Application of a coupled ecosystem-chemical equilibrium model, DayCent-Chem, to stream and soil chemistry in a Rocky Mountain watershed

Atmospheric deposition of sulfur and nitrogen species have the potential to acidify terrestrial and aquatic ecosystems, but nitrate and ammonium are also critical nutrients for plant and microbial productivity. Both the ecological response and the hydrochemical response to atmospheric deposition are of interest to regulatory and land management agencies. We developed a non-spatial biogeochemical model to simulate soil and surface water chemistry by linking the daily version of the CENTURY ecosystem model (DayCent) with a low temperature aqueous geochemical model, PHREEQC. The coupled model, DayCent-Chem, simulates the daily dynamics of plant production, soil organic matter, cation exchange, mineral weathering, elution, stream discharge, and solute concentrations in soil water and stream flow. By aerially weighting the contributions of separate bedrock/talus and tundra simulations, the model was able to replicate the measured seasonal and annual stream chemistry for most solutes for Andrews Creek in Loch Vale watershed, Rocky Mountain National Park. Simulated soil chemistry, net primary production, live biomass, and soil organic matter for forest and tundra matched well with measurements. This model is appropriate for accurately describing ecosystem and surface water chemical response to atmospheric deposition and climate change.     

植物SOD活性变化与其抗污能力的关系

研究了模拟酸雨、ＳＯ２单独与复合污染对水杉、杉木、龙柏３种抗污能力不同的植物ＳＯＤ活性、细胞汁酸度、细胞膜透性的影响。结果表明，ＳＯＤ的活性经污染后变化规律在不同植物有所不同，而这种变化与其抗污能力有关。ＳＯＤ活性升高者，其抗污能力强，反之则弱，与本底值大小无关。     

酸性媒介黄GG生物降解性能的试验研究

通过试验研究酸性媒介黄GG染料在厌氧、好氧条件下的生物降解机理、降解能力及共代谢降解效果.试验结果表明,厌氧菌能够通过葡萄糖共代谢作用很快降解酸性媒介黄GG;而好氧条件下经驯化活性污泥不能降解酸性媒介黄GG,经过较长时间驯化活性污泥能降解酸性媒介黄GG,但降解效果很差.葡萄糖浓度的升高对提高酸性媒介黄GG厌氧生物降解率有利,当葡萄糖浓度为2000 mg/L时,40mg/L酸性媒介黄GG的12和60 h厌氧生物降解率分别达到81.5%和93.5%.酸性媒介黄GG浓度对厌氧菌的生物降解能力也有影响.当葡萄糖浓度为2000 mg/L,酸性媒介黄GG(浓度为20～100 mg/L)的厌氧降解率最好,降解效率达到了94%,说明厌氧菌对酸性媒介黄GG的降解能力较好.     

钛酸铋光催化降解水中酸性大红的研究

采用异丙醇助水热法制备了钛酸铋光催化剂,UV-vis漫反射测试表明其光吸收带较TiO2发生了红移,通过多点BET法计算出其比表面积为14.16m2/g,平均孔径为21.05nm。以酸性大红为模拟污染物,在三相内循环流化床光催化反应器中进行光催化反应,研究了废水的pH值以及钛酸铋投加量对酸性大红脱色率的影响。结果表明:废水的pH=3.0,催化剂投加量为0.1g/L是最佳反应条件;当流量为10L/h时,连续运行3h后,酸性大红染料的去除率可达92.0%;当处理水量增大时,经过两级处理,酸性大红染料的总去除率仍可达到94.4%。     

超声辅助纳米铁降解酸性红G的实验研究

通过硼氢化纳还原法制备了铁纳米颗粒,并用十二烷基硫酸钠对其进行保护。所得铁纳米颗粒大小在13nm左右,体心立方相。对比了在机械搅拌和超声辅助条件下纳米铁对酸性红G的降解率,超声条件下纳米铁和微米铁对酸性红G的降解率,以及纳米铁投加量、pH值对酸性红G降解率的影响。结果表明,超声辅助下,pH=6～7时,4min内纳米铁对酸性红G有较高的降解率。机理分析表明超声辅助条件下纳米铁对酸性红G的降解主要是超声分散下纳米铁的还原作用得到提高以及纳米铁氧化产物的絮凝作用。     

不同磷源及浓度对利玛原甲藻生长和产毒的影响研究

探讨了不同磷源条件下利玛原甲藻的生长情况,分析了碱性磷酸酶在营养盐利用方面的作用,对不同营养盐条件下腹泻性贝毒(diarrhetic shellfish poison,DSP)的合成情况进行了比较和分析.结果显示,以NaH2 PO4、β-甘油磷酸钠和ATP分别作为唯一磷源时,NaH2PO4组和ATP组最大生长速率(βms)差异不大,β-甘油磷酸钠组稍低;ATP组最大生物量(X)明显高于NaH2PO4组和β-甘油磷酸钠组.实验浓度范围内,β-甘油磷酸钠组碱性磷酸酶活性均比较低,而ATP组活性较高.NaH2PO4组因其浓度的变化而有较大的差异.浓度>2μmol/L时,活性比较低,<2 μmol/L时,活性明显增高.μ-甘油磷酸钠组大田软海绵酸(okadaic acid,OA)总含量和单位藻细胞OA含量最高,NaH2O4组次之,ATP组最低.这些结果表明,利玛原甲藻町吸收利用无机磷NaH2PO4和有机磷β-甘油磷酸钠及ATP.其中,NaH2PO4和ATP的营养价值基本等效,而β-甘油磷酸钠的营养价值较低.ATP较NaH2PO4和β-甘油磷酸钠更有利于维持利玛原甲藻的生长.利玛原甲藻可以直接利用β-甘油磷酸钠;而ATP则需要碱性磷酸酶水解后才能利用.利玛原甲藻毒素的合成与营养盐的形态有关,不同营养盐条件下DSP的合成不同.β-甘油磷酸钠为磷源时,DSP合成量最多.磷盐对DSP合成的影响与该磷盐条件下利玛原甲藻的生理状态有关.     

