晋城市冬季环境空气中挥发性有机物的污染特征及来源解析

采集晋城市冬季环境空气样品,利用色谱-质谱仪分析了其挥发性有机物(VOCs)的组份特征,运用PMF、特征比值、后向轨迹模型对其来源进行了研究,并计算了臭氧和二次有机气溶胶的生成潜势,探讨了其环境影响.结果表明,观测期间,晋城市VOCs平均浓度为93.35μg·m~(-3),其中烷烃类化合物浓度为52.91μg·m~(-3),在VOCs中占比较高为56.68%;PMF分析VOCs排放源有工业排放源、燃烧源、机动车源、溶剂使用源和植物源,贡献率分别为33.71%、30.27%、26.28%、9.00%和0.74%;特征比值法分析中,苯/甲苯和异戊烷/正戊烷比值分别为1.58±0.68和2.07±0.43,介于道路来源与燃煤源之间,为两者混合来源.后向轨迹聚类3个代表性气团均来自西北方向,分别占比50%、25%和25%,西北方向的工业污染可能会对晋城市VOCs造成影响;观测期间,晋城市空气质量指数、总VOCs浓度和机动车源贡献率在风速较小时(3 m·s-1)分别为143、162.48μg·m~(-3)和46.16%,各数值均高于风速较大(3~6.9 m·s-1)时(60、35.72μg·m~(-3)和16.15%);芳香烃类化合物的臭氧和二次有机气溶胶生成潜势分别为98.89μg·m~(-3)和1.21μg·m~(-3),占总生成潜势的37.28%和97.01%,是两种生成潜势最高的VOCs化合物种类.因此,控制工业、机动车和燃烧排放是控制晋城市环境空气中VOCs污染的主要途径.     

水源水消毒副产物生成势与UV254/DOC的相关性研究

使用XAD-4和XAD-8树脂对宜兴3个水源原水中DOM进行亲疏水性分类,采用优化方法测定分类水样的DBPFP,并进行DBPFP与DOM量化指标之间的相关性分析,以确定实际生产过程DBPs生成量的主要影响因素.由三维荧光光谱图得到3个水源原水DOM组成差异较大,水质区别明显.由亲疏水性分类分析发现原水中疏水性和亲水性DOM含量较高,疏水性DOM水样的DBPFP大于原水,得到水样的DBPFP主要取决于DOM与消毒剂反应产生DBPs的效率,而不是DOM的量.引入UV_(254)/DOC这个指标,发现不同分类水样UV_(254)/DOC的差异情况与其DBPFP相吻合,对两者进行回归分析,发现水样THMFP和DHAAFP与UV_(254)/DOC之间存在明显的线性关系,线性可决系数R2分别为0.89和0.85.因此研究减小原水UV_(254)/DOC的技术工艺对于控制给水中DBPs浓度具有重要意义.     

车用钛酸锂电池生命周期评价

为评估车用钛酸锂（LTO）电池对能源、环境与资源的影响,构建了包括重制与二次使用阶段在内的车用锂电池全生命周期评价模型,以某款国产纯电动客车用钛酸锂电池包为评价对象,计算得出每kW·h钛酸锂电池全生命周期的总能量消耗（CED）、全球变暖潜值（GWP）和不可再生矿产资源耗竭潜值（ADP（e））分别为2.80×10⁴MJ、1.86×10³kg CO₂eq.以及4.77×10^-3kg Sbeq.其全生命周期CED与GWP主要与两个使用阶段中由电池充放电效率引起的能量损耗相关,生产阶段GWP主要来源于正负极材料、铝制材料和N-甲基吡咯烷酮.基于全生命周期存储-释放每MJ能量的视角,发现二次使用可显著降低电池全生命周期GWP;与已有研究中其他锂电池对比可知LTO电池生产阶段GWP最低.     

