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22741. 题目: High-efficiency degradation of organic pollutants with Fe, N co-doped biochar catalysts via persulfate activation In this study, the Fe, N co-doped biochar (Fe-N-BC) was prepared by pyrolyzing wheat straw, urea and iron salts and used to activate persulfate (peroxydisulfate, PS) for organic contaminant degradation. Iron oxide doping not only introduced magnetism into the biochar for easy separation, but also influenced its catalytic ability for PS activation. In the Fe-N-BC/PS system, almost all acid orange (AO7) was removed within 90 min with an apparent rate constant (kobs) of 0.114 min-1, which was almost 37 times larger than that of pure N-BC (0.003 min−1). Factors influencing the removal of AO7 were investigated, including PS concentration, catalyst dosage, and initial pH. The Fe-N-BC/PS system had high removal efficiencies for various organic contaminants and showed high resistance to inorganic anions in aquatic environments. The radical quenching studies, electron paramagnetic resonance (EPR) measurements, and electrochemical analyses verified that the mechanism of AO7 degradation in the Fe-N-BC/PS system included both radical and non-radical pathways involving the generation of •OH, SO4−•, O2−•, 1O2, and electron transfer. Additionally, persistent free radicals (PFRs) on the catalysts also related to their catalytic efficiencies. These results demonstrated that the Fe-N-BC/PS system had the potential for wastewater treatment applications. | |||||
22742. 题目: The effect of biochar on soil-plant-earthworm-bacteria system in metal(loid) contaminated soil Increasing biochar is applied to the metal(loid) contaminated soil. However, effects of biochar on the soil-plant-earthworm-bacteria ecosystem, especially on the gut microbes of soil animals, remain largely unknown and require further research. Here, sewage sludge biochar (SSBC) and rice straw biochar (RSBC) were used in metal(loid) contaminated soils to investigate the available metal(loid) change in soils and the impact on the metal(loid) bioaccumulation in the plant and earthworm. Moreover, effects of biochar amendments on the gut bacteria of earthworms were determined by using high throughput sequencing. Our results showed that RSBC amendments had a significant suppression on the availability of cadmium, but significantly increased arsenic availability in soils (P < 0.05). Compared with the control, the significant reduction of arsenic and cadmium accumulation was observed in plant with biochar amendments. High metal(loid) concentrations were observed in the body tissues of earthworms, in which the highest bioaccumulation factor of cadmium was 18.12 in Metaphire. californica. The earthworm gut bacteria, with high abundances of Firmicutes (39.36%), Actinobacteria (23.69%) and Proteobacteria (13.02%), was significantly different from the microbe from the soil. RSBC had more significant effect on the bacterial community of earthworm gut than SSBC. Taken together, this work indicated thatbiochar amendments could decrease concentrations of arsenic and cadmium in plant, reduce the potential risk of metal(loid)s into the food chain, and shed light on the biogeochemical behaviour of biochar in the soil-plant-earthworm-bacteria ecosystems. | |||||
22743. 题目: Interactions between the ice algae Fragillariopsis cylindrus and microplastics in sea ice High concentrations of microplastics have been found in sea ice but the mechanisms by which they get captured into the ice and which role ice algae might play in this process remain unknown. Similarly, we do not know how the presence of microplastics might impact the colonization of sea ice by ice algae. To estimate the ecological impact of microplastics for Polar ecosystems, it is essential to understand their behaviour during ice formation and possible interactions with organisms inhabiting sea ice. In this study we tested the interaction between the ice algae Fragillariopsis cylindrus and microplastic beads with and without sea ice present and, in a third experiment, during the process of ice formation. With sea ice present, we found significantly less algae cells in the ice when incubated together with microplastics compared to the incubation without microplastics. However, during ice formation, the presence of microplastics did not impact the colonisation of the ice by F. cylindrus cells. Further, we observed a strong correlation between salinity and the relative amount of beads in the water and ice. With increasing salinity of the water, the relative amount of beads in the water decreased significantly. At the same time, the relative amount of beads in the ice increased significantly with increasing ice salinity. Both processes were not influenced by the presence of F. cylindrus. Also, we found indications that the presence of algae can affect the amount of microplastic beads sticking to the container walls. This could indicate that EPS produced by ice algae plays a significant role in surface binding properties of microplastics. Overall, our results highlight that the interactions between algae and microplastics have an influence on the uptake of microplastics into sea ice with possible implications for the sea ice food web. | |||||
