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首页> 外文期刊>Frontiers in Marine Science >Microbial, Physical, and Chemical Changes in Galveston Bay Following an Extreme Flooding Event, Hurricane Harvey
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Microbial, Physical, and Chemical Changes in Galveston Bay Following an Extreme Flooding Event, Hurricane Harvey

机译:在极端洪水活动之后,加尔维斯顿湾的微生物,物理和化学变化,飓风哈维

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Hurricane Harvey (category 4 storm) made landfall along the coast of Texas (USA) and then stalled out over Texas and Louisiana, releasing 1.29 x 1011 m3 of precipitation over 5 days. This caused extensive flooding that elevated freshwater river discharge and land runoff into Galveston Bay and eventually into the Gulf of Mexico. The floodwaters delivered a significant influx of terrigenous dissolved organic matter, organic pollutants and nutrients along with terrestrial and freshwater associated microbes. Over the 24 days following the flooding event, samples were collected on five cruises across Galveston Bay from the mouth of the San Jacinto River (Houston, TX) to the Gulf of Mexico. Parameters measured for this study include: water quality (temperature, salinity, pH and dissolved oxygen), nutrients (NO3-, NO2-, NH4+, Pi, and HSiO3-), polycyclic aromatic hydrocarbons, pharmaceuticals (cotinine, carbamazepine, carbamazepine-epoxide, and prednisone), biocide (imidacloprid), dissolved organic carbon, lignin phenols, bacteria and the eukaryotic community (16S and 18S rRNA genes). In the week after the flood event, bay-wide salinities decreased to 0-5 compared to the higher pre-Harvey salinities of 20-30 (recorded 5 days before the flood). Water treatment facilities and petrochemical plants were compromised due to the heavy flooding in the region. This led to increased concentrations of nutrients, polycyclic aromatic hydrocarbons, pharmaceuticals and biocides across Galveston Bay immediately following the storm. In the 4 weeks following the storm, concentrations of nutrients and organic pollutants began to decrease coinciding with rising salinities as the freshwater was flushed into the Gulf of Mexico and seawater began moving back into the Bay. Successive blooms of chlorophytes, diatoms, and dinoflagellates occurred similar to post-storm communities from past hurricanes that have impacted estuarine systems along the Gulf of Mexico. The eukaryotic community changed substantially following Harvey and did not recover to pre-Harvey conditions during our study period, suggesting a longer recovery time compared to the prokaryotes. Although the water quality parameters and microbial community showed signs of returning to pre-Harvey conditions within the month following the flood event, long-term impacts need to be measured in the years following the flood.
机译:Hurricane Harvey(4类风暴)沿着德克萨斯州(美国)的海岸大跌,然后在德克萨斯州和路易斯安那州停滞不前,在5天内释放1.29 x 1011 m3。这造成了广泛的洪水,将淡水河流排放和土地径流升高到加尔维斯顿湾,最终进入墨西哥湾。洪水进入陆地和淡水相关微生物的陆地溶解有机物,有机污染物和营养素的显着涌入。在洪水事件发生后的24天,在加尔维斯顿湾(休斯顿,德克萨斯州)到墨西哥湾的加尔维斯顿湾的五个游轮上收集了样品。本研究测量的参数包括:水质(温度,盐度,pH和溶解氧),营养素(NO3-,NO2-,NH4 +,PI和HSIO3-),药物芳烃,药物(Cotinine,CoTinine,Carbamazepine,Carbamazepine-环氧化)和泼尼松),杀生物剂(吡虫啉),溶解有机碳,木质素酚,细菌和真核群(16s和18s rRNA基因)。在洪水事件后的一周内,与20-30的更高的哈维盐度相比,贝多湾盐度降至0-5(在洪水前5天记录)。由于该地区的大量洪水,水处理设施和石化植物受到损害。这导致在暴风雨之后立即在加尔维斯顿湾的营养成分,多环芳烃,药物和生物剂的浓度增加。在暴风雨之后的4周内,营养成分和有机污染物的浓度开始随着盐水上升而重合,因为淡水冲洗到墨西哥湾和海水开始进入海湾。叶绿素,硅藻和Dinoflagelles的连续绽放类似于来自过去飓风的暴风雨群落,这些飓风沿着墨西哥湾的河口系统受到影响。真核群落大幅改变了哈维,在我们的研究期间没有恢复到哈维先前的条件,这表明与原核生物相比更长的恢复时间。虽然水质参数和微生物群落显示出在洪水事件之后的月份返回前哈维条件的迹象,但在洪水之后的几年需要衡量长期影响。

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