氯盐对汞化合物污染土壤热脱附过程的影响

对HgCl₂、HgS、Hg(NO₃)₂·H₂O、HgO、HgSO₄ 5种试剂分别添加MgCl₂、CaCl₂和NaCl 3种氯盐,采用热重分析法进行热挥发性对比研究,以期选择对汞化合物热脱附有促进作用的氯盐,并将其添加到内蒙古2块不同污染场地的汞污染土壤样品(A、B)中,进行低温热脱附修复研究. 结果表明:5种汞化合物试剂热脱附温度由低到高依次为HgCl₂＜HgS＜Hg(NO₃)₂·H₂O＜HgO＜HgSO₄. 在汞化合物中加入MgCl₂、CaCl₂和NaCl后的热重分析发现,MgCl₂对HgS、Hg(NO₃)₂·H₂O、HgO、HgSO₄热脱附过程影响最大,降低了汞化合物热脱附的初始温度. A、B 2个污染土壤样品加入MgCl₂热脱附后,汞的去除率分别从无药剂处理的65.67%、70.74%升至81.35%、84.91%. 表明MgCl₂可以促进汞污染土壤中汞化合物的转化,有利于土壤汞污染的热脱附修复,应用前景较好.      

基于油提取的土壤与沉积物中微塑料的分离方法

微塑料作为一种全球性新兴污染物受到学界与社会的广泛关注.由于土壤和沉积物中的微塑料难以分离提取,目前关于微塑料的研究主要集中于水体中,而关于土壤与沉积物中微塑料的丰度、分布与环境行为尚不清楚,迫切需要一种经济、快速、可靠的前处理手段将微塑料从土壤或沉积物中分离出来进而开展检测与监测工作.油提取法不同于传统密度浮选法,其利用塑料的亲油性,使用植物油代替密度液分离土壤与沉积物中的微塑料.通过油提取法在砂土（二长花岗岩风化层残坡积物）、壤土（菜地黄棕壤）、黏土（稻田水稻土）、泥质湖泊沉积物中获得的总加标回收率分别为88.3%±6.29%、88.3%±3.82%、90.0%±2.50%、90.8%±1.44%.其中,对于密度浮选法较难提取的聚氯乙烯（PVC）、聚对苯二甲酸乙二醇酯（PET）,其回收率分别为93.3%±11.6%（壤土）、96.7%±5.77%（壤土）.植物油的加入会对后续微塑料的光谱表征识别产生影响,但可通过无水乙醇冲洗去除,与拉曼光谱仍具有良好的兼容性.利用该方法开展的实地研究获得黄冈市残坡积物（砂土）、武汉市菜地（壤土）、武汉市水稻田（黏土）、武汉市东湖泥质湖泊沉积物中的微塑料丰度分别为1 679、1 612、1 766、7 629个/kg.研究显示,油提取是当下密度浮选技术的可替代方案.      

Response of Lupinus albus to Pb–EDTA indicates relatively high tolerance

White lupin plants were grown in hydroponics with 0, 90 and 180 µmol L^?1 Pb(II) ethylenediaminetetraacetate complex for 30 days. Pb distribution (shoot/root ratio) was 0.34 and 0.46 for both Pb treatments. In the shoots, no decrease in biomass nor in photosynthetic pigment levels and no changes in the concentrations of malondialdehyde and glutathione were detected. In the roots, malondialdehyde increased by 20%, glutathione 2–3.6 times and phytochelatin concentrations 4–5 times. The high tolerance of white lupin makes it a valuable plant for phytoremediation of Pb-contaminated soil.     

影响土壤中钴活性的因素

用大样本统计分析上土壤性质对钴活性的影响及研究改变土壤ｐＨ值，有机质和氧化还原状况对钴活性的影响。结果表明，在其它土壤性质不变情况下，全钴提高，活性钴的数量增加，锰氧化物的作用则相反，在酸性及还原土壤中，土壤ｐＨ值，浸提剂ｐＨ值对钴的提取量有极显的影响；在中性和碱性并处于氧化状态的土壤中，影响不显，增加土壤有机质可以提高活性钴的数量。     

Biogeochemical cycles of selenium in Antarctic water

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Biogenic volatile organic compounds as a potential stimulator for organic contaminant degradation by soil microorganisms

The effects of monoterpenes on the degradation of ¹⁴C-2,4-dichlorophenol (DCP) were investigated in soils collected from areas surrounding monoterpene and non-monoterpene-emitting vegetation. Indigenous microorganisms degraded ¹⁴C-2,4-DCP to ¹⁴CO₂, after 1 d contact time. Degradation was enhanced by prior exposure of the soils to 2,4-DCP for 32 d, increasing extents of mineralisation up to 60%. Monoterpene amendments further enhanced 2,4-DCP degradation, but only following pre-exposure to both 2,4-DCP and monoterpene, with total 2,4-DCP mineralisation extents of up to 71%. Degradation was greatest at the higher monoterpene concentrations (≥1 μg kg⁻¹). Total mineralisation extents were similar between concentrations, but higher than the control and the 0.1 μg kg⁻¹ amendment, indicating that increases in monoterpene concentration has a diminishing enhancing effect. We suggest that monoterpenes can stimulate the biodegradation of 2,4-DCP by indigenous soil microorganisms and that monoterpene amendment in soils is an effective strategy for removing organic contaminants.     

