淮南煤矿区地表水和地下水水化学特征及控制因素

为厘清淮南矿区地表水和地下水水化学特征和控制因素,采集115组地下水和30组地表水样品,基于数理统计、 Piper三线图、 Gibbs图、矿物稳定场图和离子比例系数等方法,分析了淮南煤矿区地表水和地下水的水文地球化学特征,研究了其水化学特征演变规律.结果表明,淮南煤矿区地下水和地表水呈弱碱性,地表水和地下水中优势阴阳离子为HCO^-₃、 Ca⁺和Na⁺.HCO₃-Ca型和HCO₃-Ca·Na·Mg型为地表水和地下水的主要水化学类型.地下水和地表水的水化学特征主要受岩石风化作用控制,阳离子交替吸附和蒸发对其有一定的促进作用.水岩作用以硅酸盐和碳酸盐矿物的溶解为主,碳酸盐岩的溶解制约Ca²⁺、 Mg²⁺和HCO^-₃等离子的变化.地表水和地下水中Cl^-、 SO₄^2-、 NO^-₃     

Estimating Water Budgets and Vertical Leakages for Karst Lakes in North‐Central Florida (United States) Via Hydrological Modeling1

Lin, Zhulu, 2011. Estimating Water Budgets and Vertical Leakages for Karst Lakes in North‐Central Florida (United States) Via Hydrological Modeling. Journal of the American Water Resources Association (JAWRA) 1‐16. DOI: 10.1111/j.1752‐1688.2010.00513.x Abstract: Newnans, Lochloosa, and Orange Lakes are closely hydrologically connected karst lakes located in north‐central Florida, United States. The complex karst hydrology in this region poses a great challenge to the hydrological modeling that is essential to the development of Total Maximum Daily Loads for these lakes. We used a Hydrological Simulation Program – Fortran model coupled with the parallel Parameter ESTimation model calibration and uncertainty analysis software to estimate effectively the hydrological interactions between the lakes and the underlying upper Floridan aquifer and the water budgets for these three lakes. The net results of the lake‐groundwater interactions in Newnans and Orange Lakes are that both lakes recharge the underlying upper Floridan aquifer, with the recharge rate of the latter one magnitude greater than that of the former. However, for Lochloosa Lake, the net lake‐groundwater interaction is that the lake gains water from groundwater in a significant amount, approximately 40% of its total terrestrial water input. The annual average vertical leakages estimated for Newnans, Lochloosa, and Orange Lakes are 6.0 × 10⁶, ?8.9 × 10⁶, and 44.4 × 10⁶ m³, respectively. The average vertical hydraulic conductance (K_v/b) of the units between a lake bottom and the underlying upper Floridan aquifer in this region are also estimated to be from 1.26 × 10^?4 to 1.01 × 10^?3 day^?1.     

潮土中磷锌交互作用机制探讨及磷对锌吸附-解吸的影响

采用室内培养和吸附解吸两种方法,探讨了潮土中磷、锌交互作用机制。结果表明：土壤中DTPA提取态锌质量分数随添加锌量的增加而增加,低磷质量分数处理可提高土壤锌有效性,但高磷质量分数处理却降低了土壤锌的有效性;土壤速效磷质量分数均随锌添加量的增加而有所降低。在施锌25 mg.kg-1背景下,土壤中DTPA提取态锌质量分数随施磷质量分数的增加呈先增加后降低趋势,在添加磷量小于180 mg.kg-1时,土壤DTPA提取态锌质量分数显著地高于其他处理,但随添加磷量的增加,土壤DTPA提取态锌质量分数显著降低,当磷添加量大于540 mg.kg-1时,土壤DTPA提取态锌质量分数明显低于其他磷处理,说明当添加磷量小于180 mg.kg-1时,磷提高土壤中锌有效性的主要机制是二者竞争吸附土壤胶体表面吸附点位的竞争机制;当添加磷量大小540 mg.kg-1时,磷影响锌有效性的主要机制为沉淀作用。在土壤施磷量为180 mg.kg-1时,随添加锌质量分数的提高,土壤中速效磷质量分数呈先升高后降低趋势。吸附-解吸研究表明,随土壤中速效磷质量分数的提高（27.60~2773.86 mg.kg-1）,土壤对锌的吸附量先降低再增加,而KCl解吸的锌量却是先增加再降低。因此潮土中磷锌交互作用机制为,土壤中磷和锌质量分数均较低时,磷与锌有效性呈协同作用;当磷或锌质量分数过高时,协同作用减弱;磷和锌质量分数再增加二者的有效性将出现拮抗作用。     

