沙尘暴对大气背景值的影响及遥感技术应用研究

对近十多年来发生在我国西北地区的较大沙尘暴，及其对甘肃大气背景值的影响、沙尘暴降尘的沉降量、区域分布、化学组份、粒度分布，应用则沙尘暴和沙尘暴的危害等内容，进行了为期二年的调查、取样和研究，回答了沙尘暴研究者所关心的一些问题。     

沙尘暴降尘的化学组份和粒径分布特征

对发生在我国西北地区沙尘暴降尘沉积物,采用中子活化法和Ｘ射线吸收－－沉降法对其中的３８种元素和粒径分布特征进行了分析和研究。并分别以地壳元素和本区域土壤背景值为参考,讨论了沙尘暴沉降物的富集因子等问题。     

甘肃河西走廊2001年沙尘暴及其沉降物质观测研究

2001年甘肃河西走廊共发生沙尘暴15次，其特点是时间早、频率快、间隔短，强度大。收集分析其沉降物质，沉降量较高、养分含量较高。     

用洁净水体监测大气沉降物污染的新方法研究

使用标本缸做为采样装置盛放去离子水露天连续放置1 a,观测水体受到大气干、湿沉降物和沙尘暴降尘的污染状况。期间每隔5~10 d从缸内抽取一定体积的水样,分析其中的水溶性离子和B、Ba、Be、Cd、Cu、Co、Fe、Mo、Mn、Ni、Pb、Sb、Ti、Tl、V、Zn等16种金属元素,除Be在部分样品中被检出外,其余15种元素的检出率均达到100%。在水体中的浓度总体呈明显富集和逐渐升高趋势。从直观和微观的角度阐述大气干、湿沉降物和沙尘暴降尘对洁净水体的污染过程。     

东北亚地区沙尘暴监测合作机制研究

近年来,东北亚各国重视沙尘暴问题,开展了沙尘暴监测及研究等合作,逐步建立起东北亚地区沙尘暴监测合作机制.合作机制对推动东北亚地区共同治理沙尘暴问题具有积极意义.文章通过分析东北亚主要国家中国、日本和韩国的沙尘暴监测机制,探讨沙尘暴监测的合作机制模式,进而分析合作机制对推动各国在监测方法、管理机制等方面的促进作用.     

碳酸盐碳测定在沙尘暴来源地识别中的应用

根据中国大气颗粒物特点 ,在国内沙尘暴研究中首次尝试利用碳酸盐碳进行沙尘暴来源地识别。测定了一系列黄沙、大气颗粒物和沙尘暴源区土壤样品。初步了解了上述样品中碳酸盐碳含量情况 ,结合国外研究结果对影响北京的沙尘暴源区进行推测并与其他方法作了比较     

沙尘暴路径分析

从气象状况、地理条件、沙尘暴路径实际分布等几个方面论述了我省沙尘暴移动的路径。从路径的形成机理谈起：强风、沙源、热不稳定性等因素是沙尘暴路径形成的充分条件，气象状况、地理环境是形成沙尘暴路径的必要条件，通过理论分析得出影响我省的主要沙尘暴路径，勾画出我省沙尘暴的路径并依据事实进一步验证沙尘暴路径。同时对相关的内容进行必要的讨论。     

甘肃省沙尘暴的成因分析与治理思路

沙尘暴是甘肃近年来的主要灾害天气之一．文章主要从空间分布、季节、年际变化上分析了甘肃沙尘暴的发生特征、沙尘暴产生的自然及人为原因，最后就甘肃主要生态系统的环境整治、沙尘暴治理提出了一些新的思路．     

春季区域性沙尘暴对南疆及东疆城市环境空气质量的影响及应对措施

近年来,新疆境内连续发生多次区域性春季沙尘暴,影响南疆和东疆地区十几个城市,其发生时间之早、频率之高、范围之广、强度之大为50年来所罕见。依据近3年南疆及东疆春季爆发的区域性沙尘暴天气的应急监测结果,分析了区域性沙尘暴对南疆及东疆城市环境空气质量的影响,并提出应对措施。     

沙尘暴的基本特征和成因初探

从时空分布、气象要素变化等方面介绍了沙尘暴的基本特征，简要叙述了沙尘暴的危害，并从大风、沙尘物质及不稳定空气条件等方面初步分析了沙尘暴的成因，进一步提出了一些治理措施。     

