电导率加和性质及其在降水监测数据处理中的应用

采用相对电导率差（CPD）法、电导率-pH不等式法对某监测站大气降水的实测电导率和pH值等数据进行质量分析。根据分析结果认为可用CPD法来检验、评估降水中各种离子成分的分析是否完整、准确，用电导率-pH不等式法来检验电导率和pH值的测定值是否存在明显的误差。     

荆门市近十年大气降雨的变化特征分析

利用荆门市2001—2010年对城区和石化区的降水监测资料,研究分析了荆门市近十年来的大气降水量、pH及电导率的变化情况。结果表明:荆门市近十年来的年均降水量为793.27 mm,降水主要集中在5—8月,年降水量变化较大,基本呈周期性的波动趋势。荆门市城区降水的pH和电导率比较稳定,没有出现酸雨。石化区的降水年平均pH比城区低,年平均电导率比城区高,有酸雨发生,但污染并不严重。     

基于标准雨量计的降水采样方法比较

对太原市2013年7—11月的大气降水使用标准雨量计、国产A型和进口B型自动降水采样设备进行同步记录,分析国产A型和进口B型设备采集降水样品的p H、电导率和无机阴阳离子。结果表明,进口B型设备采集降水样品的降雨量(155.35 mm)比标准雨量计记录值(117.50 mm)高32.21%,而国产A型设备采集降水样品的降雨量(107.12mm)比标准雨量计记录值低8.83%。7—9月的15场降水,国产A型设备采集大多数降水样品的电导率和离子加权浓度均值基本上低于进口B型设备,差异程度分别达65.51%和62.52%;而p H则基本上高于进口B型,酸雨比例差异程度为61.53%。     

上海市某城区降水监测点位优化

通过对2009—2011年间上海市某城区降水监测数据的数理统计分析,对降水中的阴阳离子、p H值和电导率数据进行比对,在确保监测数据的代表性、合理性和连续性前提下,对于降水监测点位优化的必要性、可行性与后续影响进行评估。     

关于《酸沉降监测技术规范》(HJ/T165-2004)中的几处修正意见

介绍了降水监测数据的阴、阳离子平衡和电导率平衡检验的计算方法,对国家环保总局发布的<酸沉降监测技术规范>(HJ/T165-2004)中公式存在的几个不妥之处提出修正意见.     

南昌市降水自动监测与手工采样监测对比分析

南昌市环境监测站引进了一套降水自动监测系统,该系统由一个中心站及五台AR-107型自动监测仪(子站)组成。通过对AR-107型降水自动监测仪及手工样监测结果间的对比实验发现,自动监测与手工采样监测所获得的pH值和电导率值差异明显,并对这种差异进行了分析探讨,认为干沉降是这种差异存在的主要原因。     

山西省大气降水水质评价

为了解山西省大气降水水质状况、主要污染物及区域分布规律，山西省水文部门于1984年开始对大气降水进行监测。在全省9个地市布设测点，分别为：太原市、大同市、长治市、榆次市、临汾市以及吕梁、忻州、阳泉、运城地区。监测项目为H^2 、电导率、Ca^2 、Mg^2 、K^2 、Na^2 、NH4^2 、SO4^2-、NO3^-、Cl^-、CO3^-、HCO3^-、F^-。结果表明，除吕梁、忻州地区外。山西省各地市均有酸雨发生，但酸雨发生的频率不高，全省年平均为3．3％；酸雨的酸性程度也不高，对生态可造成明显影响的降水次数不多；山西省酸雨为典型的硫酸型，酸雨中硫酸与硝酸的质量浓度比值远高于全国平均值。     

