Uptake of lead by coen from roadside soil samples

Abstract

The uptake of Pb by young, greenhouse grown corn plants from roadside soil samples was found to be not only dependent upon the total amount of Pb in the soil, but also upon the amount of Pb in the soil relative to the soils capacity to sorb Pb. This is in agreement with the uptake of Pb by corn grown on soils amended with PbCl₂, although plant accumulation of Pb from roadside soils was much less than from PbCl₂ amended soils at comparable Pb concentrations. The use of crushed limestone as a road building material which results in high soil pH values next to the roadside is probably responsible for the reduced plant availability of Pb in the roadside soils.     

Microbial diversity and soil functions

Soil is a complex and dynamic biological system, and still in 2003 it is difficult to determine the composition of microbial communities in soil. We are also limited in the determination of microbially mediated reactions because present assays for determining the overall rate of entire metabolic processes (such as respiration) or specific enzyme activities (such as urease, protease and phosphomonoesterase activity) do not allow any identification of the microbial species directly involved in the measured processes. The central problem posed by the link between microbial diversity and soil function is to understand the relations between genetic diversity and community structure and between community structure and function. A better understanding of the relations between microbial diversity and soil functions requires not only the use of more accurate assays for taxonomically and functionally characterizing DNA and RNA extracted from soil, but also high‐resolution techniques with which to detect inactive and active microbial cells in the soil matrix. Soil seems to be characterized by a redundancy of functions; for example, no relationship has been shown to exist between microbial diversity and decomposition of organic matter. Generally, a reduction in any group of species has little effect on overall processes in soil because other microorganisms can take on its function. The determination of the composition of microbial communities in soil is not necessary for a better quantification of nutrient transformations. The holistic approach, based on the division of the systems in pools and the measurement of fluxes linking these pools, is the most efficient. The determination of microbial C, N, P and S contents by fumigation techniques has allowed a better quantification of nutrient dynamics in soil. However, further advances require determining new pools, such as active microbial biomass, also with molecular techniques. Recently investigators have separated ¹³C‐ and ¹²C‐DNA, both extracted from soil treated with a ¹³C source, by density‐gradient centrifugation. This technique should allow us to calculate the active microbial C pool by multiplying the ratio between labelled and total DNA by the microbial biomass C content of soil. In addition, the taxonomic and functional characterization of ¹³C‐DNA allows us to understand more precisely the changes in the composition of microbial communities affected by the C‐substrate added to soil.     

酸碱调控对泥浆反应去除土壤中多环芳烃的影响研究

采用摇瓶试验模拟研究了酸碱调控对泥浆反应去除污染土壤中多环芳烃的影响,结果表明,泥浆反应对污染土壤中的多环芳烃具有一定的去除效果,长期污染土壤中多环芳烃的去除率为10.6% ~ 20.7%,模拟污染土壤中的去除率为37.4% ~ 42.1%;酸碱调控对不同性质的多环芳烃的去除影响不同,整体上看,酸性条件有利于高环（五环和六环）多环芳烃的去除,而中性条件有利于低环（三环和四环）多环芳烃的去除。在实际修复中,根据污染土壤中多环芳烃的组成进行适当的酸碱调控,可以促进污染土壤的快速修复。     

The removal of butachlor from soil by wastewater-derived Rhodopseudomonas marshes

Butachlor is a systemic selective pre-emergent herbicide most commonly used to control grasses and broadleaf weeds. Residual butachlor in soil can have harmful ecotoxological effects and remediation is, therefore, important. Effects of Rhodopseudomonas marshes in wastewater effluent on biorestoration of butachlor in soil were investigated. Over a time period of one day, butachlor induced EthB gene expression to synthesize cytochrome P450 monooxygenase which led to the successful bioremediation of the herbicide. Residual organics in wastewater effluent provided sufficient carbon sources for continued growth of R. marshes beyond one day.     

