Preservation of Lipid Molecular Fossils in the Sediments from an Oil-Gas Releasing Zone in the South China Sea     

Hong Qiu  Li Zou  Minsheng Zhang  Chaoqi Zhu  Yonggang Jia 《中国海洋大学学报(英文版)》2018,17(6):1336-1342

In order to explore the standing stock and preservation of organic carbon, different forms of compound specific lipids were analyzed, based on a 1.8 m sediment core collected in the northern continental shelf of South China Sea in May, 2016. In the core sediments, 21 species of fatty acids, 6 species of alcohols, 8 species of sterols and phytol were detected. Fatty acids were dominated components with the percent of 67%–91% in the total lipids, in which saturated fatty acid C16:0 accounted for about 50%. The contents of lipid species generally decreased from the sediments at surface to those deep, except alcohols waving in a certain range at the same time. Fatty acids primarily existed in free form, followed by base hydrolytic form, and then acid hydrolytic form. Free alcohols were obviously dominated, while base and acid hydrolytic forms contributed small comparably. Phytol gave a significant priority to base hydrolytic form, while acid hydrolytic form could be neglected. Similar to phytol, sterols mostly presented in base hydrolytic form, and then in free form. The compositions of lipids and their forms suggested that organic carbon basically originated from primary production in upper waters in studying area, and were well preserved in the sediments.  相似文献   

Land-Use Changes and Human Driving in and Near the Yangtze River Delta from 1995–2015     

Meina Li  Ping Yin  Xiaoyong Duan  Jinqing Liu  Jiandong Qiu  Van Phach Phung 《中国海洋大学学报(英文版)》2018,17(6):1361-1368

We analyzed the characteristics and trends of land-use change in and near the coastal zone of the Yangtze River Delta (YRD) during five periods (1995, 2000 2005, 2010, and 2015) using remotely sensed Landsat imagery. Using automatic supervised classification combined with visual interpretation, we obtained land-use information for five study areas (Nantong, Shanghai, Jiaxing, Ningbo, and Zhoushan). Significant land-use changes have occurred in this area between 1995 and 2015, characterized in particular by large reductions in cultivated land and rapid increases in urbanized land. In addition, land reclamation was very active in this period as an effective supplement to the increased demand for land development: since 1995, 1622 km² of land was reclaimed from near-coastal regions in the study area. This increase in urbanization was jointly driven by population, economic, transportation, and policy factors. Urban areas expanded from the center outward in concentric rings, with infrastructure guiding the radial expansion of development along transportation corridors, thus forming a network of connections. Due to the influence of national land regulation policies, the expansion rate of development in the YRD gradually diminished after 2010. This indicates that the area’s resource and environmental carrying capacity has reached a saturation stage in which urbanization has transitioned from broad and incremental expansion to the intensive use of land resources.  相似文献   

氯化锌/氯化胆碱离子液体单晶合成、表征及性质研究          下载免费PDF全文

邱方龙  谢少磊  姚颖  景燕  孙进贺  贾永忠 《盐湖研究》2019,27(3)

选用溶剂挥发法,以氯化胆碱和氯化锌为原料,成功合成了一种新型的Zn(Ⅱ)单晶[Ch][ZnCl₃],并采用单晶X射线衍射、红外光谱、X-粉末衍射、元素分析等对单晶结构进行表征。结果表明:该晶体属于单斜晶系,空间点群为P 21/c,晶胞参数a= 7.322(4) ?, b = 9.423(5) ?, c = 16.688(8) ?, V = 1145.8(10) ?3, Z = 4, C5H14Cl3NOZn, Mr=275.89, Dc = 1.599 g/cm3, F (000) =560, m=2.797 mm_-1, R = 0.0524 and wR =0.1434. 通过热分分析,热分解温度为：323.5℃,具有较好的热稳定性,熔点为43℃, 相变焓94.1J.cm_-3。  相似文献   

Intra-seasonal variability of Pacific-origin sea level anomalies around the Philippine Archipelago     

Xiao Chen  Bo Qiu  Xuhua Cheng  Yiquan Qi  Yan Du 《Journal of Oceanography》2015,71(3):239-249

  相似文献   

Deformation of a sandstone–mudstone particle mixture induced by periodic saturation     

Jun-Jie Wang  Zhen-Feng Qiu  Jiping Bai  Cheng Yu  Ming-Wei Liu 《Marine Georesources & Geotechnology》2018,36(4):494-503

This study focuses on the evaluation on deformation induced by periodic saturation of a sandstone–mudstone particle mixture. Two types of triaxial tests, without and with periodic saturation, were performed. The strain–stress relationships from the two types of tests indicate that the periodic saturation may induce an increment of axial strain (Δε), and the Δε values are related to the ratio of confining to atmospheric pressure (σ₃/p_a), stress level for periodic saturation (L), and number of periodic saturation or cycles (N). The values of Δε are increasing along logarithmic curves with increment of N value from 1 to 20, and increase along straight lines with increasing L value from 0.18 to 0.82 or σ₃/p_a value from 1 to 4. Based on the analyses of experimental data, a logarithmic fitting equation, which is a function of N, L, and σ₃/p_a, is suggested to predict the Δε value. And based on the fitting equation and simple analyses on stress state, another equation, which may be used to estimate the settlement induced by periodic saturation of a large-area foundation filled using the sandstone–mudstone particle mixture, is also suggested.  相似文献   

