Mafic and felsic magmatism in the Wadi Kalalat area, South Eastern Desert, Egypt: mineralogy, geochemistry and geodynamic evolution during the Neoproterozoic in the Nubian Shield

In the south Eastern Desert of Egypt,two contrasting types of magmatism(mafic and felsic) are recorded in the Wadi Kalalat area,and form the Gabal El Motaghiarat and Gabal Batuga intrusions,respectively.The two intrusions post-dates ophiolitic and arc associations represented by serpentinite and metagabbro-diorite,respectively.The mafic intrusion has a basal ultramafic member represented by fresh peridotite,which is followed upward by olivine gabbro and anorthositic or leucogabbro.This mafic intrusion pertains to the Alaskan-type mafic-ultramafic intrusions in the Arabian-Nubian Shield(ANS)being of tholeiitic nature and emplaced in a typical arc setting.On the other hand,the Gabal Batuga intrusion comprises three varieties of fresh A-type granites of high K-calc alkaline nature,which is peraluminous and garnetbearing in parts.A narrow thermal aureole in the olivine gabbro of the mafic intrusion was developed due to the intrusion of the Batuga granites.This results in the development of a hornfelsic melagabbro variety in which the composition changed from tholeiitic to a calc-alkaline composition due to the addition of S_(i)O_(2),Al_(2)O_(3),alkalis,lithosphile elements(LILEs) such as Rb(70 ppm) and Y(28 ppm) from the felsic intrusion.Outside the thermal aureole,Rb amounts 2-8 ppm and Y lies in the range <2-6ppm.It is believed that the Gabal Batuga felsic intrusion started to emplace during the waning stage of an arc system,with transition from the pre-collisional(i.e.,arc setting) to post-collisional and within plate settings.Magma from which the Gabal Batuga granites were fractionated is high-K calc-alkaline giving rise to a typical post-collisional A-type granite(A_(2)-subtype) indicating an origin from an underplating crustal source.Accordingly,it is stressed here that the younger granites in the ANS are not exclusively post-collisional and within-plate but most likely they started to develop before closure of the arc system.The possible source(s) of mafic magmas that resulted in the formation of the two intrusions are discussed.Mineralogical and geochemical data of the post-intrusion dykes(mafic and felsic) suggest typical active continental rift/within-plate settings.

BSN:The First Light Curve Analysis of the Total Eclipse Binary System EL Tuc

We conducted the first light curve study of the binary star EL Tuc within the Binary Systems of South and North project's framework.The photometric observations were made using standard multiband BVR_cI_c filters at an observatory in Argentina.We presented a new ephemeris for EL Tuc and a linear fit to the O–C diagram,utilizing our extracted times of minima and additional literature.We employed the PHysics Of Eclipsing BinariEs Python code and the Markov chain Monte Carlo approach for the system's light curve analysis.The target system's light curve solution required a cold starspot on the hotter component.We conclude that EL Tuc is a total contact binary system with a low mass ratio of q=0.172±0.002,an orbital inclination of i=83°.74±0°.40,and a fillout factor of f=53.7%±1.6%.We used the P-a relationship and the Gaia Data Release 3 parallax method to determine the absolute parameters of EL Tuc to compare the precision of our results.This system was classified as W-type based on the mass and effective temperature of the companion stars.The positions of the systems were depicted on the M-L,M-R,T-M,and q-Lratiodiagrams.The relationship between the spectroscopic and photometric mass ratios of binaries was discussed.

CMIP 6 models simulation of the connection between North/South Pacific Meridional Mode and ENSO

The subtropical North and South Pacific Meridional Modes(NPMM and SPMM)are well known precursors of El Niño-Southern Oscillation(ENSO).However,relationship between them is not constant.In the early 1980,the relationship experienced an interdecadal transition.Changes in this connection can be attributed mainly to the phase change of the Pacific decadal oscillation(PDO).During the positive phase of PDO,a shallower thermocline in the central Pacific is responsible for the stronger trade wind charging(TWC)mechanism,which leads to a stronger equatorial subsurface temperature evolution.This dynamic process strengthens the connection between NPMM and ENSO.Associated with the negative phase of PDO,a shallower thermocline over southeastern Pacific allows an enhanced wind-evaporation-SST(WES)feedback,strengthening the connection between SPMM and ENSO.Using 35 Coupled Model Intercomparison Project Phase 6(CMIP6)models,we examined the NPMM/SPMM performance and its connection with ENSO in the historical runs.The great majority of CMIP6 models can reproduce the pattern of NPMM and SPMM well,but they reveal discrepant ENSO and NPMM/SPMM relationship.The intermodal uncertainty for the connection of NPMM-ENSO is due to different TWC mechanism.A stronger TWC mechanism will enhance NPMM forcing.For SPMM,few models can simulate a good relationship with ENSO.The intermodel spread in the relationship of SPMM and ENSO owing to SST bias in the southeastern Pacific,as WES feedback is stronger when the southeastern Pacific is warmer.

