融合时空特征的PCA-PSO-SVM臭氧(O3)预测方法研究

针对目前臭氧预测方法未能考虑臭氧污染的区域性和在时间周期内的强自相关性的问题,提出一种融合时空特征的PCA-PSO-SVM臭氧组合预测模型.利用小波分析和系统聚类提取臭氧时间序列波动特征和站点空间分布相似性特征,并通过主成分分析和粒子群算法优化的支持向量机组合模型（PCA-PSO-SVM）对臭氧日最大8h平均浓度进行预测,以2016~2018年杭州市大气污染物观测数据和气象数据进行实验验证.结果表明：融合时空特征的PCA-PSO-SVM模型预测精度有较大提升,与未融合时空特征的PCA-PSO-SVM模型相比,精度提升19%.气象因素中温度对臭氧预测效果影响最大,在气象预报数据存在一定误差的情况下,提出的模型仍得到较高精度的预测效果,具备较好的鲁棒性.     

基于工况变化的港作拖轮排放特性

利用便携式排放测试系统（PEMS）对一艘港作拖轮船进行了在变工况航行作业下的排放试验,研究了该船舶CO、碳氢化合物（THC）和NO_x的瞬态特性、颗粒物粒径分布特性、主机在不同工况下的排放因子.结果表明：拖轮主机在日常航行工况和不同发动机负荷下,颗粒物排放粒径呈单峰或双峰分布,第一峰值粒径在30~40nm之间,第二峰值粒径为191.1nm;CO和THC在进港返航工况下基于油耗排放因子显著高于其他工况,NO_x、颗粒物（PM）和颗粒物数量（PN）在离港返航时排放因子高于其他工况;各排放污染物在正顶作业时基于距离的排放因子高于其他工况;CO和THC基于功率的排放因子在正顶作业工况下最高,最高值分别为4.10和1.20g/（kW·h）,NO_x、PM、PN排放因子在倒拖作业工况下最高,最高值分别为10.28g/（kW·h）,0.28g/（kW·h）和13.97×10¹⁴个/（kW×h）.     

Effects of natural organic matter on cadmium mobility in paddy soil: A review

Cadmium (Cd) contamination in paddy soil has caused public concern. The uptake of Cd by rice plants depends on soil Cd mobility, which is in turn substantially influenced by organic matter (OM). In this review, we first summarize the fate of Cd in soil and the role of OM. We then focus on the effects of OM on Cd mobility in paddy soil and the factors influencing the remedial effectiveness of OM amendments. We further discuss the performance of straw incorporation in the remediation of Cd-contaminated paddy soils reported in laboratory and field studies. Considering the huge production of organic materials (such as straw) in agriculture, the use of natural OM for soil remediation has obvious appeal due to the environmental benefits and low cost. Although there have been successful application cases, the properties of OM amendments and soil can significantly affect the remedial performance of the OM amendments. Importantly, straw incorporation alone does not often decrease the mobility of Cd in soil or the Cd content in rice grains. Careful evaluation is required when considering natural OM amendments, and the factors and mechanisms that influence their remedial effectiveness need further investigation in paddy soil with realistic Cd concentrations.     

土壤铵氮在热活化过硫酸盐氧化过程中的转化

采用来自江苏和河北, 具有不同土壤有机质含量和NH₄⁺浓度的土壤样本, 系统地研究了NH₄⁺在热活化过硫酸盐(PS)氧化过程中的转化和归趋, 考察了反应时间、PS浓度和外加NH₄⁺对硝基副产物生成的影响.结果表明, 土壤中的NH₄⁺能够转化成3-硝基酚、4-硝基酚、2-羟基-5-硝基苯甲酸、4-羟基-3-硝基苯甲酸、2, 4-二硝基酚等副产物, 它们的生成量随着反应的进行先增加后降低.增大PS浓度可促进硝基副产物的生成.当PS浓度为30mmol/kg, 反应12h后一硝基酚和一硝基羟基苯甲酸的生成量达到最大.然而随着PS浓度进一步增大, 硝基副产物发生降解.硫酸根自由基(SO₄·^-)在硝化过程中起到了关键作用, 它能将NH₄⁺氧化生成氨基自由基(·NH₂), 随后经过一系列自由基链式反应生成二氧化氮自由基(NO₂·).同时, SO₄·^-进攻土壤有机质中的酚结构单元, 使其氧化生成苯氧自由基, 苯氧自由基进一步与NO₂·结合生成硝基副产物.天然有机质(NOM)在环境中无处不在, NH₄⁺在环境中也普遍存在, PS用于土壤和地下水污染修复时生成硝基副产物很可能是一个普遍现象.     

