Raquel
Vasconcelos Ferreira
*a,
Mário
Azevedo Cerqueira
a,
Maria Teresa
Condesso de Melo
b,
Daniela
Rebelo de Figueiredo
c and
Jan Jacob
Keizer
a
aCESAM – Centre for Environmental and Marine Studies, Department of Environment and Planning, University of Aveiro, Campus de Santiago, 3810-193, Aveiro, Portugal. E-mail: raquelferreira@ua.pt; cerqueira@ua.pt; jjkeizer@ua.pt; Fax: +00351 234 370 309; Tel: +00351 234 340 349
bCVRM/Geo-Systems Centre - Instituto Superior Técnico, Av. Rovisco Pais, 1049-001, Lisboa, Portugal. E-mail: tmelo@ua.pt; Fax: +00351 21 841 74 42; Tel: +00351 21 841 72 47
cCESAM – Centre for Environmental and Marine Studies, Department of Biology, University of Aveiro, Campus de Santiago, 3810-193, Aveiro, Portugal. E-mail: dfigueiredo@ua.pt; Fax: +00351 234 372 587; Tel: +00351 234 370 350
First published on 30th September 2009
The Cértima River is the principal source of water flowing into the Pateira de Fermentelos, which is one of the largest natural lakes of the Iberian Peninsula and has elevated conservation value. This study aims at a more comprehensive understanding of the spatial pattern in water quality and, thus, pollution problems in and especially upstream of the Pateira, including a comparison with a prior study in 2003. To this end, surface water samples were collected, in May 2007, at 29 sites covering the basin's four main types of water bodies, and analysed for electrical conductivity, dissolved oxygen, biochemical oxygen demand, total suspended solids, various nitrogen species, orthophosphate and chlorophyll a. The results confirmed the existence of marked pollution along the middle section of the Cértima's main course, which can be attributed to wastewater discharges of urban and animal husbandry origin in particular. This represents an important eutrophication risk to the Pateira. Current legislation and water management does not appear to tackle this risk in an entirely satisfactory manner, since the spatial patterns as well as actual values of key physic-chemical parameters do not appear to have changed markedly between 2003 and 2007. Amongst the various parameters, biochemical oxygen demand stands out for frequently exceeding the legal water quality standards. The type of water body proved helpful to explain part of the variation in some of the parameters. This includes clear differences in electrical conductivity between the right- and left-bank tributaries, illustrating well the heterogeneous and complex character of the Cértima basin.
Environmental impactThis study is both a follow-up and an extension of a surface water quality assessment carried out in 2003 in a Mediterranean-type basin in Portugal. It confirms the continued presence, in 2007, of marked pollution along the river's main course, especially due to pollution by urban and agro-industrial point sources at one specific urban centre. Apparently, the improvements of the public wastewater networks between 2003 and 2007 have produced no major changes in water quality and, thus, in eutrophication risk of one of the Iberian Peninsula's largest natural lakes. The densification of the 2003 sampling network has provided new insight into the importance of the catchment's four types of water bodies and, thereby, of the associated physical-environmental and land-cover/use settings. |
The present study concerns the Cértima River basin in central Portugal (Fig. 1). In addition to the conservational importance of its lake and surroundings wetlands, it is a typical example of a complex, spatially heterogeneous catchment with distinct agricultural and forestry land uses as well as pollution pressures from urban areas, cattle raising activities and various types of industrial activities, with emphasis on the ceramics and wine-growing sectors.7 It also provides clear examples of advanced degradation of aquatic habitats, especially in the case of the main course of the Cértima River where pollution problems has been documented for several decades.8–10
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Fig. 1 Location and map of the Cértima River basin. The numbers and names of the 29 sampling sites are as follows, with the numbers in italic indicating the sites of the prior study in 20037: 1, Santa Cristina; 2 (1), Póvoa do Loureiro; 3 (2), Viadores; 4, Pereiras; 5 (3), Lagoa Seca; 6, Várzeas; 7, Barrô; 8, Ponte dos Carros; 9, Curia; 10, Várzea; 11, Parada; 12, Algeriz; 13 (4), Famalicão; 14 (5), Malaposta; 15, Avelãs de Cima; 16 (6), São João da Azenha; 17, Pisão da Forcada; 18 (7), Landiosa; 19 (8), Repolão; 20, Levira; 21, Paraimo; 22, Amoreira do Repolão; 23 (10), Perrães; 24, Fermentelos (lake shore); 25, Óis da Ribeira (lake shore); 26, Lake – North; 27, Mamodeiro; 28, Lake – São Paio and 29, Requeixo. |
