苏北盆地典型地区中低温地热流体地球化学特征研究

苏北盆地作为江苏省地热地质条件最优的地区,发育丰富的中低温地热资源.文章选择存在已探明的中温地热井及干热岩验证孔所在的盆地区作为研究区,利用地热流体携带的地球化学信息,了解深部地热储层基本特征及不同深度地热资源的成生关系.结果表明:研究区地热流体中优势阳离子为Na+,阴离子呈复合离子型,以Cl-为主,Na+、TDS与C...     

地热水资源开发与环境保护

作为巨大的清洁能源,地热水资源已被大量开发及利用。但是清洁能源并不清洁,其由地下深处带到地表的一些化学物质等对地面环境势必造成严重的负面影响即危害。在介绍了地热水资源概况及开发利用现状基础上,对地热水资源开发及利用所带来的环境及环境地质问题进行了简单的介绍,特别是地面沉降、热污染及地热水资源衰减等,并分析了这些环境地质问题产生的机理。对地热水资源开发利用中存在的问题做了简要总结,并为地热水资源的合理开发、科学利用及可持续发展提出加强勘查评价工作,提高利用效率等五余个建议和对策。     

山东省临清市地热资源评价和开发利用方案建议

山东省临清市近年来在市区范围内陆续发现地下热水。本文首先通过区域地热地质背景分析、地热调查工作,建立了临清市地热概念模型。在概念模型的基础上,利用体积法计算了热储层的热水静储量,并对地下热水进行质量评价。提出了地热开采、利用方案。     

河北阳原县三马坊地区温泉井成井工艺探讨

河北省阳原县三马坊地区地热资源条件优越,该地区多年来施工温泉井较多,但成功者无几,即使成井亦无法实现井口关闭,造成资源浪费。工程实践中通过分析以往成井存在的问题,采用了三开成井的施工工艺。通过准确把握一开深度,将273mm表层套管下入至高压热储层上部的稳定隔水段后水泥封固,经试压检验确保管外封闭牢固;二开通过加大泥浆比重力求平衡钻进,钻进后期以涌水限量为依据准确把握时机抢下219mm技术套管;三开以安全钻进为前提,以涌出颗粒大小为依据,采用清水钻进适时完井,从而实现增产。最终本井顺利完工,井口安全关闭。     

地热深水井蓬堵事故的处理及预防

通过对一起地热深水井常见事故类型：填砾或投放止水泥球、固井石子发生的蓬堵事故原因的分析,提出了正冲、反吸排渣处理蓬堵事故的工艺及预防措施。并简要介绍了处理该类事故所需的机具及工艺。     

PDC钻头在天津地热井中的应用

天津地热钻井,一般采用传统的三牙轮钻头进行施工,近年来随着钻井工艺水平的进步,为了提高钻井效率,在部分井段中采用PDC钻头钻进,相比三牙轮钻头取得了更高的机械钻速,且泥岩地层造浆得到很好的控制,钻井液性能稳定,降低了维护成本。实践证明,PDC钻头使用寿命长,在提高钻进效率的同时经济效益显著。     

福州地热田人工回灌模式的探讨

采用人工回灌方法是保持地热田长久不竭,长期利用的必要技术手段,通过运用地热中心带回灌模式对福州地热田进行回灌试验．总结了福州地热田人工回灌特点,并对影响回灌的各种因素进行分析探讨。     

基于Intranet的地热地理信息系统的设计与实现

通过建立Intranet网络及地热地理信息系统,为地热资源的可持续开发利用提供帮助.该系统具有数据存储、数据查询、数据更新功能,涉及资源管理、技术开发、开采监测等三个方面;具有空间查询及分析功能,图形信息与属性信息可以相互查询,也可以独立查询,空间分析功能包括资源量计算、资源开发评价等;自动制图功能,可自动绘制井身结构图、地层柱状图等多种标准图.     

Geochemical survey of thermal system in Northeast China and their geothermometric characters

The chemical composition of several thermal springs around Changbaishan area has been investigated.Cenozoic basaltic rocks are widely distributed in Northeast China and geothermal characteristics have been described.About one hundred hot springs exist around Changbaishan Volcano at the border between China and D.P.R.Korea with high temperature about 82℃. The pH values of the spring water range from 6.9 to 7.1 and the total flow rate is about 4.8 L /sec. The chemical composition of the thermal springs is sodium carbonate; the high-mineral contents of thermal water are believed to have medicinal properties. Bathhouses are already built along the hot springs to take the advantage of the supposed healing properties. The high quality of those hot springs is believed to be utilitized for mineral water. The chemical equilibrium temperatures were estimated at about 160℃ based on the Na-K-Ca geochemical thermometer.     

A geochemical survey of thermal springs in western part of Republic of Yemen and their geothermometric characteristics

The high-mineral contents of some thermal waters are believed to have medicinal properties. Numerous spas and bathhouses might be built at these hot springs to take advantage of theses supposed healing properties such as skin diseases, rheumatism and so on. This paper is to find thermal reservoir and to classify the kinds of water. The majority of thermal springs are found discharging from igneous centers of Tertiary and Quaternary volcanic fields of the western Yemen (research area). Structurally these volcanisms are connected to N-NW faults that are parallel to the main Red Sea trend. Temperature and pH values of the thermal spring range 37℃～96℃, and 6.3 ～8.7 respectively. The Yemeni thermal waters indicate high variability in composition since they are ofNa (K) -C1, Na-HCO3 and Ca (Mg) -SO4 types, whereas the surficial waters have the typical worldwide Ca (Mg) -HCO3 composition. Different liquid phase geothermometers,such as SiO2, K2/Mg and Na/K. Estimated reservoir temperatures ranging 70 ～ 140℃ perform equilibrium temperature evaluation of the thermal reservoirs.