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172.
基于连续多孔介质原理与混合体原理引入流?固耦合模型,采用FISH语言编制程序,建立了初始渗流场设置函数、饱和?非饱和渗流分析模块、特殊应力修正模块以及非饱和单元抗剪强度修正模块,实现了利用FLAC3D进行饱和?非饱和渗流分析,同时基于饱和?非饱和渗流场修正非饱和区土体单元的有效应力以及抗剪强度,完成了将FLAC3D中饱和土流?固耦合计算原理扩展到非饱和土中。在二次开发的分析模块基础上对Liakopoulos砂柱排水试验进行数值模拟,验证了计算模型和计算程序的正确性。同时也研究了降雨入渗对土质边坡的渗流场、位移场以及稳定性演变过程的影响,揭示了降雨诱发边坡失稳的机制。 相似文献
173.
不完整井在实际工程中应用广泛,且存在某些承压不完整井,其滤管顶、底均不在含水层层面,不能直接按常规的方法进行计算。可根据流线图中的水平流线对渗流场分层后进行简化计算,但分层位置的确定非常困难。因此,提出了简便可行的渗流场分层方法,包括假设上下部渗流场渗径相等的等渗径改进方法、假设上下部渗流场中井滤管长度与其含水层厚度比值相等的等比例改进方法和以等比例方法为基础的等效阻力法,并以此为基础对计算简便、精度较高的沙金煊公式进行完善,得到了适用于滤管顶、底均不在含水层层面的承压不完整井近似计算方法。经过算例验证和与有限元比较,该方法计算精度较高,实用性较强。 相似文献
174.
175.
硫氧同位素示踪污染物来源在济南岩溶水中的应用 总被引:1,自引:0,他引:1
近年来,济南岩溶水硫酸盐浓度逐年升高,为了对硫酸盐污染区域实施有效的防治措施,保障饮用水安全,识别硫酸盐的污染来源极其重要。在系统分析研究区水文地质条件的基础上,根据实际的采样测试数据,采用硫、氧(S、O)双同位素示踪技术,分析识别了济南趵突泉泉域硫酸盐的主要污染来源,并通过IsoSource质量守恒模型,估算了硫酸盐各污染来源的贡献率。结果表明: 泉域内硫酸盐主要污染来源有大气沉降、污水和土壤; 大气沉降来源贡献率最大,均值达到53.9%; 其次是污水来源,均值为31%; 土壤来源贡献率最小,均值为15.1%。该研究为北方岩溶区地下水硫酸盐来源的定量研究提供了一种新方法,为济南趵突泉泉域硫酸盐污染防治提供了科学依据。 相似文献
176.
177.
In this work, the elastic buckling of porous solids was investigated using a lattice spring model (LSM). The capability of the LSM to solve elastic buckling problems was comprehensively verified by comparing well-established numerical and analytical solutions. Following this, the buckling of a porous solid was studied, in which two porous structures were considered, ie, the random porous model and the Voronoi porous model. The results reveal that both the porosity and the shape of the pores influence the elastic buckling bearing capacity of the porous solid. Finally, the mechanical responses of a porous solid with an extra high porosity (0.85) were numerically investigated. Our numerical results demonstrated that the nonlinear elastic response of the porous solid might come from its mesoscale elastic buckling. This work shows the ability and promise of using the LSM as a fundamental numerical tool for the deep investigation of the buckling mechanical behavior of porous solids. 相似文献
178.
Seafloor pockmarks are important indicators of submarine methane seepages and slope instabilities.In order to promote the understanding of submarine pockmarks and their relationship with sediment instabilities and climate changes,here we summarize the research results of pockmarks in the spatio-temporal distributions and shaping factors.Most of pockmarks occur along active or passive continental margins during the last 25 kyr B.P..Circular and ellipse are the most common forms of pockmarks,whereas pockmarks in a special crescent or elongated shape are indicators of slope instabilities,and ring-shape pockmarks are endemic to the gas hydrate zones.Further researches should be focused on the trigger mechanism of climate changes based on the pockmarks in the high latitudes formed during the deglaciation periods,and the role of gas hydrates in the seafloor evolution should be elucidated.In addition,the feature of pockmarks at their early stage(e.g.,developing gas chimneys and gas driving sedimentary doming)and the relations between pockmarks and mass movements,mud diapirs could be further studied to clarify the influences of rapid methane release from submarine sediments on the atmospheric carbon contents. 相似文献
179.
E.K.KRISHNA KUMAR S.ABHILASH SANKAR SYAM P.VIJAYKUMAR K.R.SANTOSH A.V.SREENATH 《大气科学进展》2023,40(4):697-710
The inverse relationship between the warm phase of the El Ni?o Southern Oscillation(ENSO) and the Indian Summer Monsoon Rainfall(ISMR) is well established. Yet, some El Ni?o events that occur in the early months of the year(boreal spring) transform into a neutral phase before the start of summer, whereas others begin in the boreal summer and persist in a positive phase throughout the summer monsoon season. This study investigates the distinct influences of an exhausted spring El Ni?o(springtime)... 相似文献
180.
The interannual variations of rainfall over southwest China (SWC) during spring and
its relationship with sea surface temperature anomalies (SSTAs) in the Pacific are analyzed,
based on monthly mean precipitation data from 26 stations in SWC between 1961 and 2010,
NCEP/NCAR re-analysis data, and Hadley global SST data. Sensitivity tests are conducted to
assess the response of precipitation in SWC to SSTAs over two key oceanic domains, using the
global atmospheric circulation model ECHAM5. The interannual variation of rainfall over SWC in
spring is very significant. There are strong negative (positive) correlation coefficients
between the anomalous precipitation over SWC and SSTAs over the equatorial central Pacific
(the mid-latitude Pacific) during spring. Numerical simulations show that local rainfall in
the northwest of the equatorial central Pacific is suppressed, and a subtropical anticyclone
circulation anomaly is produced, while a cyclonic circulation anomaly in the mid-latitude
western Pacific occurs, when the equatorial Pacific SSTAs are in a cold phase in spring.
Anomalous northerly winds appear in the northeastern part of SWC in the lower troposphere.
Precipitation increases over the Maritime Continent of the western equatorial Pacific, while a
cyclonic circulation anomaly appears in the northwest of the western equatorial Pacific. A
trough over the Bay of Bengal enhances the southerly flow in the south of SWC. The trough also
enhances the transport of moisture to SWC. The warm moisture intersects with anomalous cold
air over the northeast of SWC, and so precipitation increases during spring. On the
interannual time scale, the impacts of the mid-latitude Pacific SSTAs on rainfall in SWC
during spring are not significant, because the mid-latitude Pacific SSTAs are affected by the
equatorial central Pacific SSTAs; that is, the mid-latitude Pacific SSTAs are a feedback to
the circulation anomaly caused by the equatorial central Pacific SSTAs. 相似文献