The Cértima River basin is a medium-sized catchment with a shallow, natural lake at its final section. This “Pateira de Fermentelos” lake is one of the largest natural freshwater lakes of the Iberian Peninsula (approximately 5.3 km2) and, together with the surrounding lands, constitutes one of Portugal's principal wetland areas.11 Whilst subject to severe pressures from anthropogenic activities, the Pateira de Fermentelos is protected under Portuguese legislation as an integral part of the so-called Special Protection Area of the Ria de Aveiro coastal lagoon (ref. 12, which establishes the conservation regime of several special protection areas). The Pateira also has a special legal status as a sensitive area with respect to discharges of urban wastewater (ref. 13, which transposes the Urban Wastewater Treatment Directive).14
The first catchment-wide, quantitative assessment of surface water quality in the Cértima River basin was carried out in 2003.7 Focusing mainly on the river's main course, it revealed significant nutrient load as well as high biochemical oxygen demand values, in particular at Lagoa Seca (site 5) just downstream of the town of Mealhada. At this site, pollution levels were much more pronounced during the July sampling period than the preceding March and May periods. More recently, Manecas15 reported contamination of heavy metals in bottom sediments of the Cértima River (at Anadia) and Sena16 observed eutrophication problems in Pateira de Fermentelos that she attributed to upstream river water quality. In general, the Pateira de Fermentelos has received much more research attention than the rest of the Cértima basin, pointing out to a eutrophic to hypereutrophic lake.17–21 Even in the case of the Pateira, however, there has been no regular monitoring of its ecological and chemical status as is required for an adequate implementation of the European Union's Water Framework Directive.22
The present research is intended as a follow-up of the above-mentioned study carried out in 2003. It aims to expand the prior catchment-wide water quality assessment or, in other words, at furthering the knowledge and understanding of the spatial patterns in selected physic-chemical parameters. In addition, a biological parameter - chlorophyll a - is included as a first step towards a more integrated approach. A key element in the assessment is the comparison of the obtained results with the Portuguese legal water quality standards (ref. 23, which transposes the corresponding European Directive on this matter).
The surface water quality parameters studied here are: electrical conductivity (EC), dissolved oxygen (DO), biochemical oxygen demand (BOD), suspended solids (TSS), phosphorus (PO4–P) and various nitrogen forms (NH4–N, NO3–N, Org–N), and chlorophyll a (Chl a). EC reflects the status of inorganic pollution, and measures the total dissolved solids and ionised forms. DO represents the quantity of oxygen that is present in the water and is essential for almost all aquatic life forms. BOD estimates the degree of organic pollution. High levels of suspended solids can increase BOD and lead to depletion of DO levels. Excessive nitrogen and phosphorus levels result in eutrophication, causing proliferation of algal masses that can induce a deficit of dissolved oxygen. Chl a provides a measure of algal abundance that is often used to quantify algal blooms caused by eutrophication.5
For logistic reasons, the larger number of sites and parameters studied here had to be off-set against sampling frequency, i.e. here at a single occasion as opposed to the three occasions of the 2003 study.7 Arguably, pollution levels can be expected to be worse during summer than spring. The 2003 data clearly show this for the heavily polluted Lagoa Seca (site 5) but less clearly for the other sites. The summer-2003 values were significantly higher than the spring-2003 values for two of the seven parameters (EC and Org–N; Wilcoxon signed rank test; p < 0.05). At the same time, however, the summer- and spring-2003 values of these two parameters (plus BOD, NH4–N, TSS and DO) were strongly and significantly correlated (Spearman rank correlation coefficients; range: 0.70–0.88; p < 0.05). May was finally selected as a sampling period for this study, since the Cértima headwaters tend to become dry during the summer season.
