A Potential Strain Indicator for Brittle Failure Prediction of Low-porosity Rock: Part I—Experimental Studies Based on the Uniaxial Compression Test     

Lei Xue  Meng Qi  Siqing Qin  Guoliang Li  Pei Li  Miaomiao Wang 《Rock Mechanics and Rock Engineering》2015,48(5):1763-1772

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Kinematic analysis of pile behavior for improvement of slope stability in fractured and saturated Hoek–Brown rock masses          下载免费PDF全文

C.B. Qin  S.C. Chian  C.Y. Wang 《国际地质力学数值与分析法杂志》2017,41(6):803-827

Because of a multitude of steep slopes being constructed adjacent to roadways, there is greater concern of landslide occurrence, particularly in instances where poor geomaterials are present. Installation of piles along the slope is one commonly adopted method. This paper presents the assessment of the stability of a rock slope with stabilizing piles based on kinematic analysis. The pile effect is introduced with a resultant lateral force and a moment. Upper bound solutions of the pile's lateral force are derived with a log‐spiral rotational failure mechanism. The slope performance based on the bearing capacity of surcharge loading is also discussed with consideration of pore water pressure. In order to substantiate the derived theoretical solutions, numerical analysis with optimization technique is carried out. Results demonstrate that rock materials with high quality are conducive to ensure slope stability. Reduced lateral force on the pile is produced with lower rock weight, slope height, and surcharge loading. Finally, the safety factor and stability coefficient are discussed to complete the evaluation of the slope stability. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Water isotopes and hydrograph separation in different glacial catchments in the southeast margin of the Tibetan Plateau          下载免费PDF全文

Tao Pu  Dahe Qin  Shichang Kang  HeWen Niu  Yuanqing He  Shijin Wang 《水文研究》2017,31(22):3810-3826

Snow and glaciers are known to be important sources for freshwater; nevertheless, our understanding of the hydrological functioning of glacial catchments remains limited when compared with lower altitude catchments. In this study, a temperate glacial region located in the southeast margin of the Tibetan Plateau is selected to analyse the characteristics of δ¹⁸O and δD in different water sources and the contribution of glacier–snow meltwater to streamflow. The results indicate that the δ¹⁸O of river water ranges from ?16.2‰ to ?10.2‰ with a mean of ?14.1‰ and that the δD values range from ?117.0‰ to ?68.0‰ with a mean of ?103.1‰. These values are more negative than those of glacier–snow meltwater but less negative than those of precipitation. The d ‐excess values are found to decrease from meltwater to river to lake/reservoir water as a result of evaporation. On the basis of hydrograph separation, glacier–snow meltwater accounts for 51.5% of river water in the Baishui catchment in the melting season. In the Yanggong catchment, snow meltwater contributes 47.9% to river water in the premonsoon period, and glacier meltwater contributes only 6.8% in the monsoon period. The uncertainty in hydrograph separation is sensitive to the variation of tracer concentrations of streamflow components. The input of meltwater to a water system varies with local climate and glacier changes. The results confirm that hydrograph separation using water isotopes is valuable for evaluating the recharge sources of rivers, especially in ungauged glacial regions. This study provides insights into the hydrological processes of glacial catchments on the Tibetan Plateau, which is important for water resource management.  相似文献   

CO2 absorption of sandy soil induced by rainfall pulses in a desert ecosystem          下载免费PDF全文

Ke‐Yu Fa  Jia‐Bin Liu  Yu‐Qing Zhang  Bin Wu  Shu‐Gao Qin  Wei Feng  Zong‐Rui Lai 《水文研究》2015,29(8):2043-2051