克拉玛依市大气降水化学的统计学分析

运用相关分析、因子分析和聚类分析等统计学分析方法,对2009—2010年新疆克拉玛依市的大气降水化学组成和分布特征进行分析。结果表明,SO4^2-、Cl^-、Ca^2＋和Na^＋是降水中主要离子。降水的pH值、电导率、降水量和各离子组份均呈现明显的正偏态分布,降水样品以低离子含量的样本为主,因子分析和聚类分析2种分类方法分析降水中水溶性离子主要分为3类。SO4^2-、Cl^-、Mg^2＋、F^-主要来自人为活动的贡献,K^＋、Ca^2＋主要来源于土壤和沙尘等地壳,H^＋与其他阴、阳离子间并未表现出明显的相关关系,表明研究区域的降水酸度是所有致酸离子和各种离子综合作用的结果,而不是降水中某个单一的离子组份确定的。     

上海青浦地区大气降水的化学特征

利用上海青浦地区2003—2014年观测的大气降水监测资料,分析该区域12 a以来大气降水的酸化程度、化学组成特征,探讨降水中化学成分的不同来源及相对贡献。结果表明:降水pH年均值为4.43~6.33,酸雨频率为2.6%~86.8%,降水酸化程度大致经历了明显恶化和波动变化2个阶段。降水电导率年均值为1.77~4.01 m S/m,呈下降趋势。降水中各离子雨量加权平均当量浓度顺序为SO_4~(2-)NH_4~+Ca~(2+)NO_3~-Cl~-Na~+Mg~(2+)F-K~+,SO_4~(2-)、NH+4、Ca~(2+)和NO_3~-是降水中的主要离子,占离子总量的83.0%;降水类型由硫酸型向硫酸和硝酸混合型转变。降水离子中的二次组分SO_4~(2-)、NO_3~-和NH_4~+绝大部分来源于人为源,Ca~(2+)、Mg~(2+)和K+主要来自于土壤源和人为源的贡献,Cl~-主要来自海洋源,同时人为源的影响也不可忽视。     

2010—2019年台州市市区降水化学组成特征及变化趋势

为了解台州市市区大气降水化学成分组成特征及变化规律,对2010—2019年台州市市区降水监测数据进行了统计分析。结果表明:2010—2019年降水样品pH为4.20～4.84夏高冬低,强酸性降水频率下降显著,电导率平均值为3.16 mS/cm。SO_4~(2-)和NO_3~-是降水中最主要的阴离子,NH_4~+和Ca~(2+)是降水中最主要的阳离子。Ca~(2+)浓度在2018年开始有所抬升,SO_4~(2-)和NO_3~-浓度整体呈波动下降趋势。SO_4~(2-)与NO_3~-浓度比均值为1.50,呈下降趋势,同大气中SO_2与NO_2的质量浓度比变化趋势基本一致。SO_4~(2-)和NO_3~-相关性显著,Cl~-、Na~+及Mg~(2+)三者之间具有较好相关性。降水与气态污染物相关性不大,对颗粒物有明显冲刷去除作用。SO_2和NO_x的排放量显著下降,酸雨污染呈现改善过程。     

北京城区降水对PM2.5和PM10清除作用分析

基于北京市PM_2.5和PM₁₀质量浓度、组分浓度以及降水数据，利用数理统计、相关性分析等方法分别从降水总量、降水时长和降水前颗粒物浓度3个角度研究降水对PM_2.5、PM₁₀的清除作用，同时以一次典型降水过程为例，具体分析降水对颗粒物的影响。结果表明：降水总量的增加有助于促进PM_2.5、PM₁₀的清除，随着降水总量增加，PM_2.5、PM₁₀的平均清除率提高，有效清除的比例增加；连续降水可增强对大气颗粒物的湿清除作用，连续降水达3d可有效降低PM_2.5、PM₁₀浓度；降水对PM_2.5、PM₁₀浓度的清除率和大气颗粒物前一日的平均浓度有较好的正相关性。降水对大气颗粒物的清除可分为清除、回升和平稳3个阶段，各个阶段大气颗粒物的变化趋势不同。降水对于大气气溶胶化学组分和酸碱性的改变具有明显作用，对于大气颗粒物各种组分的清除效果不完全相同。对于大气中OC、NO₃^-、SO₄^2-和NH₄⁺去除率较高，且这4种组分主要以颗粒态形式被冲刷进入降水中，加剧了北京市降水酸化程度。     