The Cértima catchment is characterized by distinct topographic, climatic, geologic, and hydrologic settings that are reflected in its rather heterogeneous land-use patterns. The climate is Mediterranean-type, although with oceanic influences. Summers are warm and dry, whereas winters are mild and wet. During dry years, the upper stretch of the Cértima river, along the Mealhada municipality, has very low flows and even falls dry. The middle stretch has symmetrical and sheer down banks, bottom sediments consisting of fine sands and abundant aquatic vegetation. The flow rates in this section increase markedly due to the contribution of several tributaries draining the eastern, forested hillslopes (right-bank tributaries). The plains of the lower part of the basin, roughly up to the municipality of Oliveira do Bairro, are subject to flood risk, especially when intense winter rain events coincide with high tides (reflecting the connectivity with the Ria de Aveiro costal lagoon).
The geology comprises Ordovician schists in the eastern, upper part of the catchment, and modern-age alluvial sands and clays in its western, middle and lower parts. The land cover consists predominantly of Pinus pinaster and Eucalyptus globulus forests (48%), located in the upper part, and agricultural lands (44%; of which 27% are vineyards); the urban areas amount to 7% of the territory.25 The major urban centers (Mealhada, Anadia, Oliveira do Bairro) are located close to the main course of the Cértima River. The total resident population is about 85 000 inhabitants, with an average population density of 160 inhabitants per km2.26 In 2005, about 97% of the resident population were served by the public water supply systems, but only 67% and 64% were connected to the public sewage systems and wastewater treatment plants, respectively.27
Ten water quality parameters were selected for this study: electrical conductivity (EC); dissolved oxygen (DO); biochemical oxygen demand (BOD); total suspended solids (TSS); total Kjeldahl nitrogen (TKN); ammonium (NH4–N); chlorophyll a (Chl a); dissolved orthophosphate (PO4–P); dissolved nitrite (NO2–N); dissolved nitrate (NO3–N). EC and DO were measured in the field using a pre-calibrated portable meter (HANNA® Instruments). Samples for the laboratory analysis of the remaining eight parameters were collected manually by direct immersion of the containers beneath the water surface to a depth of about 20 cm. All the containers used to store the samples were pre-rinsed with hydrochloric acid (pH < 2.0), distilled and deionised water, and, immediately before sampling, with water from the selected location. All samples were then stored and transported in thermal boxes to the laboratory. Water samples for BOD and TSS analysis were collected in 1.5 L polyethylene containers and processed within 6 h after collection. For Chl a determinations, samples were collected using 1 L plastic bottles that were then stored under dark and cold conditions. For TKN and NH4–N analysis, water samples were collected into 500 mL glass containers (without any filtration step), preserved by addition of sulfuric acid (pH < 2.0), and stored in the dark at a temperature of 4 °C. Water samples of about 60 mL for PO4–P, NO2–N and NO3–N determinations were immediately filtered through a 0.45 µm pore size Milipore® HA membrane filter, stored and shipped in high density polyethylene containers for later analysis by ion chromatography, at the Activation Laboratories Ltd. (ACTLABS, Ontario, Canada). All other water quality parameters were determined at the University of Aveiro following the standard analytical methods for water quality as described in ref. 28. BOD was determined after incubation of the samples for 5 days in the dark at 20 °C, and measurement of the oxygen consumption. TSS was quantified gravimetrically after filtration of an adequate volume through a glass fibre filter and following drying to a constant weight at 105 °C. Chl a concentrations were determined by spectrophotometry (trichromatic method) after filtration and extraction in 90% acetone. TKN was determined by the Kjeldahl method (with digestion and distillation of the samples), and followed by the analysis of NH4–N by the colorimetric indophenol blue method. Subsequently, organic nitrogen (Org–N) was computed by subtraction of the NH4–N from the TKN values. The quality of laboratory data obtained at the University of Aveiro was guaranteed through the implementation of laboratory quality assurance and quality control methods, including the use of standard operation procedures, calibration with standards, analysis of blanks, recovery of known additions and analysis of replicates.
