新型同径分层止水工艺在地热探采深井的应用          下载免费PDF全文

杨联锋  段云星 《探矿工程》2021,48(8):33-39

原平大营地热探采结合深井完钻井深3088 m,为探明494~3088 m变质岩地层的水文地质参数和水源补给情况,基于岩心和测井资料划分4个抽水试验段,且试验后需要恢复目的含水层。根据“一孔同径分层止水”原则,设计了管内止水托盘止水、管外止水伞止水的新型同径分层止水工艺。该工艺简化了井身结构,避免了管外投粘土球、注水泥等堵塞含水层的情况。现场实施表明,该工艺止水效果完全满足水文地质抽水试验要求,可为同类工程提供经验和借鉴。  相似文献   

沧县隆起中段献县凸起和阜城凹陷岩溶型地热资源特征     

黄旭  沈传波  杜利  魏广仁  罗璐  唐果 《现代地质》2021,35(4):997-1008

为探究华北平原的岩溶热储分布规律,以及如何高效开发利用献县凸起和阜城凹陷地热田的地热资源,结合前人研究成果与已有地热井的测井、地震、水化学等资料,分析了岩溶热储分布规律以及献县凸起和阜城凹陷地热田的四大要素即“源、储、通、盖”等地热地质条件,建立了地热田概念模型,并精细评价了地热资源量。研究表明地热田是形成于渤海湾盆地新生代伸展断陷背景下的受深大断裂控制的传导型地热田,主要以大气降水为补给水源,深大断裂和岩溶不整合面为水运移通道。来自太行山和燕山的水再补给、汇聚,在献县凸起及阜城凹陷岩溶热储中富集,形成中-低温传导型地热系统,具有良好的盖层以及高达3.63~5.31 ℃/100 m的地温梯度。蓟县系岩溶热储顶板埋深1 400~1 500 m,有效厚度累计336.1 m;奥陶系岩溶热储顶板埋深2 000~2 500 m,有效厚度累计55.3 m。献县凸起地热田蓟县系岩溶热储可采资源量3.75×10⁹ GJ,折合标煤1.28×10⁸ t,年开采地热资源量可满足供暖面积4 523×10⁴ m²;阜城凹陷奥陶系岩溶储可采资源量0.80×10⁹ GJ,折合标煤0.27×10⁸ t,年开采地热资源量可满足供暖面积954×10⁴ m²。献县凸起及阜城凹陷地热田开发潜力巨大。  相似文献   

Fracture Characteristics and Heat Accumulation of Jixianian Carbonate Reservoirs in the Rongcheng Geothermal Field, Xiong’an New Area     

WANG Yingjin  MA Feng  XIE Heping  WANG Guiling  WANG Zhihe 《《地质学报》英文版》2021,95(6):1902-1914

Geothermal energy plays an important role in urban construction of the Xiong’an New Area. Geothermal reservoir fracture distribution of the Mesoproterozoic Jixianian Wumishan Formation (Fm.) carbonate reservoir in the Rongcheng geothermal field are evaluated based on FMI log from Wells D19 and D21. The results show carbonate reservoir fracture density of Well D19 is 15.2/100 m, greater than that of Well D21 with a value of 9.2/100 m. Reservoir porosity and permeability of Well D19 are better than that of Well D21, and the water saturation is bimodally distributed. The movable fluid volume ratio (BVM) of Well D19 is 2% to 8% with some zones exceeding 20%, while the value of Well D21 is less than 4%. Therefore, reservoir fractures in Well D19 are more conducive to fluid flow. Reservoir fractures have a similar occurrence to normal faults, indicating that the tensile stress field controlled the formation of such fractures. Developed reservoir fractures provide a good channel for groundwater convection. The circulation of regional groundwater and the heat exchange between water and rock and the multiple heat accumulation patterns form a stable and high potential heat reservoir in the Rongcheng geothermal field.  相似文献   

Genesis of Geothermal Fluid in Typical Geothermal Fields in Western Sichuan,China     

ZHAO Jiayi  WANG Guiling  ZHANG Cuiyun  XING Linxiao  LI Man  ZHANG Wei 《《地质学报》英文版》2021,95(3):873-882

