Spatial-Temporal Regularities of Hydrooptical Characteristics of the Ob River

O. Akulova, V. Bukaty, V.V. Kirillov
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Abstract

Field studies conducted in spring (March 26 — April 9, 2022) and summer (June 5-16, 2022) in the Ob River mouth region at the three hydromorphological stations „Kazym-Mys“, „Azovy“, and „Salemal“ (YaNAO) to obtain new data on the hydrooptical characteristics of water in the Lower Ob river. Also, the trophic status and ecological state of the Lower Ob river region were assessed. The greatly varying light attenuation coefficient ε(λ) was calculated at the four characteristic wavelengths of 430, 450, 550, and 670 nm, respectively. It ranges from 9.3 m-1 to 22.1 m-1 during the winter low water (freeze-up) period and from 7.3 m-1 to 33.0 m-1 during the open water (high water) period. The calculated relative spectral contributions of major optically active components of water (pure water, suspension, yellow substance, chlorophyll) to ε(λ) suggest that suspension and yellow substance make up the maximal contribution at different horizons. Additionally, the calculated coefficient of light absorption by yellow substance кys(λ) varies within the ranges from 5.5 m-1 to 9.9 m-1 (spring) and from 3.1 m-1 to 17.0 m-1 (summer), respectively. The relative transparency was measured using the Secchi disc. The concentrations of yellow substance and major photosynthetic pigments — chlorophylls a, b, c, and carotenoids — were estimated alongside. The obtained results could be useful for environmental monitoring and predicting the dynamics of aquatic ecosystems in the region under climate change and increased anthropogenic pressure caused by the use of natural resources.
奥布河水光特征的时空规律性
春季(2022 年 3 月 26 日至 4 月 9 日)和夏季(2022 年 6 月 5 日至 16 日)在鄂毕河河口地区的三个水文站 "Kazym-Mys"、"Azovy "和 "Salemal"(YaNAO)进行了实地考察,以获得有关鄂毕河下游水文光学特征的新数据。此外,还对鄂毕河下游地区的营养状态和生态状况进行了评估。在波长分别为 430、450、550 和 670 纳米的四个特征波段上,计算了变化很大的光衰减系数 ε(λ)。在冬季枯水期(结冰期),该系数介于 9.3 m-1 至 22.1 m-1 之间;在开阔水域(丰水期),该系数介于 7.3 m-1 至 33.0 m-1 之间。计算得出的水中主要光学活性成分(纯水、悬浮物、黄色物质、叶绿素)对ε(λ)的相对光谱贡献表明,悬浮物和黄色物质在不同地层的贡献最大。此外,计算得出的黄色物质光吸收系数 кys(λ) 分别在 5.5 m-1 至 9.9 m-1 (春季)和 3.1 m-1 至 17.0 m-1 (夏季)范围内变化。相对透明度是用 Secchi 圆盘测量的。同时还估算了黄色物质和主要光合色素(叶绿素 a、b、c 和类胡萝卜素)的浓度。所获得的结果可用于环境监测和预测该地区水生生态系统在气候变化和使用自然资源造成的人为压力增加情况下的动态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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