黄河流域近40年蒸发皿蒸发量的气候变化特征

利用黄河流域及其周边123个气象站1961～2000年20cm口径蒸发皿资料,分析了黄河流域蒸发皿蒸发量的气候变化趋势。结果表明,就整个流域平均而言,尽管在1960～2000年期间,黄河流域年平均温度升高了0.6℃,但蒸发皿蒸发量却呈明显下降趋势,黄河流域年蒸发皿蒸发量在20世纪80～90年代较60～70年代下降了136mm,下降幅度为7.5%;蒸发皿蒸发量的下降主要表现在夏季和春季,秋季和冬季不明显。对蒸发皿蒸发量气候变化的空间分析表明,局部区域与整个流域的气候变化趋势并不完全同步,黄河流域上游和下游蒸发皿蒸发量呈下降趋势,中游呈持平并略有上升趋势。     

教室内二氧化碳污染和新风量测定

新风量不足,呼吸产生的二氧化碳可造成教室内CO_2浓度严重超标,影响学生学习,降低课堂教学效果。以人呼出的CO_2作为示踪气体,测定研究教室有人和无人情况下教室内CO_2浓度变化,对教室新风量进行计算,其结果:室内CO_2排放条件不同,相应方程计算所得新风量基本一致,用忽略室外CO_2本底浓度的新风量计算公式,结果有约17%的误差。开启门窗产生对流,可保障教室内空气的新鲜。     

水中天然有机物的臭氧强化光催化降解研究

研究了饮用水源中大分子天然有机物（NOM）的臭氧强化光催化降解,考察了臭氧投加量、反应时间和HCO3^-浓度对NOM降解速率的影响;分析了臭氧强化光催化过程中NOM相对分子质量的变化,并比较不同相对分子质量大小NOM的降解速率.研究结果表明,臭氧强化光催化比单独臭氧氧化、光催化能更有效地降解NOM,同时增加臭氧投加量和反应时间才能有效提高臭氧强化光催化对TOC的去除率,而单独增加臭氧投加量可显著提高生物可降解性;HCO3^-显著降低光催化的降解效果,臭氧强化光催化能有效地减弱HCO3^-的不利影响;臭氧强化光催化过程中大分子NOM分解为小分子,SUVA值迅速下降,且相对分子质量越大矿化速度越快.     

Human adaptation to climate change: a review of three historical cases and some general perspectives

To study mitigation and adaptation to climate change, social scientists have drawn on different approaches, particularly sociological approaches to the future and comparative history of past societies. These two approaches frame the social and temporal boundaries of decision-making collectivities in different ways. A consideration of the responses to climate variability in three historical cases, the Classic Maya of Mexico and Central America, the Viking settlements in Greenland, and the US Dust Bowl, shows the value of integrating these two approaches.     

极端干旱气候下盐化草甸植被净初级生产力对全球变化的响应

利用作者建立的塔里木盆地北部盐化草甸植被净初级生产力模型 ,模拟了极端干旱气候下盐化草甸植被净初级生产力对全球变化的响应。结果表明 ,在一定土壤质地条件下 ,盐化草甸植被净初级生产力随地下水埋深的增加而逐渐下降。地下水埋深越大 ,盐化草甸植被净初级生产力对地下水埋深变化的响应越敏感。全球变化造成的温度升高对盐化草甸植被净初级生产力的影响 ,也是依地下水埋深的不同而有所差异。地下水埋深较小时,盐化草甸植被净初级生产力对温度升高的反应较小 ;随着地下水埋深的加大,其响应程度明显增加。因而 ,地下水埋深越大 ,盐化草甸植被净初级生产力对全球变化的响应就越明显。     

Analysis on reasons for the Yellow River''s dry-up and its  eco-environmental impacts

The Yellow River, or Huanghe, is one of the most important river in China. It is the major water resources for north and northwest China. Since 1972, the Yellow River's dry-up has occurred frequently and become even more year by year. Except the huge loss to social life and economic development, the Yellow River's dry-up brings about great impacts to eco-environment. This paper analyzed the reasons and impacts from multi-aspect: effects of climate change, influence of human activities and impacts to delta's eco-environment, aquatic life resources, agricultural eco- environment, water pollution and flood prevention as well.     

全球环境变化与全球不平等南北方的不同立场

全球环境变化给发展中国家和南北关系带来深刻影响，理解环境问题的全球不平等需要以发展中国家80年代开始的经济结构调整和沉重债务为背景。南方的环境政策优先在很大程度上与其生活的可持续性相连，而不是通常与全球环境变化的长期性风险相关，然而，全球环境变化又与发展中国家贫困人口的日常生活紧密相关。从南方的立场看，当“问题”对他们不十分迫切时，就很难同意采取措施，仅此原因，北方对全球环境变化的关切要得到成功回应，真正的全球契约就需要解决基本“发展”问题，主要是贫困。     

季节变化对海洋鱼体内EROD活性的影响

利用2001～2003年对大连大长山岛海域不同季节EROD活性的监测结果,分析了季节变化对海洋鱼体内EROD活性的影响.结果表明,春季海洋鱼体内EROD活性明显高于夏季和秋季.利用EROD活性进行海洋环境污染的监测,不宜选在背景值较高的春季进行.     

杞麓湖主要污染物的动态变化特征研究

以１９９７年杞麓湖水质监测结果为基础，运用相关分析，双因子方差分析等方法，对杞麓湖主要污染物动态变化特征的研究结果表明，杞麓湖主要污染物的空间分布较为均匀；ＢＯＤ５和ＴＮ都有较为明显的季节变化。     

Impacts of climate change on wheat development and production in the northern China

In this paper, impacts of climate change on wheat development rate and production in the northern China are discussed. The results show that the temperature is a controlling factor of development rate but the precipitation is not. The higher the temperature is. the faster the development and the shorter development period will be. Without consideration to varieties and cropping system, meteorological yield of winter wheat would decrease 170.40, 134.25, 98.70 and 97.20 kg/hm2 in the north China and 13.97, 7.95, 39.60 and 19.80 kg/hm2 in the northwest China compared with that in 1950s, 1960s, 1970s and 1980s, respectively, when the CO2 concentration in the atmosphere is doubled. In drought and semi-drought regions, the spring wheat yield would drop with the temperature rise in and raise with the precipitation increase. The influence of temperature on weight of leaf and stalk is also remarkable.