有和无源输入时海水湾物质含量水平损失率模型

Dongfang Yang, Sixi Zhu, Bailing Fan, C. Su, Xiuqin Yang
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摘要

以1981年8月胶州湾地表水中铬(Cr)为例,建立了有源输入和无源输入的海湾物质含量水平损失率模型。结果表明,在源输入情况下,Cr的水平损失率分别为10.99 ~ 36.00 YDFa和11.94 ~ 19.45 YDFr。无源输入时,Cr的水平损失率分别为YDFa和0.00 ~ 1.30 YDFr。如果有源输入,则绝对量和相对量都较高,导致Cr从地表水快速沉降到底水,水体中Cr含量的状态趋于恢复到无源输入的水平。在无源输入的情况下,绝对量和相对量均较低,导致Cr从地表水向底水体沉降较少,水体中Cr含量的状态趋于保持在无源输入的水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Horizontal Loss Rate Modeling on Matter Content in Marine Bay with and without Source Input
Taking chromium (Cr) in surface waters in Jiaozhou Bay in August 1981 as an example, this paper provided Horizontal loss rate modeling on matter content in marine bay with and without source input. Results showed that in the case of source input, the horizontal loss rate of Cr was 10.99-36.00 YDFa and 11.94-19.45 YDFr. In the case of no source input, the horizontal loss rate of Cr was YDFa and 0.00-1.30 YDFr. If there was source input, both Absolute Amount and Relative Amount were relative high, resulting in rapid settlement of Cr from surface waters to bottom waters, and the status of Cr contents in waters were tending to be returning to levels without source input. If there was no source input, both Absolute Amount and Relative Amount were relative low, resulting in little settlement of Cr from surface waters to bottom waters, and the status of Cr contents in waters were tending to be keeping to levels without source input.
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