Wet deposition chemistry studies at Suva, Fiji, a remote tropical island site in the south Pacific

A field project encompassing wet-only rainwater sampling was initiated as a bilateral Fiji/Australia activity. Normally, biweekly samples were collected, using a wet-only rainwater sampler, and analysed for H⁺, Na⁺, K⁺, Mg²⁺, NH₄ ⁺, Cl^–, NO₃ ^–, SO₄ ^2–, PO₄ ^3-, methane sulphonic acid, oxalic acid, formic acid and acetic acid. The pH of the rainwater ranged between 5.730 and 4.480 with an average value of 5.176, slightly lower than the pH of unpolluted rainwater saturated with atmospheric CO₂(pH = 5.650). Na⁺and Cl^–were the major ions with average concentrations of 98.15 M and 109.57 M respectively. There is an excellent correlation between the cation sum (average 147.71 eq L^-1) and the anion sum (average 142.12 eq L^-1) attesting to the quality of the data generated. This paper presents the detailed results of the study for a relatively clean remote island site in Suva, Fiji, latitude 18° 09 S, longitude 178° 27 E, height 6 m, and outlines prospects for further work.     

Observations of N2O5 and NO3 at a suburban environment in Yangtze river delta in China: Estimating heterogeneous N2O5 uptake coefficients

The nitrate radical (NO₃) and dinitrogen pentoxide (N₂O₅) play an important role in the nocturnal atmosphere chemistry. Observations of NO₃ radicals and N₂O₅ were performed in a semirural ground site at Tai'Zhou in polluted southern China using cavity ring down spectroscopy (CRDS) from 23 May to 15 June 2018. The observed NO₃ and N₂O₅ concentrations were relatively low, with 1 min average value of 4.4 ± 2.2 and 26.0 ± 35.7 pptV, respectively. The N₂O₅ uptake coefficient was determined to be from 0.027 to 0.107 based on steady state lifetime method. Fast N₂O₅ hydrolysis was the largest contributor to the loss of NO₃ and contributed to substantial nitrate formation, with an average value of 14.83 ± 6.01 µg/m³. Further analysis shows that the N₂O₅ heterogeneous reactions dominated the nocturnal NO_x loss and the nocturnal NO_x loss rate is 0.14 ± 0.02 over this region.     

淮南新集矿区主要充水含水层水化学特征及成因

为探明新集矿区深层地下水离子组成及其演化特征,采集了研究区砂岩水和太灰水等共20个水样,测试分析常规离子和氢氧同位素数据,采用Piper三线图、相关性分析、离子比例系数与饱和指数等方法,探讨了研究区深层地下水水化学特征及其成因。结果表明:(1)研究区砂岩水为高矿化度水,平均矿化度为2 743. 73mg/L,水化学类型主要为Cl-Na型,太灰水多为中矿化度水,平均矿化度为1 468. 33mg/L,水化学类型主要为HCO3·Cl-Na型和Cl-Na型;(2)研究区地下水的补给不仅有大气降水和地表水,还有古气候条件下形成的古溶滤-渗入水,且由于矿物质与深层地下水的水岩作用使得氧同位素发生漂移;(3)含水层中主要发生的水岩相互作用有硅酸盐和蒸发盐岩的溶解及阳离子交替吸附作用,盐岩和石膏在研究区地下水中是反应性矿物,白云石和方解石的溶解在矿区地下水中呈过饱和状态。     

超临界水氧化降解有机物的定量构效关系研究

研究了邻苯二甲酸氢钾、辛基酚、硝基苯等20种有机物在超临界水氧化中的降解效果,探究了温度(325~525℃)和停留时间(30~360s)对超临界水氧化降解有机物的影响,并分析了20种有机物降解速率常数与量子化学参数之间的关系.结果表明,超临界水氧化法能够有效降解有机物,TOC去除率最高可达99%以上.随着反应温度的升高、停留时间的延长,TOC的去除率也随之提高,并且降解规律符合一级动力学.采用密度泛函理论,通过计算得到目标物的量子化学参数,再结合有机物降解的动力学常数进行相关性分析,结果发现,q(H+)、f(-)_(min)和f(0)_(min)与目标物降解率显著相关.     

