space of dissolution 中文意思是什麼

space of dissolution 解釋
溶解空隙
  • space : n 1 空間;太空。2 空隙,空地;場地;(火車輪船飛機中的)座位;餘地;篇幅。3 空白;間隔;距離。4 ...
  • of : OF =Old French 古法語。
  • dissolution : n 1 分解,分離。2 溶解(作用),融化,液化。3 (婚約等的)取消,(職務等的)解除,(法律等的)廢...
  1. The saying about “ realize the mind consciousness ” in buddhism means to realize all the earthly phenomena, such as space, time, psychological, physiological, physical, social, natural and so on, all the anti - conversion phenomenon are nothing but the position changes of causes and reasons, changes in composition, differences in types, and then the consequence are the phenomenon of dissolution - composition, composition - dissolution, and combine - dismiss, dismiss - combine

    佛教所說的悟境,既是悟出世間的一切現象,空間的、時間的、心理的、生理的、物理的、社會的、自然的,凡是現象的起滅轉換、無非是由於因及緣的位子的變動,成份的增減,類別的出入,而產生的離合、合離及組成、解散,解散了再組成的現象。
  2. The first is the depression karst development pattern from dissolution of karst hill during indo - chinese epoch which is the key period for forming space of the reservoir

    其中印支早燕山期裸露巖溶屬溶丘(梁)窪地型巖溶發育模式,是儲集空間形成的重要時期。
  3. Therefor, in the light of theory and methods of karst hydrogeomorphology and the knowledge of transformation, balance and variation of matter and energy in karst drainage basin, we can examine stone forest within a specific scope of time and space, and reveal the mechanism and the development model of stone forest with the help of the principle of the mutual response processes among base - level, water flow and forms. just based on the understanding above, the paper, with a special reference to the lunan stone forest which is the best developed one in china, discusses the hydro - geomorphlogical structure of the bajiang river, geomorphological types and spacial distribution feature of the stone forest, and studies the erosion rate on the top of stone forest, soil erosion rate, sub - soil dissolution rate and their combined influences on the evolution of stone forest, furtherly brings forward and demostrates the " tri - level erosion " mechanism for the development of stone forest

    正是基於這種認識,本文以我國石林發育最完美的路南石林為研究對象,研究了巴江喀斯特流域的水文地貌結構特徵、石林的形態類型及其空間分佈特徵;探討了石柱頂部的剝蝕速率( a ) 、表土剝蝕速率( s ) 、土下溶蝕強度( c )及其組合對石林發育的影響,提出並論證了路南石林發育的「三重剝蝕」機制;通過對石林發育必備條件的剖析,以及對巴江喀斯特流域演變階段的定量研究、水文地貌系統的空間耦合分析,探討了巴江喀斯特流域的演變與路南石林發育間的關系,並結合該流域的演化史,提出了巴江喀斯特流域演變與路南石林發育的模式。
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