Revisiting Dust and Soil Ingestion Rates Based on Hand-to-Mouth Transfer

Soil ingestion rates calculated using a tracer-based mass balance approach may carry considerable study errors, insensitivities, and “artefacts” of analysis that result in significant uncertainty. These same soil ingestion rates are often used as surrogates for dust ingestion rates. Therefore, a more direct and mechanistic method was developed to estimate soil and dust ingestion rates. The soil and dust ingestion rates were calculated using measures of: particle loading to indoor surfaces; fraction transferred to the hands; hand surface area; fraction of hand surface area that may be mouthed or contact food; frequency of hand-to-mouth events, amount dissolved by saliva; and exposure time. Adapted specifically for the Canadian context, estimated mean indoor dust ingestion rates range from 2.2 mg/d for teenagers to 41 mg/d for toddlers; mean soil ingestion rates range from 1.2 mg/d for seniors to 23 mg/d for children. Combined soil and dust ingestion rates ranged from 3.8 mg/d for seniors to 61 mg/d for toddlers. These ingestion rates are lower than values adopted by most agencies. These ingestion rates are mechanistic, can be adjusted on a site-specific basis, can be modified into an hourly rate and are presented as a more realistic alternative to traditional mass balance approaches.

[Supplementary materials are available for this article. Go to the publisher's online edition of Human and Ecological Risk Assessment to view the free supplementary files.]     

Sediment-Associated Phototoxicity to Aquatic Organisms

Phototoxicity is a two to greater than 1000-fold increase in chemical toxicity caused by ultraviolet radiation (UV), which has been demonstrated in a broad range of marine and freshwater fish, invertebrates, and other aquatic organisms in water column exposures. Field collected sediments containing polycyclic aromatic hydrocarbons (PAHs) and other contaminants are phototoxic to sediment-dwelling organisms in laboratory tests, but in situ or field investigations of phototoxicity have not been reported. Sediment provides a pathway for the bioaccumulation of phototoxic chemicals through contact with and ingestion of bedded and suspended sediment, and maternal transfer, but risks are uncertain. Risks from sediment-associated phototoxicity will be greatest in areas of both high contaminant exposure (e.g., surficial and suspended sediments in harbors, outfall areas, and spill sites), and high UV exposure (e.g., high optical clarity or shallow depths). Organisms and life-stages most at risk will be those translucent to UV that inhabit the photic zone and near shore areas, but benthic organisms may have generally low UV exposure because of life history and morphological characteristics. Site-specific assessments are needed to characterize risks both spatially and temporally because of heterogeneous sediment contamination and large differences in species sensitivity and exposure pathways.     

Determination of Trace Phthalic Acid Monoesters in Sediments and Soils by GC-MS

A simple procedure for determining trace phthalic acid monoesters (PAMs) in sediments/soils was developed. The method used ultrasonic extraction, silylation derivatization, and GC-MS. After ultrasonic extraction, the supernatants were reextracted with dichloromethane, silylated, and did not require further clean-up before GC-MS analysis. Effects of parameters, such as extraction solvents, pH of water as extraction solvent and sediment/soil properties, on the recovery of PAMs were studied. Five sediments from Tianjin city and one red soil from Jiangxi province were used. The results showed that organic carbon (OC) content played an important role in the recovery of PAMs. The optimal extraction solvent for sediments/soils with >1% of OC content and high CEC was 0.01 M HCl aqueous solution and pure water was better for sediments/soils with <1% of OC content. In 5 g sediment/soil sample (dry weight), the method detection limit (MDL) was below 0.04 ng/g for mono-n-butyl phthalate (MBP) and 0.02 ng/g for mono-(2-ethylhexyl)-phthalate (MEHP). Average recoveries of MBP and MEHP were 81.6%?105.2% and 76.0%?95.6%, respectively, with relative standard deviations ≤ 6.6%. MBP and MEHP in the sediment and soil samples studied were detected at levels of 9.2–57.1 and 13.0–166.7 ng/g, respectively.     