新疆沙尘暴环境影响监测网络体系建设探讨

探讨了新疆沙尘暴环境影响监测网络建设的目的、意义,并探索性地提出以新疆环境监测中心站为中心,博尔塔拉、哈密、吐鲁番、巴音郭楞、阿克苏、喀什、和田环境监测站为分支的“梅花型”新疆沙尘暴环境影响监测网络体系。     

新疆大气氮沉降监测研究进展浅析

通过对新疆12个监测点氮沉降研究结果发现,无机活性氮浓度(p NH 4+、p NO 3-、NH 3、NO 2)在不同生态系统存在较大的时空差异,氮沉降通量变化随人为干扰程度呈递增趋势。总结了当前新疆大气氮沉降监测研究进展,包括主要监测方法、不同生态系统大气氮素干沉降的时空差异性分析、大气氮素干湿沉降通量估算。对大气氮素干湿沉降通量的整体估算、不同生态系统的监测常态化等还存在不足,未来评估氮沉降的综合气候效应、定量临界负荷以及生态系统对氮沉降通量急剧增加的响应是今后研究的重点方向。     

Deposition Monitoring in Europe

A monitoring station for atmospheric deposition was designed and constructed. Three such stations were applied in a pilot project for a year on three sites (Speulder forest in The Netherlands, Auchencorth in Scotland and Melpitz in Germany) in different regions in Europe to estimate local inputs and to validate deposition models which are currently used or developed to estimate ecosystem specific deposition in Europe. Fluxes at Auchencorth Moss are lowest for all components, except for those much influenced by the sea as a source. As Melpitz is located far away from seas, these components are lowest at this site. Wet deposition is the dominant source of input at Auchencorth, whereas at Speulder forest, through its roughness and pollution climate, dry deposition is dominant. At this site dry deposition velocities are highest. Melpitz is a polluted site. Particularly sulphur deposition is high. It is recommended to equip several locations in Europe with intensive deposition monitoring methods. Such a network will be an extension of existing monitoring programmes on air pollution, such as that run by Eurepean Monitoring and Evaluation Programme for the long-range transmission of air pollutants in Europe (EMEP). The intensive monitoring locations should be selected based on pollution climates and type of vegetation, common in Europe.     

冶炼厂周边区域夏季大气Cu和Cd沉降特征

为了解贵溪冶炼厂周边农田区域夏季大气重金属沉降状况,于2012年6—8月及2013年6—8月(夏季),设置8个监测点,共收集大气干湿混合样品48个,采用原子吸收分光光度法分析了Cu、Cd。结果发现,冶炼厂周边区域2012年夏季Cu、Cd沉降通量分别为42.5~421、1.01~5.06 mg/m2,平均值149、2.02 mg/m2;2013年夏季Cu、Cd沉降通量分别为40.6~94.3、0.12~0.44 mg/m2,平均值59.4、0.26 mg/m2。同1月份不同监测点Cu、Cd沉降量存在一定差异性,风向为造成该差异性的主要气象因素;不同监测点Cu、Cd月沉降通量与风向频率均具有显著相关性(r均大于0.60)。降雨量影响Cu、Cd月沉降量,Cu、Cd平均月沉降量与降雨量均呈显著相关关系(r=0.91、r=0.87,P0.05)。     

A Global Overview of Atmospheric Acid Deposition Fluxes

This paper presents a summary of globalacid deposition flux data taken from a globalassessment report on acid deposition prepared forUNEP/WMO (Whelpdale and Kaiser, 1996). There is a largevariation in the spacial coverage and reliability ofmonitoring around the world. Many more stationsmeasure wet deposition than collect appropriate datafor estimating dry deposition. The widespread regionswith highest precipitation concentrations anddeposition fluxes of sulphate and nitrate coincideclosely with the regions of highest density ofSO₂ and NO_x precursor emissions occurringprimarily in the mid-latitude, northern hemispherebelt where a large fraction of the worlds fossilfuels is consumed. Organic acids in precipitation makea minor contribution to acidity (<20%) inindustrial regions, but in the rest of the world theyare of same order, or even exceed, inorganic acids.Less is known about dry deposition, but it appears topredominate near strong emission sources with wetdeposition predominating farther downwind. The molarratio of the N/S contribution to acidic deposition isclose to 1.0 over large areas of Europe and NorthAmerica, but is highly variable elsewhere, beinghighest in equatorial regions due to biomass burningand lowest near smelters and other large sources of SO₂.     

