Principal stress rotation and cyclic shear strength for an elliptical rotation stress path     

Zhongtao Wang  Andrew Chan  Dan Jin 《Marine Georesources & Geotechnology》2017,35(8):1077-1085

Based on the analytical solutions for wave-induced soil response in an unsaturated anisotropic seabed of finite thickness, an elliptical, i.e., noncircular rotation stress path is proven to be a more common state in a soil element with the cyclic shear stresses due to the traveling linear wave. The influence of an elliptical stress path on the characterization of failure strength is analyzed using three new parameters representing the shape, size, and the orientation of the ellipse. A series of cyclic rotational shear tests on the reconstituted specimens of Chinese Fujian Standard Sand have been performed to investigate the effect of elliptical stress path. A strength function in term of failure cycles is derived to quantify the failure strength of a given sand within a seabed subjected to regular wave loading. The results provide a basis for the evaluation of liquefaction potential of seabed but also point to a unique backbone cycle shear strength curve for soil under principal stress rotation.  相似文献   

Removal rate and releases of polybrominated diphenyl ethers in two wastewater treatment plants,Korea     

Hyo Jin Lee  Gi Beum Kim 《Ocean Science Journal》2017,52(2):193-205

Wastewater treatment plants (WWTPs) play an important role in minimizing the release of many pollutants into the environment. Nineteen congeners in two WWTPs in Korea were determined to investigate the occurrence and fate of polybrominated diphenyl ethers (PBDEs) during wastewater treatment processes. The concentration of total PBDEs was 69.6 and 183 ng/L in influent, which declined to 1.59 and 2.34 ng/L in the final effluent, respectively (Tongyeong and Jinhae WWTPs). PBDEs were found to exist mostly in the particulate phase of wastewater, which rendered sedimentation efficient for the removal of PBDEs. BDE-209 was the predominant congener in the influent and sludge. Most of the PBDEs entering the WWTPs presumably ended up in the sludge, with < 2% being discharged with the final effluent. According to the mass loading estimation, every day 2.55–9.29 g PBDEs entered the two WWTPs, 2.8–10.4 g were disposed to landfill sites in sludge form and 0.06–0.12 g were discharged to the surrounding water through final effluent, respectively. Preliminary results indicated that the ecological risk to organisms in soil exposed to PBDEs through the usage of sludge application to agricultural land was relatively low. To our knowledge, this study is the first to report on the removal efficiency of PBDEs in a WWTP in Korea.  相似文献   

Effect of Ca(OH)2, NaCl,and Na2SO4 on the corrosion and electrochemical behavior of rebar     

Jin  Zuquan  Zhao  Xia  Zhao  Tiejun  Hou  Baorong  Liu  Ying 《中国海洋湖沼学报》2017,35(3):681-692

The corrosion of rebar in reinforced concrete in marine environments causes significant damage to structures built in ocean environments. Studies on the process and mechanism of corrosion of rebar in the presence of multiple ions may help to control damage and predict the service life of reinforced concrete structures in such environments. The effect of interactions between sulfate and chloride ions and calcium hydroxide on the electrochemical behavior of rebar are also important for evaluation of structure durability. In this work, electrochemical impedance spectroscopy(EIS) plots of rebar in Ca(OH)_2 solution and cement grout, including NaCl and Na_2SO_4 as aggressive salts, were measured for different immersion times. The results show that corrosion of rebar was controlled by the rate of charge transfer as the rebar was exposed to chloride solution. In the presence of high concentrations of sulfate ions in the electrolyte, generation and dissolution of the passive film proceeded simultaneously and corrosion was mainly controlled by the diffusion rate. When Na_2SO_4 and NaCl were added to Ca(OH)_2 solution, the instantaneous corrosion rate decreased by a factor of 10 to 20 as a result of the higher p H of the corroding solution.  相似文献   

牛背梁自然保护区林线不同海拔巴山冷杉径向生长对气候变化的响应     

秦进  白红英  周旗  王俊  李书恒  甘卓亭  包光 《干旱区地理》2017,40(1):147-155

近年来气候变化对秦岭植被的影响已得到众多研究的证实,牛背梁作为秦岭东部主脊和国家级自然保护区,该地区亚高山林线植被对气候变化的生态响应现状尚未得到广泛关注。依照树木年代学原理,进行响应分析并建立回归模型,探讨了牛背梁林线关键树种巴山冷杉（Abies fargesii）年表特征及对气候响应的海拔分异特征。结果表明：（1）随海拔升高,树木生长对气候的敏感性逐渐上升,但轮宽年表的同步性和信号强度呈先下降后上升的特点。（2）不同海拔树轮宽度年表的气候响应结果基本一致,对气温的敏感性均较降水强,敏感时段为当年2～8月,差异主要体现在,高海拔树木受生长季末期8月气温的影响较重,中海拔树木受生长季前期3～4月降水和上年冬季10～11月气温的促进,而低海拔树木受初春1～2月降水的限制作用明显。（3）对比分析低、中、高海拔3个回归模型中显著因子的变化趋势,发现气候变化可以促进巴山冷杉生长季的提前,但不同海拔树木的生长动态各异,说明研究区林线不同海拔巴山冷杉生长对全球变化可能具有不同的响应机制。  相似文献   