The use of turbidimeters in suspended sediment research

Accurate characterisation of the trend in suspended sediment concentration in streams throughout runoff events requires a sampling interval much shorter than the one hour typically used. For logistical reasons this is not usually feasible, so continuously recording turbidimeters offer a potential alternative. The variety of correlations and relationships between sediment concentration and turbidity reported in the literature is not surprising in view of the many confounding effects present in natural stream systems. Data from five sites in a small forested catchment indicated variability in the turbidity-suspended sediment concentration relationship, but improvements were obtained by considering the effects of very fine sediment and background water colour. Throughout runoff events variations in sediment properties, organic acids concentration and turbulence can occur. It is concluded that a good linear relationship between turbidity and suspended sediment concentration should not necessarily be expected and any observed hysteresis could actually help explain erosion and transport processes. The detail and continuity of data generated by turbidimeters provides the opportunity for greater understanding of storm sediment dynamics, however, calibration requires careful consideration of site characteristics.     

Biasing Factors for Simple Soil Ingestion Estimates in Mass Balance Studies of Soil Ingestion

Soil ingestion estimates from mass balance soil ingestion studies can be used in Monte Carlo Risk assessment. We develop and describe a simulation model based on four mass balance soil ingestion studies that enables food ingestion, soil ingestion, and transit time to be mimicked. We use the simulation to evaluate potential biases that exist in current estimates of the distribution of daily soil ingestion in children (constructed from subject specific average daily estimates). The simulation identifies the importance of the study duration on the bias in the upper percentile soil ingestion estimates, indicating that the 95% soil ingestion estimate may be positively biased by over 100%. Misspecification of play areas for soil sampling is shown to have no biasing effect, and absorption of trace elements in food of up to 30% is shown to bias the soil ingestion distribution by less than 20 mg/d. The results, based on Al and Si trace element estimates, define the limits of previously published soil ingestion estimates, and provide insight for future study design and estimation methods.     

Harbour and coastal sediment chemistry and toxicity: a preliminary assessment of dredging activities

In a project to assess the environmental impact of dumping contaminated harbour material in a coastal marine area of the Northern Tyrrhenian Sea, sediments from different sites (harbour, dumping and uncontaminated sites) were sampled in December 1993 and February 1994. In order to evaluate sediment quality, concentrations of heavy metals (Cd, Pb, Cr and Hg) and polycyclic aromatic hydrocarbons (PAHs) were determinated and toxicity tests were carried out using the sea urchin Paracentrotus lividus. Interstitial water and the sea water overlying sediments (bedded phase and suspended phase) were tested for their effects on fertilization and embryogenesis. Sediment texture was also considered. Metal concentrations, particularly cadmium content, and PAH total concentrations, in harbour sediments were generally higher than in offshore samples. No significant reductions in fertilization were observed. However, effects on the embryonic development were evident and interstitial water toxicity was shown to be greater than either bedded or suspended exposures.     

Estimation of dust ingestion rates in units of surface area per day using a mechanistic hand-to-mouth model

In order to provide dust ingestion rates that can aid the interpretation of indoor dust measurements as surface loadings (i.e., units of µg/m²), dust ingestion rates have been developed for various age groups on a surface area basis. The approach incorporates a hand-to-mouth mechanistic model that was previously developed to estimate dust ingestion rates in units of mg/day. The analysis resulted in estimated mean dust intakes that range from 0.0032 m²/d (for teenagers) to 0.061 m²/d (for toddlers) at residential settings assumed to be comprised of 50% hard surfaces and 50% soft surfaces. Intake rates assuming 100% hard surfaces and 100% soft surfaces are also presented. The values provided are intended to assist the interpretation of indoor dust investigations where substance content in dust is presented as surface loadings rather than bulk dust concentrations.     

