Origin of blocky aragonite cement in Cenozoic glaciomarine sediments,McMurdo Sound,Antarctica     

Mingyu Yang  Tracy D. Frank  Christopher R. Fielding  Megan E. Smith  Peter K. Swart 《Sedimentology》2020,67(2):721-741

Inorganic aragonite occurs in a wide spectrum of depositional environments and its precipitation is controlled by complex physio-chemical factors. This study investigates diagenetic conditions that led to aragonite cement precipitation in Cenozoic glaciomarine deposits of McMurdo Sound, Antarctica. A total of 42 sandstones that host intergranular cement were collected from the CIROS-1 core, located proximal to the terminus of Ferrar Glacier. Standard petrography, Raman spectroscopy and electron microprobe analysis reveal a prominent aragonite cement phase that occurs as a pore-filling blocky fabric throughout the core. Oxygen isotope compositions (δ¹⁸O = −30·0 to −8·6‰ Vienna Pee-Dee Belemnite) and clumped isotope temperatures (TΔ₄₇ = 13·1 to 31·5°C) determined from the aragonite cements provide precise constraints on isotopic compositions (δ¹⁸O_w) of the parent fluid, which mostly range from −10·8 to −7·2‰ Vienna Standard Mean Ocean Water. The fluid δ¹⁸O_w values are consistent with those of pore water, previously identified as cryogenic brine in the nearby AND-2A core. Petrographic and geochemical data suggest that aragonite cement in the CIROS-1 core precipitated from a similar brine. The brine likely formed and infiltrated sediments in flooded glacial valleys along the western margin of McMurdo Sound during the middle Miocene Climatic Transition, and subsequently flowed basinward in the subsurface. Consequently, the brine forms as a longstanding subsurface fluid that has saturated Cenozoic sediments below southern McMurdo Sound since at least the middle Miocene. Aragonite cementation in the CIROS-1 core is interpreted to reflect its proximal position to sites of brine formation and greater likelihood of experiencing brines with sustained high carbonate saturation states and Mg/Ca ratios. This unusual occurrence expands the range of known natural occurrences of aragonite cement. Given the potential for cryogenic brine formation in glaciomarine settings, blocky aragonite, as the end member of the spectrum of aragonite cement morphology, may be more widespread in glaciomarine sediments than currently thought.  相似文献   

台风登陆广东沿海前后亮温相对功率谱的变化特征分析     

章鑫  陈明玉 《热带海洋学报》2019,38(6):29-40

在2008—2017年间登陆广东沿海的台风多达25个, 但台风登陆区域周边出现的热辐射异常现象并未引起太多关注。本文利用中国静止气象卫星FY-2C/2E红外遥感亮温资料, 对台风登陆引起的热辐射异常进行分析, 并使用亮温相对功率谱对台风登陆前后热辐射时空分布进行量化。研究发现: 伴随台风的登陆, 大于5倍以上背景值的亮温相对功率谱经历了产生—增加—极大值—减弱—消亡的过程, 其持续时间长于台风过程; 亮温相对功率谱增强的区域与台风登陆路径有一定的相关性, 受限于陆地条件和海洋热量供给; 通过分析台风登陆路径和台风登陆过程中亮温相对功率谱变化趋势可知, 台风登陆前后热辐射持续10~20d, 期间的热异常都与台风过程相关。台风登陆导致热辐射的机制可能与海洋表面降温、水汽聚集等因素有关, 即台风吸收的海洋热量随环流上升过程被海—气相互作用所调制, 导致不同频段和区域出现热辐射差异。  相似文献   

面向治理能力现代化要求的建筑实体获取和应用北大核心CSCD     

程铭宇  吴幼丝 《测绘通报》2022,(10):166-170

城市是复杂开放的巨系统,其治理存在底盘不清、调查配合度不高的难题,亟须一种科学精准、即时落地的管理手段。本文面向治理现代化的要求,研究了一种非接触式的厘米级高精度快速城市倾斜模型采集方法,提高底盘摸查效率;同时通过结构化与简化聚合建立图元、建筑实体、建筑单体的对应逻辑关系,结合获取的基本与管理属性,搭建全周期跟踪综合管理平台。实际应用表明,本文为实现城市建设信息精细化管理提供了有效的借鉴。  相似文献   