南极拉森北部冰架表面物质损失机制探讨

基于解密航片、光学遥感影像以及卫星雷达测高数据,完成一个较长时间序列的拉森A和B冰架的范围及表面高程变化监测.在此基础上,结合NCEP/NCAR夏季逐月平均气温数据和GPCP全球降水数据这两种气象数据来探讨拉森北部冰架表面物质平衡机制.结果表明：随着气温的升高,拉森A和B冰架自1968年以来总共消失了14 000km²的浮冰.当前,拉森A冰架已经完全消失,拉森B冰架仅存2 000km².伴随着冰架的持续崩塌与退缩,拉森北部冰架展现出高程持续降低的趋势,而且拉森A冰架的降低速度（-0.45m/a）明显高于拉森B冰架（-0.09m/a）.作为冰架表面物质平衡估算的两个主要参数,拉森A冰架的夏季平均气温从1968年的0.16℃升高到近期的0.84℃;拉森B冰架的夏季平均气温从1968年的0.04℃升高到近期的0.66℃.过去几十年的降水量变化对拉森北部冰架表面物质累积产生的影响很小,反倒是夏季温暖的降雨进一步加剧该地区的表面物质负平衡.对于持续崩塌与退缩型的拉森北部冰架来说,其高程降低除了受到冰架表面冰雪融化与再凝结导致的积雪致密化驱动外,还受到冰架后退导致的背向应力减少,进而导致的冰架物质输送加快的深刻影响.总之,在全球气候变暖的背景下,拉森A和B冰架的表面物质体现出越来越明显的负平衡趋势.     

Water regime-nitrogen fertilizer incorporation interaction: Field study on methane and nitrous oxide emissions from a rice agroecosystem in Harbin, China

Water regime and nitrogen (N) fertilizer are two important factors impacting greenhouse gases (GHG) emission from paddy field, whereas their effects have not been well studied in cold region. In this study, we conducted a two-year field experiment to study the impacts of water regime and N fertilizer on rice yields and GHG emissions in Harbin, China, a cold region located in high latitudes. Our results showed that intermittent irrigation significantly decreased methane (CH₄) emission compared with continuous flooding, however, the decrement was far lower than the global average level. The N₂O emissions were very small when flooded but peaked at the beginning of the disappearance of floodwater. The N fertilizer treatments increased CH₄ emissions at low level (75kgN/ha). But both CH₄ and N₂O emissions were uninfluenced at the levels of 150kgN/ha and 225kgN/ha. Rice yields increased under intermittent irrigation and were highest at the level of 150kgN/ha. From our results, we recommended that the intermittent irrigation and 150kgN/ha as the ideal water regime-nitrogen fertilizer incorporation for this area to achieve low GHG emissions without impacting rice yields.     

A comparison of process performance during the anaerobic mono- and co-digestion of slaughterhouse waste through different operational modes

The use of consecutive feeding was applied to investigate the response of the microbial biomass to a second addition of substrates in terms of biodegradation using batch tests as a promising alternative to predict the behavior of the process. Anaerobic digestion (AD) of the slaughterhouse waste (SB) and its co-digestion with manure (M), various crops (VC), and municipal solid waste were evaluated. The results were then correlated to previous findings obtained by the authors for similar mixtures in batch and semi-continuous operation modes. AD of the SB failed showing total inhibition after a second feeding. Co-digestion of the SB + M showed a significant improvement for all of the response variables investigated after the second feeding, while co-digestion of the SB + VC resulted in a decline in all of these response variables. Similar patterns were previously detected, during both the batch and the semi-continuous modes.     

Effect of drainage on CO2, CH4, and N2O fluxes from aquaculture ponds during winter in a subtropical estuary of China

Aquaculture ponds are dominant features of the landscape in the coastal zone of China.Generally,aquaculture ponds are drained during the non-culture period in winter.However,the effects of such drainage on the production and flux of greenhouse gases(GHGs)from aquaculture ponds are largely unknown.In the present study,field-based research was performed to compare the GHG fluxes between one drained pond(DP,with a water depth of 0.05 m)and one undrained pond(UDP,with a water depth of 1.16 m)during one winter in the Min River estuary of southeast China.Over the entire study period,the mean CO_2flux in the DP was(0.75±0.12)mmol/(m~2·hr),which was significantly higher than that in the UDP of(-0.49±0.09)mmol/(m~2·hr)(p0.01).This indicates that drainage drastically transforms aquaculture ponds from a net sink to a net source of CO_2in winter.Mean CH_4and N_2O emissions were significantly higher in the DP compared to those in the UDP(CH_4=(0.66±0.31)vs.(0.07±0.06)mmol/(m~2·hr)and N_2O=(19.54±2.08)vs.(0.01±0.04)μmol/(m~2·hr))(p0.01),suggesting that drainage would also significantly enhance CH_4and N_2O emissions.Changes in environmental variables(including sediment temperature,p H,salinity,redox status,and water depth)contributed significantly to the enhanced GHG emissions following pond drainage.Furthermore,analysis of the sustained-flux global warming and cooling potentials indicated that the combined global warming potentials of the GHG fluxes were significantly higher in the DP than in the UDP(p0.01),with values of739.18 and 26.46 mg CO_2-eq/(m~2·hr),respectively.Our findings suggested that drainage of aquaculture ponds can increase the emissions of potent GHGs from the coastal zone of China to the atmosphere during winter,further aggravating the problem of global warming.     

