|
| 引用本文: | 卜庆伟,李福林,陈学群,林 琳.莱州湾东岸海底地下水来源判别及量值估算[J].海洋科学,2013,37(11):74-78. |
| |
|
| |
|
|
| 本文已被：浏览 2037次 下载 2534次 |
码上扫一扫！ |
|
|
| 莱州湾东岸海底地下水来源判别及量值估算 |
|
卜庆伟1, 李福林1, 陈学群1, 林 琳1
|
|
山东省水利科学研究院
|
|
| 摘要: |
| 采用稳定同位素——18O、D, 结合常规离子分析结果确定了莱州湾东岸海底地下水的来源, 并采用数值方法估算了其量值。结果表明: 莱州湾东岸海底地下水主要来源于波浪、潮汐的海水补给, 同时在一定程度上受地下水径流排泄的影响, 三者对海底地下水的贡献率分别为 31.0%, 56.3%和 12.7%。研究结果对于合理开发、科学保护海底地下水具有重要现实意义。 |
| 关键词: 莱州湾东岸 海底地下水径流 来源 量值 |
| DOI： |
| 分类号: |
| 基金项目:国家自然科学基金项目(40776050); 水利部公益性行业科研专项经费项目(200901076); 山东省优秀中青年科学家科研奖励基金项目(2006BS08025) |
|
| Identification and quantification of submarine groundwater discharge along the east coast of the Laizhou Bay |
|
|
| Abstract: |
| Submarine groundwater discharge(SGD) is the important pathway for the study of Land-Ocean interactions, while source identification is the premise for rational utilization of submarine groundwater resources. In this paper, attempts were made to identify the source of submarine groundwater along the east coast of the Laizhou Bay by using stable isotopes—18O and D, combined with conventional ions analysis. The quantity estimation was made using numerical methods. The results show that wave action and tidal fluctuation are the main sources influencing SGD. Moreover, the land groundwater discharge, also has certain effect on it. Contributions of, wave run-up, tidal fluctuation and groundwater runoff to groundwater are 12.7%, 31.0% and 56.3%, respectively. These results are very helpful to the rational development and scientific protection of submarine groundwater. |
| Key words: east coast of the Laizhou Bay submarine groundwater discharge source identification quantity estimation |
|
|
|
|
|
|