因子分析法在天津市主要河流水质污染程度综合评价中的应用

因子分析法作为一种常用的多元统计分析方法,可以有效地分析河流水质的变化趋势,准确地反映水体的污染状况和污染程度。本文将因子分析法应用于天津市主要河流的水质评价中,得出了天津市主要河流水质状况的综合评价结果和污染程度排名,该研究可为水环境管理与决策工作提供依据。     

PCBs降解菌的筛选及其降解特性研究

采用富集培养的方法从多氯联苯(PCBs)污染土壤中筛选到1株高效降解PCBs的细菌,命名为PS-11.经16S rDNA初步鉴定,此菌株属于嗜麦芽寡养单胞菌(Stenotrophomonas maltophilia).结果表明,菌株PS-11能够以PCBs作为唯一碳源生长并且能够降解PCBs,菌株PS-11对2 mg.L-1PCB52 4 d的降解率为31.1%,7 d的降解率可达52.9%;对难降解的高氯代多氯联苯PCB153 7 d的降解率为10.9%.此外,该菌株的环境耐受性比较好,在30℃、pH为7～9、PCB52浓度为2～10 mg.L-1的条件下生长较快、降解效果较好,尤其在pH 7、PCB52浓度为2 mg.L-1时降解率最高;碳源种类不同,菌株PS-11的生长能力也不同,其中在以蔗糖为碳源时PS-11的生长能力最强,以葡萄糖为碳源时PS-11的适应期最短,且蔗糖、葡萄糖和Tween-80均可提高PS-11对PCB52的降解率;同时菌株PS-11还可耐受一定浓度的重金属,其耐受性大小为Pb2+>Cd2+>Zn2+>Cu2+.     

Assessing the role of mineral particles in the atmospheric photooxidation of typical carbonyl compound

Mineral particles are ubiquitous in the atmosphere and exhibit an important effect on the photooxidation of volatile organic compounds (VOCs). However, the role of mineral particles in the photochemical oxidation mechanism of VOCs remains unclear. Hence, the photooxidation reactions of acrolein (ARL) with OH radical (OH) in the presence and absence of SiO₂ were investigated by theoretical approach. The gas-phase reaction without SiO₂ has two distinct pathways (H-abstraction and OH-addition pathways), and carbonyl-H-abstraction is the dominant pathway. In the presence of SiO₂, the reaction mechanism is changed, i.e., the dominant pathway from carbonyl-H-abstraction to OH-addition to carbonyl C-atom. The energy barrier of OH-addition to carbonyl C-atom deceases 21.33 kcal/mol when SiO₂ is added. Carbonyl H-atom of ARL is occupied by SiO₂ via hydrogen bond, and carbonyl C-atom is activated by SiO₂. Hence, the main product changes from H-abstraction product to OH-adduct in the presence of SiO₂. The OH-adduct exhibits a thermodynamic feasibility to yield HO₂ radical and carboxylic acid via the subsequent reactions with O₂, with implications for O₃ formation and surface acidity of mineral particles.     

Competing pathways of cresol formation in toluene photooxidation: OH-toluene adducts react with NO2 or with O2?

Methyl-hydroxy-cyclohexadienyl radicals (OTAs) are the key products of the photooxidation of toluene, with implications for the fate of toluene. Hence, we investigated the photooxidation mechanisms and kinetics of three main OTAs (o-OTA, m-OTA, and p-OTA) with NO₂ using quantum chemical calculations as well as the fate of OTAs under the different concentration ratios of NO₂ and O₂. The mechanism results show that the pathway of H-abstraction by NO₂ to anti-HONO (anti-H-abstraction) is more favorable than the syn-H-abstraction pathway, because the strong interaction between OTAs and NO₂ is formed in the transition states of the anti-H-abstraction pathways. The branching ratios of the anti-H-abstraction pathways are more than 99% in the temperature range of 216−298 K. The total rate constant of the OTA-NO₂ reaction is 9.9 × 10⁻¹² cm³/(molecule∙sec) at 298 K, which is contributed about 90% by o-OTA + NO₂, and the main products are o-cresol and anti-HONO. The half-lives of the OTA-NO₂ reaction in some polluted areas of China are 35 times longer than those of the OTA-O₂ reaction. In the atmosphere, the NO₂- and O₂- initiated reactions of OTAs have the same ability to form cresols as [NO₂] is up to 142.1 ppmV, which is impossible to achieve. It implies that under the experimental condition, the [NO₂]/[O₂] should be controlled to be less than 7.8 × 10⁻⁵ to simulate real atmospheric oxidation of toluene. Our results reveal that for the photooxidation of toluene, the yield of cresol is not affected by the concentration of NO₂ under the atmospheric environment.     