22744. 题目: Archaeoanthrosol formation in the Brazilian semiarid Multiple waves of dispersion populated South America throughout the late Pleistocene and early Holocene. The oldest rock art and artifacts in Caatinga are dated from 10,000 BP. Besides that, there is no register of ancient activities in soils in Caatinga. Four pedons were taken, described and classified in sites with a high number of artifacts littering the surface and/or rock art. Five more pedons were described to represent soil without anthropic influence. Soils are shallow and transition between horizons was predominantly clear or abrupt. Anthrosols in Caatinga have value and chroma similar to the anthropic horizons described in Amazonian dark earths. The pedons are strongly acid to slightly alkaline and predominantly have base saturation above 50% in all horizons. Anthrosols in Caatinga have up to 6 and 544 times, respectively, more soil organic carbon and phosphorus compared to adjacent soils without anthropic influence. Besides illite and kaolinite, apatite and calcite compose the clay and silt fractions and confirm the human influence in soil formation. Radiocarbon and thermoluminescence dating indicate that Anthrosols in Caatinga are contemporaneous to the majority of Amazonian dark earths. | |||||
22745. 题目: Mass, nutrients and dissolved organic carbon (DOC) lateral transports off northwest Africa during fall 2002 and spring 2003 | |||||
22746. 题目: Geochemical signatures of transgressive shale intervals from the 811 Ma Fifteenmile Group in Yukon, Canada: Disentangling sedimentary redox cycling from weathering alteration Despite iron and trace element proxies informing much of our insight into Earth's oxygenation history, the processes that controlled their accumulation and distribution in ancient sedimentary environments are not fully understood. Furthermore, deciphering between primary, depositional signals and oxidative weathering alteration poses a substantial challenge to reconstructing Earth's redox history using its sedimentary record. Here, we present a multi-proxy geochemical investigation of three transgressive shale intervals from the ca. 811 Ma Reefal assemblage (upper Fifteenmile Group) in Yukon, Canada to help resolve these issues. Systematic stratigraphic trends from low to high FeHR/FeT and FeT/Al compositions across shale intervals represent shoaling of a discrete redoxcline that separated oxygenated surface waters from anoxic, ferruginous deep waters during marine transgression. In some cases, these trends are followed by a symmetric fall, which represents a full transgressive-regressive cycle of the redoxcline. The high proportion of glauconite to total illite indicate short-term oscillating redox conditions as the redoxcline migrated across the sediment-water interface during relative sea-level rise. These conditions invigorated dissimilatory iron reduction (DIR) within anoxic sediment pore waters, which released Fe(II) into the overlying water column where it was oxidized to iron oxy(hydr)oxide and shuttled downslope. High rates of DIR within sediment replete with highly reactive iron oxy(hydr)oxide and organic matter removed isotopically light, bio-available iron, rendering the residual sediment depleted in FeT/Al relative to the detrital baseline and enriched in 56Fe. The low iron content of the detrital flux to the basin (Fe/Al ∼ 0.3) rendered the sediment susceptible to changes in its bulk δ56Fe composition by modification of its authigenic components alone and enabled fractionation from DIR to drive bulk-rock δ56Fe values up to 0.8‰. Anomalously high concentrations of redox-sensitive elements in three samples (up to 5792 ppm Cr, 586 ppm Mn, 726 ppm Mo, and 3509 ppm Ni) and their relative distribution patterns show similarities to co-enrichment due to particulate shuttling within a weakly restricted basin. However, SEM-EDS element maps and large-area BSE image mosaics show the remains of framboidal pyrite ghosts with secondary enrichment of redox-sensitive elements. Thus, these geochemical trends in redox-sensitive trace metals most likely reflect mobilization and re-accumulation following pyrite dissolution during outcrop weathering. The low primary pyrite content and local transformation of pyrite iron to iron oxy(hdr)oxide suggest that δ56Fe and FeHR/FeT data were unaltered despite indications of pyrite weathering. Ultimately, this dataset elucidates key aspects of sedimentary redox cycling directly preceding evolutionary milestones and a major perturbation to the global carbon cycle and also provides a template for evaluating the effects of outcrop weathering on commonly used sedimentary redox proxies. | |||||
