Errors in the determination of low levels of nitrate in lake sediments

Abstract

Error sources associated with the spectrophotometric determination of low levels (e.g. <2 μg g^?1) of nitrate in sediments have been examined and problems identified included incomplete nitrate recovery (attributable in part to anion resorption) and light scattering by colloidal (<0.45 μm) matter in extract solutions (minimised by using uncoloured extract in the reference beam). Optimum retrieval (>90%) of nitrate from the marine lake sediments studied was achieved with 15 min mixing with 0.1 M NH₄CI, using a sediment to extractant ratio of 1:30. The nitrate in the extracts was determined by reducing it to nitrite (using Cd powder), with subsequent colour development based on the addition of sulfanilic acid and N-1-naphthyl-ethylenediamine dihydrochloride. The reduction step was sensitive to the experimental conditions used, but was near quantitative using 0.1 M NH₄CI extracts. (Much lower transformation levels were observed when the nitrate solutions contained KCI or CaSO₄, or when Zn powder was used as the reductant). All the sediments tested sorbed nitrate ion from solution (some very avidly) and this sorbed ion was not readily retrieved by back extraction into NH₄CI solutions.     

Ecosystem health as measured from the molecular to the community level of organization,with reference to sediment bioassessment

The current recognition that chemical measurements are uncertain indicators of biological consequences of pollution has shifted the emphasis away from assessing environmental chemistry alone toward the inclusion of measurements of the health of organisms. Effects of pollutants begin with the individual, have subsequent repercussions on population level processes, and ramifications for community structure and functions. Pollutants act at a molecular level and the biochemical lesions is the first step in the manifestation of effects. Technologies that operate at the cellular level assist in elucidating toxicity. Higher levels of integration include an organism's capacity for growth. Laboratory bioassays andin situ research can monitor physiological incapacities and assist in predicting population level effects. A yet higher level of organization is that of the ecological community.     

Sediment dynamics and estuarine circulation in the turbidity maximum of the Elbe river

Data are presented from several campaigns concerning to the residual transport of water, salt and suspended particulate matter (SPM) at different depths and at different longitudinal and cross-sectional locations in the Elbe Estuary, Northern Germany. The intratidal behaviour of SPM is analysed and explained in terms of cyclic settling and resuspension. Superimposed on these local processes are advective horizontal transports of water and SPM in different vertical layers. Tidally averaged horizontal fluxes of salinity and SPM have been calculated at different depths. For the most part, they show upstream directed transport in the bottom layers, while in the upper water column SPM is carried towards the sea. Examples of the influence of vertical salinity gradients on SPM dynamics, of the lateral variation of residual transport of water and SPM, and the effects of a runoff peak are also presented.     

Terminal electron transport system (ETS)-activity in the sediment of Lake Balaton,Hungary

Terminal electron transport system (ETS)-activity of the sediment and plankton of Lake Balaton, the largest shallow lake of Central Europe was measured by tetrazolium-reduction biweekly during 1989–1990 and in the spring of 1991. Sediment proved to be enzymatically active to 30-35 cm down in the hypertrophic Keszthely Bay and to 15–20 cm down in the meso-eutrophic Siófok Basin. Sediment ETS-activity exceeded planktonic activity 15 to 24 fold.The total activity m^–2 showed one or two order of magnitude higher respiratory potential in Lake Balaton than needed for complete oxidation of the planktonic primary production; most of this potential was detected in the upper 3–5 cm sediment layer in springs. Incubations of cell-free homogenates of sediment bacteria showed that ETS remains active days after death of organisms at low temperature. Accumulated postmortem ETS-activity derived from the benthic diatoms, bacteria, plankton deposit and dead summer macrophytes seems to be responsible for the high ETS-activity of the sediment in the warming periods in springs. These enzyme fractions may contribute to the rapid oxidation of the alkaline, well-aerated lake.     

Modifications of the Ekman Sampler

Many types of sediment samplers have been designed for specific purposes and for sampling in different aquatic environments. The objective of this technical note has been to introduce two specific improvements of the traditional Ekman grab sampler, which is a well-known apparatus for sampling of soft sediments, especially in bottom faunistic contexts. The two new modifications concern the automatic closing mechanism. The jointed quadrant and the jointed, hooked axis, both made of brass, provide a much handier and more reliable operation than, e.g., the traditional automatic mechanism.     