蚯蚓与黑麦草相互作用对土壤中荧蒽去除的影响

Earthworms can promote the bioremediation of contaminated soils through enhancing plant growth and microorganism development. The individual and combined effects of earthworms and ryegrass (Lolium multiflorum Lam.) on the removal of fluoranthene from a sandy-loam alluvial soil were investigated in a 70-d microcosm experiment. The experiment was set up in a complete factorial design with treatments in four replicates: without earthworms or ryegrass (control, CK), with earthworms only (E), with ryegrass only (P), and with both earthworms and ryegrass (EP). The residual fluoranthene, microbial biomass C, and polyphenol oxidase activity in the soil changed significantly (P<0.01) with time. In general, the residual concentration of fluoranthene in the soil decreased sharply from 71.8-88.7 to 31.7-37.4 mg kg 1 in 14 d, and then decreased gradually to 19.7-30.5 mg kg 1 on the 70th d. The fluoranthene concentration left in the soil was the least with both earthworms and ryegrass, compared to the other treatments at the end of the experiment. Half-life times of fluoranthene in the E, P, and EP treatments were 17.8%-36.3% smaller than that of CK. More fluoranthene was absorbed by earthworms than ryegrass. However, the total amounts of fluoranthene accumulated in both the ryegrass and earthworms were small, only accounting for 0.01%-1.20% of the lost fluoranthene. Therefore, we assumed that microbial degradation would play a dominant functional role in fluoranthene removal from soil. We found that earthworms significantly increased microbial biomass C and polyphenol oxidase activity (P<0.01) in the presence of ryegrass at the end of the experiment. Furthermore, microbial biomass C and polyphenol oxidase activity were significantly (P<0.05) and negatively related to the residual fluoranthene concentration. This implied that earthworms might promote the removal of fluoranthene from soil via stimulating microbial biomass C and polyphenol oxidase activity.     

An electrohydrodynamic technique for removal of moisture from soil samples

Abstract

Removal of moisture from soil is of great importance in research, and any attempt in improving the existing soil drying techniques would be desirable. Evaporation rates of water from six soil samples of varying organic matter content were determined gravimetrically while exposed simultaneously to bipolar ions produced by corona electrodes and a thallium‐204 beta‐ray source. These devices produced ion fluxes of 2.63 × 10¹² positive and 2.68 × 10¹² negative ions cm^‐2 s^‐1 in air at the soil surface. Argon (A), dry air, and nitrogen (N) gases were used as ionization media for moisture loss studies. The rate of moisture loss was found to be the lowest in N. The water vapour fluxes from the exposed soil samples were enhanced by a factor of at least three compared to control samples under ambient conditions.     

Temperature-dependent oxide removal from manganese- and iron oxide-coated soil redox bars

Purpose

Soil temperature is a fundamental parameter affecting not only microbial activity but also manganese (Mn^III,IV) and iron (Fe^III) oxide reduction rates. The relationship between Mn^III,IV oxide removal from oxide-coated redox bars is missing at present. This study investigated the effect of variable soil temperatures on oxide removal by Mn^III,IV and Fe^III oxide-coated redox bars in water-saturated soil columns in the laboratory.

Materials and methods

The Mn coatings contained the mineral birnessite, whereas the Fe coatings contained a mixture of ferrihydrite and goethite. Additionally, platinum (Pt) electrodes designed to measure the redox potential (E_H) were installed in the soil columns, which were filled with either a humic topsoil with an organic carbon (C_org) content of 85 g kg^?1 (pH 5.8) or a subsoil containing 2 g C_org kg^?1 (pH 7.5). Experiments were performed at 5, 15, and 25 °C.

Results and discussion

Although elevated soil temperatures accelerated the decrease in E_H after water saturation in the topsoil, no E_H decreases regardless of soil temperature occurred in the subsoil. Besides soil temperature, the importance of soil organic matter as an electron donor is highlighted in this case. Complete removal of the Mn^III,IV oxide coating was observed after 28, 14, and 7 days in the soil columns filled with topsoil at 5, 15, and 25 °C, respectively. Along the Fe redox bars, Fe^III reducing conditions first appeared at 15 °C and oxide removal was enhanced at 25 °C because of lower E_H, with the preferential dissolution of ferrihydrite over goethite as revealed by visual differences in the Fe^III oxide coating. Oxide removal along redox bars followed the thermodynamics of the applied minerals in the order birnessite > ferrihydrite > goethite.

Conclusions

In line with Van’t Hoff’s rule, turnover rates of Mn^III,IV and Fe^III oxide reduction increased as a result of increased soil temperatures. Taking into account the stability lines of the designated minerals, E_H-pH conditions were in accordance with oxide removal. Soil temperature must therefore be considered a master variable when evaluating the oxide removal of redox bars employed for the monitoring of soil redox status.

