珠三角地区利用PM2.5反演气溶胶数浓度谱方法

大气气溶胶数浓度谱分布(PNSD)对于大气辐射和光学计算至关重要,利用目前普遍观测的气溶胶质量浓度(PM_(2.5))来反演计算PNSD,能有效补充PNSD观测的不足,对于需要PNSD信息的研究工作如大气能见度计算等有重要的实用价值.本文利用2014年11月～2015年1月在广州城市站进行同期连续观测的干气溶胶粒子的PM_(2.5)、PNSD数据进行客观分析,建立了一种使用PM_(2.5)反演PNSD的方法,并评估了该方法的适用性.结果表明该反演算法具有较好地适用性和稳定性,对于积聚模态的PNSD反演效果较好,但对于PM_(2.5)高浓度的反演结果差异较大.该反演方法将为珠三角地区的大气能见度计算和应用提供有利的依据和支撑.     

1990～2017年中国地区气溶胶光学厚度的时空分布及其主要影响类型

为准确了解中国地区气溶胶光学特性,通过1990~2017年的MERRA2数据集中的气溶胶光学厚度数据,采用Man-Kendall趋势检验法和Sen''s slope变化趋势分析法,从不同的时空尺度和气溶胶类型上分析中国地区AOD值的时空变化特征.结果表明：①从年际尺度上看,1990~2017年AOD年均值整体呈波动上升趋势;从季节尺度上看,月均值整体呈春夏秋依次递减,冬季有所提升的趋势,地形和气候环境是其主要影响因素.②在空间上,AOD年均值呈现东南高西北低的特征,西南部四川盆地、西北的塔里木与吐鲁番盆地等为AOD值的高值区,青藏高原地区为AOD值的低值区,同时AOD的MK值和Sen''s slope值也呈现由东南向西北递减的趋势.③沙尘气溶胶和硫酸盐气溶胶影响分布具有明显的区域差异.与地形、气候变化以及人类活动强度有着密切联系.     

2001～2017年全国气溶胶光学厚度时空分布及变化趋势

为探究全国大气气溶胶光学厚度（AOD）的分布及变化特征,利用最新的MODIS/Terra C6.1 550 nm AOD月数据分析了2001~2017年全国AOD的时空分布及变化趋势.结果表明,空间特征：年均AOD空间分布呈现两个显著的高值中心和低值中心,第一高值中心位于以人为气溶胶为主的华北平原、华中地区、长三角地区、珠三角地区和四川盆地,第二高值中心位于以尘埃气溶胶为主的塔克拉玛干沙漠地区,两个低值中心分别位于内蒙古地区东部至东北地区北部以及青藏高原.时间特征：各区域AOD峰值主要出现在春、夏季,塔克拉玛干沙漠地区、四川盆地和珠三角地区AOD在3~4月达到峰值,华北平原、华中地区和长三角地区AOD在5~7月达到峰值.趋势特征：2001~2006年,我国西北地区和内蒙古地区AOD呈现减少趋势,我国中东部地区和西南地区东部AOD呈现增长趋势.2007~2012年,青藏高原和塔克拉玛干沙漠地区AOD变化趋势由减少转为增长,华北平原和四川盆地AOD的增幅减弱,长三角地区AOD呈现弱的下降趋势.2013~2017年,我国大部地区AOD呈显著地下降趋势.     

混合基质3D打印可见光催化系统对病毒气溶胶的去除

利用3D打印灵活可控的特点和复合材料混合打印的优势，将可见光响应的ZnO/g-C₃N₄催化剂掺入ABS塑料，利用3D打印制成催化剂均匀稳定分布的光催化系统，使用流体动力学仿真模拟对反应器结构进行优化设计，用于处理相对密闭的室内空间中的病毒气溶胶.结果表明，病毒气溶胶比细菌气溶胶具有更强的抗逆性，添加螺旋导流板可以显著提升反应器传质性能并有效改善系统光催化效果，以提高对病毒气溶胶的去除率.以商业LED灯为光源的螺旋式反应器对高浓度病毒气溶胶（MS2、PhiX174噬菌体）和细菌气溶胶（大肠杆菌）具有高效去除效果，在3.75min停留时间可以实现对气溶胶的完全去除.     

Contribution of small-scale mining to employment,development and sustainability – an Indian scenario

Small-scale mining is more prevalent in India. The maximum production capacity of 50,000 tonnes/year has been accepted as a criterion to Indian small-scale mine. Such mines constitute about 90% of total number of mines, 42% of the total non-fuel minerals and metals, 5% of the fuel minerals. Some 3000 small scale mines account for a work force of about 0.5 million people. Yet this sector is a neglected sector in Indian economy and still considered as an unorganized sector. This paper examines the contribution of small-scale mines to employment and national mineral production, practices, and Indian policy on small-scale mining. It identifies the drawbacks in the existing Government policy and discusses the role of Government for up gradation in this sector. It focuses the need for technical up gradation and to ensure the economic and social infrastructure. It also discusses how the pursuit of sustainable livelihoods, poverty alleviation and indigenous peoples right in artisanal and small-scale mining be more effective when these communities are disadvantaged or neglected by Government policies. This paper concludes that this sector can make significant contribution to Indian economy and employment generation. It recommends that by establishing mining centre consist of shared mining and processing facilities, educating and training related initiatives it can be achieved.     