Interactions of Atmospheric Deposition with Coniferous Canopies in Estonia

Throughfall and open field bulk precipitation were measured at three coniferous sites during 1995–2002 in the framework of ICP Integrated Monitoring and at five coniferous sites during 1996–2002 in the framework of ICP Forests (Level II). The coniferous canopies acted as a sink for nitrate and ammonium and as a source for base cations: Ca²⁺, Mg²⁺ and K⁺. The estimated share of SO₄–S dry deposition from total deposition was 1.5–4 times higher for dormant period compared to growing period. During the study period average annual throughfall and bulk deposition of SO₄–S decreased significantly, 2.8 and 2.3 times, respectively. Throughfall enrichment with base cations increased in the order Mg < Na < Ca < K. Using Na as a tracer ion, average dry deposition and canopy leaching were calculated. Leaching was the dominant process for TF enrichment by potassium. Leaching of base cations occurred during growing as well as dormant period. The calculated internal flux of Ca²⁺ and Mg²⁺ varied in the range of 0.6–2.0 and 0.6–1.2 kg ha⁻¹ per year in spruce and pine stands, respectively. The internal circulation of K⁺ was significantly higher (8.9–10.9 kg ha⁻¹ per year) in spruce stands than in pine stands (2.7–4.4 kg ha⁻¹ per year).     

利用四段滤膜法进行干沉积监测

在酸雨研究领域,人们普遍是对降雨或降雪等湿沉积过程进行研究.近年来,干沉积也引起了大家的关注,但尚未建立成熟的方法.文章介绍了利用四段滤膜法进行干沉积监测的方法,作为日本全国公害研究协会的合作项目在日本神户和丰冈市进行了实际测量和评估.     

Inter- and Intra-Annual Chemical Variability During the ice-Free Season in Lakes with Different Flushing Rates and Acid Deposition Histories

Quantifying chemical variability in different lake types is important for the assessment of both chemical and biological responses to environmental change. For monitoring programs that emphasize a large number of lakes at the expense of frequent samples, high variability may influence how representative single samples are of the average conditions of individual lakes. Intensive temporal data from long-term research sites provide a unique opportunity to assess chemical variability in lakes with different characteristics. We compared the intra- and inter-annual variability of four acidification related variables (Gran alkalinity, pH, sulphate concentration, and total base cation concentration) in four lakes with different flushing rates and acid deposition histories. Variability was highest in lakes with high flushing rates and was not influenced by historic acid deposition in our study lakes. This has implications for the amount of effort required in monitoring programs. Lakes with high flushing rates will require more frequent sampling intervals than lakes with low flushing rates. Consideration of specific lake types should be included in the design of monitoring programs.     

Airbone particles dynamics: towards a theoretical approach

Wind-tunnel simulations and field experiments for dust transport by air show that deposition is predominant on the windward side of hills whereas sans deposition is mainly observed on the lee side. That and other aspects such as the existence of several deposition regimes depending on wind intensity call for theoretical explanations. We present some preliminary considerations leading to such a theoretical framework.     

Atmospheric deposition of major and trace elements in Amman, Jordan

Wet and dry deposition samples were collected in the capital of Jordan, Amman. Concentrations of Al, Ba, Bi, Cd, Co, Cr, Cu, Mn, Mo, Ni, Pb, Sb, V, Zn, Fe, Sr, Mg²⁺, Ca²⁺, Na⁺, K⁺, Cl⁻, NO₃ ⁻ and SO₄ ²⁻, along with pH were determined in collected samples. Mean trace metal concentrations were similar or less than those reported for other urban regions worldwide, while concentrations of Ca²⁺ and SO₄ ²⁻ were among the highest. High Ca²⁺ concentrations were attributed to the calcareous nature of the local soil and to the influence of the Saharan dust. However, high SO₄ ²⁻ concentrations were attributed to the influence of both anthropogenic and natural sources. Except for Cl⁻, NO₃ ⁻, SO₄ ²⁻ and Cu, monthly dry deposition fluxes of all measured species were higher than wet deposition fluxes. The annual wet deposition fluxes of trace metals were much lower than those reported for other urban areas worldwide.