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Database of petrophysical properties of the Mid-German Crystalline Rise

机译:中德晶体升高的岩石物理特性数据库

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Petrophysical properties are a key element for reservoir characterization but also for interpreting the results of various geophysical exploration methods or geophysical well logs. Furthermore, petrophysical properties are commonly used to populate numerical models and are often critically governing the model results. Despite the common need for detailed petrophysical properties, data are still very scarce and often not available for the area of interest. Furthermore, both the online research for published property measurements or compilations, as well as dedicated measurement campaigns of the selected properties, which require comprehensive laboratory equipment, can be very time-consuming and costly. To date, most published research results are often focused on a limited selection of parameters only, and hence researching various petrophysical properties, needed to account for the thermal–hydraulic–mechanical behaviour of selected rock types or reservoir settings, can be very laborious. Since for deep geothermal energy in central Europe, the majority of the geothermal potential or resource is assigned to the crystalline basement, a comprehensive database of petrophysical properties comprising rock densities, porosity, rock matrix permeability, thermal properties (thermal conductivity and diffusivity, specific heat capacity) as well as rock mechanical properties as compressional and shear wave velocities, unconfined compressive strength, Young’s modulus, Poisson’s ratio, tensile strength and triaxial shear strength was compiled from measurements conducted at the HydroThermikum lab facilities of the Technical University of Darmstadt. Analysed samples were mostly derived from abandoned or active quarries and natural or artificial outcrops such as road cuts, riverbanks or steep hillslopes. Furthermore, samples of the cored deep wells Worms 3 (samples from 2175–2195 m), Stockstadt 33R (samples from 2245–2267 m), Weiterstadt 1 (samples from 2502–2504 m), Tiefbohrung Gro?-Umstadt/Heubach, B/89–B02 and the cored shallow wells (Forschungsbohrung Messel GA 1 and 2) as well as GWM17 Zwingenberg, GWM1A Zwingenberg, Langenthal BK2/05, EWS267/1 Heubach, and archive samples of the Institut für Steinkonservierung e.V. in Mainz originating from a comprehensive large-scale sampling campaign in 2007 were investigated. The database (Weinert et al., 2020b; https://doi.org/10.25534/tudatalib-278) aims to provide easily accessible petrophysical properties of the Mid-German Crystalline Rise, measured on 224 locations in Bavaria, Hessen, Rhineland-Palatinate and Thuringia and comprising 26 951 single data points. Each data point is addressed with the respective metadata such as the sample identifier, sampling location, petrography and, if applicable, stratigraphy and sampling depth (in the case of well samples).
机译:岩石物理属性是储层特征的关键要素,但也用于解释各种地球物理勘探方法的结果或地球物理井日志。此外,岩石物理性质通常用于填充数值模型,并且通常是批判性的模型结果。尽管有常见的需求细化的岩石物理特性,但数据仍然非常稀缺,并且通常不适用于感兴趣的领域。此外,公布的房产测量或汇编的在线研究以及需要综合实验室设备的所选属性的专用测量活动,可以非常耗时和昂贵。迄今为止,大多数公布的研究结果通常集中在仅限于有限的参数上,因此研究各种岩石物理特性,需要考虑所选岩石类型或储存器设置的热液压机械行为,这可能非常费力。由于在中欧的深层地热能量以来,大部分地热潜力或资源被分配给结晶地下室,综合岩石物理性能数据库,包括岩石密度,孔隙率,岩石基质渗透性,热性能(导热率和扩散性,比热容量)以及岩石力学性能作为压缩和剪切波速,非束缚的抗压强度,杨氏模量,泊松比,巨型模量,抗拉强度和三轴剪切强度由Darmstadt技术大学Hydrothermikum实验室设施进行的测量编制。分析的样品主要来自遗弃或积极的争吵和自然或人工露头,如道路切割,河岸或陡峭的山坡。此外,核心深井蠕虫的样品3(来自2175-2195米的样品),Stockstadt 33r(来自2245-2267米的样品),Weiterstadt 1(来自2502-2504米的样品),Tiefbohrung Gro?-umstadt / Heubach,B / 89-B02和CORED浅井(FORSCHUNGSBOHRUNG MESSEL GA 1和2)以及GWM17 ZWINGENBERG,GWM1A ZWINGENBERG,Langenthal BK2 / 05,EWS267 / 1 Heubach和InstitutFürSteinkonservierung EV的档案样本在2007年源自综合大规模采样运动的美洲州被调查。数据库(Weinert等,2020B; https://doi.org/10.25534/dutatalib-278)旨在提供中德结晶崛起的易于进入的岩石物理学,以224个地点在巴伐利亚,黑森州,莱茵兰 - Palatinate和图林根和包含26 951个单数据点。每个数据点都以各个元数据寻址,例如样本标识符,采样位置,岩画,以及如果适用,地层和采样深度(在井样本的情况下)。

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