Well measurement technique is briefly presented on Marine geothermal flow.
本文对海洋地热流的井下测量技术进行了扼要的阐述。
In region of larger relief, the observed value of geothermal flow must be corrected for terrain.
在地形起伏较大地区，热流的实例值必须校正。
The technology of geothermal flow detection is of great importance for researches on Marine crustal movement, disaster prevention and reduction and detection of gas hydrates.
热流探测技术的应用对研究海洋地壳活动规律、防灾减灾与天然气水合物新能源探测具有重要意义。
In mine geothermal prediction, the instable heat transfer coefficient is an important parameter for heat transfer (between country rock and air flow) computation.
在矿井地热预测中，矿井风流与围岩之间的非稳定传热系数是传热计算的重要参数。
The schematic flow of low temperature geothermal fluids through a power station in Italy is presented in example B.
例子B是意大利一个电站利用低温地热流体的流程示意图。
Geothermal water resource can be assessed by the abnormity degree of geothermal and thermal flow quality.
地下热水的评价因子为地热异常程度及热流体质量。
Basin basement palaeo-heat flow is a basic boundary parameter condition to realize basin geothermal field simulation.
盆地基底古热流是实现盆地地热场模拟的基础边界参数条件。
The vertical flow of underground thermal fluid resulted from the opening fracture is the important cause of geothermal anomaly.
开启断裂造成的地下热流体的垂向流动是造成地下热异常的重要原因。
The general aspect of the geothermal field is distributed as follows both terrestrial heat flow and geothermal gradient or stratigraphic temperature show high in inner part of basin and…
分析了盆地的地温场高的主要因素以及地温场与岩石圈、重磁力场的关系。
The principle of determining thermal conductive factor of original formation through microdifference temperature is conservation of energy(equal density of geothermal heat flow).
利用微差井温确定原始地层的导热系数，基于能量守衡（地热流密度相等）这一原理。
The Model GHT-1C Geothermal Heat Flow Transducer measures directly, local heat fluxes in the earth.
进口工业网的GHT-1C型号低热量传感器测试土壤中直接的、局部的热通量。
This paper discussed the design criteria of material selection, the area of single unit, flow path, flow rate of a plate heat exchanger (PHE)in a geothermal heating system.
重点分析了板式换热器在地热供暖系统中材料、单片面积、流程、流道、流体流速等选取的原则；在综合考虑技术、经济、环境效益及节能的基础上，论述了对板式换热器优化设计的方法。
The mantle heat flow controlled regional geothermal field, the magmatic heat flow controlled high geothermal field in the local areas, the shear heat flow created by tectonic activity made a not...
指出地幔热流是控制区域性地热场的主要因素，岩浆热流控制了局部高地热场的分布，构造活动产生的剪切热流对俯冲带及剪切带的瞬时古地热场有重要影响。
The mantle heat flow controlled regional geothermal field, the magmatic heat flow controlled high geothermal field in the local areas, the shear heat flow created by tectonic activity made a not...
指出地幔热流是控制区域性地热场的主要因素，岩浆热流控制了局部高地热场的分布，构造活动产生的剪切热流对俯冲带及剪切带的瞬时古地热场有重要影响。
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