峨眉山风景区酸性降水的研讨

本文对峨眉山——乐山大佛风景名胜区多年来降水酸度、酸雨频率与酸性降水的地域分布以及垂直变化特征进行了研讨,并对该区酸雨与四川省酸性降水特征进行了对比。     

四川省酸雨污染现状及趋势分析

本文从酸雨成因入手,根据全省降水监测数据等资料,对四川省酸雨污染现状及变化趋势进行分析,结果表明：我省酸雨法污染面积广、频率高;酸度强,近五年,酸雨频率有下降趋势,但降水酸度无明显减弱,酸雨污染形势依然严峻;降水组份中,硫酸根离子和硝酸根离子比值逐年下降,说明大气污染特征已由煤烟型转为煤烟型与机动车尾气混合型。     

成都市区酸雨变化及降雨化学组成分析

依据成都市1995～2003年城区酸雨监测统计资料,本文对成都市城区酸雨的变化特征、离子化学组成进行了分析。结果表明:城区降水酸度变化呈现出一定的波动性,酸雨频变化表现出较大的波动性;1999年和2000年酸雨年均酸度及频率情况都较好,之后出现反弹;降水中离子含量高,雨水污染严重;降水中CSO2-的比值正在逐步缩小,酸雨状况转变为硫/CNO-34酸型和硝酸型并重的局面,大气污染物中NOx的贡献率正在升高。灰色关联分析表明:降水pH值与雨水中碱性阳离子的关联序为NH+4>Ca2+>Mg2+>K+>Na+;降水pH′值与雨水中酸性阴离子的关联序为Cl->F->SO2-3。4>NO-     

广元市降水化学组成及酸雨污染趋势分析

本文以广元市2011年9月~2012年9月的降水监测数据为基础,对降水的化学组成进行统计分析,并依据2004~2012年的降水监测统计资料,对酸雨污染变化趋势进行探讨。结果表明:降水中主要阳离子为Ca2+和NH+4,主要阴离子SO2-4;酸雨类型主要为硫酸型;降水的酸度应该受多种离子综合影响;广元市酸雨污染总体趋势稍有减轻。     

长江口北岸南通地区酸雨污染及组分变化趋势分析

分析2007～2019年南通市各子站降水监测点位数据得出,近10年来,全市酸雨污染大幅减轻,酸雨发生率渐趋下降,强中度酸雨逐渐消除,降水酸度和酸雨酸度均有减弱,现阶段酸雨污染以弱酸性酸雨污染为主。近年来全市硫酸根离子当量浓度呈现逐年明显降低的趋势,机动车尾气排放的大量致酸物质使降雨中NO_3~-占比明显上升,SO_4~(2-)与NO_3~-浓度的比值已降至1.25∶1,南通市酸雨已由硫酸型向硫酸与硝酸并重混合型过渡。全市酸雨区域分布格局总体变化不大,主要呈现东南沿江沿海略高于西北部区域。     

怀化市酸雨污染分析

本文通过对怀化市鹤城区常规酸雨监测数据分析，针对怀化市区特有的山区地形特征，初步得出怀化市区酸雨时空分布特征，酸雨形成原因是降水酸度，酸雨率季节性变化规律，并对此提出一些减少山区环境酸雨污染的合理化建议。     

浅析四川省酸性降水特征及防治对策

本文根据1983～1988年四川省27个市(县)环境监测站97个监测点进行降水监测,共采集雨样15815个:其中酸雨样品7798个,初步分析了全省降水酸度及化学组份的分布状况,以及出现酸雨的原因、规律、危害情况,并提出防治的措施意见。     

