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Accurate Establishment of Error Models for the Satellite Gravity Gradiometry Recovery and Requirements Analysis for the Future GOCE Follow-On Mission 卫星重力梯度恢复误差模型的精确建立及未来GOCE后续任务需求分析
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0019
Wei Zheng, Zhaokui Wang, Yanwei Ding, Zhaowei Li
Firstly, the new single and combined error models applied to estimate the cumulative geoid height error are efficiently produced by the dominating error sources consisting of the gravity gradient of the satellite-equipped gradiometer and the orbital position of the space-borne GPS/GLONASS receiver using the power spectral principle. At degree 250, the cumulative geoid height error is 1.769 × 10−1 m based on the new combined error model, which preferably accords with a recovery accuracy of 1.760 ×10−1 m from the GOCE-only Earth gravity field model GO_CONS_GCF_2_TIM_R2 released in Germany. Therefore, the new combined error model of the cumulative geoid height is correct and reliable in this study. Secondly, the requirements analysis for the future GOCE Follow-On satellite system is carried out in respect of the preferred design of the matching measurement accuracy of key payloads comprising the gravity gradient and orbital position and the optimal selection of the orbital altitude of the satellite. We recommend the gravity gradient with an accuracy of 10−13−10−15 /s2, the orbital position with a precision of 1-0.1 cm and the orbital altitude of 200-250 km in the future GOCE Follow-On mission.
首先,利用功率谱原理,以星载梯度计重力梯度和星载GPS/GLONASS接收机轨道位置为主要误差源,有效地建立了用于累积大地水准面高度误差估计的单一和组合误差模型;在250度处,基于新组合误差模型的累积大地水准面高度误差为1.769 ×10−1 m,较好地符合德国发布的GOCE-only地球重力场模型go_con_gcf_2_tim_r2的恢复精度为1.760 ×10−1 m。因此,本文建立的累积大地水准面高程组合误差模型是正确可靠的。其次,从重力梯度与轨道位置等关键载荷匹配测量精度的优选设计和卫星轨道高度的优化选择等方面对未来GOCE后续卫星系统进行了需求分析。我们建议未来GOCE后续任务的重力梯度精度为10−13−10−15 /s2,轨道位置精度为1-0.1 cm,轨道高度为200-250 km。
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引用次数: 4
Anomalous Variations of Ionosphere Associated with the Strong Earthquake at Pakistan-Iran Border at a Low Latitude Station Agra, India 印度阿格拉低纬度站与巴基斯坦-伊朗边界强地震相关的电离层异常变化
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0020
D. Pundhir, Birbal Singh, O. P. Singh, S. Gupta
In this paper, we analyze the TEC data for April 2013 observed at Agra station, India (geogr. lat. 27.2° N, long. 78° E) to examine the effect of earthquake of magnitude M = 7.8 which occurred on 16 April 2013 at Pakistan–Iran border region. We process the TEC data using the s statistical criterion to find out anomalous variation in TEC data. We also study the VLF propagation signal from NPM, Hawaii (21.42° N, 158° W), which is monitored at the same station (Agra station) in the light of this earthquake as well as solar flares. The nighttime fluctuation method is used to analyze the VLF data for the period of ±5 days from the day of earthquake (11–21 April 2013). The anomalous enhancements and depletions are found in TEC data on 1–9 days before the occurrence of event.
本文对印度阿格拉站2013年4月的TEC观测数据进行了分析。纬度。27.2°N,长。为了检验2013年4月16日发生在巴基斯坦-伊朗边境地区的M = 7.8级地震的影响。利用s统计准则对TEC数据进行处理,找出TEC数据的异常变化。我们还研究了夏威夷NPM(21.42°N, 158°W)的VLF传播信号,该信号是在这次地震和太阳耀斑的同一台站(Agra站)监测的。采用夜间波动法对地震当日(2013年4月11-21日)±5天的VLF数据进行分析。在事件发生前1-9天的TEC数据中发现了异常的增强和消耗。
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引用次数: 6
Variation of Wave Velocity and Porosity of Sandstone after High Temperature Heating 高温加热后砂岩波速与孔隙度的变化
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0021
Qiang Sun, Weiqiang Zhang, T. Su, Shu-yun Zhu
This paper reports the variations of mass, porosity, and wave velocity of sandstone after high temperature heating. The range of temperature to which the sandstone specimens have been exposed is 25–850°C, in a heating furnace. It has been shown that below 300°C, porosity and wave velocity change very little. Above 300°C, there is a rapid increase in porosity, but the wave velocity decreases significantly. The results of thermo gravimetric analysis (TGA), differential scanning calorimetry (DSC) and mercury intrusion porosimetry (MIP) suggest that a series of changes occurred between 400 and 600°C in sandstone could be responsible for the different patterns of variation in porosity and wave velocity.
