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淮南矿区地热地质特征与地热资源评价     地温梯度  现今地温场  热导率  大地热流  地热资源  淮南矿区       font style='font-size:12px;'> 2019/9/29
为了探索淮南矿区地热地质特征和矿井深部热害防治对策,系统收集和分析了淮南矿区钻孔井温测井资料,基于近似稳态测温数据,拟合了测温孔孔底温度校正曲线,对简易井温测井钻孔孔底温度进行了校正;采用浅钻孔测温法,对井下巷道围岩温度进行了测定;
地热田高地温异常成因机理及温度分布特征     地热甜点  热传导  构造运动  新能源  岩浆囊       font style='font-size:12px;'> 2018/4/11
在地热研究中地热田高地温的形成原因、为何地热田深部会出现低地温梯度等说法不一, 未有定论。本文对前人所提出的地温场影响因素逐一进行了分析, 采用地热场正演模拟手段, 对有异常热源供热-岩浆囊和无热源的热传导两种情况进行了研究。认为多数异常热源如岩浆囊, 相对于地质演化时间尺度而言, 其冷却速度较快, 并不能直接为地热田供热; 寻找地热田主要在浅部有一定厚度的好的热盖层和深部有高导层的区域进行; 构...
为研究地埋管换热器在不同岩性地层的换热情况,在鲁西黄河冲洪积平原、山前冲洪积平原和低山丘陵区进行了以粉土、粉质粘土、细砂,粘土、粉质粘土、中粗砂,灰岩和花岗岩为研究对象的热响应试验,初步试验结果表明:每延米换热量(W/m)和平均热导率(W/m·k)花岗岩>灰岩>粉质粘土、中粗砂>粉土、粉细砂。在岩溶地下水富水性强,径流速度快的地段灰岩平均热导率>花岗岩。此项研究结果可为不同岩性地层浅层地温能开发利...
Due to energy shortage and increasing environmental awareness, resources in shallow underground space have been rapidly exploited and utilized. So that studying variation characteristics of geothermal...
Fault has an important influence on the storage and movement of geothermal water. The Zhangzhou Basin is wholly located in a granodiorite rock mass. Due to the low permeability of granodiorite, faulte...
In the process of geothermal exploitation and utilization, the reinjection amount of used geothermal water in super-deep and porous reservoir is small and significantly decreases over time. This has b...
In this paper, the single hole heat transfer power of the ground source heat pump system in Hengshui is compared with data gained from thermal response test. The results show that maximum monitoring d...
In the enhanced geothermal systems wells, casing temperature variation produces casing thermal stresses, resulting in casing uplift or bucking. When the induced thermal stresses exceed casing material...
his paper elaborates the chemical constituent change principles of deep geothermal fluid during the process of upward movement. It summarizes research methods of hydrochemistry, isotope and numerical ...
Before 1985, there were a few Chinese participators for International Association of Hydrogeologists which founded in 1956. The Chinese team composed of senior hydrogeologists attended the 17th and 18...
海洋热流数据是开展海洋地球动力学研究和油气资源评价的基础数据.为深入认识琼东南盆地的地热特征,本文首先利用耦合沉积作用与岩石圈张裂过程的数值模型分析了张裂型盆地主要地热参数的垂向变化特征;并通过钻孔资料的详细分析,获得了琼东南盆地44口钻孔的热流数据;结合海底地热探针获取的热流数据,对琼东南盆地地热特征及其主要影响因素进行了简要分析.结果表明:沉积作用的热披覆效应对表层热流有较明显的抑制作用,由于...
Biochar is the carbon-rich product obtained when biomass, such as wood, manure or leaves, is heated in a closed container with little or no available air. In more technical terms, biochar is produced ...
Earth's surface heat flux     Earth's surface  heat flux       font style='font-size:12px;'> 2014/12/31
We present a revised estimate of Earth's surface heat flux that is based upon a heat flow data-set with 38 347 measurements, which is 55% more than used in previous estimates. Our methodology, like ot...
扫描式F-P干涉仪在MERINO观测中的热层风结果与分析     MERINO  FPI  热层  水平风  误差分析       font style='font-size:12px;'> 2014/12/19
MERINO是沿120°E/60°W子午圈的全球联网观测项目,热层中性风是其中一个十分重要的观测参数.本文介绍了武汉大学扫描式F-P干涉仪(SFPI)及其在MERINO第一轮观测中的结果,并与同站点的流星雷达在98 km高度上的测风数据进行了验证,分析表明两台设备的吻合性很好,SFPI风速测量的误差分别为8 m·s-1(557.7 nm)和7.8 m·s-1 (630.0 nm).本文对地基扫描式...
基于全天空F-P干涉仪反演热层垂直中性风     垂直中性风  全天空FPI  热层       font style='font-size:12px;'> 2014/12/19
由于测量与计算的难度,对热层垂直中性风的观测还很不够,这影响了人们对热层及热层-电离层耦合的认识.本文基于全天空法布里-珀罗干涉仪(FPI)对热层风场的观测,提出了一种反演垂直中性风的方法.利用该方法,对北极黄河站全天空FPI观测数据进行了垂直中性风的反演计算,结果表明,高热层与低热层的垂直风平均幅值分别在40 m·s-1和15 m·s-1,且垂直风日变化表现出明显的时间演变特性,且与地磁ap指数...

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