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Development of Internet-of-Things-Based Controlled-Source Ultra-Audio Frequency Electromagnetic Receiver 开发基于物联网的可控源超音频电磁接收器
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-05-21 DOI: 10.5194/gi-2024-2
Zucan Lin, Qisheng Zhang, Keyu Zhou, Xiyuan Zhang, Xinchang Wang, Hui Zhang, Feng Liu
Abstract. Electromagnetic exploration, characterized by its low cost, wide applicability, and high operational efficiency, finds extensive applications in fields such as oil and gas exploration, mineral prospecting, and engineering geology. Traditional controlled-source electromagnetic detection methods are typically confined to operating frequencies below 250 kHz, resulting in insufficient detection accuracy for applications such as shallow and intermediate-depth exploration, thereby constraining their performance in high-resolution imaging. To address these challenges, we propose a controlled-source ultra-audio frequency electromagnetic receive system based on the Internet of Things (IoT). We investigate cascaded digital filtering and sampling techniques to extend the receiver's sampling rate range, thereby elevating the operating frequency of controlled-source electromagnetic acquisition from the conventional maximum of 250 kHz to 1 MHz. The receiver achieves a sampling rate of up to 2.5 MHz, comprising three magnetic field measurement channels and two electric field measurement channels. The instrument is compact, lightweight, capable of real-time data storage locally, and real-time data transmission to an upper computer. Additionally, IoT technology is introduced, leading to the design of a cloud-based real-time remote control and data acquisition scheme. Experimental results demonstrate the stability of the instrument, meeting the requirements of field exploration.
摘要。电磁探测具有成本低、适用性广、作业效率高等特点,在油气勘探、矿产勘探和工程地质等领域有着广泛的应用。传统的受控源电磁探测方法的工作频率通常限制在 250 kHz 以下,导致探测精度不足以满足浅层和中深层勘探等应用的需要,从而制约了其在高分辨率成像方面的性能。为了应对这些挑战,我们提出了一种基于物联网(IoT)的可控源超音频电磁接收系统。我们研究了级联数字滤波和采样技术,以扩展接收器的采样率范围,从而将可控源电磁采集的工作频率从传统的最高 250 kHz 提升到 1 MHz。接收器的采样率高达 2.5 MHz,包括三个磁场测量通道和两个电场测量通道。该仪器结构紧凑、重量轻,能够在本地实时存储数据,并将数据实时传输到上位机。此外,还引入了物联网技术,设计了基于云的实时远程控制和数据采集方案。实验结果表明,该仪器性能稳定,满足野外勘探的要求。
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引用次数: 0
An underground drip water monitoring network to characterize rainfall recharge of groundwater at different geologies, environments, and climates across Australia 地下滴水监测网络,用于描述澳大利亚不同地质、环境和气候条件下地下水的降雨补给特征
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-05-02 DOI: 10.5194/gi-13-117-2024
Andy Baker, Margaret Shanafield, Wendy Timms, Martin Sogaard Andersen, Stacey Priestley, Marilu Melo Zurita
Abstract. Understanding when and why groundwater recharge occurs is of fundamental importance for the sustainable use of this essential freshwater resource for humans and ecosystems. However, accurately capturing this component of the water balance is widely acknowledged to be a major challenge. Direct physical measurements identifying when groundwater recharge is occurring are possible by utilizing a sensor network of hydrological loggers deployed in underground spaces located in the vadose zone. Through measurements of water percolating into these spaces from above, we can record the potential groundwater recharge process in action. By using automated sensors, it is possible to precisely determine when recharge occurs (which event, month, or season and for which climate condition). Combined with daily rainfall data, it is possible to quantify the “rainfall recharge threshold”, the amount of rainfall needed to generate groundwater recharge, and its temporal and spatial variability. Australia's National Groundwater Recharge Observing System (NGROS) provides the first dedicated sensor network for observing groundwater recharge at an event scale across a wide range of geologies, environments, and climate types representing a wide range of Australian hydroclimates. Utilizing tunnels, mines, caves, and other subsurface spaces located in the vadose zone, the sensors effectively record “deep drainage”, water that can move beyond the shallow subsurface and root zone to generate groundwater recharge. The NGROS has the temporal resolution to capture individual recharge events, with multiple sensors deployed at each site to constrain the heterogeneity of recharge between different flow paths, and to quantify (including uncertainty bounds) rainfall recharge thresholds. Established in 2022, the network is described here together with examples of data being generated.