22747. 题目: The contribution of aqueous catechol-silica complexes to silicification during carbonate diagenesis Pore-filling and carbonate-replacing silica is exceedingly common in carbonates, but the fundamental geochemical mechanisms that drive these silicification reactions during diagenesis remain poorly understood. An existing model has proposed that carbonate silicification proceeds through an interface-coupled dissolution-precipitation reaction, but it lacks a mechanism that enables pore fluids to reach the requisite level of supersaturation with respect to silica to allow nucleation and growth. Here, we present a sequence of batch experiments ranging in duration from 7 to 49 days designed to test the hypothesis that these reactions are facilitated by the formation and destruction of organo-silica complexes during diagenesis. Our results illustrate that the stability of organo-silica complexes is dependent upon the concentration of organic molecules in solution, as well as pH, salinity, and solution redox state. Together, these results allow us to present the following scheme for organo-silica complex mediation of silicification reactions: Firstly, the breakdown of organic matter in the presence of siliceous material creates organo-silica complexes, leading to silica-enriched pore fluids, a process which is enhanced by the anoxic conditions accompanying sediment burial. Then, as environmental conditions evolve (fO2, salinity, light, fCO2, pH…), the stability of the organo-silica complexes diminishes, and the organo-silica complexes break down. Simultaneously, the pore fluids become intensely silica-supersaturated, in direct proportion to the amount of organic material remaining in solution. The resulting supersaturation drives carbonate silicification via the precipitation of silica minerals, a process which is aided by the presence of silica nuclei (such as sponge spicules). This study contributes new data and a conceptual model that will aid in the ongoing quest to understand carbonate silicification reactions and their potential applications in hydrocarbon exploitation and geologic CO2 storage. Moreover, it helps to explain the common association between silica precipitates and organic mineral in the sedimentary rock record. | |||||
22748. 题目: Bradford quantification of Glomalin-Related Soil Protein in coloured extracts of forest soils Glomalin-related soil protein (GRSP) is thought to represent a fraction of recalcitrant organic matter in soil. But it is recognized that the autoclaved-citrate extraction procedure causes the co-extraction of humic substances which interfere (directly and indirectly) with the Bradford colorimetric assay. The aim of this work was to propose a reliable quantification method of GRSP from forest soil, very rich in organic matter and therefore in colour. We estimated the quantities of GRSP in the topsoil (0–10 cm) of 102 French forests using five methods: i) direct calibration, reasoned dilution with colour correction, ii) direct calibration, reasoned dilution but no colour correction, iii) direct calibration, 1:2 dilution, no colour correction, iv) indirect calibration and v) dilution method. Our results concur that the interference caused by the co-extracted compounds is not related simply to either the colour of the extracts or total soil organic matter content. These findings suggest that for improved accuracy of GRSP estimates using the Bradford method, extracts should be diluted, and the pH-specific absorbance of coloured extracts should be subtracted. | |||||
22749. 题目: In-situ nitrogen-doped black TiO2 with enhanced visible-light-driven photocatalytic inactivation of Microcystis aeruginosa cells: synthesization, performance and mechanism A series of nitrogen-doped black TiO2 nanocatalysts were successfully synthesized by a one-step method. It is novel to find that calcination in an N2 atmosphere completed N doping and oxygen vacancies production simultaneously. In contrast, the urea addition as N precursor inhibited the nitrogen incorporation and the oxygen vacancies production. However, it is the sample using urea as N precursor that had the higher visible-light absorption, the narrower bandgap, the more efficient excited charges separation and higher degradation efficiency for removing chlorophyll-a in Microcystis aeruginosa algae cells. Mechanism exploration indicated that the intermediate energy states existed within the bandgap of TiO2, and·O2- and·OH were the dominant radicals responsible for algae cell damage and organic matter degradation. This research will provide additional insight into the roles of N precursors and a calcining atmosphere to improve the photocatalytic activity of nitrogen-doped black TiO2 for algae inactivation and metabolites degradation. | |||||
