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Analysis of COD Transport in Qinhuangdao Coastal Waters

机译:秦皇岛沿海水域化学需氧量迁移分析

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The transport of pollutant is an important topic for self-purificationcapability and environment evaluation of ocean. Chemical oxygendemand (COD, determined by potassium permanganate) is selected as akey parameter to indicate the water pollution degree. This studyemploys field measurements and numerical model of water quality toresearch the characteristic of COD transport in Qinhuangdao coastalwaters. To investigate the seasonal distributions of COD, the fieldmonitoring of water quality at 46 sampling points was implemented inthe dry season (April) and the flood season (August) in 2013. Thecoastal waters were with a relative higher average COD concentrationof 1.43 mg/L in the flood season for the large amount of terrestrialCOD inputs, compared with the average COD concentration of 1.08mg/L in the dry season. The simulation of COD transport inQinhuangdao coastal waters in the flood season demonstrates that CODtransport is jointly controlled by the reverse tidal current in SW-NEdirections and the discharges of rivers. For the estuary with smallerriver discharge, COD transport in the coastal waters is drivendominantly by tidal current. The comparison of COD transport scope inthe spring and neap tides indicates that the river input COD wastransported farther due to low mixing in neap tide period. The newlybuiltartificial island near the coastal line hinders the nearshore waterexchange, resulting in the deterioration of water quality in the estuaryand around the island. For the estuary with large river discharge, CODtransport in the estuarine water is greatly influenced by river discharge,for example, there was little change of COD distribution at the estuaryof Luanhe River during the spring and neap tides in the same riverdischarge.
机译:污染物的运输是自净的重要课题 海洋能力和环境评估。化学氧气 需求量(COD,由高锰酸钾确定)被选为 指示水污染程度的关键参数。这项研究 利用现场测量和水质数值模型来 研究秦皇岛沿海COD的运输特征 水域。为了调查化学需氧量的季节性分布,该领域 在46个采样点对水质进行了监测 2013年的旱季(4月)和汛期(8月)。 沿海水域的平均化学需氧量浓度相对较高 大量陆生水灾,洪水季节的水含量为1.43 mg / L 化学需氧量输入,而平均化学需氧量浓度为1.08 在干燥季节为mg / L。水中COD运移的模拟。 汛期秦皇岛沿海水域表明化学需氧量 SW-NE中的逆潮流共同控制运输 方向和河流的排放。对于较小的河口 河流排放,沿海水域的化学需氧量运输受到驱动 主要由潮流引起。 COD运输范围的比较。 春季和春季潮汐表明河流输入的COD为 在潮汐期低混合,使运输更远。新建的 沿海岸线附近的人工岛阻碍了近岸水域的发展 交换,导致河口水质恶化 和周围的岛屿。对于河流量大的河口,化学需氧量 河口水的运输受到河流排放的极大影响, 例如,河口的化学需氧量分布几乎没有变化 春的River河水位和同一条河的潮汐 释放。

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