Developing nutrient criteria for the Jiulong River Estuary, Southeast China

LIU Baoli CAO Wenzhi HUANG Zheng CHEN Wenhui CHEN Huihuang LIU Lusan

刘保莉, 曹文志, 黄铮, 陈文慧, 陈辉煌, 刘录三. 中国九龙江河口营养盐基准值研究[J]. 海洋学报英文版, 2018, 37(2): 1-13. doi: 10.1007/s13131-017-1121-0
引用本文: 刘保莉, 曹文志, 黄铮, 陈文慧, 陈辉煌, 刘录三. 中国九龙江河口营养盐基准值研究[J]. 海洋学报英文版, 2018, 37(2): 1-13. doi: 10.1007/s13131-017-1121-0
LIU Baoli, CAO Wenzhi, HUANG Zheng, CHEN Wenhui, CHEN Huihuang, LIU Lusan. Developing nutrient criteria for the Jiulong River Estuary, Southeast China[J]. Acta Oceanologica Sinica, 2018, 37(2): 1-13. doi: 10.1007/s13131-017-1121-0
Citation: LIU Baoli, CAO Wenzhi, HUANG Zheng, CHEN Wenhui, CHEN Huihuang, LIU Lusan. Developing nutrient criteria for the Jiulong River Estuary, Southeast China[J]. Acta Oceanologica Sinica, 2018, 37(2): 1-13. doi: 10.1007/s13131-017-1121-0

中国九龙江河口营养盐基准值研究

doi: 10.1007/s13131-017-1121-0
基金项目: The National Natural Science Foundation of China under contract Nos 41076007 and 40676014; the National Basic Research Program of China under contract No. 2009CB421201; the Program of Introducing Talents of Discipline to Universities of China under contract No. B07036.

Developing nutrient criteria for the Jiulong River Estuary, Southeast China

  • 摘要: 河口与海岸带面临的富营养化问题与水体中过量营养盐含量是紧密相关的,寻找水体营养盐基准值可以为控制和提高地表水水质提供参考。但是目前国内已有营养盐基准值仅针对地表淡水和海水,对于具有独特水动力和生态系统的河口半咸水来说是不适用的。特别是考虑到河口咸淡水的混合作用、生态系统的响应以及营养盐内部循环对水体浓度的影响,制定一个合理的河口营养盐基准值、有效控制河口营养盐浓度迫在眉睫。为此,本研究选取中国福建九龙江河口为研究区,探索制定河口营养盐基准值方法。九龙江河口区自2000年后水质恶化速度较快,大部分区域的营养盐浓度超过国家海水水质标准第四类海水的上限。本研究首先于2013-2014年分季节对九龙江河口地区进行多航次现场采样;根据采集的河口地貌、水域盐度及生态系统特征信息,采用GIS技术将九龙江河口分为具有显著物理、生化属性区别的三个区域;再根据频数累积法和基于赤潮数据的混合模型法分析该河口区营养盐历史数据(1994-2014年)和赤潮数据,以赤潮作为生态环境崩溃的标志,推导三个分区的营养盐推荐基准值。最终确定从河口向海三个分区的DIN基准值分别为64、21、14μmol/L(0.90、0.29、0.20mg/L),SRP的基准值分别为0.89、0.76、0.89μmol/L(0.028、0.024、0.028mg/L)。需要提醒的是,不同河口区营养盐基准值因不同环境特征而异。因此,本研究希望通过示范的营养盐基准值计算方法,促进我国河口海岸水环境标准的全面研究。
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  • 收稿日期:  2017-01-02
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