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Dissolved Hydrocarbons and Related Microflora in a Fjordal Seaport: Sources Sinks Concentrations and Kinetics

机译:峡湾海港中溶解的碳氢化合物及相关微生物区系:来源汇浓度和动力学

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摘要

The continuous addition of toluene as a solute of treated ballast water from oil tankers into a well-defined estuary facilitated the study of the dynamics of dissolved hydrocarbon metabolism in seawater. Most rates of toluene oxidation were in the range of 1 to 30 pg/liter per h at 0.5 μg of toluene per liter. Near the ballast water injection point, a layer of warm ballast water, rich in bacteria, that was trapped below the less-dense fresh surface water was located. Toluene residence times were approximately 2 weeks in this layer, 2 years elsewhere in Port Valdez, and 2 decades in the surface water of a more oceanic receiving estuary adjacent. Mixing was adequate for a steady-state treatment which showed that 98% of the toluene was flushed from Port Valdez before metabolism and gave a steady-state concentration of 0.18 μg/liter. Total bacterial biomass from direct counts and organism size data was usually near 0.1 mg/liter, but ranged up to 0.8 mg/liter in the bacteria-rich layer. The origin of bacteria in this layer was traced to growth in oil tanker ballast during shipments. The biomass of toluene oxidizers in water samples was estimated from the average affinity of pure-culture isolates for toluene (28 liters per g of cells per h) and observed toluene oxidation kinetics. Values ranged from nearly all of the total bacterial biomass within the bacteria-rich layer down to 0.2% at points far removed. Because the population of toluene oxidizers was large with respect to the amount of toluene consumed and because water from a nearby nonpolluted estuary was equally active in facilitating toluene metabolism, we searched for an additional hydrocarbon source. It was found that terpenes could be washed from spruce trees by simulated rainfall, which suggested that riparian conifers provide an additional and significant hydrocarbon source to seawater.
机译:将来自油轮的经处理压载水的甲苯作为溶质连续添加到定义明确的河口中,有助于研究海水中溶解的碳氢化合物代谢的动力学。在每升甲苯0.5微克的情况下,大多数甲苯氧化速率在1至30 pg /升/小时的范围内。在压载水注入点附近,找到了一层富含细菌的温暖压载水,该压载水被困在密度较小的新鲜地表水下面。甲苯在该层的停留时间约为2周,在Valdez港的其他地方为2年,而在更靠近海洋的入海口附近的地表水中则为2年。混合足以进行稳态处理,表明代谢前98%的甲苯从Valdez港被冲出,稳态浓度为0.18μg/ L。直接计数和生物体大小数据得出的细菌总生物量通常接近0.1 mg / L,但在细菌丰富的层中最高为0.8 mg / L。在运输过程中,该层细菌的起源可追溯到油轮压载物的生长。根据纯培养物分离物对甲苯的平均亲和力(每克细胞每小时28升)和观察到的甲苯氧化动力学来估算水样品中甲苯氧化剂的生物量。其值的范围从细菌富集层中几乎所有细菌生物量的总和,到远离的点降低到0.2%。由于相对于消耗的甲苯量来说,甲苯氧化剂的数量很大,并且由于附近无污染河口的水在促进甲苯代谢方面同样活跃,因此我们寻求了另一种烃源。研究发现,可以通过模拟降雨从云杉树上洗掉萜烯,这表明河岸针叶树为海水提供了额外的重要碳氢化合物来源。

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