本文選題：鹽水入侵 + 預(yù)測(cè)模型　； 參考：《水力發(fā)電學(xué)報(bào)》2016年11期

【摘要】：鹽水入侵是河口地區(qū)較為嚴(yán)重的環(huán)境問題,對(duì)各用途用水都有一定影響。錢塘江河口作為杭州的主要飲用水源地,近年來受鹽水入侵影響較為嚴(yán)重。雖然2D和3D數(shù)值模型在鹽水入侵方面已得到廣泛應(yīng)用,然而理論預(yù)測(cè)模型只需要較少的數(shù)據(jù)即可建立,更加快速高效。本文在Savenije一維鹽度平衡方程基礎(chǔ)上,建立了錢塘江河口(地形以指數(shù)形式衰減)漲憩和落憩時(shí)刻的鹽水入侵預(yù)測(cè)模型。我們采用2012年11月7—9日(小潮)和11月14—16日(大潮)時(shí)段的實(shí)測(cè)水文、鹽度數(shù)據(jù)對(duì)模型進(jìn)行率定和驗(yàn)證。結(jié)果表明,模型鹽度計(jì)算值和實(shí)測(cè)值吻合較好,并且通過模型計(jì)算得出錢塘江鹽水入侵長(zhǎng)度也具有一定精度。
[Abstract]:Salt water intrusion is a serious environmental problem in estuarine area, which has certain influence on water use. Qiantang River estuary, as the main drinking water source in Hangzhou, has been seriously affected by salt water intrusion in recent years. Although 2D and 3D numerical models have been widely used in saltwater intrusion, theoretical prediction models need only a small amount of data and can be established more quickly and efficiently. On the basis of Savenije's one-dimensional salinity equilibrium equation, a prediction model of saltwater intrusion in Qiantang River Estuary (whose topography attenuates exponentially) is established in this paper. We use the measured hydrological and salinity data from November 7-9 (low tide) and November 14-16 (spring tide) to verify the model. The results show that the calculated values of salinity of the model are in good agreement with the measured values, and the length of salt water intrusion in Qiantang River also has a certain accuracy through the calculation of the model.
【作者單位】： 浙江大學(xué)港口海岸與近海工程研究所;
【基金】：教育部博士點(diǎn)基金資助項(xiàng)目(2120101110108)
【分類號(hào)】：P731.2

【相似文獻(xiàn)】

相關(guān)期刊論文 前1條

1 嚴(yán)志宇,殷佩海;海上溢油蒸發(fā)過程的研究進(jìn)展[J];海洋環(huán)境科學(xué);2000年02期

，

本文編號(hào)：1858849