Soil CO₂ flux is strongly influenced by precipitation in many ecosystem types, yet knowledge of the effects of precipitation on soil CO₂ flux in semi‐arid desert ecosystems remains insufficient, particularly for sandy soils. To address this, we investigated the response of sandy soil CO₂ flux to rainfall pulses in a desert ecosystem in northern China during August–September 2011. Significant changes (P < 0.05) were found in diel patterns of soil CO₂ flux induced by small (2.1 mm), moderate (12.4 mm) and large (19.7 mm) precipitation events. Further analysis indicated that rainfall pulses modified the response of soil CO₂ flux to soil temperature, including hysteresis between soil CO₂ flux and soil temperature, with F_s higher when T_s was increasing than when T_s was decreasing, and the linear relationship between them. Moreover, our results showed that rainfall could result in absorption of atmospheric CO₂ by soil, possibly owing to mass flow of CO₂ induced by a gradient of gas pressure between atmosphere and soil. After each precipitation event, soil CO₂ flux recovered exponentially to pre‐rainfall levels with time, with the recovery times exhibiting a positive correlation with precipitation amount. On the basis of the amounts of precipitation that occurred at our site during the measurement period (August–September), the accumulated rain‐induced carbon absorption evaluated for rainy days was 1.068 g C m^?2; this corresponds approximately to 0.5–2.1% of the net primary production of a typical desert ecosystem. Thus, our results suggest that rainfall pulses can strongly influence carbon fluxes in desert ecosystems. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

Modeling and sensitivity analysis of navigation parameter errors for airborne synthetic aperture radar stereo geolocation     

Lei Pang  Jixian Zhang  Qin Yan 《地球空间信息科学学报》2010,13(3):166-173

For the high-resolution airborne synthetic aperture radar (SAR) stereo geolocation application, the final geolocation accuracy is influenced by various error parameter sources. In this paper, an airborne SAR stereo geolocation parameter error model, involving the parameter errors derived from the navigation system on the flight platform, has been put forward. Moreover, a kind of near-direct method for modeling and sensitivity analysis of navigation parameter errors is also given. This method directly uses the ground reference to calculate the covariance matrix relationship between the parameter errors and the eventual geolocation errors for ground target points. In addition, utilizing true flight track parameters’ errors, this paper gave a verification of the method and a corresponding sensitivity analysis for airborne SAR stereo geolocation model and proved its efficiency.  相似文献   

基于数学形态学的测试卡图案识别方法     

王倩  贾永红  邹勤 《测绘科学》2010,35(1):101-103

提出了一种基于数学形态学的双向匹配识别方法,通过对测试运动员的测试卡图案进行识别,试验结果表明该方法不仅能良好地去除测试卡图案上噪声的影响,而且能有效识别测试卡上图案,识别正确率高达95%以上。  相似文献   

连云港海域废黄河水下三角洲北翼的沉积特征与空间分布   总被引：1，自引：0，他引：1  

秦亚超  顾兆峰 《海洋学报》2019,41(11):101-116

基于连云港海域浅地层剖面资料解释和16个站位柱状岩心的剖面观察、粒度分析、微体化石鉴定、有孔虫和腹足类纹沼螺的AMS 14C年龄，分析废黄河水下三角洲北翼的沉积结构、厚度和沉积物组成，划分沉积单元及其分布范围；识别海侵沉积区的沉积相，认识其沉积环境特征。结果表明，水下三角洲沉积体可分为三角洲前缘和前三角洲两个沉积单元，两者沿连云港海岸线呈并置关系。三角洲前缘位于埒子口至新淮河口外，为一NNE向进积、NW向倾斜的扇形楔状体，可识别出灌河叶瓣及其以东的叶瓣两个沉积中心。该沉积单元以砂质沉积为主，两个叶瓣之间的分流间湾分布有泥和砂质泥。前三角洲位于三角洲前缘西北侧，大致从埒子口外侧沿海岸带向海州湾展布。该单元为泥质沉积，厚度较薄，其北部的两个柱状岩心所揭示的沉积厚度分别为1.8 m和1.5 m。水下三角洲以北，海侵沙席分布广泛，厚度通常在20 cm左右。其分布在本区具有普遍性，只是在连云港海域被黄河泥沙所覆盖，由此也构成了废黄河水下三角洲的底界面。该界面具有侵蚀残留地貌特征。海侵沙席之下为晚更新世MIS 3阶段中早期的海陆过渡相沉积。沉积物多由黄色粉砂或砂质粉砂组成，含有较丰富的有孔虫、介形虫等，可见淡水纹沼螺。  相似文献   

