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981.
Oil gelling agents are widely used in emergency response of marine oil spills. However, the biological toxicity of oil gelling agents is not well understood. This research aimed to evaluate the environmental safety of oil gelling agents used for rapid removal and cleanup of marine oil spills. We used luminescent bacteria (Acinetobacter sp. Tox2 and Acinetobacter sp. RecA) combined with exposure experiment using marine medaka (Oryzias melastigma) juveniles to detect the acute toxicity and genotoxicity of 10 oil gelling agents. As a result, a certain level of acute toxicity was detected from the oil gelling agent FOA and GMN-01 (the toxicity equivalent to 0.067 mg/L and 0.084 mg/L of HgCl2, respectively), and a certain level of genotoxicity was detected from the oil gelling agent NORSOREX (the toxicity equivalent to 0.307 mg/L of MMC) by the luminescent bacteria test. However, no obvious acute toxicity or genotoxicity was detected from the above three oil gelling agents in fish-exposure experiments. Our results suggest that the 10 oil gelling agents have no obvious acute toxicity or genotoxicity to higher organisms (including marine medaka). The luminescent bacteria test is more sensitive in detecting biological toxicity of oil gelling agents. This study provides a reference for environmental safety evaluation of the oil gelling agents used in the cleaning up of the marine oil spills.  相似文献   
982.
983.
垃圾填埋场渗滤液溶解性有机质特性及其去除技术综述   总被引:2,自引:0,他引:2  
垃圾填埋场渗滤液所含物质种类繁多,理化特性复杂,且随填埋时间等条件而变化.本文综合分析了垃圾渗滤液溶解性有机质的组成特征、结构特征及随年代变化特征.针对垃圾渗滤液难降解有机质的特性而研发的处理技术包括物化法、高级氧化法和微电解法等,并在实际工程中得到应用.随着越来越严格的渗滤液排放要求,溶解性有机质的去除应充分考虑投资的经济、运行的稳定性和可靠性.  相似文献   
984.
The nitrogen balance can serve as an indicator of the risk to the environment of nitrogen loss from agricultural land. To investigate the temporal and spatial changes in agricultural nitrogen application and its potential threat to the environment of the Haihe Basin in China, we used a database of county-level agricultural statistics to calculate agricultural nitrogen input, output,surplus intensity, and use efficiency. Chemical fertilizer nitrogen input increased by 51.7% from1990 to 2000 and by 37.2% from 2000 to 2010, concomitant with increasing crop yields.Simultaneously, the nitrogen surplus intensity increased by 53.5% from 1990 to 2000 and by16.5% from 2000 to 2010, presenting a continuously increased environmental risk. Nitrogen use efficiency decreased from 0.46 in 1990 to 0.42 in 2000 and remained constant at 0.42 in 2010,partly due to fertilizer composition and type improvement. This level indicates that more than half of nitrogen inputs are lost in agroecosystems. Our results suggest that although the improvement in fertilizer composition and types has partially offset the decrease in nitrogen use efficiency, the environmental risk has still increased gradually over the past 20 years, along with the increase in crop yields and nitrogen application. It is important to achieve a better nitrogen balance through more effective management to significantly reduce the environmental risk,decrease nitrogen surplus intensity, and increase nitrogen use efficiency without sacrificing crop yields.  相似文献   
985.
以罗布泊"大耳朵"地区为研究区域,利用石墨炉原子吸收分光光度计(GF-990)和火焰原子吸收分光光度计(AAS-990)分析测试了沉积物中Pb、Cu、Ni和Mn元素的总量,并测定了沉积物中有机质的含量,运用SPSS软件分析了各重金属总量与有机质之间的相互关系。结果表明:罗布泊"大耳朵"地区盐壳层沉积物中Pb含量的变化范围在2.57~58.63 mg/kg,Cu含量的变化范围在6.33~39.65 mg/kg,Ni含量的变化范围在5.55~46.33 mg/kg,Mn含量的变化范围在46.33~1474.60 mg/kg;除Pb的垂直分布随着深度的增加其含量减少并趋于稳定外,重金属Cu、Ni和Mn的总量在各剖面垂直方向上大部分呈波折多峰行分布,分布趋势差异较大;重金属Pb、Cu、Ni和Mn与有机质都存在显著相关性。  相似文献   
986.