摘要。了解地下水补给发生的时间和原因对于可持续利用这一人类和生态系统不可或缺的淡水资源至关重要。然而,准确捕捉水量平衡的这一组成部分被公认为是一项重大挑战。利用部署在地下负水层空间的水文记录仪传感器网络,可以直接进行物理测量,确定地下水何时补给。通过测量从上方渗入这些空间的水量,我们可以记录潜在的地下水补给过程。通过使用自动传感器,我们可以精确地确定补给发生的时间(哪一事件、月份或季节以及哪种气候条件)。结合每日降雨量数据,可以量化 "降雨补给阈值"、产生地下水补给所需的降雨量及其时空变化。澳大利亚国家地下水补给观测系统(NGROS)提供了第一个专门的传感器网络,用于观测代表澳大利亚各种水文气候的各种地质、环境和气候类型的事件尺度的地下水补给。传感器利用隧道、矿井、洞穴和其他位于地下潮湿地带的地下空间,有效地记录了 "深层排水",即可以移动到浅层地下和根区以外产生地下水补给的水。NGROS 具有捕捉单个补给事件的时间分辨率,在每个站点部署多个传感器,以限制不同水流路径之间补给的异质性,并量化(包括不确定性边界)降雨补给阈值。该网络于 2022 年建立,本文将对其进行介绍,并举例说明所生成的数据。
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引用次数: 0
Research and application of small-diameter hydraulic fracturing in situ stress measurement system 小直径水力压裂原位应力测量系统的研究与应用
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-30 DOI: 10.5194/gi-13-107-2024
Yimin Liu, Mian Zhang, Yixuan Li, Huan Chen
Abstract. Observation and estimation of the stress state in the deep crust is a crucial challenge in in situ stress measurement work. The hydraulic fracturing method is an important borehole-based technique for absolute in situ stress measurement. The small-diameter hydraulic fracturing in situ stress measurement system described in this article consists mainly of underground measurement components (serial small-diameter packers and dual-circuit connecting installation rods) and surface control components (hydraulic fluid control system, data acquisition system, and high-pressure oil pump with controllable flow). It enables series measurement of small-sized boreholes for in situ stress and provides a maximum measurement range of 30–45 MPa. The subsequent calculation of in situ stress data adopts a uniform design method to discuss the influence of various external factors on rock fracturing values. The small-diameter hydraulic fracturing in situ stress measurement system has the advantages of simple and lightweight structure, short testing time, high success rate, and low requirements for rock integrity and pressurization equipment. It has formed a series of small-diameter in situ stress measurement equipment which has been innovatively promoted to the field of underground tunnel safety assessment in coal mines and metal mining areas. It has an important practical value and economic significance in accurately determining the in situ stress state of deep development areas.
