Efficiency of a constructed wetland for retention of sediment-associated phosphorus

A constructed wetland (2.1 ha; 2% of catchment area) in southeast Sweden, in a catchment with 35% arable land on clay soils, was investigated with respect to phosphorus (P) retention, focusing on particulate P (PP) and sediment accretion. The aims were to (i) estimate P retention and identify the dominating retention processes; (ii) investigate how well estimates of P retention based on inflow-outflow measurements compared with the amount of P accumulated in the sediment. In- and outflow of P was measured during 4 years with continuous flow measurements and flow-proportional weekly composite samples. P in the accumulated sediment was estimated based on core samples and analyzed using sequential fractionation. Total P load during 4 years was 65 kg ha⁻¹ and intensive sampling events detected 69% as PP. Based on inflow-outflow estimates the mean P retention was 2.8 kg ha⁻¹ year⁻¹, or 17%, but the amount of P accumulated in the inlet zone equated 78% of the TP load. This discrepancy showed the need to add studies of sediment accumulation to inflow-outflow estimates for an improved understanding of the P retention. The dominating P forms in the sediment were organic P (38%) and P associated with iron or aluminum (39%), i.e., potentially mobile forms. In areas colonized by Typha latifolia, the amount of P in the upper sediment layer (390 kg) was more than double the total P load of 136 kg. Cycling and release in those areas is a potential source of P that deserves further attention.     

Drainage history and land use pattern of a Swedish river system — their importance for understanding nitrogen and phosphorus load

During the 19th and the first half of the 20th century, approximately 300 km² of lakes and wetlands, representing 29% of the River Kavlingean catchment in Southern Sweden, were drained to make land available for agriculture. Published accounts of nutrient loads from the catchment indicated that until the mid 20th century, factories and urban point sources were the major contributors of both nitrogen and phosphorus. By the middle of the 20th century, the construction of sewage treatment plants had effectively reduced phosphorus pollution. Concurrently, the land drained in the previous century underwent a more intense cultivation, with productivity being maintained by commercial fertilizers. Subsequently, net nutrient loads from agriculture continued to increase, reaching an annual load of 2652 tons total-nitrogen and 70 tons total-phosphorus for the River Kävlingeån. Whilst high nutrient leakage from agricultural watersheds may be a problem which is only recently recognized, it had its origins in nearly a hundred years of commonly accepted agricultural policy.To assess the importance of agriculture as the major source of nutrients to the River Kävlingeån system, three tributary catchment areas, differing in terms of their land use patterns (high, medium and low intensity of agricultural use), were studied and compared with literature figures. Results indicated that agricultural nutrient loss areal coefficients were substantially higher than the literature figures, demonstrating the role of agriculture as source of nutrients to the River Kävlingeån system. The agricultural land use policies of the last fifty years were revealed to be most important with regard to this role. Of such land use policies, the cultivation of the last 10–15% of land employed for agricultural use (primarily riparian ecotones) may be of most significance. The literature indicates that intense agricultural use of this final 10–15% may account for a ca. 50% increase in nitrogen loss. This suggests that one solution to the problem of agricultural diffuse pollution may lie in the restoration and sustainable management of riparian ecotones of agricultural streams.     

Estimating phosphorus retention of existing and restored coastal wetlands in a tributary watershed of the Laurentian Great Lakes in Michigan,USA

Simulation modeling with uncertainty analysis was applied to the question of nonpoint source pollution control through extensive wetland restoration. The model was applied to the Quanicassee River basin, a tributary stream to Saginaw Bay on Lake Huron in northeastern Michigan, USA. An estimate of the role of the existing 695 ha of riverside and lake-side wetlands in the lower Quanicassee River basin suggests that they retain 1.2 metric tons of phosphorus per year (mt P/yr), or 2.5% of the total phosphorus load from the basin. A simple Vollenweider-type model of phosphorus retention by created wetlands, calibrated with 3-years of data from two wetland sites in Midwestern USA, was used to estimate the effect of major wetland restoration in the basin. For a wetland restoration project involving 15% of the Quanicassee River basin or 3,120 ha of wetlands, an estimated 33 mt P/yr could be retained, assuming a proper hydrologic connection between the wetlands and the river. This would represent a reduction of two-thirds of the existing phosphorus load to the Bay from the Quanicassee River basin. Large-scale wetland restoration appears to be a viable management practice for controlling phosphorus and other nonpoint source pollution from entering Saginaw Bay. It is an alternative that meets two major resource goals – developing wetland habitat and controlling pollution to the Great Lakes.     

