کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5765321 1626611 2017 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
A study of in-situ sediment flocculation in the turbidity maxima of the Yangtze Estuary
ترجمه فارسی عنوان
مطالعه فلوکولاسیون رسوبات در ناحیه ای در حداکثر آبشستگی رودخانه یانگ تسه
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
چکیده انگلیسی


- In-situ floc properties are examined in the turbidity maxima of the Yangtze Estuary.
- Flocculation exhibits strong temporal and vertical variations over a tidal cycle.
- Turbulence exerts major control on flocculation in this case.
- Tidally varying flocculation has implication on siltation in the estuarine turbidity maxima.

In order to improve our understandings of temporal and vertical variations of sediment flocculation dynamics within the turbidity maxima (TM) of the highly turbid Yangtze Estuary (YE), we deployed LISST-100C, a laser instrument for in-situ monitor of the sizes and concentrations of flocculated particles in a wet season. Field data in terms of vertical profiles of flow velocity, suspended sediment concentration (SSC), salinity, flocculated particle size distribution and volume concentration were obtained, based on field works conducted at consecutive spring, moderate, and neap tides.Data analyses show that the mean floc diameters (DM) were in the range of 14-95 μm, and flocculation exhibited strong temporal and vertical variations within a tidal cycle and between spring-neap cycles. Larger DM were observed during high and low slack waters, and the averaged floc size at neap tide was found 57% larger than at spring tide. Effective density of flocs decreased with the increase of floc size, and fractal dimension of flocs in the YE was mainly between 1.5 and 2.1. We also estimated the settling velocity of flocs by 0.04-0.6 mm s−1 and the largest settling velocity occurred also at slack waters. Moreover, it is found that turbulence plays a dominant role in the flocculation process. Floc size decreases significantly when the shear rate parameter G is > 2-3 s−1, suggesting the turbulence breaking force. Combined effects of fine sediment flocculation, enhanced settling process, and high sediment concentration resulted in a large settling flux around high water, which can in part explain the severe siltation in the TM of the YE, thus shedding lights on the navigation channel management.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Estuarine, Coastal and Shelf Science - Volume 191, 15 May 2017, Pages 1-9
نویسندگان
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