共查询到19条相似文献，搜索用时 78 毫秒
1.
2.
套管钻井技术的研究是目前国内钻井技术攻关的难题,其中测井资料的采集和解释技术评价是一项很重要的技术关键,如果不能提供较准确的测井资料,会使套管钻井技术的研究工作难于开展.经过实验设计、采集、分析对比工作,总结了利用套后自然伽马、补偿中子、碳氧比等测井资料进行套管钻井测井解释评价的方法,在吉林油田部分地区推广应用,见到了较好的效果. 相似文献
3.
自然伽马测井是通过测量地层的自然伽马值,从而划分岩性,进行地层对比.自然伽马测井的优点是可以在裸眼井、套管井和高矿化度钻井液以及干孔中进行测量.在已下入套管的井内进行自然伽马测井时,影响地层自然伽马测井曲线的主要因素有套管、环形水泥等.通过套管段及套管加环形水泥段分别与裸眼段自然伽马测井曲线进行对比分析,发现套管对地层放射性的影响比较均匀,与裸眼段相比幅值降低36％左右,不影响地层放射性曲线的整体形态;套管加上环形水泥后,由于受到第四纪地层的稳定性、分选性以及固井质量等因素的影响,难以确定裸眼自然伽马测井曲线的整体形态,因此能否利用下套管井测量的自然伽马测井数据恢复地层信息,要综合考虑地层情况、井径变化、固井质量等要素. 相似文献
4.
5.
物探测井在地热开发中的应用 总被引：1，自引：0，他引：1
地热资源的开发利用愈来愈受到广泛的重视 ,本文阐述了物探测井在地热开发中的作用 ,并介绍了视电阻率、温度、套管磁测井等方法在地热开发中的应用。 相似文献
6.
为探究江苏淮安赵集岩盐矿生产井的涌水原因,通过井筒试压、声波变密度测井、井温测井、冒落带裂隙带厚度推算等方法,分析生产井注采比异常和钻井涌水原因。经测试,井筒压力稳定在70 kg/m3,声波在1 340 m处显示异常,相对声幅为33.6%,固井质量不理想;井温在1 340 m处显示异常,有流体流出,最大冒落带厚度为22.64 m,导水裂隙带厚度约为198 m。分析认为,生产井含盐系顶板垮塌形成冒落带,溶腔内的水顺着裂隙带的导水通道渗透进砂岩地层中是造成矿井涌水的主要原因;部分井段胶结水泥环脱落破碎,致使溶腔内的卤水沿套管外壁的第一界面及第二界面漏失。对已满足服务年限或已开采至矿层顶板的盐井采用潜卤泵采卤法进行生产或实施封孔作业,可以有效防止井内流体渗透;水泥环的破损,可采取增加套管壁厚、提高套管钢级及控制合理内压等措施。 相似文献
7.
8.
通过试验研究,井温测井同其它水文测井方法一样,可以确定被钻孔揭穿的含水层位置、厚度和钻孔中各含水层之间的水力联系;确定涌水层位置;确定漏水层位置;更主要的是可以解决一般水文测井方法难于解决的问题——有套管的井段和泥浆孔的含水层位置及其各含水层之间的水力联系。因此,对于富水性强,孔内不安全的钻孔可以采取先下套管,再做井温测量。若在一个地区或矿区曾系统做过井温测量,则用井温资料可以进行钻孔或剖面的含水层对比。下面着重介绍井温测井在水文地质及工程地质中的一些应用实例。 相似文献
9.
10.
11.
12.
传统的测井仪器探测深度基本在3 m以内, 大多也没有方位分辨能力, 无法实现油气井周围较大范围地层结构与构造的成像, 故不能解决隐蔽构造与油气储层的探测问题。针对上述问题, 将地表地质雷达成像技术移植到测井中, 研发了雷达成像测井仪。为提高雷达成像测井仪探测深度、方位分辨率和下井深度, 采用纳秒脉冲源与定向接收天线对井周地层进行探测和成像, 在增大探测距离的同时, 兼顾了分辨率; 采用磁环和光耦对脉冲板做隔离, 有效地压制了噪声; 通过在电路外增加保温瓶和优选耐高温元器件提高了仪器的耐高温性能; 最后利用模型井对仪器进行了测试和标定, 并在3口油井中进行了现场应用。改进后的雷达成像测井仪下井深度可达6 000 m, 最大探测深度可达12 m, 能够对井周5 m以外孔洞、裂缝进行定位和成像, 大大地拓宽了测井技术的横向预测能力。测试与应用结果表明:该仪器能够耐受油井下的高温高压环境, 探测深度大且分辨率高, 对钻孔周围地层界面、裂缝和孔洞构造成像效果较好。 相似文献
13.