Influence of streambed sediment clogging on microbial processes in the hyporheic zone

1. The hyporheic zone plays a key role in hydrological exchange and biogeochemical processes in streambed sediments. The clogging of sediments caused by the deposition of particles in the bed of streams and rivers can decrease sediment permeability and hence greatly affect hyporheic microbial processes. 2. The main objective of this study was to determine the influence of sediment clogging on hyporheic microbial processes in three French rivers (the Usses, Drôme and Isère). In each river, microbial abundance and activity were studied at three depths (10, 30 and 50 cm) in the sediment at one unclogged (high porosity) and one clogged site (low porosity). 3. The results showed that the sediment clogging had inconsistent effects on microbial processes in the three rivers. Increases (Usses) or decreases (Drôme and Isère) in both aerobic and anaerobic processes were detected at the clogged sites compared to unclogged sites. These results suggest that microbial changes because of the sediment clogging are mainly mediated by the residence time of water within the hyporheic sediments. 4. A single model predicting the effect of clogging on hyporheic microbial processes cannot be applied generally to all rivers because the degree of clogging creates heterogeneous effects on flow rates between surface and interstitial waters. As a consequence, the influence of heterogeneous clogging on surface water–hyporheic exchanges needs to be evaluated by water tracing and hydraulic modelling to determine the links between microbial processes and hydraulic heterogeneity induced by clogging in hyporheic sediments.     

Recommendations for the Implementation of a National Sediment Quality Policy in the United States

This article was prepared prior to the author's employment by the U.S. Environmental Protection Agency and therefore does not necessarily represent agency policy. Sediments provide needed habitats to valued aquatic and marine resources and are therefore an integral and valuable component of any coastal ecosystem. Studies have found that multiple anthropogenic activities have been the primary cause of sediment contamination. There is continued evidence that contaminated sediments pose adverse impacts to biological resources even when overlying water quality is acceptable. Efforts in environmental protection should therefore incorporate sediment quality management strategies. Despite a growing awareness and interest in management of contaminated sediment, no established systematic and standardized national management program has been established in the U.S. The establishment of a national sediment policy in the U.S. would reinforce the importance of integrating sediment issues with different management objectives and reiterate the importance of protecting sediments as a natural resource. A national sediment policy could also guide and direct states in developing state sediment policies that reflect national objectives while integrating local concerns. This perspective identifies and defines issues and concerns raised by 13 states’ agency staff in managing contaminated sediments in the absence of a national policy. Recommendations are developed that address sociopolitical and scientific issues and concerns. The recommendations are integrated with stakeholder comments, state manager needs and the existing regulatory and institutional framework.     

Initial Development and Evaluation of a Sediment Quality Index for the Great Lakes Region

A sediment quality index (SQI) based on the Canadian Water Quality Index was developed and applied to the assessment of sediment quality in two Great Lakes Areas Of Concern where metals are the primary contaminants of potential concern, Peninsula Harbour (Lake Superior) and Collingwood Harbour (Lake Huron). The SQI was calculated according to an equation incorporating two elements; scope—the number of variables that do not meet guideline objectives; and, amplitude—the magnitude by which variables exceed guideline objectives. Categorizations of sediment quality were developed based on SQI scores. The robustness of the SQI was evaluated through comparison of the relative rankings of sediment quality in the two test areas with results obtained from principle components analysis (PCA) incorporating reference sites, and calculations of hazard quotients (HQs). Trends and rankings in sediment quality determined by the SQI were similar to those calculated using PCA at both test areas. The HQs also appeared to be good indicators of sediment quality. Both the SQI and HQ methods are based on existing Sediment Quality Guidelines, but the SQI had the added benefit of allowing straightforward integration of multiple contaminants. The SQI and PCA analyses appeared complementary in that the SQI incorporated information on the number of variables exceeding guideline values and the degree to which these guidelines were exceeded. The PCA allowed a simple check of the SQI by relating test conditions to regional background. It is recommended that this analysis be performed concurrently with SQI to ensure that non-anthropogenic sources of contaminants (metals in this case) are not considered as representing an anthropogenic hazard.     