大型渡槽结构动力学研究进展

大型渡槽是灌区生命线工程中的关键性建筑物,其在地震及风载作用下的安全性已是渡槽建设的瓶劲,也是国内外研究的热点。渡槽结构的抗震、减震和抗风技术的核心是渡槽结构动力学的问题,而渡槽结构动力学系属流固耦合(FSI)系统的动力学范畴。在已有研究的基础上,首先对渡槽结构FSI系统模型的研究进行了总结和评述;然后简述了渡槽结构动力特性和响应的求解技术以及抗震、隔震、减震与抗风技术的研究概况;最后总结了渡槽结构动力学的研究进展,提出了该学科进一步研究的内容和方法。     

Promotional catalytic activity and reaction mechanism of Ag-modified Ce0.6Zr0.4O2 catalyst for catalytic oxidation of ammonia

Ce_1-xZr_xO₂ composite oxides (molar, x = 0-1.0, interval of 0.2) were prepared by a cetyltrimethylammonium bromide-assisted precipitation method. The enhancement of silver-species modification and catalytic mechanism of adsorption-transformation-desorption process were investigated over the Ag-impregnated catalysts for low-temperature selective catalytic oxidation of ammonia (NH₃-SCO). The optimal 5 wt.% Ag/Ce_0.6Zr_0.4O₂ catalyst presented good NH₃-SCO performance with >90% NH₃ conversion at temperature (T) ≥ 250°C and 89% N₂ selectivity. Despite the irregular block shape and underdeveloped specific surface area (∼60 m²/g), the naked and Ag-modified Ce_0.6Zr_0.4O₂ solid solution still obtained highly dispersed distribution of surface elements analyzed by scanning electron microscope-energy dispersive spectrometer (SEM-EDS) (mapping), N₂ adsorption-desorption test and X-ray diffraction (XRD). H₂ temperature programmed reduction (H₂-TPR) and X-ray photoelectron spectroscopy (XPS) results indicated that Ag-modification enhanced the mobility and activation of oxygen-species leading to a promotion on CeO₂ reducibility and synergistic Ag⁰/Ag⁺ and Ce⁴⁺/Ce³⁺ redox cycles. Besides, Ag⁺/Ag₂O clusters could facilitate the formation of surface oxygen vacancies that was beneficial to the adsorption and activation of ammonia. NH₃-temperature programmed desorption (NH₃-TPD) showed more adsorption-desorption capacity to ammonia were provided by physical, weak- and medium-strong acid sites. Diffused reflectance infrared Fourier transform spectroscopy (DRIFTS) experiments revealed the activation of ammonia might be the control step of NH₃-SCO procedure, during which NH₃ dehydrogenation derived from NH_x-species and also internal selective catalytic reduction (i-SCR) reactions were proposed.     

不同土地利用方式对土壤细菌分子生态网络的影响

利用16S rDNA基因Illumina MiSeq高通量测序技术结合分子生态网络方法,测定了4种利用类型土地中的细菌群落组成,并分别构建了可视化的细菌网络.结果表明,旱田和水田土壤细菌网络的平均路径长度与模块性较小,而节点数、连接数、平均连通度和聚类系数较高;4个细菌网络均以正相关关系占优,天然林地负相关比例较高;酸杆菌门、厚壁菌门和变形菌门中的部分菌群在土壤细菌网络中起着重要的连接作用;4个细菌网络的部分关键节点所属的菌群相对丰度较低(1%),并非本研究区域的主体细菌;旱田土壤菌群主要受TP显著影响(P0.05);水田土壤菌群主要受黏粒、粉粒和含水量显著影响(P0.05);天然林地和城市绿地土壤菌群主要受C/N显著影响(P0.05).以上研究结果表明,旱田土壤细菌网络规模更大,物种间关系更加复杂,不同利用类型土地中的细菌均以协同合作关系为主,天然林地土壤细菌之间存在更强的竞争作用.水田和旱田土壤细菌对外界环境因子的扰动更加敏感,响应迅速,群落结构更易发生变化;部分细菌在网络间存在角色转化现象,低丰度菌群在构建土壤细菌网络中具有重要作用.     

