硫酸盐还原菌对EH40焊接钢海水腐蚀的影响

目的研究无菌和SRB体系中EH40钢焊接接头的母材区、热影响区和焊缝区腐蚀差异。方法利用金相显微镜观察、失重法、电化学测试、扫描电镜和X射线光电子能谱仪等分析手段。结果焊缝区微观组织由块状铁素体(BLF)和魏氏组织(W)组成;热影响区可再分为粗晶区(CGHAZ)和细晶区(FGHAZ)两个区;母材区主要由BLF、AF和少量珠光体组成。在无菌对照体系中,焊缝区腐蚀速率为0.0026 mm/a,混合区次之,为0.0023 mm/a,母材区最小,为0.0019 mm/a。含SRB体系中,各区的腐蚀速率为:焊缝区(0.0037 mm/a)混合区(0.0034 mm/a)母材区(0.0030 mm/a)。热影响区腐蚀产物形貌粗大,点蚀孔也较大。结论焊缝区比母材区容易腐蚀,由此易造成小阳极大阴极加速腐蚀,热影响区容易发生点蚀。SRB能促进三个区域试样腐蚀加速。     

A Global Overview of Atmospheric Acid Deposition Fluxes

This paper presents a summary of globalacid deposition flux data taken from a globalassessment report on acid deposition prepared forUNEP/WMO (Whelpdale and Kaiser, 1996). There is a largevariation in the spacial coverage and reliability ofmonitoring around the world. Many more stationsmeasure wet deposition than collect appropriate datafor estimating dry deposition. The widespread regionswith highest precipitation concentrations anddeposition fluxes of sulphate and nitrate coincideclosely with the regions of highest density ofSO₂ and NO_x precursor emissions occurringprimarily in the mid-latitude, northern hemispherebelt where a large fraction of the worlds fossilfuels is consumed. Organic acids in precipitation makea minor contribution to acidity (<20%) inindustrial regions, but in the rest of the world theyare of same order, or even exceed, inorganic acids.Less is known about dry deposition, but it appears topredominate near strong emission sources with wetdeposition predominating farther downwind. The molarratio of the N/S contribution to acidic deposition isclose to 1.0 over large areas of Europe and NorthAmerica, but is highly variable elsewhere, beinghighest in equatorial regions due to biomass burningand lowest near smelters and other large sources of SO₂.     

复合混凝剂处理印染废水

为了处理高浓度、高色度、高COD的印染废水，利用硫酸亚铁、工业废酸和金属下脚料自行配制了复合混凝剂，并将其与聚合双酸铝铁、聚合氯化铝铁、硫酸亚铁对印染废水的混凝效果进行对比。研究表明，复合混凝剂处理印染废水具有成本低、效果好的特点。当硫酸亚铁的投加量为200mg/L，复合混凝剂的投加量为1280mg／L，PAM的用量为2mg／L时，脱色率达94．9％，COD去除率达78．1％，悬浮固体（SS）去除率达90．9％。     

亚铵制浆黑液非无菌操作连续发酵生产酵母

从土壤中筛选出能在亚铵黑液中生长的毕赤酵母菌株（Ｐｉｃｈｉａ ｓｐ．Ｎｏ．１）经耐毒驯化后，可接种于酸析脱木素和汽提脱毒后的亚铵黑液中，在非无菌操作条件下连续发酵生产酵母菌体，该菌生产迅速，连续培养衡释率达０．２６ｈ＾－１，总糖的酵母得率为０．４８ｇ／ｇ（ＴＳ），ＣＯＤ去除２３％，菌体易絮凝，可自然沉降分离。     

Field measurements of dissociation of ammonium nitrate at a Beijing site

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MAP法处理氨氮废水最佳条件的研究

MAP法是一种比较新颖有效的处理氨氮的方法，该方法是通过化学沉淀的方式使废水中的氨氢浓度降到很低。而且沉淀反应不受温度、水中毒素的限制。由单项试验以及正交实验的方法对MAP法处理氨氮废水的工艺进行优化研究，结果表明，在pH=8.5，反应时间为3h,Mg:N:P=1:3:1.0:1.1时为较佳反应条件；氨氮的去除率随着反应时间的增加而增加，随着Mg:N比值的增加而增加。     

混凝法处理油墨废水色度的研究

对pH 4 .5～ 6 .5、COD 6 0 0 0～ 170 0 0 /mg·L-1、色度 10 0～ 35 0倍、SS 2 0 0～ 6 5 0 0 /mg·L-1、外观呈蓝紫色的油墨废水进行了混凝法脱色试验。对混凝剂种类及投药量、pH、助凝剂种类及投药量等工艺条件进行了优选。其中混凝剂为聚合氯化铁 ,投药量为 10 0 /mg·L-1,pH适用范围为 4 .8～ 5 .5。助凝剂为阳离子聚丙烯酰胺 ,分子量为 15 0 0万 ,离子度 4 0 % ,投药量 0 .4 /mg·L-1,处理后的废水脱色率达到 97.0 %以上     

溶济萃取法处理含硫酸及硫酸盐的废水

采用溶剂萃取法处理含硫酸及硫酸盐的工业废水，主产优质农用硫酸钾，副产氯化铵和氮钾复合肥，整个工艺过程基本无三废排放，实现了对该废水的综合有效治理。     

Rapid amino acid cycling in arctic and antarctic soils

Amino acids constitute one of the largest inputs of organic nitrogen (N) to most polar soils and have been hypothesized to be important in regulating vegetational succession and productivity in Arctic ecosystems. Our understanding of amino acid cycling in these soils, however, is poor. The aim of this study was to investigate the size and rate of turnover of the amino acid pool in a range of Arctic and Antarctic soils. Our results indicate that in polar soils with either high or low ornithogenic inputs the amino acid pool is small in comparison to the inorganic N pool (NO^–₃ and NH⁺₄). The free amino acid pool constituted only a small proportion of the total dissolved organic nitrogen (DON) pool in these soils. Here we show that these low concentrations may be due to rapid use by the soil microbial community in both Arctic and Antarctic soils. The turnover of the amino acid pool in soil was extremely rapid, with a half-life ranging from 2 to 24 h, indicating that this N pool can be turned over many hundred times each summer when polar soils are frequently unfrozen. The implications of amino acids in N cycling and plant and microbial nutrition are discussed.     

Applying metabolic fingerprinting to ecology: The use of Fourier-transform infrared spectroscopy for the rapid screening of plant responses to N deposition

The potential for metabolic fingerprinting via Fourier-transform infrared (FT-IR) spectroscopy to provide a novel approach for the detection of plant biochemical responses to N deposition is examined. An example of spectral analysis using shoot samples taken from an open top chamber (OTC) experiment simulating wet ammonium deposition is given. Sample preparation involved oven drying and homogenisation via mill grinding. Slurries of a consistent dilution were then prepared prior to FT-IR analysis. Spectra from control, 8 and 16 kg N ha^–1 yr^–1 treatments were then subjected to cross-validated discriminant function analysis. Ordination diagrams showed clear separation between the three N treatments examined. The potential for using Calluna vulgaris (L.) Hull as a bioindicator of N deposition is further evident from these results. The results also clearly demonstrate the power of FT-IR in discriminating between subtle phenotypic alterations in overall plant biochemistry as affected by ammonium pollution.