Changes of nitrogen and phosphorus loads to European seas

During the last decades human activity has altered the natural cycle of nitrogen and phosphorus on a global scale, producing significant emissions to waters. In Europe, the amount of nutrients discharged from rivers to coastal waters as well as the effects of mitigation measures in place are known only partially, with no consistent temporal and spatial cover. In this study, we quantify the loads and concentration of nitrogen and phosphorus discharged in the European seas over the period 1985–2005, and we discuss their impact on coastal ecosystems. To support our analysis, a catchment database covering the whole of Europe was developed together with data layers of nutrients diffuse and point sources, and the statistical model green was used to estimate the annual loads of nitrogen and phosphorus discharged in all European seas. The results of this study show that during the last 20 years, Europe has discharged 4.1–4.8 Tg yr^?1 of nitrogen and 0.2–0.3 Tg yr^?1 of phosphorus to its coastal waters. We show that beside the North Sea and part of the Baltic Sea, annual nutrient exports have not changed significantly, in spite of the implementation of measures to reduce nutrient sources, and that the N : P ratio has increased steadily, especially in the North, Mediterranean and Atlantic seas. The response of river basins to changes in inputs was not linear, but influenced by climatic variations and nutrients previously accumulated in soils and aquifers. An analysis of the effects of European environmental policies shows that measures to reduce phosphorus were more successful that those tackling nitrogen and that policies aimed at point sources were more effective or more effectively implemented than those controlling pollution from diffuse sources. The increase of the N : P ratio could fuel eutrophication in N‐limited coastal ecosystems, reducing biodiversity and the ecosystem's resilience to future additional anthropogenic stress, such as climate change.     

长兴县合溪水库集雨区苗木地不同施肥管理模式对径流磷素流失的影响

为保护主要饮用水源合溪水库水质,长兴县将合溪水库集雨区农业种植结构向苗木种植方式调整,但缺乏优化施肥管理模式。针对该问题,选取集雨区典型苗木种植地进行径流小区定位试验,设置了撒施(对照)、地膜覆盖、秸秆覆盖、区外设置植草缓冲带、条施、穴施6个处理,研究不同施肥管理模式下苗木地径流磷素流失特征,筛选最优施肥管理模式,实现最大化的削减农田磷素流失。结果表明:不同施肥管理模式下,苗木地地表径流年总磷素径流流失通量大小顺序为:撒施(对照)地膜覆盖条施穴施区外植草缓冲带秸秆覆盖,撒施(对照)、地膜覆盖、条施、穴施、区外设置植草缓冲带和秸秆覆盖六种施肥管理模式下的年总磷素径流流失通量分别为:9.60、9.14、5.49、4.44、2.48、1.37 kg hm-2a-1,说明穴施、区外设置植草缓冲带和秸秆覆盖是较佳的施肥管理模式,若将其优化组合将显著消减合溪水库集雨区苗木地径流磷素流失及其对合溪水库水质的潜在影响。此外,不同施肥管理模式下,苗木地径流水样磷素流失的首要形态均为颗粒态磷,其次为溶解态磷,其中,撒施(对照)、地膜覆盖、秸秆覆盖、区外植草缓冲带、条施和穴施小区径流年均流失的颗粒态磷占流失总磷的比例分别是66.09%、70.69%、67.97%、71.63%、68.11%和67.87%。     

Fish assemblage–environment relationships suggest differential trophic responses to heavy metal contamination

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These are not the trends you are looking for: poorly calibrated single-pass electrofishing data can bias estimates of trends in fish abundance

