbow lake. In the present work we shall be concerned with the experimental activities within this project, focusing on the contribution from aquatic macrophytes to organic matter detritus in an oxbow lake. It is expected that such a contribution could significantly alter the physical, chemical, and biological characteristics of the water and sediments. It can also affect the functioning of other processes in the ecosystem such as primary and secondary productions. For an oxbow lake the hydrological regime is constituted of periodical pulses and may be an important factor in a number of processes in the ecosystem, including the detritus dynamics of vegetal communities (Albuquerque, 1992; Ballester, 1994; Howard-Williams et al., 1989; Nogueira, 1989; Santos & Mozeto, 1992). For example, in Amazonian "várzea" lakes approximately 90 percent of the vegetation may die when the water level drops during the dry season (Junk, 1980).

Degradation of detritus may alter the ecosystems by several means: 1) release of organic compounds and nutrients; 2) formation and accumulation of dissolved humic compounds; 3) increase in dissolved oxygen demand; and 4) accumulation of particulate detritus in the sediments. The simplest way to monitor changes in organic resources due to degradation is by measuring their mass loss (Swift et al., 1979). Detailed analyses show that in addition to mass loss, changes also occur in the chemical composition of the remaining matter. These alterations are caused by three distinct processes: leaching, catabolism, and fragmentation (Swift et al., 1979).

Leaching is the abiotic process whereby soluble matter is removed from a resource through the action of water. It therefore causes both weight loss and changes in the original chemical composition of the detritus. In the ecosystem, leaching may promote transference of soluble compounds from one place to another, where they may suffer further decomposition (Swift et al., 1979). Catabolism is a biochemical process in which complex organic compounds are transformed into smaller and simpler organic and inorganic molecules. Over a limited given period catabolism may be incomplete, thus generating intermediate or re-synthesized compounds such as humic ones (Bianchini Jr. et al., 1984; Stevenson, 1982; Thurman, 1985; Toledo, 1973; Wetzel, 1983). In the fragmentation process, detritus particle size is reduced. Fragmentation differs from catabolism because of its physical nature, even though in some cases it may be associated with decomposer feeding activity. In this case, during digestion fragmentation may be accompanied by catabolic changes. The remaining matter is eliminated in the form of small particles whose chemical composition differs from that of the ingested food material (Swift et al., 1979). Detritus fragmentation may also occur due to climatic changes and the turbulent action of water and wind (Lush & Hynes, 1973).

In practice, these three processes act simultaneously on a given organic resource and may be very difficult to distinguish. The essays carried out here were specifically designed for investigating fragmentation effects on the decay processes of an aquatic plant species (Scirpus cubensis) dominant in an oxbow lake in the Mogi-Guaçu River (São Paulo State, Brazil). The study comprises the following steps: 1) accompanying the destination of some detritus fractions by analyzing the remaining material; 2) describing a kinetics model that accounts for the detrital biomass flow during the leaching process; 3) describing the leaching rates as a function of the initial size of the detritus particles; and 4) discussing possible effects of the leaching process on the recycling dynamics of detrital organic matter in the Lagoa do Infernão.

 

MATERIALS AND METHODS

Experimental procedures

Samples of Scirpus cubensis Poepp & Kunth were collected from an oxbow lake named Lagoa do Infernão (21º35'S and 47º51'W), located in the Jataí Ecological Station (São Paulo State, Brazil). The lake is located in the laboratory, the aquatic macrophytes were selected, washed with tap water, and dried at 60ºC to a constant weight. They were then ground and the fragments further fractionated using a pedological sieve set. This procedure resulted in 6 groups of particle sizes, as shown in Table 1. For each group, 10 bottles were filled with 80 ml distilled water and 2 g aquatic macrophyte fragments. The bottles were shaken at given periods. The particulate organic matter (POM) was separated from the dissolved matter (DOM), using filter paper, at the following times: 0, 0.5, 1.4, 2.5, 3.4, 4.7, 5.7, 7.7, 8.6, 9.9, and 11.4 days. The POM and DOM amounts were measured using the gravimetric method, for which the particulate detritus and the leachate were dehydrated at 60ºC. The use of distilled water rather than water from Lagoa do Infernão was to avoid conditions favorable to leachate consumption. Using distilled water and under anaerobic conditions, aeration and microorganism occurrences were minimized. Consequently, the DOM mineralization rates were low which made it easier to apply the kinetics model of Levenspiel (1986), as discussed in the next section.

