中国海洋大学学报(自然科学版)
中國海洋大學學報(自然科學版)
중국해양대학학보(자연과학판)
PERIODICAL OF OCEAN UNIVERSITY OF CHINA
2009年
4期
767-772
,共6页
张婷%米铁柱%石晓勇%祝陈坚
張婷%米鐵柱%石曉勇%祝陳堅
장정%미철주%석효용%축진견
北黄海%磷%形态%分布
北黃海%燐%形態%分佈
북황해%린%형태%분포
the North Yellow Sea%phosphate%forms and distribution
通过对2006年夏季对北黄海的现场调查,对该海域磷的形态和分布特征进行了探讨.结果表明: 夏季北黄海海域总磷(TP)浓度的变化范围是0.00~1.63 μmol/L,其中溶解无机磷(DIP)是最主要的存在形式,占TP的44%,溶解有机磷(DOP)略低,颗粒磷(PP)最少,总磷的分布呈现由南向北逐渐增高的趋势.北黄海海域水体中各种形态磷(除DOP外)均是表层低于底层,表底层PP的含量相差不大, 表层以DOP为主要存在形态,而底层则以DIP为主,大部分DIP浓度高的区域恰好是DOP浓度的低值区,一定程度上存在着负相关关系(r=-0.34).这样的分布趋势除了受生物活动的影响外,在底部海域还与黄海冷水团密切相关.
通過對2006年夏季對北黃海的現場調查,對該海域燐的形態和分佈特徵進行瞭探討.結果錶明: 夏季北黃海海域總燐(TP)濃度的變化範圍是0.00~1.63 μmol/L,其中溶解無機燐(DIP)是最主要的存在形式,佔TP的44%,溶解有機燐(DOP)略低,顆粒燐(PP)最少,總燐的分佈呈現由南嚮北逐漸增高的趨勢.北黃海海域水體中各種形態燐(除DOP外)均是錶層低于底層,錶底層PP的含量相差不大, 錶層以DOP為主要存在形態,而底層則以DIP為主,大部分DIP濃度高的區域恰好是DOP濃度的低值區,一定程度上存在著負相關關繫(r=-0.34).這樣的分佈趨勢除瞭受生物活動的影響外,在底部海域還與黃海冷水糰密切相關.
통과대2006년하계대북황해적현장조사,대해해역린적형태화분포특정진행료탐토.결과표명: 하계북황해해역총린(TP)농도적변화범위시0.00~1.63 μmol/L,기중용해무궤린(DIP)시최주요적존재형식,점TP적44%,용해유궤린(DOP)략저,과립린(PP)최소,총린적분포정현유남향북축점증고적추세.북황해해역수체중각충형태린(제DOP외)균시표층저우저층,표저층PP적함량상차불대, 표층이DOP위주요존재형태,이저층칙이DIP위주,대부분DIP농도고적구역흡호시DOP농도적저치구,일정정도상존재착부상관관계(r=-0.34).저양적분포추세제료수생물활동적영향외,재저부해역환여황해랭수단밀절상관.
Based on the data collected in summer 2006, the forms and distribution of phosphorus in the North Yellow Sea were discussed. The total phosphorus(TP)in summer ranged from 0.02 to 1.63 μmol/L.The uppermost form was DIP, and PP was the least. The concentration of TP was gradually increasing from south to north. All forms of phosphorus except for DOP were higher in the bottom than in the surface. Content of PP was oppositely even. DOP was the leading form in the surface layer, however, it was DIP in the bottom. DIP and DOP were negative correlation in a certain extent and the correlation factor was -0.34. The distributions of DIP and DOP were mainly affected by the biological processes, but it also related to the Yellow Sea Cold Water Mass in the bottom of the sea.