Remediation of preservative ethylparaben in water using natural sphalerite: Kinetics and mechanisms

As a typical class of emerging organic contaminants(EOCs), the environmental transformation and abatement of preservative parabens have raised certain environmental concerns. However, the remediation of parabens-contaminated water using natural matrixes(such as, naturally abundant minerals) is not reported extensively in literature. In this study, the transformation kinetics and the mechanism of ethylparaben using natural sphalerite(NS) were investigated. The results show that around 63% of ethy...     

Seasonal to sub-seasonal variations of the Asian Tropopause Aerosols Layer affected by the deep convection, surface pollutants and precipitation

The Asian Tropopause Aerosols Layer (ATAL) refers to an accumulation of aerosols in the upper troposphere and lower stratosphere during boreal summer over Asia, which has a fundamental impact on the monsoon system and climate change. In this study, we primarily analyze the seasonal to sub-seasonal variations of the ATAL and the factors potentially influencing those variations based on MERRA2 reanalysis. The ability of the reanalysis to reproduce the ATAL is well validated by CALIPSO observations from May to October 2016. The results reveal that the ATAL has a synchronous spatiotemporal pattern with the development and movement of the Asian Summer Monsoon. Significant enhancement of ATAL intensity is found during the prevailing monsoon period of July–August, with two maxima centered over South Asia and the Arabian Peninsula. Owing to the fluctuations of deep convection, the ATAL shows an episodic variation on a timescale of 7–12 days. Attribution analysis indicates that deep convection dominates the variability of the ATAL with a contribution of 62.7%, followed by a contribution of 36.6% from surface pollutants. The impact of precipitation is limited. The ATAL further shows a clear diurnal variation: the peak of ATAL intensity occurs from 17:30 to 23:30 local time (LT), when the deep convection becomes strongest; the minimum ATAL intensity occurs around 8:30 LT owing to the weakened deep convection and photochemical reactions in clouds. The aerosol components of the ATAL show different spatiotemporal patterns and imply that black carbon and organic carbon come mainly from India, whereas sulfate comes mainly from China during the prevailing monsoon period.     

宁波市地表水重金属时空分布特性和健康风险评价

分别在丰水期和枯水期,从宁波市工业区和商业区地表水中采集了120个水样,检测了6种重金属(Cd、 Cr、 Ni、 Pb、 Zn和Fe)的浓度水平,分析了它们的时空分布特征,计算了重金属间的斯皮尔曼相关系数;结合时空特征和斯皮尔曼相关系数推测了主要污染源;通过计算健康风险指数和致癌风险指数评价了地表水中重金属对暴露人群存在的风险.结果表明,宁波市工业区和商业区不同季节地表水重金属的污染特性有很大的差异.工业区丰水期和枯水期重金属浓度平均值的大小顺序分别为：Fe>Zn>Ni>Pb>Cr>Cd和Fe>Zn>Cr>Ni>Pb>Cd,超标的严重性顺序分别为：Cr>Cd?Pb和Pb>Cr=Cd,含重金属工业废水是工业区地表水重金属的主要污染源之一.商业区丰水期和枯水期重金属浓度平均值的大小顺序分别为：Fe>Pb>Ni>Zn>Cd>Cr和Fe>Pb>Ni>Zn>Cr=Cd,丰水期超标的严重性顺序为：Cd>Pb;枯水期仅有Pb超标,超标率60%,公路源污染物是商业区地表水...     

