区域一体化研究综述：尺度、联系与边界

区域一体化是当今世界最具活力的经济现象之一,它是一个多维度的空间现象,也是一个多学科参与的科学问题。地理学独特的尺度、联系和边界视角对于理解区域一体化是如何改变世界经济格局及其对国家和区域发展的影响有重要意义。文章梳理了区域一体化理论和发展,以尺度、联系和边界的分析视角重新审视了快速发展的区域一体化进程,阐述了区域一体化的网络化特征和多维联系,重新定义了区域一体化中的多重边界,并从“全球―地方”联系的角度对区域一体化进程下有关区域和地方发展的研究进行了综述。区域一体化的实践表现出越来越多的网络特征,形成了以国家权力和关系为导向,涵盖多维度邻近的立体网络空间;区域一体化的边界效应重塑了全球经济格局,同时传统的领土边界依然重要;区域一体化的制度安排深刻影响了一国边境地区的发展和经济地理格局。最后,针对区域一体化,从尺度建构、内部联系、边界效应和多元分析框架等角度指出了亟待学界解决的一些问题,并展望了未来的研究趋势。     

Are Chinese resource-exhausted cities in remote locations?

Numerous domestic scholars have argued that a remote location is the major factor preventing the transformation and sustainable development of resource-exhausted cities. Research to date, however, has not presented relevant evidence to support this hypothesis or explained how to identify the concept of ‘remoteness’. Resource-exhausted cities designated by the State Council of China were examined in this study alongside the provincial capital cities that contain such entities and three regional central cities that are closely connected to this phenomenon: Beijing, Shanghai, and Guangzhou. Spatial and temporal distances are used to calculate and evaluate the location remoteness degrees (LRDs) of resource-exhausted cities, in terms of both resource types and regions. The results indicate that resource-exhausted cities are indeed remote from the overall samples. Based on spatial distances, the LRDs are α₁ = 1.36 (i.e., distance to provincial capital city) and β₁ = 1.14 (i.e., distance to regional central city), but when based on temporal distances, α₂ = 2.02 (i.e., distance to provincial capital city) and β₂ = 1.44 (i.e., distance to regional central city). Clear differences are found in the LRDs between different regions and resource types, with those in western China and forest industrial cities the most obviously remote. Finally, the numbers of very remote resource-exhausted cities based on spatial and temporal distances (i.e., α > 1.5 ∩ β > 1.5) are 14 and 19, respectively, encompassing 17.9% and 24.4% of the total sampled. Similarly, 25 and 30 not remote resource-exhausted cities based on spatial and temporal distances (i.e., α ≤1.0 ∩ β ≤ 1.0) encompass 32.1% and 38.5% of the total, respectively. This study provided supporting information for the future development and policy making for resource-exhausted cities given different LRDs.     

重力三维聚焦反演在大盐滩深部卤水勘查中的应用

大盐滩地区盐湖企业面临水资源和盐矿资源双重危机,利用重力方法探寻新资源具有重要的实际意义。本文对该区布格重力异常进行三维聚焦反演,获得了大盐滩地区三维剩余密度结构。通过研究发现,大盐滩地区浅地表高低度异常,表征着赋存较为丰富的盐矿资源,但地层中水资源较为贫瘠,浅表水资源主要赋存在山前冲积扇及断裂带内。中深层位不仅具有多个含水层,而且出现多处低密度异常区(T1～T4),可能为深部卤水富集体的反映,是探寻新卤水资源的有利靶区。依此建议在阿尔金山山前冲积带及断裂带内寻找新的淡水资源,并在成矿有利区,开展深部卤水资源勘查工作。     