Dynamical Predictability of Leading Interannual Variability Modes of the Asian-Australian Monsoon in Climate Models

The dynamical prediction of the Asian-Australian monsoon(AAM)has been an important and long-standing issue in climate science.In this study,the predictability of the first two leading modes of the AAM is studied using retrospective prediction datasets from the seasonal forecasting models in four operational centers worldwide.Results show that the model predictability of the leading AAM modes is sensitive to how they are defined in different seasonal sequences,especially for the second mode.The first AAM mode,from various seasonal sequences,coincides with the El Niño phase transition in the eastern-central Pacific.The second mode,initialized from boreal summer and autumn,leads El Niño by about one year but can exist during the decay phase of El Niño when initialized from boreal winter and spring.Our findings hint that ENSO,as an early signal,is conducive to better performance of model predictions in capturing the spatiotemporal variations of the leading AAM modes.Still,the persistence barrier of ENSO in spring leads to poor forecasting skills of spatial features.The multimodel ensemble(MME)mean shows some advantage in capturing the spatiotemporal variations of the AAM modes but does not provide a significant improvement in predicting its temporal features compared to the best individual models in predicting its temporal features.The BCC_CSM1.1M shows promising skill in predicting the two AAM indices associated with two leading AAM modes.The predictability demonstrated in this study is potentially useful for AAM prediction in operational and climate services.

The Subsurface and Surface Indian Ocean Dipoles and Their Association with ENSO in CMIP6 models

This study assesses the reproducibility of 31 historical simulations from 1850 to 2014 in the Coupled Model Intercomparison Project phase 6(CMIP6) for the subsurface(Sub-IOD) and surface Indian Ocean Dipole(IOD) and their association with El Ni?o-Southern Oscillation(ENSO). Most CMIP6 models can reproduce the leading east-west dipole oscillation mode of heat content anomalies in the tropical Indian Ocean(TIO) but largely overestimate the amplitude and the dominant period of the Sub-IOD. Associated with the much steeper west-to-east thermocline tilt of the TIO, the vertical coupling between the Sub-IOD and IOD is overly strong in most CMIP6 models compared to that in the Ocean Reanalysis System 4(ORAS4). Related to this, most models also show a much tighter association of Sub-IOD and IOD events with the canonical ENSO than observations. This explains the more(less) regular Sub-IOD and IOD events in autumn in those models with stronger(weaker) surface-subsurface coupling in TIO. Though all model simulations feature a consistently low bias regarding the percentage of the winter–spring Sub-IOD events co-occurring with a Central Pacific(CP) ENSO, the linkage between a westward-centered CP-ENSO and the Sub-IOD that occurs in winter–spring, independent of the IOD, is well reproduced.

基于ELES模型和CD效用函数的“纵横双向”消费结构变动研究

探究消费升级对于促进共同富裕具有深远意义。基于CFPS 2010—2020年数据,结合扩展线性支出模型(ELES)、CD效用函数和门槛回归等方法构建了“纵横双向”识别模型,并实证考察了我国居民消费升级与消费结构状况。研究发现,2010—2020年我国居民家庭消费结构横向上呈升级趋势,但仍以生存型消费支出为主;细分“三型八类”消费,发现生存型与发展型的消费占比上升,享受型消费存在较大的消费偏好,表现出消费分层特征,且家庭消费结构呈多样化发展趋势;家庭年度总支出的三条约束线分别为60100元、122800元及122900元。纵向上发现预算约束线在不断后移,表明消费结构在不断升级。文章运用多门槛回归方法结合ELES模型构建了消费结构的综合识别模型,以此作为判断消费结构升级与否的依据和标准。

