台湾海峡
檯灣海峽
태만해협
JOURNAL OF OCEANOGRAPHY IN TAIWAN STRAIT
2010年
1期
81-88
,共8页
海洋地质学%沉积物%粒度%北仑河口%沉积分区
海洋地質學%沉積物%粒度%北崙河口%沉積分區
해양지질학%침적물%립도%북륜하구%침적분구
marine geology%sediment%grain size%Beilun Estuary%sedimentary zone
北仑河口84个表层沉积物样品的分析结果表明,该河口有含砾砂、砂、粉砂质砂、砂质粉砂、粉砂、砂-粉砂-粘土、粘土质粉砂等7种沉积物类型,并具有自西北往东南逐渐变细的特征;分析结果还表明北仑河口可划分为近口、河口和口外海滨3个沉积区,近口区以河流作用为主,河口区粗颗粒沉积作用主导,而口外海滨区则主要受到两种营力的共同作用.
北崙河口84箇錶層沉積物樣品的分析結果錶明,該河口有含礫砂、砂、粉砂質砂、砂質粉砂、粉砂、砂-粉砂-粘土、粘土質粉砂等7種沉積物類型,併具有自西北往東南逐漸變細的特徵;分析結果還錶明北崙河口可劃分為近口、河口和口外海濱3箇沉積區,近口區以河流作用為主,河口區粗顆粒沉積作用主導,而口外海濱區則主要受到兩種營力的共同作用.
북륜하구84개표층침적물양품적분석결과표명,해하구유함력사、사、분사질사、사질분사、분사、사-분사-점토、점토질분사등7충침적물류형,병구유자서북왕동남축점변세적특정;분석결과환표명북륜하구가화분위근구、하구화구외해빈3개침적구,근구구이하류작용위주,하구구조과립침적작용주도,이구외해빈구칙주요수도량충영력적공동작용.
This paper analyzed the grain size of 84 surface sediment samples from the Beilun Estuary. It indicates that the sediments were composed of 7 species i.e. gravel sand, sand, clayey sand, sandy clay, clay, sand-silt-clay and silt clay. Among them the most important is sand. The sediment particles become finer from the northwest to the southeast of the estuary. We also found that the sedimentary zones of Beilun Estuary can be divided into the nearshore area of estuary, estuary and offshore area of estuary. The main dynamic factor in the near shore area of estuary is the river runoff, the dominant agent affecting the estuary area is coarse particle deposition and the offshore area in the estuary is mostly affected by two agents.