摘要观测和估计深部地壳的应力状态是原位应力测量工作中的一项重要挑战。水力压裂法是一种重要的基于井眼的绝对原位应力测量技术。本文介绍的小直径水力压裂原位应力测量系统主要由井下测量部件(串联小直径封隔器和双回路连接安装杆)和地面控制部件(液压流体控制系统、数据采集系统和流量可控的高压油泵)组成。它可以对小尺寸钻孔进行原位应力系列测量,最大测量范围为 30-45 兆帕。随后的原位应力数据计算采用统一设计方法,讨论各种外部因素对岩石压裂值的影响。小直径水力压裂原位应力测量系统具有结构简单轻便、测试时间短、成功率高、对岩石完整性和加压设备要求低等优点。它已形成小直径原位应力测量设备系列,并创新性地推广到煤矿和金属矿区井下巷道安全评估领域。对准确测定深部开拓区的原位应力状态具有重要的实用价值和经济意义。
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引用次数: 0
Research and application of a flexible measuring array for deep displacement of landslides 滑坡深部位移柔性测量阵列的研究与应用
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-29 DOI: 10.5194/gi-13-97-2024
Yang Li, Zhong Li, Qifeng Guo, Yimin Liu, Daji Zhang
Abstract. The multidimensional and multi-sliding surface measurement of deep-seated displacement on landslides poses a significant technical challenge in landslide monitoring and early warning. The fixed-borehole inclinometer serves as an important measurement method based on drilling for this purpose. In this study, a novel flexible measurement array for deep-seated landslide displacement and its installation and measurement processes were developed, enabling higher accuracy in full-hole multidimensional deformation measurement. The measurement array consists of individual measurement probes as basic units, connected in series through coaxial cables and high-pressure rubber hoses, forming a flexible measurement array. Each probe is equipped with acceleration and magnetic field sensors, allowing for the measurement of borehole inclination and azimuth angles and providing a more comprehensive understanding of the deformation of deep-seated landslides. This flexible measurement array resolves the limitations of traditional fixed inclinometers, such as limited probe quantity or inaccurate installation positions that fail to reflect the deformation trend of the landslide body. Moreover, it eliminates the need for auxiliary installation accessories like pulleys and inclinometer pipes, simplifying the mechanical structure and installation process, which represents an advancement in methodology and an improvement in measurement techniques. This array provides a more comprehensive and improved monitoring tool for disaster prevention and mitigation, thereby enhancing the level of geological hazard monitoring and early warning technology.
摘要滑坡深层位移的多维度、多滑动面测量是滑坡监测与预警的重大技术挑战。固定钻孔倾角仪是一种重要的钻孔测量方法。本研究开发了一种新型深层滑坡位移柔性测量阵列及其安装和测量流程,可实现更高精度的全孔多维变形测量。测量阵列以单个测量探头为基本单元,通过同轴电缆和高压橡胶管串联,形成柔性测量阵列。每个探头都配有加速度和磁场传感器,可以测量钻孔倾角和方位角,从而更全面地了解深层滑坡的变形情况。这种灵活的测量阵列解决了传统固定式倾角仪的局限性,如探头数量有限或安装位置不准确,无法反映滑坡体的变形趋势。此外,它还无需滑轮和测斜管等辅助安装附件,简化了机械结构和安装过程,是方法学的进步和测量技术的提高。该阵列为防灾减灾提供了更全面、更完善的监测工具,从而提高了地质灾害监测和预警技术水平。
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引用次数: 0
A hydrate reservoir renovation device and its application in nitrogen bubble fracturing 水合物储层改造装置及其在氮气泡压裂中的应用
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-26 DOI: 10.5194/gi-13-75-2024
Jingsheng Lu, Yuanxin Yao, Dongliang Li, Jinhai Yang, Deqing Liang, Yiqun Zhang, Decai Lin, Kunlin Ma
Abstract. Natural gas hydrate (GH) is a significant potential energy source due to its large reserves, wide distribution, high energy density, and low pollution. However, the gas production rate of past gas hydrate production tests is much lower than the requirement of commercial gas production. Reservoir stimulation technologies like hydraulic fractures provide one potential approach to enhance gas production from GH. The reservoir reformation behavior of the hydrate-bearing sediments (HBSs), particularly sediments with a high clay content, is a complex process during a hydraulic fracturing operation which has been poorly understood and thus hardly predictable. This paper presents an experimental facility that was developed to analyze the hydraulic fracture mechanism in synthesized HBSs. This facility can be used to form GH in sediments, conduct visual observation of hydraulic fracturing experiments, and measure the permeability of HBSs under high-pressure (up to 30 MPa) and low-temperature conditions (from 253.15 to 323.15 K). It is mainly composed of a pressure control and injection unit, a low temperature and cooling unit, a cavitation unit, a visual sapphire reactor, and a data acquisition and measurement unit. The hydraulic fracture module consists of a gas cylinder, fracturing pump, hopper, proppant warehouse, and valves. The sapphire reservoir chamber is applied to observe and measure the fracture of HBSs during hydraulic fracturing. The permeability test module is composed of a constant-flux pump and pressure sensors, which can evaluate the permeability performance before and after the hydraulic fracture in HBSs. The fundamental principles of this apparatus are discussed. Some tests were performed to verify hydraulic fracture tests, and permeability tests could be practically applied in the HBS exploitation.