南充市近十年酸雨变化特征及降水化学组成研究

依据南充市2003~2012年城区降水环境监测统计资料,分析了酸雨变化特征及降水离子化学组成。研究表明:这十年,酸雨频率平均为50.4%,2007年降雨量为最高,呈波动递减趋势变化,降水年平均pH值为4.88,呈现"低—高—低"的变化特征,城区酸雨频率和降水pH值月均值变化呈现高低交替的波动趋势。城区降水中主要阳离子成分是Ca2+,主要阴离子成分是SO2-4和NO-3。(SO2-4/NO-3)比值逐年下降,平均比值为7.82,酸雨污染类型仍以硫酸型为主;降水(NH+4+Ca2+)/(SO2-4+NO-3)和Ca2+/NH+4比值呈波动性变化,2007年分别达到最高值为6.71和50.27,除2010年比值均较低小于1外,近年来均有增加趋势,表明碱性离子缓冲能力增强了,降水酸度降低,pH值增加,但2007年pH值较低,主要与降雨量有关。综合分析,降水酸度不仅是酸性离子和碱性离子中和作用,也受其他离子浓度和降雨量、风向等气候条件、距离传输以及地形等影响。     

峨眉山降水电导率变化规律初探

本文通过对峨眉山山顶和山下１９８６年～１９９５年降水电导率变化规律的分析发现,其两地电导率与降雨量及降水酸度存在一定的关系,也存在一定的差异。这差异表明山顶降水酸度来源于中长距离的传输     

酸性降水研究

本文对降水酸度的变化规律，降水ｐＨ值与电导率的关系，以及ｐＨ值与降水量，降水时间的关系等方面进行了研究，建立了ｐＨ值与ＳＯ＾２－４，Ｃａ＾２＋，ＮＨ＾＋４的三元线性回归模式。     

都匀市降水pH值的变化趋势及特征分析

ｐＨ值是衡量降水酸性的重要指标。本文研究了都匀市降水ｐＨ值的变化趋势，并对其酸性降水的特征进行分析，提出了保护大气质量，降低酸雨频率的对策建议。     

Leaching from organic matter-rich soils by rain of different qualities: I. Concentrations

Soil monoliths from an area exposed to acid precipitation and from an unpolluted area were used in a lysimeter experiment to study effects of different rain qualities on the chemical composition of the leachate from shallow soils rich in organic matter. The vegetation was either dominated by moorgrass [Molinia caerulea (L.) Moench] or heather [Calluna vulgaris (L.) Hull]. The lysimeters received either "acid rain" (pH 4.3) or "normal rain" (pH 5.3). High concentrations of dissolved organic carbon (DOC) were characteristic of the leachate. The different "rain" qualities had no significant influence on the DOC concentration. More DOC was, however, leached from lysimeters with heather vegetation. Roughly 50% of the aluminum (Al) was in complex with organic material and the Al charge was calculated to be between +1.4 and +2.0. Sulfate (SO4(2-)) was the only component that was significantly influenced by the treatment, as more was leached from lysimeters receiving "acid rain." Sulfate was poorly correlated with pH, suggesting that reduced SO4(2-) input would not necessarily lead to reduced acidity. Differences in the pH of the leachate due to the treatments were less than 0.15 pH units. Nitrate (NO3-) was only leached in very low concentrations and of little consequence for the leachate acidity. Some observations do, however, suggest that NO3- may contribute to acidification in episodes with high precipitation. High concentrations of Cl- in the leachate and a significant positive correlation between Cl-, H+, and base cations indicate that sea salt episodes may be important for soil acidification and acidity of the leachate.     

成都市区降雨中主要低分子有机酸及来源分析

为了解成都市区降水中有机酸的化学组成特征及来源,2011年3月至9月共采降水36次,用液相色谱法检测了降水中的无机阴离子及低分子有机酸,同时测定样品的pH、电导率。用SPSS软件统计得到：有机酸的含量占总阴离子量的20．19％,对自由酸度的平均贡献值分别为31．55％。相比安顺、贵阳等地,成都市区降水中单位有机酸的酸度贡献值较小,可能是降水中的大量碱性杂质削弱了有机酸对酸度的影响。甲、乙酸占有机酸含量的93．6％,表明最主要的低分子有机酸是乙酸、甲酸。相关分析显示有机酸与所有阴离子显著相关,表明有机酸来源较复杂,多样化。进一步分析得到：甲酸与乙酸的相关系数（0．900）和偏相关系数（0．822）都很高,表明甲酸与乙酸有相似的来源或者不同来源的相似源强;甲酸与NO^3-始终显著相关表明主要来自人为活动;乙酸与nss-SO4^2-。始终显著相关表明主要来自间接源;草酸与甲酸、乙酸的偏相关系数很大程度上小于相关系数表明主要来自与甲、乙酸来源相似的前体物的光化学反应。     

