共查询到20条相似文献，搜索用时 640 毫秒
1.
《Russian Geology and Geophysics》2014,55(4):515-521
An analytical model is suggested to describe the electrostatic field produced by near-surface inhomogeneities responsible for galvanic shift in magnetotelluric (MT) apparent resistivity sounding curves. The near-surface inhomogeneities are modeled in thin-sheet approximation with laterally variable longitudinal conductance and transverse resistance. The model accounts for the TM (transverse magnetic) mode secondary electric field in the conductive layered subsurface below the thin sheet. Equations have been obtained to relate the subsurface geoelectric parameters and the spatial harmonics of the secondary electrostatic field. This secondary field, which is the source of galvanic shift in MT data, turns out to be in-phase with the primary field. The equations derived to simulate galvanic distortions are applicable to long-period MT data acquired by a synchronous array. 相似文献
2.
V.V. Plotkin 《Russian Geology and Geophysics》2018,59(3):324-333
The paper presents the results of a joint inversion of magnetotelluric sounding (MTS) curves taken at several stations without preliminary selection and normalization and distorted by the presence of lateral electrical-conductivity inhomogeneities in the medium. In the calculations, we used synthetic MTS data for a three-dimensional model. Preparation and interpretation of data are carried out by the Trefftz method using a numerical model of the field and MTS curve distortions. To solve the inverse problem and optimize the subsurface model, we used a nonlinear least-squares method and an iterative process with calculation of the sensitivity matrix and its singular decomposition. The target functional is determined by the discrepancies between the model and synthetic experimental apparent-resistivity curves corresponding to the elements of the impedance tensors on the lateral diagonal. The reliability of the reconstructed subsurface model is characterized by the dispersion of the deviations of its parameters from the parameters of the known model used for the preparation of synthetic experimental data. The joint consideration of distorted apparent-resistivity curves at several stations increases the reliability of interpretation results. The obtained solution to the inverse problem is approximate and can be used as a starting model for more complex algorithms and programs. 相似文献
3.
This paper examines the torsional response of a rigid pier type foundation, with a non-uniform or hollow cross-section which is embedded in bonded contact with a layered elastic half space. The tractions which act at the axisymmetric boundary surface between the pier and the surrounding elastic medium are represented by discretized regions of uniform traction. The compatibility of deformation at the boundary is used to determine the interface stress distribution. The torque-rotation response for the, rigid pier foundation is obtained for different choices of the pier geometry and shear modulus mistnatch between the layer and the underlying half space. 相似文献
4.
Doklady Earth Sciences - The patterns of propagation of elastic surface waves in a layered geophysical medium, which can be used in the search for buried inhomogeneities, are studied. Relationship... 相似文献
5.
Using surface soil daily minimum temperature from 845 meteorological stations across China, the long-term (1971-2000) mean and spatial distribution of the near-surface soil freezing days were estimated with annual values of the number of near surface soil freezing days. The time series for the number of freezing days were constructed and compared with air temperatures in the same period.Resultsshowed that long term mean value in the number of the near surface soil freezing days increased with the increasing latitudes and altitudes over China. Near-surface soils were frozen for more than 200 days in the Qinghai Tibet Plateau, northern Xinjiang and northeast of China. The boundaries of permafrost zones coincide with the contour of (220±10) days of near-surface soil freezing. Using the mean number of 15 days of near-surface soil freezing as criterion, we found that the southern boundary of seasonally frozen ground is around the 25°N line, and the regions south of 22°N are essentially unfrozen regions. The time series of the number of freezing days showed a significant linear trend with change with a slope of -0.22days/year over a period from 1956 through 2006. After the 1990s, the linear slope was up to -1.02 days / year, indicating that the rate of decrease in the number of near-surface soil freezing days has accelerated. Changes in the number of near surface soil freezing were in a negative correlation with air temperature, i.e., the number of near-surface soil freezing days decreases with increase in air temperature.Backgroundcolor represents the contour values of the departure of near-surface soil freezing days from the 1971-2000 mean; Black dashed line is the boundary of permafrost regions, red dashed line is the boundary between frozen and unfrozen ground regions in China 相似文献
6.
Effects of galvanic distortions on magnetotelluric data: Interpretation and its correction using deep electrical data 总被引：1，自引：0，他引：1
The non-inductive galvanic disturbances due to surficial bodies, lying smaller than high frequency skin depth, cause serious
interpretational errors in magnetotelluric data. These frequency independent distortions result in a quasi-static shift between
the apparent resistivity curves known as static shift. Two-dimensional modelling studies, for the effects of surficial bodies
on magnetotelluric interpretation, show that the transverse electric (TE) mode apparent resistivity curves are hardly affected
compared to the transverse magnetic (TM) mode curves, facilitating the correction by using a curve shifting method to match
low frequency asymptotes. But in the case of field data the problem is rather complicated because of the random distribution
of geometry and conductivity of near surface inhomogeneities. Here we present the use of deep resistivity sounding (DRS) data
to constrain MT static shift. Direct current sensitivity studies show that the behaviour of MT static shift can be estimated
using DC resistivity measurements close to the MT sounding station to appreciable depths. The distorted data set is corrected
using the MT response for DRS model and further subject to joint inversion with DRS data. Joint inversion leads to better
estimation of MT parameters compared to the separate inversion of data sets. 相似文献
7.