Improved mapping of National Atmospheric Deposition Program wet-deposition in complex terrain using PRISM-gridded data sets

High-elevation regions in the United States lack detailed atmospheric wet-deposition data. The National Atmospheric Deposition Program/National Trends Network (NADP/NTN) measures and reports precipitation amounts and chemical constituent concentration and deposition data for the United States on annual isopleth maps using inverse distance weighted (IDW) interpolation methods. This interpolation for unsampled areas does not account for topographic influences. Therefore, NADP/NTN isopleth maps lack detail and potentially underestimate wet deposition in high-elevation regions. The NADP/NTN wet-deposition maps may be improved using precipitation grids generated by other networks. The Parameter-elevation Regressions on Independent Slopes Model (PRISM) produces digital grids of precipitation estimates from many precipitation-monitoring networks and incorporates influences of topographical and geographical features. Because NADP/NTN ion concentrations do not vary with elevation as much as precipitation depths, PRISM is used with unadjusted NADP/NTN data in this paper to calculate ion wet deposition in complex terrain to yield more accurate and detailed isopleth deposition maps in complex terrain. PRISM precipitation estimates generally exceed NADP/NTN precipitation estimates for coastal and mountainous regions in the western United States. NADP/NTN precipitation estimates generally exceed PRISM precipitation estimates for leeward mountainous regions in Washington, Oregon, and Nevada, where abrupt changes in precipitation depths induced by topography are not depicted by IDW interpolation. PRISM-based deposition estimates for nitrate can exceed NADP/NTN estimates by more than 100% for mountainous regions in the western United States.     

Investigation of impact of environmental changes on precipitation pattern of Pakistan

In this paper, variability in precipitation pattern of Pakistan due to environmental and climatic changes has been studied. Maps have been generated to depict global precipitation variation. Precipitation data of 25 stations of Pakistan have been used. These data were taken from Meteorological Department, Islamabad, Pakistan. The results of two global climate models, namely Australia’s Commonwealth Scientific and Industrial Research’s third generation general circulation model and National Center for Atmospheric Research’s first generation precipitation circulation model for A2 scenario have been applied to investigate the changes. It is observed that precipitation pattern will change significantly in the future. The occurrence of precipitation in all seasons for Pakistan is expected to increase with almost uniform distribution across a season. Average annual precipitation of the country will undergo an increase in the range of +57 to +71 % as compared to average of the base period.     

降雨对长三角区域PM2.5浓度的影响

利用WRF-CAMx模式分析首届中国国际进口博览会(简称进博会)期间一次降雨过程对长三角地区PM2.5浓度影响,结果表明,降雨量分布区域与因降雨造成的PM2.5浓度减少量分布区域并不完全一致,湿沉降量受降雨量、PM2.5浓度和风速等多个因素共同影响。数值模拟结果表明,降雨导致浓度下降幅度排前5位的组分分别是有机气溶胶、硫酸盐、硝酸盐、铵盐和细颗粒原生气溶胶,下降幅度分别为44. 28%、16. 55%、11. 55%、9. 53%和5. 23%。结合观测资料和数值模式模拟结果可知,首届进博会期间上海本地减排和周边区域协同控制作用使PM2.5日均质量浓度降低33. 23μg/m3,因降雨引起的湿沉降作用使上海市PM2.5质量浓度降低15. 88μg/m^3。     

乌鲁木齐市降水酸度及化学特征的初步研究

降水酸度和离子平衡研究结果表明,乌鲁木齐市降水为非酸性雨,但其PH值有较明显的季节变化,降水中的SO_4~(2-)、Ca~(2+)、和NH_4~+是影响酸度的关键离子,与其他地区相比,乌鲁木齐市降水中的Ca~(2+)浓度是酸雨区(贵阳、重庆)平均值的3.50倍,是非酸雨区(北京、天津)平均值的1.86倍。可见,乌鲁木齐市降水酸度的高低,不仅取决于酸性离子浓度,而且更重要的是取决于碱性离子浓度。     