Erosion and sediment yield in the Atna river basin

Variability in suspended sediment transport and its relation to erosion processes in two different catchments within the Atna river basin are discussed on the basis of 14 years of data collection. The upper Atna catchment is a headwater system covering 157 km². Extensive glacifluvial deposits are the main sediment source of the river. Sediment transport in the upper Atna during 1988–2001 ranged from 79.4 t to 13,200 t. The extreme upper value was due to an extreme rainflood in 1996. Suspended sediment concentrations varied from less than 1.0 mg l^?1 to a maximum of 2023.8 mg l^?1. There was no correlation between water discharge and suspended sediment concentration. Despite a fairly constant volume of total runoff, sediment concentrations remained at a high level during the first years after extreme floods, and then decreased over several more years. The complicated pattern of short term and long term variations in suspended sediment concentration and load was explained in terms of channel changes and variations in exposure of the sedimentary deposits to fluvial erosion. The catchment of the lower Atna drains an area of 672 km². Concentrations of inorganic suspended sediments were found to vary between <1.0 and 897 mg l^?1, with only a weak correlation to water discharge. The suspended sediment transport per year ranged from a minimum value of 574 t in 1991 to 60,651 t per year in 1995, the extreme flood year. The mean annual transport for all the years was 6271 t. The sediment transported in the lower Atna is derived from the same types of sources as in the upper catchment, but the sediments are supplied from a larger area. Grain size distribution analyses indicate that the transported sediments in upper Atna have a sand content of 10 to 65% compared to 2–20% in lower Atna. The transport of particulate organic matter in the upper and lower Atna catchments amounted to 9.8% and 12.6% of the total load, respectively.     

Sediment quality assessment: status and outlook

This paper is a synthesis of the 44 presentations at the First International Symposium on Sediment Quality Assessment (Sweden, August 1994). The paper includes Initial Premises, Sediments, Tools (with particular emphasis on bioassays), Strategies and Challenges. Major testable hypotheses are proposed as follows (ranging in complexity, recognizing differences apparent at the Symposium in level of expertise and knowledge): (1) there is no single perfect method of sediment assessment, there are only tools in the toolbox; (2) significant sediment pollution (contamination resulting in adverse biological effects) comes from non-anthropogenic sources; (3) artificial sediments will provide future reference comparisons; (4) knowledge of suspended sediments is required to understand bedded sediments; (5) ammonia and/or hydrogen sulfide cannot explain all sediment toxicity, in particular non-acute responses; (6) subcellular (e.g., genetic) responses are a research tool, not yet appropriate for monitoring or assessment; (7) although the effects of sediment storage cannot be predicted, non-toxic and highly toxic sediments are less affected by prolonged storage than are moderately toxic sediments; (8) sediment ingestion is a more important route of exposure than pore water for some organisms; (9) water column organisms and aqueous exposures should not be used for whole-organism sediment tests; (10) validation of sediment bioassays is not always simple or possible. Two major conclusions are: (i) generalizations are not [yet] possible regarding sediment quality; (ii) correctly assessing sediment quality is primarily a function of the correct reference comparison.     

Assessment of Trace Metals Contamination in the Suspended Matter and Sediments of a Semi-enclosed Mediterranean Gulf

This study investigates the distribution of heavy metals in the suspended particulate matter and the sediments of Kavala Gulf, located in Northern Greece. Particulate trace metals were determined in accordance to water column physicochemical parameters. Metals in sediments were related to the textural characteristics, the organic matter, and carbonate contents of surficial sediments. Results illustrated that the diverse human coastal activities influence the distribution of particulate and sediment metal concentrations, since lower trace metal levels were detected along the western (tourism) and eastern (aquaculture) coast, while increased values were observed at the central (urban and industrial). Overall, particulate metals show moderately low levels compared to other similar sites, with the exception of Ni and Cd depicting local peaks along the industrial coastal zone. Significantly increased levels for particulate lead (123.1 μg/g) and chromium (113.9 μg/g) were detected at the sites near the industrial zone. Direct effluents from a fertilizer plant appeared responsible for the increased Pb, Cr, and Cd levels, while the increased values in Zn, Cu, and Hg appear related to phosphogypsum leaching. Sediment contamination assessment indicated that the Kavala Gulf is characterized by clean to marginally polluted sediments, with moderately severe pollution levels along the urban coastline.     