Parameter/Units | Mean | Median | Stand. dev. | Min. | Max. |
---|---|---|---|---|---|
EC/µS cm −1 | 386 | 441 | 202 | 71 | 690 |
DO/% | 94 | 92 | 21 | 58 | 165 |
BOD/mg L −1 | 3.6 | 2.2 | 3.6 | 0.4 | 12.5 |
TSS/mg L −1 | 10.5 | 5.9 | 12.3 | 0.4 | 42.7 |
NO 3 –N/mg N L −1 | 3.0 | 2.2 | 2.6 | 0.2 | 11.3 |
NH 4 –N/mg N L −1 | 0.67 | 0.07 | 1.9 | 0.02 | 10.5 |
Org–N/mg N L −1 | 0.73 | 0.6 | 0.5 | 0.1 | 1.9 |
Chl a/µg L −1 | 11.6 | 4.3 | 15.5 | 2.2 | 70 |
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Fig. 2 Spatial patterns of the measured parameters in the Cértima River basin. Values given in legend reflect the category range (from minimum to maximum values). In the case of biochemical oxygen demand and ammonium, the circles in orange and red indicate values above the Portuguese legal water quality standards. |
Moderately high concentrations of Chl a, exceeding 10 µg L−1, were found at two sites along the middle section of the Cértima river, i.e. Malaposta (site 14) and São João da Azenha (site 16). This could well be related to the upstream discharges in the Mealhada urban area, in combination with local conditions propitious to phytoplankton development.
Test statistics | Water quality parameters | |||||||||
---|---|---|---|---|---|---|---|---|---|---|
EC/ µS cm−1 | DO/ % | BOD/ mg L−1 | TSS/ mg L−1 | NH4–N/ mg N L−1 | Org–N/ mg N L−1 | NO3–N/ mg N L−1 | NO2–N/ mg N L−1 | PO4–P/ mg P L−1 | Chl a/ µg L−1 | |
a ns: non significant. | ||||||||||
runs | 3 | 2 | 2 | 4 | 4 | 4 | 2 | — | 3 | 3 |
n | 5 | 5 | 5 | 5 | 5 | 5 | 5 | 0 | 3 | 5 |
significance | ns | ns | ns | ns | ns | ns | ns | ns | ns | ns |
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Fig. 3 Spatial patterns along the Cértima's main course between Lagoa Seca (site 5) and Perrães (site 23), before Pateira de Fermentelos, of nine of the ten measured parameters. |
r | EC | BOD | TSS | NH4–N | Org–N | NO3–N | NO2–N | PO4–P | Chl a | DO |
---|---|---|---|---|---|---|---|---|---|---|
EC | 1 | 0.78 | 0.68 | 0.54 | 0.66 | 0.77 | 0.16 | 0.06 | 0.31 | −0.13 |
BOD | 1 | 0.84 | 0.59 | 0.86 | 0.62 | 0.13 | 0.03 | 0.34 | −0.03 | |
TSS | 1 | 0.42 | 0.81 | 0.45 | 0.16 | −0.20 | 0.43 | −0.09 | ||
NH4–N | 1 | 0.45 | 0.48 | −0.10 | 0.37 | −0.07 | −0.06 | |||
Org–N | 1 | 0.56 | 0.19 | 0.08 | 0.25 | 0.04 | ||||
NO3–N | 1 | 0.12 | −0.01 | −0.05 | −0.31 | |||||
NO2–N | 1 | −0.16 | 0.17 | −0.14 | ||||||
PO4–P | 1 | −0.35 | 0.02 | |||||||
Chl a | 1 | 0.26 | ||||||||
DO | 1 |
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Fig. 4 Relationship of BOD with TSS as well as Org–N that correspond to the highest Spearman rank correlation coefficients in Table 3. |
The frequent significant relationships may indicate that the underlying pollution patterns in the Cértima River basin are rather straightforward, with the Mealhada urban area playing a predominant role as source area. The alternative explanation of strong parameter interactions does not seem to apply in the case of neither the various nitrogen species nor the two oxygen-related parameters. In the case of NO2–N and PO4–P, the lack of significant relationships is easily explained by the fact that the bulk of the values are not above the detection limits of the employed methods.
