首页> 外文会议>Asian conference on remote sensing;ACRS >VERTICAL VARIATION CHARACTERISTICS OF PETROLEUM CONCENTRATION AND BACKSCATTER COEFFICIENT IN PETROLEUM-POLLUTED WATER BODY
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VERTICAL VARIATION CHARACTERISTICS OF PETROLEUM CONCENTRATION AND BACKSCATTER COEFFICIENT IN PETROLEUM-POLLUTED WATER BODY

机译:石油污染水体中石油浓度和背散射系数的垂直变化特征

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August 25th to 27th, 2018, in-situ data which was used to analyze the vertical variations characteristics of petroleum concentration and backscattering coefficient, was collected at Dalian port which is located in Liaoning province, China. The analytical results of these data drew three conclusions. First of all, the regime of vertical variation of petroleum concentration is complicated, and the concentration does not decrease or increase gradually with depth increasing, due to the fact that ebb and flow of different time and stations could influence current in different way. Secondly, the minimum and second minimum of backscattering coefficient of each station are at 700nm and 590nm respectively. By the way, magnitude of backscattering coefficient is similar at 420nm, 442nm, 470nm and 5!0nm, and backscattering coefficients of these stations vary with depth consistently. Finally, there are three kinds of vertical variations of total backscattering coefficient in this study area, they are abrupt growth, steady growth and single hump. Abrupt growth backscattering coefficient varies less in the water column but growth quickly near 11.5m below the sea surface. Steady growth backscattering coefficient growth gradually with depth increasing. While single hump backscattering coefficient still has three subtypes: peak value at sea surface, peak value at middle-level of water column and peak value at bottom of water column. The maximum of backscattering coefficient of peak value at sea surface type lie in 0.5~2.5m below the sea surface, and the maximum of backscattering coefficient of peak value at middle-level of water column is located in 7~10m below the sea surface, and the maximum of backscattering coefficient of peak value at bottom of water column always occurs in the region of 10~12.5m.
机译:2018年8月25日至27日,在中国辽宁省大连港收集了用于分析石油浓度和后向散射系数的垂直变化特征的现场数据。这些数据的分析结果得出了三个结论。首先,石油浓度的垂直变化机制很复杂,浓度不会随着深度的增加而逐渐降低或逐渐增加,这是由于不同时间和站台的潮汐和潮汐会以不同的方式影响洋流的事实。其次,每个站点的反向散射系数的最小值和第二最小值分别为700nm和590nm。顺便说一下,后向散射系数的大小在420nm,442nm,470nm和5!0nm处相似,并且这些测站的后向散射系数随深度而一致地变化。最后,该研究区域总后向散射系数存在三种垂直变化,即突然增长,稳定增长和单一驼峰。水柱中突然的生长后向散射系数变化较小,但在海面以下11.5m附近生长迅速。随着深度的增加,稳定增长的后向散射系数逐渐增长。尽管单个驼峰背向散射系数仍具有三个子类型:海面的峰值,水柱中层的峰值和水柱底部的峰值。海面型峰值的后向散射系数最大值在海面以下0.5〜2.5m,水柱中层的峰值后向散射系数最大值在海面以下7〜10m,水柱底部峰值的后向散射系数最大值始终出现在10〜12.5m范围内。

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