跨界水环境治理的政府间协作机制研究

以跨界水环境治理中政府间协作关系的困境为研究对象,分别从行政分割、法律缺失、治理机制以及财政分担机制不完整等方面探讨了地方政府在跨界流域治理过程中陷入协作困境的原因,并据此提出了建议,即强化政府间认同机制、明确法律保障制度、完善水环境政府治理体制和政府投资机制等。最后以太湖流域为例,结合太湖水环境治理的特点,剖析了其治理现状及困境,提出了该流域政府间协作治理的对策建议。     

洱海水硫化物及六价铬含量的检测分析

目的:了解洱海水硫化物及六价铬含量。方法:采集洱海20个点的水样对硫化物及六价铬的含量进行检测,分别采用亚甲蓝分光光度法,二苯碳酰二肼分光光度法进行测定。结果按照《地表水环境质量标准进行评价》。结果:硫化物、六价铬合格率为100%。结论:硫化物、六价铬均达到GB 3838-2002《地表水环境质量标准》的一类水质。     

Climatic significance of n-alkanes and their compound-specific dD values from lake surface sediments on the Southwestern Tibetan Plateau

The content and hydrogen isotope ratios of n-alkanes extracted from recent lake surface sediments sampled from nine lakes in three different climate zones on the Southwestern Tibetan Plateau were analyzed.Values were compared with n-alkanes in plants from lake drainages,and dD values of meteoric water,lake water,and mean annual precipitation.The results showed that n-C23was predominantly derived from aquatic plants,and n-C27–n-C33from terrestrial higher plants.The average carbon chain length of n-C27–n-C33(ACL27–33)was positively correlated with the mean annual precipitation.dD values of the long-chain n-alkanes n-C29and n-C31of terrestrial origin(varying between-214%and-169%,and-226%and-185%,respectively)were inversely correlated with mean annual precipitation;but in accordance with the average annual variations in dD(OIPC),dD values of n-C31were strongly related to the dD values of growing season meteoric water(R2=0.74).The large difference between dD values of n-C23of aquatic origin and n-C31(an average of about 27%)demonstrates the enrichment of the lake water dD compared to precipitation,caused by strong evaporation in the semiarid–arid areas of the southwestern Tibetan Plateau.Average value of en C25 31=p(-95%)is evidently higher than the value observed in European wet regions(-128%);besides,en C31(about-116%)is constant along the study transect(SD=9),which indicates that n-C31is a useful proxy for the environment.     

Sediment records of Sb and Pb stable isotopic ratios in Lake Qinghai

A sediment core in Lake Qinghai in northwest China was collected in 2006. ¹³⁷Cs and ²¹⁰Pb activities were analyzed to investigate the chronology of the sediment core. Sb and Pb concentrations, and Pb stable isotopic ratios were analyzed to study the historical atmospheric deposition records and sources of Sb over the past 15 centuries. The Sb concentration was 4.21 ± 1.52 μg/g in the sediments, its vertical distribution of Sb shows three large peaks in the recent two centuries, 1799, 1896 and 1944, coincided with Sb contamination from large wars, respectively. The peak in 1920 responded the large earthquake that happened in northern China, which was not far away from Lake Qinghai. The Sb/Pb ratio, ²⁰⁶Pb/²⁰⁷Pb and ²⁰⁸Pb/²⁰⁶Pb results suggest that Sb and Pb were probably from the ores in South China and coals in North China before 1965, but obviously from uses of leaded gasoline after 1965.     

湖北网湖^137Cs、^210Pb计年与沉积速率研究

采用放射性核素^137Cs和^210Pb计年法测定百年来湖北网湖沉积物的年代,据此计算出网湖的沉积速率．结果表明：2种计年方法测得的沉积速率基本一致,以1954年和1963年为时标,^137Cs测得的沉积速率分别为0．594cm·a^-1和0．557cm·a^-1。^210Pb计年法CIC模式计算得到网湖平均沉积速率为0．56cm·a^-1．CRS模式得到百年来网湖沉积速率变化较大,20世纪50年代以前,平均沉积速率为0．2cm·a^-1左右;50年代至80年代中期,平均沉积速率上了一个台阶,约为0．4cm·a^-1;80年代中期以后平均沉积速率攀升至约0．6cm·a^-1,网湖沉积速率变化与湖区自然环境的改变和人类活动的影响密切相关．     

