Black carbon and polycyclic aromatic hydrocarbons (PAHs) in surface sediments of China's marginal seas

This study investigates the distribution of black carbon (BC) and its correlation with total polycyclic aromatic hydrocarbons (I PAH) pound in the surface sediments of China's marginal seas. BC content ranges from < 0.10 to 2.45 mg/g dw (grams dry weight) in the sediments studied, and varied among the different coastal regions. The Bohai Bay sediments had the highest BC contents (average 2.18 mg/g dw), which comprises a significant fraction (27%-41%) of the total organic carbon (TOC) preserved in the sediments. In comparison, BC in the surface sediments of the North Yellow Sea, Jiaozhou Bay, East China Sea and the South China Sea is less abundant and accounted for an average of 6%, 8%, 14% and 5%, respectively, of the sedimentary organic carbon pool. The concentration of I PAH pound in the surface sediments ranges from 41 to 3 667 ng/g dw and showed large spatial variations among the sampling sites of different costal regions. The Bohai Bay has the highest I PAH pound values, ranging from 79 to 3 667 ng/g dw. This reflects the high anthropogenically contaminated nature of the sediments in the bay. BC is positively correlated to TOC but a strong correlation is not found between BC and I PAH pound in the surface sediments studied, suggesting that BC and PAHs preserved in the sediments are derived from different sources and controlled by different biogeochemical processes. Our study suggests that the abundance of BC preserved in the sediments could represent a significant sink pool of carbon cycling in China's marginal seas.

One century record of contamination by polycyclic aromatic hydrocarbons and polychlorinated biphenyls in core sediments from the southern Yellow Sea

Sixteen polycyclic aromatic hydrocarbons (PAHs) and 28 polychlorinated biphenyls (PCBs) were measured at a 2-cm interval in a core sample from the middle of the southern Yellow Sea for elucidating their historical variations in inflow and sources. The chronology was obtained using the Pb-210 method. PAHs concentrations decreased generally with depth and two climax values occurred in 14-16 cm and 20-22 cm layers, demonstrating that the production and usage of PAHs might reach peaks in the periods of 1956-1962 and 1938-1944. The booming economy and the navy battles of the Second World War might explain why the higher levels were detected in the two layers. The result of principal component analysis (PCA) revealed that PAHs were primarily owing to the combustion product. Down-cored variation of PCB concentrations was complex. Higher concentrations besides the two peaks being the same as PAHs were detected from 4 to 8 cm, depositing from 1980 to 1992, which probably resulted from the disposal of the out-dated PCB-containing equipment. The average Cl percentage of PCBs detected was similar to that of the mixture of Aroclor 1254 and 1242, suggesting they might origin from the dielectrical and heat-transfer fluid. The total organic carbon (TOC) content played a prevalent role in the adsorption of high molecular weight PAHs (>= 4-ring), while no obvious relationship among total PCBs, the concentration of congeners, and TOC was found.

Production of light olefins and aromatic hydrocarbons through catalytic cracking of naphtha at lowered temperature

Naphtha catalytic cracking were carried out at 650 degrees C over modified ZSM-5. Light olefins and BTX could be obtained over the catalysts. The products showed variable distribution with different catalyst modification. Some modification, such as Fe, Cu and La favored the BTX generation and P and Mg modification favored the light olefins production. In N-2 stream cracking catalyzed by LaZSM-5, more than 50% naphtha feed were converted to BTX, while in steam cracking, with an improved modified catalyst, P, La/ZSM-5, naphtha can be converted to light olefins with high activity and long-term stability.

渤海湾海岸带表层沉积物中黑炭和多环芳烃的分布特征

黑碳（BC）是生物质和化石燃料不完全燃烧产生的高度聚合的碳质混合物，包括木炭 （char/charcoal）和烟炱碳（soot）等形式。黑碳产生后大部分储存在燃烧原地，而烟炱碳 由于粒径较小，易进入大气，滞留一到数周后回到地表。部分土壤黑碳随河流和大气的搬 运作用进入海洋环境，主要汇集在海岸带沉积物中。由于黑碳涉及到气候变化、碳循环、 环境危害、人体健康等诸多问题而成为当前气候与环境领域的研究热点。黑碳在环境介质 中比较稳定，因而可以较好的指示人类能源使用及其对环境质量的影响；同时黑碳具有很 强的吸附性，能显著影响周围介质中持久性有机污染物(如多环芳烃等)的赋存状态和生态 毒理效应。 多环芳烃（PAHs）是指两个或两个以上的苯环以稠环形式结合的芳香族化合物，主要 来源于含碳物质的不完全燃烧过程，在环境中广泛存在。由于PAHs 具有潜在的致癌性、 致畸性和致突变性（“三致”效应）而在环境研究领域中备受关注。另外由于具有主体的 同源性，PAHs 可以指示BC 的来源和环境过程。 海岸带沉积物是包括BC 和PAHs 在内的众多污染物在环境地球化学迁移过程中的主 要载体和归宿，由于受到陆地和海洋双重作用，海岸带对环境污染物尤其敏感。环渤海地 区是我国北方的社会经济中心，工业、农业和交通发达、人口稠密，污染严重。前人的研 究表明渤海湾的BC 和PAHs 污染程度明显高于我国其他海岸带，但受限制于采样区域和 样品数量，不能全面地反应BC 和PAHs 在渤海湾海岸带的分布状况及人类活动对海岸带 环境质量的影响。 本次研究在渤海湾海岸带潮间带、近海及主要入海河流系统布设了多条采样剖面，采 集表层沉积物样品85 个。首先，对国际上较为常用的化学热氧化法（CTO-375）处理沉积 物黑碳样品的方法进行了比对实验和优化，然后对全部样品进行黑碳分析；利用GC-MS 方法对样品中的PAHs（USEPA 的16 种优控物）进行了定量检测；对全部沉积物样品还进 行了粒度分析。 结果表明，该区域内黑碳的含量为0.09 到22.8 mg/g dw，其中，潮间带样品的BC 平 均含量为0.52 ± 0.39 mg/g dw，近海样品为0.84 ± 0.38 mg/g dw，河流样品（海河样品除外） 为1.88 ± 0.89 mg/g dw。BC占总有机碳的比例在潮间带、近海、河流区域分别为18.4 ± 8.3%、 14.5 ± 5.3%、14.2 ± 4.1%。潮间带黑碳存在明显的“北高南低”的趋势（以天津港码头和 海河为界），与近海和河流样品的BC 浓度有相似的变化趋势，反映了BC 在海岸带的运移 扩散具有一定的继承性；河流输入可能是近岸沉积物BC 的主要来源。同时，潮间带沉积 物粒度分析结果表明“北区细”(以粘土质粉砂主)而“南区粗”(以砂为主)，反映了两个区 域不同的水动力条件和沉积环境，可能是造成BC 浓度空间分异的主要原因。 摘要 II 多环芳烃的含量分布为33.1-7658.7 ng/g dw，其中，潮间带样品的PAHs 平均含量为 147.0 ng/g dw，近海样品为170.9 ng/g dw，河流样品（海河样品除外）为1228.5 ng/g dw。 主要成分均为三环和四环多环芳烃。PAHs 也呈现出了与BC 相似的“北高南低”的趋势， 多环芳烃与黑碳的相关性研究表明两者相关性较好（R2=0.59），表明多环芳烃和黑碳的同 源性和继承性。运用比值法（菲/蒽，荧蒽/芘，低环/高环等）对多环芳烃的来源解析显示， 整个研究区域内多环芳烃主要为燃烧源。