There is increasing interest in the potential of single-pass and timed electrofishing to assess status and trends in fish populations. However, where capture probability varies over time, there is a risk that uncalibrated electrofishing data could fail to detect, or provide biased estimates of trends. This study analysed a long-term electrofishing dataset collected over 50 years in an intensively studied catchment where egg deposition and emigrant production declined by c. 82% and 35% over the same time. The electrofishing data were used to illustrate the effects of changing capture probability on estimated trends in juvenile Atlantic salmon Salmo salar abundance. Temporal variability in capture probability was modelled. Trends in abundance were then estimated from uncalibrated single-pass electrofishing count data and compared with estimates from data calibrated for capture probability. The calibrated data revealed significant declines in S. salar fry (age 0) and parr (age ≥ 1) abundance. However, the trend estimates from the uncalibrated data were positively biased and not significant. Exploration of alternative (realistic) scenarios with different trends in true abundance and capture probability suggests that uncalibrated electrofishing data can provide very misleading estimates of trends. The problem is exacerbated in data where capture probability is low. It is recommended that single-pass and timed electrofishing methods should not be used to assess trends in fish populations without regular (annual) calibration.     

Paddy herbicide inputs in the entire river inflow reaching Lake Biwa, Japan

This study estimated the inputs of four paddy herbicides in the entire river inflow reaching Lake Biwa, the largest lake in Japan, which serves as a water resource for 14 million people. The Uso River and the Hino River, the main contaminated rivers among the inflow rivers, were selected as daily and hourly monitoring sites to provide data on the seasonal trends in the concentration and load of herbicides and to determine the effect of rainfall events on load. The monitoring was also performed four times in 15 inflow rivers. The total input to the lake was calculated from the loads during fine weather conditions and additional loads during rainfall events. The former based on the lumped load from the two rivers and by prorating for the 15 rivers, and the latter was estimated from the relation between precipitation and increased load rate. The annual losses of herbicide from the basin to Lake Biwa were estimated to be 14.5% for bromobutide, 3.0% for pretilachlor, 5.2% for molinate, and 8.8% for simetryn. The loads caused by rainfall events accounted for 9%–18% of the total annual loads.     

中国森林生态系统地表径流调节特征

径流调节是森林生态系统重要生态服务功能之一,包含着大气、水分、植被和土壤等生物物理过程,其变化将直接影响区域气候水文、植被和土壤等状况,是区域生态系统状况的重要指示器。在区域尺度上评估森林生态系统地表径流特征,对于科学认识和合理保护森林生态系统水源涵养功能具有重要意义。以森林生态系统定位监测数据为基础,探讨地表径流与降水,径流系数与植被的关系,建立径流系数与植被的回归方程,分析全国森林生态系统地表径流调节特征。结果表明:(1)各森林类型地表径流与降水相关性显著,其对地表径流的影响为37%—76%。此外,径流系数与植被也显著相关,其对径流系数的解释能力为27%—47%。(2)基于植被覆盖数据,通过植被与径流系数回归方程估算全国森林生态系统的地表径流调节特征。全国各森林生态系统径流调节能力存在差异,强弱顺序为:落叶针叶林落叶阔叶林针阔混交林常绿针叶林常绿阔叶林。     

Sediment phosphorus release in phytoplankton dominated versus macrophyte dominated shallow lakes: importance of oxygen conditions

Increased discharges of organic matter from different sources in Morales Stream, one of the main tributaries of the Matanza-Riachuelo River, caused not only an increase in its primary production but also drastic changes in the composition of its sediments, thus favoring eutrophication processes. An in situ study was carried out in order to assess the effects of an organic point source contamination (from intensive cattle rearing) on the sediments of Morales Stream. Surface water and sediment samples were analysed to determine the chemical characteristics of the water–sediment system. The amounts and forms of sediment phosphorus were determined using the `EDTA method' (Golterman, 1996) at two sites of the stream having different nutrient loads. The increase in the organic load of Morales Stream waters influences the dynamics of sediment P, producing two main effects: (1) an increase in the organic matter amount of the sediment that leads to an increase in the amount of P associated to organic fractions, which may be released by bacterial activity under anoxic conditions; and (2) a decrease in the concentration of P in the fraction bound to iron. Morales Stream sediments may act as a potential source of P, which can release this nutrient to water under the reducing conditions originated by uncontrolled discharges of organic residues to this water body.     