     

Microbial populations and phenolic acids in soil

Populations of bacteria, fungi and actinomycetes in Portsmouth A₁- and B,-soil material were affected in different ways by repeated enrichment with ferulic, p-coumaric, p-hydroxybenzoic or vanillic acids. Responses varied with type of soil material and phenolic acid, phenolic acid concentration, and inorganic nutrient status of the soil. Populations changed more frequently in B₁- than in A₁-soil material. Phenolic acids were readily metabolized by microorganisms, sometimes without detectable population changes, when adequate mineral nutrients were present. Induction of enzymes or selection of organisms capable of degrading individual phenolic acids were clearly evident. Results imply that microbial activity in bioassay systems should be defined for allelopathic studies, particularly when results from various bioassay systems are to be compared     

Microbial indicators for soil quality

The living soil is instrumental to key life support functions (LSF) that safeguard life on Earth. The soil microbiome has a main role as a driver of these LSF. Current global developments, like anthropogenic threats to soil (e.g., via intensive agriculture) and climate change, pose a burden on soil functioning. Therefore, it is important to dispose of robust indicators that report on the nature of deleterious changes and thus soil quality. There has been a long debate on the best selection of biological indicators (bioindicators) that report on soil quality. Such indicators should ideally describe organisms with key functions in the system, or with key regulatory/connecting roles (so-called keystone species). However, in the light of the huge functional redundancy in most soil microbiomes, finding specific keystone markers is not a trivial task. The current rapid development of molecular (DNA-based) methods that facilitate deciphering microbiomes with respect to key functions will enable the development of improved criteria by which molecular information can be tuned to yield molecular markers of soil LSF. This review critically examines the current state-of-the-art in molecular marker development and recommends avenues to come to improved future marker systems.     

Microbial induced nitrous oxide emissions from an arable soil during winter

Nitrous oxide (N₂O) release rates were measured from an fertilized and unfertilized plot on silty loam (Gleyic Luvisol) cropped with winter wheat. Rates were estimated using a closed soil cover box technique throughout a continuous investigation period of 12 months. The 12 months of investigation were separated into the cropping period (March to November) and the winter period (December to February). Soil management and all N-applications were made during the cropping period. The application of 220 kg N to the soil induced significantly higher N₂O losses throughout the cropping season compared to the unfertilized soil. No significant differences were found during winter, where 70% of the annual N₂O emissions were found. The temporal changes of the N₂O emission rates on both soils were highly correlated (r=0.96; P≤0.001), and could be attributed to temporal changes in soil temperature (r=0.65; P≤0.01) resulting from freezing and thawing cycles. In order to decide whether the N₂O production can be attributed to microbial or non-microbial processes in soil, the time courses of the N₂O emissions from a γ-ray sterilized and a non-sterilized soil were compared in a laboratory experiment, where the freezing and thawing cycles were simulated according to field conditions. The results indicated, that microbial processes were responsible for N₂O production in thawing and even frozen soils.     

Optimization of arsenic and pentachlorophenol removal from soil using an experimental design methodology

Purpose

In this study, a soil-washing process was investigated for arsenic (As) and pentachlorophenol (PCP) removal from polluted soils. This research first evaluates the use of chemical reagents (HCl, HNO₃, H₂SO₄, lactic acid, NaOH, KOH, Ca(OH)₂, and ethanol) for the leaching of As and PCP from polluted soils.

Materials and methods

A Box–Behnken experimental design was used to optimize the main operating parameters for soil washing. A laboratory-scale leaching process was applied to treat four soils polluted with both organic ([PCP] _i ?=?2.5–30 mg kg^?1) and inorganic ([As] _i ?=?50–250 mg kg^?1, [Cr] _i ?=?35–220 mg kg^?1, and [Cu] _i ?=?80–350 mg kg^?1) compounds.

Results and discussion

Removals of 72–89, 43–62, 52–68, and 64–98 % were obtained for As, Cr, Cu, and PCP, respectively, using the optimized operating conditions ([NaOH]?=?1 N, [cocamidopropylbetaine] _i ?=?2 % w w^?1, t?=?2 h, T?=?80 °C, and PD?=?10 %).

Conclusions

The use of NaOH, in combination with the surfactant, is efficient in reducing both organic and inorganic pollutants from soils with different levels of contamination.     

