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thermal plume meaning in English

热卷流
热烟流
热烟羽
热柱

Examples

  1. His pioneering work on the statistical behavior of individual thermal plumes led to the discovery that active and passive scalars share statistically similar features , which have been praised by his peers as " important to the field of turbulence in fluids " and " shed an original light on rayleigh - benard convection problem "
    他在研究单个热羽流的统计行为方面进行了开创性的工作,并发现主动标度量和被动标度量具有相似的统计性质。此成果被同行誉为对湍流领域的重要贡献以及对瑞利-伯纳德湍流对流做出了原创性的贡献。
  2. By physiognomy feature , it could be divided into three types of thermal structure : positive dome model , negative collapse model and border dome core collapse model . based on the depth degree or magma - thermal influenced , it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model , superficial volcano eruption hydro - thermalism and hypabyssal intrusive model , thermal anticline ( thermal dome ) model , mid - deep intrusive model , deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure . there are many interaction system could be induced into a systematic thermal interaction , include : ocean - continent system , basin - mountain interaction , superficial and mid - deep crust - mantle interaction , crust - mantle commingle interaction , vertical thermal interaction ( delamination ) etc .
    依据地貌形态分为三类:正向穹窿型、负向塌陷型、边隆核陷型:依据岩浆-热力作用影响的深浅程度或深度分为五类: (古)地热异常群集区、表浅层火山喷发-热液活动与浅成侵入型、热力背斜(热穹窿) 、中深层侵入型、深部地幔(地壳)热柱型;提出了热力构造作用空间分布的理想模式,将洋陆系统、盆山作用、浅表与中深部壳幔作用、壳幔混合、垂向热力作用(拆沉)等纳入一个整体统一的热力作用系统中,为盆地动力学研究打开了一个新窗口;研讨了热力构造研究方法。
  3. The results of the experiments indicate that : thermal plumes in the mantle ( i . e . mantle plumes ) should be divided into two types , vertical plumes , as mentioned traditionally , and non - vertical plumes , including those of inclined - columns , vortexes , etc . , and the former may be only a particular case of the latter ; under the condition of the coriolis force to be ignored
    在忽略科里奥利力的情况下,板块的下插和滞积下沉、岩石圈根的存在以及地幔介质粘度的非均匀分布等都可能构成不同形状的障碍导流体,导致地幔的涡旋运动。

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