京津地区能源、大气污染物扩散对区域元素循环的作用

对京津区域１９８０－１９９２年间能源利用状况进行分析，并通过模式计算该区域大气污染物的扩散规律，结果表明，大气污染物随能源利用增加而增加，其增加速率ＮＯｘ大于ＯＳ２，经预测，至２００４年京津地区ＳＯ２排放量增咖１１．４０％，ＮＯｘ增加５６．８０％，由于气象和地形条件所致，该区域内不利于大气污染物远距离输送，这使箱型区域内物料平衡计算可以简化。     

久效磷对海洋微藻毒性机理的初步研究Ⅲ.超氧化物歧化酶和过氧化物酶活性的变化

报道了久效磷对３种海洋微藻细胞内２种清除活性氧的关键性酶－超氧化物歧化酶和过氧化酶活性的影响。结果显示：１．在久效磷的胁迫下，扁藻和三角褐指藻细胞的超化物歧化酶活性均表现出下降的总变化趋势，而叉鞭金藻细胞的ＳＯＤ活性时而上升，时而下降，在整个胁迫过程中呈现出无规律性的变化。２．随着久铲磷胁迫时间的延长，３种微藻细胞的过氧化酶活性均逐渐下降，表现出相同的变化规律性。     

1952-2016年长江经济带天然与人为氮输入时空演变

过量氮输入是水体氮污染的关键驱动因子，解析氮输入的结构和时空变化模式成为氮素环境管理的重要基础和难点.基于1952—2016年长江经济带各地区氮活动数据，分别构建了天然氮输入和人为氮输入模型，评估了氮输入负荷的时空变化特征.结果表明：①长江经济带氮输入负荷总体越过EKC曲线拐点进入由增长向下降的发展阶段，拐点出现在人均GDP为35777~36299元·人^-1时，发生时间为"十二五"时期，主要原因是化肥和食物输入下降；②氮输入负荷存在显著的时空差异，东部地区表现为倒U型，中部为S型，西部为J型，表明氮负荷存在从东向西的空间转移，西部地区成为氮输入负荷增长的热点地区，这与东部地区化肥施用量下降有关；③人为输入是长江经济带氮输入的主要来源，输入量及其占总输入的比例均呈现显著的增长趋势，空间上表现为从西到东部逐步递增的变化规律，与氮驱动力分布一致；④植被的多年平均固氮量为1771 kg·km^-2·a^-1，其中，非农作物的固氮速率为763 kg·km^-2·a^-1，植被固氮量的年际波动较小，天然输入对长江经济带总体氮输入影响较小.     

团结协作开创未来--卢鉴章主任委员在中国煤炭学会环境保护专业委员会1999年年会暨学术研讨会上的讲话(摘要)

中国煤炭学会环境保护专业委员会1999年年会暨“煤矿矿区水资源保护与水资源化”学术研讨会今天在宜昌召开,这是我们专业委员会成立后的第四次年会,也是第四次学术研讨会。在此,谨向参加这次会议的同志们表示热烈的欢迎和感谢！     

于桥水库流域暴雨径流中锰的输送特征及其对水库水质的影响

对于桥水库流域内暴雨径流中锰含量形态的研究表明,锰主要以悬浮状态存在,其中易释放的、潜在释放的和非释放形态的锰所占比例分别为10％、60％和30％.以溶解态迁移的锰极少.流域内的锰矿-含锰页岩带提高了暴雨径流中总锰的浓度,对于桥水库水质造成了一定的影响.     

WebGIS在水资源环境监测中的应用

采取面向对象软件设计思想．利用网络数据库技术，WebGIS技术等，设计水资源环境监测系统。分析了系统结构与功能模块以及数据库构成及系统安全性保障。     

约束求解的数据模型及算法

此文针对参数化造型系统中约束方程组的求解问题,深入分析了匹配求解的核心思想,提出了一种简单实用的约束网络建模方法,并且围绕该数据模型介绍了与其相关的算法.     

Sequence analytical approach to the Upper Kimmeridgian-Lower Tithonian storm-dominated ramp deposits of the Boulonnais (Northern France). A landward time-equivalent to offshore marine source rocks

An interdisciplinary approach based on high-resolution physical stratigraphy, biostratigraphy, organic matter analysis and clay mineralogy has been applied to the mixed siliciclastic/carbonate Kimmeridgian/Tithonian deposits of the Boulonnais (north-western France). These rocks are the age-equivalents of some of the offshore marine source rocks of the North Sea and were deposited in an overall storm-dominated homoclinal ramp setting which may represent one of the most shore-proximal sediments of this age cropping out in north-western Europe. Comparison with data from the Yorkshire, Dorset, Lorraine and Aquitaine areas allows the discrimination of three major transgressive-regressive sediment packages with disconformities of interregional extent: (1) from the Baylei Zone to top Eudoxus Zone; (2) from the Autissiodorensis Zone to base Scitulus Zone; (3) from the upper Scitulus Zone to the Pectinatus Zone. The lower two regionally correlative disconformities correspond to the sequence boundaries at the top of the Eudoxus Zone and the top of the Autissiodorensis Zone, formed by high-frequency relative sea-level variations during the periods of maximum transgression of the platform. The latter disconformity (the P1 nodule bed) reflects a major tectonically induced reorganization of the north-west European intrashelf sedimentary basin, characterized by a shift in both the location of the main depocentre and the sources of sediment production.     

XII Ecdysone Workshop July 22–26, 1996 Barcelona,Spain

XII Ecdysone Workshop July 22–26, 1996 Barcelona, Spain     

Effects of atmospheric gases on terrestrial plants and critical levels of air pollution

An integrated approach was developed to determine the critical levels of air pollution for ecological standard setting based on the unified index of biological response, by taking into account the effects of all pollution components simultaneously. An empirical model of plant productivity was taken as the dose response model for gaseous pollutant effect on the productivity of trees and the annual productivity of plants was used as the above mentioned index. The CO2 increase in the lower atmosphere was considered to potentially increase plant productivity and NO2 was estimated as neutral while being dangerous for plants as a chemical precursor of ozone or as a source of acidification. The maximum permissible chronic O3 and SO2 levels for trees were estimated and it was found that O3 is much more phytotoxic, as compared to SO2 , with a rather narrow range of permissible levels (27-33 ppb) which complicates its monitoring and control.