A Study of Upper Crust Temperature Variation by Fourier Series

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dc.contributor.author鄭懌zh_tw
dc.date.accessioned2014-10-27T15:24:50Z
dc.date.available2014-10-27T15:24:50Z
dc.date.issued1989-06-??zh_TW
dc.description.abstract表層地殼之溫度變化會受到氣候因素的影響，其熱態之微分方程式可用傅式級數加以分析求解。所得之結果與一般所用之三角函數或拉普拉斯轉換法比較，有很高之 相容性。 用傅式級數分析法所得之解擴大了熱傳導方程式解之涵蓋範圍，同時也可獲得簡明而完整之物理意義。zh_tw
dc.description.abstractAn alternative mathematical method for solving the differential equation re-lating to the thermal state of the upper crust influenced by the climatic variation can be achieved by. employing the Fourier series method. The solution derived from this method is compatible to the analytical solution with a Laplace transform. This method can broaden the scope of the solution of heat conduction equation and gives an explicit and complete interpretation.en_US
dc.identifier84291358-D889-3BD2-2FB1-13B06E75E205zh_TW
dc.identifier.urihttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/17371
dc.language英文zh_TW
dc.publisher國立臺灣師範大學研究發展處zh_tw
dc.publisherOffice of Research and Developmenten_US
dc.relation(34)，313-321zh_TW
dc.relation.ispartof師大學報zh_tw
dc.subject.other上部zh_tw
dc.subject.other地穀zh_tw
dc.subject.other傅氏級數zh_tw
dc.subject.other溫度變化zh_tw
dc.titleA Study of Upper Crust Temperature Variation by Fourier Serieszh-tw
dc.title.alternative上部地穀溫度變化之傅氏級數分析zh_tw

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