新西兰海潮负荷位移建模精度分析     

刘中冠  袁林果  陈昌福  成帅  张迪 《大地测量与地球动力学》2021,41(4):387-391

为评价新西兰海潮负荷位移建模精度,利用新西兰189个GPS站11 a的实测数据,基于静态精密单点定位测定8个半日潮波及周日潮波的海潮负荷位移参数,并将其与7种全球海潮模型及4种地球模型计算的海潮负荷位移改正值进行比较。结果表明：1）TPXO7.2模型负荷位移改正值与GPS解算的海潮负荷位移参数最符合,M2、N2、O1和Q1潮波均方根误差在水平方向小于0.5 mm,垂直方向小于0.7 mm;2）不同地球模型对确定海潮负荷位移的影响主要体现在M2和N2潮波;3）GPS估值和海潮模型值之间的残差矢量呈现出大小及方向上的区域一致性,部分站点异常的残差值可能反映出当前SNREI地球模型的缺陷。  相似文献   

高淀粉水平下精氨酸对松浦镜鲤肠道形态与功能的影响     

李晋南  王常安  张圆圆  吴迪  范泽  王连生 《广东海洋大学学报》2021,(1)

【目的】探讨高淀粉饲料中添加精氨酸对松浦镜鲤(CyprinuscarpioL.)肠道消化酶活性及肠道形态的影响。【方法】选用初始体质量(6.84±0.02)g的松浦镜鲤360尾,随机分为5组,每组4个重复,每个重复18尾鱼。实验饲料分为5组,分别在45%水平的高淀粉饲料中添加质量分数0%、0.6%、1.2%、1.8%、2.4%的精氨酸,实验周期为8周,进行肠道消化酶和形态的测定。【结果】前、中、后肠的淀粉酶活性,各组之间没有显著差异(P> 0.05);添加2.4%精氨酸组的前肠脂肪酶活性显著高于对照组(P <0.05),中肠和后肠的脂肪酶活性各组间没有显著差异(P>0.05);前、中、后肠蛋白酶活性随精氨酸添加量的增加而增加,添加1.8%和2.4%精氨酸组的前肠和中肠蛋白酶活性显著高于对照组(P<0.05),添加2.4%精氨酸组后肠的蛋白酶活性显著高于对照组(P<0.05)。高淀粉饲料中添加Arg显著影响了肠道皱襞高度,但对肠绒毛宽度和肌层厚度没有显著影响。2.4%精氨酸组前肠皱襞高度显著高于其他各组(P <0.05),1.8%精氨酸组中肠和后肠皱襞高度显著高于对照组(P <0.05)。1.2%、1.8%和2.4%组肠体指数显著高于对照组(P <0.05),2.4%精氨酸组肠长指数显著高于对照组(P <0.05)。各组前、中、后肠肠绒毛密度没有显著差异,且排列较整齐。【结论】高淀粉饲料中添加1.8%~2.4%精氨酸可以增加松浦镜鲤肠道消化酶活性,同时改善了松浦镜鲤的肠道形态结构。  相似文献   

河套地区典型干线的形成及其在对流触发中的作用     

张一平  俞小鼎  王迪  郝晓珍  王金兰 《气象学报》2022,80(1):39-53

利用高空、加密地面、EC-ERA5(0.25o×0.25o)再分析和FY-2系列静止气象卫星云图(可见光星下点分辨率1.25 km,红外5 km)等资料,对黄河河套地区3次典型干线的形成及其在对流触发中的作用进行了详细分析.结果表明:(1)3次干线触发对流出现在中高纬度高空槽东移诱发蒙古气旋发展的背景下,高低空系统配置...  相似文献   

基础测绘转型升级融入自然资源管理的思考     

吴迪  汪建光 《地理空间信息》2022,20(4):44-47,146

在自然资源管理机构改革的大背景下,围绕浙江省基础测绘工作运行的实际情况,分析了浙江省基础测绘融入自然资源管理体系的现状和存在的问题.就如何提升基础测绘支撑职责"两统一"管理能力,提出了构建多种适应新形势的统筹机制,以保障基础测绘各项工作向纵深开展、优化产品形式和产品的更新频率,提升基础测绘服务水平和服务能力、提升技术水...  相似文献   

