海洋通报
海洋通報
해양통보
MARINE SCIENCE BULLETIN
2014年
6期
694-702
,共9页
周鸿权%孙昭晨%李伯根%武小勇%巩明%杨辉
週鴻權%孫昭晨%李伯根%武小勇%鞏明%楊輝
주홍권%손소신%리백근%무소용%공명%양휘
象山港%悬沙浓度%季节变化%潮周期变化%再悬浮
象山港%懸沙濃度%季節變化%潮週期變化%再懸浮
상산항%현사농도%계절변화%조주기변화%재현부
Xiangshan Bay%suspended sediment concentration%seasonal change%tidal cycle change%re-suspension
利用冬、夏两季象山港15个同步连续站和60个准同步大面站实测悬沙浓度数据,结合实测潮流、盐度等海洋水文资料,分析了象山港海域悬沙浓度变化规律。结果表明,象山港海域悬沙浓度分布具有较明显冬季大于夏季、大潮期大于小潮期以及湾口向湾顶逐渐减小的变化特征。这些特征主要受制于冬季高含沙量、低温、低盐的闽浙沿岸流与夏季高温、高盐、低含沙量的台湾暖流的交替作用和半月潮周期潮流动力变化的影响。在这种背景下,由于潮流动力作用,大小潮周期中底部沉积物与水体悬浮泥沙之间存在再悬浮与沉降的交换过程。
利用鼕、夏兩季象山港15箇同步連續站和60箇準同步大麵站實測懸沙濃度數據,結閤實測潮流、鹽度等海洋水文資料,分析瞭象山港海域懸沙濃度變化規律。結果錶明,象山港海域懸沙濃度分佈具有較明顯鼕季大于夏季、大潮期大于小潮期以及灣口嚮灣頂逐漸減小的變化特徵。這些特徵主要受製于鼕季高含沙量、低溫、低鹽的閩浙沿岸流與夏季高溫、高鹽、低含沙量的檯灣暖流的交替作用和半月潮週期潮流動力變化的影響。在這種揹景下,由于潮流動力作用,大小潮週期中底部沉積物與水體懸浮泥沙之間存在再懸浮與沉降的交換過程。
이용동、하량계상산항15개동보련속참화60개준동보대면참실측현사농도수거,결합실측조류、염도등해양수문자료,분석료상산항해역현사농도변화규률。결과표명,상산항해역현사농도분포구유교명현동계대우하계、대조기대우소조기이급만구향만정축점감소적변화특정。저사특정주요수제우동계고함사량、저온、저염적민절연안류여하계고온、고염、저함사량적태만난류적교체작용화반월조주기조류동력변화적영향。재저충배경하,유우조류동력작용,대소조주기중저부침적물여수체현부니사지간존재재현부여침강적교환과정。
Based on the data of suspended sediment concentration from 15 continuous stations and 60 quasi-synchronous grid stations in winter and summer of 2011, combined with the hydrodynamic data of tide, salinity and so on, this paper analyses the characteristics of suspended sediment concentration distribution in Xiangshan Bay. It shows that the suspended sediment concentration in winter is significantly higher than that in summer, and the magnitude is greater during spring tide than that during neap tide in the same season. Spatially, the suspended sediment concentration decreases constantly from mouth to top of the bay. Furthermore, it is concluded that the distribution of suspended sediment is mainly influenced by the alternative effect of coastal current in Fujian and Zhejiang with high suspended sediment concentration, low temperature, low salinity in winter and Taiwan warm current with high temperature, high salinity, low suspended sediment concentration in summer, and by the tidal dynamic changes in semimonthly tidal cycle. Under this condition, due to the tidal force, there is an exchange process of re-suspension and settlement between the bed sediment and suspended sediment in semimonthly tidal cycle.