摘要。天然气水合物(GH)储量大、分布广、能量密度高、污染小,是一种重要的潜在能源。然而,以往天然气水合物生产试验的产气量远低于商业天然气生产的要求。水力压裂等储层刺激技术为提高 GH 的天然气产量提供了一种潜在的方法。含水合物沉积物(HBS),尤其是粘土含量较高的沉积物的储层改造行为是水力压裂作业过程中的一个复杂过程,人们对其了解甚少,因此难以预测。本文介绍了为分析合成 HBS 的水力压裂机制而开发的实验设备。该设备可用于在沉积物中形成 GH,对水力压裂实验进行直观观察,并在高压(高达 30 兆帕)和低温(253.15 至 323.15 K)条件下测量 HBS 的渗透率。它主要由压力控制和注入单元、低温和冷却单元、空化单元、可视蓝宝石反应器以及数据采集和测量单元组成。水力压裂模块由气缸、压裂泵、料斗、支撑剂仓和阀门组成。蓝宝石储层室用于观测和测量水力压裂过程中 HBS 的裂缝。渗透率测试模块由恒定流量泵和压力传感器组成,可评估 HBS 水力压裂前后的渗透率性能。本文讨论了该设备的基本原理。进行了一些试验来验证水力压裂试验,并将渗透性试验实际应用于 HBS 的开采。
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引用次数: 0
A distributed-temperature-sensing-based soil temperature profiler 基于分布式温度传感的土壤温度剖面仪
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-26 DOI: 10.5194/gi-13-85-2024
Bart Schilperoort, César Jiménez Rodríguez, Bas van de Wiel, Miriam Coenders-Gerrits
Abstract. Storage change in heat in the soil is one of the main components of the energy balance and is essential in studying the land–atmosphere heat exchange. However, its measurement proves to be difficult due to (vertical) soil heterogeneity and sensors easily disturbing the soil. Improvements in the precision and resolution of distributed temperature sensing (DTS) equipment has resulted in its widespread use in geoscientific studies. Multiple studies have shown the added value of spatially distributed measurements of soil temperature and soil heat flux. However, due to the spatial resolution of DTS measurements (∼30 cm), soil temperature measurements with DTS have generally been restricted to (horizontal) spatially distributed measurements. This paper presents a device which allows high-resolution measurements of (vertical) soil temperature profiles by making use of a 3D-printed screw-like structure. A 50 cm tall probe is created from segments manufactured with fused-filament 3D printing and has a helical groove to guide and protect a fiber-optic (FO) cable. This configuration increases the effective DTS measurement resolution and will inhibit preferential flow along the probe. The probe was tested in the field, where the results were in agreement with the reference sensors. The high vertical resolution of the DTS-measured soil temperature allowed determination of the thermal diffusivity of the soil at a resolution of 2.5 cm, many times better than what is feasible using discrete probes. A future improvement in the design could be the use of integrated reference temperature probes, which would remove the need for DTS calibration baths. This could, in turn, support making the probes “plug and play” into the shelf instruments without the need to splice cables or experience in DTS setup design. The design can also support the integration of an electrical conductor into the probe and allow heat tracer experiments to derive both the heat capacity and the thermal conductivity over depth at high resolution.
