Release of phosphorus from sediments in Lake Biwa

Two sulfur-mediated reactions are resulting in the eutrophication of Lake Biwa, Japan. The iron (II) phosphate mineral vivianite is dissolving in sulfide-enriched sediments that in places results in porewater concentrations of phosphate exceeding 3 mg l⁻¹. The dissolution of phosphate is evident in profiles of total phosphorus where zones of dissolution and a zone of precipitation in the most oxic surface sediments are visible. At times sulfate reduction in these surface sediments results in pH values as high as 9.9, which can dissolve phosphate adsorbed to iron (III). This release of phosphorus from sediments is at least partially responsible for the recent appearance of blue-green algal blooms. Received: August 4, 2000 / Accepted: March 19, 2001     

Effects of sunlight on the production of dissolved organic and inorganic nutrients from resuspended sediments

A series of laboratory-based and field experiments was conducted to address the effects of sunlight-exposed resuspended sediments on dissolved nutrient fluxes in two different water bodies. In suspensions of tidal creek sediments in 0.2 μm-filtered creek water, measurable increases in dissolved nutrients occurred after only 2 h of exposure to simulated sunlight. During a 6-h irradiation, nutrient release rates for total dissolved nitrogen (TDN) and phosphate were 2.2 ± 0.5 (standard error; S.E.) μmol g^?1 h^?1 and 0.09 ± 0.005 μmol g^?1 h^?1 (S.E.), compared to no significant changes in dark controls. The majority of nitrogen was released as dissolved organic nitrogen (87% on average) with lesser amounts of ammonium (13%). Continental shelf sediments resuspended in unfiltered seawater also released phosphate and TDN when exposed to sunlight, suggesting that this process can occur in a variety of marine and estuarine environments. The source material for inorganic nutrients appears to be associated with sediments rather than dissolved organic matter, as no significant changes in nutrient concentrations occurred in experiments with 0.2 μm-filtered creek water or seawater alone. Results suggest that photoproduction of dissolved nutrients from resuspended sediments could be an episodically significant and previously unrecognized source of dissolved organic and inorganic nutrients to coastal ecosystems. This process may be especially important for continental margins where episodic resuspension events occur, as well as in regions experiencing high riverine sediment fluxes resulting from erosion associated with deforestation and desertification.     

Geochemistry of Lake Biwa sediments revisited

Extensive chemical data for the Lake Biwa sediments were examined with statistical factor analysis to find any correlation patterns among elements and among samples. Based on those patterns, a series of x-y correlation plots of the concentrations of selected elements was constructed to see in detail how the concentrations of elements vary among different sample groups and explain the observed variation patterns.     

Yangtse River sediments and erosion rates from source to sink traced with cosmogenic Be: Sediments from major rivers

Estimates of regional erosion and sediment mixing from different sources in the Yangtse River system are presented, based on sand samples collected from major tributaries and the trunk stream, at 23 sites between western Sichuan and the Yangtse Delta. Mixing is estimated from concentrations of Mg, Ca, Sr, Ti, Mn and Fe, which are substantially higher in sand from major tributaries in the western Yangtse River catchment than from tributaries in the eastern catchment. Intermediate concentrations occur in sand from the Yangtse Delta, both for modern samples from the surface and for early Holocene samples from drill holes. Mixing ratios indicate that 35 ± 5% of sand in the delta came from eastern sources. A similar result was obtained using cosmogenic ¹⁰Be in quartz grains as a tracer of mixing. Regional erosion rate estimated from ¹⁰Be in sand grains from high mountain catchments of the western Yangtse River are mostly similar to rates based on sediment gauging but are sometimes higher, and range to over 700 m Ma^− 1, while ¹⁰Be measured at upper Yangtse River tributaries on the northeast Tibetan plateau gave rates of 20-30 m Ma^− 1. For the eastern catchments, ¹⁰Be measurements from quartz sand and sediment gauging both gave rates of 30-70 m Ma^− 1. Eroding at this rate, the eastern catchments could not supply more than 20% of the sediment in the delta, in contrast with 35% estimated from geochemical fingerprints. The relative input from eastern sources may have been higher in Late Pleistocene times, under a different climatic regime, and reworking of Pleistocene deposits may still be in progress.     

