序率地下水模式考慮含水層之大尺度異質性

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DC Field	Value	Language
dc.contributor.author	葉仁風	en_US
dc.contributor.author	Pat Jen-Fong Yeh	en_US
dc.contributor.author	葉弘德	en_US
dc.contributor.author	Hund-Der Yeh	en_US
dc.date.accessioned	2014-12-12T02:12:45Z	-
dc.date.available	2014-12-12T02:12:45Z	-
dc.date.issued	1993	en_US
dc.identifier.uri	http://140.113.39.130/cdrfb3/record/nctu/#NT820515008	en_US
dc.identifier.uri	http://hdl.handle.net/11536/58465	-
dc.description.abstract	傳統上預測污染物傳輸的水文地質模式均假設延散現象依循Fick's定律; 濃度的分佈一般以傳流-延散方程模擬之。水文地質學家近年來認知在尺度上的不同會導致傳輸現象的改變:傳流-延散方程雖在實驗室証明其成立,但不代表必可應用於現場。在自然含水層中,導水係數的空間異質性被認為是影響污染物傳輸最主要的因子;許多的序率地下水模式,以隨機程序的理論為基礎來量化此因子對傳輸的影響,陸續的在近二十年中被提出。存在大尺度異質性的情況下,對地下水流及溶質傳輸的影響,以及將此含水層特徵溶入序率模式之需性。 Most hydrogeological models for the predictiono a prior reason to believe that the equation is valid at all field situations. pore scale dispersion, the large-scale spatial of hydrulic conductivity has been recognized by Gelhar and co-workers is applied to	zh_TW
dc.language.iso	en_US	en_US
dc.subject	序率;異質性;趨勢	zh_TW
dc.subject	Stochastic;Heterogeneity;Trend	en_US
dc.title	序率地下水模式考慮含水層之大尺度異質性	zh_TW
dc.title	Stochastic groundwater models with large-scale trend of aquifer' s hydraulic property	en_US
dc.type	Thesis	en_US
dc.contributor.department	環境工程系所	zh_TW
Appears in Collections:	Thesis