采油废水人工湿地处理效果及植物作用分析

采用水平潜流人工湿地中试系统处理采油废水,考察湿地植物生长状况对污染物去除效果的影响,运用气相色谱-质谱(GC-MS)技术分析湿地植物对有机污染的吸附情况,并分析了湿地植物对氮、磷的吸收效果。研究结果表明:人工湿地出水达GB 8987—1996《污水综合排放标准》中的一级标准。湿地植物的生长状况与人工湿地的COD及NH 4+-N去除率呈现一定的耦合关系。芦苇及藨草均能吸附多种难降解有机污染物。植物吸收是人工湿地去除氮、磷的途径之一,但并非主要途径。     

腐殖酸对针铁矿吸附磷的影响机理

通过添加HA(Humic acid,腐殖酸),研究不同环境条件下HA对针铁矿吸附磷的影响. 结果显示,加入HA能显著降低磷吸附量,pH为4.5时分别加入100和40 mg/L HA,磷的最大吸附量分别降低了26.6%和25.6%;pH为7.0时分别加入100和40 mg/L HA,磷的最大吸附量分别降低了26.8%和23.1%. 不同添加顺序试验结果表明:针铁矿对磷的吸附量大小顺序为后添加HA>同时添加HA和磷>先添加HA;无论是否添加HA,针铁矿对磷的吸附量都随着pH的升高而降低,相应的吸附等温线也都符合Langmuir吸附等温方程;总有机碳和红外光谱特征表明,HA和磷在针铁矿表面吸附点位形成竞争吸附,并且针铁矿表面的羟基在吸附磷和HA的过程中起到了一定的作用.      

Thermogravimetric coupled with Fourier transform infrared analysis study on thermal treatment of monopotassium phosphate residue

In China, safe disposal of hazardous waste is more and more a necessity, urged by rapid economic development. The pyrolysis and combustion characteristics of a residue from producing monopotassium phosphate (monopotassium phosphate residue), considered as a hazardous waste, were studied using a thermogravimetric, coupled with Fourier transform infrared analyzer (TG-FTIR). Both pyrolysis and combustion runs can be subdivided into three stages: drying, thermal decomposition, and final devolatilization. The average weight loss rate during fast thermal decomposition stage in pyrolysis is higher than combustion. Acetic acid, methane, pentane, (acetyl) cyclopropane, 2,4,6-trichlorophenol, CO, and CO₂ were distinguished in the pyrolysis process, while CO₂ was the dominant combustion product.     

The plant availability of auto-cast platinum group elements

The introduction of automobile catalysts has raised environmental concern, as this pollution control technology is also an emission source for platinum group elements (PGE). The main aim of this study was to assess soil and grass PGE concentrations in soils adjacent to five road networks. The soil and grass samples were collected from four distances at each site; they were 0, 1, 2 and 5 m from the road edges. The maximum soil Pt, Rh and Pd concentrations were measured at the road perimeters. Pd concentrations were much higher than Pt or Rh, possibly due to differences in its use, emission and/or soil chemistry. Rh and Pt soil concentrations accounted for 66 and 34% (P < 0.01) of the variability observed, respectively, in their plant concentrations. Grass Pd concentrations had no relationship with its total soil concentrations.     

氧化与还原条件下水稻土重金属形态特征的对比

还原状态下的水稻土被风干处理后氧化还原等性质发生明显变化,对重金属的形态特征产生影响,进而影响对作物有效性的评价.利用BCR连续萃取法研究了张家港市南部不同pH水稻土在还原和氧化条件下Cu、Pb、Ni和Cd的形态变化状况.结果显示,氧化还原对重金属形态分配具有显著影响,而pH对Ni在还原状态下的形态分配有显著影响,对Cu、Pb和Cd形态分布影响不显著.样品经风干氧化处理后,氧化物结合态重金属均表现为不同程度的降低;Cu残渣态比例增加25%,氧化物结合态和有机结合态比例有所降低;Pb有机结合态比例增加33%,残渣态减少33%,酸可提取态和氧化物结合态变化不大;Ni受氧化还原条件影响更为强烈,表现为酸可提取态所占比例降低超过25%,氧化物结合态亦明显降低,残渣态提高超过60%;对Cd的影响主要表现为有机结合态所占比例降低约15%,残渣态提高约35%,酸可提取态和氧化物结合态变化不明显.氧化状态下的重金属形态并不是重金属在田间的真实状况,可能高估了Pb,低估Cu、Ni和Cd重金属在土壤中的危害性.     

The fate of exogenous iodine in pot soil cultivated with vegetables

A pot experiment was conducted to explore a more effective approach to enhancing vegetable uptake of soil iodine, with the ultimate goal of using agricultural fortification as a measure to prevent iodine deficiency disorders in local communities. Two types of iodine fertilizers were added separately to pot soil samples at various dosages. The fortified soil in each of the flower pots was seeded with one of four test crops (pakchoi, celery, pepper, and radish) in an effort to examine the effect of vegetable cultivation. The fate and residual levels of the exogenous iodine in the fortified soil samples were then monitored and quantified. The data showed that the soil iodine contents decreased with time (and hence with plant growth as well). At the second cutting, iodine from the inorganic form (KI) as the exogenous source was reduced to approximately 50% (41.6–61.0%) of the applied dose, whereas that in soil fortified with the seaweed fertilizer was down to approximately 60% (53.9–71.5%). The abilities of the edible portion of the four vegetables in accumulating the soil iodine were as follows: pakchoi > celery > radish > pepper. On the whole, iodine residues were found less in soil cultivated with vegetables. Vegetable cultivation appeared to have enhanced the soil content of the water-soluble form of iodine somewhat, especially in soil fortified with the inorganic forms. There also appeared to be a significant negative correlation between the residual iodine and its dissolution rate in soil. Overall, the results of the present study pointed toward the direction that the seaweed fertilizer tends to be a (more) preferred source of agricultural fortification in promoting human iodine nutrition.     