基于多源观测数据揭示中国春季沙尘活动的变化及其环流特征

本文利用1980~2021年MERRA2(Modern-Era Retrospective analysis for Research and Applications,version 2)沙尘资料,结合ERA5大气再分析数据,系统分析了中国春季沙尘的时空分布特征及相关的大气环流异常,结果表明:西北地区沙尘主导了我国春季沙尘的长期变化,二者均具有显著的2~4年和8年以上的周期变化,表现出明显的年际和年代际特征。利用EOF分析表明,EOF1主要体现我国春季沙尘,尤其是西北沙尘的年际变化,在正位相时表现出西北沙尘的显著增加。而EOF2则主要体现我国春季沙尘的年代际变化,在空间上表现为西北与中国其他地区沙尘变化的偶极子特征,其正位相为西北沙尘负异常和其他区域的正异常;在时间上则表现为20世纪90年代末由负转正的位相转变。进一步研究表明,中国春季沙尘变化与气象要素场具有显著的联系:当春季沙尘为正异常时,多为强风控制;此外,较高的地表温度和干旱少雨的背景利于土壤解冻和抑制沙尘沉降,最终造成沙尘天气的发生。此外,影响我国春季沙尘变化的下垫面海温异常表现出类拉尼娜型海温,且海温异常能够从前冬一直持续到同期春季,因此对提前预报春季沙尘变化提供一定的可能性。

1300—2019年江苏沿海风暴潮灾害时空分布特征

历史上江苏沿海曾频发2类风暴潮灾害,给当地带来了巨大损失。建立该地区长时间尺度的风暴潮灾害序列对了解过去与预测未来意义重大。以历史文献、地方志、海洋灾害公报等记载的风暴潮资料为基础,建立了风暴潮灾害识别体系,重建了1300—2019年江苏沿海风暴潮灾害序列,分析了风暴潮灾害时空变化规律,探究了其与气候异常和黄河、长江入海口变迁之间的关系。结果表明:江苏沿海地区主要受台风风暴潮灾害的影响,1300—2019年间共发生246次风暴潮灾害,平均周期为2.9年,且近100年来发生频率有增大的趋势;小波分析结果显示,风暴潮灾害年际变化存在17年、61年和115年的时间尺度周期,其中115年周期最为明显。海气相互作用影响下,厄尔尼诺活跃年江苏沿海台风风暴潮灾害偏少;气温与台风风暴潮灾害频次有一定的正相关性,但其影响机制尚不明确。盐城、南通和苏州为风暴潮灾害高发地区,常州和无锡发生频率较小。在气候变暖与江苏海岸冲淤变化的作用下,1855年后盐城和南通地区风暴潮灾害发生频率增加,连云港地区明显增加;随着海岸线的变迁与长江河口的演变,镇江、扬州、泰州与苏锡常地区受风暴潮灾害影响减少。

从能量学角度理解气候背景场对ENSO热带和热带外遥相关的影响

厄尔尼诺—南方涛动(El Ni?o-Southern Oscillation,简称ENSO)通过遥相关过程影响全球天气气候。在热带地区,ENSO能通过影响热带对流层温度导致遥远海盆降水和海表温度异常;在热带外,ENSO能通过激发准定常罗斯贝波动造成北美、亚洲等地区气候异常。气候背景场对ENSO热带和热带外遥相关有重要影响。一方面,气候背景大气环流场可以通过正压和斜压能量转换影响ENSO遥相关波列的位置和强度。另一方面,热带气候背景海温和对流场会通过影响湿静力能分布影响ENSO热带遥相关过程。这些研究表明分析能量过程有助于理解气候背景场影响ENSO遥相关的机理。本文回顾了近几十年来国内外关于气候背景场对ENSO热带与热带外遥相关影响的能量分析研究进展,在此基础上,回顾了全球变暖背景下ENSO遥相关的可能变化,并提出了一些未来该领域内需要进一步研究的科学问题。

广西大厂铜坑银锌多金属矿地质特征及银的赋存状态

地处右江盆地东北缘的铜坑矿床是大厂矿田的重要组成部分,近年来矿区内发现多处银锌多金属矿(化)体,但对于银的赋存状态以及银多金属的富集成矿规律认识十分有限。通过野外调查以及矿物学研究,将铜坑银锌矿划分为4个阶段,包括锡石-石英阶段(Ⅰ)、锡石-硫化物阶段(Ⅱ)、含银-方铅矿阶段(Ⅲ)和石英-方解石阶段(Ⅳ),发现银矿化主要发生在含银-方铅矿阶段(Ⅲ)。运用BSE-EDS和EPMA等分析方法,对矿石矿物特征以及银的赋存状态进行研究,探究了银的产出特征与富集规律,剖析了制约银产出与富集的关键因素。结果显示,铜坑银锌矿中的银以可见银(>1μm)为主,另有少量的不可见银(<1μm);可见银以辉锑银铅矿和脆硫锑银铅矿为主。辉锑银铅矿在405中段以包裹体的形式分布于方铅矿中,在455中段则以包裹体、骨针状和正交网格状分布于方铅矿中或以不规则状产于方铅矿间隙和边缘。脆硫锑银铅矿仅产出于455中段方铅矿的边缘及其间隙。不可见银则主要以类质同象或次显微包裹体的形式赋存于方铅矿以及部分含锡硫盐矿物中;方铅矿作为重要的载银矿物,Cu^(+)和Sb^(3+)都会影响Ag^(+)进入方铅矿。Cu^(+)会结合Ag^(+)沉淀于早期黝铜矿中,而非方铅矿中。Sb通过Ag^(+)^(+)Sb^(3+)=2Pb^(2+)的方式,使Ag进入方铅矿晶格,形成成矿晚期的含银硫盐矿物。