罗马尼亚Mircea Voda剖面黄土粒度特征及其成因指示

Mircea Voda剖面是欧洲典型的黄土剖面之一,本文对Mircea Voda黄土剖面序列S0-S3进行了系统的粒度分析,并与中国黄土高原典型的黄土剖面洛川剖面、西峰剖面等进行了对比研究。结果显示,黄土粒度组成以粒径为4μm-63μm粉砂为主,其平均含量为78. 22%,呈现出风成成因的基本特征,且不同深度样品的粒度组成具有较高的均一性,显示该区黄土具有相同的物质来源。粒度频率曲线呈现为以突出的第一众数20μm～35μm,分选较好的单峰正偏态分布特征,说明粉尘在沉积之前经过了充分的混合。粒级主要组分集中在粗粒端,但在细粒端1μm附近存在第2个分量,这种特征与中国黄土高原黄土的粒度特征十分相似。计算得沉积物环境判别参数Y值均小于-2. 741 1,通过与水成沉积物判别值Y的比较,进一步证实了Mircea Voda剖面黄土为风成成因特征。     

Influences of MJO-induced Tropical Cyclones on the Circulation-Convection Inconsistency for the 2021 South China Sea Summer Monsoon Onset

The South China Sea Summer Monsoon(SCSSM) onset is characterized by an apparent seasonal conversion of circulation and convection. Accordingly, various indices have been introduced to identify the SCSSM onset date. However,the onset dates as determined by various indices can be very inconsistent. It not only limits the determination of onset dates but also misleads the assessment of prediction skills. In 2021, the onset time as identified by the circulation criteria was 20May, which is 12 days e...     

Impact of Perturbation Schemes on the Ensemble Prediction in a Coupled Lorenz Model

Based on a simple coupled Lorenz model, we investigate how to assess a suitable initial perturbation scheme for ensemble forecasting in a multiscale system involving slow dynamics and fast dynamics. Four initial perturbation approaches are used in the ensemble forecasting experiments: the random perturbation(RP), the bred vector(BV), the ensemble transform Kalman filter(ETKF), and the nonlinear local Lyapunov vector(NLLV) methods. Results show that,regardless of the method used, the ensemble ave...     

Analysis on Precipitation Efficiency of the “21.7” Henan Extremely Heavy Rainfall Event

A record-breaking heavy rainfall event that occurred in Zhengzhou, Henan province during 19–21 July 2021 is simulated using the Weather Research and Forecasting Model, and the large-scale precipitation efficiency(LSPE) and cloud-microphysical precipitation efficiency(CMPE) of the rainfall are analyzed based on the model results. Then, the key physical factors that influenced LSPE and CMPE, and the possible mechanisms for the extreme rainfall over Zhengzhou are explored. Results show that water v...     

成岩作用对低渗透砂岩储层物性的影响——以坪北油田上三叠统延长组油藏为例

通过岩石薄片、X-衍射、扫描电镜、阴极发光、压汞等分析测试手段对储层特征进行详细研究.认为该区储层岩石类型主要为细粒长石砂岩,为低孔特低渗型储层,储集空间以溶蚀粒间孔为主,孔喉以小孔细喉型、细小孔微细喉型为主.压实作用、浊沸石、方解石、绿泥石的胶结作用和浊沸石、长石的溶蚀作用是影响砂岩储集性能的主要因素.     

闽西南地区紫金山岩体锆石SHRIMP定年及其地质意义

笔者通过锆石SHRIMP定年,精确厘定了紫金山岩体的成岩成矿时代.紫金山黑云母化岗岩中锆石CL图像显示锆石分为3种形态,定年结果显示这3种锆石有不同的年龄,具有不同的地质意义.第一种锆石晶形发育、具有核一边双层结构.核部的锆石呈磨网状,这类锆石为继承性锆石,年龄为1000 Ma左右;第二种锆石晶形发育良好,但是呈不完整形态,有不清晰的生长环带或者无生长环带,呈现岩浆锆石的特征,年龄为168±4 Ma(n=13,MSWD=0.97),这一年龄应代表了岩石的结晶年龄,属于中侏罗世;第三种锆石晶形发育良好,有清晰的生长环带,这种锆石受后期改造作用,年龄为(119±15)Ma,属于早白垩世.(168±4)Ma时本区并未发生大规模的成矿事件,因此紫金山岩体主体并非含矿岩体,仅有轻微的锡矿化.紫金山花岗岩锆石SHRIMP定年的第三组年龄为(119±15)Ma是大规模成矿作用的记录,可能正是这一期的热液作用开始了本区大规模的长时期的多期次的岩浆热液作用的序幕,从而为本区铜金成矿作用奠定了基础.