Modeling the hydrochemistry of the Choptank River basin using GWLF and Arc/Info: 2. Model Validation and Application

We used the hydrochemical model GWLF to estimate terrestrial diffuse fluxes from ungauged areas of a coastal plain catchment, the Choptank River basin. The gauged area of the basin is 17% of the land surface, and we divided the remaining ungauged area into 21 subbasins. Three comparative approaches were used: (1) application of area yield coefficients based on 11 years of observations from the gauged area to extrapolate over ungauged subbasins without modeling, (2) application of GWLF to estimate export from all subbasins using model parameters calibrated in the gauged subbasin, and (3) application of GWLF with parameter adjustments based on the local characteristics in each subbasin. Comparison of the predicted export from 6 selected subbasins with observed export data showed that application of GWLF with local adjustments reduced model errors of N export from 43% to 27%. With only one adjustment for sediment P, application of GWLF alone reduced errors of P export from 92%to 40–45%, with or without local adjustments for flow and sediment retention. The data supported the hypothesis that significant spatial variations in N and P yields introduce large errors when extrapolating from gauged to ungauged subbasins, and estimated TN and TP yield coefficients varied over 1–21 kg N and 0.1–0.5 kg P ha^–1 y^–1 in ungauged areas due to varying human population densities, soil drainage characteristics, and amounts of agriculture. The most accurate estimates of terrestrial diffuse sources were combined with point source discharges and wet atmospheric inputs to estimate annual average inputs of 2.5 × 10⁶ kg N and 5.8 × 10⁴ kg P y^–1 to the Choptank estuary during 1980–1996. These results illustrate the problems of spatial extrapolation from gauged to ungauged areas and emphasize the need for application of local characteristics for accurate assessment of watershed export.     

Macroinvertebrate species and assemblages in the headwater streams of the River Tyne,northern England in relation to land cover and other environmental variables

The macroinvertebrate species and assemblages of headwater streams of the River Tyne catchment in northern England were classified and their relationship with environmental variables based on stream structure, water acidity, distance from source and land cover investigated using constrained ordination and logistic regression. Fuzzy classification of data from 322 stream sites generated five assemblages. Stream structure, quantified as an exposure index, was found to be the most important environmental variable, with water acidity also important. Distance from source and land cover had less influence on species and assemblage distribution. A considerable amount of variation in assemblage distribution was explained using a two-variable logistic regression with stream structure (exposure index) and water acidity (pH) in a template. Site structure and water acidity appeared to be related to drift, geology and topography with little anthropogenic influence. The applicability of the habitat template concept for explaining the distribution of stream macroinvertebrates is discussed.     

A water quality analysis system to evaluate the impact of agricultural activities on N outflow in river basins in Japan

We have developed a personal-computer-based water quality analysis system for river basins. The system estimates potential N outflow by model and calculates actual N outflow from monitoring data. For the former it uses the potential load factor method to estimate annual nitrogen load from various sources and runoff potential from each area of land in a basin. For the latter it analyzes water quality monitoring data in relation to meteorological data. We used the system to analyze N outflow in basins around Lake Kasumigaura and the Yahagi River in central Honshu, Japan. The land around Lake Kasumigaura is rather flat, and about 25% is periodically flooded for rice and lotus cultivation. The land around the Yahagi River is mountainous, and much less land is flooded. In the Yahagi River basin the actual N outflow agreed closely with the potential. However, the actual N outflow in the basin around Lake Kasumigaura was much less than the potential, suggesting that a large part of the N load is denitrified in flooded soils. This further indicates that a sequence of different land uses including flooded rice fields is an important factor determining N outflow in basins in Japan. On the basis of the above analyses, we incorporated a denitrification model into the system that enables us to estimate N balance in a designated basin;this system may be helpful in the formulation of scenarios of land use andsoil management for improving water quality.     

