...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Oceanology >Dissolved Inorganic Carbon in the Waters of the Southeastern Part of the Barents Sea(Pechora Sea)
【24h】

Dissolved Inorganic Carbon in the Waters of the Southeastern Part of the Barents Sea(Pechora Sea)

机译：巴伦支海（Pechora海）东南部水域中溶解的无机碳

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

Using the example of the southeastern part of the Barents Sea(Pechora Sea),the features of the seasonal dynamics and spatial distribution of the forms of dissolved inorganic carbon(C_tot and pCO_2)were considered using both archive data and those of the expeditions performed by the Shirshov Institute of Oceanology(IO RAN)in 1998 and 2003.It was shown that the spatial distribution of the carbonate system components was strongly subjected to hydrophysical factors,while the seasonal dynamics of the pCO_2 and C_tot values were mainly determined by biochemical factors.The formation of the hydrochemical structure of the Pechora Sea waters was determined by two water masses:the surface waters of the Barents Sea(relative contribution of 50-60%)and the waters of Pechora Bay(relative contribution about 40%).A certain influence may also be exerted by the water of lagoons,their relative contribution amounting,in selected cases,up to 10%.The formation of the lagoon waters is mainly caused by the surface waters of the Pechora Sea(up to 70%),by the waters of Pechora Bay(from 13 to 30%),and by the runoff waters of melt lakes(from 15 to 30%).
机译：以巴伦支海（Pechora海）东南部为例，利用档案资料和由1998年和2003年在Shirshov海洋研究所（IO RAN）进行研究。结果表明，碳酸盐体系各组分的空间分布受水物理因素的强烈影响，而pCO_2和C_tot值的季节动态主要由生化因素决定。 Pechora海水的水化学结构的形成是由两个水团决定的：巴伦支海的地表水（相对贡献50-60％）和Pechora湾的水（相对贡献约40％）。泻湖水也可能产生影响，在某些情况下，它们的相对贡献可达10％。泻湖水的形成主要是由于苏佩霍拉海的最高水位（最高70％），佩霍拉湾的水位（最高13％至30％）和融化湖的径流水（最高15％至30％）。

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