1961～2015年贵州高原≥10℃积温时空变化特征

为揭示贵州高原≥10℃积温精细动态变化,以81个气象站点1961～2015年气温资料及地理信息数据为数据源,采用积温倾向率、累计距平、滑动T检验、小波分析、多元回归分析等统计方法,分析≥10℃的积温整体变化及周期变化,模拟各年代积温带空间变化。结果表明:(1) 1961～2015年≥10℃积温平均值为5 147. 22℃,1997年前后发生由冷到暖的突变,积温变化主周期约为3～5年,8年;(2) 1961～2015年、1961～1996年、1997～2015年≥10℃积温倾向率均值分别为49. 5℃/10a、-28. 1℃/10a、123. 5℃/10a,1961～1996年表现为降温趋势,1997～2015年表现为升温趋势,三个时间段积温倾向率均未通过显著性检验;(3)多元回归拟合≥10℃积温年代际空间分布,复相关系数均高于0. 92,积温空间分布呈现由西向东、由北向南升高的趋势;(4)不同年代际间积温带动态变化差异较大,1980s后约有60%以上区域表现为积温带Ⅱ升为积温带Ⅲ,积温带Ⅲ升为Ⅳ,1990s后降温区域消失。积温资源的增加对受高原气候限制的贵州高原有重要影响,对调整农业气候区划,确定作物种植区域以及最优化利用热量资源更具有针对性。     

基于卫星遥感的湖南省甲醛时空分布及影响因素分析

利用OMI遥感的甲醛逐日数据、MODIS传感器监测的NDVI数据以及湖南省能源消耗和氮氧化物排放量数据,对2009～2017年湖南省对流层大气中甲醛柱浓度时空变化特征及其影响因素进行了探究。结果表明：湖南省甲醛柱浓度总体空间分布具有西部山区低、北部洞庭湖平原和南部南岭地区高的特征;近九年湖南省甲醛柱浓度时间分布呈先增加后减小的趋势,最高值出现在2012年,最低值出现在2017年;年内甲醛柱浓度值夏季最高,秋季、春季次之,冬季最低,最低值出现在12月,最高值出现于9月;影响因素中地形与风向因素对甲醛柱浓度的空间分布有一定的影响,甲醛柱浓度与温度的相关性较高,降水次之,植被对甲醛的产生有很大的贡献,能源消耗与氮氧化物排放是湖南省甲醛柱浓度变化的重要人为因素。     

大气污染防治综合科学决策支持平台的开发及应用

大气污染防治和环境治理的紧迫性和复杂性需要科学有效的决策,而以费效评估为标志的综合决策评估模型是支撑环境决策和管理的重要工具.当前以ABaCAS（Air Pollution Control Cost-Benefit and Attainment Assessment System,空气污染控制成本效益与达标评估系统）为代表的综合决策评估模型可以实现对特定减排方案的费效评估,然而无法支持开展基于费效的达标路径优化,以及对应不同环境目标下减排策略的优化制定.针对上述问题,建立了大气污染防治综合科学决策支持平台.该平台以ABaCAS的4个核心模块为基础,建立了新的基于环境目标的反算技术（LE-CO）及优化集成运行模式（ABaCAS-OE）,实现了对不同环境目标要求的减排量反算,并对优化的减排策略下的空气质量改善效果、目标可达性、控制成本及健康收益进行快速估算.将大气污染防治综合科学决策支持平台应用到京津冀及周边地区"2+26"城市,反算了2035年达标要求下的减排情景,以及对应减排方案的费用与效益.结果表明,相较于2015年,预测了2035年京津冀及周边地区的PM_2.5、SO₂、NO_x、VOCs、NH₃排放量需分别减排70%~87%、49%~85%、66%~74%、51%~66%、0~40%才可达标,并且该情景可以带来可观的效益,费用-效益比达3.7.未来大气污染防治综合科学决策支持平台的研究将进一步面向多目标、多行业、多组分、多区域的精细化调控技术,实现经济、能源、排放、浓度、成本、健康、生态、气候一体化的综合决策,以全面支撑我国大气污染防治的综合科学决策.