地下水污染控制修复技术研究趋势及热点分析   总被引：3，自引：2，他引：1       下载免费PDF全文

李玮  王明玉  刘丽雅  刘波  陈亚伟 《水文地质工程地质》2015,(2):120-125

对地下水污染控制修复技术SCI论文及专利数据进行检索统计,使用Cite SpaceⅢ数据可视化软件,对地下水污染控制修复技术研究发展趋势进行分析,探索潜在研究前沿及热点问题。结果显示,抽出处理等传统污染控制修复技术的研究关注度不断下降,原位修复技术、生物修复技术等为现阶段研究和应用的重点。针对砷、铀等典型污染物的修复技术,包括纳米技术、微生物技术等为目前研究的前沿,针对药品、MTBE等污染物的控制修复技术研究可能在未来成为新的研究前沿。中国地下水污染控制修复研究起步较晚,但发展迅速。  相似文献   

Cryopreservation of Veliger Larvae of Trumpet Shell, Charonia sauliae： an Essential Preparation to Artificial Propagation     

KANG Kyoung Ho 《中国海洋大学学报(英文版)》2009,8(3):265-269

Trumpet shell, Charonia sauliae, is an endangered and valuable species, but its artificial propagation protocol has not been successfully established. To estimate the possibility of cryopreservation for larvae of C. sauliae, which is a potential preparation for its artificial reproduction and further research, in this study a protocol for the cryopreservation of veliger larvae of trumpet shell was optimized. Through a two-step cryopreservation procedure, four kinds of cryoprotectants (ethylene glycol, 1, 2-propanediol, dimethyl sulfoxide and glycerol) were employed at three concentrations (1.0, 1.5 and 2.0 molL⁻¹) respectively and survival rates of larvae were determined after a storage of 1h. The larvae frozen with these four cryoprotectants after 1 h storage were cultured, and then survival rates were determined at 24, 72 and 120 h after thawing. Dimethyl sulfoxide at a concentration of 1.5 molL⁻¹ showed the best protective effect in all experiments (p<0.05). And survival rates of larvae frozen with dimethyl sulfoxide were determined after 1, 7 and 15 d of storage. The survival rates of larvae frozen with 1.5 molL⁻¹ dimethyl sulfoxide after 1 h, 1 d, 7 d and 15 d of storage were 80.77% ±7.51%, 80.34% ±11.28%, 83.10% ±9.14% and 77.23% ±6.22% respectively. No significant differences in survival rates of larvae frozen with dimethyl sulfoxide were observed after various storage periods (p>0.05).  相似文献   

Measurements Of Fine-Scale Structure At The Top Of Marine Stratocumulus     

Donald H. Lenschow  Mingyu Zhou  Xubin Zeng  Lianshou Chen  Xiangde Xu 《Boundary-Layer Meteorology》2000,97(2):331-357

During the Dynamics and Chemistry of the MarineStratocumulus (DYCOMS) experiment in July–August 1985, the NCAR Electra aircraft flew a series of flight legs just at the top of the marinestratocumulus cloud decks that cap the mixed layer off the coast of southernCalifornia. Because of the corrugated structure of the cloud-top, the aircraft, which was flown at a nearly constant level and adjusted only to maintain its altitude at the average cloud-top height, was alternately within and above the clouds – roughly half the time in each domain. These legs were used to examine the structure of the cloud-top by compositing the segments on either side of the cloud/clear-air interface, which was identified by the transitions of liquid water measured by the Forward Scattering Spectrometer Probe (either increasing or decreasing) through a threshold of 0.04 × 10^-3 kg m^-3.An equivalent vertical distance (EVD) from the cloud-top was obtained from the horizontal flight legs by estimating the average slope of the cloud-top from the cloud-top radiation temperature. The results show that a near discontinuity occurs in variables across cloud top over an EVD of 0.3 m, but that above this, the air has already been modified by boundary-layer air. Thus, cloud-top is not the limit of mixing of boundary-layer air. This mixing may extend to tens of metres or more. The bulk Richardson number in the vicinity of cloud-top increases from near zero within the cloud to about 1.2 at an EVD of 3–6 m above cloud. Fluctuations of the three velocity components within cloud are nearly equal; above cloud the vertical component structure function is about half the horizontal components. The scalar structure functions are about an order of magnitude higher above cloud than in cloud. The structure parameters of temperature and humidity measured just below cloud-top agree reasonably well with predicted values based on a previously-developed model for the clear convective boundary layer. Above cloud, the scalar structure parameters are much larger, but their interpretation is questionable, since this region does notcontain isotropic turbulence.  相似文献   