摘要土壤中热量的储存变化是能量平衡的主要组成部分之一,对研究陆地-大气热交换至关重要。然而,由于(垂直)土壤异质性和传感器容易扰动土壤,对其进行测量十分困难。分布式温度传感(DTS)设备在精度和分辨率方面的改进使其在地球科学研究中得到了广泛应用。多项研究表明,土壤温度和土壤热通量的空间分布式测量具有附加值。然而,由于 DTS 测量的空间分辨率(∼30 厘米),使用 DTS 测量土壤温度一般仅限于(水平)空间分布测量。本文介绍了一种利用三维打印螺钉状结构实现(垂直)土壤温度剖面高分辨率测量的装置。一个 50 厘米高的探头是用熔丝三维打印技术制造的,带有一个螺旋槽,用于引导和保护光纤(FO)电缆。这种配置提高了有效的 DTS 测量分辨率,并可抑制沿探头的优先流。该探头经过现场测试,结果与参考传感器一致。DTS 测量的土壤温度具有很高的垂直分辨率,可以在 2.5 厘米的分辨率范围内确定土壤的热扩散率,这比使用离散探头要好很多倍。未来的设计改进可能是使用集成参考温度探头,这样就不需要 DTS 校准浴。这反过来又可以支持将探头 "即插即用 "到架式仪器中,而无需接合电缆或 DTS 设置设计经验。这种设计还可以支持将电导体集成到探头中,并允许热示踪实验以高分辨率得出热容量和深度热导率。
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引用次数: 0
Crack damage stress in fully saturated, permeable rocks: A new detection procedure 完全饱和透水岩石的裂缝破坏应力:一种新的检测程序
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-18 DOI: 10.5194/egusphere-2024-1074
Sandra Schumacher, Werner Gräsle
Abstract. To detect the crack damage stress also known as onset of dilatancy in fully saturated rocks, we propose a new procedure which combines an innovative measurement technique using pore pressure diffusion with the well known technique of finding the pore pressure maximum. A precise determination of the crack damage stress is required to establish parameter dependencies and ultimately to develop a constitutive equation for the crack damage stress, which is of significant interest e.g. for the long-term safety analysis of repositories for radioactive waste. The new technique monitors the true axial strain as indicator for the crack damage stress during a pore pressure diffusion test. In addition to the crack damage stress, this new true axial strain method simultaneously yields pore pressure diffusion coefficients, thereby maximising the information gain. The true axial strain method was developed based on a multi-cycle, long-term experiment of one sample of Passwang Marl, but it can be applied to other types of rocks, which is demonstrated on a Bunter Sandstone.