Deposition,resuspension, and decomposition of particulate organic matter in the sediments of Lake Itasca,Minnesota, USA

Sediment traps were used to investigate the settling, resuspension, and decomposition of particulate organic matter in Lake Itasca, MN (USA). Traps were deployed in the epilimnion and hypolimnion of the deepest basin during June, 1988, sampled twice during stratified conditions (August, September) and once after the lake had mixed (October). The downward flux of particulate material increased from summer to fall. The net sedimentation of organic matter ranged from 0.6 to 2.3 g m^–2 d^–1 at 4 m and increased to 2.1 to 3.2 g m^–2 d^–1 two meters above the bottom sediment indicating that resuspended sediment was at least 33% of the settling mass during all periods. The C:N ratios of captured particles (6.8–9.5) were between the ratios of plankton (5.8 to 6.8) and the sediments (9.9 to 10.2) but smaller than the ratios of terrestrial organic materials (13.5 to 222). The monosaccharide compositions of the entrapped particles were similar to plankton samples and different from the distinct composition of the sediments. Capture of rebound particles similar to the primary flux and not decomposition may have been responsible for this similarity. Total monosaccharide concentrations were lower in the sediments than in entrapped particles. Individual sugars exhibited different patterns of accumulation in the sediments. Glucose was lowest in sediments when the relative concentrations were compared to those in source materials and entrapped particles. In contrast, sediments had the highest rhamnose and fucose concentrations. Bacterial biomass could only account for small portions of these sugars in the sediment. The distinct monosaccharide composition of resuspended sediments was not strongly recorded in materials captured by the sediment traps even after the lake had mixed.     

黄土高原多沙粗沙区侵蚀产沙的多维临界

黄土高原多沙粗沙区侵蚀产沙受到自然要素和人文要素的综合作用。从该地区侵蚀产沙的自然和人文影响要素识别入手,比较系统地揭示了各主要影响因子侵蚀产沙过程的单维临界响应及其发生的内在机理,在此基础上建立了侵蚀产沙要素交互作用的多维临界综合集成模型,并依据该模型定量计算出目前该地区自然和人文要素及各主要影响因素分别对侵蚀产沙的贡献,最后提出了该地区水土流失治理的调控目标和现有治理措施的调整思路。研究结果表明:(1)由于该地区自然和人文要素的交互作用,使得各影响因素侵蚀产沙的单维临界响应发生位移和变化,达到复合临界极值的多维临界点趋于降低或基本保持不变。(2)该地区的侵蚀强度在自然和人文要素的交互作用下仍在加剧。其中,可分离的自然因素作用占80%左右,人为因素作用占20%左右。就自然因素而言,降水对产沙强度的贡献最大约为61%;(3)该地区水土流失的治理速度抵不上人为破坏速度;(4)在多沙粗沙区人为因素产沙贡献中,农业结构的贡献最大。这意味着该地区生态环境治理与建设首先要把农业结构调整和优化置于第一位。     

Temporal changes in the metal and phosphorus content of suspended sediment transported by Yorkshire rivers,U.K. over the last 100 years,as recorded by overbank floodplain deposits

Cores of overbank deposits were collected from locations along the Rivers Swale and Aire in Yorkshire, U.K. The middle and lower reaches of the River Aire drain heavily industrialized and urbanized areas, whereas the River Swale drains a predominantly rural catchment, although Pb and Zn mining in the headwater areas in the 19th century introduced contaminated sediment. Downcore changes in the heavy and trace metal (Al, Cr, Cu, K, Pb, Sr and Zn) and phosphorus (P) content of the floodplain sediment were used to provide evidence of temporal changes in the contaminant content of the fine-grained sediment transported by the study rivers over the last ca. 100 years. The core collected from the downstream site on the River Aire shows upcore increases in P content, which reflects the expansion of the urban area during this period. Variations in the metal content of the deposited sediment over the period represented by the core reflect changes in the extent and type of industrial activity in the catchment. For the cores from the River Swale, there are no major upcore changes in the P content of the sediment, but there was a period characterized by increased levels of Pb and Zn which can be linked to metal mining activities.     

Lead-210 dating of sediments compared with accumulation rates estimated by natural markers and measured with sediment traps

Methods to provide accurate accumulation rates for lake models are discussed. Cores were taken in 1979 in two basins of Lake Lucerne, Switzerland, and accumulation rates were calculated by using Pb-210 dating and by a natural landslide marker of 1795 in one basin (Weggis). In the other basin (Horw Bay) the sediment accumulation rates based on the lead method were compared with yearly sedimentation rates measured by sediment traps in 1969/70. At the Weggis station, the core dating yielded sediment accumulation rates of about 400 g dry wt. m^–2 y^–1 with the lead method, averaged over a sediment depth of 4–20 cm; accumulation was about 700 g dry wt. m^–2 y^–1 with the marker method, averaged over 0–33 cm. In Horw Bay, the trap method yielded about 1300 g dry wt. M^–2 y^–1 compared with 400–1000 g dry wt. m^–2 y^–1 obtained with the lead method and related to various depth intervals. The characteristic sources of error of the three methods as well as several hypotheses for these discrepancies are discussed.     