Degradation and detoxification of microcystin-LR in drinking water by sequential use of UV and ozone

Microcystins (MCs) produced by cyanobacteria are strong hepatotoxins and classified as possible carcinogens.MCs pose a considerable threat to human health through tainted drinking and surface waters.Herein filtrated water from a waterworks in Harbin,China,was spiked with microcystin-LR (MC-LR) extracted from a toxic scum of microcystis aeruginosa,and the spiked sample waters were treated using UV irradiation with consequent ozonation process (UV/O3),compared with ozonation at a dose range commonly applied in water treatment plants,UV irradiation at 254 nm and UV irradiation combined with ozonation (UV+O3),respectively.The remaining of toxins were analyzed using high-performance liquid chromatography and also determined using a protein phosphatase type 2A inhibition assay,which was utilized to evaluate the reduction in toxicity.Results indicated that in comparison to other three processes (O3,UV,and UV+O3),UV/O 3 process could effectively decrease both the concentration and toxicity of MC-LR at 100 μg/L level after 5 min UV irradiation with consequent 5 min ozonation at 0.2 mg/L (below 1 μg/L),while 0.5 mg/L ozone dose was required for the level below 0.1 μg/L.The addition of an UV treatment step to the existing treatment train may induce significant transformation of micropollutants and breaks down the natural organic matters into moieties unfavorable for ozone decomposition,stabilizing the ozone residual.These findings suggested that sequential use of UV and ozone may be a suitable method for the removal of these potentially hazardous microcystins from drinking water.     

不同磷源形态对中肋骨条藻和东海原甲藻生长及磷酸酶活性的影响

研究了磷酸二氢钠（NaH₂PO₄）、三磷酸腺苷二钠盐（adenosine disodium triphosphate,ATP）、 6-磷酸葡萄糖（glucose 6-phosphate,G-6-P）和β-甘油磷酸钠（sodium β-glycerophosphate,G-P）对中肋骨条藻 （Skeletonema costatum）和东海原甲藻（Prorocentrum donghaiense）的生长以及磷酸酶活性的影响.结果发现,中肋骨条藻和东海原甲藻均既可利用无机磷酸盐又能利用有机磷化合物生长繁殖,且有机磷化合物的作用比无机磷酸盐的作用稍高.对于中肋骨条藻, 8 d后的细胞密度分别为48×10⁴（NaH₂PO₄）、 73×10⁴（ATP）、 63×10⁴（G-6-P）和54×10⁴（G-P）cells/mL;对于东海原甲藻, 10 d后4种磷源形态下的细胞密度分别为8.7×10⁴、 15.5×10⁴、 12.4×10⁴和9.5×10⁴ cells/mL. 2种藻在4种形态磷源下的磷酸酶活性在前3～4 d均呈下降趋势,而后变化不同.以NaH₂PO₄为磷源的处理组, 2种藻的碱性磷酸酶（alkaline phosphatase,AP）和酸性磷酸酶（acid phosphatase,AcP）活性均呈现升高趋势;3种有机磷处理组比较,对于中肋骨条藻,ATP和G-6-P为磷源的处理组酶活性较低且AP活性无明显变化趋势,AcP活性在试验后期呈微弱的升高趋势,以G-P为磷源的处理组酶活性最高且有升高趋势,至第8 d时,以ATP、G-6-P和G-P为磷源处理组的AP活性分别为0.004×10^-5、 0.014×10^-5和0.029×10^-5 U/cell,AcP活性分别为0.006×10^-5、 0.011×10^-5和0.018×10^-5 U/cell,对于东海原甲藻,酶活性变化趋势与中肋骨条藻相同,至第10 d时, 3种磷源处理组的AP和AcP活性顺序也为ATP相似文献   

柱淋洗法修复铬污染土壤的效果研究

以铬渣污染土壤为供试土壤,采用土柱淋洗法研究柠檬酸、草酸和盐酸单一淋洗以及复合淋洗对铬去除动态和修复效果的影响,并对淋洗前后土壤中铬形态进行分析,探讨修复机理。结果表明,各淋洗方案中,以10体积0.5 mol/L草酸溶液为淋洗剂时的修复效果最好,总Cr累计淋出量为2 304 mg/kg,上层、中层和下层土壤总Cr去除率分别为79.6%、78.1%和69.6%,Cr(VI)去除率为87.8%、86.2%和75%,且土壤Cr(VI)和总Cr随着土壤深度的增加而升高,有在底部积累的可能;淋洗后土壤明显酸化,p H值从10.5降至3左右;以酸作为淋洗剂能有效降低土壤可氧化态铬含量,将其转化为移动性较强的酸可提取态,这有助于达到预期修复效果。     

层状云降水中化学过程的数值模拟

对一维时变的层状云物理化学模式的化学过程作了研究,引入了较为细致的化学模式,并以类似化学反应方程式的方式处理了气液传输、碰并和云雨转化过程。在此基础上讨论了典型条件下的云雨酸化过程。模拟结果表明,高空云雨水组成随时间逐渐减小,地面雨水组成呈峰型分布。在降水后期pH值主要同O₃和SO₂有关;主要来自气溶胶,来自NH₃,气体和气溶胶对的贡献大致相当,和Ca￣(2＋)的云下清除约占60％～80％;在降水前期H₂O₂时S(Ⅳ)的氧化超过O₃,降水后期S(Ⅳ)的氧化主要通过O₃。