Sand as a relevant fraction in geochemical studies in intertidal environments

Soil and sediment samples from several intertidal environment exposed to different types of contamination were studied to investigate the importance of grain size in relation to the capacity of the substrates to retain trace metals. The unfractionated samples (referred to as bulk samples) were separated into the following grain/size fractions: fine–coarse sand (2?0.100 mm), very fine sand (0.100?0.050 mm), silt (0.050?0.002 mm), and clay (0.002 mm). The sample into its fractions was carried out was in a glove box under high-purity N₂ atmosphere in order to minimize any alterations to the samples. The bulk samples were characterized in terms of physicochemical properties such as pH, redox potential, and grain size. The total organic carbon (TOC), total sulfur (S), iron (Fe) pyrite, Fe, and manganese (Mn), and trace metals lead (Pb), mercury (Hg), chromium (Cr), and nickel (Ni) were analyzed in the bulk samples and in each fraction. The sand fractions were also examined by scanning electron microscopy (SEM). Comparisons of the above parameters were made between fractions and between each fraction and the corresponding bulk sample. The fine–coarse sand fraction contained high levels of the primary elements of the geochemical processes that occur in marine sedimentary environments such as TOC, total Fe, Mn, and S. The net concentrations of these four elements were higher in the fine-coarse sand fraction than in the very fine sand fraction and were similar to the net concentrations in the silt and clay fractions. Detailed SEM analysis of the sand coarse fraction revealed the presence of Fe and aluminum oxyhydroxide coatings in the oxic layers, whereas the framboidal pyrites and coatings observed in the anoxic layers were Fe sulfides. The presence of the various coatings explains why the trace metal concentrations in the sand fine–coarse fraction were similar to those in the clay fraction and higher than those in the very fine sand fraction. The present results highlight the importance of the sand fraction, which is generally disregarded in geochemical and environmental studies of sedimentary layers.     

Environmentally Friendly Polyurethane Composites: Preparation, Characterization and Mechanical Properties

The waterborne polyurethane (PU) prepolymer was prepared based on isophorone diisocyanate (IPDI), polyester polyol (N220), dimethylol propionic acid (DMPA) and hydroxyethyl methyl acrylate (HEMA). The modified waterborne polyurethane–acrylate (PUA) emulsions were obtained with different proportions of acrylate (butyl acrylate and methyl methacrylate) and initiating agent by in situ dispersion technique. The structures and thermal properties of prepared PU and PUA were analyzed and characterized with FT-IR, UV–Vis spectroscopy and DSC. The PUA hybrid samples had lower glass transition temperature of hard segment and higher decomposition temperatures than PU sample. Performances of the emulsion and film were studied by means of apparent viscidity, particle size and polydispersity, surface tension and mechanical properties. The results indicated that the particle sizes of the PUA dispersions were larger than those of the pure PU and the solvent resistance, mechanical properties of PUA films was improved compare with the unmodified polyurethane film. The film had the biggest hardness and the least water absorption when the BA/MMA mass ratio 5:5 modified PU. The obtained PUA have great potential application such as coatings, leather finishing, adhesives, sealants, plastic coatings and wood finishes.     

水稻不同生育期根际与非根际土壤胞外酶对施氮的响应

与稻田土壤碳氮循环(矿化、转化等)密切相关的酶活性可以反映微生物的生长和代谢过程.为明确水稻不同生育期根际与非根际土壤胞外酶对施氮的响应,采用根际袋法区分水稻根际和非根际土壤,利用96微孔酶标板荧光分析法,测定其碳氮过程关键酶β-1,4-葡萄糖苷酶(BG)和β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)活性,探讨根际效应、施氮和生育期对土壤酶活的影响及其调控机制.结果表明,施氮使拔节期土壤BG酶活性相对于不施氮处理降低了7.4~13.5 nmol·(g·h)~(-1),而使成熟期BG酶活性增大了7.0~31.4 nmol·(g·h)~(-1),同时根际与非根际土壤中BG酶活性也随水稻的生育期而发生相应的变化.与不施氮处理相比,施氮使水稻成熟期非根际土壤NAG酶活性增加了1.1倍,根际土壤降低了0.3倍.施氮和生育期显著影响土壤BG酶活性,而水稻生育期、施氮和根际效应及其交互作用均对NAG酶活性有极显著影响.RDA分析表明土壤微生物生物量碳(MBC)和可溶性有机碳(DOC)含量主要影响水稻根际土壤胞外酶活性;而非根际土壤中酶活性的变化主要受微生物生物量氮(MBN)和铵态氮(NH_4~+-N)的影响.土壤酶活性与多种因素存在复杂关系,需要综合考虑植物生理特征、土壤酶活性和土壤特征,分析N添加对微生物群落组成的影响.     

