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81.
82.
移动地图理论基础研究 总被引:1,自引:0,他引:1
移动地图主要指可以随用户移动的电子地图。本文首先从广义和狭义两方面介绍了移动地图的定义,认为移动地图具有易读、实时和交互性等特点。移动环境下,地图信息在制图者与用图者之间的传输是双向且不断循环的,体现了空间信息加工者和使用者之间的交互,这种交互有利于空间信息加工者和使用者对空间信息的认知达成一致,提高地图信息传输的效率,同时也反映了空间信息由静态的地图表现,发展到动态信息服务的演化过程。在空间信息传输过程中,用户一方面接收信息加工者发送的空间信息,另一方面接收客观环境刺激、并对获得的信息进行选择、分类等加工方式获得客观环境的空间信息,并综合分析和比较这两种空间信息,获得对客观世界的认识。在此过程中,需要在大脑中对地理信息空间进行旋转,该旋转时间的长短与现实生活中实际旋转一个物体所费时间的长短相应,旋转角度越大,则历时越长。人们的习惯用语中的空间术语不仅影响人们对空间关系的知觉和记忆,还会影响人们对空间关系的推理,因为不同的空间参考框架有不同的逻辑特征。最后总结了开展移动地图理论基础研究的重要意义。 相似文献
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Measuring similarity between geospatial lifelines in studies of environmental health 总被引:3,自引:0,他引:3
Many epidemiological studies involve analysis of clusters of diseases to infer locations of environmental hazards that could be responsible for the disease. This approach is however only suitable for sedentary populations or diseases with small latency periods. For migratory populations and diseases with long latency periods, people may change their residential location between time of exposure and onset of ill health. For such situations, clusters are diffused and diluted by in- and out-migration and may become very difficult to detect. One way to address the problem of diffused clusters is to include in analyses not only current residential locations, but all past locations at which cases might have been exposed to environmental hazardous. In this paper, we assume that a persons residential history provides such information and represent it through a discrete geospatial lifeline data model. Clusters of similar geospatial lifelines represent individuals who have similar residential histories—and therefore represent people who are more likely to have had similar environmental exposure histories. We therefore introduce a lifeline distance (dissimilarity) measure to detect clusters of cases, providing a basis for revealing possible regions in space-time where environmental hazards might have existed in the past. The ability of the measure to distinguish cases from controls is tested using two sets of synthetically generated cases and controls. Results indicate that the measure is able to consistently distinguish between populations of cases and controls with statistically significant results. The lifeline distance measure consistently outperforms another measure which uses only the distance between subjects residences at time of diagnosis. However, the advantages of using the entire residential history are only partly realized, since the ability to distinguish between cases and controls is only moderately better for the lifeline distance function. Future work is needed to investigate modifications to the inter-lifeline distance measure in order to enhance the potential of this approach to detect locations of environmental hazards over the lifespan.This project is supported by grant number 1 R01 ES09816-01 from the National Institute of Environmental Health Sciences, NIH. Its contents are solely the responsibility of the authors and do not necessarily represent the official views of the NIEHS or NIH. We wish to thank Peter Rogerson for helpful discussions of the migration models, and the anonymous reviewers for pointing out areas where the paper could be improved. 相似文献
85.
曹桂发 《地球信息科学学报》2003,5(2):71-73
空间信息移动用户服务系统是空间信息平民化服务的技术基础,是GIS产业商业运行的平台。本文重点介绍空间信息移动用户服务系统的系统特征,系统架构以及商用GIS基础库建设和系统运行的商业模式。 相似文献
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利用青藏高原地区2015—2020年期间流动重力观测资料,研究2021年3月19日比如6.1级地震前重力变化特征,结果表明:①本次地震前约3年的重力图像中出现穿过震中区的SN向重力变化梯度带,其形态和持续时间与现有典型指标一致,表明重力变化较为清晰地反映了本次地震孕育过程中所引起的重力异常信号;②实测重力场变化与正断型断层位错引起的重力变化在形态上基本一致,结合本次比如6.1级地震的震源机制以正断为主,推测羌塘块体EW向拉伸运动为本次地震的发震背景。 相似文献
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Deeply weathered soils cover most of the Piedmont physiographic province of the south-eastern United States of America (USA). These soils have traditionally been inferred to derive from weathered bedrock, but recent work (e.g. Ferguson et al., 2019) suggests that deposited sediments are more prevalent than recognized. Distinguishing sediment from weathered bedrock is integral to understanding critical-zone processes and overall Quaternary landscape evolution, yet the well-developed, red, clay-dominated Ultisols of this temperate and humid region mask differences between transported from non-transported material. Our goal is to determine if optically stimulated luminescence (OSL) methods can distinguish quartz sand from allochthonous (e.g. transported sediment) versus autochthonous (e.g. in situ weathered bedrock) material in soil-profile and core samples from the Redlair Observatory in southwestern North Carolina, USA. Here, we turn to OSL sensitivity and linear-modulated OSL (LM-OSL) to observe the intensity or lack thereof of the fast-decay luminescence component (most light-sensitive signal) in quartz grains from soil horizons and crystalline bedrock-derived saprolite. We find that quartz grains sampled from in situ weathered bedrock as well as from saprolotized clasts of rock have weak luminescence properties and are not dominated by a fast-decay luminescence component. In contrast, quartz grains from transported sediment (e.g. mobile regolith; colluvium; alluvium) contain sensitive grains with more dominant fast components. These results suggest that quartz luminescence sensitivity can be a tool to differentiate between in situ weathered bedrock and similar looking mobile regolith and colluvium over-printed by soil development. 相似文献
89.
为提高地震人员伤亡预评估的准确性,完善地震灾害损失评估模型,科学评估地震地质灾害可能造成的人员伤亡数量,以2014年鲁甸MS6.5地震滑坡人员死亡数据为样本,建立了一种基于公里网格单元的地震滑坡人员死亡率logistic回归模型。采用F检验法对所建模型的合理性进行检验,计算得到的F值无限接近于1,表明模型无限接近于完全模型,具有极好的数学统计意义。根据模型评估的死亡率反演得到鲁甸地震灾区滑坡致死人数为233人,比实际少17人,总精确度为93.20%,实际死亡人数与模型识别人数在空间上也有很好的一致性,说明计算得到的地震滑坡人员死亡率是实际死亡人数的良好指标。 相似文献
90.
In the eastern part of the Indian shield,late PaleozoiceMesozoic sedimentary rocks of the Talchir Basin lie precisely along a contact of Neoproterozoic age between granulites of the Eastern Ghats Mobile Belt(EGMB)and amphibolite facies rocks of the Rengali Province.At present,the northern part of the basin experiences periodic seismicity by reactivation of faults located both within the basin,and in the Rengali Province to the north.Detailed gravity data collected across the basin show that Bouguer anomalies decrease from the EGMB(wt15 mGal),through the basin(w 10 mGal),into the Rengali Province(w 15 mGal).The data are consistent with the reportedly uncompensated nature of the EGMB,and indicate that the crust below the Rengali Province has a cratonic gravity signature.The contact between the two domains with distinct sub-surface structure,inferred from gravity data,coincides with the North Orissa Boundary Fault(NOBF)that defnes the northern boundary of the Talchir Basin.Post-Gondwana faults are also localized along the northern margin of the basin,and present-day seismic tremors also have epicenters close to the NOBF.This indicates that the NOBF was formed by reactivation of a Neoproterozoic terrane boundary,and continues to be susceptible to seismic activity even at the present-day. 相似文献