青霉菌X5对活性艳蓝KN-R脱色研究

采用梯度平板筛选法，从染布厂废水池污泥中分离到一株对蒽醌染料KN－R有较强脱色能力的青霉菌X5（Penicillium sp.)，并考察该菌在不同温度，pH，培养时间，染料浓度，菌量及不同碳源氮源条件下对活性艳蓝KN－R的脱色情况，结果表明,在20－40℃温度范围内该菌对活性艳蓝KN－R的脱色率均在95％以上，其最佳脱色温度为25℃，pH为4．0，培养时间为48h，染料浓度，菌量对染料脱色有一定影响，该菌对碳源、氮源具有较宽适应范围，在最佳条件下，该菌对染料的脱色率达99．3％。     

碳纤维混凝土的耐火性能试验测试与分析*

为研究不同碳纤维体积掺量（0,0.2%,0.6%,1%,1.5%,2%）对混凝土耐火性能的影响,考察不同温度环境下（20,60,100,300,500,800 ℃）的混凝土质量损失率与抗压强度损失率的变化情况;分析高温环境下混凝土的静置时间（0,1,3,7,12 h）对混凝土抗压强度损失率的影响。结果表明:随着碳纤维掺量的增加,混凝土质量损失率与抗压强度损失率呈现先下降后增加的趋势,其纤维掺量的拐点为1%;随着环境温度的上升,纤维混凝土的质量损失率与抗压强度损失率逐渐增加,并呈非线性增长趋势。随着静置时间的增加,混凝土抗压强度损失率逐渐增加,且呈非线性增长趋势。     

关于氮肥利用率的思考

应用作者近10年在华北地区冬小麦／夏玉米中氮肥转化与去向的研究资料，对施氮量、产量、氮肥利用、残留、损失关系进行分析；认为简单的氮肥利用率很难反映不同农业生产水平条件下的氮肥利用状况；要准确反映氮肥利用状况，应综合考虑产量水平、氮肥利用、残留及损失的情况。论证了我国氮肥利用率具有很大的变幅，平常所说的30％-35％只是一个整体概念，不能以此来说明我国氮肥损失量大，对环境的污染严重。在我国农业生产中，必须研究解决既能获得尽可能高的产量，又能最大限度地减轻对环境压力的氮肥施用技术及其理论基础，而不应该一味追求多么高的氮肥利用率。     

果树光合作用研究进展

综述了果树光合作用的研究方法，观测仪器，日变化和季节变化，以及内在因素(种类、品种、年龄、叶位、叶绿素含量、酶系统)和外部因素(光照、CO2、温度、湿度、土壤、外用药剂)对果树光合作用的影响。     

塔克拉玛干4种荒漠植物气体交换与环境因子的关系初探

研究了4种荒漠植物）胡杨，疏叶骆驼刺，头状沙拐枣，多枝柽柳）气体交换的季节变化及其与环境因子的关系。结果：（1）外界环境因子中，无论是对光合速率还是蒸腾速率，光照强度都是最重要的主导因子，其次是气温，大气湿度与植物的蒸腾速率成负相关，影响程度因不同植物及其环境因子的情况而有所不同。（2）在气温越高的地方，荒漠植物的温度生态位（包括最适温度和极限温度）也随之增高。（3）水分胁迫影响气温和叶温的差异，4种植物都能调整其叶温，使之低于沙漠地区的极度高温。     

煤气管道的震害率分析

埋地管道的地震危险性分析方法可以分为理论分析法和经验统计法。震害率是经验统计法中常用的一个概念。埋地管道在地震中破坏的主要原因是地面运动和场地土液化等引起的场地土失效，另外管线的接口类型、管材、管径等也是决定其震害的因素。在查阅相关文献的基础上，对埋地管道的震害率分析方法进行了综述，并运用经验统计法提出了便于使用的煤气管道震害率估算表达式。     

对地震保险体制改革的探索

从研究地震灾害规律和保险经营特点之间的矛盾入手,叙述地震保险经营的困难,剖析我国现行地震保险体制的缺陷,提出了建立一个新的,相对科学和合理的地震保险体制的若干建议。     

