首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Nutrient dynamics in the winter thermohaline frontal zone of the northern shelf region of the South China Sea
【24h】

Nutrient dynamics in the winter thermohaline frontal zone of the northern shelf region of the South China Sea

机译:南海北部陆架地区冬季热盐碱锋区的营养动态

获取原文
获取原文并翻译 | 示例
       

摘要

As the first attempt to estimate the nutrient transport across the winter thermohaline frontal zone on the northern shelf of the South China Sea, the nutrient dynamics around the front and the effects of cross-frontal water exchange on nutrient transport were investigated using wintertime field observations. Both water temperature and salinity increased from coastal to oceanic waters, showing the presence of a thermohaline front. The concentrations of dissolved inorganic nutrients decreased oceanward, especially across the thermohaline front, while those of dissolved organic nutrients (i.e., dissolved organic nitrogen (DON) and dissolved organic phosphorus) showed patchy distributions. Ammonium was the major constituent of dissolved inorganic nitrogen, and DON was the main component of total dissolved nitrogen. Molar ratios of PO_4~(3-)/total dissolved phosphorus decreased from coastal to oceanic waters, indicating that PO_4~(3-) was rapidly removed and/or consumed from the water column and that organic matter degradation increased offshore, replenishing PO_4~(3-). Molar ratios of NO_3~-/(NH_4~+ + DON) were 0.01-0.6, indicating dominance of regenerated nitrogen. Surface water convergence and bottom water divergence were identified in the across-shore velocity field, and the calculated across-shore nutrient fluxes suggest that the presence of the winter thermohaline front promotes the offshore transport of nutrients from coastal waters. The transport path begins with convergence of surface coastal waters toward the front, followed by the sinking in the frontal region and the oceanward movement through the bottom layer of the front offshore side. With an assumption of 500 km as the length of thermohaline front on the northern shelf of the South China Sea, the calculated offshore fluxes of nutrients across the entire front are larger than those from the Zhujiang (Pearl River) and the Changjiang (Yangtze River).
机译:作为估算南海北部陆架冬季温盐环流锋区养分运移的首次尝试,利用冬季实地观测资料研究了锋面周围的养分动态以及跨额水交换对养分运移的影响。从沿海水域到海洋水域的水温和盐度都增加了,表明存在温盐线。溶解的无机营养物的浓度向海洋减小,特别是在整个热盐线前沿,而溶解的有机营养物(即,溶解的有机氮(DON)和溶解的有机磷)的浓度显示出斑片状分布。铵是溶解的无机氮的主要成分,而DON是溶解的总氮的主要成分。从沿海到海洋,PO_4〜(3-)/总溶解磷的摩尔比降低,这表明PO_4〜(3-)从水柱中快速去除和/或消耗,有机质降解增加,补充了PO_4〜。 (3-)。 NO_3〜-/(NH_4〜+ + DON)的摩尔比为0.01-0.6,表明再生氮占优势。在跨岸速度场中确定了地表水的收敛性和底部水的发散性,并且计算出的跨岸养分通量表明,冬季盐沼锋线的存在促进了沿海水域养分的向海上运输。输送路径从表层沿海水向前汇合开始,然后在前缘区域下沉并通过前近海侧的底层向海洋运动。假设南海北部陆架上的热盐盐锋长度为500 km,计算得出的整个海域营养盐的通量要大于珠江(珠江)和长江(长江)的营养盐通量。 。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号