重金属在牡蛎(Crassostrea virginica)中的生物积累及其影响因素的研究

牡蛎软体，贝壳和沉积物中Ｃｄ、Ｃｒ、Ｃｕ、Ｆｅ、Ｍｎ、Ｐｂ和Ｚｎ等重金属元素被同步分析研究，研究结果表明，重金属在牡蛎中的生物积累是牡自身的新陈代谢、重金属元素的地球化学性质和环境诸因素综合影响的结果，其中牡蛎斩生理作用对重金属在软体中的积累产生的影响尤为重要，而贝壳中重金属的积累对来自环境的影响更为敏感。     

煤矸石制取聚羟基氯化铝的研究

介绍了用煤矸石制取聚羟基氯化铝的方法,研究了酸浸、调整盐基度等过程的最佳工艺过程。     

研究海洋环境质量生物标准的意义及其内容

阐述研究制订海洋环境质量生物标准的必要性和重要意义，介绍生物标准应用的概况和国际上应用的鱼贝类污染物含量标准。依据海洋污染研究进展和我国海洋监测管理水平，探讨我国生物标准制订的内容，提出宜选用海洋双壳类，以有毒污染物含量以及微生物污染指标和赤潮毒素等为主要内容，研究制订适应我国国情的生物标准     

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。     

上海城市交通与机动车排气污染调查

上海市机动车保有量逐年增加，车辆的排气污染愈来愈严重，据调查，１９９７年机动画排放的ＣＯ，ＭＮＨＣ，ＮＯＸ和ＰＭ分别达到５８．６，９．０８，６．２０和０．２３万吨。中心城区机动车排放的ＣＯ，ＮＭＨＣ和ＮＯＸ污染物５０％以上来自于小型车，是影响上海城区环境空气质量的主要污染源。     

国际环境法中环境信息交流制度

环境信息国际交流制度，已成为国际环境法的一项基本法律制度，其内容涉及各国和国际组织在这项交流中的地位，作用及机构，权利和义务，交流范围和形式，这项制度对有效保护人类环境发挥了多方面积极作用，在尊重各国主权，合作取得和共同享有，支持发展中国家参与交流原则基础上，这项制度将日益丰富，多样，完善。     

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.