乌鲁木齐市大气降水的化学特征分析

讨论了乌鲁木齐市2004年1～12月年度降水的酸碱性、离子组分变化规律与特征，阐述了乌鲁木齐市城市降水的基本现状，分析了降水的变化规律，对主要成因进行了初步探讨，指出乌鲁木齐市的硫酸型降水污染应该从总量上控制SO2。并从源头上削减SO2的排放量。     

Throughfall,stemflow, and interception characteristics of coniferous forest ecosystems in the western black sea region of Turkey (Daday example)

This study aims to identify precipitation, throughfall, stemflow, precipitation, and interception processes in pure black pine, pure Scots pine, and mixed black pine–Scots pine forest ecosystems and present the precipitation partitioning according to different stand types. Throughfall and stemflow measurements were performed using five standard precipitation gauges in a pilot area established to represent pure black pine, pure Scots pine, and mixed black pine–Scots pine stands in the Bezirgan Basin. The total precipitation was measured in an open field close to the study area. Throughfall values were calculated as the percentage of precipitation measured in an open field. According to the results of the study, the throughfall values were 69.8% in black pine, 73.9% in Scots pine, and 77.7% in the mixed black pine–Scots pine stands; the stemflow values were 2.6% in black pine, 5.9% in Scots pine, and 3.1% in the mixed black pine–Scots pine stands; the amounts of precipitation reaching the forest floor were 72.3% in black pine, 79.8% in Scots pine, and 80.7% in the mixed black pine–Scots pine stands; and the interception values were found to be 27.7% in black pine, 20.2% in Scots pine, and 19.2% in the mixed black pine–Scots pine stands.     

The role of atmospheric circulation system playing in coupling relationship between spring NPP and precipitation in East Asia area

In many East Asia regions, spring (from March to May) precipitation is an important restricting factor to vegetation growth, and atmospheric circulation system may influence spring precipitation patter. It is helpful to under the response of ecosystem to climate change by studying the influence of atmospheric circulation system on the coupling relationship between spring net primary productivity and precipitation. Driving CASA (Carnegie-Ames-Stanford Approach) NPP (Net Primary Productivity) model, we estimated spring NPP for East Asia area (70 degrees E-1 70 degrees E, 10 degrees N-70 degrees N) from 1982 to 1999, and by the method of singular value decomposition we further analyzed the coupling features of spring NPP with precipitation. The result showed that the response features of NPP to precipitation were mainly embodied within the leading six NPP-precipitation paired-modes. The interpretation rates of the leading six paired-modes to the covariance of NPP-precipitation were 42.91, 23.29, 9.96, 5.60, 5.04 and 3.95%, respectively, and total to 90.75%. The temporal correlation coefficients of the leading six paired-modes were 0.830, 0.889, 0.841, 0.747, 0.912 and 0.923, respectively, and all the correlations were significant at significant level of 0.001. In some high latitude regions, there was no obviously corresponding relationship between NPP and precipitation in the leading two paired-modes, and the reason of it may be that spring temperature was the main restricting factor to NPP. In middle and low latitude regions, the effect of precipitation on NPP was relatively more notable. Nine atmospheric circulation factors in spring affected the patterns of NPP and precipitation greatly, and the regions with interpretation rate over 50% shared 60.41 and 65.58% of the whole study area, respectively.     

厦门市气候特征变化与酸雨形成研究

对地面风场的研究表明，厦门存在局地和海陆风环流，自1955年以来年平均风速、混合层厚度均呈现下降趋势，大气污染物的水平和垂直扩散能力也呈下降趋势。降水酸度随海拔高度的变化情况表明，海陆风环流有利于酸性污染物的积累，且锋面降水过程中的光化学污染加重了降水的酸化程度。