本文报道了高温加热后砂岩的质量、孔隙度和波速的变化。砂岩标本在加热炉中暴露的温度范围为25-850℃。研究表明,在300℃以下,孔隙度和波速变化很小。在300℃以上,孔隙度迅速增大,但波速明显减小。热重分析(TGA)、差示扫描量热分析(DSC)和压汞孔隙度分析(MIP)的结果表明,砂岩孔隙度和波速的不同变化模式可能是在400 ~ 600°C之间发生的一系列变化造成的。
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引用次数: 43
Present-day Horizontal Mobility in the Serbian Part of the Pannonian Basin; Inferences from the Geometric Analysis of Deformations 潘诺尼亚盆地塞尔维亚部分现今的水平流动性变形几何分析的推论
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0074
Z. Sušić, M. Toljić, V. Bulatović, T. Ninkov, U. Stojadinovic
In tectonically complex environments, such as the Pannonian Basin surrounded by the Alps–Dinarides and Carpathians orogens, monitoring of recent deformations represents very challenging matter. Efficient quantification of active continental deformations demands the use of a multidisciplinary approach, including neotectonic, seismotectonic and geodetic methods. The present-day tectonic mobility in the Pannonian Basin is predominantly controlled by the northward movement of the Adria micro-plate, which has produced compressional stresses that were party accommodated by the Alps-Dinarides thrust belt and partly transferred towards its hinterland. Influence of thus induced stresses on the recent strain field, deformations and tectonic mobility in the southern segment of the Pannonian Basin has been investigated using GPS measurements of the horizontal mobility in the Vojvodina area (northern Serbia).
在构造复杂的环境中,比如被阿尔卑斯-迪纳里德山脉和喀尔巴阡山脉造山带包围的潘诺尼亚盆地,监测最近的变形是非常具有挑战性的事情。有效地量化活动大陆形变需要使用多学科方法,包括新构造、地震构造和大地测量方法。潘诺尼亚盆地现今的构造运动主要受亚德里亚微板块的北移控制,亚德里亚微板块的北移产生的挤压应力部分被阿尔卑斯-迪纳里德斯冲断带容纳,部分向其腹地转移。利用GPS测量伏伊伏丁那地区(塞尔维亚北部)的水平活动性,研究了由此引起的应力对潘诺尼亚盆地南段近期应变场、变形和构造活动性的影响。
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引用次数: 4
Chaotic Behavior of Soil Radon Gas and Applications 土壤氡气的混沌行为及其应用
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0077
M. Kamislioglu, F. Külahcı
The soil 222Rn concentration non-linear patterns are investigated by the application of various chaos methodologies based on 70 272 measurement data from the East Anatolian Fault Zone, which is one of the world’s most active faults. Among these methodologies are Lyapunov exponent, surrogate data, rescaled range (R/S) analysis, Fourier spectrum, phase space reconstruction, mutual information, false nearest neighbors, and correlation dimension. The results indicate that the nonlinear dynamical approach is convenient for characterization and prediction of the 222Rn concentration dynamics, which are in turn usually used as an earthquake precursor. Behaviour of 222Rn gas is important in earthquake prediction researches.
基于东安纳托利亚断裂带70272次测量数据,应用各种混沌方法研究了土壤222Rn浓度的非线性模式。这些方法包括李亚普诺夫指数、替代数据、重标距离(R/S)分析、傅立叶谱、相空间重建、互信息、假最近邻和相关维。结果表明,非线性动力学方法可以方便地表征和预测222Rn的浓度动态,而222Rn通常被用作地震前兆。222Rn气体的性质在地震预报研究中具有重要意义。
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引用次数: 16
Magnetic and Electromagnetic Signatures around Polile Tshisa Hot Spring in the Northern Neotectonic Belt in the Eastern Cape Province, South Africa 南非东开普省北部新构造带Polile Tshisa温泉的磁、电磁特征
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0001
K. Madi, Peter K. Nyabeze, O. Gwavava, M. Sekiba, Baojin Zhao
Finding productive boreholes in the Karoo fractured aquifers has never been an easy task. Fractured Karoo aquifers in the neotectonic zones in the Eastern Cape Province can be targeted for groundwater exploration. The Polile Tshisa hot spring is located in a seismo-tectonic region beset by neotectonics. Hot springs are indicative of circulation of groundwater at great depths along fault zones, and accordingly of neotectonics. The characterisation of hot springs by means of magnetic and electromagnetic methods can help infer the occurrence of structures which are favourable for groundwater potential. The Polile Tshisa hot spring is characterised by faults, fractures, and dolerite dykes. All these structures make the hot spring a good case study for groundwater exploration.