Adsorption behaviors of Cd^2＋ on Fe2O3/MnO2 and the effects of coexisting ions under alkaline conditions   总被引：2，自引：0，他引：2  

Zuwei Wang  Xiangfeng Zeng  Xiaoman Yu  Hui Zhang  Zhaojiang Li  Di Jin 《中国地球化学学报》2010,29(2):197-203

This study describes the adsorption features of cadmium on Fe2O3 and MnO2 in alkaline saline conditions. The adsorption reached equilibrium in 6 hours under alkaline conditions. The absorption of cadmium on Fe2O3 and MnO2 was consistent with Freundlich absorption isotherms, and the corresponding adsorption capacities were 16.3 and 16.7 mg·g-1, respectively. Moreover, the adsorption quantity of cadmium on Fe2O3 and MnO2 rose with increasing pH from acidic to neutral, and reached the maximum at pH= 9. The coexisting chlorides reduced the adsorption capacity of Fe2O3 and MnO2. The influence intensities of different cations follow the order of CaCl2>>KCl>NaCl. However, the influence of sodium salts on the capacities of Fe2O3 and MnO2 to adsorb cadmium appeared more complicated: the relatively low concentrations of sodium salts could reduce the adsorption capacity; with increasing concentrations of sodium salts, e.g. NaCl and NaNO3. The adsorption capacity decreased continually. Moreover, due to the competition adsorption and precipitation effects, the adsorption capabilities of Na2CO3, NaH2PO4 and Na2HSO4 could also be reduced and cadmium concentrations in the solution were reduced as well.  相似文献   

Stratigraphic evolution from shoreface to shelf-indenting channel depositional systems during transgression: Insights from the lower Pliocene Súa Member of the basal Upper Onzole Formation,Borbón Basin,northwest Ecuador     

Claudio Di Celma  Gino Cantalamessa  Walter Landini  Luca Ragaini 《Sedimentary Geology》2010,223(1-2):162-179

Shelf-indenting canyons and their tributary systems are fairly common constituents of Quaternary shelves of active continental margins, but they have been rarely reported from older successions. Recognition of these prominent geomorphologic features in the ancient record has important implications not only for a proper understanding of shoreface-to-shelf depositional systems, but also from a petroleum exploration standpoint as they represent efficient conduits for moving coarse-grained river- and nearshore-borne sediments to the adjacent slope even during periods of relative rise in sea level.Coastal exposures of the lower Pliocene Súa Member in the surroundings of Súa (northwest Ecuador), preserve the unusual juxtaposition of incising submarine channels onto nearshore deposits. This succession accumulated along a narrow, active continental margin during tectonically induced transgression and affords a rare opportunity to evaluate the stratigraphic evolution of such systems from an outcrop perspective. A comprehensive facies characterization combined with application of sequence stratigraphic concepts has led to definition of the following physical surfaces and stratal units in ascending order. (i) A polygenetic, regionally extensive erosional surface resulting from the superposition of the wave ravinement surface onto the previous subaerial sequence boundary (SB/wRS). (ii) A nearshore, sand-prone lithofacies succession comprising a condensed basal shellbed deepening upwards through lower-shoreface bioturbated silty sandstones, into inner shelf sandy mudstones. (iii) Two steep, U-shaped erosional features (turbidite shelf-entrenchment surfaces), interpreted as shelf channels, deeply incised into the subjacent nearshore sediments and marking an abrupt deepening of facies. (iv) A thick, fining-upward sedimentary succession laid down within the confines of the channels by high- and low-density turbidity currents and including both bed-load (traction) and suspended-load deposits; the overall fining- and thinning-upward character exhibited by the infill of these channels is thought to reflect decreasing flow energies and is consistent with the gradual cut-off of clastic influx to their upper reaches in response to progressive detachment from an adjacent coastal source during relative rise in sea level.Based on detailed analysis of facies and a sequence stratigraphic interpretation of outcrop data, this study contributes to extend the existing sequence stratigraphic schemes, further attesting that shelf-sediment bypass and deep-water sedimentation can take place at sea levels other than lowstand.  相似文献   

