淠河流域不同强度等级降水变化研究

淠河流域降水时空变率大,深入分析不同强度等级降水的特征和变化,对于全面揭示研究区气候变化、合理有效利用水资源、防治洪旱灾害具有十分重要的意义。基于淠河流域12个气象站1958~2012年逐日降水资料,分析年、季不同级别降水量(频次)的变化特点,以及主汛期(5~9月)连续3d最大降水量的概率分布。结果表明,淠河流域小雨量(频次)四季分布比较均匀,级别越高,降水频次越少,分布越集中,夏季暴雨多发。淠河流域年总降水量增加趋势不显著,总降水频次则显著减少。夏季各级别降水量(频次)均呈增加趋势,其中暴雨增加最显著,冬季总降水频次无明显趋势变化,小雨、中雨量增加显著,春、秋季总降水频次和小雨频次的减少趋势极其显著。淠河流域暴雨量、暴雨频次均在1968年发生增多突变,小雨频次在1975年有极显著减少突变,年总降水量有增多突变,总降水频次则有减少突变。自20世纪70年代后期以来,研究区主汛期连续3d极端强降水出现概率加大,不同重现期极值增大,洪涝灾害风险加剧。     

Effect of acid solutions on plants studied by the optical beam deflection method

The optical beam deflection method was applied to study the effects of acid solution on both a terrestial and aquatic plants Egeria and Cerastium, which are common aquatic plant and terrestial weed respectively. A probe beam from a He-Ne laser was passed through a vicinity of a leaf of the plants, which were put in culture dishes filled with acid solutions. Deflection signals of the probe beam were monitored and compared for acid solutions with different pH values. The results of Egria showed that the deflection signals changed dramatically when pH values of acid solutions were 2.0 and 3.0, while little at pH of 4.0 and 5.0. For Cerastium when pH were below 3.0, deflection signals changed greatly with time at the begining. After a certain period of time, deflection signals changed little with time. When pH value was above 4.0, deflection signals of Cerastium were still changing with time even after 20 hours. The results suggested that the damage threshold of pH was between 3.0 and 4.0 for both the land and aquatic plants.     

模拟酸雨下铅锌冶炼废渣重金属的静态释放特征

以株洲某铅锌冶炼废水中和渣为研究对象,开展不同初始pH值（3.0,4.5,5.6和7.0）模拟酸雨静态浸出实验,研究22d浸泡过程中废渣Cd、Cu、Pb和Zn等重金属的动态释放规律及其化学形态变化和矿物相变特征.结果表明,废渣具有较强的酸缓冲潜力,浸出液pH值稳定在6.20~6.66.Cu和Pb在浸泡初期释放较快,Cd和Zn释放相对较慢.浸出液Cd浓度随浸出时间增加而上升,Zn浓度呈波动变化,Cu和Pb浓度变幅较小.提高雨水酸度促进废渣中重金属的释放,浸出液Cd、Cu、Pb和Zn浓度范围分别为1.38~8.70,0~0.02,1.21~2.26和27.2~135mg/L,其中Cd、Pb和Zn浓度分别超过我国《铅、锌工业污染物排放标准》（GB 25466-2010）限值的26.6~173倍、1.42~3.52倍和17.1~89.0倍..重金属BCR顺序提取表明,浸出液中较高Cd和Zn浓度与其赋存高活性态比例一致,且酸雨促使残渣态Cd和Pb向活性态转化.XRD分析显示,pH=3.0酸雨处理22d后原废渣中Cd和Zn的赋存矿物相消失,PbSO₄谱峰增强,表明废渣重金属的释放受其赋存矿物相及次生矿物形成的影响.重金属释放率呈现出Cd （2.50%~15.8%）> Zn （0.41%~2.13%）> Pb （0.06%~0.10%）> Cu （0.0003%~0.11%）的趋势.自然堆存酸雨作用下废渣中Cd、Pb和Zn具有较大环境风险,需加强降雨淋滤污染防治管控.     

江油市降水pH值的时间分布特征及控制对策

根据江油市2001～2009年的监测资料,首次分析江油市降水PH值的状况和变化.在降水酸碱类型的频率分布统计特征的基础上,探讨江油市降水pH值的季节分布特征及夏季酸雨的成因,并提出控制措施.     

模拟酸雨淋溶条件下紫壤淋出液中溶解性有机质的三维荧光特性

运用三维荧光技术分析了模拟酸雨淋溶紫壤淋出液中溶解性有机质（dissolved organic matter,DOM）的组分与酸度及淋溶量的关系.研究结果表明,模拟酸雨淋溶紫壤淋出液中DOM荧光峰主要为类胡敏酸和类富里酸,荧光峰的中心位于Ex/Em=305—370 nm/420—450 nm和Ex/Em=260—270...     

