磨刀门水道枯水期咸潮变化趋势及成因
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TV213

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国家自然科学基金(91547202,51479216)


Change trend and cause of salt tide in Modaomen Channel during dry seasons
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    摘要:

    在对1998—2015年磨刀门水道咸潮上溯不同时间尺度变化特征进行统计分析的基础上,采用Spearman秩相关分析识别流量、海平面、平均潮差、最高潮位、最低潮位以及降雨量等因素与咸度超标时数之间的相关性,利用主成分分析确定各因素对咸潮上溯活动变化的贡献程度。研究结果表明:1998—2015年,磨刀门水道枯水期的咸潮上溯活动表现出两阶段的变化特征,以2004—2005年枯水期为分界点,第一阶段的咸度超标时数呈现出先下降后上升的“V”型变化特征,第二阶段则总体表现为下降趋势,有利于河口地区的供水安全;咸潮高超标时数主要集中在每年12月至次年2月,且变化趋势与年际变化趋势基本一致;流量、海平面和最低潮位与咸度超标时数相关性显著,且通过了99%的显著性水平检验,而海平面与咸度超标时数的相关关系(负相关)与理论结果不一致是受到了人为活动的影响;引起第一阶段咸度超标时数“V”型变化的主要原因是自然因素(降雨)的影响,而第二阶段咸度超标时数整体呈下降趋势的原因除了自然因素外,还包括调水压咸等人为活动的干扰。

    Abstract:

    On the basis of statistical analysis of the characteristics of salt tide intrusion changes at different time scales in Modaomen Channel from 1998 to 2015, Spearman rank correlation analysis was used to identify the correlation between discharge, sea level, mean tidal range, maximum tidal level, minimum tidal level, rainfall and saltwater over-standard time. Principal component analysis was used to determine the contribution of each factor to salt tide intrusion activities. The results show that the salt tide intrusion of Modaomen Channel during the period from 1998 to 2015 shows the characteristic of two-stage change, taking the dry season of 2004—2005 as the demarcation point. In the first stage, salinity exceeding standard hours shows a “V” type change characteristic of first decreasing and then rising, while in the second stage shows a downward trend, which is conducive to the water supply safety in estuary area. The time of salinity exceeding standard seriously mainly concentrates from December to February of next year, and the change process is basically consistent with the interannual change process. Discharge, sea level and lowest tide level are significantly correlated with salinity exceeding standard hours, and pass 99% significance level test. While the correlation between sea level and salinity exceeding standard hours(negative correlation)is inconsistent with the theoretical results, which is affected by human activities. The main reason for the “V” type change of salinity exceeding standard hours in the first stage is the influence of natural factors(rainfall), while the overall decline of salinity exceeding standard hours in the second stage is due to the disturbance of human activities, such as water diversion for stemming salt tide, besides natural factors.

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王艺霖,苏程佳,陈晓宏,等.磨刀门水道枯水期咸潮变化趋势及成因[J].水资源保护,2019,35(2):37-43.(WANG Yilin, SU Chengjia, CHEN Xiaohong, et al. Change trend and cause of salt tide in Modaomen Channel during dry seasons[J]. Water Resources Protection,2019,35(2):37-43.(in Chinese))

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  • 收稿日期:2018-04-25
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  • 在线发布日期: 2019-03-28
  • 出版日期: 2019-03-20