The hydrogeochemical characteristics of geothermal fluids can reveal the genesis of geothermal systems and act as important references for developing and using geothermal resources.This study presents hydrogeochemical processes and thermal cycle mechanisms of typical geothermal fields in Western Sichuan.Based on the geological conditions in Western Sichuan,29 hot springs in three geothermal fields in the Batang and Litang areas were selected for hydrochemical and isotopic (δD andδ~(18)O) analyses.Furthermore,the temperature of the thermal reservoir was calculated and the upflow cooling process of the hot springs was analyzed.Most of the subterranean hot waters in Batang and Litang are of the HCO_3-Na hydrochemical type.The ion variation in Batang is primarily affected by water-rock interactions.There is a strong positive correlation between Na~+,B~-,and Cl~-in Litang,suggesting that they have the same material source.The Na~+and metaboric acid content is relatively high,which indicates that the groundwater runoff in both areas is relatively long-lasting,with reduced flow velocity;moreover,the metasilicic acid content is relatively high,which supports this conclusion.Both hydrogen and oxygen isotopes plot near the atmospheric precipitation line,indicating that groundwater recharge is functionally obtained from precipitation.The calculated thermal storage temperatures in Batang and Litang were 88–199°C and 96–154°C,respectively.The proportion of cold water mixing in Batang was 64%–67%,while that in Litang was 60%–68%.According to the calculated results,the initial thermal cycle depth of the Batang area (4540–4780 m) was greater than that of the Litang area (3150–3960 m).The enthalpy of the deep parental geothermal fluid in Batang was 1550 J/g with a Cl~-concentration of 37 mg/L,while that in Litang was 2100 J/g with a Cl~-concentration of 48 mg/L.  相似文献   

山东省菏泽凸起地热田岩溶地热水水化学水平演化特征   总被引：1，自引：0，他引：1  

史启朋  宋帅良  孟甲  郑慧铭 《中国岩溶》2021,40(2):310-318

在前人研究成果的基础上,选择A-A′和B-B′两条路径,采用Piper三线图解、Schoeller图解、Na－K－Mg平衡图解、饱和指数计算评价等方法,研究山东菏泽凸起地热田地热水沿路径上的循环演化特征。结果表明:沿A-A′、B-B′剖面岩溶冷水→岩溶热水,水化学类型由SO4.HCO3－Ca.Mg.Na或SO4.HCO3－Ca.Mg向SO4－Ca.Na或SO4－Ca演化,矿化度逐渐增大,HCO3-浓度逐渐减少,SO42-、Ca2+、K+浓度逐渐增大,反映出岩溶冷水向岩溶热水演化的补给特征;水化学三线图上岩溶冷水、热水处在不同的区域,显示岩溶冷水向岩溶热水演化补给;距补给区由近到远,水岩作用程度逐步提高,饱和指数逐渐增大,岩溶地热水溶滤作用增强。   相似文献   

热红外遥感技术在江西寻乌地区地热勘查中的应用     

任正情  方泓锦  王学平 《江苏地质》2021,45(3):277-282

热红外遥感是地热资源勘查中的常用技术,对江西寻乌地区的Landsat 8热红外影像采用单窗算法,根据MODIS影像计算大气水汽含量,并逐步获取反演参数,得到地表温度反演结果;利用MOD11_L2地表温度产品对结果进行对比分析,验证反演有效性。通过对已有地热资料和地质构造背景的研究,总结地热形成的有利构造条件,分析地表反演温度与已有地热及断裂构造之间的空间关系,建立地热异常区圈定依据,并剔除假异常,最终在研究区圈定了11个潜在地热异常区,为该区地热勘查提供依据。  相似文献   

计算多年冻土上限深度的地温法     

苑秀慧 《冰川冻土》1989,(3)

本文以大量实测资料为基础,探讨了季节融化层导温性能及地温峰值滞后等自然因素对多年冻土上限深度的影响。还通过地表面的热效应和气温脉动的研究,讨论了多年冻土上限深度的小区域特点和未来期望值。提出了适合青藏高原多年冻土区计算多年冻土上限深度的半经验公式。由于主要依据是地温的分布和传导特征,故称之为“地温法”。  相似文献   

渤海陆缘地震的力学特征和成因   总被引：5，自引：1，他引：5  

张之立  邓玉琼 《地球物理学报》1989,32(4):470-477

渤海陆缘是华北强震活动区,如1966年的邢台震群,1967年的河间地震,1969年的渤海地震,1975年的海城地震,1976年的唐山震群和1983年的菏泽地震,都是在该区发生的。显然,深入研究该地区的构造运动和地震成因是有重要科学意义的。本文拟从应力场角度进行研究。  相似文献   

1988年四川八美5级地震参数和前兆的研究     

程万正 《地震研究》1989,12(3):234-240

本文对1988年6月四川省道孚八美(即乾宁)4.5、5.0、4.0级地震前后地震活动进行了研究,给出了地震参数、P波初动解、余震序列和前兆变化的分析及未来地震危险性的讨论。  相似文献   

新疆乌鲁木齐地区地震水化震例深入剖析     

蔡仲琼 《内陆地震》1989,3(3):230-239

本文在水化前兆清理研究的基础上,采用统一的异常判别方法,应用适合本地区的“异常可靠性评价标准”,对新疆乌鲁木齐地区150km范围内的中强地震和反例事件进行了深入剖析,对水化异常与地震三要素的关系进行了统计分析。研究结果是制定地震水化异常判据和定量化指标的基础。  相似文献