野外多道伽马能谱测量在核环境地质评价中的应用

介绍了最新研制的CD-10野外便携式伽马全谱仪工作原理和主要技术指标。该仪器对伽马射线能量分析范围是30～3000keV,分析道数为1024道,对¹³⁷Cs的能量分辨率小于12%,取消了放射性稳谱参考源,采用数字稳谱技术,实现了无干扰天然伽马射线全谱(30～3000keV)测量,并以在核环境地质评价中的应用实例,说明了伽马全谱仪的主要特点和应用前景。     

柄海鞘Styela clava中的甾醇化合物的分离和鉴定

应用GC-MS技术从青岛海域产柄海鞘Styela clava中分离鉴定出5种甾醇化合物,分别是(22Z)-26,27-二降-麦角甾-5,22-二烯-3β-醇(1),胆甾-5,22-二稀-3β-醇(2),胆甾醇(3),胆甾烷醇(4),(22E)-麦角甾-5,22-二烯-3β-醇(5)。     

地热能是影响地球年均气温的重要因素

从地热能浅层分布情况、地表上下温度变化规律、地球平均气温与太阳辐射强度的关系等几方面分析,得出地热能是全球年均气温变化的重要影响因素的结论,并讨论了地热能影响地球年均气温的方式及地球年均气温的变化趋势。     

近20年屯堡聚落聚集区乡村聚落规模演变——以安顺市西秀区为例

以西秀区2000、2010和2020年乡村聚落斑块为基础数据,运用乡村位序-规模法则、聚落规模等级模型等方法,分析西秀区乡村聚落等级规模分布特征及演变规律,并分析屯堡聚落在该过程的发展变化。结果显示：1）乡村聚落总规模、聚落数量总体上呈增长趋势,3个时段屯堡聚落面积占乡村聚落总面积的比例超过20%;2）西秀区乡村聚落规模分布符合乡村位序-规模法则,拟合优度在0.90以上,负指数分布特征突出,并表现出“首位聚落”和“垂尾”分布特征,2000—2010年乡村聚落规模趋于集中分布,2010—2020年趋于均衡;3）不同等级乡村聚落空间分布位置相对稳定,数量上呈低等级向高等级演变;4）屯堡聚落规模稳定增长,是高位序、高规模等级聚落的重要组成部分,但少部分屯堡聚落位序出现倒退现象。未来应科学规划乡村聚落用地布局,形成合理的乡村聚落等级规模结构,保护屯堡文化,打造区域特色聚落。     

Kinematics of the Open Cluster System in the Galaxy

Absolute proper motions and radial velocities of 202 open clusters in the solar neighborhood, which can be used as tracers of the Galactic disk, are used to investigate the kinematics of the Galaxy in the solar vicinity, including the mean heliocentric velocity components (u_1,u_2,u_3) of the open cluster system, the characteristic velocity dispersions (σ_1,σ_2,σ_3), Oort constants (A, B) and the large-scale radial motion parameters (C,D) of the Galaxy. The results derived from the observational data of proper motions and radial velocities of a subgroup of 117 thin disk young open clusters by means of a maximum likelihood algorithm are: (u_1,u2,u3) = (-16.1±1.0, -7.9±1.4,-10.4±1.5) kms~(-1), (σ_1,σ_2,σ_3) = (17.0 ±0.7,12.2±0.9,8.0±1.3) kms~(-1),(A,B) = (14.8±1.0,-13.0±2.7) kms~(-1) kpc~(-1) ,and(C,D) = (1.5±0.7,-1.2±1.5) kms~(-1) kpc~(-1) . A discussion on the results and comparisons with what was obtained by other authors is given.     

Review and Prospect of Global Operational Ocean Forecasting

The marine environmental forecast plays an increasingly important role in economic growth and infrastructure development, and touches upon many fields and aspects, including marine security, energy resources development and protection, ocean shipping and fisheries. Global Ocean Data Assimilation Experiment (GODAE) OceanView supports the national research groups providing them with coordination and technical support among the partners. Forecasting centers develop and establish global operational ocean forecast systems. The global operational ocean forecasting system uses the ocean dynamic numerical model as the dynamic framework, and the near real-time high-quality observation input field is integrated into the model by data assimilation to realize the future environmental forecasts of the marine conditions covering the multi-time scale. The products are routinely validated with observations in order to assess their quality. This paper briefly introduced and reviewed the development process and current situation of the global ocean forecasting system covered by GODAE OceanView, and outlined the future development of global ocean forecasting.     

