长江南通段污染带影响因素研究

通过建立应用贴体坐标系和有限体积法求解的二维水流－水质方程的模型，对潮汐河口南通段污染带的影响因素进行研究。揭示了水深、水面比降、纵向及横向混合系数以及污染物的排放时段与污染带范围的相关关系，并进行了各影响因素的灵敏度分析，对灵敏度大小进行了排序：水深＞水面比降＞横向混合系数＞纵向混合系数＞排放时段。     

广东-海南海岸带生态系统服务价值评估

采用Costanza等的分类系统和相关服务的单位价值，根据广东省1987年海岸带和海涂资源综合调查报告和其他相关资料，初步估算出广东—海南海岸带的生态系统服务的总价值为316．97亿美元／a，其中陆地为187．38亿美元／a、海域为129.59亿美元／a。该总价值占全国总价值的407％，养分循环、水分调节、休闲和水分供给等服务的价值突出，分别为全国总价值的6．17、3.98、3．66和3.37％由于自然生态系统的复杂性和不确定性，以及计算参数和方法存在缺陷，因而得到的只是一个偏低的保守值，有待今后改进。     

有机污染物在多孔介质中的残留

土壤、地下水中的有机污染物主要以自由态、挥发态、溶解态和残留态等四种形态存在 ,其中残留态的部分是最难以去除的 ,残留量的多少是关系治理费用及治理时间长短的最关键因素。本文以柴油为代表 ,对地下水饱和区中有机物的残留进行了试验模拟 ,与非饱和区的残余饱和度进行了比较 ,揭示了饱和区中有机污染物残余的特点 ,并深入分析了其机理。结果表明 ,砂性介质中 ,地下水饱和区中有机污染物的残余饱和度显著大于非饱和区中的残余饱和度 ,因此可以有效地利用这一特性 ,通过降低地下水位使饱和区中部分残留态污染物转化为自由态 ,提高去除效率 ;与非饱和区中多孔介质粒径越小 ,残留量越大的特性相反 ,饱和区中测得的残余柴油饱和度随介质粒径的增大而增大。不同水位变动速度的试验结果表明 ,水位变动速度对粘性大于水的柴油的残余饱和度影响可以忽略不计。     

Ecological-breaking zone originates and its ecosystems reconstruction in arid area

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草原干旱对天然牧草生长发育及产量形成的影响

天然牧草是放牧畜牧业的主要物质基础 ,其生长动态和产量形成受气象条件的影响和制约 ,特别是水份条件在很大程度上决定着植物的地理分布和生物生产力水平。本文根据大气降水量及土壤水份条件与天然牧草生长动态及产量的关系 ,建立了天然牧草生长高度动态模式和草原初级气候生产力模式 ,以便进一步研究 ,为草原干旱的气候指标提供理论依据     

COALBED METHANE PRODUCT WATER CHEMISTRY IN THREE WYOMING WATERSHEDS1

ABSTRACT: The Powder River Basin in Wyoming has become one of the most active areas of coalbed methane (CBM) development in the western United States. Extraction of methane from coalbeds requires pumping of aquifer water, which is called product water. Two to ten extraction wells are manifolded into one discharge point and product water is released into nearby unlined holding ponds. The objective of this study was to evaluate the chemistry, salinity, and sodicity of CBM product water at discharge points and associated holding ponds as a function of watershed. The product water samples from the discharge points and associated holding ponds were collected from the Cheyenne River (CHR), Belle Fourche River (BFR), and Little Powder River (LPR) watersheds during the summers of 1999 and 2000. These samples were analyzed for pH, electrical conductivity (EC), total dissolved solids (TDS), alkalinity, sodium (Na), calcium (Ca), magnesium (Mg), potassium (K), sulfate (SO₄^2‐), and chloride (C^1‐). From the chemical data, practical sodium adsorption ratio (SARp) and true sodium adsorption ratio (SARt) were calculated for the CBM discharge water and pond water. The pH, EC, TDS, alkalinity, Na, Ca, Mg, K, SARp, and SARt of CBM discharge water increased significantly moving north from the CHR watershed to the LPR watershed. CBM discharge water in associated holding ponds showed significant increases in EC, TDS, alkalinity, Na, K, SARp, and SARt moving north from the CHR to the LPR watershed. Within watersheds, the only significant change was an increase in pH from 7.21 to 8.26 between discharge points and holding ponds in the LPR watershed. However, the LPR and BFR exhibited larger changes in mean chemistry values in pH, salinity (EC, TDS), and sodicity (SAR) between CBM product water discharges and associated holding ponds than the CHR watershed. For instance, the mean EC and TDS of CBM product water in LPR increased from 1.93 to 2.09 dS/m, and froml,232 to 1,336 mg/L, respectively, between discharge and pond waters. The CHR exhibited no change in EC, TDS, Na, or SAR between discharge water and pond water. Also, while not statistically significant, mean alkalinity of CBM product water in BFR and LPR watersheds decreased from 9.81 to 8.01 meq/L and from 19.87 to 18.14 meq/L, respectively, between discharge and pond waters. The results of this study suggest that release of CBM product water onto the rangelands of BFR and LPR watersheds may precipitate calcium carbonate (CaCO₃) in soils, which in turn may decrease infiltration and increase runoff and erosion. Thus, use of CBM product water for irrigation in LPR and BFR watersheds may require careful planning based on water pH, EC, alkalinity, Na, and SAR, as well as local soil physical and chemical properties.     

地下水污染潜势评估方法及应用

本文阐述了地下水污染潜势评估的重要性，介绍了三种方法，对其中的废物－土址－地点相互作用列表法作了详细介绍，并将ＷＳＳＩＭ法用于四川省什邡县化工开发区地下不污染潜势估。     

Pressures,trends, and impacts in coastal zones: Interactions between socioeconomic and natural systems

This paper assesses the status of coastal zones in the context of expected climate change and its related impacts, as well as current and future socioeconomic pressures and impacts. It is argued that external stresses and shocks relating to sea-level rise and other changes will tend to exacerbate existing environmental pressures and damage in coastal zones. Coastal zones are under increasing stress because of an interrelated set of planning failures including information, economic market, and policy intervention failures. Moves towards integrated coastal zone management are urgently required to guide the coevolution of natural and human systems. Overtly technocentric claims that assessments of vulnerability undertaken to date are overestimates of likely future damages from global warming are premature. While it is the case that forecasts of sea-level rise have been scaled down, much uncertainty remains over, for example, combined storm, sea surge, and other events. In any case, within the socioeconomic analyses of the problem, resource valuations have been at best only partial and have failed to incorporate sensitivity analysis in terms of the discount rates utilized. This would indicate an underestimation of potential damage costs. Overall, a precautionary approach is justified based on the need to act ahead of adequate information acquisition, economically efficient resource pricing and proactive coastal planning.