东疆北部地区小冰期环境特征的湖相沉积记录

本文根据新疆东疆北部巴里坤湖湖相沉积的孢粉及地球化学元素含量分析，运用因子分析法处理数据，恢复了巴里坤地区近５００年来的环境演变序列。广泛的区域性对比表明，所获结果具较高可信度，故本文不但获得了在新疆地区由湖相沉积所揭示的小冰期以来的环境演变信息，另一方面丰富了本地区短时代环境演变研究的方法和手段。     

鄱阳湖三维水质模拟软件设计与仿真

随着鄱阳湖生态经济区建设的推进,鄱阳湖水环境保护问题引起了各方高度关注。通过建立水质数学模型,用计算机进行模型求解、模拟和预测,以及设计相应的水质模拟仿真软件来进行水污染扩散仿真,是水污染控制和水环境管理的有效手段。鉴于国外三维水质数据模拟软件价格高、使用受限以及鄱阳湖三维水质数据模拟的特定应用研究需求,利用软件工程的结构化方法和图形可视化技术,设计了一个面向鄱阳湖三维水质数据模拟和分析的软件工具WSAT/H3D-PYH。通过使用该软件进行BOD和DO扩散模拟和趋势预测实验表明,软件具有较好的预测精度,并能以可视化形式直观分析和预测未来一段时间湖区水质浓度的变化趋势。此外,软件还可对局部点污染源扩散进行动态模拟,以便于对突发污染事件可能造成的后果进行提前的估计,为后续治理方案措施的制定提供很好的依据。     

Harmonizing model with transfer tax on water pollution across regional boundaries in a China’s lake basin

This paper presents a bilevel programming framework for a harmonizing model with transfer tax (HMTT) on water pollution across regional boundaries of a lake basin in China, where the administrator is the upper-level decision maker and individual regions consisting of the lake basin are the lower-level decision makers (followers). Leader’s cost is the total pollution reduction cost, whereas each region selfishly minimizes its own cost including reduction cost and transfer cost, given the transfer tax rate imposed by the leader. The HMTT guarantees that the imposed environmental quality standard is met through the transfer tax. Based on the KKT conditions of an auxiliary problem, we obtain that the solution set of the HMTT is nonempty. An algorithm is proposed, with the convergence result, to compute the cost-minimized transfer tax rate along with the reduction quantities of individual regions. Theoretical analysis and a case study for China’s Taihu Lake Basin show that the HMTT is superior to the current model of proportional share of pollution reduction (MPSPR). The HMTT not only solves the problem of conflicts over water pollution across regional boundaries but also utilizes the resources of the lake basin more efficiently.     

洞庭湖区洪涝灾害的形成机制分析

为搞好洞庭湖区洪涝灾害的预测和防灾减灾,促进湖区经济建设,本文对洞庭湖区洪涝灾害的形成机制进行了分析研究.结果表明:80 %特大洪涝灾害的发生在厄尔尼诺年的次年,其内在机制是厄尔尼诺事件所导致的全球气候异常.大气环流的异常是洪涝发生的根本原因,主要表现在有特大洪涝年汛期,位于110°~120°E的西太平洋副高脊线位置都稳定处于19°~24°N之间,且越过24°N的时间大致与城陵矶年最高水位出现时间相吻合;西风带形势稳定;印度低压偏强并持续稳定.洞庭湖区洪涝与湖区、四水流域、长江上游东部区和西部区等广泛地域的降水密切相关,汛期在这4个区域第一次大范围的强降水过程以后20 天各代表站降水量总和的平均值对洞庭湖的洪涝预测具有决定性意义.     

近代洞庭湖沉积与孕灾环境研究

通过对洞庭湖区不同沉积部位的22个钻孔取样和^210Pb放射性同位素测年分析，洞庭湖有较高的沉积速率，最高可达2．33cm／a，不同的沉积部位沉积速率也有较大的差异。由于19世纪以来四口分流形成，大量长江的泥沙进入洞庭湖，近50年的水文资料表明，洞庭湖83％的泥沙淤积来源于长江。由于人类围垦、上游森林砍伐和洲滩堤坝的逐年加高，洞庭湖水面减少了2／3，洞庭湖对长江洪水的调蓄能力已迅速减弱。洞庭湖的演变变化过程直接影响到长江中游的生态安全。