膨胀颗粒污泥床反应器在低温低浓度下的动力学研究

在考虑膨胀颗粒污泥床(EGSB)反应器的反应动力学、水力动力学和热动力学特点的基础上,建立了EGSB反应器在低浓度下的基质降解动力学模型,求出EGSB反应器在进水COD450m g/L、35,15℃(与35℃同样的液体上升流速)和15℃(提高液体上升流速至最佳)3种运行条件时的速率常数分别为3.91×102,1.07×102,2.54×102d-1。用A rrhenius方程分析了温度对速率常数的影响,计算出EGSB反应器在提高液体上升流速前后的活化能分别为4.897×104J/m o l和1.197×104J/m o。l低温使速率常数明显降低,但液体上升流速的提高却能显著提高速率常数,降低活化能。     

Long Term Effects of Acid Irrigation at the Höglwald on Seepage Water Chemistry and Nutrient Cycling

In order to test the hypothesis of aluminium toxicity induced by acid deposition, an experimental acid irrigation was carried out in a mature Norway spruce stand in Southern Germany (Höglwald). The experiment comprised three plots: no irrigation, irrigation (170 mm a^?1), and acid irrigation with diluted sulphuric acid (pH of 2.6–2.8). During the seven years of acid irrigation (1984–1990) water containing 0.43 mol_c m^?2 a^?1 of protons and sulphate was added with a mean pH of 3.2 (throughfall?+?acid irrigation water) compared to 4.9 (throughfall) on both control plots. Most of the additional proton input was consumed in the organic layer and the upper mineral soil. Acid irrigation resulted in a long lasting elevation of sulphate concentrations in the seepage water. Together with sulphate both aluminium and appreciable amounts of base cations were leached from the main rooting zone. The ratio between base cations (Ca?+?Mg?+?K) and aluminium was 0.79 during acid irrigation and 0.92 on the control. Neither tree growth and nutrition nor the pool of exchangeable cations were affected significantly. We conclude that at this site protection mechanisms against aluminium toxicity exist and that additional base cation runoff can still be compensated without further reduction of the supply of exchangeable base cations in the upper mineral soil.     

Sedimentary Processes of the Qingdao Nearshore Traced Using a Multi-radionuclide Approach

Sediment cores were collected from two sites (A2 and ZQ) in the Qingdao sea area of the Yellow Sea. Radionuclides ⁴⁰K, ¹³⁷Cs, ²¹⁰Pb, ²²⁶Ra, ²²⁸Ra, ²²⁸Th, ²³⁴Th, and ²³⁸U in the cores were measured using HPGe γ spectrometry. The sedimentation rate of the A2 Core using ²¹⁰Pb_ex and ¹³⁷Cs was 0.665 cm yr⁻¹, therefore this 32 cm long core represents a 48 year timespan leading to the sampling date in 2001. The mixing layer was restricted to the upper 5 cm as determined from the profile of ²³⁴Th. The uniformity of the activity distributions of ⁴⁰K and ²³⁸U throughout the A2 Core and the activity distributions of ²²⁶Ra, ²²⁸Ra and ²²⁸Th below the mixing layer suggested that no significant oceanographic event or change in sediment material source had occurred during this timespan. The ²¹⁰ Pb was in excess relative to ²²⁶Ra, but ²²⁶Ra was deficient with respect to ²³⁸U in the entire A2 Core, while excess ²³⁴Th and ²²⁸Th were apparent only in the surface 5 cm. Total organic matter (TOM) in Core A2 decreases with depth. The second core, taken to a depth of 14 cm, was from Site ZQ, which is located near Zhanqiao, Qingdao. The variations of the nuclide activity ratios in this core were similar to those in the A2 Core, i.e., the excess ²¹⁰ Pb and ²²⁶Ra deficiency were consistent throughout the core but excess ²²⁸Th was only in the surface to a depth of 2 cm. The ⁴⁰K activity in the ZQ Core fluctuated and showed no real trend with depth. The activities of ¹³⁷Cs, ²¹⁰Pb, ²²⁶Ra and ²³⁸U in the entire length of Core ZQ, and ²²⁸Ra and ²²⁸Th from 2 cm to the bottom, were comparable within the uncertainty of measured activity.