Microseismic studies associated with a longwall coal mining operation are described. The mine under study was located some 600 ft. below surface. Seismic events associated with controlled roof failure, and with stress development in both the roof and adjacent pillars were monitored by a seven-station near-surface array. The studies were carried out over a 6-month period during which the longwall face moved horizontally some 800 ft. below the area defined by the seismic array. Brief details are presented of the mobile monitoring system and the analysis techniques employed. Typical results obtained during the study are discussed along with suggestions for improving future studies of this type. 相似文献
8.
9.
The traveling of surface waves in a model geophysical medium with a nonsmooth boundary is studied. It is shown that relief significantly distorts the microseismic noise field recorded at the day surface. This result should be taken into consideration when interpreting the data of passive surface-wave geophysical studies of deep crustal inhomogeneities. 相似文献
10.
Seasonal and diurnal variability of thermal structure in the coastal waters off Visakhapatnam has been examined in relation
to the flow field and surface winds utilizing the hourly data of temperature and currents taken at a fixed location over a
tidal cycle at monthly intervals. The coastal currents in the pre-monsoon period and strong near-surface winter cooling processes
affect the thermal structure of the coastal sea. Upwelling which is predominant during March to May with an intermittent relaxing
event helps in the development of a strong layered thermal structure while convective mixing due to winter inversions during
November to February causes weak thermal gradients in the water column. 相似文献
11.
The equation of heat conduction is solved for a horizontally stratified medium initially at constant temperature and subject to a step-function surface temperature change. The problem is solved by Laplace transformation and by applying a concept of further stratifications of the medium into unitary layers of constant ratio of thickness to the square root of thermal diffusivity. The solution takes the form of an infinite sum of complementary error functions, with coefficients given by recursion relations, is suitable for numerical applications and offers an attractive alternative to harmonic and quasi transient approaches in calculating the penetration of transient surface temperature variations into a layered medium. Use of the theorem of superposition yields a general expression for an arbitrary surface temperature function. The utility of the theory is illustrated by modelling examples of palaeoclimatically induced subsurface temperature and heat flow perturbations. 相似文献
12.
Doklady Earth Sciences - A numerical parametric study of the scattering features of Rayleigh waves that appear during the operation of a vibroseismic source on near-surface inhomogeneities (seismic... 相似文献
13.
Br和I是卤族元素的重要成员,I用于油气勘查取得了较好的找矿效果,但是,目前还未见到国外有关Br元素勘查油气的报道。应用松辽盆地中部8.15×104km2的多目标地球化学勘查数据,在研究土壤Br元素近地表影响因素的基础上,试验了表层土壤Br和深层土壤Br的区域地球化学异常对油气的指示意义。在松辽盆地中部发现了表层土壤Br的地球化学巨省和深层土壤Br的地球化学巨环,它们与油气富集区带、大中型油气田和火山岩油气藏相联系。土壤Br元素的表生地球化学作用和油气微渗漏是表层巨省和深层巨环形成的主要机制,因而,土壤Br元素也是战略性油气地球化学填图的一个新的辅助指标。 相似文献
14.
考虑冻结壁的强制解冻过程,采用随机介质理论,建立了隧道水平冻结壁强制解冻期地表沉降的预测方法,并提出强制解冻条件下冻结壁温度场由单管解冻理论近似求解,基于所推导的单管解冻理论和崔托维奇提出的一维情况下融土层稳定融沉量公式,确定了预测方法中融土柱半径和融缩区域内半径的取值方法。将所建立的预测方法应用于隧道全断面水平冻结工程中,得到了地表沉降随强制解冻时间的分布及变化规律。研究结果表明,在冻结壁强制解冻期,其地表沉降分布规律与自然解冻期相似,但地表沉降随解冻时间呈线性增长趋势,这一特征与自然解冻期有所不同。 相似文献
15.
采用解析层元法对存在地下点热源的岩土工程问题进行解答。首先从热弹性力学三维问题的基本控制方程出发,利用拉普拉斯-傅里叶积分变换推导出其在变换域内单层介质及下卧半空间的解析层元;然后结合有限单元法原理组装得到总刚度矩阵,结合边界条件,得到其在变换域内的解答,最后应用拉普拉斯-傅里叶积分逆变换技术,得到物理域内的解。编制了相应的计算程序,算例分析表明：该结果与已有文献吻合较好,该方法求解层状半空间的热-力耦合响应问题具有较好的适用性和较高的精度;层状岩土介质体系中,热扩散系数对温度及地表隆起的变化过程影响显著,但对其初始值和最终稳定值影响不明显;分层特性对岩土介质温度分布及地表位移变化过程均有显著影响。 相似文献
16.