摘要为了检测完全饱和岩石中的裂缝破坏应力(也称膨胀开始应力),我们提出了一种新的程序,该程序将利用孔隙压力扩散的创新测量技术与众所周知的寻找孔隙压力最大值的技术相结合。裂缝破坏应力的精确测定需要建立参数依赖关系,并最终制定出裂缝破坏应力的构成方程,这对于放射性废物储存库的长期安全分析等具有重要意义。新技术在孔隙压力扩散试验中监测真实轴向应变,作为裂缝破坏应力的指标。除裂缝破坏应力外,这种新的真实轴向应变方法还能同时获得孔隙压力扩散系数,从而最大限度地获得信息。真实轴向应变方法是在对帕斯旺泥灰岩的一个样本进行多周期、长期实验的基础上开发出来的,但它也可应用于其他类型的岩石,这一点已在布恩特砂岩上得到证实。
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引用次数: 0
A free, open-source method for automated mapping of quantitative mineralogy from energy-dispersive X-ray spectroscopy scans of rock thin sections 从岩石薄片的能量色散 X 射线光谱扫描中自动绘制定量矿物学图谱的免费开源方法
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-04-09 DOI: 10.5194/egusphere-2024-1017
Miles Mark Reed, Ken L. Ferrier, William O. Nachlas, Bil Schneider, Chloé Arson, Tingting Xu, Xianda Shen, Nicole West
Abstract. Quantitative mapping of minerals in rock thin sections delivers data on mineral abundance, size, and spatial arrangement that are useful for many geoscience and engineering disciplines. Although automated methods for mapping mineralogy exist, these are often expensive, associated with proprietary software, or require programming skills, which limits their usage. Here we present a free, open-source method for automated mineralogy mapping from energy dispersive spectroscopy (EDS) scans of rock thin sections. This method uses a random forest machine learning image classification algorithm within the QGIS geographic information system and Orfeo Toolbox, which are both free and open source. To demonstrate the utility of this method, we apply it to 14 rock thin sections from the well-studied Rio Blanco tonalite lithology of Puerto Rico. Measurements of mineral abundance inferred from our method compare favourably to previous measurements of mineral abundance inferred from X-ray diffraction and point counts on thin sections. The model-generated mineral maps agree with independent, manually-delineated mineral maps at a mean rate of 95 %, with accuracies as high as 96 % for the most abundant phase (plagioclase) and as low as 72 % for the least abundant phase (apatite) in these samples. We show that the default random forest hyperparameters in Orfeo Toolbox yielded high accuracy in the model-generated mineral maps, and we demonstrate how users can determine the sensitivity of the mineral maps to hyperparameter values and input features. These results show that this method can be used to generate accurate maps of major mineral phases in rock thin sections using entirely free and open-source applications.
摘要。对岩石薄片中的矿物进行定量测绘可提供有关矿物丰度、大小和空间排列的数据,这些数据对许多地球科学和工程学科都很有用。虽然存在自动绘制矿物学图谱的方法,但这些方法通常价格昂贵,与专有软件相关,或需要编程技能,从而限制了其使用。在此,我们介绍一种免费的开源方法,用于从岩石薄片的能量色散光谱(EDS)扫描中自动绘制矿物学图谱。该方法在免费开源的 QGIS 地理信息系统和 Orfeo 工具箱中使用了随机森林机器学习图像分类算法。为了证明该方法的实用性,我们将其应用于波多黎各研究较多的 Rio Blanco 炭绿岩岩性的 14 个岩石薄片。通过我们的方法推断出的矿物丰度测量结果与之前通过 X 射线衍射和薄切片上的点计数推断出的矿物丰度测量结果相比,效果更佳。模型生成的矿物图谱与独立的人工划线矿物图谱的平均吻合率为 95%,在这些样本中,最富集相(斜长石)的准确率高达 96%,而最不富集相(磷灰石)的准确率则低至 72%。我们展示了 Orfeo 工具箱中默认的随机森林超参数对模型生成的矿物图谱产生了很高的准确性,并演示了用户如何确定矿物图谱对超参数值和输入特征的敏感性。这些结果表明,这种方法可用于生成岩石薄片中主要矿物相的精确地图,使用的是完全免费的开源应用程序。
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引用次数: 0
Airborne electromagnetic data leveling based on structured variational method 基于结构变分法的机载电磁数据平差
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-03-26 DOI: 10.5194/egusphere-2024-306
Qiong Zhang, Xin Chen, Zhonghang Ji, Fei Yan, Zhengkun Jin, Yunqing Liu
Abstract. The leveling errors are defined as the data difference among flight lines in airborne geophysical data. The differences of the signal leveling always show as a striping pattern parallel to the flight lines on the imaged maps. The fixed structured pattern inspires us to structure a guided leveling error model by an anisotropic Gabor filter. Then we embed the leveling error model in total variational framework to flexibly calculate leveling errors. The guided leveling error model constrain the noise term of total variation rather than just blind removal. Moreover, the structured variational method can be extended to remove other type of noises which have general noise priors. We have applied the method to the airborne electromagnetic, magnetic data, and apparent conductivity data collected by Ontario Geological Survey to confirm its validity and robustness by comparing the results with the published data. The structured variational method can better level airborne geophysical data based on the space properties of leveling error.