中晚全新世毛乌素沙地东南部气候变化过程   总被引：5，自引：5，他引：0  

杨帆  靳鹤龄  李孝泽  耿建伟  刘冰 《中国沙漠》2017,37(3):431-438

位于中国北方半干旱区的毛乌素沙地对气候变化响应敏感,是研究气候变化的理想区域。通过对毛乌素沙地东南部锦界剖面磁化率、有机质含量、CaCO₃含量的分析,重建了7.5 ka BP以来的气候变化过程。结果显示：中晚全新世毛乌素沙地东南部环境与气候变化可分为3个阶段：7.5～4.6 ka BP,夏季风占主导,气候暖湿,与全新世大暖期对应;4.6～3.3 ka BP,气候突变为干冷并波动频繁;3.3～2.5 ka BP气候以干冷为主。另外,存在5次千年尺度的干旱事件：7.0～6.8 ka BP、6.6～5.7 ka BP、4.6～4.1 ka BP、3.7～3.5 ka BP、3.3～2.5 ka BP。研究区气候变化与全球具有较好的一致性。  相似文献   

小冰期福建海岸沙丘的沉积环境   总被引：2，自引：2，他引：0  

靳建辉  李志忠 《中国沙漠》2017,37(6):1111-1120

选取福建东南沿海典型海岸沙丘——东海沙丘,运用GPR（Ground Penetrating Radar）技术探测海岸沙丘内部构造,辅助天然剖面和人工探槽观测,进行系统的年代采样与OSL（Optically Stimulated Luminescence）测年,并选择物理意义明确的粒度参数作为主要环境代用指标,获得了亚热带季风区砂质海岸带典型海岸沙丘的沉积年代和沉积结构。结果表明：（1）东海沙丘是由若干灌丛沙丘组成的横向沙丘,0～6 m主要是～0.45 ka BP以来形成的海岸风成沙丘,可以划分为～0.45 ka BP和0.22～0.12 ka BP两个阶段。（2）东海沙丘沉积过程是多因素共同作用的结果,冷干的气候环境是沙丘发育的适宜条件,入境台风频率增加可能加快了风沙的沉积过程。对比历史文献资料发现,气候异常期往往与社会动荡期、重要历史事件相对应。  相似文献   

Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes     

Ma  Bin  Liang  Xing  Liu  Shaohua  Jin  Menggui  Nimmo  John R.  Li  Jing 《Hydrogeology Journal》2017,25(3):675-688

Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (¹⁸O) and hydrogen (²H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted δ¹⁸O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and δ¹⁸O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water δ¹⁸O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted δ¹⁸O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater.

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Is there the Paleoproterozoic komatiite related to mantle plume in the Jifeng area,Northern Great Xing’an Range,NE China?     

Feng  Zhi-Qiang  Liu  Yong-Jiang  Jin  Wei  Li  Wei-Min  Wen  Quan-Bo 《International Journal of Earth Sciences》2017,106(6):2225-2231

International Journal of Earth Sciences -  相似文献   

柴达木盆地西部新生界陆相湖盆碳酸盐岩沉积环境与沉积模式^*   总被引：1，自引：0，他引：1       下载免费PDF全文

纪友亮  马达德  薛建勤  王鹏  吴颜雄  曾力  金力 《古地理学报》2017,19(5):757-772

利用野外露头、岩心、测井录井和分析化验资料,对柴达木盆地西部(简称“柴西地区”)新生界干柴沟组湖相碳酸盐岩进行了研究,划分了其沉积微相类型,研究了其分布规律,分析其形成环境和控制因素,并建立了相应沉积模式。该区湖相碳酸盐岩在垂向上与碎屑岩频繁互层,湖相碳酸盐岩包括颗粒灰岩、藻灰岩、泥晶灰岩和混积岩4大类11种,划分出了灰泥坪、颗粒滩、藻丘(礁)、浅湖湾以及(半)深湖泥灰岩相等5种沉积微相。通过分析不同碳酸盐岩及其微相时空展布特征,认为其发育主要受控于湖盆构造运动、湖平面变化、陆源碎屑注入、古气候与古水介质条件、古地貌与古水深环境,并在此基础上建立了柴西湖相碳酸盐岩的沉积模式。研究认为柴达木盆地西部干柴沟组沉积时期,湖盆为典型咸化湖盆,构造活动相对稳定,湖平面上升达到峰值。碳酸盐岩主要发育在湖侵期,高频湖平面变化形成了碳酸盐岩与碎屑岩频繁互层。在枯水期,盆地坡折处发育碎屑岩滩坝或三角洲前缘沉积;在湖侵期,盆地坡折处发育了鲕粒滩及藻灰岩,盆地洼陷区发育泥灰岩或灰质泥岩。  相似文献   

辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征     

彭游博  宋淑娥  刘锦  张文静  王恩德  赵辰 《地质通报》2017,36(10):1698-1707

宝兴岩体位于华北板块北缘陆缘活动带东段,岩性为花岗闪长岩,LA-ICP-MS锆石~(206)Pb/~(238)U年龄加权平均值为235.0±1.3Ma,属于中三叠世。岩石的K_2O/Na_2O平均值为1.07,属高钾钙碱性系列;富集大离子亲石元素,亏损高场强元素,具有活动陆缘钙碱性岩系特征;稀土元素总量平均值为147×10~(-6),稀土元素配分曲线右倾,属具中等负Eu异常的轻稀土元素富集、重稀土元素亏损型。通过岩石学、岩石地球化学及年代学研究,结合邻区构造演化研究,认为中三叠世研究区在伸展作用下岩石圈进行拆沉,从而形成大规模的岩浆活动。  相似文献