Morphological analysis on the coherence of kHz QPOs     

J. Wang  H. K. Chang  C. M. Zhang  D. H. Wang  L. Chen  J. L. Qu  L. M. Song 《Astrophysics and Space Science》2012,342(2):357-364

We take the recently published data of twin kHz quasi-period oscillations (QPOs) in neutron star (NS) low-mass X-ray binaries (LMXBs) as the samples, and investigate the morphology of the samples, which focuses on the quality factor, peak frequency of kHz QPOs, and try to infer their physical mechanism. We notice that: (1) The quality factors of upper kHz QPOs are low (2～20 in general) and increase with the kHz QPO peak frequencies for both Z and Atoll sources. (2) The distribution of quality factor versus frequency for the lower kHz QPOs are quite different between Z and Atoll sources. For most Z source samples, the quality factors of lower kHz QPOs are low (usually lower than 15) and rise steadily with the peak frequencies except for Sco X-1, which drop abruptly at the frequency of about 750 Hz. While for most Atoll sources, the quality factors of lower kHz QPOs are very high (from 2 to 200) and usually have a rising part, a maximum and an abrupt drop. (3) There are three Atoll sources (4U 1728-34, 4U 1636-53 and 4U 1608-52) of displaying very high quality factors for lower kHz QPOs. These three sources have been detected with the spin frequencies and sidebands, in which the source with higher spin frequency presents higher quality factor of lower kHz QPOs and lower difference between sideband frequency and lower kHz QPO frequency.  相似文献   

The rms–flux relations in different branches in Cyg X-2     

Z. B. Li  L. M. Song  J. L. Qu  Y. J. Lei  J. Y. Nie  C. M. Zhang 《Astrophysics and Space Science》2012,341(2):383-393

In this paper, the rms-flux (root mean square-flux) relation along the Z-track of the bright Z-Source Cyg X-2 is analyzed using the observational data of Rossi X-ray Timing Explorer (RXTE). Three types of rms-flux relations, i.e. positive, negative, and ‘arch’-like correlations are found in different branches. The rms is positively correlated with flux in normal branch (NB), but anti-correlated in the vertical horizontal branch (VHB). The rms–flux relation shows an ‘arch’-like shape in the horizontal branch (HB). We also try to explain this phenomenon using existing models.  相似文献   

Numerical and test study on vertical vibration characteristics of pile group in slope soil topography     

Qu Liming  Ding Xuanming  Zheng Changjie  Wu Chongrong  Cao Guangwei 《地震工程与工程振动(英文版)》2021,20(2):377-390

Topography effects on the vertical vibration responses of pile group are revealed though numerical analysis and model tests.First,a series of model tests with different topography of ground and bedrock are conducted.The results indicate that displacement amplitude of the pile head in sloping ground topography is larger than in horizontal ground.Differential displacement at various positions of the pile cap is observed in non-horizontal topography.Afterwards,a numerical algorithm is employed to further explore the essential response characteristics in group piles of different topography configurations,which has been verified by the test results.The lengths of the exposed and frictional segment,together with the thickness of the subsoil layer,are the dominant factors which cause non-axisymmetric vibration at the pile cap.  相似文献   

藏南马扎拉金-锑矿床:成矿流体性质和成矿物质来源          下载免费PDF全文

谢玉玲  杨科君  李应栩  李光明  曲云伟  董磊 《地球科学》2019,44(6):1998-2016

马扎拉金-锑矿床是藏南巨型金-锑成矿带的重要组成部分,其矿床成因目前仍存在不同认识.通过主要矿石和蚀变围岩的岩相学、矿相学、流体包裹体和稳定同位素分析,探讨了马扎拉金-锑矿床的成矿流体性质、矿质迁移和沉淀机制.结果表明,马扎拉金-锑矿床成矿流体主要来自岩浆水,主成矿期流体为中温(约255℃)、低盐度(2.8%~3.5%NaCleqv)、富CO2流体,成矿压力约150 MPa,流体演化过程中的CO2与水的不混溶是造成矿质沉淀的主要原因,成矿金属主要来源于地层,特别是区域广泛分布的海相火山岩地层.  相似文献   

