海洋科学
海洋科學
해양과학
MARINE SCIENCES
2013年
6期
83-88
,共6页
徐芳%冯秀丽%陈斌林%贺心然%魏飞
徐芳%馮秀麗%陳斌林%賀心然%魏飛
서방%풍수려%진빈림%하심연%위비
灌河口%环境敏感粒度组分%210Pb%沉积变化
灌河口%環境敏感粒度組分%210Pb%沉積變化
관하구%배경민감립도조분%210Pb%침적변화
the Guanhe Estuary%environmentally sensitive grain size component%210Pb%deposition variation
为了研究灌河口海区的沉积环境,利用激光粒度仪对位于灌河口的柱状样 GH-1孔进行了沉积物粒度分析,根据粒级-标准偏差方法对此柱状样的环境敏感粒级进行了计算,并结合对粒度概率曲线图的分析来对该区域进行沉积环境的研究,从而探讨了该环境敏感粒度组分的环境指示意义。在研究区内确定环境敏感粒度组分为250~32μm,32~16μm,代表沉积过程中的两种动力机制,分别是风暴流和沿岸流。通过该柱状样的210Pb测年可以得到沉积速率和沉积环境的变化,上段沉积速率较大为1.9 cm/a,下段20 cm沉积速率较低为0.4 cm/a。
為瞭研究灌河口海區的沉積環境,利用激光粒度儀對位于灌河口的柱狀樣 GH-1孔進行瞭沉積物粒度分析,根據粒級-標準偏差方法對此柱狀樣的環境敏感粒級進行瞭計算,併結閤對粒度概率麯線圖的分析來對該區域進行沉積環境的研究,從而探討瞭該環境敏感粒度組分的環境指示意義。在研究區內確定環境敏感粒度組分為250~32μm,32~16μm,代錶沉積過程中的兩種動力機製,分彆是風暴流和沿岸流。通過該柱狀樣的210Pb測年可以得到沉積速率和沉積環境的變化,上段沉積速率較大為1.9 cm/a,下段20 cm沉積速率較低為0.4 cm/a。
위료연구관하구해구적침적배경,이용격광립도의대위우관하구적주상양 GH-1공진행료침적물립도분석,근거립급-표준편차방법대차주상양적배경민감립급진행료계산,병결합대립도개솔곡선도적분석래대해구역진행침적배경적연구,종이탐토료해배경민감립도조분적배경지시의의。재연구구내학정배경민감립도조분위250~32μm,32~16μm,대표침적과정중적량충동력궤제,분별시풍폭류화연안류。통과해주상양적210Pb측년가이득도침적속솔화침적배경적변화,상단침적속솔교대위1.9 cm/a,하단20 cm침적속솔교저위0.4 cm/a。
In order to explore the deposition environment of the Guanhe Estuary, grain-size analysis of sediment GH-1 drilling, retrieved from Guanhe Estuary, was carried out by using a Malvern 2000 grain-size analyzer. The environmentally sensitive grain size components were calculated according to variations in the grain-size standard deviation. The deposition environment was studied combined with the analysis of grain size probability curve. At the same time, the environmental implications were discussed. Two environmentally sensitive grain-size compo-nents, 250~32 μm and 32~16 μm, were identified, representing two dynamic mechanisms in the process of sedi-mentary, storm flow and coastal current. The variation of deposition rate and sedimentary environment can be ob-tained by using the 210Pb technique. The results show that the deposition rate was larger at 1.9 cm/a, and the deposi-tion rate of the last 20 cm was smaller at 0.4 cm/a.