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1)  heat storage layer
储热层
1.
The terrestrial heat is very obvious,the heat storage layer is growing,has abundant geothermic resources and is equipped with the condition of the geothermic well to be forming.
渭河盆地北缘地质构造相对简单,地热异常明显,储热层发育,有丰富的地热资源,具备地热井成井条件。
2)  geothermal reservoir
热储层
1.
4 geothermal reservoirs can be used, and the reservoir at the lower part of Guantao formation has the highest exploration value.
可被利用的热储层有4个,最有开发利用价值的是馆陶组下段热储,该热储层顶板埋深约1100m,底板埋深约1700m,热储层厚度530~580m,含水层累积厚度158~175m,单井涌水量1500~2000m3/d,出口水温62~67℃,矿化度5000mg/L左右,具腐蚀性,结垢性弱,具较好的开发利用价值。
2.
Through analysis and study on hydro-geological condition,geothermal reservoir characterisics and geothermal field charactersitics of geothermal resource in Zhangdian area of Zibo city,on the basis of studying forming model of geothermal field,geothermal field model in Zhangdian geothermal field is established,and forming mechanism of Zhangdian geothermal field is illustrated as well.
通过对淄博张店地区地热资源形成的水文地质条件、热储层特征及地温场特征等分析研究,并对张店地热田形成模式进行了探讨,建立了张店地热田热储概念模型,阐明了张店地热田形成的机理。
3)  thermal storage beds
热液储层
4)  thermal energy storage in the same layer
同层热储
5)  reservoir [英]['rezəvwɑ:(r)]  [美]['rɛzɚ'vwɑr]
热储层
1.
This paper has studied the composing of geothermal system in East Plain of Henan province,divided the geothermal reservoir and analyzed their burying and distributing characteristics.
在平面上按照构造单元区域将河南省东部平原地热系统分为 8个亚系统 ,垂向上按照埋藏深度划分为上、中、下三个热储层 。
6)  the shallow heat reservoir
浅层热储
补充资料:热层
热层
thermosphere

    位于中间层顶(约85千米)至热层顶的地球大气区域。又称暖层。从热层底部向上,大气温度迅速增加,达到温度梯度消失时的高度,即为热层顶。热层顶高度随太阳活动变化很大,通常在300~500千米之间。热层几乎吸收了波长短于1750埃的全部太阳紫外辐射,成为主要热源,热层温度结构主要受太阳活动的支配。热层以上的空间区域称外层或外逸层。
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