分子生物学在渔业环境保护中的运用

分子生物学理论和技术在渔业环境保护与监测工作中的应用越来越得到人们的重视：生物体的多种酶已被用作监测水环境污染的指标；金属硫蛋白等生物体解毒体系在监测和防治水体重金属污染方面发挥显著作用；核酸是生物体遗传信息载体，以核酸质量变化监测水环境污染已取得较好的效果。据此就分子生物学在今后渔业环境保护中的运用提出了观点。     

Groundwater pollution due to discharge of tannery effluents in Upper Palar basin, Tamilnadu, India: an assessment through mass transport modeling

The groundwater regime in Upper Palar basin, Tamilnadu has been highly contaminated in several locations due to discharge of effluents from a large number of tanneries. At some places total dissolved solids (TDS) concentration in groundwater was found as high as 8000 mg/l. Transmissivity and storativity of the regional aquifer were estimated at a few locations. The porosity and dispersivity values were not determined in the field. These parameters were assumed based on data available for similar geological formations elsewhere. The aquifer conceptualization thus arrived at formed the basis of a numerical groundwater flow model which was constructed using the finite difference method. The flow model was calibrated for steady state and then for transient condition for the period of 1984-92. The computed heads and calibrated parameters of the flow model were used to compute groundwater velocities. The migration of contaminants for a 20 year period was computed using the hydraulic heads and effective porosity value in a pathline model using FLOWPATH software. Mass transport model was constructed using Method of Characteristics (MOC) computer code in a separate model. The seepage rate of effluent is assumed at a rate of 30% of that discharged on the surface. The mass concentration of solute in the effluent reaching the water table was assumed as 40%, the same as in the surface effluent. The mass transport model was calibrated for a 20 year period. Prediction of contaminant migration from different clusters in the basin was analyzed. The prediction results indicated elevated TDS concentration of more than 4000 mg/l from most clusters. Also the area of the contaminated zone is likely to double in 20 years from contaminated zone of 1992.     

免烧免蒸粉煤灰砖的研究

本文讨论了免烧免蒸粉煤灰砖的生产原理，制造技术。试验结果表明利用化学复合外加剂能够成功地生产出免烧免蒸粉煤从砖，且产品质量达到红砖１００号的标准。文中还分析了生产粉煤灰砖的经济效益和社会效益。     

三槽式切换氧化沟运行工况数学模式及应用

三槽式切换氧化沟运行工况呈周期性的变化。根据理论分析，建立了各槽活性污泥浓度变化及相互关系的数学模式，并进行了验证。同时就数字模式在周期程序设置及排泥方式选择时的应用做了说明。     

脉冲等离子法烟气脱硫的放大实验

锅炉烟气进行脉冲等离子法脱硫的扩大实验，得到与模拟烟气实验相近的结果。研究表明，脉冲等离子法对锅炉烟气中的ＳＯ２去除率可达９５％以上，烟气在反应器内的停留时间（ｔｓ）、脉冲电源的放电功率（Ｐ）和添加ＮＨ３等条件，对脱硫效率９η）有较大影响。ｔｓ、Ｐ越大、η越高。处理烟气量（Ｑ）、能耗（Ｐ）与η存在函数关系：η＝１１８．０（Ｐ／Ｑ）＾０．１１１１。烟气中加入适量ＮＨ３，对脱硫效率有显著提高，以ＮＨ３     

Breccias of the Adnet Formation: indicators of a Mid-Liassic tectonic event in the Northern Calcareous Alps (Salzburg/Austria)

Stratigraphy, lithology and depositional structures of Liassic red limestone-breccias of the Adnet Formation, including the 'Adnet Scheck', were studied at several outcrops of the Northern Calcareous Alps (NCA) south-east of Salzburg. A four-fold lithostratigraphic division is proposed for the Adnet Formation of the Osterhorn Mountains: the hemipelagic Schmiedwirt (Sinemurian) and Kehlbach (Carixian) members are separated from the pelagic Saubach Member (Toarcian) by a layer of amalgamated breccias (Scheck Member, probably Domerian to early Toarcian). Several other breccia beds occur locally from the base of the Kehlbach Member up to the lower Saubach Member. Although the sediments overlying the Scheck Member breccias are of coeval age, the ages of the underlying strata are very different. This can be explained by submarine Liassic erosion during a period of resedimentation from the middle Carixian until the early Toarcian. At least 10–15?m of partly lithified sediments were eroded by gravity flows. The entire Kehlbach Member and up to two-thirds of the Schmiedwirt Member were removed at Adnet. The breccias originated from submarine debris flows. Repeated flows over a long period and the depositional setting exclude a triggering by sea-level fluctuations. Most probably they arose from tectonically triggered slumps and slides of superficial sediments. The 'Scheck' was initiated on the steep upper slope of the drowned Triassic Adnet reef and flowed to the north-east.The Pliensbachian to early Toarcian period of tectonic activity indicated by the breccias was the most important during the Liassic in the Osterhorn Mountains and other parts of the NCA. From the large-scale regional distribution of the breccias and in accord with published data, a roughly north-east trending strike-slip fault zone is proposed, crossing the NCA south of the Osterhorn block, with a peaking activity during the Pliensbachian to early Toarcian as the cause of the tectonic movements.     

Latest precambrian (Cadomian) zircon ages, Nd isotopic systematics and P-T evolution of granitoid orthogneisses of the Erzgebirge, Saxony and Czech Republic

Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a ²⁰⁷Pb/²⁰⁶Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean ²⁰⁷Pb/²⁰⁶Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform ²⁰⁷Pb/²⁰⁶Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. _Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in _Nd(t) values from –7.7 to –2.8 (T _DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield.     

涕灭威在植物和土壤中的移动与分布

报道了涕灭威在花生、棉花、柑橘和土壤中的吸收、运转和分布。结果表明，涕灭威及其代谢物在柑橘叶子中的残留４０ｄ达到最高峰（３．４４９ｐｐｍ），可食部位的残留范围为０－０．０８９ｐｐｍ，低于美国ＥＰＡ规定的ＭＲＬ。涕灭威在土壤中降解较快，半衰期约１周。收获时土壤中的检出范围为０－０．１５７ｐｐｍ。涕灭威及其代谢物水溶性很强，且具有渗透和扩散性，因此使用不当可能造成地下水污染。     

氚水在模拟水稻田中的消长动力学

氚水在模拟水稻田中迁移，输运动态过程的研究表明，引入田水氚水，不仅在系统各隔室间转移和分配，而且也向系统外迅速地散逸，氚水的氚以自由水氚和结合态氚形式存在下水稻和土壤中，水稻地上部中自由水氚浓度开始增大，至第８天达最大值后便下降，而结合态氚基本上呈增中趋势，稻根中氚浓度低下地上部，表层土中二种形态氚随时间的变化与水稻植株中情况类似。     

高强铝合金超塑挤压成形

主要介绍了工业牌号高强铝合金在供应态或经简单预处理后在通用油压机上超塑成形的实例,并分析探讨了非理想组织材料超塑成形中微观组织的变化。