2011年春季东海赤潮高发区尿素分布特征及影响因素

王雪景; 石晓勇; 赵玉庭; 张传松

doi:10.3969/j.issn.0253-4193.2015.02.007

2011年春季东海赤潮高发区尿素分布特征及影响因素

doi: 10.3969/j.issn.0253-4193.2015.02.007

1.
中国海洋大学化学化工学院, 山东青岛 266100;中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100
2.
中国海洋大学化学化工学院, 山东青岛 266100;中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100;国家海洋局海洋减灾中心, 北京 100194
3.
山东省海洋资源与环境研究院, 山东烟台 264003

基金项目: 国家重点基础研究发展计划(973)项目(2010CB428701);国家自然科学基金(41376106).

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出版历程
- 收稿日期: 2014-03-19
- 修回日期: 2014-08-01

Distribution and concentration of urea in the East China Sea in spring of 2011

1.
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China
2.
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China;National Marine Hazard Mitigation Service, Beijing 100194, China
3.
Shandong Marine Resource and Environment Research Institute, Yantai 264003, China

摘要

摘要: 2011年春季(3-5月)在东海赤潮高发区硅藻和甲藻赤潮暴发及演替过程中进行了3个航次的现场调查,通过对调查资料的分析,对该海域尿素的含量变化、平面分布特征及影响因素进行了初步探讨.结果表明:调查海域尿素的含量在检出限~6.32 μmol/L范围内,平均浓度为(1.33±0.84) μmol/L,是该海域一种重要的溶解有机氮组分.其中,在DIN中所占比例8.73%~18.04%,在DON中所占比例5.63%~15.73%.赤潮的暴发对尿素含量和分布影响较大,能够影响并控制该海区尿素的实际浓度水平和分布特征.其中,硅藻赤潮暴发前后尿素和DIN含量下降百分比分别为36.67%和49.88%,甲藻赤潮暴发前后尿素和DIN含量下降百分比分别为8.78%和28.97%.硅藻赤潮期,尿素的高值区和叶绿素高值区一致,其含量明显高于正常海区;甲藻赤潮期,叶绿素的高值区对应着尿素低值区,赤潮区内尿素含量普遍降低至1 μmol/L以下,尿素是一种能够被研究海区甲藻类浮游植物吸收利用的有效氮源.在调查海域大规模硅藻和甲藻赤潮暴发和演替期间,尿素的平面分布上未呈现明显的近岸低、远岸高的分布特点,与盐度数值没有明显的相关性,该时期陆源输入不是影响该海域尿素分布的主要因素.
- 长江口 /
- 东海 /
- 赤潮 /
- 尿素 /
- 分布
Abstract: Based on the data of three cruises in Spring (March to May) of 2011 that carried out in the south of Yangtze estuary where was high frequent occurrence of harmful algal blooms, the concentration and the spatial distribution of urea were analyzed and its influencing factors were discussed. The results showed: The concentration of urea ranged from detection limit to 6.32 μmol/L and its average was(1.33±0.84 )μmol/L. Urea was an important form of dissolved organic nitrogen during the survey. The ratio of urea to DIN was 8.73%-18.04% and the proportion of urea in DON was 5.63%-15.73%.The occurrence of diatom HABs and dinoflagellate HABs could affect the content and distribution of urea in the invested area and control the urea concentration and distribution characteristics in this area. The decreased ratio of urea and DIN were 36.67%, 49.88% after diatom HABs, respectively; after dinoflagellate HABs, urea and DIN decreased 8.78% and 28.97%. In the diatom HABsarea, the zones of high urea concentration and high chlorophyll were in the same position and the urea content was significantly higher than that of normal zones. In the dinoflagellate HABs area, the zones of high chlorophyll values were corresponded to the zones of low urea values, urea generally reduced to 1 μmol/L in this area. Urea was a kind of effective nitrogen source for phytoplankton of dinoflagellate. During the large scale HABs of diatom and dinoflagellate and their succession process in the invested area, the distribution of urea had no characteristic of gradual reduction from inshore to offshore. Urea concentration and salinity had no significant correlation. During the investigation, terrigenous input was not the main factor affecting the distribution of urea.
- Yangtze estuary /
- East China Sea /
- HABs /
- urea /
- distribution

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