Microbial activity profiles in Tagus estuary salt marsh sediments

This study provides some results about microbial activity in salt marsh sediments. Microbial activity was determined by profiling extracellular enzyme activities in three Tagus estuary marshes and in two sediments horizons: surface layer (0–2 cm) and depth (8–10 cm). Five enzymatic activities were examined (β-glucosidase, cellulase, alkaline phosphatase, potential nitrification and nitrate reductase). All extracellular enzymatic activities were highest in the surface layer and decreased with depth. β-glucosidase and alkaline phosphatase prevailed both in surface sediments (1150 and 1200 ηmol h⁻¹ g⁻¹, respectively) and in deeper sediments (150 and 200 ηmol h⁻¹ g⁻¹, respectively). Microbial activities differed significantly between salt marshes. The marsh location in the estuary seemed to contribute to these differences: marshes located in the proximity of urbanised and industrial areas had higher microbial activities.     

Phosphate adsorption kinetics of resuspended sediments in a shallow lake,Neusiedlersee, Austria

The phosphate adsorption capacity of Neusiedlersee suspended sediments was evaluated using a silicone oil-filter-centrifugation technique with³²P and³H-H₂O labelling. This technique is quick, convenient and allows uptake processes to be followed during the first few seconds. The time dependent phosphate uptake was tested for concentration and pH dependency; the highest uptake was recorded at pH 9.00. The high calcite proportion in the sestonic material seems to influence the adsorption process. The kinetics of adsorption (at lake orthophosphate level and pH) could be explained by a biphasic Langmuir isotherm.     

An evaluation of the importance of sulfate reduction and temperature to P fluxes from aerobic-surfaced, lacustrine sediments

We examined the influence of temperature and sulfate reduction rates onP-release from aerobic-surfaced, littoral sediments in a coolingreservoir. Annually, significant differences in P release from sediments at twosites (thermal effluent and non-effluent) were related to differenttemperature regimes, with higher rates of P release and decomposition at highertemperatures. Site-specific differences in solute fluxes were mostpronounced in late summer, when water temperatures reached40°Cat the effluent site and solute fluxes increased dramatically. The thermaleffluent site retained 65% of its annual P load, while thenon-effluent site retained 92%. Relative P release(P-release normalized to inorganic carbon fluxes; RPR) data indicatedthat lake sediments retained P selectively (relative to C) throughout the year,except at the effluent site during late summer when stored P was released inexcess of supply rates.Sulfate reduction rates were often typical of those measured in otherfreshwater lakes, but unusually high rates were measured at thethermal-effluent site especially in early fall and suggested higher DICfluxes than we measured. These high rates suggest that sulfate reduction rateswere overestimated and/or that most sulfide was recycled within the sediments.In any case, the highest sulfate reduction rates did not coincide with thehighest P release rates. Furthermore, the total reduced inorganic sulfurcontentof surficial sediments did not significantly correlate to RPR, althoughconcentrations varied widely throughout the year. Temperature was the onlyvariable examined that significantly correlated to RPR (R² =0.53, P-value = 0.017). Coupling between temperature and sedimentP release was likely mediated through temperature effects on bioturbation andmicrobial metabolic rates.     

Spectroscopic properties of sedimentary humic acids from a salt marsh (Ria de Aveiro, Portugal): comparison of sediments colonized by Halimione portulacoides (L.) Aellen and non-vegetated sediments

The influence of the colonization of salt marsh sediments with Halimione portulacoides, on the composition of the sedimentary humic acids was evaluated. For this purpose, cores of colonized and non-colonized sediments from a salt marsh in Ria de Aveiro (Portugal) were collected, and the humic acids of different layers were extracted and characterized by Fourier transform infrared, synchronous molecular fluorescence ( = 60 nm) and UV-visible spectroscopies and also by elemental analysis. The infrared spectra suggest the presence of more peptide residues and carbohydrates in the sedimentary humic acids from surface and around the plant roots at the site colonized by H. portulacoides, when compared with the humic acids from the depth-equivalent sediment layers at the non-colonized site. The higher content of protein-type materials is confirmed by the lowest values of C/N ratios and the highest relative intensities of a band at _exc = 280 nm in the fluorescence spectra. The lowest ₂₈₀ values obtained in the UV-visible spectra, and the infrared spectra suggest a lower aromatic content of the humic acids from the colonized site.     

