从慧木碰撞谈地球安全

从慧木碰撞事件出发，根据小天体与地球相撞的史实，分析了小天体撞击地球的可能性及其效应，探讨了地球免遭个天体碰撞的可能对策。     

黄河北干流与渭河相遇洪水分析

黄河北干流与渭河位于黄土高原，暴雨是洪水的重要成因．本文分析了近２０００年的历史资料，提出该地区的洪水具有周期性，１９世纪洪水达到高峰，２０世纪洪水规模有所降低，并分析了黄河北干流与渭河及其支流径、洛河洪水相遇问题：四河相遇的概率很小，多形成特大洪水，两河相遇是较常发生的事件，多形成中等以下洪水。三门峡水库的淤积使该地区洪水灾害加剧．同时还分析了该地区洪水对黄河下游洪水的影响。     

Environmental Monitoring in The Netherlands: Past Developments and Future Challenges

During the past three decades environmental monitoringsystems covering an immense variety of environmentalproblems emerged rapidly throughout the world. In The Netherlands the entire spectrum of monitoring systemsis present. Their development is especially interesting because of the Dutch complex environmental landscape: a result of the combination of a natural setting with a high small-scale variation and an intense use of the available space by both industry and agriculture. This necessitates a well balanced environmental policy wherein monitoring ofboth environmental compartments and environmental policy itself plays an important role. In this article we focus on abiotic systems, whereby the development of monitoring will be related to that of environmental policy in general. Some general lines emerge: from quantity towards quality, from single pollutants towards environmentally harmful processes as a whole, and from a focus on human health and safety towards integrated environmental management. Because The Netherlands is a highly organized and highly educatedsociety, reacting fast and flexible to new problems, this progression has happened quickly. However, still much remains to be desired and flexibility not necessarily guarantees optimal routes of development. Paramount is the development of sophisticated and robust monitoring systems that truly support integrated environmental management. This asks forclear objectives based on solid scientific insights.     

Environmental impact assessment: The work of the OECD

This report describes the work of an international group that is supported in part by the Dutch Ministry for Environment and is chaired by Frans Evers, the Ministry's Deputy Director-General for Environmental Protection.     

全球能源消费与CO2排放量

在收集全球能源储量和流通状况的基础上，综述了世界各地区能源消费量和各国人均能源水平，汇总了全球ＣＯ２排放总量及各大洲对全球ＣＯ２排放量的贡献率，到２１００年，全球Ｃ矿量预计将从目前６０亿ｔ／ａ增加到３６０亿ｔ／ａ，同时，旨出１９９６年中世界人口１８．８％的北美、欧洲、日本、ＣＯ２排放３１．６亿ｔ（碳），占全球当年ＣＯ２排放总量的５２．４％。     

四川省金川县土地利用结构的初步研究

金川县地处青藏高原向横断山脉深切峡谷过渡地带,在土地利用上具有明显的立体结构。森林采伐、土地开垦都在不断改变土地利用的状况。怎样合理利用土地,成为目前突出的问题。本文以1/20万土地利用现状图量算面积及1984年以前的统计资料为基础,着重分析了土地利用结构及其调整问题。     

荷兰与欧盟环境培训考察报告

2002年5月19日至6月10日,荷兰鹿特丹住宅与城市发展研究学院(1HS)举办的中国市长、环保局长、专家环境管理与可持续发展培训班给我们一些有益的启示,西方国家的经验与政策对我国解决环境问题具有借鉴意义。     

Alternating nitrification-denitrification via nitrite for nitrogen removal from soybean wastewater by SBR with real-time control

A novel treating technology for nitrogen removal from soybean wastewater was studied. The process for nitrogen removal was achieved by alternating aeration and mixing, combined with real\|time control strategies. Results showed that the COD and total nitrogen removal rates are more than 90% and 92% at COD and total nitrogen loads of 1.0-1.2 kg COD/(kgMLSS·d) and 0.20-0.27 kg TN/(kgMLSS·d), respectively. In addition, it could improve sludge settling property. SVI value is less than 70 g/ml during the whole cycles. The method not only may be adapted to treat soybean wastewater with high nitrogen, but also may be applied to treat other high nitrogen wastewater.     

模拟海洋全浸区环境下A517海工钢的腐蚀机理研究

目的 探究 A517 海工钢在海洋全浸区环境下的腐蚀机理。方法 通过模拟海洋全浸区腐蚀环境,利用失重法、SEM、EDS、XRD、电化学等测试技术,分析A517钢的腐蚀行为历程,并探讨其在全浸区的腐蚀机理。结果A517钢在厚度方向上的最大电位差为 13 mV,小于发生电偶腐蚀的最小电位差50mV,说明材料在厚度方向上的腐蚀敏感性一致。随浸泡时间的延长,腐蚀质量损失量逐渐增加,平均腐蚀速率先降低、后升高、最后趋于稳定,腐蚀速率约为 0.127 mm/a。结论 腐蚀动力初期主要是由溶解氧的极限扩散控制,后期则是腐蚀产物的氧化还原电荷转移控制。腐蚀首先在 Al₂O₃、MgO 等夹杂物处萌生扩展,腐蚀产物出现明显的分层现象,外锈层主要是疏松易脱落的γ-FeOOH,内锈层主要是致密均匀的 Fe₃O₄,同时锈层中还检测到了β-FeOOH和α-FeOOH的存在。锈层中存在大量微裂纹,削弱了产物膜的保护作用,促进了腐蚀的进行。     

洪泽湖富营养化和生态状况调查与评价

为了解洪泽湖水质状况，对2000年洪泽湖富营养化状态和生态特性的调查结果进行了分析，洪泽湖水中总磷、总氮和高锰酸盐指数年均值超《地表水环境质量标准》（GHZB1-1999）中Ⅱ类水标准，超标倍数分别为12倍、10倍和0.24倍；总磷、总氮、透明度年均值超湖库特定项目V类标准，洪泽湖处于中-富营养化状态。对洪泽湖生态特性分析表明，由于洪泽源独特的湖泊形态，“藻型浊水状态“和“泥沙型浊水状态“交替出现，遏制了湖水从高营养盐含量向全面富营养化状态演变，保证了底栖动物的良好生长环境，从而形成了洪泽湖独特的环境生态平衡状态。