A Guide to Interpreting Soil Ingestion Studies. 2. Qualitative and Quantitative Evidence of Soil Ingestion

Abstract

Four major studies have attempted to qualitatively and quantitatively assess the extent of soil ingestion in children using the soil tracer methodology. The validity of the estimates of soil ingestion of each study was reevaluated in light of the inherent strengths and limitations of study design and/or execution as well as via a novel methodology to estimate the soil recovery variance of each tracer which then lead to the estimation of soil ingestion detection limits of each tracer for studies performing mass-balance analyses. Based on these analyses it is concluded that the Binder et al. (1986) and Van Wijnen et al. (1990) studies provide no convincing evidence to support qualitative and quantitative estimates of soil ingestion due to inherent limitations of their respective study designs. The Davis et al. (1990) and Calabrese et al. (1989) studies displayed convincing qualitative evidence of soil ingestion. However, the results indicate that the median soil ingestion estimates of Davis et al. were less reliable than those of Calabrese et al. The range of detection limits vary according to the tracer and the assumption of acceptable precision in recovery estimation. The minimum detection level of soil ingestion in children in the Calabrese et al. study with a variance in recovery of 100% ± 20% was 16 mg day^?1 based on Zr.

These findings are of particular regulatory significance since they provide: (1) a method of assessing the level of detection inherent in soil ingestion studies, (2) a reevaluation of the major soil ingestion studies in light of new methodology, and (3) guidance for future studies so that detection capacity can now be included in the presentation of study findings.     

Use of microcosms to determine persistence of Escherichia coli in recreational coastal water and sediment and validation with in situ measurements

AIMS: To determine the persistence of the faecal indicator organism Escherichia coli in recreational coastal water and sediment using laboratory-based microcosms and validation with in situ measurements. METHODS AND RESULTS: Intact sediment cores were taken from three distinct coastal sites. Overlying estuarine water was inoculated with known concentrations of E. coli and decay rates from both overlying water and sediment were determined following enumeration by the membrane filtration method at fixed time intervals over a 28-day period. It was demonstrated that E. coli may persist in coastal sediment for >28 days when incubated at 10 degrees C. Escherichia coli survival was found to have an inverse relationship with temperature in both water and sediment. In general the decay rate for E. coli was greater in water than in sediment. Small particle size and high organic carbon content were found to enhance E. coli survival in coastal sediments in the microcosms. CONCLUSIONS: Results of this microcosm study demonstrated the more prolonged survival of E. coli in coastal sediments compared with overlying water, which may imply an increased risk of exposure because of the possible resuspension of pathogenic micro-organisms during natural turbulence or human recreational activity. SIGNIFICANCE AND IMPACT OF THE STUDY: A more accurate estimate of exposure risk has been described which may subsequently be used in a quantitative microbial risk assessment for recreational coastal waters.     

