| 1. | The reservoir rock can be of various lithological compositions .
热储岩体的岩石成份各式各样。 |
| 2. | Heat losses from the reservoir by heat conduction cannot be prevented .
热储通过热传导的热损耗是无法阻挡的。 |
| 3. | Steam is formed if the boiling point pressure for the temperature of the reservoir is reached .
如果达到对应于热储温度的沸点压力，就会形成蒸气。 |
| 4. | Within the rock which forms the highly permeable reservoir convection currents of hot water or steam occur .
在形成高渗透性热储的岩体内，存在水或蒸汽的对流运动。 |
| 5. | The heat exchange with the reservoir is good and the temperature difference is only small between the bottom and top of the reservoir .
热储内部的热交换良好，热储顶部和底部的温度差极小。 |
| 6. | The heat contained in a natural steam field is exploited by drilling a suitable number of wells down to the reservoir .
天然蒸气田所含有的热能可以通过钻井的方法，即打适当数量的井孔到达热储的方法进行开采。 |
| 7. | Utilizing heat and water - storage functions of the pipeline , the buffering hot water tank has been eliminated
利用管路蓄热储水功能，省略了缓冲热水箱。 |
| 8. | This paper indicates that the occurrence characteristics of geo - thermal resources in the research area appears layer - like , immediately controlled h geothermal field , and handing - like , controlled by tectonic conditions
摘要地热资源赋存特征为层状热储及带状热储，层状热储受地温场的直接控制，构造条件控制带状热储的分布及出露。 |
| 9. | A lot of results are made from calculating of case for geothermal reservoir property of earth energy within 200 2000 ( m . ) ， it is helpful to analysis influence of permeability coefficient , kinematic viscosity and thermal diffusion coefficient of soils and rocks on heat transfer performance
在地表热能热储物性为200 - 2000 ( m . )的范围内进行的理论计算，得到了许多重要结果，为分析岩土层渗透系数、流体运动粘度和导温系数等对传热量的影响打下了良好基础。 |
| 10. | For a soil or rock of water - lacked , a heat transfer theoretical model is developed , which is a steady or unsteady , the results show that reservoir temperature , thermal diffusion coefficient , inlet temperature , flow rate of and run time of ground source heat pumps have an effect directly on heat transfer process of dhe . it can deduce that intermit running is favorable for this type of soils and rocks
对于贫含水地下岩土层建立了稳态与非稳态传热的理论模型，分析结果表明，岩土层的热储温度、导温系数、埋地换热器进水温度、流量以及地源热泵系统的运行时间或开停机比，都对埋地换热器的传热过程产生直接影响，可以推断，对于该类型岩土层的地源热泵系统，采用间歇运行将是有利的。 |