Measure of microbial turnover of carbon in anoxic freshwater sediments: cautionary comments

Small sediment cores were used to determine the turnover of a range of carbon substrates, particularly volatile fatty acids, by bentic bacteria. Volatile fatty acids were determined using an HPLC sytem in cojunction with a conductivity detector. At the low eluent strength used 1 μM acetate was detected with ease. Small cores were used in an attempt to maintain the natural partial pressure of hydrogen, an important factor in the control of anerobic metabolism of fatty acids. Although this is preferable to the disturbance of the sediment which occurs if it is resuspended a a slurry, problems are encountered at low substrate concentrations. The time taken for the added substrate to equilibrate in both radial and vertical planes may result in turnover times which vary with the incubation time used. Reduction of the qunatity of added substrate and increased replication may improve the accuracy of the estimates obtained, but more serious consideration must be given to the availability of the substrates to the benthic bacteria.     

Factors influencing the extent and development of the oxic zone in sediments

Dissolved oxygen concentrations in river-sediment porewaters are reported and modelled using a zero-order reaction rate and the Monod equation. After mixing the sediments and allowing settling, the dissolved oxygen profile in the bed-sediment was expected to reach a steady-state rapidly (< 1 h). However changes in the vertical profile of oxygen over a period of 38 days revealed that the penetration of oxygen increased and the dissolved oxygen flux at the interface decreased with time, probably as the oxidation kinetics of organic matter and redox reactions in the sediment changed. Experiments with three contrasting silt and sand dominated sediments (organic matter content between 0.9 and 18%) at two water velocities (ca 10 and 20 cm s^–1) showed that the dissolved oxygen profiles were independent of velocity for each of the sediments. The most important controls on the reaction rate were the organic matter content and specific surface area of the sediment. A viscous diffuse-boundary-layer above the sediment was only detected in the experiments with the silt sediment where the sediment oxygen demand was relatively high. In the coarser sediments, the absence of a diffuse layer indicated that slow oxidation processes in the sediment controlled the dissolved oxygen flux at the interface. The problem of determining a surface reference in coarse sediment is highlighted. The results are discussed with reference to other studies including those concerned with estuarine and marine sediments.     

Analysis of protease digestion patterns in tideland sediments using SDS-PAGE

A method to analyse protein hydrolysis in tideland sediments was developed using sodium lauryl sulphate (SDS)-polyacrylamide gel electrophoresis (PAGE). Bovine serum albumin was used as a substrate and sonication in SDS solution was employed to extract hydrolysed peptides from tideland sediments. By combining these techniques, digested peptides were fractionated reliably on slab gels by SDS-PAGE.Using this method, the protease activities in a tideland were found to be distributed only in the sediment fraction and not in the seawater. The protease activities in sediments were compared among three tidelands in the Seto Inland Sea. Niho tideland, the most polluted of the three tidelands examined, showed the highest levels of protease activity. Peptide cleavage patterns were very similar among the tidelands despite the differences in levels of protease activity, suggesting that the tidelands all contain common types of protease. Furthermore, the properties of proteases in tideland sediments were also characterised using the present method.     

Ecology-types determine physicochemical properties and microbial communities of sediments obtained along the Songhua River

Sediments and their associated microbial communities are a vital part of riverine ecosystems. In order to understand the effects of ecology-types on microbial communities in the riverine sediments, the sediments and water samples were collected from several ecology-types along the Songhua River, and characterized in several ways. We analyzed the microbial communities in the sediments using denaturing gradient gel electrophoresis (DGGE). Furthermore, we determined environmental parameters, such as organic matter, nutrients (total N and P) and particle size distribution. The results revealed that the sediments are grouped by ecology-types along the river, but not by their geographical location. Longitude, latitude and elevation were also partially correlated with microbial community composition. This study suggests that sites of similar ecology-types affect the microbial communities in a similar manner, and result in increased heterogeneity in ecological landscapes.     