摘要平差是指机载地球物理数据中飞行线路之间的数据差异。信号平差总是在成像图上显示为与飞行线平行的条纹状图案。这种固定的结构模式启发我们用各向异性的 Gabor 滤波器来构建一个有引导的平差误差模型。然后,我们将配平误差模型嵌入总变分法框架,以灵活计算配平误差。引导式平差误差模型限制了总变分的噪声项,而不仅仅是盲目去除。此外,结构变分法还可扩展用于去除具有一般噪声前值的其他类型噪声。我们将该方法应用于安大略省地质调查局收集的机载电磁、磁数据和视导率数据,通过与已公布数据的比较,证实了该方法的有效性和稳健性。根据平差误差的空间特性,结构变分法可以更好地平整机载地球物理数据。
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引用次数: 0
Making geoscientific lab data FAIR: a conceptual model for a geophysical laboratory database 使地球科学实验室数据 FAIR:地球物理实验室数据库的概念模型
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-03-25 DOI: 10.5194/gi-13-63-2024
Sven Nordsiek, Matthias Halisch
Abstract. The term of geoscientific laboratory measurements involves a variety of methods in geosciences. Accordingly, the resulting data comprise many different data types, formats, and sizes, respectively. Handling such a diversity of data, e.g. by storing the data in a generally applicable database, is difficult. Some discipline-specific approaches exist, but a geoscientific laboratory database that is generally applicable to different geoscientific disciplines has been lacking up to now. However, making research data available to scientists beyond a particular community has become increasingly important. Global working groups such as the Committee on Data of the International Science Council (CODATA) put effort in the development of tools to improve research data handling. International standards (e.g. ISO 19156) and ontologies (e.g. UCUM) provide a general framework for certain aspects that are elemental for the development of database models. However, these abstract models need to be adapted to meet the requirements of the geoscientific community. Within a pilot project of the NFDI4Earth initiative, we developed a conceptual model for a geoscientific laboratory database. To be able to handle the complex settings of geoscientific laboratory studies, flexibility and extensibility are key attributes of the presented approach. The model is intended to follow the FAIR (findability, accessibility, interoperability, and reusability) data principles to facilitate interdisciplinary applicability. In this study, we consider different procedures from existing database models and include these methods in the conceptual model.
摘要地球科学实验室测量涉及地球科学领域的多种方法。因此,产生的数据分别包括许多不同的数据类型、格式和大小。要处理如此多样的数据,例如将数据存储在一个普遍适用的数据库中,是很困难的。目前已有一些针对特定学科的方法,但至今仍缺乏一个普遍适用于不同地球科学学科的地球科学实验室数据库。不过,向特定社区以外的科学家提供研究数据已变得越来越重要。国际科学理事会数据委员会(CODATA)等全球工作组致力于开发改进研究数据处理的工具。国际标准(如 ISO 19156)和本体论(如 UCUM)为开发数据库模型所需的某些方面提供了总体框架。然而,这些抽象模型需要加以调整,以满足地球科学界的要求。在 NFDI4Earth 计划的一个试点项目中,我们为地球科学实验室数据库开发了一个概念模型。为了能够处理地质科学实验室研究的复杂设置,灵活性和可扩展性是所提出方法的关键属性。该模型旨在遵循 FAIR(可查找性、可访问性、可互操作性和可重用性)数据原则,以促进跨学科应用。在本研究中,我们考虑了现有数据库模型中的不同程序,并将这些方法纳入概念模型。
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引用次数: 0
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Geoscientific Instrumentation Methods and Data Systems
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