Small-scale distribution and diel vertical migration of zooplankton in a shallow lake (Lake Naardermeer,the Netherlands)

Groundwater is a major influence on the hydrological, chemical and thermal regime of chalk streams in the southern U.K. However, little is currently known about the nature of the sediment delivery system within these chalk stream systems, even though sediment-related problems have been increasingly cited as a cause of habitat degradation and of declining salmonid stocks. To address this knowledge gap, suspended sediment fluxes were monitored at 4 sites within the Hampshire Avon catchment between February 1999 and August 2000. Maximum suspended sediment concentrations ranged from nearly 45 mg l^–1 to 260 mg l^–1. Over the study period, annual suspended sediment loads ranged from 644 to 6215 t yr^–1 and annual specific sediment yields ranged from 1.4 to 12.5 t km^–2 yr^–1. The results show that, relative to other U.K. rivers, the study chalk streams are characterised by low suspended sediment concentrations and loads and less episodic behaviour.     

133-year-old well-presented top sediment from the Finnish Lake Höytiäinen in comparison with new top sediments

In 1859, the level of Lake Höytiäinen was lowered accidentally by 9.5 m and 157 km² new land was formed. The event is marked by a 2–3 cm inwash horizon of clay and fine silt in deep-water sediments. In the sediment profile, the dry weights of 2 cm thick subsamples increase from 51 mg g^–1 in the clay horizon and decrease back to 117–127 mg g^–1 below the clay horizon. Below the pale clay horizon the sediment is muddy and rich in organic substances.Loss on ignition, amount of Tot.P, Tot.N and BOD₇ are the highest below the clay horizon. The clay horizon has prevented mixing of the old sediment as well as aerobic decomposition of organic compounds. The high loss on ignition and the large proportion of biologically degradable organic substances in the old sediment resembles the new upper sediment of a typical central Finnish lake.The finding of a 133 year old well preserved top sediment sows that before the impact of waste waters and fertilizers, the upper sediment of the lake was rich in organic substances and nutrients. In spite of cultivation of new land later on, the new top sediment above the clay horizon is not as rich in organic substances and nutrients as the old one below it. This suggests that part of the organic substances may be mobile within the sediment and move to the uppermost sediment layer in the course of time in undisturbed lake sediments.     

Determination of nitrite in lake sediments

Abstract

An evaluation of nitrite determination in marine lake sediments has shown that spectrophotometric measurements can be in error due to light scattering by colloidal (<0.2 μm) matter in extract solutions and incomplete nitrite recovery. The scatter error can be minimised by using uncoloured extract in the reference beam but precision at low levels remains poor (RSD 25 to 100%). Recovery tests on ‘spiked’ sediment indicated that optimum retrieval (～85%) occurred with 30 minute mixing with 0.2 M NH₄Cl, using a sediment to extractant ratio of 1:30. To counter this variable, calibration based on standard addition to sample suspensions is recommended. Modified procedure proposed is suitable for measuring up to 10 μg g^?1 of nitrite N; the lake sediments tested contained <100 ng g^?1     

Net and gross sedimentation in relation to the phosphorus budget of Eau Galle Reservoir,Wisconsin

We compared P retention with direct measures of Psedimentation, estimated fromsediment cores (annual P sedimentation) and sedimenttraps (daily P sedimentation),to quantify P sedimentation in Eau Galle Reservoir,Wisconsin. Mean annual Pretention was similar to mean annual P sedimentation,as estimated from sediment corerates integrated over the entire lake basin,indicating that annual P mass balanceapproximated annual net P sedimentation in thisreservoir. However, sediment trap Prates, measured over the summer stratified period,overestimated P retention ratesdetermined over the same period, suggestingsubstantial deposition of internally-derived P.Inclusion of measured internal P loadings from avariety of sources in EauGalle Reservoir in a P mass balance only accounted foran additional 24% of thesummer sediment trap P rate, indicating substantialuncertainty in the overall P budget.Imbalances in the P budget may also suggest depositionof sediment from other as yetunquantified internal sources. Potential internalsources of P include sedimentresuspension and chemical release and direct uptake ofP from the sediment byphytoplankton.     