Evolution of an anticyclonic eddy southwest of Taiwan

Satellite images of sea-surface temperature, surface chlorophyll a concentration, and sea-level anomaly, together with ocean reanalysis data of Asia and Indian–Pacific Ocean (AIPOcean1.0), are utilized to study the three-dimensional characteristics and evolution of an anticyclonic warm eddy adjacent to the southwest coast of Taiwan during October and November 2006. Originated from the Kuroshio intrusion in the Luzon Strait, but unlike previously found westward moving anticyclonic eddies (AE) in the northeastern South China Sea, this AE was so close to the Taiwan coast and stayed where it was formed for over 1 month until it dissipated. Energy analysis is utilized to study the evolution process of the AE, and it shows that the barotropic instability (BTI) and baroclinic instability introduced by the Kuroshio intrusion flow appear to be the main energy sources for the AE. Periodical enhancement/relaxation of local northeasterly monsoon and its associated negative wind stress curl modify the current patterns in this region, reinforce the intraseasonal variability of the Kuroshio intrusion flow, and act together with Kuroshio to form the AE. Eddies detected from AIPOcean1.0 data also show that AEs are most likely to be generated southwest of Taiwan during the transition period of summer monsoon to winter monsoon, and generally, the BTI of Kuroshio intrusion contributes more than the direct wind stress work to the increase of the eddy kinetic energy for the generation and growth of the AEs.     

江西星子县东牯岭花岗石矿山环境地质问题及对策

长期的露天开采严重破坏了矿山地理地质环境,产生了地质灾害隐患。在介绍矿区地理地质背景的基础上,系统地描述该矿区土地、植被、地形和地貌被破坏的情况,分析崩塌、滑坡和泥石流地质灾害隐患。为改善生态环境,打造全国知名旅游景区,提出全面停止矿山开采,并进行分期治理。先期重点清除存在隐患的废石堆,然后清除边坡破碎危岩体,并辅以绿化措施。     

新密煤田翟沟井田山西组煤层特征及聚煤环境分析

以新密煤田翟沟井田勘探资料为基础,对井田区域特征、山西组煤层特征和沉积环境进行分析。研究表明：山西组下段为以泥坪＋泥炭沼泽＋泥坪沉积序列为主的潮坪沉积,山西组上段为以弱还原环境河流作用为主的三角洲沉积体系,山西组聚煤环境为滨岸潮坪环境;山西组二。煤层层位稳定,煤层结构简单,煤层厚度为0．82-12．20m,一般3—5m,平均厚度3．84m,煤层厚度的变化是受沉积环境、后期冲刷作用及构造作用综合作用的结果。     

Decadal variation of thermocline-sea surface temperature feedback in the tropical Indian Ocean and the underlying mechanisms

The thermocline-sea surface temperature (SST) feedback is the most important component of the Bjerknes feedback, which plays an important role in the development of the air-sea coupling modes of the Indian Ocean. The thermocline-SST feedback in the Indian Ocean has experienced significant decadal variations over the last 40 a. The feedback intensified in the late twentieth century and then weakened during the hiatus in global warming at the early twenty-first century. The thermocline-SST feedback is most prominent in the southeastern and southwestern Indian Ocean. Although the decadal variations of feedback are similar in these two regions, there are still differences in the underlying mechanisms. The decadal variations of feedback in the southeastern Indian Ocean are dominated by variations in the depth of the thermocline, which are modulated by equatorial zonal wind anomalies. Whereas the decadal variation of feedback in the southwestern Indian Ocean is mainly controlled by the intensity of upwelling and thermocline depth in winter and spring, respectively. The upwelling and thermocline depth are both affected by wind stress curl anomalies over the southeastern Indian Ocean, which excite anomalous Ekman pumping and influence the southwestern Indian Ocean through westward propagating Rossby waves.