Microbial response of an acid forest soil to experimental soil warming

 Effects of increased soil temperature on soil microbial biomass and dehydrogenase activity were examined on organic (O) horizon material in a low-elevation spruce-fir ecosystem. Soil temperature was maintained at 5  °C above ambient during the growing season in the experimental plots, and soil temperature, moisture, microbial biomass, and dehydrogenase activity were measured during the experiment. An incubation study was also conducted under three temperature regimes, 5, 15, and 25  °C, and under four moisture regimes of 20, 120, 220, and 320% to further evaluate these environmental factors on dehydrogenase activity and microbial biomass. Soil moisture content and microbial biomass controls were significantly lower (30% and 2 μg g^–1 soil, respectively) in the heated plots during the treatment period, suggesting that moisture content was important in controlling microbial biomass. In the incubation study, temperature appeared more important than moisture in controlling microbial biomass and dehydrogenase activity. Increasing temperature between 5  °C and 25  °C resulted in significant decreases in microbial biomass and dehydrogenase activity. Received: 7 August 1998     

茶园土壤中氟去除模型研究

在单因素试验基础上,采用二次回归正交旋转组合设计对土壤中的氟去除进行了优化,建立了土壤氟潜在去除率(y)与EDTA浓度(x1)、溶液pH值(X2)、表面活性剂(SDS)投加量(x3)和土壤含氟量(x4)4个因素间的正交回归模型:Y=62.92642-6.80471x1+2.85102x2+3.74368x3-6.65557x12-4.74638x42+2.70625x1x4+2.70625x2x3.从模型推知,当EDTA浓度0.085 mol/L、溶液pH值8.9、SDS投加量21.70 mL和土壤含氟量650.65 mg/kg时,土壤氟潜在去除率最大,达71.70%,验证结果与模型值相近.     

Crop production impacts on soil phosphorus removal and soil test levels

An 8-year field study documented the impact of tillage, crop rotations, and crop residue management on agronomic and soil parameters at Brookings, South Dakota. The greatest annual proportion of above-ground biomass phosphorus (P) removed was from the grain (78–87% of total) although crop residue removed some P as well. Greater above-ground total biomass P (grain P + crop residue P) was removed from corn than from soybean and spring wheat crops mainly due to the greater corn grain biomass harvested. Cumulative above-ground biomass P removal was greatest for the corn-soybean rotation (214 kg P ha^?1), while it was lowest for the soybean-wheat rotation (157 kg P ha^?1). Tillage treatments within crop rotation or residue management treatments did not influence annual or cumulative P removal rates. Olsen extractable soil orthophosphate-P levels declined consistently through time from a mean of 40 µg g^?1 (2004) to 26 µg g^?1 (2011). Biomass P removal was calculated to be 15.7 ha^?1 yr^?1 to decrease Olsen extractable soil orthophosphate-P levels by 1 µg g^?1 yr^?1 over 8 years of the study.     

Microbial diversity assembled from series-diluted suspensions of diseasesuppressive soil determines pathogen invasion resistance

Dear Editor,Soil microbial biodiversity loss caused by agricultural intensification, climate change, and the application of chemical fertilizer has become a serious problem that threatens humans (Wall et al., 2015). One phenomenon responsible for economic and food security issues is soil-borne diseases(Fisher et al., 2012), which were reported to be associated with microbial diversity loss (Shen et al., 2013;Fu et al.,2017).     

An initial study on soil wettability effects during entrapped LNAPL removal by surfactant flooding in coarse-grained sand media

Purpose

Non-ideal or fractional wettability conditions may exist at field sites. It was hypothesized that fractional wettability could cause larger entrapped LNAPL saturations and unexpected soil interactions during surfactant remediation. Soil wettability effects during entrapped LNAPL recovery by surfactant flooding in coarse-grained sand were investigated through a comparative study. The main objective was to identify the impacts of soil wettability on LNAPL removal via submicellar concentration surfactant flooding to remobilize entrapped LNAPL.

Materials and methods

A baseline for comparison was established by testing an ideal water-wet soil (silica sand) along with a fractionally wet soil. Two LNAPLs were tested: LNAPL from a contaminated field site and heptane, which represented an ideal lab-grade fluid. Contact angle, interfacial tension, capillary pressure–saturation, and column tests were performed to characterize wettability and identify the effects of soil wettability during entrapped LNAPL recovery. Two anionic surfactants were used for the column experiments: sodium dodecyl-benzene-sulfonate and a field site anionic surfactant. To further investigate the effects of LNAPL contact time within the soil, columns tests were performed at two different LNAPL contact times.

Results and discussion

Contact angle measurements and column tests conducted with the field LNAPL revealed its potential to establish non water-wet wettability conditions. Column test results indicated that fluid entrapment was independent of fluid type, and the wettability and contact time conditions studied. Entrapped LNAPL saturations after water flooding were approximately 19 %. Entrapped LNAPL removal by mobilization occurred at the predetermined submicellar surfactant concentration (0.5 g/L) with a maximum removal of 43 %. Entrapped LNAPL removal from fractionally wet columns was higher in comparison to water-wet columns and was found to increase with contact time.