基于摩擦纳米发电机的微塑料实时检测实验研究

采用基于自供电的摩擦纳米发电机(TENG)技术,设计开发了一种利用间断液柱检测水样内微塑料颗粒尺寸和丰度的实时快速检测方法和装置,并通过实验测试完成了对微塑料的尺寸形貌表征和化学元素组成的实时高效检测.研究发现,去离子水中加入微塑料颗粒时,溶液中zeta电位降低,改变了管壁表面的极化电场方向;随着水溶液中微塑料颗粒直径或丰度的增加,开路电压呈现减小趋势,50μm时减小了43.1%,0.250%浓度时减小了79.6%;微塑料颗粒对自来水的开路电压影响显著,以10μm微塑料颗粒为例,开路电压减小了20%,证明了TENG技术对海洋微塑料检测的可行性.     

利用CDOM吸收系数估算博斯腾湖水体表层DOC浓度

基于2021年夏秋两季西部干旱区博斯腾湖表层50个采样点位实测数据,通过对DOC特征的统计学分析、内外源因素影响的时空差异以及电导率相关性验证,将博斯腾湖划分为河口和非河口区域.然后以CDOM特征波长吸收系数a₂₅₀和a₃₆₅为自变量,以DOC浓度（c_DOC）为因变量,分别构建了基于CDOM的河口和非河口水域DOC浓度估算模型.结果表明：河流与湖泊进行水体交换的同时,会将大量陆源DOC输送到博斯腾湖中,使得河口区域DOC浓度明显高于非河口区域（t-tests,P<0.01）,河口区域的DOC浓度（c_DOC）约是非河口区域的2.2~2.3倍,且在河口区域c_DOC与电导率呈现显著相关关系（夏季：R²=0.81,P<0.01;秋季：R²=0.84,P<0.01）.本文构建拟合模型（c_DOC=α+β·α₂₅₀+γ·α₃₆₅）,并通过交叉验证的方法来检验模型精度.将夏季和秋季同区域数据统一建模,河口和非河口区域CDOM与DOC均存在较好的相关关系,且模型精度较高（河口区域：R²=0.60,RMSE=8.56%;非河口区域：R²=0.66,RMSE=8.77%）.本文所建立的模型可以在不增加环境因子变量的前提下提高精度,有利于实现卫星遥感反演.同时,本研究揭示了河流输入对博斯腾湖DOC分布和估算的时空影响,提出可利用CDOM估算DOC浓度,但需根据水文特征和c_DOC等因素区分河口和非河口区域.本研究对实现新疆水资源合理开发、有效保护以及综合治理提供科学依据,对我国西部干旱区湖泊DOC遥感动态监测具有重要意义.     

Influence of dissolved organic matter on methylmercury transformation during aerobic composting of municipal sewage sludge under different C/N ratios

Current knowledge about the transformation of total mercury and methylmercury (MeHg) in aerobic composting process is limited. In this study, the composition and transformation of mercury and dissovled organic matter (DOM) in aerobic composting process of municipal sewage sludge were were comprehensively characterized, and the differences among the three C/N ratio (20, 26 and 30) were investigated. The main form of mercury in C/N 20 and 26 was organo-chelated Hg (F3, 46%-60%); while the main form of mercury in C/N 30 was mercuric sulfide (F5, 64%-70%). The main component of DOM in C/N 20 and 26 were tyrosine-like substance (C1, 53%-76%) while the main fractions in C/N 30 were tyrosine-like substance (C1, 28%-37%) and fulvic-like substance (C2, 17%-39%). The mercury and DOM varied significantly during the 9 days composting process. Compared to C/N 20 and 26, C/N 30 produced the less MeHg after aerobic composting process, with values of 658% (C/N 20), 1400% (C/N 26) and 139% (C/N 30) of the initial, respectively. Meanwhile, C/N 30 produced the best compost showed greater degree of DOM molecular condensation and humification. Hg fraction had been altered by DOM, as indicated by a significant correlation between mercury species and DOM components. Notably, C/N 30 should be used as an appropriate C/N ratio to control the methylation processes of mercury and degration of DOM.     