在卡鲁裂缝含水层中寻找有生产力的井眼从来都不是一件容易的事。东开普省新构造带裂缝性卡鲁含水层可作为地下水勘探的目标。Polile Tshisa温泉位于受新构造运动影响的地震构造区。温泉是断裂带深部地下水循环的标志,因此也是新构造运动的标志。利用磁学和电磁学方法对温泉进行表征可以帮助推断有利于地下水潜力的构造的存在。Polile Tshisa温泉以断层、裂缝和白云岩岩脉为特征。所有这些构造使温泉成为地下水勘探的一个很好的研究案例。
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引用次数: 2
Application of Multivariate Statistical Techniques for Characterization of Groundwater Quality in the Coastal Aquifer of Nador, Tipaza (Algeria) 多元统计技术在阿尔及利亚蒂帕扎纳多尔沿海含水层地下水水质表征中的应用
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0027
A. Bouderbala, B. Remini, A. Saaed Hamoudi, A. Pulido-Bosch
The study focuses on the characterization of the groundwater salinity on the Nador coastal aquifer (Algeria). The groundwater quality has undergone serious deterioration due to overexploitation. Groundwater samplings were carried out in high and low waters in 2013, in order to study the evolution of groundwater hydrochemistry from the recharge to the coastal area. Different kinds of statistical analysis were made in order to identify the main hydrogeochemical processes occurring in the aquifer and to discriminate between different groups of groundwater. These statistical methods provide a better understanding of the aquifer hydrochem-istry, and put in evidence a hydrochemical classification of wells, showing that the area with higher salinity is located close to the coast, in the first two kilometers, where the salinity gradually increases as one approaches the seaside and suggests the groundwater salinization by sea-water intrusion.
研究的重点是纳多尔沿海含水层(阿尔及利亚)地下水盐度的特征。由于过度开采,地下水水质严重恶化。为了研究从补给区到滨海区地下水水化学的演变,2013年在高、低水位进行了地下水采样。为了识别含水层中发生的主要水文地球化学过程,并区分不同类型的地下水,进行了各种统计分析。这些统计方法提供了对含水层水化学的更好理解,并证明了井的水化学分类,表明盐度较高的区域位于靠近海岸的地方,在前两公里,随着靠近海边,盐度逐渐增加,表明地下水因海水入侵而盐渍化。
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引用次数: 14
A Preliminary Study On the Electrical Signatures of Some Iron and Stony Meteorites and Their Dependence On Nickel Content 一些铁和石质陨石的电特征及其与镍含量关系的初步研究
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0055
B. Nabawy, P. Rochette
The present study is considered as an exploratory study of electrical properties of meteorites at variable current frequencies, called the electrical signature. The electric resistivity has been measured at different frequencies, varying between 1 and 100 KHz for some iron meteorites (Mundrabilla and Gibeon meteorites), stony meteorite samples (NWA 869, NWA 7629 and Ghubara) and Fe-Ni alloys, of known Ni concentration, which have been prepared and used as standards to be compared with the studied meteorites. In addition, SEM studies supported by EDX technique have been applied. The SEM and EDX displays enabled us to obtain the chemical composition and internal structural fabrics of the studied samples. Porosity and density (bulk and grain densities) have also been measured for both types of meteorites. Porosity values of the studied meteorites are very low (∅ ≤ 3%) and correspond to micro vugs and cracks. The grain density of non-weathered samples varies from 3.48 g/cm3 for the stony meteorites to 7.91 g/cm3 for the iron meteorites. The obtained electrical signatures are diagnostic for each type and can be used to detect quantitatively the concentration of Ni. The electrical signature of stony meteorites is much simpler than that of iron meteorites, and simpler signatures have been obtained at higher Ni concentrations.