不同生存环境和磷酸盐对4株溶磷菌溶磷能力的影响

利用液体培养法研究了不同NaCl浓度、碳源、氮源、溶解氧及磷酸盐对分离自小麦(Triticum aestivum)、苜蓿(Medicago sativa)根际的4株优良溶磷细菌(Lx81、Jm92、Dm84、Lx191)溶磷能力的影响.结果表明:(1)4株溶磷菌均为高耐盐菌株,其中Jm92和Din84维持较高溶磷量的NaCl浓度最高阈值分别为4%和8%,Lx81、Lx191在NaCl浓度超过5%时溶磷活性受到抑制.(2)Lx81的最佳碳源是葡萄糖,其次为蔗糖;另外3株菌在葡萄糖和蔗糖为碳源时,均有较高的溶磷能力;4株菌都几乎不能利用淀粉.(3)Lx81和Jm92在以(NH_4)_2SO_4和NH_4 NO_3为氮源时溶磷活性均较高,(NH_4)_2SO_4 是Lx191的最佳氮源,而NH~+-N存在会导致Dm84溶磷活性降低.(4)供试4株菌均不是专性厌氧菌,但不同菌株对氧的需求量不同.(5)4株溶磷菌对Ca_3-P和Ca_8-P有较大的溶解效率,但它们几乎都不能溶解Ca_(10)-P.图3表4参14     

基于TASCC的典型农田溪流氨氮滞留及吸收动力学模拟

为揭示农田溪流氨氮滞留的动态变化性,选择NaCl为保守示踪剂、NH4Cl为添加营养盐开展野外瞬时投加示踪实验.在此基础上,采用TASCC方法和养分螺旋指标定量刻画 滞留动态,并以Michaelis-Menten模型(M-M方程)模拟 吸收动力学特性.结果表明:背景浓度的 吸收长度Sw-amb变化范围为93.94~295.54m,平均值为177.41m;质量传输系数Vf-amb变化范围为0.16~0.38mm/s,平均值为0.26mm/s;吸收速率Uamb变化范围为0.16~0.38mg/(m2×s),平均值为0.26mg/(m2×s).由M-M方程模拟得到的 最大吸收速率Umax为0.59~1.38mg/(m2×s),半饱和常数Km为1.10~5.03mg/L. 在从背景浓度到饱和浓度区间范围内展现出的Sw-add-dyn、Utot-dyn和Vf-tot-dyn动态变化性,验证了TASCC解析 滞留动态和吸收动力学特征的可行性和有效性.     

黄渤海氮磷营养盐的分布、收支与生态环境效应

基于在黄渤海的综合调查结果,分析了水体和沉积物间隙水中溶解无机氮（DIN）和溶解无机磷（DIP）的分布;结合历史数据构建了黄渤海DIN和DIP的收支模型,并分析了陆源输入变化对研究区域生态环境的影响.结果表明,黄渤海DIN和DIP的含量受季节、河流输入和沉积物界面扩散作用的影响,具有秋季高于春季和近岸高于离岸的时空分布特征.收支模型计算结果表明,底界面扩散是黄渤海水体DIN的主要来源,其次是大气、周边河流、地下水和东海的输入;黄渤海水体DIN的支出主要是通过沉积埋藏和反硝化.黄渤海水体DIP的来源主要是磷酸盐吸附解吸,占91%,底界面扩散和大气输入为其次,河流和地下水的输入贡献较小.DIP的支出主要是通过沉积埋藏和向东海的输出.黄渤海每年有11Gmol的氮在水体积累,并导致其浓度提高约0.6μmol/（L·a）.近些年来陆地向黄渤海输入氮的持续增加,加剧了氮营养盐的积累,导致非硅藻类浮游植物比例以及赤潮发生频率和面积显著增加,同时还提高了水体初级生产力和海洋磷的埋藏量以及加剧了磷限制的趋势,并可能威胁生态系统的稳定.     

Decline in metallophytes in tertiary polluted floodplain grasslands in the Netherlands: experimental evidence for metal and nutritional changes in soil as driver factors

Metallophyte vegetation along the River Geul has been almost completely replaced by grasses during the last decades. Field investigations indicated that this was accompanied by higher alkalinity and phosphate availability in the soil, related to the closure of the metal industry and intensification of agricultural practices. An experiment with a full factorial design for phosphate and zinc availability indicated that the metallophytes Silene vulgaris and Thlaspi caerulescens did not grow on zinc-poor soils, irrespective of phosphate availability. The grass Holcus lanatus performed well on phosphate-rich soil, irrespective of zinc availability. An experiment with zinc-poor and zinc-rich floodplain soils confirmed the high zinc demand of the metallophytes T. caerulescens and Armeria maritima and the zinc independence of H. lanatus. A third experiment indicated that a reduced zinc availability due to liming affected only the metallophyte T. caerulescens; it had no effect on the growth of the grass Festuca rubra. This means that increasing alkalinity leads to a decrease in zinc availability, limiting the growth of at least some metallophyte species. An increase in phosphate availability stimulates growth in more competitive fast-growing grasses under zinc-rich as well as zinc-poor conditions.