海洋学报(中文版)
海洋學報(中文版)
해양학보(중문판)
ACTA OCEANOLOGICA SINICA
2014年
2期
130-136
,共7页
韩沉花%叶瑛%潘依雯%秦华伟
韓沉花%葉瑛%潘依雯%秦華偉
한침화%협영%반의문%진화위
台湾龟山岛%海底热泉%温度%酸碱度%小波分析%潮汐周期性
檯灣龜山島%海底熱泉%溫度%痠堿度%小波分析%潮汐週期性
태만구산도%해저열천%온도%산감도%소파분석%조석주기성
Taiwan Kueishantao Islet%seafloor hydrothermal%temperature%acidity%Morlet wavelet analysis%tidal periodicity
海底热液活动及其周边环境的调查研究是海洋科学领域的热点之一。海底热液喷口环境的物理化学参数,尤其是浅水型热液,会受到潮汐变化的影响。台湾龟山岛靠近冲绳海槽南端分布有多处浅水型热液喷口(<30 m )。2010年5月,浙江大学、杭州电子科技大学和台湾中山大学对该海域实施了联合考察,利用电化学传感器获得了低温热液喷口(24.83414°N ,121.96191°E )连续87 h的温度和pH现场观测数据。基于Morlet复小波变换方法,分析了浅水型热液喷口的温度和pH现场观测时间序列的变化周期,并通过与当地潮汐记录数据作比较,获得了其与潮汐信号之间的潜在关系,证实了潮汐变化是海底白色热泉喷口物理化学参数现场观测最主要的影响因素。温度和pH现场观测数据经Morlet复小波变换后的小波系数分别存在规律的12.9 h和12.5 h变化周期,并且温度的小波系数在准半日周期尺度与潮汐高度呈负相关变化,相关系数为-0.89;p H的小波系数情况相反,相关系数为0.76。
海底熱液活動及其週邊環境的調查研究是海洋科學領域的熱點之一。海底熱液噴口環境的物理化學參數,尤其是淺水型熱液,會受到潮汐變化的影響。檯灣龜山島靠近遲繩海槽南耑分佈有多處淺水型熱液噴口(<30 m )。2010年5月,浙江大學、杭州電子科技大學和檯灣中山大學對該海域實施瞭聯閤攷察,利用電化學傳感器穫得瞭低溫熱液噴口(24.83414°N ,121.96191°E )連續87 h的溫度和pH現場觀測數據。基于Morlet複小波變換方法,分析瞭淺水型熱液噴口的溫度和pH現場觀測時間序列的變化週期,併通過與噹地潮汐記錄數據作比較,穫得瞭其與潮汐信號之間的潛在關繫,證實瞭潮汐變化是海底白色熱泉噴口物理化學參數現場觀測最主要的影響因素。溫度和pH現場觀測數據經Morlet複小波變換後的小波繫數分彆存在規律的12.9 h和12.5 h變化週期,併且溫度的小波繫數在準半日週期呎度與潮汐高度呈負相關變化,相關繫數為-0.89;p H的小波繫數情況相反,相關繫數為0.76。
해저열액활동급기주변배경적조사연구시해양과학영역적열점지일。해저열액분구배경적물이화학삼수,우기시천수형열액,회수도조석변화적영향。태만구산도고근충승해조남단분포유다처천수형열액분구(<30 m )。2010년5월,절강대학、항주전자과기대학화태만중산대학대해해역실시료연합고찰,이용전화학전감기획득료저온열액분구(24.83414°N ,121.96191°E )련속87 h적온도화pH현장관측수거。기우Morlet복소파변환방법,분석료천수형열액분구적온도화pH현장관측시간서렬적변화주기,병통과여당지조석기록수거작비교,획득료기여조석신호지간적잠재관계,증실료조석변화시해저백색열천분구물이화학삼수현장관측최주요적영향인소。온도화pH현장관측수거경Morlet복소파변환후적소파계수분별존재규률적12.9 h화12.5 h변화주기,병차온도적소파계수재준반일주기척도여조석고도정부상관변화,상관계수위-0.89;p H적소파계수정황상반,상관계수위0.76。
Investigation into seafloor hydrothermal activity and its surroundings has been one key point of studying ocean sciences .Physical and chemical parameters obtained from the hydrothermal environments would be influ -enced by the tide ,especially from the shallow hydrothermal vent .It is distributing many hydrothermal vents on the less than 30 meter shallow seafloor of Kueishantao Islet ,Northeast offshore Taiwan Island ,close to the south-ern Okinawa Trough .Zhejiang University ,Hangzhou Dianzi University ,and Taiwan Sun Yat-sen University to-gether carried a joint investigation into seafloor hydrothermal near Kueishan island sea area and obtained continuous temperature and pH field observation data of a low-temperature hydrothermal vent (24.83414° N ,121.961 91° E) for about 87 hours .Based on Morlet complex wavelet transform method ,after compared the calculating results with the recorded tidal height variance ,the potential periodic relationship between temperature and pH field ob-served time series of shallow hydrothermal vent and tide signal can be studied .The result evidenced that tide is the main impact factor for field investigating seafloor physical and chemical parameters of white hydrothermal vent . The wavelet coefficients of the in-situ temperature and pH data after Morlet complex wavelet transform exist regu-lar 12.9 h and 12.5 h periods .Besides ,wavelet coefficients of the temperature are negative correlated with the tid-al height at this semi-diurnal time scale with the correlation coefficient -0.89 ,and pH wavelet coefficient is the opposite case with the correlation coefficient 0.76 .