冬季台湾海峡²¹⁰Po和²¹⁰Pb的分布特征及颗粒物的输出     

张立浩  杨伟锋  陈敏  朱义年  王宙  方仔铭  邱雨生  李艳红 《海洋学报(英文版)》2020,39(2):12-21

~(210) Po and ~(210) Pb are increasingly used to constrain particle dynamics in the open oceans, however they are less used in coastal waters. Here, distributions and partitions of ~(210) Po and ~(210) Pb were examined in the Taiwan Strait, as well as their application to quantify particle sinking. Activity concentrations of dissolved ~(210) Po and ~(210) Pb(0.6 μm)ranged from 1.21 to 7.63 dpm/(100 L) and from 1.07 to 6.33 dpm/(100 L), respectively. Activity concentrations of particulate ~(210) Po and ~(210) Pb varied from 1.96 to 36.74 dpm/(100 L) and from 3.11 to 38.06 dpm/(100 L). Overall,particulate ~(210) Po and ~(210) Pb accounted for the majority of the bulk ~(210) Po and ~(210) Pb. 210 Po either in dissolved or particulate phases showed similar spatial patterns to 210 Pb, indicating similar mechanisms for controlling the distributions of ~(210) Po and ~(210) Pb in the Taiwan Strait. The different fractionation coefficients indicated that particles in the Zhemin Coastal Current(ZCC) inclined to absorb 210 Po prior to 210 Pb while they showed an opposite effect in the Taiwan Warm Current(TWC). Based on the disequilibria between ~(210) Po and ~(210) Pb, the sinking fluxes of total particulate matter(TPM) were estimated to range from –0.22 to 3.84 g/(m2·d), showing an overall comparable spatial distribution to previous reported sediment accumulation rates. However, our sinking fluxes were lower than the sedimentation rates, indicating a sediment resuspension in winter and horizontal transport of particulate matter from the Taiwan Strait to the East China Sea.  相似文献   

钻孔应变台站记震能力研究   总被引：4，自引：0，他引：4  

宋茉  邱泽华  唐磊 《大地测量与地球动力学》2010,30(Z2)

以昌平台体应变为例,研究了体现钻孔应变台站记震能力的方法,并对计算步骤和处理方法进行了说明.选取20套中国大陆观测时间较长且数据较好的钻孔体应变仪观测记录作为研究对象,计算出其各自的记震能力线,给出各台对6级地震的响应范围.此公式不仅可以量化钻孔应变仪的对地震的反应能力,而且是对地震仪器的一种新的科学评估方法.同时,基于地震前兆释放能量小于地震发生时释放的能量的基本理解,此结果对于确定地震前兆的位置和震级范围也有参考价值.  相似文献   

2003年甘肃民乐——山丹地震隐伏发震构造的浅层地震勘探研究   总被引：1，自引：0，他引：1       下载免费PDF全文

卢育霞  袁道阳  胡明清  裘国荣  刘琨  张莲海  王伟锋 《地震学报》2010,32(3):351-360

采用浅层高分辨率多次覆盖共中心点地震反射技术,对2003年10月25日民乐—山丹地震隐伏发震构造:民乐—永昌断裂和童子坝河断裂,进行了地球物理勘探研究.地震勘探剖面揭示,民乐—永昌隐伏断裂与先前推测的断裂性质基本一致,为逆冲断层,倾向北东,倾角越往深部越缓,约在30°—45°之间,测线处上断点深度小于15m;童子坝河隐伏断裂根据地震剖面结合地貌特征及区域应力分析,可判定具正断层特性,倾向南西,倾角约77°,并非以前所认为的逆冲断层.上述两条断裂于晚第四纪表现出了一定的新活动性,其共同作用导致了2003年10月25日民乐—山丹MS6.1和MS5.8地震的发生.  相似文献   

青海地区井水温度(地温)的数字化观测及地震前兆监测效能评估     

邱鹏成  王永刚  杨广华 《地震地磁观测与研究》2010,31(4):66-71

较为系统的分析了青海地区"十五"期间架设的12个数字化水温(地温)井的观测现状,及年、月、日不同层次上的动态特征,对其在相关的地震前兆观测中发挥效能的可能性作了宏观的评估。结果表明,有10个井孔可在地震中期前兆监测中发挥效能,有7个井孔可在地震短期的前兆监测中发挥效能,有7个井孔可在地震短临前兆监测中发挥效能。文中还介绍了主要影响数字化水温(地温)资料的干扰因素。  相似文献   

壳内岩浆层演化的盆地效应:以中国东南部中生代盆地为例   总被引：2，自引：2，他引：0       下载免费PDF全文

王晶  陈国能  Rodney Grapes  邱燕 《地学前缘》2011,18(1):24-31

中国东南部中生代发育有拗陷型、断裂型、断陷型3种不同类型的盆地,其中前者发育于晚三叠世-早侏罗世,其内多为含煤建造;次者发育于中侏罗世-早白垩世,主要为火山岩建造;后者发育于白垩纪-古近纪,主要为陆相红岩建造。研究结果表明,盆地构造类型的演化与该区中生代壳内岩浆层的演化密切相关。与联合古陆解体相伴随的古太平洋板块俯冲使得东亚陆缘岩石圈的内能逐渐升高,其结果是壳内岩浆层的形成和增厚以及其上盖层岩石的弯曲变形,导致中生代早期众多拗陷盆地的形成;燕山早期的构造运动使印支期已强烈变形的地壳进一步破裂,为壳内岩浆层的物质溢出或喷发提供了通道条件,从而在重熔界面(岩浆层上界面)埋深较浅的本区东部形成众多火山岩盆地;系统内能在晚侏罗世后逐渐下降,地壳冷却收缩使得断块的重力调整逐渐占主导位置,形成众多由正断层控制的断陷盆地。  相似文献