Alteration of dominant cyanobacteria in different bloom periods caused by abiotic factors and species interactions

Freshwater cyanobacterial blooms have drawn public attention because they threaten the safety of water resources and human health worldwide. Heavy cyanobacterial blooms outbreak in Lake Taihu in summer annually and vanish in other months. To find out the factors impacting the cyanobacterial blooms, the present study measured the physicochemical parameters of water and investigated the composition of microbial community using the 16S rRNA gene and internal transcribed spacer amplicon sequencing in the months with or without bloom. The most interesting finding is that two major cyanobacteria, Planktothrix and Microcystis, dramatically alternated during a cyanobacterial bloom in 2016, which is less mentioned in previous studies. When the temperature of the water began increasing in July, Planktothrix appeared first and showed as a superior competitor for M. aeruginosa in NO₃^?-rich conditions. Microcystis became the dominant genus when the water temperature increased further in August. Laboratory experiments confirmed the influence of temperature and the total dissolved nitrogen (TDN) form on the growth of Planktothrix and Microcystis in a co-culture system. Besides, species interactions between cyanobacteria and non-cyanobacterial microorganisms, especially the prokaryotes, also played a key role in the alteration of Planktothrix and Microcystis. The present study exhibited the alteration of two dominant cyanobacteria in the different bloom periods caused by the temperature, TDN forms as well as the species interactions. These results helped the better understanding of cyanobacterial blooms and the factors which contribute to them.     

小型四旋翼无人机悬停状态气动干扰与安全间隔研究*

为保证小型旋翼无人机近距编队悬停状态的安全性,采用数值模拟方法研究不同横向和纵向间隔双机悬停流场特征和气动参数变化规律,通过与实验结果对比,验证数值仿真方法的准确性。研究结果表明:无人机内部旋翼间的气动干扰会导致整机单旋翼拉力降低、扭矩增大,使整机气动效率下降;当双机无横向间隔时,双机下洗流场保持对称,同时2股下洗流叠加,呈现较明显的横向扩张趋势,此时后机所受气动影响主要为拉力损失,当纵向间隔大于5 D时,该影响基本消失;当横向间隔X=1 D时,位于尾流区一侧的旋翼拉力减小,后机所受俯仰力矩作用显著,无人机有侧翻风险;横向间隔X≥2 D时,2机之间气动干扰较弱,为较安全区域。     

石英砂、生物质炭、胡敏酸的相互作用及其对BDE-47吸附行为的影响

研究了生物质炭、胡敏酸、石英砂之间的相互作用对BDE-47吸附行为的影响,结果表明：（1）石英砂和生物质炭的相互作用对BDE-47的吸附行为的影响不显著;（2）在低浓度条件下（Ce=0.05Sw时）,石英砂可以促进胡敏酸对BDE-47的吸附作用,使胡敏酸的吸附能力提高16％;在高浓度条件下（Ce=0.25Sw时）,石英砂可以抑制胡敏酸对BDE-47的吸附作用,使胡敏酸的吸附能力降低64％;（3）胡敏酸和生物质炭之间的相互作用可以抑制生物质炭-胡敏酸-石英砂体系对BDE-47的吸附作用,使整体吸附能力降低35％～38％.     

Melanin-based colorations signal strategies to cope with poor and rich environments

One hypothesis for the maintenance of genetic variation states that alternative genotypes are adapted to different environmental conditions (i.e., genotype-by-environment interaction G×E) that vary in space and time. Although G×E has been demonstrated for morphological traits, little evidence has been given whether these G×E are associated with traits used as signal in mate choice. In three wild bird species, we investigated whether the degree of melanin-based coloration, a heritable trait, covaries with nestling growth rate in rich and poor environments. Variation in the degree of reddish-brown phaeomelanism is pronounced in the barn owl (Tyto alba) and tawny owl (Strix aluco), and variation in black eumelanism in the barn owl and Alpine swift (Apus melba). Melanin-based coloration has been shown to be a criterion in mate choice in the barn owl. We cross-fostered hatchlings to test whether nestlings sired by parents displaying melanin-based colorations to different extent exhibit alternative growth trajectories when raised by foster parents in poor (experimentally enlarged broods) and rich (experimentally reduced broods) environments. With respect to phaeomelanism, barn owl and tawny owl offspring sired by redder parents grew more rapidly in body mass only in experimentally reduced broods. With respect to eumelanism, Alpine swift offspring of darker fathers grew their wings more rapidly only in experimentally enlarged broods, a difference that was not detected in reduced broods. These interactions between parental melanism and offspring growth rate indicate that individuals display substantial plasticity in response to the rearing environment which is associated with the degree of melanism: at least with respect to nestling growth, phaeomelanic and eumelanic individuals are best adapted to rich and poor environments, respectively. It now remains to be investigated why eumelanism and phaeomelanism have a different signaling function and what the lifelong consequences of these melanism-dependent allocation strategies are. This is important to fully appraise the role played by environmental heterogeneity in maintaining variation in the degree of melanin-based coloration.