鹰潭市酸雨污染现状、趋势与成因分析

采用2001-2010年降水监测数据,全面系统地研究分析鹰潭市酸雨污染现状、变化规律,并从环境空气质量、区域污染物输送、气象因素和土壤性质等方面探讨酸雨形成的主要原因,得出区域输送是鹰潭市酸雨污染的主要因素。     

模拟酸雨与重金属复合胁迫对绞股蓝生长及根际微生物的影响

通过盆栽试验研究了不同pH值的模拟酸雨与Zn(30和400 mg.kg-1)、Cd(1和15 mg.kg-1)单独或复合胁迫对绞股蓝(Gynostemma pentaphyllum)药用成分——总皂甙含量以及根际土壤微生物数量和组成的影响。结果表明:不同pH值的模拟酸雨均能抑制细菌、放线菌、氮素生理类群的生长,其数量随酸雨pH值的降低而不断减少;真菌、纤维素分解菌数量随酸雨pH值的降低呈先升高后降低的变化趋势;绞股蓝茎叶总皂甙含量随酸雨pH值的降低而降低。酸雨影响下,单施低浓度的Zn(30 mg.kg-1)或Cd(1 mg.kg-1)时,根际3大类群微生物、氮素生理类群、纤维素分解菌、绞股蓝总皂甙含量均高于无重金属处理;但当Zn(400 mg.kg-1)或Cd(15 mg.kg-1)处于高浓度时,它们又明显低于无重金属处理。酸雨影响下,Zn(30 mg.kg-1)或Cd(1 mg.kg-1)为低浓度水平时,Zn-Cd复合污染对根际3大类群微生物、氮素生理类群、纤维素分解菌、绞股蓝茎叶总皂甙含量影响表现为拮抗效应;Zn(400 mg.kg-1)或Cd(15 mg.kg-1)为高浓度水平时,Zn-Cd复合污染对根...     

Assessment of Residential Rain Barrel Water Quality and Use in Cincinnati,Ohio1

The collection, storage, and reuse of rainwater collected in rain barrels from urban rooftop areas assists municipalities in achieving stormwater management objectives and in some areas also serves as an adjunct resource for domestic water supplies. In this study, rainwater reuse and levels of select microbial indicators were monitored for six residential rain barrels located in the Shepherd Creek watershed of Cincinnati, Ohio. Water from rain barrels typically had poor microbial quality and was used for watering indoor and outdoor plants. Rain barrel water chemistry was slightly acidic, exhibited wide ranges in conductivity, turbidity, and total organic carbon (TOC) concentrations and gave no evidence of the presence of cyanobacterial microcystin toxins. Selected microbial water‐quality indicators indicated that counts of total coliform and enterococci were consistently above U.S. Environmental Protection Agency standards for secondary recreational contact water‐quality standards. Residential rain barrels can provide water appropriate for low‐contact reuses (such as plant watering), although there may be transient periods of high levels of indicator bacteria in the collected water.     

VARIATION IN ADIRONDACK,NEW YORK,LAKEWATER CHEMISTRY AS FUNCTION OF SURFACE AREA1

ABSTRACT: Data from a recent survey conducted by the Adirondack Lake Survey Corporation were used to evaluate the influence of lake surface area on the acid-base status of lakes in Adirondack State Park, New York. Acid neutralizing capacity (ANC) in the small lakes (< 4 ha) occurred more frequently at extreme values (> 200, < 0 μeq L^?1), whereas larger lakes tended to be intermediate in ANC. Consequently, acidic (ANC ≤ 0) and low-pH lakes were typically small. The small lakes also exhibited lower Ca²⁺ concentration and higher dissolved organic carbon than did larger lakes. Lakes ≥ 4 ha were only half as likely to be acidic as were lakes ≥ 1 ha in area. These data illustrate the dependence of lake chemistry on lake surface area and the importance of the lower lake area limit for a statistical survey of lake water chemistry.     

Fluxes of CH4 and N2O from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China

CH4 and N2O fluxes from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China were measured for one year using closed static chamber technique and gas chromatography method. Three treatments were set in the studied field: (A) litter-free,(B) with litter, and (C) with litter and seedling. The results showed that the soil in our study was a sink of atmospheric CH4 and source of atmospheric N2O. The observed mean CH4 fluxes from treatments A, B, and C were -50.0±4.0, -35.9±2.8,-31.6±2.8 μgC/(m2·h),respectively,and calculated annual fluxes in2003 were -4.1,-3.1,and -2.9kgC/hm2,respectively.The observed mean N2O fluxes from treatments A,B,and C were 30.9±3.1,28.2±3.5,50.2±3.7μgN/(m2·h),respectively,and calculated annual fluxes in 2003 were 2.8, 2.6, and 3.7 kgN/hm2, respectively. Seasonal variations in CH4 and N2O fluxes were significant among all the three treatments. The presence of litter decreased CH4 uptake during wet season (P ＜ 0.05), but not during dry season. There was a similar increase in seedlings-mediated N2O emissions during wet and dry seasons, indicating that seedlings increased N2O emission in both seasons. A strong positive relationship existed between CH4 fluxes and soil moisture for all the three treatments, and weak relationship between CH4 fluxes and soil temperature for treatment B and treatment C. The N2O fluxes correlated with soil temperature for all the three treatments.