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镭、氡同位素示踪调水调沙对黄河口水体运移及营养盐分布特征的影响

张晓洁 许博超 夏冬 江雪艳 简慧敏

张晓洁, 许博超, 夏冬, 江雪艳, 简慧敏. 镭、氡同位素示踪调水调沙对黄河口水体运移及营养盐分布特征的影响[J]. 海洋学报, 2016, 38(8): 36-43. doi: 10.3969/j.issn.0253-4193.2016.08.004
引用本文: 张晓洁, 许博超, 夏冬, 江雪艳, 简慧敏. 镭、氡同位素示踪调水调沙对黄河口水体运移及营养盐分布特征的影响[J]. 海洋学报, 2016, 38(8): 36-43. doi: 10.3969/j.issn.0253-4193.2016.08.004
Zhang Xiaojie, Xu Bochao, Xia Dong, Jiang Xueyan, Jian Huimin. Using natural radium and radon isotopes trace the water transport process and nutrients distribution in the Yellow River Estuary under the influence of the Water-Sediment Regulation Scheme[J]. Haiyang Xuebao, 2016, 38(8): 36-43. doi: 10.3969/j.issn.0253-4193.2016.08.004
Citation: Zhang Xiaojie, Xu Bochao, Xia Dong, Jiang Xueyan, Jian Huimin. Using natural radium and radon isotopes trace the water transport process and nutrients distribution in the Yellow River Estuary under the influence of the Water-Sediment Regulation Scheme[J]. Haiyang Xuebao, 2016, 38(8): 36-43. doi: 10.3969/j.issn.0253-4193.2016.08.004

镭、氡同位素示踪调水调沙对黄河口水体运移及营养盐分布特征的影响

doi: 10.3969/j.issn.0253-4193.2016.08.004
基金项目: 国家自然科学基金(41576075,41206064,41376085);山东省自然科学基金(ZR2012DQ002);青岛市科技计划基础研究项目(13-1-4-224-jch)。

Using natural radium and radon isotopes trace the water transport process and nutrients distribution in the Yellow River Estuary under the influence of the Water-Sediment Regulation Scheme

  • 摘要: 为研究调水调沙影响下的镭、氡同位素和营养盐在黄河口的分布特征,于2013年7月调水调沙期间在黄河口及其邻近海域进行了多点的连续观测。研究发现:(1)黄河口海域镭、氡同位素分布呈现明显的“分区”现象,南北两区分别为“调水调沙影响非显著区域”和“调水调沙影响显著区域”,北部海域镭、氡同位素浓度高值主要来源于陆源输入(包括河流输入和海底地下水排放);(2)调查期间,北部海域水体年龄为(2.9±1.6)d,南部海域水体年龄为(5.0±2.1)d;水龄随潮汐变化表现出涨潮时水龄增大、落潮时水龄减小的波动趋势;(3)北部海域溶解无机氮(DIN)和溶解硅(DSi)含量明显高于南部海域,而溶解无机磷(DIP)在两个区域的含量相差不大。
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出版历程
  • 收稿日期:  2015-12-19
  • 修回日期:  2016-02-19

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