Arsenic biotransformation and an arsenite S-adenosylmethionine methyltransferase in plankton

<正>Arsenic(As)is a well-recognized toxicant and carcinogen.Chronic exposure to inorganic arsenic causes a range of human cancers(e.g.,skin,bladder,and lung)and increases the risk of developing diabetes,hypertension,and cardiovascular and neurological diseases.The prevalence of arsenic species and the severity of their health effects continue to drive and demand for extensive research(Carlin et al.,2016).     

Impacts of climate variability and changes on domestic water use in the Yellow River Basin of China

We present a methodology for using a domestic water use time series that were obtained from Yellow River Conservancy Commission, together with the climatic records from the National Climate Center of China to evaluate the effects of climate variability on water use in the Yellow River Basin. A suit of seven Global Circulation Models (GCMs) were adopted to anticipate future climate patterns in the Yellow River. The historical records showed evidences of rises in temperature and subsequent rises in domestic water demand in the basin. For Upstream of Longyangxia region, the impact was the least, with only 0.0021?×?10⁸ m³ for a temperature increase of 1 °C; while for Longyangxia-Lanzhou region, domestic water use was found to increase to 0.18?×?10⁸ m³ when temperature increases 1 °C. Downstream of Huayuankou was the region with the most changes in temperature that gave the highest increase of 1.95?×?10⁸ m³ in domestic water demand for 1 °C of change of temperature. Downstream of Huayuankou was identified as the most vulnerable area, where domestic water demand increases nearly by 42.2 % with 1 °C increase of temperature. Judging from the trends of temperature range, we concluded that future temperature in Yellow River Basin has an increasing tendency. This could worsen the existing issues of domestic water demand and even more to trigger high competition among different water-using sectors.     

HAZOP与LOPA联合分析在聚丙烯装置上的应用

阐述了危险与可操作性分析(HAZOP)和保护层分析(LOPA),两种方法间的联系及HAZOP与LOPA联合分析流程。以20×10~4t/a聚丙烯装置为研究对象,选择其中低压聚合物脱气系统为示例节点,应用HALOPA分析软件对装置进行安全评价,对潜在风险进行定性和半定量分析,并提出相应的风险控制方案。     

景观用再生水氮磷条件下两种典型水华藻类的生长及竞争规律

针对再生水景观水体的藻类控制,以BG11培养基为基础,设定不同氮磷浓度,对铜绿微囊藻和小球藻进行了纯培养和共培养实验。实验结果表明:初始总氮浓度为15 mg/L、总磷浓度为0.1 mg/L时两种藻就能出现明显的生长高峰;当总氮浓度为3⁴5 mg/L,氮磷比为3045 mg/L,氮磷比为30¹50的情况下,小球藻在与铜绿微囊藻的竞争中容易成为优势藻种。     

Effect of ammonium on nitrous oxide emission during denitrification with different electron donors

Nitrous oxide(N2O) emission during denitrification is receiving intensive attention due to its high potential to cause greenhouse effects.In this study,denitrifiers were acclimated in sequencing batch reactors with methanol or acetate as the electron donor and nitrate as the electron acceptor.The effects of ammonium on N2O emission were examined in batch experiments with various electron donors.With the addition of ammonium,N2O emission increased under all the examined conditions compared to experiments without ammonium addition.With different electron donors,the highest ratio of N2O emission to the removed oxidized nitrogen was 0.70% for methanol,5.34% for acetate,and 34.79% for polyhydroxybutyrate.     

贵州省湄潭县生态旅游发展规划研究

湄潭县旅游资源丰富,本文介绍了湄潭旅游资源的现状,从缺乏旅游精品、资源整合不足、文化挖掘不深、旅游宣传不力、旅游设施滞后、旅游人才匮乏等方面分析了旅游产业存在的不足,提出了发展生态旅游的思路,从茶文化、乡村休闲度假和浙大西迁文化和湄江山水四方面设计了生态旅游产品;从低碳旅游设施建设规划和体验式生态旅游规划两方面规划了绿色服务产品,并提出从旅游者、从业者和政府三个层面构建管理型生态旅游;最后对湄潭生态旅游发展提出了展望。