Sediment–Water Surface Area Along Rivers: Water Column Versus Benthic

Aquatic ecosystems have two distinct zones: the water column and benthic zone. Although the benthic zone has received considerable attention, recent studies have found the water column capable of accounting for a majority of whole ecosystem processes in rivers. The relative role of these zones inevitably varies across a size continuum of rivers, from headwaters to large transcontinental systems. A fundamental question in aquatic science is where along this size continuum do ecosystem processes potentially shift from occurring largely in the benthic zone to largely in the water column? Sediment structures the physical template of the benthic and water column zones of rivers and the contact area between water and sediment mediates ecological, geochemical, and physical processes. High concentrations of suspended sediments are hypothesized to cause a shift from benthic to water column dominance in rivers. We developed an analytical model for the contact area between surface water and all sediment particles in benthic and water column volumes. The model was implemented with empirical data along the main stem of major US rivers. The ratio of water column to benthic sediment contact area scaled as a power function of watershed area. There was more sediment–water contact area in the water column than the benthic zone in rivers equal to or greater than 5th to 9th order depending on the river basin. This suggests material processing could be occurring largely in the water column in rivers greater than 5th order. However, dams and variation in discharge caused rivers to oscillate between water column and benthic dominance over time and space.     

Simulation study on water quality based on sediment release flume experiment in Lake Taihu, China

Sediments have a significant influence on the overlying water, and nutrient release from sediments is an important source for lake eutrophication, particularly in shallow lakes. Sediment resuspension is primarily driven by wind-induced currents. In this research, the correlation between release rate of suspended sediment and flow velocity was studied, and an experiment on hydrodynamic forces was conducted in a rectangle flume using water and sediments collected from three sites in Lake Taihu, a eutrophic lake in China. It was shown that the starting velocities of sediment in Lake Taihu at three different incipient standards gained from the experiment were 15, 30, and 40 cm s⁻¹ and the release rate of suspended sediment could reach up to 643.4, 5377.1, and 13980.5 g m⁻² d⁻¹, respectively. Based on the experiment, a water quantity and quality numerical model of wind-induced current with sediment pollution for Lake Taihu was developed. The model was calibrated and validated by applying it to the study of the water quality of Lake Taihu. The calculated values were generally in good agreement with field observations, which indicated that the developed model could represent the dynamics of sediment resuspension to a certain extent. This study provides a new approach and a practical tool for planning and management policy and operations to protect the water quality and ecosystems of shallow lakes.     

Potential nitrogen and carbon processing in a landscape rich in milldam legacy sediments

Recent identification of the widespread distribution of legacy sediments deposited in historic mill ponds has increased concern regarding their role in controlling land–water nutrient transfers in the mid-Atlantic region of the US. At Big Spring Run in Lancaster, Pennsylvania, legacy sediments now overlay a buried relict hydric soil (a former wetland soil). We compared C and N processing in legacy sediment to upland soils to identify soil zones that may be sources or sinks for N transported toward streams. We hypothesized that legacy sediments would have high nitrification rates (due to recent agricultural N inputs), while relict hydric soils buried beneath the legacy sediments would be N sinks revealed via negative net nitrification and/or positive denitrification (because the buried former wetland soils are C rich but low in O₂). Potential net nitrification ranged from 9.2 to 77.9 g m^?2 year^?1 and potential C mineralization ranged from 223 to 1,737 g m^?2 year^?1, with the highest rates in surface soils for both legacy sediments and uplands. Potential denitrification ranged from 0.37 to 21.72 g m^?2 year^?1, with the buried relict hydric soils denitrifying an average of 6.2 g m^?2 year^?1. Contrary to our hypothesis, relict hydric layers did not have negative potential nitrification or high positive potential denitrification rates, in part because microbial activity was low relative to surface soils, as indicated by low nitrifier population activity, low substrate induced respiration, and low exoenzyme activity. Despite high soil C concentrations, buried relict hydric soils do not provide the ecological services expected from a wetland soil. Thus, legacy sediments may dampen N removal pathways in buried relict hydric soils, while also acting as substantial sources of NO₃ ^? to waterways.     

