海洋通报
海洋通報
해양통보
MARINE SCIENCE BULLETIN
2013年
5期
481-487
,共7页
马媛%魏巍%高振会%王迪%杨阳%马玉
馬媛%魏巍%高振會%王迪%楊暘%馬玉
마원%위외%고진회%왕적%양양%마옥
营养盐%钦州湾%径流%环境因子
營養鹽%欽州灣%徑流%環境因子
영양염%흠주만%경류%배경인자
nutrients%Qinzhou Bay%runoff%environmental factors
利用2008-2009年4个航次的调查资料,研究了钦州湾海域营养盐的分布变化特征。结果表明,钦州湾营养盐分布呈显著的季节变化。NO3-N和NO2-N夏季含量最高,NH4-N和PO4-P含量冬季最高,夏季最低,秋季DIN的形态以NH4-N为主,而夏季则以NO3-N为主。CN/CP夏季>春季>秋季>冬季,该海域春季和夏季浮游植物生长受P限制。NO3-N和NO2-N的平面分布基本呈现钦州湾内向湾外逐渐降低的分布规律,径流输入是影响其分布的主要因素,在外湾余流作用对其分布规律影响显著,NH4-N和PO4-P平面分布规律则受到外海环境因素的影响。经与历史资料对比,DIN和CN/CP呈逐年代大幅上升的变化趋势,钦州湾营养盐结构已从N缺乏到P缺乏转变。
利用2008-2009年4箇航次的調查資料,研究瞭欽州灣海域營養鹽的分佈變化特徵。結果錶明,欽州灣營養鹽分佈呈顯著的季節變化。NO3-N和NO2-N夏季含量最高,NH4-N和PO4-P含量鼕季最高,夏季最低,鞦季DIN的形態以NH4-N為主,而夏季則以NO3-N為主。CN/CP夏季>春季>鞦季>鼕季,該海域春季和夏季浮遊植物生長受P限製。NO3-N和NO2-N的平麵分佈基本呈現欽州灣內嚮灣外逐漸降低的分佈規律,徑流輸入是影響其分佈的主要因素,在外灣餘流作用對其分佈規律影響顯著,NH4-N和PO4-P平麵分佈規律則受到外海環境因素的影響。經與歷史資料對比,DIN和CN/CP呈逐年代大幅上升的變化趨勢,欽州灣營養鹽結構已從N缺乏到P缺乏轉變。
이용2008-2009년4개항차적조사자료,연구료흠주만해역영양염적분포변화특정。결과표명,흠주만영양염분포정현저적계절변화。NO3-N화NO2-N하계함량최고,NH4-N화PO4-P함량동계최고,하계최저,추계DIN적형태이NH4-N위주,이하계칙이NO3-N위주。CN/CP하계>춘계>추계>동계,해해역춘계화하계부유식물생장수P한제。NO3-N화NO2-N적평면분포기본정현흠주만내향만외축점강저적분포규률,경류수입시영향기분포적주요인소,재외만여류작용대기분포규률영향현저,NH4-N화PO4-P평면분포규률칙수도외해배경인소적영향。경여역사자료대비,DIN화CN/CP정축년대대폭상승적변화추세,흠주만영양염결구이종N결핍도P결핍전변。
Based on data from four cruises obtained by field survey and experiments in the Qinzhou Bay during 2008 to 2009,the distribution characteristics of nutrients were studied. The result showed that the distribution of nutrients in the Qinzhou Bay remarkably changed seasonally. The concentrations of nitrate and nitrite were highest in summer. But those of ammonia and phosphorus were lowest in summer and highest in winter. It indicated that ammonia was the main form of inorganic nitrogen during autumn,and nitrate was the main form during summer in the Qinzhou Bay. N/P ratio decreased in the sequence of summer, spring, autumn and winter gradually, and the active phosphorus was the nutrient limiting the growth of phytoplankton during spring and summer in the Qinzhou Bay. It was discovered that the contents of nitrate and nitrite constantly reduced from the inner bay to the outer bay. Their special distributions were dominated by the runoff input and influenced remarkably by the residual tidal current in the Qinzhou Bay simultaneously. The environmental factors of open sea played an important role in the ammonia and phosphorus distributions. Based on the historical data, the changes of nutrients in three decades were investigated. It was suggested that the concentrations of dissolved inorganic and N/P ratio increased distinctly. The nutrient structure had changed from N shortage to P shortage.