22750. 题目: Sustainable impact of tartaric acid as electron shuttle on hierarchical iron-incorporated biochar Metal-biochar composite is considered as a promising alternative for future carbocatalysis in environmental decontamination. Nevertheless, unavoidable metal leaching impedes its scaling-up application and remains an environmental concern in the present scientific progress. Herein, a hierarchical Fe biochar (Fe/CBC) derived from cellulose was fabricated via a hydrothermal carbonization coupled with microwave irradiation and NH3 activation. Several exterior organic electron shuttles (i.e., ascorbic acid, oxalic acid, tartaric acid, and hydroquinone) were accommodated onto Fe/CBC to introduce more electroactive functionalities (i.e., C–O and C = O). In particular, comprehensive material characterization was performed to elaborate the physicochemical properties of tartaric acid-treated biochar catalyst (Fe/CBC-TA). Synergies of inherent hierarchical structure, well-developed carbon π-electron network, and accommodated electron shuttle could mitigate the Fe leaching from 2.44 to 0.578 mg L−1 in the peroxymonosulfate (PMS) activation system for catalytic degradation of bisphenol A. Based on the results of scavenging experiments and electron paramagnetic resonance (EPR) analysis, the catalytic mechanisms transformed from a one-phase pathway (mainly •OH) for the Fe/CBC system to a two-phase pathway (first phase: 1O2; second phase: •OH) for the Fe/CBC-TA system. The increased activation energy and improved catalyst recyclability of the Fe/CBC-TA in the redox reaction further pinpointed its environmental sustainability. Overall, this work offers new strategies to fabricate efficient metal-biochar catalyst and insights into its sustainable electrocatalysis. | |||||
22751. 题目: Efficient activation of peroxydisulfate (PDS) by rice straw biochar modified by copper oxide (RSBC-CuO) for the degradation of phenacetin (PNT) In this study, rice straw biochar modified by copper oxide (RSBC-CuO) was successfully fabricated via a hydrothermal method and used as a catalyst for the degradation of organic pollutants by peroxydisulfate (PDS). RSBC-CuO-activated PDS exhibited an outstanding performance on the decomposition of phenacetin (PNT). Electron paramagnetic resonance (EPR) confirmed that the reactive oxygen species (ROS) included SO4−, OH, O2− radicals and singlet oxygen (1O2), which were in charge of the PNT destruction. Scavenger experiments further conformed that 1O2 and O2− played the crucial role in the PNT removal. RSBC-CuO also displayed an excellent stability and reusability. The rate of PNT removal after four consecutive cycles declined slightly. Furthermore, the combination of RSBC-CuO and PDS possessed a universal degradation potential towards various organic pollutants, and the degradation efficiencies of the pollutants such as paracetamol, aniline, p-chlorobenzoic acid, sulfamethazine and 2,4,6-Trichlorophenol reached a range of 86 to 100% within 10 to 30 min. Thus, it is concluded that RSBC-CuO-activated PDS is a novel and feasible approach to the removal of organic contaminants from aqueous solution. | |||||
22752. 题目: Measuring the influence of environmental conditions on dissolved organic matter biodegradability and optical properties: a combined field and laboratory study | |||||
22753. 题目: Formation of Disinfection Byproducts from Algal Organic Matter Exposed to Monochloramine: Effects of Monochloramine Dosages, pH, and Bromide Concentrations | |||||
22754. 题目: Assessing biochar application to immobilize Cd and Pb in a contaminated soil: a field experiment under a cucumber–sweet potato–rape rotation | |||||
22755. 题目: Ni(II) Adsorption on Biochars Produced from Different Types of Biomass | |||||
22756. 题目: Arsenic in groundwater in Paraíba do Sul river, Brazil: sources, hydrogeochemistry, and correlation with redox parameters | |||||
22757. 题目: Spatial distribution, source analysis, and ecological risk assessment of PBDEs in river sediment around Taihu Lake, China | |||||
22758. 题目: Variation of soil dissolved organic carbon under long-term different fertilizations and its correlation with maize yields | |||||
22759. 题目: Improvement on soil structure and water retention after application of industrial organic waste as a crop fertilizer | |||||
22760. 题目: Biochar amendment of stormwater bioretention systems for nitrogen and Escherichia coli removal: Effect of hydraulic loading rates and antecedent dry periods Bioretention systems improve stormwater infiltration and water quality; however, limited total nitrogen (TN) and fecal indicator bacteria (FIB) removal is observed in sand-based bioretention media. In this study, the fate of nitrogen and E. coli in bioretention systems was investigated through batch and column studies using sand media, with and without biochar addition. Variables investigated included biochar characteristics, hydraulic loading rate (HLR) and antecedent dry period (ADP). Total ammonia nitrogen (TAN), dissolved organic carbon (DOC), and E. coli removals were significantly higher in biochar-amended columns due to biochar's high cation exchange capacity and specific surface area. TAN adsorption resulted in increased nitrification during the ADP when aerobic conditions developed. Moisture content data revealed that saturated conditions prevailed toward the bottom of biochar-amended columns for several days, favoring denitrification and TN removal. Biochar amended columns also showed more stable TAN, DOC and E. coli effluent concentrations under varying HLR and ADP. | |||||