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Origin of the Suspended Particles with High Turbidity Area in Murasaki River Estuary

机译:村崎河口高浊度区悬浮颗粒物的起源

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摘要

To identify the cause of the high turbidity of the Murasaki River estuary, we investigated variations in suspended particle (SS) concentration and SS composition during the tide cycle in the Murasaki River estuary in June 2001 (rainy season) and September 2001 (nonrainy season). Additionally, the stable isotope ratio of carbon and nitrogen in the sediment and SS concentration and chemical composition were determined in the Murasaki River watershed over the investigation period.In September, the turbidity and SS concentration were high in the bottom layer. The SS compositions in the surface and middle layers depended on the tide phase, although in the bottom layer, SS composition did not depend on the tide phase. Moreover, the average SS composition in the bottom layer showed relatively low particulate organic carbon (POC) and chlorophyll a (Chl a) contents and high C/N and C/Chl a ratios, and the sinking particle compositions was similar to the SS composition in the bottom layer. This suggests that the origin of SSs in the bottom layer differed from those in the surface and middle layers, and the resuspension of sediment was a significant source of SSs during the nonrainy season. In June, the variation in SS composition in the surface layer did not correlate with tide level, and the average SS composition was similar to that in the river. This finding suggests that surface layer SSs were predominantly river-borne SSs.Sediments in the upper and middle reaches had a high δ 15N (+4.5‰∼+5.2‰) because of artificial pollution (small reservoir, agriculture effluent and human sewage). However, the δ 13C and δ 15N contents of the sediment in the Murasaki river estuary suggest that terrestrial C3 plants were the main source of organic matter in the sediment (δ 13C=-25.8‰, δ 15N=+2.9‰). Additionally, the δ 13C and δ 15N of sinking particles in the Murasaki river estuary suggest that the contribution of particles from the forest was higher in June (δ 13C=-25.2‰, δ 15N=+3.2‰) than in September (δ 13C=-24.4‰, δ 15N=+3.9‰). This suggests that the load from the forest brought when a storm was the main source of the organic matter in the the Murasaki River estuary sediments, and that the high turbidity of the Murasaki River estuary was caused by the resuspension of the sediment originating from the forest.
机译:为了确定村崎河河口高浊度的原因,我们调查了村崎河河口在2001年6月(雨季)和2001年9月(非雨季)的潮汐周期中悬浮颗粒(SS)浓度和SS组成的变化。 。此外,在调查期间确定了村崎河流域沉积物中碳氮的稳定同位素比以及SS浓度和化学成分.9月,底层的浊度和SS浓度较高。表面层和中间层的SS组成取决于潮汐相,尽管在底层,SS组成不取决于潮汐相。此外,底层的平均SS组成显示出相对较低的颗粒有机碳(POC)和叶绿素a(Chl a)含量,以及较高的C / N和C / Chl a比值,并且沉降颗粒组成与SS组成相似在底层。这表明底层SSs的来源与表层和中间层的SSs有所不同,在非雨季,沉积物的重新悬浮是SSs的重要来源。 6月,表层SS组成的变化与潮汐水平无关,平均SS组成与河流中的相似。这一发现表明表层SSs主要是河道SSs。由于人工污染(小水库,农业废水和人类污水),上游和中游的沉积物具有较高的δ15N(+ 4.5‰〜+ 5.2‰)。然而,村崎河口沉积物的δ13C和δ15N含量表明,陆地C3植物是沉积物中有机物的主要来源(δ13C = -25.8‰,δ15N = + 2.9‰)。另外,村崎河河口下沉颗粒的δ13C和δ15N表明,6月(δ13C = -25.2‰,δ15N = + 3.2‰)中森林颗粒的贡献高于9月(δ13C)。 = -24.4‰,δ15N = + 3.9‰)。这表明,暴风雨是村崎河河口沉积物中有机物的主要来源所带来的森林负荷,而村崎河河口的高浊度是由于森林中沉积物的重新悬浮造成的。 。

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