A water quality analysis system to evaluate the impact of agricultural activities on N outflow in river basins in Japan

We have developed a personal-computer-based water quality analysis system for river basins. The system estimates potential N outflow by model and calculates actual N outflow from monitoring data. For the former it uses the potential load factor method to estimate annual nitrogen load from various sources and runoff potential from each area of land in a basin. For the latter it analyzes water quality monitoring data in relation to meteorological data. We used the system to analyze N outflow in basins around Lake Kasumigaura and the Yahagi River in central Honshu, Japan. The land around Lake Kasumigaura is rather flat, and about 25% is periodically flooded for rice and lotus cultivation. The land around the Yahagi River is mountainous, and much less land is flooded. In the Yahagi River basin the actual N outflow agreed closely with the potential. However, the actual N outflow in the basin around Lake Kasumigaura was much less than the potential, suggesting that a large part of the N load is denitrified in flooded soils. This further indicates that a sequence of different land uses including flooded rice fields is an important factor determining N outflow in basins in Japan. On the basis of the above analyses, we incorporated a denitrification model into the system that enables us to estimate N balance in a designated basin; this system may be helpful in the formulation of scenarios of land use and soil management for improving water quality.     

How reliable is the monitoring of permanent vegetation plots? A test with multiple observers

Questions: A multiple plot design was developed for permanent vegetation plots. How reliable are the different methods used in this design and which changes can we measure? Location: Alpine meadows (2430 m a.s.l.) in the Swiss Alps. Methods: Four inventories were obtained from 40 m² plots: four subplots (0.4 m²) with a list of species, two 10m transects with the point method (50 points on each), one subplot (4m²) with a list of species and visual cover estimates as a percentage and the complete plot (40 m²) with a list of species and visual estimates in classes. This design was tested by five to seven experienced botanists in three plots. Results: Whatever the sampling size, only 45‐63% of the species were seen by all the observers. However, the majority of the overlooked species had cover < 0.1%. Pairs of observers overlooked 10‐20% less species than single observers. The point method was the best method for cover estimate, but it took much longer than visual cover estimates, and 100 points allowed for the monitoring of only a very limited number of species. The visual estimate as a percentage was more precise than classes. Working in pairs did not improve the estimates, but one botanist repeating the survey is more reliable than a succession of different observers. Conclusion: Lists of species are insufficient for monitoring. It is necessary to add cover estimates to allow for subsequent interpretations in spite of the overlooked species. The choice of the method depends on the available resources: the point method is time consuming but gives precise data for a limited number of species, while visual estimates are quick but allow for recording only large changes in cover. Constant pairs of observers improve the reliability of the records.     

Critical Load Concept to Set Restoration Goals for Liming Acidif ied Nor wegian Waters

The concept of critical load is now widely used in the management of acidified waters. In southern Norway, acidification due to long-range transported air pollutants is one of the most serious environmental problems, affecting an area of 80,000 km². To preserve and restore biodiversity, Norwegian authorities have chosen liming as a temporary mitigation measure. Critical load estimates were used to estimate the material and financial needs for this large-scale program. In 1995, more than 2000 localities ranging from small lakes to large salmon rivers were limed. Liming costs in 1996 were $18 million (U.S.). Critical load estimates also formed the basis for international negotiations on sulfur emission reductions, resulting in the second sulfur protocol for Europe and North America in 1994. The critical load estimates indicated that acidified areas in Norway would be reduced to 35,000 km² after the year 2010, after the commitments of the sulfur protocols are met. By that time, estimated liming costs would be reduced by almost 40%. Lime treatment of River Tovdalselva, with a catchment area of 1885 km², is probably the largest integrated liming project in the world. In 1990 the critical load was exceeded in 98% of the Tovdalselva catchment. After the year 2010 the exceeded area may be reduced to 44% and the liming cost by two-thirds.     

