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Depth-related influences on biodegradation rates of phenanthrene in polluted marine sediments of Puget Sound, WA

机译:深度对华盛顿州普吉特海湾污染海洋沉积物中菲生物降解速率的影响

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A whole-core injection method was used to determine depth-related rates of microbial mineralization of ~(14)C-phenanthrene added to both contaminated and clean marine sediments of Puget Sound, WA. For 26-day incubations under micro-aerobic conditions, conversions of ~(14)C-phenanthrene to ~(14)CO_2 in heavily PAH-contaminated sediments from two sites in Eagle Harbor were much higher (up to 30%) than those in clean sediments from nearby Blakely Harbor (< 3%). The averaged ~(14)C-phenanthrene degradation rates in the surface sediment horizons (0-3 cm) were more rapid (2-3 times) than in the deeper sediment horizons examined (> 6 cm), especially in the most PAH polluted EH9 site. Differences in mineralization were associated with properties of the sediments as a function of sediment depth, including grain-size distribution, PAH concentration, total organic matter and total bacterial abundance. When strictly anaerobic incubations (in N_2/H_2/CO_2 atmosphere) were used, the phenanthrene biodegradationVates at all sediment depths were two times slower than under micro-aerobic conditions, with methanogenesis observed after 24 days. The main rate-limiting factor for phenanthrene degradation under anaerobic conditions appeared to be the availability of suitable electron acceptors. Addition of calcium sulfate enhanced the first order rate coefficient (k_1 increased from 0.003 to 0.006 day~(-1)), whereas addition of soluble nitrate, even at very low concentration (< 0.5 mM), inhibited mineralization. Long-term storage of heavily polluted Eagle Harbor sediment as intact cores under micro-aerobic conditions also appeared to enhance anaerobic biodegradation rates (k_1 up to 0.11 day~(-1)).
机译:全芯注入方法用于确定与华盛顿州普吉特海湾污染和清洁的海洋沉积物中添加的〜(14)C菲的微生物矿化深度相关的速率。在微需氧条件下温育26天,来自鹰港两个地点的受PAH严重污染的沉积物中〜(14)C菲到〜(14)CO_2的转化率要比转化率高得多(高达30%)。清洁附近布雷克利港的沉积物(<3%)。表层沉积物层(0-3 cm)中的平均〜(14)C菲降解速率比所研究的较深沉积物层(> 6 cm)更快(2-3倍),尤其是在污染最严重的PAH中EH9网站。矿化作用的差异与沉积物的性质有关,后者是沉积物深度的函数,包括粒度分布,PAH浓度,总有机质和总细菌丰度。当使用严格的厌氧培养(在N_2 / H_2 / CO_2气氛中)时,在所有沉积深度处的菲生物降解速率都比微需氧条件下慢两倍,并且在24天后观察到甲烷化作用。厌氧条件下菲降解的主要限速因素似乎是合适的电子受体的可用性。硫酸钙的添加提高了一级速率系数(k_1从0.003天增加到0.006天〜(-1)),而可溶性硝酸盐的添加,即使浓度很低(<0.5 mM),也抑制了矿化作用。在微好氧条件下,长期储存污染严重的鹰港沉积物作为完整岩心,似乎也提高了厌氧生物降解率(k_1高达0.11天〜(-1))。

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