Importance of Sulfate Aerosol in Evaluating the Relative Contributions of Regional Emissions to the Historical Global Temperature Change

During the negotiations of the KyotoProtocol the delegation of Brazil presentedan approach for distributing the burden ofemissions reductions among the Partiesbased on the effect of their cumulativehistorical emissions on the global-averagenear-surface temperature. The Letter tothe Parties does not limit the emissions tobe considered to be only greenhouse gas(GHG) emissions. Thus, in this paper weexplore the importance of anthropogenicSO_x emissions that are converted tosulfate aerosol in the atmosphere, togetherwith the cumulative greenhouse gasemissions, in attributing historicaltemperature change. We use historicalemissions and our simple climate model toestimate the relative contributions toglobal warming of the regional emissions byfour Parties: OECD90, Africa and LatinAmerica, Asia, and Eastern Europe and theFormer Soviet Union. Our results show thatfor most Parties the large warmingcontributed by their GHG emissions islargely offset by the correspondingly largecooling by their SO_x emissions. Thus,OECD90 has become the dominant contributorto recent global warming following itslarge reduction in SO_x emissions after1980.     

矿产资源经济评价初步研究

本文论述了开展矿产资源经济评价对准确掌握各类矿产资源的数量和进行勘探及资源开发决策的重要性,阐述了矿产资源经济评价的基本原理,提出了经济评价基本模型及从经济角度对资源进行分类的标准和确定资源优先开发顺序的比较方法。     

长江上游及雅砻江徒步考察概况

本文对长江上游雅砻江一带的藏、汉、彝和纳西等民族混合居住地区的文化、社会、生产、生活习俗,地形、地质、地貌演变,以及森林砍伐,乱开矿山,随意捕杀动物等人为活动,造成了水土流失、滑坡、泥石流和地震等自然灾害。破坏了自然生态环境,给当地开发丰富的水资源和矿产资源带来了极大的影响。     

A natural analogue for CO2 mineral sequestration in Miocene basalt in the Kuanhsi-Chutung area, Northwestern Taiwan

In general, CO₂ sequestration by carbonation is estimated by laboratory experimentation and geochemical simulation. In this study, however, estimation is based on a natural analogue study of the Miocene basalt in the Kuanhsi-Chutung area, Northwestern Taiwan. This region has great potential in terms of geological and geochemical environments for CO₂ sequestration. Outcropping Miocene basalt in the study area shows extensive serpentinization and carbonation. The carbon stable isotopes of carbonates lie on the depleted side of the Lohmann meteoric calcite line, which demonstrates that the carbonates most probably precipitate directly from meteoric fluid, and water–rock interaction is less involved in the carbonation process. Oxygen stable isotope examinations also show much depleted ratios, representative of product formation under low temperatures (∼50–90 °C). This translates to a depth of 1–2 km, which is a practical depth for a CO₂ sequestration reservoir. According to petrographic observation and electron microprobe analysis, the diopside grains in the basalt are resistant to serpentinization and carbonation; therefore, the fluid causing alteration is likely enriched with calcium and there must be additional sources of calcium for carbon mineralization. These derived geochemical properties of the fluid support the late Miocene sandstone and enclosed basalts as having high potential for being a CO₂ sequestration reservoir. Moreover, the existing geochemical environments allow for mineralogical assemblages of ultramafic xenoliths, indicating that forsterite, orthopyroxene and feldspar minerals are readily replaced by carbonates. Based on the mineral transformation in xenoliths, the capacity of CO₂ mineral sequestration of the Miocene basalt is semi-quantitatively estimated at 94.15 kg CO₂ chemically trapped per 1 m³ basalt. With this value, total CO₂ sequestration capacity can be evaluated by a geophysical survey of the amount of viable Miocene basalt at the potential sites. Such a survey is required in the near future.     

Study of atmospheric electrical conductivity,SO2, NO2, aerosols SPM (>10 μ) and RSPM (<10 μ) in Mysore city,India

It is well known that atmospheric electrical conductivity is mainly due to the presence of small ions. Near the surface of the earth, radon and its daughter products predominantly produce small ions. In the presence of aerosol particles, the small ion concentration is reduced due to attachment of small ions to aerosol particles which decreases mobility and conductivity in the atmosphere. The ion pair production rate is estimated from the measured radon and its progeny concentrations and correlated with electrical conductivity of the atmosphere. Measurement of concentrations of suspended particulate matter (SPM), SO₂, and NO₂ of air was also carried out. Data showed that reduced electrical conductivity was related to concentration of airborne SPM.