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Fig. 5 Box-and-whiskers plots of electrical conductivity, biochemical oxygen demand, total suspended solids, ammonium, organic nitrogen, nitrate, chlorophyll a and dissolved oxygen, for the four types of water-bodies in the Cértima River basin. |
All of the eight parameters except DO reveal an overall contrast among the four types of water bodies that is statistically significant, indicating that type of water body can help explain the observed differences in these parameters' concentrations (Table 4). The subsequent multiple comparison tests show that between three and five of the six pair-wise comparisons correspond to statistically significant differences (Table 5). BOD and TSS involve the same statistical differences, i.e. a contrast between the higher values of the Pateira and the main river course, on the one hand, and, on the other, the lower values of the tributaries. This indicates that pollution in the Cértima River basin is predominantly a matter of point sources closely associated to the Cértima main course in particular, as opposed to diffuse sources due to agricultural and forestry land practices.
Test statistics | Water quality parameters | |||||||
---|---|---|---|---|---|---|---|---|
EC | DO | BOD | TSS | NH4–N | Org–N | NO3–N | Chl a | |
H | 19.47 | 5.66 | 17.41 | 15.38 | 9.34 | 17.91 | 9.34 | 9.85 |
(<0.001) | (0.13) | (0.001) | (0.002) | (0.025) | (0.001) | (<0.001) | (0.020) |
Water type groups: pair wise comparisons | Observed difference in multiple comparisons between water type groups | ||||||
---|---|---|---|---|---|---|---|
EC | BOD | TSS | NH4–N | Org–N | NO3–N | Chl a | |
1 vs. 2 | 0.52 | −3.56 | −2.54 | 2.89 | −1.63 | 1.87 | 0.28 |
1 vs. 3 | 5.45 | 9.87 | 9.09 | −6.74 | 11.20 | −0.33 | 4.76 |
1 vs. 4 | −4.77 | 4.82 | 4.96 | −9.33 | 4.16 | 4.51 | 5.97 |
2 vs. 3 | 12.29 | 7.73 | 5.29 | 3.59 | 7.29 | 8.22 | −3.34 |
2 vs. 4 | 1.97 | 2.56 | 1.02 | 3.40 | 0.13 | −2.72 | −2.30 |
3 vs. 4 | 4.74 | −1.23 | −2.85 | −6.16 | 0.94 | 10.78 | −4.83 |
The other parameters all involve distinct patterns of pair-wise significant differences. A straightforward pattern is that of Chl a, with the values of the Pateira being significantly higher than those of Cértima River's main course and its tributaries. This difference can be attributed to the much longer residence time of surface water in the lake, and points to the elevated eutrophication risk of the Pateira.33 A more complex pattern is that of EC, in which case only the values of the Pateira and of the left-bank tributaries do not differ significantly. The differences probably reflect the different lithological formations, ranging from schists in the case of the right-bank tributaries to Cretaceous sedimentary formations in the case of the left-bank tributaries and the Pateira.