职业教育数字化转型发展的内涵特征、结构要素与实践方略

职业教育数字化转型是职业教育基于数字技术增强适应性、推进现代化发展的过程,包含以技术迭代改变职业教育发展动力结构,以秩序生成适应、支撑和引领职业教育现代化,以范式转变重塑职业教育生态的内涵特征。由此,职业教育数字化转型在技术与设施、管理与服务、理念与愿景三个维度,分别形成了关键场景重建化、数据资源增值化、适应变革敏捷化的结构要素。为推进职业教育数字化转型,应当深化职业教育与数字样态的重塑,推进职业教育与公共服务均等化的同步,促进职业教育与数字经济发展的协同,加快职业教育与技能强国战略的融合,保障职业教育与数字技术的平衡。

一种交替极永磁游标电机设计与分析

提出了一种使用低成本铁氧体磁体的交替极永磁游标电机(CPPMVM).介绍了该电机拓扑结构,提出了基于特定磁导函数的等效磁场模型来推导主磁密、调制磁密和反电动势.通过解析法和有限元法分析该电机电磁性能、气隙磁密和谐波分布.结果表明:与常规表贴式永磁游标电机(SPMVM)相比,所提出的交替极永磁游标电机机械结构简单、成本低、谐波调制作用有效、转矩密度高、抗退磁能力强.

超越边界:《奥菲奥》的后人类书写

后人类主义的提出标志着人类思维方式的质变,科学技术的发展使得人与非人类的边界变得模糊和消除。理查德·鲍尔斯的小说《奥菲奥》彰显了超越生命、跨越边界、万物相连的后人类理念。从后人类主义的视角探究了小说呈现给读者的人与动物等非人类之间的多重关系,旨在引发人们关注跨物种平等共存、和谐相依的后人类愿景。

文旅融合理念下农业观光园景观设计中农业文化元素的融入路径探讨

以文旅融合为研究背景,以农业文化元素在河南省信阳市新县农业观光园景观设计中的应用为例,对农业观光园景观设计中农业文化元素的融入进行分析,从而在这种模式引导下,打造出更具深度和特色的农业观光景观。提出农业观光园景观设计应当坚持因地制宜的发展原则,从而将其农业结构、基础设施、休闲娱乐和文化教育等方面进行多元融合和立体交叉,推动文化产业与旅游业协调发展,开创农业园区规划和发展的新局面。

厄尔尼诺下崇左市极端气象干旱对甘蔗生长影响

利用崇左市7个国家级地面气象观测站1981~2023年逐日降水量数据、Hadley中心海温资料、NCEP/NCAR再分析资料,通过相关性分析、合成、HP滤波分析等方法,分析崇左市季节性极端气象干旱的成因;结合2009年以来崇左市甘蔗株高、单产数据,研究春季和夏秋季极端气象干旱对甘蔗生长的影响。研究结果表明:季节内降水量偏少,小雨、无雨日数多,中雨及以上等级的强降雨日数少等是崇左市季节性气象干旱发生的直接原因;赤道中东太平洋是影响崇左市季节性降水量的重要海温关键区。2023年厄尔尼诺发展,崇左市春季(3~5月)出现极端气象干旱,2020年厄尔尼诺衰减并快速转为拉尼娜状态,崇左市出现夏秋季(7~9月)极端气象干旱。春季极端气象干旱减缓甘蔗苗期生长速度,降低年终单产;夏秋季极端气象干旱对甘蔗茎伸长期株高影响巨大,导致株高和产量严重受损。

