嘉峪关市降水偏碱性的成因初探

通过对区域近年来的降水监测数据的收集、整理和分析,探求区域降水特点及主要成因。     

Monitoring the results of Canada/U.S.A acid rain control programs: some lake responses

Aquatic acidification by deposition of airborne pollutants emerged as an environmental issue in southeastern Canada during the 1970s. Drawing information from the extensive research and monitoring programs, a sequence of issue assessments demonstrated the necessity of reducing the anthropogenic emissions of acidifying pollutants, particularly sulphur dioxide (SO₂). The 1991 Canada-U.S. Air Quality Agreement (AQA) was negotiated to reduce North American SO₂ emissions by 40% relative to 1980 levels by 2010, and at present, both countries have reduced emissions beyond their AQA commitment. In response to reduced SO₂ emissions, atmospheric deposition of sulphate (SO₄ ^2–) and SO₄ ^2– concentrations in many lakes have declined, particularly in south-central Ontario and southern Québec. Sulphate deposition still exceeds aquatic critical loads throughout southeastern Canada however. Increasing pH or alkalinity (commonly deemed recovery) has been observed in only some lakes. Several biogeochemical factors have intervened to modify the lake chemistry response to reduced SO₄ ^2– input, notably release of stored SO₄ ^2– from wetlands following periods of drought and reduction in the export of base cations from terrestrial soils. Three examples from Ontario are presented to illustrate these responses. Significant increases in pH and alkalinity have been observed in many lakes in the Sudbury area of Ontario due to the large reductions in local SO₂ emissions; early-stage biological recovery is evident in these lakes. An integrated assessment model predicts that AQA emission reductions will not be sufficient to promote widespread chemical or biological recovery of Canadian lakes. Monitoring and modeling are mutually supporting assessment activities and both must continue.     

The Precision of Precipitation Chemistry Measurements in the Canadian Air and Precipitation Monitoring Network (CAPMoN)

Precision estimates are presented for precipitation chemistry and depth measurements made by the Canadian Air and Precipitation Monitoring Network (CAPMoN). The estimates were made for daily measurements of ion concentration and precipitation depth as well as for weekly, 28-day, seasonal and annual precipitation-weighted mean concentrations and depths. The data on which the estimates are based were collected from collocated samplers at five CAPMoN sites during the period 1985 to 1993. The data pairs from the collocated samplers were used to calculate the between-instrument error defined as 1/2 times the difference between the paired sample concentrations (or depths). For all of the ion concentrations and depths, the between-sampler errors were found not to be normally distributed, but the normality of the distributions improved with the length of the (volume-weighting) time period considered. A set of quantitative measures of overall network precision were derived in absolute (mg L^-1) and relative (%) units. These included the Modified Median Absolute Deviation (M.MAD), the P90% probability values and the Coefficient of Variation (CoV). The latter, defined as the percent ratio of the M.MAD to the median concentration (or depth), represents the relative precision at the center of the error and concentration (and depth) distributions. Based on the CoV values, the relative precision of the CAPMoN measurements was very high (better than 4%) for SO ₄ ^2- , NO ₃ ^- , pH, H⁺, NH ₄ ⁺ , sample depth and standard gauge depth, and not as high (between 10 and <35%) for Cl^-, Na⁺, Ca²⁺, Mg²⁺, and K⁺. The ions with the lowest median concentrations had the poorest relative precision since so many of the concentrations were at or near the analytical detection limit. Except for the sample and standard gauge depths, both the absolute and relative precision improved with the length of the precipitation-weighting period. Detailed statistical testing established that the precision of the daily measurements is dependent on a number of factors, the most dominant being sample depth and concentration, i.e., the absolute precision improves with increasing sample depth and decreasing concentration. The strength of these relationships diminished with the length of the precipitation-weighting period being considered. Laboratory-related sources of imprecision were found to account for less than 4% of the overall daily measurement imprecision for most species, while field-related sources of imprecision accounted for the balance. Specialized plots are shown which allow data users to estimate the absolute and relative precision at any concentration and depth value.     

宜昌市酸雨的成因

根据近１０年１０７７个降水样品监测结果，进行统计分析，阐明了宜昌市存在酸雨污染，且日趋严重的趋势。从大气污染、气象、地形等因素方面初步探讨了该市酸雨的成因。     

中越边界—河口酸沉降的来源和发展趋势分析

河口当地无工业。燃料结构以柴禾为主，但８０年代降水酸度ＰＨ值为３．８０－５．１２平均为４．４，频率高达１００％。相距五年后，９０年代进行三年连续监测，酸 雨ＰＨ值为３．８２－６．９０，平均为４．９３，频率为９７．６％。     

"九五"期间昆明市盘龙区酸雨状况分析

本文通过对盘龙区‘‘九五"期间降水监测结果进行评价,得出昆明市中心区酸雨的变化趋势,并加以分析,提出对策建议.     

我国酸雨状况和对策

我国酸雨区面积占国土面积的30％，是世界第3大酸雨区，为控制酸雨发展，应将其防治工作纳入经济和社会发展计划，调整能源结构，治理工业排放，研发治理技术和设备，加强环境管理。     

二氧化硫浓度的垂直分布对云下雨水酸化的影响

用一物理化学模式讨论了云下雨水的酸化过程.参照重庆地区的实际情况,讨论了SO_2随高度指数分布和其它分布对酸化的影响及近地面层高浓度SO_2对酸化的影响.SO_2平均浓度与实际垂直分布相比较,地面雨水成份相差较小,用平均浓度代替实际垂直分布是可行的.     

贵阳市人工边坡稳定性模糊综合评判

在充分考虑了影响人工边坡稳定性的自然地质条件、诱发因素、人类工程活动等多项指标的基础上,用模糊综合评判方法对贵阳市近十年来发生的崩滑灾害和典型人工边坡的稳定性进行了综合分析和评价,评判结果与实际一致。     

2003年陕西持续性暴雨成因分析

对2003年发生在陕西的持续性暴雨分析认为: 乌山阻高与副热带高压的配置及稳定少动为这次持续性暴雨提供了有利的背景条件.贝湖低压底部分裂出小槽引导的冷空气与副高西北侧暖湿气流在高原东侧一带反复交绥是暴雨的主要成因.高低空急流耦合使高层辐散区迭加在低层辐合区的上方而产生强烈的上升运动,为深对流的发展提供了条件,促进了暴雨时中尺度系统的生成和维持.