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91.
南海礼乐盆地海底麻坑地貌及成因分析 总被引:1,自引:0,他引:1
本文基于高分辨率多波束测深和浅地层剖面数据,首次对南海礼乐盆地南部坳陷海底麻坑进行了系统的识别研究。共识别出各类麻坑81个,其中麻坑直径最大约2.4 km,坑深最大约157 m。麻坑种类多样:按平面形态主要分为圆形、椭圆形、拉长形和新月形麻坑;按组合方式分为孤立麻坑、链状麻坑和复合麻坑;按直径分为正常麻坑和大型麻坑。区域内发育多条大型海底峡谷,峡谷侵蚀引起两侧地层稳定性降低,气体储层遭受破坏,泄露的气体沿断层或气烟囱等喷发出海底形成麻坑。而因麻坑生成时剥蚀的沉积物质与周围水体混合并逐渐发展成浊流,在一定程度上促进海底峡谷向下延伸。研究区内单个麻坑的平面形态最初为圆形或椭圆形,之后由于重力流和峡谷侵蚀的影响,逐渐发展成拉长形或新月形,麻坑之间也会发生组合形成复合麻坑。链状麻坑与冲沟的形成联系密切,沿垂直于等深线方向展布的链状麻坑在重力流的冲刷下,发育成底部平坦的麻坑冲沟。对比分析全球其他海域麻坑,发现海底麻坑尺寸与水深关系密切,在深水区域更容易发育大型麻坑。 相似文献
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93.
利用广州海洋地质调查局采集的2D和准3D地震资料,从整体形态、期次性和内部结构等方面对南海北部陆坡神狐海域内广泛发育的沉积物失稳进行了类型划分和特征描述,并将沉积物失稳的分布特征和陆坡限制型海底峡谷群的分段性进行耦合关联,进而分析沉积物失稳的空间变化规律。研究结果显示,沉积物失稳可以划分为两种类型:第一种类型位于峡谷群的下游段,几乎不受峡谷群地貌的影响,表现为多期次、内部连续和自北向南的块体运动方式,主要以“残留”的形式位于峡谷群脊部;另一种类型主要表现为沿峡谷群脊部向谷底的块体运动方式,受到峡谷群地形起伏的影响,在峡谷群头部,主要为多期次滑移体,中游段变形强度最大,滑塌体是主要的类型,而在下游段-嘴部,表现为滑移块体。第四纪以来,源自北部珠江水系充足的沉积物供给和自北向南较陡的海底地形,是沉积物失稳发育的关键控制因素;陆坡限制型海底峡谷群可能造成了沉积物的再次变形作用,使得沉积物失稳的空间变化规律与峡谷群分段性具有对应关系。此外,神狐海域含气流体的垂向运移以及水合物矿体的存在,也是研究区内沉积物失稳的重要控制因素。 相似文献
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95.
GPS/MEMS INS integrated system for navigation in urban areas 总被引:1,自引:2,他引:1
This paper evaluates the performance of a tightly coupled GPS/INS integrated system based on low cost MEMS IMUs in dense urban
areas, and investigates two different methods to improve its performance. The first method used is to derive observations
from two different constraint equations reflecting the behavior of a typical land vehicle. The first constraint equation is
derived assuming that the vehicle does not slip and always remains in contact with the ground. If these assumptions are true
the velocity of the vehicle in the plane perpendicular to the forward direction should be zero. The second constraint equation
is derived from the fact that the height does not change much in a short time interval in a land vehicular environment. Thus,
when a GPS outage occurs (partial/complete), the integrated system combines the INS and constraints-derived virtual measurements
to keep the position and velocity errors bounded. This method is suitable for use in real-time applications. The second method
is specifically suitable for a post-mission application and involves the use of Rauch-Tung-Striebel (RTS) smoother. The designed
system performance is evaluated using two data sets collected in dense urban areas. The obtained results demonstrate the effectiveness
of different algorithms considered, in controlling the INS error growth, and indicates the potential of MEMS IMUs for use
in land vehicle navigation applications. 相似文献
96.