中国优势金属供应全球需求的风险评估

随着新一轮科技革命和产业转型的发展,全球金属资源供需格局发生重大调整,美国、欧盟、日本等主要发达国家不断倒逼中国敞开优势金属供应。为保障国家金属资源安全,论文从可依赖性、可持续性、可承受性3个维度建立了一套金属资源供应风险评估体系,对中国优势金属供应全球需求的风险进行评估,结果表明：1）中国优势金属整体供应风险较高,铟、铋等两种金属风险值都在80以上,处于高风险水平;锑、锗、钡、镁、钨、稀土等6种金属风险值都是60~80之间,处于中高风险水平;镓、锶等两种金属处于中风险水平。2）在10种中国优势金属中,钡的可依赖性风险最高,达到81.88,稀土的风险最低,只有42.42。铟的可持续性风险最高,达到81.80;锑的最低,风险值为69.46。铟的可承受性风险也最高,高达100;铋的次之,风险值为89.23;钡的最低,只有33.96。3）随着未来新兴产业的快速发展,中国优势金属的供应风险将更加严峻。     

阿哈水库DOM的分离及其对消毒副产物的贡献

为研究高原喀斯特湖库DOM（dissolved organic matter,溶解性有机质）的组成及其化学特征对DBPs（disinfection by-products,消毒副产物）生成路径的影响,以西南喀斯特地区贵阳市阿哈水库的DOM为研究对象,结合XAD大孔树脂分离技术,通过化学表征〔包括UV-Vis（紫外-可见光光谱）、FTIR（红外光谱）和3D-EEM（三维荧光光谱）〕手段来研究各组分对C-DBPs（含碳消毒副产物）和N-DBPs（含氮消毒副产物）的生成贡献.不同组分芳香性的大小依次为HON（憎水中性物）> HIB（亲水碱）> HOA（憎水酸）> HIN（亲水中性物）≈HIA（亲水酸）> HOB（憎水碱）.憎水与亲水DOM的DBPs生成潜能相近.其中,HON最高,其次为HIB和HOA.HIB和HOA的主要卤代反应位分别来源于藻类有机物的蛋白质和富里酸,而HON的DBPs生成潜能的贡献主要为分子中的芳香和共轭不饱和结构.HIA和HIN的构成主要为脂肪烃,贡献较低的DBPs的生成潜能.对于C-DBPs,THMs和HAAs的生成潜能总体相近,不同组分的差异明显.对于N-DBPs,卤乙腈的生成潜能占80%以上,憎水DOM的贡献较高.DBPs的生成路径从UV-Vis、FTIR和3D-EEM的官能团和特征峰解析结果中均得到了较好的响应.      

氧化还原电位对土壤中重金属环境行为的影响研究进展

E_h（redox potential,氧化还原电位）代表土壤氧化性和还原性的相对程度,是以电位反映土壤所处氧化还原状态的指标.由于重金属易与对E_h敏感的组分发生吸附、络合、沉淀等化学反应,因此E_h的变化会直接/间接影响重金属形态从而决定其毒性和活性.E_h变化对重金属活性往往存在双向影响:①淹水环境使E_h降低,引发反硝化反应、铁锰氧化物和硫酸盐还原,使pH向中性靠拢,从而间接导致酸性土壤中游离态重金属沉淀或碱性土壤中吸附态重金属释放.②厌氧条件在使E_h发生变化的同时,会引起铁锰氧化物、有机质、硫化物的形态或含量发生改变,如铁锰氧化物还原、大分子有机质分解,分解产物与重金属离子结合增加了可溶性重金属的浓度,但厌氧条件也可以使重金属离子和硫化物产生沉淀,且还原Cr、Hg等元素,降低毒性;在氧化条件下,硫化物氧化形成硫酸盐促进了重金属释放;但铁锰离子沉淀及其氧化物形态变化形成的具有强吸附力的无定形铁锰氧化物可重新吸附游离态金属离子.这些复杂的化学变化对定量化研究E_h对重金属的影响造成困难,从而降低了E_h波动环境（水稻土、周期性覆水潮滩沉积物等）中重金属污染风险评价的准确性,也限制了通过改变E_h来原位修复重金属污染土壤的方法实施.因此,需进一步对E_h诱导下土壤颗粒界面上发生的与重金属行为相关的反应进行深入研究,并开发检测分析技术,如无损伤的物理探测方法或同位素稀释技术等,建立不同土壤中E_h与重金属形态、活性的定量关系,以揭示E_h对重金属形态的影响机制.