生态恢复对流域水沙演变趋势的影响——以北洛河上游为例

黄土高原生态环境恶劣,水土流失严重。选择退耕还林(草)程度非常显著的陕北吴旗县所在北洛河上游为研究区,探讨黄土高原丘陵沟壑区水土流失治理及大幅度退耕背景下流域水、沙等生态要素的演变规律,分析人类活动的影响贡献程度,为黄土高原生态治理及环境效应分析提供理论依据。结果表明:在1963—2009年期间年降雨量没有显著变化背景下,同时期流域年径流量和年输沙量均呈现极显著减少趋势,年均减少率分别为0.28 mm/a和180 t km-2a-1,其突变时间均发生在1979和2002年,具有很好的同步性。与1979年前相比,20世纪70—80年代水土流失综合治理以及1999年后退耕还林(草)的事件背景,使汛期和平水期径流量逐时段减少,而枯水期径流量反而持续增加。输沙量呈持续性大幅度减少态势,且其减少程度远大于径流量的变化程度。水土流失综合治理和退耕还林(草)工程实施等人类活动,对流域径流量减少的影响贡献程度分别为38.2%和51.4%,对输沙量减少的影响程度分别为74.7%和86.7%。研究结果提示,黄土高原生态环境的大幅度改善在区域尺度上已经表现出一定程度上削洪补枯的水文效应特征,以及林草措施减水更减沙的良好生物治理效果。     

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations

The measurement of sediment-water exchange of gases and solutes in aquatic sediments provides data valuable for understanding the role of sediments in nutrient and gas cycles. After cores with intact sediment-water interfaces are collected, they are submerged in incubation tanks and kept under aerobic conditions at in situ temperatures. To initiate a time course of overlying water chemistry, cores are sealed without bubbles using a top cap with a suspended stirrer. Time courses of 4-7 sample points are used to determine the rate of sediment water exchange. Artificial illumination simulates day-time conditions for shallow photosynthetic sediments, and in conjunction with dark incubations can provide net exchanges on a daily basis. The net measurement of N₂ is made possible by sampling a time course of dissolved gas concentrations, with high precision mass spectrometric analysis of N₂:Ar ratios providing a means to measure N₂ concentrations. We have successfully applied this approach to lakes, reservoirs, estuaries, wetlands and storm water ponds, and with care, this approach provides valuable information on biogeochemical balances in aquatic ecosystems.     

Sorption and release of radiocaesium from particulate matter of the Baltic coastal zone

Laboratory expriments have demonstrated that radiocaesium can be released in different proportions from Baltic sediments, depending on the type and origin of sediment, contact time and solid-to-liquid phase ratio. Rapidly accumulating sediments in areas affected by river discharge have much higher percentage of exchangeable radiocaesium than slowly accumulating marine sediments. The latter have been shown to {uptake radiocaesium from overlying sea water at high suspended loads. Pronounced radiocaesium gradients at sediment-water interface in Gda\'nsk Bay can be explained by either diffusion from pore water or desorption from sediment particles uprised by waves and/or bottom currents, or a combination of both. Desorption is likely to decrease with age of the sediment.     

Enhanced particle-feeding capacity of corals on turbid reefs (Great Barrier Reef, Australia)

Reef corals occur across a wide range of habitats, from offshore clear waters to nearshore sediment-laden environments. This study tests the hypothesis that corals from turbid nearshore areas have greater capacity to utilise suspended sediment as a food source than conspecifics from less turbid and midshelf areas. The hypothesis was tested on two common and widespread coral species on the Great Barrier Reef (Pocillopora damicornis and Acropora millepora). The particle clearance rates of samples from more turbid reefs were two-fourfold those of conspecifics from less turbid and midshelf reefs. Rates of sediment ingestion were generally a linear function of sediment load indicating no significant saturation within the concentration range of 1–30 mg dry weight l⁻¹. Estimated assimilation efficiency of particulate ¹⁴C varied between 50 and 80%, and was maximised for midshelf A. millepora at the lowest sediment concentration, suggesting that heterotrophy is more efficient in oligotrophic habitats. Based on feeding-response curves, assimilation efficiencies, and published records of ambient particle concentrations, representatives of these species on turbid inshore reefs are 10–20 times more heterotrophic on suspended sediment than their conspecifics on less turbid and midshelf reefs. Accepted: 7 September 1999