Recently, the Chinese government raised an urban planning policy which suggests communities open their private roads for public transport and establish street networks with high spatial density in cities. In this context, the purpose of this study is to analyze the potential changes to street network accessibility using GIS techniques and to provide spatial information that may influence the decision making of urban managers. In addition to the existing street network data in the case study city, Shenzhen, intra-community roads are extracted from building footprints in GIS topographic database and used to construct a potential street network with respect to the community opening policy. An automatic GIS-based method is proposed here to analyze the location advantage information in the simulated urban environment, by combining Delaunay triangulation model and graph theory concepts. Specifically, we establish a two-step framework based on the spatial relationships between roads and buildings. Firstly, intra-community roads between neighboring building footprints are generated using a Delaunay triangulation skeleton model, and with the existing inter-community roads they form the simulated network. Secondly, street centrality indices of the current and simulated networks are compared in terms of closeness, betweenness and straightness. Results indicate that after applying the policy the global accessibility in the city would be increased at some places and decreased at others, and places' directness among others would be generally improved. In addition, the skeleton of central routes for through traffic would not change much. The presented method can also be applied to other cities. 相似文献
97.
地表覆盖数据是关于土地利用信息的重要来源,在地理国情监测、气候变化研究、生态环境评估等方面发挥着重要的作用。本文以广东省广州市作为研究区域,利用OSM数据结合FROM-GLC数据和Landsat-8遥感影像数据,对研究区域地表覆盖进行分类并完成地表覆盖制图。实验结果表明,利用OSM数据进行地表覆盖制图结果总体精度较高,具有可用性,但是OSM数据空白区域占比较大,有数据区域个别要素数量较少,在参考选取样本时,样本代表性不够高,部分类型的地表覆盖分类精度较低。 相似文献
98.
采集中国沈阳市区主要交通干道街道灰尘样品,在对其重金属Cd、Cu、Pb和Zn环境影响分析的基础上,应用美国EPA人体暴露风险评估方法对街道灰尘重金属的健康风险进行评估。结果表明,手-口接触行为是人体(儿童和成人)摄入街道灰尘重金属的最主要途径,其次为皮肤吸收和呼吸吸入。重金属对人体的非致癌风险表现为:Pb大于Cd大于Cu大于Zn,均小于非致癌风险阈值1,对人体不会造成健康危害,且儿童的非致癌风险大于成人。重金属Cd目前尚未形成致癌风险,但其对儿童的潜在生态危害值得重视。 相似文献
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100.
Amphitheatre-headed canyons are common on Earth and Mars and researchers have long sought to draw inferences about canyon-forming processes from the morphology of canyon heads and associated knickpoints, often suggesting that amphitheatre heads indicate erosion by groundwater seepage erosion. However, the conditions and processes that lead to amphitheatre-headed canyon formation have been debated for many years. We consider two hypotheses that attribute the amphitheatre-headed canyon formation to fluvial erosion of strong-over-weak stratigraphy or, alternatively, groundwater spring discharge and seepage erosion. A spatial analysis of canyon-form distribution with respect to local stratigraphy along the Escalante River and on Tarantula Mesa, Utah indicates that canyon form is most closely related to variations in local sedimentary rock strata, rather than inferred groundwater spring intensity. Lateral facies variations that affect the continuity of strong layers can induce or disrupt the formation of amphitheatres. Furthermore, we find that amphitheatre retreat rate is dictated by the interaction of fluvial processes downstream of the amphitheatre headwalls and stratigraphy, rather than waterfall and groundwater processes that likely importantly influence headwall form. We conclude that fluvial erosion of strong-over-weak stratigraphic layering alone is sufficient to form amphitheatres at knickpoints and canyon heads. Thus, we re-affirm that formation process should not be inferred from canyon-head morphology, particularly where a strong-over-weak layering is known or plausible. © 2020 John Wiley & Sons, Ltd. 相似文献