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701.
702.
沈阳市丁香地区土壤重金属污染及生态风险评价 总被引:9,自引:0,他引:9
在丁香公园内设置5个点对土壤中的Cr、Hg、As、Cd、Pb进行含量分析,并用单因子指数法评价土壤污染程度,用Hakanson生态风险指数法对土壤潜在的生态风险进行评价。结果表明,丁香湖公园局部地区Hg、As、Cd超过GB15618-1995一级标准;从总的污染程度看,各污染物从大到小的顺序为:Cd>Hg>Pb>As>Cr,各点位从大到小顺序为:大转弯村>小韩村>丁香苗圃>丁香湖湖区>丁香园小区;从总的潜在生态危险程度看,各个点位的风险程度从高到低依次为:大转弯村>小韩村>丁香苗圃>丁香湖湖区>丁香园小区。 相似文献
703.
生物表面活性剂强化植物修复重金属污染土壤的可行性 总被引:1,自引:1,他引:1
利用有机配体强化植物修复重金属污染土壤是提高植物修复效果的常用措施.但大部分有机配体会引起二次污染而限制了其在土壤重金属修复中的应用。如果能将生物表面活性剂强化植物修复不仅会弥补这一不足.而且还能降低费用。生物表面活性剂在重金属污染土壤修复中的应用以及生物表面活性剂去除重金属的机理表明,将其强化植物修复是完全可行的,并且可以增加植物细胞膜透性,更好地促进植物对重金属的吸收。 相似文献
704.
Warne MS Heemsbergen D McLaughlin M Bell M Broos K Whatmuff M Barry G Nash D Pritchard D Penney N 《Environmental pollution (Barking, Essex : 1987)》2008,156(3):707-714
Laboratory-based relationships that model the phytotoxicity of metals using soil properties have been developed. This paper presents the first field-based phytotoxicity relationships. Wheat (Triticum aestivum L.) was grown at 11 Australian field sites at which soil was spiked with copper (Cu) and zinc (Zn) salts. Toxicity was measured as inhibition of plant growth at 8 weeks and grain yield at harvest. The added Cu and Zn EC10 values for both endpoints ranged from approximately 3 to 4760 mg/kg. There were no relationships between field-based 8-week biomass and grain yield toxicity values for either metal. Cu toxicity was best modelled using pH and organic carbon content while Zn toxicity was best modelled using pH and the cation exchange capacity. The best relationships estimated toxicity within a factor of two of measured values. Laboratory-based phytotoxicity relationships could not accurately predict field-based phytotoxicity responses. 相似文献
705.
Laboratory experiments assessed how bioaccumulation of weathered p,p′-DDE from soil and humic acid (HA) chemistry are affected by interactions between the plants Cucurbita pepo ssp. pepo and ssp. ovifera and the earthworms Eisenia fetida, Lumbricus terrestris, and Apporectodea caliginosa. Total organochlorine phytoextraction by ssp. pepo increased at least 25% in the presence of any of the earthworm species (relative to plants grown in isolation). Uptake of the compound by ssp. ovifera was unaffected by earthworms. Plants influenced earthworm bioaccumulation as well. When combined with pepo, p,p′-DDE levels in E. fetida decreased by 50%, whereas, in the presence of ovifera, bioconcentration by L. terrestris increased by more than 2-fold. Spectral analysis indicated a decrease in hydrophobicity of HA in each of the soils in which both pepo and earthworms were present. However, HA chemistry from ovifera treatments was largely unaffected by earthworms. Risk assessments of contaminated soils should account for species interactions, and SOM chemistry may be a useful indictor of pollutant bioaccumulation. 相似文献
706.
Sunflower, alfalfa, fodder radish and Italian ryegrass were cultivated in severely As-Cd-Co-Cu-Pb-Zn-contaminated pyrite waste discharged in the past and capped with 0.15 m of unpolluted soil at Torviscosa (Italy). Plant growth and trace element uptake were compared under ploughing and subsoiling tillages (0.3 m depth), the former yielding higher contamination (∼30%) in top soil.Tillage choice was not critical for phytoextraction, but subsoiling enhanced above-ground productivity, whereas ploughing increased trace element concentrations in plants. Fodder radish and sunflower had the greatest aerial biomass, and fodder radish the best trace element uptake, perhaps due to its lower root sensitivity to pollution. Above-ground removals were generally poor (maximum of 33 mg m−2 of various trace elements), with Zn (62%) and Cu (18%) as main harvested contaminants. The most significant finding was of fine roots proliferation in shallow layers that represented a huge sink for trace element phytostabilisation.It is concluded that phytoextraction is generally far from being an efficient management option in pyrite waste. Sustainable remediation requires significant improvements of the vegetation cover to stabilise the site mechanically and chemically, and provide precise quantification of root turnover. 相似文献
707.
Land use conversion is an important factor influencing the carbon gas exchange between land and atmosphere. The effect of land use conversion on soil organic carbon mineralization and microbial function is important for soil organic carbon sequestration and stability. This research studied the effects of land use conversion on soil chemical properties, organic carbon mineralization and microbial community structure after two years of conversion from double rice cropping (RR) to maize-maize (MM) and soybean-peanut (SP) double cropping systems in southern China. The results showed that soil pH significantly decreased by 0.50 (MM) and 0.52 (SP, P = 0.002), and dissolved organic carbon significantly increased by 23%- 35% (P = 0.016). No significant difference was found in soil organic carbon mineralization rate with the land use conversion, though the accumulated mineralization decreased after 13 days of incubation (P = 0.019). Land use conversion from paddy to upland significantly changed soil microbial community structure. The total PLFAs, bacterial, gram-positive bacterial (G+), gram-negative bacterial (G-) and actinomycetic PLFAs decreased significantly (P < 0.05), the ratio of fungal PLFAs to bacterial PLFAs (F/B) increased significantly (P = 0.006). But no significant differences in microbial groups were found between MM and SP. The accumulated mineralization at the beginning period of the incubation were significantly positively correlated with soil actinomycetic PLFAs (P = 0.034). After 13 days of incubation, soil F/B showed a positive correlation with the accumulated mineralization (P = 0.004). However, soil microbial community structure(P = 0.014)and total PLFAs(P = 0.033)showed a positive correlation with the accumulated mineralization after 108 days of incubation. Our results indicated that after conversion from paddy soils to drained soils, soil pH and total nitrogen are the key factors regulating the variations in soil microbial community structure and biomass, and then influencing soil organic carbon mineralization. 相似文献
708.
Zhenyu Yang Rong Xing Wenjun Zhou Lizhong Zhu 《Frontiers of Environmental Science & Engineering》2020,14(3):41
709.
710.
Tipping E Poskitt JM Lawlor AJ Wadsworth RA Norris DA Hall JR 《Environmental pollution (Barking, Essex : 1987)》2011,159(12):3721-3729
The median total mercury concentration in 898 UK rural topsoils, sampled between 1998 and 2008, was 0.095 μg g−1. Approximate adjustment for unreactive metal produced an estimate of 0.052 μg g−1 for reactive Hg. The highest concentrations were in the north and west, where organic-rich soils with low bulk densities dominate, but the spatial pattern was quite different if soil Hg pools (mg m−2) were considered, the highest values being near to the industrial north of England and London. Possible toxic effects of Hg were best evaluated by comparison with soil Critical Limits expressed as ratios of Hg to soil organic matter, or soil solution Hg2+ concentrations, estimated by chemical speciation modelling. Only a few percent of the rural UK soils showed exceedance, and this also applied to rural soils from the whole of Europe. UK urban and industrial soils had higher Hg concentrations and more cases of exceedance. 相似文献