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Mutual Transformation between Vertical Sediment Amount and Vertical Diluted Amount

机译:垂直沉积物量与垂直稀释量之间的相互转换

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Based on the investigation data of Hg in Jiaozhou Bay in May, August and October of 1992, the horizontal loss amount, vertical diluted amount and vertical sediment amount of Hg in both surface and bottom layers were calculated and the block diagram model of Hg level and vertical change was determined by using change model of horizontal and vertical substance content that proposed by the author. The results showed that in May, August and October, the absolutely horizontal loss amount of Hg in the surface layer and bottom layer ranged from 0.004 to 0.029 μg/L, and the horizontally relative loss amount of Hg in the surface layer and bottom layer ranged from 16.00 to 72.50%. The Hg content in both the surface and bottom layer had an absolutely vertical diluted amount of 0.000-0.033 μg/L and a relatively vertical diluted amount of 0.00-82.50%. The absolutely vertical sediment amount of Hg in both the surface and bottom layer were 0.002-0.007 μg/L, and the relatively vertical sediment amount was 15.38-38.88%.The variation of horizontal loss amount revealed that in May, August and October, in the southeast of the bay or in the center of the Bay, whether the Hg content is provided by sources or not will result in relatively high horizontal loss amount of the surface layer. In May and August, there was no source of Hg in the center of the bay. No matter in the southeast of the Bay, the loss of Hg in the bottom layer was relatively low. In October, in the southeast of the bay or in the center of the Bay, there was no source of Hg content, but the loss of Hg content in the bottom layer was relatively high. The change of vertical loss amounts revealed that: in different waters, with the change of time, the vertical sediment amounts and vertical diluted amounts of Hg content in surface and bottom layer were mutually transformed.
机译:根据1992年5月,8月和10月胶州湾汞的调查资料,计算了表层和底层Hg的水平损失量,垂直稀释量和垂直沉降量,并建立了Hg和Hg的框图模型。通过使用作者提出的水平和垂直物质含量的变化模型确定垂直变化。结果表明,在5,8,10月份,表层和底层的汞绝对水平损失量为0.004〜0.029μg/ L,表层和底层的汞水平相对损失量为0.004〜0.029μg/ L。从16.00到72.50%。表面层和底层中的Hg含量具有0.000-0.033μg/ L的绝对垂直稀释量和0.00-82.50%的相对垂直稀释量。表层和底层的Hg绝对垂直沉积量均为0.002-0.007μg/ L,相对垂直沉积量为15.38-38.88%。水平损失量的变化表明,5月,8月和10月,在海湾的东南部或在海湾的中心,汞含量是否由来源提供,都会导致表层的水平损失较高。在五月和八月,海湾中心没有汞源。无论在海湾的东南部,底层的汞损失都相对较低。 10月,在海湾的东南部或海湾的中心,没有汞含量的来源,但底层的汞含量损失相对较高。垂直损失量的变化表明:在不同的水域中,随着时间的变化,表层和底层中汞的垂直沉积物量和垂直稀释量相互转化。

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