垂向裂隙各向异性煤层地震波响应          下载免费PDF全文

李勤  李永博  李庆春 《地球物理学报》2019,62(1):306-315

煤层中存在的裂隙会导致介质表现为各向异性,本文以HTI型煤层为例,结合各向异性介质弹性矩阵和各向异性裂隙理论,推导出不同充填物的垂直裂隙中各向异性参数表达式,将其应用于地震波响应分析;通过改进的交错网格差分法和各向异性Christoffel方程波场分解法,得到地震波合成记录和分解后的P波和SV波记录;将Thomsen群速度与相速度公式,经过坐标轴旋转变换,得到HTI型煤层中不同各向异性参数的地震波速度响应表达式;建立不同类型煤层地质模型,分析了裂隙密度、裂隙充填物以及煤层厚度等参数变化时的地震波响应特征.研究结果为分析垂向裂隙各向异性薄煤层地震波传播规律提供工具,为选用相应地震数据进行地震波各向异性参数反演提供依据.  相似文献   

一种选权迭代法的半参数回归模型在滑坡预测中的应用     

杨义辉  邹进贵  李琴  韩亚坤 《大地测量与地球动力学》2018,38(8):846-850

传统抗差估计中的选权迭代法无法探测到模型的系统误差，而基于补偿最小二乘原理的半参数模型可以较好地分离出系统误差。通过建立选权迭代法的半参数回归模型，利用时间序列法、L曲线法分别确定模型中的正则化矩阵及平滑因子，并利用选权迭代法重新定权，同时降低了观测粗差和系统误差对参数估值的影响。通过仿真算例，并以重庆奉节县大坪滑坡实测数据为例，验证了选权迭代法的半参数回归方法应用到三峡库区滑坡预测的有效性和优越性。  相似文献   

U-Pb and Pb-Pb apatite ages for Antarctic achondrite Graves Nunataks 06129          下载免费PDF全文

Qin Zhou  Qing-Zhu Yin  Charles K. Shearer  Xian-Hua Li  Qiu-Li Li  Yu Liu  Guo-Qiang Tang  Chun-Lai Li 《Meteoritics & planetary science》2018,53(3):448-466

The Antarctic achondrite Graves Nunataks 06128 (GRA 06128) and Graves Nunataks 06129 (GRA 06129) represent a unique high-temperature, nonbasaltic magmatism in the early solar system. These objects have been interpreted as products of low-degree partial melting of volatile-rich chondritic material, which may have been the asteroid parent bodies of brachinite. Previous studies have investigated their crystallization and metamorphic history with various isotope systematics. Here, we report the U-Pb intercept age of 4466 ± 29 Ma and the weighted-average ²⁰⁷Pb-²⁰⁶Pb age of 4460 ± 30 Ma for the Cl-apatite grains from GRA 06129. Our apatite ages are obviously younger than that of the ²⁶Al-²⁶Mg model age (4565.9 ± 0.3 Ma; Shearer et al. 2010a ), but are the same as the ⁴⁰Ar-³⁹Ar age obtained via step-heating of the bulk rock (4460 ± 28 Ma; Fernandes and Shearer 2010 ; Shearer et al. 2010a ). Based on petrographic observations, merrillites are usually rimmed by apatite and exist as inclusions in apatite. Therefore, the apatite U-Pb age from GRA 06129 probably records a metamorphic event of replacing merrillite with apatite, caused by Cl-rich melts or fluids on their parent body. A collisional event has provided the impact heating for this metamorphic event. Increasing amounts of geochronologic evidence show that the giant impact of the Moon-forming event has affected the asteroid belt at 4450–4470 Ma (Bogard and Garrison 2009 ; Popova et al. 2013 ; Yin et al. 2014 ; Zhang et al. 2016 ). Considering the contemporary metamorphic events for GRA 06129 (4460 ± 30 Ma), it is likely that the asteroid parent body of GRA 06129 was also affected by the same giant impact as the Moon-forming event.  相似文献