Impacts of different types of El Niño and La Niña on northern tropical Atlantic sea surface temperature     

Renguang Wu  Mingyu Lin  Huamin Sun 《Climate Dynamics》2020,54(9):4147-4167

The present study investigates the dependence of the northern tropical Atlantic (NTA) sea surface temperature (SST) response to El Niño and La Niña events on the decay time and amplitude of tropical Pacific SST anomalies. It is found that the NTA SST response to La Niña events displays a notable difference between late and early decaying events, similar to that in response to El Niño events, but with a weaker signal. Latent heat flux is a dominant term in the NTA SST change in preceding winter-early spring in both El Niño and La Niña events and in the difference of the NTA SST anomaly between late and early decaying El Niño and La Niña events. The zonal and meridional advections have an opposite effect on the NTA SST warming in late decaying El Niño events. Although the warming in the NTA region is similar in late decaying moderate and strong El Niño events, the distribution of the SST anomalies in the mid-latitude North Atlantic Ocean shows a notable difference between the two types of late decaying El Niño events. The SST anomalies also display difference in the early decaying weak and moderate El Niño events. Surface heat flux differences are largely attributed to wind differences.  相似文献   

欧亚大陆极端降水事件的区域变化特征          下载免费PDF全文

李铭宇  韩婷婷  郝鑫 《大气科学学报》2020,43(4):687-698

近年来,在全球变暖的背景下,极端气候事件特别是极端降水事件,发生频率愈发上升。本文使用美国气候预测中心提供的逐日降水资料,统计分析了1979—2018年期间欧亚大陆各个子区域极端降水事件的时空变化特征。结果表明:1)从气候态的空间分布特征来看,南欧、南亚、东南亚、东亚地区为欧亚大陆全年总降水量高值区,同时也是极端强降水频发地区;而东亚地区青藏高原、中国中西部至蒙古一带,南亚地区印度次大陆以及中亚、西亚等地的部分地区则是连续性干旱事件的高频区,极端强降水事件发生频次较少;2)在21世纪初之后,东南亚、南亚、东亚、北亚、西亚和南欧这6个地区的全年总降水量发生年代际增加,且在研究时段呈显著增加趋势。在过去近40 a,南亚、东亚和中亚的RX1day(日最大降水量)、RX5day(连续5 d最大降水量)、中雨日数(R10mm)、大雨日数(R20mm)自20世纪90年代中期年代际增加,且呈长期增加趋势。南亚、北亚、东亚、中亚这4个地区的最大连续干旱日数在20世纪80年代初显著增加,但长期趋势并不显著。需要指出的是,自2014年起极端强降水事件在东南亚、南亚和东亚地区持续增多,而连续性干旱事件在北欧地区持续增多。  相似文献   

Hox genes and study of Hox genes in crustacean   总被引：1，自引：0，他引：1  

侯林陈志娟  徐明玉林盛国 王璐 《中国海洋湖沼学报》2004,22(4):392-398

  相似文献   

TIPEX高原东南部近地层湍流参数的分析   总被引：8，自引：0，他引：8  

BIAN Lingen  XU Xiangde  LU Longhu  GAO Zhiqiu  ZHOU Mingyu  LIU Huizhi 《大气科学进展》2003,20(3):369-378

The characteristics of the turbulence spectrum, turbulence variance, and turbulence flux at Qamdo overthe Southeastern Tibetan Plateau measured during the TIPEX experiment from 18 May to 30 June 1998are analyzed by the eddy correlation method. During periods of intense convection, most of the spectraof the 3D winds, temperature, and humidity follow a power law with a slope of -2/3. The normalizedvariances of the 3D winds in relation to z/L satisfy the similarity law but the normalized variances oftemperature and humidity are related to z/L by a -1/3 power law only in unstable conditions. In near-neutral stratification, σu/u* and σy/u* at Qamdo and Gerze are nearly constant in rugged terrain andσw/u* at Qamdo and Gerze is similar to the value found in plains, which indicates that the, effects oflandform on vertical turbulence is not significant over the southeast and western Tibetan Plateau. Duringthe dry period, the sensible heat dominates, comprising 81% of the heat intensity, with the other 19%being latent heat; during the wet period on the other hand, the latent heat accounts for about 64% ofthe available energy and the sensible heat only around 36%. The maximum intensity of the heating of airoccurs in the middle of the Plateau during the summertime.  相似文献