对钦杭结合带首次发现的加里东期榴闪岩进行了详细的年代学、矿物学和变质作用研究。结果表明,榴闪岩的变质时代为454±4Ma,经历了早期角闪岩相进变质、中期榴辉岩相峰期变质和晚期角闪岩相退变质三个阶段,具顺时针P-T-t轨迹。早期角闪岩相进变质作用阶段的矿物共生组合为角闪石+斜长石+石英,温压条件分别为719℃~795℃和7.56Kpa~8.30Kpa;中期榴辉岩相峰期变质作用阶段的矿物共生组合为石榴子石+绿辉石(后期退变为透辉石+钠长石)±石英,温压条件分别为668℃~821℃和26.42Kpa~33.46Kpa;晚期角闪岩相退变质作用阶段的矿物共生组合为石榴子石+角闪岩+斜长石±石英(即榴闪岩),相应的温压条件分别为611℃~854℃和4.76Kpa~9.30Kpa。结合前人资料推断,区域内加里东期可能经历了榴辉岩相超高压变质→高温麻粒岩相退变质→角闪岩相退变质的演化过程。钦杭结合带首次厘定出加里东期超高压变质作用,表明华夏和扬子两大陆块碰撞拼合发生在加里东期。  相似文献   
987.
Flower-, wire-, and sheet-like MnO2-deposited diatomites have been prepared using a hydrothermal method with Mn(Ac)2, KMnO4 and/or MnSO4 as Mn source and diatomite as support. Physical properties of the materials were characterized by means of numerous analytical techniques, and their behaviors in the adsorption of chromium(VI) were evaluated. It is shown that the MnO2-deposited diatomite samples with different morphologies possessed high surface areas and abundant surface hydroxyl groups (especially the wire-like MnO2/diatomite sample). The wire-like MnO2/diatomite sample showed the best performance in the removal of Cr(VI), giving the maximum Cr(VI) adsorption capacity of 101 mg/g.  相似文献   
988.
Flower-, wire-, and sheet-like MnO2-deposited diatomites have been prepared using a hydrothermal method with Mn(Ac)2, KMnO4 and/or MnSO4 as Mn source and diatomite as support. Physical properties of the materials were characterized by means of numerous analytical techniques, and their behaviors in the adsorption of chromium(VI) were evaluated. It is shown that the MnO2-deposited diatomite samples with different morphologies possessed high surface areas and abundant surface hydroxyl groups (especially the wire-like MnO2/diatomite sample). Thewire-like MnO2/diatomite sample showed the best performance in the removal of Cr(VI), giving the maximum Cr(VI) adsorption capacity of 101 mg/g.  相似文献   
989.
A key step in sludge treatment is sludge dewatering. However, activated sludge is generally very difficult to be dewatered. Sludge dewatering performance is largely affected by the sludge moisture distribution. Sludge disintegration can destroy the sludge structure and cell wall, so as change the sludge floc structure and moisture distribution, thus affecting the dewatering performance of sludge. In this article, the disintegration methods were ultrasound treatment, K2FeO4 oxidation and KMnO4 oxidation. The degree of disintegration (DDCOD), sludge moisture distribution and the final water content of sludge cake after centrifuging were measured. Results showed that three disintegration methods were all effective, and K2FeO4 oxidation was more efficient than KMnO4 oxidation. The content of free water increased obviously with K2FeO4 and KMnO4 oxidations, while it decreased with ultrasound treatment. The changes of free water and interstitial water were in the opposite trend. The content of bounding water decreased with K2FeO4 oxidation, and increased slightly with KMnO4 oxidation, while it increased obviously with ultrasound treatment. The water content of sludge cake after centrifuging decreased with K2FeO4 oxidation, and did not changed with KMnO4 oxidation, but increased obviously with ultrasound treatment. In summary, ultrasound treatment deteriorated the sludge dewaterability, while K2FeO4 and KMnO4 oxidation improved the sludge dewaterability.  相似文献   
990.
Measurements of surface O3 and carbon monoxide(CO) were made from September 2009 to August 2011 at Dangxiong(30.48°N, 91.10°E, 4187 m a.s.l.), a remote highland site in a southern valley of the Nyainqêntanglha Mountains in the Tibetan Plateau, China. The monthly mean O3 mixing ratio ranged from 29.1 to 51.4 ppb, with an average of 38.5 ppb, and the maximum value was observed in May. The average diurnal cycle of O3 concentration showed a minimum in early morning and a maximum in the afternoon, with a broader "high platform" from the late morning to the late afternoon, and resembled that of surface wind speed. The concentration of surface O3 was highly significantly correlated with tropospheric column O3 over the regions surrounding Dangxiong and with that of surface O3 observed at a site north of the Nyainqêntanglha Mountains, suggesting a good regional representativeness of surface O3 at Dangxiong. In the afternoon when stronger winds blew, surface air showed distinct features of free-atmospheric air, with higher O3, lower CO, and lower relative humidity(RH). The negative O3–CO and O3–RH correlations in most months indicate a significant influence of air masses from the free troposphere. Trajectory analysis suggests that air masses originating from the south of the site make a negative net contribution to surface O3 and a positive contribution to CO and humidity, and those from the northwest sector contribute conversely to the respective quantities.  相似文献   
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