首页> 外文期刊>Texas Journal of Science >TRENDS IN WATER AND SEDIMENT QUALITY FOR THE HOUSTON SHIP CHANNEL
【24h】

TRENDS IN WATER AND SEDIMENT QUALITY FOR THE HOUSTON SHIP CHANNEL

机译:休斯顿船舶通道的水和泥沙质量趋势

获取原文
获取原文并翻译 | 示例
           

摘要

Ambient monitoring data collected by the Texas Natural Resource Conservation Commission from 1971 through 1991 were assessed for five stations located on the Houston Ship Channel mainstem (Turning Basin, Greens Bayou, San Jacinto Monument, Channel Marker 120 and Morgans Point). Water quality was most impacted in the upper channel, especially at the Turning Basin, improving downstream of the San Jacinto River confluence. This is consistent with the more confined physical characteristics and the high degree of point and non-point source pollutant loading in the upper channel. Water quality has improved over the last couple of decades as demonstrated by declining trends for total organic carbon, total suspended solids, fecal coliforms, ammonia nitrogen, ortho-phosphate, total phosphate, total arsenic and total copper. Increases in nitrate nitrogen, over time were found at all sites. Declining trends for total cadmium, mercury, nickel and zinc were found for the upper (industrialized) portion of the channel only. Other findings for total metals indicated site-specific differences for silver, possible increasing trends for selenium and no trends for chromium. Increasing dissolved oxygen and decreasing biochemical oxygen demand and Kjeldahl nitrogen concentrations were evident at the upstream stations but, unexpectedly, trends reversed further downstream. Concentrations of heavy metals and PCBs in bottom sediment were greatest in the Turning Basin and dropped progressively downstream. Levels of arsenic, cadmium, lead and zinc in Turning Basin sediments decreased significantly over time. Improving water and sediment quality has enhanced utilization of the Ship Channel system by aquatic life.
机译:评估了得克萨斯州自然资源保护委员会从1971年至1991年收集的环境监测数据,该数据位于休斯敦船舶航道主干上(转向盆地,格林斯巴约,圣哈辛托纪念碑,120号航道和Morgans Point)。水质在上游水道受到的影响最大,特别是在转向盆地,这改善了圣哈辛托河汇合处的下游。这与更有限的物理特性以及上游通道中点和非点源污染物的高度负载相一致。在过去的几十年中,总有机碳,总悬浮固体,粪便大肠菌群,氨氮,正磷酸盐,总磷酸盐,总砷和总铜的下降趋势表明,水质得到了改善。随着时间的推移,在所有地点发现硝酸盐氮的增加。仅在通道的上部(工业化)部分发现了总镉,汞,镍和锌的下降趋势。总金属的其他发现表明银的位点特异性差异,硒的可能趋势增加而铬没有趋势。上游站明显增加了溶解氧,降低了生化需氧量和凯氏氮浓度,但出乎意料的是,趋势在下游进一步逆转。转向盆地底部沉积物中重金属和PCBs的浓度最大,而下游则逐渐下降。随着时间的推移,转向盆地沉积物中的砷,镉,铅和锌的含量显着下降。水和沉积物质量的提高通过水生生物提高了船舶航道系统的利用率。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号