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提出了一种高效率的数据变换方案,比ASCII码变换效率提高43%,阐述了发送接收数据的过程,给出了软件设计方法,并以此通信协议,实现了LDSS98调度机维护终端的通信,该软件经过现场长期运行表明,性能稳定。该协议对通信软件的编程有一定的参考价值,有很好的实用性和较广泛的推广价值。 相似文献
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地震监测是一项对震情应急反映要快 ,系统网络安全性要求较高的工作 ,Windows终端就是建立在系统网络的基础上 ,以允许多个用户同时登录到一台服务器并运行服务器上应用的网络系统终端。它具有成本低 ,安全性好 ,解决网络阻塞能力强 ,应急反映速度快等优势。“Windows终端”的局域网模式是目前应用较为广泛 ,使用性能较好的一种网络连接方式。本文系作者在参加福建省地震局“1 0 5 - 0 3”十五重点项目中 ,对监测中心的台网监测网络系统建设的思考。目前我局新办公楼即将竣工 ,我监测中心新的办公写字间网络系统连接方式 ,选择“Windows终端”不失为一个较好的方案。 相似文献
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辛冬根 《有色金属矿产与勘查》1996,5(1):59-61
本文在分析了计算机远程通信的应用现状和自行开发软件的必要性之后,从环境、结构、功能和实践等方面系统介绍了一个最新开发的远程通信软件。 相似文献
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崩塌灾害智能化监测预警的终端前置模式及其应用简 总被引:1,自引:0,他引:1
大多数地质灾害监测预警系统的工作模式都是“前端”采集地灾异常信息,再通过网络将数据发回后台的“终端”进行分析处理。联系系统“前端”与“终端”的网络系统出现问题时,其功能和作用必将受到影响。将系统终端前置并创建不完全依赖通讯网络的新工作模式,是提高地灾监测预警系统功效的有效途径。四川省荣县“9·1”中型地质灾害中,因前置终端对地灾判断准确可靠、预警及时有效,使崩塌危害区域内的180多人成功避险,堪称崩塌灾害智能化监测预警终端“前置”的一个成功案例。 相似文献
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个人终端消费导向的碳足迹研究框架——支撑我国环境外交的碳排放研究新思路 总被引:12,自引:1,他引:11
碳足迹揭示了终端消费领域人类活动对于全球气候变化的影响,是碳排放研究从生产层面转向消费层面的重要标志。开展碳足迹研究可以揭示人类终端消费活动导致的碳排放以及消费能力、消费结构与碳足迹的关系,并最终服务于我国的环境外交。在分析传统生产层面碳排放研究、总结碳足迹研究最新进展的基础上,从气候变化研究领域中就人类活动进行研究的3大核心命题——“规律、权益、策略”出发,提出了碳足迹研究的基本理念、基本假设和基本判断,总结了相应的原则。最后,对生存型、发展型和奢侈型消费及相应碳排放进行了初步的判断和核算。 相似文献
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塔里木盆地库车坳陷新生界终端扇沉积体系与储层研究 总被引:9,自引:1,他引:9
塔里木盆地库车坳陷新生界沉积时期气候干燥,沉积物主要为陆相碎屑岩。根据岩石学、沉积构造、沉积相序组合等分析,认为其沉积体系为终端扇体系,发育补给带、分流带、盆地带三种主要相组合类型结合储层成岩作用、储集空间、储集物性等的综合分析,认为下第三系储层质量较差,上第三系好储层主要发育于北部地区。 相似文献
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东方1-1陆上终端是国内目前天然气脱CO2规模最大的处理厂。在终端工程设计中,采用了多项新工艺、新技术。天然气处理采用先控制烃露点后增压外输流程,16亿方/年天然气脱碳装置国内领先,国内首次采用二段吸收二段再生的天然气脱碳装置,4X80m双筒型枝状段塞流捕集器设计国内首创,天然气外输解决了长输管线调峰与离心增压机正常运行的问题。终端装置2003年8月一次投产成功,工程设计荣获中国石油天然气集团公司2005年度优秀工程设计一等奖。 相似文献
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工业部门作为终端能源消费中三大主要部门之一,对经济发展具有重要作用。本文系统分析了15个发达经济体100多年来工业部门终端能源消费与人口和经济发展(GDP)的关系,发现随着人均GDP的增长,工业部门的人均终端能源消费显现缓慢增长、加速增长、减速增长到零增长或负增长的"S"形轨迹,并可分为高、中、低三个类型。通过重点解剖美、日、德、法和意大利等典型国家工业部门终端能源消费与经济发展的历史,标定了不同类型"S"形曲线的起飞点、转折点和零增长点,讨论了工业部门终端能源消费与能源消费强度、二产比例、城市化率和人均钢铁消费的内在联系,建立了"S"形曲线的一般性数学模型。工业部门终端能源消费与经济发展定量关系的确定对于国家,特别是发展中国家把握工业化过程能源消费趋势、预测能源需求和制定相关能源政策具有重要意义。 相似文献
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国有土地使用权网上挂牌交易是政府与竞买人通过土地交易系统网络平台实现国有土地使用权竞价交易。网上挂牌交易主要借助网络终端无极限的优点,扩大招拍挂竞买参与范围,减少操作环节,突显了信息化时代网络在土地使用权交易中的重要作用,在今后的国土资源工作中,必将取代传统的挂牌交易模式,成为国有土地使用权交易的主要方式。 相似文献
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Principles of Probabilistic Regional Mineral Resource Estimation 总被引:1,自引:0,他引:1
Agterberg Frits 《地球科学》2011,36(2):189-200
Five principal sources of uncertainty in quantitative mineral resource estimation are listed and illustrated by means of a simple example (mosaic model) and a case history study for large copper deposits in the Abitibi area of the Canadian Shield. Abitibi copper potential originally was estimated on the basis of 1968 estimates of production and reserves totalling 3.12 Mt Cu. This prognostication now could be evaluated on the basis of 2008 copper production and reserves totalling 9.50 Mt Cu. An earlier hindsight study performed on the basis of 1977 data (totalling 5.23 Mt Cu) showed seven new discoveries occurring either in the immediate vicinities of known deposits or on broad regional copper anomalies predicted from the 1968 inputs. By 1977, the global geographic distribution pattern of large copper deposits in the Abitibi area had stabilized. During the next 30 years, new copper was essentially found close to existing deposits, much of it deeper down in the Earth's crust. In this paper, uncertainties associated with copper ore tonnage are analyzed by comparison of 2008 data with 1968 data using (a) log-log plots of size versus rank, and (b) lognormal QQ-plots. Straight lines fitted by least squares on these plots show that 1968 slopes provide good estimates of 2008 slopes but 1968 intercepts are much less than 2008 intercepts. In each linear log-weight versus log-rank plot, the slope is related to fractal dimension of a Pareto frequency distribution, and in a lognormal QQ-plot it is determined by logarithmic variance. The difference between 2008 and 1968 intercepts represents the increase in copper ore production and reserves from 1968 to 2008. The Pareto model fits actual copper and massive sulphides increase over the past 40 years better than the lognormal frequency distribution model for 10 km×10 km cells on favorable environments in the Abitibi area. 