A method for the estimation of bacterial biomass and community structure in mangrove-associated sediments

Many recent reports have proposed that certain monocarboxylic fatty acids found in sediments originate in the in situ bacterial population. In this study we have divided the acids derived from bacteria into nine subgroups, each characteristic of a distinct compositional group of bacteria. It is proposed that the abundance of selected marker acids from each bacterial subgroup (chemotype) can be used to estimate the biomass of that chemotype. Conversion factors from acid abundance to bacterial biomass have been estimated using literature data. Since this procedure results in nine biomass parameters, bacterial communities can be compared in terms of both total biomass and chemotype distribution, that is, biomass and community structure. The ability of this procedure to resolve community structure variations is illustrated with the interpretation of the fatty acid profiles of a spatially distributed set of mangrove-associated sediments.     

Benthic fauna bio-irrigation effects on nutrient regeneration in fish farm sediments

Impacts of organic enrichment and a modified benthic fauna community (caused by fish farming) on benthic mineralization rates and nutrient cycling were studied in sediments at one Danish and one Cypriote fish farm. Sediment organic matter concentration and macrofauna community composition were manipulated in microcosms and changes in total benthic metabolism (oxygen consumption, TCO₂ production), anaerobic metabolism (sulfate reduction rates), nutrient fluxes and sediment parameters were followed for a period of 3 weeks. Mineralization rates were found to be highly correlated with irrigation velocities and largest fauna effects were found in the Danish sediments with the large and active irrigating climax species (Nereis diversicolor and Macoma balthica). Eastern Mediterranean climax species (Glycera rouxii and Naineris laevigata) also stimulated mineralization rates but to a smaller extent due to lower irrigation, whereas the opportunistic species (Capitella in Danish sediment and Hermodice carunculata in Cypriote sediment) showed less effect on mineralization. Ammonium and phosphate release increased with increasing irrigation velocities, but much less in Cyprus indicating higher nutrient retention at the ultra-oligotrophic location compared to eutrophic Danish site. Irrigation velocities, and thus mineralization rates, increased by organic matter loading, indicating larger fauna-induced oxidation in enriched environments. The result implies that a change in fauna structure in fish farm sediment towards smaller opportunistic polychaete species with lower irrigation will result in slower mineralization rates and potentially increase accumulation of organic waste products.     

Pollution characteristics of mercury (Hg) in surface sediments of major basins,China

To investigate the pollution status and potential pollution risk of mercury (Hg) in China, surface sediment samples were collected from eight hundred and eighty-one sites, including ten major basins (Songhua River Basin (SRB), Liao River Basin (LRB), Hai River Basin (HRB), Yellow River Basin (YRB), Huai River Basin (HuRB), Yangtze River Basin (YtRB), Pearl River Basin (PRB), Southeastern River Basin (SeRB), Southwestern River Basin (SwRB) and Northwestern River Basin (NwRB)). Results showed that Hg concentrations in sediments of ten basins in China ranged from 0.001 to 8.800 mg/kg, with average ± S.D. value of 0.274 ± 0.675 mg/kg, which was obviously higher than Chinese soil background value (0.038 mg/kg) and Chinese sediment background value (0.040 mg/kg). The mean Hg concentration of ten basins decreased in the order of HRB > YtRB > SRB > PRB > HuRB > SwRB > YRB > SeRB > LRB > NwRB. Moreover, it was found that the Hg concentrations in the sediments of LRB, YtRB, PRB, SeRB and SwRB were partly driven by their total organic carbon (TOC) contents, while the effect of pH on the distribution of Hg was not obvious. The Hg concentration data were also compared with those got in other periods (1994–2015) to obtain the general variation tendency of Hg level. It was recorded that Hg concentrations in HRB have remained on high levels for a long history, while Hg contamination situation in YRB after 2004 has potentially turned to be better. The results of pollution assessment by sediment quality assessment guidelines (SQGs), contamination factor (CF), geoaccumulation index (I_geo) and potential ecological risk (E_i) suggested that YRB and HRB were the most seriously polluted river basins among the ten basins. It is urgent of constructing SQGs in China to scientifically evaluate the Hg pollution in the future.     