本研究被认为是对陨石在变电流频率下的电特性的探索性研究,称为电特征。对一些铁陨石(Mundrabilla和Gibeon陨石)、石质陨石样品(NWA 869、NWA 7629和Ghubara)和已知Ni浓度的Fe-Ni合金样品在不同频率下的电阻率进行了测量,测量频率在1 ~ 100 KHz之间,这些样品已制备并用作与所研究陨石进行比较的标准。此外,还应用了EDX技术支持的SEM研究。SEM和EDX显示使我们能够获得研究样品的化学成分和内部结构织物。对这两种陨石的孔隙度和密度(体积和颗粒密度)也进行了测量。所研究陨石的孔隙度值很低(∅≤3%),对应于微孔洞和微裂纹。未风化样品的颗粒密度从石质陨石的3.48 g/cm3到铁陨石的7.91 g/cm3不等。所获得的电特征对每种类型都具有诊断性,并可用于定量检测Ni的浓度。石质陨石的电特征比铁陨石的电特征简单得多,在较高的镍浓度下也获得了更简单的电特征。
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引用次数: 10
Electromagnetic Radiation Generated by Acoustic Excitation of Rock Samples 岩石样品声激励产生的电磁辐射
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-02 DOI: 10.1515/acgeo-2016-0081
Lyudmila V. Yavorovich, A. Bespalko, P. Fedotov, R. Baksht
The paper presents an experiment on acoustic excitation of electromagnetic radiation (EMR) signals in skarn, sandstone, and magnetite ore samples. For the skarn and sandstone samples, the EMR signal amplitude was observed to decrease with increasing ultimate strength. Supposedly, this effect can be explained by assuming that EMR is generated when an acoustic wave propagates through an electrical double layer. The presence of piezoelectric inclusions (e.g., quartz) in the magnetite ore enhances the analog EMR signal and its spectral components.
在矽卡岩、砂岩和磁铁矿样品中进行了电磁辐射(EMR)信号的声激励实验。对于矽卡岩和砂岩样品,EMR信号幅度随极限强度的增加而减小。据推测,这种效应可以通过假设电磁波通过双电层传播时产生EMR来解释。磁铁矿中压电夹杂物(如石英)的存在增强了模拟EMR信号及其频谱成分。
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引用次数: 11
Enhancement of Seismic Data Processing and Interpretation of Fracture Zones on the Upper Part of Granitic Basement in Cuu Long Basin, Vietnam 越南龟龙盆地花岗岩基底上部断裂带地震资料处理与解释的改进
IF 2.3 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2016-12-01 DOI: 10.1515/acgeo-2016-0082
M. T. Tân, M. Ha, K. Marfurt, Nguyen Trung Hieu, Nguyen Thi My Hanh
The fractured granite basement is the primary oil and gas reservoir in the Cuu Long Basin, Vietnam. Due to the complexity of this nonlayered unconventional target, combined with complicated fault and fracture systems, the seismic data quality near and within the basement section is very low. For this reason, it is important to apply improved seismic data processing workflows, filtering and migration techniques, as wells as attribute processing methods to enhance the imaging quality.Our studies show that applying different types of filters, including the f-k, Radon transform and Tau-P, improves signal to noise ratio, removing multiples, revealing basement’s top and its related fractured and fault zones. In addition, the application of multi-arrival-solution migration algorithms, such as Kirchhoff Migration and Controlled Beam Migration, provides improved imaging for identifying basement top and faults and fractures within the basement. Furthermore, the application of seismic attributes such as curvature, apparent dip, or energy gradient, is important in locating faults and fractures, whereas mapping of intensity and orientation of such structures assists the delineation of “sweet spots” and assists the planning of exploration.
裂缝性花岗岩基底是越南龟龙盆地的主要油气储集层。由于非层状非常规油气藏的复杂性,加上复杂的断裂和裂缝系统,基底段附近和基底段内的地震资料质量很低。因此,采用改进的地震数据处理流程、滤波和偏移技术以及属性处理方法来提高成像质量非常重要。研究表明,采用f-k变换、Radon变换和Tau-P等不同类型的滤波器,提高了信噪比,消除了倍数,揭示了基底顶部及其相关的裂缝和断裂带。此外,Kirchhoff偏移和可控波束偏移等多到达解偏移算法的应用,为识别基底顶部和基底内的断层和裂缝提供了改进的成像技术。此外,曲率、视倾角或能量梯度等地震属性的应用对断层和裂缝的定位很重要,而这些结构的强度和方向的测绘有助于划定“甜点”,并有助于勘探规划。
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引用次数: 7
期刊
Acta Geophysica
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