柴达木盆地北缘都兰地区旺尕秀辉长杂岩的锆石LA—ICP—MS U—Pb年龄及地质意义     

朱小辉  陈丹玲  刘良  李涤 《中国区域地质》2010,(2):227-236

详细的地球化学研究表明,柴北缘旺尕秀辉长杂岩（包括辉长岩、辉绿岩和斜长岩）具有岛弧火山岩的特征,形成于岛弧环境。对辉长岩中锆石的阴极发光图像和微量元素的研究显示,所有的锆石均具有相对宽缓的振荡环带结构和轻稀土元素亏损、重稀土元素明显富集的典型基性岩浆锆石的特征。通过锆石LA—ICP—MSU-Th-Pb同位素分析,得到^206Pb／^238U加权平均年龄468Ma＋2Ma,同时得到一个最大的谐和年龄522Ma＋9Ma．表明旺尕秀辉长杂岩的形成时代应介于468-522Ma之间。岛孤型旺尕秀辉长杂岩时代的确定,结合本区已有的研究成果,表明柴北缘确实存在古生代洋盆事件,至少从中奥陶世开始发生板块的俯冲消减作用．从侧面说明柴北缘陆壳深俯冲的时代不应早于460Ma。  相似文献   

Real time monitoring of structures in task force missions: the example of the Mw = 6.3 Central Italy Earthquake, April 6, 2009     

M. Picozzi  R. Ditommaso  S. Parolai  M. Mucciarelli  C. Milkereit  M. Sobiesiak  D. Di Giacomo  M. R. Gallipoli  M. Pilz  M. Vona  J. Zschau 《Natural Hazards》2010,52(2):253-256

  相似文献   

Structural setting of the Southern Apennine fold-and-thrust belt (Italy) at hypocentral depth: The Calore Valley case history     

Daniela Di Bucci  Bruno Massa  Milly Tornaghi  Agostino Zuppetta 《Journal of Geodynamics》2006,42(4-5):175-193

The reconstruction of the main structural features of the Southern Apennines (Italy), in correspondence with the focal volume of some strong earthquakes that have affected this chain, can be attempted by analysing reflection seismic lines and deep well logs in comparison with surface geology.For instance, the Calore Valley and its surroundings have been the object of intense hydrocarbon exploration, and a wealth of subsurface data is available. Moreover, this area was affected by the 1688 Sannio earthquake (macroseismic magnitude 7.1), and a new location has recently been proposed for the related causative fault system. The present work defines the structural setting of the Southern Apennine chain in correspondence with this new location, and compares it with similar cases along the Italian peninsula.The analysis was focussed on the reconstruction of deep tectonic units (formed by the buried Apulia carbonate platform succession), which generally correspond to the hypocentral depths of strong earthquakes along the axis of the Southern Apennines. The results show that the Apulia platform succession is affected by three main thrusts, locally accompanied by backthrusts. The top of this succession is relatively shallow: the maximum depth does not exceed 1.8 s TWT (i.e. about 3500 m b.s.l.), while minimum depths occur in correspondence with the ramp anticlines culminations, at 0.5 s TWT (i.e. at about 500 m b.s.l.). Moreover, data suggest that the underlying Paleozoic basement is possibly involved in thrusting.In a regional perspective, extensional seismogenic structures along the axis of the Southern Apennines seem to share some common characteristics. Indeed, they develop (i) in correspondence with an uplifted Paleozoic basement; (ii) at the rear of a set of thrusts that account for the shallow Apulia units; (iii) at the surface, in proximity to the leading edge of a surficial tectonic unit formed by the Apennine carbonate platform succession. The 1688 seismogenic fault system fits in with these common traits. In the light of this, we finally speculate that these common characteristics in the architecture of the chain could provide a key to the location of the major seismicity along the axis of the Southern Apennines and an interpretative model for the identification of possible areas of seismic gap in this part of the Italian peninsula.  相似文献   

黄土高原夏季极端降水及其成因分析     

卢珊  胡泽勇  付春伟  樊威伟  吴笛 《高原气象》2022,(1):241-254

利用1961-2016年夏季黄土高原地区64个气象监测站的逐日降水资料及同期NCEP/NCAR再分析数据,分析了近56年黄土高原夏季极端降水的时空变化特征,并对比了极端降水强弱年以及不同年代黄土高原地区夏季大气环流形势的异同.结果表明,黄土高原夏季极端降水占夏季总降水量的54％左右,总体上呈现出东多西少的空间分布特征....  相似文献