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Fig. 6 Relationships between the May-20037 and May-2007 values of electrical conductivity, biochemical oxygen demand, total suspended solids, ammonium and organic nitrogen, dissolved oxygen and phosphorous forms, at nine sampling point in the Cértima River basin. |
The visibly higher 2007 values for BOD, NH4–N, Org–N and PO4–P were observed at Lagoa Seca (site 5). These differences can be caused by a stronger impact of the pollution sources upstream this site. Five of the six parameters reveal a strong agreement of the values of May 2007 with those of May 2003, with Spearman rank correlation coefficients ranging from 0.65 to 1.00 (Table 6). In four instances, this corresponds to a statistically significant monotonic relationship. Apparently, the spatial pattern underlying the variability in BOD, NH4–N, Org–N and possibly also DO along the main course of the Cértima river has remained unaltered over the 4-year period from 2003 to 2007 and, thus, has not been changed markedly by the extension of the sewage and wastewater treatment systems that was carried out since 2003.
Test statistics | Water quality parameters | |||||
---|---|---|---|---|---|---|
EC | DO | BOD | TSS | NH4–N | Org–N | |
r | 1.00 | 0.65 | 0.73 | −0.07 | 0.81 | 0.69 |
(<0.001) | (0.058) | (0.025) | (0.86) | (0.008) | (0.041) |
In the case of EC, BOD, NH4–N and Org–N, the consistency in spatial patterns coincides with statistically significant differences in local parameter values (Table 7). All these four parameters involve higher values in May 2007 than in 2003 (Fig. 7), whereas also DO reveals some tendency for higher 2007 than 2003 values. In two instances, those of BOD and Org–N, the 2007 values are significantly higher than the 2003 values not only at the level of the individual sampling points but also on overall terms (Table 8).
Test statistics | Water quality parameters | |||||
---|---|---|---|---|---|---|
EC | DO | BOD | TSS | NH4–N | Org–N | |
Z | 2.31 | 1.48 | 2.55 | 0.18 | 2.67 | 2.67 |
(0.021) | (0.14) | (0.011) | (0.86) | (0.008) | (0.008) |
Test statistics | Water quality parameters | |||||
---|---|---|---|---|---|---|
EC | DO | BOD | TSS | NH4–N | Org–N | |
U | 25 | 31 | 18 | 37.5 | 20 | 14 |
(0.17) | (0.40) | (0.047) | (0.79) | (0.070) | (0.019) |
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Fig. 7 Box-and-whiskers plots of the May-20037 and May-2007 values, and their differences, of electrical conductivity, biochemical oxygen demand, total suspended solids, ammonium and organic nitrogen, dissolved oxygen and phosphorous forms. |
Thus, the present results clearly suggest that the public works of improving urban wastewater discharges systems have not produced major changes in the spatial polution patterns along the Cértima's main course nor in the actual levels of key physic-chemical parameters like BOD and various N species. This can be due to various factors like failure to reduce nutrient and organic matter influxes from the principal urban and especially non-urban point sources, and mobilization of local nutrient stock that have accumulated on the streambed bottom over the past few decades. Admittedly, however, differences in antecedent weather and hydrometric conditions may interfere in the comparison of the present data with those obtained four years earlier. This is especially true for the actual pollution levels, since the spatial patterns in March, May and July 2003 were in general consistent (10 out of 14 parameter combinations were significantly correlated).
Unfortunately, antecedent rainfall data are only available for May 2007, whereas river discharge data are lacking for both periods.