Conclusions

Entrapped LNAPL saturations after water imbibition were not impacted by the wettability conditions studied. The fractionally wet soil behaved differently during the surfactant-flood; higher LNAPL removal was achieved suggesting that non-ideal wettability had a positive impact. The presence of NAPL-wet mineral grains might have favored pore scale interactions causing NAPL redistribution and increasing NAPL-surfactant solution interfacial areas contributing to LNAPL removal. Pore scale studies and subsequent testing is recommended to further this study’s findings.     

Microbial and non-biological decomposition of chlorophenols and phenol in soil

The aerobic and anaerobic degradation of phenol and selected chlorophenols was examined in a clay loam soil containing no added nutrients. A simple, efficient procedure based on the high solubility of these compounds in 95% ethanol was developed for extracting phenol and chlorophenol residues from soil. Analysis of soil extracts with UV spectrophotometry showed that phenol,o-chlorophenol,p-chlorophenol, 2,4-dichlorophenol, 2,6-dichlorophenol and 2,4,6-trichlorophenol were rapidly degraded, whilem-chlorophenol, 3,4-dichlorophenol, 2,4,5-trichlorophenol and pentachlorophenol were degraded very slowly by microorganisms in aerobically-incubated soil at 23°C. Both 3,4,5-trichlorophenol and 2,3,4,5-tetra chlorophenol appeared to be more resistant to degradation by aerobic soil microorganisms at 23°C. None of the compounds examined were degraded by microorganisms in anaerobically-incubated soil at 23°C. Direct microscopic observation revealed that phenol and selected chlorophenols stimulated aerobic and to a lesser extent, anaerobic microbial growth in soil, and aerobic soil bacteria were responsible for the degradation of 2,4-dichlorophenol in aerobically-incubated soil at 23°C. Phenol,o-chlorophenol,m-chlorophenol,p-chlorophenol and 2,4-dichlorophenol underwent rapid non-biological degradation in sterile silica sand. Non-biological decomposition contributed, perhaps substantially, to the removal of some chlorophenols from sterile aerobically-incubated soil and both sterile and non-sterile anaerobically-incubated soil.     

Effect of lead on soil respiration and dehydrogenase activity

The effect of added Pb on the respiration and dehydrogenase activity of two sandy soils, a clay soil and a peat soil, (all with different physico-chemical properties), was studied.A concentration of 375 μg Pb· g^? inhibited the respiration of the sandy soil by ca. 15%, 1500 μg Pb· g^?ca. 50%. In the clay soil 1500 μg Pb· g^? caused a 15% reduction in respiration. The inhibition of respiration in the sandy soil was still ca. 30% 40 months after the addition of Pb. Respiration of the peat soil was not affected by even 7500 μg Pb· g^?.Dehydrogenase activity was affected by Pb in a similar way to soil respiration. In the sandy soil a considerable reduction occurred, while in the clay and peat soils dehydrogenase activity was not reduced.It was concluded, that a relationship exists between the inhibitory effects of Pb and the buffering capacity of the soil as expressed by its cation-exchange capacity. Because of these different effects of the same Pb concentration on the various soil types, no single value for the permitted concentration of lead pollution in soil could be established.     

Bioavailability of zinc and lead from a contaminated soil amended with pine bark-goat manure compost

The distribution in soil and plant uptake of zinc (Zn) and lead (Pb) as influenced by pine bark-goat manure (PBG) compost additions were investigated from the soils artificially contaminated with Zn or Pb ions using maize (Zea mays L.) as a test crop. Soils were amended with four rates of pine bark-goat manure compost (0, 50, 100, and 200 tons ha^?1) and four rates (0, 300, 600 and 1200 mg kg^?1) of Zn or Pb. Maize was planted and grown for 42 days. At harvest, plants samples were analyzed for Zn and Pb concentration. Soils samples were analyzed for pH, extractable and diethylene triamine pentaacetic acid (DTPA) extractable Zn and Pb. Extractable Zn and Pb was lower in PBG compost amended soils than in unamended soils and steadily declined with increasing amount of compost applied. The extractable fraction for Zn dropped by 62.2, 65.0 and 44.6% for 300, 600 and 1200 mg Zn kg^?1, respectively when 200 t ha^?1 of PBG compost was applied. Metal uptake by maize plants were directly related to the rate of applied heavy metal ions with greater concentrations of metals ions found where metal ions were added to non-amended soils.