游渡河河口有机质来源及分解

Kaho Watanabe, S. Kobayashi, Masaki Fuchi, S. Asaoka, M. Hayashi
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引用次数: 0

摘要

日本大阪湾内部受富营养化影响,海湾西部受少营养化影响。本研究通过对大阪湾河口地区有机氮(orgn)的分布、来源和分解速率进行研究,以阐明海湾中营养物质分布不均匀的原因。大阪湾河口地区定义为从Yodo河口到海湾头的区域。河口地区的有机物氮浓度远高于淡水地区或海湾本身。颗粒有机氮占有机氮的74±11%,可能下沉到底部。溶解有机氮在100天内的分解率为29±4%,可能以低盐度的水供应给海洋。这些关于大阪湾河口地区有机物分解速率的结果可能提高陆地源养分负荷对海湾营养状况影响模型的准确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Source and Decomposition of Organic Matter in the Estuary of Yodo River
The inner part of Osaka Bay in Japan is affected by eutrophication, and the western part of the bay is affected by oligotrophic conditions. In this study, the distribution, sources, and decomposition rate of organic nitrogen ( Org-N ) in the estuarine region of Osaka Bay, defined as the region from the mouth of the Yodo River to the bay head, were studied to elucidate the cause of this uneven distribution of nutrients in the bay. Concentrations of Org-N are much higher in the estuary region than in freshwater areas or in the bay itself. Particulate organic nitrogen, which potentially sinks toward the bottom, accounted for 74 ± 11% of Org-N. The decomposition rate of dissolved organic nitrogen over 100 days, which is potentially supplied to the sea with low-salinity water, was 29 ± 4%. These results regarding the decomposition rate of organic matter in the estuarine region of Osaka Bay may improve the accuracy of models of the impact of land-sourced nutrient load on nutrient conditions in the bay.
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