沉积物质量评价"三元法"及其在近海中的应用

沉积物质量评价"三元法(sediment quality triad,SQT)"是一种基于生物效应的综合评价方法,主要包括化学、毒理、生态3个基元。尽管各基元可通过选择适当参数,单独反映沉积物中致污物的环境风险,但以证据权重法结合其三基元,则更能全面描述沉积物中有害化学物质与生物效应之间的因果逻辑关系,加强化学致污物及其污染水平的生态相关性,为环境治理及修复等提供重要依据。从基元构成和数据解译两方面回顾了SQT方法的研究进展,介绍了该法在国内外的应用实例,剖析了提高评价可靠性的相关手段,并结合我国近海沉积物环境质量评价现状,展望了SQT法的未来研究及应用前景。结果表明,通过替换、改进现有基元或增加其它基元的方式可提高SQT评价结果的可靠性,而引入新的数据解译方法则可使本方法的评价过程更加透明、评价结果更加直观。适于评估化学胁迫对沉积物等环境介质造成的损害,已广泛应用于世界各地,是目前主要的综合评价方法,具有良好的研究与应用前景。     

The change of sediment composition during recovery of two Finnish lakes induced by waste water purification and lake oxygenation

Total oxygen deficit occurred regularly during stagnation periods in the deepest part of Lake Kallavesi in the period 1973–1986. The sediment was black and anaerobic during the first sampling in 1987. After beginning of artificial lake oxygenation and efficient purification of waste waters of a paper board mill in 1986 the oxygen deficit decreased gradually and a light brown oxidized uppermost sediment layer appeared and began to thicken. The following changes in the sediment composition were observed during 1987–1996: loss on ignition, total nitrogen and BOD₇ concentrations decreased in the uppermost sediment layer (0–2 cm) and BOD₇ concentration increased in the next sediment layer beneath (2–10 cm). There were no significant change in phosphorus and iron concentrations.Lake oxygen, total phosphorus and suspended solids concentrations fluctuated in a noticeable degree in Lake Huruslahti depending on waste water input and artificial oxygenation during the years 1980–1993. Oxygen condition was good at times of successful waste water elimination and lake oxygenation while deterioration of either resulted oxygen deficiency as well as increase of total phosphorus and suspended solids concentration. Most of the internal load entered with suspended solids during periods of total oxygen deficiency.An explanation for the findings in Lake Huruslahti could be microbiological. Gas formation inside sediment lift organic material towards top of the sediment and into the water, but after the lake recovery the material retain in the sediment. Also in Lake Kallavesi microbiological gas formation resuspended sediment particles with phosphorus into the overlaying water prior to oxygenation. During oxygenation microbiological processes in uppermost sediment utilize the anaerobic metabolic products, organic acids and methane, and block gas formation. Organic substances remain in the top sediment decomposing gradually in the uppermost layer.     

An improved elutriation technique for the bioassessment of sediment contaminants

An improved method is proposed for the preparation of sediment elutriates which permits relatively realistic determination of bioavailable contaminants. It suggests the use of rotary tumbling in a cycle of 3–4 rpm to achieve sediment-water mixing. Experiments were undertaken to evaluate the mixing efficiency of the rotary tumbler as compared to that of the compressed air, wrist-action shaker, and reciprocal shaker methods. Sediment to water ratios of 0 : 1, 1 : 20, 1 : 10, and 1 : 4 were tested over 0.5, 1.0, 24, and 48-h elution periods. Elutriate evaluations were based on chemical, physico-chemical and gravimetric determinations; and also on ¹⁴C-phytoplankton bioassays using Chlorella vulgaris (Beyerinck). Results indicated that rotary tumbling produced the most consistent bioassay-supportable data. It was also the most efficient procedure when used for 1 h with 1 : 4 sediment-water mixtures.     

Metal Pollution Assessment in Sediments of the Southeastern Black Sea Coast of Turkey

The main objective of this investigation is to determine the concentration and accumulation of heavy metals in the coastal sediments of the Southeastern Black Sea of Turkey. The selected sampling area has mainly been affected by anthropogenic activities, such as agricultural, untreated domestic and treated industrial wastewater, and mining. Metal enrichment factor (EF), geo-accumulation index (I_geo), and metal pollution index (MPI) have been calculated and relative contamination levels evaluated at all stations. In this study, the maximum EF values calculated for nickel (Ni), cobalt (Co), cadmium (Cd), lead (Pb), chromium (Cr), arsenic (As), zinc (Zn), and copper (Cu) were 1.4, 3.1, 5.2, 7.8, 7.8, 20, 26, and 42, respectively. Metal pollution has decreased in recent years, but the enrichment of heavy metals has been observed to be relatively high, especially in the uppermost 3-6 cm of the core sample from the Sürmene sampling station, which has been polluted by mining activities. In addition, factor analysis revealed that the coastal sediments from the Eastern Black Sea were influenced by several sources, namely lithogenic and anthropogenic activities (mining, wastewater discharging, agriculture).