相似文献
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Huan-huan Yang Qin Wang Yan-bo Li Bin Lin Yang Song Yi-yun Wang Wen He Hong-wei Li She Li Jian-li Li Chang-cheng Liu Shi-bin Feng Tang Xin Xue-lian Fu Xin-juan Liang Qi Zhang Bei-qi Wang Yang Li 《China Geology》2022,5(1):136-159
The Tiegelongnan Cu(Au,Ag)deposit in central Tibet contains more than 10 Mt of copper ranking 29 th in the world.It is characterized by typical porphyry-epithermal alteration and mineralization.In order to improve the understanding of porphyry-epithermal copper deposit in Tibet,new zircon U-Pb age and sulfur isotope data along with published data in the Tiegelongnan are presented to investigate the formation and preservation mechanism.Ore-related intrusive rocks in the Tiegelongnan including Early Cretaceous(about 120 Ma)granodiorite porphyry and diorite porphyry are closely related to the northward subduction of Bangongco-Nujiang ocean.Sulfur mainly comes from deep magma,and ore-forming fluid is affected by both magmatic and meteoric water.The metallogenic setting of Tiegelongnan is consistent with those of Andean porphyry copper deposits in South America.The cover of the Meiriqiecuo Formation volcanic rocks,Lhasa-Qiangtang collision and India-Eurasian collision have significance in the preservation and uplift of the deposit.The formation,preservation and discovery of Tiegelongnan play an important role in exploration of ancient porphyry-epithermal deposits in Tibet. 相似文献
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Early Eocene hyperthermals are geologically short-lived global warming events and represent fundamental perturbations to the global carbon cycle and the Earth’s ecosystem due to massive additions of isotopically light carbon to the ocean-atmosphere system.They serve as ancient analogs for understanding how the oceanic carbonate system and surface-ocean ecosystem would respond to ongoing and future climate change.Here,we present a continuous carbonate record across the Eocene Thermal Maximum 2(ETM2 or H1,ca.54.1 Ma)and H2(ca.54 Ma)events from an expanded section at Ocean Drilling Program Site 1258 in tropical Atlantic.The abundant calcareous nannofossils and moderate carbonate content throughout the studied interval suggest this record was deposited above the calcite compensation depth(CCD),but below the lysocline and under the influence of terrestrial dilution.An Earth system model cGENIE is used to simulate the carbon cycle dynamics across the ETM2 and H2 to offer insights on the mechanism of the rapid warming and subsequent recovery in climate and ecosystem.The model suggests moderate changes in ocean pH(0.1–0.2 unit)for the two scenarios,biogenic methane from a rechargeable methane capacitor and organic matter oxidation from thawing of the permafrost.These pH changes are consistent with a recent independent pH estimate across the ETM2 using boron isotopes.The carbon emission flux during the ETM2 is at least an order of magnitude smaller than that during the Paleocene–Eocene Thermal Maximum(PETM)(0.015–0.05 Pg C yr-1vs.0.3–1.7 Pg C yr-1).The comparable pre-and post-event carbonate contents suggest the lysocline did not over deepen following the ETM2 at this tropical Atlantic site,indicating spatial heterogeneity in the carbonate system due to strong dilution influence from terrestrial weathering and riverine discharge at Site 1258. 相似文献