卷积完全匹配层（convolution perfectly matched layer,CPML）吸收边界是一种高效处理波动方程数值模拟中人工边界反射波的方法。本文基于传统的一阶系统CPML吸收边界条件推广并推导了新的二阶系统CPML边界条件（NCPML）。与常规二阶系统CPML边界条件不同,新边界条件推导的核心思想是在复数-频率域中忽略部分衰减因子空间变化特性,避免其在时间域产生复杂卷积算子,然后反变换至时间域得到基于CPML吸收条件的二阶标量波方程,并应用于二阶标量波方程数值模拟。均匀介质模型测试验证了NCPML吸收条件在内存使用上相对于常规二阶系统CPML与SPML（split PML）吸收条件更少。在对人工边界反射的吸收效果上,NCPML稍逊色于常规二阶系统CPML,但二者均相对于SPML优势明显。最后通过层状模型和Marmousi模型测试验证了NCPML的稳定性及其在效率上的优势。 相似文献
17.
Yu. V. Pyatakov V. I. Isaev V. I. Starostenko 《Russian Journal of Pacific Geology》2016,10(6):408-416
The task of 3-D modeling of the thermal field of a sedimentary basin during sedimentation is considered. The aim of the modeling is to determine the temperature at any point of the basin at a given moment of geological time. The mathematical model is based on a system of equations of thermal conductivity for a heterogeneous layered medium with dynamic boundaries. The conditions of the continuous temperature and thermal flow are given at the boundaries of the adjacent layers. The temperature values, which are determined by the values of the secular course of the earth temperature, are given at the upper boundary coinciding with the sedimentation surface. The thermal flow value is considered to be given at the lower boundary. The medium is approximated using a vertical triangle prism, which is accepted in algorithms of interpretation of the gravitation field and characterized by random upper and lower basements and given values of the thermal physical parameters. The equations of thermal conductivity are solved on the basis of potential theory. The precision of this algorithm is demonstrated by calculation of a test example. The thermal evolution of the sedimentary complexes and dynamics of the major zone of oil formation are reconstructed and possible errors of paleotemperature interpretations caused by ignored 3-D modeling medium are determined on the example of the sedimentary basin of the Lunskaya depression of Sakhalin. 相似文献
18.
We consider the problem of penetrative convection in the upper ocean under the conditions of sharp surface cooling and a constant
momentum flux connected with the existing system of random waves. The Langevin equation with a random right part is used to
describe a convective ensemble of thermals. The kinetic Fokker-Planck equation is built for the angular probability density
of an ensemble of convective elements. The stationary solution of this equation allows one to find an analogue of the Boltzman
distribution for convective currents over speed and height. The Maxwell speed distribution is implemented in this case for
convective thermals at a fixed depth. The results allow interpretation of certain data on turbulence in the convective near-surface
ocean layer. 相似文献
19.
Li LiState Key Laboratory of Advanced Technology for Materials Synthesis Processing Wuhan University of Technology Wuhan 《中国地质大学学报(英文版)》2001,12(3)
ＩＮＴＲＯＤＵＣＴＩＯＮＥｖｅｒｓｉｎｃｅｔｈｅｉｎｔｒｏｄｕｃｔｉｏｎｏｆｐｈｙｓｉｃａｌｖａｐｏｒｄｅｐｏｓｉｔｉｏｎｔｏｅｐｉｔａｘｉａｌｇｒｏｗｔｈｏｆｈｉｇｈｔｅｍｐｅｒａｔｕｒｅｓｕｐｅｒｃｏｎｄｕｃｔｉｎｇｃｕｐｒａｔｅｓ,ｑｕａｌｉｔｙｏｆｔｈｅｍａｔｅｒｉａｌｈａｓｂｅｅｎｇｒｅａｔｌｙｉｍｐｒｏｖｅｄ .Ａｔｐｒｅｓｅｎｔ,ｈｉｇｈ ｑｕａｌｉｔｙＹＢａ2 Ｃｕ3 Ｏ7-δ(ＹＢＣＯ)ｆｉｌｍｓｗｉｔｈＴＣ≥ 90Ｋ ,ＪＣ≥ 6× 10 6Ａ/ｃｍ2 ａｔ 77Ｋｃａｎｂｅｅａｓｉｌｙｐｒｅｐａｒｅｄｂ… 相似文献
20.
Swati Basu 《Journal of Earth System Science》2000,109(2):285-292
A global spectral model (T80L18) that is operational at NCMRWF is utilized to study the structure of the marine boundary layer
over the Bay of Bengal during the BOBMEX-Pilot period. The vertical profiles of various meteorological parameters within the
boundary layer are studied and verified against the available observations. The diurnal variation of various surface fields
are also studied. The impact of non-local closure scheme for the boundary layer parameterisation is seen in simulation of
the flow pattern as well as on the boundary layer structure over the oceanic region. 相似文献