四川酸性物湿沉降模式及预测

酸沉降是一复杂的大气物理和化学过程，涉及诸多复杂影响因素。目前，我国酸雨湿沉降模式还仅限于模拟云下洗脱成酸过程，而对云中的成酸过程还未进行深入研究，这不仅在理论上不完善，而且更重要是在许多情况下与我省实际情况不符。本课题针对四川省特定的地理，气象特点和严重的大气污染情况，并借鉴国外研究成果，提出了考虑酸性沉降的云中和云下成酸过程和各种影响因素的综合酸雨湿沉降模式，并根据此模式来估算和预测四川省酸雨     

Partial neutralization of rain by seaspray: the case of Recôncavo, Bahia-Brazil

In the Recôncavo of Bahia (located between 12°33′ and 13°10′S and 38°00′and 39°00′W), there are significant discharges of SO₂ and NO_x due to local, industrial and urban activities. The incoming air masses from the Atlantic Ocean are enriched with seaspray, which neutralizes part of the rain acidity. The extent of seaspray neutralization of rain acidity was quantified in four sites of the region, each with different loads of seaspray. Rain samples were obtained daily at the same time, integrating the precipitation of the previous 24 h, using wet-only collectors and analyzed for pH by potentiometry and for sodium by flame photometry. The amount of rain acidity in Recôncavo neutralized by seaspray ranged from <1% up to 88% and depended on the site. On average, neutralization ranged from 5% to 18%.     

用灰色系统理论GM(1,1)建立大气降水中酸雨pH值的预测模型

本文用灰色系统理论GM(1,1)建立了大气降水中pH值的预测模型。经三种不同方法检验。对我市1990—1993年大气降水中酸雨pH值进行了预测,结果令人满意。     

NITROGEN CONTENT AND ACIDITY OF RAIN ON THE GEORGIA COAST1

ABSTRACT: Since nitrogen is a nutrient frequently in short supply in coastal ecosystems, an estimate of the nitrogen input via rain was made for the Georgia coast. Water samples collected in 34 separate storms during a 12 month period were analysed for concentrations of ammonia, nitrate plus nitrite, and dissolved organic nitrogen (DON). The range and average concentration in micromoles of nitrogen per liter was 0.0 to 137 (6.3) for ammonia, 1.0 to 21 (7.9) for nitrate plus nitrite, and 0.0 to 13.6 (4.0) for DON. DON, not usually measured in rain, comprised up to 62% of the total nitrogen content. The annual amount of nitrogen contributed by rain to the coast was about 0.3 g N/m². This value is a small fraction of the calculated nitrogen requirements of coastal plants. More than half the rain samples had pH values less than the CO₂ equilibrium pH of 5.6. Values as low as 4.2 were in the range of pH values reported for acid rain in Europe and the northeastern U.S. Total titratable acidity was measured for 12 summer rainwater samples. The results fox 7 individual storms showed a highly linear relation between hydrogen ion concentration and total acidity. However, the elope of the regression line indicated that increases in acidity were not a result of addition of strong acid alone.     

中国南方酸雨的分布特征及其成因分析

本文阐述了酸雨的危害、近几年中国南方地区酸雨的污染的时空分布状况、酸雨的成因等3方面的内容。研究表明：我国南方酸雨区的酸雨污染状况基本上处在一个稳定的时期。降水pH〈5的区域有从长江中上游向长江中下游发展的趋势;在时间分布上,秋季冬季降水pH低,酸雨发生的频率高;春季夏季降水pH高,酸雨发生的频率低。在酸雨的成因上,着重讨论了大气性质、污染物的迁移和扩散、气候条件、大气中颗粒物浓度以及土壤性质对酸雨形成的影响。