准噶尔盆地玛湖凹陷三叠系源上砂砾岩扇—断—压三控大面积成藏模式   总被引：1，自引：0，他引：1  

瞿建华  杨荣荣  唐勇 《地质学报》2019,93(4):915-927

准噶尔盆地玛湖富烃凹陷下三叠统百口泉组新近发现了我国首个源上大面积连续型砂砾岩油藏群,是对全球"连续型"油气藏研究的新补充,但其成藏机理和模式并不很清楚。为加强对其的理论认识,并为下步勘探提供参考,基于油气生、储、盖、圈、运、保等基础石油地质条件,并结合油气藏特征,进行了成藏条件与成藏模式的综合研究。结果表明,优质充足的下二叠统风城组碱湖油气来源、规模有效的扇三角洲前缘砂砾岩储层、多重组合的扇三角洲平原致密砾岩、泥岩和断裂封盖保存、沟通良好的高角度断裂输导体系、平缓连续的构造背景奠定了大面积连续成藏的地质基础。在此背景下,高成熟的风城组所生成油气,在切穿烃源灶和储层的高角度压扭性断裂沟通下,优先充注物性相对好的扇三角洲前缘水下河道砂岩和砂质细砾岩,并且在地层异常高压促进下,控制着油气富集程度,使得油气成藏表现为大型缓坡浅水扇三角洲沉积控制下的源上扇-断-压三控大面积"连续型"。百口泉组油气藏具有的油质轻且含气、微裂缝广泛发育,以及异常高压等,决定了砾岩储层虽总体低孔低渗,但依旧能够高产。在油源断裂沟通的斜坡区上倾方向,叠合地层异常高压以及扇三角洲前缘水下河道砂砾岩的区域是下步有利勘探方向。  相似文献   

中国铁路风沙防治的研究进展   总被引：4，自引：1，他引：3  

张克存  屈建军  鱼燕萍  韩庆杰  王涛  安志山  胡菲 《地球科学进展》2019,(6):573-583

基于中国沙区铁路的发展历程,系统分析了铁路沙害类型、特点以及风沙防治方案、措施和技术体系。针对我国沙区地域特征和铁路沙害类型,作为个例分类剖析了途径流沙地表、高寒环境与戈壁大风区铁路风沙危害与防治技术取得的成效和面临的问题。结合目前我国沙区铁路的发展趋势,从理论研究和工程防沙实践出发,提出复杂地形、特殊环境铁路沙害是今后风沙工程学领域的重点和理论研究趋势,也是沙区铁路沙害防治的关键和难点。  相似文献   

渤中凹陷CFD18-2油田高岭石胶结作用及其对储层物性的影响     

陈思芮  曲希玉  王冠民  王清斌  曹英权 《吉林大学学报(地球科学版)》2019,49(5):1235-1246

为探究成岩作用过程中所形成的次生黏土矿物对储层物性的影响,借助偏光显微镜及扫描电镜的镜下分析,并结合储层物性等数据,对渤中凹陷附近沙垒田凸起东南部CFD18-2油田东三段高岭石的特征、类型、成因及其对储层物性的影响进行了研究。研究结果表明：1）研究区高岭石为有机酸溶蚀长石形成的自生高岭石,呈现典型的"手风琴状"及"蠕虫状",常充填于粒间孔、长石次生溶孔及碳酸盐胶结物溶孔中并形成良好的晶间孔隙。2）研究区主要发育两期高岭石,第一期主要充填于早期碳酸盐胶结物溶孔中,呈微小"蠕虫状";第二期充填于铁方解石与铁白云石胶结物溶孔中,部分高岭石具碱性溶蚀特征,且第二期高岭石与晚期伊利石共生。3）研究区东三段储层具备一定的渗流能力,使长石溶蚀形成的"副产物"被流体带走;但在破坏性成岩作用下,储层渗流能力会逐渐变差,最终使得"副产物"堆积于孔隙,降低储层物性。4）高岭石及同期硅质胶结物对储层物性的影响是一把"双刃剑",当高岭石及硅质的体积分数低于6.81%时,长石溶蚀有利于改善储层物性;当高岭石及硅质的体积分数高于6.81%时,则不利于储层物性的改善。  相似文献   

A sequential sparse polynomial chaos expansion using Bayesian regression for geotechnical reliability estimations     