 

 

Prior to DOM quantification, its pH, electrical conductivity, and optical density were measured. The pH was obtained using the potentiometric method, and optical density was measured with a photocolorimeter (at 430 nm). Before the optical density measurement, the filtrate volume was completed to 100 ml.

Theoretical model

Considering that organic resources decay processes follow a first-order kinetics (Brezonik, 1994; Jfrgensen, 1986; Mindermann, 1968), the decomposition may be simplisticly described according to the following equations:

1) POM decay (leaching and mineralization processes)

where:

CPOM1 = change per unit of time in the amount of POM fractions associated with protoplasmic portions and other soluble compounds;
CPOM2 = change per unit of time in the amount of POM refracted portions (e.g., cellulose, lignin);
k1 = Leaching constant rate (day-1);
k3 = oxidation (mineralization) constant rate (day-1).

2) Formation of DOM and mineralization

where:

CDOM = change per unit of time in DOM concentration;
k2 = mineralization constant rate (formation of inorganic substances, CO2, and other gases), day-1.

3) Formation of gases and inorganic substances (mineralization of POM refracting fractions)

where:

CCO2 = amount per unit of time of inorganic substances, CO2, and other gases.

 

RESULTS AND DISCUSSION

Time dependence of POM and DOM amounts is illustrated in Table 2. It may be concluded that the gravimetric method was not sufficiently sensitive for investigating the small changes in the biomass of the particulate detritus (POM).

 

 

This methodological incapacity is probably associated with the adherence of microorganisms during the decay and filtration processes.

The method was nevertheless sufficiently accurate for describing the leaching process based on DOM concentration estimates.

The leaching rate was evaluated by fitting the experimental data to the kinetic model of monomolecular irreversible reactions (Levenspiel, 1986), which derives from the analytical integration of Equation 2. As already mentioned in the last section, the experimental conditions employed resulted in relatively low values of DOM mineralization rates, ideally suited for the application of Levenspiel's model.

where:

POM1 = total amount of leached matter from the detritus.

It was assumed that k2 (DOM mineralization rate) was the same for all bottles since they were stored under identical conditions and, therefore, all DOM fractions should have the same rates. Based on this assumption, the leaching rate, k1, was obtained from the fitting procedure.

The Fig. 1 shows the time dependence of DOM amounts (formation and consumption) and also includes the theoretical curves obtained from the kinetics model of Equation 4. The coefficients arising from the fitting procedure are listed in Table 3. It may be observed that for Scirpus cubensis the quantity of material available for leaching is relatively low (from 5 to 8 percent) when compared to the values presented by Bianchini Jr. (1982) for the species: Nymphoides indica, Nymphaea ampla, Ludwigia sp., Poligonum sp., Pontederia cordata, Pontederia lanceolata, Mayaca sellowianna, Rinchospora gigantea, and Eleocharis mutata. In these species, the amount of leachate material varied from 16 to 47 percent. It must be considered, however, that in the present work all particulate material (detritus + microorganisms) was accounted for, whereas in the Bianchini study (1982) the litter bags method was employed in which only the fractions remaining following filtering (with a given mesh) are quantified. It can also be noted that the mechanical fragmentation process tended to increase somewhat the amount of material to be dissolved (POM1). This process, however, caused a decrease in the leaching rate, especially for fragments smaller than 1.13 mm (groups IV, V, and VI). These two effects probably appeared because fractions of refracting matter became soluble. Even though changes could be measured in the dissolution rates and the quantities of material to be dissolved, these changes were small compared to the changes imposed in the initial stages of the experiments.

 

 

 

 

As can be seen in Fig. 2, for the smaller detritus particles (groups III, IV, V, and VI) degradation caused no significant changes in pH. For the other groups (I and II) the pH approached neutrality as time elapsed. From these results it may be inferred that the a priori fragmentation of detritus, which increased its specific area, favored oxidative processes (formation of humic compounds and CO2). This is due to the following factors: i) possible chemical reaction occurrences; ii) access of microorganisms and exoenzimes to unprotected structural elements, such as the matrix which consisted of lignin and cellulose.

