引用本文:
【打印本页】   【下载PDF全文】   View/Add Comment  Download reader   Close
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 2050次   下载 4105 本文二维码信息
码上扫一扫!
分享到: 微信 更多
流沙湾海水中总有机碳的时空分布及其影响因素研究
李雪英1,2,3, 孙恢礼1,4, 孙省利3, 张瑜斌3, 施玉珍3, 张际标3
1.中国科学院 烟台海岸带研究所;2.中国科学院 研究生院;3.广东海洋大学 海洋资源与环境监测中心;4.中国科学院 南海海洋研究所
摘要:
于2008 年2 月(冬季)、5 月(春季)、8 月(夏季)和11 月(秋季)对流沙湾进行了4 次采样调查, 研究分析了流沙湾海水中总有机碳的空间分布和季节变化特征, 并探讨了TOC 与温度、盐度、pH、叶绿素a 和底泥TOC之间的相关关系。结果发现, 在2008 年度流沙湾海水TOC的浓度为0.992~5.437 mg/L,平均值为2.414 mg/L, 呈现春季>夏季>秋季>冬季的变化趋势, 整个流沙湾海域海水TOC 的平面分布相对比较均匀, 表层稍大于底层。在内外湾分布上, 冬、夏季节内湾TOC 大于外湾, 而春、秋季节外湾大于内湾; 在垂直分布上, 冬、夏和秋季表层大于底层, 而春季底层大于表层; 在地域分布上, 冬、夏季节从流沙镇一侧海域到西联镇一侧海域逐渐减小, 秋季变化趋势相反, 春季时, 两侧无明显变化。相关关系的分析结果表明, 流沙湾海水TOC 与温度、pH 呈现出正相关关系, 与温度的相关关系较为显著, 与盐度则呈现不显著的负相关关系; 与叶绿素a 存在一定的相关关系, 在叶绿素a 浓度小于2.6μg/L, 两者呈现正相关关系, 而在叶绿素a 浓度大于2.6 μg/L, 两者呈现负相关关系; 与底泥TOC 呈现出了一定的正相关关系。
关键词:  流沙湾  总有机碳  时空分布  影响因素
DOI:
分类号:
基金项目:海洋公益性行业科研专项项目(200905005-05); 广东省海洋渔业科技推广专项(A200899J01)
Temporal and spatial distribution of total organic carbon in Liusha Bay and the influence factors investigation
Abstract:
The total organic carbon (TOC) in the Liusha Bay was investigated in February (winter), May (spring), August (summer) and December (autumn) of 2008. The characteristic of temporal and spatial distribution of TOC in seawater was studied and the correlations of TOC with temperature, salinity, pH value, chlorophyl-a content and sediment TOC were analyzed. The result showed that TOC content values ranged from 0.992 to 5.437 mg/L with average of 2.414 mg/L), and TOC content changed with a trend of spring>summer>autumn>winter. In Liusha Bay, the horizontal distribution of TOC was relatively even and TOC content in surface water was a little higher than bottom water. The TOC content of inner bay was higher than outer bay in winter and summer, while reversed in spring and autumn. For the vertical distribution, TOC content of surface water was higher than that of bottom water in winter, summer and autumn, while reversed in spring. For the regional distribution, The TOC content gradually decreases from Liusha town to Xilian town in winter and summer, and contrary in autumn. However, there was no significant changes in TOC content from Liusha town to Xilian town in spring. The correlation analysis showed that the TOC content had positive correlations with temperature and pH value. The former one is very significant. The TOC content showed insignificant negative correlation with salinity and definite correlation with chlorophyl-a. The TOC content positively correlated to chlorophyl-a when the chlorophyl-a concentration was less than 2.6 μg/L, while it is reversed when the concentration was more than 2.6 μg/L. In addition,TOC of seawater showed positive correlation with sediment TOC.
Key words:  Liusha Bay  Total organic carbon (TOC)  temporal and spatial distribution  influence factors
Copyright ©  Editorial Office for Marine Sciences Copyright©2008 All Rights Reserved
Supervised by: Chinese Academy of Sciences (CAS)   Sponsored by: Institute of Oceanology, CAS
Address: 7 Nanhai Road, Qingdao, China.  Postcode: 266071  Tel: 0532-82898755  E-mail: bjb@qdio.ac.cn
Technical support: Beijing E-Tiller Co.,Ltd.