中国环境监测
中國環境鑑測
중국배경감측
Environmental Monitoring in China
2015年
5期
140-144
,共5页
柴小平%魏娜%母清林%王益鸣%任世军%何松琴
柴小平%魏娜%母清林%王益鳴%任世軍%何鬆琴
시소평%위나%모청림%왕익명%임세군%하송금
溶解氧%饱和度%分布%影响因素
溶解氧%飽和度%分佈%影響因素
용해양%포화도%분포%영향인소
dissolved oxygen%saturation%distribution%influencing factors
根据2014年春季对浙江省近岸海域溶解氧的调查结果,结合现场的温度和盐度,得出溶解氧饱和度的平面分布,并在此基础上探讨了饱和度与温度、盐度、化学需氧量、浮游植物丰度之间的关系。结果显示,浙江省近岸海域溶解氧饱和度范围为92.1%~120%,均值为100%。总体呈西部沿岸低,东部外海高的平面分布趋势。溶解氧饱和度高值区与浮游植物丰度的高值区一致。低饱和区域化学需氧量含量基本高于1 mg/L。陆源径流和有机物质耗氧分解是沿岸低饱和区域主要控制因素,外海水和浮游植物光合作用是高饱和区域主要控制因素。径流和外海水对有机物质分解和浮游植物光合作用有一定的调控作用。
根據2014年春季對浙江省近岸海域溶解氧的調查結果,結閤現場的溫度和鹽度,得齣溶解氧飽和度的平麵分佈,併在此基礎上探討瞭飽和度與溫度、鹽度、化學需氧量、浮遊植物豐度之間的關繫。結果顯示,浙江省近岸海域溶解氧飽和度範圍為92.1%~120%,均值為100%。總體呈西部沿岸低,東部外海高的平麵分佈趨勢。溶解氧飽和度高值區與浮遊植物豐度的高值區一緻。低飽和區域化學需氧量含量基本高于1 mg/L。陸源徑流和有機物質耗氧分解是沿岸低飽和區域主要控製因素,外海水和浮遊植物光閤作用是高飽和區域主要控製因素。徑流和外海水對有機物質分解和浮遊植物光閤作用有一定的調控作用。
근거2014년춘계대절강성근안해역용해양적조사결과,결합현장적온도화염도,득출용해양포화도적평면분포,병재차기출상탐토료포화도여온도、염도、화학수양량、부유식물봉도지간적관계。결과현시,절강성근안해역용해양포화도범위위92.1%~120%,균치위100%。총체정서부연안저,동부외해고적평면분포추세。용해양포화도고치구여부유식물봉도적고치구일치。저포화구역화학수양량함량기본고우1 mg/L。륙원경류화유궤물질모양분해시연안저포화구역주요공제인소,외해수화부유식물광합작용시고포화구역주요공제인소。경류화외해수대유궤물질분해화부유식물광합작용유일정적조공작용。
According to the data collected in the 2014 Zhejiang offshore spring survey, the surface dissolved oxygen ( DO ) saturation distributions were analyzed. On this basis,the relationships between DO saturation and temperature,salinity,chemical oxygen demand ( COD) and phytoplankton density were preliminarily explored. The results showed that: The Zhejiang offshore DO saturation was in the range of 92. 1% to 120%,averaged at 100%, lower in coastal area and higher in outside area. The high values area of DO saturation is quite consistent with phytoplankton density. In the low DO saturation area,the COD concentrations are above 1 mg/L mostly. In the low DO saturation area,terrestrial runoff and organic matter oxidation are the main influencing factors. In the high DO saturation area,outer seawaters and phytoplankton photosynthesis are the dominant factors. Runoff and outer seawaters also have a certain regulating effect on organic matter oxidation and phytoplankton photosynthesis.