Changing suspended sediment and particulate phosphorus loads and pathways in underdrained lowland agricultural catchments; Herefordshire and Worcestershire,U.K.

Data obtained from a small (150 ha) experimental catchment, Hereford U.K., have shown that land drains contributed >50% of the total catchment suspended sediment (SS) yield over a two year period. In one of the monitored drains, annual sediment yields were 964 and 978 kg ha^–1. Particulate phosphorus (PP) contributed >60% of total phosphorus lost through the drains and at least 73% of the total drain load came from topsoil. A major question that was not answered by the monitoring programme was whether SS and PP loads had increased since the drains had been installed between the 1960s and 1980s. To address this problem, a sediment yield record was reconstructed from the Kyre Pool catchment in Worcestershire that has a similar drainage history and soil types. Reservoir sediments were dated using the ²¹⁰Pb crs method and results suggest a fourfold increase in SS yield (300–1170 kg ha^–1 yr^–1) and PP loads (0.19–0.79 kg ha^–1 yr^–1) since the 1960s. The most recent SS and PP loads are comparable to those obtained from catchment monitoring. The high lake sediment ¹³⁷Cs inventory suggests a significant influx of eroded topsoil and ¹³⁷Cs activities in the most recent lake sediments are comparable to those of monitored land drains, supporting the hypothesis that land drainage has had a major impact on SS and PP yields and pathways.     

Detection of sensitive soil properties related to non-point phosphorus pollution by integrated models of SEDD and PLOAD

Effectively identifying soil properties in relation to non-point source (NPS) phosphorus pollution is important for NPS pollution management. Previous studies have focused on particulate P loads in relation to agricultural non-point source pollution. In areas undergoing rapid urbanization, dissolved P loads may be important with respect to conditions of surface infiltration and rainfall runoff. The present study developed an integrated model for the analysis of both dissolved P and particulate P loads, applied to the Meiliang Bay watershed, Taihu Lake, China. The results showed that NPS P loads up to 15 kg/km² were present, with particulate P loads up to 13 kg/km². The highest loads were concentrated in the southeastern region of the watershed. Although particle P was the main contributor to NPS P loads state, the contribution of dissolved P was significant, especially in sub-basins with significant amount of artificial land cover. The integration of dissolved P and particulate P loads provided more accurate evaluation of NPS P pollution. NPS P loads were found to correspond to specific soil properties. Soil organic matter and total nitrogen were shown to influence dissolved P loads, while total phosphorus and soil particle composition proportion were more closely related to particulate P loads.     

Transport and retention of nitrogen and phosphorus in the sub-tropical Richmond River estuary, Australia – A budget approach

Nitrogen and phosphorus loads in the sub-tropicalRichmond River estuary were quantified and materialbudgets were developed over two years of contrastingfreshwater discharge. During both years >74% of thenitrogen and >84% of the phosphorus load enteredthe estuary during one month when flooding occurred inthe catchment. Due to larger flood magnitude, loadsduring the 1995/96 year were 3.3 and 2.5 times greaterthan during the 1994/95 year for nitrogen andphosphorus respectively. During floods the estuarinebasin was completely flushed of brackish water and themajority of the nutrient loads passed directly throughthe estuary. The nutrient load retained in the estuaryduring floods was inversely proportional to floodmagnitude. Annual budgets show that >97% of thenutrient load entering the estuary was from diffusecatchment sources; precipitation, urban runoff, andsewage were negligible. Less than 2.5% of thenitrogen and <5.4% of the phosphorus loads enteringthe estuary were retained in sediments. During dryseasons the estuary became a net sink for nitrogeninput from the ocean and the estuarine sedimentsremained a net source of phosphorus to the watercolumn and ocean. The process of flood scouring islikely to be the cleansing mechanism responsible formaintaining water quality both on an annual basis andover the last 50 years and may also be responsible forpotential nitrogen limitation. The sub-tropicalRichmond River estuary contrasts with the majority oftemperate systems of North America and Europe whichtypically have lower inter- and intra-annual nutrientload variability, longer and less variable flushingtimes, and greater nutrient retention.