Qiujing Pan  Xingru Qu  Leilei Liu  Daniel Dias 《国际地质力学数值与分析法杂志》2020,44(6):874-889

Polynomial chaos expansions (PCEs) have been widely employed to estimate failure probabilities in geotechnical engineering. However, PCEs suffer from two deficiencies: (a) PCE coefficients are solved by the least-square minimization method which easily causes overfitting issues; (b) building a high order PCE is often computationally expensive. In order to overcome the aforementioned drawbacks, the Bayesian regression technique is employed to evaluate PCE coefficients, which not only provides a sparse solution but also avoids overfitting. With the aid of the predictive means and variances given by Bayesian analysis, a learning function is proposed to sequentially select the most informative samples that are critical to build a PCE. This sequential learning scheme can highly enhance the computational efficiency of PCEs. Besides, importance sampling (IS) is incorporated into the sequential learning (SL)-PCEs to deal with geotechnical problems with small failure probabilities. The proposed method of SL-PCE-IS is applied to three illustrative examples, which shows that the improved PCE method is more effective and efficient than the common PCEs method, leading to accurate estimations of small failure probabilities using fewer training samples.  相似文献   

祁连山疏勒河源区冻土退化对土壤微生物生物量碳氮的影响   总被引：2，自引：1，他引：1  

吴明辉  瞿德业  李婷  刘放  高雅月  陈生云  陈拓 《地理科学》2021,41(1):177-186

对青藏高原东北缘祁连山西段疏勒河源区多年冻土区0~50 cm土壤微生物生物量碳氮分布特征及其影响因素进行分析。结果表明:稳定型和极不稳定型多年冻土区0~50 cm土壤中微生物量碳含量范围分别为0.015~0.620 g/kg和0.019~0.411 g/kg,微生物量氮含量范围分别为0.644~12.770 mg/kg和0.207~3.725 mg/kg;土壤微生物量总体呈现出稳定型显著高于极不稳定型多年冻土,表明多年冻土退化（多年冻土由稳定型退化为极不稳定型）对土壤微生物量积累有明显抑制作用。土壤微生物生物量碳占有机碳、微生物生物量氮占全氮的比值在稳定型多年冻土中显著高于极不稳定型,表明多年冻土退化对土壤微生物的矿化能力有明显抑制作用。土壤微生物量及其与土壤养分的比值有显著的剖面变化特征,随土壤深度增加而减小。土壤微生物量碳氮均与土壤温度显著负相关,与地下生物量显著正相关。稳定型多年冻土中,土壤微生物量碳氮与碳氮比正相关、与氧化还原电位负相关;不稳定型多年冻土中,土壤微生物量碳氮与pH正相关。土壤微生物量碳氮与土壤温度和pH在剖面变化上显著相关。逐步回归分析表明驱动微生物生物量碳氮在不同多年冻土类型和土层之间变化的因子是不同的。  相似文献   

柴达木盆地西北部长垄状雅丹沉积物地球化学元素组成及指示意义   总被引：2，自引：2，他引：0  

郜学敏  屈欣  王萌  张思悦  张姚姚  李继彦 《中国沙漠》2021,41(3):127-136

雅丹沉积物蕴含丰富的区域环境变化和物源演变信息。以柴达木盆地西北部的长垄状雅丹为研究对象,通过对地球化学元素的研究,探讨沉积物的化学风化特征及其对物质输移的指示意义。结果表明：（1）雅丹沉积物的常量元素以SiO₂、CaO、Al₂O₃、MgO和Na₂O为主,微量元素Cl、Sr、Ba和Zr含量较高。相较于上陆壳平均化学元素组成,雅丹沉积物常量元素CaO和MgO富集程度较高,微量元素中Cl和As富集程度较高。（2）雅丹沉积物的CIA值平均为39.03,且在A-CN-K三角图上准平行于A-CN连线,主体在斜长石与钾长石连线的下方,因此雅丹沉积物的化学风化程度较低,处于初期的脱Na、Ca阶段。（3）特征元素比值表明雅丹体内赋存的大量细颗粒物质为廊道流沙的源区。细颗粒物质经过外营力的风化、剥蚀等过程而出露,在雅丹廊道内堆积并向下风向输移,遇阻堆积而形成沙丘。雅丹是否为下风向黄土的物源区,尚需进一步验证。  相似文献