Determination of the gram-positive bacterial content of soils and sediments by analysis of teichoic acid components

Many gram-positive bacteria form substituted polymers of glycerol and ribitol phosphate esters known as teichoic acids. Utilizing the relative specificity of cold concentrated hydroflouric acid in the hydrolysis of polyphosphate esters it proved possible to quantitatively assay the teichoic acid-derived glycerol and ribitol from gram-positive bacteria added to various soils and sediments. The lipids are first removed from the soils or sediments with a one phase chloroform-methanol extraction and the lipid extracted residue is hydrolyzed with cold concentrated hydrofluoric acid. To achieve maximum recovery of the teichoic acid ribitol, a second acid hydrolysis of the aqueous extract is required. The glycerol and ribitol are then acetylated after neutralization and analyzed by capillary gas-liquid chromatography. This technique together with measures of the total phospholipid, the phospholipid fatty acid, the muramic acid and the hydroxy fatty acids of the lipopolysaccharide lipid A of the gram-negative bacteria makes it possible to describe the community structure of environmental samples. The proportion of gram-positive bacteria measured as the teichoic acid glycerol and ribitol is higher in soils than in sediments and increases with depth in both.     

A new index to sort estuarine sediments according to their contaminant content

When dealing with potentially contaminated regions, simple tools are needed to identify in a fast and first approach the areas of the highest concern. In this work we propose a new, intuitive, easy-to-use and versatile tool to accomplish this task. This tool comprises the calculation of a new cumulative index, the Normalised-and-Weighted Average Concentration (NWAC) and its visualisation on a map of the area investigated using a colour based code. The NWAC is a cumulative index that is calculated for each sample using the concentration of freely selected contaminants present in that sample. The NWACs can be used to sort samples in a scale from 0 to 10 according to their contaminant content. A colour-based visualisation of the NWACs on a map facilitates an easy identification of the areas of higher concern within the studied region. The methodology has been exemplified in a case study, for example, the estuary of the Nerbioi-Ibaizabal River (Bilbao, Basque Country) using a representative set of sediments and their metals and metalloids content. The NWAC values obtained have been compared to the corresponding values of mERMq, another cumulative index of general acceptance and frequently used to estimate the toxicity of sediments, with comparable results.     

Dissolved and particulate organic matter in contrasting Zostera marina (eelgrass) sediments

The influence of seagrass Zostera marina on sediment characteristics was examined in two contrasting sediments, one organic-rich and one organic-poor. The presence of plants leads to reduced sediment redox potential in both sediment types compared to bare sediment with the largest effects in the organic-poor sediment. Z. marina stimulated the sulfate reduction rates in organic-poor sediment with ∼50% and higher pools of dissolved organic carbon (DOC) were found. In contrast, sulfate reduction rates were lower in vegetated compared to bare sites in the organic-rich sediment. Despite a low contribution of dissolved carbohydrate (DCHO) to the DOC pool (<5%), the seagrass vegetation was responsible for an increase of ∼50% in DCHO pools with a peak in the root zone suggesting that Z. marina supplied DCHO to the pore waters. The Z. marina meadows also enhanced the contribution of particulate carbohydrate (PCHO) to sedimentary particulate organic carbon (POC) pools by 6-14% compared to bare sediment. Although the PCHO pools were higher in organic-rich than organic-poor sediments, the analyses of carbohydrate composition revealed that three groups of neutral sugars including glucose, galactose and mannose+xylose were the major compounds of PCHO and contributed with >60% to sedimentary carbohydrate pools at both sites. Only glucose showed depletion with depth in the vegetated sediments, whereas the percentage of ribose and rhamnose increased indicating a selective degradation of labile carbohydrates in the meadows. Galactose and mannose+xylose appeared to represent a refractory part of carbohydrate that remained after degradation of the more labile components. The sugar content was rather constant with depth at the bare organic-rich sediment indicating that only recalcitrant carbohydrate pools were buried. There was less difference in the PCHO composition profiles between vegetated and bare organic-poor sediments.     

沈阳西部污灌渠沉积物中污染物积累与生态毒性研究

沉积物样品采自沈阳西部污水灌渠的上、中、下游．进行了污染物(重金属和矿物油)含量分析和生态毒性试验．结果表明,所有沉积物中均有污染物的积累,矿物油含量在400～12500mg·kg^-1,重金属Cd为1．6～27．2mg·kg^-1．沉积物对植物和蚯蚓都有明显的毒性效应．种子发芽根伸长抑制率为10％～60％．蚯蚓试验14d和28d死亡率分别为0%～70％和0%～85％．体重增长抑制率为-21．9%～17．7％和-18．6%～37．0%．研究表明,长期污灌导致河道沉积物中污染物积累和较强生态毒性．沉积物作为重要的污染源,其污染物迁移与释放对地下水和土壤具有潜在危害．