Influence of MBBR carrier geometrical properties and biofilm thickness restraint on biofilm properties, effluent particle size distribution, settling velocity distribution, and settling behaviour

The relatively poor settling characteristics of particles produced in moving bed biofilm reactor (MBBR) outline the importance of developing a fundamental understanding of the characterization and settleability of MBBR-produced solids. The influence of carrier geometric properties and different levels of biofilm thickness on biofilm characteristics, solids production, particle size distribution (PSD), and particle settling velocity distribution (PSVD) is evaluated in this study. The analytical ViCAs method is applied to the MBBR effluent to assess the distribution of particle settling velocities. This method is combined with microscopy imaging to relate particle size distribution to settling velocity. Three conventionally loaded MBBR systems are studied at a similar loading rate of 6.0 g/(m² •day) and with different carrier types. The AnoxK™ K5 carrier, a commonly used carrier, is compared to so-called thickness-restraint carriers, AnoxK™ Z-carriers that are newly designed carriers to limit the biofilm thickness. Moreover, two levels of biofilm thickness, 200 μm and 400 μm, are studied using AnoxK™ Z-200 and Z-400 carriers. Statistical analysis confirms that K5 carriers demonstrated a significantly different biofilm mass, thickness, and density, in addition to distinct trends in PSD and PSVD in comparison with Z-carriers. However, in comparison of thickness-restraint carriers, Z-200 carrier results did not vary significantly compared to the Z-400 carrier. The K5 carriers showed the lowest production of suspended solids (0.7 ± 0.3 g-TSS/day), thickest biofilm (281.1 ± 8.7 µm) and lowest biofilm density (65.0 ± 1.5 kg/m³). The K5 effluent solids also showed enhanced settling behaviour, consisting of larger particles with faster settling velocities.     

Seasonal variations, temperature dependence, and sources of size-resolved PM components in Nanjing, east China

Size-segregated ambient particulate matter (PM) samples were collected seasonally in suburban Nanjing of east China from 2016 to 2017 and chemically speciated. In both fine (< 2.1 µm, PM_2.1) and coarse (> 2.1 µm, PM_>2.1) PM, organic carbon (OC) accounted for the highest fractions (26.9% ± 10.9% and 23.1% ± 9.35%) of all measured species, and NO₃⁻ lead in average concentrations of water-soluble inorganic ions (WSIIs). The size distributions of measured components were parameterized using geometric mean diameter (GMD). GMD values of NO₃⁻, Cl⁻, OC, and PM for the whole size range varied from < 2.1 µm in winter to > 2.1 μm in warm seasons, which was due to the fact that the size distributions of semi-volatile components (e.g., NH₄NO₃, NH₄Cl, and OC) had a dependency on the ambient temperature. Unlike OC, elemental carbon (EC), and elements, NH₄⁺, NO₃⁻, and SO₄²⁻ exhibited an increase trend in GMD values with relative humidity, indicating that the hygroscopic growth might also play a role in driving seasonal changes of PM size distributions. Positive matrix factorization was performed using compositional data of fine and coarse particles, respectively. The secondary formation of inorganic salts contributing to the majority (> 70%) of fine PM and 20.2% ± 19.9% of speciated coarse PM. The remaining coarse PM content was attributed to a variety of dust sources. Considering that coarse and fine PM had comparable mass concentrations, more attention should be paid to local dust emissions in future air quality plans.     

Formation of regulated and unregulated disinfection byproducts during chlorination and chloramination: Roles of dissolved organic matter type, bromide, and iodide

Algal blooms and wastewater effluents can introduce algal organic matter (AOM) and effluent organic matter (EfOM) into surface waters, respectively. In this study, the impact of bromide and iodide on the formation of halogenated disinfection byproducts (DBPs) during chlorination and chloramination from various types of dissolved organic matter (DOM, e.g., natural organic matter (NOM), AOM, and EfOM) were investigated based on the data collected from literature. In general, higher formation of trihalomethanes (THMs) and haloacetic acids (HAAs) was observed in NOM than AOM and EfOM, indicating high reactivities of phenolic moieties with both chlorine and monochloramine. The formation of haloacetaldehydes (HALs), haloacetonitriles (HANs) and haloacetamides (HAMs) was much lower than THMs and HAAs. Increasing initial bromide concentrations increased the formation of THMs, HAAs, HANs, and HAMs, but not HALs. Bromine substitution factor (BSF) values of DBPs formed in chlorination decreased as specific ultraviolet absorbance (SUVA) increased. AOM favored the formation of iodinated THMs (I-THMs) during chloramination using preformed chloramines and chlorination-chloramination processes. Increasing prechlorination time can reduce the I-THM concentrations because of the conversion of iodide to iodate, but this increased the formation of chlorinated and brominated DBPs. In an analogous way, iodine substitution factor (ISF) values of I-THMs formed in chloramination decreased as SUVA values of DOM increased. Compared to chlorination, the formation of noniodinated DBPs is low in chloramination.