 

 

Time dependence of the electrical conductivity is shown in Fig. 3. It may be seen that fragmentation slightly increased the electrolyte amount released, as occurred for DOM. However, electrolyte incorporation (microbial uptake) appears to have been inhibited in the flasks containing the smallest detritus, probably due to the formation of humic compounds that may have been chelated to the electrolytes, thus preventing them from being incorporated. The results shown in Fig. 3 also suggest that the kinetics of the electrolyte material are similar to that of organic compounds. But electrolyte disappearance would be associated with the uptake and adsorption processes, while DOM decay would be associated with mineralization. It was not possible, however, to apply the kinetics model of Equation 4 to the electrolyte results because of the dispersion in the experimental results, probably caused by the high rates of re-cycling of these elements.

 

 

The results of the formation of colored compounds are shown in Fig. 4. In order to investigate the effects of the initial detritus size, optical density changes up to the 3rd day of experiments were adjusted to the first order kinetics model of Equation 5 (Jfrgensen, 1986; Thormann & Müeller, 1987). Restricting data use to that of the first 3 days was based on the assumption that after this period the formation of colored compounds should come mainly from DOM humification rather than from leaching.

 

 

From the fitting procedure, it may be concluded that fragmentation increased both the quantity (ODMAX) and the rate of appearance of colored compounds (k). Basically, the leachate becomes colored due to two interdependent processes: pigment release and humic compound formation (Bianchini Jr., 1985). The latter compounds originate from chemical reactions in the leachate and from products re-synthesized by microorganisms.

When data obtained after the 3rd day of experiments are considered, it is seen that the smaller leached fragments have stronger color if compared to the fragments from group I (10 cm). One may also infer that the trend towards the leaching of compounds prone to humification was already present even for relatively large fragments (of the order of 1 cm). Such compounds should include polyphenolics, carbohydrates, and amine-based compounds (Bianchini Jr. et al., 1984; Bianchini Jr. & Toledo, 1988; Sieburth & Jensen, 1968, 1969; Wetzel, 1983). Indeed, these results corroborate the above-mentioned assumptions that formation of humic compounds is favored by fragmentation.

The effects of particle size are summarized in Fig. 5. It must be noted that the POM1 yield increases with increasing ODMAX yield for, as shown in Fig. 5a. These results show that the mechanical fragmentation process increases the soluble detritus amount, which then enhances the rate and yield of formation of colored compounds.

 

 

On the other hand, these phenomena cause the leaching rates to decrease, probably because microorganisms have access to refracting matter (Fig. 5b). With regard to the cycling of detritus in naturally occurring aquatic systems, it is likely that the fragmentation process is mostly associated with the amount, rather than with the leaching rates, of compounds (organic and inorganic) released into the water. This process is probably even more important in qualitative modifications of particulate detritus, by inducing the formation of humic compounds and other catabolic processes involved in biological oxidations. In this context, the importance of benthic communities and other decomposers may be emphasized, for comminuition (mechanical fragmentation + digestion) can significantly enhance the degrading processes of organic resources, as in the case of the role played by insects in the terrestrial ecosystem. For the Lagoa do Infernão, in particular, ongoing studies show that the benthic community is practically nonexistent probably because of the low dissolved oxygen amounts in the sediment layer. Invertebrates typical of this community can be found, however, in the rizosphere of S. cubensis (Strixino et al., pers. com.).

 

CONCLUSIONS

Under the experimental conditions employed in the present work, one may conclude that for the Scirpus cubensis, the fragmentation process: 1) tended to increase the detritus fraction to be dissolved (POM1) and to decrease the leaching rates (k1), owing to the possible dissolution of refracting matter; 2) favored the rates of formation and increased the amount of colored compounds, probably by increasing the quantity of polyphenolics and other structural compounds (such as polysaccharides and amine-based compounds); 3) appeared to have favored the release of dissolved electrolytes; and 4) retained the acidity of the bottles.

Acknowledgments – The authors thank Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) for financing these essays (Process n. 91/1303-3) and Dr. Osvaldo N. Oliveira Jr. (IFSC-USP) for proofreading the manuscript.

 

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Correspondence to
Irineu Bianchini Jr.
Departamento de Hidrobiologia, Universidade Federal de São Carlos
Via Washington Luís, km 235
CEP 13565-905, C.P. 676, São Carlos, SP, Brazil
E-mail: irineu@power.ufscar.br

Received March 5, 2002 - Accepted August 27, 2002 - Distributed May 31, 2003

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