Effect of dietary fluoride derived from Antarctic krill (Euphausia superba) meal on growth of yellowtail (Seriola quinqueradiata)

Yellowtail (Seriola quinqueradiata) is the most important cultured marine fish in Japan. Dietary fish meal for yellowtail in aquaculture was replaced with 0.0%, 15.4% and 100.0% Antarctic krill meal (KM0, KM15, and KM100) and with 0.0%, 15.4%, and 100.0% low-fluoride krill meal (LFK0, LFK15 and LFK100). The fish was fed to duplicate fish groups for 92 d (KM trial) or 75 d (LFK trial), and fish growth was monitored.Dietary fluoride (F⁻) concentrations (mg kg⁻¹) were 110, 160, and 580 (KM0, KM15, and KM100, respectively) and 98, 120, and 190 (LFK0, LFK15, and LFK100, respectively). The growth during the experimental period, weight gain, feed intake, specific growth rate, and feed efficiency in fish fed the KM100 diet were markedly lower than the other experimental groups, which showed no marked differences in growth performance.After the experiment, dorsal muscle fluoride concentrations in each group were below the detectable limit (1 mg kg⁻¹), but vertebral bone fluoride concentrations increased with increasing proportion of KM to 655 (KM0), 870 (KM15), and 2150 (KM100) mg kg⁻¹. With increasing LFK in the feed, vertebral bone fluoride concentrations (mg kg⁻¹) increased slightly from 500 (LFK0) to 655 (LFK15), and 695 (LFK100). No histopathological changes were detected in the liver tissue in any experimental group.It has been reported that the fluoride bioavailability was reduced with increasing water hardness, however, the dietary fluoride derived from KM exoskeleton accumulates in vertebral bones of marine fish with growth inhibition, as has already been shown for freshwater fish. Vertebral bone fluoride concentrations in two krill-eating Antarctic marine fish in the wild were 33 000 mg kg⁻¹ (Champsocephalus gunnari) and 15 000 mg kg⁻¹ (Notothenia rossii), but they did not show any adverse effect of growth. Therefore, fish bone fluoride accumulation apparently depends on fish species rather than the salinity of the habitat. Consequently, krill exoskeleton must be removed during the processing of Antarctic krill if indeed these krill are to be used as fish feed. However, LFK can completely replace dietary fish meal without apparent adverse effects.     

Long-Term Effects on Soil of the Disposal of Olive Mill Waste Waters (OMW)

Disposal of untreated olive mill waste waters (OMW) is a serious environmental problem in many Mediterranean countries. The aim of this work was to assess whether changes in soil properties have occurred due to direct disposal of raw OMW on soil and in evaporation ponds, and to investigate the potential fate and transport of pollutants after olive oil production had ceased. The results clearly showed that uncontrolled OMW disposal is a significant source of pollution to surface soil and waters. Disposal of OMW on soil greatly increased electrical conductivity (EC), available phosphorous (P), exchangeable potassium (K) and magnesium (Mg), organic matter, polyphenols, total and inorganic nitrogen (N), and available micronutrients mainly in surface soil layers. The presence of a high content of clay and carbonates in soil act as barriers and prevent downward transport of pollutants. Residual levels of total carbon (C), polyphenols, total and inorganic N, exchangeable K⁺, available P, iron (Fe), and copper (Cu) were also elevated even 8 years after mill closure. The long term disposal of OMW highlights the need to establish soil quality standards for soil parameters in order to identify soils affected by the disposal of OMW.     

Evaluation of the European Space Agency Climate Change Initiative Soil Moisture Product over China Using Variance Reduction Factor

In this study, we evaluated the European Space Agency Climate Change Initiative soil moisture product v02.1 (ESA CCI SM v02.1) using in situ observations collected at 547 stations in China from 1991 to 2013. A conventional validation was first conducted, and the triple collocation errors of ESA CCI SM and the European Centre for Medium Range Weather Forecasting reanalysis data were approximately 0.053 and 0.050 m³/m³, respectively. To obtain more reliable validation results, the average soil moisture of the in situ observations per ESA CCI SM pixel was also used as the validation sites. Variance reduction factor (VRF) was adopted to quantify the accuracy of the soil moisture validation sites, and the average VRF was estimated at 4.88%. The validation results were enhanced by excluding validation sites with VRF errors greater than 5% from the statistical analysis. Although the ESA CCI SM underestimated the in situ observations with a Bias of 0.05 m³/m³, a moderately high correlation coefficient of 0.44 and a relatively small unbiased root‐mean‐square difference of 0.05 m³/m³ were observed. This study provides information on the utilization of ESA CCI SM for ecological protection, climate change, and hydrological forecasting. It also suggests the adoption of VRF for future error corrections of satellite‐based products.     

悬浮液进样FAAS法测定黄棕壤中的微量铜

本文采用悬浮进样火焰原子吸收光谱法测定黄棕壤中微量铜 ,并对样品的研磨时间、悬浮液浓度、酸度选择及校正方法等进行了探讨。实验表明 :该法的检出限 (K =3)为 0 .12μg· g-1,精密度 (RSD)为4.6 % ,加标回收率为 98～ 10 6 % ,对水系沉积物 GSD5、GSD6标准样品测定结果与推荐值吻合。