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首页> 外文期刊>Hydrology and Earth System Sciences Discussions >Impact of the Three Gorges Dam, the Southa??North Water Transfer Project and water abstractions on the duration and intensity of salt intrusions in the Yangtze River estuary
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Impact of the Three Gorges Dam, the Southa??North Water Transfer Project and water abstractions on the duration and intensity of salt intrusions in the Yangtze River estuary

机译:三峡大坝,南水北调工程和取水对长江口盐分入侵持续时间和强度的影响

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pstrongAbstract./strong This paper assesses the impacts of the Three Gorges Dam, the Southa??North Water Transfer Project and other water abstractions on the probability of long-duration salt intrusions into the Yangtze River estuary. Studies of intrusions of saltwater into estuaries are typically constrained by both the short duration of discharge records and the paucity of observations of discharge and salinity. Thus, studies of intrusions of saltwater into estuaries typically seek to identify the conditions under which these intrusions occur, using detailed observations for periods of 20a??60 days. The paper therefore first demonstrates a method by which to identify the conditions under which intense intrusions of long-duration occur and then applies that method to analyse the effect of the three projects. The paper constructs a model of the relationship between salinity and discharge and then employs Monte Carlo simulation methods to reconstruct the probability of observing intrusions of differing intensities and durations in relation to discharge. The model predicts that the duration of intrusions with chlorinity ≥ 250 mg Lsupa??1/sup (or ≥ 400 or 500 mg Lsup−1/sup) increases as the number of consecutive days with discharge ≤ 12 000 msup3/sup ssupa??1/sup (or ≤ 8000 msup3/sup ssup−1/sup increases. The model predicts that in 1950a??2014, the number of consecutive days with chlorinity ≥ 250 mg Lsupa??1/sup averaged 21.34 yrsupa??1/sup; if the three projects operate according to their normal rules, that average would rise to 41.20 yrsupa??1/sup. For a randomly selected year of discharge history from the period 1950a??2014, under normal operating rules for these projects the probability of an intrusion rises from 0.25 (for 30-day intrusions) or 0.05 (for 60-day intrusions) to 0.57 or 0.28, respectively./p.
机译:> >摘要。本文评估了三峡大坝,Southa?North调水工程和其他取水措施对盐长期浸入长江口的可能性的影响。盐水侵入河口的研究通常受到排泄记录持续时间短以及排泄和盐度观测缺乏的限制。因此,对海水侵入河口的研究通常试图通过使用20到60天的详细观测来确定这些入侵发生的条件。因此,本文首先演示了一种方法,该方法可用来识别长时间持续强烈入侵的条件,然后将该方法应用于分析这三个项目的效果。本文构建了盐度与排放量之间关系的模型,然后采用蒙特卡洛模拟方法来重建观察到与排放量有关的强度和持续时间不同的入侵的概率。该模型预测,氯的入侵持续时间为≥ 250 mg L a ?? 1 (或≥ 400或500 mg L &min ;; 1 )随着放电的连续天数增加而增加。 12000 m 3 s a ?? 1 (或≤ 8000 m 3 s − 1 增加。该模型预测,在1950a?2014年,氯含量为≥ 250 mg L a ?? 1 的连续天数平均为21.34 yr a ?? 1 ;如果这三个项目按照正常规则运行,则平均值将上升到41.20 yr a ?? 1 。对于从1950a ?? 2014年期间随机选择的排放历史年份,在这些条件下,这些项目预测入侵的可能性分别从0.25(对于30天的入侵)或0.05(对于60天的入侵)分别增加到0.57或0.28。

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