Trophic state | TN/mg N L−1 | TP/mg P L−1 | Chl a/µg L−1 | |
---|---|---|---|---|
Streams | Oligotrophic | <0.70 | <0.025 | <10 |
Mesotrophic | 0.70–1.50 | 0.025–0.075 | 10–30 | |
Eutrophic | >1.50 | >0.075 | >30 | |
Lakes | Oligotrophic | <0.50 | <0.025 | <8 |
Mesotrophic | 0.50–1.26 | 0.025–0.071 | 8–25 | |
Eutrophic | >1.26 | >0.071 | >25 |
The trophic status of the Cértima water bodies is highly variable, ranging from fully oligotrophic (i.e. with respect to TN as well as Chl a) to fully eutrophic. This variation broadly agrees with the four types of water bodies mentioned earlier. The right- and left-bank tributaries are all oligotrophic with respect to Chl a (range: 2–7 µg L−1) but vary from oligo- to eutrophic with respect to TN (range: 0.4–8 mg N L−1). In the case of the left-bank tributaries, TN values correspond to eutrophic conditions whereas in the case of the right-bank tributaries TN values appear to differ with the size of the upstream population centers. Trophic status is oligotrophic downstream of hamlets (sites 1, 11, 12), mesotrophic following small villages (2, 6, 7, 15), and eutrophic after medium-sized urban areas (sites 3, 4, 13, 17, 18). The main course of the Cértima river upstream of the Pateira is characterised by eutrophic TN conditions (range: 4–24 mg N L−1) in combination with generally oligotrophic Chl a conditions (range: 2–13 µg L−1). Chl a values are mesothropic at two sites along the Cértima's middle stretch (14 and 16), probably due to an abundant aquatic vegetation. In line with previous studies17–21 in the Pateira euthrophic conditions prevail with respect to both parameters (range: 27–70 µg L−1 and 3–4 mg N L−1 for Chl a and TN, respectively). The same is true for the Requeixo site at the Cértima's outlet, reflecting the admixture of water coming from the Pateira.
It is well-established that the trophic status of fresh water bodies may be influenced by a large number of factors, including their physic-environmental settings and the land cover and management practices of the surrounding lands. In the case of the Cértima River basin, it is likely a natural trend of nutrient enrichment exists from the uplands underlain by schists to the lowlands on unconsolidated deposits. However, a massive nutrient input of anthropogenic origin is superimposed on this trend, in particular through wastewater discharges directly into the Cértima's main course. Future plans for improving or even controlling the trophic conditions of the Pateira de Fermentelos will, therefore, have to explicitly address these upstream nutrient influxes (including those from specific point sources) and perhaps also the accumulated nutrient stocks of very heavily polluted river stretches as in Lagoa Seca (site 5). Measures like phosphate stripping at sewage treatment works and sediment trapping by vegetation buffers or mechanical removal of accumulated sediments and/or dense vegetation stands34,35 are examples of interventions that are complementary to those foreseen in the current EU-derived legislation of the EC Urban Wastewater Treatment Directive14 and the EC Nitrates Directive.36
i) the types of water bodies distinguished here are helpful to explain an important part of the variation in water quality within the catchment, reflecting complex interactions with especially geological settings, land cover/use, settlement patterns and water management;
ii) pollution is to a large extent caused by point sources of urban and non-urban wastewater discharges along the Cértima's main course and, in particular, at one of the larger urban centers (Mealhada), contributing significantly to the euthrophication risk of the Pateira de Fermentelos;
iii) in terms of accomplishment of legal water quality standards, biochemical oxygen demand (BOD) clearly is the most critical parameter;
iv) the spatial patterns as well as actual values of six key physic-chemical parameters suggest that the ongoing improvements of the sewage and wastewater networks have had no major impact on surface water quality;
v) besides Chl a, further biological parameters need to be studied to allow an integrated assessment of surface water quality as is also required for the implementation of the European Water Framework Directive.22 To this end, the present study is currently being followed up on by a quantitative characterisation of the benthic macro-invertebrate communities at a selection of the present sampling sites.
Footnotes |
† Part of a themed issue dealing with water and water related issues. |
‡ Electronic supplementary information (ESI) available: Raw data. See DOI: 10.1039/b914409a |
This journal is © The Royal Society of Chemistry 2010 |