电液复合调速器中比例电磁铁的多参数优化

比例电磁铁是柴油机电液复合调速系统的电磁驱动元件,其电磁力特性影响到整个调速系统的精确度与稳定性。首先利用Ansys Maxwell软件搭建比例电磁铁的仿真模型,并通过电磁阀测试平台验证模型的准确性。随后对电磁铁各结构尺寸进行参数化分析,得到影响比例电磁铁电磁力特性的关键参数组合。最后使用响应面法建立平均电磁力、电磁力均方差与上隔磁角、隔磁环位置、衔铁半径3个因素的二次回归模型,并结合遗传算法进行多目标优化。结果表明,相较于原方案,遗传算法优化得到的结构参数组合方案使比例电磁铁的电磁力特性得到明显改善,平均电磁力提高了8.56%,电磁力均方差下降了59.63%。

数字经济融入档案信息化转型升级的价值定位与逻辑进路研究

本文针对数字经济发展战略下档案信息化转型升级问题,在系统梳理档案信息化发展历程基础上,对档案信息化的目标、任务和要求进行分析,提出了将数字经济融入档案信息化转型升级的框架模型,并提出目标化统筹引领、阶梯化分步实施和要素化增值驱动等档案信息化转型升级的建设思路。

全自动石墨消解-ICP-MS法同时测定粮食和蔬菜中多种元素及健康风险评价

目的建立全自动石墨消解-ICP-MS测定粮食和蔬菜中20种元素检测方法,并对洛阳市售的粮食和蔬菜的有限量值8种元素进行健康风险评价。方法在全自动石墨仪上通过程序加入7 mL硝酸+1 mL高氯酸消解样品,用2%硝酸(V/V)定容到25 mL,联合ICP-MS同时测定20种元素,与微波消解-ICP-MS法比较差异性。采集90份市售粮食和蔬菜,根据国标限值和8种重金属靶标危害系数(THQ)和综合危害指数(TTHQ)值进行健康风险评价。结果20种元素工作曲线相关系数r均>0.9990,检出限在0.001~0.395 mg/kg。平行测定标物大米(n=11),相对标准偏差(RSD)均<5%,检测结果均在标准物质认定值范围内,且与微波消解-ICP-MS法比较,差异无统计学意义(Z=-0.805,P=0.421)。90份样品汞检出率最低(6.7%),平均含量前10位元素依次为钾、镁、钙、钠、铁、铝、锌、锰、锶、铜,均未超标。大米THQ、小麦和蔬菜THQ、TTHQ值均<1。结论全自动石墨消解仪与ICP-MS联用适合大批粮食和蔬菜中多种元素同时测定。

持续推动经济回升向好需要科学处理几方面重要关系

2023年我国经济在总体上呈现回升向好态势。“经济回升向好”是2023年12月召开的中央经济工作会议的重要关键词。但要持续推动我国经济回升向好,需要科学处理实现经济质的有效提升和量的合理增长、坚持高质量发展和实现高水平安全之间、扩大内需和深化供给侧结构性改革之间的关系,并就今后如何科学处理三方面的关系进行了探讨。必须把坚持高质量发展作为新时代的硬道理,努力营造高质量发展和高水平安全相互成就的发展格局,把扩大内需同深化供给侧结构性改革结合起来。

ENSO事件下西北太平洋远东拟沙丁鱼和日本鲭栖息地协同变化特征

远东拟沙丁鱼(Sardinops melanostictus)和日本鲭(Scomber japonicus)是西北太平洋海域重要的关联经济物种,探究二者栖息地变动的关联性有利于合理开发和管理渔业资源。本研究利用2017−2021年6−11月西北太平洋海域远东拟沙丁鱼和日本鲭的渔业数据,结合海表面温度、海表面高度和叶绿素a质量浓度3个关键环境变量分别构建不同权重的栖息地模型,并利用2021年的渔业数据进行验证。选取最优模型预测不同厄尔尼诺与南方涛动(El Niño-Southern Oscillation,ENSO)事件下远东拟沙丁鱼和日本鲭的最适栖息地分布,分析二者在不同ENSO事件下最适栖息地时空分布的差异性和同步性。结果表明:在不同ENSO事件下远东拟沙丁鱼适宜生境面积(高于15%)均高于日本鲭适宜生境面积(低于6%);但远东拟沙丁鱼在拉尼娜事件下最适栖息地面积增长率高于厄尔尼诺事件,前者增长率为0.197,后者增长率为0.123,相反,日本鲭在拉尼娜事件下增长率低于厄尔尼诺事件,前者增长率为1.114,后者增长率为2.082;当远东拟沙丁鱼和日本鲭的分布位置接近时,会促进二者栖息地的适宜条件,当二者分布位置相距较远时会一定程度上抑制日本鲭栖息地面积的增加。远东拟沙丁鱼和日本鲭适宜面积在不同ENSO事件下协同变化特征可能与二者种间关系(竞争/捕食−被捕食)和西北太平洋海域海流分布情况有关。