14.
15.
16.
17.
The objective of this study was to assess the subsurface strata and groundwater situation of Olomoro, Nigeria using borehole logging and electrical resistivity techniques. The borehole logging consisting of resistivity and spontaneous potential logs were conducted by using the Johnson Keck logger on a drilled well in the study area. The electrical resistivity survey involving 17 vertical electrical soundings (VES) with a maximum current electrode spacing of 100 to 150 m was conducted using the Schlumberger electrode configuration. Analysis of the well cuttings revealed that the lithology of the subsurface consist of topsoil, clay, very fine sand, medium grain sand, coarse sand and very coarse sand. Results of the downhole logging also revealed that the mean electrical conductivity and the total dissolved solid of the groundwater was obtained as 390 μS/cm and 245 mg/cm3 respectively. These values are within the acceptable limit set by the Standard Organization of Nigeria (SON) for drinking water. The result of the vertical electrical sounding interpreted using the computer iterative modeling revealed the presence of four to five geoelectric layers which showed a close correlation with result from the lithology and downhole logging. Results further showed that the resistivity of the subsurface aquifer ranged between 1584 and 5420 Ωm while the aquifer depths varied between 27.8 and 39.3 m. Groundwater development of the area is suggested using the depth and resistivity maps provided in this study. 相似文献
18.
Reinhard Jung Marion Schindler Patrick Nami Torsten Tischner 《Comptes Rendus Geoscience》2010,342(7-8):636-643
The article presents a method to derive synthetic flow logs from low rate injection tests in wells, which are otherwise not accessible for logging. The tests were carried out in the 5 km deep geothermal well GPK2 in the Enhanced Geothermal System (EGS) project of Soultz-sous-Forêts (France) and were aimed at characterizing the status of the well before chemical treatments. The method consists of injecting water at constant flow rates into the well initially filled with brine. The wellhead pressure record of this test is transformed into log of the flow velocity versus depth by a technique described in the paper. Applying this method to borehole GPK2, three outlets could be detected and quantified within the cased and uncased section of this borehole. The outlet in the cased section at 3860 m absorbed 15% of the total flow. This depth corresponds to a known casing restriction, which makes the borehole inaccessible for logging operations. The two other outlets are at the casing shoe at 4420 m (15%) and at 4670 m (70%). 相似文献
19.
K. N. S. S. S. Srinivas M. Srihari Rao P. Pavan Kishore D. Gopinadh Haris Raza Kusumita Arora H. V. S. Satyanarayana 《Journal of the Geological Society of India》2018,91(5):569-574
Boreholes are the only sources for direct measurements of geological and geophysical characteristics of the shallow subsurface of the earth. Borehole imaging tool “Acoustic Televiewer (ATV)” is an advanced probe, which records 3D image of the bore hole wall and is used to obtain oriented images of bore hole and provides substantial information regarding lithology, structural information, detection of fractures and casing of the borehole. The images are highly sensitive to the presence of fractures, the delineation of which becomes accurate and reliable based on these acoustic images. Features identified on log-derived images can be correlated with core samples or can be used as substitute in the poor core recovery zones. In the present study, ATV log from a deep borehole drilled at Khadi Kolavan in Koyna-Warna region of Ratnagiri district, Maharashtra located west of the Western Ghat escarpment in the Deccan Volcanic province, India, is used for interpretation of structural characteristics of the formation. The same was correlated with other conventional logging methods such as resistivity and full waveform sonic (FWS) as well as core logging and rock quality designations (RQD) which generated new understanding of the basement and basalt cover in this region. 相似文献