浅议提高废水污染源监测数据代表性

对废水污染源监测中影响监测数据代表性的主要因素进行了分析,并对提高废水污染源监测数据代表性提出了可行性建议。     

农业清洁生产与东圳水库饮用水源保护

以东圳水库为例论述了饮用水源保护与库区果园实行农业清洁生产的关系，并对饮用水源的保护提出一些对策措施。     

上海市扬尘污染源遥感解译及其管理信息系统

利用遥感影像资料,分析了上海市扬尘污染源的空间分布特征与规律,并计算了上海市主要扬尘源的起尘量。利用获取的基础数据,建立了上海市扬尘污染源管理地理信息系统,为上海市扬尘污染源的控制管理提供了依据。     

炼油厂污水的综合治理

针对近年炼油厂高污染负荷污水增加问题,就采取预处理措施减少污染负荷及改进污水处理工艺提高污水处理能力进行了探讨,并提出污水综合治理方案.     

任意风向时的线源扩散模式研究

给出了一个适用于风向与公路成任意夹角的有限长线源的扩散模式;讨论了不同风向、线源长度等,对线源中心下风距离的污染物地面浓度的影响;并将这个模式与CALINE-2模式和风洞试验结果进行了比较。     

松华坝饮用水源区补偿政策探讨

根据昆明政府颁布的《昆明市松华坝水源保护区生产生活补助办法（试行）》要求，在系统探讨了松华坝水源保护区实施补助的重要性和必要性的基础上，分析了办法实行可能产生的效果，并针对性地提出实施建议。     

滇池流域农田氮、磷肥施用现状与评价

2001年6月至9月分别对流域内晋宁，呈贡，西山，官渡和嵩明调查了365家农户有关化肥施用情况，调查分析和计算表明，每年从种植业流失的化肥中纯氮（N）达2575t，纯磷（P）达218t，蔬菜和花卉地的单位面积氮流失量是水田和旱地的7-20倍。菜地年每公顷流失氮204kg，水田的氮流失量最低，平均每公顷每年流失10kg。磷的流失也以蔬菜，花卉地为最高，蔬菜和花卉地的单位面积磷流失量是水田和旱地的9-10倍。研究结果证明，大量的氮，磷化肥施用，通过地表径流和地下水流入滇池是造成其水体富营养化的重要原因之一^[6]，随着农业和农村经济的发展，蔬菜，花卉等经济作物在滇池流域的种植面积将会逐年扩大，因氮，磷化肥的施用面造成的氮，磷流失量将会不断加大，为了实现减少氮，磷化肥对滇池的污染，应积极推广精确施肥，平衡施肥等科学施肥技术，提高化肥利用率，减少化肥流失。增施有机肥，降低化肥用量，同时提高农村居民的环境意识，加强环境管理，依法保护农村环境，控制农业面源污染。     

Adaptations to the dynamics of rural water supply from natural sources: A village example in semi-arid Nigeria

Domestic and agro-economic activities in the semi-arid region of Nigeria rely exclusively on rainfall, streamflow and groundwater in deep and alluvial (fadama) aquifers. Such water supply systems are subject to considerable seasonal and inter-annual variability. However, a combination of the various sources may mitigate the effects of water scarcity. This study describes the dynamics of the water sources for a village in northeastern Nigeria as an example that demonstrates the linkages between rainfall, streamflow and groundwater. Such linkages are important for developing strategies to mitigate the effects of climatic variation. Long-term records of rainfall were not available at the site so that the short-term data was interpreted in the context of the long-term climatic experience of the region. The stratigraphic profile of the aquifer was developed from resistivity methods, to supplement information obtained from well level hydrographs. Field observations and analysis of the data reveal that the beginning of the rainy season is a precarious period because none of the water sources are reliable. Rainfall infiltration recharges the shallow aquifers while lateral water flux from the floodwater-saturated fadama also contributes to water level rises in the deep wells. A study of the water level changes in response to deepening of the wells suggests that the wells are fed by an assortment of water-bearing lenses, separated by layers of low transmissivity. One major finding of this study is that there exists a close association between the wells in this riparian community and the recharge processes within the fadama. Upstream diversion, abstraction or impoundment could therefore undermine the viability of aquifer exploitation by the communities in the riparian zone. Analysis of the interactions among the various sources of water leads to the identification of several potential adaptation strategies for confronting the problem of water scarcity.     

金堆城超大型钼矿床水-岩δD-δ~(18)O同位素交换体系理论模型及成矿流体来源

基于水-岩δD-δ18O同位素交换体系理论模型的建立和计算，对金堆城超大型斑岩钼矿四个不同成矿期中成矿流体的演化和来源进行了研究，发现在成矿前期和早期，成矿流体为岩浆水与围岩在较低水／岩比值（0．1W／R＞0．001）和中、高温（t=250～500℃）条件下反应后的残余流体，而主成矿期和成矿晚期的成矿流作为大气降水在相对较高水／岩比值（0．5＞W／R0．1）和中、低温（t＝150～310℃）条件下与围岩反应后的残留流体。大气降水在金堆城钼矿成矿过程中起了重要作用。在主成矿期水／岩比值达到最高。     

抚仙湖面源污染特征及其防治对策

根据抚仙湖径流区污染物负荷量的调查结果,抚仙湖水污染特征以面源为主,面源入湖水量占98%,TP占81.4%,TN占85.9%,因此控制面源是保护抚仙湖的关键。提出了防治抚仙湖面源污染的生态治理及工程治理对策。