Fog composition along the Yangtze River basin: Detecting emission sources of pollutants in fog water

To investigate the fog chemistry along the Yangtze River basin, a field observation experiment was performed from Shanghai to Wuhan during November 2015. Fifteen fog water samples were collected by using a three-stage Caltech Active Strand Cloud water Collector(CASCC). The three-stage CASCC was mounted on the board of a ship. PH, electrical conductivity(EC), H_2O_2,HCHO, S(IV), ten inorganic ions, seven organicacids and sixteen trace metal elements were measured in this study. The p H of fog water samples ranged from weakly acidic(pH 4.3) to weakly alkaline(pH 7.05) and the EC ranged from 32.4 to 436.3 μS/cm. The main cations in fog water were NH+4 and Ca~(2+), accounting for 12.35% and 29.07% of those inorganic ions,respectively. In addition, SO_4~(2-) and NO_(-3) contributed to 25.52% and 12.93% to total anion concentrations respectively. Moreover, the dominant kinds of organicacids were formate and oxalate, occupying 45.28% and 28.03% of the total organicacids, respectively. For trace metal elements in fog samples, Al, Fe, Zn, and Ba revealed 34.6%, 16.4%, 19.3%, and 20.9%contributions to these sixteen trace element concentrations, respectively. The results indicated that pollutants were mainly from human activities, including fossil fuel combustion,biomass burning, steel-making, stone quarrying and sand digging. Besides, natural sources including natural background levels and long-range transport of sea salt particles also aggravated the pollution levels in the fog events along the Yangtze River.     

北江流域水化学时空变化及化学风化特征

为了研究我国南方湿润地区河流水化学时空变化特征及控制因素,选择珠江流域第二大水系的北江为研究对象,通过分析2015年6月（汛期）和12月（非汛期）干流和支流河水基本水质参数及主量离子,利用化学计量法及质量守恒法定量评估了自然过程及人类活动共同影响下的流域化学风化特征及其通量.结果表明:①北江河水主量离子浓度非汛期高于汛期.岩石的区域分布和矿山活动构成了河水离子浓度和水化学类型的空间异质性,其中北江干流和支流连江为Ca-HCO₃型,而支流滃江则以Ca-SO₄型为主.②岩石对北江流域化学风化贡献率依次为碳酸岩（78.44%）>硅酸岩（14.43%）>降水源（5.42%）>蒸发岩（1.71%）.基于碳酸岩是北江径流水化学的主要控制因素,滃江流域的矿山开采活动加速了碳酸岩的风化,其对北江流域化学风化的贡献为7%.③汛期与非汛期的碳酸岩风化速率分别为7.49和5.29 t/（km2·月）,年化学风化速率为87.63 t/（km2·a）.研究显示,由于受水热条件、流域面积以及岩性的影响,北江流域年化学风化速率略大于西江流域,远高于东江以及全球流域化学风化平均值,北江对整个珠江流域的风化贡献较大.      

半挥发性有机物GC/MS分析方法研究

用气相色谱／质谱（ＧＣ／ＭＳ）研究分析了环境中的半挥发性有机标准物。以十氟三苯基磷作调机物,对ＧＣ／ＭＳ仪器系统进行了调整,离子丰度值符合美国环保局（Ｕ．Ｓ．ＥＰＡ）１９８６年推荐的离子丰度标准。测定了３２种目标化合物的保留时间及相对保留因子ＲＦ值,结果表明除五氯苯酚不达标外,其余化合物的ＲＦ值均符合要求,３１种目标化合物的加标回收率为２１％～９７％,相对标准偏差为３．１％～２４．１％,符合美国环保局８２７０方法质量控制检验标准。最后对建立定量校正库与ＧＣ／ＭＳ分析进行了讨论     

水合二氧化锰界面特性及其除污染效能

研究了水合二氧化锰(δMnO2)的界面特性及其吸附性能.考察了δMnO2的比表面积、粒径分布、表面官能团及ζ电位;探讨了δMnO2对水中亚砷酸盐及腐殖酸的吸附去除效能.结果表明:δMnO2的比表面积为117.4m2·g-1,体积平均粒径为0.11μm;δMnO2表面具有丰富的表面羟基(Mn-OH);随着pH值由1.9升高至10.7,δMnO2的ζ电位由 22.7mV降低至53.5mV,其零电荷点在pH3.0附近.δMnO2对亚砷酸盐(As(III))及腐殖酸(HA)均表现出优良的吸附去除效能,其单位δMnO2质量的最大吸附量分别为137μgAs(III)·mg-1δMnO2和1.01mgTOC·mg-1δMnO2.亚砷酸盐与腐殖酸共存时,腐殖酸的存在使得亚砷酸盐的去除率下降10%—28%;而亚砷酸盐对腐殖酸的去除无明显影响.     

气相化学反应中的云盖效应

本文在ＣＢＭ－Ｉ机理的基础上考虑了ＯＨ和ＨＯ２自由基对ＳＯ２的氧化作用和云对光解率的影响，定量研究了气相色化学反应中的云盖效应。结果表明，云的存在将改变整个反应体系的平衡，气态物对云的响应是非线的。     

水中甲苯、对二甲苯磁化-光解耦合过程动力学研究

以甲苯、对二甲苯两种典型苯系污染物为研究对象 ,对其在水中的紫外光解(UV)、磁化 紫外光解 (PM UV)进行了过程动力学比较研究 ,结果证实高强度永久磁场 ( >0 1T)有促进光解的效应 ,并阐述了磁场通过影响污染物光解时 ,自由基对系间跃迁速度的变化而影响反应速度的作用机理 .